No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1313B","usgsCitation":"Froelich, A., and Leavy, B.D., 1982, Map showing mineral resources of the Culpeper Basin, Virginia and Maryland availability and planning for future needs: U.S. Geological Survey IMAP 1313, 1 Plate: 31.49 × 48.99 inches, https://doi.org/10.3133/i1313B.","productDescription":"1 Plate: 31.49 × 48.99 inches","costCenters":[],"links":[{"id":255379,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1313b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392113,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9140.htm"},{"id":255380,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1313b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255381,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1313b/report-thumb.jpg"}],"scale":"125000","country":"United States","state":"Maryland, Virginia","otherGeospatial":"Culpeper basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.28,\n 38.205\n ],\n [\n -77.218,\n 38.205\n ],\n [\n -77.218,\n 39.489\n ],\n [\n -78.28,\n 39.489\n ],\n [\n -78.28,\n 38.205\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a05c","contributors":{"authors":[{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":272890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leavy, B. D.","contributorId":38991,"corporation":false,"usgs":true,"family":"Leavy","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":272891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8193,"text":"ofr82681 - 1982 - Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr82681","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-681","title":"Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana","docAbstract":"The Cook Creek area of the Ashland coal field contains large reserves of Federally owned coal that have been identified for potential lease sale. A hydrologic study has been conducted in the potential lease area to describe existing hydrologic systems and to assess potential impacts of surface coal mining on local water resources. Hydrogeologic data collected from wells, springs, and drill holes indicate that shallow aquifers exist within the Tongue River Member of the Fort Union Formation (Paleocene age) and within valley alluvium (Pleistocene and Holocene age). Shallow aquifers within the Tonge River Member include coal beds, clinker, and lenses of sandstone and siltstone. The Knobloch coal bed, a principal shallow aquifer used for livestock watering in the area, averages about 55 feet in thickness and is completely saturated throughout most of its extent. Coarse alluvial deposits are the most productive aquifers and are a major source of stock water in the Cook Creek basin. Surface-water resources are limited to the upstream reach part of Cook Creek, which flows intermittently. The downstream reach part of Cook Creek, plus all other small drainages that originate in the study area, are ephemeral. Mining of the Knoblock and Sawyer coal beds would remove two alluvial springs, one bedrock spring, and two wells, which are all used for watering of livestock. The potentiometric surface within the Knobloch coal aquifer and the alluvial aquifer in the downstream part of the Cook Creek basin would be lowered during mining. Lowered water levels in these aquifers might substantially affect water levels in five wells outside the mine boundary. After mining, the alluvial aquifer downgradient from the mine area might show a long-term degradation in water quality as a result of leaching of soluble salts from overburden materials used to backfill mine pits. Although mining would alter the existing hydrologic systems and remove several springs and shallow wells, alternative ground-water supplies are available that could be developed to replace those lost by mining. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82681","usgsCitation":"Cannon, M.R., 1982, Potential effects of surface coal mining on the hydrology of the Cook Creek area, Ashland coal field, southeastern Montana: U.S. Geological Survey Open-File Report 82-681, 34 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82681.","productDescription":"34 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0681/report-thumb.jpg"},{"id":35805,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0681/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35806,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0681/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0681/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683848","contributors":{"authors":[{"text":"Cannon, M. R.","contributorId":99140,"corporation":false,"usgs":true,"family":"Cannon","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8186,"text":"ofr82617I - 1982 - Coordinates for and analytical values of 30 rock, and 7 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 00'00\"DP and 46 degrees 30'00\" N., and the longitudes of 112 degrees 00'00\" and 1","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82617I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-617","chapter":"I","title":"Coordinates for and analytical values of 30 rock, and 7 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 00'00\"DP and 46 degrees 30'00\" N., and the longitudes of 112 degrees 00'00\" and 1","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82617I","usgsCitation":"Campbell, W.L., McDanal, S., and Hopkins, R.T., 1982, Coordinates for and analytical values of 30 rock, and 7 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 00'00\"DP and 46 degrees 30'00\" N., and the longitudes of 112 degrees 00'00\" and 1: U.S. Geological Survey Open-File Report 82-617, 8 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82617I.","productDescription":"8 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":140382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0617i/report-thumb.jpg"},{"id":35798,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0617i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6864ba","contributors":{"authors":[{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":157303,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, R. T. Jr.","contributorId":70743,"corporation":false,"usgs":true,"family":"Hopkins","given":"R.