{"pageNumber":"7228","pageRowStart":"180675","pageSize":"25","recordCount":184617,"records":[{"id":1592,"text":"wsp751 - 1935 - Surface water supply of the United States, 1933 : Part 11. Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"751","title":"Surface water supply of the United States, 1933 : Part 11. Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp751","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933 : Part 11. Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 751, xi, 376 p. :ill. ;23 cm., https://doi.org/10.3133/wsp751.","productDescription":"xi, 376 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0751/report-thumb.jpg"},{"id":26657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0751/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697839","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":527955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1598,"text":"wsp769 - 1935 - Surface water supply of the United States, 1934 : Part 12. North Pacific slope basins : C. Pacific slope basins in Oregon and Lower Columbia River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"769","title":"Surface water supply of the United States, 1934 : Part 12. North Pacific slope basins : C. Pacific slope basins in Oregon and Lower Columbia River Basin","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp769","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1934 : Part 12. North Pacific slope basins : C. Pacific slope basins in Oregon and Lower Columbia River Basin: U.S. Geological Survey Water Supply Paper 769, vi, 165 p. :ill. ;23 cm., https://doi.org/10.3133/wsp769.","productDescription":"vi, 165 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0769/report-thumb.jpg"},{"id":26663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6961ef","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":527961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53531,"text":"naf54 - 1935 - Alaska-Yukon caribou","interactions":[],"lastModifiedDate":"2012-02-02T00:11:47","indexId":"naf54","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":58,"text":"North American Fauna","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"54","title":"Alaska-Yukon caribou","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Murie, O., 1935, Alaska-Yukon caribou: North American Fauna 54, 93 p. illus. 10 pl. on 6 l., maps (1 double) 23 cm.","productDescription":"93 p. illus. 10 pl. on 6 l., maps (1 double) 23 cm.","costCenters":[],"links":[{"id":22640,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.fwspubs.org/toc/nafa//54","linkFileType":{"id":5,"text":"html"}},{"id":175263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688283","contributors":{"authors":[{"text":"Murie, Olaus J.","contributorId":104120,"corporation":false,"usgs":true,"family":"Murie","given":"Olaus J.","affiliations":[],"preferred":false,"id":247754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4733,"text":"wsp754 - 1935 - Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; C. Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"wsp754","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"754","title":"Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; C. Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp754","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; C. Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 754, vi, 170 p. ;23 cm., https://doi.org/10.3133/wsp754.","productDescription":"vi, 170 p. ;23 cm.","costCenters":[],"links":[{"id":139609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0754/report-thumb.jpg"},{"id":31719,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0754/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69783e","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":528352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1593,"text":"wsp753 - 1935 - Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; B. Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"753","title":"Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; B. Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp753","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; B. Snake River basin: U.S. Geological Survey Water Supply Paper 753, vii, 197 p. ;24 cm., https://doi.org/10.3133/wsp753.","productDescription":"vii, 197 p. ;24 cm.","costCenters":[],"links":[{"id":137498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0753/report-thumb.jpg"},{"id":26658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0753/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69783b","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":527956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39329,"text":"pp180 - 1935 - The minerals of Franklin and Sterling Hill, Sussex County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"pp180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"180","title":"The minerals of Franklin and Sterling Hill, Sussex County, New Jersey","language":"ENGLISH","doi":"10.3133/pp180","usgsCitation":"Palache, C., 1935, The minerals of Franklin and Sterling Hill, Sussex County, New Jersey: U.S. Geological Survey Professional Paper 180, 135 p., https://doi.org/10.3133/pp180.","productDescription":"135 