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History of Harrison County


CHAPTER I


GEOLOGY AND NATURAL FEATURES


GENERAL GEOLOGY - SURFACE FEATURES - ALTITUDES - CREEKS - VALLEYS- DRAINAGE AND RELIEF-COAL MEASURE-OIL PRODUCTION-NATURAL GAS OF THE COUNTRY.


General geology, surface features, coal, gas and oil, are the only geological subjects this chapter will treat. For much in this chapter the author is indebted to the Ohio State Geological reports, especially those of 1908 and 1912.


Drainage and relief—As a whole, the surface of Harrison County may be said to consist of rounded, gently sloping ridges, thickly interspersed with valleys. The divide that separates the streams flowing into the Ohio River from those tributary to the Tuscarawas, lies in the eastern part of the county. It has everywhere an altitude of 1,200 feet above sea level and at a few places the hills lack but little of reaching the 1,400 foot contour. The Pennsylvania, Wheeling & Lake Erie, and Wabash railroads all tunnel through this dividing ridge. It crosses from Carroll County on the north and passes southward along the west edge of German Township ; thence across the corner of Green and into Cadiz Township. Here the water-shed swings to the southwestward, passes Cadiz, the county seat, and extends southward across the middle of Athens Township into Belmont County.


East of the main divide are the head waters of Cross and Short Creeks and tributaries of other streams which flow eastward across Jefferson or Belmont counties to the Ohio River. Most of these are characterized by a rapid fall. These valleys are rather open and are limited by rounded, gently sloping hills with only a few sand-stone cliffs here and there. The swift currents of these streams keep the channels clear of material washed in from time to time, by heavy rains and as a result they flow along much of the way on bed rock. Erosion of the valley bottoms is actively taking place and the tendency is to form deeper, more mature valleys.


The general character of westward flowing streams in the county is strikingly different from those east of the main divide. Drainage here has an aspect of maturity. The valleys are as a rule broad and have swampy bottom lands much scarred by abandoned meanders. The streams are sluggish and follow very crooked courses. It is true that bed rock is exposed along the channels in some places. but


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generally near the head-waters. Borings along the principal streams pass through much loose, sandy materials and usually find solid rock many feet below the surface of the valley. It is evident that in the past the streams flowed at a much lower level and for some reason the valleys have become partially filled with loose sandy material. The cause for this can be understood only after examining the early history of Tuscarawas River. Obstructed drainage is not a local feature confined to a few streams in Harrison County, but is characteristic of the entire drainage system of the Upper Tuscarawas period. In pre-glacial times there was no Muskingum River flowing southward across Muskingum County and the Tuscarawas waters continued southwestward past the location of Newark in a valley that is now buried by glacial drift. It is probable that the coming of the glaciers formed a dam near the site of Newark that pounded the waters of the Tuscarawas and forced them to find a new outlet over a divide to the southward past the site of Zanesville, thus forming the modern Muskingum River. This high level outlet necessitated a partial filling of the deep Tuscarawas Valley and its tributaries with loose sand, gravel and clay.

The southwestern portion of Harrison County is drained by Big Stillwater Creek and its tributaries. Little Stillwater gathers the waters of Franklin, Stock and Archer townships in the central part, while the northern tier of townships is traversed by Conotton Creek. All of these streams have a sluggish flow so characteristic of tributaries of the Tuscarawas. Little Stillwater has a fall of less than three feet to the mile in Franklin and Monroe townships. Big Stillwater Creek is remarkable for its complicated development of bends and ox-bows which are constantly changing. Near Tippecanoe the valley is somewhat constricted by a massive, clift-forming sand stone, but even here are remarkable loops and bends along the present channel. Every few rods the level meadows are interrupted by swampy sloughs that are witnesses to the wanderings of this creek over its flood plain.


The least elevation in Harrison County is along the valleys of the two Stillwater Creeks about 860 feet above sea-level at the Tuscarawas County line. As has been stated, the greatest elevation is along the divide in the eastern part of the county. One of the highest points is at Germano in the northeastern corner of the county, where the altitude is 1,366 feet. This gives a range of 506 feet for the

county.


