200 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


Skelton. June 10, 1865; David Shultz, June 11, 1865; Elijah M. Tam, May 22, 1865; William H. Wingrove, April 16, 1862. Ashbury Welsh was wounded at battle of Mission Ridge November 25. 1863 ; discharged June 18, 1864. Leander Warren was wounded in battle at Chickamauga June 19, 1863; discharged September 19, 1864. Daniel Thomas was captured at Stone river December 31, 1862; discharged September 19, 1864. Thomas B. Yocum, November 8, 1862 ; James Wisenburg, February 20, 1865.


DIED.


David Diday, of typhoid fever at Corinth, Miss., June 22, 1862. John Brewer, of lung fever in Kentucky, December 31, 1861. Jacob Brewer, of pneumonia at Camp Station, Tennessee, March 29, 1862. Joseph A. Bowles, of typhoid fever at Vinning Station, Ga., July 31, 1864. John Brandon was captured at the battle of Chickamauga, September 19, 1863; died in prison at Andersonville, Ga., June 30, 1864, Samuel Early died of wounds received before Kenesaw Mountain, June 21, 1864, at hospital, Chattanooga, Tenn., June 29, 1864. Isaac Green was captured and paroled at Stone River, December 31, 1862 ; died June 22, 1 864, of wounds received before Kenesaw Mountain, June 21, 1864. Christopher Hinkle, July 10, 1864, of wounds received before Kenesaw Mountain, June 21, 1864. Cyrus Hurly was captured and paroled in Kentucky, September, 1862; captured at the battle of Chickamauga, September 19, 1863; died in prison, at Andersonville, Ga., June 21, 1864. Conrad King died of pneumonia at Louisville, Ky., June 1, 1862. Edward Keiser died of diarrhae at Camp Dennison, Ohio, February 5, 1865. David Mills, July 26, 1864, of wounds received June 20, 1864, at Chattanooga, Tenn. John Orr, of chronic diarrhae at Murfreesboro, Tenn. .I my 1, 1863. Elijah B. Rowles, of wounds received at Picket's Mills, Ga., May 27, and died in field hospital May 28, 1864 James E. Ramage, June 28, of wounds received in battle at Liberty Gap June 25, 1863. Win. Scott, at Murfreesboro, Tenn., September 14, 1863, of wounds received in battle at Stone River, December 31, 1862. Abner Wilbert died of pneumonia at Mumfordsville, Ky., February 21, 1862.. Christopher Taylor, September 14, 1863, of wounds received in battle at Liberty Gap, June 25, 1863, at Murfreesboro, Tenn. Samuel Wingrove was captured in battle at Chickamauga, September 19, 1863 ; died in prison at Andersonville, Ga., June 16, 1864.


CO. K,15TH REGIMENT O. V. I.


This company was organized at Flushing, September 5, 1861. Rendezvoused at Camp Bartley for a short time. The officers and members were as follows:


Otho S. Holloway, Captain.

Robert H. Cochran, First Lieutenant.

Vesper Domeck, Second Lieutenant.

Nathan Holloway, First Sergeant..

Frank W. Sanders, Sergeant.

Alexis Cope, Sergeant.

John S. Cochran, Sergeant.

Joseph Farmer, Sergeant.

Laban Mitchell, Corporal.

.Rees Pickering, Corporal.

`Thomas Burkhead, Corporal.

.Henry E, Stewart, Corporal.

.Eli Davis, Corporal.

Thomas Bethel, Corporal.

Joseph Cordner, Corporal.

G. W. Chessel, Corporal.

Abner W. Marshall, Wagoner.


PRIVATES.—Levi Atkins, Wm. I. Ankrom, J. P. Arned, Joseph Burkhead, John W. Brown, James W. Bateman, John M. Bendure, James H. Bendure, Alvin Barton, Stephen Bricker, Robert A. Buffington, Russels Buffington, Walker Carpenter, Joshua Camp, S. W. Cowels, Brown Deselms, Thos. Dunn, James Eckles, Benjamin Eckles, Benj. Freeman, Simeon L, Faucett, Elder T. Fort, James Ferren, Landon Grimes, John Grimsley, Samuel Geller, Wm. Hazelwood, Lundy B. Hogue, Ephraim Houser, Charles Hall, Simpson G. Haines, Al. Herrick, Samuel Hutchison, John S. Hutchison, Benj. F. Johnson, John W. Looman, Christian Maul, Israel McKnight, William McKnight, James McCourt, James McConnell, Lewis C. Mechem, John Murray, Wallace McGrath, Hector McAllison, James McMillen, Balaam Norris, George W. Poorman, Leonard Pickering, Sqnire Palmer, William I. Porterfield, Peter P. Russet John Ridgeway, David Ralston, David Smith, William Stone, Edward Stone, G. W. Sballcross, Wm. Seals, John G. Sherwood, Samuel Tillett, J. Tillett, J. Q. Tillett, James Thompson, John A. Thompson, Wilson S. Vancuran, Washington I. Vance, David C. Vail, Marshall Wisley, William Walter, William H. Webb.


This company was re-organized as a veteran company.


PROMOTIONS, TRANSFERS, ETC.


Vesper Domeck entered as. a private; promoted to Second Lieutenant November 8, 1861; to First Lieutenant June 19, 1863, and to Captain January 13, 1865. Robert S, McClenahan was quartermaster sergeant to March 12, 1865, when he was promoted to first lieutenant and transferred to company K; Joseph Cordner enlisted as corporal ; promoted to sergeant January 1, 1864, and to first lieutenant March 26, 1865. David Smith promoted to sergeant January 1, 1864; wounded in arm at Kenesaw Mountain, Ga., June 21, 1864. Washington J. Vance promoted to sergeant June 1, 1862. John Q. Tillett was promoted to corporal January 1, 1864, and to sergeant March 16, 1865. Benj. F. Johnston was promoted to corporal January 1, 1864 , to sergeant June 3, 1865. Henry E. Stewart was promoted to sergeant September 1, 1862. James Eckles, promoted to corporal January 1, 1864. Deselms Brown was promoted to corporal January 13, 1865; wounded at Rocky Faced Ridge, May 3, 186-. Noble Carter was promoted to corporal January 13, 1865. Robert A. Heaney, promoted to corporal January 13, 1865. Wm. L. Reynolds, promoted to corporal January 13, 1865. W. B. Drum was promoted to corporal March 23, 1865; wounded in head at Kenesaw Mountain, Ga., June 21, 1864. Geo. W. Russell, promoted June 3, 1865, to corporal. Otho S. Holloway resigned July 1, 1862. Chandler W. Carroll entered first lieutenant, Co. E; promoted to captain and transferred to Co. K, September 25, 1862 ; mustered out at Huntsville, Ala., January 12, 1865. Robert H. Cochran, first lieutenant, resigned May 30, 1865. Reese Pickering, promoted to second lieutenant January 1, 1864; to first lieutenant January 12, 1865; promoted to captain and transferred to company I, March _9, 1865. Frank W. Sanders was promoted to first sergeant June 24,1862, and to second lieutenant June 25, 1865; killed in battle at Mission Ridge, November 25, 1863. Vincent T. Trago, promoted from first sergeant to second lieutenant March 9, 1865, and transferred to company K; promoted to first lieutenant and transferred to company H June 1, .1865.


KILLED IN BATTLE.


Thomas Bethel killed at Kenesaw Mountain, Ga., July 3, BO; promoted to sergeant April 1, 1862. Ephraim Houser killed at Peach Tree Creek, Ga., July 20, 1864. Samuel W. Cowles killed in battle at Stone River, December 31, 1862. Balaam Norris killed at Mission Ridge, Tenn., November 25, 1863. Nelson J. Reed killed at Peach Tree Creek, Ga., July 20, 1864. Samuel W. Wilson killed at Kenesaw Mountain, Ga., June 21, 1864.


DISCHARGED FOR DISABILITY.


Nathan Holloway, June 24, 1862. John S. Cochran, Septem- ber 31, 1862. Joseph Farmer, at Murfreesboro, Tenn., 1863. E. T. Frost was promoted to corporal January 1, 1864 ; promoted to sergeant January 13, 1865 ; wounded in the arm at Kenesaw Mountain, Ga., June 21, 1864; discharged June 3, 1865. Wm. Hazelwood promoted to corporal June 1, 1863 ; wounded in the leg at the battle of Chickamauga, Ga., September 19, 1863 ; discharged January 14, 1865. James H. Bendure, June 30, 1862. John M. Bendure, September 12, 1862. Allen T. Brandenburg, July 20, 1863. Stephen Bricker, January 1, 1864 ; was wounded severely in the breast at Kenesaw Mountain, June 21, 1864. Robert A. Buffington, April 22, 1863. Joshua Camp, Jnly 3, 1862. Walder C. Carpenter, January 10, 1863. Richard Coleman, July 10, 1865. James R. Cowgill, October 4, 1865. Christopher Dethling, June 10, 1865. Clark Edgington, May 22, 1865. Robert Erskine, September 9, 1862. Simeon L. Fawcett, March 27, 1865. Benj. Freeman, April 7, 1865 ; captured at Chickamauga, Ga., September 19, 1863 ; released April, 1865. Casper D. Fassee, Juno 10, 1865. Samuel Geller, July 28, 1862. James Gibson, October 4, 1864. L. B. Grimes, March 26, 1863. John Grimsley, January 6, 1863. Simpson G. Haines, December 2, 1862, on account of wounds received at the battle of Shiloh, April 7, 1862. Charles Hall, February 24, 1862. Wm. Hill, April 11, 1865. Lundy B. Hogue, October 29, 1862. Samuel Hutchison, February 21, 1862. John S. Hutchison, June 10, 1865 ; captured at Chickamauga, Ga., September 19, 1863; released April, 1865. John W. Looman, September 30, 1864.


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 201


George W. Male, June 10, 1865. Hector McAllister, January 11, 1865. Wallace McGrath, October 1, 1862, to accept promotion ; transferred as second lieutenant to company C, same date. John McFadden, June 10, 1865. James McCourt, September 30, 1864. James McMillen, June 10, 1865. Jonathan Miller, June 10, 1865. Squire Palmer, J my 21, 1862. Leonard Pickering, June 10, 1865. W. J. Porterfield, June 19, 1862. David Ralston, October 3, 1864. John Rennard, on account of wound received at Stone River, December 31, 1862. Rudolph Rine, June 10, 1865. Peter P, Russell, April 7, 1863 ; received wounds at the battle of Stone River, December 31, 1862. Henry G. Seesholtz, Christian Shrader, Geo, W. Shallcross, Wm. Soden, Wm, Stone, June 10, 1865. Edward Stone, July 16, 1862. Robert Tallman, Frederick Thorn, June 10, 1865. John A. Thompson, February 24, 1862. James W. Thompson for wounds received at Stone River, December 31, 1862. Giles Tillett for wounds received at Shiloh, April 7, 1862. Samuel Tillett, Isaac Terrell, June 10, 1865. Wilson S. Vancuran, June 10, 1865; wounded at Chickamauga, Ga., September 19; 1863. William Waller, February 11, 1862. Wm. H. Webb, June 10, 1865.


DIED.


Mitchel Laban died at Camp Wood; Ky., January 6, 1862, of typhoid fever. W. J. Ankrom, at Louisville, Ky., of dysentery, January, 1862. J. P. Arnell, at Camp Wood, Ky., March 12, 1862, of typhoid fever. Levi Atkins died at Flushing, 0., May, 1862, of wounds received at battle of Shiloh, April 7, 1862. Thomas Dunn, shot by a comrade on the picket line November 22, 1861, being mistaken for an enemy. Benj. Eckels, died at Louisville, Ky., May 3, 1862. of typhoid fever. James Farren, died at St. Clairsville, O., May 6, 1862, of consumption. A. Herrick died at Mound City, Ill., May 21, 1862, of wounds received at Shiloh, April 7, 1862. William McKnight, died at Flushing, 0., June 29, 1862, of consumption. William Seals, died at St. Louis, Mo., December 20, 1862. David C. Vail, died at Louisville, Ky., December 29, 1862, of erysipelas.


COMPANY A, 25TH REGIMENT O. V. I.


This company was organized at St. Clairsville, and arrived at Camp Jackson June 12, 1861. On the 28th of the same month the 25th Regiment was organized at Camp Chase, near Columbus. The officers and members of company A, as first organized, were as follows :


James F. Charlesworth, captain.

William Askew, first lieutenant.

Arthur Higgins, second lieutenant,

John D. Koontz, first sergeant.

W, B. Wright, sergeant.

Zenas Smith, sergeant.

Henry Johnson, sergeant.

Israel White, sergeant.

Burget McConneghey, corporal.

William H. Spear, corporal.

James Miller, corporal.

Thomas W. Fawler, corporal.

Abraham Heed, corporal.

Hiram Nichol, corporal.

Robert Kennedy, corporal.

Thomas Ferrell, corporal

George W. McBride, musician.

Robert Fawler, musician.

Thomas McBride, wagoner.


PRIVATES.-Joseph Acres, Alex. Barrett, Joseph Boggs, Levi Butler, Elias Baile, James C. Bolon, Joshua Burkhead, Leander Beall, Samuel Beall, William H. Criswell, George Cass, John

Conway, James E. Clifford, Robert Creighton, John F. Crow, Hugh Donely, Reuben Donely, Robert M. Fulton, Samuel Glasgow, Phillip Gable, Joseph Gallaher, John W. Holland, Eli Hanker; Samuel Henry, John R. Hedge, Charles Hooper, William Harrison, Hiram S. Hahn, D. C. Iverson, B. R. Johnston, A. M. Jeffers, Charles R. King, James Kelly, John W. Kent, D. C. Kinney, Patrick Kain, William Linden, William Lockwood, Henry Lambert, John McMillen, John McConnell, G. D. W. McPherson, James McMullen, Samuel McCrum, Jacob McCabe, John McKirahan, Michael Murry, Robert H. Miller, Henry Meek, John R. Mellor, John F. Peck, Samuel B. Porterfield, Jesse C. Patterson, Levi Ryan, James Russell, John Richards, E. L. Riley, Josephus F. Rial, William C. Rankin, Nathaniel Sutton, Charles Smith, Asa Taylor, Ignatius Tillett, William F. Talbert, Samuel Talbert, Hezekiah Thomas, George W. Verbeck, Simon L. Voorhies, John Weyer, Robert Wright. James G. Whittell, Henry C. White, William H. White, John Zane.


PROMOTIONS, TRANSFERS, ETC.


Capt. Wm. P. Scott assigned to Company A, March 11, 1865. First lieutenant Elisha Biggerstaff assigned to company A, June 12; 1864. Second lieutenant Daniel J. Crooks assigned to company A, September 29, 1865. First sergeant Robert M. Fulton promoted to corporal, April 1, 1864; sergeant, April, 1865 ; first sergeant, May 18, 1866. Josephus S. Kinney promoted to corporal, April 1, 1864 ; to sergeant, June 1, 1865. Joseph Acres promoted to corporal, August 1, 1864 ; promoted to sergeant. July 1, 1865 ; re-enlisted, December 31, 1863. Leander J. Beall promoted to corporal, February 1, 1865 ; to sergeant, 1865. Andrew Fulton, promoted to corporal, June 1, 1865 ; to sergeant, May 18, 1866. Simon L. Voorhies promoted to corporal, November 8, 1864. Samuel L. McClellan promoted to corporal. April 1, 1865. John W. Kent, promoted to corporal, June 1, 1865. Albert B. Wayt promoted to corporal. August 1, 1865. M. F. McKirahan promoted to corporal, Sept, 15, 1865. John M. Watkins promoted to corporal, May 1, 1866. Joshua S. Holland (recruited) March 14, 1864. John W. Nevil, Vance Vancuran.


DISCHARGED.


James F. Charlesworth, mustered out to accept promotion May 16, 1862. William Askew, to accept promotion September 25, 1861. Arthur Higgins, promoted to first lieutenant September 25, 1861 : mustered out to accept promotion November 4, 1864. Israel White, promoted to first sergeant July 1, 1862 ; discharged to accept promotion April 1, 1863. William B. Write, discharged July 18, 1864, (extra term.) Samuel Stewart, promoted to corporal January 6, 1862 ; to sergeant September 1, 1863 ; discharged by reason of enlistment December 31, 1863; Berget McConneghey, promoted from corporal, to sergeant August 1, 1862; discharged by reason of re-enlistment December 31, 1863. Abram Heed, by reason of expiration of term July 18, 1864. Thomas H. Ferrel, promoted from corporal to sergeant September 1, 1863 ; discharged to re-enlist December 31, 1863. Wm. H. Criswell, promoted to corporal September 1, 1862; discharged December 31, 1863, to re-enlist. John McKirahan, promoted June 1, 1863; discharged December 13, 1863, to re-enlist. Robert Kennedy, on disability December 10, 1863. Charles H. King, promoted to corporal January 6, 1862; discharged to accept promotion June 5, 1863; Michael Hurry, promoted to corporal April 1, 1862 ; re-enlisted December 31, 1863. Andrew D. King, promoted to corporal February 1, 1865 ; discharged July 15, 1865. Thomas W. Fawler, re-enlisted December 31, 1863. George W. McBride, re-enlisted December 31, 1863. William S. Tyrrel, December 14, 1865, (extra term:) Alexander Barrett, re-enlistdd December 31, 1863. Joseph Baggs, March 30, 1862, 'on disability. .Elias. Baile, (extra term), July 16, 1864. James C. Bolon, (extra term), July 16, 1864. Joshua Burkhead, re-enlisted December 31, 1863. Samuel Beall, September 12, 1862, on disability. Leander J. Beall, re-enlisted December 31, 1863. Isaac Bennington, October 17, 1865, (extra term.) Martin Bennington, November 23,1865. George Cross, February, 1863, on disability. John Conway, re-enlisted December 31, 1863. Robert Creighton, re-enlisted December 31, 1863. John T. Crow, (extra term.) W. D. Clark, July 16, 1865, on disability. Michael Cook, (extra term.) John B. Day, (extra term.) Robert M. Fulton, re-enlisted December 31, 1863. Samuel Glasgo, (extra term), July 16, 1864. Philip Gable, (extra term.) Joseph Gallaher, (extra term.) Eli Hanker; March 16, 1863, on disability. Samuel Henry, December 5. 1863, on disability. John R. Hedge, November 1862, on disability. Charles Hooper, re-enlisted, December 31, 1863. Hiram S. Hahn, extra term. William T. Hughes, extra term. C. D. Iverson, October 1, 1862, on disability. Benjamin R. Johnston. extra term. Andrew M. Jeffers was sent to the hospital at Strasburg, July 4, 1862, the last heard from. DeWitt C. Kinney, extra term. Josephus S. Kinney, re-enlisted, December 31, 1863, William Linder, extra term. Henry Lambert, re-enlisted, De- cembea 31, 1863. G. D. W. McPherson, October 28, 1862, on disability. Samuel McCrum, extra term. John McConnel, re-enlisted, December 31, 1863. Thomas W. McBride, re-enlisted, December 31, 1863. Jacob McCabe, reported taken prisoner and died in Richmond. James Mellor, promoted to Sergeant, extra term. Robert H. Miller, July 31, 1863, on disability. John R. Mellor, August 29, 1861, on disability. Henry Meek December 29, 1862, on disability. John Murphy, May 29, 1865,


202 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


on disability, Samuel B. Portorfield, 1862, on disability. Jesse C. Patterson, extra term. Levi Ryan, re-enlisted, December 31, 1863. James Russell, extra term. M. L. Riley, re-enlisted, December 31, 1863. J. F. Rial, May 10, on disability. Nathaniel Sutton, May 6, 1862, on disability. Charles Smith, November 10, 1862 on disability. William Simpson, September 16, 1863, on disability. Asa Taylor, extra term. W. F. Talbert, March 14, 1862, on disability. D. L. Tyrell, extra term. Robert H. Vance, extra term. Robert Wright, extra term. William H. White, wounded at Gettysburg, Pa., sent to G. H. Dis. James C. Whittle, April 19, 1864, from wounds received at Chancellorsville. Nathaniel Wallace. extra term. Adolph Weidabusch, extra term.


DIED.


John D. Koontz died January 5, 1862, of diarrhæ, at Barnesville, Ohio. W m. H. Spear died May 29, 1862, at Franklin, Va., of wounds received at the battle of McDowell, Va. Wm. L. Anderson died September 9, 1862, of diarrhæ, at Philadelphia, Pa. Levi Butler, killed May 2, 1863, at Chancellorsville, Va. James E. Clifford, killed July 1, 1863, at Gettysburg, Pa, Reuben Donnelly died October 2, 1862, at Alexandria, Va , of wounds received in the battle of Bull Run. Robert A. Fawler died February 27, 1862, at Philadelphia, Pa., of smallpox. William T. Lockwood, killed at the battle of Chancellorsville, Va., May 2, 1863. Alfred A. McFadden died April 6, 1864, in a hospital at Washington, D. C. James McMullen died January 10, 1862, at Bridgeport, Ohio, of chronic diarrhæ. John Richards, killed in battle on Allegheny Mountain, Va., December 13, 1861. Samuel Talbert froze to death on Cheate Mountain, Va., November 21, 1861. George W. Verbeck died June 15, 1862, at Glencoe, 0., of wounds received at the battle of McDowell, Va. Henry C. White died May 15, 1862, of diarrhae, at Washington, D. C. Thomas G. White, killed in the battle of Hong Hill, November 30, 1864.


Company mustered out at Columbus, Ohio, June 18, 1866.


COMPANY A, 43D REGIMENT O. V. I.


This company was made up mostly of men from Bellaire, Bridgeport and Martin's Ferry. It was recruited from October to December, 1861, when mustered into service. The officers and members of company "A" were as follows :


Jacob M. Spangler, captain.

Samuel Martin, first lieutenant.

John M. Criswell, second lieutenant.

Obediah M. Davis, first sergeant.

William Meek, musician.


PRIVATES. —John J. Albright, John B. Allen, Andrew B. Anderson, Samuel J. Banks, Robert Baggs, Joseph C. Beam, Geo. Brewer, John Beck, Henry Brown, Benjamin F. Brooks, James A. Carter, John R. Campbell, J. M. Criswell, John Conrad, W. B. Clayton, Jacob S. Clayton, John S. Clarke, John W. Campbell, John Conners, Patrick Conway, Robert Duncan, Robert Dixon, William Davis, Robert Douglass John Denn, James Douglass, Thomas C. Doherty, Thomas Douglass, John P. Eckels, Samuel Eckels, Robert S. Everett, G. W. Goodrick, Wm. H. Giffin, David Greenley, Robert Giffin, James Hollis, Patrick Heffron, William Haley, William Hipkins, Jeremiah Hutcher, Thomas G. Hosper, August Hoffman, James Henry, James Hobbs, Edmond Hannon, James Hartup, John W. Hartup, John W. Jackson, James M. Keyser, John G. C. King, John J. Levy, William A. Lilly, Philip Lang, Elias B. Lowman, Charles A. Littleton, George W. Long, William Mohoffy, James F. McGrew, John Madden, Henry McGreivy, Thomas McKail, Tobias Oliver, Hiram Oliver. Robert C. Russell, Patrick Reed, John M. Ryan, Samuel Richardson, Jacob Ruler, Levi Shipman, Luther Stewart, Joseph Samuels, Lewis Schramm, Zane Smith, Cyrus H. Strahl, Robert Turbot, Levi D. Thompson, Michael Tynane, Samuel Vanhorn, Wm. M. Vallee, Daniel Westlake, Benj. F. Westlake, Jeremiah Westlake, Makin Walsh, John Winning, George M. Wise, Warren M. Yates.


PROMOTIONS.


Obediah M. Davis was promoted from sergeant, company A, to second-lieutenant May 9, 1864, and assigned to company I; then promoted to first lieutenant January 1, 1865, assigned to company C, and then promoted to captain, March 1, 1865, and transferred to company A. George W. Goodrich was promoted to first sergeant, April 1, 1865, promoted to first lieutenant May 22,1865. John K. Campbell was promoted to second lieutenant from sergeant company A May 22, 1865. Robert Dixon was promoted to first sergeant, June 1, 1865. J. B. Smith was promoted from corporal to sergeant June 1, 1864. Jacob Rupper was promoted to sergeant from corporal, April 1, 1865. B. F. Westlake was promoted to sergeant from corporal, June 1, 1865. David Stinson was promoted to sergeant from corporal, June 1, 1868. Samuel Bishop was promoted to corporal November 1, 1864. John B. Alum was promoted to corporal, April 1, 1864. J. C. Plunket was promoted to corporal, November 1, 1864. John P. Eckels was promoted to corporal, April 1, 1865. Martin Welsh was promoted to corporal, April 1, 1865. Robert Long was promoted to corporal, June 10,1865. William Hipkins was promoted to corporal, June 1, 1865.


TRANSFERRED.


Samuel T. Calvin, Robert McNary, Luther Stewart, Hamdon Heatherington, Louis Schaum, George M. Wise.


DISCHARGED.


Samuel Martin resigned his commission as captain September 25, 1864. Zane Smith was promoted to first sergeant January 1, 1864. Mustered out to accept a commission in the 7th Louisiana C. T.


DIED.


Stacy Taylor died in hospital, Decatur, Alabama, April 26, 1864. Joseph Samuels, killed in action at. Atlanta, Georgia, August 4, 1864. George W. Long died in hospital at Marietta, Georgia, September 16, 1864, of wounds received at Atlanta, Georgia, August 4, 1864. William Aarants (drafted) died in hospital in field in South Carolina, March 17, 1865. .John Barnhart (substitute) died in hospital at Philadelphia, Tent., April 24, 1865. George Conaway died in hospital, Marietta, Ga. July, 1864. Jesse Gray died in hospital, Hiltonhead, S. C., April 4, 1865. William Palmer died in hospital at Newbern, N. C., April 16, 1865.


