{"pageNumber":"2705","pageRowStart":"67600","pageSize":"25","recordCount":68807,"records":[{"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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,{"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":500,"text":"wsp812 - 1937 - Surface water supply of the United States, 1936 : Part 12, North Pacific drainage basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp812","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":"812","title":"Surface water supply of the United States, 1936 : Part 12, North Pacific drainage basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1936 : Part 12, North Pacific drainage basins: U.S. Geological Survey Water Supply Paper 812, 161 p. ;23 cm., https://doi.org/10.3133/wsp812.","productDescription":"161 p. ;23 cm.","costCenters":[],"links":[{"id":136077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0812/report-thumb.jpg"},{"id":25063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0812/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697676","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":527472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4609,"text":"wsp783 - 1937 - Surface water supply of the United States, 1935, Part III, Ohio River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"wsp783","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":"783","title":"Surface water supply of the United States, 1935, Part III, Ohio River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp783","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935, Part III, Ohio River basin: U.S. Geological Survey Water Supply Paper 783, 400 p. ;23 cm., https://doi.org/10.3133/wsp783.","productDescription":"400 p. ;23 cm.","costCenters":[],"links":[{"id":139301,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0783/report-thumb.jpg"},{"id":31666,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0783/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697662","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":528303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1875,"text":"wsp819 - 1937 - The warm springs of Georgia, their geologic relations and origin, a summary report","interactions":[],"lastModifiedDate":"2017-02-03T12:39:19","indexId":"wsp819","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":"819","title":"The warm springs of Georgia, their geologic relations and origin, a summary report","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp819","usgsCitation":"Hewett, D.F., and Crickmay, G.W., 1937, The warm springs of Georgia, their geologic relations and origin, a summary report: U.S. Geological Survey Water Supply Paper 819, iv, 40 p. :illus., 8 pl. (incl. fold. maps: 1 in pocket) fold. diagrs. ;23 cm., https://doi.org/10.3133/wsp819.","productDescription":"iv, 40 p. :illus., 8 pl. (incl. fold. maps: 1 in pocket) fold. diagrs. ;23 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":27162,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0819/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27163,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0819/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0819/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ],\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ],\n            [\n              -83.7103271484375,\n              35.67068501330236\n            ],\n            [\n              -83.7103271484375,\n              35.67068501330236\n            ],\n            [\n              -83.71307373046874,\n              35.67068501330236\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.4072265625,\n              32.0639555946604\n            ],\n            [\n              -87.4072265625,\n              33.48185394054361\n            ],\n            [\n              -83.38623046875,\n              33.48185394054361\n            ],\n            [\n              -83.38623046875,\n              32.0639555946604\n            ],\n            [\n              -87.4072265625,\n              32.0639555946604\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62eef8","contributors":{"authors":[{"text":"Hewett, D. F.","contributorId":19927,"corporation":false,"usgs":true,"family":"Hewett","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144290,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crickmay, Geoffrey William","contributorId":105696,"corporation":false,"usgs":true,"family":"Crickmay","given":"Geoffrey","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":144291,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1739,"text":"wsp798 - 1937 - The floods of March 1936, part 1, New England rivers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp798","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":"798","title":"The floods of March 1936, part 1, New England rivers","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. G.P.O.,","doi":"10.3133/wsp798","usgsCitation":"Grover, N.C., 1937, The floods of March 1936, part 1, New England rivers: U.S. Geological Survey Water Supply Paper 798, x, 466 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp798.","productDescription":"x, 466 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0798/report-thumb.jpg"},{"id":26844,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0798/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65db1b","contributors":{"authors":[{"text":"Grover, Nathan Clifford","contributorId":66660,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan","email":"","middleInitial":"Clifford","affiliations":[],"preferred":false,"id":144050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1732,"text":"wsp800 - 1937 - The floods of March 1936, Part 3, Potomac, James, and upper Ohio Rivers","interactions":[],"lastModifiedDate":"2017-07-05T10:12:20","indexId":"wsp800","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":"800","title":"The floods of March 1936, Part 3, Potomac, James, and upper Ohio Rivers","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/wsp800","usgsCitation":"Grover, N., and Lichtblau, S., 1937, The floods of March 1936, Part 3, Potomac, James, and upper Ohio Rivers: U.S. Geological Survey Water Supply Paper 800, ix, 351 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp800.","productDescription":"ix, 351 p. :ill., maps ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":26838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0800/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0800/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65db64","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":144034,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lichtblau, Stephen","contributorId":18340,"corporation":false,"usgs":true,"family":"Lichtblau","given":"Stephen","email":"","affiliations":[],"preferred":false,"id":144035,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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}]}}
