{"pageNumber":"2714","pageRowStart":"67825","pageSize":"25","recordCount":69037,"records":[{"id":70212847,"text":"70212847 - 1938 - The significance and nature of the cone of depression in ground-water bodies","interactions":[],"lastModifiedDate":"2020-08-31T14:57:33.866613","indexId":"70212847","displayToPublicDate":"1938-12-01T09:54:52","publicationYear":"1938","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":"The significance and nature of the cone of depression in ground-water bodies","docAbstract":"<p><span>In nature the hydraulic system in an aquifer is in balance; the discharge is equal to the recharge and the water table or other piezometric surface is more or less fixed in position. Discharge by wells is a new discharge superimposed on the previous system. Before a new equilibrium can be established water levels must fall throughout the aquifer to an extent sufficient to reduce the natural discharge or increase the recharge by an amount equal to the amount discharged by the well. Until this new equilibrium is established water must be withdrawnfrom storage in the aquifer and conversely the new equilibrium cannot be established until an amount of water is withdrawn from storage by the well sufficient to depress the piezometric surface enough to change the recharge or natural discharge the proper amount. The depression of the piezometric surface is called the cone of depression.The characteristics of the cone of depression in an idealized aquifer of infinite areal extent are considered mathematically. Time is an essential variable in the description of this cone. The time rate of lateral growth of the cone is independent of the rate of discharge by the well and depends only on the physical characteristics of the aquifer. The cone must grow laterally much more rapidly in artesian aquifers than it does in nonartesian. The characteristics of the cone in actual aquifers are then considered. In finely porous artesian aquifers the cone appears to be much like the cone in the ideal aquifer. The cone in non-artesian aquifers must be somewhat warped. The theory out-lined implies that well discharge from extensive water-table aquifers must be a draft on storage in the aquifer for many generations.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.8.889","usgsCitation":"Theis, C.V., 1938, The significance and nature of the cone of depression in ground-water bodies: Economic Geology, v. 33, no. 8, p. 889-902, https://doi.org/10.2113/gsecongeo.33.8.889.","productDescription":"4 p.","startPage":"889","endPage":"902","costCenters":[],"links":[{"id":378033,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationDate":"1938-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":797699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207439,"text":"70207439 - 1938 - Sulphate minerals of the Comstock Lode, Nevada","interactions":[],"lastModifiedDate":"2019-12-19T11:35:37","indexId":"70207439","displayToPublicDate":"1938-11-01T11:30:27","publicationYear":"1938","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":"Sulphate minerals of the Comstock Lode, Nevada","docAbstract":"<p><span>Seventeen representative samples of supergene sulphates from old workings on the Comstock Lode are described. They range from simple minerals such as gypsum and epsomite to complex aggregates of four or more distinct species. All are well known species except a mineral of the copper (chalcanthite) or magnesium sulphate pentahydrate group, with about half the magnesium replaced by copper, zinc, ferrous iron, and manganese. Four new analyses of Comstock Lode mine waters are given. © 1938 Society of Economic Geologists, Inc.</span></p>","language":"English","publisher":"Society of Economic Geologists ","doi":"10.2113/gsecongeo.33.7.749","issn":"03610128","usgsCitation":"Milton, C., and Johnston, W.D., 1938, Sulphate minerals of the Comstock Lode, Nevada: Economic Geology, v. 33, no. 7, p. 749-771, https://doi.org/10.2113/gsecongeo.33.7.749.","productDescription":"23 p. 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,{"id":38039,"text":"38039 - 1938 - Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia","interactions":[],"lastModifiedDate":"2014-07-21T11:45:35","indexId":"38039","displayToPublicDate":"1938-09-01T11:45:05","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"120","title":"Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Kalmbach, E., 1938, Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia: Wildlife Leaflet 120, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":290563,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4fbee4b0b290850f2e5a","contributors":{"authors":[{"text":"Kalmbach, E.R.","contributorId":21610,"corporation":false,"usgs":true,"family":"Kalmbach","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":218766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212723,"text":"70212723 - 1938 - A recording evaporimeter","interactions":[],"lastModifiedDate":"2020-08-26T18:20:55.614369","indexId":"70212723","displayToPublicDate":"1938-08-26T13:13:11","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"A recording evaporimeter","docAbstract":"<p>The instrument herein described was originally designed and built to record the evaporation‐loss from a standard Weather Bureau pan for use in a study of the variation of flow in Santa Ana River. Valuable suggestions were made by various members of the Water Resources Branch of the Geological Survey in Southern California, and financial assistance for construction was given by F. C. Ebert and H. C. Troxell of the same organization. The typing of the paper and some of the drafting were done by Works Progress Administration help.