{"pageNumber":"357","pageRowStart":"8900","pageSize":"25","recordCount":10959,"records":[{"id":11230,"text":"ofr821019 - 1982 - A study of trends in dissolved oxygen and fecal coliform bacteria at NASQAN stations","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr821019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1019","title":"A study of trends in dissolved oxygen and fecal coliform bacteria at NASQAN stations","docAbstract":"Most stations in the U.S. Geological Survey's National Stream Quality Accounting Network show no significant trend in either dissolved oxygen concentration or fecal coliform bacteria population for the period October 1974. through October 1981. Of the stations which do show trends, however, most show improved water quality: thirty-one of a total of 276 stations show rising dissolved oxygen concentrations, while only 17 show decreasing concentrations. Decreases in fecal coliform populations have occurred at 21 stations while increases have occurred at only 12 stations. \r\n\r\nApproximately half of the stations showing improving trends in dissolved oxygen and fecal coliform bacteria are in the Missouri-Mississippi-Ohio River system. Decreases in dissolved oxygen have occurred at scattered locations in the Western and South-Central States. Rising bacterial populations occur most frequently in the Eastern and Central States \r\n\r\nTrends in dissolved oxygen concentration resulting from temperature changes occurring during the study period can be separated from trends caused by chemical or biological processes by analyzing computed values of dissolved oxygen deficit. About half of the observed trends in dissolved oxygen appear to be the result of changes in water temperature.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821019","usgsCitation":"Smith, R.A., and Alexander, R.B., 1982, A study of trends in dissolved oxygen and fecal coliform bacteria at NASQAN stations: U.S. Geological Survey Open-File Report 82-1019, [i], 8 p. maps ;28 cm., https://doi.org/10.3133/ofr821019.","productDescription":"[i], 8 p. maps ;28 cm.","costCenters":[],"links":[{"id":143993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1019/report-thumb.jpg"},{"id":39020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6120","contributors":{"authors":[{"text":"Smith, Richard A. 0000-0003-2117-2269 rsmith1@usgs.gov","orcid":"https://orcid.org/0000-0003-2117-2269","contributorId":580,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rsmith1@usgs.gov","middleInitial":"A.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":162771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, Richard B. 0000-0001-9166-0626 ralex@usgs.gov","orcid":"https://orcid.org/0000-0001-9166-0626","contributorId":541,"corporation":false,"usgs":true,"family":"Alexander","given":"Richard","email":"ralex@usgs.gov","middleInitial":"B.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":162770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42103,"text":"ofr82275 - 1982 - Altitude and configuration of the predevelopment water table in the High Plains regional aquifer, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-11-05T11:29:05","indexId":"ofr82275","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-275","title":"Altitude and configuration of the predevelopment water table in the High Plains regional aquifer, northwestern Oklahoma","docAbstract":"<p>The High Plains aquifer in Oklahoma is part of a region~l aquifer<br>system extending from South Dakota on the north through Wyoming, Colorado,<br>Nebraska, Kansas, and Oklahoma to Texas and New Mexico o~ the south.<br>(index map). The principal aquifer, the Ogallala F?rmat1on of :ert1ary<br>age, is hydraulically connected with other unconsolidated ~eposits, .<br>principally of Quaternary age. Alluvium and terrace dep?sits htdrau]ically<br>connected with the Ogallala are included in the High Pla1ns.aqu1fer in<br>Oklahoma. Parts of the underlying bedrock also are hydraul 1cally connected<br>with the Ogallala. The High Plai ns aquifer in Oklahoma has been<br>removed by erosion on the west exposing underlying rocks of Cretaceous<br>age and on the east exposing rocks of Permian age.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82275","usgsCitation":"Havens, J., 1982, Altitude and configuration of the predevelopment water table in the High Plains regional aquifer, northwestern Oklahoma: U.S. Geological Survey Open-File Report 82-275, 2 Sheets: 24.53 x 35.82 inches and 46.58 x 16.85 inches, https://doi.org/10.3133/ofr82275.","productDescription":"2 Sheets: 24.53 x 35.82 inches and 46.58 x 16.85 inches","costCenters":[],"links":[{"id":359167,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0275/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359168,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0275/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0275/report-thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.9441,36.9988],[-100.6337,36.9986],[-100.1079,36.9983],[-100.0902,36.9983],[-100.0024,36.9985],[-100.0009,36.9985],[-99.5399,36.9998],[-99.4516,37],[-99.4423,36.9923],[-99.4371,36.9874],[-99.4364,36.9783],[-99.43,36.962],[-99.4253,36.9498],[-99.4132,36.9353],[-99.4051,36.929],[-99.397,36.9217],[-99.3947,36.9159],[-99.3935,36.91],[-99.3865,36.9055],[-99.3697,36.8815],[-99.3536,36.8711],[-99.3346,36.8657],[-99.3236,36.8599],[-99.3144,36.8608],[-99.3138,36.8594],[-99.3138,36.8572],[-99.3167,36.8549],[-99.3184,36.8535],[-99.3201,36.8508],[-99.3207,36.8485],[-99.3207,36.8435],[-99.3114,36.8291],[-99.2999,36.815],[-99.2958,36.8096],[-99.2878,36.806],[-99.2797,36.8019],[-99.2751,36.8001],[-99.2687,36.7938],[-99.2578,36.7893],[-99.2394,36.7898],[-99.2314,36.7898],[-99.2193,36.7875],[-99.209,36.7916],[-99.2038,36.7916],[-99.1911,36.7899],[-99.1705,36.7876],[-99.1572,36.7854],[-99.1475,36.7795],[-99.1377,36.7727],[-99.1302,36.7654],[-99.1239,36.7596],[-99.1147,36.7559],[-99.1089,36.7559],[-99.1043,36.7519],[-99.1032,36.7491],[-99.0968,36.7396],[-99.094,36.7328],[-99.0842,36.7242],[-99.0785,36.7201],[-99.0658,36.7161],[-99.0555,36.7047],[-99.0486,36.6984],[-99.0486,36.6893],[-99.0428,36.6775],[-99.0279,36.663],[-99.025,36.654],[-99.0222,36.6454],[-99.0141,36.639],[-99.0032,36.629],[-98.9918,36.6181],[-98.9729,36.6027],[-98.9593,36.5992],[-98.9604,36.507],[-98.9611,36.4779],[-98.9606,36.247],[-98.9562,36.2469],[-98.9565,36.1587],[-99.382,36.1645],[-99.3806,36.0719],[-99.3809,36.017],[-99.3808,35.8991],[-99.374,35.8991],[-99.3736,35.8111],[-99.3763,35.67],[-99.3751,35.5497],[-99.3751,35.5488],[-99.3627,35.5489],[-99.3631,35.508],[-99.5755,35.5085],[-99.576,35.42],[-100.0009,35.4223],[-100.0014,35.4558],[-100.0011,35.6197],[-100.001,35.64],[-100.0015,35.8008],[-100.0015,35.8782],[-100.0015,35.9478],[-100.002,36.0539],[-100.0025,36.1891],[-100.003,36.3134],[-100.0031,36.3348],[-100.0038,36.4998],[-100.1458,36.4998],[-100.3204,36.4999],[-100.5459,36.4994],[-100.7022,36.5],[-100.8939,36.4998],[-100.9524,36.4998],[-101.0908,36.5003],[-101.6255,36.5025],[-101.87,36.5034],[-102.1618,36.5004],[-103.0007,36.5013],[-103.0007,36.5905],[-103.0007,36.6732],[-103.0007,36.7643],[-103.0008,36.9341],[-103.0009,36.999],[-102.7973,36.9988],[-102.7859,36.9988],[-102.7808,36.9986],[-102.7016,36.9958],[-102.6943,36.9957],[-102.6757,36.9956],[-102.5627,36.9962],[-102.5372,36.9963],[-102.5034,36.9963],[-102.4775,36.9963],[-102.4577,36.9961],[-102.3931,36.9955],[-102.351,36.9951],[-102.3247,36.9948],[-102.0423,36.9922],[-102.0417,36.9922],[-102.0281,36.9925],[-101.9881,36.9925],[-101.918,36.9929],[-101.5552,36.9951],[-101.544,36.9952],[-101.2679,36.9967],[-101.0671,36.9978],[-100.9536,36.9988],[-100.9441,36.9988]]]},\"properties\":{\"name\":\"Beaver\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686999","contributors":{"authors":[{"text":"Havens, John S.","contributorId":13949,"corporation":false,"usgs":true,"family":"Havens","given":"John S.","affiliations":[],"preferred":false,"id":225943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2487,"text":"wsp2188 - 1982 - Temporal trends in the acidity of precipitation and surface waters of New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"wsp2188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2188","title":"Temporal trends in the acidity of precipitation and surface waters of New York","docAbstract":"Statistical analyses of precipitation data from a nine-station monitoring network indicate little change in pH from 1965-78 within New York State as a whole but suggest that pH of bulk precipitation has decreased in the western part of the State by approximately 0.2 pH units since 1965 and increased in the eastern part by a similar amount. This trend is equivalent to an annual change in hydrogen-ion concentration of 0.2 microequivalents per liter. \r\n\r\nAn average annual increase in precipitation quantity of 2 to 3 percent since 1965 has resulted in an increased acid load in the western and central parts of the State. \r\n\r\nDuring 1965-78, sulfate concentration in precipitation decreased an average of 1-4 percent annually. In general, no trend in nitrate was detected. Calculated trends in hydrogen-ion concentration do not correlate with measured trends of sulfate and nitrate, which suggests variable neutralization of hydrogen ion, possibly by particles from dry deposition. Neutralization has produced an increase of about 0.3 pH units in nonurban areas and 0.7 pH units in urban areas. \r\n\r\nStatistical analyses of chemical data from several streams throughout New York suggest that sulfate concentrations decreased an average of 1 to 4 percent per year. This decrease is comparable to the sulfate decrease in precipitation during the same period. In most areas of the State, chemical contributions from urbanization and farming, as well as the neutralizing effect of carbonate soils, conceal whatever effects acid precipitation may have on pH of streams.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;\r\nFor sale by Distributions Branch, U.S. Geological Survey,","doi":"10.3133/wsp2188","usgsCitation":"Peters, N.E., Schroeder, R.A., and Troutman, D.E., 1982, Temporal trends in the acidity of precipitation and surface waters of New York (Reprinted with corrections): U.S. Geological Survey Water Supply Paper 2188, iv, 35 p. :ill., 1 map ;28 cm., https://doi.org/10.3133/wsp2188.","productDescription":"iv, 35 p. :ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":138715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2188/report-thumb.jpg"},{"id":28583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2188/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Reprinted with corrections","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627116","contributors":{"authors":[{"text":"Peters, Norman E. nepeters@usgs.gov","contributorId":1324,"corporation":false,"usgs":true,"family":"Peters","given":"Norman","email":"nepeters@usgs.gov","middleInitial":"E.