The U.S. Geological Survey in cooperation with Mississippi Bureau of Geology is conducting a hydrologic data-collection program in the potential lignite-producing areas in Mississippi. During the week of August 25-28, 1980, hydrologic data on channel characteristics were collected at 15 sites on small streams draining potential lignite mining areas in east-central Mississippi. Streamflow measurements were made and water-quality samples were collected at 11 of the 15 sites.
Main channel widths at the 15 sampling sites in east-central Mississippi ranged from 126 feet on Sucarnoochee Creek to 15 feet on Houston Creek. Maximum water depth ranged from 7 feet on Pawticfaw Creek and Tallahatta Creek to one-half foot on Okatibbee Creek. The maximum stream discharge measured was 56 cubic feet per second on Pawticfaw Creek. Four sites had no discharge. Specific conductance at sampling sites ranged from 115 micromhos on Ponta Creek to 26 micromhos on Sucarnoochee Creek. The dissolved-oxygen concentration was 5.7 milligrams per liter or higher at all sites. The concentration of suspended sediment was not greater than 38 milligrams per liter at any site. Concentrations of calcium, magnesium, sodium, potassium, chloride, and sulfate were less than 10 milligrams per liter in all samples, but were highest at site 10 on Ponta Creek. Bottom-material samples commonly contained iron, manganese, and zinc.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81421","collaboration":"Prepared in cooperation with the Mississippi Department of Natural Resources, Bureau of Geology","usgsCitation":"Arthur, J.K., 1981, Background hydrologic information in potential lignite mining areas in Mississippi, August 1980: U.S. Geological Survey Open-File Report 81-421, 19 p., https://doi.org/10.3133/ofr81421.","productDescription":"19 p.","costCenters":[],"links":[{"id":409171,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0421/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0421/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae476","contributors":{"authors":[{"text":"O'Sullivan, Robert Brett","contributorId":26695,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Robert Brett","affiliations":[],"preferred":false,"id":278867,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8471,"text":"ofr811059 - 1981 - Large-scale bedforms in the Platte River downstream from Grand Island, Nebraska; structure, process, and relationship to channel narrowing","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr811059","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":"81-1059","title":"Large-scale bedforms in the Platte River downstream from Grand Island, Nebraska; structure, process, and relationship to channel narrowing","docAbstract":"The Platte River channel in Nebraska, especially downstream from Grand Island, is characterized by large, periodic, and geometrically distinct bedforms called macroforms. Macroforms have dimensions commensurate with the width and depth of the channel and are emergent at all but the highest flow stages. The encroachment of vegetation on macroforms and their consequent stabilization since the large-scale development of irrigation in the Platte River basin is the major cause of the reduction in channel width upstream from Grand Island. From simple geometrical considerations of macroform shape, an equation is developed to predict the depth and duration of flow required to erode the stoss sides of the macroforms to remove new vegetal growth each year. The methods developed in this report to eliminate vegetal growth on macroforms may provide a useful management tool for controlling width of the Platte River channels. Although further testing is required to establish the validity of these methods at actual stream sites, a sample calculation for the Silver Creek reach shows good agreement between the flow conditions predicted by the methods developed in this report and actual flow conditions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811059","usgsCitation":"Crowley, K., 1981, Large-scale bedforms in the Platte River downstream from Grand Island, Nebraska; structure, process, and relationship to channel narrowing: U.S. Geological Survey Open-File Report 81-1059, v, 37 p. ill., map ;28 cm., https://doi.org/10.3133/ofr811059.","productDescription":"v, 37 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":141728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1059/report-thumb.jpg"},{"id":36041,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1059/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f9a","contributors":{"authors":[{"text":"Crowley, K.D.","contributorId":86769,"corporation":false,"usgs":true,"family":"Crowley","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":157774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8374,"text":"ofr81452 - 1981 - Mineral deposits and geology of northern Oman as of 1974","interactions":[],"lastModifiedDate":"2019-10-07T14:05:02","indexId":"ofr81452","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":"81-452","title":"Mineral deposits and geology of northern Oman as of 1974","docAbstract":"An investigation of the mineral resources of northern Oman was carried out under an agreement between the U. S. Geological Survey and the Ministry of Development, Sultanate of Oman, during late 1973 and early 1974. The purpose of the investigation was to provide an evaluation of the mineral potential of northern Oman and produce recommendations leading toward the utilization of any viable mineral deposits that were found. The widespread copper deposits located within the Semail volcanics appear to be mineable, the iron-nickel laterites developed upon the weathered surface of the Semail ophiolite have economic potential. Manganese and chromite deposits investigated have only a marginal value and are not likely to be of economic importance in the near future. Discovery of economic copper and iron deposits warrants further geologic mapping and mineral exploration in northern Oman. In addition to this, recommendations regarding the organization of a geological and mining group within the Directorate of Petroleum and Minerals are presented.