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":157302,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8184,"text":"ofr82617D - 1982 - Coordinates for and analytical values of 21 rock, 158 stream-sediment and soil, and 91 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 30'00\" and 47 degrees 00'00\" N., and the longitudes of 112 degrees 30'00\" and 113 degrees 00'00\" W.","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82617D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-617","chapter":"D","title":"Coordinates for and analytical values of 21 rock, 158 stream-sediment and soil, and 91 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 30'00\" and 47 degrees 00'00\" N., and the longitudes of 112 degrees 30'00\" and 113 degrees 00'00\" W.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82617D","usgsCitation":"Campbell, W.L., McDanal, S., and Hopkins, R.T., 1982, Coordinates for and analytical values of 21 rock, 158 stream-sediment and soil, and 91 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 30'00\" and 47 degrees 00'00\" N., and the longitudes of 112 degrees 30'00\" and 113 degrees 00'00\" W.: U.S. Geological Survey Open-File Report 82-617, 26 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82617D.","productDescription":"26 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":140380,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0617d/report-thumb.jpg"},{"id":35796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0617d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4814e4b07f02db4dac6d","contributors":{"authors":[{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":157297,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, R. T. Jr.","contributorId":70743,"corporation":false,"usgs":true,"family":"Hopkins","given":"R.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":157296,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8203,"text":"ofr82623 - 1982 - User's manual for RASSMP","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr82623","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-623","title":"User's manual for RASSMP","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82623","usgsCitation":"Carlson, C., 1982, User's manual for RASSMP: U.S. Geological Survey Open-File Report 82-623, 11 p. :map ;28 cm., https://doi.org/10.3133/ofr82623.","productDescription":"11 p. :map ;28 cm.","costCenters":[],"links":[{"id":140219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0623/report-thumb.jpg"},{"id":35812,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603ddc","contributors":{"authors":[{"text":"Carlson, Carl A.","contributorId":102877,"corporation":false,"usgs":true,"family":"Carlson","given":"Carl A.","affiliations":[],"preferred":false,"id":157334,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8183,"text":"ofr82617C - 1982 - Coordinates for and analytical values of 109 rock, 377 stream sediment and soil, and 237 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 30'00\" and 47 degrees 00'00\" N., and the longitu","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82617C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-617","chapter":"C","title":"Coordinates for and analytical values of 109 rock, 377 stream sediment and soil, and 237 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 30'00\" and 47 degrees 00'00\" N., and the longitu","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82617C","usgsCitation":"Campbell, W.L., McDanal, S., and Hopkins, R.T., 1982, Coordinates for and analytical values of 109 rock, 377 stream sediment and soil, and 237 panned-concentrate samples included in the Butte 1 degree by 2 degrees Quadrangle between the latitudes of 46 degrees 30'00\" and 47 degrees 00'00\" N., and the longitu: U.S. Geological Survey Open-File Report 82-617, 56 p. ;28 cm., https://doi.org/10.3133/ofr82617C.","productDescription":"56 p. ;28 cm.","costCenters":[],"links":[{"id":140654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0617c/report-thumb.jpg"},{"id":35795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0617c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686498","contributors":{"authors":[{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":157294,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hopkins, R. T. Jr.","contributorId":70743,"corporation":false,"usgs":true,"family":"Hopkins","given":"R.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":157293,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30236,"text":"wri8119 - 1982 - Water-quality characteristics of six small, semiarid watersheds in the Green River coal region of Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri8119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-19","title":"Water-quality characteristics of six small, semiarid watersheds in the Green River coal region of Colorado","docAbstract":"Analysis of major and trace constituents in streams flowing through six semiarid watersheds indicates that the stream chemistry is characterized by saturation with respect to common carbonate minerals (calcium, magnesium, iron, manganese, and lead). The solubility of the carbonate minerals may be a major control on the absolute and relative concentrations of calcium, magnesium, bicarbonate, iron, manganese, and lead; however, other mechanisms probably control the concentrations of cadmium and zinc. Statistical analyses indicate that the mean concentrations of the major ions in the two climatic areas studied are significantly (P=0.05) different from one another, with larger mean concentrations in the more arid area. Trace-metal concentrations were similar from one area to another and indistinguishable from site to site (P=0.05) for lead, cadmium, and zinc. Linear regressions of major ion concentration to specific conductance are similar in both areas for sodium, bicarbonate, sulfate, and chloride. Results of the study may be useful in providing a first approximation of stream chemistry in other watersheds with the same geologic setting, determining watersheds with similar geochemical controls, and determining future changes in stream chemistry in the watersheds studied. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8119","usgsCitation":"Turk, J.T., and Parker, R.S., 1982, Water-quality characteristics of six small, semiarid watersheds in the Green River coal region of Colorado: U.S. Geological Survey Water-Resources Investigations Report 81-19, iv, 96 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8119.","productDescription":"iv, 96 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0019/report-thumb.jpg"},{"id":59011,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859f7","contributors":{"authors":[{"text":"Turk, John T.","contributorId":53363,"corporation":false,"usgs":true,"family":"Turk","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":202908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Randolph S.","contributorId":58638,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8179,"text":"ofr82723 - 1982 - Catalog of available clear mylar templates used to determine latitude and longitude of sample localities between the latitudes of 51 degrees 00' and 71 degrees 30' at the scale of 1:63,360 and between the latitude of 49 degrees 00'00\" north or south at the scale of 1:250,000","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82723","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-723","title":"Catalog of available clear mylar templates used to determine latitude and longitude of sample localities between the latitudes of 51 degrees 00' and 71 degrees 30' at the scale of 1:63,360 and between the latitude of 49 degrees 00'00\" north or south at the scale of 1:250,000","docAbstract":"The present use of electro-mechanical plotting of sample points can give rise to location errors, particularly when map scale changes are involved, unless careful control is maintained. The following catalog of computer-generated mylar templates, with plots of latitude and longitude (longitudes equidistant north to south), sufficient to cover the latitudes between 49?00'00'' and 71?30'00'' N. or S., will help facilitate the plotting of points when there is a map scale change for two different map scales (1:63,360 and 1:250,000). Using the template overlays (available as individual page numbers in Open-File Report 82-724--xerographic clear film overlays from U.S. Geological Survey Open-File Services Section, Branch of Distribution, USGS, Box 25425, Denver, Colorado 80225, telephone (303) 234-5888), the point plotted on a composite final copy may be checked against field maps and notes when only degrees latitude and longitude are given.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82723","usgsCitation":"Campbell, W.L., and VanTrump, G., 1982, Catalog of available clear mylar templates used to determine latitude and longitude of sample localities between the latitudes of 51 degrees 00' and 71 degrees 30' at the scale of 1:63,360 and between the latitude of 49 degrees 00'00\" north or south at the scale of 1:250,000: U.S. Geological Survey Open-File Report 82-723, 4 p. ;28 cm., https://doi.org/10.3133/ofr82723.","productDescription":"4 p. ;28 cm.","costCenters":[],"links":[{"id":140633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0723/report-thumb.jpg"},{"id":35791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0723/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef99d","contributors":{"authors":[{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"VanTrump, George Jr.","contributorId":54193,"corporation":false,"usgs":true,"family":"VanTrump","given":"George","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":157285,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8127,"text":"ofr82905 - 1982 - Predevelopment flow in the Tertiary limestone aquifer, southeastern United States: A regional analysis from digital modeling","interactions":[],"lastModifiedDate":"2022-06-27T20:38:26.898567","indexId":"ofr82905","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-905","title":"Predevelopment flow in the Tertiary limestone aquifer, southeastern United States: A regional analysis from digital modeling","docAbstract":"The Tertiary limestone aquifer of the southeastern United States is a sequence of carbonate rocks that underlies all of Florida, south Georgia, and adjacent parts of Alabama and South Carolina. It is the principal source of municipal, industrial, and agricultural water supply in south Georgia and most of Florida. The aquifer, known as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina, includes various carbonate units of Paleocene to early Miocene age that are hydraulically connected in varying degrees. Very locally, in the Brunswick, Ga., area, a thin sequence of rocks of Late Cretaceous age is part of the system. In general the aquifer consists of either one vertically continuous permeable zone or two major permeable zones separated by a less permeable unit of highly variable water-transmitting characteristics. Aquifer conditions range from unconfined to confined depending upon whether the clayey Miocene and younger rocks that form the upper confining unit have been removed by erosion.\r\n\r\nDigital model simulation shows that prior to development, most flow in the aquifer occurred in the unconfined and thinly confined areas of northwest and central Florida and southwest Georgia. Springs in these areas are visible evidence of major flow activity. Spring discharge to streams accounted for about 90 percent of the average predevelopment discharge from the regional aquifer. About 18,100 cubic feet per second left the limestone aquifer as spring flow, and 2,500 cubic feet per second discharged as diffuse upward leakage from the confined areas where the vertical head gradient was upward. Most of the 20,600 cubic feet per second recharge necessary to balance total discharge entered the limestone aquifer in the unconfined and thinly confined areas. Because the areas of greatest recharge before development were near the areas of highest discharge, flow paths were generally short. Much water went into and out of the limestone quickly. A very active shallow flow system at the expense of deep circulation has evolved in unconfined and sligptly confined spring areas. Transmissivities commonly exceed 1,000,000 feet squared per day.