{"pageNumber":"2422","pageRowStart":"60525","pageSize":"25","recordCount":184617,"records":[{"id":76747,"text":"ofr20041101 - 2006 - Overview: DVD-video disc set of seafloor transects during USGS research cruises in the Pacific Ocean","interactions":[],"lastModifiedDate":"2014-10-09T15:36:30","indexId":"ofr20041101","displayToPublicDate":"2006-05-26T00:00:00","publicationYear":"2006","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":"2004-1101","title":"Overview: DVD-video disc set of seafloor transects during USGS research cruises in the Pacific Ocean","docAbstract":"<p>Many USGS research programs involve the gathering of underwater seafloor video footage. This footage was captured on a variety of media, including Beta III and VHS tapes. Much of this media is now deteriorating, prompting the migration of this video footage onto DVD-Video discs. Advantages of using DVD-Video discs are: less storage space, ease of transport, wider distribution, and non-degradational viewing of the media.</p>\n<br>\n<p>The videos in this particular collection (328 of them) were made on the ocean floor under President Reagan's Exclusive Economic Zone proclamation of 1983. There are now five copies of these 328 discs in existence: at the USGS libraries in Menlo Park, Calif., Denver, Colo., and Reston, Va.; at the USGS Publications Warehouse (masters from which to make copies for customers); and Hank Chezar's USGS Western Coastal and Marine Geology team archives.</p>\n<br>\n<p>The purpose of Open-File Report 2004-1101 is to provide users with a listing of the available DVD-Video discs (with their Open-File Report numbers) along with a brief description of their associated USGS research activities. Each disc was created by first encoding the source video and audio into MPEG-2 streams using the MediaPress Pro hardware encoder. A menu for the disc was then made using Adobe Photoshop 6.0. The disc was then authored using DVD Studio Pro and subsequently written onto a DVD-R recordable disc.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041101","usgsCitation":"Chezar, H., and Newman, I., 2006, Overview: DVD-video disc set of seafloor transects during USGS research cruises in the Pacific Ocean: U.S. Geological Survey Open-File Report 2004-1101, HTML Document, https://doi.org/10.3133/ofr20041101.","productDescription":"HTML Document","costCenters":[{"id":645,"text":"Western Coastal and Marine Geology","active":false,"usgs":true}],"links":[{"id":192270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041101.PNG"},{"id":7849,"rank":200,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1101/","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Pacific Ocean","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbd08","contributors":{"authors":[{"text":"Chezar, Henry hchezar@usgs.gov","contributorId":2964,"corporation":false,"usgs":true,"family":"Chezar","given":"Henry","email":"hchezar@usgs.gov","affiliations":[],"preferred":true,"id":287794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newman, Ivy","contributorId":86053,"corporation":false,"usgs":true,"family":"Newman","given":"Ivy","email":"","affiliations":[],"preferred":false,"id":287795,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76743,"text":"sim2921 - 2006 - Geologic map of the Western Grove quadrangle, northwestern Arkansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"sim2921","displayToPublicDate":"2006-05-25T00:00:00","publicationYear":"2006","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":"2921","title":"Geologic map of the Western Grove quadrangle, northwestern Arkansas","docAbstract":"This map summarizes the geology of the Western Grove 7.5-minute quadrangle in northern Arkansas that is located on the southern flank of the Ozark dome, a late Paleozoic regional uplift. The exposed bedrock of this map area comprises approximately 1,000 ft of Ordovician and Mississippian carbonate and clastic sedimentary rocks that have been mildly folded and broken by faults. A segment of the Buffalo River loops through the southern part of the quadrangle, and the river and adjacent lands form part of Buffalo National River, a park administered by the U.S. National Park Service. This geologic map provides information to better understand the natural resources of the Buffalo River watershed, particularly its karst hydrogeologic framework.","language":"ENGLISH","doi":"10.3133/sim2921","usgsCitation":"Hudson, M., Turner, K.J., and Repetski, J.E., 2006, Geologic map of the Western Grove quadrangle, northwestern Arkansas (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2921, 1 map sheet, approx 44 x 34 in.; GIS data files, https://doi.org/10.3133/sim2921.","productDescription":"1 map sheet, approx 44 x 34 in.; GIS data files","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":110645,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76594.htm","linkFileType":{"id":5,"text":"html"},"description":"76594"},{"id":193196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7838,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/sim/2006/2921/downloads/","linkFileType":{"id":5,"text":"html"}},{"id":7839,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/sim/2006/2921/downloads/wgrove_meta.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7837,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2006/2921/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","projection":"UTM Zone 15, NAD 27","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93,36 ], [ -93,36.1175 ], [ -92.86749999999999,36.1175 ], [ -92.86749999999999,36 ], [ -93,36 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a011","contributors":{"authors":[{"text":"Hudson, Mark R. 0000-0003-0338-6079 mhudson@usgs.gov","orcid":"https://orcid.org/0000-0003-0338-6079","contributorId":1236,"corporation":false,"usgs":true,"family":"Hudson","given":"Mark R.","email":"mhudson@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":287783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turner, Kenzie J. 0000-0002-4940-3981 kturner@usgs.gov","orcid":"https://orcid.org/0000-0002-4940-3981","contributorId":496,"corporation":false,"usgs":true,"family":"Turner","given":"Kenzie","email":"kturner@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":287782,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Repetski, John E. 0000-0002-2298-7120 jrepetski@usgs.gov","orcid":"https://orcid.org/0000-0002-2298-7120","contributorId":2596,"corporation":false,"usgs":true,"family":"Repetski","given":"John","email":"jrepetski@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":287784,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76744,"text":"ofr20061119 - 2006 - Magnetotelluric survey to locate the Archean/Proterozoic suture zone north of Wells, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:14:06","indexId":"ofr20061119","displayToPublicDate":"2006-05-25T00:00:00","publicationYear":"2006","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":"2006-1119","title":"Magnetotelluric survey to locate the Archean/Proterozoic suture zone north of Wells, Nevada","docAbstract":"It is important to know whether major mining districts in the Northern Nevada Gold Province are underlain by rocks of the Archean Wyoming craton, which are known to contain orogenic gold deposits, or by accreted rocks of the Paleoproterozoic Mojave province. It is also important to know the location and orientation of the Archean/Proterozoic suture zone between these provinces as well as major basement structures within these terranes because they may influence subsequent patterns of sedimentation, deformation, magmatism, and hydrothermal activity. The Archean was the main gold-mineralization period, and Archean lode-gold deposits were formed at mid-crustal depths along major shear zones.