Company A was mustered out on the 13th of July, 1865, at. Louisville, Ky.


CO. D, 43d REGIMENT O. V. I.


Company D, of the 43d Regiment, was recruited at St. Clairsville during the mouths of November and December, 1861. Organized with regiment at Camp Andrews, Mt. Vernon, Ohio. The officers and members were as follows :


Christian L. Poorman, Captain.

Joseph A. Harris, 2d Lieutenant.


PRIVATES.—Lewis Applegate, Crawford Armstrong, David Applegate, Thomas Ankrim, Ira Briton, Thomas B. Brown, E. S. Brown, J. C. Bolen, Henry Baxter, Isaac Billingsley, Joseph S. Barnhard, George Bright, Wilson S. Bigley, George Bailey, Elias Beal, Patrick Cochlen, Richard Creighton, James Crimble, W. H. Cope, Jacob H. Cope, John Cunnard, W. H. Crabtree, Jefferson Chamberlain, James Dunn, Robert M. Dent, John Danford, Thomas Durbin, P. S. Evins, Fowler Glenn, Daniel J. Freeman, Gaston Fox, Robert Gleespy, Stewart Harris, John S. Hamilton, Abram H. Handel, Thomas Huntsman, William V. Johnson, David Johnson,. sr., David Johnson, jr., Samuel Johnson, Westley Jones, Colostine Jones, Thomas Kinney, William Kinney, William Lindsey, Henry Miller, Mathew R. McFadden, Thomas Merrill, Henry McFadden, Robert Morrow, James B. McCormick, Andrew McKirahan, John McKeen, David H. McKeen, George F. Majors, Robert S. Moore, Nathan Moore, James Nixon, John W. Newton, George W. Nixon, William Owens, William Patterson, David Poole, Israel Perry, William Paxton, Charles W. Penn, Uriah Rimby, Alcanger Rothwell, James T. Robinson, Ephraim Stull, Richard Shepherd, Humphrey Steadman, Henry Steadman, Thomas Shepherd, Otto Strickland, Isaiah Shepherd, James V. Tiernan, J. W. Taylor, Clark Vanhorn, Henry Wilds, Milo Wilkinson, John R. Wilson, Levi Williams, Elijah M. Weekley, Martin L. Weekley, Zibar Yarnald.


PROMOTIONS, ETC.


Crawford W. Armstrong, appointed sergeant from private, December 31, 1863 ; appointed 1st sergeant, Aug. 9, 1864 ; promoted to Captain, April 1, 1865. James W. Dunn was appointed sergeant from private, Dec. 1863 ; appointed 1st sergeant April 1, 1865 ; promoted to lieutenant, May 21, 1865. William P. Weekly was appointed corporal Dee. 31, 1863 ; sergeant, April, 1865 ; 1st sergeant, June 1, 1865. William H. Crabtree was ap-


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 203


pointed corporal, Dec. 31, 1863 ; sergeant, June 8, 1864. Samuel S. Delany was appointed corporal, Dec. 31, 1863 ; sergeant, May 1, 1865. Thomas Shepherd was appointed corporal, j une 8, 1864; sergeant, June 1, 1865. Aleanzer Bothwell was appointed corporal June 8, 1864; sergeant, June 1, 1.865. William Orr was appointed corporal, Dec. 31, 1863 ; absent, no discharge furnished. Elijah S. Brown was appointed corporal, Aug. 6, 1864. Andrew McKirahan was appointed corporal, Jan. 1, 1865. Stewart Harris was appointed corporal, Jan. 1, 1875. Mathew C. Henderson was appointed corporal, April 1, 1865. Abram H. Randal was appointed corporal, June 1, 1865. C. Jones, appointed corporal, May 1, 1865, Robert M. Dent was appointed corporal, Jan 1, 1865.


RECRUITS.


Daniel I. Clark, Francis Clark, George W. Keeper, Jefferson Mayburg, Franklin Taylor. These gentlemen are from Belmont county. There were other recruits from different parts of this state, numbering in all, 36.


DISCHARGED.


John Cunnard, dicharged Jan. 1, 1865, expiation of term. Jefferson Chamberlain, discharged, Jan. 1, 1865, same. John C, Bolon, discharged, Aug. 8, 1864, to receive promotion. Joseph S. Barn hard, discharged, Jan. 1, 1865. John W. Taylor, discharged, Jan. 1, 1865, (expiration of term). Benton Bitenhour, discharged from hospital, Jan. 17, 1865. Emanuel Goldsborough.


TRANSFERRED.


Basil M. Simpson, Henry Butts, Thomas Fowler.


DIED.


Milo Wilkison, promoted from 1st Sergeant to 2nd Lieutenant, May 9, 1864; died of disease, Jan. 29, 1864, at Chattanooga, Tenn, Irwin Harrison, died of disease, Sept. 22, 1864. David Johnson, died in prison at Andersonville, Ga., Sept. 14, 1864. Patrick Martin, died in hospital, March 7, 1865. Samuel Meadly, died of disease, at Covington, , Ky., Feb. 24, 1814. George W. Nixon, died of disease, March 5, 1864. Add so Scycler, er died of disease, at Decatur, Ala., 12, 1864. Charles Taylor, died of disease, at Nashville, Tenn., July 14, 1864.


Mustered out at Louisville, Kentucky, , July 13, 1865.


CO. F, 50TH REGIMENT O. V. I.


Company F was .raised in Belmont county, and was mustered into service August 30, 1862. The company was organized as follows


Thomas Clark, Captain.

James G. Theaker, 1st Lieutenant.

Robert P. Moore, 2d Lieutenant.

Thomas C. Thoburn, 1st Sergeant.

Hugh Dubois, Sergeant.

George R. Grier, Sergeant.

James R. Griffith, Sergeant.

Andrew D. Mitchell, Sergeant.

Lords N. Soles, Corporal.

Isaac I. Cox, Corporal.

James W. Shipman, Corporal.

George W. Shipman, Corporal.

Charles D. Chandler, Corporal.

William G. Taggart, Corporal.

Tames Henry, Corporal.

Jacob K. P. Gahm, Corporal.


PRIVATES.-D. K. Allen, Jesse W. Adams, Looman Beck, Wesley Beck, John T. Beck, James Boyles, G. Bliss, John A. Barrd, Gilbert W. Briggs, Samuel Briggs, John Bereg, Robert H. Clayland, John C. Chandler, Watson D. Cochran, Wilson H. Cochran, William Conway, Louis Coy, Samuel Cox, Harry Chambers, C. Cook, I. P. Conry, George Denny, Samuel Davis, Thomas S. Ewan, William Ellis, A. S. Field, Campbell Fitch, Simon Footer, Lafayette Githans, Thomas I. Githans, Charles Goff, Peter Gorman, Robert H. Griffith, A. H. Gody, Robert Goff, James Hutchison, Seth Howell, William Harrison, William Jackson, Charles Johnson, Levi Jones, Harry Jones, Samuel Jones, John Leech, Peter Leoman, William W.. McWilliams, Cyrus S. Moore, James Miller, Thomas D. Moore, Daniel S. Megeary, Joseph Marple, William A. Miller, Samuel Munloch, Peter Murry, John A Patterson, Theodore Porter, Nathan Parker, William Peirsall, George Phus, William Ryan, Philips Renick, John W. Riley, G. P. Riley, A. H. Reed, Jacob Bennet, G. W. Snodgrass, W. T. Steedman, Richard Slocum, H. H. Sprigg, Andrew Steele, George W. Trover, S. H. Taggart, Saul Thompson, John H. Tyson, Reuben Wells, Barnard Williams, Philip Wilson, Barnard White, Henry Wooster, John Young, Stephen Yates.


PROMOTIONS, CASUALTIES, ETC.


James S. Theaker was 1st Lieutenant from August 18, 1862, until June 21, 1864, when he was promoted to Captain. Thomas Clark was discharged June 21, 1864, on Surgeon,s certificate. Seth Howell was appointed corporal, May 1, 1863 ; severely wounded in the battle, of Franklin, November 30, 1864. David K. Allen, severely wounded in the battle of Franklin, November 30, 1864. James Miller, last heard from, August, 1864, in hospital at Camp Dennison, Ohio. Joseph W. Stringer, was taken prisoner, November 30, 1864, at Franklin.


DISCHARGED.


Hugh D. Dubois, was promoted to 1st Sergeant, June 21, 1864, wounded at Franklin, November 30, 1864; discharged March 5, 1865, by reason of consolidation with the 99th Ohio Volunteer Infantry. George R. Grier, discharged, March 5, 1865, by reason of consolidation with the 99th Ohio Volunteer Infantry. Andrew D. Mitchell, discharged, March 5, 1865, by reason of consolidation with the 99th Ohio Volunteer Infantry. Charles B. Chandler, discharged, March 7, 1863, for the Marine service. Robert Goff, was appointed corporal; May 1st, 1863 ; discharged March 5, 1863 ; and consolidated with 99th Ohio Volunteer Infantry. James Henry, discharged, November 24, 1862. Thomas D. Moore, appointed corporal, December 23, 1862 ; taken prisoner, November 30, 1864, at battle of Franklin ; discharged, May 22, 1865. William Taggart, discharged April 2, 1863. Hamilton Warren, transferred from 99th Ohio Volunteer Infantry, December 31, 1864; discharged, March 5, 1865. Robert H. Clayland, was appointed corporal, September 27 1862, discharged June 7, 1865, at Wheeling, W. Va. Looman Beck, discharged on certificate of disability, March 16, 1863. John A.. Barr, discharged, May 24, 1865. Louis Coy, discharged, October 28. 1862, for disability. W, P. Cochran, discharged, March 9, 1863, for disability. W. H. Cochran, discharged, May 23, 1863, for disability. William Ellis, discharged, January 1, 1863, for disability. Campbell Fitch, discharged, January 1, 1863, tor disability. Lafayette Githers, taken prisoner, November 30, 1864, at battle of Franklin ; discharged, May 20, 1865. William Kiphart, discharged, May 24, 1865. William A. Miller, discharged, March 24, 1863, for disability. Joseph Marple, discharged, November 24, 1862, for disability. Theodore Porter, discharged, November 24, 1862, for disability. L. M. Souls, discharged, April 17, 1865. George W. Shipman, discharged, May 12, 1865. William Rynard, discharged, April 10. 1863 for

disability.


TRANSFERRED.

John Leech, William Pursell, G. P. Riley.


DIED.

James Boyles, died in hospital at Lebanon, Ky., Nov, 29, 1862, of erysipelas fever. James Francis, killed in battle of Perryville, Oct., 1862. Jacob K. P. Githens, died in hospital, Camp Dennison, 0., Oct. 3, 1864. Thomas J. Githens, died in hospital at Atlanta, Ga., Oct. 21, 1864, of dysentery. Charles Smith, taken prisoner at battle of Franklin, Nov. 30, 1864; died March 27, 1865. at Vicksburg, Miss.


DESERTED.


Gilbert Biggs, John Berry, Samuel Briggs, Samuel Cox, Harry Chambers, Charles Goff, James Hutchison.


There were 38 deserters from this company, but the above were all from Belmont county. This company was mustered out at Salisbury, N. C., June 26, 1865.


Co. O, 52D REGIMENT, O. V. I.


Company C was composed mainly of recruits raised at Barnesville and Somerton. On the 20th of August it was accepted into the service at Camp Dennison, 0., where the 52nd -Regiment was organized. The officers were :


204 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


Captain, Jacob E. Moffitt.

1st Lieutenant, Abisha C. Thomas.

2d Lieutenant, Ezekiel E. Mills.

1st Sergeant, William P. Shanklin.

Sergeant, William Starbuck.

Sergeant, Newton. McGill.

Sergeant, William J. Bradford.

Sergeant, J. N. Hunt.


Corporals—Isaac Yocum, Wm. H. Piper, John H. McHendry, C. W Grimes, James H. Curtis, Newell H. Buchannan, Wm. C. Deems.


Drummer, Charles W. Tillett,


RESIGNATIONS, TRANSFERS, ETC.


Jacob E. Moffitt, resigned, Feb. 2, 1863. Abisha C. Thomas, mustered out. William P. Shankland, resigned, June 18, 1863. Christopher W. Grimes, mustered out ; commanded Co. C, to 1865 ; commanding Co. K, since April 1, 1865. Ezekiel E. Mills, resigned, Feb. 13, 1863.


MUSTERED OUT.


William Starbuck, Newton Gill, Edwin D. Patterson, promoted from Corporal to Sergeant, March, 1865. Isaac Yocum, N. H. Buchanan, W. C. Deems, Joseph A. Parsons, Chas. T. Whitaker, promoted to corporal. Charles W. Tillett, promoted from private, March 1, 1865. Harrison Moore, promoted from private, March 1, 1865. John W. Hance, promoted to corporal. Thomas B. Barnes, John Bailey, Wm, Carter, Isaiah B. Clift, Wm H. Coventry, William Calvin, Geo. W. Calvin, John Dilliha, George W. Day, James W. Falger, Isaac Hayes, W. G. Hilton, R. W Harris, James Hines, Humphrey Baler, John N. Hunt, Clemmens Hicks, William Hadley, Gilmore Howell, John W. Hardesty, William Latham, John W. Merrill, S. W. Parker, W. H. Piper, Thomas Petticord, John Bucker, John W. Stubbs, Alfred Stiffler, James T. Woodland, W. W. Wildman, Robert Warnock.


KILLED IN BATTLE.


Fenton M. Carter, killed by cannon shot, May 14, 1864, at Resaca, Ga. L. H. Street. killed by musket shot, June 27, 1864, at Kenesaw Mountain, Ga. Boyd Forbes, killed by musket shot, June 27, 1864, at Kenesaw Mountain, Ga. Wm. F. Beatty, killed by musket shot, July 19, 1864, at Peach Tree Creek, Ga. Alfred Bruster, killed by musket shot, Sept. 1, 1864, at Jonesboro, Ga.


DIED.


E. B. Clifford, died, Oct. 20, 1862, at Harrodsburg, Ky., of typhoid fever. George W. Campbell, died Dee. 29, 1862, at Nashville, Tenn. of chronic diarrhæ, John Forbes, died Dec. 16, 1862, at Nashville, Tenn., of chronic diarrhæ Isaac Stid, died Jan. 23, 1863, at Nashville, Tenn., of erysipelas, Chapman Harner, died Nov, 11, 1862, at Bowling Green, Ky., of chronic diarrhæ. Ashbury Malone, died July. 25, 1863, at Nashville, Tenn., of chronic diarrhoea. John Malone, died March 23, 1864, at Nashville, Tenn. W. F. Lewis, died July 10, 1864, at Chattanooga, Tenn., of diarrhoea. W. J. Bradfield, died Aug, 8, 1864, at Nashville, Tenn. Mordecai Carter, died Aug. 8, 1864, at Nashville, Tenn. Alexander Hinton, died Sept. 13, 1864, at Atlanta, Ga. John W. Barnes, died March 21, 1865, near Bentonville, N. C., of wounds. James Chance, died March 25, 1865, of wounds. Ezra J. Mann, died May 1st, 1865, at New Bern, N. C.


DISCHARGED.


Amos H. Hampton, Oct. 24, 1862. E. Bailey, Dec. 19, 1862. B. F. Perky, Dec. 19, 1862. E, C. Tomlinson, Jan. 20, 1863. J. W. Hunt, Jan. 26, 1863. Asa T. Patterson, Feb. 6, 1863. John L. Brister, Feb. 20, 1863. William McDonald, December, 1862. Josiah B. McKee, Nov. 10, 1862. W. A. Brister, Nov. 10, 1862. Francis M. Acton, July 4, 1863. John H. McKendree, Aug. 20, 1864. James H. Carter, March 27, 1865. James W. Lyne, May 1, 1865. Jerome Miller, May 20, 1865.


TRANSFERRED.


Wm. L. Patton, to Engineers Corps, Aug. 31, 1864. James P. Carter, to V. R. C. Isaac Teets, mustered out June 3, 1865, at Washington, D. C.


CO. F., 52D REGIMENT, O. V. I.


Company F was recruited at Powhatan, Armstrong,s Mills, Dillie,s Bottom and Captina. It entered service at Camp Dennison, August 22, 1862. Officers were as follows:


Captain, J. B, Donaldson.

First lieutenant, John Irwin.

Second lieutenant, Samuel C. Hutchison.

Sergeant, Thomas B. Hammond.

Sergeant, James W. McFadden.

Sergeant, Samuel M. Gorden.

Sergeant, Julius Armstrong.

Sergeant, Benjamin F. Thomas.


Corporals, Sylvester L. Brice, Conrad Slupman, Albert E. Crist, Anthony T. Lockwood, James McAvoy, James G. King, Isaac Gates, Elijah R. Hudson.


RESIGNATIONS, PROMOTIONS, ETC.


James B. Donaldson, resigned May 22, 1863. Samuel C. Hutch ison, mustered out. John Irwin, resigned May 20, 1863. Sylvester L. Brice, mustered out. Julius Armstrong, promoted to first lieutenant and transferred to company H.


MUSTERED OUT.


T. B. Hammond J, W. McFadden, W. S. Swain̊, John W. Hess, Anthony Lockwood, (no dis. furn,d) sergeants ; Michael Long, Isaac Yates, E. R. Hudson, Thomas Tyrrel, Peter Griffin, corporals.


PRIVATES—John Anthony, Martin Baker, Eli Barnes, Volney Blue, Alex. C. Crist (no dis, furn,d), J. R Grist, (no dis. furn,d) David Dillon, William Duvall, Steward Doty, Robert Gates, James Gates, J. J. Gillespie, Robert Gillispie, Samuel Gillespie, Wellington Gillespie, F. J. Hendershot, Johnson Hammond, James Holland, G. W. Jones, T. H. Kirkland, John Moore, W. W. Moore, John. McVay, M. C. McCabe, (no dis. J. C. Rittman, Martin Purtiman, Salathiel Pugh, N. Pugh, (no dis. furn,d), h. Roder, William Souste, Joshua Swaney, Jas. Thornburg, James Tyrrell, Isaac Vandign, Jonathan Vandign, Perry Wright..


KILLED IN BATTLE.


Albert E. Crist, killed in action at Kenesaw Mountain, Ga., June 27, 1864. Robert J. Stewart, killed in action at Kenesaw Mountain, Ga., June 27, 1864. Augustus T. Dorsey, killed in action at Kenesaw Mountain, Ga., June 27, 1864.


DIED.


Conrad Shipman, died November 3, 1862, of consumption at Evansville, Md. James G. King died November 22;1862, of fever at Danville, .Ky. Ebenezer Gillespie died of wounds received in action at Kenesaw Mountain, Ga., June 27, 1864. Cornelius Hess died October 30, 1862, of inflammation of lungs. Valentine Bryson died November 5, 1862, of congestive chills., .near Franklin, Ky. John W. Sidles died December 2, 1862, of chronic diarrhoea,. at Bowling Green, Ky, Asa Vandign died December 19, 1862, at Nashville, Tenn. Jacob Shepherd died December 25, 1862, at Nashville, Tenn. James Lucas died January 7, 1863, at Nashville, Tenn. Joseph B. Roder died January 7, 1863, at Nashville, Tenn. Robert Owens died January 1, 1853, at Nashville, Tenn. Joshua Campbell died January 30, 1863, at Nashville, Tenn. John Kinney died January 22,1863, at Nashville, Tenn: John Hess died February 3, 1863, at Nashville, Tenn. John Siler died February 6, 1863, at Nashville, Tenn.


DISCHARGED ON DISABILITY.


Samuel M Gorden, February 9, 1863, Benjamin F. Thomas, April 6, 1863 ; James McAvoy, January 7, 1863 ; Wm. Bennett, October 27, 1862 ; John Shipman, John Jobes, November 17, 1862 ; Dorsey Danford, December 12, 1862; Robert Carpenter, February 1, 1862 ; Michael Allen, Alex. Landers, John Rush, G. W. Lindsey, February 3, 1863 ; Singleton Owens, Ed. Huffman, Henry Huffman, Daniel Groves, Alfred Doty, February 9, 1863 ; Hezekiah Laffell, February 10, 1863 ; John R. Trigg, February 16, 1863 ; W. T. Minanger, May 5,1863 ; Wm. Gatten, October 11, 1862 ; Win. Richardson, February 24, 1864 ; Frank F. Cook. discharged, but no record given ; Christian May, Oct. 27, 1864 ; Joseph H. Jones, April 25, 1864.


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 205


TRANSFERRED.


Thomas Boyers, G. W. Wallace, James B. Day, Robert A. Hammond.


PRISONERS OF WAR.


Thomas Fink, taken prisoner at Peach Tree Creek, Ga., July 16, 1863 ; supposed to have died. Wrias R. Martin, taken prisner near Goldsboro, N. C., while foraging; supposed to have teen murdered by his captives, March 17, 1865.


Mustered out June 3, 1865, at Washington, D. C.


Co. H. 618T REGIMENT O. V. I.


This company was recruited at Bellaire, Bridgeport, Martin,s Ferry, Jacobsburg and Glencoe, Belmont county, Ohio. It was enlisted between January and April, 1862. It was organized as follows :


John Garrett, Captain.

David Rankin, First Lieutenant.

Milton W. Junkins, Second Lieutenant.

Isaiah Grafton, First Sergeant.

John Wright, Sergeant.

William Smith, Sergeant.

William Whims, Sergeant.

John G. Laning, Sergeant.,

Zenas Shipman, Corporal.

James W. Grafton, Corporal.

David B. Long, Corporal.

Wilson S. Mitchell, Corporal,

John Kennedy, Corporal.

John Drum, Corporal.

Joseph B. Dean, Corporal.

Jacob H. Long, Corporal.

Musicians—John Huntsman, William Martin.

Wagoner—William Long.


PRIVATES—Wesley G. Ault, Richard Beavers, Solomon Beach, Thomas Brown, Edward Brown, John Cumford, William Clark, John Dwayer, John Detwiler, Joseph Daagan, Alexander W. Daniels, Francis Daine, Alexander Evans, Monroe Francis, Richard S. Francis, John Fry, Nelson Gray, Isaac -A. Grist, William Gaston, Nicholas Hines, Albert Hockady, Samuel Hines, William Jopland, Thomas Jackson, Jacob Jackson, John W. Jackson, John Jones, John Johnston, Sterling Johnston, William Judd, Robert A. Kelsey, Joseph H. King, Peter Kenney, William Lash, James A. Long, S. B. Long, E. M. Mitchell, Michael McClusky, John Macauley, W. A. McKirahan, Jacob May, William Miller, John Moore, George Martin, James Nich- olson, Hugh Nixon, Terrence O,Brine, Robert H. Patterson, John W. Patterson, Samuel Potts, Richard Pearce, David Porter, Walker Pittett, John Porter, John T. Rothwell, James D. Richards, James S. Smith, Alfred Shahan, John Shatzer, George Swartz John C. Taylor, Joseph Penlev. Taylor. James W. Wright, George W. Worley, Michael Welsh, James Weir, Daniel W. Wise, Charles Wright, Fedale Zarne.


Company H was partially consolidated with the 82nd regiment, Ohio Infantry, March 31, 1865, and made part of company H of that regiment.


CASUALTIES OF CO. H.


John G. Lanning, promoted to sergeant February 11, 1864. James S. Smith, promoted to corporal February 5, 1864. John T. Bothwell, promoted to corporal March 2, 1864. David Porter, promoted to corporal February 4, 1864. Westley G. Ault, promoted to corporal June 2, 1865.


DISCHARGED.


James Cain, released prisoner ; discharged by virtue of War Department. James W. Wright, discharged at Camp Dennison, Ohio, June 28, 1865. Mustered out at Louisville, Ky., July 24, 1865.


COMPANY E, 62D REGIMENT O. V. I.


Company E was organized at Somerton and rendezvoused at Camp Goddard. This company was mustered into service October 16, 1861. The company was as follows :


Henry G. Jackson, captain.

Samuel B. Taylor, second lieutenant.

Joel M. Maring, third lieutenant.

Samuel D. Hopper, first sergeant.

Francis A. Bishop, sergeant.

John Couplin, sergeant.

Charles E. Rowlen, sergeant.

Jonathan Dunn, sergeant.

Abel Hicks, corporal.

William S. Hobbs, corporal.

John B. Powell, corporal.

Aquilla Thomas, corporal.

William Sullivan, corporal.

James Smith, corporal.

Wilson Strahl, corporal.

Thomas Wilson, corporal.


PRIVATES.—Joab Bishop, James K. Bishop, Benjamin Bishop, Stephen I. Brown, Samuel H. Blaney, Charles Biddenhorn, William Burcher, Charles O. Bishop, James O. Couplin, William H. Carter, George Carpenter, Abraham Clark, Stephen Clandy, Henry Clark, Waldon Clark, John A. Driggs, Christopher Dillen, William T. Fletcher, Thomas H. Gibbins, William S. Gregg, Thomas D. Gibbins, David H. Grimes, Lawrence W. Hobbs, Alonzo M. Hobbs, Nathan H. Burford, Benj. S. Hurford, John W. Hopper, William W. Hopper, John L. Hadsall, Henry Howard, William E. Hudson, William W. Johnson, McDowell T. Koontz, George Kadle, Andrew I. Lane, John Livingstone, Franklin Morris, John R. Murrill, James Maxwell, Eli Miller, Benjamin Mahoney, George B. Monette, Washington Nelson, Vance Nelson, Joseph Nelson, Franklin Outland, Joseph Palmer, Elwood Price, Theophilus Peddicord, Lycurgus Peddicord, Gladne Patterson, Crawford Riley, Nathan Strahl, David L. Strahl, E. D. Strahl, William M. Stewart, Milton B. Stay, Thos. Starbuck, William I. Snode, Andrew C. Shepherd, Wm. Street, Evan T. Strahl, Thomas Strahl, Joseph C. Tomlinson, John W. Vandyke, William West, Leander Wiley, James L. Wharton, John Yocum, Joseph Yocum, Thomas Yarnall:


CASUALTIES.