\r\n\r\nIn contrast, predevelopment flow in the aquifer in the tightly confined areas of southeast and coastal Georgia, far west Florida, and in south Florida was sluggish. In these areas the aquifer is overlain by several hundred feet of sand and clay, except for the outcrop areas along the updip limit of the aquifer. This thick overburden severely retards discharge from the aquifer, causing lethargic flow. Large-discharge springs are nonexistent. The south Florida and southeast Georgia segments of the flow system, which taken together occupy about 50 percent of the regional system, only accounted for slightly more than 3 percent of the predevelopment regional limestone discharge. Transmissivities are on the average lower (generally less than 250,000 feet squared per day) than those in areas of high-flow activity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82905","usgsCitation":"Bush, P.W., 1982, Predevelopment flow in the Tertiary limestone aquifer, southeastern United States: A regional analysis from digital modeling: U.S. Geological Survey Open-File Report 82-905, v, 41 p., https://doi.org/10.3133/ofr82905.","productDescription":"v, 41 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":35732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0905/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402563,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35647.htm","linkFileType":{"id":5,"text":"html"}},{"id":142050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0905/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,24 ], [ -89,34 ], [ -80,34 ], [ -80,24 ], [ -89,24 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea30","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5802,"text":"pp1246 - 1982 - Chemical weathering of basalts and andesites; evidence from weathering rinds","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"pp1246","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"1246","title":"Chemical weathering of basalts and andesites; evidence from weathering rinds","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1246","usgsCitation":"Colman, S.M., 1982, Chemical weathering of basalts and andesites; evidence from weathering rinds: U.S. Geological Survey Professional Paper 1246, 51 p., https://doi.org/10.3133/pp1246.","productDescription":"51 p.","costCenters":[],"links":[{"id":117722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1246/report-thumb.jpg"},{"id":32486,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1246/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf0d","contributors":{"authors":[{"text":"Colman, Steven M.","contributorId":6439,"corporation":false,"usgs":true,"family":"Colman","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":151604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30095,"text":"wri824063 - 1982 - Water-quality assessment of White River between Lake Sequoyah and Beaver Reservoir, Washington County, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"wri824063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4063","title":"Water-quality assessment of White River between Lake Sequoyah and Beaver Reservoir, Washington County, Arkansas","docAbstract":"The Arkansas Department of Pollution Control and Ecology and U.S. Geological Survey conducted a water quality assessment be made of the White River and, that a steady-state digital model be calibrated and used as a tool for simulating changes in nutrient loading. The city of Fayetteville 's wastewater-treatment plant is the only point-source discharger of waste effluent to the river. Data collected during synoptic surveys downstream from the wastewater-treatment plan indicate that temperature, dissolved oxygen, dissolved solids, un-ionized ammonia, total phosphorus, and floating solids and depositable materials did not meet Arkansas stream standards. Nutrient loadings below the treatment plant result in dissolved oxygen concentrations as low as 0.0 milligrams per liter. Biological surveys found low macroinvertebrate organism diversity and numerous dead fish. Computed dissolved oxygen deficits indicate that benthic demands are the most significant oxygen sinks in the river downstream from the wastewater-treatment plant. Benthic oxygen demands range from 2.8 to 11.0 grams per meter squared per day. Model projections indicate that for 7-day, 10-year low-flow conditions and water temperature of 29 degrees Celsius, daily average dissolved oxygen concentrations of 6.0 milligrams per liter can be maintained downstream from the wastewater-treatment plant if effluent concentrations of ultimate carbonaceous biochemical oxygen demand and ammonia nitrogen are 7.5 (5.0 5-day demand) and 2 milligrams per liter respectively. Model sensitivity analysis indicate that dissolved oxygen concentrations were most sensitive to changes in stream temperature. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824063","usgsCitation":"Terry, J.E., Morris, E.E., and Bryant, C.T., 1982, Water-quality assessment of White River between Lake Sequoyah and Beaver Reservoir, Washington County, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 82-4063, 113 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824063.","productDescription":"113 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":119197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4063/report-thumb.jpg"},{"id":58909,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4063/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58910,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4063/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58911,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e714a","contributors":{"authors":[{"text":"Terry, J. E.","contributorId":87930,"corporation":false,"usgs":true,"family":"Terry","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, E. E.","contributorId":93493,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bryant, C. T.","contributorId":7263,"corporation":false,"usgs":true,"family":"Bryant","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":202667,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":65650,"text":"i1412 - 1982 - Controlled photomosaic of the Syrtis Major Southeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1412","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1412","subseriesTitle":"NONE","title":"Controlled photomosaic of the Syrtis Major Southeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1412","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Controlled photomosaic of the Syrtis Major Southeast Quadrangle of Mars: U.S. Geological Survey IMAP 1412, 1 map ;40 x 60 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1412.","productDescription":"1 map ;40 x 60 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":114999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1412/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":115000,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1412/plate-1.pdf","size":"6471","linkFileType":{"id":1,"text":"pdf"}},{"id":189339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1412/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6866ee","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42359,"text":"ofr82141 - 1982 - Preliminary map showing reconnaissance photogeologic interpretation of SLAR imagery of the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska","interactions":[],"lastModifiedDate":"2022-04-04T21:26:03.368781","indexId":"ofr82141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-141","title":"Preliminary map showing reconnaissance photogeologic interpretation of SLAR imagery of the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82141","usgsCitation":"Albert, N., 1982, Preliminary map showing reconnaissance photogeologic interpretation of SLAR imagery of the Bristol Bay, Ugashik, and Karluk quadrangles, Alaska: U.S. Geological Survey Open-File Report 82-141, 5 Plates: 46.69 × 38.50 inches or smaller, https://doi.org/10.3133/ofr82141.","productDescription":"5 Plates: 46.69 × 38.50 inches or smaller","costCenters":[],"links":[{"id":175673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":398074,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13668.htm"},{"id":20457,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0141/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20456,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0141/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20455,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0141/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20454,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0141/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20453,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0141/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Bristol Bay, Ugashik, and Karluk quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -158.583,\n 57\n ],\n [\n -155,\n 57\n ],\n [\n -155,\n 58\n ],\n [\n -158.583,\n 58\n ],\n [\n -158.583,\n 57\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf42","contributors":{"authors":[{"text":"Albert, Nairn","contributorId":95950,"corporation":false,"usgs":true,"family":"Albert","given":"Nairn","email":"","affiliations":[],"preferred":false,"id":226345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30206,"text":"wri824062 - 1982 - Downstream effects of reservoir releases to the Potomac River from Luke, Maryland, to Washington, D.C.","interactions":[],"lastModifiedDate":"2022-01-11T20:12:39.281543","indexId":"wri824062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4062","title":"Downstream effects of reservoir releases to the Potomac River from Luke, Maryland, to Washington, D.C.","docAbstract":"A digital computer flow-routing model was developed for the Potomac River in order to determine the downstream effects of flow releases from the Bloomington and Savage River Reservoirs. Both reservoirs are located above Luke, Maryland approximately 230 miles upstream from Washington, D. C. The downstream effects of reservoir releases were determined by using the unit-response method of flow routing implemented by a diffusion analogy. Results are in the form of unit response coefficients which are used to route flows downstream from Luke. A 24-hour sustained reservoir release input at Luke will result in 35 percent of the flow arriving at Washington, D.C., during the 4th day after the beginning of the release, followed by 61 percent and 4 percent arriving on the 5th and 6th days, respectively. For a 7-day sustained reservoir release, 47 percent of the flow will arrive during the 1st week, and 53 percent will arrive the 2d week. Two methods were used to estimate the amount of water that goes into channel storage between Luke and Washington, D.C., during sustained reservoir releases. Analysis of the flow-routing results indicates channel storage is equivalent to the volume of water releases over a 3.7-day period. Using channel geometry relationships, that volume is equal to 3.2 days ' release. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824062","usgsCitation":"Trombley, T.J., 1982, Downstream effects of reservoir releases to the Potomac River from Luke, Maryland, to Washington, D.C.: U.S. Geological Survey Water-Resources Investigations Report 82-4062, vi, 41 p., https://doi.org/10.3133/wri824062.","productDescription":"vi, 41 p.","costCenters":[],"links":[{"id":394207,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35580.htm"},{"id":58995,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4062/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4062/report-thumb.jpg"}],"country":"United States","state":"Maryland, Washington D.C.","otherGeospatial":"Potomac River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.376220703125,\n 38.79690830348427\n ],\n [\n -76.5966796875,\n 38.79690830348427\n ],\n [\n -76.5966796875,\n 39.715638134796336\n ],\n [\n -79.376220703125,\n 39.715638134796336\n ],\n [\n -79.376220703125,\n 38.79690830348427\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629db7","contributors":{"authors":[{"text":"Trombley, T. J.","contributorId":75161,"corporation":false,"usgs":true,"family":"Trombley","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8139,"text":"ofr82491 - 1982 - Geochemical reconnaissance for uranium occurrences in the Notch Peak intrusive area, House Range, Millard County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82491","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-491","title":"Geochemical reconnaissance for uranium occurrences in the Notch Peak intrusive area, House Range, Millard County, Utah","docAbstract":"Samples collected from the contact metamorphic zone