{"pageNumber":"1718","pageRowStart":"42925","pageSize":"25","recordCount":46619,"records":[{"id":60208,"text":"mf878G - 1978 - Geochemical and generalized geologic map showing distribution and abundance of barium, arsenic, boron, and vanadium in stream sediments in the Chandalar Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-05-19T20:06:04.46265","indexId":"mf878G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"878","chapter":"G","title":"Geochemical and generalized geologic map showing distribution and abundance of barium, arsenic, boron, and vanadium in stream sediments in the Chandalar Quadrangle, Alaska","docAbstract":"<p><span>This geochemical map shows the distribution and abundance of barium (Ba), arsenic (As), boron (B), and vanadium (V) in -80 mesh (177 micrometers) stream sediment samples in the Chandalar quadrangle, Alaska. The map is a part of a series of geochemical maps that together with the background information circular (Reiser and others, 1978) comprise the folio on the Chandalar quadrangle, Alaska. The data are plotted on a subdued base map showing the generalized geology, topography, and sample localities. Map symbols showing the ranges of metal values are indicated on the accompanying histograms and all values shown are considered anomalous. An explanation of sampling, preparation, analytical procedures, and geochemical raw data for all samples are discussed by O'Leary and others (1976). The -80 mesh (177 micrometers) stream sediment medium was used in this study because of the regional setting in the north-central Brooks Range. Given the rather restrictive time and manpower constraints the -80 mesh (177 micrometers) stream sediment combined with panned concentrates was determined to be the most economical and adequate medium in this case where clastic sediments are being derived from local bedrock.&nbsp;</span></p><p><span>The study area is generally one of high relief with short fast-moving streams and broad glacial valleys. All samples were taken from active streams, as close to the center channel as possible. All sediments were considered to be locally derived. Care was taken, when sampling an obviously glaciated terrane, to sample above or upstream from morainal material, wherever possible. Most samples were taken in areas where bedrock was within 30 m of the sample site.</span></p><p><span>Due to the poor sensitivity by spectrographic analysis for arsenic, 200 ppm (parts per million), all arsenic analyses were done by colorimetry.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf878G","usgsCitation":"Marsh, S., Detra, D., and Smith, S., 1978, Geochemical and generalized geologic map showing distribution and abundance of barium, arsenic, boron, and vanadium in stream sediments in the Chandalar Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 878, 1 Plate: 40.94 x 34.75 inches, https://doi.org/10.3133/mf878G.","productDescription":"1 Plate: 40.94 x 34.75 inches","costCenters":[],"links":[{"id":183637,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0878-G/report-thumb.jpg"},{"id":417264,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0878-G/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Chandalar Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,67 ], [ -150,68 ], [ -147,68 ], [ -147,67 ], [ -150,67 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae84b","contributors":{"authors":[{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":263321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":263322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":263320,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60214,"text":"mf878D - 1978 - Geochemical and generalized geologic map showing distribution and abundance of molybdenum, copper, and lead in stream sediments in the Chandalar Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-05-19T20:05:06.877696","indexId":"mf878D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"878","chapter":"D","title":"Geochemical and generalized geologic map showing distribution and abundance of molybdenum, copper, and lead in stream sediments in the Chandalar Quadrangle, Alaska","docAbstract":"<p>This geochemical map shows the distribution and abundance of molybdenum (Mo), copper (Cu), and lead (Pb) of -80 mesh (177 micrometers) stream sediment samples in the Chandalar quadrangle, Alaska. The map is a part of a series of geochemical maps that together with the background information circular (Reiser and others, 1978) comprise the folio on the Chandalar quadrangle, Alaska. The data are plotted on a subdued base map showing the generalized geology, topography, and sample localities. Map symbols showing the ranges of metal values are indicated on the accompanying histograms and all values shown are considered anomalous. An explanation of sampling, preparation, analytical procedures and geochemical raw data for all samples are discussed by O'Leary and others (1976). The -80 mesh (177 micrometers) stream sediment medium was used in this study because of the regional setting in the north-central Brooks Range. Given the rather restrictive time and manpower constraints the -80 mesh (177 micrometers) stream sediment combined with panned concentrates was determined to be the most economical and adequate medium in this case where clastic sediments are being derived from local bedrock.&nbsp;</p><p>The study area is generally one of high relief with short fast-moving streams and broad glacial valleys. All samples were taken from active streams, as close to the center channel as possible. All sediments were considered to be locally derived. Care was taken, when sampling an obviously glaciated terrane, to sample above or upstream from morainal material, wherever possible. Most samples were taken in areas where bedrock was within 30 m of the sample site.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf878D","usgsCitation":"Marsh, S., Detra, D., and Smith, S., 1978, Geochemical and generalized geologic map showing distribution and abundance of molybdenum, copper, and lead in stream sediments in the Chandalar Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 878, 1 Plate: 43.96 x 35.95 inches, https://doi.org/10.3133/mf878D.","productDescription":"1 Plate: 43.96 x 35.95 inches","costCenters":[],"links":[{"id":417262,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0878-D/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182658,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0878-D/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Chandalar Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,67 ], [ -150,68 ], [ -147,68 ], [ -147,67 ], [ -150,67 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae83d","contributors":{"authors":[{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":263329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":263330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":263328,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57475,"text":"wdrND771 - 1978 - Water resources data for North Dakota, water year 1977","interactions":[],"lastModifiedDate":"2020-10-27T17:16:34.886261","indexId":"wdrND771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-77-1","title":"Water resources data for North Dakota, water year 1977","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND771","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for North Dakota, water year 1977: U.S. Geological Survey Water Data Report ND-77-1, xi, 512 p., https://doi.org/10.3133/wdrND771.","productDescription":"xi, 512 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,{"id":60216,"text":"mf878E - 1978 - Geochemical and generalized geologic map showing distribution and abundance of zinc in stream sediments in the Chandalar Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2023-05-19T20:07:36.894933","indexId":"mf878E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"878","chapter":"E","title":"Geochemical and generalized geologic map showing distribution and abundance of zinc in stream sediments in the Chandalar Quadrangle, Alaska","docAbstract":"<p>This geochemical map shows the distribution and abundance of zinc in -80 mesh (177 micrometers) stream sediment samples in the Chandalar quadrangle, Alaska. The map is a part of a series of geochemical maps that together with the background information circular (Reiser and others, 1978) comprise the folio on the Chandalar quadrangle, Alaska. The data are plotted on a subdued base map showing the generalized geology, topography, and sample localities. Map symbols show the metal values that are considered anomalous; these symbols are defined on the accompanying histograms. An explanation of sampling, preparation, analytical procedures and the geochemical raw data for all samples are presented by O'Leary and others (1976). The -80 mesh (177 micrometers) stream sediment medium was used in this study because of the regional setting in the north-central Brooks Range. Given the rather restrictive time and manpower constraints the -80 mesh (177 micrometers) stream sediment combined with panned concentrates was determined to be the most economical and adequate medium in this case where clastic sediments are being derived from local bedrock.&nbsp;</p><p>The study area is generally one of high relief with short fast-moving streams and broad glacial valleys. All samples were taken from active streams, as close to the center channel as possible. All sediments were considered to be locally derived. Care was taken, when sampling an obviously glaciated terrane, to sample above or upstream from morainal material, wherever possible. Most samples were taken in areas where bedrock was within 30 m of the sample site.