{"pageNumber":"2937","pageRowStart":"73400","pageSize":"25","recordCount":184563,"records":[{"id":50532,"text":"ofr02379 - 2002 - Emergency assessment of potential debris-flow peak discharges, Coal Seam fire, Colorado","interactions":[],"lastModifiedDate":"2022-11-01T19:01:34.186458","indexId":"ofr02379","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-379","title":"Emergency assessment of potential debris-flow peak discharges, Coal Seam fire, Colorado","docAbstract":"<p>These maps present the results of assessments of peak discharges that can potentially be generated by debris flows issuing from the basins burned by the Coal Seam fire of June and July 2002, near Glenwood Springs, Colorado. The maps are based on a regression model for debris-flow peak discharge normalized by average storm intensity as a function of basin gradient and burned extent, and limited field checking. A range of potential peak discharges that could potentially be produced from each of the burned basins between 1 ft<sup>3</sup>/s (0.03 m<sup>3</sup>/s) and greater than 5,000 ft<sup>3</sup>/s (&gt;141 m<sup>3</sup>/s) is calculated for the 5-year, 1-hour storm of 0.80 inches (20 mm). The 25-year, 1-hour storm of 1.3 inches (33 mm). The 100- year, 1-hour storm of 1.8 inches (46 mm) produced peak discharges between 1 and greater than 8,000 ft<sup>3</sup>/s (&gt;227 m<sup>3</sup>/s). These maps are intended for use by emergency personnel to aid in the preliminary design of mitigation measures, and the planning of evacuation timing and routes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02379","usgsCitation":"Cannon, S.H., Michael, J.A., Gartner, J.E., Rea, A.H., and Garcia, S.P., 2002, Emergency assessment of potential debris-flow peak discharges, Coal Seam fire, Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2002-379, 1 Plate: 53.00 × 36.00 inches, https://doi.org/10.3133/ofr02379.","productDescription":"1 Plate: 53.00 × 36.00 inches","costCenters":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"links":[{"id":409006,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52356.htm","linkFileType":{"id":5,"text":"html"}},{"id":178354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4344,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0379/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Coal Seam fire","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.4583,\n              39.633\n            ],\n            [\n              -107.4583,\n              39.5\n            ],\n            [\n              -107.2917,\n              39.5\n            ],\n            [\n              -107.2917,\n              39.633\n            ],\n            [\n              -107.4583,\n              39.633\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60597a","contributors":{"authors":[{"text":"Cannon, Susan H. cannon@usgs.gov","contributorId":1019,"corporation":false,"usgs":true,"family":"Cannon","given":"Susan","email":"cannon@usgs.gov","middleInitial":"H.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":241715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michael, John A. jmichael@usgs.gov","contributorId":1877,"corporation":false,"usgs":true,"family":"Michael","given":"John","email":"jmichael@usgs.gov","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":241718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gartner, Joseph E. jegartner@usgs.gov","contributorId":1876,"corporation":false,"usgs":true,"family":"Gartner","given":"Joseph","email":"jegartner@usgs.gov","middleInitial":"E.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":241717,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rea, Alan H. ahrea@usgs.gov","contributorId":1813,"corporation":false,"usgs":true,"family":"Rea","given":"Alan","email":"ahrea@usgs.gov","middleInitial":"H.","affiliations":[{"id":423,"text":"National Geospatial Program","active":true,"usgs":true}],"preferred":true,"id":241716,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Garcia, Steven P.","contributorId":78009,"corporation":false,"usgs":true,"family":"Garcia","given":"Steven","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":241719,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50516,"text":"ofr02342 - 2002 - Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 2000 through December 31, 2001","interactions":[],"lastModifiedDate":"2016-09-07T15:08:43","indexId":"ofr02342","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-342","title":"Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 2000 through December 31, 2001","docAbstract":"<p>The Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, the Geophysical Institute of the University of Alaska Fairbanks, and the Alaska Division of Geological and Geophysical Surveys, has maintained seismic monitoring networks at potentially active volcanoes in Alaska since 1988 (Power and others, 1993; Jolly and others, 1996; Jolly and others, 2001). The primary objectives of this program are the seismic surveillance of active, potentially hazardous, Alaskan volcanoes and the investigation of seismic processes associated with active volcanism. This catalog reflects the status and evolution of the seismic monitoring program, and presents the basic seismic data for the time period January 1, 2000, through December 31, 2001. For an interpretation of these data and previously recorded data, the reader should refer to several recent articles on volcano related seismicity on Alaskan volcanoes in Appendix G.</p><p>The AVO seismic network was used to monitor twenty-three volcanoes in real time in 2000-2001. These include Mount Wrangell, Mount Spurr, Redoubt Volcano, Iliamna Volcano, Augustine Volcano, Katmai Volcanic Group (Snowy Mountain, Mount Griggs, Mount Katmai, Novarupta, Trident Volcano, Mount Mageik, Mount Martin), Aniakchak Crater, Pavlof Volcano, Mount Dutton, Isanotski Peaks, Shishaldin Volcano, Fisher Caldera, Westdahl Peak, Akutan Peak, Makushin Volcano, Great Sitkin Volcano, and Kanaga Volcano (Figure 1). AVO located 1551 and 1428 earthquakes in 2000 and 2001, respectively, on and around these volcanoes.</p><p>Highlights of the catalog period (Table 1) include: volcanogenic seismic swarms at Shishaldin Volcano between January and February 2000 and between May and June 2000; an eruption at Mount Cleveland between February and May 2001; episodes of possible tremor at Makushin Volcano starting March 2001 and continuing through 2001, and two earthquake swarms at Great Sitkin Volcano in 2001.</p><p>This catalog includes: (1) earthquake origin times, hypocenters, and magnitudes with summary statistics describing the earthquake location quality; (2) a description of instruments deployed in the field and their locations; (3) a description of earthquake detection, recording, analysis, and data archival systems; (4) station parameters and velocity models used for earthquake locations; (5) a summary of daily station usage throughout the catalog period; and (6) all HYPOELLIPSE files used to determine the earthquake locations presented in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02342","usgsCitation":"Dixon, J.P., Stihler, S.D., Power, J.A., Tytgat, G., Estes, S., Moran, S.C., Paskievitch, J., and McNutt, S.R., 2002, Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 2000 through December 31, 2001: U.S. Geological Survey Open-File Report 2002-342, Report: PDF, 56 p.; Report: TXT; Appendix F; Data, https://doi.org/10.3133/ofr02342.","productDescription":"Report: PDF, 56 p.; Report: TXT; Appendix F; Data","numberOfPages":"56","additionalOnlineFiles":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":176638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02342.jpg"},{"id":283822,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/of/2002/0342/catalogavo.txt"},{"id":283821,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0342/pdf/of02-342.pdf","text":"Report","size":"5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":283823,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2002/0342/pdf/appendixf.pdf","text":"Appendix F","size":"3.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Appendix F"},{"id":283824,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0342/avocatalog2000_2001.tar.z.Z","text":"Data Files","size":"2.7 MB","description":"Data Files"},{"id":4328,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0342/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,51.21 ], [ -180.0,67.0 ], [ -140.0,67.0 ], [ -140.0,51.21 ], [ -180.0,51.21 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef8a2","contributors":{"authors":[{"text":"Dixon, James P. 0000-0002-8478-9971 jpdixon@usgs.gov","orcid":"https://orcid.org/0000-0002-8478-9971","contributorId":3163,"corporation":false,"usgs":true,"family":"Dixon","given":"James","email":"jpdixon@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":241658,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stihler, Scott D.","contributorId":31373,"corporation":false,"usgs":true,"family":"Stihler","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":241659,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Power, John A. 0000-0002-7233-4398 jpower@usgs.gov","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":2768,"corporation":false,"usgs":true,"family":"Power","given":"John","email":"jpower@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":241657,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tytgat, Guy","contributorId":71152,"corporation":false,"usgs":true,"family":"Tytgat","given":"Guy","email":"","affiliations":[],"preferred":false,"id":241662,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Estes, Steve","contributorId":55881,"corporation":false,"usgs":true,"family":"Estes","given":"Steve","email":"","affiliations":[],"preferred":false,"id":241661,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Moran, Seth C. 0000-0001-7308-9649 smoran@usgs.gov","orcid":"https://orcid.org/0000-0001-7308-9649","contributorId":548,"corporation":false,"usgs":true,"family":"Moran","given":"Seth","email":"smoran@usgs.gov","middleInitial":"C.