{"pageNumber":"2681","pageRowStart":"67000","pageSize":"25","recordCount":68807,"records":[{"id":601,"text":"wsp1057 - 1948 - Surface water supply of the United States, 1946, Part VII, Lower Mississippi River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1057","title":"Surface water supply of the United States, 1946, Part VII, Lower Mississippi River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1057","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part VII, Lower Mississippi River basin: U.S. Geological Survey Water Supply Paper 1057, ix, 417 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1057.","productDescription":"ix, 417 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1057/report-thumb.jpg"},{"id":25164,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696961","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":527573,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":593,"text":"wsp1061 - 1948 - Surface water supply of the United States, 1946, Part XI, Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1061","title":"Surface water supply of the United States, 1946, Part XI, Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1061","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part XI, Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 1061, x, 431 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1061.","productDescription":"x, 431 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1061/report-thumb.jpg"},{"id":25156,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968ac","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":527565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":602,"text":"wsp1058 - 1948 - Surface water supply of the United States, 1946, Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1058","title":"Surface water supply of the United States, 1946, Part VIII, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1058","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1058, ix, 344 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1058.","productDescription":"ix, 344 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1058/report-thumb.jpg"},{"id":25165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696981","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":527574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":595,"text":"wsp1064 - 1948 - Surface water supply of the United States, 1946, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1064","title":"Surface water supply of the United States, 1946, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1064","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1064, viii, 255 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1064.","productDescription":"viii, 255 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1064/report-thumb.jpg"},{"id":25158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696873","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":527567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":592,"text":"wsp1060 - 1948 - Surface water supply of the United States, 1946, Part X, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1060","title":"Surface water supply of the United States, 1946, Part X, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1060","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part X, The Great Basin: U.S. Geological Survey Water Supply Paper 1060, vii, 198 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1060.","productDescription":"vii, 198 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1060/report-thumb.jpg"},{"id":25155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968ab","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":527564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3479,"text":"cir33 - 1948 - Geology and water-bearing properties of the \"1,400 foot\" sand in the Memphis area","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir33","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"33","title":"Geology and water-bearing properties of the \"1,400 foot\" sand in the Memphis area","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir33","usgsCitation":"Schneider, R., and Cushing, E.M., 1948, Geology and water-bearing properties of the \"1,400 foot\" sand in the Memphis area: U.S. Geological Survey Circular 33, 13 p. :ill., maps (1 folded) ;27 cm., https://doi.org/10.3133/cir33.","productDescription":"13 p. :ill., maps (1 folded) ;27 cm.","costCenters":[],"links":[{"id":118007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1948/0033/report-thumb.jpg"},{"id":30490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1948/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68406b","contributors":{"authors":[{"text":"Schneider, Robert","contributorId":102460,"corporation":false,"usgs":true,"family":"Schneider","given":"Robert","email":"","affiliations":[],"preferred":false,"id":147002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, Elliot Morse","contributorId":14390,"corporation":false,"usgs":true,"family":"Cushing","given":"Elliot","email":"","middleInitial":"Morse","affiliations":[],"preferred":false,"id":147001,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3313,"text":"cir19 - 1948 - Progress report on the ground-water hydrology of the Republican and Frenchman River valleys, with a section on the chemical quality of the ground water","interactions":[],"lastModifiedDate":"2025-07-24T18:31:40.497734","indexId":"cir19","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"19","title":"Progress report on the ground-water hydrology of the Republican and Frenchman River valleys, with a section on the chemical quality of the ground water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir19","usgsCitation":"Waite, H.A., and Swenson, H.A., 1948, Progress report on the ground-water hydrology of the Republican and Frenchman River valleys, with a section on the chemical quality of the ground water: U.S. Geological Survey Circular 19, Report: iii, 83 p.; 1 Plate: 33.82 x 14.93 inches, https://doi.org/10.3133/cir19.","productDescription":"Report: iii, 83 p.; 1 Plate: 33.82 x 14.93 