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An excellent supply of artesian water is available from the Trinity reservoir at no great depth. The first flowing well in Somervell County was drilled in 1880, and the first flowing well in Glen Rose, the county seat, was drilled in 1881. Since 1880 more than 500 wells have been constructed, probably more than half of them prior to 1900. Many of these early wells have been abandoned, either because the well hole caved in as a result of the absence or deterioration of casing or because the wells ceased to yield water by natural flow. The artesian water has always been used chiefly for domestic supply and for watering stock. Only a comparatively small area of farm land is now irrigated. The quantity used to supply the needs of tourist camps and outdoor swimming pools forms a relatively large percentage of the total amount withdrawn from the artesian reservoir in Somervell County. The artesian water is contained chiefly in the permeable sandstone beds--the basal sands for the Trinity group. Some shallow wells of small capacity are supplied by water in the crevices and solution channels in limestone that apparently is near the base of the Glen Rose formation and probably derives its water by leakage from the underlying Trinity reservoir. The wells encounter from one to three aquifers, the number depending upon their depth and location. At and around Glen Rose, the area in which most of the flowing wells are concentrated, the first aquifer is the creviced portion of the limestone, which is encountered at about 50 feet but does not everywhere yield water. The second and third aquifers, both of which are part of the 'basal sands' of the Trinity group, are much more uniform and persistent; the second is encountered at Glen Rose at depths of 100 to 135 feet, and the third at depths of about 275 to 330 feet. The artesian reservoir is supplied by water that falls as rain or snow upon the outcrop of the 'basal sands' on the higher lands west and north of Somervell County. These permeable beds dip eastward and southeastward beneath the county and are covered by the less permeable beds of the overlying Glen Rose formation. As the water that reaches the zone of saturation percolates down the dip of the beds it is confined under artesian pressure, and wells that penetrate these beds at lower altitudes yield water by natural flow. Originally the artesian pressure was sufficient to raise the water in tightly cased wells in the northwestern part of Somervell County to a maximum altitude of about 750 feet above sea level, but at Glen Rose the original artesian head was probably not more than 710 feet. From the information avail- able it would appear that the original head of the water in the upper aquifers was not nearly as great as that of the lower aquifer. The head has declined generally throughout the county. At Glen Rose in June 1930 the artesian head of the water from the deepest aquifer of the Trinity reservoir was about 639 feet above sea level, and the head of the water from the upper aquifers was about 15 feet less. The decline in head still continues, but at a very much slower rate than formerly. With the decline in head the size of the area of artesian flow has decreased, though in recent years the shrinkage has been comparatively little. The draft from the artesian reservoir in Somervell County during the summer is estimated at about 1,000,000 gallons a day, distributed as follows: Domestic use, 150,000 gallons; stock use, 60,000 gallons; recreation pools, 250,000 gallons; irrigation, 180,000 gallons; and waste, not including underground leakage, 360,000 gallons. In winter the daily draft is probably about 370,000 gallons less than in summer. The 360,000 gallons a day permitted to flow from wells without being used for any beneficial purposes is an unnecessary drain upon the artesian reservoir. The head of many of the flowing wells in Glen R
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp660","usgsCitation":"Fiedler, A.G., 1934, Artesian water in Somervell County, Texas: U.S. Geological Survey Water Supply Paper 660, iv, 86 p., https://doi.org/10.3133/wsp660.","productDescription":"iv, 86 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0660/report-thumb.jpg"},{"id":26404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0660/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c4a","contributors":{"authors":[{"text":"Fiedler, Albert George","contributorId":62192,"corporation":false,"usgs":true,"family":"Fiedler","given":"Albert","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":143592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22595,"text":"ofr6731 - 1934 - Ground-water supplies and irrigation in San Pedro Valley, Arizona","interactions":[],"lastModifiedDate":"2015-10-22T11:12:32","indexId":"ofr6731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"67-31","title":"Ground-water supplies and irrigation in San Pedro Valley, Arizona","docAbstract":"The San Pedro Valley in southeastern Arizona extends from the International Boundary northward about 120 miles to the junction of the San Pedro River with the Gila River. The river basin also extends about 75 miles into Mexico. The valley varies in width from 5 to 20 miles, being widest in its middle portion, in the vicinity of Benson. The area of the portion of the basin within the United States in about 3,770 miles.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6731","issn":"0094-9140","usgsCitation":"Bryan, K., Smith, G.E., and Waring, G., 1934, Ground-water supplies and irrigation in San Pedro Valley, Arizona: U.S. Geological Survey Open-File Report 67-31, 213 p., https://doi.org/10.3133/ofr6731.","productDescription":"213 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":155796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr6731.jpg"},{"id":310410,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","otherGeospatial":"San Pedro Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.18713378906249,\n 31.348945815579977\n ],\n [\n -111.18713378906249,\n 33.293803558346596\n ],\n [\n -109.51171875,\n 33.293803558346596\n ],\n [\n -109.51171875,\n 31.348945815579977\n ],\n [\n -111.18713378906249,\n 31.348945815579977\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a5c1","contributors":{"authors":[{"text":"Bryan, Kirk","contributorId":37308,"corporation":false,"usgs":true,"family":"Bryan","given":"Kirk","email":"","affiliations":[],"preferred":false,"id":188535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, G. E. P.","contributorId":63046,"corporation":false,"usgs":true,"family":"Smith","given":"G.","email":"","middleInitial":"E. P.","affiliations":[],"preferred":false,"id":188536,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waring, Gerald A.","contributorId":88341,"corporation":false,"usgs":true,"family":"Waring","given":"Gerald A.","affiliations":[],"preferred":false,"id":188537,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4549,"text":"wsp738 - 1934 - Surface water supply of the United States 1932 : Part 12, North Pacific drainage basins ; B. Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:51","indexId":"wsp738","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"738","title":"Surface water supply of the United States 1932 : Part 12, North Pacific drainage basins ; B. Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp738","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1934, Surface water supply of the United States 1932 : Part 12, North Pacific drainage basins ; B. Snake River basin: U.S. Geological Survey Water Supply Paper 738, vii, 197 p. ;24 cm., https://doi.org/10.3133/wsp738.","productDescription":"vii, 197 p. ;24 cm.","costCenters":[],"links":[{"id":139799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0738/report-thumb.jpg"},{"id":31606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0738/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698084","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528247,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3351,"text":"cir6 - 1934 - Mineral-water supply of the Mineral Wells area, Texas","interactions":[],"lastModifiedDate":"2019-05-10T08:54:56","indexId":"cir6","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1934","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"6","title":"Mineral-water supply of the Mineral Wells area, Texas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir6","usgsCitation":"Turner, S.F., 1934, Mineral-water supply of the Mineral Wells area, Texas: U.S. Geological Survey Circular 6, 15 p., https://doi.org/10.3133/cir6.","productDescription":"15 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":363657,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0006/report-thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.2781982421875,\n 32.675794797699766\n ],\n [\n -97.99598693847655,\n 32.675794797699766\n ],\n [\n -97.99598693847655,\n 32.88420028540548\n ],\n [\n -98.2781982421875,\n 32.88420028540548\n ],\n [\n -98.2781982421875,\n 32.675794797699766\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7473","contributors":{"authors":[{"text":"Turner, Samuel Foster","contributorId":26287,"corporation":false,"usgs":true,"family":"Turner","given":"Samuel","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":146705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221684,"text":"70221684 - 1934 - Relation of stream‐flow to ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-28T17:37:08.351486","indexId":"70221684","displayToPublicDate":"1934-06-01T12:31:54","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Relation of stream‐flow to ground‐water levels","docAbstract":"In recent years the Water Resources Branch of the United States Geological Surrey has given considerable attention to the relation of ground‐water to stream‐flow. One locality in which this relation is being studied is about 13 miles from Washington, near Colesvllle, Maryland, where a Kinnison float‐gage is being maintained in a well In connection with the operation of a gaging‐station on the Northwest Branch of the Anacostia River. The well is opposite the gaging‐station, on a gentle slope about one. fifth of a mile from the stream, where the land‐surface ia about 20 feet above the bed of the stream. The well is an abandoned dug well 20 feet deep and is lined with loose stone and presumably admits water freely. The fluctuations of the water‐level in the well are believed to afford a fairly close index of fluctuations in the water‐table at the well‐site and may be typical of the fluctuations that occur in a large part of the area drained by the Northwest Branch above the gaging‐station, consisting of about 21 square miles of gently rolling farm‐land. During the period of the observations herein considered the water‐level in the well ranged from 10 to 16 feet below the ground‐surface at the well and from 10 to 4 feet above the bed of the stream.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00414","usgsCitation":"Harrold, L., 1934, Relation of stream‐flow to ground‐water levels: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 414-416, https://doi.org/10.1029/TR015i002p00414.","productDescription":"3 p.","startPage":"414","endPage":"416","costCenters":[],"links":[{"id":386811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","city":"Colesville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77.02136993408203,\n 39.06264886527909\n ],\n [\n -76.98051452636719,\n 39.06264886527909\n ],\n [\n -76.98051452636719,\n 39.08397168286113\n ],\n [\n -77.02136993408203,\n 39.08397168286113\n ],\n [\n -77.02136993408203,\n 39.06264886527909\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Harrold, L.L.","contributorId":260661,"corporation":false,"usgs":false,"family":"Harrold","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":818424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221683,"text":"70221683 - 1934 - A study of salt‐water encroachment in the Galveston Area, Texas","interactions":[],"lastModifiedDate":"2021-06-28T17:23:06.351397","indexId":"70221683","displayToPublicDate":"1934-06-01T12:18:04","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"A study of salt‐water encroachment in the Galveston Area, Texas","docAbstract":"A survey of the ground‐water resources of the region in which Houston and Galveston are situated was started in December 1930 by the United States Geological Survey in cooperation with the Texas Board of Water Engineers. In connection with this survey a special study is being made of the geochemical relations of the ground‐waters of an area about 25 miles wide and 90 miles long, extending from Galveston northwestward through Houston. This study considers the influence on the ground‐waters of the age and degree of weathering of the outcrop formations, base‐exchange materials, salt‐domes, and salt‐water encroachment. In this paper, however, attention is confined to salt‐water encroachment along the line from Galveston to Houston (Fig. 1).