</p><p>Due to poor sensitivity for zinc by spectrographic analysis (200 ppm) all zinc analyses were done by atomic absorption.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf878E","usgsCitation":"Marsh, S., Detra, D., and Smith, S., 1978, Geochemical and generalized geologic map showing distribution and abundance of zinc in stream sediments in the Chandalar Quadrangle, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 878, 1 Plate: 46.03 x 26.23 inches, https://doi.org/10.3133/mf878E.","productDescription":"1 Plate: 46.03 x 26.23 inches","costCenters":[],"links":[{"id":182511,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0878-E/report-thumb.jpg"},{"id":417266,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0878-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Chandalar Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,67 ], [ -150,68 ], [ -147,68 ], [ -147,67 ], [ -150,67 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae804","contributors":{"authors":[{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":263335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detra, D.E.","contributorId":72358,"corporation":false,"usgs":true,"family":"Detra","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":263336,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":263334,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56461,"text":"wdrCA773 - 1978 - Water resources data for California, water year 1977; Volume 3: Southern Central Valley basins and the Great Basin from Walker River to Truckee River","interactions":[],"lastModifiedDate":"2012-06-13T01:01:47","indexId":"wdrCA773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-77-3","title":"Water resources data for California, water year 1977; Volume 3: Southern Central Valley basins and the Great Basin from Walker River to Truckee River","docAbstract":"Water-resources data for the 1977 water year for California consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; records of water levels in selected observation wells; and selected chemical analyses of ground water. Records for a few pertinent streamflow and water-quality stations in bordering States are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Winchell Smith, Assistant District Chief for Hydrologic Data and Leonard N. Jorgensen, Chief of the Basic-Data Section. These data, a contribution to the National Water Data System, were collected by the Geological Survey and cooperating local, State, and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA773","usgsCitation":"California District of the Water Resources Division, 1978, Water resources data for California, water year 1977; Volume 3: Southern Central Valley basins and the Great Basin from Walker River to Truckee River: U.S. Geological Survey Water Data Report CA-77-3, 396 p., https://doi.org/10.3133/wdrCA773.","productDescription":"396 p.","costCenters":[],"links":[{"id":185353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_77_3.jpg"},{"id":257455,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/ca-77/WDR-1977-vol3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634c31","contributors":{"authors":[{"text":"California District of the Water Resources Division","contributorId":127979,"corporation":true,"usgs":false,"organization":"California District of the Water Resources Division","id":532642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56457,"text":"wdrMO771 - 1978 - Water resources data for Missouri, water year 1977","interactions":[],"lastModifiedDate":"2025-08-19T13:32:36.654758","indexId":"wdrMO771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MO-77-1","title":"Water resources data for Missouri, water year 1977","docAbstract":"<p>Water resources data for the 1977 water year for Missouri consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water quality of ground water. This report contains discharge records for 122 gaging stations; stage records for 3 of these gaging stations; contents for 6 lakes and reservoirs; and water quality for 21 gaging stations, 11 partial record stations, 1 lake and 3 wells. Also included are data for 99 crest-stage partial record stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Missouri.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMO771","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Missouri, water year 1977: U.S. Geological Survey Water Data Report MO-77-1, viii, 277 p., https://doi.org/10.3133/wdrMO771.","productDescription":"viii, 277 p.","costCenters":[],"links":[{"id":494290,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/mo-77-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185349,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1977/mo-77-1/report-thumb.jpg"}],"country":"United 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,{"id":56456,"text":"wdrWV771 - 1978 - Water resources data for West Virginia, water year 1977","interactions":[],"lastModifiedDate":"2025-02-24T16:00:04.210111","indexId":"wdrWV771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-77-1","title":"Water resources data for West Virginia, water year 1977","docAbstract":"<p>Water resources data for the 1977 water year for West Virginia consist of records of stage, discharge, and water quality of streams and springs; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 129 gaging stations; stage only records for 2 gaging stations; stage and contents for 7 lakes and reservoirs; contents for 1 reservoir; water quality for 43 gaging stations; and water levels for 36 observation wells. Also included are 35 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data collections program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV771","collaboration":"Prepared in cooperation with the State of West Virginia and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for West Virginia, water year 1977: U.S. Geological Survey Water Data Report WV-77-1, viii, 289 p., https://doi.org/10.3133/wdrWV771.","productDescription":"viii, 289 p.","costCenters":[],"links":[{"id":482382,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/wv-77-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185348,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1977/wv-77-1/report-thumb.jpg"}],"country":"United States","state":"West 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,{"id":8527,"text":"ofr781038 - 1978 - Hydrologic data for the Antlers aquifer, southeastern Oklahoma","interactions":[{"subject":{"id":8527,"text":"ofr781038 - 1978 - Hydrologic data for the Antlers aquifer, southeastern Oklahoma","indexId":"ofr781038","publicationYear":"1978","noYear":false,"title":"Hydrologic data for the Antlers aquifer, southeastern Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":70046131,"text":"70046131 - 1981 - Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma","indexId":"70046131","publicationYear":"1981","noYear":false,"title":"Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma"},"id":1}],"supersededBy":{"id":70046131,"text":"70046131 - 1981 - Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma","indexId":"70046131","publicationYear":"1981","noYear":false,"title":"Geohydrology of the Antlers aquifer (Cretaceous), southeastern Oklahoma"},"lastModifiedDate":"2017-09-29T15:46:37","indexId":"ofr781038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1038","title":"Hydrologic data for the Antlers aquifer, southeastern Oklahoma","docAbstract":"<p>The U.S. Geological Survey has collected data on Oklahoma's ground-water resources since 1934. Most of these data were collected as part of specific ground-water studies conducted in cooperation with various Federal, State, and local agencies.</p><p>The information in this report was obtained in the field, from published reports (Davis, 1960, Hart, 1974, Havens and Bergman, 1976), and from unpublished files of the U.S. Geological Survey.</p><p>The stratigraphic nomenclature is that of the Oklahoma Geological Survey and does not necessarily agree with that of the U.S. Geological Survey.</p><p>Acknowledgement is extended to the many individuals who have provided the data included in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781038","usgsCitation":"Davis, R.E., and Hart, D.L., 1978, Hydrologic data for the Antlers aquifer, southeastern Oklahoma: U.S. Geological Survey Open-File Report 78-1038, iii, 24 p., https://doi.org/10.3133/ofr781038.","productDescription":"iii, 24 p.","numberOfPages":"31","costCenters":[],"links":[{"id":142799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1038/report-thumb.jpg"},{"id":346262,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oklahoma","otherGeospatial":"Antlers Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.5640869140625,\n              33.637489243170826\n            ],\n            [\n              -94.4659423828125,\n              33.637489243170826\n            ],\n            [\n              -94.4659423828125,\n              34.415973384481866\n            ],\n            [\n              -97.5640869140625,\n              34.415973384481866\n            ],\n            [\n              -97.5640869140625,\n              33.637489243170826\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb0a","contributors":{"authors":[{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, Donald L. Jr.","contributorId":89946,"corporation":false,"usgs":true,"family":"Hart","given":"Donald","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6306,"text":"pp1055 - 1978 - Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming","interactions":[{"subject":{"id":10654,"text":"ofr77140 - 1977 - Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming","indexId":"ofr77140","publicationYear":"1977","noYear":false,"title":"Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":6306,"text":"pp1055 - 1978 - Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming","indexId":"pp1055","publicationYear":"1978","noYear":false,"title":"Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming"},"id":1}],"lastModifiedDate":"2019-06-11T15:04:49","indexId":"pp1055","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1055","title":"Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming","docAbstract":"<p>The Precambrian of the western part of the Granite Mountains, Wyoming, contains a metamorphic complex of gneisses, schists, and amphibolites that were derived through amphibolite-grade metamorphism from a sedimentary-volcanic sequence perhaps similar to that exposed in the southeastern Wind River Mountains. Whole-rock Rb-Sr dating places the time of metamorphism at 2,860?80 million years. A high initial 87Sr/ 86 S r ratio of 0.7048 suggests that either the protoliths or the source terrane of the sedimentary component is several hundred million years older than the time of metamorphism. Following an interval of 300:t100 million years for which the geologic record is lacking or still undeciphered, the metamorphic complex was intruded by a batholith and satellite bodies of medium- to coarse-grained, generally massive biotite granite and related pegmatite and aplite. The main body of granite is dated at 2,550?60 million years by the Rb-Sr method. Limited data suggest that diabase dikes were emplaced and nephrite veins were formed only shortly after intrusion of the granite. Emplacement of the granite at about 2,550 million years ago appears to be related to a major period of regional granitic plutonism in the Precambrian of southern and western Wyoming. Granites, in the strict sense, that are dated between 2,450 and 2,600 million years occur in the Teton Range, the Sierra Madre, the Medicine Bow Mountains and the Laramie Range. This episode of granitic plutonism occurred some 50 to 100 million years later than the major tonalitic to granitic plutonism in the Superior province of northern Minnesota and adjacent Ontario-the nearest exposed Precambrian W terrane that is analogous to the Wyoming province. Initial 87Sr / 86Sr ratios of some of the Wyoming granites are higher than expected if the rocks had been derived from juvenile magmas and it is likely that older crustal rocks were involved to some degree in the generation of these granites. Slightly to highly disturbed Rb-Sr and K-Ar mineral ages are obtained on rocks of the metamorphic complex and on the granite. These ages range from about 2,400 to 1,420 million years and are part of a regional pattern of lowered mineral ages of Precambrian W rocks of southern Wyoming. A major discontinuity in these mineral ages occurs along a line extending from the northern Laramie Range, through the northern part of the Granite Mountains, to the southeastern Wind River Mountains. North of this line, Rb-Sr and K-Ar biotite ages are 2,300 million years or greater, whereas to the south, the biotite ages decrease drastically over a short distance, to a common range of 1,600-1,400 million years. We suggest that these lowered ages represent regional cooling below the 300 0 C isotherm as a consequence of uplift and erosion of the large crustal block occurring south of the age discontinuity. In this interpretation, the westerly-trending age discontinuity would be a zone of major crustal dislocation that resulted from vertical tectonics in late Precambrian X or early Precambrian Y time.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1055","usgsCitation":"Peterman, Z., and Hildreth, R.A., 1978, Reconnaissance geology and geochronology of the Precambrian of the Granite Mountains, Wyoming: U.S. Geological Survey Professional Paper 1055, 22 p., https://doi.org/10.3133/pp1055.","productDescription":"22 p.","costCenters":[],"links":[{"id":33594,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1055/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1055/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db64102e","contributors":{"authors":[{"text":"Peterman, Zell E. 0000-0002-5694-8082 peterman@usgs.gov","orcid":"https://orcid.org/0000-0002-5694-8082","contributorId":620,"corporation":false,"usgs":true,"family":"Peterman","given":"Zell E.","email":"peterman@usgs.gov","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":152480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildreth, Robert A.","contributorId":28234,"corporation":false,"usgs":true,"family":"Hildreth","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":152481,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9623,"text":"ofr78161 - 1978 - High-flow frequencies for selected streams in Oklahoma","interactions":[],"lastModifiedDate":"2017-09-29T07:46:28","indexId":"ofr78161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-161","title":"High-flow frequencies for selected streams in Oklahoma","docAbstract":"Streamflow records are analyzed statistically to determine high-flow characteristics of selected streams in Oklahoma. Tables are included which show the 2-, 5-, 10-, 25-, 50-, and 100-year high-flow frequencies for durations of 1, 3, 7, 30, 90, and 365 days. The log-Pearson Type III frequency distribution was used in the computations. Streamflow records used include data extending from 1903 to 1974.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78161","usgsCitation":"Huntzinger, T.L., 1978, High-flow frequencies for selected streams in Oklahoma: U.S. Geological Survey Open-File Report 78-161, iii, 30 p., https://doi.org/10.3133/ofr78161.","productDescription":"iii, 30 p.","numberOfPages":"40","costCenters":[],"links":[{"id":141761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0161/report-thumb.jpg"},{"id":346187,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0161/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":6427,"text":"pp1041 - 1978 - Intrusive rocks northeast of Steamboat Springs, Park Range, Colorado","interactions":[],"lastModifiedDate":"2022-02-03T22:31:35.648377","indexId":"pp1041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1041","title":"Intrusive rocks northeast of Steamboat Springs, Park Range, Colorado","docAbstract":"<p>Major Precambrian and minor Tertiary intrusive rocks northeast of Steamboat Springs in the Park Range between 40°30' and 40°45' N. lat. are described and compared with related rocks elsewhere in Colorado and Wyoming. The Precambrian intrusives were emplaced in a sequence of high-grade interlayered felsic gneisses, amphibolites, and pelitic schists of sedimentary and volcanic origin. These rocks are cut by a major northeast-trending Precambrian shear zone where mainly left lateral movement of 1/ 2 to 1 mile is certain. Cumulative movement of many miles is possible. The Precambrian intrusives consist of a batholith, the Mount Ethel pluton, a smaller Buffalo Pass pluton, and small dikes or lenses of fine-grained porphyry, pegmatites, and ultramafics. </p><p>The Mount Ethel pluton is an oval shaped body 7 miles wide by about 40 miles long (shown by geophysical data to extend beneath younger sediments in North Park). Outer batholithic contacts are sharp and dip steeply outward at about 85°. Five mappable internal variants consist, in order of decreasing age, of granodiorite, quartz monzonite porphyry of Rocky Peak, quartz monzonite of Roxy Ann Lake, granite and quartz monzonite, and. leucogranite. Internal contacts between these plutonic variants are sharp, and evidence of liquid-solid relationships abounds; despite this, all rocks except the granodiorite contribute to an Rb-Sr whole-rock isochron indicating emplacement about 1.4 b.y. (billion years) ago. The most important variants volumetrically are: the quartz monzonite porphyry of Rocky Peak, which forms an irregular 2-mile-thick carapace or mapped band around the west edge of the pluton and is lithologically similar to nearby Sherman Granite, and the quartz monzonite of Roxy Ann Lake, which forms most of the rest of the pluton and is lithologically similar to Silver Plume Granite. An apparent Sherman -Silver Plume dichotomy with similar rock types and similar relative ages is noted throughout Colorado plutons of that age. </p><p>The Buffalo Pass pluton consists of the quartz monzonite and gra- nodiorite augen gneiss of Buffalo Mountain and equigranular quartz monzonite gneiss. Internal contacts are not exposed. These rocks contribute to an Rb-Sr whole-rock isochron indicating syntectonic emplacement 1.7-1.8 b.y. ago, essentially the same as the metamorphism of the felsic gneiss wallrocks in the area of this report, and of rocks of Boulder Creek age elsewhere in Colorado. </p><p>The fine-grained porphyry dikes cut the Buffalo Pass pluton, the ultramafics, and some pegmatites. The dikes are within the age range of the Mount Ethel pluton and are older than the mylonite and shear zones. They occur in both an older northwest-trending and a somewhat younger northeast-trending set but do not appear to change compositionally from one set to the other. Regional considerations indicate that they were emplaced between about 1.1 and 1.5 b.y. ago, a time when intermediate to mafic dikes were commonly emplaced throughout Colorado, Wyoming, and southwestern Montana. The pegmatite and ultramafic bodies are not dated directly, but clustering of many pegmatites outside the contacts of the Mount Ethel pluton may indicate a genetic relation of the pegmatites to the Mount Ethel rocks.