{"pageNumber":"1634","pageRowStart":"40825","pageSize":"25","recordCount":46644,"records":[{"id":7417,"text":"ofr8236 - 1982 - Potential geologic hazards and constraints for blocks in proposed North Atlantic OCS Oil and gas lease sale 52","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr8236","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-36","title":"Potential geologic hazards and constraints for blocks in proposed North Atlantic OCS Oil and gas lease sale 52","docAbstract":"Analysis of high-resolution geophysical data collected over 540 blocks tentatively selected for leasing in proposed OCS Oil and Gas Lease Sale 52 (Georges Bank) revealed a number of potential geologic hazards to oil and gas exploration and development activities: evidence of mass movements and shallow gas deposits on the continental slope. No potential hazards were observed on the continental shelf or rise. Other geology-related problems, termed constraints because they pose a relatively low degree of risk and can be routinely dealt with by the use of existing technology have been observed on the continental shelf. Constraints identified in the proposed sale area are erosion, sand waves, filled channels and deep faults. \r\n\r\nPiston cores were collected for geotechnical analysis at selected locations on the continental slope in the proposed lease sale area. The core locations were selected to provide information on slope stability and to establish the general geotechnical properties of the sediments. Preliminary results of a testing program suggest that the surficial sediment cover is stable with respect to mass movement.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8236","usgsCitation":"Carpenter, G., Cardinell, A., Francois, D., Good, L., Lewis, R., and Stiles, N., 1982, Potential geologic hazards and constraints for blocks in proposed North Atlantic OCS Oil and gas lease sale 52: U.S. Geological Survey Open-File Report 82-36, ii, 54 p., 3 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr8236.","productDescription":"ii, 54 p., 3 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":141517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0036/report-thumb.jpg"},{"id":34823,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0036/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34824,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0036/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34825,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0036/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8801","contributors":{"authors":[{"text":"Carpenter, G.B.","contributorId":54593,"corporation":false,"usgs":true,"family":"Carpenter","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":155523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cardinell, A.P.","contributorId":59033,"corporation":false,"usgs":true,"family":"Cardinell","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":155524,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Francois, D.K.","contributorId":101666,"corporation":false,"usgs":true,"family":"Francois","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":155527,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Good, L.K.","contributorId":103279,"corporation":false,"usgs":true,"family":"Good","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":155528,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lewis, R.L.","contributorId":82306,"corporation":false,"usgs":true,"family":"Lewis","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":155526,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stiles, N.T.","contributorId":59034,"corporation":false,"usgs":true,"family":"Stiles","given":"N.T.","email":"","affiliations":[],"preferred":false,"id":155525,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":56284,"text":"wdrWA802 - 1982 - Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2025-07-21T17:52:28.421042","indexId":"wdrWA802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-80-2","title":"Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington","docAbstract":"

Water Resources data for the 1980 water year for Washington consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report in two volumes contains records for water discharge at 233 gaging stations stage only at 5 gaging stations; stage and contents at 41 lakes and reservoirs; and water quality at 39 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 14 crest-stage, and 89 water-quality partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local and Federal agencies in Washington.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA802","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-80-2, x, 332 p., https://doi.org/10.3133/wdrWA802.","productDescription":"x, 332 p.","costCenters":[],"links":[{"id":492667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/wa-80-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174737,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/wa-80-2/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0b03","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":532475,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28725,"text":"wri8184 - 1982 - Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80","interactions":[],"lastModifiedDate":"2019-12-05T08:35:31","indexId":"wri8184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-84","title":"Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80","docAbstract":"This report is a complilation of geologic, hydrologic, and water-quality data and information on test holes collected in the vicinity of gypsum stack complexes at two phosphate chemical plants and one phosphatic clayey waste disposal pond at a phosphate mine and beneficiation plant in central Florida. The data were collected from September 1979 to October 1980 at thee AMAX Phosphate, Inc., chemical plant, Piney Point; the USS AgriChemicals chemical plant, Bartow; and the International Minerals and Chemical Corporation Clear Springs mine, Bartow. Approximmmtely 5,400 field and laboratory water-quality determinations on water samples were collected from about 78 test holes and 31 surface-water, rainfall, and other sampling sites at phosphate industry beneficiation and chemical plant waste-disposal operations. Maps show locations of sampling sites. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8184","usgsCitation":"Miller, R.L., and Sutcliffe, H., 1982, Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80: U.S. Geological Survey Water-Resources Investigations Report 81-84, vii, 77 p. , https://doi.org/10.3133/wri8184.","productDescription":"vii, 77 p. 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features","indexId":"ofr82284","publicationYear":"1982","noYear":false,"title":"Digital colored residual and regional Bouguer gravity maps of the conterminous United States: Comments on significant features"},"predicate":"SUPERSEDED_BY","object":{"id":64274,"text":"gp953A - 1982 - Digital colored residual and regional Bouguer gravity maps of the conterminous United States with cut-off wavelengths of 250 km and 1000 km","indexId":"gp953A","publicationYear":"1982","noYear":false,"chapter":"A","title":"Digital colored residual and regional Bouguer gravity maps of the conterminous United States with cut-off wavelengths of 250 km and 1000 km"},"id":1}],"supersededBy":{"id":64274,"text":"gp953A - 1982 - Digital colored residual and regional Bouguer gravity maps of the conterminous United States with cut-off wavelengths of 250 km and 1000 km","indexId":"gp953A","publicationYear":"1982","noYear":false,"title":"Digital colored residual and regional Bouguer gravity maps of the conterminous United States with cut-off wavelengths of 250 km and 1000 km"},"lastModifiedDate":"2025-09-23T18:48:26.228859","indexId":"ofr82284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-284","title":"Digital colored residual and regional Bouguer gravity maps of the conterminous United States: Comments on significant features","docAbstract":"

The gravity maps were prepared from data obtained primarily from data files maintained by the Defense Mapping Agency of the Department of Defense and the Canadian Gravity Data Centre of the Earth Physics Branch of the Department of Energy, Mines, and Resources (Canada). The maps have been used in studies relating to earthquake/reactor hazards, geothermal energy, and nuclear repository site programs of the U.S. Geological Survey. Those shown here (250 km and 1000 km wavelength cut-off regional and residual gravity maps) are part of a series of digital gravity and terrain maps of the United States currently being developed by the authors.

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Water resources data for the 1981 water year for New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of ground-water wells. This volume contains records for water discharge at 105 gaging stations; stage only at 6 gaging stations; and stage and contents at 4 gaging stations and 19 other lakes and reservoirs; water quality at 29 gaging stations, 5 precipitation stations and 4 partial-record stations; and water levels at 23 observation wells. Also included are data for 50 crest-stage and 14 low-flow partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data together with the data in Volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in New York.

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No abstract available. 