of the Notch Peak intrusive area, House Range, Millard County, Utah, indicate the occurrence of low-grade uranium and thorium ore. Maximum abundances in the altered mineralized rocks in the contact zone are 450 ppm uranium and 480 ppm thorium. Interpretation of factor analysis of the spectrochemical and delayed neutron analytical data suggests the presence of five geological factors which account for 82 percent of element covariance of 34 elements in 61 samples. The factors are identified as (1) limestone source rock reactions; (2) monzonite source rock reactions; (3) hydrothermal element group 1; (4) rare earth group; and (5) hydrothermal element group 2. The last factor effects the distribution of, primarily, beryllium, uranium, copper, molybdenum, tungsten, niobium, and secondarily, thorium, tin, and zinc; it is identified as the prime mineralization factor. \r\n\r\nThe Notch Peak intrusive area has been a tungsten producing area since before the 1940's and the location of small-scale gold placer operations. This reconnaissance study was a 'follow-up' of uranium anomaly data which were developed during the U.S. Dept. of Energy National Uranium Resource Evaluation (NURE) program in 1978-80.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82491","usgsCitation":"Cadigan, R.A., and Robinson, K., 1982, Geochemical reconnaissance for uranium occurrences in the Notch Peak intrusive area, House Range, Millard County, Utah: U.S. Geological Survey Open-File Report 82-491, iii, 57 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82491.","productDescription":"iii, 57 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0491/report-thumb.jpg"},{"id":35742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0491/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade91","contributors":{"authors":[{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":157214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Keith","contributorId":80277,"corporation":false,"usgs":true,"family":"Robinson","given":"Keith","affiliations":[],"preferred":false,"id":157215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8265,"text":"ofr82425 - 1982 - Vegetation of sandy intertidal flats, Willapa Bay, Washington; summer, 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr82425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-425","title":"Vegetation of sandy intertidal flats, Willapa Bay, Washington; summer, 1978","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82425","usgsCitation":"Chin, J.L., and Hill, G.W., 1982, Vegetation of sandy intertidal flats, Willapa Bay, Washington; summer, 1978: U.S. Geological Survey Open-File Report 82-425, 24 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82425.","productDescription":"24 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0425/report-thumb.jpg"},{"id":35878,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0425/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025f1","contributors":{"authors":[{"text":"Chin, J. L.","contributorId":13625,"corporation":false,"usgs":true,"family":"Chin","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, G. W.","contributorId":85551,"corporation":false,"usgs":true,"family":"Hill","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157452,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8140,"text":"ofr821130 - 1982 - Mineralization and other geologic factors related to the Morrison Formation in particular the northern two-thirds of the Colorado Plateau region; basic data and factor-analysis results","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr821130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1130","title":"Mineralization and other geologic factors related to the Morrison Formation in particular the northern two-thirds of the Colorado Plateau region; basic data and factor-analysis results","docAbstract":"A vanadium-mercury mineralization factor and five other significant geologic factors were determined by multivariate factor analysis of data for Morrison Formation rock samples from the Colorado Plateau region. The data presented in the report were obtained from an agglomeration of 876 samples which yielded a correlation matrix of 44 variables. The variables consisted of geochemical, petrographic, and geographic location parameters. \r\n\r\nMineralization factor scores demonstrate the relative intensity of mineralization in rock samples collected in and around uranium-vanadium ore deposits. \r\n\r\nThe factors affecting composition and texture of the rocks identified from the analysis are: (1) metalliferous mudstones; (2) interstitial carbonate cements; (3) competing sources of different composition; (4) heavy mineral sources; (5) vanadium mineralization; and (6) regional and stratigraphic sampling bias.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821130","usgsCitation":"Cadigan, R.A., 1982, Mineralization and other geologic factors related to the Morrison Formation in particular the northern two-thirds of the Colorado Plateau region; basic data and factor-analysis results: U.S. Geological Survey Open-File Report 82-1130, 176 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr821130.","productDescription":"176 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142133,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1130/report-thumb.jpg"},{"id":35743,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ef6","contributors":{"authors":[{"text":"Cadigan, Robert Allen","contributorId":27051,"corporation":false,"usgs":true,"family":"Cadigan","given":"Robert","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":157216,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8252,"text":"ofr8340 - 1982 - Activities in Idaho; status of projects, fiscal years 1982-83","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr8340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"83-40","title":"Activities in Idaho; status of projects, fiscal years 1982-83","docAbstract":"Twenty-three projects were conducted by the Water Resources Division of the U.S. Geological Survey in Idaho during FY 's (fiscal year) 1982-83. These projects were done in cooperation with seven State and local and nine federal agencies. State and local cooperative funding amounted to $566,123 in