{"pageNumber":"2561","pageRowStart":"64000","pageSize":"25","recordCount":184617,"records":[{"id":70536,"text":"sir20055013 - 2005 - Ground-water flow directions and estimation of aquifer hydraulic properties in the lower Great Miami River Buried Valley aquifer system, Hamilton Area, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20055013","displayToPublicDate":"2005-05-11T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5013","title":"Ground-water flow directions and estimation of aquifer hydraulic properties in the lower Great Miami River Buried Valley aquifer system, Hamilton Area, Ohio","docAbstract":"The Great Miami River Buried Valley Aquifer System is one of the most productive sources of potable water in the Midwest, yielding as much as 3,000 gallons per minute to wells. Many water-supply wells tapping this aquifer system are purposely placed near rivers to take advantage of induced infiltration from the rivers. \r\n\r\nThe City of Hamilton's North Well Field consists of 10 wells near the Great Miami River, all completed in the lower Great Miami River Buried Valley Aquifer System. A well-drilling program and a multiple-well aquifer test were done to investigate ground-water flow directions and to estimate aquifer hydraulic properties in the lower part of the Great Miami River Buried Valley Aquifer System. Descriptions of lithology from 10 well borings indicate varying amounts and thickness of clay or till, and therefore, varying levels of potential aquifer confinement. Borings also indicate that the aquifer properties can change dramatically over relatively short distances. Grain-size analyses indicate an average bulk hydraulic conductivity value of aquifer materials of 240 feet per day; the geometric mean of hydraulic conductivity values of aquifer material was 89 feet per day. Median grain sizes of aquifer material and clay units were 1.3 millimeters and 0.1 millimeters, respectively. \r\n\r\nWater levels in the Hamilton North Well Field are affected by stream stage in the Great Miami River and barometric pressure. Bank storage in response to stream stage is evident. Results from a multiple-well aquifer test at the well field indicate, as do the lithologic descriptions, that the aquifer is semiconfined in some areas and unconfined in others. Transmissivity and storage coefficient of the semiconfined part of the aquifer were 50,000 feet squared per day and 5x10-4, respectively. The average hydraulic conductivity (450 feet per day) based on the aquifer test is reasonable for glacial outwash but is higher than calculated from grain-size analyses, implying a scale effect. Although the part of the lower Great Miami River Buried Valley Aquifer System where the Hamilton North Well Field is located is semiconfined, unconfined, or locally confined and not directly connected to the Great Miami River, the discontinuity of the clay/till layers beneath the river indicates that other, deeper parts of the aquifer system may be directly connected to the Great Miami River.","language":"ENGLISH","doi":"10.3133/sir20055013","usgsCitation":"Sheets, R., and Bossenbroek, K.E., 2005, Ground-water flow directions and estimation of aquifer hydraulic properties in the lower Great Miami River Buried Valley aquifer system, Hamilton Area, Ohio: U.S. Geological Survey Scientific Investigations Report 2005-5013, 36 p., https://doi.org/10.3133/sir20055013.","productDescription":"36 p.","costCenters":[],"links":[{"id":6904,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055013/","linkFileType":{"id":5,"text":"html"}},{"id":186152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c9ff","contributors":{"authors":[{"text":"Sheets, Rodney A. rasheets@usgs.gov","contributorId":1848,"corporation":false,"usgs":true,"family":"Sheets","given":"Rodney A.","email":"rasheets@usgs.gov","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bossenbroek, Karen E.","contributorId":29068,"corporation":false,"usgs":true,"family":"Bossenbroek","given":"Karen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70529,"text":"wdrNHVT041 - 2005 - Water resources data for New Hampshire and Vermont, water year 2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:17","indexId":"wdrNHVT041","displayToPublicDate":"2005-05-09T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NH-VT-04-1","title":"Water resources data for New Hampshire and Vermont, water year 2004","docAbstract":"Water-resources data for the 2004 water year for New Hampshire and Vermont consists of stage, discharge, and water quality of streams; contents of lakes and reservoirs; and ground-water levels. This report contains discharge records for 93 gaging stations, stage records for 6 lakes, monthend contents for 2 lakes and reservoirs, water levels for 38 observation wells. Also included are data for 37 crest-stage partial-record stations. Additional water data were collected at various sites, which are not part of the systematic data-collection program and are published as miscellaneous measurements for gaging stations in New Hampshire and Vermont. A few pertinent stations in bordering States are also included in this report. These data represent that portion of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in New Hampshire and Vermont.","language":"ENGLISH","doi":"10.3133/wdrNHVT041","usgsCitation":"Keirstead, C., Kiah, R.G., Ward, S.L., and Hilgendorf, G.S., 2005, Water resources data for New Hampshire and Vermont, water year 2004: U.S. Geological Survey Water Data Report NH-VT-04-1, 353 p., https://doi.org/10.3133/wdrNHVT041.","productDescription":"353 p.","temporalStart":"2003-10-01","temporalEnd":"2004-09-30","costCenters":[{"id":468,"text":"New Hampshire-Vermont Water Science Center","active":false,"usgs":true}],"links":[{"id":186076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6903,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-nh-04-1/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2986","contributors":{"authors":[{"text":"Keirstead, Chandlee","contributorId":10862,"corporation":false,"usgs":true,"family":"Keirstead","given":"Chandlee","email":"","affiliations":[],"preferred":false,"id":282593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kiah, Richard G. 0000-0001-6236-2507 rkiah@usgs.gov","orcid":"https://orcid.org/0000-0001-6236-2507","contributorId":2637,"corporation":false,"usgs":true,"family":"Kiah","given":"Richard","email":"rkiah@usgs.gov","middleInitial":"G.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282590,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, Sanborn L. sward@usgs.gov","contributorId":5147,"corporation":false,"usgs":true,"family":"Ward","given":"Sanborn","email":"sward@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":282592,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hilgendorf, Gregory S. gshilgen@usgs.gov","contributorId":5144,"corporation":false,"usgs":true,"family":"Hilgendorf","given":"Gregory","email":"gshilgen@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":282591,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70530,"text":"fs20053026 - 2005 - PAGER - Rapid Assessment and Notification of an Earthquake's Impact","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20053026","displayToPublicDate":"2005-05-09T00:00:00","publicationYear":"2005","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":"2005-3026","title":"PAGER - Rapid Assessment and Notification of an Earthquake's Impact","docAbstract":"PAGER (Prompt Assessment of Global Earthquakes for Response) is an automated alarm system being developed to rapidly and accurately assess the severity of damage caused by an earthquake and to provide emergency relief organizations, government agencies, and the media with an estimate of the societal impact from the potential catastrophe.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20053026","usgsCitation":"Earle, P.S., Wald, D.J., and Lastowka, L., 2005, PAGER - Rapid Assessment and Notification of an Earthquake's Impact (Superseded by FS 2007-3101): U.S. Geological Survey Fact Sheet 2005-3026, 2 p., https://doi.org/10.3133/fs20053026.","productDescription":"2 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":121169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3026.bmp"},{"id":90525,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","edition":"Superseded by FS 2007-3101","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a6c5","contributors":{"authors":[{"text":"Earle, Paul S. pearle@usgs.gov","contributorId":840,"corporation":false,"usgs":true,"family":"Earle","given":"Paul","email":"pearle@usgs.gov","middleInitial":"S.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":282595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wald, David J. 0000-0002-1454-4514 wald@usgs.gov","orcid":"https://orcid.org/0000-0002-1454-4514","contributorId":795,"corporation":false,"usgs":true,"family":"Wald","given":"David","email":"wald@usgs.gov","middleInitial":"J.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":282594,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lastowka, Lynda A. llastowka@usgs.gov","contributorId":5198,"corporation":false,"usgs":true,"family":"Lastowka","given":"Lynda A.","email":"llastowka@usgs.gov","affiliations":[],"preferred":true,"id":282596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70521,"text":"ofr20051165 - 2005 - Particle atlas of World Trade Center dust","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"ofr20051165","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1165","title":"Particle atlas of World Trade Center dust","docAbstract":"The United States Environmental Protection Agency (EPA) has begun a reassessment of the presence of World Trade Center (WTC) dust in residences, public buildings, and office spaces in New York City, New York. Background dust samples collected from residences, public buildings, and office spaces will be analyzed by multiple laboratories for the presence of WTC dust. Other laboratories are currently studying WTC dust for other purposes, such as health effects studies. To assist in inter-laboratory consistency for identification of WTC dust components, this particle atlas of phases in WTC dust has been compiled.","language":"ENGLISH","doi":"10.3133/ofr20051165","usgsCitation":"Lowers, H., and Meeker, G.P., 2005, Particle atlas of World Trade Center dust (Version 1.0, online only): U.S. Geological Survey Open-File Report 2005-1165, 6 p. with linked tables and images, https://doi.org/10.3133/ofr20051165.","productDescription":"6 p. with linked tables and images","onlineOnly":"Y","costCenters":[],"links":[{"id":185991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6898,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1165/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","edition":"Version 1.0, online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db688f46","contributors":{"authors":[{"text":"Lowers, Heather 0000-0001-5360-9264 hlowers@usgs.gov","orcid":"https://orcid.org/0000-0001-5360-9264","contributorId":710,"corporation":false,"usgs":true,"family":"Lowers","given":"Heather","email":"hlowers@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":282574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meeker, Gregory P.","contributorId":62974,"corporation":false,"usgs":true,"family":"Meeker","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70524,"text":"sir20045248 - 2005 - Evaluation of volatile organic compounds in two Mojave Desert basins-Mojave River and Antelope Valley-in San Bernardino, Los Angeles, and Kern Counties, California, June-October 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20045248","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5248","title":"Evaluation of volatile organic compounds in two Mojave Desert basins-Mojave River and Antelope Valley-in San Bernardino, Los Angeles, and Kern Counties, California, June-October 2002","docAbstract":"The California Aquifer Susceptibility Assessment of the Ground-Water Ambient Monitoring and Assessment Program was developed to assess water quality and susceptibility of ground-water resources to contamination from surficial sources. This study focuses on the Mojave River and the Antelope Valley ground-water basins in southern California. \r\n\r\nVolatile organic compound (VOC) data were evaluated in conjunction with tritium data to determine a potential correlation with aquifer type, depth to top of perforations, and land use to VOC distribution and occurrence in the Mojave River and the Antelope Valley Basins. Detection frequencies for VOCs were compiled and compared to assess the distribution in each area. Explanatory variables were evaluated by comparing detection frequencies for VOCs and tritium and the number of compounds detected. Thirty-three wells were sampled in the Mojave River Basin (9 in the floodplain aquifer, 15 in the regional aquifer, and 9 in the sewered subset of the regional aquifer). Thirty-two wells were sampled in the Antelope Valley Basin. Quality-control samples also were collected to identify, quantify, and document bias and variability in the data.