{"pageNumber":"1642","pageRowStart":"41025","pageSize":"25","recordCount":46644,"records":[{"id":9970,"text":"ofr81752 - 1981 - Basic data report and geochemical summary for stream sediments, heavy-mineral concentrates, rocks, and waters from the Golden Trout Wilderness, California","interactions":[],"lastModifiedDate":"2022-01-27T21:45:08.506286","indexId":"ofr81752","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-752","title":"Basic data report and geochemical summary for stream sediments, heavy-mineral concentrates, rocks, and waters from the Golden Trout Wilderness, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81752","usgsCitation":"Leach, D.L., Goldfarb, R., and Domenico, J.A., 1981, Basic data report and geochemical summary for stream sediments, heavy-mineral concentrates, rocks, and waters from the Golden Trout Wilderness, California: U.S. Geological Survey Open-File Report 81-752, Report: iii, 119 p.; 1 Plate: 45.28 × 40.97 inches, https://doi.org/10.3133/ofr81752.","productDescription":"Report: iii, 119 p.; 1 Plate: 45.28 × 40.97 inches","costCenters":[],"links":[{"id":395020,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12147.htm"},{"id":37771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0752/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37770,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0752/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0752/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Golden Trout Wilderness","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.6830,\n              36.117\n            ],\n            [\n              -118.017,\n              36.117\n            ],\n            [\n              -118.017,\n              36.5\n            ],\n            [\n              -118.6830,\n              36.5\n            ],\n            [\n              -118.6830,\n              36.117\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640bea","contributors":{"authors":[{"text":"Leach, D. L.","contributorId":18758,"corporation":false,"usgs":true,"family":"Leach","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldfarb, R.J.","contributorId":38143,"corporation":false,"usgs":true,"family":"Goldfarb","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":160592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Domenico, J. A.","contributorId":12028,"corporation":false,"usgs":true,"family":"Domenico","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":160590,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4055,"text":"cir801 - 1981 - Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978","interactions":[],"lastModifiedDate":"2020-09-27T17:48:12.680465","indexId":"cir801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"801","title":"Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978","docAbstract":"In 1960, the U.S. Geological Survey and the Kentucky Geological Survey began a program to map the State geologically at a scale of 1:24,000 and to publish the maps as 707 U.S. Geological Survey Geologic Quadrangle Maps. Fieldwork was completed by the spring of 1977, and all maps were published by December 1978. \r\n\r\nGeologic mapping of the State was proposed by the Kentucky Society of Professional Engineers in 1959. Wallace W. Hagan, Director and State Geologist of the Kentucky Geological Survey, and Preston McGrain, Assistant State Geologist, promoted support for the proposal among organizations such as Chambers of Commerce, industrial associations, professional societies, and among members of the State government. It was also arranged for the U.S. Geological Survey to supply mapping personnel and to publish the maps; the cost would be shared equally by the two organizations. \r\n\r\nMembers of the U.S. Geological Survey assigned to the program were organized as the Branch of Kentucky Geology. Branch headquarters, including an editorial staff, was at Lexington, Ky., but actual mapping was conducted from 18 field offices distributed throughout the State. The Publications Division of the U.S. Geological Survey established a cartographic office at Lexington to prepare the maps for publication. \r\n\r\nAbout 260 people, including more than 200 professionals, were assigned to the Branch of Kentucky Geology by the U.S. Geological Survey at one time or another. The most geologists assigned any one year was 61. To complete the mapping and ancillary studies, 661 professional man-years were required, compared with an original estimate of 600 man-years. \r\n\r\nA wide variety of field methods were used, but most geologists relied on the surveying altimeter to obtain elevations. Surface data were supplemented by drill-hole records, and several dozen shallow diamond-drill holes were drilled to aid the mapping. Geologists generally scribed their own maps, with a consequent saving of publication costs. \r\n\r\nPaleontologists and stratigraphers of the U.S. Geological Survey cooperated closely with the program. Paleontologic studies were concentrated in the Ordovician of central Kentucky, the Pennsylvanian of eastern and western Kentucky, and the Mesozoic and Cenozoic of westernmost Kentucky. \r\n\r\nIn addition to financial support, the Kentucky Geological Survey provided economic data, stratigraphic support, and drillhole records to the field offices. Geologists of the State Survey made subsurface structural interpretations, constructed bedrock topography maps, and mapped several quadrangles. \r\n\r\nSome of the problems encountered were the inadequacy of much of the existing stratigraphic nomenclature, the uneven quality of some of the mapping, and the effects of relative isolation on the professional development of some of the geologists. \r\n\r\nThe program cost a total of $20,927,500. In terms of 1960 dollars, it cost $16,035,000; this compares with an original estimate of $12,000,000. Although it is difficult to place a monetary value on the geologic mapping, the program has contributed to newly discovered mineral wealth, jobs, and money saved by government and industry. The maps are used widely in the exploration for coal, oil and gas, fluorspar, limestone, and clay. The maps are also used in planning highways and locations of dams, in evaluating foundation and excavation conditions, in preparing environmental impact statements, and in land-use planning.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir801","usgsCitation":"Cressman, E.R., and Noger, M.C., 1981, Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978: U.S. Geological Survey Circular 801, iii, 22 p., https://doi.org/10.3133/cir801.","productDescription":"iii, 22 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science 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,{"id":9915,"text":"ofr81420 - 1981 - Base flow of streams in Nassau County sewer districts 2 and 3, Long Island, New York, 1978-79","interactions":[],"lastModifiedDate":"2022-05-06T13:29:35.890969","indexId":"ofr81420","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-420","title":"Base flow of streams in Nassau County sewer districts 2 and 3, Long Island, New York, 1978-79","docAbstract":"<p>South-shore streams on Long Island, N.Y., are small, widely spaced and have few or no tributaries. Their gradients are gentle, averaging 10 feet per mile. All streams in the area studied have a mean annual discharge of less than 20 cubic feet per second, and most are from 3 to 10 miles long. Under natural conditions, about 95 percent of total streamflow originates as ground-water seepage from the upper glacial aquifer; the remaining 5 percent consists of direct runoff. Thus, the streams of Long Island function as ground-water drains, the flow of which in dry weather is controlled directly by ground-water levels adjacent to the stream channels. Monthly low-flow discharge measurements of 18 south-shore streams in Nassau County from 1978-79 are tabulated in this report. Measurement sites were established at 1,000-foot intervals between the southern tide-affected reach and the northern headwaters of each stream. The measurements provide a data base for the 'Flow Augmentation Needs Study,' supported by the U.S. Environmental Protection Agency, which will evaluate the need to replace streamflow lost through lowering of the water table as a result of sewage in Nassau County Sewer Districts 2 and 3.