Samuel H. Hopper was appointed first sergeant December 14, 1861 appointed second lieutenant August 11, 1862 ; ap- pointed first lieutenant May 16, 1863; appointed captain October 15, 1863; wounded slightly in the charge upon Fort Wag- ner, S. C. Thomas Wilson was appointed corporal December 14, 1861 ; promoted to sergeant May 15, 1862 ; promoted to first sergeant September 2, 1862; was severely wounded in the left hand and slightly in right side in the charge on Fort Wagner, S. C., July 18, 1863 ; re-enlisted February 26, 1864 ; reappointed first sergeant February 1, 1864, William S. Hobbs was appointed corporal December 14, 1861; promoted to sergeant September 2, 1862; re-enlisted January 1st, 1864; reappointed sergeant February 1, 1864. Charles E. Rowlen was appointed sergeant December 14, 1861 ; re-enlisted January 1, 1864 ; reappointed sergeant February 1, 1864. Wilson S. Strahl was appointed corporal December 14, 1861; promoted to sergeant July 1, 1863; re-enlisted January 1, 1864 ; reappointed sergeant February 1, 1864. Charles G. Bindenharn was promoted to corporal September 2, 1862 ; promoted to sergeant July 1, 1863 ; was wounded in leg by pistol shot, and take prisoner in charge upon Fort Wagner, S. C.; was exchanged July, 1863 ; re-enlisted ; reappointed sergeant, William W. Sullivan was appointed corporal December 14, 1861; re-enlisted ; reappointed corporal. McDowell T. Koontz was promoted to corporal May 16, 1862; re-enlisted ; reappointed corporal. John L. Hadshall was promoted to corporal September 2, 1862 ; was wounded in leg by shell in charge upon Fort Wagner, S. C., July 18, 1863. Wm. W. Hopper was promoted to corporal Feb. 1, 1864; re-enlisted; served in three months, service in the 17th Ohio regiment. Waldon Clark was promoted to corporal July 18, 1863 ; re-enlisted ; reappointed corporal ; was in charge on Fort Wagner July 18,1863 , B. S. Hurford was promoted to corporal July 18, 1863 ; re-enlisted ; reappointed corporal ; in charge upon Fort Wagner. Vance M. Nelson was promoted to corporal July 1, 1863; was in charge upon Fort Wagner July 18, 1863. W. H. Carter was promoted to corporal January 1, 1863 ; wounded severely by musket shot in the shoulder in the charge upon Fort Wagner, S. C., July 18, 1863. Stephen J. Brown was in charge upon Fort Wagner, S. C. Samuel H. Blaney was wounded severely in right arm by musket shot in charge upon Fort Wag ner. S. C. David T. Burr and Joseph A. Budd were in charge upon Fort Wagner, July 18, 1863. Henry S. Clark was taken prisoner in the charge upon Fort Wagner. William Craig detached as artilleryman July 20, 1862. John A. Driggs, William T. Fletcher, Thomas D. Gibbins, William S. Gregg, and Nathan H. Hurford were in charge upon Fort Wagner. Alonzo M. Hobbs was severely wounded in leg by musket shot in charge upon Fort Wagner. John T. Livingston was severely wounded


206 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


in foot by fragment shell at the siege of Fort Wagner. Franklin Morris was in charge at Fort Wagner.. Washington Nelson was in charge upon Fort Wagner July 18, 1863. Joseph Nelson, Gladne Patterson, William T. Street and John W. Snode were in charge upon Fort Wagner. Thomas Starbuck was taken prisoner at Fort Wagner. A. G, Taylor was in charge upon Fort Wagner, S. C., July 18, 1863. Leander Wiley was wounded severely in the neck by musket shot in the charge upon Fort Wagner.


DISCHARGED


Henry G. Jackson discharged May 26, 1862, on account of disabilities. Joel M. Marring was appointed as captain, December 7, 1861; resigned on surgeon's certificate, August 11, 1862. Thomas Showers, transferred from company A ; discharged on surgeon,s certificate, January 29, 1863. Able Hicks, appointed corporal December 14, 1861 ; promoted to sergeant, May 15, 1862; discharged August 4, 1862. Jonathan Dunn, appointed sergeant, December 14, 1.861 ; discharged on surgeon,s certificate, December 26, 1862. John Couplain, appointed sergeant, December 14, 1862 ; discharged on surgeon,s certificate, May 8, 1862. Aquilla Thomas, appointed corporal, December 14, 1861; discharged on Surgeon,s certificate, September 13, 1862. James Smith, appointed corporal, December 14, 1861; discharged on surgeon's certificate, September 29, 1862. George Carpenter, promoted to corporal, May 15, 1862 ; discharged on surgeon's certificate, December 23, 1862. Jacob Bishop, discharged on surgeon’s certificate, M.ay 8, 1862. James K. Bishop, discharged on surgeon,s certificate, July 5, 1863. Charles O. Bishop; discharged on surgeon,s certificate, June, 1.862. James O. Couplain was wounded severely in the leg by a musket shot; discharged from effects of wound. Stephen Clandz, discharged for disability, July 5, 1863. Christopher Dillen was taken prisoner at Strasburg, Va ; Discharged by disability, June 17, 1862. John W. Hopper, December 13, 1862, for disability. John R. Merrel, on surgeon's certificate, December 13, 1862. Lycurgus Peddicord, on surgeon's certificate, September 4, 1862. Chas. Patten, on surgeon,s certificate, July 26, 1862. Nathan P. Strahl, on surgeon,s certificate, October 14, 1862. David L. Strahl, on surgeon's certificate, March 29, 1863. Wm. M. Stewart, on surgeon's certificate, March 15, 1863. Milton M. Stay, on surgeon,s certificate; date unknown. Andrew C. Shepard, on surgeon,s certificate, June, 1863. Evan T. Strahl, on surgeon,s certificate, August 4, 186:3. Eugene Stewart, on surgeon,s certificate ; date not recorded. Wm. West, on surgeon’s certificate, January 24, 1863. Thomas Yarnall, on surgeon’s certificate, June, 1863.


TRANSFERRED


John B. Powell, Aaron D. Yocum, E. D. Strahl, Samuel J. Sill.


DIED.


B. F. Bishop, at Hampton hospital, Va., September 2, 1862, of typhoid fever. L. W. Hobbs, was killed in the charge upon Fort Wagner, July 18, 1863. Wm. E. Hudson, died a prisoner in Charleston, S. C., from wounds received in the charge upon Fort Wagner. Wm. W. Johnson was killed in the charge upon Fort Wagner. George. T. B. Monette, died at Frederick, Md., April 15, 1862, of typhoid fever. Riley W. Crawford was killed in the charge upon Fort Wagner. John W. Vandyke died at Harrison's Landing, August 11, 1862, of brain fever. James E. Stewart, died at Hilton Head, S. C., April 24, 1864, of hemorrhage of the bowels.


This company was mustered out June 1, 1864. The history of this company is identical with the history of the regiment, as it never was separated from it.


Co. E, 77TH REGIMENT O. V. I.


This company was recruited at Bellaire, Pultney township, Washington, Mead and York townships, Belmont county. It rendezvoused with the regiment at Marietta, where the regimental organization took place. .tease Hildebrand was elected Colonel, The organization of company E, with its members, were as follows :


Andrew Smith, Captain.

Thomas Garrett, First Lieutenant.

Hanson Criswell, Second Lieutenant.

Daniel McCabe, First Sergeant.

John L. McIntire, Sergeant.

Levi M, Sinclair, Sergeant.

G. W. Williams, Sr., Sergeant.

John L. Thomas, Sergeant.

Thomas Anderson, Corporal.

John K. Hepburn, Corporal.

Israel R. Heath, Corporal.

Charles J. Bloom, Corporal.

Dennis Hogan, Corporal.

Benjamin Dunlapp, Corporal.

Jacob P. Kinney, Corporal.

James M. Baker, Corporal.

John W. Stanhope, Musician.


PRIVATES—Edward Burns, Thomas Barker, Peter Brandon, Leander Barnet, Win. C. Berry, Samuel Bennington, William Bennington, J. T. Broxton, James Baxter, Thomas B. Crozier, Jesse Cross, William Craigg, Wm. Chance, Benjamin Doyel, Eli B. Davison, James A. Dumfie, Monterville Drummond, Isaac Fogle, Jeremiah A. Fish, Isaac Gilbert, Moses Gordon, Austin Gill, John Hays, G. W. Hogan, James P. Hammond, David M, Hammond, Robert Hess, Dixon M. Hepburn, Andrew J. Heath, Joseph Hubbs, Hamilton Hunter, Jerome Higgs,. Emmer Jackson, Samuel Jackson, Harrison Jackson, Jacob Johnston, George Johnston, Edward Kinney, William Kinney, Robert Knox, Nathaniel Luke, Chas. Lyttleson, John McMillen, Francis Miller, Wm. P. B. McFarland, Thomas McCormick, Wm. H. O,Neil, Francis Pitner, Jacob Prest, Hugh Paden, William Porter, William. Ritcheson, Reuben Russell, Thomas Rosser, J. C. Sissel, Arthur Sissel, John Seaber, Johnston Sinclair, William Smith, Daniel Shoup, Samuel R. Thomas, John C. Taylor, Wilson S. Venharn, Nathaniel B. Wright, George W. Williams, Jr., William Williams, Andrew Williams, James Wallace, James W. Wallace, Thomas H. Wallace, John Wingrove,. Perry Wright, James Wells.


The men of company E re-organized 8,8a portion of companies E and F of the same regiment.


PROMOTIONS, TRANSFERS, ETC.


Company E.—Robert Hess, promoted to corporal, March 20, 1864. John Kune, promoted to corporal, June 5, 1863. Francis A. Pitner, promoted to corporal, June 16, 1865. Johnson C. Sinclair, promoted to corporal,.December 1, 1865. Samuel Bennington, promoted to corporal, March 1, 1866. John Wingrove, promoted to corporal, March 1, 1866. George W. Williams, promoted to sergeant until May 31, 1865 ; discharged at same date. Jacob P. Kinney, appointed sergeant, April 27, 1865, and trans- ferred to company F. Eli B. Davison, appointed corporal, April 27, 1865, and transferred to company F. Jeremiah A. Fish, transferred to N. C. S. of regiment and appointed quartermaster sergeant. W. H. O,Neil, transferred to vet. reserve corps, April 21, 1865. Geo. W. Hogan, died of disease at hospital in Louisiana, June 11, 1865.


Mustered out at Brownsville, Texas, March 8, 1866.


Company F.—George Johnson, Jacob Prest, Reuben Russell, Thomas Rosser, Wm. Smith, James W. Wallace, Geo. W. Williams, Jacob B. Kinney, promoted to sergeant, December 12, 1861. W. P. B. McFarland, discharged on disability, May 30, 1865. Jacob D. Decker, died while a prisoner of war at Tyler, Texas, July 21, 1864.


Mustered out at Brownsville, Texas, March 8, 1866.


CO. B, 98TH REGIMENT O. V. I.


This company was enlisted at St. Clairsville and organized with regiment at Camp Mingo, near Steubenville, August 22, 1862. Its original officers and members were as follows :


Joseph R. Mitchell, Captain.

Louis Woodmansee, First Lieutenant,

Hiram J. Craft, Second Lieutenant.

Jacob L. Holloway, First Sergeant.

Thomas J. Hawthorne, Sergeant.

Samuel R. Smith, Sergeant.

Benjamin R. Griffith, Sergeant.

Jacob Hymes, Sergeant.

Henry McDonald, Corporal.

Hamilton Rogers, Corporal.

James F. Watson, Corporal.

William H. Roscoe, Corporal.

Johnston Mitchell, Corporal.

James E. Judkins, Corporal.

G. W. Makinson, Corporal.

Isaac H. Nichols, Corporal.


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 207


Jesse Brandenburgh, Musician.

William Reynolds, Musician.

John F. Smur, Wagoner.


PRIVATES.—William J, Alexander, Charles A. Allen, William Bell, Dighton Berry, John A. Bethel, Josiah Blackford, Smith Branson, James A. Brown, Albert Brown, Samuel Bruce, P. C. Campbell, Hiram Culp, Nathan G. Davis, Thomas Davis, Moses H. Dewault, David L. Dewault, Wm. F. Duff, David D. Dutton, Henry Fitzgerald, Eli M. Fowler, James Galbraith, Alfred Gardner, George H. Glenn, John Graham, George Graham, James Graham. Isaac G rimes, Johnston Hammond, Pennington Harden, Robert Hare, Wm. A. Hastings, Wilson Henderson, Jesse Huff, Job Hughs, W. B. James, John Jamison, George Jepson, Ezra Johnston, A. R. Jones, Allen M. Kirk, Evan B. Kirk, Ebenezer F. Knapp, J. B. D. Keim, Joseph P. Lees, L. S. Lilly, T. C. Martin, Wm. H. Miller, Martin Moore, James McBride, Jas. A. McNary, Mahlon Nichols, Thomas Nichols, Samuel M. Noah, W. W. Orison, John Patton, George M. Patton, Charles L. Pickering, Isaac K. Piggott, John Pollock, Reason Porter, Jesse Pratt, John Ralston, John T. Roseboro, ____ Rogers, Conrad Schmeitzer, Alex. H. Sloan, Joseph Smith, Joseph Spencer, Jerry Stinard, J. B. Stewart. James A. Stewart, Charles Stilwell, Lemuel Stilwell, William Taylor, G. W. A. Thompson, Alexander Thoborn, Ignatius Tillett, Geo. W. Vanscyol, Lewis Walter, Jesse M. Woods, O. A. Zane, Benj. Zane.


PROMOTIONS, CASUALTIES, ETC.


Joseph R. Mitchell, discharged October 14, 1864, on account of disability. Reece G. Lewis, promoted from first lieutenant company E; mustered out on separate rolls. Louis Woodmansee, discharged on account of disability December 23, 1863. Jacob A. Holloway was promoted from first lieutenant August 1, 1864. Hiram J. Craft was promoted from second lieutenant to captain of company E, July 29, 1864. George W. Makinson was promoted from corporal to sargent September 1, 1864. John Patton entered service as private ; promoted to corporal September 1, 1864. Mahlon Nichols was promoted to corporal September 1, 1864; wounded in battle at Bentonville March 19, 1865. Isaac Piggott was promoted to corporal September 1, 1864. James A. Stewart was promoted to corporal September 1, 1864. William B, James was wounded at Jonesboro, Ga., September, 1864. O. A. Zane was exchanged prisoner at Bridgeport, Ohio.


KILLED.


L. S. Lilly was killed in battle at Chickamauga, Ga., September 20, 1863. Johnson Mitchell was killed in battle at Jonesboro, Ga., September 1, 1864. Josiah Blackford was killed in battle at Chicamauga, Ga., September 20, 1863. Robert Hare was killed in battle at Perryville, Ky., October 8, 1862. John Jameson was killed in battle at Kenesaw Mountain, June 27, 1864. William H. Miller was killed in battle at Perryville, Ky., October 8, 1864. George W. A. Thompson was killed in battle at Perryville, Ky., October 8, 1862. Reason Porter was killed in battle at Perryville, Ky., October 8, 1862. Jesse M. Woods was killed in battle at Resaca, May 14, 1864.


DIED.


Hamilton Rogers died of disease at Perryville, Ky., October 19, 1862. Henry McDonald died of wounds received in battle at Jonesboro, Ga., September 1, 1864, John Pollock promoted to corporal November 25, 1862; died of wounds received at Chickamauga, September 20, 1863. Moses H. DeVault, died of wounds received in battle at Jonesboro, Ga., September 1, 1864. David D. Dutton, died of disease in hospital at Savannah, February 25, 1865. John Graham, died in hospital at Nashville, April 1, 1863, of chronic diarrhæ. George Glenn, died in Flush- ing, Ohio, February 17, 1863, of typhoid fever. George Hale, died of disease in hospital at Nashville, Tenn., August 25, 1864. Addison R. Jones, died in Lebanon, Ky., November 11, 1862, of typhoid fever. J. B. D. Kelm, died November 19, 1863, in hospital at Franklin, Tenn., of typhoid fever. Joseph P. Lees, died of wounds received in battle at Bentonville, N. C., March 10, 1865. Samuel M. Noah, died of chronic diarrhae February 6, 1863, at Lebanon, Ky. William W. Orrison, died of wounds (accidentally) at Convalescent Camp, Nashville, Tenn. Charles L. Pickering, died of disease in hospital at Lebanon, Ky., November 20, 1862. Joseph Spencer, died in hospital of disease, at Louisville, Ky., March 5, 1863. Joseph Smith, died of wounds received in skirmish near Graysville, Ga., November 26, 1863. Alexander Thorburn, died of disease at Cumberland, Ind., April, 1865.


DISCHARGED.


William T. Alexander, discharged January 31, 1862, to enlist in marine service. John A. Bethel, discharged January 31, 1863, for the same purpose. Smith Branson, discharged for disability December 11, 1862. P. C. Campbell, discharged December 30, 186, on account of wounds received in battle at Perrysville October 8, 1862. Thomas Davis discharged for disability, 1863. David L. Devault, discharged for disability December 14, 1863. Alfred N. Gardner, discharged for disability March 14, 1863. Isaac T. Grimes, discharged January 2, 1863, on account of wounds received in battle at Perryville October 8, 1862. Johnson Hammond discharged March 3, 1864, on account of wounds received in battle at Chickamauga. William A. Hastings, discharged for disability November 18, 1862. Wilson Henderson, discharged January 27, 1864, for wounds received in battle at Perrysville October 8, 1862. Allen M. Kirk, discharged for disability September 25, 1862. Thomas Nichols, wounded in battle at Perryville October 8, 1862 ; discharged for disability April 28, 1864. Jesse Pratt, discharged for disability May 29, 1863. John F. Roseborough, discharged for disability July 14, 1863. John B. Stewart, discharged for disability March 25, 1863, A. M. Sawash, discharged for disability March 21, 1865. Geo. W. Vanscyol, discharged January 19, 1862, to enlist in marine service.


TRANSFERRED.


Benj. B. Griffith, James F. Watson, Jesse Brandenburgh, Jeremiah Stinrod, William Taylor, Ignatius Tillet, Chas. M. Blackburn, Thomas E. Hale, G. L. Knapp, Philip Vilton, Hiram Riggs.


The company was mustered out June 1, 1865.


COMPANY E, 98TH REGIMENT O. V. I.


Was enlisted in Belmont county, and was mustered into service August 20, 1862. The original officers and members were as follows :

Adam Cordner, captain.

Zachary C. William, first lieutenant.

John T. Collins, second lieutenant.

Lewis G. Rece, first sergeant.

Lewis Boger, sergeant.

John H. Price, sergeant.

W. T. Harmar, sergeant.

Cyrus B. Lingo, sergeant.

E. W. Smith, corporal.

William H. White, corporal.

George C. Vanlaw, corporal.

Clark Wilkison, corporal.

Alfred W. Givens, corporal.

Thomas Bell, corporal.

Jesse Cordner, corporal.

Enfield Wineman, musician,

Dennis L. Kemp, musician.

L. C. Griffith, wagoner.


PRIVATES.—Lewis Adison, Henry Ault, John M. Battin, Wilson Battin, Henry C. Beall, Mahlon Brown, Henry Bright, Martin G. Budd, Thomas Burnes, Milton Carpenter, Thomas Carpenter, David Cecil, Evan Chandler, B. L. Craig, James Creighton, William Davis, Ezra Davis, Michael Delany, Henry Defenbaugh, William Dermolt, David R. Eggey, John E. Evans. E. D. Evans, John Finch, John Finney, Nehemiah Fisher, Ed. S. Foreman, 0. E. Folk, John Gallagher, Archy Garrett, Reuben Green, Samuel C. Green, Alex. Green, Wm. M. Green, Nicholas Gregg, Abner 1. Gregg, Robert Harris, George Hinkle, George E. Hoops, Nathan Humphrey, Abner L. Hunt, John W. Jones, Caleb Jones, William T. Jones, William L. Kemp, John A. Kemp, William Knight, B. H. Lane, B. F. Leach, Wm. K. Lightfoot, Benj. Loper, William B. Lucas, Robert N. Luke, John Moore, Wm. H. Morrison, James Murry, Edward McGinnis, Broomhall McKessen, William McKirahan, William McMannis, William H. McMillen, R. Nevill, Thos. J. Pickering, James Powell, William H. Powell, Isaac Reader, George Russell, Wm. Spencer, Wm. Thornberry; Franklin Thornberry, Jacob Francis, Lucas Topton, John Vanfassin, Enos Waters, Jas. K. White, John White, Jonathan Wheeler, Erasmus Wilson, Nicholas Wilson, Abner Wilkissen, Joseph Whitey, Alben Wilkissen.


208 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


PROMOTIONS, RESIGNATIONS, CASUALTIES, ETC.


Adam Cordner, resigned January 54, 1863; William C. Lochary, promoted to captain, February 7, 1863; killed at the battle of Chickamauga, Georgia, September 20, 1863; John T. Collins, promoted to first lieutenant February 7, 1863 ; promoted to captain January 15, 1864; resigned July 29, 1864. Hiram J. Craft was promoted to captain company E, July 29, 1864. Reece G. Lewis was promoted from corporal to sergeant, February 7, 1863 ; promoted to first lieutenant December 7, 1864. Ezekiel W. Smith, promoted from corporal to sergeant, January 1, 1863 ; to first sergeant, December 17, 1864. James Murray was promoted from corporal to sergeant, December 17, 1864. Milton Carpenter, exchanged prisoner of war.


KILLED.


Lewis Boyer, killed in action at Graysville, Georgia, Novem- ber 26, 1863. Michael Delaney, killed in action at Perryville, October 8, 1862. William H. Davis, killed in action at Bentonville, North Carolina, March 19, 1865. John E. Evans, killed in action at Perryville, Kentucky, October 8, 1862. William M. Green, killed in battle at Perryville, Kentucky, October 8, 1862. William H. McMillen, killed in battle at Jonesboro, Ga., September 1, 1864. Isaac _Reeder, killed in battle at Perryville, Kentucky, October 8, 1862,


DIED.


William T. Harmer, died November 9, 1862, of wounds received at Perryville, Kentucky, October 8, 1862. Cyrus B. Lingo, died December 24, 186-, at New Albany, Indiana, of typhoid fever. Henry C. Bell, died June 21, 1863, at Nashville, Tennessee, of phthysic. William H. White, died November 5, 1862, of wounds received at Perryville. Thomas Burns, died November 5, 1862, at Louisville, Kentucky, of disease. Martin G. Budd, died April 16, 1865, of chronic diarrhoea, at Louisville, Kentucky. Wilson Battin, died of measles at Lebanon, Kentucky, January 6, 1863. Nehemiah Fisher, died October 16, 1862, of wounds received at Perryville, Kentucky. Nicholas Gregg, died December 12, 1862, at Columbia, Kentucky, of disease. Archie Garrett, died October 1, 1864, at Nashville, Tennessee, of chronic diarrhoea. Robert Harris, -died May 6, 1864, of disease, at Chattanooga, Tennessee. William. Knight, died April 7, 1863, of measles, at Franklin,. Tennessee. Broomhall McKissen, died October 14, 1862, of wounds received at the battle of Perryville, Kentucky. George Russle, died November 30, 1862, of disease, at Lebanon, Kentucky, Wm. Spencer, died November 7, 1862, at Lebanon, Kentucky, of disease. Lucas Tipton, died December 11, 1862, at Bardstown, Kentucky, of typhoid fever.


DISCHARGED.


John H, Price, discharged Jan, 1, 1863. Jesse Cordner, discharged February 9, 1865: Clark Wilkison, discharged January 20, 1863. Enfield Winneman, discharged February 1, 1863. Henry Bright, discharged May 20, 1863. John M. Battin, discharged January 1, 1863. James Creighton, discharged May 7, 1863. Evan N, Chandler, discharged January 15, 1863. Edward S. Foreman, discharged February 2, 1863. Alexander Green, ,discharged December 20, 1862. Samuel C. Green, discharged March 4, 1863. Nathan Humphrey, discharged November 17, 1862. Caleb Jones, discharged September 13, 1862. W. T. Jones, discharged August 6, 1863. John A. Kemp, discharged January 28, 1863. Benjamin F. Leach, discharged April 25, 1863. William H. Kiraham, discharged December 31, 1862. William McMannis, discharged April 25, 1863. Thomas J. Pickering, discharged January 16, 1863. Jonathan Wheeler, discharged February 7, 1863. Abner Wilkison, discharged May 9, 1865.


TRANSFERRED.


Jacob Travis, Alban Wilkinson, R. N. J. Luke, John Moore, John Bell, Eli Garretson.


Co. E. was mustered out of service on the 1st of June, 1865, near Washington, D. C.


Co. B, 126TH REGIMENT, 0. V. I.


Captain Wm. B. Kirk recruited this company from Flushing, St. Clairsville, Barnesville, and other points in Belmont county. 1


It was mustered into service on the 4th of September, 1862. The following was the original organization :


Wm. B. Kirk, Captain.