\r\n\r\nThe nature of the crystalline basement below the Northern Nevada Gold Province and the location of major faults within it are relevant to Rodinian reconstructions, crustal development, and ore deposit models (e.g., Hofstra and Cline, 2000; Grauch and others, 2003). According to Whitmeyer and Karlstrom (2004), the Archean cratons of the northwestern United States and Canada had stabilized as continental lithosphere by 2.5 Ga, and were rifted and assembled into a large continental mass by 1.8 Ga, to which the 1.73-1.68 Ga Mohave province was accreted by 1.65 Ga. The Archean/Proterozoic suture zone has a west-southwest strike where it is exposed (Reed, 1993) at the eastern Utah and southwestern Wyoming border (Cheyenne Belt) where it is characterized by an up to 7-km-thick mylonite zone (Smithson and Boyd, 1998). In the Great Basin, the strike of the Archean/Proterozoic suture zone is poorly constrained because it is largely concealed below a Neoproterozoic-Paleozoic miogeocline and basin fill. East-west and southwest-northeast strikes for the Archean/Proterozoic suture zone have been inferred based on Sr, Nd, and Pb isotopic compositions of granitoid intrusions (Tosdal and others, 2000). To better constrain the location and strike of the Archean/Proterozoic suture zone below cover, three regional north-south magnetotelluric (MT) sounding profiles were acquired in western Utah and northeastern Nevada (Williams and Rodriguez, 2003; 2004; 2005), and one east-west MT sounding profile (fig. 1) MT sounding profile was acquired in northeastern Nevada. Resistivity modeling of the MT data can be used to investigate buried structures or sutures that may have influenced subsequent regional fluid flow and localized mineralization. The purpose of this report is to release the MT sounding data collected along the east-west profile in northeastern Nevada; no interpretation of the data is included.","language":"ENGLISH","doi":"10.3133/ofr20061119","usgsCitation":"Williams, J.M., and Rodriguez, B.D., 2006, Magnetotelluric survey to locate the Archean/Proterozoic suture zone north of Wells, Nevada (Revised and reprinted; Version 1.0): U.S. Geological Survey Open-File Report 2006-1119, iii, 93 p.; MT plot appendix [88 p.], https://doi.org/10.3133/ofr20061119.","productDescription":"iii, 93 p.; MT plot appendix [88 p.]","onlineOnly":"Y","costCenters":[],"links":[{"id":438861,"rank":101,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/F7GH9GW0","text":"USGS data release","linkHelpText":"Magnetotelluric sounding data, stations 26 to 36, north of Wells, Nevada, 2005"},{"id":192586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7840,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1119/","linkFileType":{"id":5,"text":"html"}}],"edition":"Revised and reprinted; Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494a2","contributors":{"authors":[{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":287786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":287785,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76740,"text":"ds180 - 2006 - Capitol Lake, Washington, 2004 data summary","interactions":[],"lastModifiedDate":"2014-10-23T15:48:40","indexId":"ds180","displayToPublicDate":"2006-05-23T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"180","title":"Capitol Lake, Washington, 2004 data summary","docAbstract":"At the request of the Washington Department of Ecology (WDOE), the US Geological Survey (USGS) collected bathymetry data in Capital Lake, Olympia, Wash., on September 21, 2004. The data are to be used to calculate sediment infilling rates within the lake as well as for developing the bottom boundary conditions for numerical models of water quality, sediment transport, and morphological change. In addition, the USGS collected sediment samples in Capitol Lake in February, 2005, to help characterize bottom sediment for numerical model calculations and substrate assessment.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds180","usgsCitation":"Eshleman, J., Ruggiero, P., Kingsley, E., Gelfenbaum, G., and George, D., 2006, Capitol Lake, Washington, 2004 data summary (Version 1.0): U.S. Geological Survey Data Series 180, Report: 31 p.; Metadata; 2 Data Packages, https://doi.org/10.3133/ds180.","productDescription":"Report: 31 p.; Metadata; 2 Data Packages","numberOfPages":"35","temporalStart":"2004-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":190619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds180.JPG"},{"id":7829,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/ds/2006/180/ds-180_metadata/","linkFileType":{"id":5,"text":"html"}},{"id":7830,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/ds/2006/180/ds-180_data_04.zip"},{"id":7831,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/ds/2006/180/ds-180_data_05.zip"},{"id":7828,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/180/","linkFileType":{"id":5,"text":"html"}},{"id":295699,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/2006/180/ds-180.pdf"}],"country":"United States","state":"Washington","otherGeospatial":"Capitol Lake","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5ffc","contributors":{"authors":[{"text":"Eshleman, Jodi","contributorId":41909,"corporation":false,"usgs":true,"family":"Eshleman","given":"Jodi","affiliations":[],"preferred":false,"id":287776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggiero, Peter","contributorId":15709,"corporation":false,"usgs":false,"family":"Ruggiero","given":"Peter","affiliations":[{"id":6680,"text":"Oregon State University","active":true,"usgs":false}],"preferred":false,"id":287773,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kingsley, Etienne","contributorId":25643,"corporation":false,"usgs":true,"family":"Kingsley","given":"Etienne","email":"","affiliations":[],"preferred":false,"id":287774,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gelfenbaum, Guy","contributorId":79844,"corporation":false,"usgs":true,"family":"Gelfenbaum","given":"Guy","affiliations":[],"preferred":false,"id":287777,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"George, Doug","contributorId":39068,"corporation":false,"usgs":true,"family":"George","given":"Doug","affiliations":[],"preferred":false,"id":287775,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":76739,"text":"ofr20061136 - 2006 - Aeromagnetic survey of Dillingham area in southwest Alaska, a website for the preliminary distribution of data","interactions":[],"lastModifiedDate":"2023-01-13T20:04:10.916516","indexId":"ofr20061136","displayToPublicDate":"2006-05-23T00:00:00","publicationYear":"2006","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":"2006-1136","title":"Aeromagnetic survey of Dillingham area in southwest Alaska, a website for the preliminary distribution of data","docAbstract":"An airborne high-resolution magnetic survey was completed over the Dillingham and Nushagak Bay and Naknek area in southwestern Alaska. The flying was undertaken by McPhar Geosurveys Ltd. on behalf of the United States Geological Survey (USGS). First tests and calibration flights were completed by August 26th, 2005 and data acquisition was initiated on September 1st, 2005. The final data acquisition flight was completed on October 22nd, 2005. A total of 8,630 line-miles of data were acquired during the survey.