GENERAL GEOLOGY


Rocks at the surface in Harrison County belong to the Allegheny, Conemaugh and Monongahela formations of the Pennsylvania series. The strata have a general southeastward, dip which is interrupted here and there by a few gentle anticlinal and synclinal folds. The Cadiz anticline, in the eastern part of the county, is so pronounced that it was recognized by geologists forty years ago. Its crest passes through the town of Cadiz in a northeast-southwest direction. Westward for about two miles the rocks slope rapidly, but when followed farther again resume their normal rise toward the northwest. There are other less prominent fields in the county which are sought by


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the oil and gas experts, because it has long been recognized that such structures in the rocks are favorable for the accumulation of these fuels in commercial quantities.


Since the general dip of the rocks is southeastward, the highest or youngest strata of the geologic column lies in the southeastern part of Harrison County. Here the hills have exposures of beds belonging in the Monongahela formation. When followed northwestward a few miles beyond Cadiz, the Pittsburgh coal, which is the basal member of the formation, appears only in the tops of the hills, and still farther westward the rocks are made entirely of underlying Conemaugh beds. Near the Tuscarawas County line the deepest valleys extend below the base of the Conemaugh, and a considerable thickness of underlying Allegheny strata forms the surface.


PICTURE OF OLD STANDING STONE RELIC OF THE GLACIAL PERIOD ON THE

MORAVIAN ROM) ABOUT ONE MILE NORTHWEST OF CADIZ


The Conemaugh formation covers fully two-thirds of Harrison County. The remainder is made up of Monongahela which forms a capping of the Conemaugh in the southeastern part of the county. Geologists have found the fmest exposures of the geological formations, including the Conemaugh, at points along the Pennsylvania Railway, its cuts and its tunnels ; at points in the Little Stillwater Creek ; valley of Big Stillwater Creek, and Cadiz and environments. Points much examined by scientists are at the tunnel just west of Cadiz Junction, about one mile west of Jewett another is in the immediate vicinity of Scio. There are other most interesting exposures to the west of the village of Bowerston where the railroad leaves the Conotton. valley and crosses the divide through a tunnel to Little Stillwater Creek.


PICTURE OF STEAM SHOVELS WORKING AT STRIPPING COAL IN HARRISON COUNTY


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CADIZ AND VICINITY


The village of Cadiz is near the crest on an anticline that tends northeastward across the corner of Harrison County. The town itself lies above the horizon of the Pittsburgh coal measure which outcrops in the hollows on all sides at an altitude of about 1,190 feet above sea-level. Few of the valleys to the southeastward are deep enough to uncover the Ames or "Crinoidal" limestone and the section below the coal consists mostly of sandy shale and sandstone interlain with beds of limestone and clay. Eastward to the county lines the dip of the strata is about the same as the fall of the southeastern—flowing tributaries of Short Creek. Although the same portion of the geologic column is exposed along the valleys all the way, there is an increasing sandiness in the rocks in this direction. Westward from Cadiz a few miles, along the valley of Standingstone Fork the rocks of the upper third of the Conemaugh are less sandy and the hills show a tendency to landslides.


THE COAL PRODUCTION


Of the "Pittsburgh" coal found in Harrison County, from State geologists' reports a few years ago, it is learned that the western margin of this mineral underlies the higher parts of the eastern portion of Harrison County, being found in nine townships. The seam once formed a continuous stratum over this area, that which remains being the portion which has escaped stream erosion.


Until very recently the coal was mined for local use only, for which it has had a steady demand for perhaps seventy years. About 1907 two or three mines for railroad shipment were opened, and since then much interest has been taken in the coal industry of the county.


Southward the seam extends into Belmont County and eastward into Jefferson. A few small outliers of this coal are found in the hills of Carroll County to the north.


In Short Creek Township this coal has been divided into three strips by two streams—Short Creek and Little Short Creek. The southernmost of these three strips, comprising as it does two rows extending east and west across the township, is by far the largest. The coal has not been mined in this strip except along the north side where the seam outcrops in the deep valley of Little Short Creek. Here are a number of country banks. About 1907 a railroad shipment was opened in the northeast corner of the township. In the northwestern part of the township is the well-known mine of S. P. Dunlap. For many years this coal mine was only worked winters for farm use, and a few days during the summer.


The Adena Mining Company is located in the northeastern part of this township and has a capacity of 600 tons daily (this was in 1907).


