{"pageNumber":"4917","pageRowStart":"122900","pageSize":"25","recordCount":165626,"records":[{"id":11254,"text":"ofr81941 - 1981 - Large fracture experimentation","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr81941","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":"81-941","title":"Large fracture experimentation","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81941","usgsCitation":"Sondergeld, C.H., and Spetzler, H.A., 1981, Large fracture experimentation: U.S. Geological Survey Open-File Report 81-941, 14 p., 28 cm, https://doi.org/10.3133/ofr81941.","productDescription":"14 p., 28 cm","costCenters":[],"links":[{"id":145791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0941/report-thumb.jpg"},{"id":39050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0941/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9060","contributors":{"authors":[{"text":"Sondergeld, Carl H.","contributorId":46960,"corporation":false,"usgs":true,"family":"Sondergeld","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162814,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spetzler, Hartmut A.","contributorId":10433,"corporation":false,"usgs":true,"family":"Spetzler","given":"Hartmut","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":162813,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39542,"text":"pp529N - 1981 - Atlantic continental shelf and slope of the United States: Macrobenthic invertebrate fauna of the middle Atlantic bight region — Faunal composition and quantitative distribution","interactions":[],"lastModifiedDate":"2022-01-11T19:16:10.906665","indexId":"pp529N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"529","chapter":"N","title":"Atlantic continental shelf and slope of the United States: Macrobenthic invertebrate fauna of the middle Atlantic bight region — Faunal composition and quantitative distribution","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp529N","usgsCitation":"Wigley, R.L., and Theroux, R.B., 1981, Atlantic continental shelf and slope of the United States: Macrobenthic invertebrate fauna of the middle Atlantic bight region — Faunal composition and quantitative distribution: U.S. Geological Survey Professional Paper 529, viii, 198 p., https://doi.org/10.3133/pp529N.","productDescription":"viii, 198 p.","costCenters":[],"links":[{"id":394194,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4574.htm"},{"id":67144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0529n/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0529n/report-thumb.jpg"}],"country":"United States","otherGeospatial":"middle Atlantic bight region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.1240234375,\n              35.06597313798418\n            ],\n            [\n              -68.115234375,\n              35.06597313798418\n            ],\n            [\n              -68.115234375,\n              41.77131167976407\n            ],\n            [\n              -77.1240234375,\n              41.77131167976407\n            ],\n            [\n              -77.1240234375,\n              35.06597313798418\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669aae","contributors":{"authors":[{"text":"Wigley, R. L.","contributorId":18440,"corporation":false,"usgs":true,"family":"Wigley","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":221627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theroux, R. B.","contributorId":20391,"corporation":false,"usgs":true,"family":"Theroux","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":221628,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10122,"text":"ofr81739 - 1981 - Sources of data, procedures, and bibliography for coal resource investigation of western Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr81739","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":"81-739","title":"Sources of data, procedures, and bibliography for coal resource investigation of western Maryland","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81739","usgsCitation":"Lyons, P., and Jacobsen, E.F., 1981, Sources of data, procedures, and bibliography for coal resource investigation of western Maryland: U.S. Geological Survey Open-File Report 81-739, iii, 37 p. ill. ;28 cm., https://doi.org/10.3133/ofr81739.","productDescription":"iii, 37 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0739/report-thumb.jpg"},{"id":37971,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0739/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7677","contributors":{"authors":[{"text":"Lyons, Paul C.","contributorId":79894,"corporation":false,"usgs":true,"family":"Lyons","given":"Paul C.","affiliations":[],"preferred":false,"id":160849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobsen, Edwin F.","contributorId":16020,"corporation":false,"usgs":true,"family":"Jacobsen","given":"Edwin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160848,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10013,"text":"ofr81430 - 1981 - Continuity and tectonic implications of the San Simeon-Hosgri fault zone, central California","interactions":[],"lastModifiedDate":"2022-09-27T21:47:17.929351","indexId":"ofr81430","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":"81-430","title":"Continuity and tectonic implications of the San Simeon-Hosgri fault zone, central California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81430","usgsCitation":"Leslie, R.B., 1981, Continuity and tectonic implications of the San Simeon-Hosgri fault zone, central California: U.S. Geological Survey Open-File Report 81-430, v, 64 p., https://doi.org/10.3133/ofr81430.","productDescription":"v, 64 p.","costCenters":[],"links":[{"id":37827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0430/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0430/report-thumb.jpg"},{"id":407495,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12035.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"San Simeon-Hosgri fault zone","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              35.35\n            ],\n            [\n              -121.5,\n              35.35\n            ],\n            [\n              -121.5,\n              36\n            ],\n            [\n              -121,\n              36\n            ],\n            [\n              -121,\n              35.35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f12","contributors":{"authors":[{"text":"Leslie, Rob B.","contributorId":57856,"corporation":false,"usgs":true,"family":"Leslie","given":"Rob","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":160673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10012,"text":"ofr81485 - 1981 - Evapotranspiration from rapidly growing young saltcedar in the Gila River Valley of Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr81485","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":"81-485","title":"Evapotranspiration from rapidly growing young saltcedar in the Gila River Valley of Arizona","docAbstract":"Estimates of evapotranspiration by young saltcedar, based on energy budget measurements, were made for an unfilled portion of the San Carlos Reservoir in east-central Arizona. Foty-eight days of record were obtained before the site was inundated. The young saltcedar, which had grown from seed earlier in the season , had an average daily evapotranspiration of 5.8 millimeters of water during the period August 17, 1971, to October 3, 1971. Daily values ranged from 9.2 millimeters to a low of 0.23 millimeters which occurred during a stormy day. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81485","usgsCitation":"Leppanen, O., 1981, Evapotranspiration from rapidly growing young saltcedar in the Gila River Valley of Arizona: U.S. Geological Survey Open-File Report 81-485, v, 31 p.:ill., map ;28 cm., https://doi.org/10.3133/ofr81485.","productDescription":"v, 31 p.:ill., map ;28 cm.","costCenters":[],"links":[{"id":143965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0485/report-thumb.jpg"},{"id":37826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0485/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9aa8","contributors":{"authors":[{"text":"Leppanen, O.E.","contributorId":11225,"corporation":false,"usgs":true,"family":"Leppanen","given":"O.E.","email":"","affiliations":[],"preferred":false,"id":160672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39595,"text":"pp907F - 1981 - The Nature and Use of Copper Reserve and Resource Data","interactions":[],"lastModifiedDate":"2012-02-02T00:10:18","indexId":"pp907F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"907","chapter":"F","title":"The Nature and Use of Copper Reserve and Resource Data","docAbstract":"Copper reserve, resource, and production data can be combined to produce disaggregated resource estimates and trends and, when combined with demand forecasts, can be used to predict future exploration and development requirements.