p.","costCenters":[],"links":[{"id":113489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0180/report.pdf","size":"28572","linkFileType":{"id":1,"text":"pdf"}},{"id":169978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0180/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4944","contributors":{"authors":[{"text":"Palache, Charles","contributorId":102940,"corporation":false,"usgs":true,"family":"Palache","given":"Charles","email":"","affiliations":[],"preferred":false,"id":221313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39328,"text":"pp179 - 1935 - Origin of the copper deposits of the Ducktown type in the southern Appalachian region","interactions":[],"lastModifiedDate":"2020-08-31T15:59:11.987116","indexId":"pp179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"179","title":"Origin of the copper deposits of the Ducktown type in the southern Appalachian region","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp179","usgsCitation":"Ross, C.S., 1935, Origin of the copper deposits of the Ducktown type in the southern Appalachian region: U.S. Geological Survey Professional Paper 179, 165 p., https://doi.org/10.3133/pp179.","productDescription":"165 p.","costCenters":[],"links":[{"id":169977,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0179/report-thumb.jpg"},{"id":113488,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0179/report.pdf","size":"52448","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia, North Carolina, South Carolina, Tennessee, Virginia, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.211669921875,\n              38.453588708941375\n            ],\n            [\n              -80.936279296875,\n              37.75334401310656\n            ],\n            [\n              -84.0234375,\n              36.09349937380574\n            ],\n            [\n              -84.990234375,\n              35.003003395276714\n            ],\n            [\n              -83.924560546875,\n              34.17090836352573\n            ],\n            [\n              -82.342529296875,\n              34.93097858831627\n            ],\n            [\n              -80.277099609375,\n              36.527294814546245\n            ],\n            [\n              -77.71728515624999,\n              38.25543637637947\n            ],\n            [\n              -78.211669921875,\n              38.453588708941375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a67b","contributors":{"authors":[{"text":"Ross, C. S.","contributorId":18337,"corporation":false,"usgs":true,"family":"Ross","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":221312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39327,"text":"pp177 - 1935 - The Gold Hill Mining District, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"pp177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"177","title":"The Gold Hill Mining District, Utah","docAbstract":"The Gold Hill quadrangle is in west central Utah and is limited by parallels 40? and 40?15' and meridians 113?45' and 114?. This area includes the norlh end of the Deep Creek Mountains, one of the ranges in the Great Basin. The climate of the region, like that of the major province, is relatively arid, the average annual rainfall being about 13 inches.\r\n","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp177","usgsCitation":"Nolan, T.B., 1935, The Gold Hill Mining District, Utah: U.S. Geological Survey Professional Paper 177, viii, 172 p., https://doi.org/10.3133/pp177.","productDescription":"viii, 172 p.","costCenters":[],"links":[{"id":104370,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4174.htm","linkFileType":{"id":5,"text":"html"},"description":"4174"},{"id":120463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_177.jpg"},{"id":13721,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0177/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4994e4b07f02db5b5f34","contributors":{"authors":[{"text":"Nolan, T. B.","contributorId":71610,"corporation":false,"usgs":true,"family":"Nolan","given":"T.","middleInitial":"B.","affiliations":[],"preferred":false,"id":221311,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2146,"text":"wsp676 - 1935 - Geology and ground-water resources of Atascosa and Frio Counties, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:12:39","indexId":"wsp676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"676","title":"Geology and ground-water resources of Atascosa and Frio Counties, Texas","docAbstract":"<p>Atascosa and Frio Counties are in southwestern Texas and form 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/wsp676","isbn":"pbk","usgsCitation":"Lonsdale, J.T., 1935, Geology and ground-water resources of Atascosa and Frio Counties, Texas: U.S. Geological Survey Water Supply Paper 676, Report: v, 90 p.; 2 Plates: 41.00 x 25.50 inches and 41.00 x 25.50 inches, https://doi.org/10.3133/wsp676.","productDescription":"Report: v, 90 p.; 2 Plates: 41.00 x 25.50 inches and 41.00 x 25.