In Green Township the "Pittsburgh" seam consists of a number of long narrow strips lying near the summit of high ridges. For a long period it has been mined for local use, but in the last dozen years quite extensively.


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In German Township, in northeastern Harrison County, there is not as great an amount of this coal as in Green Township. The seam is only present in the highest hills.


In Rumley Township still less coal is found and that in the hill tops in the northeast corner of the township.


In Archer Township two high and narrow ridges cross the township from northwest to southeast. These contain a small quantity of coal of the Pittsburgh variety. A small arm of this seam extends into another Township.


Cadiz Township is situated on the divide between Stillwater and Short creeks, and contains a large quantity of coal, though generally confined to the higher ridges. The seam of "Pittsburgh" has long been worked, especially in the neighborhood of the village of Cadiz. The Glover Coal Company is an old, well-known plant and has supplied the local demand for many years, and some has been shipped out by rail.


Athens Township contains in proportion to its size more acreage of the Pittsburgh coal than any other township in Harrison County. In the southeastern part of the township it is below drainage and so is not mined. In the western part of the township, a number of farmers worked the seam and it has long been their source of obtaining their supply of fuel.


Moorefield Township, west of Athens, contains a few thousand acres of coal land lying in the high ridge country. Farmers have mined this coal for many years.


Nottingham Township contains a few small outliners of coal extending west from Cadiz Township and north from Moorefield. It is only suitable for farmer use and riot fit for commercially mined coal for general shipment.


THE MEIGGS COAL 1N HARRISON COUNTY


This seam of coal was named by Prof. C. N. Brown for Meiggs Creek which stream drains the central portion of the territory. The position of this coal seam is from 80 to 100 feet above the "Pittsburgh." While this coal is due in the hills of Jefferson and other counties as far as Lawrence County, it is only found in workable quantities in Belmont, Harrison, Monroe. Washington, Noble and Morgan counties. This coal is very inferior to the "Pittsburgh."


In Harrison County this coal seam is found suitable to work in both Short Creek and Athens townships. In Cadiz Township at several points it is also quite valuable as a mineral product and adds to the other fuel resources. Here this coal is found from seventy to ninety feet above the Pittsburgh seam.


In Athens Township this coal is very extensive. In the northwestern part it is found in the highest hills only, while in the southeastern part it is much more extensive. Being high above the drainage line it has long been worked by farmers for their own use. This seam is from two to more than four feet in thickness. It has the difficulty of making a large amount of ashes, hence not so good as

"Pittsburgh."


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In Short Creek Township small patches of the Meiggs coal seam is observed in the hill tops of the northern part of the township. To the south, however, it forms almost a continuous bed, being removed in the deeper valleys only. It makes a very hot fire, but has many ashes left.


HARRISON COUNTY MINERS' DIRECTORY-1918


Mine Name

P. 0.

Adams,. Roy H.

Anderson, R. H.

Apex Coal Company, Apex No. 1

Baker, R. M.

Bates-Williams Coal Company

Bigger, William

Boats, William R., Long View

Brown, Charles R.

Cambridge Collier Company, Majestic

Campbell, J. H.

Christopher, T. B.

Crab Orchard Mining Company, Crab Orchard

Culbertson, F. S.

Culbertson Coal Company, No. 1

Czatt, M. S. and G. M.,

Dunlap, S. P.

Fleming, G. O.

Freeport Coal Company

Freshwater, J. W., McGrew

Great Lakes Coal Mining Co., No. 1

Hamnett, James H.

Harmon Creek Coal Company, Howard

Henderson & Hennen

Hildreth, A. B., Kannel

Hine, 0. C.

Hitchcock, S. G.

Hoobler, Morris

Hopkins, V. S.

Hutson Coal Company

Jankoioiko, Stony

Kane, J. J.

Keesey, J. L.

Kerr & Son, James W.

Kuhn & Burner

Long, Robert

Love, Hartzell

McGrew, J. S.

Massillon Coal Mining Company, Rose Valley

Mills, Elias

Moore, J. D.

Morris, A. J.

Mull, Loyd B.

Cadiz

Cadiz

Germano

Cadiz

Hopedale

Cadiz

Hopedale


Blairmont

Cadiz

Cadiz

Freeport

New Athens

Adena

Bowerston

Cadiz

Jewett

Freeport

Cadiz

Bobbyville

Cadiz

Hopedale

Cadiz

Cadiz

Cadiz


Germano

Cadiz

Hopedale


Cadiz

Cadiz

Cadiz

Germano

Cadiz


Cadiz


Moorefield

Short Creek

Cadiz

Jewett


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Mine Name.

