{"pageNumber":"656","pageRowStart":"16375","pageSize":"25","recordCount":16446,"records":[{"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":"<p>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.</p>\n<p>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.</p>\n<p>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.</p>\n<p>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.</p>\n<p>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.</p>\n<p>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.</p>","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":3168,"text":"wsp773E - 1936 - The New York State flood of July 1935","interactions":[],"lastModifiedDate":"2022-02-09T20:49:02.246137","indexId":"wsp773E","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":"E","title":"The New York State flood of July 1935","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1936","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp773E","usgsCitation":"Johnson, H., 1936, The New York State flood of July 1935: U.S. Geological Survey Water Supply Paper 773, iv, 36 p., https://doi.org/10.3133/wsp773E.","productDescription":"iv, 36 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":395728,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24640.htm"},{"id":30126,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0773e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0773e/report-thumb.jpg"}],"country":"United States","state":"New 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,{"id":70212999,"text":"70212999 - 1936 - Introduction: Some problems relating to fluctuations of ground‐water level","interactions":[],"lastModifiedDate":"2020-09-03T16:51:13.584707","indexId":"70212999","displayToPublicDate":"1936-09-03T11:34:28","publicationYear":"1936","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":"Introduction: Some problems relating to fluctuations of ground‐water level","docAbstract":"<p><span>When the program for the meeting of the Section of Hydrology a year ago was in preparation, it was suggested that a symposium be presented on the subject of the effects of the recent drought on ground‐water levels. The proposal was not carried out largely because at that time not enough accurate information on the subject was yet available. It has, however, seemed that this year a worth‐while group of papers could be developed on the broader subject of fluctuations of ground‐water levels.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00337","usgsCitation":"Thompson, D.G., 1936, Introduction: Some problems relating to fluctuations of ground‐water level: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 337-341, https://doi.org/10.1029/TR017i002p00337.","productDescription":"5 p.","startPage":"337","endPage":"341","costCenters":[],"links":[{"id":378139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","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":797948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212914,"text":"70212914 - 1936 - Report of the Committee on Underground Waters, 1935–36","interactions":[],"lastModifiedDate":"2020-09-01T17:53:58.343522","indexId":"70212914","displayToPublicDate":"1936-09-01T12:51:48","publicationYear":"1936","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, 1935–36","docAbstract":"<p>Interest in problems of ground‐water hydrology continues unabated. As proof of this statement it is only necessary to state that of 57 papers listed for presentation at the present annual meeting of the Section of Hydrology and of the Pacific Coast meeting of the Section on January 31 and February 1, 26 papers, or 45 per cent, related to some phase of ground‐water hydrology. In this connection, attention may be called especially to the papers on ground‐water presented at the Pacific Coast meeting and published in the present<span>&nbsp;</span><span>Transactions</span>.</p><p>At this early point in his report, the Chairman should state that at about the time he usually takes the preliminary steps in compiling data for his annual report, his official duties somewhat unexpectedly took him to field‐work in New Mexico and Colorado. Without the usual office facilities it has not been possible for him to make all desired contacts, and the present report of current ground‐water studies is necessarily somewhat incomplete.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00326","usgsCitation":"Thompson, D., 1936, Report of the Committee on Underground Waters, 1935–36: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 326-329, https://doi.org/10.1029/TR017i002p00326.","productDescription":"4 p.","startPage":"326","endPage":"329","costCenters":[],"links":[{"id":378064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David G.","contributorId":8443,"corporation":false,"usgs":true,"family":"Thompson","given":"David G.","affiliations":[],"preferred":false,"id":797808,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221656,"text":"70221656 - 1935 - Further tests of permeability with low hydraulic gradients","interactions":[],"lastModifiedDate":"2021-06-27T15:08:10.582045","indexId":"70221656","displayToPublicDate":"1935-08-01T10:04:26","publicationYear":"1935","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":"Further tests of permeability with low hydraulic gradients","docAbstract":"<p><span>Many