{"pageNumber":"2806","pageRowStart":"70125","pageSize":"25","recordCount":184612,"records":[{"id":51400,"text":"ofr03251 - 2003 - Chromium geochemistry of serpentinous sediment in the Willow core, Santa Clara County, California","interactions":[],"lastModifiedDate":"2018-12-03T11:18:42","indexId":"ofr03251","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-251","title":"Chromium geochemistry of serpentinous sediment in the Willow core, Santa Clara County, California","docAbstract":"A preliminary investigation of Cr geochemistry in serpentinous sediment completed for a multiple-aquifer ground-water monitoring well (Willow core of Santa Clara County, CA) determined sediment at depths >225 meters contains Cr concentrations ranging from 195 to 1155 mg/kg. Serpentinous sediment from this site is a potential source of non-anthropogenic Cr contamination. Chromium-bearing minerals such as Cr-spinel appear to be the main source of Cr in the sediment; however, Cr-bearing silicates and clay minerals are additional Cr sources. Aqueous Cr concentrations in the sediment are <4.6 mg/L; however, the valence of Cr was not identified in the solutions or in the sediment. Although there is no indication of Cr(VI) contamination derived from the serpentinous sediment, elevated Cr concentrations in the sediment, the observed ‘dissolution’ textures of the Cr-bearing minerals, the estimated redox environment, and water chemistry indicate the formation of Cr(VI) is potentially favorable.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03251","usgsCitation":"Oze, C.J., LaForce, M.J., Wentworth, C.M., Hanson, R.T., Bird, D.K., and Coleman, R.G., 2003, Chromium geochemistry of serpentinous sediment in the Willow core, Santa Clara County, California: U.S. Geological Survey Open-File Report 2003-251, 10 p., https://doi.org/10.3133/ofr03251.","productDescription":"10 p.","numberOfPages":"24","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":178740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03251.jpg"},{"id":285703,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0251/pdf/of03-251.pdf"},{"id":4407,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0251/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Santa Clara County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.0,37.125 ], [ -122.0,37.375 ], [ -121.625,37.375 ], [ -121.625,37.125 ], [ -122.0,37.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e2225","contributors":{"authors":[{"text":"Oze, Christopher J.","contributorId":107774,"corporation":false,"usgs":true,"family":"Oze","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":243466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaForce, Matthew J.","contributorId":65158,"corporation":false,"usgs":true,"family":"LaForce","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":243464,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wentworth, Carl M. 0000-0003-2569-569X cwent@usgs.gov","orcid":"https://orcid.org/0000-0003-2569-569X","contributorId":1178,"corporation":false,"usgs":true,"family":"Wentworth","given":"Carl","email":"cwent@usgs.gov","middleInitial":"M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":243462,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanson, Randall T. 0000-0002-9819-7141 rthanson@usgs.gov","orcid":"https://orcid.org/0000-0002-9819-7141","contributorId":801,"corporation":false,"usgs":true,"family":"Hanson","given":"Randall","email":"rthanson@usgs.gov","middleInitial":"T.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":243461,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bird, Dennis K.","contributorId":9339,"corporation":false,"usgs":true,"family":"Bird","given":"Dennis","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":243463,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Coleman, Robert G.","contributorId":88022,"corporation":false,"usgs":true,"family":"Coleman","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":243465,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":53109,"text":"ofr03326 - 2003 - Petroleum systems of the Alaskan North Slope: a numerical journey from source to trap","interactions":[],"lastModifiedDate":"2018-08-31T13:35:43","indexId":"ofr03326","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-326","title":"Petroleum systems of the Alaskan North Slope: a numerical journey from source to trap","docAbstract":"The complex petroleum province of the Alaskan North Slope contains six petroleum systems (Magoon and others, this session). Source rocks for four of these systems include the Hue-gamma ray zone (Hue-GRZ), pebble shale unit, Kingak Shale, and Shublik Formation. Geochemical data for these source rocks are investigated in greater detail and provide the basis for numerical petroleum migration models.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03326","usgsCitation":"Lampe, C., Peters, K.E., Magoon, L.B., Bird, K.J., and Lillis, P., 2003, Petroleum systems of the Alaskan North Slope: a numerical journey from source to trap: U.S. Geological Survey Open-File Report 2003-326, Sheet 1: 96.00 x 36.00 inches; Sheet 2: 93.75 x 37.50 inches; Sheet 3: 93.75 x 37.50 inches, https://doi.org/10.3133/ofr03326.","productDescription":"Sheet 1: 96.00 x 36.00 inches; Sheet 2: 93.75 x 37.50 inches; Sheet 3: 93.75 x 37.50 inches","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":173962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03326.jpg"},{"id":4670,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0326/","linkFileType":{"id":5,"text":"html"}},{"id":285777,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0326/pdf/sheet2.pdf"},{"id":285778,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0326/pdf/sheet3.pdf"},{"id":285776,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0326/pdf/sheet1.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -166.85,68.0 ], [ -166.85,71.39 ], [ -141.0,71.39 ], [ -141.0,68.0 ], [ -166.85,68.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687d77","contributors":{"authors":[{"text":"Lampe, C.","contributorId":104138,"corporation":false,"usgs":true,"family":"Lampe","given":"C.","email":"","affiliations":[],"preferred":false,"id":246668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, K. E.","contributorId":17295,"corporation":false,"usgs":true,"family":"Peters","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":246664,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Magoon, L. B.","contributorId":44531,"corporation":false,"usgs":true,"family":"Magoon","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":246666,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bird, K. J.","contributorId":57824,"corporation":false,"usgs":false,"family":"Bird","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":246667,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lillis, P. G. 0000-0002-7508-1699","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":17630,"corporation":false,"usgs":true,"family":"Lillis","given":"P. G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":246665,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":52666,"text":"ofr03246 - 2003 - Aquifer Susceptibility in Virginia: Data on Chemical and Isotopic Composition, Recharge Temperature, and Apparent Age of Water from Wells and Springs, 1998-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:11:26","indexId":"ofr03246","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-246","title":"Aquifer Susceptibility in Virginia: Data on Chemical and Isotopic Composition, Recharge Temperature, and Apparent Age of Water from Wells and Springs, 1998-2000","docAbstract":"The determination of aquifer susceptibility to contamination from near-surface sources by the use of \r\nground-water dating techniques is a critical part of Virginia's Source Water Assessment Program. As part of the Virginia Aquifer Susceptibility study, water samples were collected between 1998 and 2000 from 145 wells and 6 springs in various hydrogeologic settings across the Commonwealth. Samples were analyzed to determine water chemistry?including nitrate (NO3), dissolved organic carbon (DOC), and radon-222 (222Rn), major dissolved and noble gases?nitrogen (N2), argon (Ar), oxygen (O2), carbon dioxide (CO2), methane (CH4), helium (He), and neon (Ne), environmental tracers?chlorofluorocarbons (CFCs), sulfur hexafluoride (SF6), tritium (3H), and tritium/helium-3 (3H/3He), carbon isotopes?carbon-14 (14C) and carbon-13 (d13C), and stable isotopes of oxygen (d18O) and hydrogen (d2H). The chemical and isotopic composition, recharge temperatures, and apparent ages of these water samples are presented in this report. Data collected between 1999 and 2000 from 18 wells in Virginia as part of two other studies by the U.S. Geological Survey also are presented. Most of the sites sampled serve as public water supplies and are included in the comprehensive Source Water Assessment Program for the Commonwealth.","language":"ENGLISH","doi":"10.3133/ofr03246","usgsCitation":"Nelms, D.L., and Harlow, G., 2003, Aquifer Susceptibility in Virginia: Data on Chemical and Isotopic Composition, Recharge Temperature, and Apparent Age of Water from Wells and Springs, 1998-2000 (ONLINE ONLY): U.S. Geological Survey Open-File Report 2003-246, 101 p., 19 tables, https://doi.org/10.3133/ofr03246.","productDescription":"101 p., 19 tables","onlineOnly":"Y","costCenters":[],"links":[{"id":5164,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-246/","linkFileType":{"id":5,"text":"html"}},{"id":178376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"ONLINE ONLY","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679fd5","contributors":{"authors":[{"text":"Nelms, David L. 0000-0001-5747-642X dlnelms@usgs.gov","orcid":"https://orcid.org/0000-0001-5747-642X","contributorId":1892,"corporation":false,"usgs":true,"family":"Nelms","given":"David","email":"dlnelms@usgs.gov","middleInitial":"L.","affiliations":[{"id":37759,"text":"VA/WV Water Science Center","active":true,"usgs":true},{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":245749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harlow, George E. Jr. geharlow@usgs.gov","contributorId":383,"corporation":false,"usgs":true,"family":"Harlow","given":"George E.","suffix":"Jr.","email":"geharlow@usgs.gov","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":245748,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53070,"text":"ofr2003271 - 2003 - Archive of chirp seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June 30 - July 9 and August 1 - 12, 2001","interactions":[],"lastModifiedDate":"2022-06-29T21:25:08.550555","indexId":"ofr2003271","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-271","title":"Archive of chirp seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June 30 - July 9 and August 1 - 12, 2001","docAbstract":"In June, July, and August of 2001, the U.S. Geological Survey (USGS), in cooperation with the University of New Orleans, the U.S. Army Corps of Engineers, and the Louisiana Department of Natural Resources, conducted a shallow geophysical and sediment core survey of Timbalier Bay and the Gulf of Mexico offshore East Timbalier Island, Louisiana. This report serves as an archive of unprocessed digital seismic reflection data, trackline navigation files, trackline navigation maps, observers' logbooks, Geographic Information Systems (GIS) information, and formal Federal Geographic Data Committee (FGDC) metadata. In addition, a gained digital Graphics Interchange Format (GIF) image of each seismic profile is provided. Please see Kulp and others (2002), Flocks and others (2003), and Kulp and others (in prep.) for further information about the sediment cores collected and the geophysical results. For convenience, a list of acronyms and abbreviations frequently used in this report is also included.