George W. Hoge, 1st Lieutenant.

Robert Hillis, 2d Lieutenant.

John A. Shaffer, 1st Sergeant.

Joseph L. James, Sergeant.

William B. Johnson, Sergeant.

Henry Cecil, Sergeant.

Joseph H. Palmer, Sergeant,

Reuben McGregor, Corporal.

Joseph H. Close, Corporal.

George Bowles, Corporal.

Isaac M. Clevinger, Corporal.

Barkley Cooper, Corporal.

Thos. L. Hoge, Corporal.

Wm, Copeland, Corporal.

Samuel Bailey, Corporal,

George Clinton, Musician,

Andrew Richards, Wagoner.


PRIVATES.-G. M. Bailey, Warren Bailey, Hiram W. Ball, Robert Bendure, Abner Bethel, Wm. Boyd, Enos W. Brown; B. H. Bryan, Philander Chandler, Clark Chandler, David A. Chandler. John Clark, Wm. W. Cooper, John Crawford, Samuel Criswell, Solomon Donner, William E. Dove, Isaac Eddy, Jonas Faucett, W. W. Groves, John C. Howell, Wm. P. Huffman, George Haines, Joshua C. Howell, G. S, Huston, Abraham Kelly, Melancthon Keyser, Daniel Kibler, Joseph Knight, Oliver P. Knapp, Wm. H. Loy, Edward Mathews, N. H. Majors, George McFarland, William Moore, John A. Morris, Isaac N. Mumma, John W. Near, George Obarn, John H. Patrick, William J. Patrick, Jacob Perkins, David Polan, John A Polan, Nimrod Pumphrey, Leander J. Reynolds, Simeon L. Russell, Anthony Romans, Adam Socrist, Chester K. Smith, Daniel H. Starkey, Samuel Starkey, Philip L. Speck, Daniel Thatcher, Benj. H. Vanfossen, George Vanfossen, Washington Waddell, George Weldon, James Winrod, James Parks, John Scales, Eli- jah Ferguson, John W. Vanfossen, Henry R. Lupton, Isaac Haines, Henry Hissey.


PROMOTIONS, 'CASUALTIES, ETC.


Samuel B. Swank, took command of company, Dec. 31, 1864, to June 25, 1865. Robert Hilles, died, May 13, 1864, by reason of wounds received in battle of Wilderness, May 6, 1864. William B. Kirk, discharged, June 25, 1863, disability. Joseph C. Watson, discharged, May 15, 1865. George W. Hoge, discharged. Nov. 18, 1864, to accept a commission as Colonel of a new Regiment. George Vanfossen, promoted to sergeant from corporal, April' 1, 1865, Isaac N. Mumma, promoted to sergeant from corporal, April 1, 1865. John Clark, promoted to corporal, April 1, 1865• Benjamin Vanfossen, promoted to corporal, April 1, 1865. Anthony Romans, promoted to corporal, April 1, 1865. H. W. Ball, Was exchanged prisoner of war ; captured in Battle Monocacy, July 9, 1864 ; joined company, April 23, 1865. Daniel H. Starkey, captured in the battle of the Wilderness, May 6, 1864; Exchanged and joined company, April 25, 1865. Samuel Starkey,. promoted to corporal, April 1, 1865.


NO DISCHARGES GIVEN.


Barkley Cooper, promoted to 1st sergeant, April 30, 1864; wounded and captured in battle of Wilderness, May 6, 1864. Abranam Kelley, 1st sergeant from Nov. 1, 1862, to April 30, 1864; captured in battle of Wilderness, May 6, 1864; paroled Feb. 28, 1865. John Adams, (drafted), wounded in battle near Petersburg, Va., June 22, 1864. Geo. M. Bailey, was sick in hospital at muster out. Oliver T. Knapp, sick in hospital at muster out. Daniel Kibler, exchanged prisoner of war; captured in battle of Wilderness, May 6, 1864; paroled Feb. 28, 1865. William Moore, wounded and captured in battle of Wilderness, May 6, 1864. George, Osborn, wounded in battle of Monocacy, July 9, 1865.


DIED.


Joseph Q. James, killed in battle of Wilderness, May 6, 1864. Joseph Knight, killed in battle of Cedar Creek, Oct, 19, 1864. Adam Secrist, killed in battle of Opequan, Sept. 19, 1864. William W, Cooper, died May 8, 1864, of wounds received in battle of Wilderness, May 6, 1864. Joshua C. Howell, died, May 10, 1864, of wounds received, May 9, 1864. Waitman McDaniel,


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 209


(drafted), died of wounds received in battle of Monocacy, July 9, 1864. John A. Polan, died of wounds received in battle of Wilderness, May 19, 1864. William J. Patrick, died April 1, 1864. of wounds received in battle of Wilderness, May 6, 1864. George Weedon, died May 19, 1864, of wounds received in battle of Wilderness, May 1, 1864. Isaac H. Clevenger, died Feb. 5, 1863, pneumonia, at Martinsburg. Samuel C. Bailey, died Oct. 6, 1864, of chronic diarrhea, at St. Clairsville, Ohio. Abner Bethel, died Sept. 11, 1863, of fever, at Alexander, Va. Clark Chandler, died Jan. 17, 1863, of typhoid fever, at Martinsburg, Va. Isaac Haines, missing in battle of Wilderness, May 6, 1864, John F. Linton, (drafted), missing on march from Snickers Gap, Va., July 21, 1864. Edward Matthews, missing in battle of Monocacy, July 9, 1864.


DISCHARGED.


William E. Dove, March 24, 1865 ; Henry R. Lupton, .March 27, 1865 ; Robert Bendure, Jan. 4, 1864 ; James Parks. March 11, 1865; Leander J. Reynolds, Jan. 31; 1865; William Boyd, Aug. 6, 1863 ; B. H. Bryan, Jan. 7, 1865; Joseph H. Close, Feb. 23, 1863 ; Henry Cecil, Feb. 23, 1863 ; John Crawford, March 25, 1863 ; Isaac Eddy, May 14, 1865 ; Abel Gilbert, May 27, 1865 ; G. S. Huston, Jan. 1, 1865; Thomas L. Hoge, Dec. 2, 1862 ; all the above for disability. Demas Imes (drafted), June 28, 1864 (war department); John A. Morris, mustered out, May 18, 1865; George W. Price, May 14, 1865, for disability ; John A. Shaffer, April 29, 1864, disability ; C. K. Smith, Feb. 9, 1865, disability ; John Souls, discharged June 12, 1865, disability ; Washington Waddell, mustered out, May 24, 1865; James Winrod, June, 1865.


TRANSFERRED.


Reuben J. McGregor, William R. Johnson, David A. Chandler, Joseph H. Palmer, Philip L. Speck.


Company was mustered out near Washington, June 25th, 1865.


CO. D, 129TH REGIMENT O. V. I.


This company was composed of men from Belmont, Fairfield, Monroe and Licking counties. It was mustered into the United States service at Camp Cleveland, August 10, 1863. The following are the names of those from Belmont county :


David J, Bailey, captain.

Thomas Danford, first sergeant.

John G. Mechem, sergeant.

Charles H. Damsel, sergeant.

Lewis C. Mechem, sergeant.

Robert Crozier, corporal.

Samuel B. Crew, corporal. 

Adam Moore, corporal.

Joseph McMullen, corporal.

Daniel Stukey, corporal.


PROMOTIONS.


David S. Bailey, promoted from private to first lieutenant, July 14, 1863 ; to captain, July 22, 1863. John G. Mechem, promoted from private to first lieutenant, July 22, 1863. Thos. Danford, appointed seargeant, July 23, 1863. Charles H. Damsel, appointed sergeant, July 23, 1863. Lewis C. Mechem, appointed sergeant, July 23, 1863. Robert Crozier, appointed corporal, August 23, 1863. Samuel B. Crew, appointed corporal, July 23, 1863, Adam Moore, appointed corporal, July 23, 1863. Joseph McMullen, appointed corporal, July 23, 1863. Daniel Stuckey, appointed corporal, July 23, 1863. John W. Fays, appointed corporal, July 23, 1863.


PRIVATES—William Addair, Washington Addair, Benjamin F. Baker, James C. Davenport, Christopher Dawson, Benjamin Elliott, Joseph Ebright, John H. Ellis, C. C. Grimes, died in U. S. hospital at Camp Cleveland, Ohio, February 26, 1864; John Gallagher, William Gotten, Eli Hodgin :Edmund Hibbard, Henry Huffman, William Hannon, James W, Hinion, Levy W. Jones, Henry Lisle, Daniel Lewis, Joseph Martin, Samuel Mc: Hendrey, Thomas McCoun, Lewis C. Norris, James Porterfield, Thomas C. Payne, Reuben Powell, Samuel Roddy, John Rush Milton Reeves, John S. Scribner, A. B. Shrimp, James W. Shipman, Mead P. Strahl, James T. Stidd, David Stidd, Charles Lovel, George E. Tallman, Wm. B. Wheeler, Amos Williams, John T. Ward, John W. Wright, William Wheeler.


Mustered out at Cleveland, Ohio, March 4, 1864.


27—B.&J.Cos.


170TH REGIMENT NATIONAL GUARDS.


This regiment was recruited at Bellaire, Ohio, where it was organized May 13 and 14, 1864, to serve one hundred days. It was mustered into the United States service on the 13th of May, 1864, and left for Washington City on the 17th, but being detained by the destruction of the bridge at Harper's Ferry, it did not reach its destination until the 22d. The regiment was mustered out September 10, 1864. The field and staff officers of this regiment were as follows :


Colonel, Miles J. Saunders.

Lieutenant Colonel, Arthur Higgins.

Major, Wm. W. Junkins.

Assistant Sergeant, James B. Crawford.

Adjutant, Edward S. Affleck.

Quartermaster, John Conwell.


NON-COMMISSIONED.


Sergeant Major, George W. Baggs.

Hospital Steward, Benjamin F. West.

Commissary Sergeant, James M. Paul.

Quartermaster Sergeant, John W. Cassell.


COMPANY A.


Captain, William Robinson.

First Lieutenant, George Griffin.

Second Lieutenant, Wilber H. Tallman.


Henry Miller, Thompson S. Woods, .David Steadman, Andrew Baggs, Wm. Hastings, sergeants.


Robert T. Howell, Frank Cross, Joseph Boyles, Wm. Truman, Wesley Cross, James Enlow, Wm. S. Warfield, Wm. Church, corporals. Musician. Zera Sharp.


PRIVATES.- Wm. Alexander, W. W. Atkinson, W. W. Berry, John C. Beck, Alexander Blazier, Samuel Bales, G. W. Bailey, G. W. Baggs, (appointed sergeant major and transferred to field and staff) Wm. Brooks, George Banford, James Coss, Martin Coss, John Coss, Hamilton Crawford, Newport Campbell, Marion Chalfant, James Duncan, Wm. Dysart, James Field, Isaac Fitch, John Giffin, Jesse E. Gill, Alexander Gill, James Goudy, Henry Reason, Levi Henry, Isaac Henry, John Haley, James Haines, Wm. Hukell, J. W. Hunter, John Kinsey, Isadore Lilly, James Lyle, Washington Lyle, James Low, Edward McDowell, (captured by the enemy July 24, 1864) Peachy Miller, Reese McDonald, Jas. McDonald, Jas. McIntosh, John McKnight, Leander Neelan, Armstrong Neelan, John Neininger, Theodore Porter, Jerome Porter, Sylvannus Parker, John H. Patterson, Frederick Rasher, Charles M. Rhodes; Rittenhan, James, Ryan, Clement Russell, Sanson Scott, "Benjamin F. Stephen, John Shaffer, Samuel Short, Silas Sells, Henry Stratton, Francis Seals, Edward Trueman, Benjamin F. West, (appointed hospital steward and transferred to non-commissioned staff), Ebenezer Woods, James Weir, Charles Zane, John Watkins.


COMPANY B.


W. B. Glasco, captain.

Wm. S. Fisher, let lieutenant.

Wm. Kelley, 2d lieutenant.

Henry Fisher, sergeant,

Lewis M. Casman, sergeant.

Wm. F. Gamble, sergeant (captured, July 18, 1864, near Rocky Fording, Va.)

Joseph E. Johnston, sergeant.

Robert M. Henderson, sergeant.

Benjamin W. Hamer, corporal.

Amos Spear, corporal.

Michael Fierbaugh, corporal.

Cyrus. M. Barton, corporal.

Emanuel Bell, corporal.

William S, McKee, corporal.

L. W. Hamill, corporal,

John A. Denning, corporal.

Daniel Weyandt, musician.

Thomas B. Stubbins, musician.

Jacob Warner, wagoner.


PRIVATES—John Addleman, Maurice Albaugh, Isaac Brown, B. E. Betts, Nathan Boyer, Abraham Baker, Jeremiah Brown, (furloughed May 17 to May 27, and failed to report), Zadec Bliss (mustered out, absent—sick), Henry F, Clark, wounded in action, July 18, 1864; J. C. Creagor, furloughed for one hundred days on surgeon,s certificate ; Joshua, Cox, Phillip Cahill, John L. Caldwell, Arthur Conlin, mustered out, wounded in action


210 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


near Rocky Fording, Va., July 18, 1864 ; Stevenson Creal; mustered out, wounded in action near Rocky Fording, Va., July 18, 1864; John Cammina; died in general hospital, Annapolis, Md., August 10, 1864; Harrison 1)eLong, mustered oat, September 10, 1864; WM. Dunlap, died in general hospital at Frederick, Md., July 28, 1864 : David M. Dickson, Richard Edwards, Wm. C. Edwards, John S. Eagleson, appointed acting adjutant, August 17, 1864; Richard E. Fowler, Francis Fowler, Thomas E. Fowler, Wm. E. Fowler, Ezra Griffith, Francis A. Grace, David Greenlis, John Gundy, Daniel F. Heaston, Joseph N. Heaston, James A. Henderson, George Harper, killed in action at Rocky Fording, Va. July 18, 1864; John G. Jones, Leander Long, Isaac H. Lyons, Cyrus McCurdy, Allen Miller, Andrew McBeth. George Moore, Wm. L. McMillen, John A. Myers, Enoch Miller, Walter McClintock, James Norman, Absalom Price; Israel L. Parsons, died at Fort Simmons, June 27, 1864; John Patterson , Win. Rutter, wounded in action near Rocky Fording, Va., July 18, 1864; J: L. S. Russell, Alpha H. Sheltz, John Sams, Joshua Turner, Wm. Zimmerman, John Trawl, Daniel Turner, John Thompson, Jeremiah Warner, Lewis M. Willett, Daniel Warner died of wounds received in action at Rocky Fording, July 18, 1864; John L. Webster, wounded in action July 18; Harvey Waters, Wm. Walker.


COMPANY C.


Samuel Glover, captain.

George C. Gorden, first lieutenant.

George W. Green, second lieutenant.

John. Boger, sergeant.

George Crozier, sergeant.

Ferdinand Dorsey, sergeant.

Wm. Dent, sergeant.

William Beebout, sergeant.

Frederick Boetticher, corporal.

Joseph' L. Gorden, corporal.

W. H. Gibson, corporal.

Dorsey Orloff, corporal.

Madison Scott, corporal.

Wm. Trigg, corporal.

Daniel Steiner, corporal.

Davis P. Woodburn, corporal.

John Wade, David C. Burgundthal, musicians.


PRIVATES.—Samuel Aberigg, William Anthony, Alfred Baker, Daniel Baker, John Boston, George Brock, John Brown, Jam Burgy, Arnold Burkhart, Leander P. Barnes, George Carpenter, Robert Carpenter, Andrew J. Cline, Joseph Cross, Jo-slab Dillon, Housen .Dennis, Lewis Eggers, Armor Ewers, Samuel Gorden, Thomas Gorden, Bentley T. George, Noah J. Grimes, Sylvester Green, Michael Hess, Isaiah Helms, William Harriett, Henry Hoffman. George Kelch, William Kelch, Samuel Kocher, Gustavus A. Korner ; John H. London, wounded in the thigh and captured at Martinsburg, Va.; left in hospital at Martinsburg by the rebels ; Sylvanus Lockwood, Caleb Morrison, Alonzo Mead, Joseph Moore, Francis Miller, Thomas L. Moore, John Mosier, Henry Petzold, James L. Piggett, Charles L. Peters, Marion Runnels, Jefferson Rowles, George L. Scott, William Shepherd, James R. Simpson, P. Mead Strahl, Lewis Specht, Joshua W. Stackhouse, Moses Stricker, Isaac Starkey. Henry Warren, Milton Warren, John L. Widman, Thomas Wilkinson, William Wingrove, George W. Wright ; John Wright, promoted to corporal, June 15, 1864; Thomas Yocum, Benjamin Zercher.


COMPANY D.


Jacob Cramblet, captain.

David S. Coultrape, first lieutenant.

Benj. G. Hamilton, second lieutenant.

Elias W. Davis, sergeant.

W. H. H. Price, sergeant.

Citizen J. Kennedy, sergeant.

Robert N, Simonton, sergeant.

Daniel Smith, sergeant.

W. P. White, corporal.

David W. Adams, corporal.

Robert W. Erwin, corporal.

Edward Caves, corporal.

James Scott, corporal.

Andrew J. Wagstaff, corporal.

Joseph H. Law, corporal.

Robert C. Guthrie, corporal.

James Bliss, musician.

Wm. D. Lukens, musician.

Samuel Weaver, wagoner.


PRIVATES.—Christopher Arkle, James Adams, James H. Bendure, John Barr, Gabriel J. Crabtree, Alfred H. Clark, Wm. Copeland, John W. Copeland, Enoch C. Copeland, John Copeland, Thomas Cox, Mathew S. Cole, John N. Crowl, Wm. R. Crim. Joel Cramblet, Joseph Copeland, James P. Erwin James Eslick, John B. Evans, John E. Fowler, John Gladman, Samuel F. Gallagher, Isaiah Hoagland, J. C.. Hurless, J. H. Y. Histon, James F. :Rouse, Watson Hammel, George W. Hammond, IL W. Hest, Thomas Hillyer, Win. Hillyer, Henry Hillyer, John D. Horn, Samuel Hitchcock, G. M. limn, Alfred P. Jones, J .R. Johnson, Win. L. Johnson, D. A. Lukens, Thomas J..Lukens, John S. Moor, James H. Merryman, Fanquiker McRea, David Mahon, Joseph D. Moore, Thomas McClintock, Lafayette Martin, John Poulson, Isaac Patterson, John A. Pitts, Wm. J. Ross, Jesse Richardson, Wm. Rowland, Wm. Reynard, Joseph Robinson, David M. Scott, John Spray, Matthew W. Simpson, John K. Stine, Samuel Straus, Jacob Underhill, Archibald Underhill, Samuel Utterback. Henry W. Wilson, John D. Woods, W. R. W hite.


COMPANY E.


Albert W. Lee, captain.

Alexander C. Patton, first lieutenant.

Mathew N. Henderson, second lieutenant.

Marcus Howell, sergeant.

Wm. A. Frater, sergeant.

John P. Harvey, sergeant.

David A. Duff, sergeant.

Landon Grimes, sergeant.

Samuel B. Ward, corporal ; promoted to sergeant May 17, 1864.

John M. Linn, corporal; captured at Martinsburg July 25, 1864,

Eli Siebert; corporal.

Abram Loper, corporal.

John E. Stewart, corporal.

Robert W. Palmer, corporal.

Robert A. Todd, corporal.

John L. Grimes, corporal ; wounded in action July 18, 1864.

Joseph Linder, corporal.

Samuel Satterthwait, musician.


PRIVATES.—Robert Barnes, Robert D. Bell, Thomas Burtoff, Thomas Boyd, Wm. S. Barnes, Francis Couron, Boyd W. Dysart, J. C. Duffie, James A. Duff, Sylvanus C. Dysart, James C. Dysart, John L. Dunbar, George Frazier, J. D. Fread, James P. Ferguson, Wm. Fresh, Thomas M. Graham, Edward J. Graham, Peter Graham, George Goudy, David Gibeny, Thomas Gilhan, Chas. T. Gilhan, Win. Grimes, George W. Hayes, Alex. C. Henry, Alexander Hammond, promoted to corporal, May 12, 1864 ; Elisha Huff, William H. Johnston, Samuel Jackson, William King, Joseph Lynn, Joseph Lyle, Charles Lee, promoted to corporal July 24, 1864; Ephraim Louis, Jesse Mitchell, David K. McCance, Geo. Maholin, Wm. McNary, left sick in hospital at Pittsburgh, Aug. 26, 1864. Isaac Miliner, Leander Milburn, Marion McCallister, Jas. Moore, died at Annapolis Junction, Md., August 8, 1864, Jas. C. McConnell, T hos. McKee, Calvin Moore, Calvin Patton, Geo. W. Porter, Geo. Patterson, Geo. W. Peregoy, Leven Powell, Claudius. Richner, James M. Rogers, captured July 24, at Winchester ; returned to company. Addison Sells, Evan Stephens, Nimrod Stevens, Samuel M. Thompson, Michael Umbenhow, captured at Winchester, July 24; escaped and returned to company ; Henry Williamson, Mordecai, David Davis.


COMPANY F.


Leonard Peck, captain.

Jas. H. Graham, first lieutenant; died in hospital, August 11, 1864,

John H. Hammond, first lieutenant.

J. H. Lewis, sergeant.

Lewis W. Furbay, sergeant.

Isaac Booth, sergeant.

Elisha Moore, sergeant.

James M. Adams, sergeant.

James W. Honerth, corporal.

Ezra Thompson, corporal.

John Hanna, corporal.

James Coulter, corporal.

John E. Dutton, corporal.

John E. Keyser, corporal.


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 211


George Holmes, corporal.

Edward Hagan, corporal,

Franklin Anderson, musician.

Israel Waterman, musician.

William Harriman, wagoner.



PRIVATES.—Owen Anderson, Geo. Atkinson, Geo. Baldwin, Abner R. Blackburn, John Butler, William Barkhurst, Henry Brown, John B. Beck, Isaac Carter, Edward Carter, Ezra L. Carrick, John Clark, John Coulter, William Custard, John Darmour, Theodore Dickerson, George Ely, Isaiah Fields, jr., Geo. Frater, Benj Griffith, Samuel Gooding, Joseph M. Hargrave, John R. Hawthorne, Joseph Harrison, John Holliday, Archibald Hammond, Francis Hawthorne, Andrew Jamison, Jos. L. Kerr, Robert Kerr, Estep Lynn, John A. Lemmon, Wm. Lawrence, Sylvanus Lamb, Win. McCombs, Horner C. Moore, Jas. Minteer, W. H. H. Mercer, died in hospital at Sandy Hook, August 24, 1864; Charles McCombs, Samuel McGrew, Wm. Poland, Jacob Peterman, Wm. Perry, Charles E. Speer, James Stone, Silas Stevens, Eli Shields, John Singer, Robert B. Stevens, Jas. Smallwood, Joseph Shepherd, .Robert Smallwood, Joseph Thompson, Michael K. Tolan, John W. Townsend, Samuel Walker, Wm. A. Wallace, Abraham Wilson, Warren Worstel, George Wilson, Sylvanus White, William A. Watkins, Robert White, Willing Dickson.


COMPANY G.


____ James, captain.

Joseph J. Mead, first lieutenant.

John Smith, second lieutenant.

Robert N. Theaker, sergeant.

Luther Etzler, sergeant.

Thomas C. Mercer, sergeant.

Wm. P. Henderson, sergeant.

Wm. Henderson, corporal.

Reuben K. Ashton, corporal.

James A. Brown, corporal.

Thomas C. Dugan, corporal.

Edward J. Updegraff, corporal.

Ellis B. Steele, corporal.

Isaiah Parlett, corporal.

Benjamin White, corporal.


PRIVATES—David Ashton, James W. Alexander, wounded in action at Winchester, July 24 ; William Allander, wounded in action at Martinsburg, July 25; Thomas C. Brown, Adoniram Barton, Mathew Blackford William Brown, William Bernhard, Wilson Cochran,Brock, H. W. Bigley, Orlando Cope, Isaac G. Cope, Cochran, A. F. Clark, Charles J. Dungan, Thomas G. Dugan, Abel Dungan, W. D. Devault, John H. Denham, William Davis, William Davidson, wounded in action at Martinsburgm July 25, Oliver Embree, David Fowler, Joseph Fryman, John B. Gill James Gardner, Alexander Henderson, John L. Henderson   Perrine Henderson, Byron Hogue, David Harriott, William Jones, Henry Jones, Albert Lawson, promoted to sergeant July 8, 1864, Theodore Lash, William if. Lash, Elisha W. Lewis, John Lemmon, Isaiah Loper, Charles H. McCall, Charles Mead, Gilbert Neelan, Jesse Nichols, Mortimore Nichols, Elisha Oxley, Charles W. Perry, Thomas H. Perry, died, Jesse Pratt, Alonzo Porterfield, William Palmer, Benjamin .Renard, Samuel Roberts, Harrison Roberts, Wesley A. Steele, William Sloan, David D. Stillwell, Nathan Smith, Thomas Seals, George Shive- ly, Wm. Tarbert, Leander Vickers, Joel Walker, James Wear, wounded in action at Winchester July 24, David Wells, Benjamin Westlake, J. L. Van Pelt.


COMPANY H.


Edwin Regal, captain.

John E. Cannon, first lieutenant.

Robert P. Hanna, second lieutenant,

George A. Crew, first sergeant.

George Lanning, sergeant.

Thomas Dawson, sergeant.

James McWatty, sergeant.

Daniel L. Parish, sergeant.

Thomas A. Jobes, corporal.

William Peregoy, corporal.