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":145274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroeder, Roy A. raschroe@usgs.gov","contributorId":1523,"corporation":false,"usgs":true,"family":"Schroeder","given":"Roy","email":"raschroe@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":145275,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Troutman, David E.","contributorId":50133,"corporation":false,"usgs":true,"family":"Troutman","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4365,"text":"cir877 - 1982 - Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","interactions":[{"subject":{"id":41283,"text":"ofr82583 - 1982 - Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada","indexId":"ofr82583","publicationYear":"1982","noYear":false,"title":"Preliminary assessment of potential volcanic hazards in the Long Valley-Mono Lake area, east-central California and southwestern Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":4365,"text":"cir877 - 1982 - Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","indexId":"cir877","publicationYear":"1982","noYear":false,"title":"Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment"},"id":1}],"lastModifiedDate":"2021-10-04T12:00:46.023373","indexId":"cir877","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"877","title":"Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir877","usgsCitation":"Miller, C.D., Mullineaux, D.R., Crandell, D.R., and Bailey, R., 1982, Potential hazards from future volcanic eruptions in the Long Valley-Mono Lake area, east-central California and southwest Nevada; a preliminary assessment: U.S. Geological Survey Circular 877, iii, 10 p., https://doi.org/10.3133/cir877.","productDescription":"iii, 10 p.","costCenters":[],"links":[{"id":31475,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0877/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0877/report-thumb.jpg"},{"id":390138,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23969.htm"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Long Valley - Mono Lake area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.50927734374999,\n              37.33522435930639\n            ],\n            [\n              -118.27880859375001,\n              37.33522435930639\n            ],\n            [\n              -118.27880859375001,\n              38.40194908237822\n            ],\n            [\n              -119.50927734374999,\n              38.40194908237822\n            ],\n            [\n              -119.50927734374999,\n              37.33522435930639\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683625","contributors":{"authors":[{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":148957,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148958,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crandell, D. R.","contributorId":78385,"corporation":false,"usgs":true,"family":"Crandell","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148959,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bailey, R. A.","contributorId":87531,"corporation":false,"usgs":true,"family":"Bailey","given":"R. A.","affiliations":[],"preferred":false,"id":148960,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":56201,"text":"wdrNY811 - 1982 - Water resources data, New York, water year 1981; Volume 1. Eastern New York excluding Long Island","interactions":[],"lastModifiedDate":"2024-07-22T21:02:49.725547","indexId":"wdrNY811","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-81-1","title":"Water resources data, New York, water year 1981; Volume 1. Eastern New York excluding Long Island","docAbstract":"<p>Water resources data for the 1981 water year for New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of ground-water wells. This volume contains records for water discharge at 105 gaging stations; stage only at 6 gaging stations; and stage and contents at 4 gaging stations and 19 other lakes and reservoirs; water quality at 29 gaging stations, 5 precipitation stations and 4 partial-record stations; and water levels at 23 observation wells. Also included are data for 50 crest-stage and 14 low-flow partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data together with the data in Volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in New York.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNY811","collaboration":"Prepared in cooperation with the State of New York and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, New York, water year 1981; Volume 1. Eastern New York excluding Long Island: U.S. Geological Survey Water Data Report NY-81-1, viii, 318 p., https://doi.org/10.3133/wdrNY811.","productDescription":"viii, 318 p.","costCenters":[],"links":[{"id":431318,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/ny-81-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180910,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/ny-81-1/report-thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"eastern New York excluding Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.50726953585145,\n              44.98041799746011\n            ],\n            [\n              -76.02932029130172,\n              44.98041799746011\n            ],\n            [\n              -76.02932029130172,\n              41.044913356229046\n            ],\n            [\n              -73.50726953585145,\n              41.044913356229046\n            ],\n            [\n              -73.50726953585145,\n              44.98041799746011\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f16","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3562,"text":"cir874 - 1982 - Chemical composition of bulk precipitation in the North-Central and Northeastern United States, December 1980 through February 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"874","title":"Chemical composition of bulk precipitation in the North-Central and Northeastern United States, December 1980 through February 1981","docAbstract":"Samples of bulk precipitation were collected at 179 sites in the North-Central and Northeastern United States for 3 months during winter 1980-81 to provide data on the distribution of chemical constituents. Concentrations and average daily loads of 29 dissolved constituents were determined. Sodium and chloride deposition was relatively high in coastal areas and adjacent to some urban centers. Regional patterns of to daily loads of hydrogen ion, nitrate, lead, and iron correlate well with one another and form a concentric pattern around the center of high deposition in eastern Ohio and western Pennsylvania, suggesting an urban-industrial source. Samples from this area had low pH (<4.2), whereas samples from southern Minnesota and Illinois had a more neutral pH (>5.7). The latter samples had high concentrations of calcium and total inorganic carbon, suggesting pH control by soil-derived carbonate minerals. Deposition patterns of ammonium, nitrate, and sulfate display regional highs in Illinois, Indiana, and southwestern Michigan, suggesting agricultural sources such as fertilizer. Median loads of zinc, iron, and lead were lower than reported in previous studies for North America. The apparent decrease in lead since 1950 throughout the area is attributed to reduced consumption of leaded fuels and lower deposition in winter.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir874","usgsCitation":"Peters, N.E., and Bonelli, J.E., 1982, Chemical composition of bulk precipitation in the North-Central and Northeastern United States, December 1980 through February 1981: U.S. Geological Survey Circular 874, ii, 63 p. : ill., maps ; 26 cm., https://doi.org/10.3133/cir874.","productDescription":"ii, 63 p. : ill., maps ; 26 cm.","costCenters":[],"links":[{"id":123716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1982/0874/report-thumb.jpg"},{"id":30590,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0874/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3f9d","contributors":{"authors":[{"text":"Peters, Norman E. nepeters@usgs.gov","contributorId":1324,"corporation":false,"usgs":true,"family":"Peters","given":"Norman","email":"nepeters@usgs.gov","middleInitial":"E.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":147161,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonelli, Joseph E.","contributorId":72361,"corporation":false,"usgs":true,"family":"Bonelli","given":"Joseph","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147162,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47274,"text":"ofr82336 - 1982 - Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida","interactions":[],"lastModifiedDate":"2022-04-28T20:19:14.74335","indexId":"ofr82336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-336","title":"Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida","docAbstract":"<p>The top of the limestone unit ranges from about 25 feet above sea level in western Duval County to about 75 feet below sea level locally in the eastern part of the county. The limestone, which is part of the surficial aquifer, is the principal source of water to shallow wells in the county. The unit generally consists of a soft, friable, cavernous, sandy limestone, which ranges from about 5 to 40 feet in thickness. Along the coast and in the southern part of the county, the limestone becomes discontinuous.