inches","costCenters":[],"links":[{"id":492844,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_118695.htm","linkFileType":{"id":5,"text":"html"}},{"id":117892,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1948/0019/report-thumb.jpg"},{"id":30317,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1948/0019/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30318,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1948/0019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Republican and Frenchman River valleys","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.05,\n              40.6\n            ],\n            [\n              -102.05,\n              40\n            ],\n            [\n              -98,\n              40\n              ],\n            [\n              -98,\n              40.6\n            ],\n            [\n              -102.05,\n              40.6\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd2b","contributors":{"authors":[{"text":"Waite, Herbert A.","contributorId":40973,"corporation":false,"usgs":true,"family":"Waite","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146645,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4065,"text":"cir37 - 1948 - Discharge and runoff in the Missouri River basin","interactions":[],"lastModifiedDate":"2018-02-16T13:56:14","indexId":"cir37","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"37","title":"Discharge and runoff in the Missouri River basin","docAbstract":"<p>Within the Missouri River Basin the precipitation and temperature vary greatly with both time and geographical location. Differences in weather and climate combine with differences in topography and geology to produce large differences in runoff from time to time and from place to place in the basin. The average annual runoff ranges from a fraction of an inch for some drainage areas to more than 40 inches for a few small ungaged areas at high elevations. For some drainage areas the maximum annual discharge is 10 to 20 times the minimum.</p><p>The amounts and distribution of runoff and discharge throughout a drainage basin are essential parts of any study of the water resources of that basin. Discharge records at gaging stations are only spot samples of surface-water resources and require interpretation in order to furnish a general knowledge of the amounts and distribution of runoff and discharge. Such a knowledge is necessary to an adequate understanding of the water resources of the drainage basin. This report contains maps that show for the Missouri River Basin. Representative average rates of discharge, the distribution of the average discharge by months for several gaging stations. representative annual runoff, and minimum annual runoff. These maps are supplemented by explanations and comments and by charts that show the development of irrigation by drainage areas and by States.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir37","usgsCitation":"Colby, B.R., and Oltman, R.E., 1948, Discharge and runoff in the Missouri River basin: U.S. Geological Survey Circular 37, Report: 11 p.; 3 Plates, https://doi.org/10.3133/cir37.","productDescription":"Report: 11 p.; 3 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":120760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0037/report-thumb.jpg"},{"id":31159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":272574,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0037/plate-1.pdf"},{"id":272575,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0037/plate-2.pdf"},{"id":272576,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0037/plate-3.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aaf3","contributors":{"authors":[{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oltman, Roy E.","contributorId":88720,"corporation":false,"usgs":true,"family":"Oltman","given":"Roy","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":148105,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1164,"text":"wsp1077 - 1948 - Gaging-station records in the Missouri River Basin","interactions":[],"lastModifiedDate":"2023-01-10T20:36:35.036961","indexId":"wsp1077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1077","title":"Gaging-station records in the Missouri River Basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1077","usgsCitation":"Colby, B.R., and Oltman, R.E., 1948, Gaging-station records in the Missouri River Basin: U.S. Geological Survey Water Supply Paper 1077, Report: iv, 219 p.; 1 Plate: 37.50 x 29.50 inches, https://doi.org/10.3133/wsp1077.","productDescription":"Report: iv, 219 p.; 1 Plate: 37.50 x 29.50 inches","costCenters":[],"links":[{"id":411664,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24207.htm","linkFileType":{"id":5,"text":"html"}},{"id":25998,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1077/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25999,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1077/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137128,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1077/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Missouri River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114,\n              49\n            ],\n            [\n              -114,\n              37\n            ],\n            [\n              -90,\n              37\n            ],\n            [\n              -90,\n              49\n            ],\n            [\n              -114,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b144d","contributors":{"authors":[{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oltman, Roy Edwin","contributorId":101635,"corporation":false,"usgs":true,"family":"Oltman","given":"Roy","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":143286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4136,"text":"cir32 - 1948 - Flood of September 1946 at San Antonio, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:04:24","indexId":"cir32","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"32","title":"Flood of September 1946 at San Antonio, Texas","docAbstract":"<p>A flood occurred in the streams in and near San Antonio, Teat., during the early morning hours of September 27, 1946, as a result of heavy rains falling during the previous night. Much property damage occurred in San Antonio and below, and four lives were lost. . It is the purpose of the present report to describe this flood and its relation to the flood of September 10, 1921 the greatest of record since 1819.