</p><p>The original instrument was damaged by flood‐waters in 1934, while in operation at Baldwin Park, California. It was then redesigned and constructed of stainless materials and installed on the campus of the San Bernardino Valley Junior College. The Weather Bureau pan was replaced by a thermally insulated pan. The damping unit was added at this time by the present writers. The evaporimeter was placed in regular operation on October 30, 1937, in a study of the relative magnitudes of the various energy‐components associated with solar and sky radiation and with evaporation from water‐surfaces, from damp soil, and from plants.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i002p00609","usgsCitation":"Oliver, J., and Cummings, N., 1938, A recording evaporimeter: Eos, Transactions, American Geophysical Union, v. 19, no. 2, p. 609-612, https://doi.org/10.1029/TR019i002p00609.","productDescription":"4 p.","startPage":"609","endPage":"612","costCenters":[],"links":[{"id":377902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Oliver, J.","contributorId":167156,"corporation":false,"usgs":false,"family":"Oliver","given":"J.","affiliations":[],"preferred":false,"id":797359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, N.W.","contributorId":239604,"corporation":false,"usgs":false,"family":"Cummings","given":"N.W.","email":"","affiliations":[],"preferred":false,"id":797360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212722,"text":"70212722 - 1938 - Ground‐water for air‐conditioning on Long Island, New York","interactions":[],"lastModifiedDate":"2020-08-26T18:02:47.291952","indexId":"70212722","displayToPublicDate":"1938-08-26T12:52:04","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water for air‐conditioning on Long Island, New York","docAbstract":"<p><span>During the last five years ground‐water has been more and more extensively used for air‐conditioning on Long Island, New York. The wide‐spread occurrence of highly permeable water‐bearing material and the relatively small cost of installation and operation of a ground‐water, air‐conditioning system has resulted in many such installations by theaters, restaurants, stores, and other establishments. Many companies likewise have taken advantage of these favorable factors and are utilizing low‐temperature ground‐water for cooling purposes in the manufacture of ice. This new use of ground‐water has considerably increased the draft in the western end of Long Island where there had already been so much over‐development that the watertable was below sea‐level in an area of more than 40 square miles. In 1933 the State Legislature, recognizing the seriousness of this over‐development, passed a law requiring that the approval, of the State Water Power and Control Commission be secured before constructing a well with a capacity greater than 100,000 gallons a day. Since the passage of the law the‐policy of the Commission has been to require water pumped from new‐wells for cooling purposes to be returned to the ground. This requirement has resulted in the construction of many recharge‐wells (locally called diffusion‐wells) through which the warm water is returned to the ground.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i001p00412","usgsCitation":"Leggette, R., and Brashears, M., 1938, Ground‐water for air‐conditioning on Long Island, New York: Eos, Transactions, American Geophysical Union, v. 19, no. 1, p. 412-418, https://doi.org/10.1029/TR019i001p00412.","productDescription":"7 p.","startPage":"412","endPage":"418","costCenters":[],"links":[{"id":377901,"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":"19","issue":"1","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":797357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brashears, M.L. Jr.","contributorId":23212,"corporation":false,"usgs":true,"family":"Brashears","given":"M.