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82336","collaboration":"Prepared in cooperation with the City of Jacksonville","usgsCitation":"Spechler, R.M., 1982, Generalized configuration of the top of the limestone unit of the lower part of the surficial aquifer, Duval County, Florida: U.S. Geological Survey Open-File Report 82-336, 1 Plate: 34.92 x 28.86 inches, https://doi.org/10.3133/ofr82336.","productDescription":"1 Plate: 34.92 x 28.86 inches","costCenters":[],"links":[{"id":399852,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0336/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval 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Rick M. spechler@usgs.gov","contributorId":1364,"corporation":false,"usgs":true,"family":"Spechler","given":"Rick","email":"spechler@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":234957,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27999,"text":"wri824074 - 1982 - Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri824074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4074","title":"Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","docAbstract":"Strippable reserves of Mulberry coal underlie an area of approximately 300 square miles of Miami, Linn, and Bourbon Counties of eastern Kansas. Although subject to State reclamation law, current and projected strip mining of this relatively thin coal seam could alter and hydrologic environment of the study area. Drained by the Marais des Cygnes and Little Osage Rivers and their tributaries, this area is characterized by low relief and moderately impermeable soils. Streamflows are poorly sustained by ground-water discharge and fluctuate widely due to climatic extremes and usage of surface-water supplies. Because ground-water supplies are generally unreliable in quantity and quality, surface water is used to meet most water requirements in the study area. Primary used of surface waters are for domestic supplies, maintenance of wildlife and recreational areas, and cooling needs at LaCygne Power Plant. The prevailing chemical type of the natural streamflow is calcium bicarbonate, with concentrations of dissolved solids generally less than 500 milligrams per liter and pH near neutral. Additional streamflow and water-quality data are needed to evaluate the premining characteristics of and the anticipated changes in the hydrologic environment as strip mining proceeds within the study area. A network of data-collection stations and a sampling scheme have been established to acquire this additional information. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri824074","usgsCitation":"Kenny, J.F., Bevans, H., and Diaz, A., 1982, Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4074, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824074.","productDescription":"50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4074/report-thumb.jpg"},{"id":56826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c0f","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":199043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diaz, A.M.","contributorId":27084,"corporation":false,"usgs":true,"family":"Diaz","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":199041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29045,"text":"wri8233 - 1982 - Floods of May 1981 in west-central Montana","interactions":[],"lastModifiedDate":"2019-08-05T11:48:39","indexId":"wri8233","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-33","title":"Floods of May 1981 in west-central Montana","docAbstract":"Extensive flooding occurred in west-central Montana during May 22-23, 1981, as a result of a series of rainstorms. Flooding was particularly severe in the communities of East Helena, Belt, and Deer Lodge. Although no lives were lost, total flood damages were estimated by the Montana Disaster Emergency Services Division to be in excess of $30 million. Peak discharges were determined at 75 sites in the flooded area. At 25 sites the May 1981 peak discharge exceeded the computed 100-year frequency flood, and at 29 sites, where previous flow records are available, the May 1981 peak discharge exceeded the previous peak of record. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8233","usgsCitation":"Parrett, C., Omang, R.J., Hull, J.A., and Fassler, J.W., 1982, Floods of May 1981 in west-central Montana: U.S. Geological Survey Water-Resources Investigations Report 82-33, iv, 20 p. , https://doi.org/10.3133/wri8233.","productDescription":"iv, 20 p. ","costCenters":[],"links":[{"id":366261,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0033/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0033/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.576904296875,\n              45.836454050187726\n            ],\n            [\n              -109.5556640625,\n              45.836454050187726\n            ],\n            [\n              -109.5556640625,\n              47.45037978769006\n            ],\n            [\n              -112.576904296875,\n              47.45037978769006\n            ],\n            [\n              -112.576904296875,\n              45.836454050187726\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5df9df","contributors":{"authors":[{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":200849,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200850,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200852,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fassler, John W.","contributorId":33741,"corporation":false,"usgs":true,"family":"Fassler","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200851,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8829,"text":"ofr82888 - 1982 - Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2020-04-30T16:28:14.587118","indexId":"ofr82888","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-888","title":"Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico","docAbstract":"<p>The Mariano Lake uranium deposit, hosted by the Brushy Basin Member of the Jurassic Morrison Formation, occurs in the trough of an east-west trending syncline at the western end of the Smith Lake-Mariano Lake group of uranium deposits near Crownpoint, New Mexico. The orebody, which contains abundant amorphous organic material, is situated on the reduced side of a regional reduction-oxidation (redox) interface. The presence of amorphous organic material suggests the orebody may represent a tabular (primary) deposit, whereas the close proximity of the orebody to the redox interface is suggestive that uranium was secondarily redistributed by oxidative processes from pre-existing tabular orebodies. Uranium contents correlate positively with both organic carbon and vanadium contents. Petrographic evidence and scanning electron microscope-energy dispersive analyses point to uranium residence in the epigentically introduced amorphous organic material, which coats detrital grains and fills voids. Uranium mineralization was preceded by the following diagenetic alterations: precipitation of pyrite (ẟ<sup>34</sup>S values ranging from-11.0 to-38.2 per mil); precipitation of mixed-layer smectite-illite clays; partial dissolution of some of the detrital feldspar population; and precipitation of quartz and adularia overgrowths. Alterations associated with uranium mineralization include emplacement of amorphous organic material (possibly uranium bearing); destruction of detrital iron-titanium oxide grains; coprecipitation of chlorite and microcrystalline quartz, and precipitation of pyrite and marcasite (ẟ<sup>34</sup>S values for these sulfides ranging from -29.4 to -41.6 per mil). After mineralization, calcite, dolomite, barite, and kaolinite precipitated, and authigenic iron disulfides were replaced by ferric oxides and hydroxides. Geochemical data (primarily the positive correlation of uranium content to both organic carbon and vanadium contents) and petrographic observations (epigentically introduced amorphous organic matter and uranium residence in this organic matter) indicate that the Mariano Lake orebody is a tabular-type uranium deposit. Oxidative processes have not noticeably redistributed and reconcentrated primary uranium in the immediate vicinity of the deposit nor have they greatly modified geochemical characteristics in the ore. Preservation of the Mariano Lake deposit may not only be related to its position along the synclinal trough, where oxidative destruction of the orebody has been inhibited by stagnation of oxidizing ground waters by the structure, but also due to the deflection of ground waters (resulting from low orebody porosity) around the orebody.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82888","usgsCitation":"Fishman, N.S., and Reynolds, R.L., 1982, Origin of the Mariano Lake uranium deposit, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 82-888, iii, 52 p., https://doi.org/10.3133/ofr82888.","productDescription":"iii, 52 p.","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":141608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0888/report-thumb.jpg"},{"id":36405,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0888/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"McKinley County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.0452,36.006],[-108.7687,36.0063],[-108.3738,36.0044],[-108.2646,36.0038],[-108.1559,36.0027],[-108.1468,36.0028],[-108.1411,36.0029],[-108.1224,36.0028],[-107.8738,36.0034],[-107.8351,36.0035],[-107.6776,36.0031],[-107.66,36.0034],[-107.6423,36.0032],[-107.6247,36.0034],[-107.6213,36.003],[-107.6042,36.0032],[-107.5866,36.003],[-107.5718,36.0027],[-107.5541,36.0025],[-107.5513,36.0026],[-107.5161,36.0026],[-107.4421,36.0008],[-107.4068,36.0007],[-107.3875,36.0009],[-107.3397,36.0006],[-107.317,36.0008],[-107.3056,36.0005],[-107.3054,35.991],[-107.3058,35.9765],[-107.3055,35.9311],[-107.3051,35.8744],[-107.3049,35.8295],[-107.3047,35.8168],[-107.3053,35.7864],[-107.3054,35.7573],[-107.3057,35.7419],[-107.3049,35.7301],[-107.3052,35.7151],[-107.305,35.6997],[-107.3053,35.6852],[-107.305,35.6707],[-107.3048,35.6552],[-107.3046,35.6439],[-107.3041,35.6139],[-107.3032,35.5277],[-107.3035,35.4787],[-107.3025,35.4247],[-107.3016,35.3021],[-107.518,35.3036],[-107.5231,35.3036],[-107.6183,35.3059],[-107.6229,35.3059],[-107.6231,35.3159],[-107.6243,35.3485],[-107.7287,35.3489],[-107.7295,35.3366],[-107.7288,35.3062],[-107.7812,35.3063],[-107.8111,35.3063],[-107.8297,35.3065],[-107.8336,35.3064],[-107.9159,35.3065],[-107.9351,35.3066],[-107.9396,35.3065],[-107.974,35.3064],[-107.992,35.3066],[-108.0473,35.307],[-108.143,35.3057],[-108.151,35.307],[-108.2558,35.3077],[-108.364,35.3065],[-108.4661,35.3081],[-108.4644,35.2214],[-108.4659,35.1623],[-108.4661,35.1355],[-108.4673,35.0501],[-108.4678,34.9597],[-108.497,34.96],[-108.52,34.96],[-108.7809,34.9595],[-109.0458,34.9611],[-109.0458,35.166],[-109.0457,35.1796],[-109.0457,35.1941],[-109.0457,35.2078],[-109.0457,35.2228],[-109.0457,35.2359],[-109.0456,35.3531],[-109.0457,35.6637],[-109.0452,36.006]]]},\"properties\":{\"name\":\"McKinley\",\"state\":\"NM\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e15","contributors":{"authors":[{"text":"Fishman, Neil S.","contributorId":106464,"corporation":false,"usgs":true,"family":"Fishman","given":"Neil","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":158404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":158403,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":58575,"text":"mf1493A - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","interactions":[{"subject":{"id":46460,"text":"ofr82962 - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","indexId":"ofr82962","publicationYear":"1982","noYear":false,"title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":58575,"text":"mf1493A - 1982 - Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","indexId":"mf1493A","publicationYear":"1982","noYear":false,"chapter":"A","title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California"},"id":1}],"lastModifiedDate":"2015-10-20T13:14:35","indexId":"mf1493A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1493","chapter":"A","title":"Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California","docAbstract":"<p>Geological, geochemical, and geophysical evidence, together with a review of historical mining and prospecting activities, suggests that most of the Bighorn Mountains Wilderness Study Area has low potential for the discovery of all types of mineral and energy resources-including precious and base metals, building stone and aggregate, fossil fuels, radioactive-mineral resources, and geothermal resources. Low-grade mineralization has been documented in one small area near Rattlesnake Canyon, and this area has low to moderate potential for future small-scale exploration and development of precious and base metals. Thorium and uranium enrichment have been documented in two small areas in the eastern part of the wilderness study area; these two areas have low to moderate potential for future small-scale exploration and development of radioactive-mineral resources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1493A","usgsCitation":"Matti, J.C., Cox, B.F., Rodriguez, E.A., Obi, C.M., Powell, R.E., Hinkle, M., Griscom, A., Sabine, C., and Cwick, G.J., 1982, Mineral resource potential map of the Bighorn Mountains Wilderness Study Area (CDCA-217), San Bernardino County, California: U.S. Geological Survey Miscellaneous Field Studies Map 1493, Report: 8 p.; Plate: 45.83 x 38.60 inches, https://doi.org/10.3133/mf1493A.","productDescription":"Report: 8 p.; Plate: 45.83 x 38.60 inches","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":181313,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1493A.PNG"},{"id":310170,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1493-A/plate-1.pdf","text":"Plate"},{"id":310169,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1493-A/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75,34.200833333333335 ], [ -116.75,34.3675 ], [ -116.45083333333334,34.3675 ], [ -116.45083333333334,34.200833333333335 ], [ -116.75,34.200833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696cef","contributors":{"authors":[{"text":"Matti, Jonathan C. jmatti@usgs.gov","contributorId":3666,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","email":"jmatti@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":259862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, Brett F. bcox@usgs.gov","contributorId":5793,"corporation":false,"usgs":true,"family":"Cox","given":"Brett","email":"bcox@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":259863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodriguez, Eduardo A.","contributorId":83540,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Eduardo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":259864,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Obi, Curtis M.","contributorId":86829,"corporation":false,"usgs":true,"family":"Obi","given":"Curtis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":259865,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Powell, Robert E. 0000-0001-7682-1655 rpowell@usgs.gov","orcid":"https://orcid.org/0000-0001-7682-1655","contributorId":4210,"corporation":false,"usgs":true,"family":"Powell","given":"Robert","email":"rpowell@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":259866,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hinkle, Margaret","contributorId":36918,"corporation":false,"usgs":true,"family":"Hinkle","given":"Margaret","affiliations":[],"preferred":false,"id":259860,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":259861,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Sabine, Charles","contributorId":88407,"corporation":false,"usgs":true,"family":"Sabine","given":"Charles","email":"","affiliations":[],"preferred":false,"id":576232,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cwick, Gary J.","contributorId":86022,"corporation":false,"usgs":true,"family":"Cwick","given":"Gary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":576233,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":59050,"text":"mf1475D - 1982 - Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah","interactions":[],"lastModifiedDate":"2015-10-20T13:09:32","indexId":"mf1475D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"D","title":"Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah","docAbstract":"<p>In general, the mineral potential of the study area is low; in the past the area has yielded only several hundred tons of uranium ore, and there have been a number of unsuccessful efforts to produce gold.</p>\n<p>The generally small uraniferous deposits are in the Chinle Formation, mostly in the basal Shinarump Member, and mostly on the east side of the Paria Plateau. To the south and west, around the plateau, the Shinarump host rock pinches out or is present in only a few places, and the same relationships are likely below the plateau, where the host rocks are deeply buried, from 1,500 to 3,000 ft below the surface. These factors suggest the total uranium-copper-vanadium-silver potential to be very low.</p>\n<p>Gold and mercury occur in very low concentrations in the clayey units of the Petrified Forest Member of the Chinle. Gold concentrations are 40 ppb and less, and the gold is present in very fine particles; recovery is very difficult. Overall, the mercury concentrations are so low that no realistic mineral resource potential can be estimated.</p>\n<p>Nonmetallic mineral materials of possible value include limestone, flagstone, clay, and gravel, but they are of only local interest. No oil or gas resources are known in the study area. Coal resources within the area are nonexistent, but the Dakota Sandstone does contain coaly beds a few miles to the north.</p>\n<p>Water is perhaps the most significant resource needed in the study area. A number of perennial springs support the few local ranchers and tourist facilities. Some ground water would be available below the plateau, but drilling depths would be more than 2,000 ft (600-700 m).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1475D","usgsCitation":"Bush, A., and Lane, M., 1982, Mineral resource potential map of the Vermilion Cliffs-Paria Canyon instant study area, Coconino County, Arizona, and Kane County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1475, Report: 11 p.; Plate: 46.25 x 38.48 inches, https://doi.org/10.3133/mf1475D.","productDescription":"Report: 11 p.; Plate: 46.25 x 38.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1475D.jpg"},{"id":310159,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1475-D/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310160,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1475-D/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Coconino County, Kane County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,36.75 ], [ -112.25,37 ], [ -111.75,37 ], [ -111.75,36.75 ], [ -112.25,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357d1","contributors":{"authors":[{"text":"Bush, Alfred L.","contributorId":48977,"corporation":false,"usgs":true,"family":"Bush","given":"Alfred L.","affiliations":[],"preferred":false,"id":261327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, Michael","contributorId":39756,"corporation":false,"usgs":true,"family":"Lane","given":"Michael","affiliations":[],"preferred":false,"id":261326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11563,"text":"ofr80676 - 1982 - Estimating peak discharges of small rural streams in Massachusetts","interactions":[{"subject":{"id":11563,"text":"ofr80676 - 1982 - Estimating peak discharges of small rural streams in Massachusetts","indexId":"ofr80676","publicationYear":"1982","noYear":false,"title":"Estimating peak discharges of small rural streams in Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":2880,"text":"wsp2214 - 1983 - Estimating peak discharges of small, rural streams in Massachusetts","indexId":"wsp2214","publicationYear":"1983","noYear":false,"title":"Estimating peak discharges of small, rural streams in Massachusetts"},"id":1}],"supersededBy":{"id":2880,"text":"wsp2214 - 1983 - Estimating peak discharges of small, rural streams in Massachusetts","indexId":"wsp2214","publicationYear":"1983","noYear":false,"title":"Estimating peak discharges of small, rural streams in Massachusetts"},"lastModifiedDate":"2022-08-09T15:49:04.64596","indexId":"ofr80676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-676","title":"Estimating peak discharges of small rural streams in Massachusetts","docAbstract":"<p>Floodflows on natural-flow streams in Massachusetts with drainage areas between 0.25 square miles and 260 square miles may be estimated from drainage area, main-channel slope, mean basin elevation, and the area of swamps, lakes, and ponds. Multiple-regression techniques were used to define the relationship between a suite of basin and climatic characteristics and flood peaks in three flood-frequency regions at a total of 95 sites. Station flood-frequency data were computed following guidelines in Bulletin I7A of the U.S. Water Resources Council. The frequency analyses are based upon weighted skew values, and adjustments for high and low outliers, and historic peak data. Regression equations for estimation of peak discharges for 0.5, 0.2, 0.1, 0.04, 0.02, and 0.01 exceedance probabilities are provided for ungaged sites. An improved sample of flood peaks and gaging stations and the definition of three flood-frequency regions reduced the standard error of estimate by about 5 percent over those for the 1977 relations. Included in this analysis were the synthetic flood-frequency data at eight sites computed using historic climatic data and 10 parameters optimized by calibration of the U.S. Geological Survey's rainfall-runoff model with storm data observed over II years. The equations are applicable to streams unaffected by regulation where the usable manmade storage is less than 4.5 million cubic feet per square mile, or by diversions or urbanization. The equations are restricted to sites where the basin indices are within a specified range outside of eastern Plymouth, Barnstable, Dukes or Nantucket Counties. In these areas, the available data do not adequately define the influence of high infiltration and storage capacities of drainage basins on floodflows.