{"pageNumber":"361","pageRowStart":"9000","pageSize":"25","recordCount":10957,"records":[{"id":59612,"text":"mf1214C - 1981 - Map showing aeromagnetic interpretation of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning Areas, Modoc, Shasta, and Siskiyou counties, California","interactions":[],"lastModifiedDate":"2018-12-06T14:40:41","indexId":"mf1214C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1214","chapter":"C","title":"Map showing aeromagnetic interpretation of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning Areas, Modoc, Shasta, and Siskiyou counties, California","docAbstract":"<p>The data for the aeromagnetic map of the Baker-Cypress and Timbered crater areas were collected in 1978 and compiled at a scale of 1 :62,500 (U,S, Geological Survey, 1979). East-west traverses were spaced at 0.8-km intervals at a constant altitude of 1370 m (4500 ft) above sea level, Contour interval is 20 and 100 gammas, depending upon the steepness of local gradients in the Earth's magnetic field. A regional magnetic field (the International Geomagnetic Reference Field - 1975, updated to the month flown) of approximately 5-6 gammas/km was removed from the data be fore con touring.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1214C","usgsCitation":"Griscom, A., 1981, Map showing aeromagnetic interpretation of the Baker-Cypress BLM Instant Study Area and Timbered Crater Forest Service Further Planning Areas, Modoc, Shasta, and Siskiyou counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1214, 29.11 x 23.46 inches, https://doi.org/10.3133/mf1214C.","productDescription":"29.11 x 23.46 inches","costCenters":[],"links":[{"id":359992,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1214-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1214-C/report-thumb.jpg"}],"scale":"0","country":"United States","state":"California","county":"Modoc County, Shasta County, Siskiyou County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.58333333333333,41.083333333333336 ], [ -121.58333333333333,41.25 ], [ -121.33333333333333,41.25 ], [ -121.33333333333333,41.083333333333336 ], [ -121.58333333333333,41.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655511","contributors":{"authors":[{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":262319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68690,"text":"ha650 - 1981 - Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado","interactions":[],"lastModifiedDate":"2022-08-25T20:15:42.86453","indexId":"ha650","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"650","title":"Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado","docAbstract":"<p>The Denver ground-water basin underlies a 6,700-square-mile area extending from Greeley in the north to Colorado Springs in the south, and from the Front Range in the west to near Limon in the east.&nbsp; The four major bedrock aquifers that occur in the basin are the Laramie-Fox Hills aquifer (the deepest aquifer), the Arapahoe aquifer, the Denver aquifer, and the Dawson aquifer (the uppermost aquifer).&nbsp; The Laramie-Fox Hills aquifer, which is the subject of this report, underlies the entire area of the basin in east-central Colorado (index map, fig. 1) and is an important source of water for residents in the northern Denver suburban area and in the rural areas of eastern Jefferson, Arapahoe, and Elbert Counties, Adams County, and southern Weld and El Paso Counties.&nbsp; About 90 percent of the estimated 1,700 wells completed in the aquifer supply water to residents and livestock.&nbsp; The remaining wells supply water for commercial and industrial use and limited irrigation of commercial crops.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha650","usgsCitation":"Robson, S.G., 1981, Geologic structure, hydrology, and water quality of the Laramie-Fox Hills aquifer in the Denver basin, Colorado: U.S. Geological Survey Hydrologic Atlas 650, 3 Plates: 34.74 x 40.63 inches or smaller, https://doi.org/10.3133/ha650.","productDescription":"3 Plates: 34.74 x 40.63 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":90408,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405625,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16050.htm","linkFileType":{"id":5,"text":"html"}},{"id":187920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90409,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90410,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/650/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","country":"United States","state":"Colorado","otherGeospatial":"Denver basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.257,\n              38.661\n            ],\n            [\n              -103.603,\n              38.661\n            ],\n            [\n              -103.603,\n              40.425\n            ],\n            [\n              -105.257,\n              40.425\n            ],\n            [\n              -105.257,\n              38.661\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688117","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56286,"text":"wdrWA812 - 1981 - Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2022-12-14T00:49:08.926242","indexId":"wdrWA812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"WA-81-2","title":"Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington","docAbstract":"<p>Water-resources data for the 1981 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water. This report, in two volumes, contains records for water discharge at 229 gaging stations; stage only at 5 gaging stations; stage and contents at 39 lakes and reservoirs; water quality at 39 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 14 crest-stage and 28 water-quality partial-record stations. Locations of sites in this volume are on figures 4, 5, 6, and 22. Additional water data were collected at various sites not involved in the systematic data-collection 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, local, and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA812","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data, Washington, water year 1981: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-81-2, x, 276 p., https://doi.org/10.3133/wdrWA812.","productDescription":"x, 276 p.","costCenters":[],"links":[{"id":174739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/wa-81-2/report-thumb.jpg"},{"id":410428,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/wa-81-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":56197,"text":"wdrNY801 - 1981 - Water resources data for New York, volume 1, eastern New York, excluding Long Island","interactions":[],"lastModifiedDate":"2020-11-23T21:04:14.619679","indexId":"wdrNY801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"NY-80-1","title":"Water resources data for New York, volume 1, eastern New York, excluding Long Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY801","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data for New York, volume 1, eastern New York, excluding Long Island: U.S. Geological Survey Water Data Report 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,{"id":50766,"text":"ofr811004 - 1981 - Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","interactions":[],"lastModifiedDate":"2017-12-06T14:00:43","indexId":"ofr811004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1004","title":"Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980","docAbstract":"<p>The High Plains aquifer in Kansas is part of a regional system that extends into Colorado, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming.&nbsp; The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State.&nbsp; This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits.&nbsp; In western Kansas, the High Plains aquifer consists principally of the Ogallala Formation of late Tertiary age and the overlying deposits of Quaternary age.&nbsp; In south-central Kansas, the aquifer consists of unconsolidated deposits principally of the Quaternary age.&nbsp; Valley alluvium of Quaternary age also is included in the deposits in both areas.&nbsp; The High Plains aquifer is delimited on the east by outcrops of Permian or Cretaceous rocks and by unsaturated deposits of Quaternary age.