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061136","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2006, Aeromagnetic survey of Dillingham area in southwest Alaska, a website for the preliminary distribution of data (Version 1.0): U.S. Geological Survey Open-File Report 2006-1136, 1 Plate: 36.00 x 29.00 inches, https://doi.org/10.3133/ofr20061136.","productDescription":"1 Plate: 36.00 x 29.00 inches","costCenters":[],"links":[{"id":192163,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411911,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76593.htm","linkFileType":{"id":5,"text":"html"}},{"id":7826,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1136/","linkFileType":{"id":5,"text":"html"}},{"id":7827,"rank":3,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1136/data.html","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","projection":"UTM Zone 4N","country":"United States","state":"Alaska","otherGeospatial":"Dillingham area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -159.0903,\n              58.5583\n            ],\n            [\n              -159.0903,\n              60.0597\n            ],\n            [\n              -156,\n              60.0597\n            ],\n            [\n              -156,\n              58.5583\n            ],\n            [\n              -159.0903,\n              58.5583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ccd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76742,"text":"fs20063044 - 2006 - Freshwater diatomite deposits in the western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"fs20063044","displayToPublicDate":"2006-05-23T00:00:00","publicationYear":"2006","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":"2006-3044","title":"Freshwater diatomite deposits in the western United States","docAbstract":"Freshwater diatomite deposits in the Western United States are found in lake beds that formed millions of years ago. These diatom-rich sediments are among the Nation's largest commercial diatomite deposits. Each deposit contains billions of tiny diatom skeletons, which are widely used for filtration, absorption, and abrasives. New studies by the U.S. Geological Survey (USGS) are revealing how ancient lakes in the Western States produced such large numbers of diatoms. These findings can be used by both land-use managers and mining companies to better evaluate diatomite resources in the region.","language":"ENGLISH","doi":"10.3133/fs20063044","usgsCitation":"Wallace, A.R., Frank, D.G., and Founie, A., 2006, Freshwater diatomite deposits in the western United States (Version 1.0): U.S. Geological Survey Fact Sheet 2006-3044, 2 p., https://doi.org/10.3133/fs20063044.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":120722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3044.jpg"},{"id":7833,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3044/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8596","contributors":{"authors":[{"text":"Wallace, Alan R.","contributorId":6024,"corporation":false,"usgs":true,"family":"Wallace","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":287780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frank, David G. dfrank@usgs.gov","contributorId":3274,"corporation":false,"usgs":true,"family":"Frank","given":"David","email":"dfrank@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":287779,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Founie, Alan","contributorId":27575,"corporation":false,"usgs":true,"family":"Founie","given":"Alan","email":"","affiliations":[],"preferred":false,"id":287781,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76741,"text":"ofr20061110 - 2006 - Geophysical studies of the Crump Geyser known geothermal resource area, Oregon, in 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:14:07","indexId":"ofr20061110","displayToPublicDate":"2006-05-23T00:00:00","publicationYear":"2006","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":"2006-1110","title":"Geophysical studies of the Crump Geyser known geothermal resource area, Oregon, in 1975","docAbstract":"The U.S. Geological Survey (USGS) conducted geophysical studies in support of the resource appraisal of the Crump Geyser Known Geothermal Resource Area (KGRA). This area was designated as a KGRA by the USGS, and this designation became effective on December 24, 1970. The land classification standards for a KGRA were established by the Geothermal Steam Act of 1970 (Public Law 91-581). Federal lands so classified required competitive leasing for the development of geothermal resources. \r\n\r\nThe author presented an administrative report of USGS geophysical studies entitled 'Geophysical background of the Crump Geyser area, Oregon, KGRA' to a USGS resource committee on June 17, 1975. This report, which essentially was a description of geophysical data and a preliminary interpretation without discussion of resource appraisal, is in Appendix 1. Reduction of sheets or plates in the original administrative report to page-size figures, which are listed and appended to the back of the text in Appendix 1, did not seem to significantly degrade legibility. Bold print in the text indicates where minor changes were made. A colored page-size index and tectonic map, which also show regional geology not shown in figure 2, was substituted for original figure 1. Detailed descriptions for the geologic units referenced in the text and shown on figures 1 and 2 were separately defined by Walker and Repenning (1965) and presumably were discussed in other reports to the committee. Heavy dashed lines on figures 1 and 2 indicate the approximate KGRA boundary. \r\n\r\nOne of the principal results of the geophysical studies was to obtain a gravity map (Appendix 1, fig. 10; Plouff, and Conradi, 1975, pl. 9), which reflects the fault-bounded steepness of the west edge of sediments and locates the maximum thickness of valley sediments at about 10 kilometers south of Crump Geyser. Based on the indicated regional-gravity profile and density-contrast assumptions for the two-dimensional profile, the maximum sediment thickness was estimated at 820 meters. A three-dimensional gravity model would have yielded a greater thickness. Audiomagnotelluric measurements were not made as far south as the location of the gravity low, as determined in the field, due to a lack of communication at that time. A boat was borrowed to collect gravity measurements along the edge of Crump Lake, but the attempt was curtailed by harsh, snowy weather on May 21, 1975, which shortly followed days of hot temperature. \r\n\r\nMost of the geophysical data and illustrations in Appendix 1 have been published (Gregory and Martinez, 1975; Plouff, 1975; and Plouff and Conradi, 1975), and Donald Plouff (1986) discussed a gravity interpretation of Warner Valley at the Fall 1986 American Geophysical Union meeting in San Francisco. Further interpretation of possible subsurface geologic sources of geophysical anomalies was not discussed in Appendix 1. For example, how were apparent resistivity lows (Appendix 1, figs. 3-6) centered near Crump Geyser affected by a well and other manmade electrically conductive or magnetic objects? What is the geologic significance of the 15-milligal eastward decrease across Warner Valley? The explanation that the two-dimensional gravity model (Appendix 1, fig. 14) was based on an inverse iterative method suggested by Bott (1960) was not included. Inasmuch as there was no local subsurface rock density distribution information to further constrain the gravity model, the three-dimensional methodology suggested by Plouff (1976) was not attempted. \r\n\r\nInasmuch as the associated publication by Plouff (1975), which released the gravity data, is difficult to obtain and not in digital format, that