\r\n\r\nResults show that VOCs generally were detected slightly more often in the Antelope Valley Basin samples than in the Mojave River Basin samples. VOCs were detected more frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Tritium was detected more frequently in the Mojave River Basin samples than in the Antelope Valley Basin samples, and it was detected more frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Most of the samples collected in both basins for this study contained old water (water recharged prior to 1952). In general, in these desert basins, tritium need not be present for VOCs to be present. When VOCs were detected, young water (water recharge after 1952) was slightly more likely to be contaminated than old water.\r\n\r\nTrihalomethanes (THMs) were detected less frequently in the Mojave River Basin samples than in the Antelope Valley Basin samples. The THMs that were detected in the Mojave River Basin were detected more frequently in the floodplain aquifer than in the regional aquifer and sewered subset. Solvents were detected more frequently in the Mojave River samples than in the Antelope Valley samples. In the Mojave River Basin samples, solvents were detected less frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Benzene, toluene, ethylbenzene and xylene (BTEX) were not detected in either study area. Methyl tert-butyl ether (MTBE) was detected in one sample from both the Mojave River and Antelope Valley Basins. \r\n\r\nThe most frequently detected compound (detected in more than 10 percent of the wells) in the Mojave River Basin was chloroform. The two most frequently detected compounds in the Antelope Valley Basin were chloroform and tetrachloroethylene (PCE). \r\n\r\nIn the Mojave River Basin, aquifer type and land use within 1,640 ft (500 m) of the well head were not statistically correlated with the number of VOCs detected, although VOCs were detected more frequently in the floodplain aquifer than in the regional aquifer and the sewered subset. Depth to the top of the perforations was an explanatory factor for the number of VOCs detected in the Mojave River Basin; the detection frequency was greater for shallow wells than for deep wells. \r\n\r\nIn the Antelope Valley Basin, neither aquifer type, depth to the top of the perforations, nor land use within 1,640 ft of the well head were explanatory factors for the number of VOCs detected. Although aquifer type and depth to top of the perforations did explain the presence of tritium in the Mojave River Basin, land use within 1,640 ft of the well head was not a statistically significant explanatory factor for the presence of tritium in this basin. Aquifer type, depth to the top of the perfora","language":"ENGLISH","doi":"10.3133/sir20045248","usgsCitation":"Densmore, J., Belitz, K., Wright, M.T., Dawson, B.J., and Johnson, T.D., 2005, Evaluation of volatile organic compounds in two Mojave Desert basins-Mojave River and Antelope Valley-in San Bernardino, Los Angeles, and Kern Counties, California, June-October 2002 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5248, 51 p., https://doi.org/10.3133/sir20045248.","productDescription":"51 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6901,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5248/","linkFileType":{"id":5,"text":"html"}},{"id":186074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a26","contributors":{"authors":[{"text":"Densmore, Jill N. 0000-0002-5345-6613","orcid":"https://orcid.org/0000-0002-5345-6613","contributorId":89179,"corporation":false,"usgs":true,"family":"Densmore","given":"Jill N.","affiliations":[],"preferred":false,"id":282588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":282584,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, Michael T. 0000-0003-0653-6466 mtwright@usgs.gov","orcid":"https://orcid.org/0000-0003-0653-6466","contributorId":1508,"corporation":false,"usgs":true,"family":"Wright","given":"Michael","email":"mtwright@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":false,"id":282587,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dawson, Barbara J. 0000-0002-0209-8158 bjdawson@usgs.gov","orcid":"https://orcid.org/0000-0002-0209-8158","contributorId":1102,"corporation":false,"usgs":true,"family":"Dawson","given":"Barbara","email":"bjdawson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":282585,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johnson, Tyler D. 0000-0002-7334-9188 tyjohns@usgs.gov","orcid":"https://orcid.org/0000-0002-7334-9188","contributorId":1440,"corporation":false,"usgs":true,"family":"Johnson","given":"Tyler","email":"tyjohns@usgs.gov","middleInitial":"D.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282586,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70523,"text":"ofr20051130 - 2005 - Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005","interactions":[],"lastModifiedDate":"2022-04-26T21:01:24.783283","indexId":"ofr20051130","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1130","title":"Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005","docAbstract":"<p class=\"textindent\">This report presents abstracts of technical studies that pertain to the hydrogeologic framework of the</p><p class=\"textindent\">This report presents abstracts of technical studies that pertain to the hydrogeologic framework of the Española basin, a major subbasin of the Cenozoic Rio Grande rift. Sediments and interbedded volcanic rocks that fill the Española basin comprise an aquifer system that is an important source of water for many residents of the basin, including people in the cities of Santa Fe, Española, and Los Alamos as well as Native Americans in eleven Pueblos.</p><p class=\"textindent\">The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the forth-annual Española basin workshop, held March 1-2 of 2005 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.</p><p class=\"textindent\">The Española basin workshop was hosted by the Española basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and both the Water Research Technical Assistance Office and the Groundwater Protection Program of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.</p><p class=\"textindent\">Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Española basin.</p><p class=\"textindent\">, a major subbasin of the Cenozoic Rio Grande rift. Sediments and interbedded volcanic rocks that fill the Española basin comprise an aquifer system that is an important source of water for many residents of the basin, including people in the cities of Santa Fe, Española, and Los Alamos as well as Native Americans in eleven Pueblos.</p><p class=\"textindent\">The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the forth-annual Española basin workshop, held March 1-2 of 2005 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.</p><p class=\"textindent\">The Española basin workshop was hosted by the Española basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and both the Water Research Technical Assistance Office and the Groundwater Protection Program of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.</p><p class=\"textindent\">Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Española basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051130","usgsCitation":"McKinney, K.C., 2005, Geologic and hydrogeologic framework of the Espanola basin -- Proceedings of the 4th annual Espanola Basin Workshop, Santa Fe, New Mexico, March 1-3, 2005 (Version 1.0): U.S. Geological Survey Open-File Report 2005-1130, 33 p., https://doi.org/10.3133/ofr20051130.","productDescription":"33 p.","costCenters":[],"links":[{"id":186073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6900,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1130/","linkFileType":{"id":5,"text":"html"}},{"id":399711,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71262.htm"}],"country":"United States","state":"New Mexico","otherGeospatial":"Española basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.35314941406249,\n              35.66622234103479\n            ],\n            [\n              -105.77636718749999,\n              35.66622234103479\n            ],\n            [\n              -105.77636718749999,\n              36.38149043210595\n            ],\n            [\n              -106.35314941406249,\n              36.38149043210595\n            ],\n            [\n              -106.35314941406249,\n              35.66622234103479\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8237","contributors":{"authors":[{"text":"McKinney, Kevin C. kcmckinney@usgs.gov","contributorId":3406,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","email":"kcmckinney@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":282583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70522,"text":"ofr20051091 - 2005 - Results of chemical and isotopic analyses of sediment and water from alluvium of the Canadian River near a closed municipal landfill, Norman, Oklahoma","interactions":[],"lastModifiedDate":"2020-03-21T12:03:33","indexId":"ofr20051091","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1091","title":"Results of chemical and isotopic analyses of sediment and water from alluvium of the Canadian River near a closed municipal landfill, Norman, Oklahoma","docAbstract":"Results of physical and chemical analyses of sediment and water collected near a closed municipal landfill at Norman, Oklahoma are presented in this report. Sediment analyses are from 40 samples obtained by freeze-shoe coring at 5 sites, and 14 shallow (depth <1.3 m) sediment samples. The sediment was analyzed to determine grain size, the abundance of extractable iron species and the abundances and isotopic compositions of forms of sulfur. Water samples included pore water from the freeze-shoe core, ground water, and surface water. Pore water from 23 intervals of the core was collected and analyzed for major and trace dissolved species. Thirteen ground-water samples obtained from wells within a few meters of the freeze-shoe core sites and one from the landfill were analyzed for major and trace elements as well as the sulfur and oxygen isotope composition of dissolved sulfate. Samples of surface water were collected at 10 sites along the Canadian River from New Mexico to central Oklahoma. These river-water samples were analyzed for major elements, trace elements, and the isotopic composition of dissolved sulfate.