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":797358,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212718,"text":"70212718 - 1938 - Effect of a sea-level canal on the ground-water level of Florida","interactions":[],"lastModifiedDate":"2020-08-26T17:18:35.013879","indexId":"70212718","displayToPublicDate":"1938-08-26T12:07:34","publicationYear":"1938","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":"Effect of a sea-level canal on the ground-water level of Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.33.1.87","usgsCitation":"Thompson, D.G., Meinzer, O.E., and Stringfield, V.T., 1938, Effect of a sea-level canal on the ground-water level of Florida: Economic Geology, v. 33, no. 1, p. 87-107, https://doi.org/10.2113/gsecongeo.33.1.87.","productDescription":"21 p.","startPage":"87","endPage":"107","costCenters":[],"links":[{"id":377893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"1938-01-01","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":797347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meinzer, Oscar Edward","contributorId":12020,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":797348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":797349,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70160865,"text":"70160865 - 1938 - Records of the drilled wells of the island of Oahu, Hawaii","interactions":[],"lastModifiedDate":"2016-01-06T08:56:21","indexId":"70160865","displayToPublicDate":"1938-08-01T10:30:00","publicationYear":"1938","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":"4","title":"Records of the drilled wells of the island of Oahu, Hawaii","docAbstract":"<p>The description, location, log and meter tests of all the drilled wells on Oahu are given herein as of March 1 1938. Except for the discharges of plantation wells, which are published on pages 275 to 322 of Bulletin 1, head, chloride, and discharge records are listed only to the close of 1934, the date when this report was compiled. All head measurements and salt determinations made by the U.S. Geological Survey since 1934 will be found in the annual U.S. Geological Survey Water-Supply Papers entitled &ldquo;Water levels and artesian pressure in observation wells in the United States.&rdquo; Records of wells in the district of Honolulu are currently printed in the biennial reports of the Board of Water Supply, Honolulu. Most of the records of the plantation wells have been furnished by the owners.<br />Plate 2 shows the location of the wells, whether they are sealed, and whether the log is known. The static level or head of a well is the height above mean sea level to which the water will rise when all flow from the well is shut off. In the nonartesian wells the static level is the level of the water table of the basal zone of saturation in the basalts of the Koolau and Waianae volcanic series. Many of the wells are subartesian; that is, the water stands in the well above the level at which it was first encountered but does not overflow.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Honolulu, Oahu","collaboration":"Prepared in cooperation with the Geological Survey, United States Department of Interior","usgsCitation":"Stearns, H.T., and Vaksvik, K.N., 1938, Records of the drilled wells of the island of Oahu, Hawaii: Bulletin 4, 213 p.","productDescription":"213 p.","endPage":"213","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":221,"text":"Division of Hydrography","active":false,"usgs":true}],"links":[{"id":313174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70160865.JPG"},{"id":313173,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/stearns/Bulletin_4.pdf","size":"15.1 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568ba5dee4b0e7594ee776c1","contributors":{"authors":[{"text":"Stearns, Harold T.","contributorId":65831,"corporation":false,"usgs":true,"family":"Stearns","given":"Harold","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":584087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaksvik, Knute N.","contributorId":151030,"corporation":false,"usgs":false,"family":"Vaksvik","given":"Knute","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":584088,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32426,"text":"32426 - 1938 - The waterfowl situation: 1937-38","interactions":[],"lastModifiedDate":"2014-07-22T14:11:04","indexId":"32426","displayToPublicDate":"1938-01-01T14:09:56","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"111","title":"The waterfowl situation: 1937-38","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","collaboration":"Prepared in the Section of Distribution and Migration of Birds, Division of Wildlife Research.","usgsCitation":"U.S. Bureau of Biological Survey, 1938, The waterfowl situation: 1937-38: Wildlife Leaflet 111, 10 p.","productDescription":"10 p.","numberOfPages":"10","temporalStart":"1937-01-01","temporalEnd":"1938-01-01","costCenters":[],"links":[{"id":290729,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d34","contributors":{"authors":[{"text":"U.S. Bureau of Biological Survey","contributorId":128079,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Biological Survey","id":529376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70202627,"text":"ofr389 - 1938 - Ground-water conditions in a portion of the Rio San Jose-Bluewater valley in the