\r\n\r\nReserve estimates are subject to uncertainties due mainly to incomplete exploration and rapidly changing economic conditions. United States' reserve estimates in the past have been low mainly because knowledge of the magnitude of very large porphyry-copper deposits has been incomplete. Present estimates are considerably more reliable because mining firms tend to drill out deposits fully before mining and to release their reserve estimates to the public.\r\n\r\nThe sum of reserves and past production yields an estimate of the total ore, total metal contained in ore, and average grade of ore originally in each of the deposits known in the United States. For most deposits, estimates of total copper in ore are low relative to the total copper in mineralized rock, and many estimates are strongly affected by the economic behavior of mining firms. A better estimate of the real distribution of copper contained in deposits can be obtained by combining past production data with resource estimates.\r\n\r\nCopper resource data are disaggregated into categories that include resources in undeveloped deposits similar to those mined in the past, resources in mines closed because of unfavorable economic conditions, resources in deep deposits requiring high-cost mining methods, arid resources in deposits located in areas where environmental restrictions have contributed to delays in development. The largest resource is located in the five largest porphyry deposits. These deposits are now being mined but the resources are not included in the present mining plan. Resources in this last category will not contribute to supply until some future time when ores presently being mined are depleted.\r\n\r\nA high correlation exists between total copper contained in deposits and annual production from deposits. This correlation can be used to predict roughly the potential production from undeveloped deposits. Large deposits annually produce relatively less metal per ton of copper contained than do medium and small deposits.\r\n\r\nDividing reserves by annual production gives a depletion date for each copper mine. The sum of annual production capacity of all mines not yet depleted at any year of interest gives the minimum production capacity for that year. A graph of minimum production capacity by year combined with curves representing potential capacity from undeveloped identified resources can be compared with various demand scenarios to yield a measure of copper requirements from new sources.\r\n\r\nSince 1950 reserves have been developed in the United States at a rate of about 1 million tons of copper per year. Since 1960 the number of deposits developed per 10-year period has greatly increased without a commensurate increase in tonnage of copper. This is in part due to the fact that recent exploration successes have been increasingly represented by smaller and (or) lower grade deposits containing less metal. ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp907F","usgsCitation":"Cox, D.P., Wright, N.A., and Coakley, G.J., 1981, The Nature and Use of Copper Reserve and Resource Data: U.S. Geological Survey Professional Paper 907, vi, 19 p., https://doi.org/10.3133/pp907F.","productDescription":"vi, 19 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":119836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0907f/report-thumb.jpg"},{"id":67182,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0907f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9e9e","contributors":{"authors":[{"text":"Cox, Dennis P. dcox@usgs.gov","contributorId":2766,"corporation":false,"usgs":true,"family":"Cox","given":"Dennis","email":"dcox@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":221736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, Nancy A.","contributorId":28586,"corporation":false,"usgs":true,"family":"Wright","given":"Nancy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":221737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coakley, George J.","contributorId":83586,"corporation":false,"usgs":true,"family":"Coakley","given":"George","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":221738,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10172,"text":"ofr81513 - 1981 - User oriented, interactive Multics computer programs to create grid cell, contour, and perspective maps using Surface Display Library","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr81513","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":"81-513","title":"User oriented, interactive Multics computer programs to create grid cell, contour, and perspective maps using Surface Display Library","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81513","usgsCitation":"Mark, R.K., and Newman, E.B., 1981, User oriented, interactive Multics computer programs to create grid cell, contour, and perspective maps using Surface Display Library: U.S. Geological Survey Open-File Report 81-513, 50 p. :ill. ;28 cm., https://doi.org/10.3133/ofr81513.","productDescription":"50 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":144285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0513/report-thumb.jpg"},{"id":38019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0513/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60410c","contributors":{"authors":[{"text":"Mark, R. K.","contributorId":32159,"corporation":false,"usgs":true,"family":"Mark","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":160936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newman, E. B.","contributorId":52571,"corporation":false,"usgs":true,"family":"Newman","given":"E.","middleInitial":"B.","affiliations":[],"preferred":false,"id":160937,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10169,"text":"ofr81462 - 1981 - Catalog of earthquakes along the San Andreas fault system in central California, July-September 1977","interactions":[],"lastModifiedDate":"2023-11-20T16:42:12.238161","indexId":"ofr81462","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":"81-462","title":"Catalog of earthquakes along the San Andreas fault system in central California, July-September 1977","docAbstract":"<p>Numerous small earthquakes occur each day in the Coast Ranges of central California. The detailed study of these earthquakes provides a tool for gaining insight into the tectonic and physical processes responsible for the generation of damaging earthquakes. This catalog contains the fundamental parameters for earthquakes located within and adjacent to the seismograph network operated by the U.S. Geological Survey (USGS), during the third quarter of 1977.</p><p>The motivation for these detailed studies has been described by Pakiser and others (1969) and by Eaton and others (1970). Similar catalogs of earthquakes for the years 1969, 1970, and 1971 have been prepared by Lee and others (1972b, c and d). Catalogs for the first, second, third, and fourth quarters of 1972 and the first, second, third and fourth quarters of 1973 have been prepared by Wesson and others (1972a, b, 1973b, and 1974a and b), by Bufe and others (1975), and by Lester and others (1976a and b). Catalogs for the years 1974, 1975 and 1976 and the first quarter of 1977 have been prepared by Lester and Meagher (1978), by McHugh and Lester (1978 and 1979) and by Marks and Lester (1980a and 1980b). The basic data contained in these catalogs provide a foundation for further studies.