{"pageNumber":"2791","pageRowStart":"69750","pageSize":"25","recordCount":184617,"records":[{"id":53241,"text":"ofr03493 - 2003 - Trace element and Nd, Sr, Pb isotope geochemistry of Kilauea Volcano, Hawai'i, near-vent eruptive products: 1983-2001","interactions":[],"lastModifiedDate":"2014-03-14T09:22:59","indexId":"ofr03493","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-493","title":"Trace element and Nd, Sr, Pb isotope geochemistry of Kilauea Volcano, Hawai'i, near-vent eruptive products: 1983-2001","docAbstract":"This open-file report serves as a repository for geochemical data referred to in U.S. Geological Survey Professional Paper 1676 (Heliker, Swanson, and Takahashi, eds., 2003), which includes multidisciplinary research papers pertaining to the first twenty years of Puu Oo Kupaianaha eruption activity. Details of eruption characteristics and nomenclature are provided in the introductory chapter of that volume (Heliker and Mattox, 2003). Geochemical relations of this data are depicted and interpreted by Thornber (2003), Thornber and others (2003a) and Thornber (2001).\n\nThis report supplements Thornber and others (2003b) in which whole-rock and glass major-element data on ~1000 near-vent lava samples collected during the 1983 to 2001 eruptive interval of Kilauea Volcano, Hawai'i, are presented. Herein, we present whole-rock trace element compositions of 85 representative samples collected from January 1983 to May 2001; glass trace-element compositions of 39 Pele’s Tear (tephra) samples collected from September 1995 to September 1996, and whole-rock Nd, Sr and Pb isotopic analyses of 10 representative samples collected from September 1983 to September 1993. Thornber and others (2003b) provide a specific record of sample characteristics, location, etc., for each of the samples reported here. Spreadsheets of both reports may be integrated and sorted based upon time of formation or sample numbers. General information pertaining to the selectivity and petrologic significance of this sample suite is presented by Thornber and others (2003b). As justified in that report, this select suite of time-constrained geochemical data is suitable for constructing petrologic models of pre-eruptive magmatic processes associated with prolonged rift zone eruption of Hawaiian shield volcanoes.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03493","usgsCitation":"Thornber, C.R., Budahn, J.R., Ridley, W., and Unruh, D., 2003, Trace element and Nd, Sr, Pb isotope geochemistry of Kilauea Volcano, Hawai'i, near-vent eruptive products: 1983-2001: U.S. Geological Survey Open-File Report 2003-493, Report: 5 p.; Geochem data, https://doi.org/10.3133/ofr03493.","productDescription":"Report: 5 p.; Geochem data","numberOfPages":"5","temporalStart":"1983-01-01","temporalEnd":"2001-12-31","costCenters":[{"id":336,"text":"Hawaiian Volcano Observatory","active":false,"usgs":true}],"links":[{"id":178221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03493.jpg"},{"id":4894,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0493/","linkFileType":{"id":5,"text":"html"}},{"id":284001,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0493/pdf/of03-493.pdf"},{"id":284002,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0493/OF03-493data.xls"}],"country":"United States","state":"Hawai'i","otherGeospatial":"Kilauea Volcano","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.305533,19.38969 ], [ -155.305533,19.443418 ], [ -155.232799,19.443418 ], [ -155.232799,19.38969 ], [ -155.305533,19.38969 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627ef4","contributors":{"authors":[{"text":"Thornber, Carl R. cthornber@usgs.gov","contributorId":2016,"corporation":false,"usgs":true,"family":"Thornber","given":"Carl","email":"cthornber@usgs.gov","middleInitial":"R.","affiliations":[{"id":157,"text":"Cascades Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":247024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Budahn, James R. 0000-0001-9794-8882 jbudahn@usgs.gov","orcid":"https://orcid.org/0000-0001-9794-8882","contributorId":1175,"corporation":false,"usgs":true,"family":"Budahn","given":"James","email":"jbudahn@usgs.gov","middleInitial":"R.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":247023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ridley, W. Ian 0000-0001-6787-558X","orcid":"https://orcid.org/0000-0001-6787-558X","contributorId":17269,"corporation":false,"usgs":true,"family":"Ridley","given":"W. Ian","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":247025,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Unruh, Daniel M.","contributorId":96291,"corporation":false,"usgs":true,"family":"Unruh","given":"Daniel M.","affiliations":[],"preferred":false,"id":247026,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":47580,"text":"ofr03223 - 2003 - Potentiometric surface of the upper Floridan Aquifer, west-central Florida, September 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:10:58","indexId":"ofr03223","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-223","title":"Potentiometric surface of the upper Floridan Aquifer, west-central Florida, September 2002","language":"ENGLISH","doi":"10.3133/ofr03223","usgsCitation":"Blanchard, R.A., Knochenmus, L.A., Seidenfeld, A., and McCulloch, D.S., 2003, Potentiometric surface of the upper Floridan Aquifer, west-central Florida, September 2002: U.S. Geological Survey Open-File Report 2003-223, 1 map ; 72 x 69 cm., on sheet 87 x 77 cm., folded to 22 x 26 cm., https://doi.org/10.3133/ofr03223.","productDescription":"1 map ; 72 x 69 cm., on sheet 87 x 77 cm., folded to 22 x 26 cm.","costCenters":[],"links":[{"id":168297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84539,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0223/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682b7b","contributors":{"authors":[{"text":"Blanchard, Robert Allen","contributorId":11273,"corporation":false,"usgs":true,"family":"Blanchard","given":"Robert","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":235776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knochenmus, L. A.","contributorId":60683,"corporation":false,"usgs":true,"family":"Knochenmus","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235777,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Seidenfeld, A.V.","contributorId":90377,"corporation":false,"usgs":true,"family":"Seidenfeld","given":"A.V.","email":"","affiliations":[],"preferred":false,"id":235779,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McCulloch, D. S.","contributorId":78315,"corporation":false,"usgs":true,"family":"McCulloch","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":235778,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":69714,"text":"i2793 - 2003 - Topographic map of the Margaritifer Chaos region of Mars -- MTM 500k-10/337E OMKT","interactions":[],"lastModifiedDate":"2012-02-10T00:11:33","indexId":"i2793","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2793","title":"Topographic map of the Margaritifer Chaos region of Mars -- MTM 500k-10/337E OMKT","language":"ENGLISH","doi":"10.3133/i2793","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2003, Topographic map of the Margaritifer Chaos region of Mars -- MTM 500k-10/337E OMKT (Online only, Version 1.0): U.S. Geological Survey IMAP 2793, 1 map sheet, 28 x 40 in., https://doi.org/10.3133/i2793.","productDescription":"1 map sheet, 28 x 40 in.","onlineOnly":"Y","costCenters":[],"links":[{"id":191534,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6385,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2793/","linkFileType":{"id":5,"text":"html"}}],"scale":"502000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 20,-12.833333333333334 ], [ 20,-7.833333333333333 ], [ 25,-7.833333333333333 ], [ 25,-12.833333333333334 ], [ 20,-12.833333333333334 ] ] ] } } ] }","edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629cc7","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":534675,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69722,"text":"mf2410 - 2003 - Geologic map of the Upper Hurricane Wash and vicinity, Mohave County, northwestern Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:23","indexId":"mf2410","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2410","title":"Geologic map of the Upper Hurricane Wash and vicinity, Mohave County, northwestern Arizona","docAbstract":"      This digital map database is compiled from unpublished open file reports by the author and represents the general distribution of surficial and bedrock geology in the mapped area. The map area lies within the Shivwits and Uikaret Plateaus, together with the accompanying pamphlet, it provides current information on the geologic structure, stratigraph, and Cenozoic geology of the area.  The database delineates map units that are identified by age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution of the database to 1:31,680 or smaller.","language":"ENGLISH","doi":"10.3133/mf2410","usgsCitation":"Billingsley, G.H., and Dyer, H.C., 2003, Geologic map of the Upper Hurricane Wash and vicinity, Mohave County, northwestern Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 2410, 24 p. and 1 sheet, https://doi.org/10.3133/mf2410.","productDescription":"24 p. and 1 sheet","costCenters":[],"links":[{"id":110475,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62879.htm","linkFileType":{"id":5,"text":"html"},"description":"62879"},{"id":187816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6392,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2003/2410/","linkFileType":{"id":5,"text":"html"}}],"scale":"31680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.5,36.5 ], [ -113.5,36.75 ], [ -113.25,36.75 ], [ -113.25,36.5 ], [ -113.5,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a254","contributors":{"authors":[{"text":"Billingsley, George H.","contributorId":20711,"corporation":false,"usgs":true,"family":"Billingsley","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":281011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dyer, Helen C.","contributorId":86432,"corporation":false,"usgs":true,"family":"Dyer","given":"Helen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":281012,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69723,"text":"mf2419 - 2003 - Geologic map of the Puye Quadrangle, Los Alamos, Rio Arriba, Sandoval, and Santa Fe Counties, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:23","indexId":"mf2419","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2419","title":"Geologic map of the Puye Quadrangle, Los Alamos, Rio Arriba, Sandoval, and Santa Fe Counties, New Mexico","docAbstract":"      The Puye quadrangle covers an area on the eastern flank of the Jemez Mountains, north of Los Alamos and west of Espanola, New Mexico.  Most of the quadrangle consists of a dissected plateau that was formed on the resistant caprock of the Bandelier Tuff, which was erupted from the Valles caldera approximately 1 to 2 million years ago.  Within the canyons of the east-flowing streams that eroded this volcanic tableland, Miocene and Pliocene fluvial deposits of the Puye Formation and Santa Fe Group are exposed beneath the Bandelier Tuff.  These older units preserve sand and gravel that were deposited by streams and debris flows flowing from source areas located mostly north and northeast of the Puye quadrangle.  The landscape of the southeastern part of the quadrangle is dominated by the valley of the modern Rio Grande, and by remnants of piedmont-slope and river-terrace deposits that formed during various stages of incision of the Rio Grande drainage on the landscape.  