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York\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f26","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":532448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7689,"text":"ofr8228 - 1982 - Geophysical logs of four drill holes, Acord Lakes and Emery West quadrangles, Sevier County, Utah","interactions":[],"lastModifiedDate":"2024-04-04T22:26:03.547569","indexId":"ofr8228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-28","title":"Geophysical logs of four drill holes, Acord Lakes and Emery West quadrangles, Sevier County, Utah","docAbstract":"

This report presents the geophysical logs for four drill holes drilled during 1981 in the Skumpah Creek area (Acord Lakes quadrangle) and The Pines area (Emery West quadrangle), Sevier County, Utah. Figures 1 and 2 show drill-hole locations, and figures 3-7 are the geophysical logs. The drilling was done by a private drilling company under contract to the U.S. Geological Survey. The sites of all the drill holes are within the Wasatch Plateau Known Recoverable Coal Resource Area (KRCRA). Three of the sites are in the Richfield Ranger District of the Fishlake National Forest and one site is in the Ferron Ranger District of the Manti-LaSal National Forest. The purpose of the drilling was to identify and evaluate coal resources under public lands that may be included in a future coal leasing program.

The area is underlain by Cretaceous and younger rocks (table 1). The coal seams of economic interest are in the lower 200 ft of the Upper Cretaceous Blackhawk Formation, a complex sequence of intertonguing sandstone, shale, and coal. Regional dip of the strata in the area is approximately 2° to the northwest. The geology and coal resources of the area were described by Spieker (1931), Doelling (1972), and Smith (1981).

The drill holes were rotary drilled and the thicknesses and depths were determined from geophysical logs. In order to obtain data on the quality of the coal, the coal-bearing section in one hole was core drilled. Table 2 gives the drilling and logging information for the four completed holes. All drill holes were bottomed in the Upper Cretaceous Star Point Sandstone.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8228","usgsCitation":"Albee, H., 1982, Geophysical logs of four drill holes, Acord Lakes and Emery West quadrangles, Sevier County, Utah: U.S. Geological Survey Open-File Report 82-28, Report: 5 p.; 5 Figures: 13.44 x 136.13 inches or smaller, https://doi.org/10.3133/ofr8228.","productDescription":"Report: 5 p.; 5 Figures: 13.44 x 136.13 inches or smaller","costCenters":[],"links":[{"id":427436,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1982/0028/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427435,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1982/0028/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427434,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1982/0028/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427433,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1982/0028/figure-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427432,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1982/0028/figure-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427431,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142239,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0028/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Sevier County","otherGeospatial":"Acord Lakes Quadrangle, Emery West Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112.23445578007876,\n 38.91268818292647\n ],\n [\n -112.23445578007876,\n 38.566278446137346\n ],\n [\n -111.44459561201772,\n 38.566278446137346\n ],\n [\n -111.44459561201772,\n 38.91268818292647\n ],\n [\n -112.23445578007876,\n 38.91268818292647\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b527","contributors":{"authors":[{"text":"Albee, Howard F.","contributorId":64252,"corporation":false,"usgs":true,"family":"Albee","given":"Howard F.","affiliations":[],"preferred":false,"id":156442,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8027,"text":"ofr80557 - 1982 - Trichloroethylene in the ground-water supply of Pease Air Force Base, Portsmouth, New Hampshire","interactions":[],"lastModifiedDate":"2024-03-25T18:21:18.752437","indexId":"ofr80557","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-557","title":"Trichloroethylene in the ground-water supply of Pease Air Force Base, Portsmouth, New Hampshire","docAbstract":"

TCE (trichloroethylene) in concentrations that may be hazardous to health occurs in the water of an ice-contact largely sand and gravel aquifer (called the main aquifer) underlying much of the PAFB (Pease Air Force Base). In 1977 and 1978, the highest TCE concentration was found surrounding the most productive well, Haven well. Large quantities of TCE were used for degreasing between 1955 and 1965 and, so far as is known, TCE was used extensively up until 1973. Data on how, where, and when TCE got into the aquifer are lacking, but geochemical evidence and TCE analyses show a strong relation between the high TCE concentrations near Haven well and the extensive storm-drain system that underlies the parking apron and runway. The drains help recycle some of the TCE-contaminated ground water from the Haven well area.

Sources of TCE-free ground water on PAFB may exist in the northern parts and do exist in the southern parts of the main aquifer; however, in the southern part, either the ground water is probably already being used nearly to capacity (Smith and Harrison production wells) or further development might adversely affect off-base ground-water use. In the northern part, available subsurface data indicate that only relatively small yields are likely at any one site; thus, to get sustained yields comparable to that of the Haven well would probably require an unreasonable number of wells.

This study locates TCE contamination in the main PAFB aquifer and discusses three possible water-use alternatives: (I) Abandonment of Haven well, (2) treatment of Haven well water to remove TCE, and (3) treatment of a portion of Haven well water for domestic consumption and use of the remainder for nondomestic uses. Continued use of the Haven well, with treatment of all or part of its yield for TCE removal, is advantageous, both because the Haven well is a high-yield source of water and because cessation of pumping from it might allow TCE-contaminated ground water to move downgradient (southward), endangering the Smith and Harrison production wells. Continued study and monitoring of the TCE contamination would help in predicting when the contamination problem will no longer be threatening.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80557","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Bradley, E., 1982, Trichloroethylene in the ground-water supply of Pease Air Force Base, Portsmouth, New Hampshire: U.S. Geological Survey Open-File Report 80-557, Report: iv, 22 p.; 8 Plates: 12.40 x 10.18 inches or smaller, https://doi.org/10.3133/ofr80557.","productDescription":"Report: iv, 22 p.; 8 Plates: 12.40 x 10.18 inches or smaller","costCenters":[],"links":[{"id":427001,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427000,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426999,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426998,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426997,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426996,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426995,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426994,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1980/0557/figure-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":426993,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0557/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141499,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0557/report-thumb.jpg"}],"country":"United States","state":"New Hampshire","city":"Portsmouth","otherGeospatial":"Pease Air Force Base","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.82239490389902,\n 43.10272920652986\n ],\n [\n -70.82239490389902,\n 43.015435633341184\n ],\n [\n -70.69191552120652,\n 43.015435633341184\n ],\n [\n -70.69191552120652,\n 43.10272920652986\n ],\n [\n -70.82239490389902,\n 43.10272920652986\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6247d5","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":157011,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7296,"text":"ofr82406 - 1982 - Lode gold and silver occurrences in Alaska","interactions":[{"subject":{"id":7296,"text":"ofr82406 - 1982 - Lode gold and silver occurrences in Alaska","indexId":"ofr82406","publicationYear":"1982","noYear":false,"title":"Lode gold and silver occurrences in Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":61994,"text":"mr84 - 1984 - Map showing occurrences of lode gold and silver in Alaska","indexId":"mr84","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of lode gold and silver in Alaska"},"id":1}],"supersededBy":{"id":61994,"text":"mr84 - 1984 - Map showing occurrences of lode gold and silver in Alaska","indexId":"mr84","publicationYear":"1984","noYear":false,"title":"Map showing occurrences of lode gold and silver in Alaska"},"lastModifiedDate":"2023-09-29T20:05:34.765896","indexId":"ofr82406","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-406","title":"Lode gold and silver occurrences in Alaska","docAbstract":"