</p><p>This catalog contains data on 855 earthquakes in central California. Arrival times at 205 seismograph stations were used to locate the earthquakes listed in this catalog. Of these 193 were telemetered stations operated by USGS. Readings from the remaining 12 stations were obtained through the courtesy of the Seismographic Stations, California Institute of Technology, Pasadena, University of California, Berkeley (UCB), and the California Department of Water Resources, Sacramento.</p><p>The Seismographic Station of the University of California, Berkeley, has for many years published a bulletin describing earthquakes in northern California and the surrounding area and listing readings at UCB stations from more distant events. The purpose of the present catalog is not to replace the UCB Bulletin, but rather to supplement it, by describing the seismicity of a portion of central California in much greater detail.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81462","usgsCitation":"Marks, S., and Fluty, L., 1981, Catalog of earthquakes along the San Andreas fault system in central California, July-September 1977: U.S. Geological Survey Open-File Report 81-462, 43 p., https://doi.org/10.3133/ofr81462.","productDescription":"43 p.","costCenters":[],"links":[{"id":144266,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0462/report-thumb.jpg"},{"id":405084,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0462/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"central California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.77246093750001,\n              34.288991865037524\n            ],\n            [\n              -117.6416015625,\n              34.288991865037524\n            ],\n            [\n              -117.6416015625,\n              38.565347844885466\n            ],\n            [\n              -121.77246093750001,\n              38.565347844885466\n            ],\n            [\n              -121.77246093750001,\n              34.288991865037524\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efa6f","contributors":{"authors":[{"text":"Marks, S.M.","contributorId":33687,"corporation":false,"usgs":true,"family":"Marks","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":160932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fluty, L.","contributorId":8097,"corporation":false,"usgs":true,"family":"Fluty","given":"L.","email":"","affiliations":[],"preferred":false,"id":160931,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","interactions":[{"subject":{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"ofr81220","publicationYear":"1981","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"chapter":"E","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"id":1}],"supersededBy":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"lastModifiedDate":"2022-08-09T15:28:15.441093","indexId":"ofr81220","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":"81-220","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","docAbstract":"<p>The need for large quantities of energy has created interest in the Fort Union coal region of the Northern Great Plains. Extensive development of this coal, which may include onsite steam-power generation, gasification, liquefaction, and slurry-pipeline transport of the coal from this region, would place a heavy demand on the region's limited streamflow. Paleozoic rocks that underlie the Fort Union coal region and aquifers in these rocks, including the Red River Formation and the Madison Limestone, might supply, at least on a temporary basis, a significant part of the water required for coal development. The area of study covers approximately 200,000 square miles, and includes eastern Montana, western North Dakota and South Dakota, northeastern Wyoming, and northwestern Nebraska. This report, one of a series in the Madison Limestone study, uses hydrologic and geologic data to outline potentially favorable areas for well construction - that is, areas in which there is a good probability that large-yield wells (more than 500 gallons per minute) can be completed in the Red River Formation and in the Madison Limestone. Potentially favorable areas in terms of aquifer characteristics, for both the Red River Formation and the Madison Limestone, are given a numerical evaluation from 1 to 3 based on the number of the following criteria that are met: (1) the presence of more than 100 feet of relatively porous rock, (2) the presence of more than 100 feet of dolomite, and (3) the presence of known geologic structures which could affect yield. Areas rated 3 are those in which all three criteria are satisfied; areas rated 2 are those in which two criteria are satisfied; and areas rated 1 are those in which only one criterion is satisfied. The criteria selected for this analysis were chosen because they can be recognized and mapped over the entire study area. Local features such as minor structures, solution zones, and rock facies of small extent were not included in this regional evaluation. In addition, water quality was considered in a general way in defining the favorable areas, by excluding areas in which the electrical resistivity of formation water, as calculated from geophysical well logs, was less than 1 ohm-meter. The numerical scales of the Red River Formation and Madison Limestone are summed to show potentially favorable areas for the combined aquifers. Certain additional factors which may be important to a prospective water user were not included in the numerical ranking - these include depths to the two aquifers, calcite saturation, water temperature, total dissolved solids, and piezometric head in relation to land surface. For a complete evaluation, potential users should consider these factors plus local structures, facies, and solution zones in conjunction with the numerical rankings reflecting aquifer characteristics. To facilitate consideration of piezometric head, maps are included in this report showing areas in which the piezometric head falls in certain ranges with respect to land surface.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81220","usgsCitation":"MacCary, L., Cushing, E.M., and Brown, D.L., 1981, Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska: U.S. Geological Survey Open-File Report 81-220, Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches, https://doi.org/10.3133/ofr81220.","productDescription":"Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches","costCenters":[],"links":[{"id":405012,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0220/report-thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.13671875,\n              40.111688665595956\n            ],\n            [\n              -96.328125,\n              40.111688665595956\n            ],\n            [\n              -96.328125,\n              49.03786794532644\n            ],\n            [\n              -115.13671875,\n              49.03786794532644\n            ],\n            [\n              -115.13671875,\n              40.111688665595956\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86be","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":160852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, David L.","contributorId":55425,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160853,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10086,"text":"ofr81378 - 1981 - Baseline studies of the feasibility and reliability of using animal behavior as a component in the prediction of earthquakes","interactions":[],"lastModifiedDate":"2024-03-04T22:38:35.297835","indexId":"ofr81378","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":"81-378","title":"Baseline studies of the feasibility and reliability of using animal behavior as a component in the prediction of earthquakes","docAbstract":"<p>This project was established to determine if it were possible to advance the state of the art in earthquake prediction by learning more about claims that unusual animal behavior was an earthquake precursor. We used intensive post-earthquake interview surveys to gather objective reports both of instances of unusual animal behavior as an earthquake precursor and of instances in which animals behaved normally prior to a moderate or large earthquake. We prepared briefing volumes describing the cultural significance and interpretation of seismicity for cultures other than our own with which we were likely to have contact. This information helped us assess the impact of cultural expectations on our data set. These briefing volumes are one of the work products of our project and are included in this final report.