of the water‐bearing formations in the United States have&nbsp;</span>hydraulic<span>&nbsp;</span>gradients<span>&nbsp;of much less than 20 feet to the mile, and some may have&nbsp;</span>gradients<span>&nbsp;of less than one foot to the mile, whereas most laboratory‐</span>tests<span>&nbsp;of&nbsp;</span>permeability<span>&nbsp;are made with much higher&nbsp;</span>gradients<span>. An investigation was therefore undertaken by the writer, under the direction of 0. E. Meinzer, in the Hydrologic Laboratory of the United States Geological Survey, to determine whether Darcy's law is valid for very&nbsp;</span>low<span>&nbsp;</span>hydraulic<span>&nbsp;</span>gradients<span>—that is, whether under such&nbsp;</span>low<span>&nbsp;</span>gradients<span>&nbsp;the rate of flow remains proportional to the&nbsp;</span>gradient<span>. In a previous paper by Meinzer and the writer (Amer. Geophysical Union,15th annual meeting, pp.405–409, 1934), it was shown that for the sand tested the rate of flow varies directly with the&nbsp;</span>hydraulic<span>&nbsp;</span>gradient<span>&nbsp;down to a&nbsp;</span>gradient<span>&nbsp;of about one foot to the mile. More recently six additional&nbsp;</span>tests<span>&nbsp;have been made on this sand with the same apparatus, and these&nbsp;</span>tests<span>&nbsp;give evidence of the validity of Darcy's law for still lower&nbsp;</span>gradients<span>.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR016i002p00499","usgsCitation":"Fishel, V., 1935, Further tests of permeability with low hydraulic gradients: Eos, Transactions, American Geophysical Union, v. 16, no. 2, p. 499-503, https://doi.org/10.1029/TR016i002p00499.","productDescription":"5 p.","startPage":"499","endPage":"503","costCenters":[],"links":[{"id":386779,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":818359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221655,"text":"70221655 - 1935 - The Piezometric surface of artesian water in the Florida peninsula","interactions":[],"lastModifiedDate":"2021-06-27T15:02:05.946659","indexId":"70221655","displayToPublicDate":"1935-08-01T09:58:17","publicationYear":"1935","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 Piezometric surface of artesian water in the Florida peninsula","docAbstract":"<p><span>The ground‐</span>water<span>&nbsp;of the&nbsp;</span>Florida<span>&nbsp;</span>Peninsula<span>&nbsp;constitutes one of its most valuable natural resources and is of importance as a source of&nbsp;</span>water<span>‐supplies throughout the area. The problems relating to the development of ground‐</span>water<span>&nbsp;supplies are both quantitative and qualitative. They include such problems as the decline&nbsp;</span>in<span>&nbsp;yield of wells&nbsp;</span>in<span>&nbsp;areas of large withdrawals of&nbsp;</span>water<span>&nbsp;and salt‐</span>water<span>&nbsp;contamination of ground‐</span>water<span>&nbsp;supplies.&nbsp;</span>In<span>&nbsp;order to facilitate a better understanding and interpretation of hydrologic conditions relating to these local ground‐</span>water<span>&nbsp;problems, a general survey of the&nbsp;</span>artesian<span>&nbsp;</span>water<span>&nbsp;</span>in<span>&nbsp;the&nbsp;</span>Florida<span>&nbsp;</span>Peninsula<span>&nbsp;was made by the United States Geological Survey&nbsp;</span>in<span>&nbsp;1934.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR016i002p00524","usgsCitation":"Stringfield, V.T., 1935, The Piezometric surface of artesian water in the Florida peninsula: Eos, Transactions, American Geophysical Union, v. 16, no. 2, p. 524-529, https://doi.org/10.1029/TR016i002p00524.","productDescription":"6 p.","startPage":"524","endPage":"529","costCenters":[],"links":[{"id":386778,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.8466796875,\n              24.607069137709683\n            ],\n            [\n              -78.837890625,\n              24.607069137709683\n            ],\n            [\n              -78.837890625,\n              31.052933985705163\n            ],\n            [\n              -87.8466796875,\n              31.052933985705163\n            ],\n            [\n              -87.8466796875,\n              24.607069137709683\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"16","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":818358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221680,"text":"70221680 - 1934 - Report of the committee on underground‐water, 1933–34","interactions":[],"lastModifiedDate":"2021-06-28T16:41:37.218356","indexId":"70221680","displayToPublicDate":"1934-06-01T11:39:10","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of the committee on underground‐water, 1933–34","docAbstract":"<p><span>The by‐laws adopted at the meeting of the Section of Hydrology in&nbsp;</span>1933<span>&nbsp;provided that the membership of research committees should be reconstituted every three years. There have, accordingly, been some changes in the membership of the&nbsp;</span>Committee<span>&nbsp;on&nbsp;</span>Underground<span>‐</span>Water<span>. Certain members have retired because of pressure of other duties or because they are no longer actively engaged in ground‐</span>water<span>&nbsp;work. Dr. O. E. Meinzer, who retired as Chairman of the Section of Hydrology, has agreed to serve on the&nbsp;</span>Committee<span>, and