{"pageNumber":"5223","pageRowStart":"130550","pageSize":"25","recordCount":184617,"records":[{"id":28741,"text":"wri824071 - 1983 - Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4071","title":"Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824071","usgsCitation":"Minges, D., 1983, Selected hydrologic characteristics of the South Platte River in the vicinity of the proposed Narrows Reservoir near Fort Morgan, Colorado: U.S. Geological Survey Water-Resources Investigations Report 82-4071, iv, 25 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824071.","productDescription":"iv, 25 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4071/report-thumb.jpg"},{"id":57593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8c07","contributors":{"authors":[{"text":"Minges, D.R.","contributorId":31387,"corporation":false,"usgs":true,"family":"Minges","given":"D.R.","affiliations":[],"preferred":false,"id":200321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20717,"text":"ofr83141 - 1983 - Geohydrologic and drill-hole data for test well USW H-1, adjacent to Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:41","indexId":"ofr83141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-141","title":"Geohydrologic and drill-hole data for test well USW H-1, adjacent to Nevada Test Site, Nye County, Nevada","docAbstract":"This report presents data collected to determine the hydraulic characteristics of rocks penetrated in test well USW H-1. The well is one of a series of test wells drilled in and near the southwestern part of the Nevada Test Site, Nye County, Nevada, in a program conducted on behalf of the U.S. Department of Energy. These investigations are part of the Nevada Nuclear Waste Storage Investigations to identify suitable sites for storage of high-level radioactive wastes. Data on drilling operations, lithology, borehole geophysics, hydrologic monitoring, core analysis, ground-water chemistry and pumping and injection tests for well USW H-1 are contained in this report.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83141","usgsCitation":"Rush, F.E., Thordarson, W., and Bruckheimer, L., 1983, Geohydrologic and drill-hole data for test well USW H-1, adjacent to Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 83-141, v, 43 p. ill. ;28 cm., https://doi.org/10.3133/ofr83141.","productDescription":"v, 43 p. ill. ;28 cm.","costCenters":[],"links":[{"id":153241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0141/report-thumb.jpg"},{"id":50275,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f5c","contributors":{"authors":[{"text":"Rush, F. Eugene","contributorId":16821,"corporation":false,"usgs":true,"family":"Rush","given":"F.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":183119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":183120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruckheimer, Laura","contributorId":12869,"corporation":false,"usgs":true,"family":"Bruckheimer","given":"Laura","email":"","affiliations":[],"preferred":false,"id":183118,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":20993,"text":"ofr83535 - 1983 - Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada","interactions":[{"subject":{"id":20993,"text":"ofr83535 - 1983 - Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada","indexId":"ofr83535","publicationYear":"1983","noYear":false,"title":"Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":38540,"text":"pp1329 - 1985 - Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada","indexId":"pp1329","publicationYear":"1985","noYear":false,"title":"Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada"},"id":1}],"supersededBy":{"id":38540,"text":"pp1329 - 1985 - Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada","indexId":"pp1329","publicationYear":"1985","noYear":false,"title":"Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada"},"lastModifiedDate":"2021-01-26T20:54:04.39342","indexId":"ofr83535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-535","title":"Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada","docAbstract":"Paleoclimatic reconstructions for the Nevada Test Site, spanning the last 45,000 years, are based on plant macrofossil assemblages from radiocarbonated packrat (Neotoma spp) middens from south-central Nevada. The temperature regime during the Wisconsin glacial age, from before about 45,000 years ago until about 12,000 years ago, was characterized by lower temperatures during all seasons. Wisconsin maximum (about 18,000 years before present) winter temperatures were at least 6 deg. Celsius below those of the present, and the relative decrease in summer temperature was as much as 8 deg. Celsius. The data provide evidence for a precipitation regime drier than that proposed by many studies. The maximum estimated increase in average annual precipitation during the full-glacial period is 40 percent above current precipitation. The increase in temperature signaling the end of the Wisconsin glacial age may have begun as early as about 16,000 years ago. The oldest record of desert scrub vegetation from the Nevada Test Site area dates to about 15,000 years ago. By 10,000 years before present, average annual temperatures may have approximated present values, although seasonal temperature and precipitation regimes probably differed from those of today. Climate changes during the last 10,000 years have been relatively minor variations in a warm, dry climatic regime. Probably future climatic changes include a brief but pronounced warm period within the next 500 years, followed by a protracted transition to the next glacial age during the next 10,000 years. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83535","usgsCitation":"Spaulding, W., 1983, Vegetation and climates of the last 45,000 years in the vicinity of the Nevada Test Site, south-central Nevada: U.S. Geological Survey Open-File Report 83-535, xii, 199 p., https://doi.org/10.3133/ofr83535.","productDescription":"xii, 199 p.","costCenters":[],"links":[{"id":154290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0535/report-thumb.jpg"},{"id":382638,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0535/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Nevada Test Site","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.51275634765624,\n 37.19751842118354\n ],\n [\n -115.94970703125,\n 37.19751842118354\n ],\n [\n -115.94970703125,\n 37.42034463389752\n ],\n [\n -116.51275634765624,\n 37.42034463389752\n ],\n [\n -116.51275634765624,\n 37.19751842118354\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6887a3","contributors":{"authors":[{"text":"Spaulding, W. G.","contributorId":20704,"corporation":false,"usgs":true,"family":"Spaulding","given":"W. G.","affiliations":[],"preferred":false,"id":183636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21000,"text":"ofr83380 - 1983 - Comparison of the chemical characteristics of the uranium deposits of the Morrison Formation in the Grants uranium region, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:02","indexId":"ofr83380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-380","title":"Comparison of the chemical characteristics of the uranium deposits of the Morrison Formation in the Grants uranium region, New Mexico","docAbstract":"Statistical treatment of the chemical data of samples from the northeast Church Rock area, Ruby deposit, Mariano Lake deposit, and the Ambrosia Lake district indicates that primary ore-forming processes concentrated copper, iron, magnesium, manganese, molybdenum, selenium, vanadium, yttrium, arsenic, organic carbon, and sulfur, along with uranium. A barium halo that is associated with all of these deposits formed from secondary processes. Calcium and strontium were also enriched in the ores by secondary processes. Comparison of the chemical characteristics of the redistributed deposits in the Church Rock district to the primary deposits in the Grants uranium region indicates that calcium, manganese, strontium, yttrium, copper, iron, magnesium, molybdenum, lead, selenium, and vanadium are separated from uranium during redistribution of the deposits in the Church Rock area. Comparisons of the chemical characteristics of the Church Rock deposits and the secondary deposits at Ambrosia Lake suggest some differences in the processes that were involved in the genesis of the redistributed deposits in these two areas.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83380","usgsCitation":"Spirakis, C., and Pierson, C.T., 1983, Comparison of the chemical characteristics of the uranium deposits of the Morrison Formation in the Grants uranium region, New Mexico: U.S. Geological Survey Open-File Report 83-380, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83380.","productDescription":"22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":155861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0380/report-thumb.jpg"},{"id":50578,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0380/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adeb4","contributors":{"authors":[{"text":"Spirakis, C.S.","contributorId":46088,"corporation":false,"usgs":true,"family":"Spirakis","given":"C.S.","affiliations":[],"preferred":false,"id":183652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierson, C. T.","contributorId":57055,"corporation":false,"usgs":true,"family":"Pierson","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":183653,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10000,"text":"ofr801049 - 1983 - Ground water in the northern part of Clackamas County, Oregon","interactions":[],"lastModifiedDate":"2022-08-26T20:47:39.65998","indexId":"ofr801049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"80-1049","title":"Ground water in the northern part of Clackamas County, Oregon","docAbstract":"