</p><p>Since our goal was to increase the ability to predict earthquakes, we avoided study of earthquakes with known foreshocks since in those cases the unusual animal behavior might have resulted simply from the foreshocks. Our data indicates that unusual animal behavior occurs a few hours to a few days before some, but not most, earthquakes that do not have known foreshocks.</p><p>Our studies of earthquake folklore support the same conclusion (pp 121-144 of this report). Even when unusual animal behavior is a precursor to a particular earthquake, most individual animals behave normally. This creates a signal to noise ratio that will reduce the potential for direct use of unusual -animal behavior in earthquake prediction, but the analysis of some animals reactions might help to identify physical precursors to at least some earthquakes.</p><p>Each phase of this research program has produced one or more completed work products. These products, which follow, compose our final report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81378","usgsCitation":"Lott, D.F., Hart, B.L., and Verosub, K.L., 1981, Baseline studies of the feasibility and reliability of using animal behavior as a component in the prediction of earthquakes: U.S. Geological Survey Open-File Report 81-378, 150 p., https://doi.org/10.3133/ofr81378.","productDescription":"150 p.","costCenters":[],"links":[{"id":426295,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0378/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143973,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0378/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64887a","contributors":{"authors":[{"text":"Lott, Dale F.","contributorId":31393,"corporation":false,"usgs":true,"family":"Lott","given":"Dale","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":160796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, Benjamin L.","contributorId":40992,"corporation":false,"usgs":true,"family":"Hart","given":"Benjamin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Verosub, Kenneth L.","contributorId":78744,"corporation":false,"usgs":true,"family":"Verosub","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160798,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10089,"text":"ofr81142 - 1981 - Radionuclide concentrations in streams in the upper Blackfoot River basin, southeastern Idaho","interactions":[],"lastModifiedDate":"2013-11-21T13:28:00","indexId":"ofr81142","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":"81-142","title":"Radionuclide concentrations in streams in the upper Blackfoot River basin, southeastern Idaho","docAbstract":"Data on radionuclide concentrations in water and sediment material in the phosphate-mining area of the upper Blackfoot River basin were collected from May to October 1979. Maximum measured uranium and radium-226 concentrations dissolved in water were 3.7 micrograms per liter and 1.8 picocuries per liter , respectively. Maximum measured uranium and radium-226 concentrations in stream-bottom material were 5.5 micrograms per gram and 1.8 picocuries per gram, respectively. Maximum measured uranium and radium-226 concentrations on bottom material were 9.9 micrograms per gram and 3.9 picocuries per gram, respectively, in sediment-retention ponds, and 17 micrograms per gram and 3.5 picocuries per gram, respectively, in a mine pit. Maximum observed radon-222 concentration was 120 picocuries per liter in surface water and averaged 550 picocuries per liter at Formation Springs (site 10). All radionuclide concentrations were within existing State and Federal water-quality standards. Radionuclide concentrations were not significantly increased downstream from active mining sites. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81142","usgsCitation":"Low, W.H., 1981, Radionuclide concentrations in streams in the upper Blackfoot River basin, southeastern Idaho: U.S. Geological Survey Open-File Report 81-142, Report: v, 17 p.; 1 Plate: 16.02 X 17.36 inches, https://doi.org/10.3133/ofr81142.","productDescription":"Report: v, 17 p.; 1 Plate: 16.02 X 17.36 inches","numberOfPages":"22","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":143976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0142/report-thumb.jpg"},{"id":37941,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0142/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37942,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Blackfoot River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.9883,42.6156 ], [ -112.9883,43.6065 ], [ -111.5604,43.6065 ], [ -111.5604,42.6156 ], [ -112.9883,42.6156 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649b25","contributors":{"authors":[{"text":"Low, Walton H.","contributorId":92672,"corporation":false,"usgs":true,"family":"Low","given":"Walton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":160803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10050,"text":"ofr81404 - 1981 - A 10-year plan to study the aquifer system of Indian Wells Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr81404","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":"81-404","title":"A 10-year plan to study the aquifer system of Indian Wells Valley, California","docAbstract":"Water needs of the population of Indian Wells Valley, Calif., must be met through further development of ground-water resources. Studies show that annual ground-water pumpage there has increased since 1945 and has exceeded mean annual recharge since 1966. Continued and increased stress on the aquifer system of the valley is expected because population in the valley is predicted to double by 1998 and triple by 2020, based on 1977 population figures. The U.S. Geological Survey proposes a 10-year program to develop a data base to aid in evaluation of future water-management alternatives. A study plan has been developed that describes present and potential problems and objectives of the program, and outlines work items to be undertaken in the study area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81404","usgsCitation":"Lipinski, P., and Knochenmus, D.D., 1981, A 10-year plan to study the aquifer system of Indian Wells Valley, California: U.S. Geological Survey Open-File Report 81-404, iii, 18 p., 3 over-size sheets ;28 cm., https://doi.org/10.3133/ofr81404.","productDescription":"iii, 18 p., 3 over-size sheets ;28 cm.","costCenters":[],"links":[{"id":145608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0404/report-thumb.jpg"},{"id":37896,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0404/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37897,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0404/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37898,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0404/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37899,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0404/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd493be4b0b290850ef018","contributors":{"authors":[{"text":"Lipinski, Paul","contributorId":34144,"corporation":false,"usgs":true,"family":"Lipinski","given":"Paul","affiliations":[],"preferred":false,"id":160730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knochenmus, Darwin D.","contributorId":61043,"corporation":false,"usgs":true,"family":"Knochenmus","given":"Darwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160731,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10047,"text":"ofr81138 - 1981 - Hydrologic monitoring in the coal fields of central Utah, August 1978-September 1979","interactions":[],"lastModifiedDate":"2022-07-18T21:52:00.511532","indexId":"ofr81138","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":"81-138","title":"Hydrologic monitoring in the coal fields of central Utah, August 1978-September 1979","docAbstract":"<p>Surface-water quantity and quality were observed at 12 gaging stations downstream from mined and lease areas in the Wasatch Plateau, Book Cliff's, and Emery coal fields in central Utah. Measurements of base flow were made at 52 additional sites in the region. The report describes the hydrologic setting of this important coal region and summarizes the surface-water data collected at the monitoring sites from August 1978 through September 1979. Coal mining and lease activities in each of the monitored basins also are described.