{"pageNumber":"4672","pageRowStart":"116775","pageSize":"25","recordCount":165549,"records":[{"id":9164,"text":"ofr8327 - 1983 - Ground-water records for the area surrounding the Chickasaw National Recreation Area, Murray County, Oklahoma","interactions":[],"lastModifiedDate":"2019-11-01T11:13:57","indexId":"ofr8327","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-27","title":"Ground-water records for the area surrounding the Chickasaw National Recreation Area, Murray County, Oklahoma","docAbstract":"This report is a compilation of ground-water records, water levels, and water-quality field determinations, for wells in a 132 square-mile (342 square kilometer) area surrounding the Chickasaw National Recreational Area in south-central Oklahoma. This information was collected in cooperation with the National Park Service. The location of the study area is shown on figure 1; the well locations are shown on figure 2. Data from 101 wells are summarized in this report.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8327","usgsCitation":"Goemaat, R.L., and Willard, C.C., 1983, Ground-water records for the area surrounding the Chickasaw National Recreation Area, Murray County, Oklahoma: U.S. Geological Survey Open-File Report 83-27, 21 p. , https://doi.org/10.3133/ofr8327.","productDescription":"21 p. ","costCenters":[],"links":[{"id":368877,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0027/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","county":"Murray County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.832,34.5082],[-96.8342,34.5082],[-96.8833,34.5087],[-96.8826,34.4337],[-96.8808,34.3336],[-96.9359,34.3337],[-97.03,34.3349],[-97.036,34.3396],[-97.0415,34.3415],[-97.0437,34.3433],[-97.0436,34.3456],[-97.0419,34.3478],[-97.0363,34.3496],[-97.0356,34.3527],[-97.0393,34.3632],[-97.0394,34.3787],[-97.3529,34.3786],[-97.3512,34.5098],[-97.2497,34.5097],[-97.1449,34.5076],[-97.147,34.5131],[-97.153,34.5196],[-97.1479,34.5227],[-97.1512,34.5259],[-97.1585,34.5242],[-97.1611,34.5306],[-97.1655,34.5325],[-97.1655,34.5357],[-97.1604,34.5365],[-97.1637,34.5407],[-97.1603,34.5429],[-97.1657,34.5484],[-97.1605,34.5551],[-97.1643,34.5602],[-97.1553,34.5646],[-97.1563,34.5683],[-97.1698,34.5658],[-97.1753,34.5667],[-97.1758,34.5713],[-97.1729,34.5758],[-97.1667,34.5784],[-97.1749,34.5835],[-97.1691,34.5944],[-97.1707,34.5985],[-97.1752,34.5967],[-97.1818,34.5973],[-97.188,34.5974],[-97.193,34.5997],[-97.1961,34.6111],[-97.202,34.6199],[-97.2013,34.6235],[-97.1438,34.6235],[-97.144,34.6385],[-97.1049,34.6388],[-96.9345,34.6391],[-96.9346,34.5927],[-96.8313,34.5927],[-96.832,34.5082]]]},\"properties\":{\"name\":\"Murray\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667023","contributors":{"authors":[{"text":"Goemaat, Robert L.","contributorId":64256,"corporation":false,"usgs":true,"family":"Goemaat","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willard, Cass C.","contributorId":81908,"corporation":false,"usgs":true,"family":"Willard","given":"Cass","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8562,"text":"ofr821014 - 1983 - Hydrology of area 38, Western Region, Interior Coal Province, Iowa and Missouri","interactions":[],"lastModifiedDate":"2016-03-04T14:35:23","indexId":"ofr821014","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1014","title":"Hydrology of area 38, Western Region, Interior Coal Province, Iowa and Missouri","docAbstract":"<p>A nationwide need for information characterizing hydrologic conditions in mined and potential mine areas has become paramount with the enactment of the Surface Mining Control and Reclamation Act of 1977. This report is designed to be useful to the mine owners, operators, and others by presenting information about the existing hydrologic conditions and by identifying sources of hydrologic information. General hydrologic information is presented using a brief text with an accompanying map, chart, graph, or other illustration for each of a series of water-resources-related topics. The summation of the topical discussions provides a description of the hydrology of the area.</p>\n<p>Coal has been mined for 130 years in Area 38, but large reserves remain. Production peaked in 1917 when Iowa produced 9 million tons and Missouri produced 6 million tons. Underground mining has been replaced by surface mining in Area 38. Not all past surface-mined lands are subject to reclamation under recently enacted reclamation laws.</p>\n<p>The surface-water monitoring network in Area 38 consists of 183 stations. Streamflow varies seasonally and from year to year. Water-quality data are available for 49 stations in the study area. Measurements of specific conductance, dissolved solids, pH, alkalinity, sulfate, iron, manganese, trace metals and other constituents are available for 36 stations operated between 1978 and 1981 expressly for the collection of water-quality data within basins containing coal mines.</p>\n<p>A cumulative impact of coal mining on the mineralization of surface water is evident from specific-conductance data for stations downstream from mining activities. Alkalinity in streams in Area 38 averaged greater than 118 milligrams per liter, providing the capability to neutralize acid-mine drainage to some extent. Sulfate concentrations in streamflow averaged 88 milligrams per liter at stations upstream from coal mines and 269 milligrams per liter at stations downstream from coal mines. Significant relationships exist between totalrecoverable-iron concentrations and suspendedsediment concentrations. Manganese concentrations are larger in streams draining mined areas. Streamflow at 5 of the 36 coal-hydrology stations in Area 38, all located downstream from coal mines, exceeded acid-mine-drainage criteria at one time or another.