report is reproduced in Appendix 2. Two figures of the publication are appended to the back of the text. A later formula for the theoretical value of gravity for the given latitudes at sea level (International Association of Geodesy, 1971) should be used to re-compute gravity anomalies. To merge t","language":"ENGLISH","doi":"10.3133/ofr20061110","collaboration":"Figs. 6,7 skipped in numbering","usgsCitation":"Plouff, D., 2006, Geophysical studies of the Crump Geyser known geothermal resource area, Oregon, in 1975 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1110, 49 p., https://doi.org/10.3133/ofr20061110.","productDescription":"49 p.","numberOfPages":"49","onlineOnly":"Y","temporalStart":"1975-01-01","temporalEnd":"1975-12-31","costCenters":[{"id":378,"text":"Menlo Park Geophysical Unit","active":false,"usgs":true}],"links":[{"id":192333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7832,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1110/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c377","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":287778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76738,"text":"ds188 - 2006 - Database for the geologic map of the Sauk River 30-minute by 60-minute quadrangle, Washington (I-2592)","interactions":[],"lastModifiedDate":"2012-02-02T00:13:56","indexId":"ds188","displayToPublicDate":"2006-05-22T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"188","title":"Database for the geologic map of the Sauk River 30-minute by 60-minute quadrangle, Washington (I-2592)","docAbstract":"This digital map database has been prepared by R.W. Tabor from the published Geologic map of the Sauk River 30- by 60 Minute Quadrangle, Washington. Together with the accompanying text files as PDF, it provides information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The authors mapped most of the bedrock geology at 1:100,000 scale, but compiled most Quaternary units at 1:24,000 scale. The Quaternary contacts and structural data have been much simplified for the 1:100,000-scale map and database. The spatial resolution (scale) of the database is 1:100,000 or smaller. \r\n\r\nThis database depicts the distribution of geologic materials and structures at a regional (1:100,000) scale. The report is intended to provide geologic information for the regional study of materials properties, earthquake shaking, landslide potential, mineral hazards, seismic velocity, and earthquake faults. In addition, the report contains information and interpretations about the regional geologic history and framework. However, the regional scale of this report does not provide sufficient detail for site development purposes.","language":"ENGLISH","doi":"10.3133/ds188","collaboration":"See map I-2592","usgsCitation":"Tabor, R.W., Booth, D.B., Vance, J., and Ford, A.B., 2006, Database for the geologic map of the Sauk River 30-minute by 60-minute quadrangle, Washington (I-2592) (Version 1.0): U.S. Geological Survey Data Series 188, Unpaginated database, https://doi.org/10.3133/ds188.","productDescription":"Unpaginated database","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":191073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7824,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/ds/2006/188/srmetadata.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7823,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/ds/2006/188/srcovers4.tar.gz"},{"id":7825,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/188/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672bae","contributors":{"authors":[{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":287768,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Booth, D. B.","contributorId":42223,"corporation":false,"usgs":false,"family":"Booth","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vance, J.A.","contributorId":51361,"corporation":false,"usgs":true,"family":"Vance","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":287771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ford, A. B.","contributorId":44924,"corporation":false,"usgs":false,"family":"Ford","given":"A.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287770,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76737,"text":"ofr20061146 - 2006 - Summary of available hydrogeologic data for the northeast portion of the alluvial aquifer at Louisville, Kentucky","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"ofr20061146","displayToPublicDate":"2006-05-19T00:00:00","publicationYear":"2006","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":"2006-1146","title":"Summary of available hydrogeologic data for the northeast portion of the alluvial aquifer at Louisville, Kentucky","docAbstract":"The hydrogeologic characteristics of the unconsolidated glacial outwash sand and gravel deposits that compose the northeast portion of the alluvial aquifer at Louisville, Kentucky, indicate a prolific water-bearing formation with approximately 7 billion gallons of ground-water storage and an estimated sustainable yield of over 280 million gallons per day. This abundance of ground water and the need to properly develop and manage this resource has prompted many past investigations (since 1956), which have produced reports, maps, and data files covering a variety of topics relative to the movement, availability, and use of ground water in this area. These data have been compiled into a single report to assist in future development and use of the ground-water resources.\r\n\r\nAvailable ground-water data for the alluvial aquifer at Louisville, Kentucky, from Beargrass Creek to Harrods Creek, were compiled from the U.S. Geological Survey National Water Information System and the Kentucky Groundwater Data Repository. Data contained in these databases include ground-water well-construction details and historical ground-water levels, drillers' logs, and water-quality information. Additional data and information were gathered from project files at the U.S. Geological Survey--Kentucky Water Science Center and files at the Louisville Water Company. Information contained in these files included data from area pumping tests describing aquifer characteristics and ground-water flow.\r\n\r\nData describing current conditions of the ground-water system in the northeast portion of the alluvial aquifer also are included. Ground-water levels from a network of observation wells show recent trends in the flow system, and information from the Kentucky Division of Water-Groundwater Branch lists current permitted ground-water withdrawals in the area.","language":"ENGLISH","doi":"10.3133/ofr20061146","usgsCitation":"Unthank, M.D., and Nelson, H.L., 2006, Summary of available hydrogeologic data for the northeast portion of the alluvial aquifer at Louisville, Kentucky: U.S. Geological Survey Open-File Report 2006-1146, 60 p., https://doi.org/10.3133/ofr20061146.","productDescription":"60 p.","numberOfPages":"60","onlineOnly":"Y","costCenters":[{"id":354,"text":"Kentucky Water Science Center","active":true,"usgs":true}],"links":[{"id":193150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7820,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1146/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69936b","contributors":{"authors":[{"text":"Unthank, Michael D. 0000-0003-2483-0431 munthank@usgs.gov","orcid":"https://orcid.org/0000-0003-2483-0431","contributorId":3902,"corporation":false,"usgs":true,"family":"Unthank","given":"Michael","email":"munthank@usgs.gov","middleInitial":"D.