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0676/report-thumb.jpg"},{"id":27753,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0676/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27754,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0676/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27755,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109954,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24624.htm","linkFileType":{"id":5,"text":"html"},"description":"24624"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c12","contributors":{"authors":[{"text":"Lonsdale, John T.","contributorId":30210,"corporation":false,"usgs":true,"family":"Lonsdale","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":144737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1945,"text":"wsp657 - 1935 - Water utilization in the Snake River Basin","interactions":[],"lastModifiedDate":"2017-09-08T14:27:39","indexId":"wsp657","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"657","title":"Water utilization in the Snake River Basin","docAbstract":"<p>The purpose of this report is to describe the present utilization of the water in the Snake River Basin with special reference to irrigation and power and to present essential facts concerning possible future utilization. No detailed plan of development is suggested. An attempt has been made, however, to discuss features that should be taken into account in the formulation of a definite plan of development. On account of the size of the area involved, which is practically as large as the New England States and New York combined, and the magnitude of present development and future possibilities, considerable details have of necessity been omitted. The records of stream flow in the basin are contained in the reports on surface water supply published annually by the Geological Survey. These records are of the greatest value in connection with the present and future regulation and utilization of the basin's largest asset water.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp657","usgsCitation":"Hoyt, W.G., and Stabler, H., 1935, Water utilization in the Snake River Basin: U.S. Geological Survey Water Supply Paper 657, Report: vii, 379 p.; 5 Plates: 15.00 x 15.50 inches each, https://doi.org/10.3133/wsp657.","productDescription":"Report: vii, 379 p.; 5 Plates: 15.00 x 15.50 inches each","numberOfPages":"426","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27274,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0657/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing general vegatation in Snake River basin"},{"id":27275,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0657/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map of Snake River basin"},{"id":27276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0657/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0657/report-thumb.jpg"},{"id":27271,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0657/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing water utilization in Snake River basin"},{"id":27272,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0657/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing altitudes above sea level in Snake River basin"},{"id":27273,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0657/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing precipitation in Snake River basin"}],"country":"United States","otherGeospatial":"Snake River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4991e4b07f02db5b3dac","contributors":{"authors":[{"text":"Hoyt, William Glenn","contributorId":14382,"corporation":false,"usgs":true,"family":"Hoyt","given":"William","email":"","middleInitial":"Glenn","affiliations":[],"preferred":false,"id":144413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stabler, Herman","contributorId":83498,"corporation":false,"usgs":true,"family":"Stabler","given":"Herman","email":"","affiliations":[],"preferred":false,"id":144414,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35174,"text":"b853 - 1935 - Zinc and lead deposits of northern Arkansas","interactions":[],"lastModifiedDate":"2015-12-10T15:19:07","indexId":"b853","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"853","title":"Zinc and lead deposits of northern Arkansas","docAbstract":"<p>Zinc and lead ores occur in the northern counties of Arkansas, from the Arkansas-Oklahoma line on the west to the Coastal Plain, in Lawrence County, on the east, but are concentrated chiefly in Marion, Boone, Newton, Searcy, Sharp, and Lawrence Counties. &nbsp;Lead ore was reported in the region as early as 1818, and small reduction plants were built in the vicinity of Lead Hill in 1851 or 1852. &nbsp;The Confederate forces obtained lead from northern Arkansas during the Civil War. &nbsp;Zinc mining began at a somewhat later date and reached its peak between 1914 and 1917, but since that time mining has been at a low ebb. &nbsp;The later history of lead mining in the region has closely paralleled that of zinc. &nbsp;The production from the region since 1907, according to statistics compiled by the United States Geological Survey, has been, in round numbers, 1,900 tons of lead sulphide concentrates, 11,5000 tons of zinc sulphide concentrates, and 51,3000 tons of zinc carbonate and silicate concentrates.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b853","usgsCitation":"McKnight, E., 1935, Zinc and lead deposits of northern Arkansas: U.S. Geological Survey Bulletin 853, Report: iv, 311 p.; 6 Plates: 27.46 x 19.97 inches or smaller, https://doi.org/10.3133/b853.","productDescription":"Report: iv, 311 p.; 6 Plates: 27.46 x 19.97 inches or 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,{"id":4606,"text":"wsp743 - 1935 - Surface water supply of the United States, 1933, Part III, Ohio River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp743","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"743","title":"Surface water supply of the United States, 1933, Part III, Ohio River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp743","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933, Part III, Ohio River basin: U.S. Geological Survey Water Supply Paper 743, ix, 357 p. ;23 