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir32","usgsCitation":"Breeding, S., 1948, Flood of September 1946 at San Antonio, Texas: U.S. Geological Survey Circular 32, 19 p., https://doi.org/10.3133/cir32.","productDescription":"19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":31243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1948/0032/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1948/0032/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eebd0","contributors":{"authors":[{"text":"Breeding, Seth D.","contributorId":89505,"corporation":false,"usgs":true,"family":"Breeding","given":"Seth D.","affiliations":[],"preferred":false,"id":148269,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3892,"text":"cir39 - 1948 - Index of surface-water records, part 3, Ohio River basin, to September 30, 1948","interactions":[],"lastModifiedDate":"2016-12-27T16:41:11","indexId":"cir39","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"39","title":"Index of surface-water records, part 3, Ohio River basin, to September 30, 1948","docAbstract":"This report summarizes ground-water-quality data, for Wisconsin, stored in the U.S. Geological Survey 's computer system (WATSTORE). The summary includes water-quality data for 2,443 wells which tap one of the State 's three major aquifers (sand and gravel, Silurian dolomite, and sandstone). Data for dissolved solids, hardness, alkalinity, calcium, magnesium, sodium, potassium, iron, manganese, sulfate, chloride, fluoride, and nitrate are summarized by aquifer and by county, and locations of wells where data are available are shown for each aquifer. Calcium, magnestium, and bicarbonate (the principal component of alkalinity) are the major dissolved constituents present in Wisconsin 's ground water. High iron concentrations and hardness cause ground-water-quality problems in much of the State. Statewide summaries of trace constituent (selected trace metals, arsenic, boron, and organic carbon) concentrations show that they impair water quality in only a few isolated wells. A bibliography of published reports that describe or summarize various aspects of ground-water quality in Wisconsin is included. (USGS)","language":"English","publisher":"U.S. Dept. of the Interior, Geological Survey","doi":"10.3133/cir39","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Index of surface-water records, part 3, Ohio River basin, to September 30, 1948: U.S. Geological Survey Circular 39, 37 p., https://doi.org/10.3133/cir39.","productDescription":"37 p.","costCenters":[],"links":[{"id":124225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1948/0039/report-thumb.jpg"},{"id":30982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1948/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Ohio River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeb20","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":528140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215757,"text":"70215757 - 1948 - Some solutional features of the limestone near Lexington, Kentucky","interactions":[],"lastModifiedDate":"2020-10-28T19:58:10.057194","indexId":"70215757","displayToPublicDate":"1948-10-28T14:34:17","publicationYear":"1948","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":"Some solutional features of the limestone near Lexington, Kentucky","docAbstract":"<p><span>Field work on the Ordovician limestones and shales of the Lexington area, Kentucky, has shown that no appreciable quantity of ground water is transmitted through interstitial openings in these rocks. Ground-water movement is restricted to joint planes and, to a lesser extent, bedding planes that have been enlarged by solution. Studies of these planes indicate that solution has been effective only to a limited depth below the land surface. The bottom of the solutional zone is an exaggerated replica of the land surface, showing a greater depth of the solutional zone below stream valleys. The greater depth is attributed to the greater accumulation of ground water, the dissolving agent, in those areas. Modifications of the ideal condition are effected by the less soluble beds and the configuration of the land surface.</span></p><p><span>The underground drainage systems of the area develop in a manner similar to rectilinear stream patterns, showing a definite alignment along the two joint sets of the area. Directional solution has taken place where one of these joint sets has been developed to the exclusion of the other.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.43.1.39","usgsCitation":"Hamilton, D., 1948, Some solutional features of the limestone near Lexington, Kentucky: Economic Geology, v. 43, no. 1, p. 39-52, https://doi.org/10.2113/gsecongeo.43.1.39.","productDescription":"14 p.","startPage":"39","endPage":"52","costCenters":[],"links":[{"id":379896,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Lexington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.18798828125,\n              37.54893261064111\n            ],\n            [\n              -83.75976562499999,\n              37.54893261064111\n            ],\n            [\n              -83.75976562499999,\n              38.47939467327645\n            ],\n            [\n              -85.18798828125,\n              38.47939467327645\n            ],\n            [\n              -85.18798828125,\n              37.54893261064111\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationDate":"1948-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, D.K.","contributorId":244110,"corporation":false,"usgs":false,"family":"Hamilton","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":803313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215752,"text":"70215752 - 1948 - Quality of water in the upper Colorado River basin","interactions":[],"lastModifiedDate":"2021-04-06T15:23:39.269743","indexId":"70215752","displayToPublicDate":"1948-10-28T12:21:45","publicationYear":"1948","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":"Quality of water in the upper Colorado River basin","docAbstract":"<p>In a drainage area as large as the Colorado River Basin there are naturally large differences in the quality of the surface waters. The chemical character of the water at six gaging stations on the Colorado River from near the headwaters to near the mouth is shown by the analyses in Table 1.