</p><p> Fluorite is a common accessory mineral in the rocks of the Mount Ethel pluton; it has not been observed in this area in the petrographically similar rocks of the Buffalo Pass pluton. Fluorite was precipitated most abundantly from the Precambrian magma that formed the quartz monzonite of Roxy Ann Lake. In 70 percent of these rocks fluorite is observed in amounts as great as 2 percent and is successively less abundant in both older and younger plutonic phases. Textural evidence indicates that, although most fluorite is intergrown with and contemporaneous with other magmatic minerals, some fluorite is associated with alteration minerals in a manner demonstrating its mobility since its initial deposition.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1041","usgsCitation":"Snyder, G.L., and Hedge, C.E., 1978, Intrusive rocks northeast of Steamboat Springs, Park Range, Colorado: U.S. Geological Survey Professional Paper 1041, Report: iii, 42 p.; 1 Plate: 37.00 × 34.00 inches, https://doi.org/10.3133/pp1041.","productDescription":"Report: iii, 42 p.; 1 Plate: 37.00 × 34.00 inches","costCenters":[],"links":[{"id":395421,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4693.htm"},{"id":33837,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1041/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33836,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1041/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Steamboat Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.9333,\n              40.5\n            ],\n            [\n              -106.575,\n              40.5\n            ],\n            [\n              -106.575,\n              40.75\n            ],\n            [\n              -106.9333,\n              40.75\n            ],\n            [\n              -106.9333,\n              40.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bee4b07f02db5d1213","contributors":{"authors":[{"text":"Snyder, George L.","contributorId":6843,"corporation":false,"usgs":true,"family":"Snyder","given":"George","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, Carl E.","contributorId":76299,"corporation":false,"usgs":true,"family":"Hedge","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":152705,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6431,"text":"pp1044A - 1978 - The hydrothermal system of Long Valley Caldera, California","interactions":[{"subject":{"id":11262,"text":"ofr77347 - 1977 - The hydrothermal system of Long Valley Caldera, California","indexId":"ofr77347","publicationYear":"1977","noYear":false,"title":"The hydrothermal system of Long Valley Caldera, California"},"predicate":"SUPERSEDED_BY","object":{"id":6431,"text":"pp1044A - 1978 - The hydrothermal system of Long Valley Caldera, California","indexId":"pp1044A","publicationYear":"1978","noYear":false,"chapter":"A","title":"The hydrothermal system of Long Valley Caldera, California"},"id":1}],"lastModifiedDate":"2025-04-17T16:29:27.483672","indexId":"pp1044A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"A","title":"The hydrothermal system of Long Valley Caldera, California","docAbstract":"Long Valley caldera, an elliptical depression covering 450 km 2 on the eastern front of the Sierra Nevada in east-central California, contains a hot-water convection system with numerous hot springs and measured and estimated aquifer temperatures at depths of 180?C to 280?C. In this study we have synthesized the results of previous geologic, geophysical, geochemical, and hydrologic investigations of the Long Valley area to develop a generalized conceptual and mathematical model which describes the gross features of heat and fluid flow in the hydrothermal system. \r\n\r\nCenozoic volcanism in the Long Valley region began about 3.2 m.y. (million years) ago and has continued intermittently until the present time. The major event that resulted in the formation of the Long Valley caldera took place about 0.7 m.y. ago with the eruption of 600 km 3 or more of Bishop Tuff of Pleistocene age, a rhyolitic ash flow, and subsequent collapse of the roof of the magma chamber along one or more steeply inclined ring fractures. Subsequent intracaldera volcanism and uplift of the west-central part of the caldera floor formed a subcircular resurgent dome about 10 km in diameter surrounded by a moat containing rhyolitic, rhyodacitic, and basaltic rocks ranging in age from 0.5 to 0.05 m.y. \r\n\r\nOn the basis of gravity and seismic studies, we estimate an aver- age thickness of fill of 2.4 km above the precaldera granitic and metamorphic basement rocks. A continuous layer of densely welded Bishop Tuff overlies the basement rocks, with an average thickness of 1.4 km; the fill above the welded Bishop Tuff consists of intercalated volcanic flows and tuffs and fluvial and lacustrine deposits. Assuming the average grain density of the fill is between 2.45 and 2.65 g/cm 3 , we calculate the average bulk porosity of the total fill as from 0.11 to 0.21. Comparison of published values of porosity of the welded Bishop Tuff exposed southeast of the caldera with calculated values indicates average bulk porosity for the welded tuff (including fracture porosity) from 0.05 to 0.10. Because of its continuity and depth and the likelihood of significant fracture permeability in the more competent rocks such as the welded tuff, our model of the hydrothermal system assumes that the Bishop Tuff provides the principal hot-water reservoir. However, because very little direct information exists from drill holes below 300 m, this assumption must be considered tentative. \r\n\r\nLong Valley caldera is drained by the Owens River and several tributaries which flow into Lake Crowley in the southeast end of the caldera. Streamflow and springflow measurements for water years 1964-74 indicate a total inflow to Lake Crowley of about 10,900 L/s. In contrast, the total discharge of hot water from the hydrothermal reservoir is about 300 L/s. For modeling purposes, the ground-water system is considered as comprising a shallow subsystem in the fill above the densely welded Bishop Tuff containing relatively cold ground water, and a deep subsystem or hydrothermal reservoir in the welded tuff containing relatively hot ground water. Hydrologic, isotopic, and thermal data indicate that recharge to the hydrothermal reservoir occurs in the upper Owens River drainage basin along the western periphery of the caldera. Temperature profiles in a 2.11- km-deep test well drilled by private industry in the southeastern part of the caldera suggest that an additional flux of relatively cool ground water recharges the deep subsystem around the northeast rim. Flow in the shallow ground-water subsystem is neglected in the model except in recharge areas and along Hot Creek gorge, where approximately 80 percent of the hot-water discharge from the hydrothermal reservoir moves upward along faults toward springs in the gorge. \r\n\r\nHeat-flow data from the Long Valley region indicate that the resurgent dome overlies a residual magma chamber more circular in plan than the original magma chamber that supplied the Bishop Tuff","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044A","usgsCitation":"Sorey, M., Lewis, R.E., and Olmsted, F.H., 1978, The hydrothermal system of Long Valley Caldera, California: U.S. Geological Survey Professional Paper 1044, Report: 60 p.; 1 Plate: 34.00 x 25.00 inches, https://doi.org/10.3133/pp1044A.","productDescription":"Report: 60 p.; 1 Plate: 34.00 x 25.00 inches","costCenters":[],"links":[{"id":33842,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104540,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4695.htm","linkFileType":{"id":5,"text":"html"},"description":"4695"},{"id":33841,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117933,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044a/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley Caldera","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.0969,\n              37.7778\n            ],\n            [\n              -119.0969,\n              37.5\n            ],\n            [\n              -118.635,\n              37.5\n            ],\n            [\n              -118.635,\n              37.7778\n            ],\n            [\n              -119.0969,\n              37.7778\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64da25","contributors":{"authors":[{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":152712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Robert Edward","contributorId":73595,"corporation":false,"usgs":true,"family":"Lewis","given":"Robert","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":152713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152711,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9643,"text":"ofr78298 - 1978 - Principal facts for gravity observations in the Coso Hot Springs area, California","interactions":[],"lastModifiedDate":"2022-09-30T22:54:46.549927","indexId":"ofr78298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-298","title":"Principal facts for gravity observations in the Coso Hot Springs area, California","docAbstract":"<p>Gravity observations were made at 292 locations in the Coso Hot Springs area, California (figs. 1 and 2). The field work was completed during June 1976 by William F. Isherwood and Jerry H. Hassemer using LaCoste-Romberg Gravity Meters G-131 and G-159. The purpose of the gravity survey is to provide background geophysical data to evaluate the geothermal potential of the area. The present survey fills in gaps of coverage on previous gravity maps of the region (Nilsen and Chapman, 1971, and Chapman and others, 1971).