<br></p><p>Where possible, hydrologic impacts of coal mining are evaluated. Impacts include increases in streamflow and degradation of surface-water quality due to water discharged from underground mines. Other impacts include removal of water from ground-water storage, changes in the natural ground-water flow system, and possibly the diminution of spring flows.<br></p><p>Adequacy of the monitoring network to detect hydrologic changes due to mining is evaluated. In order to fully assess and quantify the impacts, comprehensive studies and monitoring of the ground-water system and water produced in mines are needed.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81138","usgsCitation":"Lines, G.C., and Plantz, G.G., 1981, Hydrologic monitoring in the coal fields of central Utah, August 1978-September 1979: U.S. Geological Survey Open-File Report 81-138, Report: vi, 56 p.; 1 Plate: 20.45 x 23.78 inches, https://doi.org/10.3133/ofr81138.","productDescription":"Report: vi, 56 p.; 1 Plate: 20.45 x 23.78 inches","costCenters":[],"links":[{"id":403968,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0138/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":403967,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0138/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0138/report-thumb.jpg"}],"country":"Utah","otherGeospatial":"central Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.62060546875,\n              38.18638677411551\n            ],\n            [\n              -109.951171875,\n              38.18638677411551\n            ],\n            [\n              -109.951171875,\n              39.65645604812829\n            ],\n            [\n              -113.62060546875,\n              39.65645604812829\n            ],\n            [\n              -113.62060546875,\n              38.18638677411551\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606612","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plantz, Gerald G.","contributorId":96149,"corporation":false,"usgs":true,"family":"Plantz","given":"Gerald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":160727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23161,"text":"ofr8159 - 1981 - A method of estimating average streamflow and headwater limits in U.S. Army Corps of Engineers, Mobile District, Alabama and adjacent states","interactions":[],"lastModifiedDate":"2012-02-02T00:08:04","indexId":"ofr8159","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":"81-59","title":"A method of estimating average streamflow and headwater limits in U.S. Army Corps of Engineers, Mobile District, Alabama and adjacent states","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr8159","issn":"0094-9140","usgsCitation":"Harkins, J.R., Shell, J., Carter, R., and Rumenik, R.P., 1981, A method of estimating average streamflow and headwater limits in U.S. Army Corps of Engineers, Mobile District, Alabama and adjacent states: U.S. Geological Survey Open-File Report 81-59, 2 maps ;on sheets 72 x 81 cm. and 63 x 81 cm., https://doi.org/10.3133/ofr8159.","productDescription":"2 maps ;on sheets 72 x 81 cm. and 63 x 81 cm.","costCenters":[],"links":[{"id":155762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":52499,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52500,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0059/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae022","contributors":{"authors":[{"text":"Harkins, Joe R.","contributorId":28982,"corporation":false,"usgs":true,"family":"Harkins","given":"Joe","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":189550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shell, J.D.","contributorId":66728,"corporation":false,"usgs":true,"family":"Shell","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":189552,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carter, R.F.","contributorId":101261,"corporation":false,"usgs":true,"family":"Carter","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":189553,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rumenik, Roger P.","contributorId":42626,"corporation":false,"usgs":true,"family":"Rumenik","given":"Roger","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":189551,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":38588,"text":"pp1199AE - 1981 - Shorter contributions to isotope research in the Western United States, 1980","interactions":[],"lastModifiedDate":"2025-08-22T19:19:13.420598","indexId":"pp1199AE","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1199","chapter":"A-E","title":"Shorter contributions to isotope research in the Western United States, 1980","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1199AE","usgsCitation":"Peterman, Z.E., Bunker, C.M., Bush, C.A., Bryant, B., Marvin, R.F., Naeser, C.W., Mehnert, H.H., Izett, G., Obradovich, J.D., and Cebula, G., 1981, Shorter contributions to isotope research in the Western United States, 1980: U.S. Geological Survey Professional Paper 1199, 47 p., https://doi.org/10.3133/pp1199AE.","productDescription":"47 p.","costCenters":[],"links":[{"id":494565,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74538.htm","text":"Radioelement distribution in a 3.06-kilometer drill hole in Precambrian crystalline rocks, Wind River Mountains, Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":494564,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74449.htm","text":"Potassium-argon and fission-track zircon ages of Cerro Toledo Rhyolite tephra in the Jemez Mountains, New Mexico","linkFileType":{"id":5,"text":"html"}},{"id":494563,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74448.htm","text":"Ages of igneous rocks in the South Park - 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D.","contributorId":48966,"corporation":false,"usgs":true,"family":"Obradovich","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":220122,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Cebula, G. T.","contributorId":11603,"corporation":false,"usgs":true,"family":"Cebula","given":"G. T.","affiliations":[],"preferred":false,"id":220117,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":18067,"text":"ofr81526 - 1981 - Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho, emphasis: 1974-1978","interactions":[{"subject":{"id":18067,"text":"ofr81526 - 1981 - Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho, emphasis: 1974-1978","indexId":"ofr81526","publicationYear":"1981","noYear":false,"title":"Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho, emphasis: 1974-1978"},"predicate":"SUPERSEDED_BY","object":{"id":988,"text":"wsp2191 - 1982 - Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho — Emphasis: 1974–1978","indexId":"wsp2191","publicationYear":"1982","noYear":false,"title":"Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho — Emphasis: 1974–1978"},"id":1}],"supersededBy":{"id":988,"text":"wsp2191 - 1982 - Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho — Emphasis: 1974–1978","indexId":"wsp2191","publicationYear":"1982","noYear":false,"title":"Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho — Emphasis: 1974–1978"},"lastModifiedDate":"2022-08-12T19:22:07.181971","indexId":"ofr81526","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":"81-526","title":"Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho, emphasis: 1974-1978","docAbstract":"<p>The Idaho National Engineering Laboratory (INEL) site covers about 890 square miles of the eastern Snake River Plain and overlies the Snake River Plain aquifer. Low concentrations of aqueous chemical and radio-active wastes have been discharged to shallow ponds and to shallow or deep wells on the site since 1952. The regional water table ranges from about 200 feet to more than 1,000 feet below land surface within the INEL boundaries. The gradient of the water table averages about 4 feet per mile to the south-southwest. During the latest period of record, 1974 through 1978, the position of the water table has shown a net decline that ranges from 0.2 foot near the northern boundary of the INEL to more than 10 feet in the central and southern parts of the site. Recharge from surface water has been minimal or non-existent during the latter part of this period.