\r\n\r\nThis Digital Versatile Disc (DVD) document is readable on any computing platform that has standard DVD driver software installed. Documentation on this DVD was produced using Hyper Text Markup Language (HTML) utilized by the World Wide Web (WWW) and allows the user to access the information using a web browser (i.e. Netscape, Internet Explorer). To access the information contained on these discs, open the file 'index.htm' located at the top level of each disc using a web browser. This report also contains WWW links to USGS collaborators and other agencies. These links are only accessible if access to the internet is available while viewing these DVDs.\r\n\r\nThe archived chirp seismic reflection data are in standard Society of Exploration Geophysicists (SEG) SEG-Y format (Barry et al., 1975) and may be downloaded for processing with public domain software such as Seismic Unix (SU), currently located at http://www.cwp.mines.edu/cwpcodes/index.html. Examples of SU processing scripts are provided in the CHIRP.tar file located in the SU subfolder of the SOFTWARE folder located at the top level of each disc. In-house (USGS) DOS and Microsoft Windows compatible software for viewing SEG-Y headers - DUMPSEGY.EXE (Zihlman, 1992) - is provided in the USGS subfolder of the SOFTWARE folder. Processed profile images, trackline navigation maps, logbooks, and formal metadata may be viewed with a web browser.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2003271","usgsCitation":"Calderon, K., Dadisman, S.V., Flocks, J.G., Wiese, D.S., and Kindinger, J.L., 2003, Archive of chirp seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June 30 - July 9 and August 1 - 12, 2001: U.S. Geological Survey Open-File Report 2003-271, HTML Document; 4 DVD-ROMs, https://doi.org/10.3133/ofr2003271.","productDescription":"HTML Document; 4 DVD-ROMs","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"2001-06-30","temporalEnd":"2001-08-12","costCenters":[{"id":159,"text":"Center for Coastal and Watershed Studies","active":false,"usgs":true},{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":12036,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-271/","linkFileType":{"id":5,"text":"html"}},{"id":402724,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70847.htm","linkFileType":{"id":5,"text":"html"}},{"id":181001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Louisiana","otherGeospatial":"Timbalier Bay and offshore East Timbalier Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.34582519531249,\n              29.08977693862319\n            ],\n            [\n              -90.1593017578125,\n              29.08977693862319\n            ],\n            [\n              -90.1593017578125,\n              29.286398892934763\n            ],\n            [\n              -91.34582519531249,\n              29.286398892934763\n            ],\n            [\n              -91.34582519531249,\n              29.08977693862319\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679db6","contributors":{"authors":[{"text":"Calderon, Karynna","contributorId":92739,"corporation":false,"usgs":true,"family":"Calderon","given":"Karynna","email":"","affiliations":[],"preferred":false,"id":246545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":246543,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":246542,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":246544,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kindinger, Jack L. jkindinger@usgs.gov","contributorId":815,"corporation":false,"usgs":true,"family":"Kindinger","given":"Jack","email":"jkindinger@usgs.gov","middleInitial":"L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":246541,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":52926,"text":"wri034029 - 2003 - Hydrogeology of shallow basin-fill deposits in areas of Salt Lake Valley, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2017-02-07T15:53:38","indexId":"wri034029","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4029","title":"Hydrogeology of shallow basin-fill deposits in areas of Salt Lake Valley, Salt Lake County, Utah","docAbstract":"<p>A study of recently developed residential/commercial areas of Salt Lake Valley, Utah, was done from 1999 to 2001 in areas in which shallow ground water has the potential to move to a deeper aquifer that is used for public supply. Thirty monitoring wells were drilled and sampled in 1999 as part of the study. The ground water was either under unconfined or confined conditions, depending on depth to water and the presence or absence of fine-grained deposits. The wells were completed in the shallowest water-bearing zone capable of supplying water. Monitoring-well depths range from 23 to 154 feet. Lithologic, geophysical, hydraulic-conductivity, transmissivity, water-level, and water-temperature data were obtained for or collected from the wells.</p><p>Silt and clay layers noted on lithologic logs correlate with increases in electrical conductivity and natural gamma radiation shown on many of the electromagnetic-induction and natural gamma logs. Relatively large increases in electrical conductivity, determined from the electromagnetic-induction logs, with no major changes in natural gamma radiation are likely caused by increased dissolved-solids content in the ground water. Some intervals with high electrical conductivity correspond to areas in which water was present during drilling.</p><p>Unconfined conditions were present at 7 of 20 monitoring wells on the west side and at 2 of 10 wells on the east side of Salt Lake Valley. Fine-grained deposits confine the ground water. Anthropogenic compounds were detected in water sampled from most of the wells, indicating a connection with the land surface. Data were collected from 20 of the monitoring wells to estimate the hydraulic conductivity and transmissivity of the shallow ground-water system. Hydraulic-conductivity values of the shallow aquifer ranged from 30 to 540 feet per day. Transmissivity values of the shallow aquifer ranged from 3 to 1,070 feet squared per day. There is a close linear relation between transmissivity determined from slug-test analysis and transmissivity estimated from specific capacity.</p><p>Water-level fluctuations were measured in the 30 monitoring wells from 1999 to July 2001. Generally, water-level changes measured in wells on the west side of the valley followed a seasonal trend and wells on the east side showed less fluctuation or a gradual decline during the 2-year period. This may indicate that a larger percentage of recharge to the shallow ground-water system on the west side is from somewhat consistent seasonal sources, such as canals and unconsumed irrigation water, as compared to sources on the east side. Water levels measured in monitoring wells completed in the shallow ground-water system near large-capacity public-supply wells varied in response to ground-water withdrawals from the deeper confined aquifer. Water temperature was monitored in 23 wells. Generally, little or no change in water temperature was measured in monitoring wells with a depth to water greater than about 40 feet. The shallower the water level in the well, the greater the water-temperature change measured during the study.</p><p>Comparison of water levels measured in the monitoring wells and deeper wells in the same area indicate a downward gradient on the east side of the valley. Water levels in the shallow and deeper aquifers in the secondary recharge area on the west side of the valley were similar to those on the east side. Water levels measured in the monitoring wells and nearby wells completed in the deeper aquifer indicate that the vertical gradient can change with time and stresses on the system.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/wri034029","usgsCitation":"Thiros, S.A., 2003, Hydrogeology of shallow basin-fill deposits in areas of Salt Lake Valley, Salt Lake County, Utah: U.S. Geological Survey Water-Resources Investigations Report 2003-4029, Report: viii, 23 p.; 1 Plate: 33.0 x 25.0 inches, https://doi.org/10.3133/wri034029.","productDescription":"Report: viii, 23 p.; 1 Plate: 33.0 x 25.0 inches","numberOfPages":"32","costCenters":[{"id":610,"text":"Utah Water Science 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,{"id":48851,"text":"ofr03172 - 2003 - User's Manual for the National Water-Quality Assessment Program Invertebrate Data Analysis System (IDAS) Software: Version 3","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr03172","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-172","title":"User's Manual for the National Water-Quality Assessment Program Invertebrate Data Analysis System (IDAS) Software: Version 3","docAbstract":"The Invertebrate Data Analysis System (IDAS) software provides an accurate, consistent, and efficient mechanism for analyzing invertebrate data collected as part of the National Water-Quality Assessment Program and stored in the Biological Transactional Database (Bio-TDB). The IDAS software is a stand-alone program for personal computers that run Microsoft (MS) Windows?. It allows users to read data downloaded from Bio-TDB and stored either as MS Excel? or MS Access? files. The program consists of five modules. The Edit Data module allows the user to subset, combine, delete, and summarize community data. The Data Preparation module allows the user to select the type(s) of sample(s) to process, calculate densities, delete taxa based on laboratory processing notes, combine lifestages or keep them separate, select a lowest taxonomic level