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":241656,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Paskievitch, John","contributorId":74050,"corporation":false,"usgs":true,"family":"Paskievitch","given":"John","affiliations":[],"preferred":false,"id":241663,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"McNutt, Stephen R.","contributorId":38133,"corporation":false,"usgs":true,"family":"McNutt","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":241660,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":51127,"text":"ofr2002368 - 2002 - High-Resolution Multichannel Seismic-Reflection Data Acquired in the Northern Gulf of Mexico, 1998-99","interactions":[],"lastModifiedDate":"2012-02-10T00:10:10","indexId":"ofr2002368","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-368","title":"High-Resolution Multichannel Seismic-Reflection Data Acquired in the Northern Gulf of Mexico, 1998-99","docAbstract":"During June 1998 and April 1999, the U.S. Geological Survey (USGS) conducted two research cruises in the northern Gulf of Mexico to acquire high-resolution seismic reflection data across the upper and middle continental slope as part of an investigation of the seismic character, distribution, and potential effects of naturally-occurring marine gas hydrates and related free gas within the gas hydrate stability zone. Over 1600 km of two-dimensional multichannel seismic reflection profiles were acquired during these two cruises. The specific objectives of this investigation are (a) to produce high-resolution images of the gas hydrate stability zone; (b) to study the distribution and character of potential seafloor failures and their relationship to known and inferred gas hydrate deposits; (c) to look at systematic variations in subsurface structure in gas hydrate and non-hydrate areas; and (d) to estimate, if possible, the amounts of hydrates present within the gas hydrate stability zone. The multichannel profiles provide high-quality images with approximately 5 meters of vertical resolution and up to 2 km of penetration. This report gives an overview of the acquisition and data processing of the multichannel seismic reflection profiles and provides references and links to reports with more detailed information. Geologic interpretations of these seismic profiles regarding gas hydrate occurrence and distribution within the study areas of this investigation are given in Cooper and Hart (2002).","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr2002368","usgsCitation":"Hart, P.E., Cooper, A.K., Twichell, D.C., Lee, M., and Agena, W., 2002, High-Resolution Multichannel Seismic-Reflection Data Acquired in the Northern Gulf of Mexico, 1998-99 (Version 1.0): U.S. Geological Survey Open-File Report 2002-368, Available online only, https://doi.org/10.3133/ofr2002368.","productDescription":"Available online only","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1998-06-01","temporalEnd":"1999-04-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":179208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11505,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-368/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98,25 ], [ -98,32 ], [ -79,32 ], [ -79,25 ], [ -98,25 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635699","contributors":{"authors":[{"text":"Hart, Patrick E. 0000-0002-5080-1426 hart@usgs.gov","orcid":"https://orcid.org/0000-0002-5080-1426","contributorId":2879,"corporation":false,"usgs":true,"family":"Hart","given":"Patrick","email":"hart@usgs.gov","middleInitial":"E.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":242997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooper, Alan K. acooper@usgs.gov","contributorId":2854,"corporation":false,"usgs":true,"family":"Cooper","given":"Alan","email":"acooper@usgs.gov","middleInitial":"K.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":242996,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":243000,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lee, Myung","contributorId":13690,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","affiliations":[],"preferred":false,"id":242998,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Agena, Warren","contributorId":35001,"corporation":false,"usgs":true,"family":"Agena","given":"Warren","email":"","affiliations":[],"preferred":false,"id":242999,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":51126,"text":"ofr02324 - 2002 - Digital soils survey map of the Patagonia Mountains, Arizona","interactions":[],"lastModifiedDate":"2014-03-13T13:04:19","indexId":"ofr02324","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-324","title":"Digital soils survey map of the Patagonia Mountains, Arizona","docAbstract":"<p>The ‘Soil Survey of Santa Cruz and Parts of Cochise\n      and Pima Counties, Arizona,' a product of the USDA’s\n      Soil Conservation Service and the Forest Service in\n      cooperation with the Arizona Agricultural Experiment\n      Station, released in 1979, was created according to\n      the site conditions in 1971, when soil scientists\n      identified soils types on aerial photographs. The\n      scale at which these maps were published is 1:20,000.</p>\n<br/>\n      <p>These soil maps were automated for incorporation into\n      the hydrologic modeling within a GIS. The aerial photos\n      onto which the soils units were drawn had not been\n      orthoganalized, and contained distortion. A total of 15\n      maps composed the study area. These maps were scanned\n      into TIFF format using an 8-bit black and white drum\n      scanner at 100 dpi. The images were imported into ERDAS\n      IMAGINE and the white borders were removed through\n      subset decollaring processes. Five CD-ROM’s containing\n      Digital Orthophoto Quarter Quads (DOQQ’s) were used to\n      register and rectify the scanned soils maps.  Polygonal\n      data was then attributed according to the datasets.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02324","usgsCitation":"Norman, L., Wissler, C., Guertin, D.P., and Gray, F., 2002, Digital soils survey map of the Patagonia Mountains, Arizona: U.S. Geological Survey Open-File Report 2002-324, Report: 24 p.; Readme; Metadata; Dataset; Legend; Map: JPG format, https://doi.org/10.3133/ofr02324.","productDescription":"Report: 24 p.; Readme; Metadata; Dataset; Legend; Map: JPG format","additionalOnlineFiles":"Y","costCenters":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"links":[{"id":179138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02324.jpg"},{"id":4513,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0324/","linkFileType":{"id":5,"text":"html"}},{"id":283898,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0324/00readme.txt"},{"id":283899,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0324/scs_soil.met"},{"id":283900,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0324/pdf/scs_soil.pdf"},{"id":283901,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0324/scs_soil.e00"},{"id":283902,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0324/scs_soil.avl"},{"id":283903,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0324/images/scs_soil.jpg"}],"scale":"35000","projection":"Universal Transverse Mercator","datum":"North American Datum of 1983","country":"United States","state":"Arizona","otherGeospatial":"Patagonia Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.864671,31.348635 ], [ -110.864671,31.536392 ], [ -110.642353,31.536392 ], [ -110.642353,31.348635 ], [ -110.864671,31.348635 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651835","contributors":{"authors":[{"text":"Norman, Laura","contributorId":90382,"corporation":false,"usgs":true,"family":"Norman","given":"Laura","affiliations":[],"preferred":false,"id":242995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wissler, Craig","contributorId":16912,"corporation":false,"usgs":true,"family":"Wissler","given":"Craig","affiliations":[],"preferred":false,"id":242993,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Guertin, D. Phillip","contributorId":46062,"corporation":false,"usgs":false,"family":"Guertin","given":"D.","email":"","middleInitial":"Phillip","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":242994,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gray, Floyd 0000-0002-0223-8966 fgray@usgs.gov","orcid":"https://orcid.org/0000-0002-0223-8966","contributorId":603,"corporation":false,"usgs":true,"family":"Gray","given":"Floyd","email":"fgray@usgs.gov","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":242992,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50518,"text":"ofr02346 - 2002 - Intensity distribution and isoseismal maps for the Nisqually, Washington, earthquake of 28 February 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:16","indexId":"ofr02346","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-346","title":"Intensity distribution and isoseismal maps for the Nisqually, Washington, earthquake of 28 February 2001","docAbstract":"We present isoseismal maps, macroseismic intensities, and\r\ncommunity summaries of damage for the MW=6.8\r\nNisqually, Washington, earthquake of 28 February, 2001.\r\nFor many communities, two types of macroseismic intensity\r\nare assigned, the traditional U.S. Geological Survey\r\nModified Mercalli Intensities (USGS MMI) and a type of\r\nintensity newly introduced with this paper, the USGS\r\nReviewed Community Internet Intensity (RCII). For most\r\ncommunities, the RCII is a reviewed version of the\r\nCommunity Internet Intensity (CII) of Wald and others\r\n(1999). For some communities, RCII is assigned from\r\nsuch non-CII sources as press reports, engineering reports,\r\nand field reconnaissance observations. We summarize differences\r\nbetween procedures used to assign RCII and\r\nUSGS MMI, and we show that the two types of intensity\r\nare nonetheless very similar for the Nisqually earthquake.\r\nWe do not see evidence for systematic differences between\r\nRCII and USGS MMI that would approach one intensity\r\nunit, at any level of shaking, but we document a tendency\r\nfor the RCII to be slightly lower than MMI in regions of\r\nlow intensity and slightly higher than MMI in regions of\r\nhigh intensity. The highest RCII calculated for the\r\nNisqually earthquake is 7.6, calculated for zip code 98134,\r\nwhich includes the ?south of downtown? (Sodo) area of\r\nSeattle and Harbor Island. By comparison, we assigned a\r\ntraditional USGS MMI 8 to the Sodo area of Seattle. In\r\nall, RCII of 6.5 and higher were assigned to 58 zip-code\r\nregions. At the lowest intensities, the Nisqually earthquake\r\nwas felt over an area of approximately 350,000 square km\r\n(approximately 135,000 square miles) in Washington,\r\nOregon, Idaho, Montana, and southern British Columbia,\r\nCanada. On the basis of macroseismic effects, we infer\r\nthat shaking in the southern Puget Sound region was\r\nsomewhat less for the 2001 Nisqually earthquake than for\r\nthe Puget Sound earthquake of April 13, 1949, which had\r\nnearly the same hypocenter and magnitude. Allowing for\r\ndifferences in hypocenter, shaking in the 2001 earthquake\r\nwas very similar to that produced by the Puget Sound\r\nearthquake of April 25, 1965. First-person accounts of the\r\neffects of the 2001 earthquake on individual households\r\nare given for some communities.","language":"ENGLISH","doi":"10.3133/ofr02346","usgsCitation":"Dewey, J.W., Hopper, M.G., Wald, D.J., Quitoriano, V., and Adams, E.R., 2002, Intensity distribution and isoseismal maps for the Nisqually, Washington, earthquake of 28 February 2001 (Version 1.0): U.S. Geological Survey Open-File Report 2002-346, 57 p., illus. incl. sketch maps, 23 refs, https://doi.org/10.3133/ofr02346.","productDescription":"57 p., illus. incl. sketch maps, 23 refs","costCenters":[],"links":[{"id":175485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4330,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0346/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e10f6","contributors":{"authors":[{"text":"Dewey, James W. 0000-0001-8838-2450 jdewey@usgs.gov","orcid":"https://orcid.org/0000-0001-8838-2450","contributorId":5819,"corporation":false,"usgs":true,"family":"Dewey","given":"James","email":"jdewey@usgs.gov","middleInitial":"W.