No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83514","usgsCitation":"Popenoe, P., 1983, Description of a high-resolution seismic reflection profile collected between the Chesapeake Bay, Virginia and Cape Romain, South Carolina, Sept. 26 to Oct. 2, 1981 (Cruise RV Gyre 81-G-14): U.S. Geological Survey Open-File Report 83-514, 3 p., https://doi.org/10.3133/ofr83514.","productDescription":"3 p.","costCenters":[],"links":[{"id":389313,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14080.htm"},{"id":38535,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0514/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0514/report-thumb.jpg"}],"country":"United States","state":"North Carolina, South Carolina, Virginia","otherGeospatial":"Chesapeake Bay, Cape Romain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.12353515625,\n 33.32134852669881\n ],\n [\n -74.8828125,\n 33.32134852669881\n ],\n [\n -74.8828125,\n 37.03763967977139\n ],\n [\n -79.12353515625,\n 37.03763967977139\n ],\n [\n -79.12353515625,\n 33.32134852669881\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cced","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","interactions":[{"subject":{"id":4471,"text":"cir902H - 1983 - Petroleum potential of wilderness lands in Nevada","indexId":"cir902H","publicationYear":"1983","noYear":false,"chapter":"H","title":"Petroleum potential of wilderness lands in Nevada"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":1},{"subject":{"id":4472,"text":"cir902I - 1983 - Petroleum potential of wilderness lands in New Mexico","indexId":"cir902I","publicationYear":"1983","noYear":false,"chapter":"I","title":"Petroleum potential of wilderness lands in New Mexico"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":2},{"subject":{"id":4473,"text":"cir902M - 1983 - Petroleum potential of wilderness lands in Wyoming","indexId":"cir902M","publicationYear":"1983","noYear":false,"chapter":"M","title":"Petroleum potential of wilderness lands in Wyoming"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":3},{"subject":{"id":4476,"text":"cir902C - 1983 - Petroleum potential of wilderness lands in Arizona","indexId":"cir902C","publicationYear":"1983","noYear":false,"chapter":"C","title":"Petroleum potential of wilderness lands in Arizona"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":4},{"subject":{"id":4477,"text":"cir902D - 1983 - Petroleum potential of wilderness lands in California","indexId":"cir902D","publicationYear":"1983","noYear":false,"chapter":"D","title":"Petroleum potential of wilderness lands in California"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":5},{"subject":{"id":4478,"text":"cir902F - 1983 - Petroleum potential of wilderness lands in Idaho","indexId":"cir902F","publicationYear":"1983","noYear":false,"chapter":"F","title":"Petroleum potential of wilderness lands in Idaho"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":6},{"subject":{"id":4479,"text":"cir902J - 1983 - Petroleum potential of wilderness lands in Oregon","indexId":"cir902J","publicationYear":"1983","noYear":false,"chapter":"J","title":"Petroleum potential of wilderness lands in Oregon"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":7},{"subject":{"id":4480,"text":"cir902K - 1983 - Petroleum potential of wilderness lands in Utah","indexId":"cir902K","publicationYear":"1983","noYear":false,"chapter":"K","title":"Petroleum potential of wilderness lands in Utah"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":8},{"subject":{"id":4481,"text":"cir902L - 1983 - Petroleum potential of wilderness lands in Washington","indexId":"cir902L","publicationYear":"1983","noYear":false,"chapter":"L","title":"Petroleum potential of wilderness lands in Washington"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":9},{"subject":{"id":4515,"text":"cir902G - 1983 - Petroleum potential of wilderness lands in Montana","indexId":"cir902G","publicationYear":"1983","noYear":false,"chapter":"G","title":"Petroleum potential of wilderness lands in Montana"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":10},{"subject":{"id":31073,"text":"cir902E - 1983 - Petroleum potential of wilderness lands in Colorado","indexId":"cir902E","publicationYear":"1983","noYear":false,"chapter":"E","title":"Petroleum potential of wilderness lands in Colorado"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":11}],"lastModifiedDate":"2018-10-22T18:14:50","indexId":"cir902AP","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"902","chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States","docAbstract":"In 1982-83, the U.S. Geological Survey (USGS) conducted an investigation of the oil and gas potential of the designated and proposed Wilderness Lands in the Western United States. The scope of this study was limited to the assessment of conventional recoverable petroleum resources occurring in the designated and proposed Wilderness Lands of the Western United States that are administered under four Federal agencies: Bureau of Land Management (BLM), U.S. Forest Service (USFS), National Park Service (NPS), and Fish and Wildlife Service (FWS). \r\n\r\nThe total area of the study included approximately 74 million acres of Wilderness Lands in these 11 Western States: Arizona, California, Colorado, Idaho, Montana, Nevada, New Mexico, Oregon, Utah, Washington, and Wyoming. The 74 million acres represent 31 percent of the total Federal lands within these 11 Western States. Approximately 49 percent of all the lands in