{"pageNumber":"1077","pageRowStart":"26900","pageSize":"25","recordCount":46734,"records":[{"id":39883,"text":"ofr02283 - 2002 - Color-coded contour map of Mars M 25M RKN","interactions":[],"lastModifiedDate":"2014-03-11T08:36:55","indexId":"ofr02283","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-283","title":"Color-coded contour map of Mars M 25M RKN","docAbstract":"NOTES ON BASE\n\nThis map is based on data from the Mars Orbiter Laser Altimeter (MOLA) (Smith and others, 2001), an instrument on NASA's Mars Global Surveyor (MGS) spacecraft (Albee and others, 2001). The image used for the base of this map represents more than 600 million measurements gathered between 1999 and 2001, adjusted for consistency (Neumann and others, 2001, 2002) and converted to planetary radii. These have been converted to elevations above the areoid as determined from a martian gravity field solution GMM2 (Lemoine and others, 2001), truncated to degree and order 50, and oriented according to current standards (see below). The average accuracy of each point is originally ~100 meters in horizontal position, and ~1 meter in radius (Neumann, 2001). However, the total elevation uncertainty is at least +3 m due to the global error in the areoid (+1.8 meters according to Lemoine and others, 2001) and regional uncertainties in its shape (communication from Neumann, 2002). The measurements were converted into a digital elevation model (DEM) (communication from Neumann, 2002; Neumann and others, 2001; Smith and others, 2001) using Generic Mapping Tools software (Wessel and Smith, 1998), with a resolution of 0.015625 degrees per pixel or 64 pixels per degree. In projection, the pixels are 926.17 meters in size at the equator.\n\nPROJECTION\n\nThe Mercator projection is used between latitudes +57°, with a central meridian at 0° and latitude equal to the nominal scale at 0°. The Polar Stereographic projection is used for the polar regions north of the +55° parallel and south of the –55° parallel with a central meridian set for both at 0°. The adopted equatorial radius is 3,396.19 km (Duxbury and others 2002; Seidelmann and others 2002).\n\nCOORDINATE SYSTEM\n\nThe MOLA data were initially referenced to an internally consistent inertial coordinate system, derived from tracking of the MGS spacecraft. By adopting appropriate values for the orientation of Mars as defined by the International Astronomical Union (IAU) and the International Association of Geodesy (IAG) (Seidelmann and others, 2002), these inertial coordinates were converted into the planet-fixed coordinates (longitude and latitude) used on this map. These values include the orientation of the north pole of Mars (including the effects of precession), the rotation rate of Mars, and a value for W0 of 176.630°, where W0 is the angle along the equator to the east, between the 0° meridian and the equator's intersection with the celestial equator at the standard epoch J2000.0 (Seidelmann and others, 2002). This value of W0 was chosen (Duxbury and others, 2002) in order to place the 0° meridian through the center of the small (~500 m) crater Airy-0, located in the crater Airy (de Vaucouleurs and others, 1973; Seidelmann and others, 2002). Longitude increases to the east, and latitude is planetocentric as allowed by IAU/IAG standards (Seidelmann and others, 2002) and in accordance with current NASA and USGS standards (Duxbury and others, 2002). A secondary grid (printed in red) has been added to the map as a reference to the west longitude/planetographic latitude system that is also allowed by IAU/IAG standards (Seidelmann and others, 2002) and has also been used for Mars. The figure adopted to compute this secondary grid is an oblate spheroid with an equatorial radius of 3,396.19 km and a polar radius of 3,376.2 km (Duxbury and others, 2002; Seidelmann and others, 2002).\n\nMAPPING TECHNIQUES\n\nTo create the topographic base image, the original DEM produced by the MOLA team in Simple Cylindrical projection with a resolution of 64 pixels per degree was projected into the Mercator and Polar Stereographic pieces. A shaded relief was generated from each DEM with a sun angle of 30° from horizontal and a sun azimuth of 270°, as measured clockwise from north, and a vertical exaggeration of 100%. Illumination is from the west, which follows a long-standing USGS tradition for planetary maps. This allows for continuity in the shading between maps and quadrangles, and most closely resembles lighting conditions found on imagery. The DEM values were then mapped to a smooth global color look-up table. Note that the chosen color scheme simply represents elevation changes and is not intended to imply anything about surface characteristics (e.g., past or current presence of water or ice). These two files were then merged and scaled to 1:25 million for the Mercator portion and 1:15,196,708 for the two Polar Stereographic portions, with a resolution of 300 dots per inch. The projections have a common scale of 1:13,923,113 at +56° latitude. Contours were created from the DEM at a 1-kilometer interval. Contours for features with a diameter of 3 km or less (features too small for this map scale) were removed. The contours were then simplified by removing points along the contours spaced less than 1 km apart.\n\nNOMENCLATURE\n\nNames on this sheet are approved by the IAU and have been applied for features clearly visible at the scale of this map. For a complete list of the IAU-approved nomenclature for Mars, see the Gazetteer of Planetary Nomenclature at http://planetarynames.wr.usgs.gov/. Font color was chosen for readability. Names followed by an asterisk are provisionally approved.\n\nM 25M RKN: Abbreviation for Mars, 1:25,000,000 series, shaded relief (R), with color (K) and nomenclature (N) (Greeley and Batson, 1990).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02283","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Color-coded contour map of Mars M 25M RKN: U.S. Geological Survey Open-File Report 2002-283, Map: 36.00 inches x 33.00 inches, https://doi.org/10.3133/ofr02283.","productDescription":"Map: 36.00 inches x 33.00 inches","additionalOnlineFiles":"N","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":170203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02283.jpg"},{"id":3594,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0283/","linkFileType":{"id":5,"text":"html"}},{"id":283775,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0283/pdf/of02-283.pdf"}],"scale":"250000","projection":"Mercator","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae84e","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":529929,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39928,"text":"ofr02274 - 2002 - Digital version of \"Open-File Report 92-179: Geologic map of the Cow Cove Quadrangle, San Bernardino County, California\"","interactions":[],"lastModifiedDate":"2023-06-27T15:58:12.449089","indexId":"ofr02274","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-274","title":"Digital version of \"Open-File Report 92-179: Geologic map of the Cow Cove Quadrangle, San Bernardino County, California\"","docAbstract":"<p>This is a digital map database version of a previous printed geologic map, U.S. Geological Survey Open-File Report 92–179. The original paper map has been faithfully reproduced as a geologic map database for use in a GIS, and thus does not contain updated geologic information for the map area. This publication consists of three parts:</p>\n<br/>\n<p>1. Documentation in the form of a this publication's Open File text, or readme, describing the digital data, how to obtain it, as well as the original map explanation pamphlet. The documentation also consists of FGDC metadata, and a file describing any revisions to the data in this report. All of the documentaion components are available in a variety of file formats.<br/>\n2. Three Arc/Info (ESRI) formatted coverages of the geologic database, distributed in Arc Interchange (e00) format. The spatial databases in this component of the report consist vector-based GIS datasets that represent geologic contacts, faults, map units, and volcanic vents in the study area, as well as localities of K/Ar samples discussed in the original report, and geologic structure measurements.<br/>\n3. Plottable map representations of the database at 1:24,000 scale in PostScript and Adobe PDF formats. The plottable files consist of a color geologic map derived from the spatial database, composited with a topographic base map in the form of the USGS Digital Raster Graphic for the map area. Color symbology from each of these datasets is maintained, which can cause plot file sizes to be large.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02274","usgsCitation":"Wilshire, H.G., Bedford, D., and Coleman, T., 2002, Digital version of \"Open-File Report 92-179: Geologic map of the Cow Cove Quadrangle, San Bernardino County, California\": U.S. Geological Survey Open-File Report 2002-274, Report: 27 p.; 1 Plate: 22.0 x 32.0 inches; 3 Metadata Files; 4 Data Files, https://doi.org/10.3133/ofr02274.","productDescription":"Report: 27 p.; 1 Plate: 22.0 x 32.0 inches; 3 Metadata Files; 4 Data Files","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":172487,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":283819,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0274/pdf/of02-274_3a.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":283815,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0274/pdf/of02-274_1a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":283818,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0274/of02-274data.tar"},{"id":283817,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0274/of02-274_1b.html"},{"id":3628,"rank":6,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0274/","linkFileType":{"id":5,"text":"html"}},{"id":110332,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52001.htm","linkFileType":{"id":5,"text":"html"},"description":"52001"}],"scale":"24000","projection":"Universal Transverse Mercator","datum":"1927 North American Datum","country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.75,35.25 ], [ -115.75,35.375 ], [ -115.625,35.375 ], [ -115.625,35.25 ], [ -115.75,35.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae68","contributors":{"authors":[{"text":"Wilshire, Howard G.","contributorId":68346,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":222615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, Teresa","contributorId":42282,"corporation":false,"usgs":true,"family":"Coleman","given":"Teresa","email":"","affiliations":[],"preferred":false,"id":222616,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39922,"text":"ofr2002266 - 2002 - Ice Core Depth-Age Relation for Vostok delta-D and Dome Fuji delta-18O Records Based on the Devils Hole Paleotemperature Chronology","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"ofr2002266","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-266","title":"Ice Core Depth-Age Relation for Vostok delta-D and Dome Fuji delta-18O Records Based on the Devils Hole Paleotemperature Chronology","docAbstract":"This report presents the data for the Vostok - Devils Hole chronology, termed V-DH chronology, for the Antarctic Vostok ice core record. This depth - age relation is based on a join between the Vostok deuterium profile (D) and the stable oxygen isotope ratio (18O) record of paleotemperature from a calcitic core at Devils Hole, Nevada, using the algorithm developed by Landwehr and Winograd (2001). Both the control points defining the V-DH chronology and the numeric values for the chronology are given. In addition, a plausible chronology for a deformed bottom portion of the Vostok core developed with this algorithm is presented. Landwehr and Winograd (2001) demonstrated the broader utility of their algorithm by applying it to another appropriate Antarctic paleotemperature record, the Antarctic Dome Fuji ice core 18O record. Control points for this chronology are also presented in this report but deemed preliminary because, to date, investigators have published only the visual trace and not the numeric values for the Dome Fuji 18O record. The total uncertainty that can be associated with the assigned ages is also given.