</p><p>It will be seen that the concentration of dissolved solids increased from 64 ppm (0.09 tons per ac ft) in the headwaters to 699 ppm (0.95 tons per ac ft) near the mouth.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00375","usgsCitation":"Howard, C.S., 1948, Quality of water in the upper Colorado River basin: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 375-378, https://doi.org/10.1029/TR029i003p00375.","productDescription":"4 p.","startPage":"375","endPage":"378","costCenters":[],"links":[{"id":379878,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Upper Colorado River 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":803306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215751,"text":"70215751 - 1948 - Fluctuations in concentration of dissolved solids of some southwestern streams","interactions":[],"lastModifiedDate":"2020-10-28T17:15:15.508813","indexId":"70215751","displayToPublicDate":"1948-10-28T12:11:05","publicationYear":"1948","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":"Fluctuations in concentration of dissolved solids of some southwestern streams","docAbstract":"<p><span>The concentration of dissolved solids in waters of streams of the Southwestern United Stated fluctuates widely as the stream discharge changes. These fluctuations may be extensive in a period of a few days or even a few hours. Data in this paper show the extent of the day‐to‐day changes in specific conductance and discharge of the Rio Grande at San Acacia, New Mexico, during the spring run‐off period of 1945. Data also are presented to show rapid fluctuations in concentration for the Pecos River near Artesia, New Mexico, the Gila River near Bylas, Arizona, and the Rio Grande at San Acacia during typical summer months. Hourly changes in chloride and discharge are shown for a day of approximately normal flow for the Pecos River near Malaga, New Mexico, and for a 36‐hour period of extremely low flow for the Gila River near Fort Thomas, Arizona.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i001p00080","usgsCitation":"Hem, J., 1948, Fluctuations in concentration of dissolved solids of some southwestern streams: Eos, Transactions, American Geophysical Union, v. 29, no. 1, p. 80-84, https://doi.org/10.1029/TR029i001p00080.","productDescription":"5 p.","startPage":"80","endPage":"84","costCenters":[],"links":[{"id":379877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico","otherGeospatial":"Southwestern Streams","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.41259765625,\n              32.7503226078097\n            ],\n            [\n              -108.30322265624999,\n              32.7503226078097\n            ],\n            [\n              -108.30322265624999,\n              34.488447837809304\n            ],\n            [\n              -110.41259765625,\n              34.488447837809304\n            ],\n            [\n              -110.41259765625,\n              32.7503226078097\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":803305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215693,"text":"70215693 - 1948 - Geology and ground-water resources of Iwo Jima ","interactions":[],"lastModifiedDate":"2020-10-27T20:28:58.557427","indexId":"70215693","displayToPublicDate":"1948-10-27T15:01:22","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Iwo Jima ","docAbstract":"<p>Iwo Jima, in the western Pacific Ocean, consists of Motoyama, a broad volcanic cone, at the north, and Mt. Suribachi at the south, with an undulating isthmus between. Motoyama is largely light-gray-buff tuff. A thick andesitic lava flow under Suribachi, exposed in several places, is overlain by a thick deposit of cinder and scoria. The isthmus (called Tidorigahara by the Japanese) is underlain by more than 200 feet of loose black volcanic ash and fine cinder derived from Suribachi. Several small coral reefs are located about 340 and 110 feet above present sea level.</p><p>Iwo Jima first came into existence, probably early in Pleistocene time, with the building above sea level of the tuff cone of Motoyama. Quite late in the active life of Motoyama, volcanic activity on the southwestern flank resulted in the formation of Suribachi. This activity may have started with the welling up of the andesitic lava which underlies Suribachi. Following the major eruption of Suribachi, relative sea level changed, and the sea stood about 360 feet higher than at present. The broad cone of Motoyama was beveled; the relative sea level then dropped 240 feet, with minor halts to about 120 feet above present level. As the island rose, Suribachi burst forth in its last stage of explosive activity. Wave erosion cut deeply into the andesite flow of Suribachi, and a prominent bench level was formed 120 feet above present sea level.</p><p>The Japanese on the island were often faced with serious water shortages. Americans drilled wells and obtained moderately large supplies of usable water. The temperature of the water ranges from 105° to 179° F., and the water is somewhat mineralized. The most favorable area for ground-water development is the isthmus.