Landslide deposits are common along the steep canyon walls where broad tracts of the massive caprock units have slumped toward the canyons on zones of weakness in underlying strata, particularly on silt/clay-rich lacustrine beds within the Puye Formation.","language":"ENGLISH","doi":"10.3133/mf2419","usgsCitation":"Dethier, D., 2003, Geologic map of the Puye Quadrangle, Los Alamos, Rio Arriba, Sandoval, and Santa Fe Counties, New Mexico (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2419, over-sized sheet, 40 by 30 inch, in color, https://doi.org/10.3133/mf2419.","productDescription":"over-sized sheet, 40 by 30 inch, in color","costCenters":[],"links":[{"id":110471,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62574.htm","linkFileType":{"id":5,"text":"html"},"description":"62574"},{"id":187817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6393,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2003/mf-2419/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,35.8675 ], [ -106.25,36 ], [ -106.11749999999999,36 ], [ -106.11749999999999,35.8675 ], [ -106.25,35.8675 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c074","contributors":{"authors":[{"text":"Dethier, David P.","contributorId":35285,"corporation":false,"usgs":true,"family":"Dethier","given":"David P.","affiliations":[],"preferred":false,"id":281013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69721,"text":"mf2396 - 2003 - Geologic map of the Lower Hurricane Wash and vicinity, Mohave County, Northwestern Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:23","indexId":"mf2396","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2396","title":"Geologic map of the Lower Hurricane Wash and vicinity, Mohave County, Northwestern Arizona","docAbstract":"This digital map database is compiled from published open file reports, and new mapping by the author, and represents the general distribution of surficial and bedrock geology in the mapped area. The map area lies within the Shivwits and Uinkaret Plateaus, subplateaus of the southwestern part of the Colorado Plateau hypsographic province. Together with the accompanying pamphlet, it provides current information on the geologic structure and stratigraphy of the area. The database delineates map units that are identified by age and lithology, following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution of the database to 1:31,680 or smaller.","language":"ENGLISH","doi":"10.3133/mf2396","usgsCitation":"Billingsley, G.H., and Graham, S.E., 2003, Geologic map of the Lower Hurricane Wash and vicinity, Mohave County, Northwestern Arizona (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2396, 28 p. and 1 sheet, https://doi.org/10.3133/mf2396.","productDescription":"28 p. and 1 sheet","costCenters":[],"links":[{"id":110470,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62490.htm","linkFileType":{"id":5,"text":"html"},"description":"62490"},{"id":187716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6391,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2003/2396/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.5,36.75 ], [ -113.5,37 ], [ -113.25,37 ], [ -113.25,36.75 ], [ -113.5,36.75 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d77","contributors":{"authors":[{"text":"Billingsley, George H.","contributorId":20711,"corporation":false,"usgs":true,"family":"Billingsley","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":281010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graham, Scott E. sgraham@usgs.gov","contributorId":2907,"corporation":false,"usgs":true,"family":"Graham","given":"Scott","email":"sgraham@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":281009,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53600,"text":"ofr03335 - 2003 - Data on Streamflow and Quality of Water and Bottom Sediment in and near Humboldt Wildlife Management Area, Churchill and Pershing Counties, Nevada, 1998-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr03335","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-335","title":"Data on Streamflow and Quality of Water and Bottom Sediment in and near Humboldt Wildlife Management Area, Churchill and Pershing Counties, Nevada, 1998-2000","docAbstract":"This study was initiated to expand upon previous findings that indicated concentrations of dissolved solids, arsenic, boron, mercury, molybdenum, selenium, and uranium were either above geochemical background concentrations or were approaching or exceeding ecological criteria in the lower Humboldt River system. Data were collected from May 1998 to September 2000 to further characterize streamflow and surface-water and bottom-sediment quality in the lower Humboldt River, selected agricultural drains, Upper Humboldt Lake, and Lower Humboldt Drain (ephemeral outflow from Humboldt Sink). \r\n\r\nDuring this study, flow in the lower Humboldt River was either at or above average. Flows in Army and Toulon Drains generally were higher than reported in previous investigations. An unnamed agricultural drain contributed a small amount to the flow measured in Army Drain. \r\n\r\nIn general, measured concentrations of sodium, chloride, dissolved solids, arsenic, boron, molybdenum, and uranium were higher in water from agricultural drains than in Humboldt River water during this study. Mercury concentrations in water samples collected during the study period typically were below the laboratory reporting level. However, low-level mercury analyses showed that samples collected in August 1999 from Army Drain had higher mercury concentrations than those collected from the river or Toulon Drain or the Lower Humboldt Drain. Ecological criteria and effect concentrations for sodium, chloride, dissolved solids, arsenic, boron, mercury, and molybdenum were exceeded in some water samples collected as part of this study. \r\n\r\nAlthough water samples from the agricultural drains typically contained higher concentrations of sodium, chloride, dissolved solids, arsenic, boron, and uranium, greater instantaneous loads of these constituents were carried in the river near Lovelock than in agricultural drains during periods of high flow or non-irrigation. During this study, the high flows in the lower Humboldt River produced the maximum instantaneous loads of sodium, chloride, dissolved solids, arsenic, boron, molybdenum, and uranium at all river-sampling sites, except molybdenum near Imlay. \r\n\r\nNevada Division of Environmental Protection monitoring reports on mine-dewatering discharge for permitted releases of treated effluent to the surface waters of the Humboldt River and its tributaries were reviewed for reported discharges and trace-element concentrations from June 1998 to September 1999. These data were compared with similar information for the river near Imlay. \r\n\r\nIn all bottom sediments collected for this study, arsenic concentrations exceeded the Canadian Freshwater Interim Sediment-Quality Guideline for the protection of aquatic life and probable-effect level (concentration). Sediments collected near Imlay, Rye Patch Reservoir, Lovelock, and from Toulon Drain and Army Drain were found to contain cadmium and chromium concentrations that exceeded Canadian criteria. Chromium concentrations in sediments collected from these sites also exceeded the consensus-based threshold-effect concentration. The Canadian criterion for sediment copper concentration was exceeded in sediments collected from the Humboldt River near Lovelock and from Toulon, Army, and the unnamed agricultural drains. Mercury in sediments collected near Imlay and from Toulon Drain in August 1999 exceeded the U.S. Department of the Interior sediment probable-effect level. Nickel concentrations in sediments collected during this study were above the consensus-based threshold-effect concentration. All other river and drain sediments had constituent concentrations below protective criteria and toxicity thresholds. \r\n\r\nIn Upper Humboldt Lake, chloride, dissolved solids, arsenic, boron, molybdenum, and uranium concentrations in surface-water samples collected near the mouth of the Humboldt River generally were higher than in samples collected near the mouth of Army Drain. Ecological criteria or effect con","language":"ENGLISH","doi":"10.3133/ofr03335","usgsCitation":"Paul, A.P., and Thodal, C.E., 2003, Data on Streamflow and Quality of Water and Bottom Sediment in and near Humboldt Wildlife Management Area, Churchill and Pershing Counties, Nevada, 1998-2000: U.S. Geological Survey Open-File Report 2003-335, vi, 94 p. : ill. (some col.), col. maps ; 28 cm., https://doi.org/10.3133/ofr03335.","productDescription":"vi, 94 p. : ill. (some col.), col. maps ; 28 cm.","costCenters":[],"links":[{"id":4852,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03335/","linkFileType":{"id":5,"text":"html"}},{"id":178531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c859","contributors":{"authors":[{"text":"Paul, Angela P. 0000-0003-3909-1598 appaul@usgs.gov","orcid":"https://orcid.org/0000-0003-3909-1598","contributorId":2305,"corporation":false,"usgs":true,"family":"Paul","given":"Angela","email":"appaul@usgs.gov","middleInitial":"P.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thodal, Carl E. 0000-0003-0782-3280 cethodal@usgs.gov","orcid":"https://orcid.org/0000-0003-0782-3280","contributorId":2292,"corporation":false,"usgs":true,"family":"Thodal","given":"Carl","email":"cethodal@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247883,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51994,"text":"wri034092 - 2003 - Simulation of Temperature, Nutrients, Biochemical Oxygen Demand, and Dissolved Oxygen in the Catawba River, South Carolina, 1996-97","interactions":[],"lastModifiedDate":"2017-01-20T09:51:11","indexId":"wri034092","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4092","title":"Simulation of Temperature, Nutrients, Biochemical Oxygen Demand, and Dissolved Oxygen in the Catawba River, South Carolina, 1996-97","docAbstract":"Time-series plots of dissolved-oxygen concentrations were determined for various simulated hydrologic and point-source loading conditions along a free-flowing section of the Catawba River from Lake Wylie Dam to the headwaters of Fishing Creek Reservoir in South Carolina. The U.S. Geological Survey one-dimensional dynamic-flow model, BRANCH, was used to simulate hydrodynamic data for the Branched Lagrangian Transport Model. Waterquality data were used to calibrate the Branched Lagrangian Transport Model and included concentrations of nutrients, chlorophyll a, and biochemical oxygen demand in water samples collected during two synoptic sampling surveys at 10 sites along the main stem of the Catawba River and at 3 tributaries; and continuous water temperature and dissolved-oxygen concentrations measured at 5 locations along the main stem of the Catawba River.\r\n\r\n      A sensitivity analysis of the simulated dissolved-oxygen concentrations to model coefficients and data inputs indicated that the simulated dissolved-oxygen concentrations were most sensitive to watertemperature boundary data due to the effect of temperature on reaction kinetics and the solubility of dissolved oxygen. Of the model coefficients, the simulated dissolved-oxygen concentration was most sensitive to the biological oxidation rate of nitrite to nitrate.\r\n\r\n      To demonstrate the utility of the Branched Lagrangian Transport Model for the Catawba River, the model was used to simulate several water-quality scenarios to evaluate the effect on the 24-hour mean dissolved-oxygen concentrations at selected sites for August 24, 1996, as simulated during the model calibration period of August 23 27, 1996. The first scenario included three loading conditions of the major effluent discharges along the main stem of the Catawba River (1) current load (as sampled in August 1996); (2) no load (all point-source loads were removed from the main stem of the Catawba River; loads from the main tributaries were not removed); and (3) fully loaded (in accordance with South Carolina Department of Health and Environmental Control National Discharge Elimination System permits). Results indicate that the 24-hour mean and minimum dissolved-oxygen concentrations for August 24, 1996, changed from the no-load condition within a range of - 0.33 to 0.02 milligram per liter and - 0.48 to 0.00 milligram per liter, respectively. Fully permitted loading conditions changed the 24-hour mean and minimum dissolved-oxygen concentrations from - 0.88 to 0.04 milligram per liter and - 1.04 to 0.00 milligram per liter, respectively. A second scenario included the addition of a point-source discharge of 25 million gallons per day to the August 1996 calibration conditions. The discharge was added at S.C. Highway 5 or at a location near Culp Island (about 4 miles downstream from S.C. Highway 5) and had no significant effect on the daily mean and minimum dissolved-oxygen concentration.