The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dam sites, and locations where hydrologic data are available. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556G","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., Herrick, E., and Norman, N., 1982, Drainage areas of surface water bodies of the St. John River basin in northern Maine: U.S. Geological Survey Open-File Report 78-556, v, 70 p., https://doi.org/10.3133/ofr78556G.","productDescription":"v, 70 p.","costCenters":[],"links":[{"id":142631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-g/report-thumb.jpg"},{"id":430928,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"St. John River basin in northern Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.02136034098795,\n 46.547182982038095\n ],\n [\n -67.67131838020025,\n 46.547182982038095\n ],\n [\n -67.67131838020025,\n 47.453446770397846\n ],\n [\n -70.02136034098795,\n 47.453446770397846\n ],\n [\n -70.02136034098795,\n 46.547182982038095\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e9e","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herrick, Emily","contributorId":99143,"corporation":false,"usgs":true,"family":"Herrick","given":"Emily","email":"","affiliations":[],"preferred":false,"id":158471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Norman, Nancy","contributorId":12857,"corporation":false,"usgs":true,"family":"Norman","given":"Nancy","email":"","affiliations":[],"preferred":false,"id":158470,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8872,"text":"ofr78556H - 1982 - Drainage areas of surface water bodies of eastern Maine coastal river basins","interactions":[{"subject":{"id":8872,"text":"ofr78556H - 1982 - Drainage areas of surface water bodies of eastern Maine coastal river basins","indexId":"ofr78556H","publicationYear":"1982","noYear":false,"chapter":"H","title":"Drainage areas of surface water bodies of eastern Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:40:06.808527","indexId":"ofr78556H","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":"78-556","chapter":"H","title":"Drainage areas of surface water bodies of eastern Maine coastal river basins","docAbstract":"The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dam sites, and locations where hydrologic data are available. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556H","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., 1982, Drainage areas of surface water bodies of eastern Maine coastal river basins: U.S. Geological Survey Open-File Report 78-556, v, 54 p., https://doi.org/10.3133/ofr78556H.","productDescription":"v, 54 p.","costCenters":[],"links":[{"id":142629,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-h/report-thumb.jpg"},{"id":430922,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Maine","otherGeospatial":"eastern Maine coastal river basins","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -68.9618726405488,\n 46.003610330553045\n ],\n [\n -68.9618726405488,\n 44.18635392825826\n ],\n [\n -66.92340130518438,\n 44.18635392825826\n ],\n [\n -66.92340130518438,\n 46.003610330553045\n ],\n [\n -68.9618726405488,\n 46.003610330553045\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635ee9","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","interactions":[{"subject":{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","indexId":"ofr78556I","publicationYear":"1982","noYear":false,"chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:41:50.444588","indexId":"ofr78556I","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":"78-556","chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins","docAbstract":"The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dam sites, and locations where hydrologic data are available. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556I","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., 1982, Drainage areas of surface water bodies of central Maine coastal river basins: U.S. Geological Survey Open-File Report 78-556, v, 27 p., https://doi.org/10.3133/ofr78556I.","productDescription":"v, 27 p.","costCenters":[],"links":[{"id":422920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142628,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-i/report-thumb.jpg"}],"country":"United States","state":"Maine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -70.14536238431826,\n 44.57917477028707\n ],\n [\n -70.14536238431826,\n 43.6956341707274\n ],\n [\n -68.91970281136494,\n 43.6956341707274\n ],\n [\n -68.91970281136494,\n 44.57917477028707\n ],\n [\n -70.14536238431826,\n 44.57917477028707\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dcc","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8870,"text":"ofr82507 - 1982 - Cost effective stream-gaging strategies for Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr82507","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":"82-507","title":"Cost effective stream-gaging strategies for Maine","docAbstract":"This report documents the successful application of the traveling-hydrographer program developed by Moss and Gilroy to stream-gaging operations. This application was novel in the consideration of winter discharge records for the period of backwater effects due to ice. The current level of operation in Maine was identified as requiring a budget of $195,000 and having a total uncertainty of 374 cubic feet per second. Stream-gaging strategies were identified that could reduce the level of uncertainty in the system by as much as 45.8%, assuming the budgetary level remained constant. Alternately, practical stream-gaging strategies were also indentified that could reduce the total level of funding by as much as 19.2%, assuming the current level of uncertainty was deemed acceptable. Several alternatives of concurent budgeting and levels of uncertainty were identified. These relationships provide flexibility to the network manager. The results, documented in the report, were based on a sparse data base and should be applied in that context. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82507","usgsCitation":"Fontaine, R.A., 1982, Cost effective stream-gaging strategies for Maine: U.S. Geological Survey Open-File Report 82-507, 47 p. ill., map ;28 cm., https://doi.org/10.3133/ofr82507.","productDescription":"47 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":142955,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0507/report-thumb.jpg"},{"id":36440,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0507/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68402e","contributors":{"authors":[{"text":"Fontaine, R. A.","contributorId":78331,"corporation":false,"usgs":true,"family":"Fontaine","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8866,"text":"ofr82335 - 1982 - Compilation of selected ground-water-quality data from the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr82335","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":"82-335","title":"Compilation of selected ground-water-quality data from the San Joaquin Valley, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82335","usgsCitation":"Fogelman, R.P., 1982, Compilation of selected ground-water-quality data from the San Joaquin Valley, California: U.S. Geological Survey Open-File Report 82-335, iii, 279 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82335.","productDescription":"iii, 279 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":142809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0335/report-thumb.jpg"},{"id":36438,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0335/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a967c","contributors":{"authors":[{"text":"Fogelman, R. P.","contributorId":96688,"corporation":false,"usgs":true,"family":"Fogelman","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":158460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8850,"text":"ofr82597 - 1982 - Phase 3 geophysical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr82597","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":"82-597","title":"Phase 3 geophysical studies in the Wadi Bidah District, Kingdom of Saudi Arabia","docAbstract":"Detailed geophysical measurements have been made in the Rabathan area, Wadi Bidah district, Kingdom of Saudi Arabia, at the site of diamond drill holes RAB-1, -2, and -3; these measurements suggest that the causative source for the anomalous EM (electromagnetic) and SP (self-potential) responses is probably highly conductive zones of Precambrian siliceous-carbonaceous rocks. Although many of the zones are no more than a few meters wide, they commonly contain 50 to 80 percent carbonaceous material and locally abundant pyrite. In places, several thin layers of highly concentrated carbonaceous material interlayered with chert form a multiple conductive zone that is seen in the geophysical data as complex anomaly patterns. In the geologic environment of Wadi Bidah, massive sulfide-bearing zones cannot be distinguished from siliceous-carbonaceous zones on the basis of the EM-SP responses. In North America in similar environments, complex resistivity methods used in experimental research have successfully discriminated between sulfide and carbonaceous conductors. Tests of such methods in the Wadi Bidah district are recommended. \r\n\r\nGeologic, geochemical, and geophysical data at the Jabal Mohr prospect suggest the possibility of mineralized rocks at depth over a possible strike length of 400 m.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82597","usgsCitation":"Flanigan, V.J., Sadek, H., and Smith, C.W., 1982, Phase 3 geophysical studies in the Wadi Bidah District, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 82-597, ii, 47 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82597.","productDescription":"ii, 47 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0597/report-thumb.jpg"},{"id":36429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0597/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686875","contributors":{"authors":[{"text":"Flanigan, V. J.","contributorId":81097,"corporation":false,"usgs":true,"family":"Flanigan","given":"V.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sadek, Hamdy","contributorId":97491,"corporation":false,"usgs":true,"family":"Sadek","given":"Hamdy","affiliations":[],"preferred":false,"id":158435,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, C. W.","contributorId":57457,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158433,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":"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 (ẟ34S 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 (ẟ34S 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.