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81452","collaboration":"Prepared on behalf of the Directorate General of Petroleum and Minerals, Ministry of Development, Sultanate of Oman","usgsCitation":"Coleman, R.G., and Bailey, E.H., 1981, Mineral deposits and geology of northern Oman as of 1974: U.S. Geological Survey Open-File Report 81-452, Report: viii, 127 p.; 1 Plate: 20.29 x 13.99 inches, https://doi.org/10.3133/ofr81452.","productDescription":"Report: viii, 127 p.; 1 Plate: 20.29 x 13.99 inches","costCenters":[],"links":[{"id":35957,"rank":400,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1981/0452/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":141294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0452/report-thumb.jpg"},{"id":35958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0452/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Oman","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 55.8709716796875,\n 21.80030805097259\n ],\n [\n 59.9359130859375,\n 21.80030805097259\n ],\n [\n 59.9359130859375,\n 24.90138485280086\n ],\n [\n 55.8709716796875,\n 24.90138485280086\n ],\n [\n 55.8709716796875,\n 21.80030805097259\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635924","contributors":{"authors":[{"text":"Coleman, Robert Griffin","contributorId":89527,"corporation":false,"usgs":true,"family":"Coleman","given":"Robert","email":"","middleInitial":"Griffin","affiliations":[],"preferred":false,"id":157621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, Edgar Herbert","contributorId":85179,"corporation":false,"usgs":true,"family":"Bailey","given":"Edgar","email":"","middleInitial":"Herbert","affiliations":[],"preferred":false,"id":157620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61117,"text":"mf1160D - 1981 - Map showing mineral resource potential of the Paiute Instant (Primitive) Study Area, Mohave County, Arizona","interactions":[{"subject":{"id":48533,"text":"ofr80984 - 1980 - Map showing mineral resource potential of the Paiute instant (primitive) study area, Mohave County, Arizona","indexId":"ofr80984","publicationYear":"1980","noYear":false,"title":"Map showing mineral resource potential of the Paiute instant (primitive) study area, Mohave County, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":61117,"text":"mf1160D - 1981 - Map showing mineral resource potential of the Paiute Instant (Primitive) Study Area, Mohave County, Arizona","indexId":"mf1160D","publicationYear":"1981","noYear":false,"chapter":"D","title":"Map showing mineral resource potential of the Paiute Instant (Primitive) Study Area, Mohave County, Arizona"},"id":1}],"lastModifiedDate":"2015-10-22T14:09:09","indexId":"mf1160D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1160","chapter":"D","title":"Map showing mineral resource potential of the Paiute Instant (Primitive) Study Area, Mohave County, Arizona","docAbstract":"A geologic and geochemical investigation and a survey of the existing mines and prospects have been conducted to determine the mineral resource potential of the Paiute Instant (Primitive) Study Area, Mohave County, Ariz. The study area encompasses part of the Virgin Mountains and the Sullivans Canyon area. Precambrian metamorphic and igneous rocks are exposed in the core and are overlain by folded and faulted Paleozoic and Mesozoic quartzose and carbonate rocks. Mesozoic sedimentary rocks are overlain by Cenozoic volcanic and sedimentary units. The geochemical and mines and prospects survey indicates that the study area contains some mineral deposits that presently are not economically significant. Oil and gas has not been discovered in the area, and the resource potential is apparently nil or at best very low; any future oil and gas exploration would most likely be conducted outside the study area where favorable exploration localities exist. Other combustibles such as coal and oil shale are not known to occur in the study area. There is no evidence of geothermal activity or surficial radioactive mineralization.
\nSeveral areas in the Paiute Instant Study Area are judged to have at best a low mineral potential. These include areas of copper, lead, manganese, molybdenum, nickel, silver, tungsten, and zinc mineralization, as well as occurrences of dumortierite, beryllium, arsenic, barium, gypsum, gem minerals, sand, gravel, and limestone. The metallic deposits and dumortieri te, beryllium, and arsenic occur over small surface areas. Significant production has not resulted from mining activity in mineralized areas. Sand, gravel, limestone, gem minerals, gypsum, and barium occurrences are far from major markets. Currently, there are no active mining operations in the study area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1160D","usgsCitation":"Villalobos, H.A., and Hamm, L.W., 1981, Map showing mineral resource potential of the Paiute Instant (Primitive) Study Area, Mohave County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1160, Report: 5 p.; Plate: 43.13 x 40.16 inches, https://doi.org/10.3133/mf1160D.","productDescription":"Report: 5 p.; Plate: 43.13 x 40.16 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310535,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1160-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310536,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1160-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}},{"id":187416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1160D.jpg"}],"country":"United States","state":"Arizona","county":"Mohave County","otherGeospatial":"Paiute Instant (Primitive) Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.60937499999999,\n 35.02999636902566\n ],\n [\n -114.60937499999999,\n 36.92793899776678\n ],\n [\n -113.2965087890625,\n 36.92793899776678\n ],\n [\n -113.2965087890625,\n 35.02999636902566\n ],\n [\n -114.60937499999999,\n 35.02999636902566\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af14","contributors":{"authors":[{"text":"Villalobos, Hector A.","contributorId":71052,"corporation":false,"usgs":true,"family":"Villalobos","given":"Hector","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":265015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamm, Louis W.","contributorId":59290,"corporation":false,"usgs":true,"family":"Hamm","given":"Louis","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7340,"text":"ofr81578 - 1981 - Mineral resources of the Comanche-Big South, Neota-Flat Top, and Never Summer Wilderness Study Areas, north-central Colorado","interactions":[],"lastModifiedDate":"2021-11-22T20:54:55.849724","indexId":"ofr81578","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":"81-578","title":"Mineral resources of the Comanche-Big South, Neota-Flat Top, and Never Summer Wilderness Study Areas, north-central Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81578","usgsCitation":"Pearson, R.C., Braddock, W.A., Flanigan, V.J., and