The following references give data, as of September 1, 1981, on localities where lode gold or silver has been found and are keyed to locations shown on the accompanying map. An asterisk (*) preceding a locality name indicates recorded production. In most instances the report(s) cited for each occurrence is a summary of data in older reports and was compiled since 1975. Most of the summary reports contain lists of the reports used in their compilation. Citations are in standard bibliographic format with the exception that each includes, in parentheses, an abbreviation for the report series and the number of the report. Abbreviations are: AOF, State of Alaska Division of Geological and Geophysical Surveys Open-File Report; B, U.S. Geological Survey Bulletin; BMOF, U.S. Bureau of Mines Open-File Report; MF, U.S. Geological Survey Miscellaneous Field Studies Map; OF, U.S. Geological Survey Open-File Report.

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Edward H.","contributorId":64689,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward H.","affiliations":[],"preferred":false,"id":155109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9364,"text":"ofr82434 - 1982 - Flood data in West Windsor Township, Mercer County, New Jersey, through 1981 water year","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-434","title":"Flood data in West Windsor Township, Mercer County, New Jersey, through 1981 water year","docAbstract":"Flood stages and peak discharges are described for 13 sites on streams in West Windsor Township, Mercer County, New Jersey, and surrounding areas, collected by the U.S. Geological Survey through the 1981 water year. Included are descriptions and elevations of floodmarks at 30 sites located by the West Windsor Township Environmental Commission after the September 25-27, 1975 flood. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82434","usgsCitation":"Harriman, D., and Velnich, A., 1982, Flood data in West Windsor Township, Mercer County, New Jersey, through 1981 water year: U.S. Geological Survey Open-File Report 82-434, 27 p., map ;28 cm., https://doi.org/10.3133/ofr82434.","productDescription":"27 p., map ;28 cm.","costCenters":[],"links":[{"id":140861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0434/report-thumb.jpg"},{"id":37074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0434/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b7e4b07f02db5cc5ac","contributors":{"authors":[{"text":"Harriman, D.A.","contributorId":27860,"corporation":false,"usgs":true,"family":"Harriman","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":159548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Velnich, A. J.","contributorId":25149,"corporation":false,"usgs":true,"family":"Velnich","given":"A. J.","affiliations":[],"preferred":false,"id":159547,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7253,"text":"ofr821001 - 1982 - Proceedings, Illinois water-data-users meeting","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr821001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1001","title":"Proceedings, Illinois water-data-users meeting","docAbstract":"The increased demand for water and concern for the quality of the water resources of Illinois have lead to increased demand for water-resources data. Representatives of the major water-data-collecting and water-data-using agencies met in Peoria, Illinois, on February 23-24, 1982, to (1) exchange information on current water-data programs and needs; (2) identify areas where data are needed; and (3) foster coordination and cooperation between agencies.\r\nRecommendations of the group included (1) annual meetings of agencies for coordination of activities; (2) standard methods for collecting and analyzing water data be adopted; (3) a centralized data system be established as a means of sharing water data; (4) water data should be indexed and cataloged, either by each agency or by some centralized system; (5) a statewide water-data-coordination committee should be formed with members from all water-related agencies; (6) a work group be formed to consider the use of uniform water-data codes; and (7) a cooperative working agreement be developed among all water-data-collection agnecies in the State to coordinate and maximize efforts on basin-intensive projects.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821001","usgsCitation":"Toler, L., 1982, Proceedings, Illinois water-data-users meeting: U.S. Geological Survey Open-File Report 82-1001, iii, 93 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr821001.","productDescription":"iii, 93 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1001/report-thumb.jpg"},{"id":34631,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66034a","contributors":{"authors":[{"text":"Toler, L. G. (compiler)","contributorId":60633,"corporation":false,"usgs":true,"family":"Toler","given":"L. G.","suffix":"(compiler)","affiliations":[],"preferred":false,"id":154911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3677,"text":"cir881 - 1982 - Assessment of undiscovered conventionally recoverable petroleum resources of the Arabian-Iranian Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"cir881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"881","title":"Assessment of undiscovered conventionally recoverable petroleum resources of the Arabian-Iranian Basin","docAbstract":"The estimates of undiscovered conventionally recoverable petroleum resources in the Arabian-Iranian basin at probability levels of 95 percent, 5 percent, and statistical mean are for oil (in billions of barrels): 72, 337, and 174; and for gas (in trillions of cubic feet): 299, 1792, and 849. The occurrence of petroleum can be accounted for in five definitive geological settings or plays. The assessment of undiscovered resource potential assumes that the new discoveries will expand the occurrence of petroleum in these basic plays; no additional plays with significant petroleum potential were recognized. The five plays listed by geologic age are: (I) Upper Cretaceous and Tertiary, (II) Lower and Middle Cretaceous sandstone, (III) Lower and Middle Cretaceous limestone, (IV) Jurassic, and (V) Permian. The Permian play, located in the south-central Arabian Gulf region and extending northeast-southwest from southern Iran to the Ar Rub' al Khali in Saudi Arabia, accounts for over four-fifths of the mean estimate of undiscovered gas. The remainder of the gas is divided about equally among the other four plays. The Jurassic play, located on the south side of the Arabian Gulf, accounts for slightly less than one-third of the estimated undiscovered oil, which is split equally between Saudi Arabia and Iraq. The Lower and Middle Cretaceous limestone play is located in the southern Gulf region and accounts for about one-fifth of the undiscovered oil, most of which is located in Saudi Arabia and the remainder in the United Arab Emirates. The Lower and Middle Cretaceous sandstone play is centralized in Kuwait at the head of the Arabian Gulf with significant potential extending to the northwest in Iraq; the play accounts for about one-third of the undiscovered oil, the great majority of which is estimated to be in Iraq with the remainder divided between Saudi Arabia and Kuwait. The upper Cretaceous-Tertiary play is located in the Zagros fold belt of Iran and Iraq and accounts for about one-fifth of the undiscovered oil. \r\n\r\nEstimation of the resources in this vast area is hindered by lack of data from certain broad regions, abandoned wells, and several significant dry holes, but the regional geology is well enough reported that geologic projections can be made and inferences from selected wells can be drawn to permit estimation of the resource potential.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir881","usgsCitation":"Masters, C.D., Klemme, H.D., and Coury, A.B., 1982, Assessment of undiscovered conventionally recoverable petroleum resources of the Arabian-Iranian Basin: U.S. Geological Survey Circular 881, v, 12 p. :ill. ;26 cm., https://doi.org/10.3133/cir881.","productDescription":"v, 12 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":124437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0881/report-thumb.jpg"},{"id":30725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0881/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d8c3","contributors":{"authors":[{"text":"Masters, Charles D.","contributorId":38969,"corporation":false,"usgs":true,"family":"Masters","given":"Charles","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":147392,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klemme, H. Douglas","contributorId":80653,"corporation":false,"usgs":true,"family":"Klemme","given":"H.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":147393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coury, Anny B.","contributorId":91470,"corporation":false,"usgs":true,"family":"Coury","given":"Anny","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147394,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8002,"text":"ofr811008 - 1982 - Irrigation-water quality in the Sulphur Creek basin, Yakima and Benton counties, Washington, April 1976 through March 1977","interactions":[],"lastModifiedDate":"2021-09-08T12:11:44.546053","indexId":"ofr811008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1008","title":"Irrigation-water quality in the Sulphur Creek basin, Yakima and Benton counties, Washington, April 1976 through March 1977","docAbstract":"A water-quality-sampling network was designed for the Sulphur Creek basin to observe the effects of farming practices on irrigation. Sediment and nutrient yield, discharge, and water temperature data were collected during the 1976 irrigation season and the following fall and winter. The suspended-sediment yield of the basin during this period was 2.0 tons per acre of irrigated cropland. Only about 3% of the net outflow of sediment occurred during the nonirrigation season. The yield computed by subbasin ranged from 0.7 to 7 tons per acre, depending mainly on land slope, but a high percentage of orchard land in the subbasins was probably also significant in reducing loads. Nutrient outflows during the study period were 1,180,000 pounds of nitrogen and 120,000 pounds of phosphorous. Nitrate-plus-nitrite represent 70% of the nitrogen outflow in the irrigation season and 84% in the nonirrigation season. The monitoring network was discontinued at the end of the study period, due largely to insufficient farmer participation. Network sensitivity in the control subbasins was inadequate to detect the effects of a planned demonstration program of best management practices. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811008","usgsCitation":"Boucher, P.R., and Fretwell, M.O., 1982, Irrigation-water quality in the Sulphur Creek basin, Yakima and Benton counties, Washington, April 1976 through March 1977: U.S. Geological Survey Open-File Report 81-1008, Report: vii, 68 p.; 1 Plate: 21.07 × 25.65 inches, https://doi.org/10.3133/ofr811008.","productDescription":"Report: vii, 68 p.; 1 Plate: 21.07 × 25.65 inches","costCenters":[],"links":[{"id":140339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1008/report-thumb.jpg"},{"id":388920,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11859.htm"},{"id":35563,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1008/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35562,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1008/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"Benton County, Yakima County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.7500,\n 46.5\n ],\n [\n -120.0830,\n 46.5\n ],\n [\n -120.0830,\n 46.2500\n ],\n [\n -119.7500,\n 46.2500\n ],\n [\n -119.7500,\n 46.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db62424e","contributors":{"authors":[{"text":"Boucher, P. R.","contributorId":108088,"corporation":false,"usgs":true,"family":"Boucher","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":156966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fretwell, M. O.","contributorId":50518,"corporation":false,"usgs":true,"family":"Fretwell","given":"M.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":156965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7978,"text":"ofr82585 - 1982 - The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations","interactions":[{"subject":{"id":7978,"text":"ofr82585 - 1982 - The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations","indexId":"ofr82585","publicationYear":"1982","noYear":false,"title":"The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations"},"predicate":"SUPERSEDED_BY","object":{"id":38521,"text":"pp1355 - 1988 - The Giles County, Virginia, seismic zone– Seismological results and geological interpretations","indexId":"pp1355","publicationYear":"1988","noYear":false,"title":"The Giles County, Virginia, seismic zone– Seismological results and geological interpretations"},"id":1}],"supersededBy":{"id":38521,"text":"pp1355 - 1988 - The Giles County, Virginia, seismic zone– Seismological results and geological interpretations","indexId":"pp1355","publicationYear":"1988","noYear":false,"title":"The Giles County, Virginia, seismic zone– Seismological results and geological interpretations"},"lastModifiedDate":"2026-01-21T17:27:41.443217","indexId":"ofr82585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-585","title":"The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations","docAbstract":"