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Hugh L. hlnelson@usgs.gov","contributorId":4158,"corporation":false,"usgs":true,"family":"Nelson","given":"Hugh","email":"hlnelson@usgs.gov","middleInitial":"L.","affiliations":[{"id":354,"text":"Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287767,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76736,"text":"tm6A18 - 2006 - User's guide to the Variably Saturated Flow (VSF) process to MODFLOW","interactions":[],"lastModifiedDate":"2012-03-08T17:16:19","indexId":"tm6A18","displayToPublicDate":"2006-05-19T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"6-A18","title":"User's guide to the Variably Saturated Flow (VSF) process to MODFLOW","docAbstract":"A new process for simulating three-dimensional (3-D) variably saturated flow (VSF) using Richards' equation has been added to the 3-D modular finite-difference ground-water model MODFLOW. Five new packages are presented here as part of the VSF Process--the Richards' Equation Flow (REF1) Package, the Seepage Face (SPF1) Package, the Surface Ponding (PND1) Package, the Surface Evaporation (SEV1) Package, and the Root Zone Evapotranspiration (RZE1) Package. Additionally, a new Adaptive Time-Stepping (ATS1) Package is presented for use by both the Ground-Water Flow (GWF) Process and VSF. The VSF Process allows simulation of flow in unsaturated media above the ground-water zone and facilitates modeling of ground-water/surface-water interactions.\r\n\r\nModel performance is evaluated by comparison to an analytical solution for one-dimensional (1-D) constant-head infiltration (Dirichlet boundary condition), field experimental data for a 1-D constant-head infiltration, laboratory experimental data for two-dimensional (2-D) constant-flux infiltration (Neumann boundary condition), laboratory experimental data for 2-D transient drainage through a seepage face, and numerical model results (VS2DT) of a 2-D flow-path simulation using realistic surface boundary conditions. A hypothetical 3-D example case also is presented to demonstrate the new capability using periodic boundary conditions (for example, daily precipitation) and varied surface topography over a larger spatial scale (0.133 square kilometer). The new model capabilities retain the modular structure of the MODFLOW code and preserve MODFLOW's existing capabilities as well as compatibility with commercial pre-/post-processors. The overall success of the VSF Process in simulating mixed boundary conditions and variable soil types demonstrates its utility for future hydrologic investigations.\r\n\r\nThis report presents a new flow package implementing the governing equations for variably saturated ground-water flow, four new boundary condition packages unique to unsaturated flow, the Adaptive Time-Stepping Package for use with both the GWF Process and the new VSF Process, detailed descriptions of the input and output files for each package, and six simulation examples verifying model performance.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Book 6: Modeling techniques, Section A. Ground-water","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/tm6A18","usgsCitation":"Thoms, R.B., Johnson, R.L., and Healy, R.W., 2006, User's guide to the Variably Saturated Flow (VSF) process to MODFLOW: U.S. Geological Survey Techniques and Methods 6-A18, 58 p., https://doi.org/10.3133/tm6A18.","productDescription":"58 p.","numberOfPages":"58","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":192439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7819,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2006/tm6a18/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603dba","contributors":{"authors":[{"text":"Thoms, R. Brad","contributorId":64746,"corporation":false,"usgs":true,"family":"Thoms","given":"R.","email":"","middleInitial":"Brad","affiliations":[],"preferred":false,"id":287765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Richard L.","contributorId":32626,"corporation":false,"usgs":true,"family":"Johnson","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Healy, Richard W. 0000-0002-0224-1858 rwhealy@usgs.gov","orcid":"https://orcid.org/0000-0002-0224-1858","contributorId":658,"corporation":false,"usgs":true,"family":"Healy","given":"Richard","email":"rwhealy@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":287763,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76729,"text":"ds186 - 2006 - Database for the geologic map of the Snoqualmie Pass 30-minute by 60-minute quadrangle, Washington (I-2538)","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"ds186","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"186","title":"Database for the geologic map of the Snoqualmie Pass 30-minute by 60-minute quadrangle, Washington (I-2538)","docAbstract":"This digital map database has been prepared by R.W. Tabor from the published Geologic map of the Snoqualmie Pass 30' X 60' Quadrangle, Washington. Together with the accompanying text files as PDF, it provides information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The authors mapped most of the bedrock geology at 1:100,000 scale, but compiled Quaternary units at 1:24,000 scale. The Quaternary contacts and structural data have been much simplified for the 1:100,000-scale map and database. The spatial resolution (scale) of the database is 1:100,000 or smaller.\r\n\r\nThis database depicts the distribution of geologic materials and structures at a regional (1:100,000) scale. The report is intended to provide geologic information for the regional study of materials properties, earthquake shaking, landslide potential, mineral hazards, seismic velocity, and earthquake faults. In addition, the report contains information and interpretations about the regional geologic history and framework. However, the regional scale of this report does not provide sufficient detail for site development purposes. ","language":"ENGLISH","doi":"10.3133/ds186","collaboration":"Accompanies Miscellaneous Investigations Series Map I-2538","usgsCitation":"Tabor, R.W., Frizzell, V.A., Booth, D.B., and Waitt, R., 2006, Database for the geologic map of the Snoqualmie Pass 30-minute by 60-minute quadrangle, Washington (I-2538) (Version 1.0): U.S. Geological Survey Data Series 186, Database files, https://doi.org/10.3133/ds186.","productDescription":"Database files","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":195446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7802,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/i2538/","linkFileType":{"id":5,"text":"html"}},{"id":7803,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/ds/2006/186/snpcovers4.tar.gz"},{"id":7801,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/186/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673f03","contributors":{"authors":[{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":287736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frizzell, V. A. Jr.","contributorId":39376,"corporation":false,"usgs":true,"family":"Frizzell","given":"V.