\r\n\r\n","language":"ENGLISH","doi":"10.3133/ofr2002266","usgsCitation":"Landwehr, J., 2002, Ice Core Depth-Age Relation for Vostok delta-D and Dome Fuji delta-18O Records Based on the Devils Hole Paleotemperature Chronology: U.S. Geological Survey Open-File Report 2002-266, 53 p. (1 figure, 5 tables, 6 p. of text), https://doi.org/10.3133/ofr2002266.","productDescription":"53 p. (1 figure, 5 tables, 6 p. of text)","costCenters":[],"links":[{"id":172383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9160,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr02-266/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f965c","contributors":{"authors":[{"text":"Landwehr, Jurate Maciunas","contributorId":106522,"corporation":false,"usgs":true,"family":"Landwehr","given":"Jurate Maciunas","affiliations":[],"preferred":false,"id":222601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39929,"text":"ofr02275 - 2002 - Geology, mineralization, and hydrothermal alteration and relationships to acidic and metal-bearing surface waters in the Palmetto Gulch area, southwestern Colorado","interactions":[],"lastModifiedDate":"2017-03-07T15:56:58","indexId":"ofr02275","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-275","title":"Geology, mineralization, and hydrothermal alteration and relationships to acidic and metal-bearing surface waters in the Palmetto Gulch area, southwestern Colorado","docAbstract":"The Palmetto Gulch area is affected by low pH and metal-bearing drainage from abandoned mines, and perhaps, from natural weathering around vein zones. To investigate these anthropogenic and potential natural sources of acidity and metals, we mapped the geology, veins, and hydrothermally altered areas; conducted mine dump leachate studies; and collected reconnaissance water quality data. Several small abandoned mines are present in the Palmetto Gulch area that produced small amounts of relatively high-grade silver ore from fault-controlled polymetallic vein deposits. These veins are hosted in lavas, breccias, and related volcaniclastic sediments that ponded within the 28 Ma San Juan-Uncompahgre caldera complex. These rock units generally have conformable contacts and have shallow dips to the northwest. Lava flows of pyroxene andesite, which host the Roy-Pray mine, are massive near their base and typically grade upward into tightly jointed rock with 2-15 cm joint spacing. In general, most hydrothermally altered rock within the Palmetto Gulch area is restricted to envelopes surrounding the mineralized veins and faults. Composite zones of vein-related alteration vary from about 50 to 80 m wide along the high ridgelines and narrow to less than 10 to 15 m beneath an elevation of about 5,462 m. Where unaffected by surficial oxidation, these altered zones contain as much as 7 to 10 volume percent finely-disseminated pyrite. The majority of rocks in the area were affected by regional and vein-related propylitic alteration. These greenish-colored rocks have alteration products consisting of chlorite, illite, and calcite; and feldspars are typically weakly altered. Most of these rocks have detectable amounts of calcite, while as much as 11 percent by weight was detected in samples collected during this study. The Palmetto Gulch area is affected by low pH and metal-bearing drainage from abandoned mines, and perhaps, from natural weathering around vein zones. To investigate these anthropogenic and potential natural sources of acidity and metals, we mapped the geology, veins, and hydrothermally altered areas; conducted mine dump leachate studies; and collected reconnaissance water quality data. Several small abandoned mines are present in the Palmetto Gulch area that produced small amounts of relatively high-grade silver ore from fault-controlled polymetallic vein deposits. These veins are hosted in lavas, breccias, and related volcaniclastic sediments that ponded within the 28 Ma San Juan-Uncompahgre caldera complex. These rock units generally have conformable contacts and have shallow dips to the northwest. Lava flows of pyroxene andesite, which host the Roy-Pray mine, are massive near their base and typically grade upward into tightly jointed rock with 2-15 cm joint spacing. In general, most hydrothermally altered rock within the Palmetto Gulch area is restricted to envelopes surrounding the mineralized veins and faults. Composite zones of vein-related alteration vary from about 50 to 80 m wide along the high ridgelines and narrow to less than 10 to 15 m beneath an elevation of about 5,462 m. Where unaffected by surficial oxidation, these altered zones contain as much as 7 to 10 volume percent finely-disseminated pyrite. The majority of rocks in the area were affected by regional and vein-related propylitic alteration. These greenish-colored rocks have alteration products consisting of chlorite, illite, and calcite; and feldspars are typically weakly altered. Most of these rocks have detectable amounts of calcite, while as much as 11 percent by weight was detected in samples collected during this study.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02275","usgsCitation":"Bove, D.J., Kurtz, J.P., and Wright, W.G., 2002, Geology, mineralization, and hydrothermal alteration and relationships to acidic and metal-bearing surface waters in the Palmetto Gulch area, southwestern Colorado: U.S. Geological Survey Open-File Report 2002-275, 35 p., https://doi.org/10.3133/ofr02275.","productDescription":"35 p.","costCenters":[],"links":[{"id":110335,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52039.htm","linkFileType":{"id":5,"text":"html"},"description":"52039"},{"id":3629,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0275/","linkFileType":{"id":5,"text":"html"}},{"id":173053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Colorado","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c61f","contributors":{"authors":[{"text":"Bove, Dana J. dbove@usgs.gov","contributorId":4855,"corporation":false,"usgs":true,"family":"Bove","given":"Dana","email":"dbove@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":222618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurtz, Jeffrey P.","contributorId":108174,"corporation":false,"usgs":true,"family":"Kurtz","given":"Jeffrey","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":222620,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, Winfield G.","contributorId":27044,"corporation":false,"usgs":true,"family":"Wright","given":"Winfield","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222619,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44280,"text":"ofr02193 - 2002 - Strategic vision for the U. S. Geological Survey in the Great Lakes-St. Lawrence Region, 2001-2010","interactions":[],"lastModifiedDate":"2020-03-27T06:49:53","indexId":"ofr02193","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-193","title":"Strategic vision for the U. S. Geological Survey in the Great Lakes-St. Lawrence Region, 2001-2010","docAbstract":"<p>The U.S. Geological Survey's (USGS) strategic vision for the Great Lakes-St. Lawrence Region is that of a healthy ecosystem, whose ecological integrity and economic health are nurtured and sustained through sound resource-management decisions based on reliable, timely, and objective scientific information and data. The USGS is a leader in providing reliable, relevant, timely, and objective scientific data and information at local, statewide, regional, national, and international scales to assist in the management and restoration of the natural resources in the Great Lakes-St. Lawrence Region. The mission of the USGS in the Great Lakes-St. Lawrence Region is to provide natural science information to the broad community of policymakers, resource managers, regulators, scientists, and private citizens who contribute to informed decisions concerning natural-resource management practices and ecosystem quality and integrity. The strategic vision for the USGS in the Great Lakes-St. Lawrence Region is a plan to address complex issues that require integrated natural-science information. </p><p>The strategic vision describes how the USGS will coordinate existing programs and draw upon the strengths of the entire organization. It provides the framework for long-term coordination and integration of USGS Programs and activities over the next decade (2001-10). The strategic vision describes the role of the USGS in the Great Lakes-St. Lawrence Region, the coordination of activities within and outside the Bureau and Department of Interior, and interactions between the USGS and its cooperators, partners, and stakeholders in the Region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02193","usgsCitation":"Myers, D.N., Chambers, M., Dawson, V.K., Eberts, S.M., Fisher, M., Foose, M.P., Freiberger, H.J., Gannon, J., Greene, D.A., Hutchinson, D., McNeal, J.M., Milton, N., Nicholas, J.R., Peters, C.A., Stone, B.D., Varanka, D.E., Hickman, C.E., and Wiltshire, D.A., 2002, Strategic vision for the U. S. Geological Survey in the Great Lakes-St. Lawrence Region, 2001-2010: U.S. Geological Survey Open-File Report 2002-193, iv, 16 p., https://doi.org/10.3133/ofr02193.","productDescription":"iv, 16 p.","costCenters":[],"links":[{"id":172349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0193/report-thumb.jpg"},{"id":81640,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0193/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Canada, United States","otherGeospatial":"Great Lakes-St. Lawrence region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -69.60937499999999,\n              47.07012182383309\n            ],\n            [\n              -70.6201171875,\n              47.724544549099676\n   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dnmyers@usgs.gov","orcid":"https://orcid.org/0000-0001-6359-2865","contributorId":512,"corporation":false,"usgs":true,"family":"Myers","given":"Donna","email":"dnmyers@usgs.gov","middleInitial":"N.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":531536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chambers, M.J.","contributorId":93009,"corporation":false,"usgs":true,"family":"Chambers","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":785547,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dawson, Verdel K.","contributorId":81836,"corporation":false,"usgs":true,"family":"Dawson","given":"Verdel","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":785548,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eberts, Sandra M. 0000-0001-5138-8293 smeberts@usgs.gov","orcid":"https://orcid.org/0000-0001-5138-8293","contributorId":127844,"corporation":false,"usgs":true,"family":"Eberts","given":"Sandra","email":"smeberts@usgs.gov","middleInitial":"M.","affiliations":[{"id":38131,"text":"WMA - Office of Planning and Programming","active":true,"usgs":true}],"preferred":true,"id":785549,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fisher, Marion","contributorId":19871,"corporation":false,"usgs":true,"family":"Fisher","given":"Marion","email":"","affiliations":[],"preferred":false,"id":785550,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":785551,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Freiberger, Herbert 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and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":785555,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"McNeal, James M. jmcneal@usgs.gov","contributorId":2810,"corporation":false,"usgs":true,"family":"McNeal","given":"James","email":"jmcneal@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":785556,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Milton, Nancy","contributorId":85188,"corporation":false,"usgs":true,"family":"Milton","given":"Nancy","affiliations":[],"preferred":false,"id":785557,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Nicholas, James R.","contributorId":149200,"corporation":false,"usgs":false,"family":"Nicholas","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":785558,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Peters, Charles A. capeters@usgs.gov","contributorId":214,"corporation":false,"usgs":true,"family":"Peters","given":"Charles","email":"capeters@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":785559,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Stone, Byron D. 0000-0001-6092-0798 bdstone@usgs.gov","orcid":"https://orcid.org/0000-0001-6092-0798","contributorId":1702,"corporation":false,"usgs":true,"family":"Stone","given":"Byron","email":"bdstone@usgs.gov","middleInitial":"D.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":785560,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Varanka, Dalia E. 0000-0003-2857-9600 dvaranka@usgs.gov","orcid":"https://orcid.org/0000-0003-2857-9600","contributorId":1296,"corporation":false,"usgs":true,"family":"Varanka","given":"Dalia","email":"dvaranka@usgs.gov","middleInitial":"E.","affiliations":[{"id":404,"text":"NGTOC Rolla","active":true,"usgs":true},{"id":5074,"text":"Center for Geospatial Information Science (CEGIS)","active":true,"usgs":true}],"preferred":true,"id":785561,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Hickman, Charles E.","contributorId":223598,"corporation":false,"usgs":false,"family":"Hickman","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":785562,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Wiltshire, Denise A.","contributorId":78717,"corporation":false,"usgs":true,"family":"Wiltshire","given":"Denise","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":785563,"contributorType":{"id":1,"text":"Authors"},"rank":18}]}}