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00432","usgsCitation":"Turner, S., and Foster, M.D., 1934, A study of salt‐water encroachment in the Galveston Area, Texas: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 432-435, https://doi.org/10.1029/TR015i002p00432.","productDescription":"4 p.","startPage":"432","endPage":"435","costCenters":[],"links":[{"id":386810,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","city":"Galveston","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.8175048828125,\n 29.439597566602902\n ],\n [\n -95.0372314453125,\n 29.216904948184734\n ],\n [\n -95.29541015625,\n 28.9913248161703\n ],\n [\n -95.25146484374999,\n 28.926439238621036\n ],\n [\n -94.69390869140625,\n 29.26962881522664\n ],\n [\n -94.47143554687499,\n 29.470687864832556\n ],\n [\n -94.50164794921875,\n 29.537619205973428\n ],\n [\n -94.8175048828125,\n 29.439597566602902\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Turner, Samuel F.","contributorId":23982,"corporation":false,"usgs":true,"family":"Turner","given":"Samuel F.","affiliations":[],"preferred":false,"id":818422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, Margaret D.","contributorId":21141,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":818423,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221680,"text":"70221680 - 1934 - Report of the committee on underground‐water, 1933–34","interactions":[],"lastModifiedDate":"2021-06-28T16:41:37.218356","indexId":"70221680","displayToPublicDate":"1934-06-01T11:39:10","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the committee on underground‐water, 1933–34","docAbstract":"The by‐laws adopted at the meeting of the Section of Hydrology in 1933 provided that the membership of research committees should be reconstituted every three years. There have, accordingly, been some changes in the membership of the Committee on Underground‐Water. Certain members have retired because of pressure of other duties or because they are no longer actively engaged in ground‐water work. Dr. O. E. Meinzer, who retired as Chairman of the Section of Hydrology, has agreed to serve on the Committee, and probably two or three other men will be appointed to make contact with special phases of the field covered by the Committee. It is with regret that the Chairman reports the loss to the Committee by the death of A. F. Melcher, who had contributed much to the science of ground‐water hydrology by his studies on permeability and absorption of sedimentary formations for water, oil, and gas. ©1934
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00312","usgsCitation":"Thompson, D.G., 1934, Report of the committee on underground‐water, 1933–34: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 312-316, https://doi.org/10.1029/TR015i002p00312.","productDescription":"5 p.","startPage":"312","endPage":"316","costCenters":[],"links":[{"id":386806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221679,"text":"70221679 - 1934 - The transmission of pressure in artesian aquifers","interactions":[],"lastModifiedDate":"2021-06-28T16:37:27.430459","indexId":"70221679","displayToPublicDate":"1934-06-01T11:34:13","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The transmission of pressure in artesian aquifers","docAbstract":"The water in artesian aquifers is confined under pressure. Under ideal conditions in a perfectly rigid artesian reservoir a change of pressure in one part of the reservoir should produce a corresponding change of pressure in all other parts of the reservoir. Theoretically, the transmission of pressure should take place rapidly and without any movement of water other than the small amount resulting from the compressibility of water. However, observations under natural conditions show that the transmission of pressure is not always rapid and that the rate of transmission appears to be determined in great part by the distance traversed and the magnitude of the change of pressure. There are many reasons for believing that artesian aquifers and their confining beds are not perfectly rigid but that they are elastic and capable of compression and dilation (O. E. Meinzer, Compressibility and elasticity of artesian aquifers, Econ. Geol., v. 23, pp. 263–291, 1928). This appears to be the cause of the lack of rapidity of transmission of pressure in artesian aquifers.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00409","usgsCitation":"Leggette, R., and Taylor, G., 1934, The transmission of pressure in artesian aquifers: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 409-413, https://doi.org/10.1029/TR015i002p00409.","productDescription":"5 p.","startPage":"409","endPage":"413","costCenters":[],"links":[{"id":386804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":818416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":818417,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221673,"text":"70221673 - 1934 - Appendix A—permeability","interactions":[],"lastModifiedDate":"2021-06-28T15:56:06.937317","indexId":"70221673","displayToPublicDate":"1934-06-01T10:52:41","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix A—permeability","docAbstract":"In the paper entitled “The measurement of the permeability of porous media for homogeneous fluids” by R. D. Wyckoff and others [42] a unit of permeability is proposed which is based on centimeters, seconds, and atmospheres of pressure (76 centimeters of mercury).