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Booth, D. B.","contributorId":42223,"corporation":false,"usgs":false,"family":"Booth","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287738,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Waitt, R. B.","contributorId":78766,"corporation":false,"usgs":true,"family":"Waitt","given":"R. B.","affiliations":[],"preferred":false,"id":287739,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76732,"text":"ds187 - 2006 - A database of lotic invertebrate traits for North America","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"ds187","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"187","title":"A database of lotic invertebrate traits for North America","docAbstract":"The assessment and study of stream communities may be enhanced if functional characteristics such as life-history, habitat preference, and reproductive strategy were more widely available for specific taxa. Species traits can be used to develop these functional indicators because many traits directly link functional roles of organisms with controlling environmental factors (for example, flow, substratum, temperature). In addition, some functional traits may not be constrained by taxonomy and are thus applicable at multiple spatial scales. Unfortunately, a comprehensive summary of traits for North American invertebrate taxa does not exist. Consequently, the U.S. Geological Survey's National Water-Quality Assessment Program in cooperation with Colorado State University compiled a database of traits for North American invertebrates. A total of 14,127 records for over 2,200 species, 1,165 genera, and 249 families have been entered into the database from 967 publications, texts and reports. Quality-assurance procedures indicated error rates of less than 3 percent in the data entry process. Species trait information was most complete for insect taxa. Traits describing resource acquisition and habitat preferences were most frequently reported, whereas those describing physiological tolerances and reproductive biology were the least frequently reported in the literature. The database is not exhaustive of the literature for North American invertebrates and is biased towards aquatic insects, but it represents a first attempt to compile traits in a web-accessible database. This report describes the database and discusses important decisions necessary for identifying ecologically relevant, environmentally sensitive, non-redundant, and statistically tractable traits for use in bioassessment programs.","language":"ENGLISH","doi":"10.3133/ds187","usgsCitation":"Vieira, N.M., Poff, N.L., Carlisle, D.M., Moulton, S.R., Koski, M.L., and Kondratieff, B.C., 2006, A database of lotic invertebrate traits for North America: U.S. Geological Survey Data Series 187, 19 p., https://doi.org/10.3133/ds187.","productDescription":"19 p.","numberOfPages":"19","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":195753,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7810,"rank":9999,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/ds/ds187/htodcs/InvertTraitsTable_v1.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7809,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/ds187/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af16f","contributors":{"authors":[{"text":"Vieira, Nicole M. K.","contributorId":104172,"corporation":false,"usgs":false,"family":"Vieira","given":"Nicole","email":"","middleInitial":"M. K.","affiliations":[{"id":17860,"text":"Colorado State University, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":287752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poff, N. LeRoy","contributorId":90843,"corporation":false,"usgs":true,"family":"Poff","given":"N.","email":"","middleInitial":"LeRoy","affiliations":[],"preferred":false,"id":287751,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlisle, Daren M. 0000-0002-7367-348X dcarlisle@usgs.gov","orcid":"https://orcid.org/0000-0002-7367-348X","contributorId":513,"corporation":false,"usgs":true,"family":"Carlisle","given":"Daren","email":"dcarlisle@usgs.gov","middleInitial":"M.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":287747,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Moulton, Stephen R. II","contributorId":10451,"corporation":false,"usgs":true,"family":"Moulton","given":"Stephen","suffix":"II","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":287748,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Koski, Marci L.","contributorId":76035,"corporation":false,"usgs":true,"family":"Koski","given":"Marci","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287750,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kondratieff, Boris C.","contributorId":24868,"corporation":false,"usgs":false,"family":"Kondratieff","given":"Boris","email":"","middleInitial":"C.","affiliations":[{"id":17860,"text":"Colorado State University, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":287749,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":76727,"text":"ofr20061135 - 2006 - Mineral facilities of Africa and the Middle East","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"ofr20061135","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2006-1135","title":"Mineral facilities of Africa and the Middle East","docAbstract":"This map displays over 1,500 mineral facilities in Africa and the Middle East. The mineral facilities include mines, plants, mills, or refineries of aluminum, cement, coal, copper, diamond, gold, iron and steel, nickel, platinum-group metals, salt, and silver, among others. The data used in this poster were compiled from multiple sources, including the 2004 USGS Minerals Yearbook (Africa and Middle East volume), Minerals Statistics and Information from the USGS Web site (http://minerals.usgs.gov/minerals/), and data collected by USGS minerals information country specialists. Data reflect the most recent published table of industry structure for each country. Other sources include statistical publications of individual countries, annual reports and press releases of operating companies, and trade journals. Due to the sensitivity of some energy commodity data, the quality of these data should be evaluated on a country-by-country basis. Additional information and explanation is available from the country specialists. See Table 1 for general information about each mineral facility site including country, location and facility name, facility type, latitude, longitude, mineral commodity, mining method, main operating company, status, capacity, and units.","language":"ENGLISH","doi":"10.3133/ofr20061135","usgsCitation":"Eros, J., and Candelario-Quintana, L., 2006, Mineral facilities of Africa and the Middle East (Version 1.0): U.S. Geological Survey Open-File Report 2006-1135, 1 map sheet, 61 x 46 in., https://doi.org/10.3133/ofr20061135.","productDescription":"1 map sheet, 61 x 46 in.","onlineOnly":"Y","costCenters":[],"links":[{"id":192779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7796,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2006/1135/table1.xls"},{"id":7797,"rank":9999,"type":{"id":14,"text":"Image"},"url":"https://pubs.usgs.gov/of/2006/1135/2006-1135.ai"},{"id":7798,"rank":9999,"type":{"id":14,"text":"Image"},"url":"https://pubs.usgs.gov/of/2006/1135/2006-1135.