probably two or three other men will be appointed to make contact with special phases of the field covered by the&nbsp;</span>Committee<span>. It is with regret that the Chairman reports the loss to the&nbsp;</span>Committee<span>&nbsp;by the death of A. F. Melcher, who had contributed much to the science of ground‐</span>water<span>&nbsp;hydrology by his studies on permeability and absorption of sedimentary formations for&nbsp;</span>water<span>, oil, and gas. ©19</span>34</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00312","usgsCitation":"Thompson, D.G., 1934, Report of the committee on underground‐water, 1933–34: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 312-316, https://doi.org/10.1029/TR015i002p00312.","productDescription":"5 p.","startPage":"312","endPage":"316","costCenters":[],"links":[{"id":386806,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":818418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221673,"text":"70221673 - 1934 - Appendix A—permeability","interactions":[],"lastModifiedDate":"2021-06-28T15:56:06.937317","indexId":"70221673","displayToPublicDate":"1934-06-01T10:52:41","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix A—permeability","docAbstract":"<p>In the paper entitled “The measurement of the permeability of porous media for homogeneous fluids” by R. D. Wyckoff and others [42] a unit of permeability is proposed which is based on centimeters, seconds, and atmospheres of pressure (76 centimeters of mercury).</p><p>In 1923, when the Hydrologic Laboratory of the United States Geological Survey was organized, much study was given to the question of a coefficient of permeability, and a coefficient was adopted which is based on feet and gallons a day (U.S. Geol. Survey Water-Supply Paper 596, p. 148). This coefficient has been extensively used and has proved very satisfactory in ground-water work. It has the merit of being readily applicable to field-conditions. It is, moreover, of convenient size, the coefficients of most water-bearing materials being integers of two or three figures, that is, between 10 and 1000. It was adopted in place of Slichter's “transmission-constant” (U.S. Geol. Survey Water-Supply Paper 67, p. 27, 1902), after much careful consideration, largely because the “transmission-constant” of most water-bearing materials is inconvenient in being only a small decimal.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00316","usgsCitation":"Meinzer, O.E., 1934, Appendix A—permeability: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 316-317, https://doi.org/10.1029/TR015i002p00316.","productDescription":"2 p.","startPage":"316","endPage":"317","costCenters":[],"links":[{"id":386798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818403,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221668,"text":"70221668 - 1934 - Appendix C—A selected list of papers relating to ground‐water hydrology","interactions":[],"lastModifiedDate":"2021-06-29T14:00:10.563864","indexId":"70221668","displayToPublicDate":"1934-06-01T09:04:11","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix C—A selected list of papers relating to ground‐water hydrology","docAbstract":"<p><span>In the following&nbsp;</span>list<span>&nbsp;brief statements have been added to certain references to call attention to special phases of&nbsp;</span>ground<span>‐</span>water<span>&nbsp;problems which are not apparent from the titles. Abstracts of most of these&nbsp;</span>papers<span>&nbsp;have been or will be published in the Annotated Bibliography of Economic Geology.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00318","usgsCitation":"Sayre, A., 1934, Appendix C—A selected list of papers relating to ground‐water hydrology: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 318-320, https://doi.org/10.1029/TR015i002p00318.","productDescription":"3 p.","startPage":"318","endPage":"320","costCenters":[],"links":[{"id":386848,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":818496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221667,"text":"70221667 - 1934 - Appendix B—Lake and ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-28T14:02:22.088463","indexId":"70221667","displayToPublicDate":"1934-06-01T08:58:02","publicationYear":"1934","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Appendix B—Lake and ground‐water levels","docAbstract":"<p>An outstanding achievement of the Section of Hydrology has been the work of the Committee on Glaciers in assembling the existing records of the advance and retreat of the glaciers in the Western States and in Alaska, encouraging various agencies in making periodic observations, systematizing and standardizing the work, and providing for the compilation and preservation of the data obtained from year to year.</p><p>The fluctuation of lake levels is a closely related subject that is equally fundamental in the study of hydrology. In 1922 I published a map giving the distribution of 68 Pleistocene lakes in the Basin and Range province and showed that the desiccation of these lakes could have been caused by change in temperature as well as change in precipitation (Geol. Soc. Amer. Bull., v. 33. pp. 541–552. 