</p>\n<p>In Area 38 dissolved-solids concentrations in water from the Cambrian-Ordovician aquifer range from 300 to 15,000 milligrams per liter; in southcentral Iowa and where the aquifer underlies the Missouri River alluvium, as in Boone County, Missouri, dissolved-solids concentrations are less than 1,000 milligrams per liter. In these areas the Cambrian-Ordovician aquifer is suitable for domestic and other uses. Chemical quality of water from Quaternary aquifers generally is suitable for domestic uses and other uses, dissolved-solids concentrations averaged less than 1,000 milligrams per liter. Iron, manganese and nitrate are excessive in some instances. Chemical quality of water from Mississippian and Pennsylvanian aquifers is unsuitable for domestic use and may be unsuitable for other uses. The Pennsylvanian and Misissippian aquifers have average sulfate concentrations in excess of 1,000 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr821014","usgsCitation":"Detroy, M., and Skelton, J., 1983, Hydrology of area 38, Western Region, Interior Coal Province, Iowa and Missouri: U.S. Geological Survey Open-File Report 82-1014, v, 105 p.: ill., maps (some col.); 28 cm., https://doi.org/10.3133/ofr821014.","productDescription":"v, 105 p.: ill., maps (some col.); 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":9609,"text":"ofr83753 - 1983 - Ground-water data for Michigan 1982","interactions":[],"lastModifiedDate":"2016-12-29T10:58:52","indexId":"ofr83753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-753","title":"Ground-water data for Michigan 1982","docAbstract":"<p>Water levels, locations, depths, and aquifers tapped are given for 117 observation wells. Tabulated data include extremes of water levels for 1982 and for the period of record, pumpage of most major ground-water users in the State, and quality data on selected wells. The largest reported user of ground-water, the city of Lansing, pumped 8.2 billion gallons from the Saginaw Formation and glacial deposits.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr83753","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Huffman, G., 1983, Ground-water data for Michigan 1982: U.S. Geological Survey Open-File Report 83-753, iv, 54 p., https://doi.org/10.3133/ofr83753.","productDescription":"iv, 54 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0753/report-thumb.jpg"},{"id":37339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0753/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":9607,"text":"ofr83713 - 1983 - RDARL4, a Fortran interface for transferring chemical analytical data from an Applied Research Laboratories electron microprobe to a PDP-11 computing system","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr83713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-713","title":"RDARL4, a Fortran interface for transferring chemical analytical data from an Applied Research Laboratories electron microprobe to a PDP-11 computing system","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83713","usgsCitation":"Huebner, J., 1983, RDARL4, a Fortran interface for transferring chemical analytical data from an Applied Research Laboratories electron microprobe to a PDP-11 computing system: U.S. Geological Survey Open-File Report 83-713, 40 p.  ;28 cm., https://doi.org/10.3133/ofr83713.","productDescription":"40 p.  ;28 cm.","costCenters":[],"links":[{"id":141714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0713/report-thumb.jpg"},{"id":37338,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fc7","contributors":{"authors":[{"text":"Huebner, J.S.","contributorId":41422,"corporation":false,"usgs":true,"family":"Huebner","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":159990,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8634,"text":"ofr83459 - 1983 - Sedimentology of the lower part of the upper Triassic Chinle Formation and its relationship to uranium deposits, White Canyon area, southeastern Utah","interactions":[],"lastModifiedDate":"2022-10-27T19:14:24.617058","indexId":"ofr83459","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-459","title":"Sedimentology of the lower part of the upper Triassic Chinle Formation and its relationship to uranium deposits, White Canyon area, southeastern Utah","docAbstract":"Closely spaced measured stratigraphic sections of the lower part of the Late Triassic Chinle Formation in the White Canyon area of southeastern Utah depict a fluvial-deltaic-lacustrine depositional sequence that hosts uranium deposits in basal fluvial sandstones. The basal Shinarump Member consists of predominantly trough-crossbedded, coarse-grained sandstone and minor gray, carbonaceous mudstone and is interpreted as a valley-fill sequence overlain by deposits of a braided stream system. The overlying Monitor Butte Member is composed of cyclic- and foreset-bedded siltstone, sandstone, and mudstone and is interpreted as a succession of low-energy fluvial, deltaic and orqanicrich, lacustrine-marsh sediments. The overlying Moss Back Member is composed of a laterally extensive, coarse- to medium-grained, conglomeratic sandstone and is interpreted as a braided-stream system that flowed north to northwest. The entire sequence was deposited in response to changes in local base level associated with a large lake that lay to the west. \r\n\r\nIsopachs of lithofacies indicate distinct lacustrine basins and a correspondence between these facies and modern structural synclines. Facies changes and coincidence of isopach thicks suggest that structural synclines were active in the Late Triassic and influenced the pattern of sediment distribution within the basins. Uranium mineralization appears to be related to certain low-energy depositional environments in that uranium is localized in fluvial sandstones that lie beneath organic-rich lacustrine-marsh mudstones and carbonaceous delta-front sediments. The reducing environment preserved in these facies may have played an important role in the localization of uranium.