these States are federally owned. \r\n\r\nThe objective of this study was to assemble through various means all the available pertinent information that could be brought together within the USGS and integrate these data into a computer-based digital cartographic data system that was focused upon the single issue of reviewing the known geological and geophysical data to determine the geologic characteristics favorable or unfavorable for the occurrence of petroleum resources in these Wilderness Lands. In a joint effort in the USGS between the Geologic Division (GD) and the National Mapping Division (NMD) all of the mappable information used in this study was prepared and processed by using digital cartographic techniques. These include digitizing the location and boundaries of the Wilderness Lands; acreage calculations; the boundaries of the USGS petroleum provinces; and the geologic and tectonic boundaries within each petroleum province and State. In addition, searches were conducted on well data files which provided the locations and geologic information on over 5,000 wells drilled within or immediately adjacent to the Wilderness Lands. \r\n\r\nAn analysis of all the geologic characteristics favorable or unfavorable for petroleum occurrence in conjunction with the geologic settings for the Wilderness Lands scattered within the framework of the petroleum provinces was performed by a team of geologists on each of the wilderness tracts. The geologic characteristics reviewed for each tract included the presence or absence of the following: adequate source beds and reservoir rocks; adequate trapping mechanisms; favorable thermal and maturation histories; presence of petroleum seeps or adjacent wells with shows or production; and the presence of favorable sedimentary rock sections underlying volcanic terrane or faulted and overthrust areas. \r\n\r\nA description of the geology and geologic framework is provided for each State along with an explanation of the interpretative geology and evaluation of the petroleum potential within the locale of each of the wilderness tracts. \r\n\r\nThe assessment of the petroleum resources on the Wilderness Lands was completed in two separate stages. In the first stage the geologists evaluated the geological characteristics for the favorability or lack of favorability for the occurrence of oil and natural gas within each wilderness tract and assigned a qualitative rating for each tract's potential for the occurrence of recoverable oil and gas resources. In the second stage in evaluating the petroleum potential for the wilderness tracts, an effort was made to arrive at a quantitative assessment within the framework of the USGS's latest published resource estimates which are made on a province basis. The geologic characteristics evaluated for the favorability of petroleum occurrence within each of the clusters of wilderness tracts were the determining factors for the subjective assessments of the petroleum potential for each wilderness tract occurring within the respective basin or province. The quantitative resource","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir902AP","usgsCitation":"1983, Petroleum potential of wilderness lands in the Western United States: U.S. Geological Survey Circular 902, 197 p. in various pagings :ill., maps ;26 cm., https://doi.org/10.3133/cir902AP.","productDescription":"197 p. in various pagings :ill., maps ;26 cm.","costCenters":[],"links":[{"id":117587,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0902a-p/report-thumb.jpg"},{"id":31474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0902a-p/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c4d","contributors":{"editors":[{"text":"Miller, Betty M.","contributorId":46929,"corporation":false,"usgs":true,"family":"Miller","given":"Betty","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":749261,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":28683,"text":"wri834028 - 1983 - Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:35","indexId":"wri834028","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":"83-4028","title":"Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834028","usgsCitation":"Meisler, H., 1983, Computer simulation model of the Pleistocene valley-fill aquifer in southwestern Essex and southeastern Morris counties, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 83-4028, 76 p. :maps ;28 cm., https://doi.org/10.3133/wri834028.","productDescription":"76 p. :maps ;28 cm.","costCenters":[],"links":[{"id":121639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4028/report-thumb.jpg"},{"id":57523,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4028/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7662","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":200226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9599,"text":"ofr83489 - 1983 - Mineral resource potential of the Granite Peak Roadless Area, Trinity County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr83489","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":"83-489","title":"Mineral resource potential of the Granite Peak Roadless Area, Trinity County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83489","usgsCitation":"Huber, D., and Nelson, S., 1983, Mineral resource potential of the Granite Peak Roadless Area, Trinity County, California: U.S. Geological Survey Open-File Report 83-489, 10 p. :maps ;28 cm., https://doi.org/10.3133/ofr83489.","productDescription":"10 