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051091","usgsCitation":"Breit, G.N., Tuttle, M.L., Cozzarelli, I.M., Christenson, S.C., Jaeschke, J.B., Fey, D.L., and Berry, C.J., 2005, Results of chemical and isotopic analyses of sediment and water from alluvium of the Canadian River near a closed municipal landfill, Norman, Oklahoma (Version 1.0): U.S. Geological Survey Open-File Report 2005-1091, 43 p., illus., https://doi.org/10.3133/ofr20051091.","productDescription":"43 p., illus.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":185992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6899,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1091/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Oklahoma ","city":"Norman","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.55,35.14 ], [ -97.55,35.35 ], [ -97.18,35.35 ], [ -97.18,35.14 ], [ -97.55,35.14 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6249fe","contributors":{"authors":[{"text":"Breit, George N. 0000-0003-2188-6798 gbreit@usgs.gov","orcid":"https://orcid.org/0000-0003-2188-6798","contributorId":1480,"corporation":false,"usgs":true,"family":"Breit","given":"George","email":"gbreit@usgs.gov","middleInitial":"N.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tuttle, Michele L.W. mtuttle@usgs.gov","contributorId":47839,"corporation":false,"usgs":true,"family":"Tuttle","given":"Michele","email":"mtuttle@usgs.gov","middleInitial":"L.W.","affiliations":[],"preferred":false,"id":282582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":282580,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282578,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Jaeschke, Jeanne B. 0000-0002-6237-6164 jaeschke@usgs.gov","orcid":"https://orcid.org/0000-0002-6237-6164","contributorId":3876,"corporation":false,"usgs":true,"family":"Jaeschke","given":"Jeanne","email":"jaeschke@usgs.gov","middleInitial":"B.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37464,"text":"WMA - Laboratory & Analytical Services Division","active":true,"usgs":true}],"preferred":true,"id":282581,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fey, David L. dfey@usgs.gov","contributorId":713,"corporation":false,"usgs":true,"family":"Fey","given":"David","email":"dfey@usgs.gov","middleInitial":"L.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":282576,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Berry, Cyrus J. cjberry@usgs.gov","contributorId":946,"corporation":false,"usgs":true,"family":"Berry","given":"Cyrus","email":"cjberry@usgs.gov","middleInitial":"J.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282577,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70520,"text":"fs20053027 - 2005 - Assessment of undiscovered oil and gas resources of the Raton Basin-Sierra Grande uplift province of New Mexico and Colorado, 2004","interactions":[],"lastModifiedDate":"2018-01-08T13:21:18","indexId":"fs20053027","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-3027","title":"Assessment of undiscovered oil and gas resources of the Raton Basin-Sierra Grande uplift province of New Mexico and Colorado, 2004","language":"ENGLISH","doi":"10.3133/fs20053027","usgsCitation":"Higley, D.K., Cook, T.A., Pollastro, R.M., Charpentier, R., Klett, T., and Schenk, C.J., 2005, Assessment of undiscovered oil and gas resources of the Raton Basin-Sierra Grande uplift province of New Mexico and Colorado, 2004 (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3027, 2 p., https://doi.org/10.3133/fs20053027.","productDescription":"2 p.","costCenters":[],"links":[{"id":6897,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3027/","linkFileType":{"id":5,"text":"html"}},{"id":122458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3027.bmp"}],"scale":"24000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671c4f","contributors":{"authors":[{"text":"Higley, Debra K. 0000-0001-8024-9954 higley@usgs.gov","orcid":"https://orcid.org/0000-0001-8024-9954","contributorId":152663,"corporation":false,"usgs":true,"family":"Higley","given":"Debra","email":"higley@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282569,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, Troy A.","contributorId":52519,"corporation":false,"usgs":true,"family":"Cook","given":"Troy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282573,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":282572,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Charpentier, Ronald R. charpentier@usgs.gov","contributorId":934,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","email":"charpentier@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":282571,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":282568,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282570,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70525,"text":"ofr20051176 - 2005 - Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"ofr20051176","displayToPublicDate":"2005-05-06T00:00:00","publicationYear":"2005","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":"2005-1176","title":"Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine","docAbstract":"The Androscoggin River flooded the town of Canton, Maine in December 2003, resulting in damage to and (or) evacuation of 44 homes. Streamflow records at the U.S. Geological Survey (USGS) streamflow-gaging stations at Rumford (USGS station identification number 01054500) and Auburn (01059000) were used to estimate the peak streamflow for the Androscoggin in the town of Canton for this flood (December 18-19, 2003). The estimated peak flood streamflow at Canton was approximately 39,800 ft3/s, corresponding to an estimated recurrence interval of 4.4 years; however, an ice jam downstream from Canton Point on December 18-19 obstructed river flow resulting in a high-water elevation commensurate with an open-water flood approximately equal to a 15-year event. The high water-surface elevations attained during the December 18-19 flood event in Canton were higher than the expected open-water flood water-surface elevations; this verified the assumption that the water-surface elevation was augmented due to the downstream ice jam\r\n\r\nThe change in slope of the riverbed from upstream of Canton to the impoundment at the downstream corporate limits, and the river bend near Stevens Island are principal factors in ice-jam formation near Canton. The U.S. Army Corps of Engineers Ice Jam Database indicates five ice-jam-related floods (including December 2003) for the town of Canton: March 13, 1936; January 1978; March 12, 1987; January 29, 1996; and December 18-19, 2003. There have been more ice-jam-related flood events in Canton than these five documented events, but the exact number and nature of ice jams in Canton cannot be determined without further research.","language":"ENGLISH","doi":"10.3133/ofr20051176","usgsCitation":"Dudley, R.W., 2005, Flooding of the Androscoggin River during December 18-19, 2003, in Canton, Maine (Online only): U.S. Geological Survey Open-File Report 2005-1176, 13 p., https://doi.org/10.3133/ofr20051176.","productDescription":"13 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6902,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1176/","linkFileType":{"id":5,"text":"html"}},{"id":186075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a621","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70209893,"text":"70209893 - 2005 - Are there active glaciers on Mars? (Reply)","interactions":[],"lastModifiedDate":"2020-05-06T16:27:10.152762","indexId":"70209893","displayToPublicDate":"2005-05-05T14:14:05","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Are there active glaciers on Mars? (Reply)","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p><a href=\"https://www.nature.com/articles/nature04357\" data-mce-href=\"https://www.nature.com/articles/nature04357\">Gillespie<span>&nbsp;</span><i>et al</i>.</a><sup><a id=\"ref-link-section-d101162e424\" title=\"Gillespie, A. R., Montgomery, D. R. &amp; Mushkin, A. Nature 438, doi:\n                    10.1038/nature04357\n                    \n                   (2005).\" href=\"https://www.nature.com/articles/nature04358#ref-CR1\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 1\" data-mce-href=\"https://www.nature.com/articles/nature04358#ref-CR1\">1</a></sup><span>&nbsp;</span>concur with our interpretation that certain lobate equatorial and mid-latitude features on Mars are due to debris-covered glaciers formed largely during past periods of increased spin-axis obliquity, when climate regimes favoured snow and ice accumulation and glacial flow<sup><a id=\"ref-link-section-d101162e428\" title=\"Head, J. W. et al. Nature 434, 346–351 (2005).\" href=\"https://www.nature.com/articles/nature04358#ref-CR2\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 2\" data-mce-href=\"https://www.nature.com/articles/nature04358#ref-CR2\">2</a></sup>. They suggest that the ‘hourglass’ deposit, dated at more than 40 Myr old<sup><a id=\"ref-link-section-d101162e432\" title=\"Head, J. W. et al. Nature 434, 346–351 (2005).\" href=\"https://www.nature.com/articles/nature04358#ref-CR2\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 2\" data-mce-href=\"https://www.nature.com/articles/nature04358#ref-CR2\">2</a></sup>, could be active today owing to an additional mechanism that supports “local augmentation of accumulation from snowfall” without climate change on Mars. This mechanism requires the present, or very recent, release of groundwater to the surface to form<span>&nbsp;</span><i>aufeis</i><span>&nbsp;</span>(groundwater-fed ‘glaciers’) where the groundwater is generated by dewatering of hydrous compounds or melting by magmatic or impact-generated heat. We assess whether this suggestion applies to the deposits in question — it was previously proposed for much older deposits in other areas of Mars<sup><a id=\"ref-link-section-d101162e439\" title=\"Carr, M. J. Geophys. Res. 100, 7479–7507 (1995).\" href=\"https://www.nature.com/articles/nature04358#ref-CR3\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 3\" data-mce-href=\"https://www.nature.com/articles/nature04358#ref-CR3\">3</a>,<a id=\"ref-link-section-d101162e442\" title=\"Lucchitta, B. K. J. Geophys. Res. 89, suppl.B 409–418 (1984).\" href=\"https://www.nature.com/articles/nature04358#ref-CR4\" data-track=\"click\" data-track-action=\"reference anchor\" data-track-label=\"link\" data-test=\"citation-ref\" aria-label=\"Reference 4\" data-mce-href=\"https://www.nature.com/articles/nature04358#ref-CR4\">4</a></sup>. We make particular reference to the key relationships in the accumulation zones.