","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":8827,"text":"ofr82749 - 1982 - Geochemical and mineralogic data from the Lamprecht and Felder uranium deposits, Live Oak County, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82749","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":"82-749","title":"Geochemical and mineralogic data from the Lamprecht and Felder uranium deposits, Live Oak County, Texas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82749","usgsCitation":"Fishman, N., Reynolds, R.L., and Goldhaber, M., 1982, Geochemical and mineralogic data from the Lamprecht and Felder uranium deposits, Live Oak County, Texas: U.S. Geological Survey Open-File Report 82-749, ii, 35 p., ill. ;28 cm., https://doi.org/10.3133/ofr82749.","productDescription":"ii, 35 p., ill. ;28 cm.","costCenters":[],"links":[{"id":141606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0749/report-thumb.jpg"},{"id":36403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0749/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6d8","contributors":{"authors":[{"text":"Fishman, N.S.","contributorId":59441,"corporation":false,"usgs":true,"family":"Fishman","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":158398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, R. L. 0000-0002-4572-2942","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":79885,"corporation":false,"usgs":true,"family":"Reynolds","given":"R.","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":158399,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goldhaber, M. B. 0000-0002-1785-4243","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":103280,"corporation":false,"usgs":true,"family":"Goldhaber","given":"M. B.","affiliations":[],"preferred":false,"id":158400,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8796,"text":"ofr82265 - 1982 - Selected hydrogeologic data from southern Sweet Grass County, south-central Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82265","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":"82-265","title":"Selected hydrogeologic data from southern Sweet Grass County, south-central Montana","docAbstract":"Selected hydrogeologic data from Sweet Grass County south of the Yellowstone River have been compiled to show baseline ground-water conditions. Included are records from a 1981 onsite inventory of 94 water wells and 30 springs. Chemical analyses of water show the major cation and anion concentrations for 40 wells and 14 springs. Concentrations of 17 trace elements in water from 12 of the wells and 9 of the springs were determined by an argon coupled emission spectrometer. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82265","usgsCitation":"Feltis, R., and Wood, W., 1982, Selected hydrogeologic data from southern Sweet Grass County, south-central Montana: U.S. Geological Survey Open-File Report 82-265, 17 p., 1 over-size sheet, ill., maps ;28 cm., https://doi.org/10.3133/ofr82265.","productDescription":"17 p., 1 over-size sheet, ill., maps ;28 cm.","costCenters":[],"links":[{"id":142754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0265/report-thumb.jpg"},{"id":36380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0265/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36381,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0265/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f933b","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":158347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, W.A.","contributorId":6048,"corporation":false,"usgs":true,"family":"Wood","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":158346,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8793,"text":"ofr82324 - 1982 - Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr82324","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":"82-324","title":"Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis","docAbstract":"Multivariate statistical analyses were performed on data from 156 mineral-spring sites in nine Western States to analyze relationships among the various parameters measured in the spring waters. Correlation analysis and R-mode factor analysis indicate that three major factors affect water composition in the spring systems studied: (1) duration of water circulation, (2) depth of water circulation, and (3) partial pressure of carbon dioxide. An examination of factor scores indicates that several types of hydrogeologic systems were sampled. Most of the samples are (1) older water from deeper circulating systems having relatively high salinity, high temperature, and low Eh or (2) younger water from shallower circulating systems having relatively low salinity, low temperature, and high Eh. The rest of the samples are from more complex systems. Any of the systems can have a relatively high or low content of dissolved carbonate species, resulting in a low or high pH, respectively. Uranium concentrations are commonly higher in waters of relatively low temperature and high Eh, and radium concentrations are commonly higher in waters having a relatively high carbonate content (low pH) and, secondarily, relatively high salinity. \r\n\r\nWater samples were collected and (or) measurements were taken at 156 of the 171 mineral-spring sites visited. Various samples were analyzed for radium, uranium, radon, helium, and radium-228 as well as major ions and numerous trace elements. On-site measurements for physical properties including temperature, specific conductance, pH, Eh, and dissolved oxygen were made. All constituents and properties show a wide range of values. Radium concentrations range from less than 0.01 to 300 picocuries per liter; they average 1.48 picocuries per liter and have