</p>","largerWorkType":{"id":18,"text":"Report"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80676","collaboration":"Prepared in cooperation with the Massachusetts Department of Public Works and the U.S. Department of Highway Transportation, Federal Highway Administration","usgsCitation":"Wandle, S.W., 1982, Estimating peak discharges of small rural streams in Massachusetts: U.S. Geological Survey Open-File Report 80-676, iv, 33 p., https://doi.org/10.3133/ofr80676.","productDescription":"iv, 33 p.","costCenters":[],"links":[{"id":405034,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0676/report-thumb.jpg"}],"country":"United 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William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":163363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40934,"text":"ofr82565 - 1982 - Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:51:53.126062","indexId":"ofr82565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-565","title":"Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of water in the Upper Cretaceous Eagle Sandstone and equivalent units (Virgelle Sandstone and Telegraph Creek Formation) is shown on a base map at a scale of 1:1,000,000. The map is one of a series of maps produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great plains of Montana. The contour interval is 200 feet. The map shows that the directions of regional ground-water movement is from west to east except in the extreme northwestern corner where the movement is from east to west. Water is discharged from the Eagle Sandstone to the Missouri River south of the Bearpaw Mountains. In the area north of the Bearpaw Mountains, depressurization from gas production may account for the decline in the potentiometric surface. The average discharge from 115 wells is about 23 gallons per minute and the specific capacity of 85 wells averages 1.4 gallons per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82565","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Eagle Sandstone and equivalent units in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-565, 1 Plate: 40.81 × 22.83 inches, https://doi.org/10.3133/ofr82565.","productDescription":"1 Plate: 40.81 × 22.83 inches","costCenters":[],"links":[{"id":78824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0565/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407484,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75643.htm","linkFileType":{"id":5,"text":"html"}},{"id":171535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.5,\n              45\n            ],\n            [\n              -104.0417,\n              45\n            ],\n            [\n              -104.0417,\n              49\n            ],\n            [\n              -112.5,\n              49\n            ],\n            [\n              -112.5,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b88","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59546,"text":"mf1415B - 1982 - Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee","interactions":[],"lastModifiedDate":"2018-09-14T12:52:09","indexId":"mf1415B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1415","chapter":"B","title":"Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee","docAbstract":"<p>The contiguous Cohutta Wilderness and Hemp Top Roadless Area are in the western part of the Blue Ridge physiographic province of northern Georgia and southeastern Tennessee (fig. 1).&nbsp; All of the study area is in Georgia except an irregular strip of land about 1 mi at its widest on the northern end of the Cohutta Wilderness in Tennessee.&nbsp; The area of the Cohutta Wilderness is 34,650 acres; that of the Hemp Top Roadless Area is 2,800 acres.&nbsp; The areas are in rugged mountainous terrain- a strongly dissected upland ranging in altitude from about 980 to 4,200 ft above sea level.&nbsp; Local altitude differences of 1,450-2,000 ft and slopes steeper than 25° are common.&nbsp; The north end of the Cohutta Wilderness is about 6 mi south of the Ocoee River gorge, 10 mi west-southwest of the major copper-and sulfur-mining district at Ducktown, Tenn., and approximately 22 mi southeast of Cleveland, Tenn., in Bradley County, west of the area shown in figure 1.&nbsp; The eastern, central, and northwestern parts of the wilderness are drained by Jacks River and it tributaries; the southwestern part, by the Conasauga River and its tributaries; and the Hemp Top Roadless Area, by Tumbling Creek and some of its western tributaries.&nbsp; All drainage ultimately goes to the Ocoee River and from these into the Hiwassee River.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1415B","usgsCitation":"Gair, J.E., 1982, Geochemical survey of the Cohutta Wilderness and the Hemp Top Roadless Area, northern Georgia and southeastern Tennessee: U.S. Geological Survey Miscellaneous Field Studies Map 1415, 2 Plates: 52.33 x 39.84 inches and 48.70 x 31.49 inches, https://doi.org/10.3133/mf1415B.","productDescription":"2 Plates: 52.33 x 39.84 inches and 48.70 x 31.49 inches","costCenters":[],"links":[{"id":183161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1415-B/report-thumb.jpg"},{"id":357341,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1415-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":357342,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1415-B/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Georgia, Tennessee","otherGeospatial":"Cohutta Wilderness, Hemp Top Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.66666666666667,34.833333333333336 ], [ -84.66666666666667,35.016666666666666 ], [ -84.45083333333334,35.016666666666666 ], [ -84.45083333333334,34.833333333333336 ], [ -84.66666666666667,34.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6aba72","contributors":{"authors":[{"text":"Gair, Jacob E.","contributorId":18381,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":262200,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19994,"text":"ofr82159 - 1982 - Simulation of ground-water flow in the vicinity of Hyde Park landfill, Niagara Falls, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr82159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-159","title":"Simulation of ground-water flow in the vicinity of Hyde Park landfill, Niagara Falls, New York","docAbstract":"The Hyde Park landfill is a 15-acre chemical waste disposal site located north of Niagara Falls, New York. Underlying the site in descending order are: (1) low permeability glacial till, (2) a moderately permeable fractured rock aquifer--the Lockport Dolomite, and (3) a low permeability unit--the Rochester Shale. The site is bounded on three sides by ground-water drains; the Niagara River Gorge, the Niagara Power Project canal, and the power project conduits. \r\n\r\nA finite element model was used to simulate ground-water flow along an east-west section through the Hyde Park site (from the power project conduits to the Niagara Gorge). Steady-state conditions were simulated with an average annual recharge rate of 5 inches per year. The calibrated model simulated measured water levels within 5 feet in the glacial till and upper unit of the Lockport Dolomite and approximated the configuration of the water table. \r\n\r\nBased on simulation, ground-water flow near the Hyde Park site can be summarized as follows: \r\n\r\n1. Specific discharge (Darcy velocity) ranges from about 0.01 to 0.1 foot per day in the upper unit of the Lockport Dolomite to less than 0.00001 foot per day in the Rochester Shale. Real velocities are highest in the upper unit of the Lockport, ranging from about 1.5 to 4.8 feet per day. \r\n\r\n2. A ground-water divide exists east of the landfill, indicating that all ground water originating near or flowing beneath the landfill will flow toward and discharge in the gorge. \r\n\r\n3. The zone of highest velocities (and presumably greatest potential for transporting chemical contaminants) includes the upper unit of the Lockport and part of the lower unit of the Lockport Dolomite between the landfill and the gorge. The time required for ground water to move from the landfill to the gorge in the Lockport Dolomite is estimated to be 5 to 7 years.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82159","usgsCitation":"Maslia, M., and Johnston, R., 1982, Simulation of ground-water flow in the vicinity of Hyde Park landfill, Niagara Falls, New York: U.S. Geological Survey Open-File Report 82-159, v, 19 p., 5 over-size sheets, ill., (some folded) ;28 cm., https://doi.org/10.3133/ofr82159.","productDescription":"v, 19 p., 5 over-size sheets, ill., (some folded) ;28 cm.","costCenters":[],"links":[{"id":151328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0159/report-thumb.jpg"},{"id":49519,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0159/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49520,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0159/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49521,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0159/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49522,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0159/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49523,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0159/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0159/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f24ff","contributors":{"authors":[{"text":"Maslia, M.L.","contributorId":24090,"corporation":false,"usgs":true,"family":"Maslia","given":"M.L.","affiliations":[],"preferred":false,"id":181870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnston, R.H.","contributorId":19536,"corporation":false,"usgs":true,"family":"Johnston","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":181869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8110,"text":"ofr82264 - 1982 - Availability and quality of water from the Dakota aquifer, northwest Iowa","interactions":[{"subject":{"id":8110,"text":"ofr82264 - 1982 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"ofr82264","publicationYear":"1982","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"wsp2215","publicationYear":"1984","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"id":1}],"supersededBy":{"id":1089,"text":"wsp2215 - 1984 - Availability and quality of water from the Dakota aquifer, northwest Iowa","indexId":"wsp2215","publicationYear":"1984","noYear":false,"title":"Availability and quality of water from the Dakota aquifer, northwest Iowa"},"lastModifiedDate":"2022-11-18T20:38:04.864552","indexId":"ofr82264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-264","title":"Availability and quality of water from the Dakota aquifer, northwest Iowa","docAbstract":"<p>The Dakota aquifer in northwest Iowa consists of sandstones in the Dakota Formation. It underlies most of the study area and is the most extensive source of ground water in the area. Individual sandstone beds are from less than 10 to more than 150 feet thick. The cumulative thickness of sandstone is more than 200 feet throughout much of the area. The aquifer is confined by overlying Cretaceous limestone and shale, Quaternary glacial deposits and loess. The underlying confining material is shale of the Dakota Formation, undifferentiated Paleozoic age rocks, or Precambrian crystalline rock.