1922). Abundant and convincing evidences of changes in climate in the Pleistocene epoch or at its end are afforded both by the ancient drift-sheets and by the ancient lake features, but the question as to the relative importance of changes in temperature and changes in precipitation is still very obscure.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR015i002p00317","usgsCitation":"Meinzer, O.E., 1934, Appendix B—Lake and ground‐water levels: Eos, Transactions, American Geophysical Union, v. 15, no. 2, p. 317-318, https://doi.org/10.1029/TR015i002p00317.","productDescription":"2 p.","startPage":"317","endPage":"318","costCenters":[],"links":[{"id":386792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","otherGeospatial":"western United States and Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -166.46484375,\n              57.51582286553883\n            ],\n            [\n              -135.87890625,\n              57.51582286553883\n            ],\n            [\n              -135.87890625,\n              70.72897946208789\n            ],\n            [\n              -166.46484375,\n              70.72897946208789\n            ],\n            [\n              -166.46484375,\n              57.51582286553883\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -125.5078125,\n              32.84267363195431\n            ],\n            [\n              -109.3359375,\n              32.84267363195431\n            ],\n            [\n              -109.3359375,\n              48.80686346108517\n            ],\n            [\n              -125.5078125,\n              48.80686346108517\n            ],\n            [\n              -125.5078125,\n              32.84267363195431\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":818395,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221749,"text":"70221749 - 1933 - Specific yield determined from a Thiem's Pumping‐Test","interactions":[],"lastModifiedDate":"2021-06-30T18:55:53.005509","indexId":"70221749","displayToPublicDate":"1933-06-01T13:52:40","publicationYear":"1933","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":"Specific yield determined from a Thiem's Pumping‐Test","docAbstract":"<p>The specific yield of a water-bearing formation is defined as the ratio of (1) the volume of water, which after being saturated, it will yield by gravity to (2) its own volume (O. E. Meinzer, Outline of ground-water hydrology, U.S. Geol. Sur. Water-Supply Paper 494, p. 28, 1923). It is a measure of the quantity of water that a formation will yield when it is drained by lowering of the water-table. The determination of the specific yield is essential in many quantitative ground-water investigations.</p><p>In 1931 a pumping-test was made in the Platte River Valley, in Nebraska, to determine by Thiem's method the permeability of the water-bearing sand and gravel that underlie the Valley. This test, which constitutes a part of a cooperative investigation by the Conservation and Survey Department of the University of Nebraska and the United States Geological Survey, was briefly described in the 1932 Transactions of the American Geophysical Union (p. 393). The well was pumped continuously for 48 hours, and measurements of the discharge were made every 30 minutes. During the period of pumping and after pumping stopped about 5,000 measurements were made of the depths to the water-surfaces in 80 observation-wells, which were located on lines radiating from the pumped well to distances up to 1,200 feet. Instrumental levels were run to the measuring points on each of the wells so that the altitudes of the water-surfaces could be determined for any time. From the data obtained in this test the average coefficient of permeability was computed to be about 700. In the present paper a method is presented for determining the specific yield of the water-bearing material from the data collected in this test, and the results of the computations are given. This method for determining specific yield was suggested by Meinzer (O. E. Meinzer, Outline of methods for estimating ground-water supplies, U.S. Geol. Sur. water-Supply Paper 638-c, p. 136, 1932).</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00475","usgsCitation":"Wenzel, L., 1933, Specific yield determined from a Thiem's Pumping‐Test: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 475-477, https://doi.org/10.1029/TR014i001p00475.","productDescription":"3 p.","startPage":"475","endPage":"477","costCenters":[],"links":[{"id":386909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, L.K.","contributorId":18733,"corporation":false,"usgs":true,"family":"Wenzel","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":818608,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221745,"text":"70221745 - 1933 - Geophysical interpretation of ground‐water levels","interactions":[],"lastModifiedDate":"2021-06-30T16:31:51.062153","indexId":"70221745","displayToPublicDate":"1933-06-01T11:28:11","publicationYear":"1933","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":"Geophysical interpretation of ground‐water levels","docAbstract":"<p><span>The theory of rock‐pressure as a cause of artesian‐head dates back at least to early Grecian times. Thus the philosopher Thales, about 600 B.C., taught that the springs derive their&nbsp;</span>water<span>&nbsp;from the ocean through subterranean channels and that the&nbsp;</span>water<span>&nbsp;is lifted to the springs by rook‐pressure. The theory of rock‐pressure has had a number of recent advocates, chief among whom was the British geologist, J. W. Gregory, but apparently no effective attempt was made by any of them to apply critical data to the problem. In general, geologists and hydrologists have rejected rock‐pressure as a vague heresy and have assumed that the artesian formations function as perfectly rigid and inert containers, not recognizing the fact that the data in regard to the performance of wells appear to conflict with such an&nbsp;</span>interpretation<span>.