Northern Clackamas County is part of the rapidly growing Portland metropolitan area. Population of this 250-square-mile area increased about 50 percent between 1970 and 1976. The study area includes a small segment of the Willamette River alluvial valley near Canby, and extends northward to the Clackamas River and eastward to the western boundary of Mount Hood National Forest. Also included is the narrow, well-populated corridor along U.S. Highway 26 from Cherryville to Government Camp.

The main part of the study area is largely a rolling upland underlain by volcanic and stream-deposited rocks ranging in age from Eocene to Holocene. In most places, these rocks yield water in quantities adequate for individual homes. Locally, ground-water supplies are adequate for small irrigation, industrial, or public-supply uses. Depths of wells range from 50 to 1,000 feet; wells generally are shallowest in lowlands near streams and deepest in upland locations near deeply incised stream valleys.

All aquifers receive recharge at sufficient rates to sustain present rates of natural and man-produced discharge. All aquifers could supply additional water, but careful engineering is needed to avoid overdevelopment problems for the Columbia River Basalt Group near Oregon City.

Chemical analyses indicate that the ground water in the study area is of good quality for drinking and other uses. Mineralized water reported from some wells northeast of Canby may be from rocks of the Skamania Volcanics, which locally are at shallow depth. Although ground water locally may be subject to bacterial contamination where it occurs at shallow depths in alluvium and other unconsolidated deposits, no contaminated water was identified during the study.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801049","collaboration":"Prepared in cooperation with the Oregon Water Resources Department","usgsCitation":"Leonard, A., and Collins, C.A., 1983, Ground water in the northern part of Clackamas County, Oregon: U.S. Geological Survey Open-File Report 80-1049, Report: v, 85 p., 2 Plates: 34.53 x 24.34 inches and 34.96 x 24.88 inches, https://doi.org/10.3133/ofr801049.","productDescription":"Report: v, 85 p., 2 Plates: 34.53 x 24.34 inches and 34.96 x 24.88 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":405726,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1049/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405725,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1049/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1049/report-thumb.jpg"},{"id":405724,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Clackamas County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.76123046875,\n 45.01141864227728\n ],\n [\n -121.84936523437499,\n 45.01141864227728\n ],\n [\n -121.84936523437499,\n 45.45627757127799\n ],\n [\n -122.76123046875,\n 45.45627757127799\n ],\n [\n -122.76123046875,\n 45.01141864227728\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d750","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":160652,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Collins, C. A.","contributorId":43731,"corporation":false,"usgs":true,"family":"Collins","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":160651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10323,"text":"ofr83116 - 1983 - Specifications for updating USGS land use and land cover maps","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr83116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-116","title":"Specifications for updating USGS land use and land cover maps","docAbstract":"To meet the increasing demands for up-to-date land use and land cover information, a primary goal of the U.S. Geological Survey's (USGS) national land use and land cover mapping program is to provide for periodic updating of maps and data in a timely and uniform manner. The technical specifications for updating existing USGS land use and land cover maps that are presented here cover both the interpretive aspects of detecting and identifying land use and land cover changes and the cartographic aspects of mapping and presenting the change data in conventional map format. They provide the map compiler with the procedures and techniques necessary to then use these change data to update existing land use and land cover maps in a manner that is both standardized and repeatable. Included are specifications for the acquisition of remotely sensed source materials, selection of compilation map bases, handling of data base corrections, editing and quality control operations, generation of map update products for USGS open file, and the reproduction and distribution of open file materials. These specifications are planned to become part of the National Mapping Division's Technical Instructions.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83116","usgsCitation":"Milazzo, V.A., 1983, Specifications for updating USGS land use and land cover maps: U.S. Geological Survey Open-File Report 83-116, iii, 65 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83116.","productDescription":"iii, 65 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":143654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0116/report-thumb.jpg"},{"id":38174,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e03","contributors":{"authors":[{"text":"Milazzo, Valerie A.","contributorId":88717,"corporation":false,"usgs":true,"family":"Milazzo","given":"Valerie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28202,"text":"wri834143 - 1983 - Storm runoff as related to urbanization based on data collected in Salem and Portland, and generalized for the Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2017-02-07T08:01:20","indexId":"wri834143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4143","title":"Storm runoff as related to urbanization based on data collected in Salem and Portland, and generalized for the Willamette Valley, Oregon","docAbstract":"Storm runoff as related to urbanization is defined by a series of regression equations for Salem and for the Willamette Valley, Oregon. In addition to data from 17 basins monitored in the Salem area, data from 24 basins gaged in a previous study in Portland, Oregon - Vancouver, Washington were used defining the Willamette Valley equations. Basins used to define equations ranged in size from 0.2 to 26 square miles. Rainfall intensity varied from 1.8 to 2.2 inches for the 6 hour, 0.2 exceedance probability. Sensitivity analyses of equations indicate that urbanization of an undeveloped basin can increase peak discharge more than three times and almost double runoff volume. Much of Portland and Vancouver are located on porous river terraces where dry wells are used to shunt runoff. Much of East Salem is located on previously farmed land where drain tiles used to dewater soils still connect directly to streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri834143","usgsCitation":"Laenen, A., 1983, Storm runoff as related to urbanization based on data collected in Salem and Portland, and generalized for the Willamette Valley, Oregon: U.S. Geological Survey Water-Resources Investigations Report 83-4143, vi, 88 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834143.","productDescription":"vi, 88 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":57040,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4143/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4143/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b31e4b07f02db6b411e","contributors":{"authors":[{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":199386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38620,"text":"pp1170D - 1983 - Merced Peak quadrangle, central Sierra Nevada, California— Analytic data","interactions":[],"lastModifiedDate":"2021-10-27T20:12:59.636263","indexId":"pp1170D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1170","chapter":"D","title":"Merced Peak quadrangle, central Sierra Nevada, California— Analytic data","docAbstract":"

No abstract available.