P. O.

Neff, E. J., New Briar Hill

Newton Coal & Mining Company, "Newton".

Ohio Wheeling Coal Company, No. 1

Phillips, Charles

Pickering, C. C.

Pittsburgh Block Coal Co., Kenwood

Sheets, William

Short Creek Coal Company, Nos. 1, 2, 3,

Stellar Coal Mining Company

Stillwater Mining Coal Company, "Stillwater"

Stinard, William, Bigger

Unity Coal Company, Copeton

Webb, Samuel

Webster, Jose

Tippecanoe

Bowerston

Harrisville

Cadiz

Cadiz

Blairmont

Cadiz

Adena


Tippecanoe


Jewett

New Athens

Jewett


COAL PRODUCED IN HARRISON COUNTY-1919


Tons Pick Mined

Tons Machine Mined

Tons Stripped

Total Tons

33,903

1,013,181

404,977

1,452,061


Total number mines reported in operation, 43. Thirty-four were slope mines, eight drift mines and one a shaft.


ACCIDENTS


In 1917 the total number of coal miners employed in Harrison County was 1,798; number of tons coal mined, 1,222,561 ; fatal accidents, 2; men employed per life lost, 899; tons coal mined per life lost, 611,288.


PETROLEUM AND NATURAL GAS


As seen through the eyes of writers on such topics in 1895, the following is found in a standard work on Geology of Ohio.


These subjects, especially the latter have recently acquired such wide-spread interest and importance in the country that a separate section will be given to their consideration.


The introduction of natural gas on the large scale is of comparatively recent date. It was begun in Pittsburgh and in the region around it a dozen years since (1883) but it is only within the last six years that it has made a deep impression on the country at large.


The cheapness of the new fuel, the economy resulting from several different factors m its use, the improvement of product in a number of lines of manufacture, all combine to give a decided advantage to the centers that have been fortunate enough to secure it, and to make competition seem almost hopeless to the towns that are without it.


In consequence, an earnest and eager search for natural gas has been begun throughout the entire State, and vast amounts of money have been used in carrying forward these explorations. Next


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to Western Pennsylvania, Northwestern Ohio has scored the most signal success and, following the experience of Ohio, Eastern Indiana has also found one of the most valuable fields of the country.


Harrison County, while not in the belt just mentioned, is so nearly connected that discoveries were made in the `80s and '90s of paying amounts of both oil and natural gas, which industries have been further developed until for a number of years, both of these wonderful natural mineral products have been a blessing to the county, in way of both light and heat. Pipe lines are now found trailing hither and yon throughout the domain of the county, carrying the gas by which the county seat and smaller villages are well lighted and heated. As the older or original wells become exhausted, new ones are discovered, thus keeping the supply about up to the requirements of the population. The oil industry in this county has made scores of men and women wealthy, but at present there are more dry wells than those producing oil, but the natural gas product is still one of immense magnitude and it is sanguinely believed that as time passes enough new gas wells may be struck to keep pace with the increasing demands of the county.


This county has been extensively tested for both oil and gas, and still the work goes on. In 1903 it was stated in the State reports on geology that Harrison county had pools as follows:


1. Cadiz.

2. Bricker.

3. Snyder.

4. Maxwell

5. Tewett.

6. Scio.

7. Bowerston.

8. New Philadelphia Road.

9. Plum Run.


There may be said to be two distinct groups—four in one and five in the other of the above mentioned pools.


The surface strata in Harrison County lie almost entirely in the Conemaugh or Lower Barren and the Monongahela or Upper Coal measures. Along the western side of the county the Upper Freeport or No. 7 coal, which lies just below the Lower Barren Measures, is found a short distance above drainage, while in the southeastern corner of the county, the Pittsburgh or No. 8 coal which makes the base of the Upper Productive Measure, is not far above drainage.