Patten, L.L., 1981, Mineral resources of the Comanche-Big South, Neota-Flat Top, and Never Summer Wilderness Study Areas, north-central Colorado: U.S. Geological Survey Open-File Report 81-578, Report: iii, 73 p.; 3 Plates: 47.51 × 36.78 inches or smaller, https://doi.org/10.3133/ofr81578.","productDescription":"Report: iii, 73 p.; 3 Plates: 47.51 × 36.78 inches or smaller","costCenters":[],"links":[{"id":34740,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0578/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34739,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0578/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34738,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0578/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392011,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12085.htm"},{"id":34741,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0578/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0578/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Comanche-Big South, Neota-Flat Top, and Never Summer Wilderness Study Areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106,\n 40.375\n ],\n [\n -105.5,\n 40.37\n ],\n [\n -105.5,\n 40.75\n ],\n [\n -106,\n 40.75\n ],\n [\n -106,\n 40.375\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69adcd","contributors":{"authors":[{"text":"Pearson, R. C.","contributorId":30978,"corporation":false,"usgs":true,"family":"Pearson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":155310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braddock, W. A.","contributorId":102148,"corporation":false,"usgs":true,"family":"Braddock","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":155313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":155312,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patten, L. L.","contributorId":72374,"corporation":false,"usgs":true,"family":"Patten","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155311,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":61232,"text":"mf1053M - 1981 - Map and tables showing geochronology and whole-rock geochemistry, Chignik and Sutwik Island quadrangles, Alaska","interactions":[],"lastModifiedDate":"2017-06-07T17:00:29","indexId":"mf1053M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1053","chapter":"M","title":"Map and tables showing geochronology and whole-rock geochemistry, Chignik and Sutwik Island quadrangles, Alaska","language":"ENGLISH","doi":"10.3133/mf1053M","usgsCitation":"Wilson, F.H., Gaum, W., and Herzon, P., 1981, Map and tables showing geochronology and whole-rock geochemistry, Chignik and Sutwik Island quadrangles, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 1053, 1 map ;44 x 112 cm. +2 sheets 70 x 84 cm., 77 x 105 cm., https://doi.org/10.3133/mf1053M.","productDescription":"1 map ;44 x 112 cm. +2 sheets 70 x 84 cm., 77 x 105 cm.","costCenters":[],"links":[{"id":187255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":105443,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6427.htm","linkFileType":{"id":5,"text":"html"},"description":"6427"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -160.5,56 ], [ -160.5,57 ], [ -156,57 ], [ -156,56 ], [ -160.5,56 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655569","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":265227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gaum, W.C.","contributorId":88433,"corporation":false,"usgs":true,"family":"Gaum","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":265229,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herzon, P. L.","contributorId":26353,"corporation":false,"usgs":true,"family":"Herzon","given":"P. L.","affiliations":[],"preferred":false,"id":265228,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7484,"text":"ofr81704 - 1981 - Research and development program; Conservation Division Outer Continental Shelf oil and gas operations; Technical report 1981","interactions":[],"lastModifiedDate":"2022-11-04T17:31:06.204552","indexId":"ofr81704","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":"81-704","title":"Research and development program; Conservation Division Outer Continental Shelf oil and gas operations; Technical report 1981","docAbstract":"As a result of recommendations several years ago from the National Academy of Sciences, the University of Oklahoma, and the National Aeronautics and Space Administration (NASA), the U.S. Geological Survey has embarked upon a program of research and development to provide the technological insights needed for its regulatory operations offshore—operations which provide assurances to the public for safety and for the prevention of pollution in oil and gas drilling and production. These clear objectives are, therefore, those of the research program, not the economics of operations, which are of concern to industry.
The Program is a contract research program and is an integral part of the Conservation Division. It is a focal point for deriving possible solutions from the university community, private industry, and the Federal laboratory system for identified offshore operational problems. This vast interdisciplinary body of science and technology provides the kind of research needed by the Division in its Outer Continental Shelf (OCS) operations which involve such problematic areas as structural dynamics, fluid flow, and geotechnology.
The Program encourages innovation and creativity which can be accomplished only by talented scientists and engineers who are dedicated to man's endeavor to make breakthroughs in science and technology.