\r\n\r\n      A third scenario evaluated the phosphorus loading into Fishing Creek Reservoir; four loading conditions of phosphorus into Catawba River were simulated. The four conditions included fully permitted and actual loading conditions, removal of all point sources from the Catawba River, and removal of all point and nonpoint sources from Sugar Creek. Removing the point-source inputs on the Catawba River and the point and nonpoint sources in Sugar Creek reduced the organic phosphorus and orthophosphate loadings to Fishing Creek Reservoir by 78 and 85 percent, respectively.","language":"ENGLISH","doi":"10.3133/wri034092","usgsCitation":"Feaster, T., Conrads, P., Guimaraes, W.B., Sanders, C.L., and Bales, J.D., 2003, Simulation of Temperature, Nutrients, Biochemical Oxygen Demand, and Dissolved Oxygen in the Catawba River, South Carolina, 1996-97: U.S. Geological Survey Water-Resources Investigations Report 2003-4092, 123 p., https://doi.org/10.3133/wri034092.","productDescription":"123 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":177533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4568,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034092/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","otherGeospatial":"Catabwa River","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"properties\":{},\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.7657470703125,35.567980458012094],[-81.8756103515625,35.536696378395035],[-82.0074462890625,35.572448615622804],[-82.0623779296875,35.585851593232356],[-82.16812133789062,35.54060755592023],[-82.22579956054688,35.59255224089235],[-82.24159240722656,35.65729624809628],[-82.20794677734374,35.74818410650582],[-82.08915710449219,35.801664652427895],[-82.02598571777344,35.81001773806242],[-81.96418762207031,35.821153818963175],[-81.95594787597656,35.92019610057511],[-81.95182800292969,35.98078444581272],[-81.903076171875,36.053540128339755],[-81.8536376953125,36.05798104702501],[-81.76712036132812,36.055760619006755],[-81.71905517578125,36.04021586880111],[-81.66824340820312,35.98245135784044],[-81.5679931640625,35.9157474194997],[-81.31393432617188,35.95911138558121],[-81.26998901367188,36.03244234269516],[-81.19171142578125,36.0779620797358],[-81.08322143554688,36.06353184297193],[-80.79620361328125,35.89350026142572],[-80.71929931640624,35.69299463209881],[-80.7275390625,35.53110865111194],[-80.69869995117188,35.43381992014202],[-80.70556640625,35.34425514918409],[-80.80718994140625,35.15584570226544],[-80.81268310546874,34.95349314197422],[-80.771484375,34.89494244739732],[-80.71105957031249,34.65467425162703],[-80.68084716796875,34.51787261401661],[-80.52978515625,34.35704160076073],[-80.4583740234375,34.23905366851639],[-80.518798828125,34.03900467904445],[-80.496826171875,33.88865750124075],[-80.60394287109375,33.75060604160645],[-80.71998596191406,33.82992730179868],[-80.74745178222656,34.05209051767928],[-80.83328247070312,34.27083595165],[-80.8971405029297,34.3201881768449],[-80.98915100097656,34.40634314091266],[-81.04133605957031,34.487881874939866],[-81.10588073730469,34.710009159224946],[-81.12167358398438,34.84311278917537],[-81.16905212402344,35.07271701786369],[-81.15669250488281,35.18222692831516],[-81.12373352050781,35.25627309169437],[-81.12648010253906,35.460669951495305],[-81.2384033203125,35.567980458012094],[-81.3922119140625,35.58138418324621],[-81.595458984375,35.59925232772949],[-81.7657470703125,35.567980458012094]]]}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a186","contributors":{"authors":[{"text":"Feaster, Toby D. 0000-0002-5626-5011 tfeaster@usgs.gov","orcid":"https://orcid.org/0000-0002-5626-5011","contributorId":1109,"corporation":false,"usgs":true,"family":"Feaster","given":"Toby D.","email":"tfeaster@usgs.gov","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":244635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Conrads, Paul 0000-0003-0408-4208 pconrads@usgs.gov","orcid":"https://orcid.org/0000-0003-0408-4208","contributorId":764,"corporation":false,"usgs":true,"family":"Conrads","given":"Paul","email":"pconrads@usgs.gov","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true},{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":244634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guimaraes, Wladmir B. wbguimar@usgs.gov","contributorId":3818,"corporation":false,"usgs":true,"family":"Guimaraes","given":"Wladmir","email":"wbguimar@usgs.gov","middleInitial":"B.","affiliations":[{"id":559,"text":"South Carolina Water Science Center","active":true,"usgs":true}],"preferred":true,"id":244636,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sanders, Curtis L. Jr.","contributorId":76391,"corporation":false,"usgs":true,"family":"Sanders","given":"Curtis","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":244637,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bales, Jerad D. 0000-0001-8398-6984 jdbales@usgs.gov","orcid":"https://orcid.org/0000-0001-8398-6984","contributorId":683,"corporation":false,"usgs":true,"family":"Bales","given":"Jerad","email":"jdbales@usgs.gov","middleInitial":"D.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":244633,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":53465,"text":"wri034190 - 2003 - Estimated water use and availability in the lower Blackstone River basin, northern Rhode Island and south-central Massachusetts, 1995-99","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"wri034190","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4190","title":"Estimated water use and availability in the lower Blackstone River basin, northern Rhode Island and south-central Massachusetts, 1995-99","docAbstract":"The Blackstone River basin includes approximately 475 square miles in northern Rhode Island and south-central Massachusetts. The study area (198 square miles) comprises six subbasins of the lower Blackstone River basin. The estimated population for the study period 1995?99 was 149,651 persons. Water-use data including withdrawals, use, and return flows for the study area were collected. Withdrawals averaged 29.869 million gallons per day (Mgal/d) with an estimated 12.327 Mgal/d exported and an estimated 2.852 Mgal/d imported; this resulted in a net export of 9.475 Mgal/d. Public-supply withdrawals were 22.694 Mgal/d and self-supply withdrawals were 7.170 Mgal/d, which is about 24 percent of total withdrawals. Two users withdrew 4.418 Mgal/d of the 7.170 Mgal/d of self-supply withdrawals. Total water use averaged 20.388 Mgal/d. The largest aggregate water use was for domestic supply (10.113 Mgal/d, 50 percent of total water use), followed by industrial water use (4.127 Mgal/d, 20 percent), commercial water use (4.026 Mgal/d, 20 percent), non-account water use (1.866 Mgal/d, 9 percent) and agricultural water use (0.252 Mgal/d, 1 percent). Wastewater disposal averaged 15.219 Mgal/d with 10.395 Mgal/d or 68 percent disposed at National Pollution Discharge Elimination System (NPDES) outfalls for municipal wastewater-treatment facilities. The remaining 4.824 Mgal/d or 32 percent was self-disposed, 1.164 Mgal/d of which was disposed through commercial and industrial NPDES outfalls.\r\n\r\n\r\nWater availability (base flow plus safe-yield estimates minus streamflow criteria) was estimated for the low-flow period, which included June, July, August, and September. The median base flow for the low-flow period from 1957 to 1999 was estimated at 0.62 Mgal/d per square mile for sand and gravel deposits and 0.19 Mgal/d per square mile for till deposits. Safe-yield estimates for public-supply reservoirs totaled 20.2 Mgal/d. When the 7-day, 10-year low flow (7Q10) was subtracted from base flow, an estimated median rate of 50.5 Mgal/d of water was available for the basin during August, the lowest base-flow month. In addition, basin-wide water-availability estimates were calculated with and without streamflow criteria for each month of the low-flow period at the 75th, 50th, and 25th percentiles of base flow. These water availability estimates ranged from 42.3 to 181.7 Mgal/d in June; 20.2 to 96.7 Mgal/d in July; 20.2 to 85.4 Mgal/d in August, and 20.2 to 97.5 Mgal/d in September. Base flow was less than the Aquatic Base Flow (ABF), minimum flow considered adequate to protect aquatic fauna, from July through September at the 25th percentile and in August and September at the 50th percentile.\r\n\r\n\r\nA basin-stress ratio, which is equal to total withdrawals divided by water availability, was also calculated. The basin-stress ratio for August at the 50th percentile of base flow minus the 7Q10 was 0.68 for the study area. For individual subbasins, the ratio ranged from 0.13 in the Chepachet River subbasin to 0.95 in the Abbot Run subbasin. In addition, basin-stress ratios with and without streamflow criteria for all four months of the low-flow period were calculated at the 75th, 50th, and 25th percentiles of base flow. These values ranged from 0.19 to 0.83 in June, 0.36 to 1.50 in July, 0.40 to 1.14 in August, and 0.31 to 0.78 in September. Ratios could not be calculated by using the ABF at the 50th and 25th percentiles in August and September because the estimated base flow was less than the ABF.\r\n\r\n\r\nThe depletion of the Blackstone River flows by Cumberland Water Department Manville well no. 1 in Rhode Island was estimated with the computer program STRMDEPL and specified daily pumping rates. STRMDEPL uses analytical solutions to calculate time-varying rates of streamflow depletion caused by pumping at wells. Results show that streamflow depletions were about 97 percent of average daily pumping rates for 1995 through 1999. Relative streamflow depletions for","language":"ENGLISH","doi":"10.3133/wri034190","usgsCitation":"Barolw, L.K., 2003, Estimated water use and availability in the lower Blackstone River basin, northern Rhode Island and south-central Massachusetts, 1995-99: U.S. Geological Survey Water-Resources Investigations Report 2003-4190, 85 p., https://doi.org/10.3133/wri034190.","productDescription":"85 p.","costCenters":[],"links":[{"id":4683,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034190/","linkFileType":{"id":5,"text":"html"}},{"id":177662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a009","contributors":{"authors":[{"text":"Barolw, Lora K.","contributorId":36212,"corporation":false,"usgs":true,"family":"Barolw","given":"Lora","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":247666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53147,"text":"wri034203 - 2003 - Occurrence and distribution of nutrients, suspended sediment, and pesticides in the Mobile River Basin, Alabama, Georgia, Mississippi, and Tennessee, 1999-2001","interactions":[],"lastModifiedDate":"2017-01-20T10:19:29","indexId":"wri034203","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4203","title":"Occurrence and distribution of nutrients, suspended sediment, and pesticides in the Mobile River Basin, Alabama, Georgia, Mississippi, and Tennessee, 1999-2001","docAbstract":"The Mobile River Basin is one of more than 50 river basins and aquifer systems being investigated as part of the U.S. Geological Survey's National Water- Quality Assessment (NAWQA) Program. This basin is the sixth largest river basin in the United States and the fourth largest in terms of streamflow. The Mobile River Basin encompasses parts of Alabama, Georgia, Mississippi, and Tennessee, and almost two-thirds of the 44,0000-square-mile basin is located in Alabama. The extensive water resources of the Mobile River Basin are influenced by an array of natural and cultural factors, which impart unique and variable qualities to the streams, rivers, and aquifers and provide abundant habitat to sustain the diverse aquatic life in the basin.\r\n\r\nFrom January 1999 to December 2001, a study was conducted of the occurrence and distribution of nutrients, suspended sediment, and pesticides in surface water of the Mobile River Basin. Nine sampling sites were selected on the basis of land use. The nine sites included two streams draining agricultural areas, two urban streams, and five large rivers with mixed land use. Surface-water samples were collected from one to four times each month to characterize the spatial and temporal variation in nutrient and pesticide concentrations.