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83459","usgsCitation":"Dubiel, R.F., 1983, Sedimentology of the lower part of the upper Triassic Chinle Formation and its relationship to uranium deposits, White Canyon area, southeastern Utah: U.S. Geological Survey Open-File Report 83-459, ii, 48 p., https://doi.org/10.3133/ofr83459.","productDescription":"ii, 48 p.","costCenters":[],"links":[{"id":408817,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14047.htm","linkFileType":{"id":5,"text":"html"}},{"id":36240,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0459/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0459/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"White Canyon area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110,\n              38.344\n            ],\n            [\n              -110.5,\n              38.344\n            ],\n            [\n              -110.5,\n              37.5\n            ],\n            [\n              -110,\n              37.5\n            ],\n            [\n              -110,\n              38.344\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbb64","contributors":{"authors":[{"text":"Dubiel, Russell F. 0000-0002-1280-0350 rdubiel@usgs.gov","orcid":"https://orcid.org/0000-0002-1280-0350","contributorId":1294,"corporation":false,"usgs":true,"family":"Dubiel","given":"Russell","email":"rdubiel@usgs.gov","middleInitial":"F.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":158064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9599,"text":"ofr83489 - 1983 - Mineral resource potential of the Granite Peak Roadless Area, Trinity County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr83489","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-489","title":"Mineral resource potential of the Granite Peak Roadless Area, Trinity County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83489","usgsCitation":"Huber, D., and Nelson, S., 1983, Mineral resource potential of the Granite Peak Roadless Area, Trinity County, California: U.S. Geological Survey Open-File Report 83-489, 10 p. :maps ;28 cm., https://doi.org/10.3133/ofr83489.","productDescription":"10 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0489/report-thumb.jpg"},{"id":37330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d566","contributors":{"authors":[{"text":"Huber, D.F.","contributorId":93905,"corporation":false,"usgs":true,"family":"Huber","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":159979,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, S.C.","contributorId":30625,"corporation":false,"usgs":true,"family":"Nelson","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":159978,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9592,"text":"ofr83795 - 1983 - Geology and mineral resource potential of the Palisade Wilderness Study Area, Mesa County, Colorado (GEM phase 2)","interactions":[],"lastModifiedDate":"2022-09-01T18:11:26.851335","indexId":"ofr83795","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-795","title":"Geology and mineral resource potential of the Palisade Wilderness Study Area, Mesa County, Colorado (GEM phase 2)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83795","usgsCitation":"Hovorka, D.S., Patterson, C., and Toth, M.I., 1983, Geology and mineral resource potential of the Palisade Wilderness Study Area, Mesa County, Colorado (GEM phase 2): U.S. Geological Survey Open-File Report 83-795, Report: iii, 24 p.; 2 Plates: 40.71 × 32.06 inches and 23.42 × 20.58 inches, https://doi.org/10.3133/ofr83795.","productDescription":"Report: iii, 24 p.; 2 Plates: 40.71 × 32.06 inches and 23.42 × 20.58 inches","costCenters":[],"links":[{"id":108476,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14222.htm","linkFileType":{"id":5,"text":"html"},"description":"14222"},{"id":37322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0795/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37321,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0795/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37320,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0795/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0795/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Mesa County","otherGeospatial":"Palisade Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.042,\n              38.675\n            ],\n            [\n              -108.8,\n              38.675\n            ],\n            [\n              -108.8,\n              38.824\n            ],\n            [\n              -109.042,\n              38.824\n            ],\n            [\n              -109.042,\n              38.675\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46f8","contributors":{"authors":[{"text":"Hovorka, D. S.","contributorId":60210,"corporation":false,"usgs":true,"family":"Hovorka","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, C. G.","contributorId":87132,"corporation":false,"usgs":true,"family":"Patterson","given":"C. G.","affiliations":[],"preferred":false,"id":159968,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Toth, M. I.","contributorId":82695,"corporation":false,"usgs":true,"family":"Toth","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":159967,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9591,"text":"ofr83245 - 1983 - Analytical data on the Meade Peak Phosphatic Shale Member of the Phosphoria Formation in the central Wooley Range, southeastern Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr83245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-245","title":"Analytical data on the Meade Peak Phosphatic Shale Member of the Phosphoria Formation in the central Wooley Range, southeastern Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83245","usgsCitation":"Hovland, R.D., 1983, Analytical data on the Meade Peak Phosphatic Shale Member of the Phosphoria Formation in the central Wooley Range, southeastern Idaho: U.S. Geological Survey Open-File Report 83-245, 31 p. maps ;28 cm., https://doi.org/10.3133/ofr83245.","productDescription":"31 p. maps ;28 cm.","costCenters":[],"links":[{"id":142118,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0245/report-thumb.jpg"},{"id":37319,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0245/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f9d4","contributors":{"authors":[{"text":"Hovland, R. David","contributorId":96687,"corporation":false,"usgs":true,"family":"Hovland","given":"R.