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81420","collaboration":"Prepared in cooperation with the Nassau County Department of Public Works","usgsCitation":"Ku, H.F., and Simmons, D.L., 1981, Base flow of streams in Nassau County sewer districts 2 and 3, Long Island, New York, 1978-79: U.S. Geological Survey Open-File Report 81-420, Report: iv, 32 p.; 1 Plate: 22.87 x 17.29 inches, https://doi.org/10.3133/ofr81420.","productDescription":"Report: iv, 32 p.; 1 Plate: 22.87 x 17.29 inches","costCenters":[],"links":[{"id":400270,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12031.htm"},{"id":400171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0420/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0420/report-thumb.jpg"},{"id":400172,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0420/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.63449096679688,\n              40.5983133693247\n            ],\n            [\n              -73.50540161132812,\n              40.5983133693247\n            ],\n            [\n              -73.50540161132812,\n              40.665014570215\n            ],\n            [\n              -73.63449096679688,\n              40.665014570215\n            ],\n            [\n              -73.63449096679688,\n              40.5983133693247\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64925e","contributors":{"authors":[{"text":"Ku, Henry F.","contributorId":52182,"corporation":false,"usgs":true,"family":"Ku","given":"Henry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, Dale L. dsimmons@usgs.gov","contributorId":575,"corporation":false,"usgs":true,"family":"Simmons","given":"Dale","email":"dsimmons@usgs.gov","middleInitial":"L.","affiliations":[{"id":5072,"text":"Office of Communication and Publishing","active":true,"usgs":true}],"preferred":true,"id":160504,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9902,"text":"ofr81500 - 1981 - Hydrogeologic data from selected wells and test holes in Suffolk County, Long Island, New York, 1972-80","interactions":[],"lastModifiedDate":"2022-08-12T19:19:39.286069","indexId":"ofr81500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-500","title":"Hydrogeologic data from selected wells and test holes in Suffolk County, Long Island, New York, 1972-80","docAbstract":"<p>The population of Suffolk County, New York, an area of 922 square miles, has increased rapidly, from less than 200,000 in 1940 to about 1.3 million in 1978. Ground-water pumpage has increased from an average of 42 million gallons per day in 1950 to about 257 million gallons per day in 1978. To help supply the hydrologic information needed to anticipate and prevent shortages, this report presents hydrogeologic and well-completion data on over 700 wells and test holes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81500","collaboration":"Prepared in cooperation with the Suffolk County Department of Health Services and the Suffolk County Water Authority","usgsCitation":"Krulikas, R.K., 1981, Hydrogeologic data from selected wells and test holes in Suffolk County, Long Island, New York, 1972-80: U.S. Geological Survey Open-File Report 81-500, Report: iv, 27 p.; 1 Plate: 33.71 x 19.74 inches, https://doi.org/10.3133/ofr81500.","productDescription":"Report: iv, 27 p.; 1 Plate: 33.71 x 19.74 inches","costCenters":[],"links":[{"id":142910,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0500/report-thumb.jpg"},{"id":405119,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405120,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0500/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.82012939453125,\n              40.78885994449482\n            ],\n            [\n              -71.82037353515625,\n              40.78885994449482\n            ],\n            [\n              -71.82037353515625,\n              41.20345619205131\n            ],\n            [\n              -72.82012939453125,\n              41.20345619205131\n            ],\n            [\n              -72.82012939453125,\n              40.78885994449482\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6289ea","contributors":{"authors":[{"text":"Krulikas, Richard K.","contributorId":36910,"corporation":false,"usgs":true,"family":"Krulikas","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":160485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9860,"text":"ofr82157 - 1981 - Discharge data at water-quality monitoring stations in Arkansas, 1980 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-157","title":"Discharge data at water-quality monitoring stations in Arkansas, 1980 water year","docAbstract":"Discharge data were computed for a network of water-quality monitoring stations operated by the Arkansas Department of Pollution Control and Ecology. Some of the sites are located at U.S. Geological Survey of U.S. Army Corps of Engineers daily-discharge stations, but most sites are at points where discharges are not regularly measured. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82157","usgsCitation":"Knott, R., 1981, Discharge data at water-quality monitoring stations in Arkansas, 1980 water year: U.S. Geological Survey Open-File Report 82-157, ii, 37 p., 28 cm., https://doi.org/10.3133/ofr82157.","productDescription":"ii, 37 p., 28 cm.","costCenters":[],"links":[{"id":142660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0157/report-thumb.jpg"},{"id":37654,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0157/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aa2a","contributors":{"authors":[{"text":"Knott, R.K.","contributorId":102484,"corporation":false,"usgs":true,"family":"Knott","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":160419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4232,"text":"cir802 - 1981 - The Alaskan Mineral Resource Assessment Program; background information to accompany folio of geologic and resources maps of the Chignik and Sutwik Island quadrangles, Alaska","interactions":[],"lastModifiedDate":"2025-08-22T13:58:22.298212","indexId":"cir802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"802","title":"The Alaskan Mineral Resource Assessment Program; background information to accompany folio of geologic and resources maps of the Chignik and Sutwik Island quadrangles, Alaska","docAbstract":"The Chignik and Sutwik Island quadrangles (1:250,000) are a part of the Alaska Peninsula in southwestern Alaska. This circular and a companion folio of maps represent results of integrated field and laboratory studies by an interdisciplinary team on geology, geophysics, geochemistry, mineral resources, geochronology, and energy resources to provide a modern assessment of the mineral and energy resources of the quadrangles. The maps contain descriptive text, explanatory material, tables and diagrams, and pertinent references. This circular provides the background data for the mineral and energy resource assessment and integrates the component maps. A comprehensive bibliography cites both specific and general references relevant to the geology and resources of the quadrangles.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir802","usgsCitation":"Detterman, R.L., Case, J.E., Cox, D.P., Detra, D., Miller, T.P., and Wilson, F.H., 1981, The Alaskan Mineral Resource Assessment Program; background information to accompany folio of geologic and resources maps of the Chignik and Sutwik Island quadrangles, Alaska: U.S. Geological Survey Circular 802, iii, 16 p., https://doi.org/10.3133/cir802.","productDescription":"iii, 16 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":31346,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1981/0802/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139313,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1981/0802/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683437","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":148500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":148499,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cox, D. P.","contributorId":82689,"corporation":false,"usgs":true,"family":"Cox","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":148502,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":148501,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Miller, T. P.","contributorId":49345,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":148498,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":148497,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":2346,"text":"wsp2075 - 1981 - Tracing ground-water movement by using the stable isotopes of oxygen and hydrogen, upper Penitencia Creek alluvial fan, Santa Clara Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp2075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"2075","title":"Tracing ground-water movement by using the stable isotopes of oxygen and hydrogen, upper Penitencia Creek alluvial fan, Santa Clara Valley, California","docAbstract":"Starting in 1965 the Santa Clara Valley Water District began importing about i00,000 acre-feet per year of northern California water. About one-half of this water was used to artificially recharge the Upper Penitencia Creek alluvial fan in Santa Clara Valley. In order to determine the relative amounts of local ground water and recharged imported water being pumped from the wells, stable isotopes of oxygen and hydrogen were used to trace the movement of the imported water in the alluvial fan. To trace the movement of imported water in the Upper Penitencia Creek alluvial fan, well samples were selected to give areal and depth coverage for the whole fan. The stable isotopes of oxygen-16, oxygen-18, and deuterium were measured in the water samples of imported water and from the wells and streams in the Santa Clara Valley. The d18oand dD compositions of the local runoff were about -6.00 o/oo (parts per thousand) and -40 o/oo, respectively; the average compositions for the local native ground-water samples were about -6.1 o/oo and -41 o/oo, respectively; and the average compositions of the imported water samples were -10.2 o/oo and -74 o/oo, respectively. (The oxygen isotopic composition of water samples is reported relative to Standard Mean Ocean Water, in parts per thousand.) The difference between local ground water and recharged imported water was about 4.1 o/oo in d18o and 33 o/oo in dL.\r\n\r\nThe isotopic data indicate dilution of northern California water with local ground water in a downgradient direction. Two wells contain approximately 74 percent northern California water, six wells more than 50 percent. Data indicate that there may be a correlation between the percentage of northern California water and the depth or length of perforated intervals in wells.","language":"ENGLISH","publisher":"G.P.O.,","doi":"10.3133/wsp2075","usgsCitation":"Muir, K.S., and Coplen, T.B., 1981, Tracing ground-water movement by using the stable isotopes of oxygen and hydrogen, upper Penitencia Creek alluvial fan, Santa Clara Valley, California: U.S. Geological Survey Water Supply Paper 2075, vi, 18 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp2075.","productDescription":"vi, 18 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2075/report-thumb.jpg"},{"id":28266,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f16e3","contributors":{"authors":[{"text":"Muir, K. S.","contributorId":53764,"corporation":false,"usgs":true,"family":"Muir","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplen, Tyler B. 0000-0003-4884-6008 tbcoplen@usgs.gov","orcid":"https://orcid.org/0000-0003-4884-6008","contributorId":508,"corporation":false,"usgs":true,"family":"Coplen","given":"Tyler","email":"tbcoplen@usgs.gov","middleInitial":"B.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":145055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9833,"text":"ofr81909 - 1981 - A method of estimating flood-frequency parameters for streams in Idaho","interactions":[],"lastModifiedDate":"2023-03-10T23:06:10.358969","indexId":"ofr81909","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-909","title":"A method of estimating flood-frequency parameters for streams in Idaho","docAbstract":"Skew coefficients for the log-Pearson type III distribution are generalized on the basis of some similarity of floods in the Snake River basin and other parts of Idaho. Generalized skew coefficients aid in shaping flood-frequency curves because skew coefficients computed from gaging stations having relatively short periods of peak flow records can be unreliable. Generalized skew coefficients can be obtained for a gaging station from one of three maps in this report. The map to be used depends on whether (1) snowmelt floods are domiant (generally when more than 20 percent of the drainage area is above 6,000 feet altitude), (2) rainstorm floods are dominant (generally when the mean altitude is less than 3,000 feet), or (3) either snowmelt or rainstorm floods can be the annual miximum discharge. For the latter case, frequency curves constructed using separate arrays of each type of runoff can be combined into one curve, which, for some stations, is significantly different than the frequency curve constructed using only annual maximum discharges. For 269 gaging stations, flood-frequency curves that include the generalized skew coefficients in the computation of the log-Pearson type III equation tend to fit the data better than previous analyses. Frequency curves for ungaged sites can be derived by estimating three statistics of the log-Pearson type III distribution. The mean and standard deviation of logarithms of annual maximum discharges are estimated by regression equations that use basin characteristics as independent variables. Skew coefficient estimates are the generalized skews. The log-Pearson type III equation is then applied with the three estimated statistics to compute the discharge at selected exceedance probabilities. Standard errors at the 2-percent exceedance probability range from 41 to 90 percent. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81909","usgsCitation":"Kjelstrom, L., and Moffatt, R.L., 1981, A method of estimating flood-frequency parameters for streams in Idaho: U.S. Geological Survey Open-File Report 81-909, Report: iv, 101 p.;  4 Plates: 26.90 × 25.97 inches or smaller, https://doi.org/10.3133/ofr81909.","productDescription":"Report: iv, 101 p.;  4 Plates: 26.90 × 25.97 inches or 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,{"id":9810,"text":"ofr81400 - 1981 - Single-channel, high-resolution seismic data from six areas of the northern Gulf of Mexico continental slope","interactions":[],"lastModifiedDate":"2024-05-22T20:40:51.358543","indexId":"ofr81400","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-400","title":"Single-channel, high-resolution seismic data from six areas of the northern Gulf of Mexico continental slope","docAbstract":"<p>During the R/V GYRE cruise 80-G-4 in May-June 1980, the U.S. Geological Survey conducted high-resolution seismic studies over five intraslope basins and over one selected area of special interest in the northern Gulf of Mexico (fig. 1). Data from each area suggest that the intraslope basins are directly related to past and present salt-diapir activities and sea-level changes. The study areas had been selected on the basis of results of previous high-resolution seismic studies in the northern Gulf of Mexico.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81400","usgsCitation":"Kindinger, J.L., and Bouma, A.H., 1981, Single-channel, high-resolution seismic data from six areas of the northern Gulf of Mexico continental slope: U.S. Geological Survey Open-File Report 81-400, 4 p., https://doi.org/10.3133/ofr81400.","productDescription":"4 p.","costCenters":[],"links":[{"id":429168,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0400/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141827,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0400/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Louisiana, Mississippi, Texas","otherGeospatial":"northern Gulf of Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -98.48568064182483,\n              30.51983035090467\n            ],\n            [\n              -98.48568064182483,\n              26.701172625915575\n            ],\n            [\n              -82.47534593349111,\n              26.701172625915575\n            ],\n            [\n              -82.47534593349111,\n              30.51983035090467\n            ],\n            [\n              -98.48568064182483,\n              30.51983035090467\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1785","contributors":{"authors":[{"text":"Kindinger, Jack