FY 1982 and $570,000 (projected monies) in FY 1983; Federal funding amounted to $2,083,748 in FY 1982 and $1,656,494 (projected monies) in FY 1983. Eighty-three persons were employed as of September, FY 1982--40 full time and 43 other than full time. Sixty-five persons were employed as of October, FY 1983--35 full time and 30 other than full time. In addition, the Water Resources Division maintains a project office at the Idaho National Engineering Laboratory. Work there is done in cooperation with the U.S. Department of Energy, which provides most of the funding. Some Federal funds are provided for special projects. Projects other than continuing programs for collection of hydrologic data included flood-mapping studies, geothermal-resource investigations, groundwater-quality assessments, basin-and region-wide water-resource investigations , river quality-of-water monitoring studies, volcanic-ash-related studies, groundwater trends and stream gaging-program evaluations, river erosion and sediment-transport studies, water-budget and groundwater-use determinations, and a sole-source aquifer appraisal. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8340","usgsCitation":"Channel, L.K., 1982, Activities in Idaho; status of projects, fiscal years 1982-83: U.S. Geological Survey Open-File Report 83-40, 48 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr8340.","productDescription":"48 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0040/report-thumb.jpg"},{"id":35868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544759","contributors":{"authors":[{"text":"Channel, Linda K. (compiler)","contributorId":35734,"corporation":false,"usgs":true,"family":"Channel","given":"Linda","suffix":"(compiler)","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":157427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8361,"text":"ofr82103 - 1982 - Quality of surface water at selected sites in the Suwannee River basin, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr82103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-103","title":"Quality of surface water at selected sites in the Suwannee River basin, Florida","docAbstract":"This report presents the results of analyses of water-quality samples collected from 14 surface-water sites in the Suwannee River basin in Florida from January through December 1980. The analyses of samples collected routinely included: nutrients, total organic carbon, and 5-day biochemical oxygen demand, bimonthly; and trace metals, annually. The array of constituents sampled was expanded in October 1978 at three of the original nine stations to provide quality-of-water information for streams draining an industrial area: Rocky Creek near Belmont, Hunter Creek near Belmont, and Swift Creek at Facil. Data collected at these three sites now include: major chemical constituents, six times per year: radium-226, two times per year; and trace metals, one time per year. These constituents are determined in addition to nutrients, total organic carbon, and bio-chemical oxygen demand which continue to be analyzed six times per year. All results of analyses of the water-quality samples collected from January through December 1980 remained within, or near, previously measured ranges and water-quality fluctuations were similar to those noted from data collected since 1971. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82103","usgsCitation":"Coffin, J., 1982, Quality of surface water at selected sites in the Suwannee River basin, Florida: U.S. Geological Survey Open-File Report 82-103, x, 117 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82103.","productDescription":"x, 117 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":140310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0103/report-thumb.jpg"},{"id":35934,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db640ffd","contributors":{"authors":[{"text":"Coffin, J.E.","contributorId":75913,"corporation":false,"usgs":true,"family":"Coffin","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":157596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42378,"text":"ofr82610 - 1982 - Reconnaissance geology of the Jabal Shaqran Quadrangle, sheet 17/44 B, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr82610","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-610","title":"Reconnaissance geology of the Jabal Shaqran Quadrangle, sheet 17/44 B, Kingdom of Saudi Arabia","docAbstract":"The Jabal Shaqran quadrangle lies in the southeastern Asir province, mostly within the westernmost part of the Rub al Khali desert, and is largely covered by Quaternary deposits. Proterozoic crystalline rocks are exposed as inselbergs or rock pediment surfaces along the western border of the quadrangle. The crystalline basement is metavolcanic rock intruded by plutonic to hypabyssal rocks consisting of diorite and gabbro, biotite tonalite gneiss, biotite-hornblende monzogranite, biotite-sodic amphibole granite, and syenogranite to quartz syenite, listed in the inferred order of emplacement. Rhyolite-dacite fels, associated with andesitic to basaltic metavolcanic flow rocks and minor amphibolite, is interpreted to have resulted from metasomatic alteration of the flow rocks during emplacement of granitic plutons. \r\n\r\nThe Wajid Sandstone, of Cambrian to Ordovician age, is largely a coarse-grained quartz arenite with pebbly phases; common crossbedds indicate north-northwest to north-northeast directions of sand transport. Beds are cemented by iron oxide, carbonate, and minor quartz. The Wajid Sandstone is exposed only in the northwestern and northern parts of the quadrangle. \r\n\r\nQuaternary deposits record a climate that became increasingly more arid. They include Holocene and Pleistocene(?) alluvial and fluvial deposits of sand, gravel, and silt, minor carbonate crusts, and eolian sand and silt. Gravel terraces and gravel plains less than 10 m above the present major wadi channels are widespread and commonly are overlain by marly silt along the wadis. Between major wadis, which discharge into the Rub al Khali basin, gravel-topped surfaces are partly covered by a complex of low, sinuous, discontinuous, generally northwest trending transverse sand dunes. Normal to this trend, higher and more extensive