William McCullough, corporal.

Thomas H. Baldwin, corporal.

Thomas H. Culberson, corporal.

W. W. Mansfield, corporal.

John C. Dickerson, corporal.

John W. P. Gallaher, corporal.

Geo. W. Rife, musician.

Jonathan Copeland, musician.

Jonathan McGuire, wagoner.


PRIVATES.—David R. Beatty, John Beatty, Anthony Beck, David Boals, Benjamin Bogardus, John C. Brown, Samuel H. Brown, Samuel Bruner, John Calderhead, died of typhoid fever at Camp Parole, Annapolis, Md., August 3, 1864, Moses W. Cannon, John W. Cassell, John A. Chandler, Silas Clark, John P. Cramblet, Robert D. Crawford, John Crumley, Samuel H. Culbertson, Homer Day, Joshua Dickerson, William J. Dickerson, Joseph Dyson, George Fogle, John W. Fogle, Nathan Fogle, Daniel Garvin, David Gutshell, James F. Hanna, Harmon Har ris, Francis W. Hibbard, John Hill, Samuel Howell, A. R. Kennedy, J. C. Kilgore, Joseph V. Lee, Lemuel Luke, Thomas Mansfield, James Maxwell, David McCall, William McCall, Alexander McConnell, Barnet McCoy, Andrew McFarland, Robert McFarland, William McLaughlin, William McMillan, W. V. Minteer, John T. Morrow, Cyrus Paul, Joshua Polen, James Poulson, William Rowland, Noah Scott, Shannon Leslie, Jas. T. Shannon, Milton Taggart, William S. Tweed, Benjamin Van Kirk, William Welsh, James White, David J. Wiggans, George B. Williams, James Wilson, Robert Wilson, Walding Young, William A. Pittinger, .Robert A. Hammond, J. M. Lee.


COMPANY I.


Nathan H. Rowles, captain.

Elias B. Lowman, first lieutenant.

Daniel Westlake, second lieutenant.

William Rankin, sergeant.

Samuel S. Martin, sergeant.

Cyrus H. Strahl, sergeant.

John T. Wortman, sergeant.

Jas. F. Anderson, sergeant.

Nelson Moid, corporal ; captured at Martinsburg, W. Va., July 25; rejoined company Aug. 24. James K. Crozier, corporal.

Joseph H. Heatherington, corporal ; captured at Martinsburg, Va., July 25, 1864.

C. W. Hall, corporal.

Leander Greenlee, corporal.

William McFarland, corporal ; appointed sergeant Aug. 11, 1864.

John Dunfee, corporal.

James McGregor, corporal.


PRIVATES.—Lafayette Austin, Lycurgus Austin, Isaac Anderson, John C. Abel, Daniel W Archer, Frederick Bickel, John Bair, Samuel Boyd, John W. Cunningham, Robert Clark ; died at Division Hospital, Sandy Hook, Md,, July 27, 1864; Jacob Dunfee, Alfred Dean, James Davis, William Fry, Charles A. Fuller, William J. Forbes, Joshua Foster, W. H. Ferry, Patrick Gibler, W. H. Greenlee, Frederick Garlach, Edward Grubb, Melvin Groff, William Hall, John E. Heatherington, John Goldsworthy, captured at Martinsburg, W. Va., July 25, 1864; Samuel Hines, Alexander Hammond, John H. Henderson, Stephen Hipkins, Hiram M. Ingler, W. W. Jones, Isaac A. Keyser, William A. Keyser, Jesse B. Keyser, Jacob T. Keyser, Jacob P. Keyser, George King, J. H. Long Alexander Lyal, Thomas McMahon, James McMahon, Samuel McMillen, Robert McClellan, Henry Murz, Joseph C. Nelson, John Nesbit, A. R. Norman, Abraham Porter, W. S. Patterson, John W. Patterson, Harrison Richardson, Samuel Richardson, John T. Steele, Abraham Sprowl, W. A. Starkey, Jacob Turnbull, Thomas Reese, Harvey J. Tarbet, William F. Tarbet, Joshua Vessels, Joseph Vessels, George W. Westlake, Albert G. Wineman, Harrison Williams, W. C. White, Samuel Zimmerman.


COMPANY K.


Lewis Lewton, captain, mustered out as colonel of the 170th regiment O. N. G., August 15, 1864.

William H. Oglevie, first lieutenant.

George W. Healer, second lieutenant.

James Gilbert, sergeant.

James M. Paul, sergeant.

William Philips, sergeant.

W. S. Grove, sergeant.

John W. Osborn, sergeant.

Robert Wilkins, corporal, promoted to sergeant July 18, 1864.

William S. Haverfield, corporal.

M. K. Turner, corporal.

Samuel A. Osborne, corporal.

James H. Haverfield, corporal.

Morrison Moorehead, corporal.

Thomas Miller, corporal.

John Stubbins, musician.

George W. Lewton, musician,

Eli Nicholas, wagoner.


212 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


PRIVATES.—Jesse Arnold, James A. Amspoker, William B. Adams, Evan Berry, Jacob Brough, Samuel Browning, Clarkson Bower, Stewart Beebe, Joseph W. Chaney, Thompson Craig, J. M. Clark, W. A. Clark, Abel Carson, promoted to corporal July 18, 1864; Dunlap Dickerson, B, Dickerson, Albert Dewey, William H. Duffield, Abraham Eli, Samuel Finney, C. J. Ferrell, Nathan B. Haverfield, Joseph H. Haverfield, William Henderson, Henry Hagadorn, Samuel M. Hines, Christian A. Hines, John W. Hines, Geo. W. Howard, William T. Hedge, Hiram Merriman, Thomas Johnston, died of typhoid fever in hospital near Sandy Hook, Md., August 11, 1864; Joseph L. Johnston, Alexander B. Kerr, discharged on account of disability June 22, 1864; Samuel Leeper, Archibald Leeper, died of fever in Pleasant Valley Hospital, near Sandy Hook, Md., August 12, 1864; William Lee, Adison Layport, W. C. Laizure, Stephen R. Magee, John A. McAfee, Henry Mattern, James R. Marsh, John McBride, Henry McKee, Wm. Maggett, John B. Marshall, Nathan H. Mansfield, Samuel B. McConnell, John H. Nichols, discharged for disability June 18, ; James A. Penn, John A. Penn, Thos. Phillips, Griffith 'Roberts, Wm. T. Ramsey, Thos. J. Ritchey, R. M. Sheets, Thomas H. Selby, George Shivers, Samuel Shivers, Emanuel Smith, promoted to corporal July 18, 1864 ; Thomas W. Thompson, Albert Tipton, Randolph Tipton, Lafayette West, Finney Ray, promoted to corporal July 18, 1864.


MISCELLANEOUS.


The following is a list of recruits and veteran volunteers mustered into West Virginia organizations and credited to Belmont county, Ohio, since January 1, 1864:


FIRST W. VA. CAVALRY.


Jesse Chamberlain, Calvin C, Hasson, John C. Majors, John Cass, Joseph P. Burdett, Adam Coss, William Heskett, Josiah Hatcher, George W. Jeffries, Wm. D. McKirahan, James Martin, Jonathan Milburn, Curtis B. Stedd, Jacob Watson, William Gill, John Estep, Patrick Menehan, Robert Armstrong, W. H. Brown, Reuben H. Lucas, Aaron Moore, John N. Elliott.


FIRST INFANTRY.


William Humphreyville, John Barton.


FIFTH CAVALRY.


William Fowler, Stephen G. Jones, William Clark.


FIRST ARTILLERY.


Erasmus F. Baily.


Co. C,116th REGIMENT O. V. I.


This company was composed of Monroe county men, with the exception of five from Belmont county. It was mustered into service under Capt. Frederick H. Arckenoe on the 19th of September, 1862. The company was mustered out of service at :Richmond, Va., June 14, 1865. The following named gentlemen were from Belmont county :


Abel C. Barnes, wounded at Cedar Creek ; Franklin Barnes, mustered out at expiration of service; Miller Brown, three months, extra pay as a prisoner of war confined in Libby prison ; Samuel Dobbins, three months, extra pay as a prisoner of war, confined in Libby prison ; Walter Theaker was appointed cor poral June 15, 1863.


Co. H, 86TH REGIMENT O. V. I.


Abraham Porter and Campbell K. Smith, of Bellaire, Ohio, were members of this company. It was mustered into the service of the United States for six months at Camp Cleveland, O., July 14, 1863. .Mustered out February 10, 1S64.


Co. K, 78th REGIMENT O. V. I.


William E. Barnes enlisted December 11, 1861. Mustered out with company at. Louisville, Ky., July 11, 1865.


COMPANY C, 60TH REGIMENT O. V. I.


Captain B. Kyle's company was mustered into the service at Camp Chase, April 5, 1864. Belmont county contributed about twenty-five men to this company, as follows :


PROMOTIONS.


John R. Merrill, promoted to sergeant, June 1. 1865. Adam Stewart, promoted to corporal, November 5, 1864. Oliver C. Torbet, promoted to corporal, February 1, 1865.


PRIVATES,—Oliver C. Jones, John T. Skinner, James W. Skinner, George A. Shry, Joseph G. Snade, Allen B. Thomas.


DISCHARGED ON DISABILITY.


Jeremiah Horton, July 4, 1865. James A. Barnes, May 12, 1865. Joshua Fred, April 27, 1865. Wm. W. Clark, January 13, 1865. IN . C. Manning, Philip S. Williams, June 21, 1865,


DIED.


Jesse E. Berry, killed in action at Petersburg, Va., June 17. 1864. Joseph Mayhugh, killed on duty near Petersburg, Va., June 28, 1864. John D. Bryan, killed in action at Nye River, Va,, May 12, 1864. Charles W. Carter, died in Camp Chase of disease, April 10, 1864. John M. Johnson, died at Baltimore, Md., October 8, 1864, of disease. Wm. W. Kyser, died July 22, 1864, of wounds received while in action. Tillman Nichols, died of wounds received in action at Cold Harbor, Va., July 2, 1864. Milton H. Shry, died October 6, 1864. John S. Summers, died September 2, 1864. Thomas Stephenson, killed in action, Oct. 27, 1864, at Matcher,s Run, Va.


Company mustered out at Delaney House, D. C., July 28, 1865.


COMPANY D, 60TH REGIMENT O. V. I.


This company was composed of men from different counties in the state. Those from belmont county are indicated below. The company was organized by Captain W. W. Robbins and went into Camp Chase, April 6, 1864. It was mustered out at Delaney House, D. C., July 28, 1865.


PROMOTIONS.


Joseph E. Lewis, sergeant. Wm. J. Parsons, sergeant, DeL. Eckels Marquis, promoted to sergeant, May 1, 1865. Corporals —Samuel W. Gordon, Hemy S. Barnes, Ellis Brill.


PRIVATES.—John Alwood, Owen Delong, Wm. S. Dyer, John H. Ellis, George W, Gebhart, Calvin N. Malone, Anthony B. Shimp, Cornelius Stidd, Israel A. Thompson, George H. Tillman.


DISCHARGED.


John W. Hays, April 17, 1865. Wm. H. Barnes, February 9, 1865. Evan Dickison, May 19, 1865. G. W. Hance, Juno 72 1865. Wm. M. Nace, January 17, 1865.


DIED.


James A. Vance, died December 30, 1864, in Salisbury, N. C., in rebel prison, while a prisoner, of war. James Barnes, died May 10, 1864, in ambulance, caused by a gun shot wound in hip; received May 9, 1864, at Nye River. by W. Crew, died October 10, 1864, in Alexandria, Va., of chronic diarrhoea. Samuel Griffith, May 12, 1864, killed at Spottsylvania, Va.; shot through head in a charge against the enemy. John H. Moore, died August 28, 1864, in A ndersonville, Ga., of dysentery, while a prisoner of war. Charles 0. Morrow, died December 26, 1864, in Salisbury, N. C., prison. Dewitt Steel, May 9, 1864, in Fredericksburg, Va., of measles.


CONCLUDING REMARKS.


The historian, in making out the above record of Belmont county, has endeavored to give as complete a list of the volunteer soldiers who enlisted from said county, as was possible for him to do. It may be that there yet remains some names which are omitted, of persons who enlisted from this county at remote points in this and other states, and which were not disclosed to the author. There were four companies of "Departmentals," from the county, the rosters of which were not on file in Columbus. An effort to get them from Washington City was unsuccessful.


Belmont county has borne a conspicuous part in the suppression of the rebellion. Many of its noble patriots fell in defending the Union. It early responded to the President’s call for three months, men, and sent three companies into the field—most of whom subsequently re-enlisted. Over two thousand served in the three years' sevice, many of whom became veter-


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 213


ans. The 170th regiment of hundred day men were all from this county, and like those who preceded them, did good service and acquitted themselves like men.


But, alas! many who left the county as brave soldiers, full of hope and patriotic zeal, never returned again. Some may ask where are they ? Ah! their lives have gone out on the memorable battle fields of Shiloh, Corinth, Stone River, Chickamauga, Mission Ridge, Kenesaw Mountain, Atlanta, Nashville, Cheat Mountain, Chancellorsville, Gettysburg, McDowell, Greenbrier, Second Bull Run, Little Rock, Jonesboro, Wilderness, Monocacy, Spottsylvania, Cold Harbor, and many others.


Belmont also contributed to the long list of starved soldiers of the horrible prisons of Andersonville and Libby.


Its war record is a good one, and is well worthy the space it occupies in this history.


CHAPTER XX.


GEOLOGICAL SKETCH OF BELMONT COUNTY


BY T. W. EMERSON.


GENERAL PRINCIPLES.


It is thought proper to introduce this geological sketch of Belmont county by a brief outline of such of the general principles of geology as will enable those who have given little or no attention to the subject to read the sketch with interest and profit. Only such of these principles will be introduced as are necessary to a full understanding of the subject, and those in as brief a manner as is consistent with clearness, the use of scientific terms being avoided so far as it is possible to do so without sacrificing scientific accuracy. Yet, as the work is intended to be useful rather than merely readable, the use of technical terms will, of necessity, be resorted to, especially in the general articles on sandstone, limestone, and coal.


Geology is sometimes poetically called "the story of the rocks. It might be more logically defined to be the history of the earth as determined by the rocks. Imperfect, as all human sciences must necessarily be, it can not properly be called a complete history of the earth ; but, so far as it goes, it is a clear translation from the rocky records of at least an outline of the world's history : a chronicle of the perpetual changes and succession of great events which have wrought out of the gray vague of chaos the varied and beautiful world of to-day. It is a. history, without dates; written, not in the mutable language of human speech; not in the perishable and infinitely varied characters which represent human thought ; but in the plain picture-language of Nature—a language without idiom or inflection, perfect, simple, and universal ; the same in Europe, India, and the islands of the sea. True, geology, like other sciences, has become more or less involved in technicalities ; but that arises from the imperfection of human language; from the inability of the translators of Nature,s book to express in their own dialect that which is plain and simple in the original. The literal translation sacrifices half its beauty for accuracy; the free translation loses its accuracy in attempting to reproduce the beauty. There is but one way to preserve both : that is to read the simple record from the original. "To him who, in the love of Nature, holds communion with her visible forms," there need be—there can be—no difficulty in understanding the "various language" which she speaks.


KINDS OF ROCKS.


The geologist is accustomed to regard the earth,s crust as consisting of masses and layers of rocks miles in thickness, covered generally with a thin robe of soil at most a few inches deep. It is his business to divest each locality of its thin garment of soil, and to study the solid structure beneath. This he cannot do literally but by studying the exposures of solid rock here and there, and comparing and collating the various results. he can arrive at length at a very satisfactory knowledge of the whole structure. The nature and method of formation of each kind of rock being known, we have only to determine the kinds of rock of a certain locality, and the order in which they occur, and we are then enabled to reproduce the entire geological history of the locality.


It is hardly necessary to state that there is no great variety-in the kinds of rocks of Belmont county. To treat of the numerous kinds of minerals that may be found among the pebbles and river stones of the Ohio river basin, or of other similar deposits, would be foreign to our subject. The framework of our hills consists mostly of deposits of sand stone, lime stone, and clay in their various forms, interlaid with seams of coal. Of these four minerals, therefore, it is necessary to treat somewhat in detail. The names and character of other minerals will be introduced only so far as they are connected with these.


SANDSTONE AND CLAY.


In our every day experience we are accustomed to think of sand as pulverized sandstone, but it would be more strictly correct to regard sandstone as consolidated sand. The sand we see along our roads has of course been worn off from the stones of the road-bed by travel and weather, and washed into beds by rains. A bed of sand thus collected, mixed with quantities of iron in small particles, would, if undisturbed, solidify in the course of years. The iron would rust, and the oxide thus formed would cement the sand into solid rock. The sands at the bottom of the sea are often found hardened into stone, where lost anchors, cannons and other articles of iron have lain for several years. The same result is sometimes produced where springs containing some of the forms of lime in solution flow among sand-beds; the calcareous matter acting as a cement to the loose grains of sand. There is considerable proportion of iron in the sandstones of our higher formation. The yellow color of the higher soils and clays is due mostly to the yellow oxide of iron, or rust. The red color of bricks is due to another oxide of iron, formed by the union of the oxygen of the air with the iron which the clay contained. It is not uncommon in this county to find sandstones containing blue iron ore ; but most of the iron at the surface of the ground, when the air and moisture can reach it, is in the form of yellow oxide.


Sandstone, then, being composed of grains of sand cemented together by forms of iron or lime, it is worth while to inquire further into the nature of sand itself. Pure sand is rarely, if ever found in the interior. It may be seen along the seashore and on the shores of lakes, where it is washed clear of the mud and clayey particles, which form so large a part of our interior sands. Pure sand is perfectly white. It is called silica, and substances containing it are said to be silicious. Silica, or pure sand, consists of little irregular shaped particles of a mineral, called quartz. Quartz exists in a great variety of forms ; but all the different kinds may be grouped into two classes, the crystallized and uncrystallized. The uncrystallized forms are flint, jasper, chalcedony, hornstone and sandstone. In its crystallized, form it takes various names according to its color. The crystals are regular six-sided prisms, as shown in Fig. 1.* When it is free from coloring matter it is transparent as the most perfect glass ; in which case it is called pellucid, or limpid quartz. Some of the pellucid quartz found near Hot Springs, Arkansas, are so pure and hard, that they are called "Rocky Mountain-diamonds." The amethysts used for sets in jewelry are violet-colored quartz-crystals ; and the agates so common in jewelry stores, are half-pellucid quartz, with dark bands, or with figures of the appearance of moss. Opal is another form of quartz, usually containing a little water in composition. Quartz is one of the hardest of all minerals ; it is so hard that it cannot be scratched by the hardest steel point. It does not melt in the hottest fire ; it will not dissolve in water ; and neither aqua fortis, muriatic, or sulphuric acid, produce any effect upon it. Yet stubborn and unrelenting as this mineral is, it may easily be dissolved by pulverizing it into sand and heating it with potash, lime, (quicklime), or soda (not the substance commonly called soda, but that chemically so called). It is by this process of heating quartz, in the form of sand, with potash, lime or soda, that glass is made.


So we see that our common, coarse, and too often unvalued sandstone comes of a good family, and has many eminently respectable relations. It would be an easy matter to show him near of kin to the great family of granites, and to many other families less useful but more highly appreciated than himself; but want of space forbids.


There are usually other elements besides quartz and and iron in sandstone. The most conspicuous of these is mica. The little, glittering scales which school-boys call "isinglass," are mica scales


* See illustrations Geological Essay.


214 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


Like the quartz, with which it is associated, it has been broken up into very small fragments, and pretty thoroughly mixed up with the general mass. In its native state, mica consists of large thin plates or Scales, sometimes as much as a yard in diameter. Specimens of native mica may often be seen used as windows in the doors of parlor stoves. Still another substance called alumina is usually present in sandstone, of which it is proper to speak here, since it is the principal ingredient of clay —a .substance pretty generally known in Belmont 'county. Alumina in its pure form is the hardest of all minerals, except the diamond. The only pure form are the ruby and the sapphire, both of which are well known gems of great value. The garnet consists of alumina and silica colored with oxide of iron. Emery is composed mostly of alumina. Alum is another well known mineral having alumina for its base—whence the name. When sulphur exists in connection with alumina, it sometimes, by a curious chemical process, absorbs oxygen from the air, and is thereby changed into sulphuric acid; this unites with the alumina, and thus forms basic alum, which is chemically called sulphate of alumina. These facts may help to explain the presence of alum in connection with some of our Belmont county sandstones : notably, the well-known "Alum Rocks" of Wayne township. Alumina is composed of oxygen united with a brilliant white metal, called aluminum, which possesses more than twice the strength of iron.


Thus we .see that clay, being a silicate of alumina, also conies of good stock, being respectably. connected on both sides.


When sands containing clay consolidate into sandstones, they make what are called flagstones. A great deal of the sandstones of the higher formation of Belmont county are of this nature. Some of these make very beautiful paving stones. Those guarried near Badgersburg, in Goshen township, can scarcely be excelled for that. purpose.


LIMESTONE.


Limestone, marble and chalk are but different forms of the same substance. Limestone is chalk broken up and redeposited by the action of water, and hardened by pressure, heat, or other agencies. Marble is limestone with a crystalline structure produced by the action of heat. When we speak of limestone in its broadest sense, therefore, we include all grades of calcareous rocks, from the hardest marble of the bills of Carrara to the soft chalk we use on our black-boards in school. Only the intermediate form, or limestone proper, is found in this county; and it is in reference to this form alone that the word will be used ; but it may be necessary to speak of the other forms, chalk and marble, in order to explain the true nature of limestone.


Limestone is often found crystallized ; that is, turned to beautiful glassy crystals having a cleavage in three directions, at snch angles that the substance always splits into rhomboidal blocks, of the shape of Fig. 2. These crystals, called in general talc spar, have various specific names according to their character. If the limestone contains certain impurities the crystals are of a muddy color, and are called simply rhomb spar, in allusion to their shape ; but this name would apply equally well to any other variety of caic spar. if it is pure, the crystals are as clear and transparent as the most perfect glass, and are known as Iceland spar. In this county, however, the limestones are generally uncrystallized. Occasionally one may be seen which, when broken, shows small " blossoms," and not unfrequently we find beautiful specimens of calc spar in. iron concretions. But no large masses of glistening spar are found, such as may be found in eastern Indiana or northern Kentucky, for example. Our limestones consist of beds of gray, blue, or yellow calcareous rock, usually arranged in layers of hard stone alternating with softer deposits of the same substance; that is the appearance, at least, presented by the outcrops of the Limestone Series along our larger creeks. But the soft, earthy deposits which separate the harder layers are produced by the weathering of stone containing a larger proportion of carbonate or sulphate of magnesia. This variety is consequently called magnesian limestone by chemists. The yellow variety, of which there are two 'conspicuous beds in this county, owes its peculiar color to the yellow oxide of iron. Those varieties with little or no magnesium or silica make excellent quick lime, and are valuable as a. flux or slag in iron smelting. The higher beds of our region are used very extensively for both these purposes.


Origin of Limestone.—It is by the study of chalk that we are enabled to go back farthest in the history of limestone. A piece of chalk examined under a microscope will be found to be composed of the shells of minute: sea-animals, called foraminifers. The remarkable little creatures which form these shells are described as "animals that have no organs of sense, and, in gen- eral, not even a mouth to eat with. When a particle of the desired food touches the body, and is perhaps held there by its power of stinging, that part of the body begins to be depressed, and continues to sink inward until the food is in a cavity inside made for the occasion ; then the food is digested, and any part of it not digested is thrown out by restoring the body to its former state."—(Dana.) Some of the shells of these animals are represented in Fig. 3, (from Encyclopædia Britannica, Vol. IX,) all highly magnified. They are so small that they make a fine-grained rock. An ordinary chalk-mark destroys hundreds, perhaps thousands, of these little shells. One variety called the globigerina is by. far the most common and best known. The scientific expedition sent out a few years ago by the British Government, in Her Majesty,s ship Challenger, to study the minute life in and at the bottom of the sea, made some very interesting discoveries concerning the globigerina. The observations made on the sea-bottom by this expedition, together with those made by the Coast Survey of our own country, and others, enable us to say positively that limestone formation is going on to-day at the bottom of the sea by the deposition of globigerina shells. Not only that, but we have now positive information as to the life and habits of these animals, They live in the sea at all depths, but chiefly at the surface. "They are more abundant and of a larger size in warmer seas."—(Prof. Wyville Thompson’s Report to the Royal Society.) The shells of the living animals are clear and transparent, differing from the dead shells found at the sea-bottom, much as a living snail-shell differs from a dead one. Within a zone extending fifty or sixty degrees on each side of the equator, the E eas at present swarm with these little creatures ; and at the bottom is forming a bed of soft calcareous mud, usually spoken of as globigerinoe ooze, which serves as a clue by which we may trace out the whole history of limestone. This history may be briefly told: Chalk is formed at the bottom of the sea, of the dead shells of globigerinoe and other foraminifers ; limestone is formed by a breaking up and redepositing of chalk, together with other shells, corals, and crinoids. Says Prof, Huxley : "A hundred years ago the singular insight of Linnaeus enabled him to say that 'fossils are not the children but the parents of rocks,, and the whole effect of the discoveries made since his time has been to compile a larger and larger commentary upon this text. It is, at present, a perfectly tenable hypothesis that all silicious and calcareous rocks are either directly, or indirectly, derived from material which has, at one time or other, formed part of the organized framework of living organisms. Whether the same generalization may be extended to aluminous rocks, depends upon the conclusions to be drawn from the facts respecting the red clay areas brought to light by the Challenger. If we accept the view taken by Mr. Wyville Thompson and his colleagues—that the red clay is the residuum left after the calcareous matter of the Globigerinae ooze has been dissolved away—then clay is as much a product of life as limestone, and all known derivations of clay may have formed part of animal bodies."—[Popular Science Monthly, May, 1875.