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78298","usgsCitation":"Isherwood, W., and Plouff, D., 1978, Principal facts for gravity observations in the Coso Hot Springs area, California: U.S. Geological Survey Open-File Report 78-298, 14 p., https://doi.org/10.3133/ofr78298.","productDescription":"14 p.","costCenters":[],"links":[{"id":407753,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0298/Report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0298/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Coso Hot Springs area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.73223876953124,\n              35.666501265360395\n            ],\n            [\n              -117.6697540283203,\n              35.666501265360395\n            ],\n            [\n              -117.6697540283203,\n              35.72421761691415\n            ],\n            [\n              -117.73223876953124,\n              35.72421761691415\n            ],\n            [\n              -117.73223876953124,\n              35.666501265360395\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668122","contributors":{"authors":[{"text":"Isherwood, William F.","contributorId":71547,"corporation":false,"usgs":true,"family":"Isherwood","given":"William F.","affiliations":[],"preferred":false,"id":160040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":160041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6510,"text":"pp1003 - 1978 - Effects of urbanization on streamflow and sediment transport in the Rock Creek and Anacostia River basins, Montgomery County, Maryland, 1962-74","interactions":[{"subject":{"id":48093,"text":"ofr72455 - 1972 - Sediment yields of urban construction sources, Montgomery County, Maryland; a progress report, Rock Creek-Anacostia River Basins","indexId":"ofr72455","publicationYear":"1972","noYear":false,"title":"Sediment yields of urban construction sources, Montgomery County, Maryland; a progress report, Rock Creek-Anacostia River Basins"},"predicate":"SUPERSEDED_BY","object":{"id":6510,"text":"pp1003 - 1978 - Effects of urbanization on streamflow and sediment transport in the Rock Creek and Anacostia River basins, Montgomery County, Maryland, 1962-74","indexId":"pp1003","publicationYear":"1978","noYear":false,"title":"Effects of urbanization on streamflow and sediment transport in the Rock Creek and Anacostia River basins, Montgomery County, Maryland, 1962-74"},"id":1}],"lastModifiedDate":"2022-08-22T19:53:51.871944","indexId":"pp1003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1003","title":"Effects of urbanization on streamflow and sediment transport in the Rock Creek and Anacostia River basins, Montgomery County, Maryland, 1962-74","docAbstract":"<p>Land use, precipitation, streamflow, and sediment discharge data were collected from nine small drainage basins in Montgomery County, Maryland, to evaluate runoff and sediment response to sediment-control practices in areas undergoing urban development. Drainage basins ranged in size from 0.35 to 21.1 sq mi and land use ranged from rural to 60 percent urban. Urbanization did not affect low and medium flows, but it did result in increased storm runoff and peak flows. Suspended sediment transported from one of the basins that underwent urban development, the 21.1 sq mi Anacostia River basin, averaged 15 ,400 tons/yr between 1962 and 1974. Bedload was estimated as 5 to 11 percent of the total load. Cropland, urban land, and construction sites were the major sources of sediment. Average annual sediment yields ranged from 065 to 4.3 tons/acre for cropland, 3.7 tons/acre for urban land, and 7 to 100 tons/acre for urban construction sites. The magnitude of the yields from construction sites was significantly affected by (1) the slope of the sites, (2) the proximity of stream channels, (3) buffer zones of natural vegetation, and (4) sediment-control measures. Sediment controls, particularly those enforced under a 1971 sediment-control ordinance, apparently decreased construction-site sediment yields by 60 to 80 percent.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1003","usgsCitation":"Yorke, T.H., and Herb, W.J., 1978, Effects of urbanization on streamflow and sediment transport in the Rock Creek and Anacostia River basins, Montgomery County, Maryland, 1962-74: U.S. Geological Survey Professional Paper 1003, Report: vi, 71 p.; 3 Plates: 21.50 × 31.00 inches, https://doi.org/10.3133/pp1003.","productDescription":"Report: vi, 71 p.; 3 Plates: 21.50 × 31.00 inches","costCenters":[],"links":[{"id":405401,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4672.htm"},{"id":33975,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1003/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33974,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1003/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33973,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1003/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33972,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1003/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1003/report-thumb.jpg"}],"country":"United States","state":"Maryland","county":"Montgomery County","otherGeospatial":"Rock Creek and Anacostia River basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.1208,\n              39.0594\n            ],\n            [\n              -76.9833,\n              39.0594\n            ],\n            [\n              -76.9833,\n              39.1872\n            ],\n            [\n              -77.1208,\n              39.1872\n            ],\n            [\n              -77.1208,\n              39.0594\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c82a","contributors":{"authors":[{"text":"Yorke, Thomas H.","contributorId":83109,"corporation":false,"usgs":true,"family":"Yorke","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":152844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":152843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6512,"text":"pp993 - 1978 - Historic ground failures in Northern California triggered by earthquakes","interactions":[],"lastModifiedDate":"2021-02-26T16:11:31.116168","indexId":"pp993","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"993","title":"Historic ground failures in Northern California triggered by earthquakes","docAbstract":"A major source of earthquake-related damage and casualties in northern California has been ground failures generated by the seismic shaking, including landslides, lateral spreads, ground settlement, and surface cracks. The historical record shows that, except for offshore shocks, the geographic area affected and the quantity and general severity of ground failures increase markedly with Richter magnitude. Hence, the largest historical event, the 1906 San Francisco earthquake, has been the most important generator of ground failures. Because of recent population growth and land development in northern California, the potential for damage in future events is enormous compared with that existing in 1906.\r\n\r\nReports of the 1906 San Francisco earthquake and other northern California earthquakes and descriptions of ground failures therein are used to (1) identify and clarify the types of ground failures associated with earthquakes, (2) provide a guide for engineers, planners, and others responsible for minimizing seismic hazards, and (3) form a data base for other geotechnical studies of earthquake-triggered pound failures.\r\n\r\nGeologic, hydrologic, and topographic setting have an important influence on ground failure development as well as distance from the causative fault. Areas especially vulnerable to ground failure in northern California have been oversteepened slopes, such as mountain cliffs, streambanks, and coastal bluffs, and lowland deposits, principally Holocene fluvial deposits, deltaic deposits, and poorly compacted fills. Liquefaction has been the direct cause of most lowland failures. The historical record suggests that ground failures during future large earthquakes are most likely to occur at the same or geologically similar locations as failures during previous earhquakes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp993","usgsCitation":"Youd, T.L., and Hoose, S.N., 1978, Historic ground failures in Northern California triggered by earthquakes: U.S. Geological Survey Professional Paper 993, Report: iv, 177 p.; 5 Plates: 34.00 x 21.00 inches and smaller; 2 Photographs folders, https://doi.org/10.3133/pp993.","productDescription":"Report: iv, 177 p.; 5 Plates: 34.00 x 21.00 inches and smaller; 2 Photographs folders","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":650,"text":"Western Earthquake Hazards Team","active":false,"usgs":true}],"links":[{"id":123718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_993.jpg"},{"id":9879,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/","linkFileType":{"id":5,"text":"html"}},{"id":383646,"rank":10,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/photographs/web-resolution","text":"Web-resolution Photographs folder","linkFileType":{"id":5,"text":"html"}},{"id":383645,"rank":9,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/photographs/print-resolution","text":"Print-resolution Photographs folder","linkFileType":{"id":5,"text":"html"}},{"id":383644,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383639,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383640,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383641,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383642,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383643,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1978/pp0993/pp993_plate4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,35 ], [ -124,41 ], [ -119,41 ], [ -119,35 ], [ -124,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68864d","contributors":{"authors":[{"text":"Youd, T. Leslie","contributorId":107678,"corporation":false,"usgs":true,"family":"Youd","given":"T.","email":"","middleInitial":"Leslie","affiliations":[],"preferred":false,"id":152848,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoose, Seena N.","contributorId":95870,"corporation":false,"usgs":true,"family":"Hoose","given":"Seena","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":152847,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6515,"text":"pp1051 - 1978 - Field determination of vertical permeability to air in the unsaturated zone","interactions":[{"subject":{"id":11605,"text":"ofr77346 - 1977 - Field determination of vertical permeability to air in the unsaturated zone","indexId":"ofr77346","publicationYear":"1977","noYear":false,"title":"Field determination of vertical permeability to air in the unsaturated zone"},"predicate":"SUPERSEDED_BY","object":{"id":6515,"text":"pp1051 - 1978 - Field determination of vertical permeability to air in the unsaturated zone","indexId":"pp1051","publicationYear":"1978","noYear":false,"title":"Field determination of vertical permeability to air in the unsaturated zone"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1051","title":"Field determination of vertical permeability to air in the unsaturated zone","docAbstract":"The vertical permeability to air of layered materials in the unsaturated zone may be determined from air pressure data obtained at depth during a period when air pressure is changing at land surface. Such data may be obtained by monitoring barometric pressure with a microbarograph or surveying altimeter and simultaneously measuring down-hole pneumatic head differences in specially constructed piezometers. These data, coupled with air-filled porosity data from other sources, may be compared with the results of electric-analog or numerical solution of the one-dimensional diffusion equation to make a trial-and-error determination of the air permeability for each layer. The permeabilities to air may in turn be converted to equivalent hydraulic conductivity values if the materials are well drained, are permeable enough that the Klinkenberg effect is small, and are structurally unaffected by wetting. The method offers potential advantages over present methods to evaluate sites for artificial recharge by spreading; to evaluate ground-water pollution hazards from feedlots, sanitary landfills , and land irrigated with sewage effluent; and to evaluate sites for temporary storage of gas in the unsaturated zone. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1051","usgsCitation":"Weeks, E.P., 1978, Field determination of vertical permeability to air in the unsaturated zone: U.S. Geological Survey Professional Paper 1051, 41 p., https://doi.org/10.3133/pp1051.","productDescription":"41 p.","costCenters":[],"links":[{"id":123710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1051/report-thumb.jpg"},{"id":33981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1051/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5735","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":152852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6527,"text":"pp1029 - 1978 - Hydraulic geometry of river cross sections; theory of minimum variance","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp1029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1029","title":"Hydraulic geometry of river cross sections; theory of minimum variance","docAbstract":"This study deals with the rates at which mean velocity, mean depth, and water-surface width increase with water discharge at a cross section on an alluvial stream. Such relations often follow power laws, the exponents in which are called hydraulic exponents. The Langbein (1964) minimum-variance theory is examined in regard to its validity and its ability to predict observed hydraulic exponents. The variables used with the theory were velocity, depth, width, bed shear stress, friction factor, slope (energy gradient), and stream power. Slope is often constant, in which case only velocity, depth, width, shear and friction factor need be considered. The theory was tested against a wide range of field data from various geographic areas of the United States. The original theory was intended to produce only the average hydraulic exponents for a group of cross sections in a similar type of geologic or hydraulic environment. The theory does predict these average exponents with a reasonable degree of accuracy. An attempt to forecast the exponents at any selected cross section was moderately successful. Empirical equations are more accurate than the minimum variance, Gauckler-Manning, or Chezy methods. Predictions of the exponent of width are most reliable, the exponent of depth fair, and the exponent of mean velocity poor. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1029","usgsCitation":"Williams, G.P., 1978, Hydraulic geometry of river cross sections; theory of minimum variance: U.S. Geological Survey Professional Paper 1029, 47 p., https://doi.org/10.3133/pp1029.","productDescription":"47 p.","costCenters":[],"links":[{"id":123811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1029/report-thumb.jpg"},{"id":34006,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a22c","contributors":{"authors":[{"text":"Williams, Garnett P.","contributorId":100361,"corporation":false,"usgs":true,"family":"Williams","given":"Garnett","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":152870,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9181,"text":"ofr78807 - 1978 - Low-flow and flow duration of Tennessee streams","interactions":[{"subject":{"id":22966,"text":"ofr5833 - 1958 - Summary of flow duration and low flow at stream-gaging stations in Tennessee","indexId":"ofr5833","publicationYear":"1958","noYear":false,"title":"Summary of flow duration and low flow at stream-gaging stations in Tennessee"},"predicate":"SUPERSEDED_BY","object":{"id":9181,"text":"ofr78807 - 1978 - Low-flow and flow duration of Tennessee streams","indexId":"ofr78807","publicationYear":"1978","noYear":false,"title":"Low-flow and flow duration of Tennessee streams"},"id":1},{"subject":{"id":45982,"text":"ofr6047 - 1960 - Low-flow frequency data in Tennessee","indexId":"ofr6047","publicationYear":"1960","noYear":false,"title":"Low-flow frequency data in Tennessee"},"predicate":"SUPERSEDED_BY","object":{"id":9181,"text":"ofr78807 - 1978 - Low-flow and flow duration of Tennessee streams","indexId":"ofr78807","publicationYear":"1978","noYear":false,"title":"Low-flow and flow duration of Tennessee streams"},"id":2}],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr78807","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-807","title":"Low-flow and flow duration of Tennessee streams","docAbstract":"Low-flow frequency and duration data are presented to define variations of the low flow of Tennessee streams both in time and place. Analysis has been made of 204 continuous record stations, both regulated and unregulated and 651 partial-record stations operated either by the U.S. Geological Survey or Tennessee Valley Authority through the 1975 water year. Flow duration and frequency data have been tabulated for the continuous record sites using the digital computer and graphical methods. Frequency data only is presented for partial-record sites computed in most cases by comparing several discharge measurements at the site with concurrent daily mean flow for an appropriate gaging station. Flow duration data can be used to define a flow duration curve, with the slope at points on that curve used to establish the dependability of the stream to sustain a particular flow. Low-flow frequency data are presented to predict the probability that a specified flow or lesser flow will recur through time. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78807","usgsCitation":"Gold, R., 1978, Low-flow and flow duration of Tennessee streams: U.S. Geological Survey Open-File Report 78-807, 402 p. :ill., maps (1 fold. in pocket); 27 cm., https://doi.org/10.3133/ofr78807.","productDescription":"402 p. :ill., maps (1 fold. in pocket); 27 cm.","costCenters":[],"links":[{"id":141610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9111,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1978/ofr_78-807/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644a33","contributors":{"authors":[{"text":"Gold, Robert L.","contributorId":78324,"corporation":false,"usgs":true,"family":"Gold","given":"Robert L.","affiliations":[],"preferred":false,"id":159235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9165,"text":"ofr78721 - 1978 - Selected water-level records for Oklahoma, 1975-1977","interactions":[],"lastModifiedDate":"2023-02-23T23:58:30.364303","indexId":"ofr78721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-721","title":"Selected water-level records for Oklahoma, 1975-1977","docAbstract":"<p>A systematic program to collect water-level records in Oklahoma began in 1937. The objectives of this program are (1) to provide long-term records of water-level fluctuations in representative wells, (2) to facilitate the prediction of water-level trends and indicate future availability of ground-water supplies, and (3) to provide information for use in basic research.</p><p>Water-level data in table 1 are from wells that are measured annually, prior to the irrigation season to achieve the most natural representation of the static water level. Water-level measurements listed in the column under 1976 may have been made during December, 1975 or January, February, March, April, or May, 1976. Measurements listed in the column 1977 may have been made during December, 1976 or January, February, March, or April, 1977. Figure 1 shows the counties and number of wells therein, where data were obtained for this report.