Because the Division's mission is operational, in a sense like the U.S. Navy, the R&D Program must progress in a timely manner even though technological advances cannot really be scheduled. As the Navy's Office of Naval Research (ONR) has so successfully coped with the seeming dichotomy of anticipating the occurrence of innovations, so must the Conservation Division. Thus, USGS, like ONR, makes use of the unsolicited proposal and the best effort contract to accomplish its objectives. Good science and technology can only be accomplished when several variables converge: a talented investigator doing his own research, which happens to coincide with our needs, availability of resources, time scales, etc. Our task is to \"beat the bushes\" so that these people come to us with their innovative ideas and concepts. They have done so by learning of our interests through announcements of the Program in the Federal Register, reading reports which emanate from the Program, and by attending our seminars.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81704","usgsCitation":"Gregory, J.B., and Smith, C.E., 1981, Research and development program; Conservation Division Outer Continental Shelf oil and gas operations; Technical report 1981: U.S. Geological Survey Open-File Report 81-704, v, 87 p., https://doi.org/10.3133/ofr81704.","productDescription":"v, 87 p.","costCenters":[],"links":[{"id":409173,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0704/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db681080","contributors":{"authors":[{"text":"Gregory, John B.","contributorId":62209,"corporation":false,"usgs":true,"family":"Gregory","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Charlie E.","contributorId":241279,"corporation":false,"usgs":false,"family":"Smith","given":"Charlie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":856462,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7344,"text":"ofr81510 - 1981 - Mineral resources of the Gros Ventre Wilderness Study Area, Teton and Sublette counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr81510","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":"81-510","title":"Mineral resources of the Gros Ventre Wilderness Study Area, Teton and Sublette counties, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81510","usgsCitation":"Simons, F.S., Love, J.D., Keefer, W.R., Harwood, D.S., and Bienewski, C., 1981, Mineral resources of the Gros Ventre Wilderness Study Area, Teton and Sublette counties, Wyoming: U.S. Geological Survey Open-File Report 81-510, iii, 98 p., 4 over-size sheets, scale 1:48,000 ;28 cm., https://doi.org/10.3133/ofr81510.","productDescription":"iii, 98 p., 4 over-size sheets, scale 1:48,000 ;28 cm.","costCenters":[],"links":[{"id":140146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0510/report-thumb.jpg"},{"id":34749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0510/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2ec","contributors":{"authors":[{"text":"Simons, Frank S.","contributorId":42203,"corporation":false,"usgs":true,"family":"Simons","given":"Frank","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Love, J. D.","contributorId":64620,"corporation":false,"usgs":true,"family":"Love","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":155337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keefer, W. R.","contributorId":21538,"corporation":false,"usgs":true,"family":"Keefer","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":155334,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Harwood, D. S.","contributorId":48937,"corporation":false,"usgs":true,"family":"Harwood","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155336,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bienewski, C.L.","contributorId":73055,"corporation":false,"usgs":true,"family":"Bienewski","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":155338,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":11810,"text":"ofr811132 - 1981 - Preliminary composite magnetic anomaly map of the conterminous United States","interactions":[{"subject":{"id":11810,"text":"ofr811132 - 1981 - Preliminary composite magnetic anomaly map of the conterminous United States","indexId":"ofr811132","publicationYear":"1981","noYear":false,"title":"Preliminary composite magnetic anomaly map of the conterminous United States"},"predicate":"SUPERSEDED_BY","object":{"id":64288,"text":"gp954A - 1982 - Composite magnetic anomaly map of the United States: Part A: Conterminous United States","indexId":"gp954A","publicationYear":"1982","noYear":false,"chapter":"A","title":"Composite magnetic anomaly map of the United States: Part A: Conterminous United States"},"id":1}],"supersededBy":{"id":64288,"text":"gp954A - 1982 - Composite magnetic anomaly map of the United States: Part A: Conterminous United States","indexId":"gp954A","publicationYear":"1982","noYear":false,"title":"Composite magnetic anomaly map of the United States: Part A: Conterminous United States"},"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr811132","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":"81-1132","title":"Preliminary composite magnetic anomaly map of the conterminous United States","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811132","usgsCitation":"Zietz, I., 1981, Preliminary composite magnetic anomaly map of the conterminous United States: U.S. Geological Survey Open-File Report 81-1132, 5 p. :col. maps ;28 cm. +3 slides (col.), https://doi.org/10.3133/ofr811132.","productDescription":"5 p. :col. maps ;28 cm. +3 slides (col.)","costCenters":[],"links":[{"id":145050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c701","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":163767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28193,"text":"wri8141 - 1981 - Limnological and geochemical survey of Williams Lake, Hubbard County, Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T12:41:41","indexId":"wri8141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-41","title":"Limnological and geochemical survey of Williams Lake, Hubbard County, Minnesota","docAbstract":"A limnological and geochemical survey of Williams Lake, Minnesota, was made in 1979 to provide an initial interpretive description of the lake and the contiguous ground-water system. This survey was made as part of a continuing research program related to the investigation of the interaction of lakes and their contiguous ground-water systems at Williams Lake, Minnesota, as well as other sites within the continental United States.
\nDuring 1979, Williams Lake was dimictic, and the lake had high optical transparency; light penetrated to the lakebed throughout most of the lake. Aquatic macrophytes were present along the western shore and in the southern bay of the lake. Although the lake had clinograde-oxygen distributions during part of this survey, anaerobic conditions were not observed. The lake is moderately fertile with respect to its total phosphorus content. Nutrient data indicate phosphorus limits phytoplankton biomass levels in Williams Lake. Blue-green algae were the dominant group of the phytoplankton community and copepods were the dominant group of the zooplankton community when the lake was thermally stratified during the open-water season. Diatoms and rotifers were dominant when the lake was isothermal in the autumn.