,{"id":39927,"text":"ofr02273 - 2002 - Digital version of \"Open-File Report 92-183: Geologic map of the Granite Spring Quadrangle, San Bernardino County, California\"","interactions":[],"lastModifiedDate":"2023-06-27T15:51:08.37388","indexId":"ofr02273","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-273","title":"Digital version of \"Open-File Report 92-183: Geologic map of the Granite Spring Quadrangle, San Bernardino County, California\"","docAbstract":"<p>This is a digital map database version of a previous printed geologic map, U.S. Geological Survey Open-File Report 92–183. The original paper map has been faithfully reproduced as a geologic map database for use in a GIS, and thus does not contain updated geologic information for the map area. This publication consists of three parts:</p>\n<br/>\n<p>1. Documentation in the form of a this publication's Open File text, or readme, describing the digital data, how to obtain it, as well as the original map explanation pamphlet. The documentation also consists of FGDC metadata, and a file describing any revisions to the data in this report. All of the documentaion components are available in a variety of file formats.<br/>\n2. Three Arc/Info (ESRI) formatted coverages of the geologic database, distributed in Arc Interchange (e00) format. The spatial databases in this component of the report consist vector-based GIS datasets that represent geologic contacts, faults, map units, and volcanic vents in the study area, as well as localities of K/Ar samples discussed in the original report, and geologic structure measurements.<br/>\n3. Plottable map representations of the database at 1:24,000 scale in PostScript and Adobe PDF formats. The plottable files consist of a color geologic map derived from the spatial database, composited with a topographic base map in the form of the USGS Digital Raster Graphic for the map area. Color symbology from each of these datasets is maintained, which can cause plot file sizes to be large.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02273","usgsCitation":"Wilshire, H.G., Bedford, D., and Coleman, T., 2002, Digital version of \"Open-File Report 92-183: Geologic map of the Granite Spring Quadrangle, San Bernardino County, California\": U.S. Geological Survey Open-File Report 2002-273, Report: 27 p.; 1 Plate: 22.0 x 32.0 inches; 3 Metadata Files; 4 Data Files, https://doi.org/10.3133/ofr02273.","productDescription":"Report: 27 p.; 1 Plate: 22.0 x 32.0 inches; 3 Metadata Files; 4 Data Files","numberOfPages":"27","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":172486,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02273.jpg"},{"id":110331,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52000.htm","linkFileType":{"id":5,"text":"html"},"description":"52000"},{"id":3627,"rank":6,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0273/","linkFileType":{"id":5,"text":"html"}},{"id":283811,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0273/of02-273data.tar"},{"id":283810,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0273/pdf/of02-273_3a.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":283808,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0273/pdf/of02-273_1a.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":283809,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0273/of02-273_1b.html"}],"scale":"24000","projection":"Universal Transverse Mercator","datum":"1927 North American Datum","country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.875,35.25 ], [ -115.875,35.375 ], [ -115.75,35.375 ], [ -115.75,35.25 ], [ -115.875,35.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bc3","contributors":{"authors":[{"text":"Wilshire, Howard G.","contributorId":68346,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":222612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, Teresa","contributorId":42282,"corporation":false,"usgs":true,"family":"Coleman","given":"Teresa","email":"","affiliations":[],"preferred":false,"id":222613,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39930,"text":"ofr02278 - 2002 - June 2002 floods in the Red River of the North basin in northeastern North Dakota and northwestern Minnesota","interactions":[],"lastModifiedDate":"2023-12-04T21:16:55.323764","indexId":"ofr02278","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-278","title":"June 2002 floods in the Red River of the North basin in northeastern North Dakota and northwestern Minnesota","docAbstract":"<p>The Red River of the North is a complex river system in the north-central plains of the United States.&nbsp; The river continues to affect the people and property within its basin.&nbsp; During June of 2002, major flooding occurred for the third time in 5 years in the Red River of the North Basin, especially on tributaries in northwestern Minnesota.&nbsp; The worst damage occurred in Roseau, Minn., where about 95 percent of the town was inundated.&nbsp; Extensive damage to roads, bridges, and crops occurred throughout the flooded area in northwestern Minnesota and northeastern North Dakota.&nbsp; Roseau County, Minn., was designated a major disaster area on June 14, 2002, by President Bush and later twelve more counties were added to the disaster declaration.&nbsp; Unlike the 1997 floods, which were the result of record-high, region-wide snowpacks and a late spring blizzard, the June 2002 floods were the result of heavy rainfall that swept across the region on June 9-10 and again on June 22-24, 2002.&nbsp;</p>\n<p>Flooding in the Red River of the North Basin commonly is caused by spring snowmelt, and the severity of the flooding is affected by (1) substantial precipitation in the fall that produces high levels of soil moisture; (2) above-normal snowfall in the winter; (3) moist, frozen ground that prohibits infiltration of moisture; (4) a late spring thaw; (5) above-normal precipitation during spring thaw; and (6) ice jams (temporary dams of ice) on rivers and streams.&nbsp; Flooding during June 2002, however, was not caused by most factors usually associated with major flooding in the Red River Basin.&nbsp; In fact, precipitation had been below normal since late last summer and as of June 1, 2002, the flooded area was in a moderate drought based on the Palmer Drought Severity Index.&nbsp;</p>\n<p>The U.S. Geological Survey (USGS), one of the principal Federal agencies responsible for the collection and interpretation of water-resources data, works with other Federal, State, and local agencies to ensure that accurate and timely data are available for making decisions regarding the public's welfare (a listing of cooperators in the Red River Basin is given at the end of this report).&nbsp; This report presents preliminary meteorologic data provided by the National Weather Service, Grand Forks Office and water-resources 2002 flood data that were obtained from selected streamflow-gaging stations located in the Red River of the North Basin (fig. 1).</p>\n<p>Historical peak stages and peak discharges and the June 2002 peak stages, peak discharges, and recurrence intervals are shown in table 1.&nbsp; The streamflow-gaging stations are listed in downstream order by station number, and station locations are shown in figure 1.&nbsp; The June 2002 peak stages and peak discharges given in this preliminary report may be revised as site surveys are completed and additional field data are reviewed in the upcoming months.&nbsp; The peak discharges are used to determine the probability, often expressed in recurrence intervals, that a given discharge will be exceeded in the future.&nbsp; For example, a flood that has a 1-percent chance of exceedance in any given year would, on the long-term average, be expected to occur only about once a century; therefore, the flood would be termed a \"100-year flood.\"&nbsp; However, the chance of such a flood occurring in any given year is 1 percent.&nbsp; Thus, a 100-year flood can occur in successive years at the same location.&nbsp; In some instances, recurrence interval estimates can be based on periods of regulated flow or made with historic adjustments when historic data are available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02278","usgsCitation":"Wiche, G.J., Guttormson, K., Robinson, S., Mitton, G., and Bramer, B., 2002, June 2002 floods in the Red River of the North basin in northeastern North Dakota and northwestern Minnesota: U.S. Geological Survey Open-File Report 2002-278, 8 p., https://doi.org/10.3133/ofr02278.","productDescription":"8 p.","numberOfPages":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":3630,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/ofr02278/ofr02278.pdf","text":"Report","size":"342 kB","linkFileType":{"id":1,"text":"pdf"}},{"id":319951,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02278.JPG"}],"country":"United States","state":"Minnesota, North Dakota","otherGeospatial":"Red River of the North basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.4052734375, 49.001843917978526 ], [ -99.99755859375, 48.99463598353408 ], [ -99.964599609375, 48.915279853443806 ], [ -99.755859375, 48.88639177703194 ], [ -99.755859375, 48.719961222646276 ], [ 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-95.350341796875, 48.65468584817256 ], [ -95.372314453125, 48.741700879765396 ], [ -95.3173828125, 48.821332549646634 ], [ -95.33935546875, 48.90805939965008 ], [ -95.4052734375, 49.001843917978526 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48df","contributors":{"authors":[{"text":"Wiche, Gregg J. gjwiche@usgs.gov","contributorId":1675,"corporation":false,"usgs":true,"family":"Wiche","given":"Gregg","email":"gjwiche@usgs.gov","middleInitial":"J.","affiliations":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guttormson, K.G.","contributorId":78359,"corporation":false,"usgs":true,"family":"Guttormson","given":"K.G.","affiliations":[],"preferred":false,"id":222623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robinson, S.M.","contributorId":79162,"corporation":false,"usgs":true,"family":"Robinson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":222624,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mitton, G.B.","contributorId":104517,"corporation":false,"usgs":true,"family":"Mitton","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":222625,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bramer, B.J.","contributorId":42093,"corporation":false,"usgs":true,"family":"Bramer","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":222622,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":39806,"text":"wri024158 - 2002 - Evaluation of factors affecting ice forces at selected bridges in South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"wri024158","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-4158","title":"Evaluation of factors affecting ice forces at selected bridges in South Dakota","docAbstract":"During 1998-2002, the U.S. Geological Survey, in cooperation with the South Dakota Department of Transportation (SDDOT), conducted a study to evaluate factors affecting ice forces at selected bridges in South Dakota. The focus of this ice-force evaluation was on maximum ice thickness and ice-crushing strength, which are the most important variables in the SDDOT bridge-design equations for ice forces in South Dakota.\r\n\r\nSix sites, the James River at Huron, the James River near Scotland, the White River near Oacoma/Presho, the Grand River at Little Eagle, the Oahe Reservoir near Mobridge, and the Lake Francis Case at the Platte-Winner Bridge, were selected for collection of ice-thickness and ice-crushing-strength data. Ice thickness was measured at the six sites from February 1999 until April 2001. This period is representative of the climate extremes of record in South Dakota because it included both one of the warmest and one of the coldest winters on record. The 2000 and 2001 winters were the 8th warmest and 11th coldest winters, respectively, on record at Sioux Falls, South Dakota, which was used to represent the climate at all bridges in South Dakota.\r\n\r\nIce thickness measured at the James River sites at Huron and Scotland during 1999-2001 ranged from 0.7 to 2.3 feet and 0 to 1.7 feet, respectively, and ice thickness measured at the White River near Oacoma/Presho site during 2000-01 ranged from 0.1 to 1.5 feet. At the Grand River at Little Eagle site, ice thickness was measured at 1.2 feet in 1999, ranged from 0.5 to 1.2 feet in 2000, and ranged from 0.2 to 1.4 feet in 2001. Ice thickness measured at the Oahe Reservoir near Mobridge site ranged from 1.7 to 1.8 feet in 1999, 0.9 to 1.2 feet in 2000, and 0 to 2.2 feet in 2001. At the Lake Francis Case at the Platte-Winner Bridge site, ice thickness ranged from 1.2 to 1.8 feet in 2001.