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811004","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1981, Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980: U.S. Geological Survey Open-File Report 81-1004, 43.21 x 31.20 inches, https://doi.org/10.3133/ofr811004.","productDescription":"43.21 x 31.20 inches","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":349811,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1004/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1004/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"High Plains Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102,\n              40\n            ],\n            [\n              -102,\n              37\n            ],\n            [\n              -97,\n              37\n            ],\n            [\n              -97,\n              39\n            ],\n            [\n              -99,\n              39\n            ],\n            [\n              -99,\n              40\n            ],\n            [\n              -102,\n              40\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686ac3","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242259,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68748,"text":"oc113 - 1981 - Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah","interactions":[],"lastModifiedDate":"2019-12-26T07:46:24","indexId":"oc113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"113","title":"Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from Salt Valley to Dewey Bridge in east-central Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/oc113","usgsCitation":"O'Sullivan, R., 1981, Stratigraphic sections of Middle Jurassic Entrada Sandstone and related rocks from 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,{"id":61399,"text":"mf1195 - 1981 - Map showing vegetation distribution in the central part of the East Tintic Mountains, Utah","interactions":[],"lastModifiedDate":"2016-08-23T10:31:33","indexId":"mf1195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1195","title":"Map showing vegetation distribution in the central part of the East Tintic Mountains, Utah","docAbstract":"<p>With the development of remote sensing technology has come the capability of defining and mapping plant communities by means of their spectral properties. &nbsp;Such maps will be an important aid in resource evaluation and management, especially in densely vegetated and remote areas of the world.</p>\n<p>This study in part of a broader program to determine the usefulness of multispectral scanner aircraft and satellite images for mapping lithologic units and vegetation communities (Rowan and others, 1974; 1977; Abrams and others, 1997; Rowan and Abrams, 1978a; 1978b; Kahle and Rowan, 1979, written commun.).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1195","usgsCitation":"Milton, N., and Madura, D.P., 1981, Map showing vegetation distribution in the central part of the East Tintic Mountains, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1195, 34.68 x 25.43 inches, https://doi.org/10.3133/mf1195.","productDescription":"34.68 x 25.43 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1195.PNG"},{"id":327594,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1195/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Utah","otherGeospatial":"Eastern Tintic Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.11749999999999,39 ], [ -112.11749999999999,40 ], [ -112,40 ], [ -112,39 ], [ -112.11749999999999,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69e473","contributors":{"authors":[{"text":"Milton, Nancy","contributorId":85188,"corporation":false,"usgs":true,"family":"Milton","given":"Nancy","affiliations":[],"preferred":false,"id":265580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Madura, Daryl P.","contributorId":173056,"corporation":false,"usgs":false,"family":"Madura","given":"Daryl","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":265579,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48721,"text":"ofr81458 - 1981 - Equal-area base map of the Bering Sea, plate 4: Aleutian east","interactions":[],"lastModifiedDate":"2021-10-22T16:32:10.686685","indexId":"ofr81458","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-458","title":"Equal-area base map of the Bering Sea, plate 4: Aleutian east","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81458","usgsCitation":"Jones, D., and Swenson, P.A., 1981, Equal-area base map of the Bering Sea, plate 4: Aleutian east: U.S. Geological Survey Open-File Report 81-458, 1 Plate: 40.44 × 34.36 inches, https://doi.org/10.3133/ofr81458.","productDescription":"1 Plate: 40.44 × 34.36 inches","costCenters":[],"links":[{"id":170308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108152,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12046.htm","linkFileType":{"id":5,"text":"html"},"description":"12046"},{"id":85528,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0458/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -176,\n              52\n            ],\n            [\n              -164,\n              52\n            ],\n            [\n              -164,\n              58\n            ],\n            [\n              -176,\n              58\n            ],\n            [\n              -176,\n              52\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe34d","contributors":{"authors":[{"text":"Jones, D.R.","contributorId":80670,"corporation":false,"usgs":true,"family":"Jones","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":238111,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swenson, P. A.","contributorId":38632,"corporation":false,"usgs":true,"family":"Swenson","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238110,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61501,"text":"mf1217 - 1981 - Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California","interactions":[{"subject":{"id":24125,"text":"ofr80662 - 1980 - Preliminary map showing recently active breaks along the Maacama fault zone between Hopland and Laytonville, Mendocino County, California","indexId":"ofr80662","publicationYear":"1980","noYear":false,"title":"Preliminary map showing recently active breaks along the Maacama fault zone between Hopland and Laytonville, Mendocino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":61501,"text":"mf1217 - 1981 - Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California","indexId":"mf1217","publicationYear":"1981","noYear":false,"title":"Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California"},"id":1}],"lastModifiedDate":"2018-12-06T15:29:01","indexId":"mf1217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1217","title":"Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California","docAbstract":"<p>The southernmost 15 km of this map is a product of a study that began in 1975 as part of a study of recency of faulting in coastal California (Ziony and others, 1974; Buchanan-Banks and others, 1978; Pampeyan , 1979). In February 1975, after being shown evidence of recent faulting in the vicinity of Ukiah by E. C. Winterhalder, Principal Engineering Geologist for Harding - Lawson Associates, Pampeyan extended the study area northward to the vicinity of Willits . After the Willits earthquake of November 22, 1977 (Simon and others, 1978; Warren and others, 1979), field investigations in the epicentral area revealed a series of distressed pavements, curbs, and sidewalks all showing right-lateral offset (Harsh and others, 1978; 1981). These features traverse the city of Willits and define a line coincident with a photolineament extending southeastward from Willits. Subsequently, additional sites of distressed pavements discovered both east and north of Ukiah alone; other lineaments of the photogeologic study verified the existence of tectonic creep in the Maacama fault zone.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1217","usgsCitation":"Pampeyan, E., Harsh, P., and Coakley, J., 1981, Preliminary map showing recently active breaks along the Maacama Fault zone between Hopland and Laytonville, Mendocino County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1217, 3 Sheets: 58.01 x 42.00 inches or smaller, https://doi.org/10.3133/mf1217.","productDescription":"3 Sheets: 58.01 x 42.00 inches or smaller","costCenters":[],"links":[{"id":180223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1217/report-thumb.jpg"},{"id":360001,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1217/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360002,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1217/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360003,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1217/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","county":"Mendcino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.5,38.8675 ], [ -123.5,39.75 ], [ -123,39.75 ], [ -123,38.8675 ], [ -123.5,38.