This paper describes and interprets a newly-recognized 40-km-long seismogenic zone, which is inferred to have been the locus of a damaging earthquake in 1897. That shock was the second largest known to have occurred in the southeastern United States (MMI VIII, mb estimated at 5.8, felt over 725,000 km2). It struck Giles County in southwestern Virginia, and a recurrence would affect populous regions on and near the central Atlantic seaboard. This paper attempts to aid in evaluating that hazard by presenting and synthesizing new seismological data with geological inferences and deductions.

A five-station, 60-km aperture seismic network has been in operation in the Giles County locale since early 1978. For the subsequent 3-year monitoring period, 10 microearthquakes (M < 2) have been detected. Eight of those 10 events, plus an additional 4 relocated felt earthquakes (3.2 < M < 4.1; 1959-1976) have a tabular distribution centered at Pearisburg, Virginia. That distribution is about 40 km long, 10 km wide, strikes N. 43° E., and has a nearly vertical extent of from 5 km to 25 km in depth. Thus, a Giles County seismogenic zone is defined presently by 12 earthquakes that span 4 orders of magnitude (0 < M < 4) and 2 decades of time (1959-1980). We conclude that the 1897 earthquake occurred on that seismogenic zone. From the orientation of the tabular zone, from evidence that greatest horizontal compressive stress trends east-northeasterly at seismogenic depths in and near Giles County and from sparse P-wave first-motion data, we infer that the monitored microseismicity probably occurs by right-reverse motion on the seismogenic zone, with the southeast side dropping down with respect to the northwest side.

In the Giles County locale, the upper 3-6 km of the crust are Paleozoic sedimentary rocks that have moved some tens of kilometers northwest on nearly horizontal detachment faults. The above-mentioned reliable hypocenters for the region lie below the deepest likely detachment, indicating that Giles County seismicity probably has no simple relationship to surface geology.

Since Precambrian time, three deformational episodes could have formed steep faults under today's surface structures, at the observed hypocentral depths. These episodes were as follows: (1) As the Iapetus Ocean (Atlantic's predecessor) opened in late Precambrian or early Paleozoic time, northeast-striking normal faults formed, probably at the inferred Iapetan continental edge in central Virginia and at least as far northwest of that locus as Giles County. (2) In late Paleozoic time, detachment faults loaded the crust with several kilometers of overthrust sedimentary rocks, perhaps forming northeast-striking thrust-load faults in a brittle analogue of isostatic depression caused by thrust masses and much lighter continental glaciers. (3) As the Atlantic Ocean opened in Mesozoic time, other northeast-striking normal faults formed on the present continental margin and inland of it.