This is indeed a broad generalization ; but it is warranted by. ample evidence, Which it is not within the province of a sketch like this to consider; It is enough that our Belmont, county limestones contain sufficient evidence, both in their arrangement and in the fossils they contain, of their having been deposited in uniform layers as. sediment at the bottom of the sea, or other vast body of water. Hundreds of minute marine shells of the family of gasteropoda may be seen, even with the naked eye, in the limestone quarried on the farm of Mr. Porterfield, north of St. Clairsville, and used for macadamizing. Many larger species, both of gasteropods and brachiopods, are found in our limestones; to say nothing of the still more minute species which the microscope may reasonably be expected to reveal,


As to the silicious rocks, including sand, there is unquestionable evidence, that materials for such rocks are accumulating at the bottom of the polar seas of to-day, and these materials are the remains of plants and animals. There is reason, also, both in fact and by analogy, to believe that our clay material is of smiliar origin ; but while the organic origin of sandstone and limestone is considered by geologists to be. established, the origin of clay from organic remains, is not satisfactorily proved.


Limestone Chemically Considered—It is well known that if a piece of pure limestone be subjected to great heat, in other words, burnt, it will become a substance of entirely different nature, quicklime. Whence this change? What has really happened to so change the nature of the substance.? The mpg() is


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 216


limply this : The limestone has been decomposed into two separate elements, one of which, an invisible gas, has been driven off by the heat to mingle with the atmosphere, while the other, I solid quicklime, remains. These two elements are so important in geology that it is necessary to speak of each somewhat ,n detail. Carbonic dioxide is the name by which the invisible /as which is driven off from burning lime is now known. It is be well-known gas formerly called by chemists, carbonic acid. it is composed of two equivalents of oxygen combined with one )f carbon. In its natural state it is a colorless gas, about one Ind a half times the weight of air, Being thus heavier than the ttmosphere, it does not rise like the lighter gases, but seeks the lower levels; and consequently it may be handled by the expert chemist in much the same manner as water. Though perfectly invisible, it may be dipped or poured from one vessel to another, may be bottled up, and may be experimented with in various ways which would be impossible in the case of the lighter gases. If a living animal, as a mouse, be placed in a vessel of pure carbonic dioxide, it will quickly become insensible and die. In the same way men often lose their lives by descending into wells or caves where this gas, which they call dead air or damp, has collected. It is produced in large quantities by the burning of wood and coal, and by the decaying of animal and vegetable matter everywhere ; consequently there is a greater or less amount of it in the atmosphere at all times. It is usually obtained for experiments by the action of sulphuric or nitric acid, or even strong vinegar; upon powdered limestone, marble, chalk, or animal shells. It is obtained in this manner in large quantities for the purpose of charging the beverage misnamed "soda-water."


Although it is a gas under ordinary circumstances, carbonic dioxide may, like most other gases, be reduced to a liquid, and even to a solid. An English chemist, Prof. Faraday, found that this gas under powerful pressure sinks into a clear, limpid liquid. Thilorier, a French chemist, repeated Faraday,s experiments, and found that the condensed gas, subjected to a pressure of six hundred pounds to the square inch, turns to beautiful snowy crystals. It has since been reduced to a clear crystaline solid lice ice, by freezing the temperature required being something like one hundred degrees below zero.


The other element of limestone, quicklime, is so well known that it needs little description. It is composed of the common gas oxygen united with a metal called calcium. This metal is never found native. It is so rare in its pure state that few people ever have an opportunity of seeing a specimen. Its affinity for oxygen en s so strong that it has to be kept in a carbon oil to protect it from the air and moisture. It is so difficult to obtain, and so hard to keep when obtained, as to render it quite expensive. In appearance it is a beautiful silvery metal, so soft that it can easily be cut with a knife. When freshly cut it has a bright silvery lustre, like a piece of lead ore, or the face of a piece of freshly cut lead ; but its lustre begins to tarnish as soon as it is exposed to the atmosphere. The only natural and permanent form in which this metal exists is in composition with other elements : goneraly united with oxygen and carbonic dioxide in the form of limestone, or with oxygen and phosphoric acid in the form of phosphate of lime, the substance of which the bones of animals are chiefly composed. Thus it will be seen that lime plays an important part in the animal world : its carbonate forming the solid parts (shells) of the lower order of animals, and its phosphate forming the solid parts (skeletons) of the higher orders.


How The Lower Orders of Animals Form Their Shells.—To make the history of limestone complete, it will be necessary to show the manner in which the lower animals form their shells of carbonate of lime. Limestone (carbonate of lime) cannot be dissolved in water ; but when it takes on another part of carbonic dioxide it becomes the bicarbonate of lime, a substance which cold water easily dissolves. Water containing bicarbonate of lime in solution is called "hard water"—an element too well known, even in our sandstone regions, to require any description. When hard water is heated, one equivalent of carbonic dioxide is driven off, leaving the insoluble carbonate of lime, which settles to the bottom of the vessel. As most waters in their natural state contain more or less carbonic dioxide the waters of those regions where there are nothing but limestone formations, are usually hard. In many regions there is no other kind than hard water—springs, wells, creeks, rivers, all heavily charged with bicarbonate of lime. Naturally, the tendency of all calcareous matter is to exist in the form of limestone, or of bicarbonate of lime dissolved in water. From this dissolved bicarbonate the soft-bodied sea-animals form their shells, by taking it into the system and eliminating or throwing off the superfluous part of carbonic dioxide.


Now, supposing water and carbonic dioxide to have been sufficiently plentiful, there might have been a time, before the seas were "gathered together into one place," when almost all calcareous substances existed in the form of bicarbonate of lime in solution. Such a period, we have a right to believe, would have been a good time for sea-animals having shells. That there was a time when such animals did exist, and that the seas of that period swarmed with animal life just such as we would expect, a glance at some of the older rocks of our globe is sufficient to convince any unprejudiced mind. Some of the older rock-formations are literally made up of such shells. The rocks which form the hills around Cincinnati are splendid illustrations of this point.


Cement Limestone.—The subject of cement, or hydraulic limestone demands some attention here, since there are important beds of this substance in Belmont county. Some have insisted that it is carbonate of magnesia which gives to cement its peculiar properties ; while others have claimed the honor variously for oxide of iron, oxide of manganese and soda. The absurdity of some of these views is obvious from the fact that the best cement rocks of Belmont county contain neither soda nor oxide of manganese, and only slight traces of iron. (See table of analysis below). The earlier opinions upon the subject were mostly drawn from an analysis of the cement rock of the Island of Sheppey, England, from which cement was first made for the English market, by a Mr. Parker, who patented it under the name of " Roman Cement." A table of the analysis of this rock is given below, together with an analysis of the famous cement rock of Kingston, N. Y., and analyses of some of those of Belmont county. In each case 100 parts are supposed to be taken, so that the figures represent percentages of the whole amount. No, 1 is an analysis, made by Dr. E. S. Wayne, of Cincinnati, of rock from the cement works of Messrs. T. C. Parker & Son., near Barnesville. No. 2 is from the lowest stratum of cement rock at Bellaire, analyzed by Prof. Wormley, chemist of the Ohio Geological Survey.


ANALYSES OF CEMENT ROCKS.



 

Eng’h

N.Y’k

Belmont County

Carbonate of lime

Carbonate of Magnesia

Oxide of iron

Oxide of Manganese

Silica

Alumina

Water, loss, &c

69.00

.20

3.70

1.20

18.00

6.60

1.30

100.00

59.70

12.35

2.35


15.37

9.13

1.10

100.00

72.10

11.15

3.10


8.47

 4.85

.33

100.00

42.70

25. 50

19..10

11.60

.70

100.0()




From this table it is evident that the adhesive property Of cement is due to the presence of either magnesia, silica, or alumina. The best opinion seems to be that it is due to silicate of alumina (clay), and it is stated "as a general rule" that "limestone must contain from 25 to 35 per cent. of clay, in order to yield a good, quick-setting cement, though 10 to 12 per cent. will suffice to give it hydraulic properties." (New American Encyclopaedia, Art. " Cement.")


COAL.


Few facts of science are better established than that coal is derived from vegetation. "The vegetable origin of coal," says Prof. Dana, "is beyond all reasonable doubt." When we think of the nature of coal, of the mere probabilities of such a method of formation, and of the improbabilities of any other method, we are led to strongly suspect that coal must have originated from some organic source ; and we would undoubtedly accept this as conclusive, provided we could conceive of such conditions ever having existed as would admit of our broad, continuous coal-beds being so formed, and reconcile this conclusion with the fact of their various depths, covered as they are with thick beds of solid rock. But when we find wood and coal, of nearly the same composition, in all stages of the change; when we find trees turned to coal, having preserved their original shapes and markings ; and, above all, when we find leaves imbedded in the coal-bearing rocks, showing their veins, and fruits showing their attachments, we are forced to conclude that Nature has not left


216 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


herself without a record. But when we find all the surrounding facts pointing to the former existence of conditions favorable to such formation, what at first seemed impossible appears not only probable, hut clear, positive, and conclusive.


To trace, then, the history of coal ; to show its nature as allied to that of wood ; to show the process by which it is derived from vegetation ; to determine the kinds of trees and plants from which our coals have been derived, and how they grew—these subjects, with other matters closely related to them, will occupy this division of our sketch.


Nature of Coal as allied to Wood.—It is only through the aid of chemistry that the true character of any substance can be accurately determined. We may know the properties of any form of matter from a mere acquaintance with it in mass, but the question, What is it ? only chemistry can answer. That science penetrates to the inner character of the minutest particle of matter, tracking the secret of Nature back to its last recess, and unlooses the silver cord of affinities by which she binds her few simple elements into the infinite variety of strength and beauty around us. Through chemistry science unravels the finest texture of Dame Nature,s weaving, as well as the coarsest; untwists the warp and woof, and reveals the simple plan and plain materials with which that cunning artist builds the giant mountain or shapes the petal of a flower. Through chemistry we learn that out of sixty-five simple elements is formed all this endless variety : the pebble, the plant and the planet ; the simple life-cell and the complex organism ; the enduring mountain and the vanishing summer-cloud. Through chemistry we learn, also, the nature of each of these elements : how, like human beings, they manifest their affinities and change their conduct with their company. Some of these principles may be gleaned from what has already been said of oxygen, carbon, and others of these simple elements, in the articles on sandstone and limestone. Of all these the most important is the gas oxygen. It is the most abundant element in nature. "It is of universal distribution through our atmosphere, forming one-fifth part of the air we breathe. The total quantity contained in the atmosphere has been computed to be about 1,178,158,000,000,000 tons, which, if forming a separate layer of uniform density upon the earth’s surface, would be one mile deep. It constitutes eight-ninths of water by weight, besides being a constituent of nearly all the rocks of the globe ; and entering largely into the organized structure of plants and animals.--(Youmans.) Carbon, a solid element, is perhaps the next most important in this discussion. The well known compound of carbon and oxygen, carbonic dioxide, has been spoken of at sufficient length. Hydrogen, a gas at ordinary temperatures, is principally known as one of the elements of water, of which it constitutes about one ninth by weight. Iron and sulphur are sufficiently well known. If other elements are required to be mentioned in the discussion of coal, the connection will sufficiently indicate their nature.


Dry wood is composed of carbon, oxygen and hydrogen. Lignite, a substance which occupies an intermediate position between wood and coal, having many of the properties of each, and the appearance of woody fiber in its transition into coal, is also composed of the same elements, but having a larger proportion of carbon. Coal itself consists of the same three elements, with the proportion of carbon still increased. The following table (Encyclopaedia Britannica, Vol. VII, p. 4) shows the constitution of these substances—the amount of oxygen and hydrogen in each to the 100 parts of carbon, no account being taken of the ash.




 

Carbon

Oxygen

Hydrogen

Wood

Lignite

Coal (English)

Coal (American Anthracite)

100

100

100

100

83.07

42.42

21.23

1.74

12.13

8.37

6.12

4.73




It will be noticed from this table, that a little more than half of wood is carbon, the proportion being 100 parts of carbon to 95.25 of both the other elements ; and that the proportion of carbon increases—or, rather, the proportion of oxygen and hydrogen diminishes—till in anthracite we find 100 parts of carbon to 6.49 parts of the other two elements ; that is to say, in anthracite coal there are more than fifteen times as much carbon as of the other elements combined. It is clear, therefore, that the chemical change of wood to lignite, and thence to coal, consists in the loss of oxygen and hydrogen, leaving a larger proportion of carbon in each new substance than in the one from which it is derived. Let us see if we can account for this change.


If a piece of wood be burned in the open air, the oxygen and hydrogen, united in the form of water, are driven off as vapor; and the solid element, carbon, unites with the oxygen of the air to form the gas carbonic dioxide. If the wood be left to decay, which is nothing more than a process of slow burning, the same changes will occur. But if the wood be burned in a retort, or in any other method which will prevent the air from reaching it. there will be an entirely different result : the oxygen and hydrogen of the wood will unite, as before, to form vapor of water ; but, as the air is excluded, there is no oxygen to unite with the carbon, and that substance is left pure in the form of light, porous charcoal. Suppose, then, the slow burning or decomposition of a large mass of wood to take place under water, so that the air would be excluded : most of the oxygen and hydrogen would be driven off, leaving a black-looking mass, mostly carbon, chemically the same as coal. Suppose, next, this mass to become covered over by hundreds of feet thickness of rock-material, and to lay for centuries under the enormous pressure : the vegetable traces would be pressed out, and the mass would shrink into a compact bed of carbonaceous mineral—in other words, coal. It is probable, however that the chemical changes here assumed are not quite those which actually take place in coal-making. The wood certainly loses most of its gaseous elements: but the mass being covered and permeated with water, it is hardly likely that those elements also turn to water. The substances which are formed are carburetted hydrogen, a gas, and bitumen, or "mineral tar." This bitumen is composed of carbon, oxygen and hydrogen, in the proportion of 20 of the first to 6 of the second and 16 of the last. It is the tarry-looking substance we often see distilling out at the cracks of burning coals. No one can fail to have noticed the escaping of the gas which forms within this bitumen. This is the carburetted hydrogen spoken of above. It is composed, as its name implies, of carbon and hydrogen. That this gas is one of the products of coal-making seems probable from the fact that vast reservoirs of it are sometimes found in the earth. The village of Fredonia, N. Y., is lighted by light carburetted hydrogen gas which comes from one of these underground reservoirs. They are often struck in boring oil wells and salt wells, and the gas frequently rises in such quantities that it is used for driving the pumping-engines.


Impurities.—So far, we have spoken of wood and coal as pure. In fact neither is ever free from other substances than those spoken of, as is shown by the ash left after burning. The ash of wood consists of silica and potash. The potash dissolves in the process of coal-making, but the silica appears in the ash of coal. If there are no other impurities than this, the ash of coal is fine and white; but there are almost always more or less slate and iron pyrites. Most coal beds have thin slate partings between the layers of coal. The slate composing these partings, consisting of silica and alumina, colored by bitumen, are usually broken up and mingled with the coal, and consequently appear in the ash, whitened by the burning out of the bitumen. But the most troublesome of the impurities in coal is iron pyrites. This is the hard 'substance which strikes fire from the miners, picks and emits a sulphury smell. When heated it sometimes bursts with a loud noise, and pieces fly in all directions, Its color, copperish to golden, has given it, in some localities, the absurd name of " copperas;" in other localities it is less absurdly called " fool,s gold." Chemically it is called sulphuret of iron, to indicate that it is composed of sulphur and iron. We have seen that most geological formations contain iron. When we consider with this the fact that traces of sulphur occur in all vegetable matter, the presence of iron pyrites in coal is easily explained. When coal containing pyrites is burned the surplus is driven off, leaving the iron in the form of "cinders" or "clinkers."


KINDS OF PLANTS WHICH HAVE ENTERED INTO THE FORMATION OF COAL.


Enough is known of the vegetation from which our coal-beds have been formed to enable us to say that they consisted of both land and fresh water species. The highest order of plants in the coal flora were cone-bearing trees allied to the pine tribe of the present day. Strictly speaking, these belong to the division of flowering plants. Of the flowerless plants there were three classes, Lycopods, Equiseta, and Ferns.


Lycopods.—Of the Lycopods, or ground-pine family, the most important form is called the Lepidodendron, from two Greek words, meaning "scale-tree," because the trunks of these trees are found with the bark, turned to coal, arranged in scales. Each scale represents the attachment of a leaf showing that the leaves were attached directly to the trunk. These trees sometimes ran up to the height of eighty feet, or more, and bristled with long slender leaves, like those of the pine or spruce, except


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 217


that they were often more than a foot long. Fig. 4 represents the extremity of a branch of Lepidodendron. These trees are known only through the remains found in coal-bearing rocks. Fig, 5, taken from Prof. Lesquereux,s new Coal Flora Atlas (plate LXIII) represents a new species named and described by the author of that important contribution to Bcier, ce. It is called Lepidodendron, scutatum,* from its shield-shaped scales, the latter, or specific name, being a Latin word signifying "armed with a shield." Specimens of Lepidodendron have been found in the rocks of Belmont county ; but none so well preserved as that given.


Another curious tribe of the Lycopods is called Sigillaria, from a Latin word meaning "seal," on account of the leaf-scars on the trunk, which resemble impressions made by a seal. Like the Lepidodendrons, these trees are known only through their fossil remains found in the coal-bearing strata. They grew up as single trunks without leaves or branches, to the height of thirty or forty, and often as much as sixty feet. In Fig. 17 the tree in the centre, with a tuft of leaves at the top, represents a Sigillaria. Fig. .6 is from a specimen found in Wheeling township, of this county, in a slate formation lying just below the Pittsburgh coal. This species is quite common, both in this country and in the Old World. It was first described by the great French naturalist, Brongniart, in the early part of the present century, The specimen represented by Fig. 6 shows portions of the bark, turned to coal, still adhering to the trunk.


Another common form of coal-plant is the Stigmaria, a specimen of which is represented in Fig. 7, taken from Lesquereux’s Coal Flora Atlas, (Plate LXXIV). The name Stigmaria is from the Latin stigma, a dot, and was given to these plants on account of the dotted appearance of the stems. These may have been, as some regard them, the roots of Sigillariae ; but Prof. Lesquereux, who is our best authority on the subject of coal-plants, maintains that they are sometimes stems, and not roots.


Equiseta— The most common form of the Equiseta, or "horsetail" family, is the tribe known as Calamites (Greek Kalamos, a reed). "The stems were fluted, hollow, and jointed, with leaves in whorls, growing from the joints."—(Andrews.) They often grow to the height of twenty feet, and were sometimes as much as a foot in diameter. Calamites are found in great numbers in some of the shales over our coals, and the impressions of the stems are sometimes preserved in sandstones of fine texture. Some well defined stems of these plants have been found by Mr. Oliver Dowdell, of Goshen township, in a sandstone formation lying fifteen or twenty feet above the Badgersburg flagstone horizon. Fig. 8 represents a specimen of calamite; and Figs 9 and 14 represent other equiseta formed in the rocks of Belmont county. The specimen represented in Fig. 9, with fruit attached, taken from Lesquereux's Goal Flora Atlas, was found in Wheeling township, in the slate formation before mentioned. Fig. 10 (Lesqx., C. F. Atlas, Plate III.) is from a specimen found in Colerain township in the same formation,


Ferns—The last family of coal plants is the Ferns—a family with which all are more or less familiar through our modern varieties. The modern species, however, differ very greatly from those of the coal age. Some of the ferns which grew in the coal forests were tree ferns, but most of them were herbaceous. Some fronds (leaves) of these were six to eight feet in length. A great many specimens of fossil ferns have been found in Belmont county, representing thirty or more different species. Only a few of these can be noticed here. Fig. 4 represents a new species discovered in Wheeling township. This species was named by Prof. Lesquereux, and is described by him in his coal Flora of the United States, and figured in the Coal Flora Atlas—both of which works are published as parts of the Report of the Second Geological Survey of Pennsylvania. Fig 1.2 represents a specimen found on the farm of Mr. Wilkins, about half a mile from St. Clairsville, in a soapstone formation lying a few feet below Coal No. 12. This is a very common species, however, and may be found in almost all our coal-bearing formations. It was discovered by Lesquereux and described by him in the Geological Survey of Illinois. Fossil remains of fruits which grew on the trees of the coal forest are often found.


* The confusion incident to the use of loose and inaccurate* "common names" would, of itself, be a sufficient excuse for the introduction of the scientific names of the species here described. But, fortunately for science, these plants have no "common names," so that we must call them by their technical names, of not at all. These names, it is hoped, will not tend to confuse. The name is usually either descriptive of the nature of the plant, or is derived from the name of the discoverer. The "Lx.," or "Lesqx.," is for Lesquereux, the naturalist who first named and described the species. In like manner, "Brgt.," or "Bt ," is a contraction for Brongniart, the name of an eminent French naturalist; "Scloth," for Schlotheim; "Nwby.," for Newberry ; "Germ.," for Germar.


28-B. & J. Cos.


Fig. 13 (Andrews) represents a species first described-by Dr. Newberry, of which specimens have been found in Belmont county. It is not known certainly on what trees these nutlets grew ; but they are supposed to belong to the Cordaites, a tree allied to the conifers or "cone-bearers. The rocks of Belmont county are peculiarly rich in fossil plants. In the shales over and beneath the various coal-seams, and in other formations of texture sufficiently fine to preserve the impressions, there are doubtless hundreds of species. But these formations have not as yet been well studied. The work in this line, the results of which are here outlined, is the mere pastime of a period less than two years. Except a few scattering investigations in the horizons of Coals No. 12 and No. 13, nothing has been done to develop the fossil flora of the Upper Coal Measures of Belmont county; and the species of Our Lower Measures so far identified are known through specimens obtained by Dr. G. A. Close, of St. Clairsville, and the writer of this sketch, from excavations made along the line of the C., T. V. & W. Railroad.


The Coal Basin.—It will be seen from the map (Fig. 15) that there are four principal coal fields in the United States ; and that the one to which our eastern Ohio coal district belongs, is a long, narrow, irregular strip, extending from the northern boundary of Pennsylvania, in a southwesterly direction, to near central Alabama, covering considerable tracts in southwestern Pennsylvania and southeastern Ohio, with a large portion of West Virginia, and parts of Kentucy, Tennessee and Alabama. This great coal field, it will be observed, trends southwest, almost parallel with the Atlantic coast and with the Blue Ridge Mountains, which form its eastern boundary. It is separated from the coal fields of the west by an upheaval of the underlying strata, forming an arch, or anticlinal, as it is called, trending in the same direction—a little east of north—from the southern boundary of Tennessee, through Nashville and Cincinnati to Lake Erie. This is called by our state geologists the Cincinnati Arch. East of this Arch the strata dip generally in a line perpendicular to it ; so that, the surface being assumed to be generally level, the various formations from the highest strata of the eastern portion of the state to the lowest seen on the summit of the Arch, will in turn become the surface rock. Fig. 16 represents a section of the strata from Bellaire to Cincinnati, showing the dip of the strata, and how the _different formations became in turn the surface rocks.


Until recently it was supposed that all the great coal fields were formed together, and consequently that the basin in which the coal forests grew, extended almost over the entire continent, from the islands of the Arctic Ocean to near the present shores of the Gulf of Mexico, and from the Blue Ridge Mountains which existed at that time, to the district where the Rocky Mountains now stand—that district, as it is well known, being then at the bottom of the sea. It seems, however, from the investigations of the eminent geologists of our State Geological Corps, that the coal field of which our Ohio district is a part, was formed independently of the rest, and has never, at any time, been connected with the coal fields of the west. This is proved by the fact that the Cincinnati Arch is older than the coal-bearing formations. The Allegheny mountains did not exist when the coal measures were formed. This is shown by the fact that the upheaval of these mountains bent and cracked the strata of the coal measures, and carried them out of their original horizontal position. Of course the trough in which the Ohio river now flows did not exist in the coal-forming period, as the center of depression of the coal basin, is known to have been further east in the Appalachian region, at least during the early part of the coal-forming period. Within this long, narrow basin, then, bounded on one side by the Blue Ridge Mountains, and on the other by the Cincinnati Arch, and deepest in the Appalachian region, grew the coal forests. In order to understand the state of affairs which then existed, we must get rid of our ideas of things as they now exist over the same districts. We must not think for a moment of a country of hills and hollows, threaded by rivers, creeks and brooks; but must picture to ourselves a vast plain stretching over the bottom of this basin, varied by gentle undulations, which raised portions of it above the level of the lakes, lagoons and marshes which covered a large proportion of the area. On the dry lands grew the Conifers and Lepidodendrids, while the Sigillarias probably grew in the marshes, as did the Ferns and Equiseta Centipedes ; land snails, spiders scorpions, May flies, cockroaches and crickets, lived on the land; and fresh water mollusks crawled among the Equiseta of the marshes. Along the brink of the' waters were reptiles of the amphibian nature; in the lagoons sported swimming reptiles ; while in the deeper lakes swam shark-like fishes. A still, warm,


218 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


moist, impure atmosphere, hovered over the plain. Not a flower blossomed, not a bird sang, in all this wide horizon of solitude ; but a dull, monotonous stillness instead, broken only by the croaking of batrachians, the hum of insects, or the bubbling of gases exuding from the marshes. Fig. 17 (from Dana) represents an ideal carboniferous landscape.