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":159965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9589,"text":"ofr83468 - 1983 - Mineral resource potential of the Sheep Mountain Wilderness, Albany County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr83468","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-468","title":"Mineral resource potential of the Sheep Mountain Wilderness, Albany County, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83468","usgsCitation":"Houston, R.S., Patten, L.L., and Gersic, J., 1983, Mineral resource potential of the Sheep Mountain Wilderness, Albany County, Wyoming: U.S. Geological Survey Open-File Report 83-468, 21 p. :maps ;28 cm., https://doi.org/10.3133/ofr83468.","productDescription":"21 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0468/report-thumb.jpg"},{"id":37315,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0468/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69bf5e","contributors":{"authors":[{"text":"Houston, R. S.","contributorId":93897,"corporation":false,"usgs":true,"family":"Houston","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":159959,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patten, L. L.","contributorId":72374,"corporation":false,"usgs":true,"family":"Patten","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159957,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gersic, Joseph","contributorId":85966,"corporation":false,"usgs":true,"family":"Gersic","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":159958,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8965,"text":"ofr83517 - 1983 - Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83517","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-517","title":"Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83517","usgsCitation":"Gardner, J.V., and Klise, D.H., 1983, Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California: U.S. Geological Survey Open-File Report 83-517, 35 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83517.","productDescription":"35 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0517/report-thumb.jpg"},{"id":36585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0517/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e88","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":158636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klise, David H.","contributorId":13977,"corporation":false,"usgs":true,"family":"Klise","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":158635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8440,"text":"ofr8354 - 1983 - Statistical tables, sample locality maps, and an explanation of data sets for samples from the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli Counties, Montana","interactions":[],"lastModifiedDate":"2022-09-22T19:00:22.418716","indexId":"ofr8354","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-54","title":"Statistical tables, sample locality maps, and an explanation of data sets for samples from the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli Counties, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8354","usgsCitation":"Coxe, B.W., and Toth, M.I., 1983, Statistical tables, sample locality maps, and an explanation of data sets for samples from the Selway-Bitterroot Wilderness, Idaho County, Idaho, and Missoula and Ravalli Counties, Montana: U.S. Geological Survey Open-File Report 83-54, Report: 94 p.; 2 Plates: 38.00 × 42.00 inches and 38.00 × 41.00 inches, https://doi.org/10.3133/ofr8354.","productDescription":"Report: 94 p.; 2 Plates: 38.00 × 42.00 inches and 38.00 × 41.00 inches","costCenters":[],"links":[{"id":20775,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0054/plate-1-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407234,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14094.htm","linkFileType":{"id":5,"text":"html"}},{"id":20777,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0054/plate-2-preview.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20776,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0054/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36004,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0054/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0054/report-thumb.jpg"},{"id":20774,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0054/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Montana","county":"Idaho County, Missoula County, Ravalli County","otherGeospatial":"Selway-Bitterroot Wilderness","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.437,\n              45.667\n            ],\n            [\n              -114.166,\n              45.667\n            ],\n            [\n              -114.166,\n              46.692\n            ],\n            [\n              -115.437,\n              46.692\n            ],\n            [\n              -115.437,\n              45.667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e12f1","contributors":{"authors":[{"text":"Coxe, Berton W.","contributorId":44918,"corporation":false,"usgs":true,"family":"Coxe","given":"Berton","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toth, Margo I.","contributorId":18365,"corporation":false,"usgs":true,"family":"Toth","given":"Margo","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":157718,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9159,"text":"ofr83760 - 1983 - Ground-water levels in observation wells in Oklahoma, 1980-82","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-760","title":"Ground-water levels in observation wells in Oklahoma, 1980-82","docAbstract":"In the 1980-82 Climatic Years, the U. S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, collected ground-water level data in Oklahoma from 1,122 sites in 77 counties. This report presents this data.