for analysis, delete rare taxa, and resolve taxonomic ambiguities. The Calculate Community Metrics module allows the user to calculate over 130 community metrics, including metrics based on organism tolerances and functional feeding groups. The Calculate Diversities and Similarities module allows the user to calculate nine diversity and eight similarity indices. The Data export module allows the user to export data to other software packages and produce tables of community data that can be imported into spreadsheet and word-processing programs. Though the IDAS program was developed to process invertebrate data downloaded from USGS databases, it will work with other data sets that are converted to the USGS (Bio-TDB) format. Consequently, the data manipulation, analysis, and export procedures provided by the IDAS program can be used by anyone involved in using benthic macroinvertebrates in applied or basic research.","language":"ENGLISH","doi":"10.3133/ofr03172","usgsCitation":"Cuffney, T.F., 2003, User's Manual for the National Water-Quality Assessment Program Invertebrate Data Analysis System (IDAS) Software: Version 3 (Version 3): U.S. Geological Survey Open-File Report 2003-172, 114 p., https://doi.org/10.3133/ofr03172.","productDescription":"114 p.","costCenters":[],"links":[{"id":169785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4071,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03172/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db603f9c","contributors":{"authors":[{"text":"Cuffney, Thomas F. 0000-0003-1164-5560 tcuffney@usgs.gov","orcid":"https://orcid.org/0000-0003-1164-5560","contributorId":517,"corporation":false,"usgs":true,"family":"Cuffney","given":"Thomas","email":"tcuffney@usgs.gov","middleInitial":"F.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":238429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51968,"text":"wri034080 - 2003 - Simulation of ground-water flow in the Cedar River alluvium, northwest Black Hawk County and southwest Bremer County, Iowa","interactions":[],"lastModifiedDate":"2023-04-04T19:33:04.183409","indexId":"wri034080","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4080","title":"Simulation of ground-water flow in the Cedar River alluvium, northwest Black Hawk County and southwest Bremer County, Iowa","docAbstract":"<p>Flooding and high ground-water levels after large or frequent rainstorms have occurred in an area of about 30 square miles along the eastern bank of the Cedar River from Cedar Falls in northwest Black Hawk County to Janesville in southwest Bremer County, Iowa. The U.S. Geological Survey, in cooperation with Black Hawk County, conducted a hydrologic study of the Cedar River alluvium in the northwest Black Hawk and southwest Bremer Counties, to improve understanding of the ground-water flow system and evaluate the effects of hypothetical variations in recharge and discharge conditions.</p>\n<p>A steady-state ground-water flow model was constructed for the area using November 2001 hydrologic conditions. The model was discretized into an 83-row by 47-column grid of cells measuring approximately 500 feet by 500 feet. Two model layers, one for the alluvium and one for the underlying bedrock units, were used to represent flow in the area.</p>\n<p>Precipitation during 2001 was similar to historical normals. Precipitation during 1999, especially during the summer when flooding occurred, was well above the historical normals. Borings in the unconsolidated deposits in the study area confirmed the presence of a bedrock valley dipping to the south in the central part of the study area. Water-level measurements in 2001 indicate that ground-water flow in much of the alluvial aquifer parallels the direction of flow in the Cedar River toward the south rather than following shorter flow paths to the west toward the Cedar River.</p>\n<p>Under steady-state conditions and 2001 pumpage, primary sources of inflow to the ground-water flow system are the Cedar River (65.5 percent), recharge through infiltration of precipitation and upland runoff (31.4 percent), and subsurface flow across the lateral boundaries (3.1 percent). The primary components of outflow from the ground-water flow system are intermittent streams (56.0 percent) and the Cedar River (43.7 percent).</p>\n<p>Two hypothetical scenarios were used to assess the potential effects of higher river levels and increased recharge compared to the steadystate conditions. For one scenario, river levels were set to bankfull conditions, and a recharge of 1.2 times the steady-state rate was applied. This simulation was used to evaluate the effects of wet conditions. This scenario led to increased water levels, in general, and large areas of shallow (0 to 10 feet) depths to water along the eastern part of the model area near Highway 218. For the second scenario, conditions were the same as for the first scenario, but streambed conductance of intermittent streams modeled as drains was increased to 10 times the steady-state value to simulate increased flow of water from the shallow groundwater flow system. The area with depth to water of 0 to 10 feet along the eastern part of the model area was substantially smaller than that of the first scenario.</p>\n<p>In general, once high ground-water levels occur, either because of high Cedar River water Abstract levels or above normal local precipitation or both, ground-water in the central part of the study area along Highway 218 flows toward the south rather than following shorter flow paths to the Cedar River. Intermittent streams in the study area discharge substantial amounts of water from the ground-water flow system.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri034080","collaboration":"Prepared in cooperation with Black Hawk County, Iowa","usgsCitation":"Schaap, B.D., Savoca, M.E., and Turco, M.J., 2003, Simulation of ground-water flow in the Cedar River alluvium, northwest Black Hawk County and southwest Bremer County, Iowa: U.S. Geological Survey Water-Resources Investigations Report 2003-4080, iv, 42 p., https://doi.org/10.3133/wri034080.","productDescription":"iv, 42 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":415184,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":53085,"text":"ofr03349 - 2003 - Interpreting DNAPL saturations in a laboratory-scale injection with GPR data and direct core measurements","interactions":[],"lastModifiedDate":"2012-02-02T00:11:56","indexId":"ofr03349","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-349","title":"Interpreting DNAPL saturations in a laboratory-scale injection with GPR data and direct core measurements","docAbstract":"Ground penetrating radar (GPR) is used to track a dense non-aqueous phase liquid (DNAPL) injection in a laboratory sand tank. Before data reduction, GPR data provide a qualitative measure of DNAPL saturation and movement. One-dimensional (1D) GPR modeling provides a quantitative interpretation of DNAPL volume within a given thickness during and after the injection. This is confirmed qualitatively by visual inspection of cores and two-dimensional GPR modeling. DNAPL saturation in sub-layers of that thickness could not be quantified because calibration of the 1D GPR model is non-unique when both permittivity and depth of multiple layers are unknown. Accurate quantitative interpretation of DNAPL volumes using 1D GPR modeling requires: 1) identification of a suitable target that produces a strong reflection and is not subject to any multidimensional interference; 2) knowledge of the exact depth of that target; and 3) use of two-way radar-wave travel times through the medium to the target to determine the permittivity of the intervening material, which eliminates reliance upon reflection amplitude. With geologic conditions that are suitable for GPR surveys (i.e., shallow depths and low electrical conductivities), the procedures in this laboratory study can be adapted to a field site to identify DNAPL source zones after a release has occurred.","language":"ENGLISH","doi":"10.3133/ofr03349","usgsCitation":"Johnson, R.H., and Poeter, E.P., 2003, Interpreting DNAPL saturations in a laboratory-scale injection with GPR data and direct core measurements (Version 1.0): U.S. Geological Survey Open-File Report 2003-349, 39 p., https://doi.org/10.3133/ofr03349.","productDescription":"39 p.","costCenters":[],"links":[{"id":182030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5283,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-349/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e02ee","contributors":{"authors":[{"text":"Johnson, Raymond H. rhjohnso@usgs.gov","contributorId":707,"corporation":false,"usgs":true,"family":"Johnson","given":"Raymond","email":"rhjohnso@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":246594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poeter, Eileen P.","contributorId":78805,"corporation":false,"usgs":true,"family":"Poeter","given":"Eileen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":246595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53087,"text":"ofr03360 - 2003 - Shaded relief aeromagnetic map of the Santa Clara Valley and vicinity, California","interactions":[],"lastModifiedDate":"2023-06-22T16:53:43.931696","indexId":"ofr03360","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-360","title":"Shaded relief aeromagnetic map of the Santa Clara Valley and vicinity, California","docAbstract":"This aeromagnetic map covers the southern portion of San Francisco Bay, the Santa Clara Valley and surrounding mountains, part of which has been modelled in threedimensions (Jachens and other, 2001). The magnetic anomaly map has been compiled from existing digital data. Data was obtained from six aeromagnetic surveys that were flown at different times, spacings and elevations. The International Geomagnetic Reference Field (IGRF) for the date of each survey had been removed in the initial processing. The resulting residual magnetic anomalies were analytically continued onto a common surface 305 m (1000 ft) above terrain. Portions of each survey were substantially above the specified flight height listed in the table. The surveys were then merged together using a commercial software package called Oasis Montage. The gray lines on the map indicate the extent of each survey. The program used these regions of overlap to determine the best fit between surveys. Black dots show probable edges of magnetic bodies defined by the maximum horizontal gradient determined using a computer program by Blakely (1995).