\r\n\r\nNutrient and suspended-sediment concentrations were highest in watersheds dominated by urban or agricultural land uses. Forty-two percent of the total phosphorus concentrations at all nine sites exceeded the U.S. Environmental Protection Agency's recommended maximum concentration of 0.1 milligram per liter. Flow-weighted mean concentrations at the Mobile River Basin sites generally were in the lower to middle percentile ranges compared with data from other NAWQA studies across the Nation. However, flow-weighted mean concentrations of ammonia, total nitrogen, orthophosphate, and total phosphorus at Bogue Chitto Creek, an agricultural watershed, ranked in the upper 20th percentile of agricultural sites sampled across the Nation as part of the NAWQA Program. Nutrient loads in the Tombigbee River were nearly twice as high compared with nutrient loads in the Alabama River. Nutrient yields were highest in Bogue Chitto Creek, Cahaba Valley Creek, and Threemile Branch because of agricultural and urban land uses in these watersheds.\r\n\r\nOf the 104 pesticides and degradation products analyzed in the stream samples, 69 were detected in one or more samples. Of the 69 detected pesticides, 51 were herbicides, 15 were insecticides, and 3 were fungicides. A relatively small number of heavily used herbicides accounted for most of the detections, including atrazine and its metabolites (deethylatrazine, 2-hydroxyatrazine, deisopropylatrazine, and deethyldeisopropylatrazine), simazine, metolachlor, tebuthiuron, prometon, diuron, and 2,4-D. Diazinon, chlorpyrifos, and carbaryl were the most frequently detected insecticides; metalaxyl was the most frequently detected fungicide in the Mobile River Basin.\r\n\r\nConcentrations of pesticides detected in surface water of the Mobile River Basin were among the highest concentrations recorded nationally by the NAWQA Program during 1991 to 2001. The three highest concentrations of atrazine detected at sites across the country were recorded at Bogue Chitto Creek; the highest concentrations of 2,4-D, imazaquin, and malathion recorded nationally were detected at Threemile Branch. Aquatic-life criteria were exceeded by concentrations of five herbicides (2,4-D, atrazine, cyanazine, diuron, and metolachlor), six insecticides (carbaryl, chlorpyrifos, diazinon, dieldrin, malathion, and p,p'-DDE), and one fungicide (chlorothalonil). Drinking-water standards were exceeded by concentrations of four herbicides (2,4-D, atrazine, cyanazine, and simazine), three insecticides (alpha- HCH, diazinon, and dieldrin), and one fungicide (chlorothalonil).\r\n\r\nThe types and concentrations of pesticides found in surface water are linked to land use and to the types of pesti","language":"ENGLISH","doi":"10.3133/wri034203","usgsCitation":"McPherson, A.K., Moreland, R.S., and Atkins, J.B., 2003, Occurrence and distribution of nutrients, suspended sediment, and pesticides in the Mobile River Basin, Alabama, Georgia, Mississippi, and Tennessee, 1999-2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4203, 109 p., https://doi.org/10.3133/wri034203.","productDescription":"109 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":177202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4732,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034203/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama, Georgia, Mississippi, Tennessee","otherGeospatial":"Mobile River 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States\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69625b","contributors":{"authors":[{"text":"McPherson, Ann K.","contributorId":15240,"corporation":false,"usgs":true,"family":"McPherson","given":"Ann","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":246762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moreland, Richard S. rsmore@usgs.gov","contributorId":3877,"corporation":false,"usgs":true,"family":"Moreland","given":"Richard","email":"rsmore@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":246761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atkins, J. Brian","contributorId":49781,"corporation":false,"usgs":true,"family":"Atkins","given":"J.","email":"","middleInitial":"Brian","affiliations":[],"preferred":false,"id":246763,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53125,"text":"wri034142 - 2003 - Spatial variability of sedimentary interbed properties near the Idaho Nuclear Technology and Engineering Center at the Idaho National Engineering and Environmental Laboratory, Idaho","interactions":[],"lastModifiedDate":"2020-02-11T06:52:14","indexId":"wri034142","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4142","title":"Spatial variability of sedimentary interbed properties near the Idaho Nuclear Technology and Engineering Center at the Idaho National Engineering and Environmental Laboratory, Idaho","docAbstract":"The subsurface at the Idaho National Engineering and Environmental Laboratory (INEEL) is complex, comprised primarily of thick, fractured basalt flows interbedded with thinner sedimentary intervals. The unsaturated zone can be as thick as 200 m in the southwestern part of the INEEL. The Vadose Zone Research Park (VZRP), located approximately 10 km southwest of the Idaho Nuclear Technology and Engineering Center (INTEC), was established in 2001 to study the subsurface of a relatively undisturbed part of the INEEL. Waste percolation ponds for the INTEC were relocated to the VZRP due to concerns that perched water within the vadose zone under the original infiltration ponds (located immediately south of the INTEC) could contribute to migration of contaminants to the Snake River Plain aquifer.\r\n\r\nKnowledge of the spatial distribution of texture and hydraulic properties is important for developing a better understanding of subsurface flow processes within the interbeds, for example, by identifying low permeability layers that could lead to the formation of perched ground-water zones. Because particle-size distributions are easier to measure than hydraulic properties, particle size serves as an analog for determining how the unsaturated hydraulic properties vary both vertically within particular interbeds and laterally within the VZRP. As part of the characterization program for the subsurface at the VZRP, unsaturated and saturated hydraulic properties were measured on 10 core samples from six boreholes. Bulk properties, including particle size, bulk density, particle density, and specific surface area, were determined on material from the same depth intervals as the core samples, with an additional 66 particle- size distributions measured on bulk samples from the same boreholes. \r\n\r\nFrom lithologic logs of the 32 boreholes at the VZRP, three relatively thick interbeds (in places up to 10 m thick) were identified at depths of 35, 45, and 55 m below land surface. The 35-m interbed extends laterally over a distance of at least 900 m from the Big Lost River to the new percolation pond area of the VZRP. Most wells within the VZRP were drilled to depths less than 50 m, making it difficult to infer the lateral extent of the 45-m and 55-m interbeds. The 35-m interbed is uniform in texture both vertically and laterally; the 45-m interbed coarsens upward; and the 55-m interbed contains alternating coarse and fine layers. Seventy-one out of 90 samples were silt loams and 9 out of 90 samples were classified as either sandy loams, loamy sands, or sands. The coarsest samples were located within the 45-m and 55-m interbeds of borehole ICPP-SCI-V-215, located near the southeast corner of the new percolation pond area. \r\n\r\nAt the tops of some interbeds, baked-zone intervals were identified by their oxidized color (yellowish red to red) compared to the color of the underlying non-baked material (pale yellow to brown). The average geometric mean particle diameter of baked-zone intervals was only slightly coarser, in some cases, than the underlying non-baked sediment. This is likely due to both depositional differences between the top and bottom of the interbeds and the presence of small basalt clasts in the sediment. Core sample hydraulic properties from baked zones within the different interbeds did not show effects from alteration caused during basalt deposition, but differed mainly by texture.\r\n\r\nSaturated hydraulic conductivities (Ksat) for the 10 core samples ranged from 10-7 to 10-4 cm/s. Low permeability layers, with Ksat values less than 10-7 cm/s, within the 35-m and 45-m interbeds may cause perched ground-water zones to form beneath the new percolation pond area, leading to the possible lateral movement of water away from the VZRP.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri034142","usgsCitation":"Winfield, K.A., 2003, Spatial variability of sedimentary interbed properties near the Idaho Nuclear Technology and Engineering Center at the Idaho National Engineering and Environmental Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 2003-4142, 41 p., https://doi.org/10.3133/wri034142.","productDescription":"41 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":177766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4704,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034142/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Engineering and Environmental Laboratory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.16629028320312,\n              43.402054267905655\n            ],\n            [\n              -111.87515258789062,\n              43.402054267905655\n            ],\n            [\n              -111.87515258789062,\n              43.68872888432795\n            ],\n            [\n              -112.16629028320312,\n              43.68872888432795\n            ],\n            [\n              -112.16629028320312,\n              43.402054267905655\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e66bc","contributors":{"authors":[{"text":"Winfield, Kari A.","contributorId":63874,"corporation":false,"usgs":true,"family":"Winfield","given":"Kari","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":246706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53154,"text":"ds79 - 2003 - Coastal erosion and wetland change in Louisiana: selected USGS products","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ds79","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79","title":"Coastal erosion and wetland change in Louisiana: selected USGS products","docAbstract":"This Digital Data Series (DDS) report is primarily a selection of USGS science products that were previously published as paper atlases and maps but are no longer available in their original form. We have made an attempt to preserve the paper atlases by having them scanned in an efficient compressed digital format that provides a print-on-demand as well as a programmed viewing capability of the original material. We included additional materials bearing on aspects to enhance the scientific understanding of coastal erosion and wetland loss in Louisiana. In addition, this report contains multimedia-based publications including photographs, a 48-minute video, and map tools to allow the user to experience the many scientifically based research activities that are in progress along the coast of Louisiana.","language":"ENGLISH","doi":"10.3133/ds79","isbn":"0607954930","usgsCitation":"Williams, S.J., Reid, J.M., Cross, V.A., and Polloni, C.F., 2003, Coastal erosion and wetland change in Louisiana: selected USGS products: U.S. Geological Survey Data Series 79, 1 DVD-ROM : ill. (some col.), maps (some col.); 4 3/4 in., https://doi.org/10.3133/ds79.","productDescription":"1 DVD-ROM : ill. (some col.), maps (some col.); 4 3/4 in.","costCenters":[{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":179195,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8196,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/dds/dds79/","linkFileType":{"id":5,"text":"html"}},{"id":8198,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/dds/dds79/HTMLDOCS/catalog.htm","linkFileType":{"id":5,"text":"html"}},{"id":8197,"rank":9999,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/dds/dds79/HTMLDOCS/readme.