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83760","usgsCitation":"Goemaat, R.L., Mize, L.D., and Spiser, D.E., 1983, Ground-water levels in observation wells in Oklahoma, 1980-82: U.S. Geological Survey Open-File Report 83-760, viii, 612 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83760.","productDescription":"viii, 612 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0760/report-thumb.jpg"},{"id":36786,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66762b","contributors":{"authors":[{"text":"Goemaat, Robert L.","contributorId":64256,"corporation":false,"usgs":true,"family":"Goemaat","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mize, Lionel D.","contributorId":20326,"corporation":false,"usgs":true,"family":"Mize","given":"Lionel","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":159199,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spiser, Dannie E.","contributorId":42214,"corporation":false,"usgs":true,"family":"Spiser","given":"Dannie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159200,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8617,"text":"ofr83425 - 1983 - Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-425","title":"Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards","docAbstract":"An 1800-joule sparker survey of the West Florida continental slope between about 26?N and 29?15?N showed a top bed of Pleistocene age forming an irregular drape over a surface that is probably Pliocene. The contact between the top two layers is unconformable in the south and, in some places, shows karst collapse and solution features. Karst topography grades into a more hummocky erosional surface to the north, which in turn smoothes out; the contact become conformable still further north. A period of folding, which is widespread over the outer portion of the study area and which may be related to large scale mass wasting, occurred at about the same time represented by the unconformity. Significant subsidence has occurred as late as Pleistocene. \r\n\r\nThe surface layer thins to a minimum (0 in the south) at about 525-meters water depth and then thickens again dramatically to the west, downslope. This thinning is interpreted to be due to the Loop Current, which flows from north to south in the area and which acts to block deposition and scour the bottom. \r\n\r\nDespite the fact that the margin is dominated by carbonates, usually associated with low sedimentation rates, there is widespread evidence of mass wasting affecting ancient and surficial deposits on the outer part of the upper slope. \r\n\r\nThree potential groups of geohazards identified are: \r\n\r\n1. Potential bottom failure in areas where a thin top layer overlies the karst surface. \r\n2. Potential for sliding and slumping. \r\n3. Scour due to currents which could also affect drilling and engineering activities.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83425","usgsCitation":"Doyle, L.J., 1983, Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards: U.S. Geological Survey Open-File Report 83-425, 21 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83425.","productDescription":"21 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0425/report-thumb.jpg"},{"id":36208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0425/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f40a9","contributors":{"authors":[{"text":"Doyle, Larry J.","contributorId":43352,"corporation":false,"usgs":true,"family":"Doyle","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8745,"text":"ofr83128 - 1983 - Appraisal of data for ground-water quality in Nebraska","interactions":[{"subject":{"id":8745,"text":"ofr83128 - 1983 - Appraisal of data for ground-water quality in Nebraska","indexId":"ofr83128","publicationYear":"1983","noYear":false,"title":"Appraisal of data for ground-water quality in Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":1321,"text":"wsp2245 - 1984 - Appraisal of data for ground-water quality in Nebraska","indexId":"wsp2245","publicationYear":"1984","noYear":false,"title":"Appraisal of data for ground-water quality in Nebraska"},"id":1}],"supersededBy":{"id":1321,"text":"wsp2245 - 1984 - Appraisal of data for ground-water quality in Nebraska","indexId":"wsp2245","publicationYear":"1984","noYear":false,"title":"Appraisal of data for ground-water quality in Nebraska"},"lastModifiedDate":"2020-07-28T15:49:56.130277","indexId":"ofr83128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-128","title":"Appraisal of data for ground-water quality in Nebraska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83128","usgsCitation":"Engberg, R., 1983, Appraisal of data for ground-water quality in Nebraska: U.S. Geological Survey Open-File Report 83-128, vi, 99 p., https://doi.org/10.3133/ofr83128.","productDescription":"vi, 99 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,{"id":9158,"text":"ofr83345 - 1983 - MAGPOLY; a modification of a three-dimensional magnetic modelling program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-345","title":"MAGPOLY; a modification of a three-dimensional magnetic modelling program","docAbstract":"The three-dimensional magnetic modelling program of Donald Plouff (Plouff, 1975) has been made operational on a Honeywell Multics 68/80 computer. Modifications were made to input and output procedures to make the program compatible with U.S. Geological Survey (USGS) standard geophysical input and output formats.