L. jkindinger@usgs.gov","contributorId":815,"corporation":false,"usgs":true,"family":"Kindinger","given":"Jack","email":"jkindinger@usgs.gov","middleInitial":"L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":160339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bouma, Arnold H.","contributorId":48172,"corporation":false,"usgs":true,"family":"Bouma","given":"Arnold","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":160340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9796,"text":"ofr81823 - 1981 - Hydrologic data for North Creek, Trinity River basin, Texas, 1979","interactions":[],"lastModifiedDate":"2022-01-03T18:38:32.290754","indexId":"ofr81823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-823","title":"Hydrologic data for North Creek, Trinity River basin, Texas, 1979","docAbstract":"<p>This report contains rainfall and runoff data collected during the 1979 water year for the 21.6-square mile area above the stream-gaging station North Creek near Jacksboro, Texas. A continuous water-stage recording gage was installed at one representative floodwater-retarding structure (site 28-A) on Oct. 5, 1972. The data are collected to compute the contents, surface area, inflow, and outflow at this site. The stream-gaging station on North Creek near Jacksboro continuously records the water level which, with measurements of streamflow, is used to compute the runoff from the study area. Streamflow records at this gage began on Aug. 8, 1956. Detailed rainfall-runoff computations are included for one storm during the 1979 water year at the stream-gaging station. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81823","collaboration":"Prepared in cooperation with the Tarrant County Water Control and Improvement District No. 1, the Soil Conservation Service, and the Texas Department of Water Resources","usgsCitation":"Kidwell, C., 1981, Hydrologic data for North Creek, Trinity River basin, Texas, 1979: U.S. Geological Survey Open-File Report 81-823, 38 p., https://doi.org/10.3133/ofr81823.","productDescription":"38 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":141766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0823/report-thumb.jpg"},{"id":393765,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0823/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"North Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ec9a","contributors":{"authors":[{"text":"Kidwell, C.C.","contributorId":54998,"corporation":false,"usgs":true,"family":"Kidwell","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":160316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4716,"text":"twri07C3 - 1981 - A model for simulation of flow in singular and interconnected channels","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri07C3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"07-C3","title":"A model for simulation of flow in singular and interconnected channels","docAbstract":"A one-dimensional numerical model is presented for simulating the unsteady flow in singular riverine or estuarine reaches and in networks of reaches composed of interconnected channels. The model is both general and flexible in that it can be used to simulate a wide range of flow conditions for various channel configurations. The channel geometry of the network to be modeled should be sufficiently simple so as to lend itself to characterization in one spatial dimension. The flow must be substantially homogenous in density, and hydrostatic pressure must prevail everywhere in the network channels. The slope of each channel bottom ought to be mild and reasonably constant over its length so that the flow remains subcritical. The model accommodates tributary inflows and diversions and includes the effects of wind shear on the water surface as a forcing function in the flow equations. Water-surface elevations and flow discharges are computed at channel junctions, as well as at specified intermediate locations within the network channels.\r\nThe one-dimensional branch-network flow model uses a four-point, implicit, finite-difference approximation of the unsteady-flow equations. The flow equations are linearized over a time step, and branch transformations are formulated that describe the relationship between the unknowns at the end points of the channels. The resultant matrix of branch-transformation equations and required boundary-condition equations is solved by Gaussian elimination using maximum pivot strategy.\r\nFive example applications of the flow model are illustrated. The applications cover such diverse conditions as a singular upland river reach in which unsteady flow results from hydropower regulations, coastal rivers composed of sequentially connected reaches subject to unsteady tide-driven flow, and a multiply connected network of channels whose flow is principally governed by wind tides and seiches in adjoining lakes.\r\nThe report includes a listing of the FORTRAN IV computer program and a description of the input data requirements. Model supporting programs for the processing and input of initial and boundary-value data are identified, various model output formats are illustrated, and instructions are given to permit the production of graphical output using the line printer, electromechanical pen plotters, cathode-ray-tube display units, or microfilm recorders.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri07C3","issn":"0565-596X","usgsCitation":"Schaffranek, R.W., Baltzer, R., and Goldberg, D., 1981, A model for simulation of flow in singular and interconnected channels (1981 edition): U.S. Geological Survey Techniques of Water-Resources Investigations 07-C3, x, 110 p. :ill., maps ;26 cm., https://doi.org/10.3133/twri07C3.","productDescription":"x, 110 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":139210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":344,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri7c3/","linkFileType":{"id":5,"text":"html"}}],"edition":"1981 edition","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf77","contributors":{"authors":[{"text":"Schaffranek, Raymond W.","contributorId":86314,"corporation":false,"usgs":true,"family":"Schaffranek","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":149668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baltzer, R.A.","contributorId":86321,"corporation":false,"usgs":true,"family":"Baltzer","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":149669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldberg, D.E.","contributorId":66245,"corporation":false,"usgs":true,"family":"Goldberg","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":149667,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9744,"text":"ofr81694 - 1981 - Modification of the Tangborn short-term hydrometeorological model, with trial results from the Baker River basin, Washington","interactions":[],"lastModifiedDate":"2022-08-16T17:41:32.902534","indexId":"ofr81694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-694","title":"Modification of the Tangborn short-term hydrometeorological model, with trial results from the Baker River basin, Washington","docAbstract":"<p>This report presents a modification of the short-term hydrometeorological model (Tangborn, 1978) for estimating river-basin snowmelt runoff. A multiple linear regression replaces a nonlinear regression scheme to correct for temperature effects of snowmelt runoff. Results based on data from the Baker River basin, Washington, indicate that model performance is improved by the modification in a majority of applications, and, additionally, use of the model is simplified and computer time is reduced.