","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","doi":"10.3133/pp1170D","usgsCitation":"Peck, D., and Van Kooten, G.K., 1983, Merced Peak quadrangle, central Sierra Nevada, California— Analytic data: U.S. Geological Survey Professional Paper 1170, 29 p., https://doi.org/10.3133/pp1170D.","productDescription":"29 p.","costCenters":[],"links":[{"id":391035,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74408.htm"},{"id":65443,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1170d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1170d/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Merced Peak quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.25,\n 37.75\n ],\n [\n -119.5,\n 37.75\n ],\n [\n -119.5,\n 37.5\n ],\n [\n -119.25,\n 37.5\n ],\n [\n -119.25,\n 37.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db61420a","contributors":{"authors":[{"text":"Peck, D. L.","contributorId":53784,"corporation":false,"usgs":true,"family":"Peck","given":"D. L.","affiliations":[],"preferred":false,"id":220176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Kooten, G. K.","contributorId":41499,"corporation":false,"usgs":true,"family":"Van Kooten","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":220175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10156,"text":"ofr83143 - 1983 - Hydrologic data from the Johnson Brook phosphorus loading study, Kennebec County, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr83143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-143","title":"Hydrologic data from the Johnson Brook phosphorus loading study, Kennebec County, Maine","docAbstract":"Streamflow, water quality, and precipitation data collected during the 1980 and 1981 water years are reported. The purpose was to document changes in total phosphorus loads resulting from a change in agricultural waste management practices in the Johnson Brook watershed in Maine. Streamflow data include mean-daily discharges for the period May 12, 1980, through September 30, 1981, and instantaneous discharges determined during water quality sampling. Water quality data for the period March 1980 to September 1981 include total phosphorus concentrations determined from samples collected using cross-sectional depth-integrating sampling techniques and from samples collected using a pumping sampler. Suspended sediment concentrations, and water temperature and specific conductance values are also included. The precipitation data are daily totals for the period October 1980 through September 1981. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83143","usgsCitation":"Maloney, T.J., Dominie, D.R., and Nichols, W.J., 1983, Hydrologic data from the Johnson Brook phosphorus loading study, Kennebec County, Maine: U.S. Geological Survey Open-File Report 83-143, iv, 27 p. maps ;28 cm., https://doi.org/10.3133/ofr83143.","productDescription":"iv, 27 p. maps ;28 cm.","costCenters":[],"links":[{"id":144281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0143/report-thumb.jpg"},{"id":38000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60784b","contributors":{"authors":[{"text":"Maloney, Thomas J.","contributorId":35736,"corporation":false,"usgs":true,"family":"Maloney","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160907,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dominie, David R.","contributorId":11227,"corporation":false,"usgs":true,"family":"Dominie","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nichols, William J.","contributorId":20752,"corporation":false,"usgs":true,"family":"Nichols","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11604,"text":"ofr83352 - 1983 - A search for stratiform massive-sulfide exploration targets in Appalachian Devonian rocks; a case study using computer-assisted attribute-coincidence mapping","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr83352","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-352","title":"A search for stratiform massive-sulfide exploration targets in Appalachian Devonian rocks; a case study using computer-assisted attribute-coincidence mapping","docAbstract":"The empirical model for sediment-associated, stratiform, exhalative, massive-sulfide deposits presented by D. Large in 1979 and 1980 has been redesigned to permit its use in a computer-assisted search for exploration-target areas in Devonian rocks of the Appalachian region using attribute-coincidence mapping (ACM). Some 36 gridded-data maps and selected maps derived therefrom were developed to show the orthogonal patterns, using the 7-1/2 minute quadrangle as an information cell, of geologic data patterns relevant to the empirical model. From these map and data files, six attribute-coincidence maps were prepared to illustrate both variation in the application of ACM techniques and the extent of possible significant exploration-target areas. As a result of this preliminary work in ACM, four major (and some lesser) exploration-target areas needing further study and analysis have been defined as follows: 1) in western and central New York in the outcrop area of lowermost Upper Devonian rocks straddling the Clarendon-Linden fault; 2) in western Virginia and eastern West Virginia in an area largely coincident with the well-known 'Oriskany' Mn-Fe ores; 3) an area in West Virginia, Maryland, and Virginia along and nearby the trend of the Alabama-New York lineament of King and Zietz approximately between 38- and 40-degrees N. latitude; and 4) an area in northeastern Ohio overlying an area coincident with a significant thickness of Silurian salt and high modern seismic activity. Some lesser, smaller areas suggested by relatively high coincidence may also be worthy of further study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83352","usgsCitation":"Wedow, H., 1983, A search for stratiform massive-sulfide exploration targets in Appalachian Devonian rocks; a case study using computer-assisted attribute-coincidence mapping: U.S. Geological Survey Open-File Report 83-352, 84 p. maps ;28 cm., https://doi.org/10.3133/ofr83352.","productDescription":"84 p. maps ;28 cm.","costCenters":[],"links":[{"id":146100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0352/report-thumb.jpg"},{"id":39464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0352/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b18e4b07f02db6a7031","contributors":{"authors":[{"text":"Wedow, Helmuth","contributorId":67495,"corporation":false,"usgs":true,"family":"Wedow","given":"Helmuth","affiliations":[],"preferred":false,"id":163428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10229,"text":"ofr83779 - 1983 - Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr83779","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-779","title":"Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska","docAbstract":"This report is an effort to describe and decipher the mid-Paleozoic to Lower Cretaceous stratigraphy and the orogenic evolution of the western Brooks Range. The western Brooks Range primarily is composed of stacks of complexly deformed thrust sheets that contain mostly coeval sequences of rocks with slightly different lithologic facies. In order to simplify the thrust-faulted stratigraphy and palinspastic restoration, the rocks are grouped into eight principal structural levels. The lowest structural level is believed to be autochthonous or parautochthonous and above that, each succeeding