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83345","usgsCitation":"Godson, R.H., 1983, MAGPOLY; a modification of a three-dimensional magnetic modelling program: U.S. Geological Survey Open-File Report 83-345, 64 p. ill. ;28 cm., https://doi.org/10.3133/ofr83345.","productDescription":"64 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142648,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0345/report-thumb.jpg"},{"id":36785,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0345/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648b51","contributors":{"authors":[{"text":"Godson, Richard H.","contributorId":11190,"corporation":false,"usgs":true,"family":"Godson","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9157,"text":"ofr83346 - 1983 - GRAVPOLY; a modification of a three-dimensional gravity modeling program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-346","title":"GRAVPOLY; a modification of a three-dimensional gravity modeling program","docAbstract":"The three-dimensional magnetic modelling program of Donald Plouff (Plouff, 1975) has been made operational on a Honeywell Multics 68/80 computer. Modifications were made to input and output procedures to make the program compatible with U.S. Geological Survey (USGS) standard geophysical input and output formats.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83346","usgsCitation":"Godson, R.H., 1983, GRAVPOLY; a modification of a three-dimensional gravity modeling program: U.S. Geological Survey Open-File Report 83-346, 55 p. ill. ;28 cm., https://doi.org/10.3133/ofr83346.","productDescription":"55 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0346/report-thumb.jpg"},{"id":36784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4889e4b07f02db51b822","contributors":{"authors":[{"text":"Godson, Richard H.","contributorId":11190,"corporation":false,"usgs":true,"family":"Godson","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8960,"text":"ofr83267 - 1983 - Cane Creek flood-flow characteristics at State Route 30 near Spencer, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-267","title":"Cane Creek flood-flow characteristics at State Route 30 near Spencer, Tennessee","docAbstract":"The Tennessee Department of Transportation has constructed a new bridge and approaches on State Route 30 over Cane Creek near Spencer, Tennessee. The old bridge and its approaches were fairly low, permitting considerable flow over the road during high floods. The new bridge and its approaches are considerably higher, causing different flow conditions at the site. Analysis of the effects of the new bridge, as compared to the old bridge, on floods of the magnitude of the May 27, 1973, flood is presented. The May 27, 1973, flood was greater than a 100-year flood. Analysis of the 50- and 100-year floods for the new bridge are also presented. Results of the study indicate that the new construction will increase the water-surface elevation for a flood equal to the May 27, 1973, flood by approximately 1 foot upstream from bridge. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83267","usgsCitation":"Gamble, C.R., 1983, Cane Creek flood-flow characteristics at State Route 30 near Spencer, Tennessee: U.S. Geological Survey Open-File Report 83-267, 15 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83267.","productDescription":"15 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0267/report-thumb.jpg"},{"id":36582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0267/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0267/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6cda","contributors":{"authors":[{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":158627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8629,"text":"ofr83370 - 1983 - Mineral potential of selected felsic plutons in the eastern and southeastern Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-22T17:28:11","indexId":"ofr83370","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-370","title":"Mineral potential of selected felsic plutons in the eastern and southeastern Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"<p>Sixteen well-defined geochemical anomalies associated with felsic plutons and (or) muscovite-bearing plutons of Proterozoic age have been identified in the eastern and southeastern Arabian Shield. The majority of these plutons are highly evolved, granitophile-element-enriched muscovite-bearing granites that are weakly peraluminous.</p>\n<p>A followup study of the mineral potential of these plutons included detailed geologic mapping, extensive geochemical sampling, ground traverses, and petrographic and petrologic studies. A total of 212 samples were collected for geochemical analysis, and a lesser number were collected for petrographic studies.</p>\n<p>Most of the plutons studied are similar to metallogenically specialized granites described elsewhere in the world and found associated with deposits of tin, tungsten, or molybdenum and other rare metals. Only four of the plutons, the Sitarah, Tarban, and Gaharra monzogranites and the Bwana granite, contained highly anomalous amounts of tin, tungsten, or molybdenum and altered zones- and (or) numerous quartz veins and otherwise appeared to have noteworthy mineral potential. Additional work on at least these four plutons is suggested.