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81694","collaboration":"Prepared in cooperation with Puget Sound Power and Light Company","usgsCitation":"Karlinger, M., and Wilson, J.D., 1981, Modification of the Tangborn short-term hydrometeorological model, with trial results from the Baker River basin, Washington: U.S. Geological Survey Open-File Report 81-694, iii, 63 p., https://doi.org/10.3133/ofr81694.","productDescription":"iii, 63 p.","costCenters":[],"links":[{"id":405198,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0694/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Baker River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.47283935546874,\n              48.398208936781806\n            ],\n            [\n              -121.57745361328125,\n              48.398208936781806\n            ],\n            [\n              -121.57745361328125,\n              48.629278127969414\n            ],\n            [\n              -122.47283935546874,\n              48.629278127969414\n            ],\n            [\n              -122.47283935546874,\n              48.398208936781806\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6994f3","contributors":{"authors":[{"text":"Karlinger, M.R.","contributorId":95039,"corporation":false,"usgs":true,"family":"Karlinger","given":"M.R.","affiliations":[],"preferred":false,"id":160220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, J. D.","contributorId":25154,"corporation":false,"usgs":true,"family":"Wilson","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160219,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9733,"text":"ofr81406 - 1981 - Quality of water in Tibbee Creek and tributaries near West Point, Mississippi","interactions":[],"lastModifiedDate":"2022-08-10T13:46:14.777396","indexId":"ofr81406","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-406","title":"Quality of water in Tibbee Creek and tributaries near West Point, Mississippi","docAbstract":"<p>An intensive water-quality study was conducted on Tibbee Creek and two of its tributaries, Town Creek and Catalpa Creek, on June 19-22, 1979. The data were collected during a period of low discharge and high air temperatures. The water in Tibbee Creek and Catalpa Creek was of much better quality than water in Town Creek. Large quantities of nitrogen, phosphorus, and dissolved solids and high densities of fecal coliform were present in Town Creek. The five-day biochemical oxygen demand values averaged 14 mg/L, and the mean total nitrogen concentration was 56 mg/L. The mean concentrations of ammonia, nitrate plus nitrite nitrogen, and organic nitrogen were 1.8 mg/L, 50 mg/L, and 3.7 mg/L, respectively. A total phosphorus load of more than 400 pounds per day, more than 91 percent of the total phosphorus load leaving the study area, was carried by Town Creek into Tibbee Creek. Total phosphorus concentrations averaged 14 mg/L in Town Creek and 0.11 and 0.12 mg/L in Tibbee and Catalpa Creeks respectively. Bacterial densities were higher at site 2 in Town Creek than at sites 1 and 3 in Tibbee and Catalpa Creeks respectively. The median fecal coliform bacterial density was 25,000 col/100 mL (colonies per 100 milliliters) in Town Creek and less than 200 col/100 mL in Tibbee and Catalpa Creeks. Median fecal streptococcal densities were 1,000 col/100 mL in Town Creek, 210 col/100 mL in Tibbee Creek, and 800 col/100 mL in Catalpa Creek. Fecal coliform to fecal streptococcal ratios were greater than 4.0 in Town Creek, indicating wastes of human origin were probably present during the study. Ratios were less than 0.7 in Tibbee and Catalpa Creeks, indicating human wastes were probably absent during the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81406","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources Bureau of Pollution Control","usgsCitation":"Kalkhoff, S.J., 1981, Quality of water in Tibbee Creek and tributaries near West Point, Mississippi: U.S. Geological Survey Open-File Report 81-406, v, 42 p., https://doi.org/10.3133/ofr81406.","productDescription":"v, 42 p.","costCenters":[],"links":[{"id":405069,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75487.htm","linkFileType":{"id":5,"text":"html"}},{"id":143076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0406/report-thumb.jpg"},{"id":405013,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0406/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","city":"West Point","otherGeospatial":"Tibbee Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.71734619140625,\n              33.57687060377715\n            ],\n            [\n              -88.58551025390624,\n              33.57687060377715\n            ],\n            [\n              -88.58551025390624,\n              33.6283419913718\n            ],\n            [\n              -88.71734619140625,\n              33.6283419913718\n            ],\n            [\n              -88.71734619140625,\n              33.57687060377715\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bc87a","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160203,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9724,"text":"ofr81365 - 1981 - Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake","interactions":[{"subject":{"id":9724,"text":"ofr81365 - 1981 - Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake","indexId":"ofr81365","publicationYear":"1981","noYear":false,"title":"Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake"},"predicate":"SUPERSEDED_BY","object":{"id":70047764,"text":"70047764 - 1981 - Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake","indexId":"70047764","publicationYear":"1981","noYear":false,"title":"Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake"},"id":1}],"supersededBy":{"id":70047764,"text":"70047764 - 1981 - Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake","indexId":"70047764","publicationYear":"1981","noYear":false,"title":"Peak horizontal acceleration and velocity from strong-motion records including records from the 1979 imperial valley, California, earthquake"},"lastModifiedDate":"2022-08-09T15:30:39.458696","indexId":"ofr81365","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-365","title":"Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake","docAbstract":"<p>We have taken advantage of the recent increase in strong-motion data at close distances to derive new attenuation relations for peak horizontal acceleration and velocity. Acceleration data from 183 recordings of 24 earthquakes and velocity data from 62 recordings of 10 earthquakes have been used. This new analysis uses a magnitude-independent shape for the attenuation curve based on geometrical spreading and anelastic attenuation. A magnitude-dependent shape could be accommodated by the method, but the data do not support it. An innovation in technique is introduced that decouples the determination of the distance dependence of the data from the magnitude dependence.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81365","usgsCitation":"Joyner, W.B., Boore, D.M., and Porcella, R.L., 1981, Peak horizontal acceleration and velocity from strong motion records including records from the 1979 Imperial Valley, California, earthquake: U.S. Geological Survey Open-File Report 81-365, 46 p., https://doi.org/10.3133/ofr81365.","productDescription":"46 p.","costCenters":[],"links":[{"id":405015,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0365/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0365/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Imperial Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.58029174804686,\n              32.713355353177555\n            ],\n            [\n              -114.67391967773436,\n              32.713355353177555\n            ],\n            [\n              -114.67391967773436,\n              33.002905178377304\n            ],\n            [\n              -115.58029174804686,\n              33.002905178377304\n            ],\n            [\n              -115.58029174804686,\n              32.713355353177555\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6889cb","contributors":{"authors":[{"text":"Joyner, William B.","contributorId":39786,"corporation":false,"usgs":true,"family":"Joyner","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":160188,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porcella, Ronald L.","contributorId":26674,"corporation":false,"usgs":true,"family":"Porcella","given":"Ronald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160190,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9706,"text":"ofr81469 - 1981 - Geologic data for borehole ERDA-9, Eddy County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr81469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-469","title":"Geologic data for borehole ERDA-9, Eddy County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81469","usgsCitation":"Jones, C., 1981, Geologic data for borehole ERDA-9, Eddy County, New Mexico: U.S. Geological Survey Open-File Report 81-469, ii, 49 p., 3 over-size sheets ;28 cm., https://doi.org/10.3133/ofr81469.","productDescription":"ii, 49 p., 3 over-size sheets ;28 