level is designated allochthon one through seven. Allochthon seven is composed of the remnants of an extensive ophiolite sheet. Allochthon six is composed of pillow basalt with subordinate intermediate volcanic rocks, chert, and Devonian limestone. It is not certain whether this allochthon was formed in a continental or oceanic setting. Allochthons five through one consist of distinctive and coeval sequences of Devonian to Lower Cretaceous sedimentary rocks that were deposited in a continental setting. The present geographic distribution of each structural level is shown on the allochthon map of the western Brooks Range. \r\n\r\nThe stratigraphy of the southern part of northern Alaska has been reconstructed by systematically unstacking lower allochthons to the north of higher allochthons. The palinspastic map that results from this procedure shows that the minimum thrust displacement between allochthon seven and the autochthon is approximately 700 to 800 km. Schematic cross sections drawn across the palinspastic map show how the stratigraphy of the southern part of northern. Alaska most likely appeared prior to the orogeny. During Devonian and Mississippian time, the sedimentary sequences that are now part of allochthons one to five are inferred to have been deposited in an ensialic basin with both northern and southern margins. During Pennsylvanian time, the sequences seem to have become part of a southward-sloping continental shelf when a southern land area moved away from northern Alaska by an inferred plate tectonic process of rifting or strike-slip motion. In Early Jurassic time just prior to the Brooks Range orogeny, northern Alaska probably was an extensive continental shelf with oceanic conditions to the south and land to the north. \r\n\r\nThe Brooks Range orogeny seems to have begun in the Middle Jurassic as the Arctic Alaska plate was underthrust (subducted) southward beneath oceanic crust of allochthon seven. At progressively later stages in the underthrusting process, the upper parts of the continental shelf were detached from the subthrust basement on which they were deposited, resulting in the other allochthons of the western Brooks Range. The period of major thrusting ceased by Albian time in the Early Cretaceous. During middle and Late Cretaceous time, epeirogenic uplift in the Brooks Range caused large quantities of clastic detritus to be shed into successor basins to the north and south. Broad folds and reverse faults in Upper Cretaceous sediments north of the Brooks Range provide evidence for a later period(s) of less intense deformation in northern Alaska.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83779","usgsCitation":"Mayfield, C.F., Tailleur, I.L., and Ellersieck, I., 1983, Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska: U.S. Geological Survey Open-File Report 83-779, ii, 61 p., 5 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr83779.","productDescription":"ii, 61 p., 5 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":144308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0779/report-thumb.jpg"},{"id":38093,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38094,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38095,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38096,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38097,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0779/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38098,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0779/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a530f","contributors":{"authors":[{"text":"Mayfield, Charles F.","contributorId":13623,"corporation":false,"usgs":true,"family":"Mayfield","given":"Charles","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tailleur, Irvin L.","contributorId":105304,"corporation":false,"usgs":true,"family":"Tailleur","given":"Irvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161045,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellersieck, Inyo","contributorId":34914,"corporation":false,"usgs":true,"family":"Ellersieck","given":"Inyo","affiliations":[],"preferred":false,"id":161044,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10025,"text":"ofr83129 - 1983 - Selective annotated bibliography of ground-water resources, records of wells and springs, and availability of streamflow data on Indian reservations in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr83129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-129","title":"Selective annotated bibliography of ground-water resources, records of wells and springs, and availability of streamflow data on Indian reservations in Montana","docAbstract":"A compilation was made, for each of the seven Indian reservations in Montana, of the availability of hydrologic data. The report consists of an annotated bibliography of ground-water resources reports, selected data for wells and springs from the data bases of the U.S. Geological Survey and Montana Bureau of Mines and Geology, and a listing of all sites where streamflow has been measured and water-quality samples collected by the U. S.Geological Survey. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83129","usgsCitation":"Levings, G., and White, M.K., 1983, Selective annotated bibliography of ground-water resources, records of wells and springs, and availability of streamflow data on Indian reservations in Montana: U.S. Geological Survey Open-File Report 83-129, iv, 141 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83129.","productDescription":"iv, 141 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0129/report-thumb.jpg"},{"id":37865,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7d29","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":160692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Melvin K. mwhite@usgs.gov","contributorId":1563,"corporation":false,"usgs":true,"family":"White","given":"Melvin","email":"mwhite@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":160691,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10208,"text":"ofr83728 - 1983 - Distribution and quantitative assessment of world crude oil reserves and resources","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr83728","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-728","title":"Distribution and quantitative assessment of world crude oil reserves and resources","docAbstract":"World Demonstrated Reserves of crude oil are approximately 723 billion barrels of oil (BBO). Cumulative production is 445 BBO and annual production is 20 BBO. Demonstrated Reserves of crude-oil have declined over the past 10 years consistent with discoveries lagging production over the same period. The assessment of Undiscovered Resources shows a 90 percent probability that the amount discoverable lies between 321 and 1,417 BBO, 550 BBO being the most likely value. The most likely value for Ultimate recoverable resources is 1,718 BBO. The distribution of Ultimate Resources of crude oil will remain highly skewed toward the Middle East; no frontier areas that have potentials large enough to significantly affect present distribution are recognized. Rates of discovery have continued to decline over the past 20 years even though exploration activity has increased in recent years. Prudence dictates, therefore, that the low side of the assessment of Undiscovered Resources be responsibly considered and that alternate energy sources be a part of future planning. \r\n\r\nExtra-heavy oil and bitumen are assessed separately, with Reserves being figured as the annual productive capacity of installed facilities times 25 years. The annual production of extra-heavy oil is about 8 million barrels and of bitumen about 60 million barrels.