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":241671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopper, Margaret G. hopper@usgs.gov","contributorId":2227,"corporation":false,"usgs":true,"family":"Hopper","given":"Margaret","email":"hopper@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":241670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wald, David J. 0000-0002-1454-4514 wald@usgs.gov","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":795,"corporation":false,"usgs":true,"family":"Wald","given":"David","email":"wald@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":241669,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Quitoriano, Vincent","contributorId":29514,"corporation":false,"usgs":true,"family":"Quitoriano","given":"Vincent","email":"","affiliations":[],"preferred":false,"id":241672,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Adams, Elizabeth R.","contributorId":56102,"corporation":false,"usgs":true,"family":"Adams","given":"Elizabeth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":241673,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50531,"text":"ofr02374 - 2002 - A helicopter-borne magnetic survey over Dixie Valley geothermal field, Nevada: A web site for distribution of data","interactions":[],"lastModifiedDate":"2021-12-16T22:01:43.787364","indexId":"ofr02374","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-374","title":"A helicopter-borne magnetic survey over Dixie Valley geothermal field, Nevada: A web site for distribution of data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02374","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Pearson DeRidder & Johnson Inc., 2002, A helicopter-borne magnetic survey over Dixie Valley geothermal field, Nevada: A web site for distribution of data: U.S. Geological Survey Open-File Report 2002-374, 36 p.; Electronic Data, https://doi.org/10.3133/ofr02374.","productDescription":"36 p.; Electronic Data","costCenters":[],"links":[{"id":178353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393024,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52354.htm"},{"id":4343,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0374/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","otherGeospatial":"Dixie Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.11676025390625,\n              39.675484393594814\n            ],\n            [\n              -117.60314941406249,\n              39.675484393594814\n            ],\n            [\n              -117.60314941406249,\n              40.092781012494065\n            ],\n            [\n              -118.11676025390625,\n              40.092781012494065\n            ],\n            [\n              -118.11676025390625,\n              39.675484393594814\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4cf","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":532060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson DeRidder & Johnson Inc.","contributorId":128049,"corporation":true,"usgs":false,"organization":"Pearson DeRidder & Johnson Inc.","id":532059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50520,"text":"ofr02350 - 2002 - Sociocultural dimensions of supply and demand for natural aggregate; examples from the Mid-Atlantic region, United States","interactions":[],"lastModifiedDate":"2018-11-19T10:22:25","indexId":"ofr02350","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-350","title":"Sociocultural dimensions of supply and demand for natural aggregate; examples from the Mid-Atlantic region, United States","docAbstract":"The United States uses large quantities of natural aggregate to build and maintain a continuously expanding infrastructure. In recent years, per capita demand for aggregate in the United States has grown to about 9.7 metric tons (10.7 tons) per person per year. Over the next 25 years, the aggregate industry expects to mine quantities equivalent to all aggregate mined in the United States over the past 100 years. The issues surrounding supply and demand for aggregate in the mid-Atlantic states of Maryland, Pennsylvania, Virginia, and West Virginia illustrate competing requirements for industrial minerals and many simultaneous social and environmental objectives.","language":"ENGLISH","doi":"10.3133/ofr02350","usgsCitation":"Robinson, G.R., and Brown, W., 2002, Sociocultural dimensions of supply and demand for natural aggregate; examples from the Mid-Atlantic region, United States (Version 1.0): U.S. Geological Survey Open-File Report 2002-350, 44 p., illus. incl. 2 tables, 50 refs, https://doi.org/10.3133/ofr02350.","productDescription":"44 p., illus. incl. 2 tables, 50 refs","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":175598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4332,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-350/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5edd62","contributors":{"authors":[{"text":"Robinson, Gilpin R. Jr. grobinso@usgs.gov","contributorId":3083,"corporation":false,"usgs":true,"family":"Robinson","given":"Gilpin","suffix":"Jr.","email":"grobinso@usgs.gov","middleInitial":"R.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":241675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, William M.","contributorId":83104,"corporation":false,"usgs":true,"family":"Brown","given":"William M.","affiliations":[],"preferred":false,"id":241676,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50522,"text":"ofr02352 - 2002 - Preliminary report on geophysical data in Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2023-06-27T14:24:15.185096","indexId":"ofr02352","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-352","title":"Preliminary report on geophysical data in Yavapai County, Arizona","docAbstract":"Recently acquired geophysical data provide information on the geologic framework and its effect of groundwater flow and on stream/aquifer interaction in Yavapai County, Arizona. High-resolution aeromagnetic data reflect diverse rock types at and below the topographic surface and have permitted a preliminary interpretation of faults and underlying rock types (in particular, volcanic) that will provide new insights on the geologic framework, critical input to future hydrologic investigations. Aeromagnetic data map the western end of the Bear Wallow Canyon fault into the sedimentary fill of Verde Valley. Regional gravity data indicate potentially significant accumulations of low-density basin fill in Big Chino, Verde, and Williamson Valleys. Electrical and seismic data were also collected and help evaluate the approximate depth and extent of recent alluvium overlying Tertiary and Paleozoic sediments. These data will be used to ascertain the potential contribution of shallow ground-water subflow that cannot be measured by gages or flow meters and whether stream flow in losing reaches is moving as subflow or is being lost to the subsurface. The geophysical data will help produce a more robust groundwater flow model of the region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02352","usgsCitation":"Langenheim, V., Hoffmann, J., Blasch, K., DeWitt, E., and Wirt, L., 2002, Preliminary report on geophysical data in Yavapai County, Arizona: U.S. Geological Survey Open-File Report 2002-352, Report: PDF, 29 p.; Report: TXT, https://doi.org/10.3133/ofr02352.","productDescription":"Report: PDF, 29 p.; Report: TXT","numberOfPages":"30","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":283851,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02352.jpg"},{"id":86332,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0352/pdf/of02-352.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":4334,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0352/","linkFileType":{"id":5,"text":"html"}},{"id":283850,"rank":1,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/of/2002/0352/ofr02-352.txt","linkFileType":{"id":2,"text":"txt"}}],"country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Bear Wallow Canyon, Big Chino Valley, Verde Valley, Williamson Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.9999,34.348 ], [ -112.9999,35.268 ], [ -111.5977,35.268 ], [ -111.5977,34.348 ], [ -112.9999,34.348 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cba5","contributors":{"authors":[{"text":"Langenheim, V.E. 0000-0003-2170-5213","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":54956,"corporation":false,"usgs":true,"family":"Langenheim","given":"V.E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":241682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffmann, J.P.","contributorId":76389,"corporation":false,"usgs":true,"family":"Hoffmann","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":241684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blasch, K.W.","contributorId":29877,"corporation":false,"usgs":true,"family":"Blasch","given":"K.W.","affiliations":[],"preferred":false,"id":241681,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DeWitt, Ed","contributorId":65081,"corporation":false,"usgs":true,"family":"DeWitt","given":"Ed","affiliations":[],"preferred":false,"id":241683,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wirt, Laurie","contributorId":13204,"corporation":false,"usgs":true,"family":"Wirt","given":"Laurie","affiliations":[],"preferred":false,"id":241680,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50523,"text":"ofr02353 - 2002 - Gravity map and data of the eastern half of the Big Bear Lake, 100,000 scale quadrangle, California and analysis of the depths of several basins","interactions":[],"lastModifiedDate":"2025-05-14T15:20:51.917223","indexId":"ofr02353","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-353","title":"Gravity map and data of the eastern half of the Big Bear Lake, 100,000 scale quadrangle, California and analysis of the depths of several basins","docAbstract":"Gravity surveys are useful tools for helping to understand the 3-dimensional geology of an area. Many gravity measurements were made in the 1960s and 1970s by various groups in order to produce gravity maps covering California at a scale of 1:250,000 for the California Division of Mines and Geology. (For this area see Biehler et. al. 1988.) More recent surveys have focused on specific areas and problems. This report includes new data on the southern portion of the Marine Corps Air Ground Combat Center (MCAGCC) Twentynine Palms and the Yucca Valley-Joshua Tree-Twentynine Palms area and presents the map and basin analyses that were prepared with these data.