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0489/report-thumb.jpg"},{"id":37330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d566","contributors":{"authors":[{"text":"Huber, D.F.","contributorId":93905,"corporation":false,"usgs":true,"family":"Huber","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":159979,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, S.C.","contributorId":30625,"corporation":false,"usgs":true,"family":"Nelson","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":159978,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10675,"text":"ofr83711 - 1983 - Geology of the Volga-Ural petroleum province and detailed description of the Ramashkino and Arlan oil fields","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr83711","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":"83-711","title":"Geology of the Volga-Ural petroleum province and detailed description of the Ramashkino and Arlan oil fields","docAbstract":"The Volga-Ural petroleum province is in general coincident with the Volga-Ural regional high, a broad upwarp of the east-central part of the Russian (East European) platform. The central part of the province is occupied by the Tatar arch, which contains the major share of the oil fields of the province. The Perm-Bashkir arch forms the northeastern part of the regional high, and the Zhigulevsko-Orenburg arch makes up the southern part. These arches are separated from one another by elongate downwarps. \r\n\r\nThe platform cover overlies an Archean crystalline basement and consists of seven main sedimentation cycles as follows: 1) Riphean (lower Bavly) continental sandstone, shale, and conglomerate beds from 500 to 5,000 m thick deposited in aulacogens. 2) Vendian (upper Bavly) continental and marine shale and sandstone up to 3,000 m thick. 3) Middle Devonian-Tournaisian transgressive deposits, which are sandstone, siltstone, and shale in the lower part and carbonates with abundant reefs in the upper; thickness is 300-1,000 m. In the upper carbonate part is the Kamsko-Kinel trough system, which consists of narrow interconnected deep-water troughs. 4) The Visean-Namurian-Bashkirian cycle, which began with deposition of Visean clastics that draped over reefs of the previous cycle and filled in an erosional relief that had formed in some places on the sediments of the previous cycle. The Visean clastics are overlain by marine carbonates. Thickness of the cycle is 50-800 m. 5) Early Moscovian-Early Permian terrigenous clastic deposits and marine carbonate beds 1,000-3,000 m thick. 6) The late Early Permian-Late Permian cycle, which reflects maximum growth of the Ural Mountains and associated Ural foredeep. Evaporites were first deposited, then marine limestones and dolomites, which intertongue eastward with clastic sediments from the Ural Mountains. 7) Continental redbeds of Triassic age and mixed continental and marine elastic beds of Jurassic and Cretaceous age, which were deposited on the southern, southwestern, and northern margins of the Russian platform; they are generally absent in the Volga-Ural province, however. \r\n\r\nThe Volga-Ural oil and gas basin is a single artesian system that contains seven aquifers separated by seals. The areas of greatest hydraulic head are in the eastern parts of the basin near areas where the aquifers crop out on the western slopes of the Ural Mountains. The Peri-Caspian basin is the principal drainage area of the artesian system. \r\n\r\nApproximately 600 oil and gas fields and 2,000 pools have been found in the Volga-Ural province. Nine productive sequences are recognized as follows: 1) Upper Proterozoic (Bavly beds), which are promising but not yet commercial. 2) Clastic Devonian, which contains the major reserves and includes the main pays of the super-giant Romashkino field. 3) Carbonate Upper Devonian and lowermost Carboniferous, which is one of the main reef-bearing intervals. 4) Visean (Lower Carboniferous) elastics, which are the main pays in the super-giant Arian field. 5) Carbonate Lower and Middle Carboniferous. 6) Clastic Middle Carboniferous Moscovian. 7) Carbonate Middle and Upper Carboniferous. 8) Carbonate-evaporite Lower Permian, which contains the major gas reserves and the lower part of the Melekess tar deposits. 9) Clastic-carbonate Upper Permian, which contains the major part of the Melekess tar deposits.\r\n\r\nThe Volga-Ural province is divided into several productive regions on a basis of differences in structure, distribution of reservoir and source-rock facies, and general composition of the petroleum accumulations. These regions are the Tatar arch, Birsk saddle, Upper Kama depression, Perm-Bashkir arch, Ufa-Orenburg monocline, Melekess-Sernovodsko-Abdulino basin, Zhligulevsko-Orenburg arch, Ural foredeep, and north borders of the Peri-Casplan depression. \r\n\r\nExploration activity has declined in recent years; however, interest remains high in several parts of the province, particula","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83711","usgsCitation":"Peterson, J.A., and Clarke, J.W., 1983, Geology of the Volga-Ural petroleum province and detailed description of the Ramashkino and Arlan oil fields: U.S. Geological Survey Open-File Report 83-711, vii, 175 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83711.","productDescription":"vii, 175 