</p><p>Water flows through the aquifer from the north-central part of the study area to the east, south and southwest. Recharge is dominantly by infiltration from the land surface through the confining materials. Discharge is to underlying Paleozoic aquifers and to the alluvium and glacial outwash deposits along the Missouri and Big Sioux Rivers in the southwest part of the area. Flow components toward bedrock valleys may reflect discharge to Quaternary sand and gravel deposits in these valleys.</p><p>Pumping tests conducted in the study area indicate a narrow range of hydraulic conductivities of the Dakota aquifer, from 37 to 50 feet per day. Consequently, an average hydraulic conductivity of 40 feet per day was used to estimate the potential yield to wells completed in the aquifer. Yields of more than 250 gallons per minute can be expected throughout much of the study area and more than 1000 gallons per minute could be produced in some areas.</p><p>The quality of water from the Dakota is a calcium, magnesium, sulfate type. It is generally suitable for irrigation purposes, based on comparisons of sodium adsorption ratios and electrical conductivities. In some areas the aquifer has water with high salinity hazard that may restrict its use to irrigation of only well drained types of soil. The concentration of radium226 and other radionuclides exceed recommended limits at several sites.</p><p>The quality of water pumped from the aquifer may be altered by induced leakage from the underlying aquifers in Paleozoic age rocks if withdrawals reverse the pattern of natural flow from the Dakota into the Paleozoic aquifers. Evidence for such a reversal exists in the area around the city of LeMars.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82264","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Burkart, M.R., 1982, Availability and quality of water from the Dakota aquifer, northwest Iowa: U.S. Geological Survey Open-File Report 82-264, Report: 83 p.; 8 Plates: 17.84 x 21.84 inches or smaller, https://doi.org/10.3133/ofr82264.","productDescription":"Report: 83 p.; 8 Plates: 17.84 x 21.84 inches or smaller","costCenters":[],"links":[{"id":409478,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409477,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409476,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409475,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409474,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409473,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409472,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409471,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0264/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409470,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0264/report-thumb.jpg"}],"country":"United 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R.","contributorId":42190,"corporation":false,"usgs":true,"family":"Burkart","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7738,"text":"ofr821023 - 1982 - Selected hydrologic data for northern Utah Valley, Utah, 1935-82","interactions":[],"lastModifiedDate":"2022-09-19T22:17:45.843729","indexId":"ofr821023","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1023","title":"Selected hydrologic data for northern Utah Valley, Utah, 1935-82","docAbstract":"<p>This report contains hydrologic data collected in northern Utah Valley from 1935 to 1982. Northern Utah Valley is approximately the northern half of an alluvial-filled basin partly occupied by Utah Lake in north-central Utah. The report area is bounded by the Wasatch Range on the east, the Lake Mountains on the west, and the Traverse Mountains on the north. Its southern boundary is the boundary between Townships 7 and 8 south, Salt Lake Base Line and Meridian.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821023","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Appel, C.L., Clark, D.W., and Fairbanks, P.E., 1982, Selected hydrologic data for northern Utah Valley, Utah, 1935-82: U.S. Geological Survey Open-File Report 82-1023, Report: iv, 97 p.; 1 Plate: 19.07 x 23.94 inches, https://doi.org/10.3133/ofr821023.","productDescription":"Report: iv, 97 p.; 1 Plate: 19.07 x 23.94 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":407017,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1023/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407016,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1023/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Utah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.96441650390625,\n              40.054949943999496\n            ],\n            [\n              -111.62384033203124,\n              40.054949943999496\n            ],\n            [\n              -111.62384033203124,\n              40.44276659332215\n            ],\n            [\n              -111.96441650390625,\n              40.44276659332215\n            ],\n            [\n              -111.96441650390625,\n              40.054949943999496\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publicComments":"This report was also published as Utah Hydrologic Data Report 39","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a144","contributors":{"authors":[{"text":"Appel, Cynthia L.","contributorId":34509,"corporation":false,"usgs":true,"family":"Appel","given":"Cynthia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":156517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, David W.","contributorId":77146,"corporation":false,"usgs":true,"family":"Clark","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":156519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fairbanks, Paul E.","contributorId":66254,"corporation":false,"usgs":true,"family":"Fairbanks","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":156518,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40899,"text":"ofr82562 - 1982 - Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","interactions":[],"lastModifiedDate":"2022-09-27T20:57:58.601919","indexId":"ofr82562","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-562","title":"Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana","docAbstract":"<p>The potentiometric surface of the Judith River Formation is mapped at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water in the Judith River Formation occurs under water-table and artesian conditions. The direction of regional ground-water movement is from west to east. Water is discharged from the Judith River Formation to the Milk River from near Havre, Montana, to Malta and to the Missouri River south of the Bearpaw and Little Rocky Mountains. The average discharge from 236 wells is about 10 gallons per minute, and the specific capacity of 186 wells averages 0.66 gallon per minute per foot of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82562","usgsCitation":"Levings, G., 1982, Potentiometric-surface map of water in the Judith River Formation in the northern Great Plains area of Montana: U.S. Geological Survey Open-File Report 82-562, 1 Plate: 40.47 × 23.06 inches, https://doi.org/10.3133/ofr82562.","productDescription":"1 Plate: 40.47 × 23.06 inches","costCenters":[],"links":[{"id":407485,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75640.htm","linkFileType":{"id":5,"text":"html"}},{"id":78781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0562/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              45\n            ],\n            [\n              -104.0418,\n              45\n            ],\n            [\n              -104.0418,\n              49\n            ],\n            [\n              -111,\n              49\n            ],\n            [\n              -111,\n              45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2f5","contributors":{"authors":[{"text":"Levings, Gary W.","contributorId":106889,"corporation":false,"usgs":true,"family":"Levings","given":"Gary W.","affiliations":[],"preferred":false,"id":224137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10619,"text":"ofr811121 - 1982 - Water resources of the Ochlockonee River area, northwest Florida","interactions":[],"lastModifiedDate":"2022-08-31T19:15:04.672539","indexId":"ofr811121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-1121","title":"Water resources of the Ochlockonee River area, northwest Florida","docAbstract":"<p>The Ochlockonee River area comprises about 1,420 square miles in the panhandle of northwest Florida. In 1975, the population of the area was about 48,000. Water use averaged 11.4 million gallons per day; about half was pumped from wells and half from streams.</p><p>The area receives 57 inches of precipitation per year on the average. Much of this water enters the surficial sand aquifer, seeps to streams, or enters the underlying water-bearing zone of the upper confining unit and the Floridan aquifer.</p><p>The water-bearing zone of the upper confining unit is used for rural domestic supplies and is also important because the water it stores is a source of recharge to the underlying Floridan aquifer.