The N. 43° E.-striking seismogenic zone seems most likely to have resulted from compressional reactivation of an Iapetan normal fault, which also may have been reactivated by late Paleozoic compression and Mesozoic extension. First, the seismogenic zone probably does not occur on a thrust-load fault. The zone underlies detached structures of southern Appalachian orientations (east-northeast), but those structures are not known to be displaced where they cross the zone. Thus, if the zone occurs on a thrust-load fault, the fault and its coeval causative central Appalachian detachments would pre-date the southern Appalachian structures. That deduction contradicts stratigraphic and structural estimates of relative ages of southern and central Appalachian detachments. Second, the zone probably does not result from a Mesozoic normal fault, because known locations of Mesozoic normal faults and grabens are well to the southeast of Giles County.

Not yet known is where else in the East reactivated Iapetan normal faults might generate shocks similar to that of 1897. However, our analysis enables us to suggest specific geological and geophysical investigations that may produce results useful in answering that question. Such investigations can concentrate on defining the area of probable occurrence of other Iapetan normal faults, and on determining whether the one inferred to underlie Giles County is uniquely active or is typical of others that might exist elsewhere.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82585","usgsCitation":"Bollinger, G.A., and Wheeler, R.L., 1982, The Giles County, Virginia, seismogenic zone-- Seismological results and geological interpretations: U.S. Geological Survey Open-File Report 82-585, iv, 136 p., https://doi.org/10.3133/ofr82585.","productDescription":"iv, 136 p.","costCenters":[],"links":[{"id":412470,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0585/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140332,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0585/report-thumb.jpg"}],"country":"United States","state":"Virginia","county":"Giles County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-80.4761,37.4269],[-80.4506,37.3704],[-80.4417,37.3506],[-80.428,37.3194],[-80.4481,37.3088],[-80.4756,37.2905],[-80.4912,37.2822],[-80.5049,37.273],[-80.5147,37.2688],[-80.5302,37.2633],[-80.5551,37.2608],[-80.5787,37.2542],[-80.6075,37.2467],[-80.6219,37.2425],[-80.6724,37.2239],[-80.6828,37.2197],[-80.7051,37.209],[-80.7218,37.2039],[-80.7794,37.1888],[-80.804,37.1786],[-80.8286,37.1615],[-80.856,37.1476],[-80.8678,37.157],[-80.8824,37.1686],[-80.8624,37.1797],[-80.8725,37.1928],[-80.8947,37.1798],[-81.0099,37.2746],[-80.9785,37.294],[-80.9777,37.2934],[-80.9772,37.2932],[-80.9756,37.2931],[-80.9686,37.2927],[-80.9651,37.2932],[-80.9595,37.294],[-80.9566,37.2948],[-80.949,37.2971],[-80.9394,37.2999],[-80.9347,37.3015],[-80.9209,37.307],[-80.9111,37.3107],[-80.8985,37.3171],[-80.8916,37.3218],[-80.8859,37.3264],[-80.8813,37.33],[-80.8795,37.3312],[-80.8767,37.3332],[-80.8735,37.3352],[-80.8709,37.3368],[-80.8646,37.3401],[-80.8627,37.3411],[-80.859,37.3434],[-80.8544,37.3453],[-80.8516,37.3476],[-80.8504,37.3495],[-80.8532,37.3533],[-80.8705,37.371],[-80.8736,37.3737],[-80.8782,37.3777],[-80.8817,37.3817],[-80.8824,37.3848],[-80.8808,37.3889],[-80.8778,37.3926],[-80.8643,37.4096],[-80.8655,37.4132],[-80.8661,37.4159],[-80.8662,37.4184],[-80.8661,37.4189],[-80.8633,37.423],[-80.8627,37.4239],[-80.8575,37.4304],[-80.853,37.4278],[-80.8484,37.4256],[-80.8451,37.4257],[-80.842,37.4257],[-80.8367,37.4248],[-80.8321,37.4222],[-80.8244,37.4168],[-80.8157,37.4115],[-80.8097,37.4062],[-80.8051,37.4012],[-80.8021,37.3981],[-80.8004,37.3963],[-80.7986,37.3954],[-80.7968,37.395],[-80.7963,37.3948],[-80.7939,37.3946],[-80.7934,37.3945],[-80.7899,37.3945],[-80.7864,37.3936],[-80.7834,37.3923],[-80.7793,37.3878],[-80.7757,37.382],[-80.7709,37.3729],[-80.7629,37.3748],[-80.7531,37.3776],[-80.7507,37.3784],[-80.7423,37.3812],[-80.7307,37.3849],[-80.7248,37.3874],[-80.7198,37.3895],[-80.7052,37.3958],[-80.7048,37.396],[-80.684,37.4056],[-80.6696,37.4116],[-80.6518,37.4199],[-80.6363,37.4282],[-80.6276,37.4328],[-80.6219,37.4361],[-80.6176,37.4385],[-80.613,37.4404],[-80.6077,37.4427],[-80.6052,37.4439],[-80.603,37.445],[-80.5986,37.4473],[-80.5899,37.4523],[-80.5807,37.4583],[-80.5732,37.4628],[-80.5673,37.4661],[-80.5563,37.4707],[-80.55,37.4729],[-80.5407,37.4752],[-80.5309,37.4768],[-80.5182,37.4796],[-80.5156,37.48],[-80.5124,37.4806],[-80.5083,37.481],[-80.5054,37.4802],[-80.5026,37.4789],[-80.5002,37.4761],[-80.4984,37.473],[-80.4954,37.4666],[-80.4932,37.4596],[-80.4931,37.4528],[-80.4937,37.4487],[-80.4939,37.4467],[-80.4942,37.4446],[-80.4936,37.4419],[-80.4919,37.4396],[-80.4905,37.4379],[-80.4901,37.4374],[-80.4884,37.4356],[-80.486,37.4333],[-80.4831,37.4319],[-80.4802,37.4283],[-80.4761,37.4269]]]},\"properties\":{\"name\":\"Giles\",\"state\":\"VA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c56e","contributors":{"authors":[{"text":"Bollinger, G. A.","contributorId":55809,"corporation":false,"usgs":true,"family":"Bollinger","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":156924,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":156925,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27657,"text":"wri824019 - 1982 - Model modifications for simulation of flow through stratified rocks in eastern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri824019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4019","title":"Model modifications for simulation of flow through stratified rocks in eastern Ohio","docAbstract":"A quasi three-dimensional groundwater flow model is being used as part of a study to determine impacts of coal-strip mining on local hydrologic systems. Modifications to the model were necessary to simulate local hydrologic conditions properly. Perched water tables required that the method of calculating vertical flow rate be changed. A head-dependent spring-discharge function and a head-dependent stream aquifer-interchange function were added to the program. Modifications were also made to allow recharge from precipitation to any layer. The modified program, data deck instructions, and sample input and output are presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824019","usgsCitation":"Helgesen, J.O., Razem, A., and Larson, S.P., 1982, Model modifications for simulation of flow through stratified rocks in eastern Ohio: U.S. Geological Survey Water-Resources Investigations Report 82-4019, iv, 113 p. :ill. ;28 cm., https://doi.org/10.3133/wri824019.","productDescription":"iv, 113 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122914,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4019/report-thumb.jpg"},{"id":56512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a2f","contributors":{"authors":[{"text":"Helgesen, J. O.","contributorId":62600,"corporation":false,"usgs":true,"family":"Helgesen","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":198482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Razem, A. C.","contributorId":34924,"corporation":false,"usgs":true,"family":"Razem","given":"A. C.","affiliations":[],"preferred":false,"id":198481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198480,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":47549,"text":"wdrIL812 - 1982 - Water resources data for Illinois, water year 1981; Volume 2, Illinois River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"wdrIL812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IL-81-2","title":"Water resources data for Illinois, water year 1981; Volume 2, Illinois River basin","language":"ENGLISH","doi":"10.3133/wdrIL812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Illinois, water year 1981; Volume 2, Illinois River basin: U.S. Geological Survey Water Data Report IL-81-2, 547 p., https://doi.org/10.3133/wdrIL812.","productDescription":"547 p.","costCenters":[],"links":[{"id":135818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6d1c","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":531750,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9598,"text":"ofr82109 - 1982 - Potential impacts of a proposed reservoir on hydrologic and water-quality conditions in Little Rush Creek watershed, Fairfield County, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr82109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-109","title":"Potential impacts of a proposed reservoir on hydrologic and water-quality conditions in Little Rush Creek watershed, Fairfield County, Ohio","docAbstract":"Water-quality and discharge measurements were made at three sites on Indian Run and one site on Little Rush Creek between February and December, 1979. Indian Run was observed above and below the U.S. Soil Conservation Service Reservoir, VI-D. Little Rush Creek was observed 1.1 miles downstream from the proposed U.S. Soil Conservation Reservoir, VI-A, site. Data from the Indian Run sites were used to predict the potential water-quality conditions in and downstream from the proposed Little Rush Creek Reservoir. \r\n\r\nTemperatures measured in Indian Run at the reservoir outflow were as much as 4oc greater than those at the inflow. Dissolved-oxygen saturation ranged from 62 to 110 percent in the inflow and from 57 to 120 percent in the outflow. Indian Run and Little Push Creek are characterized by moderately hard to very hard calcium bicarbonate water. The concentration of dieldrin in water samples from both Little Rush Creek and the outflow from the reservoir on Indian Run was 0.01 micrograms per liter, and in reservoir-surface samples it was 0.02 micrograms per liter. Chlordane concentration in a bottom material sample from the reservoir was 26 micrograms per kilogram. Catfish taken from the reservoir contained 190 micrograms per kilogram chlordane. \r\n\r\nAll sites showed a good diversity in benthic invertebrate communities. Blue-green algal blooms occurred in the reservoir, indicating nutrient-enriched conditions. \r\n\r\nBecause of similarities in land use and watershed characteristics, water in the proposed reservoir VI-A is expected to be similar in quality to that of reservoir VI-D. The new reservoir will not significantly affect downstream water quality.