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0711/report-thumb.jpg"},{"id":38498,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0711/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c9b7","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clarke, James W.","contributorId":35297,"corporation":false,"usgs":true,"family":"Clarke","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161779,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":29578,"text":"wri834021 - 1983 - A reconnaissance of ground-water contamination at selected landfills in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri834021","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":"83-4021","title":"A reconnaissance of ground-water contamination at selected landfills in Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nOpen-File Services Section [distributor],","doi":"10.3133/wri834021","usgsCitation":"Schneider, P.A., and Turk, J., 1983, A reconnaissance of ground-water contamination at selected landfills in Colorado: U.S. Geological Survey Water-Resources Investigations Report 83-4021, iv, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834021.","productDescription":"iv, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119408,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4021/report-thumb.jpg"},{"id":58406,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a869a","contributors":{"authors":[{"text":"Schneider, P. A. Jr.","contributorId":18771,"corporation":false,"usgs":true,"family":"Schneider","given":"P.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201754,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turk, J.T.","contributorId":94259,"corporation":false,"usgs":true,"family":"Turk","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":201755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7762,"text":"ofr8386 - 1983 - An earthquake catalog for the Basin and Range Province, 1803-1977","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr8386","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":"83-86","title":"An earthquake catalog for the Basin and Range Province, 1803-1977","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8386","usgsCitation":"Askew, B., and Algermissen, S.T., 1983, An earthquake catalog for the Basin and Range Province, 1803-1977: U.S. Geological Survey Open-File Report 83-86, 42 p. maps ;28 cm., https://doi.org/10.3133/ofr8386.","productDescription":"42 p. maps ;28 cm.","costCenters":[],"links":[{"id":142266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0086/report-thumb.jpg"},{"id":35237,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35238,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0086/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35239,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0086/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35240,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0086/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684e1c","contributors":{"authors":[{"text":"Askew, Bonny","contributorId":85593,"corporation":false,"usgs":true,"family":"Askew","given":"Bonny","email":"","affiliations":[],"preferred":false,"id":156557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":156558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11338,"text":"ofr821007 - 1983 - Low-flow characteristics of Indiana streams","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr821007","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":"82-1007","title":"Low-flow characteristics of Indiana streams","docAbstract":"Knowledge of low-flow data for Indiana streams is essential to the planners and developers of water resources for municipal, industrial, and recreational uses in the State. Low-flow data for 219 continuous-record gaging stations through the 1978 water year and for some stations since then are presented in tables and curves. Flow-duration and low-flow-frequency data were estimated or determined for continuous-record stations having more than 10 years of record. In addition, low-flow-frequency data were estimated for 248 partial-record stations. Methods for estimating these data are included in the report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821007","usgsCitation":"Stewart, J.A., 1983, Low-flow characteristics of Indiana streams: U.S. Geological Survey Open-File Report 82-1007, ix, 284 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr821007.","productDescription":"ix, 284 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1007/report-thumb.jpg"},{"id":39146,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648610","contributors":{"authors":[{"text":"Stewart, J. A.","contributorId":50158,"corporation":false,"usgs":true,"family":"Stewart","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28366,"text":"wri834113 - 1983 - Effects of specific land uses on nonpoint sources of suspended sediment, nutrients, and herbicides, Pequea Creek basin, Pennsylvania, 1979-80","interactions":[],"lastModifiedDate":"2017-06-22T08:26:05","indexId":"wri834113","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":"83-4113","title":"Effects of specific land uses on nonpoint sources of suspended sediment, nutrients, and herbicides, Pequea Creek basin, Pennsylvania, 1979-80","docAbstract":"The Susquehanna River Basin Commission and the U.S. Environmental Protection Agency cooperated with the U.S. Geological Survey in a study to quantify nonpoint-source loadings from an agricultural area in Pennsylvania. Pequea Creek, a tributary to the Susquehanna River, drains a 154-square mile agricultural area in