\nCalcium and bicarbonate represent more than 90 percent of the dissolved constituents in Williams Lake and the contiguous ground-water system. Major mineralogical constituents of the lake sediments are quartz, dolomite, and calcite. Marl is present only in the littoral zone of the lake. Organic sediments in the lake consist of loose organic floe and gyttja.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wri8141","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources","usgsCitation":"LaBaugh, J.W., Groschen, G., and Winter, T.C., 1981, Limnological and geochemical survey of Williams Lake, Hubbard County, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 81-41, v, 38 p., https://doi.org/10.3133/wri8141.","productDescription":"v, 38 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":119026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0041/report-thumb.jpg"},{"id":57031,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Williams Lake","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5226","contributors":{"authors":[{"text":"LaBaugh, J. W.","contributorId":23484,"corporation":false,"usgs":true,"family":"LaBaugh","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Groschen, G.E.","contributorId":17260,"corporation":false,"usgs":true,"family":"Groschen","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":199370,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":199372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67307,"text":"i1330 - 1981 - Geologic map of Pre-Quaternary rocks of the Salt Lake City North Quadrangle, Davis and Salt Lake counties, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i1330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1330","subseriesTitle":"NONE","title":"Geologic map of Pre-Quaternary rocks of the Salt Lake City North Quadrangle, Davis and Salt Lake counties, Utah","language":"ENGLISH","doi":"10.3133/i1330","usgsCitation":"Van Horn, R., 1981, Geologic map of Pre-Quaternary rocks of the Salt Lake City North Quadrangle, Davis and Salt Lake counties, Utah: U.S. Geological Survey IMAP 1330, 1 map :col. ;58 x 44 cm., https://doi.org/10.3133/i1330.","productDescription":"1 map :col. ;58 x 44 cm.","costCenters":[],"links":[{"id":106697,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9155.htm","linkFileType":{"id":5,"text":"html"},"description":"9155"},{"id":188074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,40.75 ], [ -112,40.8675 ], [ -111.86749999999999,40.8675 ], [ -111.86749999999999,40.75 ], [ -112,40.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e924","contributors":{"authors":[{"text":"Van Horn, R.","contributorId":20839,"corporation":false,"usgs":true,"family":"Van Horn","given":"R.","affiliations":[],"preferred":false,"id":275960,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67045,"text":"i1273 - 1981 - Map showing lava flows in the northwest part of the Thaumasia Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:24","indexId":"i1273","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1273","subseriesTitle":"NONE","title":"Map showing lava flows in the northwest part of the Thaumasia Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1273","usgsCitation":"Scott, D.H., and Tanaka, K.L., 1981, Map showing lava flows in the northwest part of the Thaumasia Quadrangle of Mars: U.S. Geological Survey IMAP 1273, 1 map :col. ;52 x 58 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1273.","productDescription":"1 map :col. ;52 x 58 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":438975,"rank":401,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9CYXW67","text":"USGS data release","linkHelpText":"Map showing lava flows in the northwest part of the Thaumasia Quadrangle of Mars"},{"id":187558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101392,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1273/plate-1.pdf","size":"9671","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a494f","contributors":{"authors":[{"text":"Scott, D. H.","contributorId":73565,"corporation":false,"usgs":true,"family":"Scott","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":275510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tanaka, K. L.","contributorId":31394,"corporation":false,"usgs":false,"family":"Tanaka","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67061,"text":"i1280 - 1981 - Map showing lava flows in the southeast part of the Amazonis Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:31","indexId":"i1280","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1280","subseriesTitle":"NONE","title":"Map showing lava flows in the southeast part of the Amazonis Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1280","usgsCitation":"Scott, D.H., and Tanaka, K.L., 1981, Map showing lava flows in the southeast part of the Amazonis Quadrangle of Mars: U.S. Geological Survey IMAP 1280, 1 map :col. ;40 x 59 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1280.","productDescription":"1 map :col. ;40 x 59 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":256417,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1280/plate-1.pdf","size":"7224","linkFileType":{"id":1,"text":"pdf"}},{"id":256418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1280/report.pdf","size":"26","linkFileType":{"id":1,"text":"pdf"}},{"id":256419,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1280/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658337","contributors":{"authors":[{"text":"Scott, D. H.","contributorId":73565,"corporation":false,"usgs":true,"family":"Scott","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":275540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tanaka, K. L.","contributorId":31394,"corporation":false,"usgs":false,"family":"Tanaka","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275539,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67527,"text":"i1229 - 1981 - Geologic map of the Chignik and Sutwik Island quadrangles, Alaska","interactions":[],"lastModifiedDate":"2017-01-27T11:46:33","indexId":"i1229","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1229","title":"Geologic map of the Chignik and Sutwik Island quadrangles, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/i1229","usgsCitation":"Detterman, R.L., Miller, T.P., Yount, M.E., and Wilson, F.H., 1981, Geologic map of the Chignik and Sutwik Island quadrangles, Alaska: U.S. Geological Survey IMAP 1229, 1 Map: 45.76 x 32.54 inches, https://doi.org/10.3133/i1229.","productDescription":"1 Map: 45.76 x 32.54 inches","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":186528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106654,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9047.htm","linkFileType":{"id":5,"text":"html"},"description":"9047"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Chignik quadrangle, Sutwik Island quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -160.5,56 ], [ -160.5,57 ], [ -156,57 ], [ -156,56 ], [ -160.5,56 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69cbbe","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":276564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, T. P.","contributorId":49345,"corporation":false,"usgs":true,"family":"Miller","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":276563,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yount, M. E.","contributorId":76748,"corporation":false,"usgs":true,"family":"Yount","given":"M.","middleInitial":"E.","affiliations":[],"preferred":false,"id":661238,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":661239,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":28152,"text":"wri80107 - 1981 - Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-20T14:39:25","indexId":"wri80107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-107","title":"Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin","docAbstract":"Various changes in the management practices for the Winnebago pool have been proposed. The objectives of the proposed changes are protecting wetlands adjacent to the lakes in the pool and assuring adequate flow in the Fox River downstream from Lake Winnebago. Three proposed operation plans for the Winnebago pool were studied to determine the effects on lake stage and discharge. A digital reservoir model simulated daily lake stage and discharge from the Winnebago pool.
\nInflow for this simulation was computed from daily discharge, recorded at Rapide Croche Dam, and daily stage, recorded at Oshkosh. This computed inflow is net inflow, combining the effects of streamflow, precipitation, evaporation, and net ground-water inflow.
\nThe model was adapted to simulate operation of the Winnebago pool according to each of the proposed plans. Because the important features of each operation plan were expressed in terms of stages to be attained at certain dates, simulated discharge was adjusted daily to keep simulated lake stage close to that specified in the plan.
\nThe simulated lake stage for each of the proposed plans exceeded the allowable maximum in some years. However, the simulated stage exceeded the allowable maximum less frequently and for shorter periods than did the observed stage.