THE CADIZ POOL


In the summer of 1887 the Cadiz Oil & Gas Company drilled a well on the R. R. Cochran farm one mile north of the courthouse. Its cost was $1.25 per foot, including casings and all work. When the salt sand was reached a heavy flow of brine was liberated which ran from the top of the well, and the Berea sand, which was struck at a depth of 1,414 feet and was fifty feet thick, yielded neither oil or gas. But the company was not discouraged but that autumn commenced drilling a well on the farm of W. D. Rogers in the southwest quarter of section 29 Cadiz Township. Here but little gas was obtained and the well was abandoned.


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Then a preliminary survey was made in which State Geologist Edward Orton took part. Wells were drilled here and there, but no paying ones obtained.


In the fall of 1888 a new organization, the "Berea Grit Oil & Gas Company" was formed with a capital stock of $20,000 and its object was to further test the cadiz district. A dozen or more gas and oil wells were obtained within a few years. In 1901 there were eight oil and two gas wells producing in this field. This mile long pool lies in section 33 of Cadiz Township and section 27 of Green Township. The biggest thing accomplished by the company above noted was supplying Cadiz with natural gas. This gas was sold at 75 cents per 1,000 feet for fuel and $1.00 per 1,000 for illuminating purposes. Since April, 1901, there have been rival companies supplying the town with gas—the Cadiz Gas Company and the T. N. Donaldson Company, the former deriving its gas from the Fryer wells, and supplied 300 families during the winter of 1900-01, and the charges made were 25 cents a 1,000 feet after April, 1901. The second company derived its supply of gas from the Jewett field, five miles north of Cadiz. Fifty families were being served by this company in the summer of 1901.


THE BRICKER POOL


This lies wholly in the eastern part of section 30, Green Township, and in 1901 was developed only in about a half mile square. The pool was surrounded by many dry holes, hence the field cannot be productive of much more of the oil products. Oil was there discovered in October, 1899, by the Bricker Oil Company, which drilled a well on the Bricker farm. It flowed 125 barrels a day for sometime and in all 13,040 barrels were had during the first 120 days. The producing sand is the Berea. Some of these wells produce much gas and others oil to quite an extent. At first a number of these wells flowed, but later had to be pumped.


THE SNYDER POOL


This pool is located in the south half of section 20, and the northeast quarter of section 19, Green Township. In August there were twenty-five wells flowing or being pumped. The pool was discovered in the spring of 1900, the first well having been drilled on the William Croskey farm. The second site was on the Snyder farm, where twenty-five barrels daily were produced. This well is 1,512 feet deep. Many wells were sunk but comparatively few were paying propositions.


THE MAXWELL POOL


This pool lies in Shortcreek Township and is confined largely to the southwest quarter of section 21. In July, 1901, the number of producing wells was less than a dozen, Work was started here in the autumn of 1899, starting with a five barrel well. The gas present at first was sufficient to cause the oil to flow to the surface and higher.


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THE JEWETT POOL


This pool is situated in the townships of Archer, Green and Rum- ley. This was opened in the fall of 1895 on land owned by A. M. Busby on section 35 of Archer Township. From this well gas was piped to Jewett and used until the fall of 1899 when it was abandoned. A local company—the Jewett Oil & Gas Company—handled this proposition until 1896 when it was transferred to the Ohio Oil Company, which drilled and obtained other wells. July, 1901, the number of producers was seventy-five, of which eight were gas wells. At that date the companies operating there were the Ohio Oil Company, The Scott Oil Company and the F. N. Donaldson. The products of these wells find markets at Jewett, Cadiz and Scio.


THE GREAT SCIO POOL


This lies principally in North Township in sections 3, 9, 2, 33, 32, 1, 31, 26, 25, 30, 36 and 35. Also runs over into Rumley Township in sections 13, 18, 19 and 24 and passes over into Carroll County. This oil-gas field is three by five miles in extent. As early as 1872 a number of derricks were standing along the edge of the village of Scio. One of these was at the Spiker farm, and was drilled by the old-fashioned spring-pole method an entire summer having been consumed in the work. One of these wells was opened by H. A. Snyder, who twenty-five years later organized the Scio Oil & Gas Company, which opened the pool. Again another historic event was that of the well on the Spiker farm on which a well was drilled, later became one of the most valuable properties m the field, more than $540,000 worth of oil having been secured from it up to 1903. The early efforts of Spiker failed simply because they did not go deep enough.