In 1923, when the Hydrologic Laboratory of the United States Geological Survey was organized, much study was given to the question of a coefficient of permeability, and a coefficient was adopted which is based on feet and gallons a day (U.S. Geol. Survey Water-Supply Paper 596, p. 148). This coefficient has been extensively used and has proved very satisfactory in ground-water work. It has the merit of being readily applicable to field-conditions. It is, moreover, of convenient size, the coefficients of most water-bearing materials being integers of two or three figures, that is, between 10 and 1000. It was adopted in place of Slichter's “transmission-constant” (U.S. Geol. Survey Water-Supply Paper 67, p. 27, 1902), after much careful consideration, largely because the “transmission-constant” of most water-bearing materials is inconvenient in being only a small decimal.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00316","usgsCitation":"Meinzer, O.E., 1934, Appendix A—permeability: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 316-317, https://doi.org/10.1029/TR015i002p00316.","productDescription":"2 p.","startPage":"316","endPage":"317","costCenters":[],"links":[{"id":386798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221672,"text":"70221672 - 1934 - Report of the committee on chemistry of natural waters, 1933–34","interactions":[],"lastModifiedDate":"2021-06-28T15:51:28.732707","indexId":"70221672","displayToPublicDate":"1934-06-01T10:48:13","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the committee on chemistry of natural waters, 1933–34","docAbstract":"The personnel of this Committee during the past year, practically the same as during the previous year, has been as follows: C. S. Howard, Chairman—United States Geological Survey, Washington, D.C. L. C. Case—Gypsy Oil Company, Tulsa, Oklahoma. W. D. Collins—United States Geological Survey, Washington, D.C. H. F. Flynn—United States Engineer Office, 35 South Ninth Street, Philadelphia, Pennsylvania. W. P. Kelley—University of California, Riverside, California. Alfred C. Lane—Tufts College, Tufts College, Massachusetts. Augustus Locke—477 Mills Building, San Francisco, California. R. D. Leitch—United States Bureau of Mines, Pittsburgh, Pennsylvania. H. T. Logan—United States Bureau of Standards, Washington, D.C. Thomas S. Lovering—United States Geological Survey, Washington, D.C. Thomas E. Means—111 Sutter Street, San Francisco, California. F. B. Plummer—University of Texas, Austin, Texas. J. W. Sale—United States Food and Drug Administration, Washington, D.C. C S. Scofield—Bureau of Plant Industry, Department of Agriculture, Washington, D.C. Thomas G. Thompson—University of Washington, Seattle, Washington.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00322-2","usgsCitation":"Howard, C.S., 1934, Report of the committee on chemistry of natural waters, 1933–34: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 322-325, https://doi.org/10.1029/TR015i002p00322-2.","productDescription":"4 p.","startPage":"322","endPage":"325","costCenters":[],"links":[{"id":386797,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":818402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221668,"text":"70221668 - 1934 - Appendix C—A selected list of papers relating to ground‐water hydrology","interactions":[],"lastModifiedDate":"2021-06-29T14:00:10.563864","indexId":"70221668","displayToPublicDate":"1934-06-01T09:04:11","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix C—A selected list of papers relating to ground‐water hydrology","docAbstract":"In the following list brief statements have been added to certain references to call attention to special phases of ground‐water problems which are not apparent from the titles. Abstracts of most of these papers have been or will be published in the Annotated Bibliography of Economic Geology.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00318","usgsCitation":"Sayre, A., 1934, Appendix C—A selected list of papers relating to ground‐water hydrology: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 318-320, https://doi.org/10.1029/TR015i002p00318.","productDescription":"3 p.","startPage":"318","endPage":"320","costCenters":[],"links":[{"id":386848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":818496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221667,"text":"70221667 - 1934 - Appendix B—Lake and ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-28T14:02:22.088463","indexId":"70221667","displayToPublicDate":"1934-06-01T08:58:02","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix B—Lake and ground‐water levels","docAbstract":"An outstanding achievement of the Section of Hydrology has been the work of the Committee on Glaciers in assembling the existing records of the advance and retreat of the glaciers in the Western States and in Alaska, encouraging various agencies in making periodic observations, systematizing and standardizing the work, and providing for the compilation and preservation of the data obtained from year to year.