</p></div></div>","language":"English","publisher":"Springer Nature","doi":"10.1038/nature04358","usgsCitation":"Head, J., Neukum, G., Jaumann, R., Hiesinger, H., Hauber, E., Carr, M.H., Masson, P., Foing, B., Hoffmann, H., Kreslavsky, M., Milkovich, S., and Van Gasselt, S., 2005, Are there active glaciers on Mars? (Reply): Nature, v. 438, p. E10-E10, https://doi.org/10.1038/nature04358.","productDescription":"1 p.","startPage":"E10","endPage":"E10","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477666,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1038/nature04358","text":"Publisher Index Page"},{"id":374489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"438","noUsgsAuthors":false,"publicationDate":"2005-12-07","publicationStatus":"PW","contributors":{"authors":[{"text":"Head, J.W.","contributorId":67982,"corporation":false,"usgs":true,"family":"Head","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":788517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neukum, G.","contributorId":105443,"corporation":false,"usgs":true,"family":"Neukum","given":"G.","email":"","affiliations":[],"preferred":false,"id":788518,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jaumann, R.","contributorId":81232,"corporation":false,"usgs":false,"family":"Jaumann","given":"R.","email":"","affiliations":[],"preferred":false,"id":788519,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hiesinger, H.","contributorId":62808,"corporation":false,"usgs":true,"family":"Hiesinger","given":"H.","affiliations":[],"preferred":false,"id":788520,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hauber, E.","contributorId":81659,"corporation":false,"usgs":true,"family":"Hauber","given":"E.","affiliations":[],"preferred":false,"id":788521,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":788522,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Masson, P.","contributorId":21318,"corporation":false,"usgs":true,"family":"Masson","given":"P.","email":"","affiliations":[],"preferred":false,"id":788523,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Foing, B.","contributorId":91761,"corporation":false,"usgs":true,"family":"Foing","given":"B.","email":"","affiliations":[],"preferred":false,"id":788525,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hoffmann, H.","contributorId":51464,"corporation":false,"usgs":true,"family":"Hoffmann","given":"H.","email":"","affiliations":[],"preferred":false,"id":788582,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Kreslavsky, M.","contributorId":17108,"corporation":false,"usgs":true,"family":"Kreslavsky","given":"M.","email":"","affiliations":[],"preferred":false,"id":788583,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Milkovich, S.","contributorId":33598,"corporation":false,"usgs":true,"family":"Milkovich","given":"S.","affiliations":[],"preferred":false,"id":788584,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Van Gasselt, S.","contributorId":58855,"corporation":false,"usgs":true,"family":"Van Gasselt","given":"S.","email":"","affiliations":[],"preferred":false,"id":788585,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}}
,{"id":70209892,"text":"70209892 - 2005 - New Perspectives on Ancient Mars","interactions":[],"lastModifiedDate":"2020-05-06T11:52:21.820641","indexId":"70209892","displayToPublicDate":"2005-05-05T13:57:20","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"New Perspectives on Ancient Mars","docAbstract":"<p><span>Mars was most active during its first billion years. The core, mantle, and crust formed within ∼50 million years of solar system formation. A magnetic dynamo in a convecting fluid core magnetized the crust, and the global field shielded a more massive early atmosphere against solar wind stripping. The Tharsis province became a focus for volcanism, deformation, and outgassing of water and carbon dioxide in quantities possibly sufficient to induce episodes of climate warming. Surficial and near-surface water contributed to regionally extensive erosion, sediment transport, and chemical alteration. Deep hydrothermal circulation accelerated crustal cooling, preserved variations in crustal thickness, and modified patterns of crustal magnetization.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.1101812","usgsCitation":"Solomon, S., Aharonson, O., Aurnou, J., Banerdt, W.B., Carr, M.H., Dombard, A.J., Frey, H.V., Golombek, M., Hauck, S., Head, J., Jakosky, B.M., Johnson, C., McGovern, P., Neumann, G., Phillips, R., Smith, D., and Zuber, M., 2005, New Perspectives on Ancient Mars: Science, v. 307, no. 5713, p. 1214-1220, https://doi.org/10.1126/science.1101812.","productDescription":"8 p.","startPage":"1214","endPage":"1220","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477668,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://escholarship.org/uc/item/0gk963r3","text":"External Repository"},{"id":374469,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"307","issue":"5713","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Solomon, S.C.","contributorId":39960,"corporation":false,"usgs":true,"family":"Solomon","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":788500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aharonson, O.","contributorId":105030,"corporation":false,"usgs":false,"family":"Aharonson","given":"O.","affiliations":[],"preferred":false,"id":788501,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Aurnou, J.M.","contributorId":224467,"corporation":false,"usgs":false,"family":"Aurnou","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":788502,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Banerdt, W. B.","contributorId":196350,"corporation":false,"usgs":false,"family":"Banerdt","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":788503,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carr, Michael H.","contributorId":61894,"corporation":false,"usgs":true,"family":"Carr","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":788504,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Dombard, A. J.","contributorId":224469,"corporation":false,"usgs":false,"family":"Dombard","given":"A.","middleInitial":"J.","affiliations":[],"preferred":false,"id":788505,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Frey, H. V.","contributorId":152669,"corporation":false,"usgs":false,"family":"Frey","given":"H.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":788506,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Golombek, Matthew P.","contributorId":93180,"corporation":false,"usgs":true,"family":"Golombek","given":"Matthew P.","affiliations":[],"preferred":false,"id":788507,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Hauck, S.A. II","contributorId":224473,"corporation":false,"usgs":false,"family":"Hauck","given":"S.A.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":788508,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Head, J.W.","contributorId":67982,"corporation":false,"usgs":true,"family":"Head","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":788509,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Jakosky, Bruce M.","contributorId":67240,"corporation":false,"usgs":true,"family":"Jakosky","given":"Bruce","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":788510,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Johnson, C.L.","contributorId":98546,"corporation":false,"usgs":true,"family":"Johnson","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":788511,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"McGovern, P.J.","contributorId":224474,"corporation":false,"usgs":false,"family":"McGovern","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":788512,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Neumann, G.A.","contributorId":11767,"corporation":false,"usgs":true,"family":"Neumann","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":788513,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Phillips, R.J.","contributorId":93174,"corporation":false,"usgs":true,"family":"Phillips","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":788514,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Smith, D.E.","contributorId":44109,"corporation":false,"usgs":true,"family":"Smith","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":788515,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Zuber, Maria","contributorId":200800,"corporation":false,"usgs":false,"family":"Zuber","given":"Maria","email":"","affiliations":[],"preferred":false,"id":788516,"contributorType":{"id":1,"text":"Authors"},"rank":17}]}}
,{"id":70517,"text":"wdrKY041 - 2005 - Water resources data, Kentucky, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"wdrKY041","displayToPublicDate":"2005-05-05T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"KY-04-1","title":"Water resources data, Kentucky, water year 2004","docAbstract":"Water resources data for the 2004 water year for Kentucky consist of records of stage, discharge, and water-quality of streams and lakes; and water levels of wells. This report includes daily discharge records for 131 stream-stations. It also includes water-quality data for 15 stations sampled at regular intervals, continuous temperature at 7 stations, and continuous water-quality at 11 stations. Ground-water levels are published for 8 recording and 22 partial record sites. Precipitation data at a regular interval are published for two sites. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Kentucky.","language":"ENGLISH","doi":"10.3133/wdrKY041","usgsCitation":"McClain, D.L., Moses, C.R., and Darnell, R.S., 2005, Water resources data, Kentucky, water year 2004: U.S. Geological Survey Water Data Report KY-04-1, v., 675 p. : charts, maps ; 28 cm. \r\n, https://doi.org/10.3133/wdrKY041.","productDescription":"v., 675 p. : charts, maps ; 28 cm. \r\n","costCenters":[],"links":[{"id":6476,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ky-04-1/","linkFileType":{"id":5,"text":"html"}},{"id":187900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1326","contributors":{"authors":[{"text":"McClain, Dennis L.","contributorId":43860,"corporation":false,"usgs":true,"family":"McClain","given":"Dennis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moses, Clifford R.","contributorId":69245,"corporation":false,"usgs":true,"family":"Moses","given":"Clifford","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282567,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darnell, Roy S.","contributorId":25641,"corporation":false,"usgs":true,"family":"Darnell","given":"Roy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":282565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70184347,"text":"70184347 - 2005 - Beringia: Intercontinental exchange and diversification of high latitude mammals and their parasites during the Pliocene and Quaternary","interactions":[],"lastModifiedDate":"2017-03-07T16:25:42","indexId":"70184347","displayToPublicDate":"2005-05-05T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5178,"text":"Mammal Study","active":true,"publicationSubtype":{"id":10}},"title":"Beringia: Intercontinental exchange and diversification of high latitude mammals and their parasites during the Pliocene and Quaternary","docAbstract":"<p><span>Beringia is the region spanning eastern Asia and northwestern North America that remained ice-free during the full glacial events of the Pleistocene. Numerous questions persist regarding the importance of this region in the evolution of northern faunas. Beringia has been implicated as both a high latitude refugium and as the crossroads (Bering Land Bridge) of the northern continents for boreal mammals. The Beringian Coevolution Project (BCP) is an international collaboration that has provided material to assess the pattern and timing of faunal exchange across the crossroads of the northern continents and the potential impact of past climatic events on differentiation. Mammals and associated parasite specimens have been collected and preserved from more than 200 field sites in eastern Russia, Alaska and northwestern Canada since 1999. Previously, fossils and taxonomic comparisons between Asia and North America mammals have shed light on these events. Molecular phylogenetics based on BCP specimens is now being used to trace the history of faunal exchange and diversification. We have found substantial phylogeographic structure in the Arctic and in Beringia in mustelid carnivores, arvicoline rodents, arctic hares and soricine shrews, including spatially concordant clades and contact zones across taxa that correspond to the edges of Beringia. Among the tapeworms of these mammalian hosts, new perspectives on diversity have also been developed. </span><i>Arostrilepis horrida</i><span> (Hymenolepididae) was considered to represent a single widespread and morphologically variable species occurring in a diversity of voles and lemmings in eastern and western Beringia and more broadly across the Holarctic region. The BCP has demonstrated a complex of at least 10 species that are poorly differentiated morphologically. The diversity of </span><i>Paranoplocephala</i><span> spp. and </span><i>Anolocephaloides</i><span> spp. (Anoplocephalidae) in Beringia included relatively few widespread and morphologically variable species in arvicolines. BCP collections have changed this perspective, allowing the recognition of a series of highly endemic species of </span><i>Paranoplocephala</i><span> that demonstrate very narrow host specificity, and additional species complexes among arvicolines. Thus, extensive, previously unrecognized, diversity for tapeworms of 2 major families characterizes the Beringian fauna. By elucidating evolutionary relationships and phylogeographic variation among populations, species and assemblages, refined views of the sequence and timing of biotic expansion, geographic colonization and impact of episodic climate change have been developed for Beringia. Ultimately, Beringia was a determining factor in the structure and biogeography of terrestrial faunas across the Nearctic and Neotropical regions during the Pliocene and Quaternary.