Lancaster County, Pennsylvania. Previous studies defined the Pequea Creek basin as a contributor of sediment, nutrients, and pesticides from nonpoint sources to the Susquehanna River. \r\n\r\nThe purpose of this intensive watershed investigation was to determine the effects of various land uses on water quality of receiving streams. Streamflow was measured and monthly base-flow samples and water-weighted composite storm samples were analyzed for suspended sediment, nutrients, organic carbon, and triazine herbicides. Constituent loadings were calculated to quantify their discharge from the entire Pequea Creek basin and from four specific subbasins: forest, cornfield, rural residential, and pasture. Soil samples were analyzed for nutrients and selected herbicides, and land use and application data were collected to determine the source of loadings. Precipitation amounts and chemistry were also measured. \r\n\r\nPrecipitation and streamflow were below average for much of the investigation period, May 1979 to December 1980. The annual precipitation for 1980 was 10 inches below normal, with drought conditions the last half of the year. \r\n\r\nDuring base flow, the highest concentrations of individual constituents generally observed were: 4.0 milligrams per liter total organic nitrogen and 1.4 milligrams per liter total phosphorus from the downstream pasture site; 24 milligrams per liter total nitrate nitrogen and 3.9 micrograms per liter total atrazine from the cornfield site; and 0.5 micrograms per liter total prometone, and 2.3 micrograms per liter total simazine from the residential site. Nearly all total nitrate nitrogen concentrations from the cornfield site during base flow were about double the U.S. Environmental Protection Agency (1977) criterion of 10 milligrams per liter. The highest constituent concentrations found in composite storm samples were nearly all in samples from the cornfield site. \r\n\r\nThe highest concentrations found were: 16,000 milligrams per liter suspended sediment, 54 milligrams per liter total organic nitrogen, 41 milligrams per liter total nitrate nitrogen, 19 milligrams per liter total phosphorus, and 200 micrograms per liter total atrazine. The highest concentrations found in composite storm samples for total prometone was 6.4 micrograms per liter at the residential site and for total simazine was 4.8 micrograms per liter at the downstream pasture site. \r\n\r\nGenerally, concentrations of all the constituents, except nitrate, were higher during storms than during base flow at all sites. Total concentrations of the constituents increase during storms predominantly due to increases in suspended concentrations. The highest storm concentrations of most constituents occurred at the cornfield site. Fertilizer and herbicide applications increase the available sources of nutrients and herbicides for transport to the stream. The highest phosphorus, atrazine, and suspended-sediment concentrations at the cornfield site occurred during intense storms soon after application and planting. \r\n\r\nConstituent yields (tons per square mile) from storms, about evenly distributed throughout the basin, were compared from the other specific land-use sites to the forest site, which represents a relatively undisturbed land use. During storms, yields for suspended sediment, total organic nitrogen, and total phosphorus were highest for the pasture and lowest for the forest site. Total nitrate-nitrogen yields were highest for the cornfield and about the same for the forest and residential sites. Yields of total organic carbon were about the same for the cornfield and residential sites, which were both slightly higher than the forest ","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834113","usgsCitation":"Lietman, P., Ward, J.R., and Behrendt, T., 1983, Effects of specific land uses on nonpoint sources of suspended sediment, nutrients, and herbicides, Pequea Creek basin, Pennsylvania, 1979-80: U.S. Geological Survey Water-Resources Investigations Report 83-4113, viii, 96 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834113.","productDescription":"viii, 96 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":57173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4113/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610ce7","contributors":{"authors":[{"text":"Lietman, P. L.","contributorId":63040,"corporation":false,"usgs":true,"family":"Lietman","given":"P. L.","affiliations":[],"preferred":false,"id":199680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ward, J. R.","contributorId":18015,"corporation":false,"usgs":false,"family":"Ward","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Behrendt, T.E.","contributorId":27887,"corporation":false,"usgs":true,"family":"Behrendt","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":199679,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11271,"text":"ofr83123 - 1983 - General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr83123","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":"83-123","title":"General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data","docAbstract":"Two satellite systems launched by the National Aeronautics and Space Administration (NASA) in 1978 carried sensors which operated in the thermal infrared (IR) region of the electromagnetic spectrum, The final IR radiation data provide spectral information about the physical properties of the Earth's surficial materials not duplicated in either