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82109","usgsCitation":"Hren, J., and Jones, R., 1982, Potential impacts of a proposed reservoir on hydrologic and water-quality conditions in Little Rush Creek watershed, Fairfield County, Ohio: U.S. Geological Survey Open-File Report 82-109, v, 67 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82109.","productDescription":"v, 67 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":142155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0109/report-thumb.jpg"},{"id":37326,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0109/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37327,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0109/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37328,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0109/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37329,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c04f","contributors":{"authors":[{"text":"Hren, Janet","contributorId":69554,"corporation":false,"usgs":true,"family":"Hren","given":"Janet","email":"","affiliations":[],"preferred":false,"id":159977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, R.L.","contributorId":39785,"corporation":false,"usgs":true,"family":"Jones","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":159976,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10916,"text":"ofr82239 - 1982 - Analyzing thematic maps and mapping for accuracy","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr82239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-239","title":"Analyzing thematic maps and mapping for accuracy","docAbstract":"Two problems which exist while attempting to test the accuracy of thematic maps and mapping are: (1) evaluating the accuracy of thematic content, and (2) evaluating the effects of the variables on thematic mapping. Statistical analysis techniques are applicable to both these problems and include techniques for sampling the data and determining their accuracy. In addition, techniques for hypothesis testing, or inferential statistics, are used when comparing the effects of variables. A comprehensive and valid accuracy test of a classification project, such as thematic mapping from remotely sensed data, includes the following components of statistical analysis: (1) sample design, including the sample distribution, sample size, size of the sample unit, and sampling procedure; and (2) accuracy estimation, including estimation of the variance and confidence limits. Careful consideration must be given to the minimum sample size necessary to validate the accuracy of a given. classification category. \r\n\r\nThe results of an accuracy test are presented in a contingency table sometimes called a classification error matrix. Usually the rows represent the interpretation, and the columns represent the verification. The diagonal elements represent the correct classifications. The remaining elements of the rows represent errors by commission, and the remaining elements of the columns represent the errors of omission. For tests of hypothesis that compare variables, the general practice has been to use only the diagonal elements from several related classification error matrices. These data are arranged in the form of another contingency table. The columns of the table represent the different variables being compared, such as different scales of mapping. The rows represent the blocking characteristics, such as the various categories of classification. The values in the cells of the tables might be the counts of correct classification or the binomial proportions of these counts divided by either the row totals or the column totals from the original classification error matrices. In hypothesis testing, when the results of tests of multiple sample cases prove to be significant, some form of statistical test must be used to separate any results that differ significantly from the others. In the past, many analyses of the data in this error matrix were made by comparing the relative magnitudes of the percentage of correct classifications, for either individual categories, the entire map or both. More rigorous analyses have used data transformations and (or) two-way classification analysis of variance. A more sophisticated step of data analysis techniques would be to use the entire classification error matrices using the methods of discrete multivariate analysis or of multiviariate analysis of variance.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82239","usgsCitation":"Rosenfield, G., 1982, Analyzing thematic maps and mapping for accuracy: U.S. Geological Survey Open-File Report 82-239, iii, 20 p. ;28 cm., https://doi.org/10.3133/ofr82239.","productDescription":"iii, 20 p. ;28 cm.","costCenters":[],"links":[{"id":142415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0239/report-thumb.jpg"},{"id":38683,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4882e4b07f02db5171bc","contributors":{"authors":[{"text":"Rosenfield, G.H.","contributorId":94670,"corporation":false,"usgs":true,"family":"Rosenfield","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":162204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27677,"text":"wri8175 - 1982 - Results of deep-well injection testing at Mulberry, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri8175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-75","title":"Results of deep-well injection testing at Mulberry, Florida","docAbstract":"At the Kaiser Aluminum and Chemical Corporation plant, Mulberry, Fla., high-chloride, acidic liquid wastes are injected into a dolomite section at depths below about 4,000 feet below land surface. In 1975, a satellite monitor well was drilled 2,291 feet from the injection well and a series of three injection tests were performed. Duration of the tests ranged from 240 to 10,020 minutes and injection rates ranged from 110 to 230 gallons per minute. Based on an evaluation of factors that affect hydraulic response, water-level data suitable for interpretation of hydraulic characteristics of the injection zone were identified to occur from 200 to 1,000 minutes during the 10,020-minute test. Transmissivity of the injection zone was computed to be within the range from 700 to 1,000 feet squared per day and storage coefficient of the injection zone was computed to be within the range from .00001 to .00005. The confining bed accepting most of the leakage appears to be the underlying bed. Also, it appears that the overlying beds are probably relatively impermeable and significantly retard the vertical movement of neutralized waste effluent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8175","usgsCitation":"Hickey, J.J., and Wilson, W., 1982, Results of deep-well injection testing at Mulberry, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-75, iv, 15 p. :ill., map ;28 cm., https://doi.org/10.3133/wri8175.","productDescription":"iv, 15 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0075/report-thumb.jpg"},{"id":56527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605789","contributors":{"authors":[{"text":"Hickey, John J.","contributorId":39763,"corporation":false,"usgs":true,"family":"Hickey","given":"John","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, W.E.","contributorId":100831,"corporation":false,"usgs":true,"family":"Wilson","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":198518,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7778,"text":"ofr82607 - 1982 - High-resolution seismic-reflection profiles from the R/V Columbus Iselin, cruise CI 7-78-2, over the continental shelf and slope in the Georges Bank area","interactions":[],"lastModifiedDate":"2018-06-20T10:39:47","indexId":"ofr82607","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-607","title":"High-resolution seismic-reflection profiles from the R/V Columbus Iselin, cruise CI 7-78-2, over the continental shelf and slope in the Georges Bank area","docAbstract":"

