{"pageNumber":"2716","pageRowStart":"67875","pageSize":"25","recordCount":69037,"records":[{"id":70212782,"text":"70212782 - 1937 - The use of resistivity‐methods in the location of salt‐water bodies in the El Paso, Texas, Area","interactions":[],"lastModifiedDate":"2021-10-22T19:39:20.628529","indexId":"70212782","displayToPublicDate":"1937-08-27T13:57:10","publicationYear":"1937","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 use of resistivity‐methods in the location of salt‐water bodies in the El Paso, Texas, Area","docAbstract":"

During 1935 and 1936 the Ground‐Water Division of the United States Geological Survey made an investigation of the ground‐water resources of the El Paso, Texas, Area. Geological and hydrological studies comprised the principal part of the investigation, and these studies were supplemented by measurements of earth‐resistivity made largely by the Geophysical Section of the Geological Survey along traverses aggregating 51 miles. The extent to which resistivity‐methods may be useful in ground‐water work has been the subject of much discussion. A full evaluation of the method can not be made at this time. However, the work in the El Paso Area indicates that the presence of faults and of underground bodies of salt water may be definitely determined by resistivity‐measurements.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00393","usgsCitation":"Sayre, A., and Stephenson, E., 1937, The use of resistivity‐methods in the location of salt‐water bodies in the El Paso, Texas, Area: Eos, Transactions, American Geophysical Union, no. 18, p. 393-398, https://doi.org/10.1029/TR018i002p00393.","productDescription":"6 p.","startPage":"393","endPage":"398","costCenters":[],"links":[{"id":377956,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"El Paso","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.41048431396484,\n 31.74977366876081\n ],\n [\n -106.32362365722656,\n 31.74977366876081\n ],\n [\n -106.32362365722656,\n 31.803476141595862\n ],\n [\n -106.41048431396484,\n 31.803476141595862\n ],\n [\n -106.41048431396484,\n 31.74977366876081\n ]\n ]\n ]\n }\n }\n ]\n}","issue":"18","edition":"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":825605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephenson, E.L.","contributorId":98382,"corporation":false,"usgs":true,"family":"Stephenson","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":797458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70212780,"text":"70212780 - 1937 - Ground‐water in Utah","interactions":[],"lastModifiedDate":"2020-08-27T18:28:31.097458","indexId":"70212780","displayToPublicDate":"1937-08-27T13:18:40","publicationYear":"1937","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":"Ground‐water in Utah","docAbstract":"

In common with many of the arid and semiarid States, the prosperity of Utah probably is more dependent upon the amount of water available than upon any other natural resource. Although only about four per cent of the State is irrigated, a shortage of water for irrigation becomes a major calamity. A large part of the water‐supply for the State is derived from surface‐streams, but a most valuable supplement to this supply is the water available from underground sources. Ground‐water is used extensively for domestic, stock‐watering, and industrial purposes as well as for irrigation. The primary source of the municipal water‐supply for Salt Lake City is from streams entering the Jordan River Valley from the western slope of the Wasatch Mountains. However, since the drought‐year of 1931, a supplementary municipal supply has been obtained from ground‐water, and, among the 17 wells developed by the City during the extreme drought of 1934, one—yielding about ten cubic feet per second, or 4500 gallons a minute—is probably the largest in the State. Ogden, the second largest city in Utah, with a population of about 40,000, obtains the major part of its municipal water‐supply from a group of artesian wells in Ogden Valley about 12 miles east of the City. A considerable part of the water‐supply for the City of Brigham is obtained from wells. Springs constitute the source of most of the water‐supply for Logan, Provo, and many smaller towns and localities in the State. In nearly every developed area of the State ground‐water is used for some purpose, and in some areas the water‐supply is obtained almost entirely from wells.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00536","usgsCitation":"Taylor, G.H., 1937, Ground‐water in Utah: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 536-541, https://doi.org/10.1029/TR018i002p00536.","productDescription":"6 p.","startPage":"536","endPage":"541","costCenters":[],"links":[{"id":377954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Ground Water Provinces","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.84033203125,\n 38.272688535980976\n ],\n [\n -113.51074218749999,\n 37.3002752813443\n ],\n [\n -112.3681640625,\n 37.64903402157866\n ],\n [\n -111.29150390625,\n 39.977120098439634\n ],\n [\n -109.423828125,\n 40.12849105685408\n ],\n [\n -110.74218749999999,\n 40.64730356252251\n ],\n [\n -111.4453125,\n 40.863679665481676\n ],\n [\n -111.15966796875,\n 41.95131994679697\n ],\n [\n -113.99414062499999,\n 41.78769700539063\n ],\n [\n -113.84033203125,\n 40.730608477796636\n ],\n [\n -112.8076171875,\n 40.16208338164617\n ],\n [\n -113.13720703125,\n 39.13006024213511\n ],\n [\n -113.84033203125,\n 38.272688535980976\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Taylor, George H.","contributorId":24386,"corporation":false,"usgs":true,"family":"Taylor","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":797455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212777,"text":"70212777 - 1937 - Extraordinary topaz‐replacement body in the Brewer Mine, South Carolina","interactions":[],"lastModifiedDate":"2020-08-28T12:46:30.919473","indexId":"70212777","displayToPublicDate":"1937-08-27T13:00:29","publicationYear":"1937","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":"Extraordinary topaz‐replacement body in the Brewer Mine, South Carolina","docAbstract":"

A large body of massive topaz forms a part of the gold‐bearing lode at the Brewer Mine, South Carolina. This gold‐mine was opened 100 years ago and merits the distinction of being one of the early gold‐discoveries of the Southern Appalachian Region. The Brewer Mine is located near Jefferson, in Chesterfield County, near the northern boundary of South Carolina, and on the eastern edge of the Piedmont Province.