</span></p>","language":"English","publisher":"Mammal Society of Japan","doi":"10.3106/1348-6160(2005)30[33:BIEADO]2.0.CO;2","usgsCitation":"Cook, J.A., Hoberg, E.P., Koehler, A., Henttonen, H., Wickstrom, L., Haukisalmi, V., Galbreath, K.E., Chernyavski, F., Dokuchaev, N., Lahzuhtkin, A., MacDonald, S.O., Hope, A.G., Waltari, E., Runck, A., Veitch, A., Jenkins, E., Kutz, S., and Eckerlin, R., 2005, Beringia: Intercontinental exchange and diversification of high latitude mammals and their parasites during the Pliocene and Quaternary: Mammal Study, v. 30, no. sp1, p. S33-S44, https://doi.org/10.3106/1348-6160(2005)30[33:BIEADO]2.0.CO;2.","productDescription":"12 p.","startPage":"S33","endPage":"S44","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":494170,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3106/1348-6160(2005)30[33:bieado]2.0.co;2","text":"Publisher Index Page"},{"id":336987,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, Russia, United States","otherGeospatial":"Berengia","volume":"30","issue":"sp1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58bfd4ffe4b014cc3a3ba538","contributors":{"authors":[{"text":"Cook, Joseph A.","contributorId":70318,"corporation":false,"usgs":true,"family":"Cook","given":"Joseph","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":681110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoberg, Eric P.","contributorId":102448,"corporation":false,"usgs":false,"family":"Hoberg","given":"Eric","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":681111,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koehler, Anson V.","contributorId":73740,"corporation":false,"usgs":true,"family":"Koehler","given":"Anson V.","affiliations":[],"preferred":false,"id":681112,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Henttonen, Heikki","contributorId":187632,"corporation":false,"usgs":false,"family":"Henttonen","given":"Heikki","email":"","affiliations":[],"preferred":false,"id":681113,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wickstrom, Lotta","contributorId":187633,"corporation":false,"usgs":false,"family":"Wickstrom","given":"Lotta","email":"","affiliations":[],"preferred":false,"id":681114,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Haukisalmi, Voitto","contributorId":187634,"corporation":false,"usgs":false,"family":"Haukisalmi","given":"Voitto","email":"","affiliations":[],"preferred":false,"id":681115,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Galbreath, Kurt E.","contributorId":48867,"corporation":false,"usgs":true,"family":"Galbreath","given":"Kurt","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":681116,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Chernyavski, Felix","contributorId":187635,"corporation":false,"usgs":false,"family":"Chernyavski","given":"Felix","email":"","affiliations":[],"preferred":false,"id":681117,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Dokuchaev, Nikolai","contributorId":187636,"corporation":false,"usgs":false,"family":"Dokuchaev","given":"Nikolai","email":"","affiliations":[],"preferred":false,"id":681118,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lahzuhtkin, Anatoli","contributorId":187637,"corporation":false,"usgs":false,"family":"Lahzuhtkin","given":"Anatoli","email":"","affiliations":[],"preferred":false,"id":681119,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"MacDonald, Stephen O.","contributorId":187638,"corporation":false,"usgs":false,"family":"MacDonald","given":"Stephen","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":681120,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Hope, Andrew G. 0000-0003-3814-2891 ahope@usgs.gov","orcid":"https://orcid.org/0000-0003-3814-2891","contributorId":4309,"corporation":false,"usgs":true,"family":"Hope","given":"Andrew","email":"ahope@usgs.gov","middleInitial":"G.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":681121,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Waltari, Eric","contributorId":105946,"corporation":false,"usgs":false,"family":"Waltari","given":"Eric","affiliations":[],"preferred":false,"id":681122,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Runck, Amy","contributorId":187640,"corporation":false,"usgs":false,"family":"Runck","given":"Amy","email":"","affiliations":[],"preferred":false,"id":681123,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Veitch, Alasdair","contributorId":187641,"corporation":false,"usgs":false,"family":"Veitch","given":"Alasdair","email":"","affiliations":[],"preferred":false,"id":681124,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Jenkins, Emily","contributorId":187643,"corporation":false,"usgs":false,"family":"Jenkins","given":"Emily","email":"","affiliations":[],"preferred":false,"id":681125,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Kutz, Susan","contributorId":187644,"corporation":false,"usgs":false,"family":"Kutz","given":"Susan","affiliations":[],"preferred":false,"id":681126,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Eckerlin, Ralph P.","contributorId":17087,"corporation":false,"usgs":true,"family":"Eckerlin","given":"Ralph P.","affiliations":[],"preferred":false,"id":681127,"contributorType":{"id":1,"text":"Authors"},"rank":18}]}}
,{"id":70510,"text":"sir20055008 - 2005 - Hydrogeologic framework and estimates of ground-water volumes in Tertiary and upper Cretaceous hydrogeologic units in the Powder River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20055008","displayToPublicDate":"2005-05-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5008","title":"Hydrogeologic framework and estimates of ground-water volumes in Tertiary and upper Cretaceous hydrogeologic units in the Powder River basin, Wyoming","docAbstract":"The Powder River Basin in Wyoming and Montana is an important source of energy resources for the United States. Coalbed methane gas is contained in Tertiary and upper Cretaceous hydrogeologic units in the Powder River Basin. This gas is released when water pressure in coalbeds is lowered, usually by pumping ground water. Issues related to disposal and uses of by-product water from coalbed methane production have developed, in part, due to uncertainties in hydrologic properties. One hydrologic property of primary interest is the amount of water contained in Tertiary and upper Cretaceous hydrogeologic units in the Powder River Basin. The U.S. Geological Survey, in cooperation with the Bureau of Land Management, conducted a study to describe the hydrogeologic framework and to estimate ground-water volumes in different facies of Tertiary and upper Cretaceous hydrogeologic units in the Powder River Basin in Wyoming.\r\n\r\nA geographic information system was used to compile and utilize hydrogeologic maps, to describe the hydrogeologic framework, and to estimate the volume of ground water in Tertiary and upper Cretaceous hydrogeologic units in the Powder River structural basin in Wyoming. Maps of the altitudes of potentiometric surfaces, altitudes of the tops and bottoms of hydrogeologic units, thicknesses of hydrogeologic units, percent sand of hydrogeologic units, and outcrop boundaries for the following hydrogeologic units were used: Tongue River-Wasatch aquifer, Lebo confining unit, Tullock aquifer, Upper Hell Creek confining unit, and the Fox Hills-Lower Hell Creek aquifer. Literature porosity values of 30 percent for sand and 35 percent for non-sand facies were used to calculate the volume of total ground water in each hydrogeologic unit. Literature specific yield values of 26 percent for sand and 10 percent for non-sand facies, and literature specific storage values of 0.0001 ft-1 (1/foot) for sand facies and 0.00001 ft-1 for non-sand facies, were used to calculate a second volume of ground water for each hydrogeologic unit. Significant figure considerations limited estimates of ground-water volumes to two significant digits.\r\n\r\nA total ground-water volume of 2.0x1014 ft3 (cubic feet) was calculated using porosity values, and a total ground-water volume of 3.6x1013 ft3 was calculated using specific yield and specific storage values. These results are consistent with retention properties, which would have some of the total water being retained in the sediments.\r\n\r\nSensitivity analysis shows that the estimates of ground-water volume are most sensitive to porosity. The estimates also are sensitive to confined thickness and saturated thickness. Better spatial information for hydrogeologic units could help refine the ground-water volume estimates.","language":"ENGLISH","doi":"10.3133/sir20055008","usgsCitation":"Hinaman, K., 2005, Hydrogeologic framework and estimates of ground-water volumes in Tertiary and upper Cretaceous hydrogeologic units in the Powder River basin, Wyoming: U.S. Geological Survey Scientific Investigations Report 2005-5008, 24 p., https://doi.org/10.3133/sir20055008.","productDescription":"24 p.","costCenters":[],"links":[{"id":6473,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5008/","linkFileType":{"id":5,"text":"html"}},{"id":187805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627e3e","contributors":{"authors":[{"text":"Hinaman, Kurt","contributorId":23226,"corporation":false,"usgs":true,"family":"Hinaman","given":"Kurt","affiliations":[],"preferred":false,"id":282560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70514,"text":"sir20045290 - 2005 - Distribution and mass of nitrate in the unconfined aquifer beneath the intensively cultivated area north of the Rio Grande, San Luis Valley, Colorado, 1997 through 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20045290","displayToPublicDate":"2005-05-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5290","title":"Distribution and mass of nitrate in the unconfined aquifer beneath the intensively cultivated area north of the Rio Grande, San Luis Valley, Colorado, 1997 through 2001","docAbstract":"Current (1997?2001) and historical (1948?49, 1968?69) nitrate-concentration and water-level data collected from wells completed in the unconfined aquifer in the intensively cultivated