An oilspill risk analysis was conducted to determine the relative environmental hazards of developing oil in different regions of the North Atlantic (Proposed Sale 52) Outer Continental Shelf (OCS) lease area. The probability of spill occurrences, likely movement of oil slicks, and locations of resources vulnerable to spilled oil were analyzed. The times between spill occurrence and contact with various resources were also estimated. The combined results yielded estimates of the overall risks associated with development of the proposed lease area. Assuming that oil exists in the lease area (a 40-percent chance) and depending upon the routes chosen to transport oil from OCS platforms to the shore, the leasing of the tracts proposed for OCS Sale 52 will result in an expected 10.2 oilspills (of 1,000 barrels or larger). The estimated probability that land will be contacted by one or more oilspills (of 1,000 barrels or larger) that have been at sea less than 30 days is 0.71. If existing transportation of oil in the area is considered, this probability increases greatly, to more than 0.99.
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This report presents the results of the first year (1979) of an ongoing study. By 1932, water in the Prairie du Chien-Jordan aquifer, the region 's major source of ground water, was contaminated 3,500 feet from the plant. The hydraulic characteristics of the Prairie du Chien-Jordan aquifer , its long contamination history, and fluctuating pumpage combine to creat a complex distribution of coal-tar derivatives observed in the aquifer. The Prairie du Chien-Jordan aquifer underlies the area at depths of 250 to 500 feet and is overlain by two bedrock aquifers (Platteville and St. Peter), two confining beds (Glenwood and basal part of St. Peter), and 70 to 100 feet of glacial drift. Multiaquifer wells in the area have permitted contaminated water from near-surface aquifers to flow downward into the Prairie du Chien-Jordan aquifer. Flow rates of 20 to 150 gallons per minute from the shallower aquifers into the Prairie du Chien-Jordan aquifer were observed in five wells. In the drift, a hydrocarbon fluid phase is moving vertically downward relative to the aqueous phase. Dissolved constituents in the drift and Platteville aquifer, the uppermost bedrock unit over most of the area, have moved at least 4,000 feet. Low-molecular-weight compounds are moving preferentially through the drift and Platteville aquifer system. (USGS)
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28 cm.), https://doi.org/10.3133/ofr811092.","productDescription":"1 map ;39 x 43 cm. +lithology on sheet 56 x 49 cm. and text (22 p. ; 28 cm.)","costCenters":[],"links":[{"id":134921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1092/report-thumb.jpg"},{"id":81085,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1092/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81086,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1092/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81087,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c941","contributors":{"authors":[{"text":"Rytuba, James J. jrytuba@usgs.gov","contributorId":3043,"corporation":false,"usgs":true,"family":"Rytuba","given":"James","email":"jrytuba@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":228058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minor, S.A.","contributorId":65047,"corporation":false,"usgs":true,"family":"Minor","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":228060,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":228059,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":43320,"text":"ofr81838 - 1981 - Joint patterns in sandstone and quartzose siltstone in the Appalachian basin","interactions":[],"lastModifiedDate":"2022-08-29T18:23:10.361919","indexId":"ofr81838","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-838","title":"Joint patterns in sandstone and quartzose siltstone in the Appalachian basin","docAbstract":"No abstract available.