The country rock is described by J. T. Pardee and C. F. Park, Jr., (Gold‐deposits of the Southern Appalachians, U. S. Geol. Surv. Prof. Paper, in preparation) as a quartz‐sericite schist that locally preserves the structure of a fine‐grained, waterlaid tuff, probably a rhyolite,from which it was derived. Exposures of granite that intrude the schist appear on the north and west at distances of a mile to a mile and a half.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i001p00243","usgsCitation":"Glass, J.J., 1937, Extraordinary topaz‐replacement body in the Brewer Mine, South Carolina: Eos, Transactions, American Geophysical Union, v. 18, no. 1, p. 243-246, https://doi.org/10.1029/TR018i001p00243.","productDescription":"4 p.","startPage":"243","endPage":"246","costCenters":[],"links":[{"id":377976,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Jefferson","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.42953491210938,\n 34.616256875628956\n ],\n [\n -80.34576416015625,\n 34.616256875628956\n ],\n [\n -80.34576416015625,\n 34.6704879985043\n ],\n [\n -80.42953491210938,\n 34.6704879985043\n ],\n [\n -80.42953491210938,\n 34.616256875628956\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Glass, Jewell J.","contributorId":106948,"corporation":false,"usgs":true,"family":"Glass","given":"Jewell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":797453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212775,"text":"70212775 - 1937 - Appendix A—A selected list of papers relating to ground‐water hydrology","interactions":[],"lastModifiedDate":"2020-08-27T17:31:16.707426","indexId":"70212775","displayToPublicDate":"1937-08-27T12:24:01","publicationYear":"1937","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—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 the papers have been or will be published in the Annotated Bibliography of Economic Geology.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00325","usgsCitation":"Sayre, A.N., 1937, Appendix A—A selected list of papers relating to ground‐water hydrology: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 325-328, https://doi.org/10.1029/TR018i002p00325.","productDescription":"4 p.","startPage":"325","endPage":"328","costCenters":[],"links":[{"id":377946,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, Albert Nelson","contributorId":83102,"corporation":false,"usgs":true,"family":"Sayre","given":"Albert","email":"","middleInitial":"Nelson","affiliations":[],"preferred":false,"id":797449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212774,"text":"70212774 - 1937 - Amount of ground‐water recharge in the southern High Plains","interactions":[],"lastModifiedDate":"2020-08-27T17:11:47.399447","indexId":"70212774","displayToPublicDate":"1937-08-27T12:02:29","publicationYear":"1937","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":"Amount of ground‐water recharge in the southern High Plains","docAbstract":"

For the last six years the United States Geological Survey, in cooperation with the State Engineer of New Mexico, has been making somewhat intensive studies of ground‐water in the part of the High Plains that lies in New Mexico, and in 1933 and 1934 the Geological Survey, with funas allocated by the Public Works Administration, made an extensive reconnaissance‐survey of the ground‐water conditions in the southern High Plains. These studies have resulted in considerable data that throw much light on the quantity of recharge to the ground‐water in this area. An estimate of the quantity of recharge is of immediate value for this area, because the use of ground‐water is constantly being increased. In addition, it has a general value in serving as a criterion for estimating recharge in other areas in the Southwest for which fewer data are available. Estimates of the recharge in the High Plains as previously made without the advantage of quantitative data have ranged from less than three or four inches a year [see 1 of “References” at end of paper] to less than six inches [2]. The work of the last few years indicates they should be greatly reduced.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00564","usgsCitation":"Theis, C.V., 1937, Amount of ground‐water recharge in the southern High Plains: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 564-568, https://doi.org/10.1029/TR018i002p00564.","productDescription":"5 p.","startPage":"564","endPage":"568","costCenters":[],"links":[{"id":377945,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas, Oklahoma, Texas","otherGeospatial":"Southern High Plains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.623046875,\n 30.826780904779774\n ],\n [\n -97.119140625,\n 30.826780904779774\n ],\n [\n -97.119140625,\n 39.90973623453719\n ],\n [\n -103.623046875,\n 39.90973623453719\n ],\n [\n -103.623046875,\n 30.826780904779774\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":797448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212735,"text":"70212735 - 1937 - The value of geophysical methods in ground‐water studies","interactions":[],"lastModifiedDate":"2021-03-16T20:58:10.592291","indexId":"70212735","displayToPublicDate":"1937-08-26T16:19:40","publicationYear":"1937","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 value of geophysical methods in ground‐water studies","docAbstract":"