The discovery of oil near the neighboring town of Jewett in 1895, appears to have encouraged Snyder to renew his search in the vicinity of Scio. He accordingly began taking leases for oil purposes and secured options on about 2,000 acres near the village. His next step was to organize a company to test the territory, and in March, 1898 the Scio Oil & Gas Company was incorporated with a capital stock of $10,000, divided into shares of $25 each. The people, however, had little faith in the venture, and consequently the stock did not sell rapidly. Only fifty-six shares were disposed of, and even after the first well had been drilled and oil secured, there was difficulty in inducing the stockholders to double the amount already paid. This, however, resulted more from their inability rather than from their lack of confidence in the project. After the second well had been completed the stockholders decided to double again their subscriptions, making necessary a payment of $100 for each share originally taken. The amount of money raised by the three assessments combined was $5,600. The company drilled two additional wells and put up rigs for two more, and then sold out to Myers & Brown for $100,000.


When the Scio Oil & Gas Company was organized Snyder transferred to it his leases, the consideration being 4 per cent of the oil secured and 2 per cent of the gas, after the land-holder had received his royalty. Much of the territory covered by these leases was dry,


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and other tracts were forfeited by the non-payment of rent. Nevertheless Snyder received a handsome fortune in return for his perseverance.


The first well drilled to the Berea sand in this pool was located on a small tract of land owned by Matthew Henry, situate one-fourth of a mile north of the village. The well was completed June 7, 1898 and after having been shot with eighty quarts of nitro-glycerine began producing eighteen barrels of oil per day. The second well located on land of William Donaldsons' started producing twenty-two barrels, but the necessary tanks not being at hand the well was left idle several days the tools hanging in the well. When these were removed the well began flowing, and the gas catching fire from the boiler burned the derrick. This accident was widely published, and as is usual under such circumstances, the production of the well was exaggerated. The accident attracted the attention of oil men from near and far, and started a boom which in a short time revolutionized the village.


The third well was drilled late in the fall of 1898 on a lot owned by Jacob Strayer within the corporation limits. This began producing seventy-five barrels per day, and of course added fresh fuel to the excitement. After -this, wells were completed in rapid succession and all were producers. Early in December the leasing of town lots began and wells by the score were soon drilled on them, the owners vieing with each other in their anxiety to have their property tested.


According to the gauger for the Buckeye Pipe Line the largest number of producing wells in the field was in January, 1900, when it was 850. The most the field ever has had of producing wells is 1,000. Of this large number of oil and gas wells 250 were within he corporation but in 1901 only twenty of these inside the limits were producing oil. It is believed that the reason for this failure is the fact that the wells were drilled too close together. The one on the Given lot produced, however, $30,000 worth of oil. Three were drilled on the college campus, but the royalty derived was not large. The average cost of a complete well in the field was about $3,000; 1,190 feet was the depth of many of these wells. It was in 1901 that the Standard Oil Company got control of most of the oil in this section and it was shipped to Toledo and Cleveland where it was refined.


Monroe Township from 1894 on had many wells drilled, but nearly all proved unsuccessful, but some were fair producers for a time.


Of other deep wells in Harrison County let it be stated that a dry hole on the Luther farm in section 29 of German Township ; a dry hole in section 18 on the Ralston farm; a dry hole on the Johnson farm in section 25 and three dry holes near New Jefferson in section 26, tells the story to date.


In Rumley Township, on the Crabb farm, and one on the Kimmell farm, are all of any note up to 1903.


Archer, Franklin, Stock, Moorefield, Washington, Freeport, Athens and Cadiz townships have all had many dry wells, but few of paying oil. The term "dry hole" describes a larger part of the experiments made, with now and then one marked by geologists as "producer."


In 1894 on the A. Wyant farm in Monroe Township in section 33, a hole was drilled to the depth of 3,950 feet ; it had been intended to go down 4,400 feet but the tools were lost and the work abandoned.


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Today (1920) the most of the developments in a mineral way in Harrison County consists of drilling for natural gas and coal, both of which are becoming quite numerous in the last year or two. Many farms are being stripped in places and coal taken up by means of steam shovels. Hundreds of acres are thus being stripped and the coal taken out and shipped on spurs of the various railroads. In the way of gas, all that is hoped for is to gain enough for home demand, but the coal beds of Harrison County are sufficient to afford scores of years of constant mining.