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The criteria used to evaluate the basins were (1) theoretical aquifer response to pumping, (2) alternative sources of water, and (3) chemical quality of water. The basins were ranked relative to each other for the three criteria and in overall suitability. On the basis of subjective analysis, the basins were ranked in the following order for overall suitability: (1) Calzona-Vidal Valley, (2) Middle Amargosa Valley, (3) Chuckwalla Valley, (4) Soda Lake Valley, and (5) Caves Canyon Valley. 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S. Geological Survey has conceptually defined a candidate Operational Land Remote Sensing Satellite. A conceptual design study of this system, known as MAPSAT, has been completed by Itek Optical Systems, a division of Itek Corporation, and the TRW Defense Systems and Space Group. The concept of MAPSAT is based on LANDSAT mission, sensing, and data communication characteristics, but reflects the evolution of technological and application responsiveness.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8126","usgsCitation":"Colvocoresses, A.P., 1981, Mapsat conceptual design; system overview: U.S. Geological Survey Open-File Report 81-26, 26 p., https://doi.org/10.3133/ofr8126.","productDescription":"26 p.","costCenters":[],"links":[{"id":155616,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0026/report-thumb.jpg"},{"id":427471,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6063ff","contributors":{"authors":[{"text":"Colvocoresses, Alden P.","contributorId":72779,"corporation":false,"usgs":true,"family":"Colvocoresses","given":"Alden","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":188817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47275,"text":"ofr811168 - 1981 - Generalized geologic map and hydrologic properties of Potter Creek area, Municipality of Anchorage, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:46","indexId":"ofr811168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1168","title":"Generalized geologic map and hydrologic properties of Potter Creek area, Municipality of Anchorage, Alaska","language":"ENGLISH","doi":"10.3133/ofr811168","usgsCitation":"Schmoll, H.R., and Emanuel, R.P., 1981, Generalized geologic map and hydrologic properties of Potter Creek area, Municipality of Anchorage, Alaska: U.S. Geological Survey Open-File Report 81-1168, 1 map ;33 x 41 cm., https://doi.org/10.3133/ofr811168.","productDescription":"1 map ;33 x 41 cm.","costCenters":[],"links":[{"id":108101,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11906.htm","linkFileType":{"id":5,"text":"html"},"description":"11906"},{"id":171170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1168/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6af94d","contributors":{"authors":[{"text":"Schmoll, Henry R. schmoll@usgs.gov","contributorId":3793,"corporation":false,"usgs":true,"family":"Schmoll","given":"Henry","email":"schmoll@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":234958,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emanuel, Richard P.","contributorId":98287,"corporation":false,"usgs":true,"family":"Emanuel","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":234959,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9875,"text":"ofr81899 - 1981 - Stress analysis of a deeply eroded analog of the San Andreas Fault, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr81899","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-899","title":"Stress analysis of a deeply eroded analog of the San Andreas Fault, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81899","usgsCitation":"Kohlstedt, D.L., and Bird, J.M., 1981, Stress analysis of a deeply eroded analog of the San Andreas Fault, California: U.S. Geological Survey Open-File Report 81-899, 11 p. ill. ;28 cm., https://doi.org/10.3133/ofr81899.","productDescription":"11 p. ill. ;28 cm.","costCenters":[],"links":[{"id":140925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0899/report-thumb.jpg"},{"id":37667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0899/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c39","contributors":{"authors":[{"text":"Kohlstedt, David L.","contributorId":21159,"corporation":false,"usgs":true,"family":"Kohlstedt","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, John M.","contributorId":99138,"corporation":false,"usgs":true,"family":"Bird","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160442,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9876,"text":"ofr81900 - 1981 - Stress analysis of deeply eroded analogs of the San Andreas Fault (a renewal)","interactions":[],"lastModifiedDate":"2025-09-15T13:51:42.366924","indexId":"ofr81900","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-900","title":"Stress analysis of deeply eroded analogs of the San Andreas Fault (a renewal)","docAbstract":"We have studied deformation-induced microstructures in quartzo-feldspathic rocks from the Nordre Stromfjord shear zone, within the central part of the Nagssugtoqidian mobile belt of West Greenland (Figure 1).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81900","usgsCitation":"Kohlstedt, D.L., and Bird, J.M., 1981, Stress analysis of deeply eroded analogs of the San Andreas Fault (a renewal): U.S. Geological Survey Open-File Report 81-900, 12 p., https://doi.org/10.3133/ofr81900.","productDescription":"12 p.","costCenters":[],"links":[{"id":140926,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0900/report-thumb.jpg"},{"id":495484,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0900/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4c3f","contributors":{"authors":[{"text":"Kohlstedt, David L.","contributorId":21159,"corporation":false,"usgs":true,"family":"Kohlstedt","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160443,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, John M.","contributorId":99138,"corporation":false,"usgs":true,"family":"Bird","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160444,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44143,"text":"ofr81507 - 1981 - Surficial geologic map of the eastern Snake River Plain and adjacent areas, 111° -115° W., Idaho and Wyoming","interactions":[{"subject":{"id":44143,"text":"ofr81507 - 1981 - Surficial geologic map of the eastern Snake River Plain and adjacent areas, 111° -115° W., Idaho and 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Wyoming"},"lastModifiedDate":"2022-04-14T19:18:40.600202","indexId":"ofr81507","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-507","title":"Surficial geologic map of the eastern Snake River Plain and adjacent areas, 111° -115° W., Idaho and Wyoming","docAbstract":"This map portrays the distribution of surficial materials that cover most of the landscape of the eastern Snake River Plain and adjoining areas in a larger part of southeastern Idaho and a very small area in western Wyoming (fig. 1). Almost 350,000 people or 40 percent of Idaho's (estimating 1979 population from Rand McNally (1979)) live in the area, which constitutes about 30 percent of Idaho's land area.