Two meanings are unfortunately given to the term geophysics. In the broad sense, based on the etymology of the term, geophysics means the physics of the Earth. This is its significance in the names “Geophysical Laboratory of the Carnegie Institution of Washington,” “International Union of Geodesy and Geophysics,” and “American Geophysical Union.” In this sense the sciences of geology and hydrology are largely geophysics, although in part they are geochemistry or biology. Geologists and hydraulic engineers who are elected to membership in the American Geophysical Union are, however, often surprised to find that they are regarded as “geophysicists.” I hope that when the Union establisnes a journal, its name will include the expression “Earth physics” or “Physics of the Earth,” in order that there will be no misunderstanding as to its scope.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00385","usgsCitation":"Meinzer, O.E., 1937, The value of geophysical methods in ground‐water studies: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 385-387, https://doi.org/10.1029/TR018i002p00385.","productDescription":"3 p.","startPage":"385","endPage":"387","costCenters":[],"links":[{"id":377920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","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":797375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212734,"text":"70212734 - 1937 - The mutual interference of artesian wells on Long Island, New York","interactions":[],"lastModifiedDate":"2020-08-26T21:18:32.579474","indexId":"70212734","displayToPublicDate":"1937-08-26T15:59:58","publicationYear":"1937","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 mutual interference of artesian wells on Long Island, New York","docAbstract":"

The withdrawal of water from a well necessarily produces a drop in water‐level in the well. The ground‐water level in the vicinity of the well from which the water is withdrawn likewise declines, but the amount of decline decreases with increasing distance from the well, so that a cone of depression of the water‐surface in the vicinity of the well is produced. The cone of depression is an actual water‐surface if the ground‐water is not confined under pressure. If the ground‐water is under artesian pressure, the cone of depression is a depression in the piezometric surface. If the cones of depression of two or more wells ending in the same formation overlap, interference of the wells occurs. In this case (the combined yield of the wells when pumped simultaneously will be less than the sum of the individual yields if the wells are pumped separately. In choosing the proper spacing of wells from the operator's point of view, it is important to know the lateral extent of the cones of depression of supply‐wells ending in a given formation. In many installations two or more wells are so closely spaced that their mutual interference is excessive.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00490","usgsCitation":"Leggette, R., 1937, The mutual interference of artesian wells on Long Island, New York: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 490-494, https://doi.org/10.1029/TR018i002p00490.","productDescription":"5 p.","startPage":"490","endPage":"494","costCenters":[],"links":[{"id":377919,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","county":"Kings, Nassau, Queens","otherGeospatial":"Western Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.02484893798827,\n 40.68584503000698\n ],\n [\n -74.05918121337889,\n 40.64209354784049\n ],\n [\n -74.04956817626952,\n 40.606654663050506\n ],\n [\n -74.00287628173827,\n 40.552417649142086\n ],\n [\n -73.91635894775389,\n 40.52110706370053\n ],\n [\n -73.73233795166014,\n 40.562851259102025\n ],\n [\n -73.61286163330077,\n 40.559721346848406\n ],\n [\n -73.42884063720702,\n 40.58162765924272\n ],\n [\n -73.34506988525389,\n 40.606654663050506\n ],\n [\n -73.51673126220702,\n 40.942564441333296\n ],\n [\n -73.74332427978513,\n 40.88444793903562\n ],\n [\n -73.78452301025389,\n 40.82004508671653\n ],\n [\n -73.80374908447264,\n 40.79613778833381\n ],\n [\n -73.85318756103514,\n 40.79925662005228\n ],\n [\n -73.86417388916014,\n 40.77846164090358\n ],\n [\n -73.90262603759764,\n 40.79197911810959\n ],\n [\n -73.93558502197264,\n 40.783660996197945\n ],\n [\n -73.96854400634764,\n 40.74621655456364\n ],\n [\n -73.96751403808592,\n 40.72358364851732\n ],\n [\n -73.98090362548827,\n 40.7066689811733\n ],\n [\n -74.02484893798827,\n 40.68584503000698\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"18","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":797374,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212733,"text":"70212733 - 1937 - Report of the committee on chemistry of natural waters, 1936–37 ","interactions":[],"lastModifiedDate":"2020-08-26T20:58:04.302743","indexId":"70212733","displayToPublicDate":"1937-08-26T15:56:12","publicationYear":"1937","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, 1936–37 ","docAbstract":"

The membership of this Committee is as follows: C. S. Howard, Chairman, U. S. Geological Survey, Washington, D.C.

D. G. Thompson, U. S. Geological Survey, Washington, D.C.

A. C. Lane, 22 Arlington Street, Cambridge, Massachusetts

C. S. Scofield, Bureau of Plant Industry, U. S. Dept. Agri., Washington, D. C.

I. A. Denison, U.S. Bureau of Standards, Washington, D.C.

T. G. Thompson, University of Washington, Seattle, Washington

W. P. Kelley, Citrus Experiment Station, Riverside, California

In order to provide for close cooperation between the work of the different research‐committees of the American Geophysical Union it was decided to have the chairmen of certain committees serve on other committees. The Chairman of the Committee on the Chemistry of Natural Waters is serving on the Committee of Underground waters and D. G. Thompson as Chairman of the Committee on Underground Waters is serving on the Committee on Chemistry of Natural Waters

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00342","usgsCitation":"Howard, C.S., 1937, Report of the committee on chemistry of natural waters, 1936–37 : Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 342-343, https://doi.org/10.1029/TR018i002p00342.","productDescription":"2 p.","startPage":"342","endPage":"343","costCenters":[],"links":[{"id":377917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","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":797373,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212732,"text":"70212732 - 1937 - Report of the committee on underground waters, 1936–37","interactions":[],"lastModifiedDate":"2021-04-02T14:32:30.962811","indexId":"70212732","displayToPublicDate":"1937-08-26T15:47:12","publicationYear":"1937","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 waters, 1936–37","docAbstract":"