the visible or reflective IR wavelength regions. Landsat 3, launched on March 5, 1978, contained a thermal sensor as part of the multispectral scanner (MSS) system. The sensor operated in the 10.4- to 12.6-?m (band 8) wavelength region and produced imagery with a ground resolution of approximately 235 m. \r\n\r\nLaunched on April 26) 1978) the Heat Capacity Mapping Mission (HCMM) spacecraft carried a sensor, the heat capacity mapping radiometer (HCMR) which operated in the 10.5- to 12.5?m wavelength region and produced imagery with a ground resolution of approximately 600 m at nadir. The HCMM satellite acquired over 6,600 data passes of visible (0.55-1.1 ?m), as well as thermal IR data, over North America, Europe, and Australia. \r\n\r\nGeneral characteristics and availability of Landsat 3 and HCMM thermal IR data are discussed. Landsat 3 reflected IR band 7 (0.55-1.1 ?m) and Landsat 3 band 8 thermal data acquired over the eastern and western United States are analyzed and compared with HCMM visible, thermal IR, thermal inertia, and day-night temperature difference imagery for geologic applications. Digitally processed and enhanced HCMM data (high-pass filters, diagonal derivatives, and band ratios), produced by the U.S. Geological Survey, Flagstaff) Ariz., are presented for geologic interpretation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83123","usgsCitation":"Southworth, C.S., 1983, General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data: U.S. Geological Survey Open-File Report 83-123, 30 p. maps (some col.) ;28 cm., https://doi.org/10.3133/ofr83123.","productDescription":"30 p. maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":142961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0123/report-thumb.jpg"},{"id":39063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec45","contributors":{"authors":[{"text":"Southworth, C. Scott 0000-0002-7976-7807 ssouthwo@usgs.gov","orcid":"https://orcid.org/0000-0002-7976-7807","contributorId":1608,"corporation":false,"usgs":true,"family":"Southworth","given":"C.","email":"ssouthwo@usgs.gov","middleInitial":"Scott","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":162841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10731,"text":"ofr83745 - 1983 - Hoffa Reef: a shelf-edge calcareous prominence in the northern Gulf of Mexico","interactions":[],"lastModifiedDate":"2014-12-16T12:53:24","indexId":"ofr83745","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":"83-745","title":"Hoffa Reef: a shelf-edge calcareous prominence in the northern Gulf of Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83745","usgsCitation":"Poppe, L., and Circe, R., 1983, Hoffa Reef: a shelf-edge calcareous prominence in the northern Gulf of Mexico: U.S. Geological Survey Open-File Report 83-745, i, 14 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83745.","productDescription":"i, 14 p. ill., maps ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":143527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0745/report-thumb.jpg"},{"id":38541,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0745/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bfd7","contributors":{"authors":[{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Circe, R.C.","contributorId":90300,"corporation":false,"usgs":true,"family":"Circe","given":"R.C.","affiliations":[],"preferred":false,"id":161871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8133,"text":"ofr83328 - 1983 - Effect of soil structure interaction on seismograms","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr83328","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":"83-328","title":"Effect of soil structure interaction on seismograms","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83328","usgsCitation":"Bycroft, G., and Mork, P., 1983, Effect of soil structure interaction on seismograms: U.S. Geological Survey Open-File Report 83-328, 8, 19 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83328.","productDescription":"8, 19 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0328/report-thumb.jpg"},{"id":35737,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0328/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6254dd","contributors":{"authors":[{"text":"Bycroft, G.N.","contributorId":106903,"corporation":false,"usgs":true,"family":"Bycroft","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":157203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mork, P.","contributorId":67513,"corporation":false,"usgs":true,"family":"Mork","given":"P.","affiliations":[],"preferred":false,"id":157202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4515,"text":"cir902G - 1983 - Petroleum potential of wilderness lands in Montana","interactions":[{"subject":{"id":4515,"text":"cir902G - 1983 - Petroleum potential of wilderness lands in Montana","indexId":"cir902G","publicationYear":"1983","noYear":false,"chapter":"G","title":"Petroleum potential of wilderness lands in Montana"},"predicate":"IS_PART_OF","object":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"chapter":"A-P","title":"Petroleum potential of wilderness lands in the Western United States"},"id":1}],"isPartOf":{"id":4364,"text":"cir902AP - 1983 - Petroleum potential of wilderness lands in the Western United States","indexId":"cir902AP","publicationYear":"1983","noYear":false,"title":"Petroleum potential of wilderness lands in the Western United States"},"lastModifiedDate":"2022-06-28T18:56:23.400709","indexId":"cir902G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"902","chapter":"G","title":"Petroleum potential of wilderness lands in Montana","docAbstract":"No abstract available.