cm., https://doi.org/10.3133/wsp743.","productDescription":"ix, 357 p. ;23 cm.","costCenters":[],"links":[{"id":139594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0743/report-thumb.jpg"},{"id":31663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0743/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697827","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":528300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4607,"text":"wsp748 - 1935 - Surface water supply of the United States, 1933, Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"748","title":"Surface water supply of the United States, 1933, Part VIII, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp748","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933, Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 748, vi, 180 p. ;23 cm., https://doi.org/10.3133/wsp748.","productDescription":"vi, 180 p. ;23 cm.","costCenters":[],"links":[{"id":139595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0748/report-thumb.jpg"},{"id":31664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0748/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6977e2","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":528301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159038,"text":"ar56 - 1935 - Fifty-sixth annual report of the Director of the Geological Survey","interactions":[],"lastModifiedDate":"2015-10-14T10:27:09","indexId":"ar56","displayToPublicDate":"1940-01-01T00:00:00","publicationYear":"1935","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":"56","title":"Fifty-sixth annual report of the Director of the Geological Survey","docAbstract":"<p>During the fiscal year 1934-35, although directly appropriated funds for the support of the Survey's regular activities have been at a low ebb (see details in later pages), these have been augmented by substantial allocations for closely related work made by the Public Works Administration.</p>","language":"English","publisher":"U.S. Printing Office","publisherLocation":"Washington, 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,{"id":70160862,"text":"70160862 - 1935 - Geology and ground-water resources of the island of Oahu, Hawaii","interactions":[],"lastModifiedDate":"2016-01-06T08:55:05","indexId":"70160862","displayToPublicDate":"1939-01-01T10:00:00","publicationYear":"1935","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":"1","title":"Geology and ground-water resources of the island of Oahu, Hawaii","docAbstract":"<p>Oahu, one of the islands of the Hawaiian group, lies in the Mid-Pacific 2,100 miles southwest of San Francisco. The principal city is Honolulu. The Koolau Range makes up the eastern part of the island, and the Waianae Range the western part. Both are extinct basaltic volcanoes deeply dissected by erosion. The Koolau Volcano was the later to become extinct.<br /> The Waianae Range is made up of three groups of lavas erupted in Tertiary and possibly in early Pleistocene time. The exposed part of the older lava is nearly 2,000 feet thick and consists largely of thin-bedded pahoehoe. It is separated in most places from the middle lavas by an angular unconformity and talus breccia and in a few places by an erosional unconformity. The middle basalts are about 2,000 feet thick and closely resemble the lower ones except that they contain more aa. The upper lavas reach a thickness of about 2,300 feet and are mostly massive aa flows. The last eruptions produced large cinder cones and some nephelite basalts. The Waianae Volcano, like other Hawaiian volcanoes, produced only small amounts of ash, and the lavas were largely extruded from fissures a few feet wide, now occupied by dikes. The center of activity was near Kolekole Pass, at the head of Lualualei Valley.<br />The Koolau Volcano is made up of two groups of lavas extruded in Tertiary and early Pleistocene (?) time. The older group, the Kailua volcanic series, is greatly altered by hydrothermal action and was extruded from fissures near Lanikai. The flows of the younger group, the Koolau volcanic series, were extruded from fissures about a mile south of the Kailua rift and have an exposed thickness of about 3,000 feet. The Koolau Volcano produced even less ash than the Waianae Volcano, and its flows are thin-bedded pahoehoe and aa. The eruptive center of the Koolau Volcano lies between Kaneohe and Waimanalo. <br />Great amounts of both the Waianae and Koolau Ranges were removed by fluvial and marine erosion during the Pleistocene. The master streams are characterized by deep amphitheater-headed valleys. After this erosion cycle the island was submerged more than 1,200 feet, and these great valleys were drowned and alluviated. Besides this submergence, several strand lines, preserved up to 100 feet above present sea level occur, which may be due to world-wide changes in sea level in response to the withdrawal and restoration of water concurrent with the advances and recessions of the polar ice caps and to accompanying changes in the ocean floor. During this time of shifting ocean levels spasmodic eruptions occurred on the southeast end of the Koolau Range, producing numerous lava flows and tuff cones, most of which are nephelite basalt. <br />The last of these eruptions occurred in Recent time. A description of the climate, rates of run-off, and results of experiments to determine evaporation and transpiration in the areas of high rainfall are given. It was found that the consumptive use decreases materially and becomes a very small percentage