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83370","usgsCitation":"du Bray, E.A., 1983, Mineral potential of selected felsic plutons in the eastern and southeastern Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-370, 60 p., https://doi.org/10.3133/ofr83370.","productDescription":"60 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":36232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0370/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0370/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              43,\n              18\n            ],\n            [\n              43,\n              24.5\n            ],\n            [\n             45,\n              24.5\n            ],\n            [\n             45,\n             18\n            ],\n            [\n              43,\n             18\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635635","contributors":{"authors":[{"text":"du Bray, Edward A. 0000-0002-4383-8394 edubray@usgs.gov","orcid":"https://orcid.org/0000-0002-4383-8394","contributorId":755,"corporation":false,"usgs":true,"family":"du Bray","given":"Edward","email":"edubray@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":158055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9150,"text":"ofr83142 - 1983 - Hydrologic data for Point MacKenzie area, south-central Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr83142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-142","title":"Hydrologic data for Point MacKenzie area, south-central Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83142","usgsCitation":"Glass, R.L., 1983, Hydrologic data for Point MacKenzie area, south-central Alaska: U.S. Geological Survey Open-File Report 83-142, 47 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83142.","productDescription":"47 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0142/report-thumb.jpg"},{"id":36781,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ec52","contributors":{"authors":[{"text":"Glass, R. L.","contributorId":80279,"corporation":false,"usgs":true,"family":"Glass","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":159186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8449,"text":"ofr83550 - 1983 - Nonparametric tests for trends in water-quality data using the statistical analysis system","interactions":[],"lastModifiedDate":"2016-06-01T15:43:25","indexId":"ofr83550","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-550","title":"Nonparametric tests for trends in water-quality data using the statistical analysis system","docAbstract":"<p>Two nonparametric procedures to test for trends in water-quality data (SEASKEN AND SEASRS) have been developed for the Statistical Analysis System* (SAS). The procedure SEASKEN tests for a monotonic trend in time by a modified form of Kendall's tau, the Seasonal Kendall test. The procedure SEASRS tests for a step trend between two different periods in a time series using a modified form of the Wilcoxon (Mann-Whitney) rank sum test, the Mann-WhitneyWilcoxon rank sum test for seasonal data. Examples are presented using the two procedures. The source code and user's guide for each of the two procedures are also presented.</p>\n<p>Procedures for flow adjusting water-quality data by the SAS procedures REG and SYSREG and techniques for plotting water-quality data as a time series by the SAS procedure PLOT are presented.</p>\n<p>Additionally, examples are presented to demonstrate the use of the U.S. Geological Survey procedures QWRETR, DVRETR, QWSAS, and DVINPUT to retrieve data from the Geological Survey WATSTORE system and make it available to SAS.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83550","usgsCitation":"Crawford, C.G., Slack, J.R., and Hirsch, R.M., 1983, Nonparametric tests for trends in water-quality data using the statistical analysis system: U.S. Geological Survey Open-File Report 83-550, iv, 102 p., https://doi.org/10.3133/ofr83550.","productDescription":"iv, 102 p.","numberOfPages":"106","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":140525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0550/report-thumb.jpg"},{"id":36022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0550/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684672","contributors":{"authors":[{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":157734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, James R.","contributorId":43778,"corporation":false,"usgs":true,"family":"Slack","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":157735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9577,"text":"ofr83179 - 1983 - Estimation of earthquake effects associated with a great earthquake in the New Madrid seismic zone","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr83179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-179","title":"Estimation of earthquake effects associated with a great earthquake in the New Madrid seismic zone","docAbstract":"Estimates have been made of the effects of a large Ms = 8.6, Io = XI earthquake hypothesed to occur anywhere in the New Madrid seismic zone. The estimates are based on the distributions of intensities associated with the earthquakes of 1811-12, 1843 and 1895 although the effects of other historical shocks are also considered. The resulting composite type intensity map for a maximum intensity XI is believed to represent the upper level of shaking likely to occur. Specific intensity maps have been developed for six cities near the epicentral region taking into account the most likely distribution of site response in each city. Intensities found are: IX for Carbondale, IL; VIII and IX for Evansville, IN; VI and VIII for Little Rock, AR; IX and X for Memphis, TN; VIII, IX, and X for Paducah, KY; and VIII and X for Poplar Bluff, MO. On a regional scale, intensities are found to attenuate from the New Madrid seismic zone most rapidly to the west and southwest sides of the zone, most slowly to the northwest along the Mississippi River, on the northeast along the Ohio River, and on the southeast toward Georgia and South Carolina. Intensities attenuate toward the north, east, and south in a more normal fashion. Known liquefaction effects are documented but much more research is needed to define the liquefaction potential.