\nFor the 61 years simulated (water years 1918-78), the simulated 7-day, 10- year low flow ((57,10) at Rapide Croche Dam was 1,000 ft^/s compared with 900 ft^/s for the observed record. The 7-day, 2-year low flow (Qy 2) was 1,500 ft^/s (simulated) versus 1,600 ft3/s (observed).
\nThe model predicted that executing the proposed operation plan would result in monthly Q7 JQ for August and September of 1,100 ft-Vs. This is no change for August and a 12-percent increase for September.
\nIn addition, the study illustrated that the discharge from the Winnebago pool could be managed to guarantee that the discharge in the Fox River downstream would not fall below a specified discharge up to 1,500 ft^/s. In most years this would have no effect on the stage of the pool. In a few years there would be a conflict between releasing water from the pool to maintain the desired discharge and maintaining water levels above the required minimum stage. The frequency of this possible conflict varies with the level of discharge desired in the Fox River from 1 year in 60 for a discharge of 1,100 ft^/s to about 1 year in 15 for a discharge of 1,500 ft^/s.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri80107","collaboration":"Prepared in cooperation with Wisconsin Department of Natural Resources, Fox Valley Water Quality Planning Agency","usgsCitation":"Krug, W.R., 1981, Hydrologic effects of proposed changes in management practices, Winnebago Pool, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 80-107, iv, 19 p., https://doi.org/10.3133/wri80107.","productDescription":"iv, 19 p.","numberOfPages":"25","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":158637,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0107/report-thumb.jpg"},{"id":56982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Fox River, Lake Butte des Morts, Lake Poygan, Lake Winneconne, Lake Winnebago","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.2911376953125,\n 42.867912483915305\n ],\n [\n -90.2911376953125,\n 44.70770622183535\n ],\n [\n -87.57202148437499,\n 44.70770622183535\n ],\n [\n -87.57202148437499,\n 42.867912483915305\n ],\n [\n -90.2911376953125,\n 42.867912483915305\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606f7d","contributors":{"authors":[{"text":"Krug, William R.","contributorId":53381,"corporation":false,"usgs":true,"family":"Krug","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28236,"text":"wri80116 - 1981 - User's guide for a general purpose dam-break flood simulation model (K-634)","interactions":[],"lastModifiedDate":"2020-05-22T17:40:39.359024","indexId":"wri80116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-116","title":"User's guide for a general purpose dam-break flood simulation model (K-634)","docAbstract":"An existing computer program for simulating dam-break floods for forecast purposes has been modified with an emphasis on general purpose applications. The original model was formulated, developed and documented by the National Weather Service. This model is based on the complete flow equations and uses a nonlinear implicit finite-difference numerical method. The first phase of the simulation routes a flood wave through the reservoir and computes an outflow hydrograph which is the sum of the flow through the dam 's structures and the gradually developing breach. The second phase routes this outflow hydrograph through the stream which may be nonprismatic and have segments with subcritical or supercritical flow. The results are discharge and stage hydrographs at the dam as well as all of the computational nodes in the channel. From these hydrographs, peak discharge and stage profiles are tabulated. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri80116","usgsCitation":"Land, L.F., 1981, User's guide for a general purpose dam-break flood simulation model (K-634): U.S. Geological Survey Water-Resources Investigations Report 80-116, iv, 101 p., https://doi.org/10.3133/wri80116.","productDescription":"iv, 101 p.","numberOfPages":"110","costCenters":[],"links":[{"id":367496,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/80/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/80/0116/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603b98","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27826,"text":"wri8153 - 1981 - Hydrologic and chemical evaluation of the ground-water resources of northwest Elkhart County, Indiana","interactions":[],"lastModifiedDate":"2020-11-04T18:05:32.65912","indexId":"wri8153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-53","title":"Hydrologic and chemical evaluation of the ground-water resources of northwest Elkhart County, Indiana","docAbstract":"A 3-year study in northwest Elkhart County, Indiana, was done to (1) de-fine the general flow and quality of water in the outwash aquifer system, (2) determine if a well field proposed for a site at the Elkhart Municipal Airport would draw leachate from the Himco landfill, and (3) define the areal extent of the ground water affected by the landfill and an east-side industrial-park area.
The outwash aquifers are mainly composed of sand and gravel and are separated by a silt and clay bed. The saturated thickness of these deposits averages 175 feet and ranges from 85 to 500 feet. Where present, the silt and clay bed confines the underlying aquifer. The confining bed is absent in the area underlying the landfill and part of the airport. Average hydraulic conductivities of the sand, and the sand and gravel, are 80 and 400 feet per day, respectively. Regional ground-water flow is toward the St. Joseph River.
A quasi-three-dimensional ground-water flow model, calibrated to match measured water levels and river seepages, was used to simulate proposed pumpings in the airport area. Drawdowns for simulated pumpings of 7.5-, 10-, and 20-million gallons per day were small percentages of the saturated thick-nesses of the unconfined aquifer underlying the airport area. Model-simulated streamflow reductions in Christiana Creek for these pumpings were 9, 12, and 23 percent of base flow, respectively. The model-simulated, steady-state water-level maps for the 7.5- and 10-million-gallons-per-day pumping experiments indicated that these pumpings would not draw water from the land-fill area to the pumping center at the airport. The simulated map for the 20-million-gallons-per-day pumping indicated that only a small part of the flow into the pumping center could come from the landfill area.
The general quality of ground water in the study area, defined by analyses of 68 water samples from 35 observation wells, included slightly basic pH (7-8), average hardness greater than 200 milligrams per liter as calcium carbonate, average alkalinity greater than 150 milligrams per liter as calcium carbonate, and, in more than 90 percent of the analyses, a calcium bicarbonate water type.