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[995:GAGROI]2.0.CO;2","usgsCitation":"Swenson, F.A., 1948, Geology and ground-water resources of Iwo Jima : GSA Bulletin, v. 59, no. 10, p. 995-1008, https://doi.org/10.1130/0016-7606(1948)59[995:GAGROI]2.0.CO;2.","productDescription":"14 p.","startPage":"995","endPage":"1008","costCenters":[],"links":[{"id":379832,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Iwo Jima","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              141.251220703125,\n              24.693814995267424\n            ],\n            [\n              141.4057159423828,\n              24.693814995267424\n            ],\n            [\n              141.4057159423828,\n              24.85092688067188\n            ],\n            [\n              141.251220703125,\n              24.85092688067188\n            ],\n            [\n              141.251220703125,\n              24.693814995267424\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Swenson, F. A.","contributorId":71622,"corporation":false,"usgs":true,"family":"Swenson","given":"F.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":803152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215685,"text":"70215685 - 1948 - Report of Committee on Ground Water, 1945–1946","interactions":[],"lastModifiedDate":"2021-03-17T14:36:25.886627","indexId":"70215685","displayToPublicDate":"1948-10-27T13:19:47","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of Committee on Ground Water, 1945–1946","docAbstract":"<p><span>The principal activity of the Committee during the year was the arranging and presentation of a symposium on methods of estimating ground‐water supplies. The response was gratifying and resulted in the presentation of 11 interesting papers at the 1946 meeting. The report of the Subcommittee on Permeability by C. E. Jacob, Chairman, is given as Appendix A. At a meeting of the Executive Committee of the Section of Hydrology in June 1946, this Subcommittee of the Committee on Ground Water was changed to the Committee on Permeability of the Section of Hydrology, with Jacob continuing as Chairman. This will give the new Committee much greater latitude in dealing with a subject which is of concern to several of the Research Committees.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i001p00117","usgsCitation":"Lohman, S.W., 1948, Report of Committee on Ground Water, 1945–1946: Eos, Transactions, American Geophysical Union, v. 29, no. 1, p. 117-123, https://doi.org/10.1029/TR029i001p00117.","productDescription":"7 p.","startPage":"117","endPage":"123","costCenters":[],"links":[{"id":379876,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":803144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215684,"text":"70215684 - 1948 - Development of limestone reservoirs in Comal County, Texas","interactions":[],"lastModifiedDate":"2020-10-28T12:00:02.648533","indexId":"70215684","displayToPublicDate":"1948-10-27T13:13:15","publicationYear":"1948","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":"Development of limestone reservoirs in Comal County, Texas","docAbstract":"<p><span>The Edwards limestone, and to a lesser extent the Comanche Peak limestone and the lower part of the Glen Rose limestone below, all of Lower Cretaceous age, form one of the most extensive ground‐water reservoirs in Texas. As a result of normal faulting, these formations are connected by underground channels to form a hydrologic unit which is partly artesian and partly unconfined. Observations in Comal County show that the development of the reservoir by solution is closely related to the geologic history, in which complex faulting and the disconformity between the Edwards and Georgetown limestones are important factors. Various phases of development are shown in different fault blocks, depending upon length of exposure at the surface. The Edwards limestone, which contains the main channels of underground drainage, is almost uniformly permeable from top to bottom, whereas the older, but more recently exposed lower part of the Glen Rose limestone is generally relatively impermeable except where exposed by mature streams.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i004p00503","usgsCitation":"George, W., 1948, Development of limestone reservoirs in Comal County, Texas: Eos, Transactions, American Geophysical Union, v. 29, no. 4, p. 503-510, https://doi.org/10.1029/TR029i004p00503.","productDescription":"8 p.","startPage":"503","endPage":"510","costCenters":[],"links":[{"id":379823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Comal County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.2986,30.0395],[-98.1102,29.9036],[-98.0389,29.8493],[-97.9996,29.7537],[-98.0895,29.6857],[-98.2045,29.6363],[-98.3124,29.5973],[-98.3149,29.6014],[-98.3191,29.6033],[-98.3279,29.6053],[-98.3295,29.6058],[-98.3305,29.6086],[-98.3341,29.6109],[-98.3383,29.6128],[-98.3419,29.6147],[-98.3445,29.6175],[-98.3439,29.623],[-98.3432,29.6303],[-98.3452,29.6345],[-98.3478,29.6381],[-98.3498,29.6423],[-98.3492,29.645],[-98.3475,29.6496],[-98.3464,29.6523],[-98.3479,29.6551],[-98.3516,29.657],[-98.3589,29.6589],[-98.361,29.6603],[-98.3625,29.6631],[-98.364,29.6645],[-98.3677,29.6659],[-98.3724,29.6656],[-98.3772,29.6638],[-98.3793,29.6643],[-98.3803,29.6657],[-98.3833,29.6721],[-98.3842,29.6786],[-98.3826,29.6822],[-98.3794,29.6849],[-98.3783,29.689],[-98.3787,29.6913],[-98.3813,29.6945],[-98.3828,29.6973],[-98.3828,29.7001],[-98.3806,29.7028],[-98.3779,29.7046],[-98.3722,29.705],[-98.3601,29.7048],[-98.3543,29.7047],[-98.3511,29.7051],[-98.3458,29.7101],[-98.3425,29.715],[-98.3419,29.7192],[-98.3424,29.7228],[-98.3449,29.7265],[-98.3527,29.7308],[-98.3559,29.7317],[-98.3606,29.7318],[-98.3638,29.7282],[-98.3676,29.7237],[-98.3734,29.7215],[-98.376,29.7215],[-98.377,29.7261],[-98.3779,29.7316],[-98.3795,29.7348],[-98.3889,29.7345],[-98.3941,29.736],[-98.3978,29.737],[-98.3988,29.7397],[-98.4014,29.7439],[-98.4045,29.7467],[-98.4081,29.7476],[-98.4134,29.7468],[-98.4182,29.7446],[-98.4203,29.7419],[-98.4219,29.7391],[-98.4226,29.7341],[-98.4216,29.73],[-98.4216,29.729],[-98.4253,29.7277],[-98.4279,29.7278],[-98.4296,29.726],[-98.4301,29.7241],[-98.4291,29.7218],[-98.4291,29.7195],[-98.4318,29.7182],[-98.4371,29.7178],[-98.4402,29.7188],[-98.4428,29.7188],[-98.4449,29.7202],[-98.4459,29.723],[-98.4458,29.7276],[-98.4452,29.7326],[-98.4462,29.734],[-98.4499,29.7345],[-98.4546,29.7327],[-98.4588,29.7337],[-98.463,29.7361],[-98.4661,29.7379],[-98.4719,29.7376],[-98.4772,29.7353],[-98.4851,29.735],[-98.5008,29.738],[-98.5086,29.7413],[-98.5122,29.7436],[-98.5143,29.