linear dunes and dune complexes, including seif (irq) dunes as high as 50 m, have encroached southwestward. The transverse and linear dunes may represent two stages of advance separated by a pluvial cycle. Studies of aerial photographs indicate that the dunes have not changed appreciably in shape or size between 1951 and 1959, although some seif dunes have advanced their leading edges 15 to 25 m. \r\n\r\nNo potentially economic mineral resources other than sand and gravel were found.","language":"ENGLISH","doi":"10.3133/ofr82610","usgsCitation":"Sable, E.G., 1982, Reconnaissance geology of the Jabal Shaqran Quadrangle, sheet 17/44 B, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-610, 1 map :photocopy ;56 x 53 cm., on sheet 70 x 78 cm. +1 text (iii, 19 p. ill. ; 28 cm.), https://doi.org/10.3133/ofr82610.","productDescription":"1 map :photocopy ;56 x 53 cm., on sheet 70 x 78 cm. +1 text (iii, 19 p. ill. ; 28 cm.)","costCenters":[],"links":[{"id":136880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0610/report-thumb.jpg"},{"id":80142,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0610/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0610/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640949","contributors":{"authors":[{"text":"Sable, Edward G.","contributorId":51273,"corporation":false,"usgs":true,"family":"Sable","given":"Edward","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":226368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30380,"text":"wri8115 - 1982 - Digital-transport model study of the potential effects of coal-resource development on the ground-water system in the Yampa River Basin, Moffat and Routt Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:09:08","indexId":"wri8115","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-15","title":"Digital-transport model study of the potential effects of coal-resource development on the ground-water system in the Yampa River Basin, Moffat and Routt Counties, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8115","usgsCitation":"Warner, J.W., and Dale, R.H., 1982, Digital-transport model study of the potential effects of coal-resource development on the ground-water system in the Yampa River Basin, Moffat and Routt Counties, Colorado: U.S. Geological Survey Water-Resources Investigations Report 81-15, vi, 70 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8115.","productDescription":"vi, 70 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0015/report-thumb.jpg"},{"id":59161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0015/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ad8b","contributors":{"authors":[{"text":"Warner, James W.","contributorId":106119,"corporation":false,"usgs":true,"family":"Warner","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":203155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dale, Robert H.","contributorId":85190,"corporation":false,"usgs":true,"family":"Dale","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":203154,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42606,"text":"ofr82394 - 1982 - Preliminary geologic map of the Patterson Quadrangle, Stanislaus County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:01","indexId":"ofr82394","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-394","title":"Preliminary geologic map of the Patterson Quadrangle, Stanislaus County, California","language":"ENGLISH","doi":"10.3133/ofr82394","usgsCitation":"Dibblee, T.W., 1982, Preliminary geologic map of the Patterson Quadrangle, Stanislaus County, California: U.S. Geological Survey Open-File Report 82-394, 1 map ;58 x 46 cm., https://doi.org/10.3133/ofr82394.","productDescription":"1 map ;58 x 46 cm.","costCenters":[],"links":[{"id":101911,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_174.htm","linkFileType":{"id":5,"text":"html"},"description":"174"},{"id":168024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80379,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0394/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae0e","contributors":{"authors":[{"text":"Dibblee, T. W. Jr.","contributorId":95445,"corporation":false,"usgs":true,"family":"Dibblee","given":"T.","suffix":"Jr.","middleInitial":"W.","affiliations":[],"preferred":false,"id":226811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47653,"text":"wri824028 - 1982 - Map showing total thickness of the Judith River Formation, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"wri824028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4028","title":"Map showing total thickness of the Judith River Formation, Montana","language":"ENGLISH","doi":"10.3133/wri824028","usgsCitation":"Feltis, R.D., 1982, Map showing total thickness of the Judith River Formation, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4028, 1 map ; 45 x 68 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/wri824028.","productDescription":"1 map ; 45 x 68 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":169625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84565,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660f35","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235964,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47658,"text":"wri824033 - 1982 - Map showing total thickness of the Eagle Sandstone and Telegraph Creek Formation, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"wri824033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4033","title":"Map showing total thickness of the Eagle Sandstone and Telegraph Creek Formation, Montana","language":"ENGLISH","doi":"10.3133/wri824033","usgsCitation":"Feltis, R.D., 1982, Map showing total thickness of the Eagle Sandstone and Telegraph Creek Formation, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4033, 1 map ; 45 x 68 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/wri824033.","productDescription":"1 map ; 45 x 68 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":169630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84570,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4033/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660e8d","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235969,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}