\r\n\r\nHistorical ice-thickness data measured by the U.S. Geological Survey (USGS) at eight selected streamflow-gaging stations in South Dakota were compiled for 1970-97. The gaging stations included the Grand River at Little Eagle, the White River near Oacoma, the James River near Scotland, the James River near Yankton, the Vermillion River near Wakonda, the Vermillion River near Vermillion, the Big Sioux River near Brookings, and the Big Sioux River near Dell Rapids.\r\n\r\nThree ice-thickness-estimation equations that potentially could be used for bridge design in South Dakota were selected and included the Accumulative Freezing Degree Day (AFDD), Incremental Accumulative Freezing Degree Day (IAFDD), and Simplified Energy Budget (SEB) equations. These three equations were evaluated by comparing study-collected and historical ice-thickness measurements to equation-estimated ice thicknesses. Input data required by the equations either were collected or compiled for the study or were obtained from the National Weather Service (NWS). An analysis of the data indicated that the AFDD equation best estimated ice thickness in South Dakota using available data sources with an average variation about the measured value of about 0.4 foot.\r\n\r\nMaximum potential ice thickness was estimated using the AFDD equation at 19 NWS stations located throughout South Dakota. The 1979 winter (the coldest winter on record at Sioux Falls) was the winter used to estimate the maximum potential ice thickness. The estimated maximum potential ice thicknesses generally are largest in northeastern South Dakota at about 3 feet and are smallest in southwestern and south-central South Dakota at about 2 feet.\r\n\r\nFrom 1999 to 2001, ice-crushing strength was measured at the same six sites where ice thickness was measured. Ice-crushing-strength measurements were done both in the middle of the winter and near spring breakup. The maximum ice-crushing strengths were measured in the mid- to late winter before the spring thaw. Measured ice-crushing strengths were much smaller near spring breakup.\r\n\r\nIce-crushing strength measured at the six sites ","language":"ENGLISH","doi":"10.3133/wri024158","usgsCitation":"Niehus, C.A., 2002, Evaluation of factors affecting ice forces at selected bridges in South Dakota: U.S. Geological Survey Water-Resources Investigations Report 2002-4158, v, 102 p. : ill. (some col.), maps (some col.) ; 28 cm., https://doi.org/10.3133/wri024158.","productDescription":"v, 102 p. : ill. (some col.), maps (some col.) ; 28 cm.","costCenters":[],"links":[{"id":3547,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024158/","linkFileType":{"id":5,"text":"html"}},{"id":173314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fadea","contributors":{"authors":[{"text":"Niehus, Colin A.","contributorId":86815,"corporation":false,"usgs":true,"family":"Niehus","given":"Colin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":222231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39926,"text":"ofr02272 - 2002 - Digital version of \"Open-File Report 92-181: Geologic map of the Indian Spring quadrangle, San Bernardino County, California\"","interactions":[],"lastModifiedDate":"2023-06-27T15:49:08.460559","indexId":"ofr02272","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-272","title":"Digital version of \"Open-File Report 92-181: Geologic map of the Indian Spring quadrangle, San Bernardino County, California\"","docAbstract":"This is a digital map database version of a previous printed geologic map, U.S. Geological Survey Open-File Report 92–181. The original paper map has been faithfully reproduced as a geologic map database for use in a GIS, and thus does not contain updated geologic information for the map area. This publication consists of three parts:\n\nDocumentation in the form of a this publication's Open File text, or readme, describing the digital data, how to obtain it, as well as the original map explanation pamphlet. The documentation also consists of FGDC metadata, and a file describing any revisions to the data in this report. All of the documentaion components are available in a variety of file formats.\nThree Arc/Info (ESRI) formatted coverages of the geologic database, distributed in Arc Interchange (e00) format. The spatial databases in this component of the report consist vector-based GIS datasets that represent geologic contacts, faults, map units, and volcanic vents in the study area, as well as localities of K/Ar samples discussed in the original report, and geologic structure measurements.\nPlottable map representations of the database at 1:24,000 scale in PostScript and Adobe PDF formats. The plottable files consist of a color geologic map derived from the spatial database, composited with a topographic base map in the form of the USGS Digital Raster Graphic for the map area. Color symbology from each of these datasets is maintained, which can cause plot file sizes to be large.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02272","usgsCitation":"Wilshire, H.G., Bedford, D., and Coleman, T., 2002, Digital version of \"Open-File Report 92-181: Geologic map of the Indian Spring quadrangle, San Bernardino County, California\": U.S. Geological Survey Open-File Report 2002-272, Report: 27 p.; 1 Plate: 22.00 × 32.00 inches; Metadata, https://doi.org/10.3133/ofr02272.","productDescription":"Report: 27 p.; 1 Plate: 22.00 × 32.00 inches; Metadata","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":172485,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02272.jpg"},{"id":283713,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0272/pdf/of02-272_3a.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":3626,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0272/","linkFileType":{"id":5,"text":"html"}},{"id":283712,"rank":3,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0272/of02-272_1b.html"},{"id":283711,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0272/pdf/of02-272_1a.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.875,35.125 ], [ -115.875,35.250 ], [ -115.750,35.250 ], [ -115.750,35.125 ], [ -115.875,35.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae6e","contributors":{"authors":[{"text":"Wilshire, Howard G.","contributorId":68346,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":222609,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, Teresa","contributorId":42282,"corporation":false,"usgs":true,"family":"Coleman","given":"Teresa","email":"","affiliations":[],"preferred":false,"id":222610,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39925,"text":"ofr02271 - 2002 - Digital version of \"Open-File Report 92-182: Geologic map of the Marl Mountains quadrangle, San Bernardino County, California\"","interactions":[],"lastModifiedDate":"2023-06-27T15:47:04.802615","indexId":"ofr02271","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-271","title":"Digital version of \"Open-File Report 92-182: Geologic map of the Marl Mountains quadrangle, San Bernardino County, California\"","docAbstract":"This is a digital map database version of a previous U.S. Geological Survey Open-File Report, OF92-182. It contains 3 Arc/Info formatted coverages, distributed in Arc Interchange format, a plottable map representation of the database at 1:24,000 scale in Postscript and Adobe PDF formats, and the original map explanation pamphlet in text, Postscript, and Adobe PDF formats.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02271","usgsCitation":"Wilshire, H.G., Bedford, D., and Coleman, T., 2002, Digital version of \"Open-File Report 92-182: Geologic map of the Marl Mountains quadrangle, San Bernardino County, California\": U.S. Geological Survey Open-File Report 2002-271, Report: 27 p.; Metadata, https://doi.org/10.3133/ofr02271.","productDescription":"Report: 27 p.; Metadata","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":172386,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02271.jpg"},{"id":283628,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0271/","linkFileType":{"id":5,"text":"html"}},{"id":397964,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51998.htm"},{"id":283629,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0271/of02-271_1b.html"},{"id":283630,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0271/pdf/of02-271_1a.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Marl Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.750,35.125 ], [ -115.750,32.250 ], [ -115.625,32.250 ], [ -115.625,35.125 ], [ -115.750,35.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64afde","contributors":{"authors":[{"text":"Wilshire, Howard G.","contributorId":68346,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222608,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedford, David R.","contributorId":26352,"corporation":false,"usgs":true,"family":"Bedford","given":"David R.","affiliations":[],"preferred":false,"id":222606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coleman, Teresa","contributorId":42282,"corporation":false,"usgs":true,"family":"Coleman","given":"Teresa","email":"","affiliations":[],"preferred":false,"id":222607,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39921,"text":"ofr02240 - 2002 - Preliminary data from analysis of base-flow separation in part of the Republican River Basin, Nebraska, Kansas, and Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"ofr02240","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-240","title":"Preliminary data from analysis of base-flow separation in part of the Republican River Basin, Nebraska, Kansas, and Colorado","language":"ENGLISH","doi":"10.3133/ofr02240","usgsCitation":"Landon, M.K., and McGuire, V.L., 2002, Preliminary data from analysis of base-flow separation in part of the Republican River Basin, Nebraska, Kansas, and Colorado: U.S. Geological Survey Open-File Report 2002-240, 7 p. plus electronic files, https://doi.org/10.3133/ofr02240.","productDescription":"7 p. plus electronic files","costCenters":[],"links":[{"id":172382,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6a9","contributors":{"authors":[{"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":222599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGuire, Virginia L. 0000-0002-3962-4158 vlmcguir@usgs.gov","orcid":"https://orcid.org/0000-0002-3962-4158","contributorId":404,"corporation":false,"usgs":true,"family":"McGuire","given":"Virginia","email":"vlmcguir@usgs.gov","middleInitial":"L.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39918,"text":"ofr02157 - 2002 - Hawaiian Volcano Observatory summary 101: Part 1, seismic data, January to December 2001","interactions":[],"lastModifiedDate":"2022-10-14T18:52:09.01045","indexId":"ofr02157","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-157","title":"Hawaiian Volcano Observatory summary 101: Part 1, seismic data, January to December 2001","docAbstract":"<p>The Hawaiian Volcano Observatory (HVO) summary presents seismic data gathered during the year and a chronological narrative describing the volcanic events. The seismic summary is offered without interpretation as a source of preliminary data. It is complete in the sense that all data for events of M>1.5 routinely gathered by the Observatory are included. The emphasis in collection of tilt and deformation data has shifted from quarterly measurements at a few water-tube tilt stations (\"wet\" tilt) to a larger number of continuously recording borehole tiltmeters, repeated measurements at numerous spirit-level tilt stations (\"dry\" tilt), and surveying of level and trilateration networks. Because of the large quantity of deformation data now gathered and differing schedules of data reduction, the seismic and deformation summaries are published separately.</p>\n<br/>\n<p>The HVO summaries have been published in various forms since 1956. Summaries prior to 1974 were issued quarterly, but cost, convenience of preparation and distribution, and the large quantities of data dictated an annual publication beginning with Summary 74 for the year 1974. Summary 86 (the introduction of CUSP at HVO) includes a description of the seismic instrumentation, calibration, and processing used in recent years. The present summary includes enough background information on the seismic network and processing to allow use of the data and to provide an understanding of how they were gathered.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02157","usgsCitation":"Nakata, J.S., and Heliker, C., 2002, Hawaiian Volcano Observatory summary 101: Part 1, seismic data, January to December 2001: U.S. Geological Survey Open-File Report 2002-157, i, 70 p., https://doi.org/10.3133/ofr02157.","productDescription":"i, 70 p.","numberOfPages":"72","temporalStart":"2001-01-01","temporalEnd":"2001-12-31","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":283465,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02157.jpg"},{"id":408338,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51557.htm","linkFileType":{"id":5,"text":"html"}},{"id":67740,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0157/pdf/of02-157.