7446],[-98.5196,29.7455],[-98.5238,29.7456],[-98.5254,29.7447],[-98.529,29.7452],[-98.5332,29.7485],[-98.5357,29.7526],[-98.5399,29.7541],[-98.5441,29.7527],[-98.5473,29.7528],[-98.5499,29.7547],[-98.5493,29.756],[-98.5488,29.7565],[-98.5488,29.7592],[-98.5498,29.7602],[-98.5524,29.7606],[-98.5535,29.7602],[-98.5545,29.7588],[-98.5562,29.7566],[-98.5572,29.7557],[-98.5604,29.7534],[-98.5662,29.7526],[-98.5741,29.7504],[-98.5783,29.7495],[-98.5805,29.7473],[-98.5816,29.7445],[-98.5837,29.7432],[-98.5874,29.7446],[-98.59,29.7469],[-98.5936,29.7488],[-98.5983,29.7489],[-98.6015,29.7494],[-98.6051,29.7499],[-98.6052,29.748],[-98.6047,29.7457],[-98.6026,29.7448],[-98.6016,29.7425],[-98.6048,29.7407],[-98.61,29.7399],[-98.6137,29.7395],[-98.6174,29.7409],[-98.6216,29.7423],[-98.6231,29.7428],[-98.6257,29.7437],[-98.6321,29.7429],[-98.6384,29.7416],[-98.6431,29.7403],[-98.6458,29.7403],[-98.6468,29.7426],[-98.6478,29.7477],[-98.4138,29.9442],[-98.2986,30.0395]]]},\"properties\":{\"name\":\"Comal\",\"state\":\"TX\"}}]}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"George, W.O.","contributorId":41886,"corporation":false,"usgs":true,"family":"George","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":803143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215683,"text":"70215683 - 1948 - Hydrology of limestone terrane in Schoharie County, New York","interactions":[],"lastModifiedDate":"2021-04-07T13:48:14.233831","indexId":"70215683","displayToPublicDate":"1948-10-27T13:02:34","publicationYear":"1948","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":"Hydrology of limestone terrane in Schoharie County, New York","docAbstract":"<p><span>During the summer of 1946 the writer studied the ground‐water resources of Schoharie County, New York, as a part of the program of ground‐water investigation being carried on in cooperation between the United States Geological Survey and the New York State Water Power and Control Commission. Because the outcrop belt of Devonian and Upper Silurian carbonate rocks is wider in Schoharie County than in other parts of the State, the effects of solution on these formations is better displayed here than elsewhere. The conditions described below probably apply on a smaller scale to the areas to the west, where the upper formations are cut out by an unconformity, and to the east in the Helderberg area, where similar effects have been described by Goldring [see “References” at end of paper, 1935]. However, it is probable that solution in the limestones in the Hudson Valley is not comparable because of the folded condition of the rocks.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00251","usgsCitation":"Berdan, J.M., 1948, Hydrology of limestone terrane in Schoharie County, New York: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 251-253, https://doi.org/10.1029/TR029i002p00251.","productDescription":"3 p.","startPage":"251","endPage":"253","costCenters":[],"links":[{"id":379822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","county":"Schoharie County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-74.264,42.7981],[-74.2622,42.7963],[-74.2579,42.7949],[-74.2548,42.793],[-74.2529,42.7898],[-74.2511,42.7857],[-74.2506,42.7825],[-74.2525,42.7798],[-74.2545,42.7707],[-74.2572,42.7621],[-74.261,42.7585],[-74.266,42.7572],[-74.2729,42.7573],[-74.2848,42.7569],[-74.2941,42.7566],[-74.2998,42.7552],[-74.3035,42.7535],[-74.3042,42.7521],[-74.3067,42.7485],[-74.2779,42.7196],[-74.2711,42.7195],[-74.2687,42.714],[-74.2424,42.7174],[-74.2393,42.7178],[-74.2026,42.7107],[-74.1838,42.7123],[-74.1773,42.73],[-74.1619,42.7166],[-74.168,42.6912],[-74.1684,42.674],[-74.1697,42.6672],[-74.1718,42.6595],[-74.1757,42.6499],[-74.1833,42.64],[-74.1878,42.6342],[-74.1903,42.6324],[-74.1949,42.6201],[-74.1963,42.6165],[-74.2197,42.5927],[-74.2198,42.5899],[-74.2218,42.5845],[-74.2237,42.5813],[-74.23,42.5764],[-74.2338,42.5737],[-74.2357,42.5705],[-74.2392,42.5488],[-74.2321,42.5323],[-74.2298,42.521],[-74.2263,42.5046],[-74.227,42.5014],[-74.2354,42.4837],[-74.2425,42.4688],[-74.2457,42.4648],[-74.2509,42.4516],[-74.2652,42.4177],[-74.2636,42.4063],[-74.253,42.4071],[-74.246,42.3839],[-74.246,42.3816],[-74.2472,42.3807],[-74.2497,42.3807],[-74.2547,42.3812],[-74.2591,42.3795],[-74.2666,42.3732],[-74.2748,42.3673],[-74.2804,42.3647],[-74.2861,42.3629],[-74.2954,42.363],[-74.2997,42.363],[-74.306,42.3599],[-74.3078,42.359],[-74.3141,42.3595],[-74.3227,42.3605],[-74.3314,42.3601],[-74.3389,42.3602],[-74.3426,42.3584],[-74.3469,42.3594],[-74.3513,42.3617],[-74.358,42.3676],[-74.3617,42.3699],[-74.3685,42.3704],[-74.3778,42.3701],[-74.389,42.3697],[-74.3977,42.3675],[-74.4432,42.3547],[-74.6168,42.4219],[-74.7145,42.5175],[-74.671,42.5654],[-74.652,42.5926],[-74.6317,42.6242],[-74.6382,42.6511],[-74.6501,42.6935],[-74.6621,42.7322],[-74.6681,42.7513],[-74.668,42.764],[-74.6645,42.7917],[-74.6504,42.828],[-74.5619,42.8092],[-74.4562,42.7716],[-74.3311,42.7828],[-74.2893,42.7838],[-74.264,42.7981]]]},\"properties\":{\"name\":\"Schoharie\",\"state\":\"NY\"}}]}","volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Berdan, Jean Milton","contributorId":86758,"corporation":false,"usgs":true,"family":"Berdan","given":"Jean","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":803142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215681,"text":"70215681 - 1948 - Runoff from rain and snow","interactions":[],"lastModifiedDate":"2021-04-02T14:46:48.221141","indexId":"70215681","displayToPublicDate":"1948-10-27T12:31:09","publicationYear":"1948","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":"Runoff from rain and snow","docAbstract":"<p><span>The basic principles of the idealized hydrologic cycle are reviewed with emphasis on storage and movement of water in the soil. A distinction is made between ground‐water runoff and overland runoff in terms of storage and lag, expressed as accumulated deviations from uniform flow over a period of several years. These functions are presented for the period 1920 through 1945 for three rivers in central Oregon: John Day, Deschutes, and Metolius, which exemplify minimum, moderate, and maximum effects, respectively, of storage and lag. The Metolius River is shown to have extremely small fluctuations in discharge from year to year, ascribed to a great portion of its flow being derived from ground‐water runoff; and its response to fluctuations in annual precipitation lags behind that of the John Day River by about five years. Specific techniques and measures for improving seasonal water supply forecasts are suggested.