</p><p>A large body of perched ground water has formed in the basalt underlying the waste disposal ponds in the Test Reactor Area. This perched zone contains tritium, chromium-51, cobalt-60, strontium-90, and several nonradioactive ions. Tritium is the only mappable waste constituent in that portion of the Snake River Plain aquifer directly underlying this perched zone.</p><p>Low concentrations of chemical and low-level radioactive wastes enter directly into the Snake River Plain aquifer through the Idaho Chemical Processing Plant (ICPP) disposal well. From 1974 through 1978, this 600-foot well was used to discharge a total of 1,861 million gallons of waste water which contained 1,697 curies of radioactivity, ninety-five percent of which was tritium. Tritium has been discharged to the well since 1953 and has formed the largest waste plume, about 28 square miles in area, in the regional aquifer, and minute concentrations have migrated downgradient a horizontal distance of 7.5 miles.</p><p>Other waste plumes south of the ICPP contain sodium, chloride, nitrate, and the resultant specific conductance. These plumes have similar configurations, flow southward, and the contaminants are in general laterally dispersed in that portion of the aquifer underlying the INEL. Other waste plumes, containing strontium-90 and iodine-129, cover small areas near their points of discharge because strontium-90 is sorbed from solution as it moves through the aquifer and iodine-129 is discharged in very low quantities. Cesium-137 is also discharged through the well but it is strongly sorbed from solution and has never been detected in a sample of ground water at the INEL. Radionuclide plume size and concentrations therein are controlled by aquifer flow conditions, the quantity discharged, radioactive decay, sorption, dilution by dispersion, and perhaps other chemical reactions. Distributions of non-radoactive chemical wastes are subject to the same processes except for radioactive decay.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81526","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Barraclough, J.T., Lewis, B.D., and Jensen, R.G., 1981, Hydrologic conditions at the Idaho National Engineering Laboratory, Idaho, emphasis: 1974-1978: U.S. Geological Survey Open-File Report 81-526, v, 77 p., https://doi.org/10.3133/ofr81526.","productDescription":"v, 77 p.","costCenters":[],"links":[{"id":405122,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0526/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0526/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.09625244140625,\n              43.51370083689698\n            ],\n            [\n              -111.98501586914062,\n              43.51370083689698\n            ],\n            [\n              -111.98501586914062,\n              43.57641143300888\n            ],\n            [\n              -112.09625244140625,\n              43.57641143300888\n            ],\n            [\n              -112.09625244140625,\n              43.51370083689698\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611676","contributors":{"authors":[{"text":"Barraclough, Jack T.","contributorId":8822,"corporation":false,"usgs":true,"family":"Barraclough","given":"Jack","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":178479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Barney D.","contributorId":93873,"corporation":false,"usgs":true,"family":"Lewis","given":"Barney","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":178481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jensen, Rodger G.","contributorId":27420,"corporation":false,"usgs":true,"family":"Jensen","given":"Rodger","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":178480,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10134,"text":"ofr81633 - 1981 - Map showing the potentiometric surface of the Magothy aquifer in southern Maryland, August 1980","interactions":[],"lastModifiedDate":"2022-11-04T17:32:26.739761","indexId":"ofr81633","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":"81-633","title":"Map showing the potentiometric surface of the Magothy aquifer in southern Maryland, August 1980","docAbstract":"<p>This map is based on measurements made in a network of 77 observation wells. Highest levels of the potentiometric surface, 61 to 64 feet above sea level, were near the outcrop or subcrop of the aquifer in topographically high areas of Anne Arundel and northern Prince Georges Counties. The potentiometric surface slopes toward centers of pumpage near Annapolis, in northern Charles County, and southern Prince Georges County. Two separate , distinct, and extensive cones of depression have developed in the surface around the well fields of Waldorf, in northern Charles County, and the Chalk Point power plant, in southern Prince Georges County. The cone of depression in the Annapolis area has coalesced with a more shallow cone that includes the Broadneck Peninsula. The network of wells was developed and is operated and maintained as part of the cooperative program between the U.S. Geological Survey and agencies of the Maryland Department of Natural Resources.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81633","collaboration":"Prepared in cooperation with the Maryland Geological Survey and the Maryland Energy Administration","usgsCitation":"Mack, F., Wheeler, J.C., and Curtin, S.E., 1981, Map showing the potentiometric surface of the Magothy aquifer in southern Maryland, August 1980: U.S. Geological Survey Open-File Report 81-633, 1 Plate: 8.11 x 10.50 inches, https://doi.org/10.3133/ofr81633.","productDescription":"1 Plate: 8.11 x 10.50 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,{"id":10057,"text":"ofr81791 - 1981 - Preliminary geologic report for the Alenaio stream flood damage reduction study area, Hilo, Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr81791","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":"81-791","title":"Preliminary geologic report for the Alenaio stream flood damage reduction study area, Hilo, Hawaii","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81791","usgsCitation":"Lockwood, J.P., and Buchanan-Banks, J.M., 1981, Preliminary geologic report for the Alenaio stream flood damage reduction study area, Hilo, Hawaii: U.S. Geological Survey Open-File Report 81-791, 14 p. ill., map ;28 cm., https://doi.org/10.3133/ofr81791.","productDescription":"14 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":144407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0791/report-thumb.jpg"},{"id":37906,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0791/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0791/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f12","contributors":{"authors":[{"text":"Lockwood, John P. 0000-0002-6562-0222","orcid":"https://orcid.org/0000-0002-6562-0222","contributorId":30976,"corporation":false,"usgs":true,"family":"Lockwood","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":160745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan-Banks, Jane M.","contributorId":29421,"corporation":false,"usgs":true,"family":"Buchanan-Banks","given":"Jane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160744,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9991,"text":"ofr801298 - 1981 - Magnitude and chemical quality of base flow of Otter Creek, Tongue River, and Rosebud Creek, southeastern Montana, October 26-November 5, 1977","interactions":[],"lastModifiedDate":"2024-06-04T21:30:23.997764","indexId":"ofr801298","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":"80-1298","title":"Magnitude and chemical quality of base flow of Otter Creek, Tongue River, and Rosebud Creek, southeastern Montana, October 26-November 5, 1977","docAbstract":"<p>Hydrologic and chemical data were collected during base-flow conditions on three streams in southeastern Montana from October 26 to November 5, 1977, to characterize groundwater discharge. Maximum measured flow of Otter Creek, an interrupted stream, was 1.2 cubic feet per second. The water chemistry was dominated by sodium, magnesium, and sulfate ions, with a maximum dissolved-solids concentration of 3,540 milligrams per liter. Chemistry of groundwater inflow is dominated by sodium, magnesium, and sulfate. A discharge of 156 cubic feet per second from the Tongue River Reservoir into the Tongue River complicated interpretation of groundwater discharge to the reach downstream from the reservoir. Many reaches of gain and loss were observed along the Tongue River; the flow near the mouth was 233 cubic feet per second. Minor changes in quality of the base flow indicate groundwater discharges dominated by sodium, sulfate, and bicarbonate plus carbonate. Dissolved-solids concentration increased from 506 milligrams per liter near the dam to 630 milligrams per liter near the mouth. Maximum measured flow of Rosebud Creek was 19.0 cubic feet per second. Water quality in the upper reaches was dominated by magnesium, calcium , and bicarbonate, with dissolved-solids concentrations ranging from 560 to 703 milligrams per liter. Sodium, sulfate, and dissolved solids increase downstream.