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83728","usgsCitation":"Masters, C.D., Root, D.H., and Dietzman, W.D., 1983, Distribution and quantitative assessment of world crude oil reserves and resources: U.S. Geological Survey Open-File Report 83-728, 1 v. (various foliations) :ill. ;28 cm., https://doi.org/10.3133/ofr83728.","productDescription":"1 v. (various foliations) :ill. ;28 cm.","costCenters":[],"links":[{"id":142483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0728/report-thumb.jpg"},{"id":38064,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0728/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64962f","contributors":{"authors":[{"text":"Masters, Charles D.","contributorId":38969,"corporation":false,"usgs":true,"family":"Masters","given":"Charles","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":161005,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Root, David H.","contributorId":92232,"corporation":false,"usgs":true,"family":"Root","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dietzman, William D.","contributorId":77532,"corporation":false,"usgs":true,"family":"Dietzman","given":"William","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":161006,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38613,"text":"pp1239 - 1983 - Tectonic setting of late Miocene, Pliocene, and Pleistocene rocks in part of the Coast Ranges north of San Francisco, California","interactions":[],"lastModifiedDate":"2025-08-22T19:27:11.097859","indexId":"pp1239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1239","title":"Tectonic setting of late Miocene, Pliocene, and Pleistocene rocks in part of the Coast Ranges north of San Francisco, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1239","usgsCitation":"Fox, K., 1983, Tectonic setting of late Miocene, Pliocene, and Pleistocene rocks in part of the Coast Ranges north of San Francisco, California: U.S. Geological Survey Professional Paper 1239, Report: iii, 33 p.; 1 Plate: 22.00 x 18.00 inches, https://doi.org/10.3133/pp1239.","productDescription":"Report: iii, 33 p.; 1 Plate: 22.00 x 18.00 inches","costCenters":[],"links":[{"id":65431,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1239/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65430,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1239/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120248,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1239/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Coast Ranges","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123,\n 38.7444\n ],\n [\n -123,\n 38.1375\n ],\n [\n -122.0864,\n 38.1375\n ],\n [\n -122.0864,\n 38.7444\n ],\n [\n -123,\n 38.7444\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858f1","contributors":{"authors":[{"text":"Fox, K. F. Jr.","contributorId":46554,"corporation":false,"usgs":true,"family":"Fox","given":"K. F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":220166,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18261,"text":"ofr83140 - 1983 - Data compilation of benthic invertebrates from tributary streams in Yampa and North Platte River Basins, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:14","indexId":"ofr83140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-140","title":"Data compilation of benthic invertebrates from tributary streams in Yampa and North Platte River Basins, northwestern Colorado","docAbstract":"Benthic invertebrates were collected from Trout Creek, Fish Creek, and the Williams Fork (tributaries of the Yampa River in Routt and Moffat Counties), and Little Grizzly and Grizzly Creeks (tributaries of the North Platte River in Jackson County). Stream-sampling sites were upstream and downstream from potential, existing, or historical coal-mining areas. Field water-quality measurements of water temperature, specific conductance, pH, and dissolved oxygen were also made to aid in assessing stream water-quality conditions. The purpose of the study was to describe and quantify the benthic invertebrate communities in selected streams in coal-mining areas. Sampling was conducted on a near bimonthly basis throughout the growing season, beginning in April and May 1980, and continuing through September 1981. This report describes the methods of data collection and presents qualitative and quantitative results of benthic invertebrates and associated water-quality data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83140","usgsCitation":"Britton, L.J., 1983, Data compilation of benthic invertebrates from tributary streams in Yampa and North Platte River Basins, northwestern Colorado: U.S. Geological Survey Open-File Report 83-140, iv, 110 p. :maps ;28 cm., https://doi.org/10.3133/ofr83140.","productDescription":"iv, 110 p. :maps ;28 cm.","costCenters":[],"links":[{"id":149183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0140/report-thumb.jpg"},{"id":47616,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c96c","contributors":{"authors":[{"text":"Britton, L. J.","contributorId":39788,"corporation":false,"usgs":true,"family":"Britton","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":178802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28663,"text":"wri834003 - 1983 - Water quality at and adjacent to the south Dade County solid-waste disposal facility, Florida","interactions":[],"lastModifiedDate":"2022-01-10T12:42:17.030178","indexId":"wri834003","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4003","title":"Water quality at and adjacent to the south Dade County solid-waste disposal facility, Florida","docAbstract":"A water-quality reconnaissance was conducted at the south Dade County solid-waste landfill near Goulds, Florida, from December 1977 through August 1978. The landfill is located directly on the unconfined Biscayne aquifer, which, in the study area, is affected by saltwater intrusion. Water samples collected from six monitor well sites at two depths and four surface-water sites were analyzed to determine the chemical, physical, and biological conditions of the ground water and surface water of the study area. Results indicated that water quality beneath the landfill was highly variable with location and depth. Leachate was generally more evident in the shallow wells and during the dry-season sampling, but was greatly diluted and dispersed in the deep wells and during the wet season. High concentrations of contaminants were generated primarily in areas of the landfill with the most recent waste deposits. Chloride (limited to the shallow wells and the dry season), alkalinity, ammonia, iron, manganese, lead, phosphorus, and organic nitrogen indicate leachate contamination of the aquifer. Water-quality characteristics in the surface waters were generally only slightly above background levels. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri834003","collaboration":"Prepared in cooperation with Dade County Department of Public Works","usgsCitation":"McKenzie, D., 1983, Water quality at and adjacent to the south Dade County solid-waste disposal facility, Florida: U.S. Geological Survey Water-Resources Investigations Report 83-4003, v, 42 p., https://doi.org/10.3133/wri834003.","productDescription":"v, 42 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":158336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4003/coverthb.jpg"},{"id":57504,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4003/wri834003.pdf","text":"Report","size":"1.77 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 83-4003"}],"country":"United States","state":"Florida","county":"Dade County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5572509765625,\n 25.591994180254712\n ],\n [\n -79.95574951171875,\n 25.591994180254712\n ],\n [\n -79.95574951171875,\n 26.162833742569937\n ],\n [\n -80.5572509765625,\n 26.162833742569937\n ],\n [\n -80.5572509765625,\n 25.591994180254712\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"