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f5c","contributors":{"authors":[{"text":"Perry, William J. Jr.","contributorId":32498,"corporation":false,"usgs":true,"family":"Perry","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":149383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rice, Dudley D.","contributorId":11601,"corporation":false,"usgs":true,"family":"Rice","given":"Dudley","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":149382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maughan, Edwin K.","contributorId":85172,"corporation":false,"usgs":true,"family":"Maughan","given":"Edwin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":149384,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9702,"text":"ofr83463 - 1983 - Description and history of mercury-tube tiltmeters used in the San Francisco Bay area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr83463","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":"83-463","title":"Description and history of mercury-tube tiltmeters used in the San Francisco Bay area, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83463","usgsCitation":"Jones, A.C., 1983, Description and history of mercury-tube tiltmeters used in the San Francisco Bay area, California: U.S. Geological Survey Open-File Report 83-463, 16 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83463.","productDescription":"16 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0463/report-thumb.jpg"},{"id":37416,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0463/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd7a","contributors":{"authors":[{"text":"Jones, Alan C.","contributorId":94307,"corporation":false,"usgs":true,"family":"Jones","given":"Alan","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160155,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8407,"text":"ofr83605 - 1983 - Novice's guide to PACER-GARNET for use with the National Coal Resources Data System; a flow chart","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr83605","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":"83-605","title":"Novice's guide to PACER-GARNET for use with the National Coal Resources Data System; a flow chart","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83605","usgsCitation":"Connor, C.W., 1983, Novice's guide to PACER-GARNET for use with the National Coal Resources Data System; a flow chart: U.S. Geological Survey Open-File Report 83-605, 4 p. ill. ;28 cm., https://doi.org/10.3133/ofr83605.","productDescription":"4 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0605/report-thumb.jpg"},{"id":35974,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0605/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968c1","contributors":{"authors":[{"text":"Connor, Carol Waite","contributorId":87943,"corporation":false,"usgs":true,"family":"Connor","given":"Carol","email":"","middleInitial":"Waite","affiliations":[],"preferred":false,"id":157665,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3421,"text":"cir1001 - 1983 - Estimated Use of Water in the United States in 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir1001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1001","title":"Estimated Use of Water in the United States in 1980","docAbstract":"Water use in the United States in 1980 was estimated to be an average of 450 bgd (billion gallons per day) of fresh and saline water for offstream uses- an 8-percent increase from the 1975 estimate and a 22-percent increase from the 1970 estimate. Average per capita use for all offstream uses was 2,000 gpd (gallons per day) of fresh and saline water, and 1,600 gpd of fresh water; this represents a slight increase since 1975. Offstream uses include (1) public supply (domestic, public, commercial, and industrial uses), (2) rural (domestic and livestock uses), (3) irrigation, and (4) self-supplied industrial uses (including thermoelectric power). From 1975 to 1980, public supply use increased 15 percent to 34 bgd, rural use increased 14 percent to 5.6 bgd, irrigation use increased 7 percent to 150 bgd, and self-supplied industrial use increased 8 percent to 260 bgd. Within the industrial category, thermoelectric power generation increased 9 percent to 210 bgd, whereas other self-supplied industrial uses remained approximately constant at 45 bgd. Total fresh water consumed- that part of water withdrawn that is no longer available for subsequent use- by these offstream uses increased 7 percent to 100 bgd, with irrigation accounting for the largest part of water consumed, estimated at 83 bgd. Estimates of withdrawals by source indicate that from 1975 to 1980, total groundwater withdrawals increased 7 percent to 89 bgd, and total surface-water withdrawals increased 9 percent to 360 bgd. Total saline-water withdrawals increased by about 2 bgd to 72 bgd, of which 71 bgd was saline surface water. Reclaimed sewage amounted to about 0.5 bgd in 1980, an 11-percent decrease from 1975. Water used for hydroelectric power generation, an instream use, remained unchanged from 1975 at 3,300 bgd. This is in contrast to the increasing trend from 1950 to 1975. Although 1980 estimates of water use were higher than the 1975 estimates for all offstream categories, trends establishing during the periods 