The great majority of this population resides in the major irrigated agricultural areas along the Snake River between American Falls and Ashton and between Bliss and Lake Walcott, which contain the important and growing commercial centers of Rexberg, Idaho Falls, Blackfoot, Pocatello, Burley-Rupert, Twin Falls, and Jerome. These areas encompass almost two-thirds of Idaho's irrigated croplands, and, along with water, are the region's most important resource. Major products include potatoes, sugar beets, alfalfa, small grains, and other crops.
Along the margins of the Plain and in adjacent basins, smaller areas of irrigated farming and population are present, such as Teton Basin, Mud Lake area, Big and Little Lost River Valleys, Big and Little Wood River Valleys, and Raft River Valley. In several of these basins and in nearby upland areas, dry farming of grains is important. Some of these lands are now being converted to irrigated croplands. Grazing is the dominant economic use of grasslands on the Plain in adjacent basins and uplands. At present, industry assumes a minor role in the region's economy, although food processing and nuclear research at the Idaho National Engineering Laboratory (INEL) locally or important.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81507","usgsCitation":"Scott, W.E., 1981, Surficial geologic map of the eastern Snake River Plain and adjacent areas, 111° -115° W., Idaho and Wyoming: U.S. Geological Survey Open-File Report 81-507, 2 Plates: 55.58 x 48.43 inches and 40.09 x 47.29 inches, https://doi.org/10.3133/ofr81507.","productDescription":"2 Plates: 55.58 x 48.43 inches and 40.09 x 47.29 inches","costCenters":[],"links":[{"id":398749,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12058.htm","linkFileType":{"id":5,"text":"html"}},{"id":398735,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0507/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398734,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0507/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0507/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Idaho, Wyoming","otherGeospatial":"Snake River Plain","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c61","contributors":{"authors":[{"text":"Scott, William E. 0000-0001-8156-979X wescott@usgs.gov","orcid":"https://orcid.org/0000-0001-8156-979X","contributorId":1725,"corporation":false,"usgs":true,"family":"Scott","given":"William","email":"wescott@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":229228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53612,"text":"ofr81690 - 1981 - Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:11","indexId":"ofr81690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-690","title":"Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky","docAbstract":"This report provides water users with detailed information on the location, quantity, and quality of water available from underground coal mines in the Breathitt Formation of Pennsylvanian age in part of eastern Kentucky. The principal coal seams mined are the Van Lear in Johnson County and the Alma in Martin County. Coal mines that contained water were located by field inventory and coal-mine maps.\r\n\r\nThe principal factors that affect the occurrence of water in coal mines are the size of the recharge area overlying the mine, the intensity and duration of precipitation, and the altitude of the mine relative to that of the nearest perennial stream.\r\n\r\nTen above-drainage mines (that is, mines at higher elevations than that of the nearest perennial stream) are considered potential sources of water. Discharge from these mines ranged from 12 to 1,700 gallons per minute. The highest sustained discharge from a mine ranged from 750 to 1,200 gallons per minute.\r\n\r\nThe water in coal mines is part of the hydrologic system and varies seasonally with precipitation. Annual discharge from most above-drainage mines ranged from 3 to 10 percent of annual precipitation on the 1and-surface area above the mine.\r\n\r\nEight below-drainage mines are considered potential sources of water. Two were test-pumped at rates of 560 to 620 gallons per minute for as long as 6 hours. After test pumping the Warfield Mining No. 1 mine during September 1977 and March 1978, the recovery (or recharge) rates were significantly different. In September, the recharge rate was about 1,150 gallons per minute, but in March the recharge rate was 103,500 gallons per minute. This difference reflects the seasonal variations in the amount of water available to the ground-water system. Estimates of water stored in below-drainage mines ranged from 22 to 1,462 million gallons. This storage represents a safety factor sufficient to provide water through periods of limited recharge to the mine.\r\n\r\nMost mine water is of the calcium magnesium sulfate type. In general, water from below-drainage mines had lower concentrations of dissolved constituents and higher pH than water from mines above drainage. The hardness of water ranged from soft to very hard and pH ranged -from 3.1 to 8.0 units. Dissolved iron ranged from 0.01 to 64 milligrams per liter. Phenol concentrations in water from eight coal mines ranged from 0 to 5 micrograms per liter.