</p><p>Records of water levels in Oklahoma are collected through a cooperative program by the U.S. Geological Survey and the Oklahoma Water Resources Board. The records are tabulated and published by the U.S. Geological Survey on an annual basis.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78721","collaboration":"Prepared in cooperation with the Oklahoma Water Resources Board","usgsCitation":"Goemaat, R.L., and Spiser, D.E., 1978, Selected water-level records for Oklahoma, 1975-1977: U.S. Geological Survey Open-File Report 78-721, vi, 54 p., https://doi.org/10.3133/ofr78721.","productDescription":"vi, 54 p.","costCenters":[],"links":[{"id":142776,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0721/report-thumb.jpg"},{"id":413374,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0721/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7f1b","contributors":{"authors":[{"text":"Goemaat, Robert L.","contributorId":64256,"corporation":false,"usgs":true,"family":"Goemaat","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spiser, Dannie E.","contributorId":42214,"corporation":false,"usgs":true,"family":"Spiser","given":"Dannie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159212,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9677,"text":"ofr78179 - 1978 - A literature review of interaction of oxidized uranium species and uranium complexes with soluble organic matter","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr78179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-179","title":"A literature review of interaction of oxidized uranium species and uranium complexes with soluble organic matter","docAbstract":"Organic material is commonly found associated with uranium ores in sandstone-type deposits. This review of the literature summarizes the classes and separations of naturally occurring organic material but the emphasis is on soluble organic species. The main class of materials of interest is humic substances which are high-molecular-weight complex molecules that are soluble in alkaline solution. These humic substances are able to solubilize (make soluble) minerals and also to complex [by ion exchange and (or) chelation] many cations. The natural process of soil formation results in both mineral decomposition and element complexing by organic species. Uranium in solution, such as ground water, can form many species with other elements or complexes present depending on Eh and pH. In natural systems (oxidizing Eh, pH 5-9) the uranium is usually present as a complex with hydroxide or carbonate. Thermodynamic data for these species are presented. \r\n\r\nInteracting metals and organic materials have been observed in nature and studied in the laboratory by many workers in diverse scientific disciplines. The results are not easily compared. Measurements of the degree of complexation are reported as equilibrium stability constant determinations. This type of research has been done for Mn, Fe, Cu, Zn, Pb, Ni, Co, Mg, Ca, Al, and to a limited degree for U. The use of Conditional Stability Constants has given quantitative results in some cases. The methods utilized in experiments and calculations are reviewed.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78179","usgsCitation":"Jennings, J.K., and Leventhal, J., 1978, A literature review of interaction of oxidized uranium species and uranium complexes with soluble organic matter: U.S. Geological Survey Open-File Report 78-179, 48 leaves :ill. ;28 cm.; (21 p. - PGS), https://doi.org/10.3133/ofr78179.","productDescription":"48 leaves :ill. ;28 cm.; (21 p. - PGS)","costCenters":[],"links":[{"id":140943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0179/report-thumb.jpg"},{"id":37402,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0179/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae189","contributors":{"authors":[{"text":"Jennings, Joan K.","contributorId":53378,"corporation":false,"usgs":true,"family":"Jennings","given":"Joan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":160109,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leventhal, J.S.","contributorId":60640,"corporation":false,"usgs":true,"family":"Leventhal","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":160110,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9151,"text":"ofr78680 - 1978 - Sediment sources and Holocene sedimentation history in Tillamook Bay, Oregon; data and preliminary interpretations","interactions":[],"lastModifiedDate":"2016-07-08T08:57:53","indexId":"ofr78680","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-680","title":"Sediment sources and Holocene sedimentation history in Tillamook Bay, Oregon; data and preliminary interpretations","docAbstract":"<p>Surface and core sediments from Tillamook Bay, Oregon, have been&nbsp;analyzed to determine modern and Holocene sediment sources and sedimentation&nbsp;history. Heavy mineral analyses established three sediment sources: (1) the&nbsp;five major rivers draining the volcanic and associated sedimentary rocks of&nbsp;the Coast Range, (2) small streams draining the sedimentary uplands that&nbsp;form the shoreline adjacent to Tillamook Bay and erosion of the shoreline&nbsp;by waves and currents, and (3) marine sediments carried to Tillamook&nbsp;Bay by longshore drift from drainage basins north or south of the bay.&nbsp;Stratigraphic and radiocarbon analyses show that the Holocene fill in&nbsp;Tillamook Bay began to accumulate sometime before about 9,000 years ago&nbsp;in deep parts of prefill river valleys. The rate of accumulation&nbsp;generally coincided with the rate of world-wide sea-level rise--faster<br />(greater than about 3 meters per 1,000 years) up to about 7,000 years&nbsp;ago and slower (less than about 2 meters per 1,000 years) since that&nbsp;time. The vertical rate of accumulation at one core site seems to have&nbsp;been about the same from 3,300 years B.P. (before present) to the&nbsp;present, as it was from about 5,200 years B.P. to 3,300.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr78680","usgsCitation":"Glenn, J.L., 1978, Sediment sources and Holocene sedimentation history in Tillamook Bay, Oregon; data and preliminary interpretations: U.S. Geological Survey Open-File Report 78-680, Report: iv, 64 p.; Figure: 18.05 x 22.52 inches, https://doi.org/10.3133/ofr78680.","productDescription":"Report: iv, 64 p.; Figure: 18.05 x 22.52 inches","numberOfPages":"74","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":142945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78680.jpg"},{"id":324857,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0680/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":324856,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0680/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Tillamook Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.98311614990234,\n              45.46326106069966\n            ],\n            [\n              -123.98311614990234,\n              45.57463894211682\n            ],\n            [\n              -123.85746002197266,\n              45.57463894211682\n            ],\n            [\n              -123.85746002197266,\n              45.46326106069966\n            ],\n            [\n              -123.98311614990234,\n              45.46326106069966\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbf79","contributors":{"authors":[{"text":"Glenn, Jerry L.","contributorId":54969,"corporation":false,"usgs":true,"family":"Glenn","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9697,"text":"ofr78809 - 1978 - Local magnetic field measurements, fault creep observations and local earthquakes on the San Andreas fault","interactions":[],"lastModifiedDate":"2024-02-02T20:59:03.645158","indexId":"ofr78809","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-809","title":"Local magnetic field measurements, fault creep observations and local earthquakes on the San Andreas fault","docAbstract":"<p>Simultaneous records of local variations in magnetic field, fault creep and the occurrence times of local earthquakes have been obtained for the period early 1974 through mid-1977 along the San Andreas fault between the most southern extent of the 1906 earthquake fault break and the most northern extent of the 1857 break. The data utilized are primarily from stations located near the two ends of this section of the fault where strains accumulation is expected. The magnetic data show that local magnetic field variations up to 1.8 gammas with durations of a few minutes to several months have occurred. The creep data indicate both episodic events and changes in creep rate of up to 10 mm/yr lasting for six months or more. No clear magnetic transients or offsets are evident either simultaneous with or preceding the occurrence times of the episodic creep events by up to a day or so. Although some patterns of creep onset times at adjacent stations appear to correspond to some periods of longer term change in local magnetic field, these changes do not always occur and other groups of creep events have no corresponding changes in local magnetic field. Earthquakes with magnitudes less than 4.0 do not appear to correspond in time to local changes in magnetic field greater than 0.8 gamma or variations in the creep rate.