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83179","usgsCitation":"Hopper, M.G., Algermissen, S.T., and Dobrovolny, E.E., 1983, Estimation of earthquake effects associated with a great earthquake in the New Madrid seismic zone: U.S. Geological Survey Open-File Report 83-179, 101 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83179.","productDescription":"101 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0179/report-thumb.jpg"},{"id":37302,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0179/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb8ec","contributors":{"authors":[{"text":"Hopper, Margaret G. hopper@usgs.gov","contributorId":2227,"corporation":false,"usgs":true,"family":"Hopper","given":"Margaret","email":"hopper@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":159938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":159940,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dobrovolny, Ernest E.","contributorId":71980,"corporation":false,"usgs":true,"family":"Dobrovolny","given":"Ernest","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159939,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9148,"text":"ofr83478 - 1983 - Bibliography of reports by U.S. Geological Survey personnel on studies of underground nuclear test sites and on waste management studies at the Nevada Test Site and the Waste Isolation Pilot Plant site, New Mexico, January 1 to December 31, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83478","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-478","title":"Bibliography of reports by U.S. Geological Survey personnel on studies of underground nuclear test sites and on waste management studies at the Nevada Test Site and the Waste Isolation Pilot Plant site, New Mexico, January 1 to December 31, 1981","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83478","usgsCitation":"Glanzman, V., 1983, Bibliography of reports by U.S. Geological Survey personnel on studies of underground nuclear test sites and on waste management studies at the Nevada Test Site and the Waste Isolation Pilot Plant site, New Mexico, January 1 to December 31, 1981: U.S. Geological Survey Open-File Report 83-478, 13 p. :maps ;28 cm., https://doi.org/10.3133/ofr83478.","productDescription":"13 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0478/report-thumb.jpg"},{"id":36779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0478/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627e7c","contributors":{"authors":[{"text":"Glanzman, V.M.","contributorId":102065,"corporation":false,"usgs":true,"family":"Glanzman","given":"V.M.","email":"","affiliations":[],"preferred":false,"id":159184,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8452,"text":"ofr83526 - 1983 - Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents","interactions":[],"lastModifiedDate":"2022-12-06T22:28:21.895193","indexId":"ofr83526","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-526","title":"Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents","docAbstract":"Water-quality data for selected sites in the Cape Fear River basin collected by the U.S. Geological Survey, the North Carolina Department of Natural Resources and Community Development and the University of North Carolina at Chapel Hill are analyzed and interpreted in this report. Emphasis is given to the Cape Fear River at Lock 1 near Kelly, where data are most complete. Other data included in the report were collected from the Cape Fear River at Lillington, the Haw River near the Jordan Dam, and the Deep River at Moncure. \r\n\r\nAvailable data indicate that concentrations of dissolved oxygen at study sites are almost always within U.S. Environmental Protection Agency criteria; however, on two sampling dates, the concentration of dissolved oxygen in the Cape Fear at Lock 1 fell slightly below the 5.0 mg/L recommended for fish populations. Measurements of pH from all stations were frequently below the lower limit of 6.5 pH units recommended for protection of freshwater aquatic life. \r\n\r\nMajor dissolved ions detected are sodium and bicarbonate. Sodium concentration averages 8.6 mg/L and bicarbonate averages 17.5 mg/L at Lock 1. Concentrations of dissolved substances and suspended sediment decrease in the downstream direction, presumably because the more heavily populated part of the basin is near the headwaters of the system. \r\n\r\nHeavy metals, with the exceptions of cadmium and mercury, rarely exceed Environmental Protection Agency criteria for the protection of aquatic life. Concentrations of mercury in the Haw River, which exceed the recommended 0.20 mg/L needed to protect aquatic life, have frequently been reported by other authors. Several of the most toxic metals, arsenic, cadmium, and cobalt, are about five times more concentrated in water from the Haw River site than from other study sites in the basin. Iron and manganese frequently exceed North Carolina water-quality standards. \r\n\r\nAvailable nitrogen averages 1.21 mg/L and available phosphorus averages 0.21 mg/L at Lock 1. Nuisance algal growths have not been identified as a problem in the river. \r\n\r\nComparisons of water-quality data for baseline (natural) and present conditions indicate that more than 50 percent of most dissolved substances and over 80 percent of certain forms of nitrogen and phosph6rus result from development.\r\n\r\nOver the past 25 years, increases in concentrations of specific conductance, dissolved magnesium, dissolved sodium, dissolved potassium, dissolved sulfate, dissolved solids, and total nitrite plus nitrate nitrogen were detected in the Cape Fear River at Lock 1. Values for pH and dissolved silica are decreasing. Concentrations of most dissolved constituents at Lock 1 are increasing. 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