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeaff","contributors":{"authors":[{"text":"Williams, S. Jeffress 0000-0002-1326-7420 jwilliams@usgs.gov","orcid":"https://orcid.org/0000-0002-1326-7420","contributorId":2063,"corporation":false,"usgs":true,"family":"Williams","given":"S.","email":"jwilliams@usgs.gov","middleInitial":"Jeffress","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":246784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, Jamey M.","contributorId":68386,"corporation":false,"usgs":true,"family":"Reid","given":"Jamey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246785,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cross, VeeAnn A.","contributorId":103311,"corporation":false,"usgs":true,"family":"Cross","given":"VeeAnn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":246787,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Polloni, Christopher F.","contributorId":93087,"corporation":false,"usgs":true,"family":"Polloni","given":"Christopher","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":246786,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53628,"text":"pp1675 - 2003 - Hydrological, chemical, and biological characteristics of a prairie pothole wetland complex under highly variable climate conditions: The Cottonwood Lake area, east-central North Dakota","interactions":[],"lastModifiedDate":"2024-06-17T20:22:49.253759","indexId":"pp1675","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1675","title":"Hydrological, chemical, and biological characteristics of a prairie pothole wetland complex under highly variable climate conditions: The Cottonwood Lake area, east-central North Dakota","docAbstract":"<p>Geologic deposits in the Cottonwood Lake area consist largely of silty, clayey glacial till that contains numerous fractures and small, randomly distributed sand and gravel deposits. The sand deposits can have a substantial effect on groundwater flow between wetlands in the area and can cause some to drain while others have relatively stable inflow. Direct precipitation and runoff from snowmelt are the primary sources of water to the wetlands and evaporation accounts for the largest loss of water from the wetlands. The wetlands in the study area have a range of functions with respect to their interaction with ground water. Some of the seasonal wetlands recharge ground water and others recharge ground water and receive ground-water discharge. The semipermanent wetlands receive ground-water discharge much of the time, but some have reversals of flow between them and the groundwater system nearly every year. Ground-water flow toward the wetlands is caused by recharge in the uplands and by focused recharge near the wetland perimeters. Flow from the semipermanent wetlands to the ground-water system occurs when the wetland water levels are higher than the contiguous water table, resulting in bank storage, and when evapotranspiration directly from the ground-water system causes seepage around the wetland perimeters. Substantial climate variability during the study period caused the wetlands to range from being completely dry to having such high water levels that some of the wetlands merged to become large lakes. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp1675","isbn":"0607894318","usgsCitation":"Winter, T.C., Rosenberry, D.O., LaBaugh, J.W., Swanson, G.A., Euliss, N., Hanson, B.A., Mushet, D.M., Poiani, K.A., and Johnson, W., 2003, Hydrological, chemical, and biological characteristics of a prairie pothole wetland complex under highly variable climate conditions: The Cottonwood Lake area, east-central North Dakota: U.S. Geological Survey Professional Paper 1675, xii, 109 p., https://doi.org/10.3133/pp1675.","productDescription":"xii, 109 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":430333,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68873.htm","linkFileType":{"id":5,"text":"html"}},{"id":87490,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1675/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120702,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1675/report-thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Cottonwood Lake area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -100.6873102516428,\n              47.88744597352692\n            ],\n            [\n              -100.6873102516428,\n              47.85382694765144\n            ],\n            [\n              -100.64658994226839,\n              47.85382694765144\n            ],\n            [\n              -100.64658994226839,\n              47.88744597352692\n            ],\n            [\n              -100.6873102516428,\n              47.88744597352692\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e947","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":247951,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenberry, Donald O. 0000-0003-0681-5641 rosenber@usgs.gov","orcid":"https://orcid.org/0000-0003-0681-5641","contributorId":1312,"corporation":false,"usgs":true,"family":"Rosenberry","given":"Donald","email":"rosenber@usgs.gov","middleInitial":"O.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":904313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LaBaugh, James W. 0000-0002-4112-2536 jlabaugh@usgs.gov","orcid":"https://orcid.org/0000-0002-4112-2536","contributorId":1311,"corporation":false,"usgs":true,"family":"LaBaugh","given":"James","email":"jlabaugh@usgs.gov","middleInitial":"W.","affiliations":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true}],"preferred":true,"id":904314,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swanson, George A.","contributorId":49654,"corporation":false,"usgs":true,"family":"Swanson","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":904315,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Euliss, Ned H. Jr.","contributorId":178233,"corporation":false,"usgs":false,"family":"Euliss","given":"Ned H. Jr.","affiliations":[],"preferred":false,"id":904316,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hanson, Bruce A.","contributorId":193072,"corporation":false,"usgs":false,"family":"Hanson","given":"Bruce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":904317,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mushet, David M. 0000-0002-5910-2744 dmushet@usgs.gov","orcid":"https://orcid.org/0000-0002-5910-2744","contributorId":1299,"corporation":false,"usgs":true,"family":"Mushet","given":"David","email":"dmushet@usgs.gov","middleInitial":"M.","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":904318,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Poiani, Karen A.","contributorId":86280,"corporation":false,"usgs":true,"family":"Poiani","given":"Karen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":904319,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Johnson, W. Carter","contributorId":17548,"corporation":false,"usgs":true,"family":"Johnson","given":"W. Carter","affiliations":[],"preferred":false,"id":904320,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":53243,"text":"ofr03488 - 2003 - Logs and Data from Trenches Across the Hayward Fault at Tyson's Lagoon (Tule Pond), Fremont, Alameda County, California, 2001-2003","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr03488","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-488","title":"Logs and Data from Trenches Across the Hayward Fault at Tyson's Lagoon (Tule Pond), Fremont, Alameda County, California, 2001-2003","language":"ENGLISH","doi":"10.3133/ofr03488","usgsCitation":"Lienkaemper, J.J., Williams, P.L., Dawson, T.E., Personius, S.F., Seitz, G., Heller, S., and Schwartz, D.P., 2003, Logs and Data from Trenches Across the Hayward Fault at Tyson's Lagoon (Tule Pond), Fremont, Alameda County, California, 2001-2003 (Version 2.0): U.S. Geological Survey Open-File Report 2003-488, 6 p. and 8 sheets, https://doi.org/10.3133/ofr03488.","productDescription":"6 p. and 8 sheets","costCenters":[],"links":[{"id":178223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4896,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-488/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 2.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c5c3","contributors":{"authors":[{"text":"Lienkaemper, James J. 0000-0002-7578-7042 jlienk@usgs.gov","orcid":"https://orcid.org/0000-0002-7578-7042","contributorId":1941,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"James","email":"jlienk@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":247032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Patrick L.","contributorId":70472,"corporation":false,"usgs":true,"family":"Williams","given":"Patrick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":247036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, Timothy E.","contributorId":24429,"corporation":false,"usgs":false,"family":"Dawson","given":"Timothy","email":"","middleInitial":"E.","affiliations":[{"id":7099,"text":"Calif. Geol. Survey","active":true,"usgs":false}],"preferred":false,"id":247034,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Personius, Stephen F. personius@usgs.gov","contributorId":1214,"corporation":false,"usgs":true,"family":"Personius","given":"Stephen","email":"personius@usgs.gov","middleInitial":"F.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":247030,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Seitz, Gordon G.","contributorId":17303,"corporation":false,"usgs":false,"family":"Seitz","given":"Gordon G.","affiliations":[{"id":7099,"text":"Calif. Geol. Survey","active":true,"usgs":false}],"preferred":false,"id":247033,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Heller, Samuel J.","contributorId":25633,"corporation":false,"usgs":true,"family":"Heller","given":"Samuel J.","affiliations":[],"preferred":false,"id":247035,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schwartz, David P. 0000-0001-5193-9200 dschwartz@usgs.gov","orcid":"https://orcid.org/0000-0001-5193-9200","contributorId":1940,"corporation":false,"usgs":true,"family":"Schwartz","given":"David","email":"dschwartz@usgs.gov","middleInitial":"P.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":247031,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":53392,"text":"b2213 - 2003 - Resource potential and geology of the Grand Mesa, Uncompahgre, and Gunnison (GMUG) National Forests and vicinity, Colorado","interactions":[],"lastModifiedDate":"2025-08-21T20:31:38.453725","indexId":"b2213","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2213","title":"Resource potential and geology of the Grand Mesa, Uncompahgre, and Gunnison (GMUG) National Forests and vicinity, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2213","usgsCitation":"Bankey, V., 2003, Resource potential and geology of the Grand Mesa, Uncompahgre, and Gunnison (GMUG) National Forests and vicinity, Colorado (Version 1.0): U.S. Geological Survey Bulletin 2213, viii, 276 p., https://doi.org/10.3133/b2213.","productDescription":"viii, 276 p.","costCenters":[],"links":[{"id":178765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402020,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62645.htm"},{"id":5172,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/2213/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Grand Mesa, Uncompahgre, and Gunnison (GMUG) National Forests","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.95690917968749,\n              37.65773212628272\n            ],\n            [\n              -105.8477783203125,\n              37.65773212628272\n            ],\n            [\n              -105.8477783203125,\n              39.33429742980725\n            ],\n            [\n              -108.95690917968749,\n              39.33429742980725\n            ],\n            [\n              -108.95690917968749,\n              37.65773212628272\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629dcf","contributors":{"authors":[{"text":"Bankey, Viki viki@usgs.gov","contributorId":1238,"corporation":false,"usgs":true,"family":"Bankey","given":"Viki","email":"viki@usgs.gov","affiliations":[],"preferred":true,"id":247486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53739,"text":"wri034046 - 2003 - Oxidation-reduction processes in ground water at Naval Weapons Industrial Reserve Plant, Dallas, Texas","interactions":[],"lastModifiedDate":"2017-02-15T13:15:35","indexId":"wri034046","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4046","title":"Oxidation-reduction processes in ground water at Naval Weapons Industrial Reserve Plant, Dallas, Texas","docAbstract":"Concentrations of trichloroethene in ground water at the Naval Weapons Industrial Reserve Plant in Dallas, Texas, indicate