{"pageNumber":"2707","pageRowStart":"67650","pageSize":"25","recordCount":68807,"records":[{"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":"<p><span>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.</span></p>","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":"<p><span>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.</span></p>","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":"<p>The membership of this Committee is as follows: C. S. Howard, Chairman, U. S. Geological Survey, Washington, D.C.</p><p>D. G. Thompson, U. S. Geological Survey, Washington, D.C.</p><p>A. C. Lane, 22 Arlington Street, Cambridge, Massachusetts</p><p>C. S. Scofield, Bureau of Plant Industry, U. S. Dept. Agri., Washington, D. C.</p><p>I. A. Denison, U.S. Bureau of Standards, Washington, D.C.</p><p>T. G. Thompson, University of Washington, Seattle, Washington</p><p>W. P. Kelley, Citrus Experiment Station, Riverside, California</p><p>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</p>","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":"<p><span>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.</span></p>","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":"<p><span>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.</span></p>","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":"<p><span>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.</span></p>","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":"<p>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.</p>","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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,{"id":952,"text":"wsp796E - 1937 - Ground water in Avra-Altar Valley, Arizona","interactions":[],"lastModifiedDate":"2023-03-10T21:55:27.406154","indexId":"wsp796E","displayToPublicDate":"1937-01-01T00:00:00","publicationYear":"1937","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":"796","chapter":"E","title":"Ground water in Avra-Altar Valley, Arizona","docAbstract":"<p>No abstract available.</p>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","docAbstract":"<p>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.</p>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>: 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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>","docAbstract":"<p>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.</p>","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 <i>Twentieth biennial report of the State Engineer to the governor of Utah: 1935-1936</i>: 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":"<p>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.</p>\n<p>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.</p>\n<p>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</p>\n<p>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.</p>\n<p>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.</p>\n<p>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.</p>\n<p>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, &nbsp;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.</p>","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":1655,"text":"wsp777 - 1936 - Water levels and artesian pressure in observation wells in the United States in 1935 : with statements concerning previous work and results","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp777","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":"777","title":"Water levels and artesian pressure in observation wells in the United States in 1935 : with statements concerning previous work and results","language":"ENGLISH","publisher":"U.S. Govt. print. off.,","doi":"10.3133/wsp777","usgsCitation":"Meinzer, O.E., and Wenzel, L., 1936, Water levels and artesian pressure in observation wells in the United States in 1935 : with statements concerning previous work and results: U.S. Geological Survey Water Supply Paper 777, 268 p. :ill. ;24 cm., https://doi.org/10.3133/wsp777.","productDescription":"268 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0777/report-thumb.jpg"},{"id":26710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0777/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa0bf","contributors":{"authors":[{"text":"Meinzer, Oscar Edward","contributorId":12020,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":143927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wenzel, Leland K.","contributorId":46077,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland K.","affiliations":[],"preferred":false,"id":143928,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4608,"text":"wsp762 - 1936 - Surface water supply of the United States, 1934, Part VII, Lower Mississippi River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"wsp762","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":"762","title":"Surface water supply of the United States, 1934, Part VII, Lower Mississippi River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp762","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1936, Surface water supply of the United States, 1934, Part VII, Lower Mississippi River basin: U.S. Geological Survey Water Supply Paper 762, v, 129 p. ;23 cm., https://doi.org/10.3133/wsp762.","productDescription":"v, 129 p. ;23 cm.","costCenters":[],"links":[{"id":139295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0762/report-thumb.jpg"},{"id":31665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0762/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69773e","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":528302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":"<p>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.</p><p>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.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp771","collaboration":"Prepared in collaboration with the Water Planning Committee of the National Resources Board and its predecessor the Mississippi Valley Committee","usgsCitation":"Jarvis, C.S., 1936, Floods in the United States — Magnitude and frequency: U.S. Geological Survey Water Supply Paper 771, 495 p., https://doi.org/10.3133/wsp771.","productDescription":"495 p.","numberOfPages":"500","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true},{"id":610,"text":"Utah Water Science 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