vicinity of Grants, New Mexico","interactions":[],"lastModifiedDate":"2019-03-14T09:47:18","indexId":"ofr389","displayToPublicDate":"1938-01-01T10:47:02","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"38-9","title":"Ground-water conditions in a portion of the Rio San Jose-Bluewater valley in the vicinity of Grants, New Mexico","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr389","usgsCitation":"Morgan, A., 1938, Ground-water conditions in a portion of the Rio San Jose-Bluewater valley in the vicinity of Grants, New Mexico: U.S. Geological Survey Open-File Report 38-9, 23 p., https://doi.org/10.3133/ofr389.","productDescription":"23 p.","costCenters":[],"links":[{"id":362060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1938/0009/report-thumb.jpg"},{"id":362061,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1938/0009/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","city":"Grants","otherGeospatial":"San Jose - Bluewater Valley","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, Arthur M.","contributorId":59051,"corporation":false,"usgs":true,"family":"Morgan","given":"Arthur M.","affiliations":[],"preferred":false,"id":759293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159036,"text":"ar59 - 1938 - Fifty-ninth annual report of the Director of the Geological Survey","interactions":[],"lastModifiedDate":"2015-10-14T10:29:33","indexId":"ar59","displayToPublicDate":"1938-01-01T10:15:00","publicationYear":"1938","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":"59","title":"Fifty-ninth annual report of the Director of the Geological Survey","docAbstract":"<p>Basically important in the general program of conservation and development were the results of the Geological Survey's work during the fiscal year 1938. Investigations of the Nation's mineral and water supplies were conducted with all possible vigor and dispatch, thousands of square miles were surveyed for topographic maps, and technical supervision was given to prospecting, mining, and producing operations on public and Indian lands. This work was accomplished through the use of the regularly appropriated funds, the co-operative funds from States, counties, and municipalities, the funds transferred from other departments of the Government for types of work within the Survey's field, and the emergency funds derived chiefly from the Public Works Administration and devoted largely to mapping of various types and to studies of floods. The aggregate expenditures amounted to $5,248,000, which was 265,000 less than the amount expended during the preceding year.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/ar59","usgsCitation":"Mendenhall, W.C., 1938, Fifty-ninth annual report of the Director of the Geological Survey: U.S. Geological Survey Annual Report 59, 48 p., https://doi.org/10.3133/ar59.","productDescription":"48 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309872,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":309881,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ar/59/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":70195887,"text":"70195887 - 1938 - The municipal ground water supplies of North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T13:10:14","indexId":"70195887","displayToPublicDate":"1938-01-01T00:00:00","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5645,"text":"North Dakota Geological Survey Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"The municipal ground water supplies of North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"North Dakota Geological Survey","usgsCitation":"Abbott, G.A., and Voedisch, F.W., 1938, The municipal ground water supplies of North Dakota: North Dakota Geological Survey Bulletin 11, Report: 100 p.; 2 Plates.","productDescription":"Report: 100 p.; 2 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352281,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6f57e4b0da30c1bfe571","contributors":{"authors":[{"text":"Abbott, G. A.","contributorId":203049,"corporation":false,"usgs":false,"family":"Abbott","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":730398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voedisch, F. W.","contributorId":203050,"corporation":false,"usgs":false,"family":"Voedisch","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":730399,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000400,"text":"1000400 - 1938 - The food of the lake trout (Cristivomer namaycush namaycush) and of the lawyer (Lota maculosa) of Lake Michigan","interactions":[],"lastModifiedDate":"2016-02-04T10:04:43","indexId":"1000400","displayToPublicDate":"1938-01-01T00:00:00","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The food of the lake trout (Cristivomer namaycush namaycush) and of the lawyer (Lota maculosa) of Lake Michigan","docAbstract":"<p><span>This paper reports on a qualitative and quantitative analysis of the contents of 4,979 lake trout stomachs (593 examined in 1930 and 1,253 