\r\n\r\nThere seems to be a significant difference in the chemical quality of water from above- and below-drainage mines. The concentration of most constituents was lower in water from below-drainage mines than it was from above-drainage mines.\r\n\r\nThe better quality water from below-drainage mines may reflect (1) lower mineralization resulting from less atmospheric oxygen available to react with pyrite or, (2) the result of sampling only the upper zones of water in below-drainage mines where the water has been diluted by less mineralized surface water or inflow or recharge.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr81690","collaboration":"Prepared in cooperation with the Kentucky Geological Survey and the University of Kentucky","usgsCitation":"Mull, D.S., Cordivio1a, S., and Risser, D.W., 1981, Availability and Quality of Water from Underground Coal Mines in Johnson and Martin Counties, Kentucky (WRI/OFR 81-690): U.S. Geological Survey Open-File Report 81-690, viii, 55 p.; Plates, https://doi.org/10.3133/ofr81690.","productDescription":"viii, 55 p.; Plates","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":175253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0690/report-thumb.jpg"},{"id":87487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83,37.666666666666664 ], [ -83,38 ], [ -82.58333333333333,38 ], [ -82.58333333333333,37.666666666666664 ], [ -83,37.666666666666664 ] ] ] } } ] }","edition":"WRI/OFR 81-690","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64afa8","contributors":{"authors":[{"text":"Mull, D. S.","contributorId":43331,"corporation":false,"usgs":true,"family":"Mull","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordivio1a, Steven","contributorId":26357,"corporation":false,"usgs":true,"family":"Cordivio1a","given":"Steven","email":"","affiliations":[],"preferred":false,"id":247909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Risser, Dennis W. 0000-0001-9597-5406 dwrisser@usgs.gov","orcid":"https://orcid.org/0000-0001-9597-5406","contributorId":898,"corporation":false,"usgs":true,"family":"Risser","given":"Dennis","email":"dwrisser@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":43311,"text":"ofr81848 - 1981 - Geophysical data collected across the Oregon continental shelf along Line 2, USGS R/V S. P. Lee, Cruise 3-76","interactions":[],"lastModifiedDate":"2024-11-25T22:15:49.806836","indexId":"ofr81848","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-848","title":"Geophysical data collected across the Oregon continental shelf along Line 2, USGS R/V S. P. Lee, Cruise 3-76","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81848","usgsCitation":"Snavely, P.D., 1981, Geophysical data collected across the Oregon continental shelf along Line 2, USGS R/V S. P. Lee, Cruise 3-76: U.S. Geological Survey Open-File Report 81-848, 1 Plate: 24.93 x 26.79 inches, https://doi.org/10.3133/ofr81848.","productDescription":"1 Plate: 24.93 x 26.79 inches","costCenters":[],"links":[{"id":135217,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81071,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0848/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464507,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75549.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon","otherGeospatial":"Oregon continental shelf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -125,\n 44.3\n ],\n [\n -125,\n 44.1667\n ],\n [\n -124.25,\n 44.1667\n ],\n [\n -124.25,\n 44.3\n ],\n [\n -125,\n 44.3\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c1a4","contributors":{"authors":[{"text":"Snavely, Parke Detweiler Jr.","contributorId":48535,"corporation":false,"usgs":true,"family":"Snavely","given":"Parke","suffix":"Jr.","email":"","middleInitial":"Detweiler","affiliations":[],"preferred":false,"id":228018,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43781,"text":"ofr811067 - 1981 - Hydraulic data for Coosa River in vicinity of Walter Bouldin and Jordan Dams near Wetumpka, Alabama","interactions":[],"lastModifiedDate":"2021-11-29T22:36:46.761746","indexId":"ofr811067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1067","title":"Hydraulic data for Coosa River in vicinity of Walter Bouldin and Jordan Dams near Wetumpka, Alabama","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811067","usgsCitation":"Nelson, G.H., and Ming, C.O., 1981, Hydraulic data for Coosa River in vicinity of Walter Bouldin and Jordan Dams near Wetumpka, Alabama: U.S. Geological Survey Open-File Report 81-1067, Report: v, 8 p.; 43 Plates: 38.92 × 8.57 inches or smaller, https://doi.org/10.3133/ofr811067.","productDescription":"Report: v, 8 p.; 43 Plates: 38.92 × 8.57 inches or 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Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75587.htm"}],"country":"United States","state":"Alabama","city":"Wetumpka","otherGeospatial":"Coosa River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.28524780273438,\n 32.46806060917602\n ],\n [\n -86.14723205566406,\n 32.46806060917602\n ],\n [\n -86.14723205566406,\n 32.62549671451373\n ],\n [\n -86.28524780273438,\n 32.62549671451373\n ],\n [\n -86.28524780273438,\n 32.46806060917602\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a2cb","contributors":{"authors":[{"text":"Nelson, G. 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