</p><p>In order to explain the observations presented in this study, it appears necessary to allow for a substantial amount of deep aseismic slip without any obvious attendant changes in the time distribution or size of the local earthquakes. Changes in stress related to the surface expression of aseismic slip on the San Andreas fault can be estimated from dislocation models fit to these data and to observations of simultaneous strains and tilts at points near the fault. These stress values are on average less than one bar near the surface but are probably more than 10 bars in localized regions at depths of a kilometer or so.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78809","usgsCitation":"Johnston, M., Smith, B., and Mueller, R.M., 1978, Local magnetic field measurements, fault creep observations and local earthquakes on the San Andreas fault: U.S. Geological Survey Open-File Report 78-809, 15 p., https://doi.org/10.3133/ofr78809.","productDescription":"15 p.","costCenters":[],"links":[{"id":142328,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0809/report-thumb.jpg"},{"id":425329,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0809/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Andreas fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.5134730637543,\n              37.91905600189389\n            ],\n            [\n              -122.5134730637543,\n              32.75570813429434\n            ],\n            [\n              -116.96878062048438,\n              32.75570813429434\n            ],\n            [\n              -116.96878062048438,\n              37.91905600189389\n            ],\n            [\n              -122.5134730637543,\n              37.91905600189389\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b209","contributors":{"authors":[{"text":"Johnston, M.J.S. 0000-0003-4326-8368","orcid":"https://orcid.org/0000-0003-4326-8368","contributorId":104889,"corporation":false,"usgs":true,"family":"Johnston","given":"M.J.S.","affiliations":[],"preferred":false,"id":160148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, B.E.","contributorId":36495,"corporation":false,"usgs":true,"family":"Smith","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":160146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mueller, Robert Martin","contributorId":89531,"corporation":false,"usgs":true,"family":"Mueller","given":"Robert","email":"","middleInitial":"Martin","affiliations":[],"preferred":false,"id":160147,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9700,"text":"ofr78516 - 1978 - Planning report for the southeastern limestone regional aquifer system analysis","interactions":[],"lastModifiedDate":"2023-11-20T21:56:19.315191","indexId":"ofr78516","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-516","title":"Planning report for the southeastern limestone regional aquifer system analysis","docAbstract":"<p>The southeastern limestone aquifer system is one of the major sources of ground water in the United States. Over 3 billion gallons of water are pumped daily making the aquifer the principal source of municipal, industrial, and agricultural water supply in large parts of Florida and Georgia and to a lesser extent in South Carolina, and Alabama. Another important use is the disposal of industrial wastes and treated sewage into parts of the limestone system containing saline water. A variety of problems have developed in the aquifer in recent years, principally declining water levels, saltwater intrusion in coastal areas, water-quality degradation, and inadequate supplies of fresh ground water locally.</p><p>In 1978 the U.S. Geological Survey began a study whose goal is to provide a complete description of the hydrogeologic framework, geochemistry, and regional flow system of the limestone aquifer. A 4-year effort is planned that will include: (1) synthesis of all existing data and presentation on a series of regional hydrogeological and geochemical maps; (2) obtaining new hydrogeological information to fill data voids -- particularly where ongoing State and Federal programs are not likely to generate such data; and (3) design and calibration of a regional digital model of the aquifer system and detailed models of problem areas. Computer simulation will be used extensively to assess the effects of large withdrawals of ground water and waste injection into the aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78516","usgsCitation":"Johnston, R.H., 1978, Planning report for the southeastern limestone regional aquifer system analysis: U.S. Geological Survey Open-File Report 78-516, iii, 26 p., https://doi.org/10.3133/ofr78516.","productDescription":"iii, 26 p.","costCenters":[],"links":[{"id":422740,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0516/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142350,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0516/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia, South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.1863243360107,\n              25.592077877776376\n            ],\n            [\n              -80.1863243360107,\n              32.677897021016406\n            ],\n            [\n              -88.37090332184287,\n              32.677897021016406\n            ],\n            [\n              -88.37090332184287,\n              25.592077877776376\n            ],\n            [\n              -80.1863243360107,\n              25.592077877776376\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6852d6","contributors":{"authors":[{"text":"Johnston, Richard H.","contributorId":95860,"corporation":false,"usgs":true,"family":"Johnston","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":160151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9703,"text":"ofr79854 - 1978 - Instrumentation for obtaining seismic anisotropy data from ocean bottom using moored sonobuoys","interactions":[],"lastModifiedDate":"2022-07-18T16:03:19.545703","indexId":"ofr79854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-854","title":"Instrumentation for obtaining seismic anisotropy data from ocean bottom using moored sonobuoys","docAbstract":"<p>Using observations by Raitt and Shor, Hess (1964) noted that there was a correlation of compressional wave velocity in the mantle with seismic profile direction, suggesting that seismic anisotropy existed over a broad area of the Pacific basin. This paper describes a system developed and used to look for the existence and extent of this seismic anisotropy.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79854","usgsCitation":"Jones, A.C., 1978, Instrumentation for obtaining seismic anisotropy data from ocean bottom using moored sonobuoys: U.S. Geological Survey Open-File Report 79-854, 46 p., https://doi.org/10.3133/ofr79854.","productDescription":"46 p.","costCenters":[],"links":[{"id":403915,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0854/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0854/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5edb8a","contributors":{"authors":[{"text":"Jones, Alan C.","contributorId":94307,"corporation":false,"usgs":true,"family":"Jones","given":"Alan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160156,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9132,"text":"ofr7823 - 1978 - Selected hydrologic data, Yampa River basin and parts of the White River basin, northwestern Colorado and south-central Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr7823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-23","title":"Selected hydrologic data, Yampa River basin and parts of the White River basin, northwestern Colorado and south-central Wyoming","docAbstract":"Selected hydrologic data are presented from four energy-related projects conducted by the U.S. Geological Survey in the Yampa River basin and parts of the White River basin in northwestern Colorado and south-central Wyoming. Water-quality data during 1974 and 1975 and parts of 1976 for 129 ground-water sites and 119 surface-water sites are tabulated. For most samples, major cations, anions, and trace metals were analyzed. For the same time period, field measurements of specific conductance, temperature, and pH were made on 252 springs and wells. These samplings sites, as well as the locations of 20 climatological stations, 18 snow-course sites, and 43 surface-water gaging stations, are shown on maps. Geologic units that contain coal deposits or supply much of the water used for stock and domestic purposes in the area also are shown on a map. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7823","usgsCitation":"Giles, T., and Brogden, R.E., 1978, Selected hydrologic data, Yampa River basin and parts of the White River basin, northwestern Colorado and south-central Wyoming: U.S. Geological Survey Open-File Report 78-23, iii, 91 p. :ill., 2 fold. maps ;31 cm.; (106 p., 2 sheets - PGS), https://doi.org/10.3133/ofr7823.","productDescription":"iii, 91 p. :ill., 2 fold. maps ;31 cm.; (106 p., 2 sheets - PGS)","costCenters":[],"links":[{"id":142040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0023/report-thumb.jpg"},{"id":36761,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36762,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0023/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0023/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f83b6","contributors":{"authors":[{"text":"Giles, T.F.","contributorId":83096,"corporation":false,"usgs":true,"family":"Giles","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":159157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brogden, Robert E.","contributorId":56202,"corporation":false,"usgs":true,"family":"Brogden","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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