collected in 1931 from southern Lake Michigan, 1,446 from northern Lake Michigan and 1,687 from Green Bay in 1932), and of a total of 1,528 lawyer stomachs (172 examined in 1930 and 734 collected in 1931 from southern Lake Michigan, 612 from northern Lake Michigan and 10 from Green Bay in 1932). The food of the trout consisted of 98 per cent by volume of fish of which Cottidae and Coregonidae were the principal constituents. Cottidae were dominant in southern Lake Michigan (72 per cent by volume), Coregonidae in northern Lake Michigan (51 per cent) but the lake shiner, Notropis atherinides, was most important in Green Bay in the spring of the year (64 per cent). The lawyer food consisted of 74 per cent by volume of fish and 26 per cent invertebrates. Dominant items were Cottidae (76 per cent by volume) in southern Lake Michigan, Coregonidae (51 per cent) and Pontoporeia (37 per cent) in northern Lake Michigan, and Percopsis (34 per cent) and Mysis (26 per cent) in Green Bay. Data are also presented on the frequency of occurrence (number of stomachs) of the food items and its variation with the sizes of the trout and lawyers, depths of water, seasons, and localities; on the number of individual fish of each species destroyed by the trout and lawyers; and on the calculated volume of the food fishes preceding digestion. The lake trout and lawyer are competitors for the same food, are both predators of the commercially important Coregonidae, and the lawyer through its consumption of invertebrates is a food competitor of the Coregonidae.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1937)67[155:TFOTLT]2.0.CO;2","usgsCitation":"Van Oosten, J., and Deason, H.J., 1938, The food of the lake trout (Cristivomer namaycush namaycush) and of the lawyer (Lota maculosa) of Lake Michigan: Transactions of the American Fisheries Society, v. 67, no. 1, p. 155-177, https://doi.org/10.1577/1548-8659(1937)67[155:TFOTLT]2.0.CO;2.","productDescription":"22 p.","startPage":"155","endPage":"177","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":130290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65daec","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":308510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deason, Hilary J.","contributorId":66628,"corporation":false,"usgs":true,"family":"Deason","given":"Hilary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70040214,"text":"70040214 - 1937 - Record of wells in Kings County, N.Y.","interactions":[],"lastModifiedDate":"2012-10-05T17:16:22","indexId":"70040214","displayToPublicDate":"2012-01-01T12:40:00","publicationYear":"1937","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-3","title":"Record of wells in Kings County, N.Y.","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Leggette, R., 1937, Record of wells in Kings County, N.Y.: Bulletin GW-3, 175 p.; 1 Plate.","productDescription":"175 p.; 1 Plate","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262409,"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":"50e4a276e4b0e8fec6cdb5f2","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":467916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70006904,"text":"70006904 - 1937 - Furunculosis in wild trout","interactions":[],"lastModifiedDate":"2015-12-21T08:16:47","indexId":"70006904","displayToPublicDate":"2012-01-01T12:33:04","publicationYear":"1937","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Furunculosis in wild trout","docAbstract":"Furunculosis, or as it has been more appropiately termed, \"fish septicemia,\" is a disease primarily affecting salmon and trout. It is caused by the invasion and growth of Bacterium salmonicida Emmerich and Weibel, a Gram negative, non-spore forming, diplobacterium belonging to the family Bacteriaceae Cohn. After gaining entrance to the host, presumably by way of the digestive tract, the organism is spread by the blood stream and produces focal necrosis and subsequent liquefaction throughout the tissues. The more conspicuous gross lesions are those of the body musculature, characterized by the formation of deep seated \"boils\" or \"bloody blotches\"&mdash;blisters filled with liquefied muscle tissue and blood. Under favorable conditions, the muscle lesions enlarge rapidly and eventually rupture through the skin producing a characteristic, ragged, deep, undermining type of ulcer. Although the muscle lesions are most conspicuous, essentially the same progressive necrosis and liquefaction are to be found throughout the internal organs, particularly in the spleen and kidneys. The host has no adequate defense mechanism against this disease and no verified recovery from furunculosis has ever been recorded. Cases may be arrested by low water temperatures or other adverse factors, only to break out with renewed vigor when conditions again become favorable. The reader is referred to Plehn, Davis, Williamson, and Duff and Stewart for a more complete description of