In accordance with the by‐laws of the Section, the Committee on Underground Waters has been reconstituted during the past year. With their research interests turning to other subjects, several members have dropped out, and four new men have been appointed. In order to maintain contact with the work of related committees, Charles H. Lee, Chairman of the Committee on Absorption and Transpiration, and C. S. Howard, Chairman of the Committee on Cnemistry of Natural Waters, have become members of the Committee on Underground Waters. The personnel of the Committee is as follows: H. F. Blaney C. S. Howard M. M. Leighton H. E. Simpson G. M. Fair F. H. Lahee O. E. Meinzer A. C. Swinnerton Willard Gardner C. H. Lee A. M. Piper D. G. Thompson, Chairman.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR018i002p00318","usgsCitation":"Thompson, D.G., 1937, Report of the committee on underground waters, 1936–37: Eos, Transactions, American Geophysical Union, v. 18, no. 2, p. 318-325, https://doi.org/10.1029/TR018i002p00318.","productDescription":"7 p.","startPage":"318","endPage":"325","costCenters":[],"links":[{"id":377916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","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":797372,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212727,"text":"70212727 - 1937 - Recent geologic studies on Long Island with respect to ground-water supplies","interactions":[],"lastModifiedDate":"2021-04-06T13:40:18.910153","indexId":"70212727","displayToPublicDate":"1937-08-26T14:08:30","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Recent geologic studies on Long Island with respect to ground-water supplies","docAbstract":"

Recent studies have shown that relatively impermeable clay beds are widespread on Long Island but that erosion channels cutting through them permit restricted recharge of the underlying beds in some parts of the island. Of the more than 200,000,000 gallons of water a day now pumped from wells, about 65 per cent. comes from the surficial beds of Illinoian or Wisconsin age. Because of the restricted recharge of the lower beds and the desirability of saving these beds for use in localities where the upper beds may more easily be contaminated by salt water, any future large developments of ground water should be drawn from the surficial beds.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.32.4.451","usgsCitation":"Thompson, D.G., Wells, F.G., and Blank, H., 1937, Recent geologic studies on Long Island with respect to ground-water supplies: Economic Geology, v. 32, no. 4, p. 451-470, https://doi.org/10.2113/gsecongeo.32.4.451.","productDescription":"20 p.","startPage":"451","endPage":"470","costCenters":[],"links":[{"id":377909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.04922485351562,\n 40.564937785967224\n ],\n [\n -73.80752563476562,\n 40.564937785967224\n ],\n [\n -73.80752563476562,\n 40.77430186363723\n ],\n [\n -74.04922485351562,\n 40.77430186363723\n ],\n [\n -74.04922485351562,\n 40.564937785967224\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"32","issue":"4","noUsgsAuthors":false,"publicationDate":"1937-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David Grosh","contributorId":19141,"corporation":false,"usgs":true,"family":"Thompson","given":"David","email":"","middleInitial":"Grosh","affiliations":[],"preferred":false,"id":797366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, Francis Gerritt","contributorId":38628,"corporation":false,"usgs":true,"family":"Wells","given":"Francis","email":"","middleInitial":"Gerritt","affiliations":[],"preferred":false,"id":797367,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blank, Horace Richard","contributorId":95101,"corporation":false,"usgs":true,"family":"Blank","given":"Horace Richard","affiliations":[],"preferred":false,"id":797368,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70206431,"text":"70206431 - 1937 - Preliminary report on the North Atlantic deep‐sea cores taken by the Geophysical Laboratory, Carnegie Institution","interactions":[],"lastModifiedDate":"2019-11-02T19:40:37","indexId":"70206431","displayToPublicDate":"1937-07-01T19:26:50","publicationYear":"1937","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}},"displayTitle":"Preliminary report on the North Atlantic deep‐sea cores taken by the Geophysical Laboratory, Carnegie Institution","title":"Preliminary report on the North Atlantic deep‐sea cores taken by the Geophysical Laboratory, Carnegie Institution","docAbstract":"

A series, of 11 cores from the North Atlantic sea‐bottom between the Newfoundland Banks and the banks off the Irish Coast have been studied by a group of geologists of the United States Geological Survey. These cores were taken by Dr. C. S. Piggot of the Carnegie Institution's Geophysical Laboratory from the cable ship Lord Kelvin with the explosive type of sounding‐apparatus, which he designed (C. S. Piggot, Apparatus to secure core‐samples from the oceanbottom, Bull. Geol. Soc. Amer., v. 47, pp. 675–684, 1936). This preliminary report is based largely on the results obtained by M. N. Bramlette, who studied the lithology, and Jos. A. Cushman, who studied the forarainifera. The geographic position, the depth of water at each station, and the length of core obtained are given in Table 1. ©1937. American Geophysical Union. All Rights Reserved.