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00036","usgsCitation":"Meinzer, O.E., 1933, Geophysical interpretation of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 36-37, https://doi.org/10.1029/TR014i001p00036.","productDescription":"2 p.","startPage":"36","endPage":"37","costCenters":[],"links":[{"id":386904,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","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":818604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221744,"text":"70221744 - 1933 - Some relations between ground‐water hydrology and oceanography","interactions":[],"lastModifiedDate":"2021-06-30T16:23:44.914113","indexId":"70221744","displayToPublicDate":"1933-06-01T11:19:31","publicationYear":"1933","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":"Some relations between ground‐water hydrology and oceanography","docAbstract":"<p>In many areas along the sea-coasts of the world the water-supply for human use is derived largely, and in some areas wholly, from underground sources. Because of the proximity to the ocean in these areas, in some respects the geologic and hydrologic conditions that govern the occurrence and movement of ground-water are quite different from those in inland areas, and to properly interpret them the ground-water hydrologist must avail himself of facts developed by the oceanographer.</p><p>These conditions are encountered in a marginal zone that in different localities may extend only a few feet or many miles inland from the coast, and presumably for greater or less distances out beneath the ocean. These special conditions have been recognized and extensively studied for many years, for example, in the lowland-area of Holland that lies between the Zuider Zee and the North Sea, and on Long Island, New York. Within recent years more or less attention has been given to these conditions in many of the coastal states of the United States, and in the Hawaiian Islands and Cuba. It is the purpose of this statement to indicate some of the problems of groundwater hydrology that are related to oceanography.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00030","usgsCitation":"Thompson, D., 1933, Some relations between ground‐water hydrology and oceanography: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 30-33, https://doi.org/10.1029/TR014i001p00030.","productDescription":"4 p.","startPage":"30","endPage":"33","costCenters":[],"links":[{"id":386903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David G.","contributorId":8443,"corporation":false,"usgs":true,"family":"Thompson","given":"David G.","affiliations":[],"preferred":false,"id":818603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221743,"text":"70221743 - 1933 - Deep‐well salinity‐exploration","interactions":[],"lastModifiedDate":"2021-06-30T16:05:47.249003","indexId":"70221743","displayToPublicDate":"1933-06-01T11:00:20","publicationYear":"1933","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":"Deep‐well salinity‐exploration","docAbstract":"<p><span>One of the outstanding accomplishments of recent years in connection with the study of the geologic source of groundwater and the quality of water yielded by different formations has been the development of methods and equipment for the&nbsp;</span>exploration<span>&nbsp;of wells. The description and use of the&nbsp;</span>deep<span>‐</span>well<span>&nbsp;current‐meter on&nbsp;</span>well<span>‐</span>exploration<span>&nbsp;work in Hawaii and New Mexico has already appeared in published literature (John McCombs and A. G. Fiedler, Methods of exploring and repairing leaky artesian wells, U.S. Geol. Sur. Water‐Supply Paper 596, pp. 1–32, 1928) on hydrology but recent developments in the application of electrical conductivity‐measurements for determining the&nbsp;</span>salinity<span>&nbsp;of water in wells have not heretofore been presented. In addition to being of considerable scientific importance in connection with problems of ground‐water hydrology, the practical value of locating the place at which salt water is entering a&nbsp;</span>well<span>&nbsp;and contaminating a potable water‐supply is great. Such information may be the means of preventing the loss of large investments in industries, irrigation‐projects, and cities that are dependent upon&nbsp;</span>well<span>‐water supplies that may at some time become contaminated by salty or other highly mineralized water.