furunculosis.","language":"English","publisher":"American Society of Icthyologists and Herpetologists","publisherLocation":"Lawrence, KS","usgsCitation":"Fish, F.F., 1937, Furunculosis in wild trout: Copeia, v. 1, p. 37-40.","productDescription":"4 p.","startPage":"37","endPage":"40","numberOfPages":"4","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":258357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258342,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/1437366","linkFileType":{"id":5,"text":"html"}}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a142ce4b0c8380cd54937","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":355433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040179,"text":"70040179 - 1937 - Engineering report on the water supplies of Long Island","interactions":[],"lastModifiedDate":"2012-10-03T17:16:16","indexId":"70040179","displayToPublicDate":"2012-01-01T10:49:00","publicationYear":"1937","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-2","title":"Engineering report on the water supplies of Long Island","language":"English","publisher":"New York State Water Power and Control Commission","publisherLocation":"Albany, NY","usgsCitation":"Suter, R., 1937, Engineering report on the water supplies of Long Island: Bulletin GW-2, 64 p.; 7 Plates.","productDescription":"64 p.; 7 Plates","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262268,"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":"50db6523e4b061270600afae","contributors":{"authors":[{"text":"Suter, Russell","contributorId":107142,"corporation":false,"usgs":true,"family":"Suter","given":"Russell","email":"","affiliations":[],"preferred":false,"id":467833,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1731,"text":"wsp799 - 1937 - The floods of March 1936, part 2, Hudson River to Susquehanna River region","interactions":[],"lastModifiedDate":"2017-07-05T10:13:12","indexId":"wsp799","displayToPublicDate":"1994-01-01T00:00:00","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":"799","title":"The floods of March 1936, part 2, Hudson River to Susquehanna River region","docAbstract":"During the period March 9-22, 1936, there occurred in close succession over the northeastern United States, from the James and upper Ohio River Basins in Virginia and Pennsylvania to the river basins of Maine, two extraordinarily heavy storms, in which the precipitation was almost entirely in the form of rain. The depths of rainfall mark this period as one of the greatest concentrations of precipitation, in respect to time and magnitude of the area covered, of which there is record in this country. \r\n\r\nAt the time of the rain there were also accumulations of snow on the ground over much of the storm-affected region that were large for the season. The comparatively warm temperatures associated with the storms thawed the snow and added materially to the quantities of water to be disposed of by drainage into the waterways, by surface storage in lakes, ponds, and reservoirs, by absorption in the ground, and, probably in comparatively negligible degree, by evaporation. \r\n\r\nThe total quantity of water that had to be disposed of in these ways ranged between 10 and 30 inches in depth over much of the region. The water disposed of by natural storage, absorption, and evaporation amounted to average depths over the many river basins generally within the range of 1 to 3 inches, with a significant degree of uniformity and systematic areal distribution. The remainder of the rain and snow water, generally much larger or even several times larger in amount than surface storage, absorption, and evaporation, required accommodation by the channels of the brooks, creeks, and rivers. \r\n\r\nThere were generally two distinct flood peaks, and in many of the basins the destruction was seriously aggravated, especially during the first flood, by the break-up of thick ice cover accumulated through a winter of exceptionally continuous and severe cold weather. The resulting floods were extraordinarily severe, and records of river stages, extending on some streams back to or nearly to the time of settlement by white men, were broken many of them by wide margins. The peak of the Connecticut River at Hartford, Conn., was 8.6 feet higher than had been experienced since the settlement by white men, 300 years ago. The Susquehanna River at Harrisburg, Pa., was 3.5 feet higher than had been known in a period of record covering about 200 years. The Ohio River at Pittsburgh, Pa., was 6.1 feet higher than had been known in the period beginning 1762. \r\n\r\nThis volume presents many of the facts of these notable floods with respect to the New England rivers, for permanent record and for study and reference by engineers concerned with the building of highways, bridges, and industrial plants, planners of river development, and others. Similar volumes for the region from the Hudson River to the Susquehanna River and for the Potomac, James, and upper Ohio River Basins are presented in companion Water-Supply Papers 799 and 800 respectively. In this volume records of stage and discharge for the period Including the floods are presented for about 150 measurement stations; peak discharges with comparative data for other floods at more than 400 measurement points are summarized; crest stages along an aggregate length of stream channel of 2,820 miles are tabulated; and results of detailed studies of the rainfall and run-off and many other kinds of flood information are presented.