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02353","usgsCitation":"Roberts, C., Jachens, R., Katzenstein, A., Smith, G., and Johnson, R., 2002, Gravity map and data of the eastern half of the Big Bear Lake, 100,000 scale quadrangle, California and analysis of the depths of several basins: U.S. Geological Survey Open-File Report 2002-353, HTML Document, https://doi.org/10.3133/ofr02353.","productDescription":"HTML Document","additionalOnlineFiles":"N","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":4335,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0353/","linkFileType":{"id":5,"text":"html"}},{"id":283797,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0353/intro.html","linkFileType":{"id":5,"text":"html"}},{"id":175600,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02353.gif"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.49971,34.00002 ], [ -116.49971,34.49920 ], [ -115.999146,34.49920 ], [ -115.999146,34.00002 ], [ -116.49971,34.00002 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a27b3","contributors":{"authors":[{"text":"Roberts, Carter","contributorId":44610,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","affiliations":[],"preferred":false,"id":241686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachens, Robert","contributorId":54660,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","affiliations":[],"preferred":false,"id":241687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Katzenstein, Allan","contributorId":77589,"corporation":false,"usgs":true,"family":"Katzenstein","given":"Allan","email":"","affiliations":[],"preferred":false,"id":241688,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Gregory","contributorId":42651,"corporation":false,"usgs":true,"family":"Smith","given":"Gregory","affiliations":[],"preferred":false,"id":241685,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Russell","contributorId":83193,"corporation":false,"usgs":true,"family":"Johnson","given":"Russell","email":"","affiliations":[],"preferred":false,"id":241689,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50525,"text":"ofr02361 - 2002 - Digital aeromagnetic datasets for the conterminous United States and Hawaii: A companion to the North American magnetic anomaly map","interactions":[],"lastModifiedDate":"2022-12-20T22:34:39.095023","indexId":"ofr02361","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-361","title":"Digital aeromagnetic datasets for the conterminous United States and Hawaii: A companion to the North American magnetic anomaly map","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02361","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Digital aeromagnetic datasets for the conterminous United States and Hawaii: A companion to the North American magnetic anomaly map: U.S. Geological Survey Open-File Report 2002-361, HTML Document; DVD-ROM, https://doi.org/10.3133/ofr02361.","productDescription":"HTML Document; DVD-ROM","costCenters":[],"links":[{"id":175710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4337,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-361/","linkFileType":{"id":5,"text":"html"}},{"id":410827,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54134.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Conterminous United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"geometry\": {\n        \"type\": \"MultiPolygon\",\n        \"coordinates\": [\n       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         34.078\n              ],\n              [\n                -119.43884,\n                34.34848\n              ],\n              [\n                -120.36778,\n                34.44711\n              ],\n              [\n                -120.62286,\n                34.60855\n              ],\n              [\n                -120.74433,\n                35.15686\n              ],\n              [\n                -121.71457,\n                36.16153\n              ],\n              [\n                -122.54747,\n                37.55176\n              ],\n              [\n                -122.51201,\n                37.78339\n              ],\n              [\n                -122.95319,\n                38.11371\n              ],\n              [\n                -123.7272,\n                38.95166\n              ],\n              [\n                -123.86517,\n                39.76699\n              ],\n              [\n                -124.39807,\n                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   ],\n              [\n                -122.58736,\n                47.096\n              ],\n              [\n                -122.34,\n                47.36\n              ],\n              [\n                -122.5,\n                48.18\n              ],\n              [\n                -122.84,\n                49\n              ],\n              [\n                -120,\n                49\n              ],\n              [\n                -117.03121,\n                49\n              ],\n              [\n                -116.04818,\n                49\n              ],\n              [\n                -113,\n                49\n              ],\n              [\n                -110.05,\n                49\n              ],\n              [\n                -107.05,\n                49\n              ],\n              [\n                -104.04826,\n                48.99986\n              ],\n              [\n                -100.65,\n                49\n              ],\n              [\n                -97.22872,\n                49.0007\n              ],\n              [\n                -95.15907,\n                49\n              ],\n              [\n                -95.15609,\n                49.38425\n              ],\n              [\n                -94.81758,\n                49.38905\n              ]\n            ]\n          ]\n        ]\n      },\n      \"properties\": {\n        \"name\": \"United States\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5d4","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":532058,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50533,"text":"ofr02384 - 2002 - High-resolution aeromagnetic survey to image shallow faults, Dixie Valley geothermal field, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:22","indexId":"ofr02384","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-384","title":"High-resolution aeromagnetic survey to image shallow faults, Dixie Valley geothermal field, Nevada","language":"ENGLISH","doi":"10.3133/ofr02384","usgsCitation":"Grauch, V.J., 2002, High-resolution aeromagnetic survey to image shallow faults, Dixie Valley geothermal field, Nevada (Version 1.0): U.S. Geological Survey Open-File Report 2002-384, 13 p., illus., https://doi.org/10.3133/ofr02384.","productDescription":"13 p., illus.","costCenters":[],"links":[{"id":178425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4345,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0384/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fbe1","contributors":{"authors":[{"text":"Grauch, V. J. S. 0000-0002-0761-3489","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":34125,"corporation":false,"usgs":true,"family":"Grauch","given":"V.","email":"","middleInitial":"J. S.","affiliations":[],"preferred":false,"id":241720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69390,"text":"mf2395 - 2002 - Geologic map of the Battle Ground 7.5-minute quadrangle, Clark County, Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"mf2395","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2395","title":"Geologic map of the Battle Ground 7.5-minute quadrangle, Clark County, Washington","docAbstract":"This digital map database, compiled from previously published and unpublished data, and new mapping by the authors, represents the general distribution of bedrock and surficial deposits of the Battle Ground 7.5 minute quadrangle. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution (scale) of the database to 1:24,000 or smaller.","language":"ENGLISH","doi":"10.3133/mf2395","usgsCitation":"Howard, K.A., 2002, Geologic map of the Battle Ground 7.5-minute quadrangle, Clark County, Washington: U.S. Geological Survey Miscellaneous Field Studies Map 2395, 18 p. and 1 sheet, https://doi.org/10.3133/mf2395.","productDescription":"18 p. and 1 sheet","costCenters":[],"links":[{"id":110350,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52491.htm","linkFileType":{"id":5,"text":"html"},"description":"52491"},{"id":187453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6332,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/2395/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.61749999999999,45.75 ], [ -122.61749999999999,45.8675 ], [ -122.5,45.8675 ], [ -122.5,45.75 ], [ -122.61749999999999,45.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ee4b07f02db69ff28","contributors":{"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":280309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39952,"text":"wri024216 - 2002 - Water quality and geochemical modeling of water at an abandoned coal mine reclaimed With coal combustion by-products","interactions":[],"lastModifiedDate":"2019-04-17T08:20:54","indexId":"wri024216","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-4216","displayTitle":"Water Quality and Geochemical Modeling of Water at an Abandoned Coal Mine Reclaimed With Coal Combustion By-Products","title":"Water quality and geochemical modeling of water at an abandoned coal mine reclaimed With coal combustion by-products","docAbstract":"<p>An abandoned coal mine in eastern Ohio was reclaimed with 125 tons per acre of pressurized fluidized bed combustion (PFBC) by-product. Water quality at the site (known as the Fleming site) was monitored for 7 years after reclamation; samples included water from soil-suction lysimeters (interstitial water), wells, and spring sites established downgradient of the application area. This report presents a summary of data collected at the Fleming site during the period September 1994 through June 2001. Additionally, results of geochemical modeling are included in this report to evaluate the potential fate of elements derived from the PFBC by-product.</p><p>Chemical analyses of samples of interstitial waters within the PFBC by-product application area indicated elevated levels of pH and specific conductance and elevated concentrations of boron, calcium, chloride, fluoride, magnesium, potassium, strontium, and sulfate compared to water samples collected in a control area where traditional reclamation methods were used. Magnesium-to-calcium (Mg:Ca) mole ratios and sulfur-isotope ratios were used to trace the PFBC by-product leachate and showed that little, if any, leachate reached ground water. Concentrations of most constituents in interstitial waters in the application-area decreased during the seven sampling rounds and approached background concentrations observed in the control area; however, median pH in the application area remained above 6, indicating that some acid-neutralizing capacity was still present. Although notable changes in water quality were observed in interstitial waters during the study period, quality of ground water and spring water remained poor. Water from the Fleming site was not potable, given exceedances of primary and secondary Maximum Contaminant Levels (MCLs) for inorganic constituents in drinking water set by the U.S. Environmental Protection Agency. Only fluoride and sulfate, which were found in higher concentrations in application-area interstitial waters than in control-area interstitial waters, could be related to the PFBC by-product. Concentrations of arsenic, lead, and selenium typically were at or below the detection limits (generally 1 or 2 micrograms per liter).</p><p>Elements detected at elevated concentrations in PFBC by-product application-area interstitial waters were not evident in downgradient ground water or spring water. Dilution of leachate by ground water was confirmed with a mixing model generated by the computer code NETPATH. Additionally, thermodynamic modeling of the chemical composition of water samples by use of the computer code PHREEQC indicated favorable conditions for precipitation of secondary minerals in the unsaturated zone and in aquifer materials. Because of low application rates of PFBC by-product and precipitation and sorption of elements in the unsaturated zone, it is improbable that concentrations of any toxic elements of concern (arsenic, lead, or selenium) will exceed drinking-water standards at this site or other sites where similar volumes of PFBC by-products are used.