of the rainfall in the areas of high precipitation. <br />The lava rocks of the island are very permeable and, because of a rainfall reaching a maximum of 300 inches a year, carry large amounts of ground water, confined and unconfined, basal and perched. The basal ground water floats on salt water because of its lower specific gravity. Consequently for each foot the water table stands above sea level, salt water lies about 42 feet below sea level, in accordance with the sea along the coast as basal ground water. In most places the lava rocks along the shore are overlain by an impermeable or nearly impermeable caprock consisting of submerged lateritic soils and marine noncalcareous sediments. These deposits retard the escape of basal ground water into the sea and give rise to artesian water, but unlike most other artesian systems, this one has no lower restraining formation. <br />The artesian water is the principal source of domestic, municipal, and irrigation supplies. The average annual quantity pumped for the period 1928 to 1933 amounted to about 105,000,000,000 gallons, nearly 90 percent of which came from Koolau hasalt and the remainder from Waianae basalt. <br />There are ten artesian areas in the Koolau Range and two in the Waianae Range. Hydraulic gradients in these basins were found to range from 1.2 to 3 feet to the mile. Because of these extremely flat gradients and the high permeability of the aquifers it is possible to reverse the hydraulic gradients by draft and make the water flow from one artesian area to another. <br />The artesian water levels fluctuate in response to seasonal variations in draft and recharge and in a lesser way to tidal, barometric, and seismic pressures. <br />The water, as shown by chemical analysis, is of excellent quality except where it is contaminated with sea water. Methods have been devised for freshening wells that have gone salty, for detecting leaks, for sealing leaky and defective wells, and for recharging the artesian basins. <br />Owing to the danger of the wells becoming brackish with increased draft, it is believed that further large developments will be more successful if shafts are sunk to sea level in the basalt as far inland as practicable, and tunnels are driven from the bottom of the shafts near the top of the saturated zone. Favorable places for such development exist in Honolulu.<br />In addition to the basal water in the volcanic rocks, water is found in the recent gravel, beach, and dune deposits, and the emerged reef limestone. This water has been recovered by wells and tunnels, and there are favorable localities for developing additional water of this type. <br />The island contains two types of basal springs&mdash;those like the Pearl Harbor Springs, which issue from basalt and are supplied by overflow and leakage from the artesian basin, and those which issue from the coastal-plain sediments and are mainly return irrigation water. The total quantity of basal ground water issuing as springs is estimated to be 100,000,000 gallons a day. <br />Ground water occurs at high levels, confined by dikes and perched on tuff, alluvium, and soil beds. These structures give rise to innumerable high-level springs. In the Koolau Range 60 tunnels yield about 33,000,000 gallons daily, of which about 95 percent is obtained from tunnels penetrating the dike complex of the Koolau volcanic series, about 2 percent from tunnels entering post-Koolau ash or tuff deposits, and the remainder from tunnels whose geologic relations are not certainly known. The average daily yield of the tunnels that recover dike water is 2,330 gallons a foot, but the average daily yield of the tunnels in post-Koolau tuff is 450 gallons a foot, and that of the tunnels in alluvium or soil is only 23 gallons a foot. <br />Owing largely to the much lower rainfall on the Waianac Range, its 35 tunnels (not including two new tunnels under construction) yield only about 2,400,000 gallons daily, about 94 percent of which is believed to be obtained from dike systems. The average daily yield of the tunnels in this range that are supplied by dike systems is 581 gallons a foot, as compared to 5 gallons a foot from tunnels in ash or tuff. <br />An extensive tunnel system is proposed to develop a large supply of high-level water for Honolulu from the dike complex of the Koolau series, and high-level water can be recovered by tunnels at many other places. <br />The average daily discharge of all high-level springs in the Koolau Range is about 58,000,000 gallons, of which about 94 percent comes from the Koolau dike complex and about 6 percent from post-Koolau volcanic rocks. The average daily discharge of all high-level springs in the Waianae Range is about 500,000 gallons of which about 81 percent issues from the dike complex.