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf7f","contributors":{"authors":[{"text":"Pampeyan, E. H.","contributorId":14493,"corporation":false,"usgs":true,"family":"Pampeyan","given":"E. H.","affiliations":[],"preferred":false,"id":265828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harsh, Philip W.","contributorId":18028,"corporation":false,"usgs":true,"family":"Harsh","given":"Philip W.","affiliations":[],"preferred":false,"id":265829,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coakley, J.M.","contributorId":32557,"corporation":false,"usgs":true,"family":"Coakley","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":265830,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60018,"text":"mf1290B - 1981 - Geochemical survey of Shining Rock Wilderness, Heywood County, North Carolina","interactions":[],"lastModifiedDate":"2018-10-25T10:00:17","indexId":"mf1290B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1290","chapter":"B","title":"Geochemical survey of Shining Rock Wilderness, Heywood County, North Carolina","docAbstract":"<p>The U.S. Geological Survey (USGS) made a reconnaissance geochemical survey of the Shining Rock Wilderness (fig. 1) to test for unidentified or unexposed mineral deposits that might be recognized by their geochemical halos.&nbsp; Similar geochemical survey based on trace-element analyses have been credited with the discovery of many types of mineral deposits (Hawkes and Webb, 1962).&nbsp; Although no metallic mineral deposits are known in the study area, the same sequence of rocks that is exposed there contains small deposits of copper-bearing sulfides 10-18 mi (16-28 km) west and southwest of the wilderness (Gair and Slack, 1979).&nbsp; Keith (1907, p. 8) reports minor amounts of copper sulfides and iron sulfides in schist and in quartz veins cutting schist near Retreat, 4 mi (6.5 km) northwest of the wilderness.&nbsp; An old gold mine, the Boylston mine, on Forge Mountain 10 mi (16 km) east of the wilderness (Nitze and Hanna, 1896, p. 181-191) is in metasedimentary rocks of the Great Smoky Group (Hadley and Nelson, 1971) which are probably younger than the rocks exposed in the wilderness.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1290B","usgsCitation":"Lesure, F.G., 1981, Geochemical survey of Shining Rock Wilderness, Heywood County, North Carolina: U.S. Geological Survey Miscellaneous Field Studies Map 1290, 42.00 x 55.52 inches, https://doi.org/10.3133/mf1290B.","productDescription":"42.00 x 55.52 inches","costCenters":[],"links":[{"id":358787,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1290-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1290-B/report-thumb.jpg"}],"scale":"0","country":"United States","state":"North Carolina","county":"Haywood County","otherGeospatial":"Shining Rock Wilderness","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.91666666666667,\n              35.333333333333336\n            ],\n            [\n              -82.91666666666667,\n              35.416666666666664\n            ],\n            [\n              -82.78416666666666,\n              35.416666666666664\n            ],\n            [\n              -82.78416666666666,\n              35.333333333333336\n            ],\n            [\n              -82.91666666666667,\n              35.333333333333336\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abb31","contributors":{"authors":[{"text":"Lesure, Frank G.","contributorId":20068,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":262999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10797,"text":"ofr81950 - 1981 - Ice-gouge data, Beaufort Sea, Alaska, 1972-1980","interactions":[],"lastModifiedDate":"2023-06-26T19:24:32.913553","indexId":"ofr81950","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-950","title":"Ice-gouge data, Beaufort Sea, Alaska, 1972-1980","docAbstract":"<p>The interaction of sea ice with the sea floor is an important factor affecting geologic processes on high latitude shelves. One of the most obvious forms of this interaction is the formation of furrow-like gouges or the sea floor. These gouges are caused by wind- and current-driven ice masses that rake the seabed with their keels. Since the advent of side-scanning sonar about 1970, the morphology and character of these seabed features have been under study. Ice gouges have been reported from the Bering Sea (Thor and Nelson, 1980); from the Chukchi Sea (Rex, 1955; Toimil, 1978); from the Beaufort Sea off Alaska (Brooks, 1974; Carsola, 1954; Reimnitz et al., 1972); from the Beaufort Sea off Canada (Kindle, 1924; Lewis, 1978; Pelletier and Shearer, 1972; Wahlgren, 1979); from the east coast of Canada (Harris, 1974); from the northeast Atlantic (Belderson et al., 1973); and from the Great Lakes (Berkson and Clay, 1973).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81950","usgsCitation":"Rearic, D.M., Barnes, P.W., and Reimnitz, E., 1981, Ice-gouge data, Beaufort Sea, Alaska, 1972-1980: U.S. Geological Survey Open-File Report 81-950, 22 p., https://doi.org/10.3133/ofr81950.","productDescription":"22 p.","costCenters":[],"links":[{"id":418471,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0950/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143883,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0950/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Beaufort Sea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -158.9068868579794,\n              73.12276506117749\n            ],\n            [\n              -158.9068868579794,\n              69.54049536847626\n            ],\n            [\n              -141.13582197059608,\n              69.54049536847626\n            ],\n            [\n              -141.13582197059608,\n              73.12276506117749\n            ],\n            [\n              -158.9068868579794,\n              73.12276506117749\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb784","contributors":{"authors":[{"text":"Rearic, Douglas M.","contributorId":52969,"corporation":false,"usgs":true,"family":"Rearic","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":161984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Peter W.","contributorId":6042,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161982,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":161983,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27596,"text":"wri8114 - 1981 - The surficial aquifer in east-central St. Johns County, Florida","interactions":[],"lastModifiedDate":"2019-07-10T09:54:31","indexId":"wri8114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-14","title":"The surficial aquifer in east-central St. Johns County, Florida","docAbstract":"The surficial aquifer, a composite of confined and unconfined water-bearing zones overlying the Miocene Hawthorn Formation, is an important source of water in St. Johns County, Fla. The water from wells open to the surficial aquifer generally meets quality standards recommended by the U.S. Environmental Protection Agency for public water supplies, except for concentrations of iron that for most wells are substantially greater than the recommended limit of 0.3 milligrams per liter. Data from 12 test wells drilled to the top of the Hawthorn formation, about 100 feet below land surface, indicate that the productive zones and confining beds in the surficial aquifer are discontinuous. Test well yields from individual zones range from less than 1 to 42 gallons per minute from depths between 20 and 100 feet below land surface. The most productive zones were generally found in the Tillman Ridge area, about 10 square miles in the west-central part of the area of investigation. Analysis of an aquifer test on a well in the Tillman Ridge area indicates a transmissivity of about 6,500 to 7,000 feet squared per day. The best local source of good quality water for development of a relatively large water supply is in the vicinity of Tillman Ridge. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8114","usgsCitation":"Hayes, E.C., 1981, The surficial aquifer in east-central St. Johns County, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-14, v, 19 p. , https://doi.org/10.3133/wri8114.","productDescription":"v, 19 p. ","costCenters":[],"links":[{"id":158815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0014/report-thumb.jpg"},{"id":365428,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0014/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"St. Johns County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6159a1","contributors":{"authors":[{"text":"Hayes, Eugene C.","contributorId":46918,"corporation":false,"usgs":true,"family":"Hayes","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10615,"text":"ofr81917 - 1981 - Revised techniques for estimating magnitude and frequency of floods in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr81917","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-917","title":"Revised techniques for estimating magnitude and frequency of floods in Montana","docAbstract":"Relations for estimating the flood magnitudes for ungaged sites in Montana have been updated. The State was divided into eight regions and separate multiple-regression equations for each region were developed that relate logarithms of annual flood magnitude to logarithms of basin characteristics for exceedance probabilities of 50, 20, 10, 4, 2, and 1 percent. The standard errors of estimate for an exceedance probability of 1 percent ranged from 39 to 58 percent in the western and central parts of the State and from 47 to 83 percent in the eastern part. The standard errors of estimate indicate a substantial improvement over previous studies. Techniques for transferring annual flood-frequency information at gaged sites to ungaged sites on the same stream have been updated. Included are curves relating flood-frequency information to drainage area for eight major streams in the State. Maximum known flood peaks in Montana are compared with estimated 1-percent-chance flood peaks and with national maximum known flood peaks. Values of flood discharges for selected exceedance probabilities and values of significant basin characteristics for all gaging stations used in the analysis are tabulated. Included are data for 339 stations in Montana and 34 nearby stations in Canada and adjoining States. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81917","usgsCitation":"Parrett, C., and Omang, R.J., 1981, Revised techniques for estimating magnitude and frequency of floods in Montana: U.S. Geological Survey Open-File Report 81-917, iv, 70 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81917.","productDescription":"iv, 70 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0917/report-thumb.jpg"},{"id":38450,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0917/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38451,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0917/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654b63","contributors":{"authors":[{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":161684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161685,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10608,"text":"ofr81545 - 1981 - Time-of-travel study in the Sebasticook River basin, Maine","interactions":[],"lastModifiedDate":"2024-03-25T19:29:06.079889","indexId":"ofr81545","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-545","title":"Time-of-travel study in the Sebasticook River basin, Maine","docAbstract":"<p>Time of travel was determined for four reaches of the Sebasticook River, two on the East Branch Sebasticook River, and two on the main stem of the Sebasticook River. Reach A included 7.8 miles of the East Branch Sebasticook River from Dexter to Corinna, Maine. Reach B included 8 miles of the East Branch Sebasticook River from Newport to its mouth, and 1 mile of the Sebasticook River to Peltoma bridge near Pittsfield, Maine. Reach C included 3.5 miles of the Sebasticook River from Hartland to West Palmyra, Maine. Reach D included 31.4 miles of the Sebasticook River from Pittsfield to Winslow, Maine. Using a 20-percent solution of rhodamine WT fluorescent dye, three dye-tracer type time-of-travel study runs were made in each reach. Water samples were collected at 10 sites in the study area. The samples were then analyzed for dye concentrations.</p><p>Time-of-travel data for each subreach are depicted in a series of illustrations and summarized in tabular form. Examples are given to illustrate use of the data presented.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81545","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Parker, G.W., 1981, Time-of-travel study in the Sebasticook River basin, Maine: U.S. Geological Survey Open-File Report 81-545, Report: vi, 17 p.; Appendixes: A-C, https://doi.org/10.3133/ofr81545.","productDescription":"Report: vi, 17 p.; Appendixes: A-C","costCenters":[],"links":[{"id":142531,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0545/report-thumb.jpg"},{"id":427065,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0545/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"Sebasticook River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -69.33766500023974,\n              45.042811639545846\n            ],\n            [\n              -69.33766500023974,\n              44.887473237000506\n            ],\n            [\n              -69.20587080375181,\n              44.887473237000506\n            ],\n            [\n              -69.20587080375181,\n              45.042811639545846\n            ],\n            [\n              -69.33766500023974,\n              45.042811639545846\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b565","contributors":{"authors":[{"text":"Parker, Gene W. gwparker@usgs.gov","contributorId":1392,"corporation":false,"usgs":true,"family":"Parker","given":"Gene","email":"gwparker@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":161672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10505,"text":"ofr81685 - 1981 - Hydrology and the effects of industrial pumping in the Nikiski area, Alaska","interactions":[],"lastModifiedDate":"2023-08-01T22:19:07.162703","indexId":"ofr81685","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-685","title":"Hydrology and the effects of industrial pumping in the Nikiski area, Alaska","docAbstract":"<p>Ground-water consumption for industrial use at Nikiski increased from about 1 million gallons per day in 1968 to 4.2 million gallons per day in 1979. Water managers and local citizens are concerned that industrial pumping may reduce the esthetic and recreational value of local lakes. Some lake levels have declined as much as 8 feet since pumping began; the greatest declines occurred in lakes nearest the center of pumping.</p><p>Ground water occurs in three aquifers. The upper aquifer is unconfined and is hydraulically connected to most lakes and streams in the area. The upper two aquifers are hydraulically connected through a leaky confining layer, and water levels in the two aquifers fluctuate synchronously with changes in precipitation and changes in pumping from either aquifer. The hydraulic connection of the lower confined aquifer, the deepest of the three aquifers, to the other two aquifers is poor. Drawdowns caused by pumping have stabilized in all three aquifers. This indicates that the pumping is in equilibrium with the hydrologic boundaries. In the lower two aquifers, the potentiometric surfaces near some production wells are below sea level; however, no salt water has intruded the aquifers as far as the pumped wells. If intrusion occurs or if additional water supplies are needed, another potential site for ground-water development is the middle Beaver Creek basin, 7-10 miles east of the industrial area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81685","collaboration":"Prepared in cooperation with the Alaska Department of Natural Resources and Kenai Peninsula Borough","usgsCitation":"Nelson, G.L., 1981, Hydrology and the effects of industrial pumping in the Nikiski area, Alaska: U.S. Geological Survey Open-File Report 81-685, iv, 22 p., https://doi.org/10.3133/ofr81685.","productDescription":"iv, 22 p.","costCenters":[],"links":[{"id":144638,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0685/report-thumb.jpg"},{"id":419484,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0685/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Nikiski","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -151.45826580748331,\n              60.746844331157206\n            ],\n            [\n              -151.45826580748331,\n              60.6716276310604\n            ],\n            [\n              -151.2111813821138,\n              60.6716276310604\n            ],\n            [\n              -151.2111813821138,\n              60.746844331157206\n            ],\n            [\n              -151.45826580748331,\n              60.746844331157206\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e83f","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4055,"text":"cir801 - 1981 - Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978","interactions":[],"lastModifiedDate":"2020-09-27T17:48:12.680465","indexId":"cir801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"801","title":"Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978","docAbstract":"In 1960, the U.S. Geological Survey and the Kentucky Geological Survey began a program to map the State geologically at a scale of 1:24,000 and to publish the maps as 707 U.S. Geological Survey Geologic Quadrangle Maps. Fieldwork was completed by the spring of 1977, and all maps were published by December 1978. \r\n\r\nGeologic mapping of the State was proposed by the Kentucky Society of Professional Engineers in 1959. Wallace W. Hagan, Director and State Geologist of the Kentucky Geological Survey, and Preston McGrain, Assistant State Geologist, promoted support for the proposal among organizations such as Chambers of Commerce, industrial associations, professional societies, and among members of the State government. It was also arranged for the U.S. Geological Survey to supply mapping personnel and to publish the maps; the cost would be shared equally by the two organizations. \r\n\r\nMembers of the U.S. Geological Survey assigned to the program were organized as the Branch of Kentucky Geology. Branch headquarters, including an editorial staff, was at Lexington, Ky., but actual mapping was conducted from 18 field offices distributed throughout the State. The Publications Division of the U.S. Geological Survey established a cartographic office at Lexington to prepare the maps for publication. \r\n\r\nAbout 260 people, including more than 200 professionals, were assigned to the Branch of Kentucky Geology by the U.S. Geological Survey at one time or another. The most geologists assigned any one year was 61. To complete the mapping and ancillary studies, 661 professional man-years were required, compared with an original estimate of 600 man-years. \r\n\r\nA wide variety of field methods were used, but most geologists relied on the surveying altimeter to obtain elevations. Surface data were supplemented by drill-hole records, and several dozen shallow diamond-drill holes were drilled to aid the mapping. Geologists generally scribed their own maps, with a consequent saving of publication costs. \r\n\r\nPaleontologists and stratigraphers of the U.S. Geological Survey cooperated closely with the program. Paleontologic studies were concentrated in the Ordovician of central Kentucky, the Pennsylvanian of eastern and western Kentucky, and the Mesozoic and Cenozoic of westernmost Kentucky. \r\n\r\nIn addition to financial support, the Kentucky Geological Survey provided economic data, stratigraphic support, and drillhole records to the field offices. Geologists of the State Survey made subsurface structural interpretations, constructed bedrock topography maps, and mapped several quadrangles. \r\n\r\nSome of the problems encountered were the inadequacy of much of the existing stratigraphic nomenclature, the uneven quality of some of the mapping, and the effects of relative isolation on the professional development of some of the geologists. \r\n\r\nThe program cost a total of $20,927,500. In terms of 1960 dollars, it cost $16,035,000; this compares with an original estimate of $12,000,000. Although it is difficult to place a monetary value on the geologic mapping, the program has contributed to newly discovered mineral wealth, jobs, and money saved by government and industry. The maps are used widely in the exploration for coal, oil and gas, fluorspar, limestone, and clay. The maps are also used in planning highways and locations of dams, in evaluating foundation and excavation conditions, in preparing environmental impact statements, and in land-use planning.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir801","usgsCitation":"Cressman, E.R., and Noger, M.C., 1981, Geologic mapping of Kentucky: A history and evaluation of the Kentucky Geological Survey--U.S. Geological Survey Mapping Program, 1960-1978: U.S. Geological Survey Circular 801, iii, 22 p., https://doi.org/10.3133/cir801.","productDescription":"iii, 22 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science 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,{"id":10195,"text":"ofr802008 - 1981 - Mekometer measurements in the Imperial Valley","interactions":[],"lastModifiedDate":"2022-04-18T16:07:43.315449","indexId":"ofr802008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-2008","title":"Mekometer measurements in the Imperial Valley","docAbstract":"<p>During the six weeks following the October 15, 1979 earthquake, parts of the Imperial Valley Mekometer network (Fig. 1) around the Imperial fault to the east of El Centro were re-measured, some repeatedly, in an attempt to assess the coseismic and postearthquake slip on the fault, and horizontal strain adjustment around it. This report presents the results, together with the most recent pre-earthquake measurements, for comparison. It includes also a brief discussion of the results.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr802008","usgsCitation":"Mason, R.G., Crook, C., and Wood, P., 1981, Mekometer measurements in the Imperial Valley: U.S. Geological Survey Open-File Report 80-2008, 25 p., https://doi.org/10.3133/ofr802008.","productDescription":"25 p.","costCenters":[],"links":[{"id":398931,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2008/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2008/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Imperial Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.58990478515625,\n              32.803436166989265\n            ],\n            [\n              -115.21087646484375,\n              32.803436166989265\n            ],\n            [\n              -115.21087646484375,\n              33.261656767328006\n            ],\n            [\n              -115.58990478515625,\n              33.261656767328006\n            ],\n            [\n              -115.58990478515625,\n              32.803436166989265\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2be4b07f02db613082","contributors":{"authors":[{"text":"Mason, Ronald G.","contributorId":6856,"corporation":false,"usgs":true,"family":"Mason","given":"Ronald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":160983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crook, C.N.","contributorId":104064,"corporation":false,"usgs":true,"family":"Crook","given":"C.N.","email":"","affiliations":[],"preferred":false,"id":160985,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wood, P.R.","contributorId":102068,"corporation":false,"usgs":true,"family":"Wood","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":160984,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25511,"text":"wri80117 - 1981 - Flow routing in the Susquehanna River Basin: Part IV - Routing reservoir releases in the eastern Susqehanna river basin in New York State","interactions":[],"lastModifiedDate":"2013-02-28T07:54:12","indexId":"wri80117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"80-117","title":"Flow routing in the Susquehanna River Basin: Part IV - Routing reservoir releases in the eastern Susqehanna river basin in New York State","docAbstract":"Flow-routing models for six reaches of major streams in the eastern Susquehanna River basin in New York were developed and used to trace releases of water from East Sidney Lake and Whitney Point Lake to gaged points downstream. Daily streamflow during 1942-77 was modeled for the following reaches: Susquehanna River--Unadilla to Conklin, Conklin to Vestal, and Vestal to Waverly; Chenango River--Sherburne to Greene, and Greene to Chenango Forks; Tioughnioga River--Cortland to Itaska. The models were developed with convolution techniques and were based on the unit-response method of flow routing, assuming the diffusion analogy and using multilinearization. Overall accuracy of the models, as measured by the average difference between observed and simulated daily flows over the base period, was within the stated accuracy of published gaging-station records. As an example of one application of the models, hypothetical releases from East Sidney Lake and Whitney Point Lake during low flow were traced downstream to the Waverly gaging station at the lower end of the area studied. The leading edge of the East Sidney release arrived in 4 days, and the full release arrived in 6 days. The leading edge of the Whitney Point release arrived in 1 day, and the full release arrived in 3 days. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri80117","usgsCitation":"Zembrzuski, T.J., 1981, Flow routing in the Susquehanna River Basin: Part IV - Routing reservoir releases in the eastern Susqehanna river basin in New York State: U.S. Geological Survey Water-Resources Investigations Report 80-117, 31 p. ill., maps ;28 cm., https://doi.org/10.3133/wri80117.","productDescription":"31 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":157252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":268520,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0117/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de830","contributors":{"authors":[{"text":"Zembrzuski, Thomas J. Jr.","contributorId":37371,"corporation":false,"usgs":true,"family":"Zembrzuski","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":193995,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24172,"text":"ofr81418 - 1981 - Map showing ground-water conditions in the Sacramento Valley area, Mohave County, Arizona; 1979","interactions":[],"lastModifiedDate":"2023-06-20T20:16:34.424775","indexId":"ofr81418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-418","title":"Map showing ground-water conditions in the Sacramento Valley area, Mohave County, Arizona; 1979","docAbstract":"<p>The Sacramento Valley area includes about 800<sup>2</sup> miles in northwestern Arizona and is bounded on the west by the Black and Buck Mountains and on the east by the Cerbat and Hualapai Mountains. The Black Mountains consist mainly of volcanic rocks; the Buck, Cerbat, and Hualapai Mountains consist of igneous, metamorphic, and volcanic rocks (Gillespie and Bentley, 1971, pl. 1). Sacramento Valley slopes gently southward and is underlain by alluvium and volcanic rocks to depths of more than 4,000 ft. Gillepsie and Bentley (1971, p. 1-15) divided the alluvium into three units - older, intermediate, and younger alluvium - and the volcanic rocks into two units - older and younger volcanic rocks.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81418","issn":"0094-9140","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Pfaff, C., and Clay, D., 1981, Map showing ground-water conditions in the Sacramento Valley area, Mohave County, Arizona; 1979: U.S. Geological Survey Open-File Report 81-418, 1 Plate: 32.90 x 41.01 inches, https://doi.org/10.3133/ofr81418.","productDescription":"1 Plate: 32.90 x 41.01 inches","costCenters":[],"links":[{"id":418253,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0418/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155466,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0418/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Mohave County","otherGeospatial":"Sacramento Valley area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.33889558143002,\n              35.215132970767584\n            ],\n            [\n              -114.33889558143002,\n              34.86922802153721\n            ],\n            [\n              -114.05539989357865,\n              34.86922802153721\n            ],\n            [\n              -114.05539989357865,\n              35.215132970767584\n            ],\n            [\n              -114.33889558143002,\n              35.215132970767584\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ddf","contributors":{"authors":[{"text":"Pfaff, C.L.","contributorId":47777,"corporation":false,"usgs":true,"family":"Pfaff","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":191441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clay, D.M.","contributorId":63044,"corporation":false,"usgs":true,"family":"Clay","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":191442,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","interactions":[{"subject":{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"ofr81220","publicationYear":"1981","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"chapter":"E","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"id":1}],"supersededBy":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"lastModifiedDate":"2022-08-09T15:28:15.441093","indexId":"ofr81220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-220","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","docAbstract":"<p>The need for large quantities of energy has created interest in the Fort Union coal region of the Northern Great Plains. Extensive development of this coal, which may include onsite steam-power generation, gasification, liquefaction, and slurry-pipeline transport of the coal from this region, would place a heavy demand on the region's limited streamflow. Paleozoic rocks that underlie the Fort Union coal region and aquifers in these rocks, including the Red River Formation and the Madison Limestone, might supply, at least on a temporary basis, a significant part of the water required for coal development. The area of study covers approximately 200,000 square miles, and includes eastern Montana, western North Dakota and South Dakota, northeastern Wyoming, and northwestern Nebraska. This report, one of a series in the Madison Limestone study, uses hydrologic and geologic data to outline potentially favorable areas for well construction - that is, areas in which there is a good probability that large-yield wells (more than 500 gallons per minute) can be completed in the Red River Formation and in the Madison Limestone. Potentially favorable areas in terms of aquifer characteristics, for both the Red River Formation and the Madison Limestone, are given a numerical evaluation from 1 to 3 based on the number of the following criteria that are met: (1) the presence of more than 100 feet of relatively porous rock, (2) the presence of more than 100 feet of dolomite, and (3) the presence of known geologic structures which could affect yield. Areas rated 3 are those in which all three criteria are satisfied; areas rated 2 are those in which two criteria are satisfied; and areas rated 1 are those in which only one criterion is satisfied. The criteria selected for this analysis were chosen because they can be recognized and mapped over the entire study area. Local features such as minor structures, solution zones, and rock facies of small extent were not included in this regional evaluation. In addition, water quality was considered in a general way in defining the favorable areas, by excluding areas in which the electrical resistivity of formation water, as calculated from geophysical well logs, was less than 1 ohm-meter. The numerical scales of the Red River Formation and Madison Limestone are summed to show potentially favorable areas for the combined aquifers. Certain additional factors which may be important to a prospective water user were not included in the numerical ranking - these include depths to the two aquifers, calcite saturation, water temperature, total dissolved solids, and piezometric head in relation to land surface. For a complete evaluation, potential users should consider these factors plus local structures, facies, and solution zones in conjunction with the numerical rankings reflecting aquifer characteristics. To facilitate consideration of piezometric head, maps are included in this report showing areas in which the piezometric head falls in certain ranges with respect to land surface.