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA  ","doi":"10.3133/wri024216","collaboration":"Prepared in cooperation with the West Virginia University<br>The Ohio Department of Natural Resources, Division of Mineral Resources Management<br>  The Ohio Minelands Partnership","usgsCitation":"Haefner, R.J., 2002, Water quality and geochemical modeling of water at an abandoned coal mine reclaimed With coal combustion by-products: U.S. Geological Survey Water-Resources Investigations Report 2002-4216, 28 p., https://doi.org/10.3133/wri024216.","productDescription":"28 p.","costCenters":[],"links":[{"id":165560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4216/coverthb.jpg"},{"id":3647,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4216/wri20024216.pdf","text":"Report","size":"1.51 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2002-4216"}],"contact":"<p><a href=\"mailto:oh_dc@usgs.gov\" data-mce-href=\"mailto:oh_dc@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Ohio Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Blvd. <br>Columbus, OH 43229</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Previous Investigations</li><li>Study Methods</li><li>Hydrogeologic Setting</li><li>Water Quality</li><li>Geochemical Modeling</li><li>Summary and Conclusions</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd47b","contributors":{"authors":[{"text":"Haefner, Ralph J. 0000-0002-4363-9010 rhaefner@usgs.gov","orcid":"https://orcid.org/0000-0002-4363-9010","contributorId":1793,"corporation":false,"usgs":true,"family":"Haefner","given":"Ralph","email":"rhaefner@usgs.gov","middleInitial":"J.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44708,"text":"wri994174 - 2002 - Simulated pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2020-02-16T11:36:52","indexId":"wri994174","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"99-4174","title":"Simulated pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts","docAbstract":"A numerical model was used to simulate pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts. Simulation results show that pond-bottom hydraulic conductivity, which represents the degree of hydraulic connection between the pond and the aquifer, is an important control on these interactions. As this parameter was incrementally increased from 10 to 350 feet per day, the rate of ground-water inflow into the pond under natural conditions increased by about 250 percent, the associated residence times of water in the pond decreased by about 50 percent, and ground-water inflow to the pond shifted closer to the pond shore. Most ground-water inflow (90 to 98 percent) was in the upper model layer, which corresponded to shallow, near-shore areas of the pond, over the entire range of pond-bottom hydraulic conductivity. Ground-water flow paths into the pond became more vertical, the contributing area to the pond became larger, and the pond captured water from greater depths in the aquifer as the hydraulic conductivity of the pond bottom was increased. The pond level, however, remained nearly constant, and regional ground-water levels and gradients differed little over the range of pond-bottom hydraulic conductivity, indicating that calibrated models with similar head solutions can have different pond-aquifer interaction characteristics.\r\n\r\n\r\nHydrologic stresses caused by a simulated plume-containment system that specifies the extraction and injection of large volumes of ground water near the pond increased the pond level by about 0.4 foot and ground-water inflow rates into the pond by about 25 percent. Several factors related to the operation of the simulated containment system are affected by the hydraulic conductivity of the pond bottom. With increasing pond-bottom hydraulic conductivity, the amount of injected water that flows into Snake Pond increased and the amount of water recirculated between extraction and injection wells decreased. Comparison of simulations in which pond-bottom hydraulic conductivity was varied throughout the pond and simulations in which hydraulic conductivity was varied only in areas corresponding to shallow, near-shore areas of the pond indicate that the simulated hydraulic conductivity of the pond bottom in deeper parts of the pond had little effect on pond-aquifer interactions under both natural and stressed conditions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri994174","usgsCitation":"Walter, D.A., Masterson, J., and LeBlanc, D.R., 2002, Simulated pond-aquifer interactions under natural and stressed conditions near Snake Pond, Cape Cod, Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 99-4174, v, 35 p. , https://doi.org/10.3133/wri994174.","productDescription":"v, 35 p. ","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":172716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3750,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri994174/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.7080078125,\n              41.57436130598913\n            ],\n            [\n              -69.89501953125,\n              41.57436130598913\n            ],\n            [\n              -69.89501953125,\n              42.049292638686836\n            ],\n            [\n              -70.7080078125,\n              42.049292638686836\n            ],\n            [\n              -70.7080078125,\n              41.57436130598913\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f9af","contributors":{"authors":[{"text":"Walter, Donald A. 0000-0003-0879-4477 dawalter@usgs.gov","orcid":"https://orcid.org/0000-0003-0879-4477","contributorId":1101,"corporation":false,"usgs":true,"family":"Walter","given":"Donald","email":"dawalter@usgs.gov","middleInitial":"A.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masterson, John P. 0000-0003-3202-4413 jpmaster@usgs.gov","orcid":"https://orcid.org/0000-0003-3202-4413","contributorId":1865,"corporation":false,"usgs":true,"family":"Masterson","given":"John P.","email":"jpmaster@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":230296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"LeBlanc, Denis R. 0000-0002-4646-2628 dleblanc@usgs.gov","orcid":"https://orcid.org/0000-0002-4646-2628","contributorId":1696,"corporation":false,"usgs":true,"family":"LeBlanc","given":"Denis","email":"dleblanc@usgs.gov","middleInitial":"R.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":230295,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51125,"text":"ofr02204 - 2002 - Conversion of historical topographic sheets (T-sheets) from paper to digital form; Florida Everglades and vicinity","interactions":[],"lastModifiedDate":"2025-04-18T15:33:42.888476","indexId":"ofr02204","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-0204","title":"Conversion of historical topographic sheets (T-sheets) from paper to digital form; Florida Everglades and vicinity","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02204","isbn":"0607990627","usgsCitation":"Conversion of historical topographic sheets (T-sheets) from paper to digital form; Florida Everglades and vicinity; 2002; OFR; 2002-204; Smith, Thomas J., III; Foster, Ann M.; Briere, Peter R.; Jones, John W.; Van Arsdall, Carson","productDescription":"HTML Document: 1 CD-ROM","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":4512,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0204/","linkFileType":{"id":5,"text":"html"}},{"id":179137,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0204/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.09479583359331,\n              26.643885296477606\n            ],\n            [\n              -82.09479583359331,\n              24.327972112803963\n            ],\n            [\n              -80.11513304200784,\n              24.327972112803963\n            ],\n            [\n              -80.11513304200784,\n              26.643885296477606\n            ],\n            [\n              -82.09479583359331,\n              26.643885296477606\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"2002-11-01","noUsgsAuthors":false,"publicationDate":"2002-11-01","publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6865d5","contributors":{"authors":[{"text":"Smith, Thomas J. III tom_j_smith@usgs.gov","contributorId":1615,"corporation":false,"usgs":true,"family":"Smith","given":"Thomas","suffix":"III","email":"tom_j_smith@usgs.gov","middleInitial":"J.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":242987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, Ann M. amfoster@usgs.gov","contributorId":3545,"corporation":false,"usgs":true,"family":"Foster","given":"Ann","email":"amfoster@usgs.gov","middleInitial":"M.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":242989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briere, Peter R.","contributorId":14789,"corporation":false,"usgs":true,"family":"Briere","given":"Peter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":242990,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jones, John 0000-0001-6117-3691 jwjones@usgs.gov","orcid":"https://orcid.org/0000-0001-6117-3691","contributorId":2220,"corporation":false,"usgs":true,"family":"Jones","given":"John","email":"jwjones@usgs.gov","affiliations":[{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true},{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true}],"preferred":true,"id":242988,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Van Arsdall, Carson","contributorId":73271,"corporation":false,"usgs":true,"family":"Van Arsdall","given":"Carson","email":"","affiliations":[],"preferred":false,"id":242991,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50535,"text":"ofr02391 - 2002 - Multibeam bathymetry and selected perspective views of main part of Glacier Bay, Alaska","interactions":[],"lastModifiedDate":"2014-03-12T13:16:02","indexId":"ofr02391","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-391","title":"Multibeam bathymetry and selected perspective views of main part of Glacier Bay, Alaska","docAbstract":"Glacier Bay is a diverse fjord ecosystem with multiple tidewater glaciers and complex biological, geological, and oceanographic patterns that vary greatly along its length. The bay was completely glaciated prior to the 1700's, and subsequently experienced the fastest glacial retreat recorded in historical times. As a result, some of the highest rates of glacial sedimentation and uplift are observed here.\n\nGlacier Bay is the deepest silled fjord in Alaska, with depths of over 450 meters. The variety of physical processes and depths creates many diverse habitats within a relatively small area. Mapping benthic (seafloor) habitats is thus crucial to understanding and managing Glacier Bay's complex marine ecosystem and the marine species therein. High-resolution multibeam mapping of the bay, funded jointly by USGS and the National Park System, provides an unprecedented new baseline for resource and habitat assessment. Full integration of the new data set will require additional ground-truthing data (sampling) and analysis. The USGS goal is to develop integrated geological and oceanographic habitat models for the marine benthos in Glacier Bay, as a step toward determining the habitat relationships of critical species and resources within the Park.