</p>","language":"English","publisher":"Maui Publishing Company, Limited","publisherLocation":"Wailuku, Maui","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Stearns, H.T., and Vaksvik, K.N., 1935, Geology and ground-water resources of the island of Oahu, Hawaii: Bulletin 1, xx, 479 p.","productDescription":"xx, 479 p.","numberOfPages":"536","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":221,"text":"Division of Hydrography","active":false,"usgs":true}],"links":[{"id":313171,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70160862.JPG"},{"id":313170,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/stearns/Oahu.pdf","size":"64.5 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":70205107,"text":"70205107 - 1935 - Early stages of glacial Lake Souris, North Dakota","interactions":[],"lastModifiedDate":"2019-09-03T12:30:32","indexId":"70205107","displayToPublicDate":"1935-09-03T12:21:35","publicationYear":"1935","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2572,"text":"Journal of the Washington Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Early stages of glacial Lake Souris, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Washington Academy of Sciences","issn":" 0043-0439","usgsCitation":"Andrews, D.A., 1935, Early stages of glacial Lake Souris, North Dakota: Journal of the Washington Academy of Sciences, v. 25, no. 12, p. 568-569.","productDescription":"2 p.","startPage":"568","endPage":"569","costCenters":[],"links":[{"id":367142,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Lake Souris","volume":"25","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Andrews, David Arthur","contributorId":218730,"corporation":false,"usgs":false,"family":"Andrews","given":"David","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":770053,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32522,"text":"32522 - 1935 - Wildlife of the Atlantic coast salt marshes","interactions":[],"lastModifiedDate":"2014-07-22T09:32:21","indexId":"32522","displayToPublicDate":"1935-09-01T09:31:53","publicationYear":"1935","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":"17","title":"Wildlife of the Atlantic coast salt marshes","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"McAtee, W., 1935, Wildlife of the Atlantic coast salt marshes: Wildlife Leaflet 17, 22 p.","productDescription":"22 p.","numberOfPages":"22","costCenters":[],"links":[{"id":290653,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb85e4b0824b2d178e8a","contributors":{"authors":[{"text":"McAtee, W.L.","contributorId":95176,"corporation":false,"usgs":true,"family":"McAtee","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":208638,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206680,"text":"70206680 - 1935 - Welded rhyolitic tuffs in southeastern Idaho","interactions":[],"lastModifiedDate":"2019-11-16T17:31:00","indexId":"70206680","displayToPublicDate":"1935-08-31T17:26:12","publicationYear":"1935","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Welded rhyolitic tuffs in southeastern Idaho","docAbstract":"<p><span>Rocks of rhyolitic type in eastern Idaho and adjacent parts of Wyoming were observed by the Teton Division of the Hayden Surveys under Orestes St. John (Report of the geological field work of the Teton Division, U.S. Geol. and Geog. Surv. Terr., 11th Ann. Rep., pp. 498–504, 1879), who described them as trachytes. He noted their relations to different types of underlying sedimentary rocks and their tendency to conform with the preexisting topography, but considered them all as flows. ©1935. American Geophysical Union. All Rights Reserved.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR016i001p00308","issn":"00028606","usgsCitation":"Mansfield, G.R., and Ross, C., 1935, Welded rhyolitic tuffs in southeastern Idaho: Eos, Transactions, American Geophysical Union, v. 16, no. 1, p. 308-321, https://doi.org/10.1029/TR016i001p00308.","productDescription":"14 p. 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 \"}}]}","volume":"16","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Mansfield, G. 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,{"id":70206795,"text":"70206795 - 1935 - Pre‐Cambrian and Paleozoic vulcanism of interior Alaska","interactions":[],"lastModifiedDate":"2019-11-21T15:24:58","indexId":"70206795","displayToPublicDate":"1935-08-31T15:21:28","publicationYear":"1935","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Pre‐Cambrian and Paleozoic vulcanism of interior Alaska","docAbstract":"<p><span>The history of vulcanism in Alaska is a topic of great universal interest, but one which has had no adequate treatment. For some years the writer has been accumulating comparative data on this subject, and it is hoped that this information may some time be sufficiently amplified and coordinated to justify a general description of the sequential igneous history of Alaska. The scope of such an undertaking, however, can well be appreciated from the statement that Alaska is nearly a fifth the size of the United States, and that geologic studies have shown that igneous rocks have originated in Alaska in every geologic period, excepting perhaps the Cambrian and the Silurian. Therefore, in the present paper, it has seemed best to present only a part of this interesting record, and perhaps in subsequent papers to expand the areal and geologic limits of discussion. ©1935. American Geophysical Union. All Rights Reserved.</span></p>","language":"English ","publisher":"American Geophysical Union ","doi":"10.1029/TR016i001p00292","issn":"00028606","usgsCitation":"Mertie, J., 1935, Pre‐Cambrian and Paleozoic vulcanism of interior Alaska: Eos, Transactions, American Geophysical Union, v. 16, no. 1, p. 292-302, https://doi.org/10.1029/TR016i001p00292.","productDescription":"11 p. ","startPage":"292","endPage":"302","costCenters":[],"links":[{"id":369417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Mertie, J.B. Jr.","contributorId":29383,"corporation":false,"usgs":false,"family":"Mertie","given":"J.B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":775764,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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