\n\nCrystalline rocks generally contain sufficient magnetic minerals to cause variations in the Earth’s magnetic field that can be mapped by aeromagnetic surveys. Sedimentary rocks are generally weakly magnetized and consequently have a small effect on the magnetic field: thus a magnetic anomaly map can be used to “see through” the sedimentary rock cover and can convey information on lithologic contrasts and structural trends related to the underlying crystalline basement (see Nettleton,1971; Blakely, 1995). Faults often cut magnetic bodies and offset magnetic anomalies can thus be used to help determine fault motion. Serpentinite, which is highly magnetic, is often found along faults. On this map areas of low magnetic anomalies are shown in blues and green while highs are shown in reds and magentas. Faults are from Brabb and others, 1998a,1998b, Graymer and others 1996, Lienkaemper, 1992 and Wentworth and others 1998.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03360","usgsCitation":"Roberts, C.W., and Jachens, R.C., 2003, Shaded relief aeromagnetic map of the Santa Clara Valley and vicinity, California: U.S. Geological Survey Open-File Report 2003-360, 1 Plate: 36.00 inches x 48.00 inches, https://doi.org/10.3133/ofr03360.","productDescription":"1 Plate: 36.00 inches x 48.00 inches","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":180790,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03360.jpg"},{"id":285817,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0360/pdf/of03-360.pdf"},{"id":285782,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0360/"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.25,37.0000 ], [ -122.25,37.6333 ], [ -121.50,37.6333 ], [ -121.50,37.0000 ], [ -122.25,37.0000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4a24","contributors":{"authors":[{"text":"Roberts, Carter W.","contributorId":45282,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":246602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":246601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53092,"text":"ofr03377 - 2003 - Empirical modified Mercalli intensity site corrections for towns in eastern North America","interactions":[],"lastModifiedDate":"2014-04-07T13:56:58","indexId":"ofr03377","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-377","title":"Empirical modified Mercalli intensity site corrections for towns in eastern North America","docAbstract":"Modified Mercalli intensity (MMI) assignments for earthquakes in eastern North America (ENA) were used by Bakun et al. (2003) and Bakun and Hopper (in press) to develop models for estimating the location and moment magnitude M of earthquakes in ENA from MMI observations. The MMI empirical site corrections developed and used by Bakun et al. (2003) and Bakun and Hopper (in press) are listed in this Open-file Report.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03377","usgsCitation":"Bakun, W.H., and Hopper, M.G., 2003, Empirical modified Mercalli intensity site corrections for towns in eastern North America: U.S. Geological Survey Open-File Report 2003-377, 33 p., https://doi.org/10.3133/ofr03377.","productDescription":"33 p.","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":180887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03377.jpg"},{"id":285837,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0377/"},{"id":285838,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0377/pdf/of03-377.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db603f41","contributors":{"authors":[{"text":"Bakun, W. H.","contributorId":67055,"corporation":false,"usgs":true,"family":"Bakun","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":246621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hopper, M. G.","contributorId":39389,"corporation":false,"usgs":true,"family":"Hopper","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":246620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52903,"text":"fs08503 - 2003 - 2002 Assessment of undiscovered oil and gas resources: Cretaceous Travis Peak and Hosston Formations, Jurassic Smackover Interior Salt Basins Total Petroleum System, Louisiana-Mississippi Salt Basins Province, northern Gulf Coast Region","interactions":[],"lastModifiedDate":"2022-07-01T19:17:16.282444","indexId":"fs08503","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"085-03","title":"2002 Assessment of undiscovered oil and gas resources: Cretaceous Travis Peak and Hosston Formations, Jurassic Smackover Interior Salt Basins Total Petroleum System, Louisiana-Mississippi Salt Basins Province, northern Gulf Coast Region","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs08503","usgsCitation":"Dyman, T.S., Condon, S.M., Charpentier, R., Cook, T.A., Crovelli, R., Klett, T., Lewan, M.D., Pollastro, R.M., Schenk, C.J., and Schmoker, J., 2003, 2002 Assessment of undiscovered oil and gas resources: Cretaceous Travis Peak and Hosston Formations, Jurassic Smackover Interior Salt Basins Total Petroleum System, Louisiana-Mississippi Salt Basins Province, northern Gulf Coast Region (Version 1.0): U.S. Geological Survey Fact Sheet 085-03, 2 p., https://doi.org/10.3133/fs08503.","productDescription":"2 p.","costCenters":[],"links":[{"id":122263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_085_03.jpg"},{"id":4966,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/fs-085-03/","linkFileType":{"id":5,"text":"html"}},{"id":402870,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_58864.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alabama, Arkansas, Florida, Louisiana, Mississippi, Texas","otherGeospatial":"Gulf Coast","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.3310546875,\n              30.107117887092357\n            ],\n            [\n              -87.6708984375,\n              32.36140331527543\n            ],\n            [\n              -89.8681640625,\n              33.50475906922609\n            ],\n            [\n              -91.93359375,\n              33.65120829920497\n            ],\n            [\n              -94.21875,\n              34.23451236236987\n            ],\n            [\n              -95.5810546875,\n              34.05265942137599\n            ],\n            [\n              -97.822265625,\n              33.063924198120645\n            ],\n            [\n              -98.0419921875,\n              29.99300228455108\n            ],\n            [\n              -93.6474609375,\n              30.486550842588485\n            ],\n            [\n              -89.4287109375,\n              30.675715404167743\n            ],\n            [\n              -86.9677734375,\n              30.56226095049944\n            ],\n            [\n              -84.3310546875,\n              30.107117887092357\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd491de4b0b290850eee73","contributors":{"authors":[{"text":"Dyman, T. S.","contributorId":21161,"corporation":false,"usgs":false,"family":"Dyman","given":"T.","middleInitial":"S.","affiliations":[],"preferred":false,"id":246183,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condon, S. M.","contributorId":107688,"corporation":false,"usgs":true,"family":"Condon","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Charpentier, Ronald R.","contributorId":33674,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","affiliations":[],"preferred":false,"id":246184,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cook, T. A.","contributorId":60169,"corporation":false,"usgs":true,"family":"Cook","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":246187,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crovelli, R. A.","contributorId":40969,"corporation":false,"usgs":true,"family":"Crovelli","given":"R. A.","affiliations":[],"preferred":false,"id":246185,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klett, T. R. 0000-0001-9779-1168","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":83067,"corporation":false,"usgs":true,"family":"Klett","given":"T. R.","affiliations":[],"preferred":false,"id":246190,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lewan, M. D.","contributorId":46540,"corporation":false,"usgs":true,"family":"Lewan","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":246186,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pollastro, R. M.","contributorId":6809,"corporation":false,"usgs":true,"family":"Pollastro","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246182,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schenk, Christopher J. 0000-0002-0248-7305","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":72344,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":246189,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":246188,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":53091,"text":"ofr03374 - 2003 - Preliminary geochemical, microbiological, and epidemiological investigations into possible linkages between lignite aquifers, pathogenic microbes, and kidney disease in northwestern Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:11:56","indexId":"ofr03374","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-374","title":"Preliminary geochemical, microbiological, and epidemiological investigations into possible linkages between lignite aquifers, pathogenic microbes, and kidney disease in northwestern Louisiana","docAbstract":"In May 2002, 15 wells and four surface water sites were sampled, and in September 2002, those same wells and sites plus four additional surface sites were sampled in five parishes of northwestern Louisiana. A geographic information system (GIS) was used to select residential water wells for sampling. Well water samples were analyzed for pH, conductivity, organic compounds, and nutrient and anion concentrations. All samples were further tested for presence of fungi (maintained for up to 28 days and colonies counted and identified microscopically), and metal and trace element concentration by inductively-coupled plasma mass spectrometry and atomic emission spectrometry. Surface water samples were tested for dissolved oxygen and evidence of leptospiral bacterial presence. A polymerase chain reaction protocol was optimized for detection of pathogenic leptospires, and the sensitivity of the assay was determined. The Spearman correlation method was used to assess the association between the endpoints for these field/laboratory analyses and the incidence of cancer of the renal pelvis obtained from the Louisiana Tumor Registry. Significant associations were revealed between the cancer rate and the overall number of organic compounds, the fungi Zygomycetes, the nutrients PO4 and NH3, and thirteen chemical elements (As, B, Br, Cl, Cr, F, Li, Na, P, Rb, Se, Sr, W) from the well water as compared to the controls. Among the species of fungi from the total of 136 isolates were 12 Penicillium spp., at