","language":"English ","publisher":"Elsevier ","doi":"10.1029/TR018i001p00224","issn":" 00028606","usgsCitation":"Bradley, W., Bramlette, M.N., Cushman, J., Henbest, L., Lahman, K., and Trask, P., 1937, Preliminary report on the North Atlantic deep‐sea cores taken by the Geophysical Laboratory, Carnegie Institution: Eos, Transactions, American Geophysical Union, v. 18, no. 1, p. 224-226, https://doi.org/10.1029/TR018i001p00224.","productDescription":"3 p.","startPage":"224","endPage":"226","costCenters":[],"links":[{"id":368909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, Ireland","state":"Newfoundland and Labrador","otherGeospatial":"between Newfoundland banks and Irish Coast","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, W.H.","contributorId":220222,"corporation":false,"usgs":false,"family":"Bradley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":774517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bramlette, M. N.","contributorId":120878,"corporation":false,"usgs":true,"family":"Bramlette","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":774518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cushman, J.A.","contributorId":97162,"corporation":false,"usgs":true,"family":"Cushman","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":774519,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henbest, L.G.","contributorId":61492,"corporation":false,"usgs":true,"family":"Henbest","given":"L.G.","affiliations":[],"preferred":false,"id":774520,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lahman, K.E.","contributorId":220223,"corporation":false,"usgs":false,"family":"Lahman","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":774521,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Trask, P.D.","contributorId":12545,"corporation":false,"usgs":true,"family":"Trask","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":774522,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70159039,"text":"ar58 - 1937 - Fifty-eighth annual report of the Director of the Geological Survey","interactions":[],"lastModifiedDate":"2015-10-14T10:28:41","indexId":"ar58","displayToPublicDate":"1937-01-01T10:30:00","publicationYear":"1937","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":304,"text":"Annual Report","code":"AR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"58","title":"Fifty-eighth annual report of the Director of the Geological Survey","docAbstract":"

During the fiscal year 1937 the Geological Survey continued its systematic work in investigating, mapping, and reporting on the geology, the mineral and water resources, and the physical features of the United States. The results of this work are basic in all conservational activities, as those who plan and direct the conservation policies toward the wise development and use of the Nation's resources must first have the facts about the quantity, quality, distribution, and availability of those resources and adequate maps with which to pursue and record further studies. Through its technical supervision of prospecting, mining, and producing operations on public and Indian land under permits, leases, and licenses, the Survey was directly engaged in the practical application of conservation policies.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/ar58","usgsCitation":"Mendenhall, W.C., 1937, Fifty-eighth annual report of the Director of the Geological Survey: U.S. Geological Survey Annual Report 58, 38 p., https://doi.org/10.3133/ar58.","productDescription":"38 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309874,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":309880,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ar/58/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp796E","usgsCitation":"Andrews, D.A., 1937, Ground water in Avra-Altar Valley, Arizona: U.S. Geological Survey Water Supply Paper 796, ii, 18 p.;, https://doi.org/10.3133/wsp796E.","productDescription":"ii, 18 p.;","costCenters":[],"links":[{"id":25473,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0796e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0796e/report-thumb.jpg"},{"id":413980,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24650.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona","otherGeospatial":"Avra-Altar Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111,\n 32.537\n ],\n [\n -111.6,\n 32.537\n ],\n [\n -111.6,\n 31.329\n ],\n [\n -111,\n 31.329\n ],\n [\n -111,\n 32.537\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db8b","contributors":{"authors":[{"text":"Andrews, David A.","contributorId":38964,"corporation":false,"usgs":true,"family":"Andrews","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":142908,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180141,"text":"70180141 - 1936 - Stream-gaging work: Section 2 of Chapter 6 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","interactions":[],"lastModifiedDate":"2017-01-24T15:11:23","indexId":"70180141","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","chapter":"6","title":"Stream-gaging work: Section 2 of Chapter 6 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","docAbstract":"

Stream gaging is primarily the work of collecting basic data relating to the surface-water supplies of the State. These records are used as the basis for all developments involving the use of water.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","usgsCitation":"Purton, A., 1936, Stream-gaging work: Section 2 of Chapter 6 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936: Utah State Engineer Biennial Report 20, 10 p.","productDescription":"10 p.","startPage":"51","endPage":"60","numberOfPages":"10","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333850,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333849,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-365","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5888770de4b05ccb964bab6b","contributors":{"authors":[{"text":"Purton, A.B.","contributorId":18338,"corporation":false,"usgs":true,"family":"Purton","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":660483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180145,"text":"70180145 - 1936 - Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","interactions":[],"lastModifiedDate":"2017-01-24T15:25:32","indexId":"70180145","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5276,"text":"Utah State Engineer Biennial Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","chapter":"8","title":"Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","docAbstract":"