area north of the Rio Grande in south-central Colorado were used to determine the distribution and mass of nitrate and to determine short- and long-term trends in the concentration and mass of nitrate in the unconfined aquifer. ","language":"ENGLISH","doi":"10.3133/sir20045290","usgsCitation":"Stogner, 2005, Distribution and mass of nitrate in the unconfined aquifer beneath the intensively cultivated area north of the Rio Grande, San Luis Valley, Colorado, 1997 through 2001 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5290, v, 62 p., https://doi.org/10.3133/sir20045290.","productDescription":"v, 62 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6475,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045290/","linkFileType":{"id":5,"text":"html"}},{"id":187899,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649659","contributors":{"authors":[{"text":"Stogner 0000-0002-3185-1452 rstogner@usgs.gov","orcid":"https://orcid.org/0000-0002-3185-1452","contributorId":938,"corporation":false,"usgs":true,"family":"Stogner","email":"rstogner@usgs.gov","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70512,"text":"sir20055063 - 2005 - Variability of differences between two approaches for determining ground-water discharge and pumpage, including effects of time trends, Lower Arkansas River Basin, southeastern Colorado, 1998-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:13:32","indexId":"sir20055063","displayToPublicDate":"2005-05-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5063","title":"Variability of differences between two approaches for determining ground-water discharge and pumpage, including effects of time trends, Lower Arkansas River Basin, southeastern Colorado, 1998-2002","docAbstract":"In the mid-1990s, the Colorado Division of Water Resources (CDWR) adopted rules governing measurement of tributary ground-water pumpage for the Arkansas River Basin. The rules allowed ground-water pumpage to be determined using one of two approaches?power conversion coefficient (PCC) or totalizing flowmeters (TFM). In addition, the rules allowed a PCC to be applied to the electrical power usage up to 4 years in the future to estimate ground-water pumpage. \r\n\r\nAs a result of concerns about potential errors in applying the PCC approach forward in time, a study was done by the U.S. Geological Survey, in cooperation with CDWR and Colorado Water Conservation Board, to evaluate the variability in differences in pumpage between the two approaches, including the effects of time trends.\r\n\r\nThis report compared measured ground-water pumpage using TFMs to computed ground-water pumpage using PCCs by developing statistical models of relations between explanatory variables, such as site, time, and pumping water level, and dependent variables, which are based on discharge, PCC, and pumpage. When differences in pumpage (diffP) were computed using PCC measurements and power consumption for the same year (1998-2002), the median diffP, depending on the year, ranged from +0.1 to -2.9 percent; the median diffP for the entire period was -1.5 percent. However, when diffP was computed using PCC measurements applied to the next year's power consumption, the median diffP was -0.3 percent; and when PCC measurements were applied 2, 3, or 4 years into the future, median diffPs were +1.8 percent for a 2-year forward lag and +5.3 percent for a 4-year forward lag, indicating that pumpage computed with the PCC approach, as generally applied under the ground-water pumpage measurement rules by CDWR, tended to overestimate pumpage as compared to pumpage using TFMs when PCC measurement was applied to future years of measured power consumption. \r\n\r\nAnalyses were done to better understand the causes of the time trend; an estimate of the overall trend with time (uncorrected for pumping water-level changes) yielded a trend of about 2.2 percent per lag year for diffP. A separate analysis that incorporated a surface-water diversion term in the statistical model rendered the time-trend term insignificant, indicating that the time trend in the models served as a surrogate for other variables, some of which reflect underlying hydrologic conditions. A more precise explanation of the potential causes of the time trend was not obtained with the available data. However, the model results with the surface-water diversion term indicate that much of the trend of 2.2 percent per lag year in diffP resulted from applying a PCC to estimate pumpage under hydrologic conditions different from those under which the PCC was measured. Although there is no evidence to conclude that the upward time trend determined in the data for this 5-year period would hold in the future, historical static ground-water levels in the study area generally have exhibited small variations over multidecadal time scales. Therefore, the approximately 2 percent per lag year trend determined in these data is expected to be a reasonable guideline for estimating potential errors in the PCC approach resulting from temporally varying hydrologic conditions between time of PCC measurement and pumpage estimation. \r\n\r\nComparisons also were made between total, or aggregated, pumpage for a network of wells as computed by the PCC approach and the TFM approach. For 100 wells and a lag of 4 years between PCC measurement and pumpage estimation, there was a 95-percent probability that the difference between total network pumpage measured by the PCC approach and that measured using a TFM would be between 5.2 and 14.4 percent. These estimates were based on a bias of 2.2 percent per lag year estimated for the period 1998-2002 during which hydrologic conditions were known to have changed. Using the same assumptions, the estimated d","language":"ENGLISH","doi":"10.3133/sir20055063","usgsCitation":"Troutman, B., Edelmann, P., and Dash, R.G., 2005, Variability of differences between two approaches for determining ground-water discharge and pumpage, including effects of time trends, Lower Arkansas River Basin, southeastern Colorado, 1998-2002 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5063, 166 p., https://doi.org/10.3133/sir20055063.","productDescription":"166 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6474,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5063/","linkFileType":{"id":5,"text":"html"}},{"id":120986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2005_5063.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602bb2","contributors":{"authors":[{"text":"Troutman, Brent M.","contributorId":41040,"corporation":false,"usgs":true,"family":"Troutman","given":"Brent M.","affiliations":[],"preferred":false,"id":282561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edelmann, Patrick","contributorId":86305,"corporation":false,"usgs":true,"family":"Edelmann","given":"Patrick","affiliations":[],"preferred":false,"id":282563,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dash, Russell G.","contributorId":64695,"corporation":false,"usgs":true,"family":"Dash","given":"Russell","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282562,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70507,"text":"sim2884 - 2005 - Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies","interactions":[],"lastModifiedDate":"2022-12-14T21:20:58.248532","indexId":"sim2884","displayToPublicDate":"2005-05-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2884","title":"Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies","docAbstract":"Idaho lies within the northern sector of the U.S. Cordillera astride the \r\n        boundary between the Proterozoic continent (Laurentia) to the east and \r\n        the Permian to Jurassic accreted terranes to the west.  The continental \r\n        basement is mostly covered by relatively undeformed Mesoproterozoic \r\n        metasedimentary rocks and intruded or covered by Phanerozoic igneous \r\n        rocks; accordingly, knowledge of the basement geology is poorly \r\n        constrained.  Incremental knowledge gained since the pioneering studies \r\n        by W. Lindgren, C.P. Ross, A.L. Anderson, A. Hietanen, and others during \r\n        the early- and mid-1900's has greatly advanced our understanding of the \r\n        general geology of Idaho.  However, knowledge of the basement geology \r\n        remains relatively poor, partly because of the remoteness of much of the \r\n        region plus the lack of a stimulus to decipher the complex assemblage of \r\n        high-grade gneisses and migmatite of central Idaho.  The availability of \r\n        an updated aeromagnetic anomaly map of Idaho (North American Magnetic \r\n        Anomaly Group, 2002) provides a means to determine the regional \r\n        Precambrian geologic framework of the State.  The combined geologic and \r\n        aeromagnetic data permit identification of previously unrecognized \r\n        crystalline basement terranes, assigned to Archean and Paleoproterozoic \r\n        ages, and the delineation of major shear zones, which are expressed in \r\n        the aeromagnetic data as linear negative anomalies (Finn and Sims, \r\n        2004).  Limited geochronologic data on exposed crystalline basement \r\n        aided by isotopic studies of zircon inheritance, particularly Bickford \r\n        and others (1981) and Mueller and others (1995), provide much of the \r\n        geologic background for our interpretation of the basement geology.  In \r\n        northwestern United States, inhomogeneities in the basement inherited \r\n        from Precambrian tectogenesis controlled many large-scale tectonic \r\n        features that developed during the Phanerozoic.  Two basement \r\n        structures, in particular, provided zones of weakness that were \r\n        repeatedly rejuvenated:  (1) northeast-trending ductile shear zones \r\n        developed on the northwest margin of the Archean Wyoming province during \r\n        the Paleoproterozoic Trans-Montana orogeny (Sims and others, 2004), and \r\n        (2) northwest-trending intra-continental faults of the Mesoproterozoic \r\n        Trans-Rocky Mountain strike-slip fault system (Sims, unpub. data, 2003).  \r\n        In this report, geologic ages are reported in millions of years (Ma) and \r\n        generalized ages are given in billions of years (Ga).  The subdivision \r\n        of Precambrian rocks used herein is the time classification recommended \r\n        by the International Union of Geological Sciences (Plumb, 1991).