cm.","costCenters":[],"links":[{"id":142356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0469/report-thumb.jpg"},{"id":37421,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0469/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37422,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0469/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37423,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0469/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0469/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a63c1","contributors":{"authors":[{"text":"Jones, C.L.","contributorId":60218,"corporation":false,"usgs":true,"family":"Jones","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":160159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9705,"text":"ofr81468 - 1981 - Geologic data for borehole ERDA-6, Eddy County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr81468","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-468","title":"Geologic data for borehole ERDA-6, Eddy County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81468","usgsCitation":"Jones, C., 1981, Geologic data for borehole ERDA-6, Eddy County, New Mexico: U.S. Geological Survey Open-File Report 81-468, ii, 60 p., 2 over-size sheets ;28 cm., https://doi.org/10.3133/ofr81468.","productDescription":"ii, 60 p., 2 over-size sheets ;28 cm.","costCenters":[],"links":[{"id":142355,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0468/report-thumb.jpg"},{"id":37418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0468/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37419,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0468/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37420,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0468/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a639e","contributors":{"authors":[{"text":"Jones, C.L.","contributorId":60218,"corporation":false,"usgs":true,"family":"Jones","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":160158,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9644,"text":"ofr81143 - 1981 - Aquatic biology of the Redwood Creek and Mill Creek drainage basins, Redwood National Park, Humboldt and Del Norte counties, California","interactions":[],"lastModifiedDate":"2021-02-22T22:21:27.062244","indexId":"ofr81143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-143","title":"Aquatic biology of the Redwood Creek and Mill Creek drainage basins, Redwood National Park, Humboldt and Del Norte counties, California","docAbstract":"<p>A 2-year study of the aquatic biota in the Redwood Creek and Mill Creek drainage basins of Redwood National Park indicated that the aquatic productivity is low. </p><p>Densities of coliform bacteria were low except in Prairie Creek, a tributary to Redwood Creek, where a State park, county fish hatchery, grazing land, lumber mill, and scattered residential areas are potential sources of fecal coliform bacteria. </p><p>Benthic invertebrate data indicated a diverse fauna which varied considerably between streams and among stream sections. Noteworthy findings include: (1) benthic invertebrates rapidly recolonized the streambed following a major storm, and (2) man-caused disruption or sedimentation of the streambed during low flow can result in drastic reductions of the benthic invertebrate community. </p><p>Seven species of fish representing species typically found in northern California coastal streams were captured during the study. Nonparametric statistical tests indicate that condition factors of steelhead trout were significantly larger at sampling stations with more insolation, regardless of drainage basin land-use history. </p><p>Periphyton and phytoplankton communities were diverse, variable in numbers, and dominated by diatoms. Seston concentrations were extremely variable between stations and at each station sampled. </p><p>The seston is influenced seasonally by aquatic productivity at each station and amount of allochthonous material from the terrestrial ecosystem. Time-series analysis of some seston data indicated larger and sharper peak concentrations being flushed from the logged drainage basin than from the control drainage basin. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr81143","usgsCitation":"Iwatsubo, R.T., and Averett, R., 1981, Aquatic biology of the Redwood Creek and Mill Creek drainage basins, Redwood National Park, Humboldt and Del Norte counties, California: U.S. Geological Survey Open-File Report 81-143, v, 115 p., https://doi.org/10.3133/ofr81143.","productDescription":"v, 115 p.","costCenters":[],"links":[{"id":383529,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0143/report-thumb.jpg"}],"country":"United States","state":"California","county":"Del Norte County, Humboldt County","otherGeospatial":"Redwood National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.04388427734374,\n              41.20242295382758\n            ],\n            [\n              -123.93951416015626,\n              41.20242295382758\n            ],\n            [\n              -123.93951416015626,\n              41.24890252240322\n            ],\n            [\n              -124.04388427734374,\n              41.24890252240322\n            ],\n            [\n              -124.04388427734374,\n              41.20242295382758\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a08a","contributors":{"authors":[{"text":"Iwatsubo, Rick T.","contributorId":11602,"corporation":false,"usgs":true,"family":"Iwatsubo","given":"Rick","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":160042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":160043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9628,"text":"ofr811109 - 1981 - Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska","interactions":[],"lastModifiedDate":"2022-04-12T17:29:54.327941","indexId":"ofr811109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1109","title":"Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska","docAbstract":"<p>The Platte River in south-central Nebraska flows generally eastward in a broad, flat valley. The river banks and many areas adjacent to the river support thick stands of cottonwood and willow trees. Brush, grass, pasture land, and cultivated fields occupy most of the remaining area. This is the habitat for many types of wildlife that live in the area or stop over in the area during annual migrations. Both sandhill cranes and whooping cranes are part of the annual migration. There is concern that water-management changes, such as surface-water diversions or ground-water withdrawals for irrigation, may alter the hydrologic environment of the wetland areas and be harmful to the wildlife habitat. In order to determine what affect changes in water management might have on ground-water levels in the wetland areas, detailed data were collected from Crane Meadows Wildlife Area, which is on an island in the Platte River near Grand Island, Nebr. Ground-water levels beneath the island respond to changes in river stage, to recharge from snowmelt and precipitation, and to evapotranspiration by riparian vegetation and from areas where the water table is close to the land surface. The data show that ground-water levels respond rapidly to changes in river stage-usually within 24 hours for distances up to 2,500 feet from the edge of the river. Thus changes in river stage due to changes in surface-water diversions will not have a long-term effect on ground-water levels. Changes in ground-water withdrawals will have the double effect of changing ground-water levels due to changes in drawdown and due to changes in river stage caused by the effects of pumping on river flow. These effects will develop slowly and be long lasting.