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":7795,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1135/","linkFileType":{"id":5,"text":"html"}}],"scale":"11000000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635a44","contributors":{"authors":[{"text":"Eros, J.M.","contributorId":55098,"corporation":false,"usgs":true,"family":"Eros","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":287729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Candelario-Quintana, Luissette","contributorId":39077,"corporation":false,"usgs":true,"family":"Candelario-Quintana","given":"Luissette","email":"","affiliations":[],"preferred":false,"id":287728,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76731,"text":"sir20065069 - 2006 - Effects of irrigation practices on water use in the groundwater management districts within the Kansas high plains, 1991-2003","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"sir20065069","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2006-5069","title":"Effects of irrigation practices on water use in the groundwater management districts within the Kansas high plains, 1991-2003","docAbstract":"Data compiled for the High Plains region of Kansas that includes five Groundwater Management Districts (GMDs) were analyzed for trends in irrigation water use, acres irrigated, precipitation, irrigation system types, and irrigated crop types to determine the effects of irrigation practices on water use over time. For the study period 1991 through 2003, precipitation decreased significantly (with 95-percent confidence) in northwestern and west-central Kansas but not in the southwestern and south-central parts of the State. Irrigation water use had no statistically significant trend during this period. There was a good (R= -0.77) relation between average regional precipitation and total GMD irrigation water use. When irrigation water use was adjusted for this relation, there was a positive trend (90-percent confidence level) in the adjusted irrigation water use. Another adjustment to water use was made using the ratio of annual precipitation to 1991-2005 average precipitation, which resulted in a negative trend (95-percent confidence level) in irrigation water use. This demonstrated the contradictory nature of precipitation adjustments to water use, making their utility somewhat suspect. GMD 3 in southwestern Kansas used 63 percent of the total acre-feet of irrigation water within all the GMDs.\r\n\r\nWhen all GMDs are considered, the number of irrigated acres for flood and center pivot systems without drop nozzles decreased significantly during the study period. At the same time the number of drop nozzle irrigated acres increased significantly. The number of irrigated acres of water-intensive crops (corn, alfalfa, and soybeans) also increased significantly, whereas the number of less- or non-water-intensive crops (grain sorghum and wheat), and multiple crop type acres decreased. Drop nozzle irrigation systems used approximately 2 percent less water in a year-by-year comparison than center pivot systems and 8 to 11 percent less water than flood irrigation.\r\n\r\nThe best estimator of irrigation water use incorporated total acres irrigated and annual average or March-October regional precipitation. A conclusion that can be drawn from the trend analyses described in this report is that, although irrigation water use for all GMDs showed no statistically significant trend, an apparent increased efficiency of center pivots irrigation systems with drop nozzles has allowed more water-intensive crops to be grown on more irrigated acres.","language":"ENGLISH","doi":"10.3133/sir20065069","usgsCitation":"Perry, C.A., 2006, Effects of irrigation practices on water use in the groundwater management districts within the Kansas high plains, 1991-2003: U.S. Geological Survey Scientific Investigations Report 2006-5069, 93 p., https://doi.org/10.3133/sir20065069.","productDescription":"93 p.","numberOfPages":"93","temporalStart":"1991-01-01","temporalEnd":"2003-12-31","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":195726,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7808,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5069/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e24","contributors":{"authors":[{"text":"Perry, Charles A. cperry@usgs.gov","contributorId":2093,"corporation":false,"usgs":true,"family":"Perry","given":"Charles","email":"cperry@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":287746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76733,"text":"fs20063049 - 2006 - Undiscovered oil and gas resources underlying the U.S. portions of the Great Lakes, 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:14:13","indexId":"fs20063049","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2006-3049","title":"Undiscovered oil and gas resources underlying the U.S. portions of the Great Lakes, 2005","docAbstract":"The U.S. Geological Survey (USGS) completed an assessment of the undiscovered oil and gas potential of the U.S. portions of the Appalachian Basin and the Michigan Basin in 2002 and 2004, respectively. Following the assessments of these two basins, oil and gas allocations were assigned to the U.S. portions of the Great Lakes - Lake Superior (Michigan, Minnesota, and Wisconsin), Lake Michigan (Illinois, Indiana, Michigan, and Wisconsin), Lake Huron (Michigan), Lake Erie (Michigan, New York, Ohio, and Pennsylvania), and Lake Ontario (New York). Allocations for Lake St. Clair (Michigan) were included with those of Lake Erie.\r\n\r\nThe allocations are based on the geologic elements of each total petroleum system defined in the region and the projected extent of those elements from onshore beneath each of the lakes. These geologic elements include the hydrocarbon source rocks, reservoir rocks, and traps. By using this geologic framework, the USGS defined 8 total petroleum systems and 21 assessment units within the Great Lakes and estimated the quantity of undiscovered technically recoverable oil and gas resources within 16 of the 21 assessment units in the Great Lakes.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Assessment of Oil and Gas Fact Sheets","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/fs20063049","usgsCitation":"Coleman, J.L., Swezey, C., Ryder, R., and Charpentier, R., 2006, Undiscovered oil and gas resources underlying the U.S. portions of the Great Lakes, 2005: U.S. Geological Survey Fact Sheet 2006-3049, 2 p., https://doi.org/10.3133/fs20063049.","productDescription":"2 p.","numberOfPages":"2","additionalOnlineFiles":"Y","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":407,"text":"National Assessment of Oil and Gas Project","active":false,"usgs":true}],"links":[{"id":120848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3049.jpg"},{"id":7814,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/fs/2006/3049/table1.xls"},{"id":7813,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2006/3049/fs2006-3049.doc"},{"id":7812,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3049/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f607","contributors":{"authors":[{"text":"Coleman, James L. Jr. 0000-0002-5232-5849 jlcoleman@usgs.gov","orcid":"https://orcid.org/0000-0002-5232-5849","contributorId":549,"corporation":false,"usgs":true,"family":"Coleman","given":"James","suffix":"Jr.","email":"jlcoleman@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":287753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swezey, Christopher S.","contributorId":52640,"corporation":false,"usgs":true,"family":"Swezey","given":"Christopher S.","affiliations":[],"preferred":false,"id":287755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ryder, Robert T.","contributorId":77918,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert T.","affiliations":[],"preferred":false,"id":287756,"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":287754,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":76726,"text":"ofr20051025 - 2006 - Geologic map of the Colonial Beach South 7.5-minute quadrangle, Virginia","interactions":[],"lastModifiedDate":"2012-02-10T00:11:38","indexId":"ofr20051025","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2005-1025","title":"Geologic map of the Colonial Beach South 7.5-minute quadrangle, Virginia","docAbstract":"The Open-File Report includes a geologic map with cross section, and composite stratigraphic section of the Tertiary stratigraphy and of the Quaternary stratigraphy. The Tertiary map units are presented and interpreted for erodability and derived surficial deposits.