</p><p>The Floridan aquifer underlies all of the Ochlockonee River area and, except for the city of Quincy, is the principal source of municipal water supply. Well yields range from as little as 20 gallons per minute in Gadsden County to as much as 4,500 gallons per minute in Leon County. The transmissivity of the Floridan aquifer ranges from about 170 feet squared per day in the southern part of the area to 5,100 feet squared per day in the northern part. Storage coefficients calculated from two aquifer tests are 2 x 10-4 and 2.6 x 10-4. At Tallahassee, directly east of the Ochlockonee River, transmissivity is as high as 130,000 feet squared per day. The Floridan aquifer is recharged by downward leakage of water from the surficial sand aquifer and from the water-bearing zone of the upper confining unit. The Floridan aquifer is also recharged directly by rainfall in northern Leon County and in southern Georgia where it is near or at land surface. Ground water moves toward the southeast from the potentiometric high in southwestern Gadsden County and south from Leon County toward Wakulla Springs, located about 10 miles south of Tallahassee. The potentiometric surface of the upper part of the Floridan aquifer ranges from about 50 feet higher than that of the middle and lower part of the Floridan aquifer in southwestern Gadsden County to about 10 feet higher near Midway in eastern Gadsden County. The aquifer discharge in the basin area is by wells and by natural discharge through seeps and springs along the Ochlockonee River and at Ochlockonee Bay.</p><p>Water levels in the Floridan aquifer fluctuate in response to seasonal and long-term variations in rainfall. Hydrographs do not show evidence of any long-term water-level declining trend.</p><p>Saline water (more than 1,000 milligrams per liter of dissolved solids) occurs naturally within the Floridan aquifer throughout the Ochlockonee River area at depths ranging from 200 to 600 feet below sea level. The depth below which dissolved solids in water exceed 500 milligrams per liter in the Havana area ranges from 200 to 250 feet below sea level; in the Quincy area, from 400 to 450 feet below; and in the Greensboro area, from 200 to 250 feet below.</p><p>Concentrations of dissolved solids in water pumped from wells tapping the Floridan aquifer in the Ochlockonee River area range from 60 to 1,370 milligrams per liter; chloride from 0 to 630 milligrams per liter; sulfate from 0.0 to 280 milligrams per liter; and fluoride from 0.0 to 1.3 milligrams per liter.</p><p>Streamflow originating in the Ochlockonee River area in Florida averages about 1,000 million gallons per day; minimum discharge during dry periods is about 285 million gallons per day. Stream yields range from 0.90 to 2.62 cubic feet per second per square mile. Quincy Creek, at State Highway 267 at Quincy, the primary source of water for the city of Quincy, yields an average flow of 19 million gallons per day, has a 7-day 10-year low flow of 2.8 million gallons per day, and contains water of acceptable quality. The chemical quality of most streams in the basin is acceptable for most uses. Dissolved-solids concentration is generally less than 135 milligrams per liter; pH ranges from 5.3 to 7.3 units; color from 20 to 90 platinum-cobalt units; and turbidity from 3 to 85 Jackson turbidity units. Variations in chloride concentration in water from the Ochlockonee River (5.2 to 140 milligrams per liter) are influenced by discharge of food processing waste and municipal sewage plant effluent to the river.</p><p>The three large lakes in the basin range from 4,000 to 7,000 acres in surface area. All are now used primarily for recreation. Dissolved-solids concentrations of water from the lakes range from less than 20 to 50 milligrams per liter. A major flood occurred in 1975 when the Ochlockonee River near Havana reached the third highest stage of record and the peak flood at the Sopchoppy River exceeded that for the period of record (11 years in 1975); no significant damage occurred.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811121","collaboration":"Prepared in cooperation with the Northwest Florida Water Management District, Gadsden County and the City of Quincy","usgsCitation":"Pascale, C.A., and Wagner, J.R., 1982, Water resources of the Ochlockonee River area, northwest Florida: U.S. Geological Survey Open-File Report 81-1121, vii, 114 p., https://doi.org/10.3133/ofr811121.","productDescription":"vii, 114 p.","costCenters":[],"links":[{"id":406025,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1121/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1121/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Ochlockonee River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.75814819335936,\n              29.846599772557077\n            ],\n            [\n              -84.38735961914062,\n              29.846599772557077\n            ],\n            [\n              -84.38735961914062,\n              30.198552988693212\n            ],\n            [\n              -84.75814819335936,\n              30.198552988693212\n            ],\n            [\n              -84.75814819335936,\n              29.846599772557077\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0499","contributors":{"authors":[{"text":"Pascale, Charles A.","contributorId":99978,"corporation":false,"usgs":true,"family":"Pascale","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wagner, Jeffry R.","contributorId":48179,"corporation":false,"usgs":true,"family":"Wagner","given":"Jeffry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11000,"text":"ofr821095 - 1982 - GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979","interactions":[],"lastModifiedDate":"2018-06-19T08:27:45","indexId":"ofr821095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-1095","title":"GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979","docAbstract":"<p>A cruise on the- DESV STARELLA was conducted between October 23. 1979, and November 8, 1979, by the U.S. Geologic.al Survey (USGS) in cooperation with the United Kingdom's Institute of Oceanographic Sciences (IOS). The purpose of the study was to gain an overview of the morphology of large areas of the Continental Slope and upper Continental Rise off the eastern ·united States. Sidescan-sonar and single-channel seismic-reflection data were collected along the tracklines. The ship's position. was monitored using LORAN_C and satellite navigation techniques.</p><p>The sidescan data were collected using the !OS-developed Geologic Long­-Range Inclined Asdic, Mark II (GLORIA II) system. GLORIA was operated at either a 20-second or 40-second sweep, giving maximum slant-range distances of 15 or 30 kilometers, respectively, to each side of the towed fish. The sidescan data were collected on graphic recorders and analog tapes. The tapes were played onto photographic paper in a facsimile machine; then these prints were photographically stretched to produce approximately isometric images .. The images were not corrected for slant-range distortion. Mosaics at a scale of 1:250,000 (Mercator projection) were made from the photographic images.</p><p>The seismic· data consist of 40-in<sup>3</sup> airgun and 10-kHz echo-sounder profiles. The airgun data were recorded on EPC recorders at both 8- and 4- second sweep rates. The 10-kHz echo-sounder data were recorded on a wet-paper recorder at a 2-second sweep rate.</p><p>Approximately 4,820 km of seismic and sonar-data wera collected from four areas of interest and along the lines connecting those areas. Area 1 includes the Continental Slope and upper Rise seaward of Georges Bank, between Northeast Channel and Alvin Canyon. Numerous lines were run here, resulting in approximately 2,500 km of seismic data and complete and overlapping GLORIA coverage of the area. A similar survey, consisting of approximately 1 2 200 km of trackline, was run in area 2, which includes the Continental Slope and upper Rise seaward of the middle Atlantic states between Hudson Canyon and Baltimore Canyon. A single line, 250 km long, was run through area 3 along the base of the Continental Slope from Cape Hatteras to latitude 33°N. off North and South Carolina. Two parallel lines, totaling 870 km, were run through area 4 along the Blake Escarpment, from the Blake Spur south to latitude 27°40'N. One line was run along the top of the escarpment and the other was run along the base of the escarpment.</p><p>All the data can be studied at the U.S. Geological Survey offices in Woods Hole, MA 02543. Microfilm copies of the sidescan-monitor record as well as the airgun and 10-kHz profiles can be purchased only from the National Geophysical Data Center, NOAA, Code E64, 325 Broadway, Boulder, CO 80303 (303/497-6338). Photographic copies of the GLORIA mosaics can also be obtained only from this address.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr821095","usgsCitation":"Scanlon, K.M., 1982, GLORIA sidescan and seismic data collected by the DESV STARELLA along the continental slope and upper continental rise of the Eastern United States in 1979: U.S. Geological Survey Open-File Report 82-1095, 3 p., https://doi.org/10.3133/ofr821095.","productDescription":"3 p.","costCenters":[],"links":[{"id":143369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr821095.PNG"},{"id":259857,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1095/ofr19821095.pdf","text":"Report","size":"1.94 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1982-1095"}],"contact":"<p><a href=\"https://woodshole.er.usgs.gov/\" data-mce-href=\"https://woodshole.er.usgs.gov/\">Coastal and Marine Geology Program</a> U.S. Geological Survey<br> 384 Woods Hole Road<br> Woods Hole, MA 02543</p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1603","contributors":{"authors":[{"text":"Scanlon, Kathryn M.","contributorId":6816,"corporation":false,"usgs":true,"family":"Scanlon","given":"Kathryn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":162353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11247,"text":"ofr82701 - 1982 - Preliminary results of gravity investigations at Yucca Mountain and vicinity, southern Nye County, Nevada","interactions":[],"lastModifiedDate":"2024-06-03T17:15:28.48172","indexId":"ofr82701","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-701","title":"Preliminary results of gravity investigations at Yucca Mountain and vicinity, southern Nye County, Nevada","docAbstract":"<p>Exploration for a high-level-nuclear-waste-repository site in the Yucca Mountain area, Nev., resulted in the addition of 423 new gravity stations during the past 2 years to the 934 existing stations to form the data base of this study. About 100 surface-rock samples, three borehole gamma-gamma logs, and one borehole gravity study provide excellent density control. A linear increase in density of 0.26 g/cm3 per km is indicated in the thick tuff sequences. This steady increase of density within the tuff sequences makes the density contrast across the basal contact of the tuff the only strong source of gravity fluctuations. Isostatic and 2.0-g/cm3 Bouguer corrections were applied to the observed gravity values to remove deep-crust-related regional gradients and topographic effects, respectively. The resulting residual-gravity plot shows significant gravity anomalies that correlate closely with the structures inferred from drill-hole and surface geologic studies.