three source areas of chlorinated solvents?building 1, building 6, and an off-site source west of the facility. The presence of daughter products of reductive dechlorination of trichloroethene, which were not used at the facility, south and southwest of the source areas are evidence that reductive dechlorination is occurring. In places south of the source areas, dissolved oxygen concentrations indicated that reduction of oxygen could be the dominant process, particularly south of building 6; but elevated dissolved oxygen concentrations south of building 6 might be caused by a leaking water or sewer pipe. The nitrite data indicate that denitrification is occurring in places; however, dissolved hydrogen concentrations indicate that iron reduction is the dominant process south of building 6. The distributions of ferrous iron indicate that iron reduction is occurring in places south-southwest of buildings 6 and 1; dissolved hydrogen concentrations generally support the interpretation that iron reduction is the dominant process in those places. The generally low concentrations of sulfide indicate that sulfate reduction is not a key process in most sampled areas, an interpretation that is supported by dissolved hydrogen concentrations. Ferrous iron and dissolved hydrogen concentrations indicate that ferric iron reduction is the primary oxidation-reduction process. Application of mean first-order decay rates in iron-reducing conditions for trichloroethene, dichloroethene, and vinyl chloride yielded half-lives for those solvents of 231, 347, and 2.67 days, respectively. Decay rates, and thus half-lives, at the facility are expected to be similar to those computed. A weighted scoring method to indicate sites where reductive dechlorination might be likely to occur indicated strong evidence for anaerobic biodegradation of chlorinated solvents at six sites. In general, scores were highest for samples collected on the northeast side of the facility.","language":"English","doi":"10.3133/wri034046","collaboration":"In cooperation with the Southern Division Naval Facilities Engineering Command ","usgsCitation":"Jones, S., Braun, C.L., and Lee, R.W., 2003, Oxidation-reduction processes in ground water at Naval Weapons Industrial Reserve Plant, Dallas, Texas: U.S. Geological Survey Water-Resources Investigations Report 2003-4046, HTML Document; Report: iv, 37 p., https://doi.org/10.3133/wri034046.","productDescription":"HTML Document; Report: iv, 37 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":124700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_2003_4046.jpg"},{"id":5101,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri03-4046/","linkFileType":{"id":5,"text":"html"}},{"id":335548,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri03-4046/pdf/wri03-4046.pdf","text":"Report","size":"1.65 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Dallas","otherGeospatial":"Naval Weapons Industrial Reserve Plant","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97,\n              32.75\n            ],\n            [\n              -96.95,\n              32.75\n            ],\n            [\n              -96.95,\n              32.7\n            ],\n            [\n              -97,\n              32.7\n            ],\n            [\n              -97,\n              32.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e483be4b07f02db4f12d9","contributors":{"authors":[{"text":"Jones, S.A.","contributorId":38596,"corporation":false,"usgs":true,"family":"Jones","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":248270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braun, Christopher L. 0000-0002-5540-2854 clbraun@usgs.gov","orcid":"https://orcid.org/0000-0002-5540-2854","contributorId":925,"corporation":false,"usgs":true,"family":"Braun","given":"Christopher","email":"clbraun@usgs.gov","middleInitial":"L.","affiliations":[{"id":48595,"text":"Oklahoma-Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248269,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":248271,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53577,"text":"wri034076 - 2003 - Aquatic assemblages and their relation to temperature variables of least-disturbed streams in the Salmon River basin, central Idaho, 2001","interactions":[],"lastModifiedDate":"2014-05-05T14:51:35","indexId":"wri034076","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4076","title":"Aquatic assemblages and their relation to temperature variables of least-disturbed streams in the Salmon River basin, central Idaho, 2001","docAbstract":"In the late 1990s, Idaho’s established stream\ntemperature criteria for the protection of coldwater\nbiota and salmonid spawning were considered\ninadequate because the criteria did not agree with\nobserved biological conditions in many instances\nand did not allow for variability in environmental\ncondition or species diversity across a broad area\nsuch as the entire State of Idaho.\nIn 2001, benthic invertebrate and fish assemblages\nin 34 least-disturbed streams in the Salmon\nRiver Basin, central Idaho, were evaluated in relation\nto stream temperature and other environmental\nvariables. The Salmon River Basin retains\nwatersheds that are minimally affected by human\nactivities. These “natural” stream conditions provide\na basis for deriving attainable stream temperatures\nthat can be used to set new, and revise existing,\nwater-quality criteria for stream habitats\naffected by human activities.\nDuring July through September 2001, data\nwere collected to document the thermal regime of\nleast-disturbed streams, characterize the distribution\nof aquatic biota at streams representing a gradient\nof temperature, and describe the relations\nbetween environmental variables and benthic\ninvertebrate and fish assemblages. Nine stream\ntemperature metrics were compared with the U.S.\nEnvironmental Protection Agency’s criterion of\n10\n°\nC (degrees Celsius) for bull trout spawning and\njuvenile rearing. The maximum weekly-maximum\ntemperature at all 33 sites where temperature data\nwere available exceeded this criterion. The maximum\ndaily-maximum temperature (MDMT) at 30\nof the sites exceeded the Idaho Department of\nEnvironmental Quality (IDEQ) criterion of 13.0\n°\nC\nfor the protection of salmonid spawning; and the\nmaximum daily-average temperature at all 33 sites\nexceeded the 9.0\n°\nC criterion for the protection of\nsalmonid spawning. The thermal regime at most\nsites did not exceed the IDEQ criteria for the protection\nof coldwater biota. Nine environmental\nvariables—water-surface gradient, discharge,\nwetted channel width, width:depth ratio, aspect,\ntotal seasonal thermal input, open canopy, riparian\ncanopy density, and elevation were selected for\ncorrelation with the nine stream temperature metrics.\nElevation showed the strongest inverse correlation\nwith the stream temperature metrics.\nTwo hundred and one benthic invertebrate\ntaxa from the 34 sampling sites were identified.\nThe most abundant taxa were <i>Baetis tricaudatus</i>,\nOligochaeta, <i>Tvetenia bavarica</i> gr., Acari,\n<i>Rhithrogena</i>, <i>Cinygmula</i>, <i>Heterlimnius</i>,\n<i>Micropsectra</i>, <i>Eukiefferiella devonica</i> gr.,\n<i>Drunella doddsi</i>, and <i>Cricotopus</i>. Of the 201\nbenthic invertebrate taxa collected during this\nstudy, 57 taxa (present at a minimum of 5 sampling\nsites) were significantly correlated with one\nor more of the stream temperature metrics. Among\nthe invertebrate taxa collected, 32 were identified\nas coldwater taxa. Of the coldwater taxa collected,\n<i>Zapada oregonensis</i> gr. showed the strongest\ninverse correlation with the stream temperature\nmetrics and was collected at sites where maximum\nweekly-maximum temperature (based on date of\nsample and 6 days prior) ranged from 11.3\n° to\n18.5\n°C.\nTen species of fish in the families Salmonidae,\nCottidae, and Cyprinidae were collected.\nTwo species (bull trout and chinook salmon) listed\nas threatened under the U.S. Fish and Wildlife Service\nEndangered Species Act were collected.\nAmong all species, bull trout showed the strongest\ninverse correlation between relative fish abundance\nand stream temperature. Bull trout and juvenile\nbull trout densities were inversely correlated with stream temperature. The probability of occurrence\nof juvenile bull trout was significantly correlated\nwith MDMT on the basis of results from a\nlogistic regression model developed during this\nstudy. However, this model differed from a similar\nmodel developed by the U.S. Forest Service on the\nbasis of regional data collected in the Pacific\nNorthwest. The regression model based on data\ncollected during this study showed higher probabilities\nof occurrence of bull trout at colder stream\ntemperatures (10\n° to 15\n°\nC) and lower probabilities\nof occurrence at warmer stream temperatures (16\n°\nto 21\n°\nC) than did the model based on regional\ndata. The model comparisons suggest that regional\nor local differences need to be considered when\nderiving stream temperature criteria.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri034076","collaboration":"Prepared in cooperation with Idaho Department of Environmental Quality","usgsCitation":"Ott, D.S., and Maret, T.R., 2003, Aquatic assemblages and their relation to temperature variables of least-disturbed streams in the Salmon River basin, central Idaho, 2001: U.S. Geological Survey Water-Resources Investigations Report 2003-4076, Report: v, 45 p.; Data files, https://doi.org/10.3133/wri034076.","productDescription":"Report: v, 45 p.; Data files","numberOfPages":"52","temporalStart":"2001-07-01","temporalEnd":"2001-09-30","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":262378,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2003/4076/report.pdf"},{"id":262379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2003/4076/report-thumb.jpg"},{"id":286901,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/wri/2003/4076/data/"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0656,43.7998 ], [ -117.0656,46.062 ], [ -112.9153,46.062 ], [ -112.9153,43.7998 ], [ -117.0656,43.7998 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a0c4","contributors":{"authors":[{"text":"Ott, Douglas S. dott@usgs.gov","contributorId":3552,"corporation":false,"usgs":true,"family":"Ott","given":"Douglas","email":"dott@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":247836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maret, Terry R. trmaret@usgs.gov","contributorId":953,"corporation":false,"usgs":true,"family":"Maret","given":"Terry","email":"trmaret@usgs.gov","middleInitial":"R.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247835,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53597,"text":"wri034136 - 2003 - Environmental effects of the Big Rapids dam remnant removal, Big Rapids, Michigan, 2000-02","interactions":[],"lastModifiedDate":"2016-10-06T11:55:16","indexId":"wri034136","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-4136","title":"Environmental effects of the Big Rapids dam remnant removal, Big Rapids, Michigan, 2000-02","docAbstract":"<p>The U.S. Geological Survey (USGS), in cooperation with the city of Big Rapids, investigated the environmental effects of removal of a dam-foundation remnant and downstream cofferdam from the Muskegon River in Big Rapids, Mich. The USGS applied a multidiscipline approach, which determined the water quality, sediment character, and stream habitat before and after dam removal. Continuous water-quality data and discrete water-quality samples were collected, the movement of suspended and bed sediment were measured, changes in stream habitat were assessed, and streambed elevations were surveyed. </p><p>Analyses of water upstream and downstream from the dam showed that the dam-foundation remnant did not affect water quality. Dissolved-oxygen concentrations downstream from the dam remnant were depressed for a short period (days) during the beginning of the dam removal, in part because of that removal effort. Sediment transport from July 2000 through March 2002 was 13,800 cubic yards more at the downstream site than the upstream site. This increase in sediment represents the remobilized sediment upstream from the dam, bank erosion when the impoundment was lowered, and contributions from small tributaries between the sites. </p><p>Five habitat reaches were monitored before and after dam-remnant removal. The reaches consisted of a reference reach (A), upstream from the effects of the impoundment; the impoundment (B); and three sites below the impoundment where habitat changes were expected (C, D, and E, in downstream order). Stream-habitat assessment reaches varied in their responses to the dam-remnant removal. Reference reach A was not affected. In impoundment reach B, Great Lakes and Environmental Assessment Section (GLEAS) Procedure 51 ratings went from fair to excellent. For the three downstream reaches, reach C underwent slight habitat degradation, but ratings remained good; reach D underwent slight habitat degradation with ratings changing from excellent to good; and, in an area affected by a 1966 sediment release, reach E habitat rated fair in April 2000 and remained fair in September 2001. The most noticeable habitat change in the three reaches downstream from the dam site was a measurable increase in siltation and embeddedness. </p><p>Bed-elevation profiles show that bed material upstream from the dam site was remobilized as suspended sediment and bedload, and was redeposited in the reaches below the cofferdam. Deposition was greater in the deep, slow-moving pools than the shallow, fast-moving riffles. For the most part, where deposition took place, deposits were less than 1 foot in thickness. In the year following the removal of the cofferdam, much of the sediment deposited below the dam was moved out of the study reach. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri034136","collaboration":"Prepared in cooperation with the City of Big Rapids, Michigan","usgsCitation":"Healy, D.F., Rheaume, S.J., and Simpson, J.A., 2003, Environmental effects of the Big Rapids dam remnant removal, Big Rapids, Michigan, 2000-02: U.S. Geological Survey Water-Resources Investigations Report 2003-4136, vii, 54 p., https://doi.org/10.3133/wri034136.","productDescription":"vii, 54 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":4849,"rank":100,"type":{"id":15,"text":"Index 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F.","contributorId":46514,"corporation":false,"usgs":true,"family":"Healy","given":"Denis","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":247877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rheaume, Stephen J.","contributorId":50512,"corporation":false,"usgs":true,"family":"Rheaume","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":247878,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Simpson, J. Alan","contributorId":82390,"corporation":false,"usgs":true,"family":"Simpson","given":"J.","email":"","middleInitial":"Alan","affiliations":[],"preferred":false,"id":247879,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53242,"text":"ofr03489 - 2003 - Isotopes and ages in the northern Peninsular Ranges batholith, southern California","interactions":[],"lastModifiedDate":"2023-06-22T16:43:10.767691","indexId":"ofr03489","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-489","title":"Isotopes and ages in the northern Peninsular Ranges batholith, southern California","docAbstract":"Strontium, oxygen and lead isotopic and rubidium-strontium geochronologic studies have been completed on Cretaceous and Jurassic (?) granitic rock samples from the northern Peninsular Ranges batholith in southern California. Many of these samples were collected systematically and studied chemically by A. K. Baird and colleagues (Baird and others, 1979). The distribution of these granitic rocks is shown in the Santa Ana, Perris, and San Jacinto Blocks, bounded by the Malibu Coast-Cucamonga, Banning, and San Andreas fault zones, and the Pacific Ocean on the map of the Peninsular Ranges batholith and surrounding area, southern California. The granitic rock names are by Baird and Miesch (1984) who used a modal mineral classification that Bateman and others (1963) used for granitic rocks in the Sierra Nevada batholith. In this classification, granitic rocks have at least 10% quartz. Boundaries between rock types are in terms of the ratio of alkali-feldspar to total feldspar: quartz diorite, 0-10%; granodiorite, 10-35%; quartz monzonite 35-65%; granite >65%. Gabbros have 0-10% quartz.\n\nData for samples investigated are giv in three tables: samples, longitude, latitude, specific gravity and rock type (Table 1); rubidium and strontium data for granitic rocks of the northern Peninsular Ranges batholith, southern California (Table 2); U, Th, Pb concentrations, Pb and Sr initial isotopic compositions, and δ<sup>18</sup>O permil values for granitic rocks of the northern Peninsular Ranges batholith (table 3).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03489","usgsCitation":"Kistler, R., Wooden, J., and Morton, D.M., 2003, Isotopes and ages in the northern Peninsular Ranges batholith, southern California: U.S. Geological Survey Open-File Report 2003-489, 45 p., https://doi.org/10.3133/ofr03489.","productDescription":"45 p.","numberOfPages":"45","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":178222,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4895,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0489/","linkFileType":{"id":5,"text":"html"}},{"id":283984,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0489/pdf/of03-489.pdf"},{"id":407013,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62280.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Peninsular Ranges","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.2333,\n              32.9444\n            ],\n            [\n              -116.0833,\n              32.9444\n            ],\n            [\n              -116.0833,\n              34.0556\n            ],\n            [\n              -117.2333,\n              34.0556\n            ],\n            [\n              -117.2333,\n              32.9444\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667029","contributors":{"authors":[{"text":"Kistler, Ronald W.","contributorId":56969,"corporation":false,"usgs":true,"family":"Kistler","given":"Ronald W.","affiliations":[],"preferred":false,"id":247029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wooden, Joseph L.","contributorId":32209,"corporation":false,"usgs":true,"family":"Wooden","given":"Joseph L.","affiliations":[],"preferred":false,"id":247028,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":247027,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53250,"text":"ofr2003434 - 2003 - Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera","interactions":[{"subject":{"id":53250,"text":"ofr2003434 - 2003 - Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera","indexId":"ofr2003434","publicationYear":"2003","noYear":false,"title":"Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera"},"predicate":"SUPERSEDED_BY","object":{"id":74483,"text":"pp1697 - 2005 - Metallogenesis and tectonics of the Russian Far East, Alaska, and the Canadian Cordillera","indexId":"pp1697","publicationYear":"2005","noYear":false,"title":"Metallogenesis and tectonics of the Russian Far East, Alaska, and the Canadian Cordillera"},"id":1}],"supersededBy":{"id":74483,"text":"pp1697 - 2005 - Metallogenesis and tectonics of the Russian Far East, Alaska, and the Canadian Cordillera","indexId":"pp1697","publicationYear":"2005","noYear":false,"title":"Metallogenesis and tectonics of the Russian Far East, Alaska, and the Canadian Cordillera"},"lastModifiedDate":"2012-02-02T00:11:44","indexId":"ofr2003434","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-434","title":"Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera","language":"ENGLISH","doi":"10.3133/ofr2003434","usgsCitation":"Nokleberg, W.J., Bundtzen, T., Eremin, R.A., Ratkin, V.V., Dawson, K.M., Shpikerman, V.I., Goryachev, N., Byalobzhesky, S.G., Frolov, Y.F., Khanchuk, A.I., Koch, R.D., Monger, J.W., Pozdeev, A.I., Rozenblum, I.S., Rodionov, S.M., Parfenov, L.M., Scotese, C.R., and Sidorov, A.A., 2003, Metallogenesis and Tectonics of the Russian Far East, Alaska, and the Canadian Cordillera (Version 1.0, Superseded by PP 1697): U.S. Geological Survey Open-File Report 2003-434, 425 p., https://doi.org/10.3133/ofr2003434.","productDescription":"425 p.","costCenters":[],"links":[{"id":112006,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/13562","linkFileType":{"id":5,"text":"html"}},{"id":174901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0, Superseded by PP 1697","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db628674","contributors":{"authors":[{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":247054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bundtzen, Thomas K.","contributorId":83560,"corporation":false,"usgs":true,"family":"Bundtzen","given":"Thomas K.","affiliations":[],"preferred":false,"id":247069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eremin, Roman A.","contributorId":105759,"corporation":false,"usgs":true,"family":"Eremin","given":"Roman","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":247071,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ratkin, Vladimir V.","contributorId":79924,"corporation":false,"usgs":true,"family":"Ratkin","given":"Vladimir","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":247068,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dawson, Kenneth M.","contributorId":97525,"corporation":false,"usgs":true,"family":"Dawson","given":"Kenneth","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":247070,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shpikerman, Vladimir I.","contributorId":35766,"corporation":false,"usgs":true,"family":"Shpikerman","given":"Vladimir","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":247060,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Goryachev, Nikolai A.","contributorId":7318,"corporation":false,"usgs":true,"family":"Goryachev","given":"Nikolai A.","affiliations":[],"preferred":false,"id":247056,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Byalobzhesky, Stanislav G.","contributorId":73684,"corporation":false,"usgs":true,"family":"Byalobzhesky","given":"Stanislav","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":247066,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Frolov, Yuri F.","contributorId":16041,"corporation":false,"usgs":true,"family":"Frolov","given":"Yuri","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":247058,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Khanchuk, Alexander I.","contributorId":19585,"corporation":false,"usgs":true,"family":"Khanchuk","given":"Alexander","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":247059,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Koch, Richard D. rkoch@usgs.gov","contributorId":4413,"corporation":false,"usgs":true,"family":"Koch","given":"Richard","email":"rkoch@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":247055,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Monger, James W.H.","contributorId":53900,"corporation":false,"usgs":true,"family":"Monger","given":"James","email":"","middleInitial":"W.H.","affiliations":[],"preferred":false,"id":247062,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Pozdeev, Anany I.","contributorId":10454,"corporation":false,"usgs":true,"family":"Pozdeev","given":"Anany","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":247057,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Rozenblum, Ilya S.","contributorId":77960,"corporation":false,"usgs":true,"family":"Rozenblum","given":"Ilya","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247067,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Rodionov, Sergey M.","contributorId":64726,"corporation":false,"usgs":true,"family":"Rodionov","given":"Sergey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":247064,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Parfenov, Leonid M.","contributorId":59112,"corporation":false,"usgs":true,"family":"Parfenov","given":"Leonid","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":247063,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Scotese, Christopher R.","contributorId":66357,"corporation":false,"usgs":true,"family":"Scotese","given":"Christopher","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":247065,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Sidorov, Anatoly A.","contributorId":36589,"corporation":false,"usgs":true,"family":"Sidorov","given":"Anatoly","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":247061,"contributorType":{"id":1,"text":"Authors"},"rank":18}]}}