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811109","usgsCitation":"Hurr, R.T., 1981, Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska: U.S. Geological Survey Open-File Report 81-1109, iv, 16 p., https://doi.org/10.3133/ofr811109.","productDescription":"iv, 16 p.","costCenters":[],"links":[{"id":398556,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1109/report-thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Hall County","otherGeospatial":"Mormon Island Crane Meadows wildlife area near Grand Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.37741851806639,\n              40.82160395916235\n            ],\n            [\n              -98.36797714233398,\n              40.82160395916235\n            ],\n            [\n              -98.36797714233398,\n              40.82712467108559\n            ],\n            [\n              -98.37741851806639,\n              40.82712467108559\n            ],\n            [\n              -98.37741851806639,\n              40.82160395916235\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668a6e","contributors":{"authors":[{"text":"Hurr, R. Theodore","contributorId":27023,"corporation":false,"usgs":true,"family":"Hurr","given":"R.","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":160016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9620,"text":"ofr811225 - 1981 - Digitizing procedure for the National Coal Resources Data System of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr811225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1225","title":"Digitizing procedure for the National Coal Resources Data System of the U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811225","usgsCitation":"Hunter, J.F., Crowley, S.S., and Medlin, A.L., 1981, Digitizing procedure for the National Coal Resources Data System of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 81-1225, 10 p.  ill. ;28 cm., https://doi.org/10.3133/ofr811225.","productDescription":"10 p.  ill. ;28 cm.","costCenters":[],"links":[{"id":141758,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1225/report-thumb.jpg"},{"id":37352,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1225/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64acc0","contributors":{"authors":[{"text":"Hunter, Judy F.","contributorId":50895,"corporation":false,"usgs":true,"family":"Hunter","given":"Judy","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crowley, Sharon S.","contributorId":78325,"corporation":false,"usgs":true,"family":"Crowley","given":"Sharon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Medlin, Antoinette L.","contributorId":84370,"corporation":false,"usgs":true,"family":"Medlin","given":"Antoinette","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160007,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9613,"text":"ofr8169 - 1981 - Low-flow frequency data for selected stream gaging stations in Florida","interactions":[],"lastModifiedDate":"2013-08-02T07:15:54","indexId":"ofr8169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-69","title":"Low-flow frequency data for selected stream gaging stations in Florida","docAbstract":"This report contains tables of low-flow frequency data for 161 stream-gaging stations in Florida. The selected stations represent those having suitable flow records spanning 7 or more years. Flow values representing the annual minimum average flow for selected periods ranging from 1 to 183 days are presented for recurrence intervals ranging from 2 to 50 years. The low-flow frequency data of relatively short-term stations were adjusted where possible on basis of records of long-term stations to reduce the possible bias introduced by short-term climatic trends. (USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr8169","usgsCitation":"Hughes, G., 1981, Low-flow frequency data for selected stream gaging stations in Florida: U.S. Geological Survey Open-File Report 81-69, ix, 110 p. :maps ;28 cm., https://doi.org/10.3133/ofr8169.","productDescription":"ix, 110 p. :maps ;28 cm.","costCenters":[],"links":[{"id":141735,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0069/report-thumb.jpg"},{"id":275907,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0069/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64874c","contributors":{"authors":[{"text":"Hughes, G.H.","contributorId":73975,"corporation":false,"usgs":true,"family":"Hughes","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":159996,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9611,"text":"ofr81811 - 1981 - Ground-water data for Michigan, 1980","interactions":[],"lastModifiedDate":"2017-07-12T10:38:15","indexId":"ofr81811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-811","title":"Ground-water data for Michigan, 1980","docAbstract":"<p>The purpose of this report is to make available the 1980 records of water levels and related data for the principal aquifers of the State. This report is written for municipalities, industries, institutions, consultants, drillers, hydrologists and other people interested in the ground-water resources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr81811","usgsCitation":"Huffman, G., 1981, Ground-water data for Michigan, 1980: U.S. Geological Survey Open-File Report 81-811, iv, 57 p., https://doi.org/10.3133/ofr81811.","productDescription":"iv, 57 p.","numberOfPages":"65","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343665,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0811/report-thumb.jpg"}],"country":"United 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,{"id":9597,"text":"ofr81816 - 1981 - U.S. Geological Survey reports on the water resources of Florida, 1886-1980","interactions":[{"subject":{"id":23401,"text":"ofr81337 - 1980 - United States Geological Survey reports on the water resources of Florida, 1886-1979","indexId":"ofr81337","publicationYear":"1980","noYear":false,"title":"United States Geological Survey reports on the water resources of Florida, 1886-1979"},"predicate":"SUPERSEDED_BY","object":{"id":9597,"text":"ofr81816 - 1981 - U.S. Geological Survey reports on the water resources of Florida, 1886-1980","indexId":"ofr81816","publicationYear":"1981","noYear":false,"title":"U.S. Geological Survey reports on the water resources of Florida, 1886-1980"},"id":1}],"lastModifiedDate":"2022-11-09T18:29:23.094384","indexId":"ofr81816","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-816","title":"U.S. Geological Survey reports on the water resources of Florida, 1886-1980","docAbstract":"<p>The U.S. Geological Survey has been making investigations of the water resources of Florida since the latter part of the 19th century. The earlier work consisted mainly of data collection at a few spring and river sites at intermittent intervals with the exception of a statewide ground-water study made during 1910-12 (Matson and Sanford, 1913).</p><p>Since 1930, when an office was established for surface-water studies and in 1938 for ground-water studies in Florida, practically all of the water-resources investigations made by the U.S. Geological Survey have been in cooperation with state and local agencies.</p><p>This second edition of \"United States Geological Survey Reports on the Water Resources of Florida, 1886-1980\" includes reports approved for release in calendar year 1980. In addition to updating the first edition (1980) several reports released prior to 1979, which were inadvertently omitted, have been added.</p><p>The bibliographic list of publications which follows is arranged alphabetically by senior author.</p><p>The publications are also indexed by geographic area and by subject. Only two lines are used for each publication in the indexes; thus the complete reference is given only in the bibliographic list.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81816","usgsCitation":"Hoy, N.D., Simmons, J.D., and Claiborne, M., 1981, U.S. Geological Survey reports on the water resources of Florida, 1886-1980 (Second Edition): U.S. Geological Survey Open-File Report 81-816, viii, 212 p., https://doi.org/10.3133/ofr81816.","productDescription":"viii, 212 p.","costCenters":[],"links":[{"id":409271,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0816/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0816/report-thumb.jpg"}],"country":"United 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,{"id":9583,"text":"ofr81111 - 1981 - The Sea Data 651-4 data logger","interactions":[],"lastModifiedDate":"2022-07-18T21:57:02.952678","indexId":"ofr81111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-111","title":"The Sea Data 651-4 data logger","docAbstract":"<p>This paper describes a digital data logger used as the primary controller and data collection device for the U.S. Geological Survey Sediment Monitoring Tripod Program. The tripods are deployed at sea in water depths up to 100 m for periods of 3 to 6 months. The system measures bottom current speed and direction, pressure, temperature, light transmission, and photographs the bottom. This report is intended to provide