&nbsp;</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR014i001p00478","usgsCitation":"Fiedler, A., 1933, Deep‐well salinity‐exploration: Eos, Transactions, American Geophysical Union, v. 14, no. 1, p. 478-480, https://doi.org/10.1029/TR014i001p00478.","productDescription":"3 p.","startPage":"478","endPage":"480","costCenters":[],"links":[{"id":386902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Nevada, Hawaii","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.984375,\n              31.42866311735861\n            ],\n            [\n              -103.22753906249999,\n              31.42866311735861\n            ],\n            [\n              -103.22753906249999,\n              37.09023980307208\n            ],\n            [\n              -108.984375,\n              37.09023980307208\n            ],\n            [\n              -108.984375,\n              31.42866311735861\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -161.54296875,\n              18.396230138028827\n            ],\n            [\n              -151.875,\n              18.396230138028827\n            ],\n            [\n              -151.875,\n              23.483400654325642\n            ],\n            [\n              -161.54296875,\n              23.483400654325642\n            ],\n            [\n              -161.54296875,\n              18.396230138028827\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fiedler, A.G.","contributorId":11272,"corporation":false,"usgs":true,"family":"Fiedler","given":"A.G.","email":"","affiliations":[],"preferred":false,"id":818602,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","interactions":[{"subject":{"id":25083,"text":"wsp659A - 1932 - A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","indexId":"wsp659A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah"},"predicate":"IS_PART_OF","object":{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","indexId":"wsp659","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States, 1932"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1932","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":"659","title":"Contributions to the hydrology of the United States, 1932","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey,","doi":"10.3133/wsp659","usgsCitation":"Grover, N., 1932, Contributions to the hydrology of the United States, 1932: U.S. Geological Survey Water Supply Paper 659, v, 209 p. :ill., maps (2 maps in pocket) ;23 cm., https://doi.org/10.3133/wsp659.","productDescription":"v, 209 p. :ill., maps (2 maps in pocket) ;23 cm.","costCenters":[],"links":[{"id":137070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0659/report-thumb.jpg"},{"id":26547,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0659/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26548,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0659/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0659/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68be27","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":143744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","interactions":[{"subject":{"id":25079,"text":"wsp638A - 1932 - A preliminary report on the artesian water supply of Memphis, Tennessee","indexId":"wsp638A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A preliminary report on the artesian water supply of Memphis, Tennessee"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":1},{"subject":{"id":25080,"text":"wsp638B - 1932 - Water-power resources of the Rogue River drainage basin, Oregon","indexId":"wsp638B","publicationYear":"1932","noYear":false,"chapter":"B","title":"Water-power resources of the Rogue River drainage basin, Oregon"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":2},{"subject":{"id":25081,"text":"wsp638C - 1932 - Outline of methods for estimating ground-water supplies","indexId":"wsp638C","publicationYear":"1932","noYear":false,"chapter":"C","title":"Outline of methods for estimating ground-water supplies"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":3},{"subject":{"id":25082,"text":"wsp638D - 1932 - Quality of water of the Colorado River in 1928-1930","indexId":"wsp638D","publicationYear":"1932","noYear":false,"chapter":"D","title":"Quality of water of the Colorado River in 1928-1930"},"predicate":"IS_PART_OF","object":{"id":3212,"text":"wsp638 - 1932 - Contributions to the hydrology of the United States 1931","indexId":"wsp638","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States 1931"},"id":4}],"lastModifiedDate":"2024-02-05T21:21:47.532833","indexId":"wsp638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1932","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":"638","title":"Contributions to the hydrology of the United States 1931","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp638","usgsCitation":"Grover, N., 1932, Contributions to the hydrology of the United States 1931: U.S. Geological Survey Water Supply Paper 638, v, 162 p., https://doi.org/10.3133/wsp638.","productDescription":"v, 162 p.","costCenters":[],"links":[{"id":30204,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0638/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139042,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0638/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691299","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":146441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25083,"text":"wsp659A - 1932 - A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","interactions":[{"subject":{"id":25083,"text":"wsp659A - 1932 - A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","indexId":"wsp659A","publicationYear":"1932","noYear":false,"chapter":"A","title":"A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah"},"predicate":"IS_PART_OF","object":{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","indexId":"wsp659","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States, 1932"},"id":1}],"isPartOf":{"id":1450,"text":"wsp659 - 1932 - Contributions to the hydrology of the United States, 1932","indexId":"wsp659","publicationYear":"1932","noYear":false,"title":"Contributions to the hydrology of the United States, 1932"},"lastModifiedDate":"2023-09-21T21:11:59.936443","indexId":"wsp659A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1932","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":"659","chapter":"A","title":"A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah","docAbstract":"<p>Fluctuations of water levels in wells, if critically studied, may give much information as to the occurrence, movement, and quantity of available ground water. In some localities the ground-water level has been observed to decline during the day and to rise at night, the decline beginning at about the same hour every morning and the rise at about the same hour every night. This daily decline is due to the withdrawal of ground water from the zone of saturation by plants, and the rise at night is due to upward movement of water under slight artesian pressure from permeable beds of sand and gravel at some depth beneath the water table.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1932 (Water Supply Paper 659)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp659A","usgsCitation":"White, W.N., 1932, A method of estimating ground-water supplies based on discharge by plants and evaporation from soil: Results of investigations in Escalante Valley, Utah: U.S. Geological Survey Water Supply Paper 659, Report: 105 p.; 1 Plate: 14.65 x 21.52 inches, https://doi.org/10.3133/wsp659A.","productDescription":"Report: 105 p.; 1 Plate: 14.65 x 21.52 inches","numberOfPages":"115","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":421031,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24621.htm","linkFileType":{"id":5,"text":"html"}},{"id":54081,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0659a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264574,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0659a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156866,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0659a/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Escalante Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.69688804144857,\n              37.53657815987634\n            ],\n            [\n              -113.16519847993968,\n              37.662594400449564\n            ],\n            [\n              -112.86981539021227,\n              37.91040066781825\n            ],\n            [\n              -112.86981744366477,\n              38.42843951649698\n            ],\n            [\n              -112.87890615411786,\n              38.62042242875168\n            ],\n            [\n              -113.51057153061132,\n              38.517384159387944\n            ],\n            [\n              -113.92410785622891,\n              37.81712147838752\n            ],\n            [\n              -113.69688804144857,\n              37.53657815987634\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae054","contributors":{"authors":[{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":193180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220411,"text":"70220411 - 1932 - Investigations of underground water problems in Arizona, California, New Mexico, and Oregon","interactions":[],"lastModifiedDate":"2021-05-12T12:34:20.907919","indexId":"70220411","displayToPublicDate":"1932-05-12T07:26:58","publicationYear":"1932","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":"Investigations of underground water problems in Arizona, California, New Mexico, and Oregon","docAbstract":"<div id=\"article__content\" class=\"col-sm-12 col-md-8 col-lg-8 article__content article-row-left\"><div class=\"article__body \"><div class=\"article-section__content en main\"><p>This report is a summary of investigations in progress in 1932 in the southwestern portion of the United States. It covers only those investigations that deal with water in the zone of saturation, and excludes those that deal primarily with water in the zone of aeration. Arizona H. C. Schwalen, Irrigation Engineer, Agricultural Experiment‐Station, Tucson, Arizona, has proposed to undertake a study of the effect of pumping from wells, and of the capacity of water‐bearing strata, but no report of progress is available. Several other hydrologic investigations are now being made by the Agricultural Experiment‐ Station, but relate primarily to infiltration and transpiration.</p></div></div></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR013i001p00308","usgsCitation":"Piper, A., 1932, Investigations of underground water problems in Arizona, California, New Mexico, and Oregon: Eos, Transactions, American Geophysical Union, v. 13, no. 1, p. 308-310, https://doi.org/10.1029/TR013i001p00308.","productDescription":"3 p.","startPage":"308","endPage":"310","costCenters":[],"links":[{"id":385583,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, New Mexico, 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