Eight volatile organic compounds were detected in water from 8 of 19 wells sampled in the industrial-park area. The health-effects advisory limit for chronic exposure to trichloroethylene was exceeded in samples from six of these wells. Areally, the results did not define a plume or a source of the volatile organic compounds.
Concentrations of dissolved solids, bicarbonate, bromide, chloride, sulfate, ammonia, calcium, magnesium, manganese, potassium, sodium, and dis-solved organic carbon in the leachate were at least five times their back-ground concentrations. Concentrations of bromide and dissolved solids were the best indicators of leachate. Bromide concentrations plotted areally indicated that the landfill was the source of the leachate, the leachate plume extended between 3,100 and 5,600 feet downgradient from the landfill, and the plume had not spread laterally much farther than the original width of the landfill. Bromide and dissolved-solids concentrations plotted in cross section indicated that the leachate plume was sinking as it spread downgradient in the shallow unconfined aquifer and the leachate was present in deep wells under and immediately downgradient from the landfill. All chemical constituents were attenuated within approximately 1 mile downgradient from the landfill.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8153","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources and the Elkhart Water Works","usgsCitation":"Imbrigiotta, T., and Martin, A., 1981, Hydrologic and chemical evaluation of the ground-water resources of northwest Elkhart County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 81-53, ix, 140 p., https://doi.org/10.3133/wri8153.","productDescription":"ix, 140 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380154,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0053/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Elkhart County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.7874,41.7615],[-85.7591,41.7613],[-85.6606,41.7608],[-85.6589,41.699],[-85.6575,41.6122],[-85.6554,41.5251],[-85.6542,41.4733],[-85.6552,41.4384],[-85.7704,41.4377],[-85.8874,41.4379],[-86.0008,41.4375],[-86.059,41.4367],[-86.0594,41.4644],[-86.0593,41.474],[-86.0593,41.479],[-86.0592,41.4935],[-86.0598,41.4999],[-86.0624,41.7619],[-85.932,41.7623],[-85.7874,41.7615]]]},\"properties\":{\"name\":\"Elkhart\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118d0","contributors":{"authors":[{"text":"Imbrigiotta, Thomas E. 0000-0003-1716-4768 timbrig@usgs.gov","orcid":"https://orcid.org/0000-0003-1716-4768","contributorId":2466,"corporation":false,"usgs":true,"family":"Imbrigiotta","given":"Thomas E.","email":"timbrig@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":198744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Angel Jr.","contributorId":42571,"corporation":false,"usgs":true,"family":"Martin","given":"Angel","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":198745,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10206,"text":"ofr811027 - 1981 - Assessment of conventionally recoverable petroleum resources, Volga-Urals Basin, U.S.S.R.","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr811027","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":"81-1027","title":"Assessment of conventionally recoverable petroleum resources, Volga-Urals Basin, U.S.S.R.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811027","usgsCitation":"Masters, C.D., and Peterson, J.A., 1981, Assessment of conventionally recoverable petroleum resources, Volga-Urals Basin, U.S.S.R.: U.S. Geological Survey Open-File Report 81-1027, 8 p. ill., map ;28 cm., https://doi.org/10.3133/ofr811027.","productDescription":"8 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1027/report-thumb.jpg"},{"id":38063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67281e","contributors":{"authors":[{"text":"Masters, Charles D.","contributorId":38969,"corporation":false,"usgs":true,"family":"Masters","given":"Charles","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":161002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161003,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28010,"text":"wri8170 - 1981 - Two-dimensional ground-water flow model of the Cretaceous aquifer system of Lee County and vicinity, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri8170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-70","title":"Two-dimensional ground-water flow model of the Cretaceous aquifer system of Lee County and vicinity, Mississippi","docAbstract":"A two-dimensional ground-water flow model of the Eutaw-McShan and Gordo aquifers in the area of Lee County, Miss., was successfully calibrated and verified using data from six long-term observation wells and two intensive studies of areal water levels. The water levels computed by the model were found to be most sensitive to changes in simulated aquifer hydraulic conductivity and to changes in head in the overlying Coffee Sand aquifer. The two-dimensional model performed reasonably well in simulating the aquifer system except possibly in southern Lee County and southward where a clay bed at the top of the Gordo Formation partially isolated the Gordo from the overlying Eutaw-McShan aquifer. The verified model was used to determine theoretical aquifer response to increased ground-water withdrawal to the year 2000. Two estimated rates of increase and five possible well field locations were examined. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8170","usgsCitation":"Kernodle, J.M., 1981, Two-dimensional ground-water flow model of the Cretaceous aquifer system of Lee County and vicinity, Mississippi: U.S. Geological Survey Water-Resources Investigations Report 81-70, vi, 53 leaves :ill., maps ;28 cm., https://doi.org/10.3133/wri8170.","productDescription":"vi, 53 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":56835,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0070/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6238fd","contributors":{"authors":[{"text":"Kernodle, John Michael","contributorId":99171,"corporation":false,"usgs":true,"family":"Kernodle","given":"John","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":199064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28255,"text":"wri8135 - 1981 - Ground-water resources of the White River basin, Madison County, Indiana","interactions":[],"lastModifiedDate":"2020-11-04T18:03:15.372006","indexId":"wri8135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-35","title":"Ground-water resources of the White River basin, Madison County, Indiana","docAbstract":"The ground-water resources of the White River basin in and near Madison County, Indiana, were investigated by mapping the aquifers, estimating their hydraulic properties, determining the distribution of potentiometric head in the aquifers, and estimating some of the components of the ground-water budget from data collected in the field. This information was used to construct and calibrate a five-layer, digital ground-water flow model. The model, constructed and calibrated to ground-water-level and seepage data collected during the study, simulates conditions for the autumn of 1976. The model was used to provide estimates of ground-water potential in terms of yield, drawdown, and depletion in streamflow.