Thus, during the long, dreamy ages existed the desolate plain. Trees and herbs grew up, fulfilled their years, and added their remains to the accumulating mass of vegetable debris. Crawling centuries passed away, and the mighty mass grew more solid and deeper. But no phase of Nature can endure forever ; and even this long, listless scene closed at last. The unstable surface sunk down, till at length the waters triumphed and covered the whole plain. Then began the formation of beds of sediment over the buried mass of vegetation. Now currents sweep from one direction, bearing particles of calcareous matter, washed from some old Silurian or Devonian continent, which, deposited in layers at the bottom, are to harden into a bed of limestone. Again it changes its direction, and bears grains of sand, washed and silted, perhaps, from the disintegrated particles of some old granite hills. Again the water was parted by the rising surface, and anew forest grew, followed in turn by another subsidence, and new deposits of rock-materials. Thus the process went on, in an endless cycle of change, repeating itself for each successive coal formation.


This is no mere ideal picture. True, no eye of man was present to look upon that dreary landscape ; but Nature, here as elsewhere, has not left herself without witnesses. The coals, the rocks, the fossils, all bear undoubted testimony as to the exist, ence of such a condition of affairs.


THE EARTH'S CRUST.


That the earth consists of a mass of intensely-heated fluid or molten rock-material, surrounded by a crust of. solid rocks, is a proposition which cannot be doubted, or at least is not doubted by any who have qualified themselves to express an opinion on the subject. It is the crust of solid rocks with which geology has most particularly to deal. There are so many kinds of minerals entering into the structure of this crust that a list of them would bewilder any one who is not a professional mineralogist, But all these may he grouped into two classes: First, a layer of crystalline rocks encircling the globe of molten matter, consisting of granites, porphyries and others of like nature ; and, second, a sphere of rocks arranged in layers or strata, consisting of sandstones and limestones in their various forms, overlying the crystalline rocks, and forming the surface of a large portion of the earth. The first class is called Azoic rocks; the second Stratified or Sedimentary rocks: the first term having reference to their arrangement in strata or layers; the second signifying that these layers wore formed of materials deposited as sediment at the bottom of bodies of water. It is impossible to give any idea of the thickness of the azoic beds underlying the sedimentary rocks of Ohio ; but the sedimentary rocks themselves have been studied so carefully by our State Geological Corps that it is possible to arrive at an approximate idea of their depth. and arrangement. They are divided into three classes: 1. The Silurian, consisting of vast beds of sandstone and limestone, containing fossil remains of animals of the lower orders, and lying upon the azoic rocks; 2. The Devonian, consisting of layers lying upon the silurian, and differing from them mainly in the kinds of fossil remains which they contain, fishes being the characteristic fossil; and, 3. The Carboniferous, or coal-bearing strata, overlying the Devonian, characterized mainly by fossil plants. The relations of these rooks in Ohio are shown by Fig. 16. It will be observed that the surface formations of Belmont county belong to the carboniferous. An approximate section of the sedimentary rocks of Ohio is given in Fig, 18. The lower part of this section is from the notes of an artesian well sunk at Columbus to the depth of 1775 feet. At this depth the bottom of the sedimentary rocks was not reached ; and it is impossible to tell how much greater depth would have been required to reach the azoic beds. The upper part of the section was completed by adding to the notes of the well the thickness of the various deposits, as estimated by the state geologists. The complete section as platted in the figure is as fol-




I. Carboniferous.


1. Coal Measures


2. Lower Carboniferous appear



II. Devonian.


III. Silurian.

(Upper Barren Measures.

(Upper Coal Measures

(Lower Barren Measures.

(Lower Coal Measures

( Carboniferous Conglomerate

(Lower Carb, Limestone 

( Waverly Sandstone

(Huron Shale.  

(Corniferous Limestone 

(Oriskany Sandstone 

(Upper 

(Lower

Total

300 feet

430 “

352 "

505 "

88 feet

20 “

460 “

275 "

138 "

2 "

648 "

1849 "

5067 feet.




Here then is a sedimentary rocks nearly a mile in thickness. There is every reason to believe that the depth of the sedimentary rocks, from the top of one of our Belmot county hills to the azoic beds beneath, is considerably greater than this estimate. In the first place, only the lowest possible estimates are given ; in the second place, the section does not pretend to reach the bottom ; and, lastly, there are very strong reasons for believing that all these formations are thicker here than farther west where the figures given were obtained, since the same deposits are known to reach the enormous thickness of seven miles in the Appalachian region of Pennsylvania, and to thin out gradually towards the west; consequently, in this region, lying nearly mid-way between the points where these rock4 have been definitely studied, they would be expected to have an intermediate thickness. It is not unreasonable to suppose that the sedimentary rocks of Belmont county would aggregate much more nearly three miles than one. But this is more of a surmise rocksan estimate, since there is no basis upon which an estimate can be made, except that given.


The Coal Measures.—It will be noticed from the section (Fig: 18) that the carboniferous formation is divided into two groups, the lower carboniferous and the coal measures. The lower carboniferons rocks, as is determined by fossils which they contain, belong to the same geological age as the coal measures ; but unlike the latter, they contain no coal-seams. The coal measures are, strictly, speaking, the true carboniferous, or coal-carboniferousions. These are the rocks which it is important to study minutely in order to understand the geology of this region.


By reference to the section (Fig. 18) it will be observed that, lying immediately upon the rocks of the lower carboniferous, there is a group of strata about 500 feet in thickness, containing seven persistent seams of coal, besides two or three seams which do not cover the whole area of coal field. This group is called the lower coal measures. The coal-seams of this group are numbered by our state geologists from 1 up to 7, beginning with the lowest. Coal No. 1 varies from 3 to 6 feet in thickness; No. 2, from 1 to 5 feet; No. 3, from 1 to 4 feet ; No. 4, from 1 to 4 feet ; No. 5, from 2 to 5 feet; No. 6, from 3 to 12 feet ; No. 7, from 2 to 7 feet. Between No. 6 and No. 7 is a seam 6 feet thick, seen by Prof. Andrews in the southern part of the coal field, which, according

to Dr. Newberry, does not appear in the northern. This is therefore called No. 6A. There aiA) other seams not shown in the section ; but they are neither persistent nor important. All these persistent seams, and perhaps others, underlie the roareof Belmont county, though none of them are exposed within the limits of the county. No. 7 is mined at Cambridge, Guernsey county, and also in the shaft at Steubenville, Jefferson county. These are the nearest points at which any seam of the lower measures is worked.


Lying upon the lower measures, there is a group of strata, about 350 feet thick (often much more) consisting of sandstone shales, with some thin beds of limestone, and an abundance of red and gray shales, marls and clays, but containing little or no coal. This series was first definitely studied by the Pennsylvania geologists, and was designated by them the "lower barren measures," a very appropriate name, which has very properly been adopted by the geological corps of our own state. The lower barren measures contain little that is interesting to the geologist, the mineralogist, the manufacturer or the farmer. There are several exposures of the upper part of this group in Belmont county, the greatest being some 200 to 250 feet in Flushing township. None of the lands of Belmont county, however, belong to the lower barren measures. The exposures are along the valleys of creeks which have cut down through the overlying strata and into the barren series. The soils of the hillsides belong to the upper coal measures, while the alluvial soils of the valleys are from the same source. Above the lower barren measures lies a series of strata ranging from 400 to 500 feet in thickness, and containing, in this county, nine coal seams. This series is called the upper coal measures. Upon this lies another series reaching, in this county, the thickness of


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 219


300 feet, or upwards. This is called the upper barren measures. It is to these two series that the rocks of Belmont county belong; and consequently the study of these is essentially the study of


THE GEOLOGY OF BELMONT COUNTY


Many of the most interesting features of the geology of Belmont county, have been given as illustrations of the general principles treated of in the foregoing outline. It remans now to apply these principles in tracing the geology of a locality which may fairly be said to be the most interesting part of the upper coal measures of Ohio. The surface structure of Belmont county is such as to give us a fine opportunity to study the whole range of the upper coal measures, while .there are ample exposures of the lower barren measures at the north, and of the upper barren measures at the south, to serve as illustrations of those formations, and to show clearly our geological relations to the remainder of the great coal field of which our region forms a part. On the north and west, in Jefferson, Harrison and Guernsey counties, the formations which give to Belmont its peculiar interest, are known only by groups of strata crowning the hill-tops, or have entirely disappeared, and given place to the lower barren measures. In Monroe, on our south, the upper barren measures predominate. In Belmont, better perhaps than in any other locality west of the Ohio river, can the upper coal measures be seen and studied in their full scope, and in all their relations.


Surface Features.—The surface of Belmont county has two general slopes : the one eastward toward the Ohio river; the other westward toward the Muskingum. The dividing ridge between these slopes is a tortuous line beginning near the middle of the southern boundary of Somerset township and running north into Warren, thence east into Goshen. thence north, through Union and Flushing to the northern boundary of the county. This line of divide is shown on the map of the county, found elsewhere in this work. Branching off from this divide, and continuous with it, are the ridges separating the drainage systems of the eastern slope. Much the larger portion of the surface of the county belongs to the eastern slope. This slope is drained by the three large creeks, Captina, McMahon's and Wheeling, together with numerous smaller streams, the most important of which are Pipe creek and Wegee. The western slope is drained principally by Stillwater and Leatherwood.


The Dip.—If the rock-strata of the county were level and uniform we should expect to find the highest geological formations along the ridges as shown on the map, and the lowest at the mouths of the larger creeks. The strata are not horizontal, however, but have a general dip or fall toward the Ohio river, in a line a little south of east. The result of this is that the highest geological formations of the county are found on the hills of York, Mead and Washington townships, and the lowest are found along the valley of Stillwater, in Kirkwood and Flushing townships.— This will appear clearly from Fig. 19, representing a diagonal section of the county from northwest to southeast, that is, passing through Flushing, Union, Smith and York townships, and merely touching the corners of others. The dip of the strata is not uniformly towards the southeast. On the western slope, along Leatherwood, the direction of the dip appears to be reversed. On the eastern slope, too, there is an anticlinal running east of north through York, Mead, Pultney, Pease and Colerain townships, which appears to have raised the strata something like forty feet higher than their natural position in a uniform dip. From this axis the strata dip very rapidly to the Ohio; so much so that the Pittsburgh coal, which is forty feet above the creek bed at Quincy, sinks to the level of the river at Bellaire, and at Dillie's Bottom, opposite Moundsville, it is reached by a shaft at the depth of 80 or 90 feet below the level of the river. Want of time in gathering the materials for this sketch has prevented any accurate measurements on the dip of the strata of this county.


The Strata.—In tracing the relations of strata, geologists, as a general rule, begin with the lowest. The reason of this rule is obvious : the lowest strata were, of course, first formed; and geology, being substantially a history, must follow the order of time. This order has been followed in this sketch, though no attempt has been made to give a historical treatment of the subject. The facts are given just as they exist, and also the principles which applied to the facts show the historical bearing of the subject. (See article on Coal.) Following the historic Order, let us, as briefly as may be, inquire into the structure of the formations which compose the frame-work under the soils of


I-28—B. & J. Cos.

Belmont county. This must be done in a manner somewhat general, as the space allowed will not permit of separate treatment of the geology of each township. It is to be hoped, however, that this general treatment may make the excellent sketches of local geology given in our State Reports intelligible to all. Continual reference to the sections represented in Figs. 20 and 21 will greatly assist in understanding the text. The first, Fig. 20, is a section taken in York township, which will serve as an illustration of the general structure of the Eastern Slope. The second (Fig. 21) is an accurately measured section taken by Mr. Dawson, of Barnesville—the lower part from the coal shaft at that place, and the upper part completed by mathematical measurements of the intervals between the coal-seams in the surrounding hills. It will be remembered that the last or highest coal-seam of the Lower Coal Measures, the "Cambridge Coal," was No. 7. The first, or lowest, seam of the Upper Measures, then, is known as Coal No. 8. This is the great "Pittsburgh Coal," of which more remains to be said further on. The next seam, supposed to be persistent, is Coal No. 9, and so on up to the highest known to be persistent, which is Coal No. 13. Between No. 8 and No. 9 there are three seams, the last of which is of considerable importance, called respectively, No. 8 A, No. 8 B, No. 8 c. Between No. 12 and No. 13, likewise, there is a thin seam which. may conveniently be called No, 12 A. Above No. 13 there are other small seams ; but they are of little importance.


By reference to the sections it will be seen that the strata below Coal No. 9 are mostly limestone, while those above that seam are mostly sandstone. Thus the strata naturally group themselves into two series, the lower of which we may designate as the Limestone Series; 1 he upper, the Sandstone Series.


Enough has been said of the lower barren measures. We will consider the limestone series of the upper coal measures, beginning with the lowest stratum, namely, the Pittsburgh coal. This seam doubtless underlies the entire area of Belmont county. It is the great seam so extensively mined at Pittsburgh, so well known in the iron manufactories, and which has for years supplied so large a part of the coal commerce of the Ohio river. This seam is mined at outcrops in ten of the sixteen townships of Belmont county. The rise of the stratum towards the north-west brings it to the surface along the creek valleys in Flushing, Kirkwood and Union townships. The same cause, together with the great depth to which the stream has eroded, makes this seam accessible along Wheeling creek and its larger tributaries for the distance of nineteen miles from the river: that is, in Wheeling, Colerain, Richland and Pease townships. It is accessible all along the eastern border of the last named township, of course, by virtue of the depth of the river valley ; and down the river to Bellaire, where the dip carries it below the river level, The anticlinal axis before mentioned (see county map,) brings it to the surface along McMahon's creek and its larger tributaries, for the distance of six miles. It disappears below the level of the creek at Franklin Station, at which point it is largely mined. In Mead Township, near the mouth of Pipe creek, it again outcrops, as it does also in York township, for the distance of five miles along Captina, where that stream crosses the anticlinal. In Washington and Wayne Townships it could easily be reached by shafts at almost any point along the valley of Captina. On the old Danford homestead, near the Wayne township line, an oil well sunk by Mr. A. C. Danford, reached the Pittsburgh seam at the depth of 39 feet, and the seam is reported to .be 171 feet thick at this point. This is the greatest thickness this seam is known to have ; the next greatest, perhaps, is at an outcrop in Union township, on the land of Mr. Isaiah Lee, in section 31. Here it reaches the thickness of 10 feet. Its usual thickness is about 6 or 7 feet; but it has a common range of from 4 to 8 feet.


In Warren township the Pittsburgh coal, if indeed it does not outcrop, would be easily accessible by shaft along Stillwater. Down the Leatherwood, west of Barnesville, a seam (the same mined in the Barnesville shaft) believed to be the Pittsburgh, is mined in hillsides ; but it is not overwhelmingly certain that this is the Pittsburgh coal. In Goshen and Smith the Pittsburgh coal is not seen ; but it might, if it were needed, be reached by shafts in either of these townships.


Over the Pittsburgh coal and separated from it usually by four or five feet of slate or soapstone shales, there is a seam of limestone about twenty-five feet thick. This seam appears to be persistent all over the eastern slope. Upon this limestone lies coal No. 8 A, a thin and unimportant seam, sometimes reaching the thickness of 2 ½ feet, but usually about 1 to 11 feet. Between this and the next coal seam above (No. 8 B) there


220 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


is an interval of 30 to 40 feet. This interval is filled mostly with limestone, one bed of which, about six feet in thickness, pos sesses good hydraulic properties, and is known as the Bellaire cement. About seven feet, sometimes less, above this cement lies coal No. 8 B, a seam usually a foot or eighteen inches in thickness, but sometimes reaching four feet, in which case it has 80 many slate and clay partings as to be of no practical value: Between this seam and the next above (No. 8 c) there is a variable interval, sometimes not more than 12 or 15 feet, and again as much as 35 feet. At the east this interval is usually less than 20 feet, and is almost wholly sandstone. Towards the northwest it seems to thicken up, and to contain a bed of limestone over the sandstone. Coal No. 8c is the third seam in importance of the coals of Belmont county. Lying from 80 to 90 feet above the Pittsburgh coal, it is scarcely noticed where that seam is accessible : but it outcrops along the creeks, sometimes for many miles, after its great neighbor has disappeared, in which cases its true value is recognized. Along Captina it is visible as far as Armstrong's Mills. It disappears beneath the creek bed at the northern extremity- of the " Three Mile Bend," two miles above Armstrong's. In Wayne township it is again brought to the surface, perhaps by an anticlinal arch, where it is well known as the " Horeb coal." On McMahon's creek it is known as the " Glencoe coal."* It is mined along Wheeling creek, above where the Pittsburgh seam disappears, as far as the crossing of the Uniontown and Flushing turnpike. At Flushing it is now known as the "Tunnel Seam." There is a strong probability that this is the seam worked at the bottom of the Barnesville shaft, though the weight of authority pronounces that the Pittsburgh coal.


Between coal No. 8 c and the next seam above (No. 9) there is an interval of about 70 feet, though it seems to be as little as 40 feet at some places and as much as 85 feet at others. This interval is filled with a greater variety of strata than any other series of equal extent in the. county. It contains the famous Parker Cement, together with a great variety of limestones, sandstones, slates and sandy shales. In the river townships it is almost entirely limestone : first, immediately over coal No. 8 c, a bastard limestone about 40 feet in thickness; then a thin belt of yellow limestone which readily crumbles by the action of the weather, and is interesting to geologists on account of its persistency, which makes it a good landmark ; then a thin layer of' green-looking chloritic rock of fine texture, which Mr. Potts, of York township, calls " whetstone rock ;" then another layer of limestone, 8 or 10 feet thick, upon which lies another thin stratum Of " whetstone rock ;" then two beds of limestone, aggregating 10 to 15 feet, separated by three feet of mongrel sandstone.


On the western slope this interval is quite different, as may be seen by examining Fig. 21. The heavy limestone formation below is replaced by an equally heavy sandstone ; while the limestone and cement above are much more simple in arrangement. At Flushing the whole interval is filled with a slate formation.


Coal No. 9 is a comparatively thin and unimportant seam ; but it is reported by Prot, Stevenson, of the State Survey, to be "very persistent," and "seldom less than thirty inches thick," In the Barnesville shaft it is found in its proper place, immediately over the limestone series, and is two feet thick.


We pass now into the sandstone series. From this point upwards there is more uniformity between the eastern and western slopes. While the strata of the limestone series were being deposited, there is reason to believe that the centre of depression of the Allegheny coal basin was at some point far to the east of the Ohio river. After the formation of Coal No. 9 it appears to have changed to some point west of the Ohio, and southwest of Belmont county.


The interval between Coals No. 9 and No. 10 is sometimes as little as fifteen feet, but is often thirty-five to fifty feet, It consists of both sandstone and limestone.


Coal No. 10, known generally in Belmont county, as the Badgersburg coal," and in Guernsey and Noble counties as the "Cumberland Coal," is second in importance only to the Pittsburgh seam, of all the coals of the Upper Measures: It is accessible in those townships, where the Pittsburgh seam is not; and hence it may be called the complement of the Pittsburgh Coal. It is very thin towards the river, but thickens up toward the south-west, until, in the Barnesville shaft it reaches a thick-


*In the excellent sections taken by Prof. Andrews along the line of the Central Ohio Railroad (Ohio Geology, Vol. II, p. 555-563, and accompanying Map XIV), this seam is called the Cumberland coal (No 10). The error arises front not making sufficient allowance for the dip of the strata. The Cumberland seam is a 'little below the horizon of the railroad-bed at Lewis' Mills. It is the seam mentioned by Prof. Andrews, (p. 556) as "the coal in the deep cut just east of Lewis' Mill."


ness of 5 feet, clear. Over this seam lies an immense body of sandstone and limestone, 80 to 100 feet at the west, but thinning out at the north-east to a few feet of shaly sandstone. Within this body, about 75 feet above Coal No. 10, in Goshen Township, lies a fine flagstone formation. Coal No. 11, the next in order, is an unimportant seam, either thin or so split up with slate or clay partings, as to be et little value. In Goshen township, where it seems to be best developed, it is usually found to be nearly 4 feet thick, with a seam of tough slate nearly a foot thick near the middle. Under it, separated from it by a few feet of sandstone, there is generally a bed of limestone which makes an excellent quicklime. Thirty-five or forty feet above Coal No. 11, in the western part of the county, lies Coal No. 12 ; but this interval thins out towards the north-east. It is filled mostly with a shaly sandstone. Coal No, 12 is a much thicker and better vein than No. 11. It is mined extensively and is valued highly by the farmers of the ridge sections. Above this, and separated from it by an interval of sandstone shales, of not far from 100 feet, is Coal No. 13. This seam is seen in the hilltops (generally double) as far north as Morristown and St. Clairsville. It thickens toward the south, till, in Washington township, it reaches a thickness of six feet. Between Coals No. 12 and No. 13, nearly middle way, lies a thin seam of coal, which deserves to be mentioned, principally because it has been the means of misleading geoligists in their identification of the higher coals.* It is accompanied by a bed of fire-clay, arid a thin stratum of very blue limestone. It is very persistent throughout the northern part of the county, and may often be detected in the southern.


Above Coal No. 13, at an interval of about 10 feet, there is a six inch seam of splint coal, which has been supposed to be the highest seam of the county ; but there is an eighteen inch seam of the Upper Barren measures, at least 250 feet higher than this; and doubtless there are many others of like nature ; but they are of little importance.


The 300 feet of barren strata above Coal No. 13, is of comparatively little interest. It may be divided into three groups: First, the Clay Group, comprising about one hundred feet of sandstone and clay lying upon Coal No. 13 ; second, the Red Shale Group, comprising about 70 feet of strata, characterized by the presence of several deposits of red clayey shale, which weathers into a sort of marl, very striking on account of its color ; and third, the Shaly Sandstone Group, comprising from fifty to two hundred feet of argillaceous sandstone, which caps the highest hills (geologically speaking) of the county.


Formation of Hills and Valleys.—At the close of the formation of the upper barren measures a new geological era begun. The crust of the earth, at the center of the depression of the great Allegheny coal basin, was broken and folded upwards into the ridges now known as the Allegheny mountains, and other ridges of the same system. Between these mountain ranges and the Cincinnati arch there was, of course, a line of lowest depression, or trough : in that trough now flows the Ohio river. It is not necessary to tell any observing person that the surface irregularities of Belmont county are not the work of such forces as produced the mountains east of the river. The strata of this region are undisturbed or very slightly displaced at a few localities. Besides, the ridges on this side of the river are perpendicular to the trend of the mountains and the river ; whereas, if they were due to the same cause, they would be parallel with them. The true explanation of the variations of our surface features is, that the valleys and ravines have been carved out by the streams which flow in them, leaving portions of the strata as they were originally formed ; and these constitute the dividing ridges. The continuity of the strata, broken only by the troughs of the streams, sufficiently proves this. In a single trip from the Ohio river up one of our larger streams, one may satisfy himself on this point, not only as to the fact that the valleys are thus formed, but also that the process of erosion is going on to-day just as it has been for centuries. About two hundred and seventy-five feet above the level of the river, there will be noticed a broad bench or terrace on the hillside, and this will be observed to follow round the bend of the hill and continue up every stream, which flows into the river, on both sides of the valley. If the observer will climb to this terrace, he will find that its bench is a hard sandstone stratum, projecting out from the hillside. By following it up the stream, he will find that it turns every angle of the hill, and is continuous up every ravine, on both sides. A short distance up one of those precipitous ra-



* This is the seam in the cut at Burr's Mills, which Prof. Andrews mistook for the Barnesville Tunnel Seam. (No.12) Geology, Vol. II, p. 553.


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 221


vines, he will find that the ledges of the opposite sides come together into a continuous stratum, which forms a table rock, over which a cataract usually falls. Large. fragments of the table- rock will probably be found strewn along the bottom of the ra- vine, some of them at considerable distances from the jutting ledge of which they once formed a part. Under the table-rock, behind the cataract, will usually be found a semi-circular cavern, formed by the crumbling and washing away, of the soft shale upon which the table rock formerly rested. The spray raised by the falling water, moistens this shale, which, drying when the water is low in summer, with alternate freezing and thawing in winter, gradually wastes away, till the over-hanging rocks, unsupported, falls of its own weight, and a new waterfall it formed further up the stream, only to repeat the same order of events. Let our observer continue his journey up the main stream, and he will notice that the terrace approaches the bed of the creek, or rather, that the bed of the stream rises towards the terrace, till finally the two ledges unite in a continuous stratum which disappears beneath the creek-bed, usually forming falls or rapids. These falls or rapids are wearing back, up the stream, just as in the ravine. In this manner have been formed all our valleys, hollows and ravines. When we think of the immense masses of rock material which must have been removed in forming the hundreds of winding hollows and deep ravines of Belmont county, it seems improbable that it should have been removed in this way. But when we think, for a moment, of the thousands of little springs and rivulets at work night and day, softening, loosening, and carrying away, grain by grain ; of the air, the mosturo, and the frost, disintegrating the solid rocks of the hills into soil ; of the dashing rains which carry away these soils ; of the tons of sedimentary matter which Captina, or McMahon's, or Wheeling creek, when high and muddy, must carry away in a single hour—when we think of all these, we must be led to the conclusion that the idea that our surface variations have been produced by erosion is at least rational, if not certainly true. An estimate of the amount of rock-material carried away from our area in a year, would be amazing to many, and would tend to make one wonder that he bad ever doubted on this point.


ECONOMIC GEOLOGY.