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02391","usgsCitation":"Carlson, P.R., Hooge, P., Cochrane, G., Stevenson, A., Dartnell, P., and Lee, K., 2002, Multibeam bathymetry and selected perspective views of main part of Glacier Bay, Alaska: U.S. Geological Survey Open-File Report 2002-391, HTML page, https://doi.org/10.3133/ofr02391.","productDescription":"HTML page","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":4347,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0391/","linkFileType":{"id":5,"text":"html"}},{"id":178427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02391.jpg"},{"id":283892,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0391/intro.html"}],"country":"United States","state":"Alaska","otherGeospatial":"Glacier Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -137.0187,58.3049 ], [ -137.0187,59.0615 ], [ -135.3983,59.0615 ], [ -135.3983,58.3049 ], [ -137.0187,58.3049 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b485c","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":241727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hooge, Philip","contributorId":51644,"corporation":false,"usgs":true,"family":"Hooge","given":"Philip","affiliations":[],"preferred":false,"id":241725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cochrane, Guy","contributorId":104164,"corporation":false,"usgs":true,"family":"Cochrane","given":"Guy","affiliations":[],"preferred":false,"id":241729,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stevenson, Andrew","contributorId":102787,"corporation":false,"usgs":true,"family":"Stevenson","given":"Andrew","affiliations":[],"preferred":false,"id":241728,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dartnell, Pete","contributorId":33412,"corporation":false,"usgs":true,"family":"Dartnell","given":"Pete","email":"","affiliations":[],"preferred":false,"id":241724,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, Kristen","contributorId":78809,"corporation":false,"usgs":true,"family":"Lee","given":"Kristen","affiliations":[],"preferred":false,"id":241726,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":40018,"text":"fs10002 - 2002 - Western Phosphate Field, U.S.A.; science in support of land management","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"fs10002","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"100-02","title":"Western Phosphate Field, U.S.A.; science in support of land management","language":"ENGLISH","doi":"10.3133/fs10002","usgsCitation":"Hein, J.R., 2002, Western Phosphate Field, U.S.A.; science in support of land management (Version 1.0): U.S. Geological Survey Fact Sheet 100-02, 2 p.; 1 sheet : col. ill., col. map ; 28 x 18 cm., https://doi.org/10.3133/fs10002.","productDescription":"2 p.; 1 sheet : col. ill., col. map ; 28 x 18 cm.","costCenters":[],"links":[{"id":119445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_100_02.bmp"},{"id":3528,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/fs-100-02/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a01","contributors":{"authors":[{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":222841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51160,"text":"ofr02392 - 2002 - Mineralogical characterization of weathered and less weathered strata of the Meade Peak phosphatic shale member of the Permian Phosphoria Formation: Measured sections E and F, Rasmussen Ridge, and measured sections G and H, Sage Creek area of the Webster Range, Caribou County, Idaho","interactions":[],"lastModifiedDate":"2023-06-27T14:04:28.971879","indexId":"ofr02392","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-392","title":"Mineralogical characterization of weathered and less weathered strata of the Meade Peak phosphatic shale member of the Permian Phosphoria Formation: Measured sections E and F, Rasmussen Ridge, and measured sections G and H, Sage Creek area of the Webster Range, Caribou County, Idaho","docAbstract":"The Permian Phosphoria Formation of the western U.S. includes one of the largest\nphosphate deposits in the world. Despite the economic significance of this formation, its\nfine-grained nature has discouraged detailed mineralogical characterization and\nquantitative studies. Recently, selenium and other potentially hazardous trace elements\nin mine wastes have drawn increased attention to these rocks and motivated more\nextensive study. Part of this effort has focused on a more detailed geological and\nmineralogical characterization of the rocks. This study uses powder X-ray diffraction\n(XRD) with Rietveld quantification software to characterize the mineralogy of channel\nsamples from stratigraphic sections measured by the U.S. Geological Survey in the\nMeade Peak Phosphatic Shale Member of the Permian Phosphoria Formation. Measured\nsections are at the Rasmussen Ridge mine and at the Smoky Canyon mine approximately\n15 and 25 miles, respectively, northeast of Soda Springs, Idaho.\nThe dominant minerals present in these samples are carbonate-fluorapatite, which\nis the most common phosphatic ore mineral in this and other marine phosphorites, quartz,\nmuscovite, albite, orthoclase, the ammonium feldspar buddingtonite (NH4AlSi3O8),\ndolomite, and calcite. Because of their potential for hosting trace elements such as Se,\nthe presence of minor pyrite and sphalerite is also noteworthy. Analysis of the carbonate\ncontent in the carbonate-fluorapatite by Rietveld refinement shows relatively low\ncarbonate contents, generally between 2 ? 3% (wt.) CO3\n2- in the apatite structure,\ncompared to other marine phosphorites.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02392","usgsCitation":"Knudsen, A.C., Gunter, M.E., Herring, J., and Grauch, R., 2002, Mineralogical characterization of weathered and less weathered strata of the Meade Peak phosphatic shale member of the Permian Phosphoria Formation: Measured sections E and F, Rasmussen Ridge, and measured sections G and H, Sage Creek area of the Webster Range, Caribou County, Idaho: U.S. Geological Survey Open-File Report 2002-392, 37 p., https://doi.org/10.3133/ofr02392.","productDescription":"37 p.","onlineOnly":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":177784,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02392.jpg"},{"id":389455,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52495.htm","linkFileType":{"id":5,"text":"html"}},{"id":283883,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0392/pdf/OF02-392.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":4574,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0392/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.5,\n              42.8\n            ],\n            [\n              -111.1,\n              42.8\n            ],\n            [\n              -111.1,\n              42.6\n            ],\n            [\n              -111.5,\n              42.6\n            ],\n            [\n              -111.5,\n              42.8\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696ad8","contributors":{"authors":[{"text":"Knudsen, A. C.","contributorId":46562,"corporation":false,"usgs":true,"family":"Knudsen","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243073,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gunter, M. E.","contributorId":104937,"corporation":false,"usgs":true,"family":"Gunter","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243074,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":243072,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grauch, R. I. 0000-0002-1763-0813","orcid":"https://orcid.org/0000-0002-1763-0813","contributorId":107698,"corporation":false,"usgs":true,"family":"Grauch","given":"R. I.","affiliations":[],"preferred":false,"id":243075,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50478,"text":"ofr0279 - 2002 - Streamflow gain/loss in the Republican River basin, Nebraska, May 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr0279","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-79","title":"Streamflow gain/loss in the Republican River basin, Nebraska, May 1975","docAbstract":"This arc and point data set contains streamflow-measurement sites and reaches indicating streamflow gain or loss under base-flow conditions along Republican River tributaries in Dundy and Chase Counties, Nebraska during May 19 to 20, 1975 (U.S. Geological Survey, 1976). The streamflow measurements were made to obtain data on ground-water/surface-water interaction. Flow was observed visually to be zero, was measured, or was estimated at 55 sites. Tributaries were followed upstream until the first road crossing where zero flow was encountered. For selected streams, points of zero flow upstream of the first zero flow site also were checked. \r\n\r\nStreamflow gain or loss for each stream reach was calculated by subtracting the streamflow values measured at the upstream end of the reach and values for contributing tributaries from the downstream value. The data obtained reflected base-flow conditions suitable for estimating streamflow gains and losses for stream reaches between sites. \r\n\r\nThis digital data set was created by manually plotting locations of streamflow measurements. These points were used to designate steam-reach segments to calculate gain/loss per river mile. Reach segments were created by manually splitting the lines from a 1:250,000-scale hydrography data set (Soenksen and others, 1999) at every location where the streams were measured. Each stream-reach segment between streamflow-measurement sites was assigned a unique reach number. All other lines in the hydrography data set without reach numbers were omitted.\r\n\r\nThis data set was created to archive the calculated streamflow gains and losses of tributary streams to the Republican River in Dundy and Chase Counties, Nebraska, in May 1975, and make the data available for use with geographic information systems (GIS).\r\n\r\nIf measurement sites are used separately from reaches, the maximum scale of 1:100,000 should not be exceeded. When used in conjunction with the reach segments, the maximum scale should not exceed 1:250,000.","language":"ENGLISH","doi":"10.3133/ofr0279","usgsCitation":"Johnson, M., Stanton, J.S., Cornwall, J.F., and Landon, M.K., 2002, Streamflow gain/loss in the Republican River basin, Nebraska, May 1975: U.S. Geological Survey Open-File Report 2002-79, 2 refs, https://doi.org/10.3133/ofr0279.","productDescription":"2 refs","costCenters":[],"links":[{"id":179023,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4287,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-079/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eb5","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241549,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Jennifer S. 0000-0002-2520-753X jstanton@usgs.gov","orcid":"https://orcid.org/0000-0002-2520-753X","contributorId":830,"corporation":false,"usgs":true,"family":"Stanton","given":"Jennifer","email":"jstanton@usgs.gov","middleInitial":"S.