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i004p00511","usgsCitation":"Piper, A.M., 1948, Runoff from rain and snow: Eos, Transactions, American Geophysical Union, v. 29, no. 4, p. 511-524, https://doi.org/10.1029/TR029i004p00511.","productDescription":"14 p.","startPage":"511","endPage":"524","costCenters":[],"links":[{"id":379816,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Piper, A. M.","contributorId":102865,"corporation":false,"usgs":true,"family":"Piper","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":803140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215680,"text":"70215680 - 1948 - Trends in runoff in the Pacific Northwest","interactions":[],"lastModifiedDate":"2021-03-19T22:32:03.584067","indexId":"70215680","displayToPublicDate":"1948-10-27T12:12:00","publicationYear":"1948","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":"Trends in runoff in the Pacific Northwest","docAbstract":"<p><span>The diminution in runoff in the Pacific Northwest, particularly the Columbia River Basin, during the past 50 years, and its hydrologic significance are discussed in this paper. An analysis of the rainfall‐runoff relations for the Basin is made in order to explain the different influence of short‐ and long‐term precipitation factors on the diminution of runoff. The indicated effects of long‐term precipitation may reflect the influence of ground‐water storage.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00387","usgsCitation":"McDonald, C.C., and Langbein, W.B., 1948, Trends in runoff in the Pacific Northwest: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 387-397, https://doi.org/10.1029/TR029i003p00387.","productDescription":"11 p.","startPage":"387","endPage":"397","costCenters":[],"links":[{"id":379814,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Pacific 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":803138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":803139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215679,"text":"70215679 - 1948 - Quality of water in the northwest","interactions":[],"lastModifiedDate":"2021-03-16T20:54:25.168523","indexId":"70215679","displayToPublicDate":"1948-10-27T11:52:33","publicationYear":"1948","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":"Quality of water in the northwest","docAbstract":"<h3 class=\"article-section__header main main\">Abstract</h3><div class=\"article-section__content en main\"><p>The quality of natural waters, as judged by the dissolved mineral content, is quite varied throughout the Northwest. The concentrations of dissolved solids range from less than 50 ppm for many of the surface waters in Washington and Oregon, to several thousand ppm in the alkaline lakes of these states. On the whole, the quality of the natural waters is good but in some areas the waters have become unsatisfactory for many purposes, including irrigation, through contamination with wastes from industrial processes, which may include drainage from irrigated lands.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00379","usgsCitation":"Howard, C.S., 1948, Quality of water in the northwest: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 379-383, https://doi.org/10.1029/TR029i003p00379.","productDescription":"5 p.","startPage":"379","endPage":"383","costCenters":[],"links":[{"id":379801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"The 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":803128,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215677,"text":"70215677 - 1948 - Effect of water temperature on flow of a natural stream","interactions":[],"lastModifiedDate":"2020-10-27T16:42:53.600045","indexId":"70215677","displayToPublicDate":"1948-10-27T11:34:00","publicationYear":"1948","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":"Effect of water temperature on flow of a natural stream","docAbstract":"<p><span>Approximately three per cent of the variation in streamflow of the Kootenai River near Copeland, Idaho, has been found to be associated with variation in water temperature. This has been determined by correlation analysis of residuals in streamflow that were not accounted for by either gage height or slope.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00240","usgsCitation":"Eisenlohr, W.S., 1948, Effect of water temperature on flow of a natural stream: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 240-242, https://doi.org/10.1029/TR029i002p00240.","productDescription":"3 p.","startPage":"240","endPage":"242","costCenters":[],"links":[{"id":379798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Eisenlohr, William Stewart Jr.","contributorId":115220,"corporation":false,"usgs":false,"family":"Eisenlohr","given":"William","suffix":"Jr.","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":803113,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215629,"text":"70215629 - 1948 - Ground-water investigations in the United States","interactions":[],"lastModifiedDate":"2020-10-26T18:59:38.907332","indexId":"70215629","displayToPublicDate":"1948-10-26T13:54:10","publicationYear":"1948","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":"Ground-water investigations in the United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.43.7.547","usgsCitation":"Sayre, A., 1948, Ground-water investigations in the United States: Economic Geology, v. 43, no. 7, p. 547-552, https://doi.org/10.2113/gsecongeo.43.7.547.","productDescription":"6  p.","startPage":"547","endPage":"552","costCenters":[],"links":[{"id":379773,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"7","noUsgsAuthors":false,"publicationDate":"1948-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":803035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215628,"text":"70215628 - 1948 - A sensitive field test for heavy metals in water","interactions":[],"lastModifiedDate":"2020-10-26T18:53:18.257784","indexId":"70215628","displayToPublicDate":"1948-10-26T13:45:34","publicationYear":"1948","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":"A sensitive field test for heavy metals in water","docAbstract":"<p><span>A semiquantitative colorimetric analytical method using dithizone to detect traces of heavy metals in natural water is described. Although reagents of exceptional purity are required, only simple equipment is needed and the test can be made in a few minutes in the field. A combined mixed color and mono color technique makes the test suitable for a wide range of concentrations. The test is very sensitive; as little as 0.01 part per million of either copper, lead, zinc or any combination of the three metals can be detected readily.The dithizone test permits rapid field identification of drainage elements which contain significant concentrations of heavy metals. An example is given showing how the test can be used to trace the heavy metal content of a drainage system back to its source. It is possible that, under favorable conditions, the field test may facilitate prospecting by detecting metals discharged by the weathering of hidden ore bodies. However, until the method receives further investigation, it would be premature to predict its value.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.43.8.675","usgsCitation":"Huff, L.C., 1948, A sensitive field test for heavy metals in water: Economic Geology, v. 43, no. 8, p. 675-684, https://doi.org/10.2113/gsecongeo.43.8.675.","productDescription":"10 p.","startPage":"675","endPage":"684","costCenters":[],"links":[{"id":379772,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","county":"Gilpin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-105.6743,39.93],[-105.6089,39.9302],[-105.4968,39.9298],[-105.4728,39.9302],[-105.4638,39.9292],[-105.4584,39.9297],[-105.4398,39.9364],[-105.4362,39.9364],[-105.4296,39.9327],[-105.426,39.9318],[-105.4212,39.9309],[-105.3966,39.9326],[-105.3968,39.9117],[-105.3958,39.8827],[-105.3939,39.8251],[-105.3945,39.7499],[-105.4035,39.7499],[-105.4101,39.7486],[-105.4143,39.7459],[-105.4185,39.745],[-105.4203,39.7454],[-105.4215,39.7482],[-105.4239,39.7518],[-105.4262,39.7527],[-105.4274,39.7532],[-105.4424,39.7528],[-105.4454,39.7528],[-105.4609,39.7551],[-105.4759,39.7566],[-105.4854,39.7566],[-105.4932,39.7584],[-105.4992,39.7603],[-105.5081,39.7631],[-105.5207,39.7654],[-105.532,39.7681],[-105.5392,39.7718],[-105.5434,39.7759],[-105.5445,39.78],[-105.5451,39.7818],[-105.5457,39.785],[-105.554,39.7909],[-105.5743,39.8018],[-105.5755,39.8036],[-105.5755,39.8109],[-105.576,39.8186],[-105.5778,39.8209],[-105.579,39.8213],[-105.5814,39.8213],[-105.5892,39.8177],[-105.5922,39.8159],[-105.597,39.8164],[-105.6,39.8182],[-105.603,39.8196],[-105.6119,39.8223],[-105.6191,39.8255],[-105.6239,39.8301],[-105.6274,39.8346],[-105.6298,39.8396],[-105.6334,39.8419],[-105.6471,39.846],[-105.6531,39.8474],[-105.6597,39.8474],[-105.6651,39.8465],[-105.6723,39.8461],[-105.6795,39.8466],[-105.6849,39.8484],[-105.6884,39.8507],[-105.6908,39.8548],[-105.6926,39.8634],[-105.6955,39.8734],[-105.6961,39.8783],[-105.6955,39.8861],[-105.6955,39.8892],[-105.6925,39.8933],[-105.6895,39.8978],[-105.6864,39.9064],[-105.684,39.91],[-105.6804,39.9141],[-105.6798,39.9182],[-105.6779,39.9241],[-105.6743,39.93]]]},\"properties\":{\"name\":\"Gilpin\",\"state\":\"CO\"}}]}","volume":"43","issue":"8","noUsgsAuthors":false,"publicationDate":"1948-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huff, Lyman C.","contributorId":47440,"corporation":false,"usgs":true,"family":"Huff","given":"Lyman","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":803034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215627,"text":"70215627 - 1948 - Geology and ground water of the Casablanca Basin, Chile","interactions":[],"lastModifiedDate":"2021-03-25T16:14:57.539396","indexId":"70215627","displayToPublicDate":"1948-10-26T13:32:37","publicationYear":"1948","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":"Geology and ground water of the Casablanca Basin, Chile","docAbstract":"<p><span>\"In the uplands the Cretaceous granodiorite and granite contain water in the weathered zones, and in joints and fractures. These yield small supplies of good water to springs and to shallow domestic and stock wells. The alluvial fill of the lowlands contains a zone of saturation that is sustained by infiltration from rainfall and from the runoff of the uplands.... Where present in the zone of saturation, the coarse-grained members of the alluvial fill yield moderate to large supplies of good water to wells.\"</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.43.8.661","usgsCitation":"Taylor, G.C., 1948, Geology and ground water of the Casablanca Basin, Chile: Economic Geology, v. 73, no. 8, p. 661-674, https://doi.org/10.2113/gsecongeo.43.8.661.","productDescription":"14 p.","startPage":"661","endPage":"674","costCenters":[],"links":[{"id":379771,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Chile","otherGeospatial":"Casablanca Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.7791748046875,\n              -34.25267611710151\n            ],\n            [\n              -69.71923828125,\n              -34.25267611710151\n            ],\n            [\n              -69.71923828125,\n              -32.65787573695528\n            ],\n            [\n              -71.7791748046875,\n              -32.65787573695528\n            ],\n            [\n              -71.7791748046875,\n              -34.25267611710151\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"73","issue":"8","noUsgsAuthors":false,"publicationDate":"1948-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Taylor, G. C. Jr.","contributorId":21628,"corporation":false,"usgs":true,"family":"Taylor","given":"G.","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":803033,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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