least two Aspergillus spp., a number of other genera (Alternaria sp., Eupenicillium lapidosum, Cladosporium sp., Epicoccum sp., Trichoderma sp., Paecilomyces sp., Chrysosporium sp., Chloridium sp.), and Zygomycetes, and Coelmycetes -- some of which are known mycotoxin producers. The two control wells yielded a mean of 6.5 (SD = 3.5355) individual isolates, while the mean number of isolates from all other sites was 7.6 (SD = 4.4866). Presence of human pathogenic leptospires was detected in 4/8 (50 percent) of the surface water sites sampled. These initial results suggest that additional investigation into these relationships is warranted.","language":"ENGLISH","doi":"10.3133/ofr03374","usgsCitation":"Bunnell, J.E., Bushon, R.N., Stoeckel, D.M., Gifford, A.M., Beck, M., Lerch, H.E., Shi, R., McGee, B., Hanson, B.C., Kolak, J., and Warwick, P.D., 2003, Preliminary geochemical, microbiological, and epidemiological investigations into possible linkages between lignite aquifers, pathogenic microbes, and kidney disease in northwestern Louisiana (Version 1.0, Online only): U.S. Geological Survey Open-File Report 2003-374, 59 p., https://doi.org/10.3133/ofr03374.","productDescription":"59 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":180886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5288,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-374/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0, Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c341","contributors":{"authors":[{"text":"Bunnell, Joseph E. jbunnell@usgs.gov","contributorId":556,"corporation":false,"usgs":true,"family":"Bunnell","given":"Joseph","email":"jbunnell@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":246609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bushon, Rebecca N. rnbushon@usgs.gov","contributorId":2304,"corporation":false,"usgs":true,"family":"Bushon","given":"Rebecca","email":"rnbushon@usgs.gov","middleInitial":"N.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":246612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoeckel, Donald M.","contributorId":78384,"corporation":false,"usgs":true,"family":"Stoeckel","given":"Donald","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246618,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gifford, Amie M.","contributorId":106083,"corporation":false,"usgs":true,"family":"Gifford","given":"Amie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246619,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Beck, Marisa","contributorId":61899,"corporation":false,"usgs":true,"family":"Beck","given":"Marisa","email":"","affiliations":[],"preferred":false,"id":246617,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lerch, Harry E. tlerch@usgs.gov","contributorId":600,"corporation":false,"usgs":true,"family":"Lerch","given":"Harry","email":"tlerch@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":246610,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Shi, Runhua","contributorId":43032,"corporation":false,"usgs":true,"family":"Shi","given":"Runhua","email":"","affiliations":[],"preferred":false,"id":246615,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"McGee, Benton","contributorId":16917,"corporation":false,"usgs":true,"family":"McGee","given":"Benton","affiliations":[],"preferred":false,"id":246613,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hanson, Bradford C.","contributorId":55076,"corporation":false,"usgs":true,"family":"Hanson","given":"Bradford","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":246616,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Kolak, Jonathan","contributorId":29889,"corporation":false,"usgs":true,"family":"Kolak","given":"Jonathan","affiliations":[],"preferred":false,"id":246614,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Warwick, Peter D. 0000-0002-3152-7783 pwarwick@usgs.gov","orcid":"https://orcid.org/0000-0002-3152-7783","contributorId":762,"corporation":false,"usgs":true,"family":"Warwick","given":"Peter","email":"pwarwick@usgs.gov","middleInitial":"D.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":246611,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":53093,"text":"ofr03383 - 2003 - Bathymetric and geophysical surveys of Englebright Lake, Yuba-Nevada Counties, California","interactions":[],"lastModifiedDate":"2023-03-02T22:11:53.868565","indexId":"ofr03383","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-383","title":"Bathymetric and geophysical surveys of Englebright Lake, Yuba-Nevada Counties, California","docAbstract":"Harry L. Englebright Lake is a 9-mile-long (14-kilometer) reservoir located in the Sierra Nevada foothills of northern California on the Yuba River gorge known as The Narrows. The reservoir is impounded by Englebright Dam (Photo 1), a concrete arch structure spanning 348 meters (1,142 feet) across and 79 meters (260 feet) high. The dam was constructed in 1941 for the primary purpose of trapping sediment derived from anticipated hydraulic mining operations in the Yuba River watershed. Hydraulic mining in the Sierra Nevada was halted in 1884 but resumed on a limited basis until the 1930's under the regulation of the California Debris Commission. Although no hydraulic mining in the upper Yuba River watershed resumed after the construction of the dam, the historical mine sites continued to contribute sediment to the river. Today, Englebright Lake is used primarily for recreation and hydropower. In 2001 and 2002, the U.S. Geological Survey (USGS) conducted bathymetric, geophysical, and geological studies of the reservoir under the auspices of the Upper Yuba River Studies Program (UYRSP), a multi-disciplinary investigation into the feasibility of introducing anadromous fish species to the Yuba River system upstream of Englebright Dam. A primary purpose of these studies was to assess the quantity and nature of the sediment that has accumulated behind the dam over the past 60 years. This report presents the results of those surveys, including a new bathymetric map of the reservoir and estimates of the total accumulated sediment volume.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03383","usgsCitation":"Childs, J.R., Snyder, N., and Hampton, M.A., 2003, Bathymetric and geophysical surveys of Englebright Lake, Yuba-Nevada Counties, California: U.S. Geological Survey Open-File Report 2003-383, 20 p., https://doi.org/10.3133/ofr03383.","productDescription":"20 p.","numberOfPages":"20","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":180888,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03383.jpg"},{"id":285843,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0383/intro.html"},{"id":5289,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0383/","linkFileType":{"id":5,"text":"html"}},{"id":413632,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_59089.htm","linkFileType":{"id":5,"text":"html"}},{"id":285842,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0383/pdf/of03-383.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Nevada County, Yuba County","otherGeospatial":"Englebright Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.2778,\n              39.2375\n            ],\n            [\n              -121.2778,\n              39.3278\n            ],\n            [\n              -121.1958,\n              39.3278\n            ],\n            [\n              -121.1958,\n              39.2375\n            ],\n            [\n              -121.2778,\n              39.2375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a9a","contributors":{"authors":[{"text":"Childs, Jonathan R. jchilds@usgs.gov","contributorId":3155,"corporation":false,"usgs":true,"family":"Childs","given":"Jonathan","email":"jchilds@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":246622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, Noah P.","contributorId":43848,"corporation":false,"usgs":true,"family":"Snyder","given":"Noah P.","affiliations":[],"preferred":false,"id":246624,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampton, Margaret A.","contributorId":13688,"corporation":false,"usgs":true,"family":"Hampton","given":"Margaret","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":246623,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53108,"text":"ofr03250 - 2003 - Bed-sediment grain-size and morphologic data from Suisun, Grizzly, and Honker Bays, CA, 1998-2002","interactions":[],"lastModifiedDate":"2016-07-27T10:55:54","indexId":"ofr03250","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-250","title":"Bed-sediment grain-size and morphologic data from Suisun, Grizzly, and Honker Bays, CA, 1998-2002","docAbstract":"<p>The USGS Place Based Studies Program for San Francisco Bay investigates this sensitive estuarine system to aid in resource management. As part of the inter-disciplinary research program, the USGS collected side-scan sonar data and bed-sediment samples from north San Francisco Bay to characterize bed-sediment texture and investigate temporal trends in sedimentation. The study area is located in central California and consists of Suisun Bay, and Grizzly and Honker Bays, sub-embayments of Suisun Bay. During the study (1998-2002), the USGS collected three side-scan sonar data sets and approximately 300 sediment samples. The side-scan data revealed predominantly fine-grained material on the bayfloor. We also mapped five different bottom types from the data set, categorized as featureless, furrows, sand waves, machine-made, and miscellaneous. We performed detailed grain-size and statistical analyses on the sediment samples. Overall, we found that grain size ranged from clay to fine sand, with the coarsest material in the channels and finer material located in the shallow bays. Grain-size analyses revealed high spatial variability in size distributions in the channel areas. In contrast, the shallow regions exhibited low spatial variability and consistent sediment size over time.