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cornwall, James F.","contributorId":74067,"corporation":false,"usgs":true,"family":"Cornwall","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241550,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241547,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50481,"text":"ofr0283 - 2002 - Streamflow gain/loss in the Republican River basin, Nebraska, October 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr0283","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-83","title":"Streamflow gain/loss in the Republican River basin, Nebraska, October 1978","docAbstract":"This arc and point data set contains streamflow-measurement sites and reaches indicating streamflow gain or loss under base-flow conditions along the Republican River and tributaries in Nebraska during October 10 to 18, 1978 (U.S. Geological Survey, 1980). The streamflow measurements were made to obtain data on ground-water/surface-water interaction. Flow was observed visually to be zero, was measured, or was estimated at 254 sites. The measurements were made on the main stem of the Republican River and all flowing tributaries that enter the Republican River between Swanson and Harlan County reservoirs in the Nebraska part of the Republican River Basin. Tributaries were followed upstream until the first road crossing where zero flow was encountered. For selected streams, points of zero flow upstream of the first zero flow site also were checked.\r\n\r\nStreamflow gain or loss for each stream reach was calculated by subtracting the streamflow values measured at the upstream end of the reach and values for contributing tributaries from the downstream value. The data obtained reflected base-flow conditions suitable for estimating streamflow gains and losses for stream reaches between sites. \r\n\r\nThis digital data set was created by manually plotting locations of streamflow measurements. These points were used to designate stream-reach segments to calculate gain/loss per river mile. Reach segments were created by manually splitting the lines from a 1:250,000 hydrography data set (Soenksen and others, 1999) at every location where the streams were measured. Each stream-reach segment between streamflow-measurement sites was assigned a unique reach number. All other lines in the hydrography data set without reach numbers were omitted.\r\n\r\nThis data set was created to archive the calculated streamflow gains and losses in part of the Republican River Basin, Nebraska, in October 1978, and make the data available for use with geographic information systems (GIS).\r\n\r\nIf measurement sites are used separately from reaches, the maximum scale of 1:100,000 should not be exceeded. When used in conjunction with the reach segments, the maximum scale should not exceed 1:250,000.","language":"ENGLISH","doi":"10.3133/ofr0283","usgsCitation":"Johnson, M., Stanton, J.S., Cornwall, J.F., and Landon, M.K., 2002, Streamflow gain/loss in the Republican River basin, Nebraska, October 1978: U.S. Geological Survey Open-File Report 2002-83, 2 refs, https://doi.org/10.3133/ofr0283.","productDescription":"2 refs","costCenters":[],"links":[{"id":179176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4290,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-083/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf9c","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":241561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Jennifer S. 0000-0002-2520-753X jstanton@usgs.gov","orcid":"https://orcid.org/0000-0002-2520-753X","contributorId":830,"corporation":false,"usgs":true,"family":"Stanton","given":"Jennifer","email":"jstanton@usgs.gov","middleInitial":"S.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cornwall, James F.","contributorId":74067,"corporation":false,"usgs":true,"family":"Cornwall","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241562,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241559,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50526,"text":"ofr02363 - 2002 - Preliminary gravity inversion model of Frenchman Flat Basin, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2023-06-27T14:21:50.437693","indexId":"ofr02363","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-363","title":"Preliminary gravity inversion model of Frenchman Flat Basin, Nevada Test Site, Nevada","docAbstract":"The depth of the basin beneath Frenchman Flat is estimated using a gravity inversion method. Gamma-gamma density logs from two wells in Frenchman Flat constrained the density profiles used to create the gravity inversion model. Three initial models were considered using data from one well, then a final model is proposed based on new information from the second well. The preferred model indicates that a northeast-trending oval-shaped basin underlies Frenchman Flat at least 2,100 m deep, with a maximum depth of 2,400 m at its northeast end. No major horst and graben structures are predicted. Sensitivity analysis of the model indicates that each parameter contributes the same magnitude change to the model, up to 30 meters change in depth for a 1% change in density, but some parameters affect a broader area of the basin. The horizontal resolution of the model was determined by examining the spacing between data stations, and was set to 500 square meters.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02363","usgsCitation":"Phelps, G., and Graham, S.E., 2002, Preliminary gravity inversion model of Frenchman Flat Basin, Nevada Test Site, Nevada: U.S. Geological Survey Open-File Report 2002-363, Report: 23 p.; 1 Plate: 21.61 x 30.53 inches, https://doi.org/10.3133/ofr02363.","productDescription":"Report: 23 p.; 1 Plate: 21.61 x 30.53 inches","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":175711,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02363.jpg"},{"id":283852,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0363/pdf/of02-363plate1.pdf","text":"Plate 1"},{"id":283855,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0363/of02-363depthdata.asc"},{"id":283854,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0363/of02-363metadata.txt"},{"id":283853,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0363/pdf/of02-363.pdf"},{"id":4338,"rank":6,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0363/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"Universal Transverse Mercator, zone 11","datum":"North American Datum of 1927","country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.000,36.750 ], [ -116.000,36.875 ], [ -115.800,36.875 ], [ -115.800,36.750 ], [ -116.000,36.750 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697503","contributors":{"authors":[{"text":"Phelps, Geoffrey A.","contributorId":17262,"corporation":false,"usgs":true,"family":"Phelps","given":"Geoffrey A.","affiliations":[],"preferred":false,"id":241693,"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":241692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50519,"text":"ofr02349 - 2002 - Human impact on the planet: an earth system science perspective and ethical considerations","interactions":[],"lastModifiedDate":"2014-09-05T10:15:08","indexId":"ofr02349","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-349","title":"Human impact on the planet: an earth system science perspective and ethical considerations","docAbstract":"The modern Earth Narrative, the scientific story of the 4.5 billion-year natural and human history of the Earth, has emerged from the solid foundation of two factual concepts: Deep (or Geologic) Time and Biological Evolution. spread acceptance of the Earth Narrative is critically important as we begin the third millennium, because it provides a clear understanding of the growing impact of human population growth and associated activities on the Earth System, especially the negative impact on Earth?s biosphere. It is important for humans to realize that we are but one of 4,500 species of mammals that exist on Earth and that we are but one species in the estimated 30 to 100 million species that form the complex biosphere. We also need to recognize that all species exist within the physical limits imposed by the geosphere. We are totally dependent on the biosphere for food, oxygen, and other necessities of life. mans are one of the latest results of biological evolution operating over a long period of Geologic Time. We find ourselves on Earth, after 4.5 billion years of Earth history by chance, not by design. Humans have become so successful at modifying their environment that many of the natural limitations on the expansion of populations of our fellow animals have been overcome by technological and cultural innovations. According to Peter Raven, ?Humans, at a current population of 6 billion [expected to nearly double by 2050], are consuming or wasting about 50 percent of the total net biological productivity on land and 50 percent of the available supply of freshwater. The overwhelming and expanding human presence leaves less and less room in the environment for other biota.? st century will be a pivotal time in the fate of Earth?s biosphere. Whereas human modification of the geosphere will slowly recover over time, human changes to the biosphere are a far more consequential matter? extinction of a species is forever! Will humans effectively use our new knowledge of natural and human history to stop further degradation of Earth?s ecosystems and extinction of its biota? The fate of the biosphere, including humanity, depends on a reaffirmation by all humans of all cultures and religions of the global importance of a planet-wide conservation of the Earth?s biotic heritage. For the world?s religions it means elevation of stewardship of the Earth to a moral imperative and a goal of complete preservation of the Earth?s biotic inheritance, one which is based on a Do No Harm ethic.","language":"ENGLISH","doi":"10.3133/ofr02349","usgsCitation":"Williams, R., 2002, Human impact on the planet: an earth system science perspective and ethical considerations (version 1.0): U.S. Geological Survey Open-File Report 2002-349, 81 p., illus., https://doi.org/10.3133/ofr02349.","productDescription":"81 p., illus.","costCenters":[],"links":[{"id":175486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4331,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-349/","linkFileType":{"id":5,"text":"html"}}],"edition":"version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a5fc","contributors":{"authors":[{"text":"Williams, Richard S. Jr.","contributorId":90679,"corporation":false,"usgs":true,"family":"Williams","given":"Richard S.","suffix":"Jr.","affiliations":[],"preferred":false,"id":241674,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50484,"text":"ofr0286 - 2002 - Streamflow gain/loss in the Republican River basin, Nebraska, October 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr0286","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-86","title":"Streamflow gain/loss in the Republican River basin, Nebraska, October 1981","docAbstract":"This arc and point data set contains streamflow-measurement sites and reaches indicating streamflow gain or loss under base-flow conditions along the Republican River and tributaries in Nebraska during October 19 to 20, 1981 (Engel and others, 1984). The streamflow measurements were made to obtain data on ground-water/surface-water interaction. Flow was observed visually to be zero, was measured, or was estimated at 105 sites. The measurements were made on the main stem of the Republican River and all flowing tributaries that enter the Republican River between Muddy Creek in western Furnas County and Harlan County Reservoir in the Nebraska part of the Republican River Basin. Tributaries were followed upstream until the first road crossing where zero flow was encountered. For selected streams, points of zero flow upstream of the first zero flow site were also checked. \r\n\r\nStreamflow gain or loss for each stream reach was calculated by subtracting the streamflow values measured at the upstream end of the reach and values for contributing tributaries from the downstream value. The data obtained reflected base-flow conditions suitable for estimating streamflow gains and losses for stream reaches between sites. \r\n\r\nThis digital data set was created by manually plotting locations of streamflow measurements. These points were used to designate stream-reach segments to calculate gain/loss per river mile. Reach segments were created by manually splitting the lines from a 1:250,000 hydrography data set (Soenksen and others, 1999) at every location where the streams were measured. Each stream-reach segment between streamflow-measurement sites was assigned a unique reach number. All other lines in the hydrography data set without reach numbers were omitted.