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801298","usgsCitation":"Lee, R.W., Slagle, S.E., and Stimson, J.R., 1981, Magnitude and chemical quality of base flow of Otter Creek, Tongue River, and Rosebud Creek, southeastern Montana, October 26-November 5, 1977: U.S. Geological Survey Open-File Report 80-1298, Report: iv, 29 p.; 1 Plate: 19.02 x 18.56 inches, https://doi.org/10.3133/ofr801298.","productDescription":"Report: iv, 29 p.; 1 Plate: 19.02 x 18.56 inches","costCenters":[],"links":[{"id":429509,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11517.htm","linkFileType":{"id":5,"text":"html"}},{"id":37801,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1298/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37802,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1298/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1298/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.25,\n              46.5\n            ],\n            [\n              -107.25,\n              45\n            ],\n            [\n              -105.5,\n              45\n            ],\n            [\n              -105.5,\n              46.5\n            ],\n            [\n              -107.25,\n              46.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494e7","contributors":{"authors":[{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stimson, James R.","contributorId":77152,"corporation":false,"usgs":true,"family":"Stimson","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160630,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11504,"text":"ofr801287 - 1981 - Water resources of Cold Spring Valley, a growing urban area northwest of Reno, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr801287","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":"80-1287","title":"Water resources of Cold Spring Valley, a growing urban area northwest of Reno, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801287","usgsCitation":"Van Denburgh, A.S., and Katzer, T.L., 1981, Water resources of Cold Spring Valley, a growing urban area northwest of Reno, Nevada: U.S. Geological Survey Open-File Report 80-1287, vii, 85 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr801287.","productDescription":"vii, 85 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1287/report-thumb.jpg"},{"id":39369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1287/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0824","contributors":{"authors":[{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":163265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Katzer, T. L.","contributorId":15211,"corporation":false,"usgs":true,"family":"Katzer","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":163264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10151,"text":"ofr81569 - 1981 - Geologic factors pertinent to the proposed A. J. Wiley Hydroelectric Project No. 2845, Bliss, Idaho","interactions":[],"lastModifiedDate":"2013-11-19T13:33:27","indexId":"ofr81569","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":"81-569","title":"Geologic factors pertinent to the proposed A. J. Wiley Hydroelectric Project No. 2845, Bliss, Idaho","docAbstract":"The A.J. Wiley Hydroelectric Project is a proposal by the Idaho Power Company to develop hydroelectricity near Bliss, Idaho, by building a dam on the Snake River (fig. 1). The proposed dam would impound a narrow reservoir as deep as 85 feet in a free-flowing reach of the river that extends from the upper reach of water impounded by the Bliss Dam to the foot of the Lower Salmon Falls Dam, nearly 8 miles farther upstream. The proposed dam would be built in three sections: a spillway section and a powerhouse (intake) section to be constructed of concrete in the right-handed part, and an embankment section to be constructed as a zoned-fill of selected earth materials in the left-hand part. (Right and left are to be understood in the sense of looking downstream.) In August, 1979, the Idaho Power Company was granted a 3-year permit (Project No. 2845) by the Federal Energy Regulatory Commission (FERC) to make site investigations and environmental studies in the project area. A year later, on August 26, 1980, the company applied to FERC for a license to construct the project. On October 8, 1980, as explained in a letter by William W. Lindsay, Director of the Office of Electric Power Regulation, the company was given 90 days to correct certain deficiencies in the application. Because several of the deficiencies identified by Mr. Lindsay pertain to geologic aspects of the project, his letter is attached to this report as Appendix A. Hereafter in this report, the deficiencies listed by Mr. Lindsay are identified by the numerical entries in his letter. The Idaho Power Company is referred to as the applicant.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81569","usgsCitation":"Malde, H.E., 1981, Geologic factors pertinent to the proposed A. J. Wiley Hydroelectric Project No. 2845, Bliss, Idaho: U.S. Geological Survey Open-File Report 81-569, v, 75 p., https://doi.org/10.3133/ofr81569.","productDescription":"v, 75 p.","numberOfPages":"80","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":142591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0569/report-thumb.jpg"},{"id":37993,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","city":"Bliss","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.958664,42.919657 ], [ -114.958664,42.931423 ], [ -114.93494,42.931423 ], [ -114.93494,42.919657 ], [ -114.958664,42.919657 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a61f5","contributors":{"authors":[{"text":"Malde, Harold E.","contributorId":45706,"corporation":false,"usgs":true,"family":"Malde","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10560,"text":"ofr81827 - 1981 - Grain size data compilation and parameters of sediment samples; lower Cook Inlet, Alaska, 1976 through 1979","interactions":[],"lastModifiedDate":"2023-11-24T18:02:00.459383","indexId":"ofr81827","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":"81-827","title":"Grain size data compilation and parameters of sediment samples; lower Cook Inlet, Alaska, 1976 through 1979","docAbstract":"<p>Lower Cook Inlet is the southern part of the large tidal inlet that connects Anchorage with the Pacific Ocean (fig. 1). During the summer field seasons of 1976, 1977, 1978, and 1979, the U.S. Geological Survey under contract with the Bureau of Land Management through the National Oceanic and Atmospheric Administration conducted geo-environmental studies in lower Cook Inlet (note Table 1) (Bouma and Hampton, 1976; Bouma and others, 1978, Hampton and Bouma 1979, 1980).</p><p>The USGS research vessel SEA SOUNDER was used to obtain continuous seismic reflection profiles and to collect seafloor sediment samples. In addition, bottom samples were taken by the University of Alaska during benthic biological studies aboard the R/V MOANA WAVE (April 1976) and the NOAA vessel MILLER FREEMAN (October1976, Feder,1977). Textural analyses were carried out on sediment samples taken at 117 station locations. Sample collection was influenced by the nature of the substrate, texture, equipment malfunction and weather. Figure 2 presents a map with station locations. Station locations and other data are tabulated in Appendix I.