The fluctuation of lake levels is a closely related subject that is equally fundamental in the study of hydrology. In 1922 I published a map giving the distribution of 68 Pleistocene lakes in the Basin and Range province and showed that the desiccation of these lakes could have been caused by change in temperature as well as change in precipitation (Geol. Soc. Amer. Bull., v. 33. pp. 541–552. 1922). Abundant and convincing evidences of changes in climate in the Pleistocene epoch or at its end are afforded both by the ancient drift-sheets and by the ancient lake features, but the question as to the relative importance of changes in temperature and changes in precipitation is still very obscure.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00317","usgsCitation":"Meinzer, O.E., 1934, Appendix B—Lake and ground‐water levels: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 317-318, https://doi.org/10.1029/TR015i002p00317.","productDescription":"2 p.","startPage":"317","endPage":"318","costCenters":[],"links":[{"id":386792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"western United States and Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -166.46484375,\n 57.51582286553883\n ],\n [\n -135.87890625,\n 57.51582286553883\n ],\n [\n -135.87890625,\n 70.72897946208789\n ],\n [\n -166.46484375,\n 70.72897946208789\n ],\n [\n -166.46484375,\n 57.51582286553883\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -125.5078125,\n 32.84267363195431\n ],\n [\n -109.3359375,\n 32.84267363195431\n ],\n [\n -109.3359375,\n 48.80686346108517\n ],\n [\n -125.5078125,\n 48.80686346108517\n ],\n [\n -125.5078125,\n 32.84267363195431\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. 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Fish pathologists have contributed a great deal to our knowledge of fish diseases, but there is still much to be learned, particularly concerning better methods of preventing and eliminating diseases among our trout. In this era of circular pools and raceways, our disease elimination is way back in the early days of standard troughs.","language":"English","publisher":"American Fisheries Society","publisherLocation":"Bethesda, MD","doi":"10.1577/1548-8659(1933)63[158:TCDOTP]2.0.CO;2","usgsCitation":"Fish, F.F., 1933, The chemical disinfection of trout ponds: Transactions of the American Fisheries Society, v. 63, no. 1, p. 158-163, https://doi.org/10.1577/1548-8659(1933)63[158:TCDOTP]2.0.CO;2.","productDescription":"6 p.","startPage":"158","endPage":"163","numberOfPages":"6","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":258324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258308,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8659(1933)63[158:TCDOTP]2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa2ae4b08c986b322737","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":355424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45317,"text":"b836C - 1933 - Mineral resources of Alaska, report on progress of investigations in 1930. Surface water supply of southeastern Alaska, 1909-1930","interactions":[],"lastModifiedDate":"2012-02-02T00:10:13","indexId":"b836C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1933","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"836","chapter":"C","title":"Mineral resources of Alaska, report on progress of investigations in 1930. Surface water supply of southeastern Alaska, 1909-1930","language":"ENGLISH","doi":"10.3133/b836C","usgsCitation":"Henshaw, F., 1933, Mineral resources of Alaska, report on progress of investigations in 1930. Surface water supply of southeastern Alaska, 1909-1930: U.S. Geological Survey Bulletin 836, 137-218 p., https://doi.org/10.3133/b836C.","productDescription":"137-218 p.","costCenters":[],"links":[{"id":113975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0836c/report.pdf","size":"7223","linkFileType":{"id":1,"text":"pdf"}},{"id":170328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0836c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b7b2","contributors":{"authors":[{"text":"Henshaw, F.F.","contributorId":41805,"corporation":false,"usgs":true,"family":"Henshaw","given":"F.F.","email":"","affiliations":[],"preferred":false,"id":231414,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}