In September 1978, the U. S. Geological Survey (USGS) collected 5,029 km of single-channel seismic-reflection data from the Georges Bank area of the Atlantic Continental Shelf and Slope during the R/V COLUMBUS ISELIN cruise CI 7-78-2. The purpose of the cruise was to determine the location and frequency of mass sediment movement and other geologic hazards along the Continental Slope.

Navigation of the COLUMBUS ISELIN was by LORAN-C; position fixes were automatically recorded at 5-minute intervals and manually plotted and recorded at 15-minute intervals. The navigation equipment included a Northstar 6000 LORAN receiver and a Texas Instruments Silent 700 tape and paper recorder.

The seismic equipment consisted of a 40-in3 airgun, a 5-in3 airgun, a Teledyne 600-joule mnisparker, and ORE (Ocean Research Equipment Inc.) 3.5-kHz transducer. The seismic profiles obtained were recorded on paper by EPC (EPC Labs Inc.) recorders and on magnetic tape by a 7-channel analog tape recorder. Overall, the data quality is excellent, and penetration and resolution are good although in some areas, the underlying structure was obscured by rough topography.

The original records may be viewed at the USGS office in Woods Hole, Massachusetts. Microfilm copies of the data may be purchased only from the National Geophysical and Solar-Terrestrial Data Center, NOAA/EDIS/NGSDC, Code D621, 325 Broadway, Boulder, CO 80303 (Telephone: 303-497-6338).

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82607","usgsCitation":"Bailey, N.G., and Aaron, J.M., 1982, High-resolution seismic-reflection profiles from the R/V Columbus Iselin, cruise CI 7-78-2, over the continental shelf and slope in the Georges Bank area: U.S. Geological Survey Open-File Report 82-607, 2 p., https://doi.org/10.3133/ofr82607.","productDescription":"2 p.","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":141235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":259854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0607/ofr1982607.pdf","text":"Report","size":"2.04 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-607"}],"contact":"

Coastal and Marine Geology Program
U.S. Geological Survey
384 Woods Hole Road
Woods Hole, MA 02543

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f285","contributors":{"authors":[{"text":"Bailey, Norman G.","contributorId":59439,"corporation":false,"usgs":true,"family":"Bailey","given":"Norman","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":156583,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aaron, John M.","contributorId":10031,"corporation":false,"usgs":true,"family":"Aaron","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156582,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9631,"text":"ofr821002 - 1982 - Plankton studies in San Francisco Bay; V, Zooplankton species composition and abundance in the South Bay, 1980-1981","interactions":[],"lastModifiedDate":"2016-07-27T11:35:38","indexId":"ofr821002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1002","title":"Plankton studies in San Francisco Bay; V, Zooplankton species composition and abundance in the South Bay, 1980-1981","docAbstract":"