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03250","usgsCitation":"Hampton, M.A., Snyder, N., Chin, J., Allison, D.W., and Rubin, D.M., 2003, Bed-sediment grain-size and morphologic data from Suisun, Grizzly, and Honker Bays, CA, 1998-2002: U.S. Geological Survey Open-File Report 2003-250, Report: 25 p.; Plate: 22.58 x 14.82 inches, https://doi.org/10.3133/ofr03250.","productDescription":"Report: 25 p.; Plate: 22.58 x 14.82 inches","numberOfPages":"25","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true}],"links":[{"id":173864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03250.jpg"},{"id":285697,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0250/pdf/of03-250.pdf"},{"id":4669,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0250/","linkFileType":{"id":5,"text":"html"}},{"id":285698,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0250/pdf/plate1.pdf"}],"country":"United States","state":"California","otherGeospatial":"Grizzly Bay, Honker Bay, San Francisco Bay, Suisun Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.153356,38.010233 ], [ -122.153356,38.167784 ], [ -121.879103,38.167784 ], [ -121.879103,38.010233 ], [ -122.153356,38.010233 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63dc05","contributors":{"authors":[{"text":"Hampton, Margaret A.","contributorId":13688,"corporation":false,"usgs":true,"family":"Hampton","given":"Margaret","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":246660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, Noah P.","contributorId":43848,"corporation":false,"usgs":true,"family":"Snyder","given":"Noah P.","affiliations":[],"preferred":false,"id":246662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chin, John L.","contributorId":98291,"corporation":false,"usgs":true,"family":"Chin","given":"John L.","affiliations":[],"preferred":false,"id":246663,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Allison, Dan W.","contributorId":26969,"corporation":false,"usgs":true,"family":"Allison","given":"Dan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":246661,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rubin, David M. 0000-0003-1169-1452 drubin@usgs.gov","orcid":"https://orcid.org/0000-0003-1169-1452","contributorId":3159,"corporation":false,"usgs":true,"family":"Rubin","given":"David","email":"drubin@usgs.gov","middleInitial":"M.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":246659,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":52902,"text":"fs07003 - 2003 - Heavy Oil and Natural Bitumen : strategic petroleum resources","interactions":[],"lastModifiedDate":"2012-02-02T00:11:40","indexId":"fs07003","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"070-03","title":"Heavy Oil and Natural Bitumen : strategic petroleum resources","language":"ENGLISH","doi":"10.3133/fs07003","usgsCitation":"Meyer, R.F., and Attanasi, E., 2003, Heavy Oil and Natural Bitumen : strategic petroleum resources (Online Version 1.0): U.S. Geological Survey Fact Sheet 070-03, 2 p., https://doi.org/10.3133/fs07003.","productDescription":"2 p.","costCenters":[],"links":[{"id":122704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_070_03.jpg"},{"id":4965,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/fs070-03/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ae4b07f02db63ce68","contributors":{"authors":[{"text":"Meyer, Richard F.","contributorId":67963,"corporation":false,"usgs":true,"family":"Meyer","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":246181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Attanasi, Emil 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":1809,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246180,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53088,"text":"ofr03363 - 2003 - Publications of the Western Earth Surface Processes Team 2002","interactions":[],"lastModifiedDate":"2023-06-22T16:58:33.054297","indexId":"ofr03363","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-363","title":"Publications of the Western Earth Surface Processes Team 2002","docAbstract":"The Western Earth Surface Processes Team (WESPT) of the U.S. Geological Survey (USGS) conducts geologic mapping and related topical earth science studies in the western United States. This work is focused on areas where modern geologic maps and associated earth-science data are needed to address key societal and environmental issues such as ground-water quality, landslides and other potential geologic hazards, and land-use decisions. Areas of primary emphasis in 2001 included southern California, the San Francisco Bay region, the Pacific Northwest, and the Las Vegas urban corridor. The team has its headquarters in Menlo Park, California, and maintains smaller field offices at several other locations in the western United States. The results of research conducted by the WESPT are released to the public as a variety of databases, maps, text reports, and abstracts, both through the internal publication system of the USGS and in diverse external publications such as scientific journals and books. This report lists publications of the WESPT released in 2002 as well as additional 1998 and 2001 publications that were not included in the previous list (USGS Open-File Report 00-215, USGS Open-File Report 01-198, and USGS Open-File Report 02-269). Most of the publications listed were authored or coauthored by WESPT staff. The list also includes some publications authored by non-USGS cooperators with the WESPT, as well as some authored by USGS staff outside the WESPT in cooperation with WESPT projects. Several of the publications listed are available on the World Wide Web; for these, URL addresses are provided. Many of these web publications are USGS open-file reports that contain large digital databases of geologic map and related information. Information on ordering USGS publications can be found on the World Wide Web or by calling 1-888-ASK-USGS. The U.S. Geological Survey’s web server for geologic information in the western United States is located at http://geology.wr.usgs.gov. More information is available about the WESPT is available on-line at the team website.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03363","usgsCitation":"Powell, C., and Graymer, R., 2003, Publications of the Western Earth Surface Processes Team 2002: U.S. Geological Survey Open-File Report 2003-363, 22 p., https://doi.org/10.3133/ofr03363.","productDescription":"22 p.","numberOfPages":"23","temporalStart":"2002-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":180791,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03363.jpg"},{"id":5285,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0363/","linkFileType":{"id":5,"text":"html"}},{"id":285787,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0363/pdf/of03-363.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655e50","contributors":{"authors":[{"text":"Powell, Charles II","contributorId":96362,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","affiliations":[],"preferred":false,"id":246604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graymer, R. W.","contributorId":21174,"corporation":false,"usgs":true,"family":"Graymer","given":"R. W.","affiliations":[],"preferred":false,"id":246603,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50854,"text":"wri034027 - 2003 - External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 1997-99","interactions":[],"lastModifiedDate":"2012-02-02T00:11:30","indexId":"wri034027","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4027","title":"External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 1997-99","docAbstract":"Five external quality-assurance programs were operated by the U.S. Geological Survey for the National Atmospheric Deposition Program/ National Trends Network (NADP/NTN) during 1997 through 1999: the intersite-comparison program, the blind-audit program, the field- audit program, the interlaboratory-comparison program, and the collocated-sampler program. The intersite-comparison program assesses the accuracy of pH and specific-conductance determinations made by NADP/NTN site operators. In two 1997 intersite-comparison studies, 83.7 and 85.8 percent of the pH determinations met the NADP/NTN accuracy goals, whereas 97.3 and 92.4 percent of the specific-conductance determinations met the NADP/NTN accuracy goals. The percentage of pH and specific-conductance determinations that met the accuracy goals in 1998 were, for the most part, higher than in 1997. In two 1998 studies, 90.9 and 90.3 percent of the pH determinations met the accuracy goals compared to 94.7 and 96.0 percent of the specific- conductance measurements meeting the accuracy goals. In one 1999 intersite-comparison study, 89.5 percent and 99.4 percent of pH and specific- conductance determinations, respectively, met the NADP/NTN accuracy goals. The blind-audit program evaluates the effects of routine sample handling, processing, and shipping on the analytical bias and precision of weekly precipitation samples. A portion of the blind-audit sample subject to the normal onsite handling and processing of a weekly precipitation sample is referred to as the bucket portion, whereas the portion receiving only minimal handling is referred to as the bottle portion. Positive bias in regard to blind-audit results indicates that the bucket portion has a higher concentration than the bottle portion. The paired t-test for the 1997 through 1999 blind- audit data indicates that routine sample handling, processing, and shipping introduced a positive bias (a=0.05) for calcium and chloride and a negative bias (cz=0.05) for hydrogen ion. During 1997 through 1999, the median paired differences between the bucket and bottle portions ranged from 0.00 milligram per liter for nitrate and ammonium to +0.010 milligram per liter for both chloride and sulfate. The median paired difference between the bucket and bottle portions for hydrogen ion was -1.086 microequivalents per liter, whereas for specific conductance, the median paired difference between the bucket and bottle portions was -0.200 microsiemen per centimeter during 1997 through 1999. Surface-chemistry effects due to variable amounts of precipitation contacting prewashed sample-collection and shipping-container surfaces were studied in the blind-audit program by using three different sample volumes. The sample- collection and shipping containers used for the blind-audit study were obtained from the site operator's supply and could have been used for precipitation samples. Results of a Kruskal-Wallis analysis of variance test of the relation between paired blind-audit sample differences in units of concentration and sample volume were statistically significant for magnesium, chloride, sulfate, and hydrogen ion during 1997 through 1999. Before 1994, at least 5 of the 10 analytes displayed a statistically significant difference between paired blind-audit differences in units of concentration and sample volume, supporting the premise that chemical reactions between the 13-liter bucket shipping container (primarily the butadiene o-ring lid of the shipping container) and the sample, which resulted in an increasing loss of hydrogen ion with increasing volume, have been eliminated by the new l-liter bottle sample- shipping protocol. The field-audit program measures the effects of field exposure, handling, and processing on the chemistry of NADP/NTN precipitation samples. In the field-audit