During the past few years of drouth the importance of ground-water supplies has become more fully appreciated. During this time, because of subnormal replenishment of the ground-water reservoirs and the increased withdrawals from wells, the ground-water levels have declined in most developed areas in the State, a condition which has made the well owners acutely aware that ground water is not inexhaustible. Numerous cases of contention between well owners resulted in increased demands for adequate regulation of the appropriation and use of ground water. Realizing that more information concerning the ground water of the State was imperative, not only to administer the ground-water regulations but to prepare for the conservation and replenishment of existing supplies and development of new supplies, the State Legislature enacted, during its 1935 session, Senate Bill 206, which authorized the State Engineer to make an investigation of the ground water of the State. To provide for the expenses of the investigation, the bill allotted /$10,000 to the State Engineer, this sum to be matched by a State or Federal organization, and the investigation to be carried out co-operatively during the biennium beginning July 1, 1935. A co-operative agreement between the State Engineer and the United States Geological Survey was made on July 1, 1935.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"language":"English","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Taylor, G., and Thomas, H.E., 1936, Ground water investigations in Utah to June 30, 1936: A part of Chapter 8 in Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936: Utah State Engineer Biennial Report 20, 16 p.","productDescription":"16 p.","startPage":"91","endPage":"106","numberOfPages":"16","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333855,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333854,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-365","text":"Full Text of Biennial Report"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5888770de4b05ccb964bab69","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":660502,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":660503,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70040178,"text":"70040178 - 1936 - Withdrawal of ground water on Long Island, N.Y.","interactions":[],"lastModifiedDate":"2012-10-03T17:16:16","indexId":"70040178","displayToPublicDate":"2012-01-01T10:21:47","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-1","title":"Withdrawal of ground water on Long Island, N.Y.","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Thompson, D.G., and Leggette, R., 1936, Withdrawal of ground water on Long Island, N.Y.: Bulletin GW-1, 28 p.; 1 Plate.","productDescription":"28 p.; 1 Plate","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.75138888888888,40.48444444444444 ], [ -79.75138888888888,45.00111111111111 ], [ -71.78388888888888,45.00111111111111 ], [ -71.78388888888888,40.48444444444444 ], [ -79.75138888888888,40.48444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e58739e4b0a4aa5bb09f96","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":467832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":467831,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70159187,"text":"70159187 - 1936 - Supplementary report on the ground-water supplies of the Atlantic City region","interactions":[],"lastModifiedDate":"2015-11-12T13:46:31","indexId":"70159187","displayToPublicDate":"2010-02-02T05:15:00","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":135,"text":"Special Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"6","title":"Supplementary report on the ground-water supplies of the Atlantic City region","docAbstract":"

This report is the second progress report on the ground-water investigations in the Atlantic City region. Many important problems still remain to be solved, however, and it is in no sense a final report.

\n

The report covers the area immediately surrounding Atlantic City, extending from Brigantine to Sea Isle City along the coast and from Absecon to Somers Point on the mainland. In addition to this, a few data are presented bearing on the area along the coast as far south as Wildwood. The area lies in the southern part of the New Jersey Coastal Plain, and the water-bearing formations considered are all unconsolidated and of Miocene or more recent age. The major formations in the region dip gently toward the ocean and possibly extend out under the ocean to the edge of the Continental Shelf, about 100 miles from Atlantic City. The principal ground-water supplies in the area are derived from the so-called \"800-foot sand,\" a member of the Kirkwood formation, and from the overlying Cohansey sands. The 800-foot sand is of wide extent and apparently fairly uniform. The Cohansey sands, on the other hand, cover a wide area but are by no means uniform. At the Atlantic City Water Works two Cohansey sands are recognized-the so-called \"100-foot\" and \"200-foot\" sands. Neither of these sands can be differentiated from the other sands of the Cohansey formation over a distance greater than 4 or 5 miles in any direction.

\n

In addition to the supplies derived from ground water, some surface water is used at present by two of the public water supplies. The quality of the water from all the sources of supply now used is satisfactory. The total consumption of water in the region has increased gradually over the entire period of record, except for a moderate decline from 1929 to 1934. Additional water supplies can be obtained from either of two fairly large streams near the region, and possibly also from a more widespread development of the Cohansey sands. The 800-foot sand should not be counted upon as a source of additional water supply, in view of its liability to salt-water contamination. The same danger also exists in the Cohansey sands on the mainland near the shore, but farther inland it is not a serious menace to the supply from these sands

\n

The 100-foot sand at the Atlantic City Water Work has been overdeveloped since 1930, with the result that the head of the water in it has been lowered materially and salt water has been drawn into it through holes in the overlying clay beneath the nearby salt marshes. Three of the five new large-capacity wells drilled to this sand in 1930 have been temporarily or permanently abandoned on account of salt-water intrusion, and the two others will probably have to be abandoned also, unless suitable remedial measures are promptly adopted. It is recommended that the wells to the 100-foot sand be used only when needed to supply the seasonal peak demand and that consideration be given to a project to transform the tidal marshes into a fresh-water pond by means of a suitable dam in order to protect the formation from further contamination. If detailed study proves that the dam and fresh-water pond would not be economically justified, a smaller pond and an embankment and tide gates on the main stream to keep the salt water from flooding the marshes are recommended as less effective but less expensive remedial measures. In view of the experience with the 100-foot sand at the Atlantic City Water Works, it is further recommended that any additional development of the Cohansey sands be preceded by a comprehensive test-well program that will indicate not only the capacity of the sands, but the location of salt water in them and the possibility of its being drawn into existing wells or the proposed new wells.

\n

The salt-water intrusion into the 100-foot sand was effectively studied by means of driven-well points, which, it was found, could easily be driven to a depth of about 100 feet. The fact that the screen of these wells was driven with the casing and that no water was used in the drilling process made it possible to collect true samples of water from every sand encountered in them. This, in turn, made it possible to study the vertical distribution of salt water in each well. The interpretation of the vertical distribution of salt water in these wells was very helpful in arriving at a final decision as to the source of the salt water.

\n

The 200-foot sand at the Atlantic City Water Works has also been subjected to a considerably increased draft since 1930. Although there is no evidence at present that this sand has been overdeveloped, a study of its characteristics suggests that it may not be capable of yielding permanently the capacity of the present wells that tap it. Three test wells have been installed between the well field and the source from which this sand might derive salt water, and they should be sampled regularly to determine the danger of salt-water intrusion into the sand. In a landward direction this sand merges into the other Cohansey sands. It is therefore advisable that any additional development of the Cohansey sands should be undertaken so far inland that the pumping from it will not affect the present wells to the 200-foot sand and thereby increase the danger of salt-water contamination in them.