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":3622,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0157/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Hawai'i","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.0678,\n              18.9083\n            ],\n            [\n              -154.8047,\n              18.9083\n            ],\n            [\n              -154.8047,\n              20.275\n            ],\n            [\n              -156.0678,\n              20.275\n            ],\n            [\n              -156.0678,\n              18.9083\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f1cf","contributors":{"authors":[{"text":"Nakata, Jennifer S.","contributorId":18364,"corporation":false,"usgs":true,"family":"Nakata","given":"Jennifer","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":222595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heliker, C.","contributorId":7763,"corporation":false,"usgs":true,"family":"Heliker","given":"C.","affiliations":[],"preferred":false,"id":222594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39924,"text":"ofr02268 - 2002 - Porphyry copper deposits of the world: Database, maps, and preliminary analysis","interactions":[{"subject":{"id":39924,"text":"ofr02268 - 2002 - Porphyry copper deposits of the world: Database, maps, and preliminary analysis","indexId":"ofr02268","publicationYear":"2002","noYear":false,"title":"Porphyry copper deposits of the world: Database, maps, and preliminary analysis"},"predicate":"SUPERSEDED_BY","object":{"id":70877,"text":"ofr20051060 - 2005 - Porphyry copper deposits of the world: database, map, and grade and tonnage models","indexId":"ofr20051060","publicationYear":"2005","noYear":false,"title":"Porphyry copper deposits of the world: database, map, and grade and tonnage models"},"id":1}],"supersededBy":{"id":70877,"text":"ofr20051060 - 2005 - Porphyry copper deposits of the world: database, map, and grade and tonnage models","indexId":"ofr20051060","publicationYear":"2005","noYear":false,"title":"Porphyry copper deposits of the world: database, map, and grade and tonnage models"},"lastModifiedDate":"2023-06-27T16:00:21.716856","indexId":"ofr02268","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-268","title":"Porphyry copper deposits of the world: Database, maps, and preliminary analysis","docAbstract":"Mineral deposit models are important in exploration planning and quantitative resource assessments for two reasons: (1) grades and tonnages among deposit types are significantly different, and (2) many types occur in different geologic settings that can be identified from geologic maps. Mineral deposit models are the keystone in combining the diverse geoscience information on geology, mineral occurrences, geophysics, and geochemistry used in resource assessments and mineral exploration. Far too few thoroughly explored mineral deposits are available in most local areas for reliable identification of the important geoscience variables or for robust estimation of undiscovered deposits—thus we need mineral-deposit models. Globally based deposit models, such as those presented here, allow recognition of important features because the global models demonstrate how common different features are. Well-designed and -constructed deposit models allow geologists to know from observed geologic environments the possible mineral deposit types that might exist, and allow economists to determine the possible economic viability of these resources in the region. Thus, mineral deposit models play the central role in transforming geoscience information to a form useful to policy makers. The foundation of mineral deposit models is information about known deposits—the purpose of this publication is to make this kind of information available in digital form for a group of porphyry copper deposits.\n\nThis publication contains a computer file of information on porphyry copper deposits around the world. It also presents new grade and tonnage models for three subtypes of porphyry copper deposits, maps showing locations and general ages of these deposits, and a preliminary analysis with a number of figures summarizing many of the properties of these porphyry-style deposits. These summaries can be considered a new, quantified, form of most parts of descriptive models such as those in Cox and Singer (1986). The value of this information and analyses depends critically on the consistent manner of data gathering. For this reason, we first discuss the rules used in this compilation. Next the fields of the data file are considered. Finally, we discuss some of the things that can be done with the data.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02268","usgsCitation":"Singer, D.A., Berger, V.I., and Moring, B.C., 2002, Porphyry copper deposits of the world: Database, maps, and preliminary analysis: U.S. Geological Survey Open-File Report 2002-268, Report: 61 p.; 6 Plates 48.00 inches x 36.00 inches or smaller; Data Files, https://doi.org/10.3133/ofr02268.","productDescription":"Report: 61 p.; 6 Plates 48.00 inches x 36.00 inches or smaller; Data Files","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":172385,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02268.jpg"},{"id":283636,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/map2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":283635,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/map1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":283633,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0268/","linkFileType":{"id":5,"text":"html"}},{"id":283634,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/of02-268.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":283641,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/map6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":283640,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/map5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":283638,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/map4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":283637,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0268/pdf/map3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683cc2","contributors":{"authors":[{"text":"Singer, Donald A. dsinger@usgs.gov","contributorId":5601,"corporation":false,"usgs":true,"family":"Singer","given":"Donald","email":"dsinger@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":222604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, Vladimir I.","contributorId":15246,"corporation":false,"usgs":true,"family":"Berger","given":"Vladimir","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":222605,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moring, Barry C. 0000-0001-6797-9258 moring@usgs.gov","orcid":"https://orcid.org/0000-0001-6797-9258","contributorId":2794,"corporation":false,"usgs":true,"family":"Moring","given":"Barry","email":"moring@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":222603,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39802,"text":"wri024107 - 2002 - Effects of wastewater and combined sewer overflows on water quality in the Blue River basin, Kansas City, Missouri and Kansas, July 1998-October 2000","interactions":[],"lastModifiedDate":"2023-03-07T20:37:16.268822","indexId":"wri024107","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-4107","title":"Effects of wastewater and combined sewer overflows on water quality in the Blue River basin, Kansas City, Missouri and Kansas, July 1998-October 2000","docAbstract":"Samples were collected from 16 base-flow\r\nevents and a minimum of 10 stormflow events\r\nbetween July 1998 and October 2000 to characterize\r\nthe effects of wastewater and combined sewer\r\noverflows on water quality in the Blue River\r\nBasin, Kansas City, Missouri and Kansas. Waterquality\r\neffects were determined by analysis of\r\nnutrients, chloride, chemical and biochemical oxygen\r\ndemand, and suspended sediment samples\r\nfrom three streams (Blue River, Brush Creek, and\r\nIndian Creek) in the basin as well as the determination\r\nof a suite of compounds known to be indicative\r\nof wastewater including antioxidants,\r\ncaffeine, detergent metabolites, antimicrobials,\r\nand selected over-the-counter and prescription\r\npharmaceuticals. Constituent loads were determined\r\nfor both hydrologic regimes and a measure\r\nof the relative water-quality impact of selected\r\nstream reaches on the Blue River and Brush Creek\r\nwas developed. Genetic fingerprint patterns of\r\nEscherichia coli bacteria from selected stream\r\nsamples were compared to a data base of knownsource\r\npatterns to determine possible sources of\r\nbacteria.\r\nWater quality in the basin was affected by\r\nwastewater during both base flows and stormflows;\r\nhowever, there were two distinct sources\r\nthat contributed to these effects. In the Blue River\r\nand Indian Creek, the nearly continuous discharge\r\nof treated wastewater effluent was the primary\r\nsource of nutrients, wastewater indicator compounds,\r\nand pharmaceutical compounds detected\r\nin stream samples. Wastewater inputs into Brush\r\nCreek were largely the result of intermittent stormflow\r\nevents that triggered the overflow of combined\r\nstorm and sanitary sewers, and the\r\nsubsequent discharge of untreated wastewater into\r\nthe creek. A portion of the sediment, organic matter,\r\nand associated constituents from these events\r\nwere trapped by a series of impoundments constructed\r\nalong Brush Creek where they likely continued\r\nto affect water quality during base flow.\r\nConcentrations and loads of most wastewater\r\nconstituents in the Blue River and Indian Creek were\r\nsignificantly greater than in Brush Creek, especially\r\nduring base flow. However, wastewater indicator\r\ncompound concentrations were sometimes greater\r\nin some Brush Creek stormflow samples. Selected\r\nstream reaches along the mid-portion of Brush\r\nCreek showed higher effects relative to other sites,\r\nprimarily because these sites were in impounded\r\nreaches with the greatest density of wastewater\r\ninputs, or had relatively small drainage areas.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri024107","usgsCitation":"Wilkison, D.H., Armstrong, D., and Blevins, D.W., 2002, Effects of wastewater and combined sewer overflows on water quality in the Blue River basin, Kansas City, Missouri and Kansas, July 1998-October 2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4107, iv, 162 p., https://doi.org/10.3133/wri024107.","productDescription":"iv, 162 p.","costCenters":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"links":[{"id":413784,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52033.htm","linkFileType":{"id":5,"text":"html"}},{"id":8500,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri02-4107/","linkFileType":{"id":5,"text":"html"}},{"id":172592,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Kansas, Missouri","city":"Kansas City","otherGeospatial":"Blue River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.875,\n              38.750\n            ],\n            [\n              -94.875,\n              39.125\n            ],\n            [\n              -94.5667,\n              39.125\n            ],\n            [\n              -94.5667,\n              38.750\n            ],\n            [\n              -94.875,\n              38.750\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fc33","contributors":{"authors":[{"text":"Wilkison, Donald H. wilkison@usgs.gov","contributorId":3824,"corporation":false,"usgs":true,"family":"Wilkison","given":"Donald","email":"wilkison@usgs.gov","middleInitial":"H.","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armstrong, Daniel J. armstron@usgs.gov","contributorId":3823,"corporation":false,"usgs":true,"family":"Armstrong","given":"Daniel J.","email":"armstron@usgs.gov","affiliations":[{"id":396,"text":"Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":222223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blevins, Dale W. dblevins@usgs.gov","contributorId":2729,"corporation":false,"usgs":true,"family":"Blevins","given":"Dale","email":"dblevins@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":222222,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39882,"text":"ofr02282 - 2002 - Topographic map of Mars M 25M RKN","interactions":[],"lastModifiedDate":"2014-03-10T16:02:23","indexId":"ofr02282","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-282","title":"Topographic map of Mars M 25M RKN","docAbstract":"NOTES ON BASE\n\nThis map is based on data from the Mars Orbiter Laser Altimeter (MOLA) (Smith and others, 2001), an instrument on NASA's Mars Global Surveyor (MGS) spacecraft (Albee and others, 2001). The image used for the base of this map represents more than 600 million measurements gathered between 1999 and 2001, adjusted for consistency (Neumann and others, 2001, 2002) and converted to planetary radii. These have been converted to elevations above the areoid as determined from a martian gravity field solution GMM2 (Lemoine and others, 2001), truncated to degree and order 50, and oriented according to current standards (see below). The average accuracy of each point is originally ~100 meters in horizontal position, and ~1 meter in radius (Neumann, 2001). However, the total elevation uncertainty is at least +3 m due to the global error in the areoid (+1.8 meters according to Lemoine and others, 2001) and regional uncertainties in its shape (communication from Neumann, 2002). The measurements were converted into a digital elevation model (DEM) (communication from Neumann, 2002; Neumann and others, 2001; Smith and others, 2001) using Generic Mapping Tools software (Wessel and Smith, 1998), with a resolution of 0.015625 degrees per pixel or 64 pixels per degree. In projection, the pixels are 926.17 meters in size at the equator.