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81220","usgsCitation":"MacCary, L., Cushing, E.M., and Brown, D.L., 1981, Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska: U.S. Geological Survey Open-File Report 81-220, Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches, https://doi.org/10.3133/ofr81220.","productDescription":"Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches","costCenters":[],"links":[{"id":405012,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0220/report-thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.13671875,\n              40.111688665595956\n            ],\n            [\n              -96.328125,\n              40.111688665595956\n            ],\n            [\n              -96.328125,\n              49.03786794532644\n            ],\n            [\n              -115.13671875,\n              49.03786794532644\n            ],\n            [\n              -115.13671875,\n              40.111688665595956\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86be","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":160852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, David L.","contributorId":55425,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160853,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10111,"text":"ofr81171 - 1981 - Measured sections of the Browns Park Formation (Miocene) in Moffat County, Colorado, 1980","interactions":[],"lastModifiedDate":"2015-09-29T12:56:11","indexId":"ofr81171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-171","title":"Measured sections of the Browns Park Formation (Miocene) in Moffat County, Colorado, 1980","docAbstract":"<p>Eight partial sections of the Browns Park Formation of Miocene age were measured in Moffat County, northwestern Colorado, during the 1980 field season, as part of a study of the stratigraphy and depositional environments of the formation. These newly measured sections are intended to complement other surface sections of the Browns Park Formation measured (Hansen, 1965) to the west in Uintah County, Utah, and measured (Buffler, 1967) or diagrammed (Kucera, 1968) to the east in, respectively, Routt and Rio Blanco Counties, Colorado.</p>\n<p>Rock samples collected, indicated parenthetically by 80-SL prefixes, are shown in the section descriptions purely for reference purposes; petrographic and analytical results will be reported in later publications. Color names with numbers are based on comparison with the rock-color chart by Goddard and others (1948).</p>\n<p>Field investigations were supported by the National Uranium Resource Evaluation (NUKE) program of the Grand Junction Office, U. S. Department of Energy, under contract No. DE-A113-78GJ01686.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81171","usgsCitation":"Luft, S.J., and Thoen, W.L., 1981, Measured sections of the Browns Park Formation (Miocene) in Moffat County, Colorado, 1980: U.S. Geological Survey Open-File Report 81-171, i, 35 p., https://doi.org/10.3133/ofr81171.","productDescription":"i, 35 p.","numberOfPages":"37","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":37960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0171/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0171/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Moffat County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-107.3181,41.0035],[-107.3178,40.9852],[-107.3177,40.9789],[-107.3175,40.9707],[-107.3171,40.9503],[-107.317,40.9412],[-107.3173,40.929],[-107.3171,40.9145],[-107.3167,40.8596],[-107.3166,40.856],[-107.3157,40.8378],[-107.3145,40.7748],[-107.3144,40.7716],[-107.3131,40.7013],[-107.3131,40.699],[-107.3128,40.6854],[-107.3126,40.6723],[-107.3121,40.6142],[-107.3119,40.5997],[-107.3688,40.5996],[-107.3683,40.5429],[-107.427,40.5427],[-107.427,40.5132],[-107.4276,40.4238],[-107.4294,40.3612],[-107.4297,40.3467],[-107.43,40.3322],[-107.4402,40.3321],[-107.4382,40.2618],[-107.4389,40.2235],[-107.4396,40.219],[-107.7614,40.2214],[-107.8192,40.2211],[-107.8758,40.2207],[-107.8945,40.2209],[-107.9144,40.221],[-107.9523,40.2213],[-107.9891,40.2217],[-108.0084,40.2218],[-108.0855,40.2224],[-108.1042,40.2225],[-108.1626,40.2225],[-108.1819,40.2226],[-108.2011,40.2227],[-108.218,40.2229],[-108.2367,40.2225],[-108.256,40.2226],[-108.2945,40.2224],[-108.3313,40.2222],[-108.3891,40.2225],[-108.4083,40.2221],[-108.4445,40.2223],[-108.5023,40.2221],[-108.5216,40.2217],[-108.5577,40.2219],[-108.5975,40.2215],[-108.6553,40.2212],[-108.6692,40.2214],[-109.051,40.2228],[-109.0514,40.2608],[-109.0514,40.2753],[-109.0514,40.2844],[-109.0513,40.292],[-109.0512,40.3206],[-109.0509,40.3583],[-109.0509,40.3874],[-109.0509,40.4041],[-109.0508,40.419],[-109.0507,40.4491],[-109.0508,40.4636],[-109.0508,40.4713],[-109.0508,40.4767],[-109.0505,40.4931],[-109.0503,40.5317],[-109.0501,40.5774],[-109.0501,40.5793],[-109.0501,40.5933],[-109.0501,40.6096],[-109.0501,40.6515],[-109.0501,40.6545],[-109.0499,40.666],[-109.0501,40.6949],[-109.0499,40.7516],[-109.0499,40.7693],[-109.0498,40.7834],[-109.0497,40.824],[-109.0493,40.8433],[-109.0493,40.8453],[-109.0492,40.8587],[-109.0488,40.8866],[-109.0489,40.9036],[-109.0487,40.9107],[-109.049,40.9268],[-109.0488,40.9479],[-109.049,41],[-108.9729,41.0002],[-108.9315,41.0001],[-108.912,41.0001],[-108.7655,41.0002],[-108.746,41.0002],[-108.6516,41.0005],[-108.6321,41.0005],[-108.5699,41.0003],[-108.3781,40.9997],[-108.3745,40.9997],[-108.3118,41],[-108.2923,41.0001],[-108.263,41.0003],[-108.2186,41.0007],[-108.1808,41.001],[-108.0007,41.0025],[-107.966,41.0028],[-107.9154,41.0029],[-107.888,41.0029],[-107.8801,41.0029],[-107.8521,41.0029],[-107.8391,41.0028],[-107.8326,41.0028],[-107.8206,41.0028],[-107.8131,41.0028],[-107.7845,41.0028],[-107.7078,41.0028],[-107.6767,41.0028],[-107.6049,41.0028],[-107.5288,41.0026],[-107.5136,41.0026],[-107.5093,41.0026],[-107.4947,41.0026],[-107.4575,41.0027],[-107.4137,41.0029],[-107.3948,41.003],[-107.3674,41.0032],[-107.3437,41.0033],[-107.3181,41.0035]]]},\"properties\":{\"name\":\"Moffat\",\"state\":\"CO\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610e4b","contributors":{"authors":[{"text":"Luft, Stanley J.","contributorId":30634,"corporation":false,"usgs":true,"family":"Luft","given":"Stanley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thoen, William L.","contributorId":105720,"corporation":false,"usgs":true,"family":"Thoen","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160834,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9891,"text":"ofr81984 - 1981 - Seismicity of the lower east rift zone of Kilauea Volcano, Hawaii, 1960 to 1980","interactions":[],"lastModifiedDate":"2022-12-28T21:26:27.630353","indexId":"ofr81984","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-984","title":"Seismicity of the lower east rift zone of Kilauea Volcano, Hawaii, 1960 to 1980","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81984","usgsCitation":"Koyanagi, R.Y., Nakata, J.S., and Tanigawa, W.R., 1981, Seismicity of the lower east rift zone of Kilauea Volcano, Hawaii, 1960 to 1980: U.S. Geological Survey Open-File Report 81-984, i, 15 p., https://doi.org/10.3133/ofr81984.","productDescription":"i, 15 p.","costCenters":[],"links":[{"id":37684,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0984/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411146,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12231.htm","linkFileType":{"id":5,"text":"html"}},{"id":141176,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0984/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -155.45,\n              19.517\n            ],\n            [\n              -155.45,\n              19.167\n            ],\n            [\n              -154.75,\n              19.167\n            ],\n            [\n              -154.75,\n              19.517\n            ],\n            [\n              -155.45,\n              19.517\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa8b8","contributors":{"authors":[{"text":"Koyanagi, Robert Y.","contributorId":52561,"corporation":false,"usgs":true,"family":"Koyanagi","given":"Robert","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":160468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakata, Jennifer S.","contributorId":18364,"corporation":false,"usgs":true,"family":"Nakata","given":"Jennifer","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":160467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tanigawa, Wilfred R.","contributorId":91102,"corporation":false,"usgs":true,"family":"Tanigawa","given":"Wilfred","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160469,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9628,"text":"ofr811109 - 1981 - Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska","interactions":[],"lastModifiedDate":"2022-04-12T17:29:54.327941","indexId":"ofr811109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1109","title":"Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska","docAbstract":"<p>The Platte River in south-central Nebraska flows generally eastward in a broad, flat valley. The river banks and many areas adjacent to the river support thick stands of cottonwood and willow trees. Brush, grass, pasture land, and cultivated fields occupy most of the remaining area. This is the habitat for many types of wildlife that live in the