\n

At present more potable water is taken from the Atlantic City 800-foot sand than from any other source of supply for the region. This sand is the sole source for some of the smaller communities on the barrier beaches. The original static head of the water in it at Atlantic City was between 20 and 25 feet above sea level. The head has been lowered more than 50 feet over much of the region,  and in parts of Atlantic City it has been lowered considerably more than 100 feet. A consideration of the principles governing the relation between salt water and fresh water in water-bearing sands indicates that the 800-foot sand probably contained salt water at a distance of 5 or 10 miles out from Atlantic City before any water was pumped from it. The evidence collected in this investigation indicates that the cone of depression created by the pumping from this sand in the Atlantic City region has probably extended inland to the intake area of the sand, the nearest part of which is probably about 40 miles from Atlantic City. If this is so, the conclusion is almost inescapable that it has also extended oceanward for a distance considerably greater than the 5 or 10 miles to the original zone of contact between the fresh and salt waters, and that salt water is probably being drawn toward the Atlantic City region through this sand. The time of its arrival will depend primarily upon the rate of pumping in the region and upon how much of the fresh water that originally lay between the region and the zone of contact must be removed before the salt water can reach the region. It may arrive in the near future if it advances in the form of a narrow tongue. On the other hand, if it advances along a broader front; so that more of the intervening fresh water must be pumped out of the formation, its arrival may be delayed for some time.

","language":"English","publisher":"State of New Jersey State Water Policy Commission","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Barksdale, H.C., Sundstrom, R.W., and Brunstein, M.S., 1936, Supplementary report on the ground-water supplies of the Atlantic City region: Special Report 6, 150 p.","productDescription":"150 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310010,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159187.jpg"},{"id":311253,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159187/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"New Jersey","otherGeospatial":"Atlantic City, Brigantine, Somers Point, Sea Isle City, Absecon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -74.49554443359375,\n 39.528407312645825\n ],\n [\n -74.29229736328125,\n 39.49874248613119\n ],\n [\n -74.33624267578125,\n 39.4255858195144\n ],\n [\n -74.38842773437499,\n 39.37677199661635\n ],\n [\n -74.47219848632812,\n 39.31623792008409\n ],\n [\n -74.54360961914062,\n 39.299236474818194\n ],\n [\n -74.59854125976562,\n 39.24182610848299\n ],\n [\n -74.70840454101561,\n 39.118341154165186\n ],\n [\n -74.73175048828124,\n 39.11407918425643\n ],\n [\n -74.77294921875,\n 39.132190775931036\n ],\n [\n -74.77706909179688,\n 39.14603767446419\n ],\n [\n -74.63973999023438,\n 39.301361881349244\n ],\n [\n -74.5697021484375,\n 39.42346418978382\n ],\n [\n -74.49554443359375,\n 39.528407312645825\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5623712fe4b06217fc47deab","contributors":{"authors":[{"text":"Barksdale, Henry C.","contributorId":11463,"corporation":false,"usgs":true,"family":"Barksdale","given":"Henry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":577791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sundstrom, Raymond W.","contributorId":8080,"corporation":false,"usgs":true,"family":"Sundstrom","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":577792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brunstein, Maurice S.","contributorId":149293,"corporation":false,"usgs":false,"family":"Brunstein","given":"Maurice","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":577793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":486,"text":"wsp759 - 1936 - Surface water supply of the United States, 1934, Part IV, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp759","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"759","title":"Surface water supply of the United States, 1934, Part IV, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp759","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1936, Surface water supply of the United States, 1934, Part IV, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 759, vi, 159 p. ;23 cm., https://doi.org/10.3133/wsp759.","productDescription":"vi, 159 p. ;23 cm.","costCenters":[],"links":[{"id":136648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0759/report-thumb.jpg"},{"id":25049,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0759/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69778b","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":527458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2137,"text":"wsp773D - 1936 - Ground-water resources of Kleberg County, Texas","interactions":[],"lastModifiedDate":"2016-08-16T11:38:47","indexId":"wsp773D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"773","chapter":"D","title":"Ground-water resources of Kleberg County, Texas","docAbstract":"

Abundant supplies of fresh water are obtained from deep artesian wells In all parts of Kleberg County. The water is derived from a stratum of sand, 10 to 150 feet thick, which usually has been referred to the Goliad sand but possibly may be at the base of the LIssie formation. The top of the sand Is reached at depths of around 400 feet In the western part of the county, 600 to 700 feet In the locality of Klngsville, and 1,250 to 1,450 feet In the eastern part of the county. Small supplies of fairly good water are obtained from shallow wells In very sandy areas in the eastern and southern parts of the county, but with this exception, so far as known, no good water has been obtained In the county either above or below the artesian fresh-water horizon.

\n

The fresh artesian water Is supplied by percolation from the outcrop of the water-bearing sands, which is many miles to the west In Jim Wells, Brooks, and Duval Counties. The estimated average replenishment from the outcrop to the wells of Kleberg County is 3,000,000 gallons a day.