an anomaly threshold value of 171 picocuries per liter for the samples studied. Uranium concentrations range from less than 0.01 to 120 micrograms per liter and average 0.26 micrograms per liter; they have an anomaly threshold value of 48.1 micrograms per liter. Radon content ranges from less than 10 to 110,000 picocuries per liter, averages 549 picocuries per liter and has an anomaly threshold of 20,400 picocuries per liter. Helium content ranges from -1,300 to +13,000 parts per billion relative to atmospheric helium; it averages +725 parts per billion and has an anomaly threshold of 10,000 parts per billion. Radium-228 concentrations range from less than 2.0 to 33 picocuries per liter; no anomaly threshold was determined owing to the small number of samples. All of the anomaly thresholds may be somewhat high because the sampling was biased toward springs likely to be radioactive. \r\n\r\nThe statistical variance in radium and uranium concentrations unaccounted for by the identified factors testifies to the complexity of some hydrogeologic systems. Unidentified factors related to geologic setting and the presence of uranium-rich rocks in the systems also affect the observed concentrations of the radioactive elements in the water. The association of anomalous radioactivity in several springs with nearby known uranium occurrences indicates that other springs having anomalous radioactivity may also be associated with uranium occurrences as yet undiscovered.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82324","usgsCitation":"Felmlee, J., and Cadigan, R.A., 1982, Radioactivity and geochemistry of selected mineral-spring waters in the Western United States; basic data and multivariate statistical analysis: U.S. Geological Survey Open-File Report 82-324, ii, 107 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82324.","productDescription":"ii, 107 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0324/report-thumb.jpg"},{"id":36377,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634cbd","contributors":{"authors":[{"text":"Felmlee, J.K.","contributorId":106114,"corporation":false,"usgs":true,"family":"Felmlee","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":158341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":158340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8787,"text":"ofr82156 - 1982 - Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina","interactions":[],"lastModifiedDate":"2016-12-14T12:22:31","indexId":"ofr82156","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":"82-156","title":"Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina","docAbstract":"Geologic and hydrologic investigations by the U.S. Geological Survey have defined stratigraphic and hydraulic anomalies suggestive of faulting within Coastal Plain sediments between the Ogeechee River in east-central Georgia and the Edisto River in west-central South Carolina. Examination of borehole cuttings, cores, and geophysical logs from test wells indicate that Triassic rocks and Upper Cretaceous and lower Tertiary Coastal Plain sediments near the Barnwell-Allendale County line near Millett, South Carolina, are offset by a northeast-trending fault downthrown to the northwest. The location of this suspected Coastal Plain fault generally coincides with the location of an inferred fault in basement rocks as interpreted from aeromagnetic surveys. Apparent vertical offsets range from about 700 feet at the base of Upper Cretaceous sediments to about 20 feet in strata of Late Eocene age. As a result, the Upper Cretaceous Middendorf Formation which directly overlies crystalline and Triassic rocks updip (northwest) of this fault, is absent immediately downdip of the fault. The thickness of Tipper Cretaceous sediments is also sharply reduced from about 700 feet to about 180 feet across the fault.\r\n\r\nSediments of the basal Coastal Plain aquifer are largely truncated by uplifted Triassic rocks at the fault near Millett, South Carolina. Lateral ground-water flow near the Savannah River Is consequently disrupted updip of the fault and ground water is transferred vertically into overlying sediments and possibly into the Savannah River. At several locations, abrupt changes in potentiometric head occur across this fault. Computed transmissivity of the basal Coastal Plain aquifer is also radically reduced downdip of the fault, sharply reversing a downdip trend of rapidly increasing aquifer transmissivity. \r\n\r\nOther anomalous potentiometric data along a northeast-trending line between Statesboro, Georgia, and Fairfax, South Carolina, suggest the possibility of similar faulting in correlative geologic units. The location of the suspected fault near Statesboro, Georgia, generally coincides with the eastward extension of the Gulf Trough, a regional potentiometric anomaly in central Georgia.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82156","usgsCitation":"Faye, R., and Prowell, D., 1982, Effects of Late Cretaceous and Cenozoic faulting on the geology and hydrology of the coastal plain near the Savannah River, Georgia and South Carolina: U.S. Geological Survey Open-File Report 82-156, 85 p., 8 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82156.","productDescription":"85 p., 8 over-size sheets, ill., maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-379","title":"WOLF; automatic typing program","docAbstract":"A FORTRAN IV program for the Hewlett-Packard 1000 series computer provides for automatic typing operations and can, when employed with manufacturer's text editor, provide a system to greatly facilitate preparation of reports, letters and other text. The input text and imbedded control data can perform nearly all of the functions of a typist. A few of the features available are centering, titles, footnotes, indentation, page numbering (including Roman numerals), automatic paragraphing, and two forms of tab operations. This documentation contains both user and technical description of the program.