Glacial drift covers nearly the entire study area and ranges in thickness from 0 to approximately 300 feet. Beneath the drift lie Ordovician to Devonian limestone, dolomite, and shale. A bedrock valley trends west-northwest through the center of the study area. Relief of the bedrock surface is approximately 325 feet.
Four confined sand and gravel aquifers interbedded in the glacial drift, a bedrock aquifer, and an unconfined outwash aquifer are the three most important aquifer systems in the study area. The nearly horizontal, areally discontinuous, confined sand and gravel aquifers have an average thickness of about 15 feet and an average hydraulic conductivity estimated to be 433 feet per day. The bedrock aquifer underlying the entire study area has a thick-ness estimated to be 150 feet and an average transmissivity estimated in previous studies in the basin to be 1,340 square feet per day. The unconfined outwash aquifer, although thin and narrow, is an important aquifer because of its proximity to sources of induced recharge.
Water-level fluctuations in observation wells in the basin indicate that the ground-water system is in dynamic equilibrium. Ground-water seepage to streams at 90-percent flow duration on October 1, 1976, was estimated to be between 15.9 and 74.4 cubic feet per second. Ground-water pumpage for 1976 was estimated to be 19.7 million gallons per day (30.5 cubic feet per second). The water budget, as simulated in the model, indicates that the rate of inflow to the ground-water system in the modeled area is 92.4 cubic feet per second. Of this, 78 percent is from effective areal recharge of precipitation, and 22 percent is from ground-water flow across the boundaries into the study area. Thirty-three percent of the ground-water outflow is pumpage, 59 percent is seepage to streams, and the remaining 8 percent is ground-water flow across the boundaries out of the study area.
Model simulations of eight pumping plans provide a general assessment of the water-yielding potential of the three major aquifer systems and indicate that as much as 2.5 million gallons per day can be obtained from well fields about half a square mile in area. Model results also indicate that, for as much as 2.5-million gallons per day pumping, flow in the large streams will not be significantly affected, whereas flow in the small streams may be significantly affected. In addition, simulations indicate that adding more wells to the well field northwest of Anderson, Ind., would probably be no more advantageous than increasing the pumpage in the existing wells. How-ever, well interference, well hydraulics, and pumping-level constraints were not considered in the investigation of alternative methods of expanding the well field. In developing the ground-water system in the area, use of many small, scattered well fields that produce less than about 3 million gallons per day may be more favorable hydrologically than a few, heavily pumped well fields.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8135","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Lapham, W.W., 1981, Ground-water resources of the White River basin, Madison County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 81-35, vii, 112 p., https://doi.org/10.3133/wri8135.","productDescription":"vii, 112 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0035/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Madison","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.5784,40.3794],[-85.5763,40.0769],[-85.5774,39.9459],[-85.8624,39.9436],[-85.863,40.139],[-85.8617,40.2201],[-85.8621,40.3784],[-85.5784,40.3794]]]},\"properties\":{\"name\":\"Madison\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64931a","contributors":{"authors":[{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8379,"text":"ofr81705 - 1981 - Outer Continental Shelf Oil and Gas Information Program: Atlantic index (December 1980 - June 1981)","interactions":[],"lastModifiedDate":"2022-11-04T17:29:01.987679","indexId":"ofr81705","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":"81-705","title":"Outer Continental Shelf Oil and Gas Information Program: Atlantic index (December 1980 - June 1981)","docAbstract":"In an effort to develop the oil and gas resources of the Outer Continental Shelf (OCS), the United States currently conducts a leasing program for these resources. The Secretary of the Department of the Interior has been designated by the Outer Continental Shelf Lands Act of 1953 (43 U.S.C. 1331-1343), as amended by the Outer Continental Shelf Lands Acts of 1978, to manage and regulate many of the activities that relate to the leasing, exploration, development, and production of the OCS mineral resources. Many of the Secretary's responsibilities have been delegated to the Bureau of Land Management (BLM) and the U.S. Geological Survey (USGS).
Under OCS Lands Act an Outer Continental Shelf Oil and Gas Information Program was created and is managed by the BLM and the USGS. Authorities and operating procedures are detailed in the Code of Federal Regulations at 30 CFR 252 and 43 CFR 3300.
Under this program regional indexes are prepared by the U.S. Geological Survey in conjunction with the Bureau of Land Management, and they list all relevant, actual, or proposed programs, plans, reports, environmental impact statements, and other lease sale information. The indexes are provided on a regular basis to affected States and, upon request, to local governments.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81364A","usgsCitation":"Cobb, E.H., 1981, Summaries of data on and lists of references to metallic and selected nonmetallic mineral occurrences in the Teller quadrangle, Alaska: Supplement to Open-File Report 75-587, part A — Summaries of data to January 1, 1980: U.S. Geological Survey Open-File Report 81-364, 25 p., https://doi.org/10.3133/ofr81364A.","productDescription":"25 p.","costCenters":[],"links":[{"id":35927,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0364a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0364a/report-thumb.jpg"},{"id":403703,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75483.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Teller quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -168,\n 65\n ],\n [\n -165,\n 65\n ],\n [\n -165,\n 66\n ],\n [\n -168,\n 66\n ],\n [\n -168,\n 65\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699793","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":157557,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}