area or stop over in the area during annual migrations. Both sandhill cranes and whooping cranes are part of the annual migration. There is concern that water-management changes, such as surface-water diversions or ground-water withdrawals for irrigation, may alter the hydrologic environment of the wetland areas and be harmful to the wildlife habitat. In order to determine what affect changes in water management might have on ground-water levels in the wetland areas, detailed data were collected from Crane Meadows Wildlife Area, which is on an island in the Platte River near Grand Island, Nebr. Ground-water levels beneath the island respond to changes in river stage, to recharge from snowmelt and precipitation, and to evapotranspiration by riparian vegetation and from areas where the water table is close to the land surface. The data show that ground-water levels respond rapidly to changes in river stage-usually within 24 hours for distances up to 2,500 feet from the edge of the river. Thus changes in river stage due to changes in surface-water diversions will not have a long-term effect on ground-water levels. Changes in ground-water withdrawals will have the double effect of changing ground-water levels due to changes in drawdown and due to changes in river stage caused by the effects of pumping on river flow. These effects will develop slowly and be long lasting.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811109","usgsCitation":"Hurr, R.T., 1981, Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska: U.S. Geological Survey Open-File Report 81-1109, iv, 16 p., https://doi.org/10.3133/ofr811109.","productDescription":"iv, 16 p.","costCenters":[],"links":[{"id":398556,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1109/report-thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Hall County","otherGeospatial":"Mormon Island Crane Meadows wildlife area near Grand Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.37741851806639,\n              40.82160395916235\n            ],\n            [\n              -98.36797714233398,\n              40.82160395916235\n            ],\n            [\n              -98.36797714233398,\n              40.82712467108559\n            ],\n            [\n              -98.37741851806639,\n              40.82712467108559\n            ],\n            [\n              -98.37741851806639,\n              40.82160395916235\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668a6e","contributors":{"authors":[{"text":"Hurr, R. Theodore","contributorId":27023,"corporation":false,"usgs":true,"family":"Hurr","given":"R.","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":160016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9584,"text":"ofr81585 - 1981 - Clay mineralogy of Devonian shales in the Appalachian Basin","interactions":[],"lastModifiedDate":"2022-02-04T20:37:27.0429","indexId":"ofr81585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-585","title":"Clay mineralogy of Devonian shales in the Appalachian Basin","docAbstract":"<p>A study of the clay mineralogy of the Devonian black shales of the Appalachian basin was undertaken to help predict areas for potential gas resources. More than 2,100 samples from 84 drill holes representing 11 shale units were analyzed for clay mineralogy or whole—rock mineralogy or both. Approximately 1,300 samples were from drill cores and about 800 samples were from drill cuttings. Illite (2M) recrystallized during diagenesis is more or less uniformly present throughout all shale units. Chlorite formed during low grade metamorphism is least abundant in the younger units and more abundant in the older units. Illite—smectite mixed—layer clay, which supplied the material for the formation of chlorite, is most abundant in the younger units and least abundant in the older units. Illite—chlorite mixed—layer clay occurs as a trace in all shale units. Kaolinite, the only unaltered detrital clay mineral, occurs in about 25 to 30 percent of the samples. The source of the kaolinite appears to have been to the east and northeast of the basin of deposition. The color of the shale units is primarily due to the organic content; however, those shales that contain calcite are darker than those that do not for equal amounts of organic carbon. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81585","usgsCitation":"Hosterman, J.W., and Whitlow, S.I., 1981, Clay mineralogy of Devonian shales in the Appalachian Basin: U.S. Geological Survey Open-File Report 81-585, Report: iii, 170 p.; 1 Plate: 26.20 x 27.92 inches, https://doi.org/10.3133/ofr81585.","productDescription":"Report: iii, 170 p.; 1 Plate: 26.20 x 27.92 inches","costCenters":[],"links":[{"id":395483,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0585/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395482,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0585/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":373916,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0585/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Appalachian Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672b49","contributors":{"authors":[{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitlow, Sallie I.","contributorId":8854,"corporation":false,"usgs":true,"family":"Whitlow","given":"Sallie","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":159950,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32592,"text":"pp1231A - 1981 - The central Virginia volcanic-plutonic belt:  An island arc of Cambrian(?) age","interactions":[],"lastModifiedDate":"2021-12-14T23:21:34.353069","indexId":"pp1231A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"1231","chapter":"A","title":"The central Virginia volcanic-plutonic belt:  An island arc of Cambrian(?) age","docAbstract":"<p>Pre-Ordovician, probable Early Cambrian metavolcanic and somewhat younger meta-intrusive rocks form a linear belt in the central Virginia Piedmont. On the basis of the geologic and geochemical features of these rocks in the Fredericksburg area, and insofar as this area is representative of the entire belt, it is concluded that this belt constitutes an ancient island-arc sequence. The westernmost Chopawamsic Formation consists of a tholeiitic island-arc suite and associated calcalkaline metavolcanic rocks. Prior to Upper Ordovician time, low-potassic tonalitic plutons of plagiogranitic (pretectonic) and trondhjemitic (late-tectonic) affinities were intruded into the Chopawamsic terrane. The tholeiitic amphibolites of the Ta River Metamorphic Suite are considered to be an eastern, oceanward facies of the Chopawamsic Formation.</p><p> The James Run Formation of Maryland is probably a northern lateral equivalent of the central Virginia volcanic-plutonic belt. It may have formed as part of the ancient Virginia belt or along a penecontemporaneous but independent volcanic arc. The metavolcanic rocks and associated plutons of the Carolina slate belt in the southeast Piedmont are considered to have formed independently of the central Virginia volcanic-plutonic belt and perhaps in a different tectonic environment.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the geology of the Virginia Piedmont","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1231A","usgsCitation":"Pavlides, L., 1981, The central Virginia volcanic-plutonic belt:  An island arc of Cambrian(?) age: U.S. Geological Survey Professional Paper 1231, iv, 34 p., https://doi.org/10.3133/pp1231A.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":392930,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74472.htm"},{"id":60453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1231a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1231a/report-thumb.jpg"}],"country":"United States","state":"Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.875,\n              38\n            ],\n            [\n              -77.375,\n              38\n            ],\n            [\n              -77.375,\n              38.5\n            ],\n            [\n              -77.875,\n              38.5\n            ],\n            [\n              -77.875,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669561","contributors":{"authors":[{"text":"Pavlides, Louis","contributorId":79444,"corporation":false,"usgs":true,"family":"Pavlides","given":"Louis","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":208748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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