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp799","usgsCitation":"Grover, N., 1937, The floods of March 1936, part 2, Hudson River to Susquehanna River region: U.S. Geological Survey Water Supply Paper 799, x, 380 p. :ill. ;23 cm., https://doi.org/10.3133/wsp799.","productDescription":"x, 380 p. :ill. ;23 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":136978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0799/report-thumb.jpg"},{"id":26837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0799/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69756a","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":144033,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":306,"text":"wsp795 - 1937 - Surface water supply of Hawaii : July 1, 1934 to June 30, 1935","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp795","displayToPublicDate":"1994-01-01T00:00:00","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":"795","title":"Surface water supply of Hawaii : July 1, 1934 to June 30, 1935","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp795","usgsCitation":"Grover, N., and Carson, M.H., 1937, Surface water supply of Hawaii : July 1, 1934 to June 30, 1935: U.S. Geological Survey Water Supply Paper 795, 138 p. ;23 cm., https://doi.org/10.3133/wsp795.","productDescription":"138 p. ;23 cm.","costCenters":[],"links":[{"id":136061,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0795/report-thumb.jpg"},{"id":24868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0795/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698299","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":142217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carson, Max H.","contributorId":21132,"corporation":false,"usgs":true,"family":"Carson","given":"Max","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":142218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2100,"text":"wsp796D - 1937 - Geology and ground-water resources of Ogden Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-07T15:18:03","indexId":"wsp796D","displayToPublicDate":"1994-01-01T00:00:00","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":"D","title":"Geology and ground-water resources of Ogden Valley, Utah","docAbstract":"<p>Ogden Valley is a fault trough bounded on both the east and west by faults that dip toward the middle of the valley. This fault trough contains unconsolidated deposits of clay, sand, and gravel, whose thickness is more than 600 feet. These materials are stream and lake deposits and in places are well sorted and stratified. The lake sediments were laid down in a small lake that occupied Ogden Valley and that was connected with glacial Lake Bonneville at its high stage by an arm of water that occupied Ogden Canyon. During this stage of Lake Bonneville the Ogden Valley was completely filled with lake sediments up to an altitude of about 4,900 feet. These sediments include about 70 feet of clay, sand, and gravel in alternating layers, below which is a bed of varved clay whose maximum thickness is about 70 feet. This clay is continuous under the lower parts of the valley and is the confining bed that produces the artesian conditions. Below the varved clay is a deposit of silt, sand, and gravel of unknown thickness, most of which is believed to be pre-Bonneville alluvium.</p><p>In most summers the streams entering Ogden Valley are diverted for irrigation, and the upper parts of their channels are generally dry during the irrigation season. Lower down in the valley seepage water appears in the channels, and below these points there is continuous flow. The flow of the Ogden River increases as it passes through Ogden Canyon. This gain in flow is believed to be derived chiefly from ground-water seepage from the canyon walls, although there is probably some groundwater underflow from Ogden Valley at the head of Ogden Canyon. Some of the gain is also due to leakage from pipe lines in the canyon.</p><p>Of the 146 wells whose records are given in this report, 70 are flowing wells. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp796D","collaboration":"Prepared in cooperation with the City of Ogden","usgsCitation":"Leggette, R., and Taylor, G., 1937, Geology and ground-water resources of Ogden Valley, Utah: U.S. Geological Survey Water Supply Paper 796, iv, p. 63 p.; 6 Plates: 23.50 x 18.50 inches or smaller, https://doi.org/10.3133/wsp796D.","productDescription":"iv, p. 63 p.; 6 Plates: 23.50 x 18.50 inches or smaller","startPage":"99","endPage":"161","numberOfPages":"67","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":247109,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-39.pdf","text":"Plate 39","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Stream flow in Ogden valley, 1933-34"},{"id":247108,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-38.pdf","text":"Plate 38","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of observation wells in Ogden valley and the flow of south fork of Ogden River"},{"id":247110,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-40.pdf","text":"Plate 40","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Well logs, Ogden Valley, Utah"},{"id":138192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0796d/report-thumb.jpg"},{"id":27674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0796d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247105,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-35.pdf","text":"Plate 35","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Annual cumulative departure from normal precipitation at Ogden, Utah, and annual precipitation at Ogden and Huntsville, Utah"},{"id":247106,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-36.pdf","text":"Plate 36","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of a part of Ogden Valley, Weber County, Utah"},{"id":247107,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0796d/plate-37.pdf","text":"Plate 37","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Graphs of the flow of south fork of Ogden river, the precipitation at Ogden, the withdrawal of ground water at Artesian park, and the water levels in five observation wells in Ogden valley, 1932-35"}],"country":"United States","state":"Utah","county":"Weber County","otherGeospatial":"Ogden Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859d7","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":144675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":144674,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":45305,"text":"b883A - 1937 - Spirit leveling in Texas. Part 1, Western Texas, 1896-1935","interactions":[],"lastModifiedDate":"2012-02-02T00:04:53","indexId":"b883A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1937","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"883","chapter":"A","title":"Spirit leveling in Texas. Part 1, Western Texas, 1896-1935","language":"ENGLISH","doi":"10.3133/b883A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Spirit leveling in Texas. Part 1, Western Texas, 1896-1935: U.S. Geological Survey Bulletin 883, 1-50 p., https://doi.org/10.3133/b883A.","productDescription":"1-50 p.","costCenters":[],"links":[{"id":93969,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0883a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0883a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a47","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":531580,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":1602,"text":"wsp813 - 1937 - Surface water supply of the United States, 1936 : Part 13 Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp813","displayToPublicDate":"1994-01-01T00:00:00","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":"813","title":"Surface water supply of the United States, 1936 : Part 13 Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp813","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1936 : Part 13 Snake River basin: U.S. Geological Survey Water Supply Paper 813, 242 p. :ill. ;23 cm., https://doi.org/10.3133/wsp813.","productDescription":"242 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0813/report-thumb.jpg"},{"id":26667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0813/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697677","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":527965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":4535,"text":"wsp790 - 1937 - Surface water supply of the United States, 1935 : Part 10, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp790","displayToPublicDate":"1994-01-01T00:00:00","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":"790","title":"Surface water supply of the United States, 1935 : Part 10, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp790","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935 : Part 10, The Great Basin: U.S. Geological Survey Water Supply Paper 790, 94 p. ;23 cm., https://doi.org/10.3133/wsp790.","productDescription":"94 p. ;23 cm.","costCenters":[],"links":[{"id":139702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0790/report-thumb.jpg"},{"id":31592,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0790/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697686","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":528233,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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