,{"id":53395,"text":"ofr03463 - 2003 - Preliminary evaluation of a precipitation threshold for anticipating the occurrence of landslides in the Seattle, Washington, area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr03463","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-463","title":"Preliminary evaluation of a precipitation threshold for anticipating the occurrence of landslides in the Seattle, Washington, area","language":"ENGLISH","doi":"10.3133/ofr03463","usgsCitation":"Chleborad, A.F., 2003, Preliminary evaluation of a precipitation threshold for anticipating the occurrence of landslides in the Seattle, Washington, area (Version 1.0 ): U.S. Geological Survey Open-File Report 2003-463, 15 figs., 5 tables, https://doi.org/10.3133/ofr03463.","productDescription":"15 figs., 5 tables","costCenters":[],"links":[{"id":178874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5174,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-463/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0 ","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c442","contributors":{"authors":[{"text":"Chleborad, Alan F.","contributorId":87578,"corporation":false,"usgs":true,"family":"Chleborad","given":"Alan","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":247495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53222,"text":"ofr03395 - 2003 - USGS Digital Spectral Library splib05a","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr03395","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-395","title":"USGS Digital Spectral Library splib05a","docAbstract":"We have assembled a digital reflectance spectral library of spectra that covers wavelengths from the ultraviolet to near-infrared along with sample documentation. The library includes samples of minerals, rocks, soils, physically constructed as well as mathematically computed mixtures, vegetation, microorganisms, and man-made materials. The samples and spectra collected were assembled for the purpose of using spectral features for the remote detection of these and similar materials.","language":"ENGLISH","doi":"10.3133/ofr03395","usgsCitation":"Clark, R.N., Swayze, G.A., Wise, R.K., Livo, E., Hoefen, T.M., Kokaly, R., and Sutley, S.J., 2003, USGS Digital Spectral Library splib05a (Version 1.0): U.S. Geological Survey Open-File Report 2003-395, 5 figs, 3 tables, https://doi.org/10.3133/ofr03395.","productDescription":"5 figs, 3 tables","costCenters":[],"links":[{"id":179686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4848,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-395/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6271b9","contributors":{"authors":[{"text":"Clark, Roger N. 0000-0002-7021-1220 rclark@usgs.gov","orcid":"https://orcid.org/0000-0002-7021-1220","contributorId":515,"corporation":false,"usgs":true,"family":"Clark","given":"Roger","email":"rclark@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":246975,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swayze, Gregg A. 0000-0002-1814-7823 gswayze@usgs.gov","orcid":"https://orcid.org/0000-0002-1814-7823","contributorId":518,"corporation":false,"usgs":true,"family":"Swayze","given":"Gregg","email":"gswayze@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":246976,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wise, Richard K.","contributorId":71435,"corporation":false,"usgs":true,"family":"Wise","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":246979,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Livo, Eric 0000-0001-7331-8130","orcid":"https://orcid.org/0000-0001-7331-8130","contributorId":52270,"corporation":false,"usgs":true,"family":"Livo","given":"Eric","affiliations":[],"preferred":false,"id":246978,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoefen, Todd M. 0000-0002-3083-5987 thoefen@usgs.gov","orcid":"https://orcid.org/0000-0002-3083-5987","contributorId":403,"corporation":false,"usgs":true,"family":"Hoefen","given":"Todd","email":"thoefen@usgs.gov","middleInitial":"M.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246974,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kokaly, Raymond F. 0000-0003-0276-7101","orcid":"https://orcid.org/0000-0003-0276-7101","contributorId":81442,"corporation":false,"usgs":true,"family":"Kokaly","given":"Raymond F.","affiliations":[],"preferred":false,"id":246980,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Sutley, Steve J.","contributorId":33774,"corporation":false,"usgs":true,"family":"Sutley","given":"Steve","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":246977,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":53730,"text":"ofr03501 - 2003 - Surficial and bedrock geologic map database of the Kelso 7.5 Minute quadrangle, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-06-22T16:42:12.611638","indexId":"ofr03501","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-501","title":"Surficial and bedrock geologic map database of the Kelso 7.5 Minute quadrangle, San Bernardino County, California","docAbstract":"This geologic map database describes geologic materials for the Kelso 7.5 Minute Quadrangle, San Bernardino County, California. The area lies in eastern Mojave Desert of California, within the Mojave National Preserve (a unit of the National Parks system). Geologic deposits in the area consist of Proterozoic metamorphic rocks, Cambrian-Neoproterozoic sedimentary rocks, Mesozoic plutonic and hypabyssal rocks, Tertiary basin fill, and Quaternary surficial deposits. Bedrock deposits are described by composition, texture, and stratigraphic relationships. Quaternary surficial deposits are classified into soil-geomorphic surfaces based on soil characteristics, inset relationships, and geomorphic expression.\n\nThe surficial geology presented in this report is especially useful to understand, and extrapolate, physical properties that influence surface conditions, and surface- and soil-water dynamics. Physical characteristics such as pavement development, soil horizonation, and hydraulic characteristics have shown to be some of the primary drivers of ecologic dynamics, including recovery of those ecosystems to anthropogenic disturbance, in the eastern Mojave Desert and other arid and semi-arid environments.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03501","usgsCitation":"Bedford, D., 2003, Surficial and bedrock geologic map database of the Kelso 7.5 Minute quadrangle, San Bernardino County, California: U.S. Geological Survey Open-File Report 2003-501, 1 Plate: 45.00 x 30.00 inches; Metadata, https://doi.org/10.3133/ofr03501.","productDescription":"1 Plate: 45.00 x 30.00 inches; Metadata","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":179525,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03501.jpg"},{"id":398354,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62491.htm"},{"id":284012,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0501/pdf/of03-501_3a.pdf"},{"id":284006,"rank":10,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_1b.txt"},{"id":284005,"rank":9,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_1b.html"},{"id":284003,"rank":8,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0501/"},{"id":284010,"rank":7,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_2.tar"},{"id":284009,"rank":6,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_2b.e00"},{"id":284008,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_2a.e00"},{"id":284007,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_1bfaq.html"},{"id":284011,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_3a.eps"},{"id":284004,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0501/of03-501_1revs.txt"}],"scale":"24000","projection":"Universal Transverse Mercator projection","datum":"National Geodetic Datum of 1929","country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Kelso 7.5 minute quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.75,35.0 ], [ -115.75,35.125 ], [ -115.625,35.125 ], [ -115.625,35.0 ], [ -115.75,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689461","contributors":{"authors":[{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":248248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53722,"text":"ofr03452 - 2003 - Specific sequestration volumes; a useful tool for CO<sub>2</sub> storage capacity assessment","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr03452","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2003-452","title":"Specific sequestration volumes; a useful tool for CO<sub>2</sub> storage capacity assessment","language":"ENGLISH","doi":"10.3133/ofr03452","usgsCitation":"Brennan, S.T., and Burruss, R.A., 2003, Specific sequestration volumes; a useful tool for CO<sub>2</sub> storage capacity assessment (Version 1.0): U.S. Geological Survey Open-File Report 2003-452, 14 p., https://doi.org/10.3133/ofr03452.","productDescription":"14 p.","costCenters":[],"links":[{"id":177351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5064,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-452/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e8a","contributors":{"authors":[{"text":"Brennan, Sean T. 0000-0002-7102-9359 sbrennan@usgs.gov","orcid":"https://orcid.org/0000-0002-7102-9359","contributorId":559,"corporation":false,"usgs":true,"family":"Brennan","given":"Sean","email":"sbrennan@usgs.gov","middleInitial":"T.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":248226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burruss, Robert A. 0000-0001-6827-804X burruss@usgs.gov","orcid":"https://orcid.org/0000-0001-6827-804X","contributorId":558,"corporation":false,"usgs":true,"family":"Burruss","given":"Robert","email":"burruss@usgs.gov","middleInitial":"A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":248225,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69695,"text":"mf2418 - 2003 - Geologic map of upper Clayhole Valley and vicinity, Mohave County, northwestern Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:34","indexId":"mf2418","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2003","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":"2418","title":"Geologic map of upper Clayhole Valley and vicinity, Mohave County, northwestern Arizona","docAbstract":"      This digital map database is compiled from unpublished data and new mapping by the authors and represents the general distribution of surficial and bedrock geology in the mapped area. Together with the accompanying pamphlet, it provides current information on the geologic structure and stratigraphy of the area. The database delineates map units that are identified by age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution of the database to 1:31,680 or smaller.","language":"ENGLISH","doi":"10.3133/mf2418","usgsCitation":"Billingsley, G.H., and Priest, S.S., 2003, Geologic map of upper Clayhole Valley and vicinity, Mohave County, northwestern Arizona (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2418, 29 p. and 1 sheet, https://doi.org/10.3133/mf2418.","productDescription":"29 p. and 1 sheet","costCenters":[],"links":[{"id":110431,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_55231.htm","linkFileType":{"id":5,"text":"html"},"description":"55231"},{"id":6368,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2003/2418/","linkFileType":{"id":5,"text":"html"}},{"id":191049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"31680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.25,36.5 ], [ -113.25,36.75 ], [ -113,36.75 ], [ -113,36.5 ], [ -113.25,36.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688786","contributors":{"authors":[{"text":"Billingsley, George H.","contributorId":20711,"corporation":false,"usgs":true,"family":"Billingsley","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":280914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Priest, Susan S. spriest@usgs.gov","contributorId":30204,"corporation":false,"usgs":true,"family":"Priest","given":"Susan","email":"spriest@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":false,"id":280915,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}