</p><p>Gravity highs over the three Paleozoic rock outcrops within the study area--Bare Mountain, the Calico Hills, and the Striped Hills--served as reference points for the gravity models. The Bare Mountain gravity high, which peaks at 48 mGal, connects with a larger gravity high over the Funeral Mountains to the south; together, these highs may result from a continuous block of mildly metamorphosed Precambrian and Paleozoic rocks stretching from the east edge of Death Valley to Bare Mountain. The Calico Hills gravity high appears more likely to originate from a northeast-trending remanent topographic high of buried Paleozoic rocks rather than from an isolated structural dome. This buried ridge may extend southwestward beneath Busted Butte, 5 km southeast of the proposed repository, where 2 1/2- and 3dimensional modeling indicates that the pre-Cenozoic rocks may be less than 1,000 m deep.</p><p>At least 3,000 m of tuff fills a large steep-sided depression in the prevolcanic rocks beneath Yucca Mountain and Crater Flat. The gravity low and thick tuff section probably lie within a large collapse area comprising the Crater Flat-Timber Mountain-Silent Canyon caldera complexes. Gravity lows in Crater Flat itself are thought to coincide with the source areas of the Prow Pass Member, the Bullfrog Member, and the unnamed member of the Crater Flat Tuff. Southward extension of the broad gravity low associated with Crater Flat into the Amargosa Desert is evidence for sector graben-type collapse segments related to Timber Mountain caldera and superimposed on the other structures within Crater Flat.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82701","usgsCitation":"Snyder, D., and Carr, W.J., 1982, Preliminary results of gravity investigations at Yucca Mountain and vicinity, southern Nye County, Nevada: U.S. Geological Survey Open-File Report 82-701, iv, 36 p., https://doi.org/10.3133/ofr82701.","productDescription":"iv, 36 p.","costCenters":[],"links":[{"id":429467,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0701/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39042,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0701/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143712,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0701/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"Yucca Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.54199992341728,\n              36.969218668834756\n            ],\n            [\n              -116.54199992341728,\n              36.7955322232273\n            ],\n            [\n              -116.33873566687758,\n              36.7955322232273\n            ],\n            [\n              -116.33873566687758,\n              36.969218668834756\n            ],\n            [\n              -116.54199992341728,\n              36.969218668834756\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b2f8","contributors":{"authors":[{"text":"Snyder, D.B.","contributorId":99141,"corporation":false,"usgs":true,"family":"Snyder","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":162801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, W. James","contributorId":16014,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":162800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56284,"text":"wdrWA802 - 1982 - Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington","interactions":[],"lastModifiedDate":"2025-07-21T17:52:28.421042","indexId":"wdrWA802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-80-2","title":"Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington","docAbstract":"<p>Water Resources data for the 1980 water year for Washington consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report in two volumes contains records for water discharge at 233 gaging stations stage only at 5 gaging stations; stage and contents at 41 lakes and reservoirs; and water quality at 39 gaging stations (including 6 lakes and reservoirs) and 100 wells; and water levels at 164 observation wells. Also included are data for 14 crest-stage, and 89 water-quality partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA802","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Washington, water year 1980: Vol. 2 - Eastern Washington: U.S. Geological Survey Water Data Report WA-80-2, x, 332 p., https://doi.org/10.3133/wdrWA802.","productDescription":"x, 332 p.","costCenters":[],"links":[{"id":492667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1980/wa-80-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174737,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1980/wa-80-2/report-thumb.jpg"}],"country":"United 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,{"id":9314,"text":"ofr82148 - 1982 - Chemical and mineralogical variation in the Pioneer Batholith, southwest Montana","interactions":[],"lastModifiedDate":"2022-08-17T19:26:33.808343","indexId":"ofr82148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-148","title":"Chemical and mineralogical variation in the Pioneer Batholith, southwest Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82148","usgsCitation":"Hammarstrom, J.M., 1982, Chemical and mineralogical variation in the Pioneer Batholith, southwest Montana: U.S. Geological Survey Open-File Report 82-148, ii, 177 p., https://doi.org/10.3133/ofr82148.","productDescription":"ii, 177 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":405276,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75619.htm","linkFileType":{"id":5,"text":"html"}},{"id":37034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0148/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0148/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.125,\n              45.35\n            ],\n            [\n              -112.75,\n              45.35\n            ],\n            [\n              -112.75,\n              45.75\n            ],\n            [\n              -113.125,\n              45.75\n            ],\n            [\n              -113.125,\n              45.35\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e487a","contributors":{"authors":[{"text":"Hammarstrom, J. M.","contributorId":34513,"corporation":false,"usgs":true,"family":"Hammarstrom","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":159466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9854,"text":"ofr82849 - 1982 - Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr82849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-849","title":"Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States","docAbstract":"Linear features are relatively short, distinct, non-cultural linear elements mappable on Landsat multispectral scanner images (MSS). Most linear features are related to local topographic features, such as cliffs, slope breaks, narrow ridges, and stream valley segments that are interpreted as reflecting directed aspects of local geologic structure including faults, zones of fracturing (joints), and the strike of tilted beds. \r\n\r\n6,050 linear features were mapped on computer-enhanced Landsat MSS images of 11 Landsat scenes covering an area from the Rio Grande rift zone on the east to the Grand Canyon on the west and from the San Juan Mountains, Colorado, on the north to the Mogollon Rim on the south. Computer-aided statistical analysis of the linear feature data revealed 5 statistically important trend intervals: 1.) N. 10W.-N.16E., 2.) N.35-72E., 3.) N.33-59W., 4.) N. 74-83W., and 5.) N.89-9-W. and N. 89-90E. Subsequent analysis of the distribution of the linear features indicated that only the first three trend intervals are of regional geologic significance. Computer-generated maps of the linear features in each important trend interval were prepared, as well as contour maps showing the relative concentrations of linear features in each trend interval. These maps were then analyzed for patterns suggestive of possible regional tectonic lines. \r\n\r\n20 possible tectonic lines, or lineaments, were interpreted from the maps. One lineament is defined by an obvious change in overall linear feature concentrations along a northwest-trending line cutting across northeastern Arizona. Linear features are abundant northeast of the line and relatively scarce to the southwest. The remaining 19 lineaments represent the axes of clusters of parallel linear features elongated in the direction of the linear feature trends. Most of these lineaments mark previously known structural zones controlled by linear features in the Precambrian basement or show newly recognized relationships to geological and/or geophysical patterns that suggest probable influence by buried basement features. The remaining few lineaments are not strongly correlative with geological or geophysical patterns, but on the basis of existing data they cannot be dismissed as being possible expressions of basement features.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82849","usgsCitation":"Knepper, D.H., 1982, Lineaments derived from analysis of linear features mapped from Landsat images of the Four Corners region of the Southwestern United States: U.S. Geological Survey Open-File Report 82-849, 81 p., 1 over-size sheet, ill., maps ;30 cm., https://doi.org/10.3133/ofr82849.","productDescription":"81 p., 1 over-size sheet, ill., maps ;30 cm.","costCenters":[],"links":[{"id":141873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0849/report-thumb.jpg"},{"id":37635,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0849/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0849/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50c8","contributors":{"authors":[{"text":"Knepper, Daniel H. dknepper@usgs.gov","contributorId":1242,"corporation":false,"usgs":true,"family":"Knepper","given":"Daniel","email":"dknepper@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":160411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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