No equal portion of the mile or more of sedimentary rocks of Ohio contains so great. an amount of mineral wealth as the fifteen hundred feet of strata in which the coal-seams are included. The value of these strata depend upon their variety as well as upon the presence of coal. The strata of the Silurian and Devonian ages furnish excellent limestones and sandstones, well adapted to all purposes for which sandstone and limestone can be used ; but there is generally so little variety in the structure of the Silurian and Devonian formation; that frequently over immense areas there is but a single kind of rock to be seen. Here, on the other hand, we have all varieties within the area of a few square miles. We have, in Belmont county, nine seams of coal, fifteen beds of limestone, two beds of cement, and ten different sandstone formations, interlaid with numerous deposits of fire-clay, soapstone, slates, marls and shales of various kinds. In round numbers, the hills of Belmont county are made up of rock aggregating six hundred feet, of which the coal-seams aggregate about twenty-five feet, the limestone strata about two hundred feet, the sandstone and shales about three hundred, the rest consisting of fire-clays, slates, marls and soapstones. This is a showing difficult to excel in variety—hardly to be equaled, in fact, except in mountain regions, or in localities where the strata have been folded and displaced by the action of internal forces.


Value of Our Coal.---The true value of coals must be looked .for in the light of political economy, rather than from an individual standpoint, He who owns lands underlaid with stores of good coal may or may not be considered as possessing individual wealth. The personal value of his resources depends upon their accessibility, upon the amount of competition, upon the markets, and upon various other local influences. But the state or nation which is underlaid with seams of coal, such as those of Ohio, must be regarded as possessing a wealth which, if it does not outshine, is at least far more substantial and trustworthy and productive of far more happiness and general prosperity than the fabled wealth of Ormus and Ind." Says Dr. Newberry, the eminent chief of our State Geological Corps, "Of all the nations of Europe England is the most powerful, because she is the richest. Though occupying a group of islands insignificant in area, she has spread her power over the entire globe, and it is her boast that the sun never sets on her possessions. It is wall known to the political economist that the source of England's wealth has been her manufacturing industry ; and the main-spring of her industry has been her stores of coal. In this respect she enjoys a great pre-eminence over all the nations of Europe. The United Kingdoms have a coal area that has been reckoned at 10,000 square miles, while in round numbers Belgium has 500, France 2,000, Spain 9,000, and the other nations of Europe still less. The annual coal production of Great Britain is now more than 100,000,000 tons, and a very short calculation will suffice to show what an important contribution this makes to her national wealth. The power developed in the combustion of a pound of coal is reckoned by engineers as equal to 1,500,000 foot-pounds. The power exerted by a man of ordinary strength during a day of labor is about the same ; so that a pound of coal may be regarded as equivalent to a day's labor of a man. Hence 300 pounds will represent the labor of a man for a year. It has been estimated that 20,000.000 tons of the annual product of Great. Britain is devoted to the development of motive power, and that this is equivalent to the labor of 133,000,000 of men. These men, in this calculation, are considered as exerting merely "brute force; " but since they may all be regarded as producers only, and not consumers —the profit on the balance of her coal product fully 'covering all expenses—we are safe in estimating the contribution to the wealth of Great Britain by her annual coal product as equal to that of 133,000,000 of' skilled operatives laboring for her enrichment,"—(Ohio Geological Survey, 1869).


The productive coal area of Ohio is, according to the same high authority, " not less than 10,000 square miles, or quite equal to that possessed by Great Britain," while the annual production of the State was then (ten years ago) less than one thirtieth of that of Great Britain. The United States, with a coal area fifteen times as great as that of England, and with an inexhaustible store 01 iron known to be unexcelled in quality, was then purchasing a large proportion of her supplies of manufactured iron in English markets. But these things can not always be. The good sense of our people, assisted by that science which some have been wont to consider a tissue of idle speculations, has perceived our advantages, and already the tide of trade is turning. Observe the hundreds of car loads of iron ore which pass over our trunk railroads to the furnaces of the Ohio coal fields ; then notice the brands upon the new steel rails by which the railroad companies are replacing the old iron rails which were imported from England ; observe also the brands upon which some of the best grades of our new cutlery : these are the straws which show that the old current has ceased ; while there are ample facts and figures to show that, in tho matter of manufactures, we are, at no distant day, destined to supply the old world with products as the old world has heretofore supplied us. In this great movement Ohio is destined to take an important part, since " the coals of the Allegheny coal fields are superior to those of the west, and it is certain that nowhere can an abundant supply of mineral fuel suitable for smelting the Lake Superior ores be so cheaply obtained as in Ohio."—(Newberry.) There are already two iron manufactories within the limits of Belmont county, both of which take the Lake Superior ores in their native state and turn them into an excellent quality of manufactured iron. The following table, from the report of the Secretary of State (Ohio statistics, 1878) shows the part taken by Belmont county in the coal and iron industries. It should be remembered, meanwhile, that "Ohio ranks as the second state in the Union in iron manufacture," (Ib. 1872, p. 223), Pennsylvania being the first, the annual product of that state being nearly one-half of the entire product of the United States.


COAL AND IRON PRODUCTS OF OHIO,


The table on the succeeding page exhibits the amount of coal and iron ore mined in Ohio, as reported by township assessors to the county Auditors in May, 1878.


222 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.







Counties

Stone Coal

Iron ore

Bushels mined

Tons mined

Tons from other states

Tons from other counties

Ashland

Athens

Belmont

Carroll

Columbiana

Coshocton

Cuyahoga

Gallia

Guernsey

Harrison

Hocking

Holmes

Jackson

Jefferson

Lawrence

Mahoning

Meigs

Monroe

Morgan

Noble

Perry

Portage

Scioto

Stark

Summit

Trumbull

Tuscarawas

Vinton

Washington

Wayne

Totals

1,000

9,829,991

6,868,003

273,475

9,586,660

1,162,200

...........

919,402

1,479, 300

390,165

4,513,365

242,750

1,714,831

3,641,160

2,701,839

3,929,403

7,332,880

71,700

251,495

157,199

11,672,138

70,100

47,300

8,427,446

4,051,849

11,317,481

4,437,050

1,185,910

216,225

2,959,220

98,750,537

....

17,000

....

....

26,410

....

....

....

....

....

20,758

....

32,757

10,409

83.759

....

....

....

....

....

72,954

....

11,500

1,320

....

10,021

10

....

....

....

286,886

....

400

14,000

....

36,000

....

328,962

....

....

....

300

....

....

....

8,850

8.595

....

....

....

....

....

....

....

....

....

....

....

....

....

....

897,107

....

....

....

....

....

....

....

....

....

....

160

....

....

....

....

....

....

....

....

....

....

....

....

....

....

....

....

....

....

....

160




 

From this table it will be seen that Belmont county ranks as seventh in the production of coal, those counties of the Lower Coal Measures, in which Coal No. 6 outcrops, ranking ahead. It will also be seen that Belmont imported for manufacture, in 1877, fourteen thousand tons of iron ore, ranking as third in this line, Columbiana being second, and Cuyahoga, first. The following table shows more clearly and specifically the present position of Belmont among the iron manufacturing counties of Ohio. Cuyahoga, containing the great rolling-mills of Cleveland, takes the lead; and this, notwithstanding she must import her ore from Michigan and her coal and limestone for slagging from other parts of Ohio.


Table showing the amount of rolled steel and iron produced in Ohio, as reported by Township Assessors to the county Auditors in May, 1878 :


Fire Clay --Under each seam of coal there is usually a bed of tough, white, or grayish-white clay, called the under-clay. Sometimes clay of this kind is found independent of coal beds. It is from such clay that stoneware, fire-bricks, tiles and sewer pipes are manufactured, for which reason it is called "fire-clay." Beneath coals No. 3, No. 5, and No. 1, which belong to the lower measures, and consequently are not found at the surface in Belmont county, there are important beds of fire clay, the first of which alone "supplies the material from which stoneware, fire-bricks, &c., are manufactured to the value of more than a million dollars per annum."— (Newberry.) None of the fire-clays of the upper measures, so far as yet known, can compare in value with those of the lower measures ; but so little attention has, as yet, been paid to these deposits, that no definite idea can be formed of their economic value.


Fire clay performs another important office, not usually considered. Most of the rocks of our upper measures are so loose and jointed in their structure, that water falling as rain readily percolates through them, till it reaches a compact stratum not permeable, where it gathers into underground streams. These streams follow the stratum till they come to the surface, where they issue as springs, such as those with which the people of Belmont county are so familiar, and which are of such inestimable value, to the farming interests of this region. The strata most likely to form the beds of underground streams are fire-clays: hence we generally find springs in great numbers issuing from the ground along the out-crops of a coal seam. A little observation will show that there is a strong tendency to system in the location of springs, and that a series of them along a certain horizon usually indicates the presence of a bed of fire-clay.*


The coal and fire-clay strata of the upper measures are so nicely distributed, and the overlying rocks so well adapted as filters, that it would be indeed difficult to find a region better watered than our own.


Limestone.—The distribution and quantity of limestone of this region have already been noted. It remains to speak briefly of their quality. The limestones of the sandstone series, are generally excellent carbonates, and make a good quality of quicklime. Their relation to the coal seams appears to hint at something of a more general use than the present limited demand for quicklime for building purposes : it suggests the use of these strata as fertilizers of the high lands ; and the time may not be far distant when our upland farmers will take the hint which nature has thus broadly thrown out. Some of the strata of the limestone series are good carbonates ; but generally they are not so pure as those of the higher formations.


Cements.—The thickness and location of the cement rocks have already been pointed oat. It is in these, perhaps more than in any other formations, that the peculiar advantages of Belmont county lie. The lower measures can, at present, produce more coal, and can put it into market cheaper than we can do. Their fire-clays are beyond comparison with ours. "In one respect only," says Dr. Newberry, can superiority be claimed for the upper coal measures over the lower, and that is in their hydraulic line. In the upper coal measures, under coal No. 9, is a stratum of hydraulic limestone, from which is manufactured a large amount of cement. proved by ample tests to be fully equal in quality to any other made in this country."—(Ohio Geol., Vol. 1I, p. 158.) It is not improbable that these two beds of cement rock—the Bellaire and the Barnesville beds—may sometime become the source of an important manufacturing industry in Belmont county ; for nowhere are these strata more easily accessible or of better quality.


Sandstone.—Sandstone is chiefly used for building purposes and for paving. Belmont county has ample supplies of sandstones well adapted to both these purposes, and more than sufficient for home use. Yet it is hardly to be expected that any considerable commerce can ever be established in the building stones of this region, in the face of the fact that the Waverly Sandstone has almost monopolized the business of supplying those cities and districts within our range, which require foreign supplies. The stratum of flagstone between Coals No. 10 and No. 11, in Goshen township, may sometime be the source of a considerably more general supply for paving purposes than at present.


The Soils.—In level countries, where the soils are not greatly varied, the range of crops is necessarily more or less limited. In Belmont county we have a great variety of soil. These soils, formed by the disintegration of the rock-strata, consist of five principal kinds: limestone, sandstone, clay, marl and alluvial lands. The lowest of these soils is, of course, the alluvial, formed along the valleys. It consists of materials washed down from the higher lands, and consequently contains almost all the


*As a hint to the young geologist, it may be remarked that coal seams may be traced all over our country by the springs and land slides of which the underground streams of their accompanying fire-clays are the cause. Dwellings, too, being often located with reference to springs, may help to enable the observer to follow the horizon of a coal bed. The author has frequently been enabled by these means to trace seams of coal for miles, while merely enjoying a pleasant drive.


HISTORY OF BELMONT AND JEFFERSON COUNTIES - 221


various elements of our rock formations. For this reason . our bottom lands' will produce almost any kind of crop that will thrive in a valley climate, and will bear farming continuously without rest for many years. The next variety of soil, limestone land, is found principally in this county, below the horizon of Coal No. 9. The crumbling nature of the great belt of Magnesian limestone of the horizon between Coals No. 8 and No. 9, sufflciently explains this fact. There are some thin belts of limestone soil along the ridges ; but, as the carbonate limestones are not easily disintegrated by the action of the weather, these belts are, as we would expect, limited : so much so, that it is not uncommon to find both limestone and sandstone soils in the same field. Sandstone soil is found in almost all the higher lands above Coal No. 9. It is best developed in the ridge sections of Warren, Goshen and the northern parts of Wayne and Somerset townships, where the sandstone belt between Coals No. 12 and No. 13 forms the surface. The timber of this horizon is varied in kind and of good quality. The oaks seem to attain greater perfection here than in any other horizon. The chestnut may be considered the characteristic tree of this formation in Belmont county, The sandstone soils are favorable to the production of almost all the common cereals, and are especially adapted to fruits, berries, and garden vegetables. They are not so favorable for corn as the limestone soils, nor so favorable to wheat as the marl lands ; but they have perhaps a wider range of productions than either of the other soils, except the alluvial; while, their higher altitudes render them much better adapted to gardening and the production of fruits. The fourth variety of soil occurs where the clay belt (see section) forms the surface. It is found in limited belts- along hillsides in the southeastern portion of the county, sometimes forming the surface of a ridge.locality over a small area ; but it has neither range nor quality to entitle it to any important place. The last kind of soil, which, for want of a better name, is here called the " marl belt," is formed by the weathering of two principal beds of red shale lying over the clay-belt, each varying from 5 to 8 feet, and separated by a deposit of sandstone shale. Where this red soil forms the surface; as it does along the ridges of Smith township, and on some of the ridges in townships west, east and south of Smith, we generally find good wheat crops : so much so that this might properly be called the wheat horizon. The soil above this belt, on the high ridges of York, Washington and Mead townships, is a compact sandstone soil.


ORES AND MINERAL DEPOSITS.


Iron.—There are some considerable deposits of iron ore in Belmont county, but no bed that pays for working at the present state of the trade : not that our ores are not good, but that others are better. There is a seam of iron-bearing limestone in Pease township, which was worked at one time, but never to any great extent. Immediately under coal No. 13, at several points, there is a stratum of black-band ore, often reaching a thickness of ten feet. The iron concretions in this formation have a good degree of purity, and world probably be used were it not for the vast stores of this mineral elsewhere over the country, so pure and so easily accesible as to defy competition. With whole mountains of excellent ore in Missouri, and vast stores, of the purest quality, in Michigan, besides goodly stores elsewhere in our own state, Belmont county seems destined to take a small part in furnishing the ores from which the world's supplies of iron are to be drawn. But in the working of the metal she stands a better show. With good smelting coal and excellent slagging limestone, both easily accessible in the same hillside, and with good railroad facilities for bringing in the ore and for putting the manufactured iron into market, she is in fine condition to demand her share of the iron industry.


Lead.—A great deal has been said as to the existence of deposits of lead in various parts of Belmont county. It is confidently alleged that lead veins were known and mined by the Indians at several points : on Brushy creek, in Wayne township ; on Piney, near Beallsville ; and in the hills along the river between Bellaire and Bridgeport. Considerable time has been spent in searching for these imaginary deposits. A few extracts from the reports of our state geologists will show how little importance should be attached to these traditions. Mr. M. C. .Read, in his report on Holmes county, says : "Almost every county has its local traditions of lead mines formerly worked by the Indians ; and the testimony is often as positive as secondhand testimony can be, pointing to a definite location from which the Indian hunters obtained their supply of this metal.. The Indians were no architects, and erected nothing deserving the name of buildings, either for residences or store-houses ; and it is probable that all these traditions have their origin in the fact that they were compelled to insure safety of all their surplus supplies by burying them in the earth. Such deposits of lead, known only to a few, and visited by stealth, would readily give rise to the traditions of lead mining."—(Ohio Geology, vol. III., p. 560.) Prof. Stevenson, in his report on Harrison county, says : "The lead tradition is strong in several localities, and one enthusiastic individual expended a good deal of time and some money in exploration, but without success. No lead, silver, zinc, tin, copper, or gold will ever be found in economical quantities among the rocks of the coal measures. Where lead has been found, it belonged to stores accumulated by the Indians and is no evidence of lead deposits in the vicinity, for lead never occurs in metallic conditions."—(Ib., p. 218.)


Petroleum.—Several oil wells have been sunk in Belmont county, but with little success. There are very evident indications of the existence of petroleum and there is nothing in the geological structure of our sedimentary rocks to contradict the theory of its existence in the Devonian strata underlying our carboniferous deposits. But it does not, as yet, appear that any part of the county lies over a belt of oil-fissures resembling that so extensively worked on Oil creek, Pennsylvania, or any of those known to exist in Ohio. Oil is supposed, by good authority, to have been distilled from the vegetable deposits of the Huron shales (a division of the Devonian formation) and to have been forced upwards by hydrostatic pressure through the crevices of the overlying rocks, and collected in the fissures along the ridges of upheaved and broken strata. "No oil is found in the horizontal rocks," says an accurate student of this subject,* "but it occurs along the disturbed and broken tilted strata." For this reason, oil belts in this locality would be expected to trend northeast and southwest, parallel with the Cincinnati axis, and the Allegheny mountains. But no such belt has yet been discovered within the county, nor any without the county which trends towards it. Slight deposits of petroleum we undoubtedly have ; but whether in paying quantities remains, as yet, to be proved. If such do occur, they would most probably occur along the line of the Quincy anticlinal, and that axis which brings coal No. 8c to the surface at Horeb church, in AN ayne township.


GEOLOGY AND MORALS.


Next to the influence of climate there is nothing which so powerfully affects the character of a people as the geological structure of the territory which they occupy. This determines their occupations, and their occupations determine their char: actor. We all recognize the difference, socially and politically, between manufacturing and agricultural districts—a difference so striking in the United States that political economists have no difficulty in tracing its influence among the causer which led to the late war—so striking as to give rise to serious apprehensionsin the minds of some philosophical statesmen as to the political future of our country. A manufacturing district, with its smoky atmosphere, its noise, its busy, bustling, floating population, now strung up to the extreme of exertion, now relaxed into the other extreme of listless, languid inaction, must necessarily have a social character and political interest widely different from those induced by the even, easy-going life of an agricultural district. Ohio has agricultural and manufacturing interests both well developed; and consequently is in a good position to maintain the balance of political power which she now holds. Both interests are well developed in Belmont county; and this it is which has given to our population the motley character which distinguishes it so widely from those parts of the state which are distinctively agricultural. Our diversity of character depends upon our diversity of occupation, our diversity of occupation upon the diversity of our geological structure; so that it may well be said of the sandstones, limestones, shales and coals of Belmont county what Newberry says of the clays which underlie the Western Reserve: "That they have not only determined the occupation of a large portion of our people, but have affected all their modes of thought and action, and they may almost be said to underlie our manners and morals as they do our farms and towns."


CURIOUS PHENOMENA.


Caves.—True caves are found only in limestone formations. The property which water contai fling carbonic dioxide possesses, of dissolving limestone, gives an easy explanation of the whole


* Prof. H. B. Cornwall in "The Popular Science Monthly," June, 1876.



224 - HISTORY OF BELMONT AND JEFFERSON COUNTIES.


theory of caves. "Such water passes down through the crevices, and along the partings and cracks in the limestones, and dissolves .away the edges and sides of the rocks, thus making, in the course of ages, large passage ways."--(Andrews.) Pseudo-caves, or caverns, often occur in sandstone formations, caused by the crumbling away of soft rock, and the consequent, falling and irregular piling of the harder rocks above. The "Cat Den," in Goshen township, lying in the sandstone horizon between coals No. 12 and No. 13, is an example of this. In the same horizon, in various parts of the southern tier of townships, there are curious results from the same cause. The "Raven Rocks," on Piney, in Wayne township, are in this same formation. For grandeur and rugged, picturesque beauty, this little glen can scarcely be excelled. All along Piney, below the "Raven Rocks," great massive fragments of sandstone, disconnected by the disintegration of the rocks. upon which they once, rested, may be seen strewn along the tops of the hills, on both sides of the creek. In Washington township, near Armstrong's Mills, the scenery of the same horizon is quite picturesque. The "Alum Rocks" in "Wayne township," and "The Devil's Tea Table" in Warren, belong to the same formation.


Concretions.—Curious shapes are sometimes formed by the gathering together of rock-substance into variously-shaped masses. The kidney-shaped masses of iron ore found in the black-band deposits, are concretions. Sometimes these are found to contain beautiful crystals of rhomb spar, or of iron pyrites, and sometimes they contain beautiful fern-leaf impressions. Limestone concretions are some times found which have the appearance of petrified turtles. "When a flattened spheroidal con- cretion was cracked after it was formed, and the cracks were subsequently filled with other material or the same, the effect is quite turtle-like."—(Dana.) Several very interesting specimens of this nature were found, a few years ago, by Mr. L. P. Bailey, of Warren township.


Petrifications.—Pieces of "petrified wood" are frequently found, in various parts of the country. These petrifications are usually silica, and are more properly called silicified wood. It is convenient to speak of them as petrifactions, but it must not be understood that the wood has actually turned to stone. The change is brought about by the slow decomposition of wood in water charged with rock-substance in solution, the particles of mineral replacing the decaying particles of wood so slowly, and in such order, that every appearance of the wood is preserved. Mounds, pictured rocks, and other curious phenomena of that class, are subjects which do not belong to the science of geology, and hence do not come within the scope of this sketch.


CONCLUSION.


Though this sketch has already exceeded the bounds originally intended, the author feels that he ought not to let it go to the public without a few words of acknowledgment of indebtedness to the various friends who have assisted in the collection of the materials which he has used. His thanks are due to Prof. Leo Lesquereux, of Columbus, for explanations and illustrations kindly furnished; to the Smithsonian Institution, Washington, D. C., for a copy of the valuable hypsometric tables of Delcros, Loomis and Guyot ; to Mr. J. B. Ryan, of the State School Commissioner's office, for copies of valuable works of the Ohio Geological Survey; to Dr. Close, of St. Clairsville; Mr. Chalkley Dawson, of Barnesville, and many other friends, for kind assistance and interest in the work. His thanks are also due to the publishers for their liberality in furnishing the means of illustration. In the preparation of the sketch free use has been made of the works of Prof. Dana, and of the excellent "Elementary Geology" of Prof. Andrews. The Ohio Reports, have been freely used as has Prof. Lesquereux' Coal Flora Atlas, recently published by the Second Pennsylvania Geological Survey.


To the readers it should be said, that the unsatisfactory character of the work is partly due to the fact that the study of our local geology is yet in its infancy. A dozen men or fewer, in a territory so large as the State of Ohio, working on limited time and still more limited appropriations, may do—and have done —a great work. But they cannot descend into the minute structure of each locality. Local observation, and that alone, can develop all the details of the science. Yet local observation is about the last step in the development of a science. We are prone to study that which is distant and curious, rather than that which is near and plain. Man learned to decipher the strange inscriptions on the tombs of Egypt long enough before he thought to read the plain handwriting of God on the coarse stone at his own doorstep. The former were strange and curious; the latter unpretensious and common—too common to attract attention—hidden by its very commonness—like the stars at noon-day, lost in light. The same silent force§ 'which wrought out the varied features of our beautiful landscapes are acting to-day. Change, perpetual change, is carved on every precipice, and written on every slope. It is the story which the breeze whispers and the little brook murmurs. It may be heard as plainly in sparkling music of 'the little cascade in the quiet dell, as in the thunders of "dread Niagara." Let us hope that these voices of nature will at length be heard and understood by all : that our beautiful out-door science may soon cease to be wholly a thing of books and schools ; and that our people, like true students of nature, may


"Find tongues in trees, books in the running brooks,

Sermons in stones, and good in everything."


St. Clairsville, O., August 13th, 1879.


CHAPTER XXI.


HISTORY OF THE TOWS AND TOWNSHIPS


OF


Belmont County.


ST. CLAIRSVILLE.


The location of St. Clairsville is on an elevated and beautiful site, overlooking a rich agricultural scope of country, undulating in surface, but very picturesque in appearance. It is on the line, of the National Road, cloven miles west of Wheeling, and one hundred and sixteen east of Columbus. Its elevation above sea level is about 1180 feet, and above the Ohio river at Bridgeport, 560 feet. It was made the seat of justice for Belmont county in 1804, Before the days of railroads it formed quite a business centre, although it yet remains an active trading point.


This town was laid out by David Newell and surveyed by Mr. Israel. The original town contained 65 acres, 2 rood, 18 perches.. In 1803, William Mathers laid out an addition of about eight acres on the south side of town. What is known as Barnes addition, on the east, was laid out August 31, 1805, by James Barnes, Notley Hays and William Brown, and contains 19 acres and 20 perches. In 1839, William Booker laid out an addition of eight lots to the west end of the town.


The founder of St. Clairsville was of Scotch extraction and migrated from Westmoreland county, Pennsylvania, along in 1795-6. Little of his history is known. Soon after the town was laid out, he (Newell) named it in honor of his cousin, who was then governor of the territory. It was locally known as Newellstown for some years, but the court records call it St. Clairsville in 1802. A sketch is herewith subjoined of the old hero after whom the town was named :


GENERAL ARTHUR ST. CLAIR


was born in Edinburgh, Sootland, in 1735. He received a classical education in one of the most celebrated universities of his native country. After completing his collegiate course he studied medicine, but being of a military turn of mind, he soon abandoned the notion of physics. Early in May, 1755, he migrated to North America with Edward Boscawen, an English Admiral, obtained a subaltern's appointment, and was with Wolfe in the storming of Quebec. After the peace of 1763 he was assigned the command of Fort Ligonier, in Pennsylvania, and received there a grant of one thousand acres. Prior to the revolutionary war he held several civil offices. At the breaking out of said war he was appointed Colonel of Continentals. Served as Brigadier General, to which rank he had been promoted at the battles of Trenton and Princeton in the winter of 1776-7. In February, 1777, he was appointed a Major General and ordered to repair to Ticonderoga, where he commanded the garrison. When Burgoyne, with more than ten thousand men,