Data are presented that summarize zooplankton species composition and abundance in South San Francisco Bay during 1980 and 1981. Sampling was conducted at least twice monthly at thirteen stations, from the southern extremity of the South Bay to the Golden Gate Bridge between January 1980 and May 1981. Samples were collected by pump at three depths in the shipping channel and one depth over the shoals. Subsamples were enumerated while alive. Total zooplankton biomass as carbon was calculated from estimated carbon quotas and abundances of each organism enumerated.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr821002","usgsCitation":"Hutchinson, A., 1982, Plankton studies in San Francisco Bay; V, Zooplankton species composition and abundance in the South Bay, 1980-1981: U.S. Geological Survey Open-File Report 82-1002, 151 p., https://doi.org/10.3133/ofr821002.","productDescription":"151 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":37362,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1002/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685581","contributors":{"authors":[{"text":"Hutchinson, Anne","contributorId":45316,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Anne","email":"","affiliations":[],"preferred":false,"id":160019,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7918,"text":"ofr82939 - 1982 - LSTRAT; a standard output routine for USTRAT file stratigraphic data in the National Coal Resources Data System (NCRDS)","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82939","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-939","title":"LSTRAT; a standard output routine for USTRAT file stratigraphic data in the National Coal Resources Data System (NCRDS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82939","usgsCitation":"Blake, D., 1982, LSTRAT; a standard output routine for USTRAT file stratigraphic data in the National Coal Resources Data System (NCRDS): U.S. Geological Survey Open-File Report 82-939, 9 p., 28 cm., https://doi.org/10.3133/ofr82939.","productDescription":"9 p., 28 cm.","costCenters":[],"links":[{"id":140704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0939/report-thumb.jpg"},{"id":35457,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0939/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4745","contributors":{"authors":[{"text":"Blake, Dorsey","contributorId":91487,"corporation":false,"usgs":true,"family":"Blake","given":"Dorsey","email":"","affiliations":[],"preferred":false,"id":156831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7920,"text":"ofr82391 - 1982 - Temperatures and interval geothermal-gradient determinations from wells in National Petroleum Reserve in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82391","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-391","title":"Temperatures and interval geothermal-gradient determinations from wells in National Petroleum Reserve in Alaska","docAbstract":"Temperature and related records from 28 wells in the National Petroleum Reserve in Alaska (NPRA) although somewhat constrained from accuracy by data gathering methods, extrapolate to undisturbed formation temperatures at specific depths below permafrost, and lead to calculated geothermal gradients between these depths. Tabulation of the results show that extrapolated undisturbed temperatures range from a minimum of 98?F (37?C) at 4,000 feet (1,220 m) to a maximum of 420?F (216?C) at 20,260 feet (6,177 m) and that geothermal gradients range from 0.34?F/100' (6?C/km) between 4,470 feet to 7,975 feet (Lisburne (1) and 3.15?F/100? (57?C/km) between 6,830 feet to 7,940 feet (Drew Point #1). Essential information needed for extrapolations consists of: time-sequential 'bottom-hole' temperatures during wire-line logging of intermediate and deep intervals of the bore hole; the times that circulating drilling fluids had disturbed the formations; and the subsequent times that non-circulating drilling fluids had been in contact with the formation. In several wells presumed near direct measures of rock temperatures recorded from formation fluids recovered by drill stem tests (DST) across thin (approx. 10-20 foot) intervals are made available. \r\n\r\nWe believe that the results approach actual values close enough to serve as approximations of the thermal regimes in appropriate future investigations. Continuous temperature logs obtained at the start and end of final logging operations, conductivity measurements, and relatively long-term measurements of the recovery from disturbance at shallow depths in many of the wells will permit refinements of our values and provide determination of temperatures at other depths.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82391","usgsCitation":"Blanchard, D., and Tailleur, I., 1982, Temperatures and interval geothermal-gradient determinations from wells in National Petroleum Reserve in Alaska: U.S. Geological Survey Open-File Report 82-391, ii, 82 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82391.","productDescription":"ii, 82 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0391/report-thumb.jpg"},{"id":35458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0391/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7f83","contributors":{"authors":[{"text":"Blanchard, D.C.","contributorId":18763,"corporation":false,"usgs":true,"family":"Blanchard","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":156834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tailleur, I.L.","contributorId":59027,"corporation":false,"usgs":true,"family":"Tailleur","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":156835,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8363,"text":"ofr82361 - 1982 - Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr82361","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-361","title":"Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida","docAbstract":"Hydrologic, geologic, and water-quality data collected in Escambia County, Florida, October 1962 through September 1980 are presented. The data were collected by the U.S. Geological Survey as part of a cooperative investigation with the city of Pensacola and Escambia County to provide information on the quality and quantity of water available from the sand-and-gravel aquifer and selected surface-water sites in Escambia County. Ground-water data include records of 440 wells, chemical and physical analyses of water quality for 325 wells, 6 long-term hydrographs, and 19 lithologic logs. Surface-water data include streamflow measurements and analyses of water collected at 9 sites. Maps of the county show the locations of the data-collection sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82361","usgsCitation":"Coffin, J., 1982, Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida: U.S. Geological Survey Open-File Report 82-361, 136 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82361.","productDescription":"136 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0361/report-thumb.jpg"},{"id":35935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0361/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980e9","contributors":{"authors":[{"text":"Coffin, J.E.","contributorId":75913,"corporation":false,"usgs":true,"family":"Coffin","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":157598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":45833,"text":"ofr8253 - 1982 - Locality map for scintillometer and analytical data collected in 1981, Ugashik and Karluk quadrangles, Alaska","interactions":[{"subject":{"id":45833,"text":"ofr8253 - 1982 - Locality map for scintillometer and analytical data collected in 1981, Ugashik and Karluk quadrangles, Alaska","indexId":"ofr8253","publicationYear":"1982","noYear":false,"title":"Locality map for scintillometer and analytical data collected in 1981, Ugashik and Karluk quadrangles, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":61233,"text":"mf1539C - 1986 - Maps and tables showing data and analyses of semiquantitative emmission spectrometry and atomic-absorption spectrophotometry of rock samples, Ugashik, Bristol Bay, and part of Karluk quadrangles, Alaska","indexId":"mf1539C","publicationYear":"1986","noYear":false,"chapter":"C","title":"Maps and tables showing data and analyses of semiquantitative emmission spectrometry and atomic-absorption spectrophotometry of rock samples, Ugashik, Bristol Bay, and part of Karluk quadrangles, Alaska"},"id":1}],"supersededBy":{"id":61233,"text":"mf1539C - 1986 - Maps and tables showing data and analyses of semiquantitative emmission spectrometry and atomic-absorption spectrophotometry of rock samples, Ugashik, Bristol Bay, and part of Karluk quadrangles, Alaska","indexId":"mf1539C","publicationYear":"1986","noYear":false,"title":"Maps and tables showing data and analyses of semiquantitative emmission spectrometry and atomic-absorption spectrophotometry of rock samples, Ugashik, Bristol Bay, and part of Karluk quadrangles, Alaska"},"lastModifiedDate":"2023-03-24T20:11:37.143884","indexId":"ofr8253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-53","title":"Locality map for scintillometer and analytical data collected in 1981, Ugashik and Karluk quadrangles, Alaska","docAbstract":"

Scintillometer data were collected routinely in 1981 as part of the field investigations in the Ugashik and Karluk quadrangles. The instrument used was a Geometrics Model GR-101A, mounted in the helicopter. The data, in counts per second (cps), were obtained at most of the sites by the helicopter pilot (Svec) while geologists were occupying the sample site. Scintillometer localities are indicated on the map by a dot.

The sites are concentrated in the southeastern part of the map area where previous work (OF 81-253) had outlined an area with anomalously high cps. The bedrock at these sites is a Late Tertiary hornblende granodiorite instrusive dated at 9.4 my. Hornfelsed sedimentary rock overlying the batholith gave cps nearly as high as the intrusive rock. Samples routinely checked by semiquantitative spectrographic analysis for thorium failed to detect the element. 

In general the Ugashik and Karluk quadrangles have a low level of gamma radiation. A majority of the sites, 52 percent, gave readings of less than 35 cps, and only 10 percent had values of greater than cps. Thick alluvium or glacial deposits generally gave low values. Readings from sedimentary bedrock were extremely erratic and no generalization can be made concerning their level of gamma radiation. The hornblende granodiorite and overlying hornfelsed sedimentary rock are all greater than 30 cps, but again, the values are somewhat erratic and no definitive pattern is readily apparent. 

Bedrock samples are collected for analysis are on the map by a triangle. 

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