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim2884","usgsCitation":"Sims, P., Lund, K., and Anderson, E., 2005, Precambrian crystalline basement map of Idaho: An interpretation of aeromagnetic anomalies (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2884, Report: 21 p.; 1 Plate: 56.50 × 36.50 inches; Metadata: Downloads Directory, https://doi.org/10.3133/sim2884.","productDescription":"Report: 21 p.; 1 Plate: 56.50 × 36.50 inches; Metadata: Downloads Directory","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":187804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110559,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71261.htm","linkFileType":{"id":5,"text":"html"},"description":"71261"},{"id":6472,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2884/","linkFileType":{"id":5,"text":"html"}}],"country":"United 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H.","contributorId":41469,"corporation":false,"usgs":true,"family":"Lanier","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282554,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Melendez, F.","contributorId":91922,"corporation":false,"usgs":true,"family":"Melendez","given":"F.","email":"","affiliations":[],"preferred":false,"id":282555,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70505,"text":"sir20055064 - 2005 - Distribution and sources of polychlorinated biphenyls in Woods Inlet, Lake Worth, Fort Worth, Texas, 2003","interactions":[],"lastModifiedDate":"2017-05-30T10:04:25","indexId":"sir20055064","displayToPublicDate":"2005-05-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5064","title":"Distribution and sources of polychlorinated biphenyls in Woods Inlet, Lake Worth, Fort Worth, Texas, 2003","docAbstract":"Woods Inlet is a flooded stream channel on the southern shore of Lake Worth along the western boundary of Air Force Plant 4 in Fort Worth, Texas, where elevated polychlorinated biphenyl (PCB) concentrations in sediment were detected in a previous study. In response, the U.S. Geological Survey, in cooperation with the U.S. Air Force, conducted a study in 2003 to map the extent of elevated PCB concentrations in Woods Inlet and to identify possible sources (or more specifically, source areas) of PCBs in the watershed of Woods Inlet. Three gravity cores (penetration to pre-reservoir sediment at three sites) and 17 box cores (surficial bottom sediment samples) were collected in Woods Inlet. Suspended sediment in stormwater runoff and streambed sediment were sampled in tributaries to Woods Inlet following storms. Assemblages of PCB congeners in surficial inlet sediments and suspended and streambed sediments were analyzed to indicate sources of PCBs in the inlet sediments on the basis of chemical signatures of PCBs. Woods Inlet receives runoff primarily from three tributaries: (1) Gruggs Park Creek, (2) the small unnamed creek that drains a Texas National Guard maintenance facility, called TNG Creek for this report, and (3) Meandering Road Creek. Twenty-seven of 209 possible PCB congeners were analyzed. The sum of the congeners was used as a measure of total PCB. The spatial distribution of total PCB concentrations in the inlet indicates that most PCBs are originating in the Meandering Road Creek watershed. Peak total PCB concentrations in the three gravity cores occurred at depths corresponding to sediment deposition dates of about 1960 for two of the cores and about 1980 for the third core. The magnitudes of peak total PCB concentrations in the gravity cores followed a spatial distribution generally similar to that of surficial bottom sediment concentrations. Total PCB concentrations in suspended and streambed sediment varied greatly between sites and indicated a likely source of PCBs associated with a sampling site that receives runoff from Air Force Plant 4. Three approaches to the analyses of congener assemblages indicate that PCBs in surficial bottom sediment of Woods Inlet primarily enter Lake Worth from Meandering Road Creek and that runoff from Air Force Plant 4 is a source of the PCBs in Meandering Road Creek. Although current (2003) transport of PCBs from Air Force Plant 4 to the creek is occurring, large decreases in PCB concentrations with decreasing age in two cores indicate that PCB loading to the inlet has decreased greatly since the 1960s. Because runoff entering Meandering Road Creek from some parts of Air Force Plant 4 was not measured or sampled in this study, it cannot be said with certainty that the Air Force Plant 4 site sampled is the only source of PCBs to Meandering Road Creek.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055064","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Besse, R.E., Van Metre, P., and Wilson, J.T., 2005, Distribution and sources of polychlorinated biphenyls in Woods Inlet, Lake Worth, Fort Worth, Texas, 2003: U.S. Geological Survey Scientific Investigations Report 2005-5064, iv, 40 p., https://doi.org/10.3133/sir20055064.","productDescription":"iv, 40 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":341816,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5064/pdf/sir2005-5064.pdf","text":"Report","size":"17.6 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":6470,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5064/","linkFileType":{"id":5,"text":"html"}},{"id":187700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Fort Worth","otherGeospatial":"Lake Worth","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.5,\n              32.77\n            ],\n            [\n              -97.4,\n              32.77\n            ],\n            [\n              -97.4,\n              32.87\n            ],\n            [\n              -97.5,\n              32.87\n            ],\n            [\n              -97.5,\n              32.77\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641a76","contributors":{"authors":[{"text":"Besse, Richard E.","contributorId":10104,"corporation":false,"usgs":true,"family":"Besse","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Metre, Peter C.","contributorId":34104,"corporation":false,"usgs":true,"family":"Van Metre","given":"Peter C.","affiliations":[],"preferred":false,"id":282551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, Jennifer T. 0000-0003-4481-6354 jenwilso@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-6354","contributorId":1782,"corporation":false,"usgs":true,"family":"Wilson","given":"Jennifer","email":"jenwilso@usgs.gov","middleInitial":"T.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282549,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70239109,"text":"70239109 - 2005 - Comparison of the deep crustal structure and seismicity of North America with the Indian subcontinent","interactions":[],"lastModifiedDate":"2022-12-27T22:03:05.434708","indexId":"70239109","displayToPublicDate":"2005-05-01T15:25:15","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1359,"text":"Current Science","onlineIssn":"0011-3891","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of the deep crustal structure and seismicity of North America with the Indian subcontinent","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Current Science Association","usgsCitation":"Mooney, W.D., Rao, V., Reddy, P., Chulick, G.S., and Detweiler, S.T., 2005, Comparison of the deep crustal structure and seismicity of North America with the Indian subcontinent: Current Science, v. 88, no. 10, p. 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Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":860079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rao, V.V.","contributorId":43959,"corporation":false,"usgs":true,"family":"Rao","given":"V.V.","email":"","affiliations":[],"preferred":false,"id":860080,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reddy, P.R.","contributorId":30806,"corporation":false,"usgs":true,"family":"Reddy","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":860081,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Chulick, Gary S.","contributorId":36823,"corporation":false,"usgs":true,"family":"Chulick","given":"Gary","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":860082,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Detweiler, Shane T. 0000-0001-5699-011X shane@usgs.gov","orcid":"https://orcid.org/0000-0001-5699-011X","contributorId":680,"corporation":false,"usgs":true,"family":"Detweiler","given":"Shane","email":"shane@usgs.gov","middleInitial":"T.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":860083,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70239865,"text":"70239865 - 2005 - Digital terrain modeling","interactions":[],"lastModifiedDate":"2023-01-23T19:32:51.282332","indexId":"70239865","displayToPublicDate":"2005-05-01T13:23:10","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Digital terrain modeling","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of social measurement","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Elsevier","doi":"10.1016/B0-12-369398-5/00357-1","usgsCitation":"Pike, R.J., 2005, Digital terrain modeling, chap. <i>of</i> Encyclopedia of social measurement, p. 669-675, https://doi.org/10.1016/B0-12-369398-5/00357-1.","productDescription":"7 p.","startPage":"669","endPage":"675","costCenters":[],"links":[{"id":412232,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Kempf-Leonard, Kimberly","contributorId":301141,"corporation":false,"usgs":false,"family":"Kempf-Leonard","given":"Kimberly","email":"","affiliations":[],"preferred":false,"id":862202,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Pike, Richard J. rpike@usgs.gov","contributorId":5753,"corporation":false,"usgs":true,"family":"Pike","given":"Richard","email":"rpike@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":862201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70238534,"text":"70238534 - 2005 - Radioisotopic and biostratigraphic age relations in the Coast Range Ophiolite, northern California: Implications for the tectonic evolution of the Western Cordillera","interactions":[],"lastModifiedDate":"2022-11-28T19:06:26.49107","indexId":"70238534","displayToPublicDate":"2005-05-01T12:52:19","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Radioisotopic and biostratigraphic age relations in the Coast Range Ophiolite, northern California: Implications for the tectonic evolution of the Western Cordillera","docAbstract":"<p>The Coast Range ophiolite (CRO) in northern California includes two distinct remnants. The Elder Creek ophiolite is a classic suprasubduction zone ophiolite with three sequential plutonic suites (layered gabbro, wehrlit-pyroxenite, quartz diorite), a mafic to felsic dike complex, and mafic-felsic volcanic rocks; the entire suite is cut by late mid-oceanic-ridge basalt (MORB) dikes and overlain by ophiolitic breccia. The Stonyford volcanic complex (SFVC) comprises three volcanic series with intercalated chert horizons that form a submarine volcano enclosed in sheared serpentinite. Structurally below this seamount are mélange blocks of CRO similar to Elder Creek.</p><p>U/Pb zircon ages from plagiogranite and quartz diorites at Elder Creek range in age from 165 Ma to 172 Ma. U/Pb zircon ages obtained from CRO mélange blocks below the SFVC are similar (166–172 Ma).<span>&nbsp;</span><sup>40</sup>Ar-<sup>39</sup>Ar ages of alkali basalt glass in the upper SFVC are all younger at ≈164 Ma. Radiolarians extracted from chert lenses intercalated with basalt in the SFVC indicate that the sedimentary strata range in age from Bathonian (Unitary Association Zone 6–6 of<span>&nbsp;</span><a class=\"link link-ref xref-bibr\" data-modal-source-id=\"I0016-7606-117-5-633-BAUMGARTNER1\">Baumgartner et al., 1995a</a>) near the base of the complex to late Callovian to early Kimmeridgian (Unitary Association Zones 8–10) in the upper part. The SFVC sedimentary record preserves evidence of a major faunal change wherein relatively small sized, polytaxic radiolarian faunas were replaced by very robust, oligo-taxic, nassellarian-dominated faunas that included<span>&nbsp;</span><i>Praeparvicingula</i><span>&nbsp;</span>spp.</p><p>We suggest that CRO formation began after the early Middle Jurassic (172–180 Ma) collision of an exotic or fringing arc with North America and initiation of a new or reconfigured east-dipping subduction zone. The data show that the CRO formed prior to the Late Jurassic Nevadan orogeny, probably by rapid forearc extension above a nascent subduction zone. We infer that CRO spreading ended with the collision of an oceanic spreading center ca. 164 Ma, coincident with the oldest high-grade blocks in the structurally underlying Franciscan assemblage. We further suggest that the “classic” Nevadan orogeny represents a response to spreading center collision, with shallow subduction of young lithosphere causing the initial compressional deformation and with a subsequent change in North American plate motion to rapid northward drift (J2 cusp) causing sinistral transpression and transtension in the Sierra foothills. These data are not consistent with models for Late Jurassic arc collision in the Sierra foothills or a backarc origin for the CRO.