a description of the unit and its operation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81111","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Hosom, D.S., and Butman, B., 1981, The Sea Data 651-4 data logger: U.S. Geological Survey Open-File Report 81-111, vii, 85 p., https://doi.org/10.3133/ofr81111.","productDescription":"vii, 85 p.","costCenters":[],"links":[{"id":403969,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0111/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0111/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4a0","contributors":{"authors":[{"text":"Hosom, David S.","contributorId":64257,"corporation":false,"usgs":true,"family":"Hosom","given":"David","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":159948,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9564,"text":"ofr81961 - 1981 - E-field ratio telluric survey near the Big Maria Mountains, Riverside County, California","interactions":[],"lastModifiedDate":"2021-09-15T20:09:24.529001","indexId":"ofr81961","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-961","title":"E-field ratio telluric survey near the Big Maria Mountains, Riverside County, California","docAbstract":"<p>The U.S. Geological Survey (USGS) under the Wilderness Act (Public Law 88-577) and the Federal Land Policy and Management Act (Public Law 94-579) has the responsibility, along with the U.S. Bureau of Mines, to survey certain areas in order to determine their mineral resource potential. This report presents results of three electric-field ratio telluric traverses conducted as part of the Bureau of Land Management Wilderness Program in the Big Maria Mountains, Riverside County, Calif. The telluric traverses were run on the southwest side of the Big Maria Mountains in an attempt to define the location of major buried faults near the eroded front of the range.</p><p>E-field ratio tellurics is a descriptive name applied to the electrical exploration technique used in this survey. The telluric method refers to the measurement of the earth's electric field generated by induction from natural electromagnetic waves arriving at the surface. The E-field ratio telluric method uses a receiving array of three electrodes spaced equidistant and inline. This array is, in effect, two colinear dipoles sharing a common electrode. The potential difference across each dipole is then proportional to the component of the telluric field in the direction of the array. This configuration permits the measurement of the ratio of the telluric field at each dipole in the direction of the dipole line, and hence the name. The traverse data is extended by moving the three-electrode array forward one dipole length so that the forward electrode becomes the center electrode for the next ratio measurement.</p><p>Electric-field data so obtained are proportional to the square root of the apparent resistivity of the earth at the location of the dipoles. However, because the apparent resistivity can be a function of the dipole direction, it is important to know the orientation of the dipoles with respect to major structures. Because the resistivity of fluid-saturated earth materials is largely dependent on the porosity of the rocks, the salinity of the pore fluid, and the presence of clays or similar material where surface conduction is high, alluvial fill, argillite and similar rocks tend to have low resistivities whereas igneous or high-grade metamorphic rocks have high resistivities. Variation in the electrical properties along a traverse may then be used to infer lithologic or structural changes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81961","usgsCitation":"Hoover, D.B., Broker, M.M., and Stambaugh, T., 1981, E-field ratio telluric survey near the Big Maria Mountains, Riverside County, California: U.S. Geological Survey Open-File Report 81-961, 15 p., https://doi.org/10.3133/ofr81961.","productDescription":"15 p.","costCenters":[],"links":[{"id":389296,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0961/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0961/report-thumb.jpg"}],"country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Big Maria Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.98016357421875,\n              33.543683878655926\n            ],\n            [\n              -114.26742553710936,\n              33.543683878655926\n            ],\n            [\n              -114.26742553710936,\n              34.023071367612125\n            ],\n            [\n              -114.98016357421875,\n              34.023071367612125\n            ],\n            [\n              -114.98016357421875,\n              33.543683878655926\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f545","contributors":{"authors":[{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":159901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broker, Michael M.","contributorId":6058,"corporation":false,"usgs":true,"family":"Broker","given":"Michael","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159902,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stambaugh, T.","contributorId":6448,"corporation":false,"usgs":true,"family":"Stambaugh","given":"T.","email":"","affiliations":[],"preferred":false,"id":159900,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9552,"text":"ofr811061 - 1981 - Flow model of Saginaw River near Saginaw, Michigan","interactions":[],"lastModifiedDate":"2017-07-12T10:39:57","indexId":"ofr811061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1061","title":"Flow model of Saginaw River near Saginaw, Michigan","docAbstract":"<p>An unsteady-flow simulation model was applied to a 19.5-mile reach of Saginaw River. The model provides a method of determining instantaneous discharge for flows from -8,000 to 12,000 cubic feet per second. The currently used slope-rating method can be utilized to compute discharge only under steady and high-flow conditions. Unsteady flow frequently occurs in the Saginaw River as a result of lake seiching. </p><p>Model computations are based on solution of the continuity and momentum flow equations, on hydraulic characteristics of Saginaw River, and on time-dependent boundary conditions. An implicit, finite-difference technique is used to solve the one-dimensional flow equations. Channel storage and conveyance characteristics were obtained from data collected during a 1979 field survey and through model calibration. Boundary conditions are specified by stage or discharge data at the model extremities. Optionally, wind velocity data are incorporated in the flow simulations. </p><p>The model can simulate instantaneous stage and discharge data and summarize or plot the data. Simulations of low-flows are sensitive to small errors in stage data and to gentle breezes. Simulation of high flows for present channel conditions requires additional data and further study.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr811061","usgsCitation":"Holtschlag, D.J., 1981, Flow model of Saginaw River near Saginaw, Michigan: U.S. Geological Survey Open-File Report 81-1061, v, 20 p., https://doi.org/10.3133/ofr811061.","productDescription":"v, 20 p.","numberOfPages":"30","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1061/report-thumb.jpg"},{"id":343667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","otherGeospatial":"Saginaw River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.40521240234375,\n              43.29320031385282\n            ],\n            [\n              -83.69384765625,\n              43.29320031385282\n            ],\n            [\n              -83.69384765625,\n              43.79092385423618\n            ],\n            [\n              -84.40521240234375,\n              43.79092385423618\n            ],\n            [\n              -84.40521240234375,\n              43.29320031385282\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df2d6","contributors":{"authors":[{"text":"Holtschlag, David J. 0000-0001-5185-4928 dholtschlag@usgs.gov","orcid":"https://orcid.org/0000-0001-5185-4928","contributorId":5447,"corporation":false,"usgs":true,"family":"Holtschlag","given":"David","email":"dholtschlag@usgs.gov","middleInitial":"J.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":true,"id":159878,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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