\n\nPROJECTION\n\nThe Mercator projection is used between latitudes +57°, with a central meridian at 0° and latitude equal to the nominal scale at 0°. The Polar Stereographic projection is used for the polar regions north of the +55° parallel and south of the –55° parallel with a central meridian set for both at 0°. The adopted equatorial radius is 3,396.19 km (Duxbury and others 2002; Seidelmann and others 2002).\n\nCOORDINATE SYSTEM\n\nThe MOLA data were initially referenced to an internally consistent inertial coordinate system, derived from tracking of the MGS spacecraft. By adopting appropriate values for the orientation of Mars as defined by the International Astronomical Union (IAU) and the International Association of Geodesy (IAG) (Seidelmann and others, 2002), these inertial coordinates were converted into the planet-fixed coordinates (longitude and latitude) used on this map. These values include the orientation of the north pole of Mars (including the effects of precession), the rotation rate of Mars, and a value for W0 of 176.630°, where W0 is the angle along the equator to the east, between the 0° meridian and the equator's intersection with the celestial equator at the standard epoch J2000.0 (Seidelmann and others, 2002). This value of W0 was chosen (Duxbury and others, 2002) in order to place the 0° meridian through the center of the small (~500 m) crater Airy-0, located in the crater Airy (de Vaucouleurs and others, 1973; Seidelmann and others, 2002). Longitude increases to the east, and latitude is planetocentric as allowed by IAU/IAG standards (Seidelmann and others, 2002) and in accordance with current NASA and USGS standards (Duxbury and others, 2002). A secondary grid (printed in red) has been added to the map as a reference to the west longitude/planetographic latitude system that is also allowed by IAU/IAG standards (Seidelmann and others, 2002) and has also been used for Mars. The figure adopted to compute this secondary grid is an oblate spheroid with an equatorial radius of 3,396.19 km and a polar radius of 3,376.2 km (Duxbury and others, 2002; Seidelmann and others, 2002).\n\nMAPPING TECHNIQUES\n\nTo create the topographic base image, the original DEM produced by the MOLA team in Simple Cylindrical projection with a resolution of 64 pixels per degree was projected into the Mercator and Polar Stereographic pieces. A shaded relief was generated from each DEM with a sun angle of 30° from horizontal and a sun azimuth of 270°, as measured clockwise from north, and a vertical exaggeration of 100%. Illumination is from the west, which follows a long-standing USGS tradition for planetary maps. This allows for continuity in the shading between maps and quadrangles, and most closely resembles lighting conditions found on imagery. The DEM values were then mapped to a smooth global color look-up table. Note that the chosen color scheme simply represents elevation changes and is not intended to imply anything about surface characteristics (e.g., past or current presence of water or ice). These two files were then merged and scaled to 1:25 million for the Mercator portion and 1:15,196,708 for the two Polar Stereographic portions, with a resolution of 300 dots per inch. The projections have a common scale of 1:13,923,113 at +56° latitude.\n\nNOMENCLATURE\n\nNames on this sheet are approved by the IAU and have been applied for features clearly visible at the scale of this map. For a complete list of the IAU-approved nomenclature for Mars, see the Gazetteer of Planetary Nomenclature at http://planetarynames.wr.usgs.gov/. Font color was chosen for readability. Names followed by an asterisk are provisionally approved.\n\n*M 25M RKN: Abbreviation for Mars, 1:25,000,000 series, shaded relief (R), with color (K) and nomenclature (N) (Greeley and Batson, 1990)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02282","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Topographic map of Mars M 25M RKN: U.S. Geological Survey Open-File Report 2002-282, Map: 36.00 inches x 34.00 inches, https://doi.org/10.3133/ofr02282.","productDescription":"Map: 36.00 inches x 34.00 inches","additionalOnlineFiles":"N","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":169765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02282.jpg"},{"id":3593,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0282/pdf/of02-282.pdf","linkFileType":{"id":5,"text":"html"}},{"id":283768,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0282/"}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699881","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":529928,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39923,"text":"ofr02267 - 2002 - Aeromagnetic surveys in the Anchorage, Iliamna, and Tyonek quadrangles, Alaska: A website for the distribution of data","interactions":[],"lastModifiedDate":"2022-10-31T20:49:35.130052","indexId":"ofr02267","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-267","title":"Aeromagnetic surveys in the Anchorage, Iliamna, and Tyonek quadrangles, Alaska: A website for the distribution of data","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02267","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2002, Aeromagnetic surveys in the Anchorage, Iliamna, and Tyonek quadrangles, Alaska: A website for the distribution of data: U.S. Geological Survey Open-File Report 2002-267, HTML Document, https://doi.org/10.3133/ofr02267.","productDescription":"HTML Document","costCenters":[],"links":[{"id":172384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3625,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0267/","linkFileType":{"id":5,"text":"html"}},{"id":408939,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51979.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Anchorage, Iliamna, and Tyonek quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156,\n              59\n            ],\n            [\n              -147,\n              59\n            ],\n            [\n              -147,\n              62\n            ],\n            [\n              -156,\n              62\n            ],\n            [\n              -156,\n              59\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c0b","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":529930,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39917,"text":"ofr02156 - 2002 - Data set of world phosphate mines, deposits, and occurrences: Part A. Geologic data. Part B. Location and mineral economic data","interactions":[],"lastModifiedDate":"2023-06-27T15:44:09.770735","indexId":"ofr02156","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-156","title":"Data set of world phosphate mines, deposits, and occurrences: Part A. Geologic data. Part B. Location and mineral economic data","docAbstract":"An inventory of more than 1,600 world phosphate mines, deposits, and occurrences was compiled from smaller data sets collected as part of multiple research efforts by Carlotta Chernoff, University of Arizona, and Greta Orris, U.S. Geological Survey. These data have been utilized during studies of black shale depositional environments and to construct phosphate deposit models. The compiled data have been edited for consistency and additional location information has been added where possible. The database of compiled phosphate information is being released in two sections; the geologic data in one section and the location and mineral economic data in the second. This report, U.S. Geological Survey Open-File Report 02–156–A, contains the geologic data and is best used with the complimentary data contained in Open-File Report 02–156–B. U.S. Geological Survey Open-File Report 02–156–B contains commodity data, location and analytical data, a variety of mineral economic data, reference information, and pointers to related records in the U.S. Geological Survey National mineral databases—MASMILS and MRDS.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02156","usgsCitation":"Chernoff, C.B., and Orris, G., 2002, Data set of world phosphate mines, deposits, and occurrences: Part A. Geologic data. Part B. Location and mineral economic data: U.S. Geological Survey Open-File Report 2002-156, Report Part A: 352 p.; Report Part B: 328 p.; Readme; Metadata; 2 Data Tables, https://doi.org/10.3133/ofr02156.","productDescription":"Report Part A: 352 p.; Report Part B: 328 p.; Readme; Metadata; 2 Data Tables","numberOfPages":"680","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":173618,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02156.jpg"},{"id":282562,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0156/pdf/OF02-156B.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":3621,"rank":9,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0156/","linkFileType":{"id":5,"text":"html"}},{"id":282563,"rank":6,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0156/README.doc"},{"id":282564,"rank":5,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0156/phos.met"},{"id":282565,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0156/OF02-156A.xls"},{"id":282566,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0156/OF02-156B.xls"},{"id":282561,"rank":7,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0156/pdf/OF02-156A.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406799,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52047.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c7a","contributors":{"authors":[{"text":"Chernoff, Carlotta B.","contributorId":30541,"corporation":false,"usgs":true,"family":"Chernoff","given":"Carlotta","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":222592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orris, G. J.","contributorId":80252,"corporation":false,"usgs":true,"family":"Orris","given":"G. J.","affiliations":[],"preferred":false,"id":222593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39915,"text":"ofr02140 - 2002 - Schlumberger soundings at the Amargosa Desert Research Site, Nevada","interactions":[],"lastModifiedDate":"2020-02-19T19:34:50","indexId":"ofr02140","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-140","title":"Schlumberger soundings at the Amargosa Desert Research Site, Nevada","docAbstract":"<p>In 1999 the U.S. Geological Survey made 38 direct current (dc) electrical soundings at the Amargosa Desert Research Site (ADRS) near Beatty, Nevada (fig. 1.) using the Schlumberger array. An additional 16 Schlumberger soundings were made in 2000. The soundings were made to determine the subsurface resistivity distribution, and the location of faults. The purpose of this report is to present the data, its automatic interpretation, cross sections and resistivity depth maps. Figure 2 is a map of the sounding locations. The soundings are represented by circles. The 1999 data are numbered 1 through 38 and the 2000 data are numbered 101 through 116. Table 1 gives the sounding number, x coordinate, and y coordinate of the soundings in UTM zone 11 NAD27. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02140","usgsCitation":"Bisdorf, R.J., 2002, Schlumberger soundings at the Amargosa Desert Research Site, Nevada: U.S. Geological Survey Open-File Report 2002-140, 65 p., https://doi.org/10.3133/ofr02140.","productDescription":"65 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":3619,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0140/","linkFileType":{"id":5,"text":"html"}},{"id":173616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.3774871826172,\n              36.3588219885685\n            ],\n            [\n              -116.20548248291016,\n              36.3588219885685\n            ],\n            [\n              -116.20548248291016,\n              36.50384103238002\n            ],\n            [\n              -116.3774871826172,\n              36.50384103238002\n            ],\n            [\n              -116.3774871826172,\n              36.3588219885685\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd463","contributors":{"authors":[{"text":"Bisdorf, Robert J.","contributorId":107277,"corporation":false,"usgs":true,"family":"Bisdorf","given":"Robert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":222590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39916,"text":"ofr02145 - 2002 - Ground-water levels and water-quality data from monitoring wells in Windham, Maine, water years 1997-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:10:36","indexId":"ofr02145","displayToPublicDate":"2002-08-01T00:00:00","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":"2002-145","title":"Ground-water levels and water-quality data from monitoring wells in Windham, Maine, water years 1997-2001","docAbstract":"Ongoing data collection in an established well network in Windham, Maine, serves as an indicator of the hydrologic and water-quality conditions in the aquifer. This report presents data collected from 1997 through 2001, including ground-water levels, measurements of water-quality field parameters, and concentrations of nutrients and arsenic.","language":"ENGLISH","doi":"10.3133/ofr02145","usgsCitation":"Caldwell, J.M., 2002, Ground-water levels and water-quality data from monitoring wells in Windham, Maine, water years 1997-2001: U.S. Geological Survey Open-File Report 2002-145, 17 p., https://doi.org/10.3133/ofr02145.","productDescription":"17 p.","costCenters":[],"links":[{"id":173617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3620,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02-145/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a37a","contributors":{"authors":[{"text":"Caldwell, J. M.","contributorId":93934,"corporation":false,"usgs":true,"family":"Caldwell","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":222591,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32803,"text":"pp1644 - 2002 - Geologic investigations in the Lake Valley area, Sierra County, New Mexico","interactions":[{"subject":{"id":21829,"text":"ofr98347 - 1998 - Geology and mineral resources of the Lake Valley area, Sierra County, New Mexico","indexId":"ofr98347","publicationYear":"1998","noYear":false,"title":"Geology and mineral resources of the Lake Valley area, Sierra County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":32803,"text":"pp1644 - 2002 - Geologic investigations in the Lake Valley area, Sierra County, New Mexico","indexId":"pp1644","publicationYear":"2002","noYear":false,"title":"Geologic investigations in the Lake Valley area, Sierra County, New Mexico"},"id":1}],"lastModifiedDate":"2025-01-16T22:20:59.195566","indexId":"pp1644","displayToPublicDate":"2002-08-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1644","title":"Geologic investigations in the Lake Valley area, Sierra County, New Mexico","docAbstract":"At the request of the Bureau of Land Management, the U.S. Geological Survey evaluated the area of the historic Lake Valley mining district and townsite, Sierra County, New Mexico, for its potential for undiscovered mineral resources. The four chapters of this report describe the geology of the area, present the results of geophysical investigations carried out to aid in interpreting subsurface geology, describe the mining history and character of the region's ore deposits, and present geochemical data on potential for contamination from abandoned mine dumps in the mining district.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1644","usgsCitation":"O’Neill, J., Lindsey, D.A., Hedlund, D.C., Nutt, C., Ratte, J., Klein, D.P., Kleinkopf, M.D., Wise, R.A., McLemore, V., and Herring, J., 2002, Geologic investigations in the Lake Valley area, Sierra County, New Mexico (Supersedes Open-File Report 98-347): U.S. Geological Survey Professional Paper 1644, Report: iv, 78 p.; 1 Plate: 37.00 x 49.00 inches, https://doi.org/10.3133/pp1644.","productDescription":"Report: iv, 78 p.; 1 Plate: 37.00 x 49.00 inches","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":122557,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1644/report-thumb.jpg"},{"id":3347,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/p1644/","linkFileType":{"id":5,"text":"html"}},{"id":60784,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1644/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":60783,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1644/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":397887,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51842.htm","text":"Geology of the Lake Valley area [Sierra County, New Mexico]","linkFileType":{"id":5,"text":"html"}},{"id":477596,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51843.htm","text":"Geophysical investigations in the Lake Valley area","linkFileType":{"id":5,"text":"html"}},{"id":477597,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51844.htm","text":"Mineral deposits of the Lake Valley mining district, with a geochemistry appendix","linkFileType":{"id":5,"text":"html"}},{"id":477598,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51845.htm","text":"Geochemistry of mine dump material from the Lake Valley mining district","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"New Mexico","county":"Sierra County","otherGeospatial":"Lake Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.6381,\n              32.875\n            ],\n            [\n              -107.5,\n              32.875\n            ],\n            [\n              -107.5,\n              32.6928\n            ],\n            [\n              -107.6381,\n              32.6928\n            ],\n            [\n              -107.6381,\n              32.875\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Supersedes Open-File Report 98-347","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ff2","contributors":{"editors":[{"text":"O’Neill, J.M.","contributorId":85562,"corporation":false,"usgs":true,"family":"O’Neill","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":696675,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"O’Neill, J.M.","contributorId":85562,"corporation":false,"usgs":true,"family":"O’Neill","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":696665,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":696666,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":696667,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nutt, C.J.","contributorId":52577,"corporation":false,"usgs":true,"family":"Nutt","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":696673,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ratte, J.C.","contributorId":10416,"corporation":false,"usgs":true,"family":"Ratte","given":"J.C.","affiliations":[],"preferred":false,"id":696668,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klein, D. P.","contributorId":36555,"corporation":false,"usgs":true,"family":"Klein","given":"D.","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":696669,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kleinkopf, M. D.","contributorId":10036,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","middleInitial":"D.","affiliations":[],"preferred":false,"id":696670,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wise, R. A.","contributorId":79124,"corporation":false,"usgs":true,"family":"Wise","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":696671,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McLemore, V. T.","contributorId":15225,"corporation":false,"usgs":true,"family":"McLemore","given":"V. T.","affiliations":[],"preferred":false,"id":696672,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":696674,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":70201651,"text":"70201651 - 2002 - Mars Geodesy/Cartography Working Group recommendations on Mars cartographic constants and coordinate systems","interactions":[],"lastModifiedDate":"2019-02-25T10:55:20","indexId":"70201651","displayToPublicDate":"2002-07-19T14:52:32","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mars Geodesy/Cartography Working Group recommendations on Mars cartographic constants and coordinate systems","docAbstract":"<p>NASA's Mars Geodesy/Cartography Working Group (MGCWG), established in 1998 and chaired since 2000 by one of us (TCD), consists of leading researchers in planetary geodesy and cartography at such diverse institutions as JPL, NASA Ames and Goddard Centers, Purdue and Ohio State Universities, Malin Space Science Systems, the German Center for Aerospace Research DLR, and the US Geological Survey, as well as representatives of the current and future Mars mission teams that are the customers for Mars maps. The purpose of the group is the coordinate the activities of the many agencies active in Mars geodesy and cartography in order to minimize redundant effort and ensure that the products needed by mission customers are generated. A specific objectives has been to avoid repeating the experience of the 1970s-80s, when competing researchers produced geodetic control solutions and maps of Mars that were mutually inconsistent. To this end, the MGCWG has recently assembled a set of preferred values for Mars cartographic constants, based on the best available data. These values have been transmitted to the International Astronomical Union and appear in the report of the IAU/IAG Working Group on Cartographic Coordinates and Rotational Elements of the Planets and Satellites as the officially recommended constants for Mars (Seidelmann et al., 2002). The MGCWG has also recommended to NASA that the USGS adopt the IAU-approved coordinate system of planetocentric latitude and east longitude for future maps of Mars, in the place of the (also IAU-approved) planetographic system with west longitude positive. This recommendation has recently been approved by NASA. In this paper we present the preferred values for Mars cartographic constants with discussion of the process by which they were derived, then discuss the rationale and implications of the use of east/planetocentric coordinates in future Mars maps.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geospatial Theory, Processing and Applications: ISPRS Commission IV Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Geospatial Theory, Processing and Applications: ISPRS Commission IV","conferenceDate":"July 9-12, 2002","conferenceLocation":"Ottawa, Canada","language":"English","publisher":"International Society for Photogrammetry and Remote Sensing","usgsCitation":"Duxbury, T.C., Kirk, R.L., Archinal, B.A., and Neumann, G., 2002, Mars Geodesy/Cartography Working Group recommendations on Mars cartographic constants and coordinate systems, <i>in</i> Geospatial Theory, Processing and Applications: ISPRS Commission IV Proceedings, Ottawa, Canada, July 9-12, 2002, 4 p.; DVD-ROM.","productDescription":"4 p.; DVD-ROM","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":360573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":360572,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.isprs.org/proceedings/XXXIV/part4/"}],"otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c1b66e8e4b0708288c71d42","contributors":{"authors":[{"text":"Duxbury, T. C.","contributorId":91983,"corporation":false,"usgs":true,"family":"Duxbury","given":"T.","email":"","middleInitial":"C.","affiliations":[{"id":36392,"text":"Jet Propulsion Laboratory","active":true,"usgs":false}],"preferred":false,"id":754712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754714,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Neumann, G.A.","contributorId":11767,"corporation":false,"usgs":true,"family":"Neumann","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":754715,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70201650,"text":"70201650 - 2002 - USGS high resolution topo-mapping of Mars with Mars Orbiter Camera Narrow-Angle images","interactions":[],"lastModifiedDate":"2019-02-25T10:53:27","indexId":"70201650","displayToPublicDate":"2002-07-19T14:35:53","publicationYear":"2002","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"USGS high resolution topo-mapping of Mars with Mars Orbiter Camera Narrow-Angle images","docAbstract":"<p>We describe our initial experiences producing controlled digital elevation models (DEMs) of Mars with horizontal resolutions of ≤10 m and vertical precisions of ≤2 m. Such models are of intense interest at all phases of Mars exploration and scientific investigation, from the selection of safe landing sites to the quantitative analysis of the morphologic record of surface processes. Topomapping with a resolution adequate to address many of these issues has only become possible with the success of the Mars Global Surveyor (MGS) mission. The Mars Orbiter Laser Altimeter (MOLA) on MGS mapped the planet globally with absolute accuracies &lt;10 m vertically and ~100 m horizontally but relatively sparse sampling (300 m along track, with gaps of &gt;1 km between tracks common at low latitudes). We rely on the MOLA data as the best available source of control and process images from the narrow-angle Mars Orbiter Camera (MOC-NA) with stereo and photoclinometric (shape-from-shading) techniques to produce DEMs with significantly better horizontal resolution. The techniques described here enable mapping not only with MOC but also with the high-resolution cameras (Mars Express HRSC, Mars Reconnaissance Orbiter HiRISE) that will orbit Mars in the next several years.