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/B25443.1","usgsCitation":"Shervais, J., Murchey, B.L., Kimbrough, D.L., Renne, P.R., and Hanan, B., 2005, Radioisotopic and biostratigraphic age relations in the Coast Range Ophiolite, northern California: Implications for the tectonic evolution of the Western Cordillera: GSA Bulletin, v. 117, no. 5-6, p. 633-653, https://doi.org/10.1130/B25443.1.","productDescription":"21 p.","startPage":"633","endPage":"653","costCenters":[],"links":[{"id":409741,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Coast Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.73012721058606,\n              40.36957762617669\n            ],\n            [\n              -123.95470669447536,\n              40.192835793178716\n            ],\n            [\n              -123.71751337101955,\n              39.91839653077014\n            ],\n            [\n              -123.32586858112697,\n              39.481255320560564\n            ],\n            [\n              -122.5536112489444,\n              39.591862843388554\n            ],\n            [\n              -122.49845001093107,\n              39.753202807470814\n            ],\n            [\n              -122.54809512514294,\n              39.83373143404421\n            ],\n            [\n              -122.53154675373919,\n              39.994505732745694\n            ],\n            [\n              -122.68048209637419,\n              40.20547553087849\n            ],\n            [\n              -122.73012721058606,\n              40.36957762617669\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"117","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shervais, John W.","contributorId":237914,"corporation":false,"usgs":false,"family":"Shervais","given":"John W.","affiliations":[{"id":6682,"text":"Utah State University","active":true,"usgs":false}],"preferred":false,"id":857761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murchey, Benita L. bmurchey@usgs.gov","contributorId":504,"corporation":false,"usgs":true,"family":"Murchey","given":"Benita","email":"bmurchey@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":857762,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kimbrough, David L.","contributorId":211569,"corporation":false,"usgs":false,"family":"Kimbrough","given":"David","email":"","middleInitial":"L.","affiliations":[{"id":6608,"text":"San Diego State University","active":true,"usgs":false}],"preferred":false,"id":857763,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Renne, Paul R. 0000-0003-1769-5235","orcid":"https://orcid.org/0000-0003-1769-5235","contributorId":229577,"corporation":false,"usgs":false,"family":"Renne","given":"Paul","email":"","middleInitial":"R.","affiliations":[{"id":37390,"text":"Department of Earth and Planetary Science, University of California, Berkeley","active":true,"usgs":false}],"preferred":false,"id":857764,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hanan, Barry","contributorId":299415,"corporation":false,"usgs":false,"family":"Hanan","given":"Barry","email":"","affiliations":[{"id":6608,"text":"San Diego State University","active":true,"usgs":false}],"preferred":false,"id":857765,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70238531,"text":"70238531 - 2005 - A review of the genus Eclipidrilus (Annelida: Clitellata: Lumbricul-idae), with description of a new species from western North America","interactions":[],"lastModifiedDate":"2022-11-28T18:03:53.717086","indexId":"70238531","displayToPublicDate":"2005-05-01T11:51:32","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3814,"text":"Zootaxa","onlineIssn":"1175-5334","printIssn":"1175-5326","active":true,"publicationSubtype":{"id":10}},"displayTitle":"A review of the genus <i>Eclipidrilus</i> (Annelida: Clitellata: Lumbricul-idae), with description of a new species from western North America","title":"A review of the genus Eclipidrilus (Annelida: Clitellata: Lumbricul-idae), with description of a new species from western North America","docAbstract":"<p><i>Eclipidrilus</i><span>&nbsp;</span><i>pacificus</i><span>&nbsp;n. sp., from northwestern USA, is distinguished from other&nbsp;</span><i>Eclipidrilus</i><span>&nbsp;by having a single atrium with midventral male pore, small penis, prostomium without a proboscis, and non-spiraling atrial musculature. Most populations also differ from congeners in having paired spermathecal pores anterior to the ventral chaetae, but specimens from the Columbia River have variable number and placement of the spermathecae. An unusual spiral orientation of the atrial musculature has previously been used to define&nbsp;</span><i>Eclipidrilus.</i><span>&nbsp;However, orientation of the atrial muscle layers varies among the previously described species, and does not provide a distinctive synapomorphy for the genus as a whole. Consequently, the genus is redefined to include species having elongate-petiolate atria with an inner, near-transverse muscle layer and an outer, longitudinal to spiral muscle layer.</span></p>","language":"English","publisher":"Magnolia Press","doi":"10.11646/zootaxa.969.1.1","usgsCitation":"Fend, S.V., 2005, A review of the genus Eclipidrilus (Annelida: Clitellata: Lumbricul-idae), with description of a new species from western North America: Zootaxa, v. 969, no. 1, p. 1-42, https://doi.org/10.11646/zootaxa.969.1.1.","productDescription":"42 p.","startPage":"1","endPage":"42","costCenters":[],"links":[{"id":409717,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Montana, Oregon, 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,{"id":70234166,"text":"70234166 - 2005 - Book review: The race to seismic safety: Protecting California's transportation system","interactions":[],"lastModifiedDate":"2022-08-02T14:30:57.828546","indexId":"70234166","displayToPublicDate":"2005-05-01T09:21:21","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Book review: The race to seismic safety: Protecting California's transportation system","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"SAGE Publishing","doi":"10.1193/8755-2930-21.2.613","usgsCitation":"Borcherdt, R.D., 2005, Book review: The race to seismic safety: Protecting California's transportation system: Earthquake Spectra, v. 21, no. 2, p. 613-615, https://doi.org/10.1193/8755-2930-21.2.613.","productDescription":"3 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 \"}}]}","volume":"21","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":848068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179759,"text":"70179759 - 2005 - Symbiotic lifestyle expression by fungal endophytes and the adaptation of plants to stress: unraveling the complexities of intimacy","interactions":[],"lastModifiedDate":"2017-01-17T12:30:29","indexId":"70179759","displayToPublicDate":"2005-05-01T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Symbiotic lifestyle expression by fungal endophytes and the adaptation of plants to stress: unraveling the complexities of intimacy","docAbstract":"<p><span>The fossil record indicates that fungal symbionts have been associated with plants since the Ordovician period (approximately 400 million years ago), when plants first became established on land (Pirozynski and Malloch, 1975; Redecker et al., 2000; Remy et al., 1994; Simon et al., 1993). Transitioning from aquatic to terrestrial habitats likely presented plants with new stresses, including periods of desiccation. Since symbiotic fungi are known to confer drought tolerance to plants (Bacon, 1993; Read and Camp, 1986), it has been suggested that fungal symbiosis was involved with or responsible for the establishment of land plants (Pirozynski and Malloch, 1975). Symbiosis was first defined by De Bary in 1879, and since that time, all plants in natural ecosystems have been found to be colonized with fungal and bacterial symbionts. It is clear that individual plants represent symbiotic communities with microorganisms associated in or on tissues below- and aboveground.</span><br><span>There are two major classes of fungal symbionts associated with internal plant tissues: fungal endophytes that reside entirely within plants and may be associated with roots, stems leaves, or flowers; and mycorrhizal fungi that reside only in roots but extend out into the rhizosphere. In addition, fungal endophytes may be divided into two classes: (1) a relatively small number of fastidious species that are limited to a few monocot hosts (Clay and Schardl, 2002), and (2) a large number of tractable species with broad host ranges, including both monocots and eudicots (Stone et al., 2000). While significant resources and research have been invested in mycorrhizae and class 1 endophytes, comparatively little is known about class 2 endophytes, which may represent the largest group of fungal symbionts. This is partially because the symbiotic functionalities of class 2 endophytes have only recently been elucidated and shown to be responsible for the adaptation of some plants to high-stress environments (Redman et al., 1999, 2001, 2002a; Arnold et al., 2003; Dingle and McGee, 2003; Ernst et al., 2003).</span><br><span>In this chapter, we focus on symbiotic interactions between class 2 endophytes and a variety of monocot and eudicot host species. Specifically, we will discuss the ability of endophytes to express more than one symbiotic lifestyle, fungal taxonomy vs. lifestyle expression, the adaptive nature of symbioses, mechanisms of symbiotically conferred stress tolerance, and the evolutionary implications of adaptive symbiosis. We will refer to class 2 endophytes as fungal endophytes throughout the text.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The fungal community its organization and role in the ecosystem","language":"English","publisher":"CRC","doi":"10.1201/9781420027891.ch34","usgsCitation":"Redman, R.S., Henson, J.M., and Rodriguez, R.J., 2005, Symbiotic lifestyle expression by fungal endophytes and the adaptation of plants to stress: unraveling the complexities of intimacy, chap. <i>of</i> The fungal community its organization and role in the ecosystem, p. 683-695, https://doi.org/10.1201/9781420027891.ch34.","productDescription":"13 p. ","startPage":"683","endPage":"695","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333250,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2009-12-15","publicationStatus":"PW","scienceBaseUri":"587f3dbae4b0d96de256456b","contributors":{"authors":[{"text":"Redman, Regina S. 0000-0001-5108-7570","orcid":"https://orcid.org/0000-0001-5108-7570","contributorId":75829,"corporation":false,"usgs":true,"family":"Redman","given":"Regina","email":"","middleInitial":"S.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":658573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henson, Joan M.","contributorId":168935,"corporation":false,"usgs":false,"family":"Henson","given":"Joan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":658574,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rodriguez, Russell J.","contributorId":75035,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Russell","email":"","middleInitial":"J.","affiliations":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"preferred":false,"id":658575,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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