1970 to 1975 and 1975 to 1980 indicate a general slackening in the rate of increase of total withdrawls in comparison to the period 1965 to 1970. (USGS)","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/cir1001","usgsCitation":"Solley, W.B., Chase, E.B., and Mann, W.B., 1983, Estimated Use of Water in the United States in 1980: U.S. Geological Survey Circular 1001, vii, 56 p., https://doi.org/10.3133/cir1001.","productDescription":"vii, 56 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":123908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/1001/report-thumb.jpg"},{"id":30436,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/1001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd54","contributors":{"authors":[{"text":"Solley, Wayne B.","contributorId":61409,"corporation":false,"usgs":true,"family":"Solley","given":"Wayne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mann, William B. IV","contributorId":8838,"corporation":false,"usgs":true,"family":"Mann","given":"William","suffix":"IV","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146872,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9549,"text":"ofr83271 - 1983 - Ground water in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":9549,"text":"ofr83271 - 1983 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr83271","publicationYear":"1983","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":1903,"text":"wsp2248 - 1987 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2248","publicationYear":"1987","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"supersededBy":{"id":1903,"text":"wsp2248 - 1987 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2248","publicationYear":"1987","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"lastModifiedDate":"2021-03-05T02:11:45.24522","indexId":"ofr83271","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":"83-271","title":"Ground water in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"The potential for developing oil-shale resources in the southeastern Uinta Basin of Utah and Colorado has created the need for information on the quantity and quality of water available in the area. This report describes the availability and chemical quality of ground water, which might provide a source or supplement of water supply for an oil-shale industry.
Ground water in the southeastern Uinta Basin occurs in three major aquifers. Alluvial aquifers of small areal extent are present in valley-fill deposits of six major drainages. Consolidated-rock aquifers include the bird's-nest aquifer in the Parachute Creek Member of the Green River Formation, which is limited to the central part of the study area; and the Douglas Creek aquifer, which includes parts of the Douglas Creek Member of the Green River Formation and parts of the intertonguing Renegade Tongue of the Wasatch Formation; this aquifer underlies most of the study area.
The alluvial aquifers are recharged by infiltration of streamflow and leakage from consolidated-rock aquifers. Recharge is estimated to average about 32,000 acre-feet per year. Discharge from alluvial aquifers, primarily by evapotranspiration, also averages about 32,000 acre-feet per year. The estimated volume of recoverable water in storage in alluvial aquifers is about 200,000 acre-feet. Maximum yields to individual wells are less than 1,000 gallons per minute.
Recharge to the bird's-nest aquifer, primarily from stream infiltration and downward leakage from the overlying Uinta Formation, is estimated to average 670 acre-feet per year. Discharge from the bird's-nest aquifer, which is primarily by seepage to Bitter Creek and the White River, is estimated to be 670 acre-feet per year. The estimated volume of recoverable water in storage in the bird's-nest aquifer is 1.9 million acre-feet. Maximum yields to individual wells in some areas may be as much as 5,000 gallons per minute.
A digital-computer model of the flow system was used to evaluate the effects of oil-shale development on the bird's-nest aquifer at the Federal lease tracts Ua and Ub. Results of model simulations indicate that during construction of a vertical access shaft, a pumping rate of about 900 gallons per minute would be required to dewater the aquifer. The model also indicates that the construction of a proposed reservoir on the White River may raise water levels in the bird's-nest aquifer near the reservoir site by as much as 45 feet.
The flow model was used to evaluate the potential ground-water supply available for oil-shale development in the vicinity of the Federal lease tracts Ua and Ub. The results of the simulation indicate that the bird's-nest aquifer could supply about 10,000 acre-feet of water per year at that site, for a period of 20 years. Drawdown after 20 years of pumping would exceed 250 feet near the simulated well field. Based on the results of the model simulation, it is estimated that the aquifer could simultaneously supply another 10,000 acre-feet of water per year in the northern part of the study area, but some interference between well fields could be expected.
The Douglas Creek aquifer is recharged by precipitation and stream infiltration at an average rate of about 20,000 acre-feet per year. Discharge is estimated to be about the same and is primarily through springs and diffuse seepage. The estimated volume of recoverable water in storage is 16 million acre-feet. Maximum yields to individual wells are estimated to be less than 500 gallons per minute.