</p><p>A modified Van Veen grab sampler, capable of taking an undisturbed surface sample of 40X60X30 cm was used to collect unconsolidated sediment. In addition, a 3-m gravity corer and a 2-m vibracorer were used at selected sites. The top ten centimeters of each sample were used for grain size analysis. Most samples were taken from bedform fields that occupy much of central lower Cook Inlet. Water depths in the lower inlet range from 40 to 170 m, averaging approximately 70 m. Strong tidal currents are present and surface water velocities of 3-5 knots (150-250 cm/sec) are common during flood and ebb tides (Bouma and Hampton, 1978).</p><p>The bottom of central lower Cook Inlet is almost completely covered by sand. Bedrock material can be observed at the seafloor on seismic records in isolated areas. The sand occurs in bedform patterns; textural data are important when determining the relationship between the currents and migrating sand bodies patterns. Immediate and long-term effects of sand movement over and around obstructions placed on the seafloor should be studied to prevent damage or destruction to the sensitive ecosystem of lower Cook Inlet.</p><p>This report presents textural grain-size data that have been gathered for lower Cook Inlet samples, the method of collection, and analytical processes. The data in Appendix 2 can be used to compare calculated parameters in order to properly assess the sedimentary environment of lower Cook Inlet.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81827","usgsCitation":"Orlando, R.C., and Martin, A., 1981, Grain size data compilation and parameters of sediment samples; lower Cook Inlet, Alaska, 1976 through 1979: U.S. Geological Survey Open-File Report 81-827, 11 p., https://doi.org/10.3133/ofr81827.","productDescription":"11 p.","costCenters":[],"links":[{"id":422891,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0827/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142411,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0827/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"lower Cook Inlet","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -153.007354534289,\n              60.206774150854926\n            ],\n            [\n              -153.007354534289,\n              58.78930420832526\n            ],\n            [\n              -151.59863723061684,\n              58.78930420832526\n            ],\n            [\n              -151.59863723061684,\n              60.206774150854926\n            ],\n            [\n              -153.007354534289,\n              60.206774150854926\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672cfb","contributors":{"authors":[{"text":"Orlando, Robert C.","contributorId":86220,"corporation":false,"usgs":true,"family":"Orlando","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":161592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Ann","contributorId":96529,"corporation":false,"usgs":true,"family":"Martin","given":"Ann","email":"","affiliations":[],"preferred":false,"id":161593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11222,"text":"ofr811279 - 1981 - Permit requirements for energy and other natural resource for the State of South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:36","indexId":"ofr811279","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":"81-1279","title":"Permit requirements for energy and other natural resource for the State of South Dakota","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811279","usgsCitation":"Smith, J., 1981, Permit requirements for energy and other natural resource for the State of South Dakota: U.S. Geological Survey Open-File Report 81-1279, 66 p. :map ;28 cm., https://doi.org/10.3133/ofr811279.","productDescription":"66 p. :map ;28 cm.","costCenters":[],"links":[{"id":144551,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1279/report-thumb.jpg"},{"id":39012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1279/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688570","contributors":{"authors":[{"text":"Smith, J.K.","contributorId":39383,"corporation":false,"usgs":true,"family":"Smith","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":162760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11471,"text":"ofr81832 - 1981 - Geologic mapping of the Vista and Steamboat 7.5-minute quadrangles, Nevada","interactions":[],"lastModifiedDate":"2022-11-02T21:35:10.487269","indexId":"ofr81832","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":"81-832","title":"Geologic mapping of the Vista and Steamboat 7.5-minute quadrangles, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81832","usgsCitation":"Trexler, D.T., and Pease, R., 1981, Geologic mapping of the Vista and Steamboat 7.5-minute quadrangles, Nevada: U.S. Geological Survey Open-File Report 81-832, Report: 32 p.; 5 Plates: 28.47 × 26.46 inches or smaller, https://doi.org/10.3133/ofr81832.","productDescription":"Report: 32 p.; 5 Plates: 28.47 × 26.46 inches or smaller","costCenters":[],"links":[{"id":39339,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0832/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39342,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0832/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39341,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0832/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39340,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0832/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409090,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75547.htm","linkFileType":{"id":5,"text":"html"}},{"id":39338,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0832/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0832/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0832/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Vista and Steamboat quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.75,\n              39.625\n            ],\n            [\n              -119.75,\n              39.375\n            ],\n            [\n              -119.625,\n              39.375\n            ],\n            [\n              -119.625,\n              39.625\n            ],\n            [\n              -119.75,\n              39.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68864b","contributors":{"authors":[{"text":"Trexler, Dennis T.","contributorId":61828,"corporation":false,"usgs":true,"family":"Trexler","given":"Dennis","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":163192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pease, Robert C.","contributorId":25574,"corporation":false,"usgs":true,"family":"Pease","given":"Robert C.","affiliations":[],"preferred":false,"id":163191,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57476,"text":"wdrND801 - 1981 - Water resources data for North Dakota, water year 1980","interactions":[],"lastModifiedDate":"2024-07-12T19:35:35.159824","indexId":"wdrND801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-80-1","title":"Water resources data for North Dakota, water year 1980","docAbstract":"<p>Water resources data for the 1980 water year for North Dakota consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report contains discharge records for 144 gaging stations; stage only records for 22 gaging stations; stage and contents for 13 lakes and reservoirs; water quality for 87 gaging stations, 33 partial-record stations, 39 lakes, 80 wells, and water levels for 32 observation wells. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in North Dakota.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrND801","collaboration":"Prepared in cooperation with the State of North Dakota and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1981, Water resources data for North Dakota, water year 1980: U.S. Geological Survey Water Data Report ND-80-1, xii, 803 p., https://doi.org/10.3133/wdrND801.","productDescription":"xii, 803 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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