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","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b2f","contributors":{"authors":[{"text":"McKenzie, D.J.","contributorId":75134,"corporation":false,"usgs":true,"family":"McKenzie","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":200195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11729,"text":"ofr83747 - 1983 - Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","interactions":[],"lastModifiedDate":"2022-09-23T20:16:56.047888","indexId":"ofr83747","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-747","title":"Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","docAbstract":"Hydration-rind ages based on hydration-rind thicknesses of obsidian and an assumed hydration rate of 5 microns /1000 yrs have been determined for the 26 exposed Mono domes and coulees. Hydration-rind thickness data give good estimates of relative age differences between the domes, but determination of absolute ages will depend upon calibration to radiometric ages. \r\n\r\nThe first extrusion of highly differentiated, sparsely porphyritic rhyolite occurred an estimated 32,000 to 40,000 yrs ago and consists of a small dome at the northwest end of the contiguous chain. The next major extrusive event occurred about 24,000 yrs ago and is represented by two domes and a major tephra. About 10,000 yrs ago the frequency of eruptive activity increases and rhyolite lave was extruded at an average rate of 0.2 km3/1000 yrs; periods of dormancy ranging in length from 300 to 2000 yrs. About 2000 to 3000 yrs ago the rate of extrusion increased dramatically to 0.8 km3/1000 yrs beginning with the eruption of the South Coulee and its associated tephra. At the same time, the nature of erupted magma changed from sparsely porphyritic (3 to 10 per cent sanidine) to aphyric rhyolite. All eruptions since 2000 radiocarbon yrs BP have produced magma that is aphyric but is of the same chemical composition as the earlier porphyritic magma. Volumes of porphyritic and aphyric extrusives, each of which includes volumes of lava and volumes of pumiceous pyroclastics reduced for porosity, are nearly equal and together total about 4 km3. Projecting the recent rate of extrusion over the time since the last major eruption, 1185 radiocarbon yrs ago suggests that a future eruption in the Mono Chain could release as much as 1 km 3 of magma. The recent increase in extrusion rate and the contemporaneous change in the nature of the magma are attributed to an event in the magma chamber that allowed the release of hotter, more fluid, crystal-free magma. The young age for the beginning of rhyolite volcanism from the mono magma chamber suggests that rhyolite magma may have been emplaced in the shallow crust as recently as 32,000 to 40,000 yrs ago. Calculations by Lachenbruch et al. (1976, Jour. Geophys. Research, v. 81, p. 769-784) that a thermal disturbance at this age would have propagated upward by solid conduction only 4 km and offer an explanation for the lack of a heat-flow anomaly and surface indications of hydrothermal activity over the Mono magma chamber and its associated ring-fracture system. This report also contains new information on the age and chemistry of volcanics on the Mono Lake island, the Inyo domes, and tephras within the Long Valley Caldera. \r\n\r\nA newly discovered rhyolite tuff ring of late Quaternary age in the Toowa volcanic field of the southern Sierra Nevada is briefly described for it represents a new area that should be examined for potential as a geothermal area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83747","usgsCitation":"Wood, S.H., 1983, Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California: U.S. Geological Survey Open-File Report 83-747, vii, 76 p., https://doi.org/10.3133/ofr83747.","productDescription":"vii, 76 p.","costCenters":[],"links":[{"id":407293,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14207.htm","linkFileType":{"id":5,"text":"html"}},{"id":143964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0747/report-thumb.jpg"},{"id":39615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0747/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Long Valley and Mono Basin geothermal area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.129,\n 37.681\n ],\n [\n -118.922,\n 37.681\n ],\n [\n -118.922,\n 38.046\n ],\n [\n -119.129,\n 38.046\n ],\n [\n -119.129,\n 37.681\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e073f","contributors":{"authors":[{"text":"Wood, S. H.","contributorId":66261,"corporation":false,"usgs":true,"family":"Wood","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":163631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26542,"text":"wri824070 - 1983 - Chloride concentrations in the coastal margin of the Floridan Aquifer, southwest Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri824070","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4070","title":"Chloride concentrations in the coastal margin of the Floridan Aquifer, southwest Florida","docAbstract":"The Floridan aquifer is the principal source of freshwater supply in southwest Florida. The freshwater part of the aquifer is underlain by saltwater in lower formations and is bounded on the west by saltwater in the coastal parts of the aquifer. A zone of mixing lies between the saltwater and freshwater. The saltwater and freshwater boundaries are defined by chloride concentrations of 19,000 milligrams per liter on the coastward side and 250 milligrams per liter on the landward side. Lateral intrusion of saltwater can occur along the coast in areas where the hydraulic gradient declines and upconing can occur in inland areas of heavy ground-water withdrawals. Safeguards against saltwater intrusion in these areas are necessary because flushing of the aquifer is a very slow process. A network of chloride monitor wells is proposed for the zone of mixing in the upper producing zone of the floridan aquifer. Seventy wells were selected at 54 sites to monitor chloride concentrations along the 250-milligram-per-liter line of equal chloride concentration. One-fourth of the wells are located in areas of increasing chloride concentrations or heavy ground-water withdrawals and the remaining wells are intended to improve delineation of the interface and to monitor long-term changes in chloride concentrations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824070","usgsCitation":"Causseaux, K., and Fretwell, J.D., 1983, Chloride concentrations in the coastal margin of the Floridan