program, the site operator is instructed to process and submit a quality- control sample following a standard 7-day, Tuesday-to-Tuesday sampling period with no ","language":"ENGLISH","doi":"10.3133/wri034027","usgsCitation":"Gordon, J.D., Latysh, N.E., and Lindholm, S.J., 2003, External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 1997-99: U.S. Geological Survey Water-Resources Investigations Report 2003-4027, vi, 75 p. : ill. (some col.), col. map ; 28 cm., https://doi.org/10.3133/wri034027.","productDescription":"vi, 75 p. : ill. (some col.), col. map ; 28 cm.","costCenters":[],"links":[{"id":122274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2003/4027/report-thumb.jpg"},{"id":86375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2003/4027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489edf","contributors":{"authors":[{"text":"Gordon, John D. 0000-0001-8396-8524 jgordon@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-8524","contributorId":347,"corporation":false,"usgs":true,"family":"Gordon","given":"John","email":"jgordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":242457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Latysh, Natalie E.","contributorId":39860,"corporation":false,"usgs":true,"family":"Latysh","given":"Natalie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lindholm, Sandy J.","contributorId":85260,"corporation":false,"usgs":true,"family":"Lindholm","given":"Sandy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":242459,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53064,"text":"ofr032 - 2003 - Texture, Carbonate Content, and Preliminary Maps of Surficial Sediments of the Flower Garden Banks Area, Northwestern Gulf of Mexico Outer Shelf","interactions":[],"lastModifiedDate":"2017-11-10T18:28:58","indexId":"ofr032","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-2","title":"Texture, Carbonate Content, and Preliminary Maps of Surficial Sediments of the Flower Garden Banks Area, Northwestern Gulf of Mexico Outer Shelf","docAbstract":"<p>The purpose of this report is to release texture and carbonate content analyses of 107 seafloor sediments collected within and near the East and West Flower Garden Banks areas of the Sanctuary and to show relationships between these data and existing bathymetric data. The sediment data, in conjunction with previously collected geological, geophysical and biological data were used to construct a reconnaissance-scale map of the distribution of seafloor sediment types. This map will be useful for resource managers and can be used, with additional data, as a basis for future habitat mapping.</p>","language":"ENGLISH","doi":"10.3133/ofr032","isbn":"0607937211","usgsCitation":"Scanlon, K.M., Ackerman, S.D., and Rozycki, J.E., 2003, Texture, Carbonate Content, and Preliminary Maps of Surficial Sediments of the Flower Garden Banks Area, Northwestern Gulf of Mexico Outer Shelf: U.S. Geological Survey Open-File Report 2003-2, 1 CD-ROM ; 4 3/4 in., https://doi.org/10.3133/ofr032.","productDescription":"1 CD-ROM ; 4 3/4 in.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":177465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":297450,"rank":101,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-002/"},{"id":5204,"rank":100,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/of03-002/of03_002metafaq.htm","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683712","contributors":{"authors":[{"text":"Scanlon, Kathryn M.","contributorId":6816,"corporation":false,"usgs":true,"family":"Scanlon","given":"Kathryn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ackerman, Seth D. 0000-0003-0945-2794 sackerman@usgs.gov","orcid":"https://orcid.org/0000-0003-0945-2794","contributorId":178676,"corporation":false,"usgs":true,"family":"Ackerman","given":"Seth","email":"sackerman@usgs.gov","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":246469,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rozycki, Jill E.","contributorId":78397,"corporation":false,"usgs":true,"family":"Rozycki","given":"Jill","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":246470,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51257,"text":"wri034175 - 2003 - Ground-Water Levels and Water-Quality Data for Wells in the Crumpton Creek Area near Arnold Air Force Base, Tennessee, November 2001 to January 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:31","indexId":"wri034175","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4175","title":"Ground-Water Levels and Water-Quality Data for Wells in the Crumpton Creek Area near Arnold Air Force Base, Tennessee, November 2001 to January 2002","docAbstract":"From November 2001 to January 2002, a study of the ground-water resources in the Crumpton Creek area of Middle Tennessee was conducted to determine whether volatile organic compounds (VOCs) from Arnold Air Force Base (AAFB) have affected local private water supplies and to advance understanding of the ground-water-flow system in this area. VOC samples were collected from private wells that were not included in previous sampling efforts conducted in the Crumpton Creek area near AAFB. Ground-water-flow directions were investigated by measuring water levels in wells and constructing a potentiometric-surface map of the Manchester aquifer in the study area. Data were collected from a total of 68 private wells, 82 monitoring wells, and 1 cave during the period of study. Ground-water levels were determined for 42 of the private wells and for all 82 monitoring wells. Of the 82 monitoring wells, 81 withdraw water from the Manchester aquifer and 1 well withdraws water from the overlying shallow aquifer. The Manchester aquifer wells range in depth from 20 to 150 feet. Water-level altitudes for the Manchester aquifer ranged from 956 to 1,064 feet above the National Geodetic Vertical Datum of 1929. Water levels ranged from approximately 6 feet above land surface to 94 feet below land surface. Water-quality samples were collected from all 68 private wells, 8 of the monitoring wells, and the 1 cave. \r\n\r\nOf the 55 VOCs analyzed, 42 were not detected. Thirteen VOCs were detected; however, only tetrachloroethylene (PCE), methylene chloride, and toluene were detected at concentrations equal to or above reporting levels for the analytical method used. PCE was detected in water samples from 15 private wells and was the only VOC that exceeded drinking water maximum contaminant levels for public water systems. PCE concentrations in samples from five of the wells were below the reporting level and ranged from estimated concentrations of 0.46 to 0.80 microgram per liter (?g/L). Samples from 10 wells contained concentrations equal to or greater than the analytical reporting level of 1 ?g/L for PCE. Samples from one of these wells contained PCE concentrations (12 ?g/L and 11 ?g/L) exceeding the drinking water maximum contaminant level of 5 ?g/L for PCE. The spatial distribution of PCE detections and the relative concentrations of PCE and trichloroethylene suggest that the PCE detections are associated with a small and localized ground-water contamination plume unrelated to AAFB ground-water contamination.","language":"ENGLISH","doi":"10.3133/wri034175","usgsCitation":"Williams, S.D., 2003, Ground-Water Levels and Water-Quality Data for Wells in the Crumpton Creek Area near Arnold Air Force Base, Tennessee, November 2001 to January 2002: U.S. Geological Survey Water-Resources Investigations Report 2003-4175, 28 p., https://doi.org/10.3133/wri034175.","productDescription":"28 p.","costCenters":[],"links":[{"id":4631,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034175/","linkFileType":{"id":5,"text":"html"}},{"id":178487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d17c","contributors":{"authors":[{"text":"Williams, Shannon D. swilliam@usgs.gov","contributorId":4133,"corporation":false,"usgs":true,"family":"Williams","given":"Shannon","email":"swilliam@usgs.gov","middleInitial":"D.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":243235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69704,"text":"i2732B - 2003 - Shaded relief and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts","interactions":[],"lastModifiedDate":"2025-07-31T16:26:17.645713","indexId":"i2732B","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2732","subseriesTitle":"Geolgoic Investigations Series","chapter":"B","title":"Shaded relief and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2732B","usgsCitation":"Butman, B., Hayes, L., Danforth, W.W., and Valentine, P.C., 2003, Shaded relief and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts: U.S. Geological Survey IMAP 2732, 1 Plate: 40.00 × 35.00 inches, https://doi.org/10.3133/i2732B.","productDescription":"1 Plate: 40.00 × 35.00 inches","costCenters":[],"links":[{"id":493244,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/i2732C","text":"IMAP 2732-C","linkHelpText":"Backscatter intensity, shaded relief, and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts"},{"id":191161,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":493245,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/i2732A","text":"IMAP 2732-A","linkHelpText":"Sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts"},{"id":110466,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62423.htm","linkFileType":{"id":5,"text":"html"},"description":"62423"},{"id":6374,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-2732b/","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","country":"United States","state":"Massachusetts","otherGeospatial":"Massachusetts Bay, Quadrangle 2","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.8833,\n              42.3217\n            ],\n            [\n              -70.6,\n              42.3217\n            ],\n            [\n              -70.6,\n              42.4417\n            ],\n            [\n              -70.8833,\n              42.4417\n            ],\n            [\n              -70.8833,\n              42.3217\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4a2f","contributors":{"authors":[{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, Laura 0000-0002-4488-1343 lhayes@usgs.gov","orcid":"https://orcid.org/0000-0002-4488-1343","contributorId":2791,"corporation":false,"usgs":true,"family":"Hayes","given":"Laura","email":"lhayes@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":280942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Danforth, William W. 0000-0002-6382-9487 