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82379","usgsCitation":"Evenden, G., 1982, WOLF; automatic typing program: U.S. Geological Survey Open-File Report 82-379, iv, 45 p., 28 cm., https://doi.org/10.3133/ofr82379.","productDescription":"iv, 45 p., 28 cm.","costCenters":[],"links":[{"id":141874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0379/report-thumb.jpg"},{"id":36337,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0379/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c399","contributors":{"authors":[{"text":"Evenden, G. I.","contributorId":52960,"corporation":false,"usgs":true,"family":"Evenden","given":"G. 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The range of exponents of simple power-function relations is large, both between different reaches of the river, and among different sections within a given reach. The at-a-station exponents plot in several fields of the b-f-m diagram, suggesting that morphologic and hydraulic changes with increasing discharge vary considerably. Systematic changes in the plotting positions of the exponents with time indicate that in general, the width exponent has decreased, although trends are not readily apparent in the other exponents. Plots of the hydraulic-geometry relations indicate that simple power functions are not the proper model in all instances. For these sections, breaks in the slopes of the hydraulic geometry relations serve to partition the data sets. Power functions fit separately to the partitioned data described the width-, depth-, and velocity-discharge relations more accurately than did a single power function. Plotting positions of the exponents from hydraulic geometry relations of partitioned data sets on b-f-m diagrams indicate that much of the apparent variations of plotting positions of single power functions results because the single power functions compromise both subsets of partitioned data. For several sections, the shape of the channel primarily accounts for the better fit of two-power functions to partitioned data than a single power function over the entire range of data. These non-log linear relations may have significance for channel maintenance. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr82436","usgsCitation":"Eschner, T., 1982, Hydraulic geometry of the Platte River in south-central Nebraska: U.S. Geological Survey Open-File Report 82-436, iv, 59 p., https://doi.org/10.3133/ofr82436.","productDescription":"iv, 59 p.","costCenters":[],"links":[{"id":379137,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0436/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0436/report-thumb.jpg"}],"country":"United States","state":"Nebraska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.699951171875,\n 40.718119379753446\n ],\n [\n -100.4150390625,\n 40.718119379753446\n ],\n [\n -100.4150390625,\n 41.90636538970964\n ],\n [\n -103.699951171875,\n 41.90636538970964\n ],\n [\n -103.699951171875,\n 40.718119379753446\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627e94","contributors":{"authors":[{"text":"Eschner, T.R.","contributorId":45700,"corporation":false,"usgs":true,"family":"Eschner","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":158279,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8747,"text":"ofr82910 - 1982 - Selected ground-water data, Sevier Desert, Utah, 1935-82","interactions":[],"lastModifiedDate":"2020-06-16T21:17:15.316532","indexId":"ofr82910","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":"82-910","title":"Selected ground-water data, Sevier Desert, Utah, 1935-82","docAbstract":"No abstract available.
The ground—water level data presented in this report were collected in conjunction with a study of the Mississippi River Valley alluvial aquifer in part of the Yazoo River Basin. Funding for the collection of water—level data was provided by the Vicksburg District, Corps of Engineers, who also drilled the observation wells and surveyed elevations of the top of the casing of each well. The wells were drilled to obtain data on seasonal changes in ground—water levels, areas of recharge and/or discharge, and on direction of movement of water in the alluvial aquifer. This report is intended to document the data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82369","collaboration":"Prepared in cooperation with U. S. Department of the Army Vicksburg District, Corps of Engineers","usgsCitation":"Darden, D., 1982, Hydrologic monitoring in the area of the proposed Yazoo River navigation project, west-central Mississippi, 1978-80: U.S. Geological Survey Open-File Report 82-369, iii, 71 p., https://doi.org/10.3133/ofr82369.","productDescription":"iii, 71 p.","costCenters":[],"links":[{"id":412471,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0369/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142954,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0369/report-thumb.jpg"}],"country":"United 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