,{"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}]}}
,{"id":3153,"text":"wsp679B - 1937 - Thermal springs in the United States","interactions":[],"lastModifiedDate":"2024-02-01T22:18:55.044119","indexId":"wsp679B","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":"679","chapter":"B","title":"Thermal springs in the United States","docAbstract":"<p>The earliest extensive studies of thermal springs in the United States were made by physicians. In 1831 Dr. John Bell issued a book entitled \"Baths and Mineral Waters\" in which he listed 21 spring localities. In the edition of his work published in 1855 the number was increased to 181. The earliest report on a geologic study of thermal springs was that of W. B, Rogers in 1840 on the thermal springs of Virginia. In 1875 G. K. Gilbert published a map and table showing thermal springs in the United States and pointed out that they are present chiefly in the mountainous areas of folded and faulted rocks. Early geologic study of them was principally inspired by the information which they afford at a few places on the deposition of minerals. The relation of hot springs to volcanic action has been studied in the Yellowstone National Park and near Lassen Peak in California. Studies in recent years have been concerned with the source of the water as well as of its heat.</p><p>All the notable thermal springs in the eastern United States are in the Appalachian Highlands, principally in the region of folded rocks. The Atlantic Coastal Plain contains no appreciably warm springs. In Florida there are large springs whose water rises from a depth of a few hundred feet and is about 5° above the mean annual temperature, but they are not usually classed as thermal.</p><p>The only warm springs in the great Interior Plains region are at and near Hot Springs, S. Dak., in the vicinity of the Black Hills uplift of crystalline rocks. In the Interior Highlands thermal springs occur only in the Ozark region, the largest group being at Hot Springs, Ark.</p><p>The Rocky Mountain System includes the Yellowstone National Park, with its world-famous hot springs and geysers (see pis. 7,12), and there are many other hot springs within this great mountainous region. In the Intermontane areas of great lava plains and faulted lava mountains in Utah, Nevada, southern Idaho, and eastern Oregon there are many hot springs, closely associated with the larger faults. In the Pacific Mountain System, including the Cascade Range and Sierra Nevada, there are many warm and hot springs, some of which issue in areas of granite, and others in areas of lava. In the Coast Ranges of California many thermal springs issue from different geologic formations.</p><p>Of the total of more than 1,000 thermal-spring localities listed in this paper more than half are situated in the three States of Idaho, California, and Nevada, each of which contains more than 150 thermal-spring localities. Wyoming, including the Yellowstone National Park, contains more than 100 hot-spring localities. Oregon, Utah, Colorado, Montana, and New Mexico contain several dozen thermal springs each, of which the principal ones are developed as resorts. The other thermal springs are scattered through 12 States, of which Massachusetts, New York, Pennsylvania, and North Carolina contain one spring or group each. More than half of the total number are developed as resorts or used for irrigation or water supply, but many have remained undeveloped because they are not easily accessible. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp679B","usgsCitation":"Stearns, N., Stearns, H.T., and Waring, G.A., 1937, Thermal springs in the United States: U.S. Geological Survey Water Supply Paper 679, Report: iv, 147 p.; 1 Plate: 29.00 x 20.00 inches, https://doi.org/10.3133/wsp679B.","productDescription":"Report: iv, 147 p.; 1 Plate: 29.00 x 20.00 inches","startPage":"59","endPage":"206","numberOfPages":"175","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science 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New Mexico","linkFileType":{"id":5,"text":"html"}},{"id":425258,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24627.htm","text":"Idaho, Montana, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":425257,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24627.htm","text":"Georgia","linkFileType":{"id":5,"text":"html"}},{"id":425256,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24627.htm","text":"California - Nevada","linkFileType":{"id":5,"text":"html"}}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n          [\n            [\n              [\n                -94.81758,\n                49.38905\n              ],\n              [\n                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A.","contributorId":100365,"corporation":false,"usgs":true,"family":"Waring","given":"Gerald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146342,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2147,"text":"wsp778 - 1937 - Geology and ground-water resources of Webb County, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:17:50","indexId":"wsp778","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":"778","title":"Geology and ground-water resources of Webb County, Texas","docAbstract":"<p>Webb County is in southwestern Texas and is a part of the Winter Garden district. The purpose of the investigation here recorded was to determine the source, quantity, and quality of the ground water used for irrigation and other purposes in the area.</p>","language":"English","publisher":"U. S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp778","usgsCitation":"Lonsdale, J.T., and Day, J.R., 1937, Geology and ground-water resources of Webb County, Texas: U.S. Geological Survey Water Supply Paper 778, Report: v, 104 p.; Plate: 46.35 x 35.00 inches, https://doi.org/10.3133/wsp778.","productDescription":"Report: v, 104 p.; Plate: 46.35 x 35.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0778/report-thumb.jpg"},{"id":27756,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0778/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27757,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0778/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109958,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24643.htm","linkFileType":{"id":5,"text":"html"},"description":"24643"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685816","contributors":{"authors":[{"text":"Lonsdale, John T.","contributorId":30210,"corporation":false,"usgs":true,"family":"Lonsdale","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, James R.","contributorId":81474,"corporation":false,"usgs":true,"family":"Day","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144739,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":490,"text":"wsp792 - 1937 - Surface water supply of the United States, 1935 : Part 12, North Pacific drainage basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp792","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":"792","title":"Surface water supply of the United States, 1935 : Part 12, North Pacific drainage basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp792","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935 : Part 12, North Pacific drainage basins: U.S. Geological Survey Water Supply Paper 792, 166 p. ;23 cm., https://doi.org/10.3133/wsp792.","productDescription":"166 p. ;23 cm.","costCenters":[],"links":[{"id":136676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0792/report-thumb.jpg"},{"id":25053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0792/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697701","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":527462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":493,"text":"wsp782 - 1937 - Surface water supply of the United States, 1935, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp782","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":"782","title":"Surface water supply of the United States, 1935, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp782","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 782, 233 p. ;23 cm., https://doi.org/10.3133/wsp782.","productDescription":"233 p. ;23 cm.","costCenters":[],"links":[{"id":135991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0782/report-thumb.jpg"},{"id":25056,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0782/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976f9","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":527465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":492,"text":"wsp781 - 1937 - Surface water supply of the United States, 1935, Part I, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp781","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":"781","title":"Surface water supply of the United States, 1935, Part I, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp781","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1937, Surface water supply of the United States, 1935, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 781, 421 p. ;23 cm., https://doi.org/10.3133/wsp781.","productDescription":"421 p. ;23 cm.","costCenters":[],"links":[{"id":135990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0781/report-thumb.jpg"},{"id":25055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0781/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976d5","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":527464,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2833,"text":"wsp796C - 1937 - Flood in La Canada Valley, California, January 1, 1934","interactions":[],"lastModifiedDate":"2018-12-17T10:04:57","indexId":"wsp796C","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":"C","title":"Flood in La Canada Valley, California, January 1, 1934","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp796C","usgsCitation":"Troxell, H., and Peterson, J., 1937, Flood in La Canada Valley, California, January 1, 1934: U.S. Geological Survey Water Supply Paper 796, p.iii-iv, 53-98, [11] leaves of plates :ill. (some folded), charts, map ;24 cm., https://doi.org/10.3133/wsp796C.","productDescription":"p.iii-iv, 53-98, [11] leaves of plates :ill. (some folded), charts, map ;24 cm.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":138840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0796c/report-thumb.jpg"},{"id":29400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0796c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef0d3","contributors":{"authors":[{"text":"Troxell, H.C.","contributorId":69124,"corporation":false,"usgs":true,"family":"Troxell","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":145873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, John Q.","contributorId":76292,"corporation":false,"usgs":true,"family":"Peterson","given":"John Q.","affiliations":[],"preferred":false,"id":145874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53029,"text":"ofr372 - 1937 - Ground water in Creek County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:26","indexId":"ofr372","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1937","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":"37-2","title":"Ground water in Creek County, Oklahoma","docAbstract":"Creek County has been designated as a problem area by the Land Use Planning Section of the Resettlement Administration. Some of the earliest oil fields to brought into production were situated in and near this county, and new fields have been opened from time to time during the ensuing years. The production of the newer fields, however, has not kept pace with the exhaustion of the older fields, and the county now presents an excellent picture of the problems involved in adjusting a population to lands that are nearly depleted of their mineral wealth. Values of land have been greatly depressed; tax collection is far in arrears; tenancy is widespread; and in addition more people will apparently be forced to depend on the income from agriculture than the land seems capable of supporting. The county as a whole is at best indifferently suitable for general farming. The Land Use planning Section proposes to study the present and seemingly immanent maladjustments of population to the resources of the land, and make recommendations for their correction.\r\nThe writer was detailed to the Land Use Planning Section of Region VIII for the purposes of making studies of ground water problems in the region. In Creek County two investigations were made. In September, 1936, the writer spent about ten days investigating the availability of ground water for the irrigation of garden crops during drouths. If it proved feasible to do this generally throughout the county, the Land Use Planning Section might be able to encourage this practice. The second investigation made by the writer was in regard to the extent to which ground water supplies have been damaged by oil well brines. He was in county for four days late in January 1937, and again in March, 1937. During part of the second field trip he was accompanied by R.M. Dixon, sanitary engineer of the Water Utilization Unit of the Resettlement Administration.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr372","usgsCitation":"Cady, R.C., 1937, Ground water in Creek County, Oklahoma: U.S. Geological Survey Open-File Report 37-2, 12 leaves ; 28 cm., https://doi.org/10.3133/ofr372.","productDescription":"12 leaves ; 28 cm.","costCenters":[],"links":[{"id":178656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db42","contributors":{"authors":[{"text":"Cady, Richard Carlysle","contributorId":11587,"corporation":false,"usgs":true,"family":"Cady","given":"Richard","email":"","middleInitial":"Carlysle","affiliations":[],"preferred":false,"id":246398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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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