\r\n\r\nThis data set was created to archive the calculated streamflow gains and losses of selected streams in the Republican River Basin, Nebraska, in October 1981, and make the data available for use with geographic information systems (GIS).\r\n\r\nIf measurement sites are used separately from reaches, the maximum scale of 1:100,000 should not be exceeded. When used in conjunction with the reach segments, the maximum scale should not exceed 1:250,000.","language":"ENGLISH","doi":"10.3133/ofr0286","usgsCitation":"Johnson, M., Stanton, J.S., Cornwall, J.F., and Landon, M.K., 2002, Streamflow gain/loss in the Republican River basin, Nebraska, October 1981: U.S. Geological Survey Open-File Report 2002-86, 2 refs, https://doi.org/10.3133/ofr0286.","productDescription":"2 refs","costCenters":[],"links":[{"id":179673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4293,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-086/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8206","contributors":{"authors":[{"text":"Johnson, Michaela R. 0000-0001-6133-0247 mrjohns@usgs.gov","orcid":"https://orcid.org/0000-0001-6133-0247","contributorId":1013,"corporation":false,"usgs":true,"family":"Johnson","given":"Michaela R.","email":"mrjohns@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":241573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, Jennifer S. 0000-0002-2520-753X jstanton@usgs.gov","orcid":"https://orcid.org/0000-0002-2520-753X","contributorId":830,"corporation":false,"usgs":true,"family":"Stanton","given":"Jennifer","email":"jstanton@usgs.gov","middleInitial":"S.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cornwall, James F.","contributorId":74067,"corporation":false,"usgs":true,"family":"Cornwall","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":241574,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Landon, Matthew K. 0000-0002-5766-0494 landon@usgs.gov","orcid":"https://orcid.org/0000-0002-5766-0494","contributorId":392,"corporation":false,"usgs":true,"family":"Landon","given":"Matthew","email":"landon@usgs.gov","middleInitial":"K.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":241571,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":50507,"text":"ofr02299 - 2002 - Cobalt recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:11:20","indexId":"ofr02299","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-299","title":"Cobalt recycling in the United States in 1998","docAbstract":"This report is one of a series of reports on metals recycling. It defines and quantifies the 1998 flow of cobalt-bearing materials in the United States, from imports and stock releases through consumption and disposition, with particular emphasis on the recycling of industrial scrap (new scrap) and used products (old scrap). Because of cobalt?s many and diverse uses, numerous types of scrap were available for recycling by a wide variety of processes. In 1998, an estimated 32 percent of U.S. cobalt supply was derived from scrap. The ratio of cobalt consumed from new scrap to that from old scrap was estimated to be 50:50. Of all the cobalt in old scrap available for recycling, an estimated 68 percent was either consumed in the United States or exported to be recycled.","language":"ENGLISH","doi":"10.3133/ofr02299","usgsCitation":"Shedd, K.B., 2002, Cobalt recycling in the United States in 1998 (version 1.0): U.S. Geological Survey Open-File Report 2002-299, p. 16, illus. incl. 1 table, 60 refs, https://doi.org/10.3133/ofr02299.","productDescription":"p. 16, illus. incl. 1 table, 60 refs","costCenters":[],"links":[{"id":176759,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4319,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-299/","linkFileType":{"id":5,"text":"html"}}],"edition":"version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9d9","contributors":{"authors":[{"text":"Shedd, Kim B. kshedd@usgs.gov","contributorId":2896,"corporation":false,"usgs":true,"family":"Shedd","given":"Kim","email":"kshedd@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":241637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50517,"text":"ofr02344 - 2002 - Results of weekly chemical and isotopic monitoring of selected springs in Norris Geyser Basin, Yellowstone National Park during June-September, 1995","interactions":[],"lastModifiedDate":"2023-06-27T14:40:52.565165","indexId":"ofr02344","displayToPublicDate":"2002-11-01T00:00:00","publicationYear":"2002","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":"2002-344","title":"Results of weekly chemical and isotopic monitoring of selected springs in Norris Geyser Basin, Yellowstone National Park during June-September, 1995","docAbstract":"Each year at Norris Geyser Basin, generally in August or September, a widespread hydrothermal 'disturbance' occurs that is characterized by simultaneous changes in the discharge characteristics of many springs, particularly in the Back Basin. During the summer season of 1995, water samples from eight widely distributed hot springs and geysers at Norris were collected each week and analyzed to determine whether chemical and isotopic changes also occurred in the thermal waters at the time of the disturbance. In addition, Beryl Spring in Gibbon Canyon, 5.8 km southwest of Norris Geyser Basin, was included in the monitoring program. Waters discharged by four of the monitored hot springs and geysers appear to issue from relatively deep reservoirs where temperatures are at least 270 C and possibly higher than 300 C. At the time of, and for several days after, the onset of the 1995 disturbance, the normally neutral-chloride waters discharged by these four features all picked up an acid-sulfate component and became isotopically heavier. The acid-sulfate component appears to be similar in composition to some waters discharged in 100 Spring Plain that issue from subsurface regions where temperatures are in the range 170-210 C. However, the two monitored springs that discharge acid-chloride-sulfate waters in the 100 Spring Plain region did not show any significant chemical or isotopic response to the annual disturbance. Beryl Spring, and two neutral-chloride hot springs at Norris that appear to draw their water from reservoirs where temperatures are 250 C or less, also did not show any significant chemical or isotopic response to the annual disturbance. After the start of the annual disturbance, chloride concentrations in water sampled from Double Bulger Geyser in the Back Basin increased from about 800 ppm to about 1500 ppm, nearly twice as high as any previously reported chloride concentration in a thermal water at Yellowstone. The isotopic composition of that water precludes an origin of the high chloride by evaporation at atmospheric pressure. One way to account for the unique chemical and isotopic composition of this highly concentrated wateris by recirculation of water that had gone through one cycle of adiabatic cooling during upflow (decompressional boiling) back down into the hydrothermal system, where it is reheated to greater than 220 C. This previously boiled water then undergoes additional cycles of decompressional boiling during subsequent upflow. Another way the unique chemical and isotopic composition of Double Bulger water might evolve is by excess boiling in the formation that results from a decrease in fluid pressure within the channels of upflow. The annual disturbance at Norris Geyser Basin generally appears to be triggered by a cyclic up and down movement of the boilingpoint curve within the hydrothermal system in response to changes in the potentiometric surface of the cold water that is adjacent to, and interconnected with, that hydrothermal system. Annual disturbance phenomena that are easily recognized at Norris Geyser Basin may not be easily recognized elsewhere in Yellowstone National Park because (1) the neutral-chloride waters at Norris ascend directly from higher-temperature and higherpressure reservoirs (270 to >300 C at Norris compared to 180-215C at Upper and Lower Geyser Basins) that are capable of producing massive amounts of high-pressure steam, and (2) the clay that makes hot spring and geyser waters become turbid at Norris, heralding the start of the disturbance, comes from acid altered rocks that are widely distributed at intermediate depths at Norris, and that are rare in other geyser basins.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02344","usgsCitation":"Fournier, R., Weltman, U., Counce, D., White, L.D., and Janik, C.J., 2002, Results of weekly chemical and isotopic monitoring of selected springs in Norris Geyser Basin, Yellowstone National Park during June-September, 1995: U.S. Geological Survey Open-File Report 2002-344, 49 p., https://doi.org/10.3133/ofr02344.","productDescription":"49 p.","numberOfPages":"50","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":175382,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02344.jpg"},{"id":415129,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52496.htm","linkFileType":{"id":5,"text":"html"}},{"id":283828,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0344/pdf/of02-344.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":4329,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0344/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.7117,\n              44.7333\n            ],\n            [\n              -110.7117,\n              44.7203\n            ],\n            [\n              -110.6975,\n              44.7203\n            ],\n            [\n              -110.6975,\n              44.7333\n            ],\n            [\n              -110.7117,\n              44.7333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60460b","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":241668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weltman, U.","contributorId":33379,"corporation":false,"usgs":true,"family":"Weltman","given":"U.","email":"","affiliations":[],"preferred":false,"id":241666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Counce, D.","contributorId":36165,"corporation":false,"usgs":true,"family":"Counce","given":"D.","affiliations":[],"preferred":false,"id":241667,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"White, L. 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