bdanforth@usgs.gov","orcid":"https://orcid.org/0000-0002-6382-9487","contributorId":3292,"corporation":false,"usgs":true,"family":"Danforth","given":"William","email":"bdanforth@usgs.gov","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280943,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280941,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":69705,"text":"i2732C - 2003 - Backscatter intensity, shaded relief, and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts","interactions":[],"lastModifiedDate":"2025-07-31T16:28:47.861211","indexId":"i2732C","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2732","subseriesTitle":"Geolgoic Investigations Series","chapter":"C","title":"Backscatter intensity, shaded relief, and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2732C","usgsCitation":"Butman, B., Hayes, L., Danforth, W.W., and Valentine, P.C., 2003, Backscatter intensity, shaded relief, and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts: U.S. Geological Survey IMAP 2732, 1 Plate: 40.00 × 35.00 inches, https://doi.org/10.3133/i2732C.","productDescription":"1 Plate: 40.00 × 35.00 inches","costCenters":[],"links":[{"id":493247,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/i2732B","text":"IMAP 2732-B","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Shaded relief and sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts"},{"id":493246,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/i2732A","text":"IMAP 2732-A","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Sea floor topography of Quadrangle 2 in western Massachusetts Bay offshore of Boston, Massachusetts"},{"id":110467,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62424.htm","linkFileType":{"id":5,"text":"html"},"description":"62424"},{"id":6377,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-2732c/","linkFileType":{"id":5,"text":"html"}},{"id":191280,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","country":"United States","state":"Massachusetts","otherGeospatial":"Massachusetts Bay, Quadrangle 2","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -70.8833,\n              42.3217\n            ],\n            [\n              -70.6,\n              42.3217\n            ],\n            [\n              -70.6,\n              42.4417\n            ],\n            [\n             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Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":280946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Danforth, William W. 0000-0002-6382-9487 bdanforth@usgs.gov","orcid":"https://orcid.org/0000-0002-6382-9487","contributorId":3292,"corporation":false,"usgs":true,"family":"Danforth","given":"William","email":"bdanforth@usgs.gov","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280947,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valentine, Page C. 0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":280945,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70222382,"text":"70222382 - 2003 - Correlates to survival of juvenile sea otters in Prince William Sound, Alaska, 1992-1993","interactions":[],"lastModifiedDate":"2021-07-26T17:24:00.99648","indexId":"70222382","displayToPublicDate":"2003-09-30T12:18:13","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1176,"text":"Canadian Journal of Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Correlates to survival of juvenile sea otters in Prince William Sound, Alaska, 1992-1993","docAbstract":"<p><span>We estimated&nbsp;</span>survival<span>&nbsp;of&nbsp;</span>sea<span>&nbsp;</span>otters<span>&nbsp;(Enhydra lutris) for 1 year post weaning during&nbsp;</span>1992<span>-</span>1993<span>&nbsp;</span>in<span>&nbsp;</span>Prince<span>&nbsp;</span>William<span>&nbsp;</span>Sound<span>&nbsp;(PWS), location of the 1989 Exxon Valdez oil spill. We sampled 38 pups&nbsp;</span>in<span>&nbsp;eastern PWS (EPWS), an unoiled area occupied by&nbsp;</span>sea<span>&nbsp;</span>otters<span>&nbsp;for &lt;15 years, and 33 pups from oiled western PWS (WPWS), occupied for &gt;25 years. We compared&nbsp;</span>survival<span>&nbsp;between areas, sexes, and condition groups. We also examined the relation of blood parameters to&nbsp;</span>survival<span>.&nbsp;</span>Survival<span>&nbsp;was estimated at 0.74&nbsp;</span>in<span>&nbsp;EPWS and 0.52&nbsp;</span>in<span>&nbsp;WPWS. Female&nbsp;</span>survival<span>&nbsp;was 0.86&nbsp;</span>in<span>&nbsp;EPWS and 0.64&nbsp;</span>in<span>&nbsp;WPWS, whereas male&nbsp;</span>survival<span>&nbsp;was lower, 0.61&nbsp;</span>in<span>&nbsp;EPWS and 0.44&nbsp;</span>in<span>&nbsp;WPWS.&nbsp;</span>Sea<span>&nbsp;</span>otters<span>&nbsp;from EPWS were&nbsp;</span>in<span>&nbsp;better condition (mass/length) than WPWS&nbsp;</span>sea<span>&nbsp;</span>otters<span>. Pups&nbsp;</span>in<span>&nbsp;better condition had higher&nbsp;</span>survival<span>&nbsp;</span>in<span>&nbsp;EPWS but not&nbsp;</span>in<span>&nbsp;WPWS. Foraging success was greater&nbsp;</span>in<span>&nbsp;EPWS than&nbsp;</span>in<span>&nbsp;WPWS, consistent with either an effect of length of occupation or the effects of oil on the prey base or a combination of these effects. Area differences&nbsp;</span>in<span>&nbsp;blood parameters suggested liver damage&nbsp;</span>in<span>&nbsp;WPWS&nbsp;</span>sea<span>&nbsp;</span>otters<span>, perhaps resulting from continued exposure to oil. Thus, both length of occupation and oiling history likely influenced&nbsp;</span>juvenile<span>&nbsp;</span>survival<span>&nbsp;</span>in<span>&nbsp;PWS.</span></p>","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/z03-121","usgsCitation":"Ballachey, B.E., Bodkin, J.L., Howlin, S., Doroff, A., and Rebar, A., 2003, Correlates to survival of juvenile sea otters in Prince William Sound, Alaska, 1992-1993: Canadian Journal of Zoology, v. 81, no. 9, p. 1494-1510, https://doi.org/10.1139/z03-121.","productDescription":"17 p.","startPage":"1494","endPage":"1510","costCenters":[],"links":[{"id":387431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Alaska","otherGeospatial":"Prince William Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -148.86474609375,\n              59.701013531997326\n            ],\n            [\n              -145.43701171875,\n              59.701013531997326\n            ],\n            [\n              -145.43701171875,\n              61.13262899079795\n            ],\n            [\n              -148.86474609375,\n              61.13262899079795\n            ],\n            [\n              -148.86474609375,\n              59.701013531997326\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"81","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ballachey, Brenda E. 0000-0003-1855-9171 bballachey@usgs.gov","orcid":"https://orcid.org/0000-0003-1855-9171","contributorId":2966,"corporation":false,"usgs":true,"family":"Ballachey","given":"Brenda","email":"bballachey@usgs.gov","middleInitial":"E.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":819892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodkin, James L. 0000-0003-1641-4438 jbodkin@usgs.gov","orcid":"https://orcid.org/0000-0003-1641-4438","contributorId":748,"corporation":false,"usgs":true,"family":"Bodkin","given":"James","email":"jbodkin@usgs.gov","middleInitial":"L.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":819893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howlin, S.","contributorId":94624,"corporation":false,"usgs":true,"family":"Howlin","given":"S.","affiliations":[],"preferred":false,"id":819894,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Doroff, A. M.","contributorId":92995,"corporation":false,"usgs":false,"family":"Doroff","given":"A. M.","affiliations":[],"preferred":false,"id":819895,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rebar, A.H.","contributorId":40150,"corporation":false,"usgs":true,"family":"Rebar","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":819896,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70178303,"text":"70178303 - 2003 - Evidence of change in a low-elevation forest bird community of Hawai'i since 1979","interactions":[],"lastModifiedDate":"2018-01-04T13:04:52","indexId":"70178303","displayToPublicDate":"2003-09-29T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1048,"text":"Bird Conservation International","active":true,"publicationSubtype":{"id":10}},"title":"Evidence of change in a low-elevation forest bird community of Hawai'i since 1979","docAbstract":"<p><span>We evaluated the abundance and distribution of low-elevation forest birds on windward Hawai'i Island during August 1993-February 1994, and present evidence of changes in the species composition of the forest bird community since 1979. Endemic Hawaiian birds occurred in native-dominated forests as low as 120 m elevation. Non-native species were detected at all survey locations. We observed non-native Saffron Finch </span><i><span class=\"italic\">Sicalis flaveola</span></i><span>, previously unrecorded in Puna. Variable circular plot surveys of Kahauale'a Natural Area Reserve indicated the disappearance of two native species ('I'iwi </span><i><span class=\"italic\">Vestiaria coccinea</span></i><span> and 'O'u </span><i><span class=\"italic\">Psittitostra psittacea</span></i><span>), and two non-native additions (Red-billed Leiothrix </span><span class=\"italic\"><i>Leiothrix lutea</i>&nbsp;</span><span>and Kalij Pheasant </span><i><span class=\"italic\">Lophura leucomelana</span></i><span>) to the study area since the Hawai'i Forest Bird Survey conducted in 1979. We present evidence that native 'Elepaio </span><i><span class=\"italic\">Chasiempsis sandwichensis</span></i><span> has experienced a decrease in population density and an elevational range contraction since 1979. Surveys indicate Puna's forest bird community has had increasing aliens and declining native species since 1979. The persistence of some native bird species within the range of avian disease vectors such as </span><i><span class=\"italic\">Culex quinquefasciatus</span></i><span> in forests below 1,000 m elevation presents an important enigma that requires additional study.</span></p>","language":"English","publisher":"BirdLife International","publisherLocation":"Cambridge, England","doi":"10.1017/S0959270903003149","usgsCitation":"Reynolds, M.H., Camp, R., Nielson, B.M., and Jacobi, J.D., 2003, Evidence of change in a low-elevation forest bird community of Hawai'i since 1979: Bird Conservation International, v. 13, no. 3, p. 175-187, https://doi.org/10.1017/S0959270903003149.","productDescription":"13 p.","startPage":"175","endPage":"187","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":478341,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1017/s0959270903003149","text":"Publisher Index Page"},{"id":330954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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