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geospatial Theory, Processing and Applications: ISPRS Commission IV Proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Geospatial Theory, Processing and Applications: ISPRS Commission IV","conferenceDate":"July 9-12, 2002","conferenceLocation":"Ottawa, Canada","language":"English","publisher":"International Society for Photogrammetry and Remote Sensing","usgsCitation":"Kirk, R.L., Soderblom, L.A., Howington-Kraus, E., and Archinal, B.A., 2002, USGS high resolution topo-mapping of Mars with Mars Orbiter Camera Narrow-Angle images, <i>in</i> Geospatial Theory, Processing and Applications: ISPRS Commission IV Proceedings, Ottawa, Canada, July 9-12, 2002, 10 p.; DVD-ROM.","productDescription":"10 p.; DVD-ROM","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":360571,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":360570,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.isprs.org/proceedings/XXXIV/part4/"}],"otherGeospatial":"Comet Borrelly","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c1b66e8e4b0708288c71d45","contributors":{"authors":[{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soderblom, Laurence A. 0000-0002-0917-853X lsoderblom@usgs.gov","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":2721,"corporation":false,"usgs":true,"family":"Soderblom","given":"Laurence","email":"lsoderblom@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howington-Kraus, Elpitha 0000-0001-5787-6554 ahowington@usgs.gov","orcid":"https://orcid.org/0000-0001-5787-6554","contributorId":2815,"corporation":false,"usgs":true,"family":"Howington-Kraus","given":"Elpitha","email":"ahowington@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754710,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":754711,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006435,"text":"70006435 - 2002 - Threats to desert tortoise populations: a critical review of the literature","interactions":[],"lastModifiedDate":"2014-07-01T11:47:46","indexId":"70006435","displayToPublicDate":"2002-07-09T11:30:24","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Threats to desert tortoise populations: a critical review of the literature","docAbstract":"<p>Decision in resource management are generally based on a combination of sociopolitical, economic, and environmental factors, and may be biased by personal values.  These three components often contradict each other resulting in controversy.  Controversies can usually be reduced when solid scientific evidence is used to support or refute a decision.  However, it is important to recognize that data often do little to alter antagonists' positions when differences in values are the bases if the dispute.  But, supporting data can make the decision more defensible, both legally and ethically, especially if the data supporting all opposing viewpoints are included in the decision-making process.</p>\n<br/>\n<p>Resource management decisions must be made using the best scientific information currently available.  However, scientific data vary in two important measures of quality: reliability and validity.  The reliability of the data is a measure of the degree to which the observations or conclusion can be repeated.  Validity of the data is a measure of the degree to which the observation or conclusion reflects what actually occurs in nature.  How the data are collected strongly affects the reliability of validity of ecological conclusions that can be made.  Research data potentially relevant to management come from different sources, and the source often provides clues to the reliability and, to a certain extent, validity of data.  Understanding the quality of data being used to make management decisions helps to separate the philosophical or value-based aspects of arguments from the objective ones, thus helping to clarify the decisions and judgments that need to be made.</p>\n<br/>\n<p>The West Mojave Plan is a multispecies, bioregional plan for the management of natural resources within a 9.4 million-acre area of the Mojave Desert in California.  The plan addresses the legal requirements for the recovery of the desert tortoise (<i>Gopherus agazzizii</i>), a threatened species, but also covers an additional approximately 80 species of plants and animals assigned special status by the Bureau of Land Management, U. S. Fish and Wildlife Service, and California Department of Fish and Game.  Within the planning area, 28 separate jurisdictions (counties, cities, towns, military installations, etc.) seek programmatic prescriptions that will facilitate streamlined environmental review, result in expedited authorization for development projects, and protect listed and unlisted species into the foreseeable future to avoid or minimize conflicts between proposed development and species' conservation and recovery.  All of the scientific data available concerning the biology and management of these approximately 80 species and their habitats must be evaluated to develop a scientifically credible plan.</p>\n<br/>\n<p>This document provides an overview and evaluation of the knowledge of the major threats to the persistence and recovery of desert tortoise populations.  I was specifically asked to evaluate the scientific veracity of the data and reports available.  I summarize the data presently available with particular focus on the West Mojave Desert, evaluate the scientific integrity of the data. and identify major gaps in the available knowledge.  I do not attempt to provide in-depth details on each study or threat; for more details I encourage the reader to consult the individual papers or reports city throughout this report (many of which are available at most university libraries and at the West Mojave Plan office in Riverside, California).  I also do not attempt to characterize or evaluate the past or present management actions, except where they have direct bearing on evaluation of threats, nor do I attempt, for the most part, to acquire, generate, or evaluate new or existing, but uninterpreted data.</p>","language":"English","publisher":"U.S. Geological Survey, Western Ecological Research Center","publisherLocation":"Sacramento, CA","usgsCitation":"Boarman, W.I., 2002, Threats to desert tortoise populations: a critical review of the literature, v, 86 p.","productDescription":"v, 86 p.","numberOfPages":"91","costCenters":[],"links":[{"id":289306,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"West Mojave Desert","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.9789,34.1607 ], [ -117.9789,35.7233 ], [ -115.5164,35.7233 ], [ -115.5164,34.1607 ], [ -117.9789,34.1607 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b3d874e4b07c5f79a7f36e","contributors":{"authors":[{"text":"Boarman, William I.","contributorId":51683,"corporation":false,"usgs":true,"family":"Boarman","given":"William","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":354489,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185669,"text":"70185669 - 2002 - Role of ground water in geomorphology, geology, and paleoclimate of the southern High Plains, USA","interactions":[],"lastModifiedDate":"2018-11-28T10:31:24","indexId":"70185669","displayToPublicDate":"2002-07-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Role of ground water in geomorphology, geology, and paleoclimate of the southern High Plains, USA","docAbstract":"<p><span>Study of ground water in the Southern High Plains is central to an understanding of the geomorphology, deposition of economic minerals, and climate change record in the area. Ground water has controlled the course of the Canadian and Pecos rivers that isolated the Southern High Plains from the Great Plains and has contributed significantly to the continuing retreat of the westward escarpment. Evaporative and dissolution processes are responsible for current plateau topography and the development of the signature 20,000 small playa basins and 40 to 50 large saline lake basins in the area. In conjunction with eolian processes, ground water transport controls the mineralogy of commercially valuable mineral deposits and sets up the distribution of fine efflorescent salts that adversely affect water quality. As the water table rises and retreats, lunette and tufa formation provides valuable paleoclimate data for the Southern High Plains. In all these cases, an understanding of ground water processes contributes valuable information to a broad range of geological topics, well beyond traditional interest in water supply and environmental issues.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.2002.tb02522.x","usgsCitation":"Wood, W., 2002, Role of ground water in geomorphology, geology, and paleoclimate of the southern High Plains, USA: Groundwater, v. 40, no. 4, p. 438-447, https://doi.org/10.1111/j.1745-6584.2002.tb02522.x.","productDescription":"10 p. ","startPage":"438","endPage":"447","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":498965,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1745-6584.2002.tb02522.x","text":"Publisher Index Page"},{"id":338377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, New Mexico, Texas","otherGeospatial":"Southern High Plains ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.34814453125,\n              31.541089879585808\n            ],\n            [\n              -99.00878906249999,\n              31.541089879585808\n            ],\n            [\n              -99.00878906249999,\n              37.59682400108367\n            ],\n            [\n              -104.34814453125,\n              37.59682400108367\n            ],\n            [\n              -104.34814453125,\n              31.541089879585808\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"40","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-12-13","publicationStatus":"PW","scienceBaseUri":"58da2538e4b0543bf7fda845","contributors":{"authors":[{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":686301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33002,"text":"ofr200234 - 2002 - Historical Ice-Out Dates for 29 Lakes in New England","interactions":[],"lastModifiedDate":"2012-03-08T17:16:16","indexId":"ofr200234","displayToPublicDate":"2002-07-01T00:00:00","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":"2002-34","title":"Historical Ice-Out Dates for 29 Lakes in New England","docAbstract":"Historical ice-out dates for 29 lakes in New England were compiled and are presented in this report. The length of record for the lakes ranges from 64 to 163 years, with an average of 108 years. Many lakes in New England had their latest recorded ice-out date in 1888. Ice-out dates for lakes are an important hydrologic data series for climate researchers and other interested parties.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr200234","usgsCitation":"Hodgkins, G.A., and James, I.C., 2002, Historical Ice-Out Dates for 29 Lakes in New England: U.S. Geological Survey Open-File Report 2002-34, 41 p., https://doi.org/10.3133/ofr200234.","productDescription":"41 p.","costCenters":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"links":[{"id":3163,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://me.water.usgs.gov/reports/OFR02-34.pdf","size":"538","linkFileType":{"id":1,"text":"pdf"}},{"id":161135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0034/report-thumb.jpg"},{"id":60877,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74,41 ], [ -74,48 ], [ -67,48 ], [ -67,41 ], [ -74,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae307","contributors":{"authors":[{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":209653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James, Ivan C. III","contributorId":88404,"corporation":false,"usgs":true,"family":"James","given":"Ivan","suffix":"III","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":209654,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}