Aquifer, southwest Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4070, iv, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824070.","productDescription":"iv, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4070/report-thumb.jpg"},{"id":55407,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4070/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e27ae","contributors":{"authors":[{"text":"Causseaux, K.W.","contributorId":7306,"corporation":false,"usgs":true,"family":"Causseaux","given":"K.W.","affiliations":[],"preferred":false,"id":196579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fretwell, J. D.","contributorId":97933,"corporation":false,"usgs":true,"family":"Fretwell","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":196580,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65430,"text":"i1525 - 1983 - Controlled photomosaic of the Casius Southwest Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:14","indexId":"i1525","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1525","subseriesTitle":"NONE","title":"Controlled photomosaic of the Casius Southwest Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1525","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Controlled photomosaic of the Casius Southwest Quadrangle of Mars: U.S. Geological Survey IMAP 1525, 1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1525.","productDescription":"1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251313,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1525/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":251314,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1525/plate-1.pdf","size":"10482","linkFileType":{"id":1,"text":"pdf"}},{"id":252211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1525/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c21","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":533817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28441,"text":"wri8242 - 1983 - Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida","interactions":[],"lastModifiedDate":"2019-11-26T11:15:19","indexId":"wri8242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-42","title":"Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida","docAbstract":"Hydrologic data collected on nine small urban watersheds in the Tampa Bay area of west-central Florida and a method for estimating peak discharges in the study area are described. The watersheds have mixed land use and range in size from 0.34 to 3.45 square miles. Watershed soils, land use, and storm-drainage system data are described. Urban development ranged from a sparsely populated area with open-ditch storm sewers and 19% impervious area to a completely sewered watershed with 61% impervious cover. The U.S. Geological Survey natural-basin and urban-watershed models were calibrated for the nine watersheds using 5-minute interval rainfall data from the Tampa, Florida, National Weather Service rain gage to simulate annual peak discharge for the period 1906-52. A log-Pearson Type III frequency analysis of the simulated annual maximum discharge was used to determine the 2-, 5-, 10-, 25-, 50-, and 100-year flood discharges for each watershed. Flood discharges were related in a multiple-linear regression to drainage area, channel slope, detention storage area, and an urban-development factor determined by the extent of curb and gutter street drainage and storm-sewer system. The average standard error for the regional relations ranged from + or - 32 to + or - 42%. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8242","usgsCitation":"Lopez, M.A., and Woodham, W.M., 1983, Magnitude and frequency of flooding on small urban watersheds in the Tampa Bay area, west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 82-42, vi, 52 p. , https://doi.org/10.3133/wri8242.","productDescription":"vi, 52 p. ","costCenters":[],"links":[{"id":369640,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0042/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Tampa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.6336669921875,\n 27.81478637667891\n ],\n [\n -82.1832275390625,\n 27.81478637667891\n ],\n [\n -82.1832275390625,\n 28.14950321154457\n ],\n [\n -82.6336669921875,\n 28.14950321154457\n ],\n [\n -82.6336669921875,\n 27.81478637667891\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649519","contributors":{"authors":[{"text":"Lopez, M. A.","contributorId":12493,"corporation":false,"usgs":true,"family":"Lopez","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodham, W. M.","contributorId":72356,"corporation":false,"usgs":true,"family":"Woodham","given":"W.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47748,"text":"wri8130 - 1983 - Reservoir-development impacts on surface-water quantity and quality in the Yampa River basin, Colorado and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:20","indexId":"wri8130","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-30","title":"Reservoir-development impacts on surface-water quantity and quality in the Yampa River basin, Colorado and Wyoming","docAbstract":"Development of coal resources and associated economy is accelerating in the Yampa River basin in northwestern Colorado and south-central Wyoming. Increased use of the water resources of the area will have a direct impact on their quantity and quality. As part of 18 surface-water projects, 35 reservoirs have been proposed with a combined total storage of 2.18 million acre-feet, 41% greater than the mean annual outflow from the basin. Three computer models were used to demonstrate methods of evaluating future impacts of reservoir development in the Yampa River basin. Four different reservoir configurations were used to simulate the effects of different degrees of proposed reservoir development. A multireservoir-flow model included both within-basin and transmountain diversions. Simulations indicated that in many cases diversion amounts would not be available for either type of diversion. A corresponding frequency analysis of reservoir storage levels indicated that most reservoirs would be operating with small percentages of total capacities and generally with less than 20% of conservation-pool volumes. Simulations using a dissolved-solids model indicated that extensive reservoir development could increase average annual concentrations at most locations. Simulations using a single-reservoir model indicated no significant occurrence of water-temperature stratification in most reservoirs due to limited reservoir storage. (USGS)","language":"ENGLISH","doi":"10.3133/wri8130","usgsCitation":"Adams, D.B., Bauer, D.P., Dale, R.H., and Steele, T.D., 1983, Reservoir-development impacts on surface-water quantity and quality in the Yampa River basin, Colorado and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 81-30, 98 p. ill., maps ;28 cm., https://doi.org/10.3133/wri8130.","productDescription":"98 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":169769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0030/report-thumb.jpg"},{"id":84659,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62ba17","contributors":{"authors":[{"text":"Adams, D. Briane","contributorId":35707,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"Briane","affiliations":[],"preferred":false,"id":236148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bauer, Daniel