\n

Available Information regarding most of the wells of the county Is given in the table of well records. Of the 43V wells listed 34 are not In use, and the water supplies from the others are used as follows: , Entirely for stock, 151; domestic use and stock, 241; public supply, 3; Industrial supply, 2; Irrigation, 4; railroad supply, 1; unrecorded, 1. About 80 are flowing wells In the southern and eastern parts of the county.

\n

It is concluded that the total withdrawal from those wells averages about 4,000,000 gallons a day. Some water is wasted, but the amount is not very great.

\n

There has been a general decline In the artesian head throughout the county. The largest decline has been in the western part of the county and In the vicinity of Klngsville, where the water level is now 15 to 45 feet below the surface in wells that once had a strong flow. Wells continue to flow in the southern and eastern parts of the county, but under less head than formerly. There was a small net loss in head in most parts of the county between the winters of 1932-33 and 1934-35, indicating that the decline is slowly continuing. Originally the artesian pressure In the fresh-water sands was much higher than the pressure In the overlying saltwater sands, but this relation has been reversed in the western part of the county and In the district around Klngsville, as a result of the decline in artesian head.

\n

Water obtained from the fresh-water horizon is comparatively fresh in the western and central parts of the county but contains a somewhat higher proportion of chlorides toward the Gulf. Samples obtained from about 100 wells, located for the most part in the central part of the county, showed a. higher chloride content than is normal for the freshwater beds in the area. These wells are believed in large part to be defective and to be admitting salt water. This was demonstrated and the leaks located in several wells that were tested. No evidence was found of salt-water contamination by percolation through the formations, however. The leaky wells should be repaired, If practicable, or sealed to prevent them from contaminating the fresh-water sand. The chances of leaks developing can be largely eliminated If the wells are properly drilled and provided with casing of good grade, and the casing is adequately seated.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp773D","usgsCitation":"Livingston, P.P., and Bridges, T.W., 1936, Ground-water resources of Kleberg County, Texas: U.S. Geological Survey Water Supply Paper 773, 197-232 p., https://doi.org/10.3133/wsp773D.","productDescription":"197-232 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0773d/report-thumb.jpg"},{"id":27737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0773d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fca","contributors":{"authors":[{"text":"Livingston, Penn Poore","contributorId":79452,"corporation":false,"usgs":true,"family":"Livingston","given":"Penn","email":"","middleInitial":"Poore","affiliations":[],"preferred":false,"id":144722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bridges, Thomas W.","contributorId":106870,"corporation":false,"usgs":true,"family":"Bridges","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144723,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2139,"text":"wsp773B - 1936 - Water resources of the Edwards limestone in the San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-22T11:44:21","indexId":"wsp773B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"773","chapter":"B","title":"Water resources of the Edwards limestone in the San Antonio area, Texas","docAbstract":"

The water discharged from the large springs of San Antonio and most of the deep wells of the San Antonio area comes from a common reservoir in fissures and solution channels in the Edwards limestone.

\n

The water enters the limestone in a zone of outcrop along the Balcones escarpment, which crosses the northern parts of Bexar and Medina Counties and extends a long distance both to the east and west of these counties. It is estimated that the combined annual losses into the limestone from the Medina, Prio, Dry Prio, Nueces, and Sabinal Rivers and Hondo Creek may average as much as 150,000 acre-feet a year, the equivalent of a continuous flow of about 134,000,000 gallons a day. Smaller streams also contribute to the underground reservoir, and additional recharge is provided from rainfall on the outcrop of the limestone by direct penetration and by seepage from innumerable storm-water channels.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp773B","usgsCitation":"Livingston, P., Sayre, A., and White, W.N., 1936, Water resources of the Edwards limestone in the San Antonio area, Texas: U.S. Geological Survey Water Supply Paper 773, 59-113 p. :ill., 1 folded map ;24 cm., https://doi.org/10.3133/wsp773B.","productDescription":"59-113 p. :ill., 1 folded map ;24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137793,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0773b/report-thumb.jpg"},{"id":27739,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0773b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d9e","contributors":{"authors":[{"text":"Livingston, Penn","contributorId":104977,"corporation":false,"usgs":true,"family":"Livingston","given":"Penn","affiliations":[],"preferred":false,"id":144727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":144728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, W. N.","contributorId":69954,"corporation":false,"usgs":true,"family":"White","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":144726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1968,"text":"wsp771 - 1936 - Floods in the United States — Magnitude and frequency","interactions":[],"lastModifiedDate":"2022-01-31T22:17:10.857095","indexId":"wsp771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1936","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":"771","title":"Floods in the United States — Magnitude and frequency","docAbstract":"

From time immemorial floods have transformed beneficent river waters into a menace to humanity. Man's progress toward economic stability has been repeatedly halted or even thrown backward by the interruption of his efforts to make effective use of rivers and of valley lands. This handicap is not imposed by the destructiveness of large rivers alone, or of rivers in widely separated areas, for there are few if any streams, brooks, or rivulets that are not subject to flows beyond their channel capacities. Yet, though man for ages has suffered seriously from recurring floods, he has not been deterred from continuing to extend his activities in areas that are virtually foredoomed to flood damage.

Today in the United States serious floods may occur in any section in any year, and even, in some regions, several times a year. Many of these floods leave behind them the tragedy of death and disease and of property irreparably damaged. The aggregate direct property damage caused by floods in this country has been estimated roughly to average $35,000,000 a year. In addition there are serious indirect and intangible losses of great but not precisely calculable magnitude.

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