P.","contributorId":24337,"corporation":false,"usgs":true,"family":"Bauer","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":236147,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dale, Robert H.","contributorId":85190,"corporation":false,"usgs":true,"family":"Dale","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":236149,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steele, Timothy Doak","contributorId":88723,"corporation":false,"usgs":true,"family":"Steele","given":"Timothy","email":"","middleInitial":"Doak","affiliations":[],"preferred":false,"id":236150,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":10178,"text":"ofr83442 - 1983 - Arsenic and gold mineralization in the McFarland Canyon-Story Mine area, Maricopa County, Arizona","interactions":[],"lastModifiedDate":"2023-03-01T22:22:28.263696","indexId":"ofr83442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-442","title":"Arsenic and gold mineralization in the McFarland Canyon-Story Mine area, Maricopa County, Arizona","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83442","usgsCitation":"Marsh, S.P., 1983, Arsenic and gold mineralization in the McFarland Canyon-Story Mine area, Maricopa County, Arizona: U.S. Geological Survey Open-File Report 83-442, Report: i, 22 p.; 1 Plate: 17.06 x 29.27 inches, https://doi.org/10.3133/ofr83442.","productDescription":"Report: i, 22 p.; 1 Plate: 17.06 x 29.27 inches","costCenters":[],"links":[{"id":413579,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14044.htm","linkFileType":{"id":5,"text":"html"}},{"id":38025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0442/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38024,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0442/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143175,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0442/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Maricopa County","otherGeospatial":"McFarland Canyon-Story Mine area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.529,\n 33.978\n ],\n [\n -111.529,\n 33.967\n ],\n [\n -111.517,\n 33.967\n ],\n [\n -111.517,\n 33.978\n ],\n [\n -111.529,\n 33.978\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672e09","contributors":{"authors":[{"text":"Marsh, Sherman P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20834,"text":"ofr83915 - 1983 - Electrical and magnetic properties of rock and soil","interactions":[],"lastModifiedDate":"2012-02-02T00:07:39","indexId":"ofr83915","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-915","title":"Electrical and magnetic properties of rock and soil","docAbstract":"Field and laboratory measurements have been made to determine the electrical conductivity, dielectric constant, and magnetic permeability of rock and soil in areas of interest in studies of electromagnetic pulse propagation. Conductivity is determined by making field measurements of apparent resisitivity at very low frequencies (0-20 cps), and interpreting the true resistivity of layers at various depths by curve-matching methods. Interpreted resistivity values are converted to corresponding conductivity values which are assumed to be applicable at 10^2 cps, an assumption which is considered valid because the conductivity of rock and soil is nearly constant at frequencies below 10^2 cps. Conductivity is estimated at higher frequencies (up to 10^6 cps) by using statistical correlations of three parameters obtained from laboratory measurements of rock and soil samples: conductivity at 10^2 cps, frequency and conductivity measured over the range 10^2 to 10^6 cps. Conductivity may also be estimated in this frequency range by using field measurements of water content and correlations of laboratory sample measurements of the three parameters: water content, frequency, and conductivity measured over the range 10^2 to 10^6 cps. This method is less accurate because nonrandom variation of ion concentration in natural pore water introduces error. \r\n\r\nDielectric constant is estimated in a similar manner from field-derived conductivity values applicable at 10^2 cps and statistical correlations of three parameters obtained from laboratory measurements of samples: conductivity measured at 10^2 cps, frequency, and dielectric constant measured over the frequency range 10^2 to 10^6 cps. Dielectric constant may also be estimated from field measurements of water content and correlations of laboratory sample measurements of the three parameters: water content, frequency, and dielectric constant measured from 10^2 to 10^6 cps, but again, this method is less accurate because of variation of ion concentration of pore water. \r\n\r\nSpecial laboratory procedures are used to measure conductivity and dielectric constant of rock and soil samples. Electrode polarization errors are minimized by using an electrode system that is electrochemically reversible-with ions in pore water.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83915","usgsCitation":"Scott, J.H., 1983, Electrical and magnetic properties of rock and soil: U.S. Geological Survey Open-File Report 83-915, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83915.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0915/report-thumb.jpg"},{"id":50429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0915/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47e8e4b07f02db4bd20b","contributors":{"authors":[{"text":"Scott, J. H.","contributorId":15204,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":183331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10115,"text":"ofr82690 - 1983 - Analyses of native water, bottom material, elutriate samples, and dredged material from selected southern Louisiana waterways and selected areas in the Gulf of Mexico, 1979-81","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr82690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-690","title":"Analyses of native water, bottom material, elutriate samples, and dredged material from selected southern Louisiana waterways and selected areas in the Gulf of Mexico, 1979-81","docAbstract":"The U.S. Geological Survey was requested by the U.S. Army Corps of Engineers, New Orleans District, to provide water-quality data to evaluate environmental effects of dredging activities in selected reaches of the Calcasieu River in southwestern Louisiana. Samples were collected from the upper and lower Calcasieu River between January 1980 and March 1981. Thirty-three samples (22 native-water and 11 effluent) were collected from eleven dredging sites. In addition, a series of elutriate studies were conducted between July 1979 and July 1981 to determine water quality as a basis for assessing possible environmental effects of proposed dredging activities in the following areas: Grand Bayou and Martins Canal near Happy Jack, unnamed bayou near Port Sulphur, Grand Bayou and Pipeline Canal near Port Sulphur and Bayou des Plantins near Empire; Mississippi River Gulf Outlet and Inner Harbor Navigation Canal; Southwest Pass; Barataria Bay; Atchafalaya Bay at Eugene Island; Calcasieu Ship Channel. Samples of native water and samples of bottom material were collected from 22 different sites and elutriate (mixtures of native water and bottom material) samples were prepared and analyzed. Four proposed ocean-disposal sites were sampled for bottom material only. Samples were analyzed for selected chemical and biological constituents and physical properties. 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