\r\n\r\nThe map area contains the George Washington Birthplace National Monument. The map facilitates the interpretation of the natural history of the Park including processes such as bog (wetlands) formation and coastal erosion. Two cores of Holocene estuarine deposits are sited on the map. They present the transition from terrestrial to estuarine depositional environments.","language":"ENGLISH","doi":"10.3133/ofr20051025","usgsCitation":"Newell, W., Bricker, O.P., and Robertson, M.S., 2006, Geologic map of the Colonial Beach South 7.5-minute quadrangle, Virginia (Version 1.0): U.S. Geological Survey Open-File Report 2005-1025, 1 map sheet, 53 x 34 in., https://doi.org/10.3133/ofr20051025.","productDescription":"1 map sheet, 53 x 34 in.","onlineOnly":"Y","costCenters":[],"links":[{"id":110644,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76572.htm","linkFileType":{"id":5,"text":"html"},"description":"76572"},{"id":192405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7794,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1025/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -38.25,77 ], [ -38.25,77.86749999999999 ], [ -37.134166666666665,77.86749999999999 ], [ -37.134166666666665,77 ], [ -38.25,77 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b97d","contributors":{"authors":[{"text":"Newell, Wayne L.","contributorId":48538,"corporation":false,"usgs":true,"family":"Newell","given":"Wayne L.","affiliations":[],"preferred":false,"id":287726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bricker, Owen P.","contributorId":25142,"corporation":false,"usgs":true,"family":"Bricker","given":"Owen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":287725,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Robertson, Meredith S.","contributorId":106586,"corporation":false,"usgs":true,"family":"Robertson","given":"Meredith","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":287727,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76728,"text":"ds173 - 2006 - Idaho and Montana non-fuel exploration database 1980-1997","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"ds173","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"173","title":"Idaho and Montana non-fuel exploration database 1980-1997","docAbstract":"This report describes a relational database containing information about mineral exploration projects in the States of Idaho and Montana for the years 1980 through 1997 and a spatial (geographic) database constructed using data from the relational database. The focus of this project was to collect information on exploration for mineral commodities with the exception of sand, gravel, coal, geothermal, oil, and gas. The associate databases supplied with this report are prototypes that can be used or modified as needed. The following sources were used to create the databases-serial mining periodicals; annual mineral publications; mining company reports; U.S. Bureau of Mines (USBM) and U.S. Geological Survey (USGS) publications; an Idaho mineral property data base developed by Dave Boleneus, USGS, Spokane, Washington; Montana state publications; and discussions with representatives of Montana, principally the Montana Bureau of Mines and Geology and the Department of Environmental Quality.\r\n\r\nFifty commodity groups were reported between the 596 exploration projects identified in this study. Precious metals (gold, silver, or platinum group elements) were the primary targets for about 67 percent of the exploration projects. Information on 17 of the projects did not include commodities. No location could be determined for 51 projects, all in Idaho. During the time period evaluated, some mineral properties were developed into large mining operations (for example Beal Mountain Mine, Stillwater Mine, Troy Mine, Montana Tunnels Mine) and six properties were reclaimed. Environmental Impact Statements were done on four properties. Some operating mines either closed or went through one or more shutdowns and re-openings. Other properties, where significant resources were delineated by recent exploration during this time frame, await the outcome of important factors for development such as defining additional reserves, higher metal prices, and the permitting process. Many of these projects examined relatively minor mineral occurrences.\r\n\r\nApproximately half of the exploration projects are located on Federal lands and about 40 percent were on lands managed by the U.S. Forest Service. More than 75 percent of the exploration occurred in areas with significant previous mineral activity. ","language":"ENGLISH","doi":"10.3133/ds173","usgsCitation":"Buckingham, D.A., DiFrancesco, C.A., Porter, K.E., Bleiwas, D.I., Causey, J.D., and Ferguson, W.B., 2006, Idaho and Montana non-fuel exploration database 1980-1997: U.S. Geological Survey Data Series 173, 80 p., https://doi.org/10.3133/ds173.","productDescription":"80 p.","numberOfPages":"80","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1980-01-01","temporalEnd":"1997-12-31","costCenters":[{"id":659,"text":"Western Mineral Resources Program","active":false,"usgs":true}],"links":[{"id":195420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7800,"rank":9999,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/ds/2006/173/ds-173_data.zip"},{"id":7799,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/173/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c730","contributors":{"authors":[{"text":"Buckingham, David A.","contributorId":57947,"corporation":false,"usgs":true,"family":"Buckingham","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DiFrancesco, Carl A.","contributorId":105400,"corporation":false,"usgs":true,"family":"DiFrancesco","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287735,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porter, Kenneth E.","contributorId":12558,"corporation":false,"usgs":true,"family":"Porter","given":"Kenneth","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":287732,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bleiwas, Donald I. bleiwas@usgs.gov","contributorId":1434,"corporation":false,"usgs":true,"family":"Bleiwas","given":"Donald","email":"bleiwas@usgs.gov","middleInitial":"I.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":287730,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Causey, J. Douglas","contributorId":41398,"corporation":false,"usgs":true,"family":"Causey","given":"J.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":287733,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Ferguson, William B. wbfergus@usgs.gov","contributorId":3146,"corporation":false,"usgs":true,"family":"Ferguson","given":"William","email":"wbfergus@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":287731,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":76730,"text":"sir20065026 - 2006 - Geology, ground-water hydrology, geochemistry, and ground-water simulation of the Beaumont and Banning Storage Units, San Gorgonio Pass area, Riverside County, California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"sir20065026","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2006-5026","title":"Geology, ground-water hydrology, geochemistry, and ground-water simulation of the Beaumont and Banning Storage Units, San Gorgonio Pass area, Riverside County, California","docAbstract":"Ground water has been the only source of potable water supply for residential, industrial, and agricultural users in the Beaumont and Banning storage units of the San Gorgonio Pass area, Riverside County, California. Ground-water levels in the Beaumont area have declined as much as 100 feet between the early 1920s and early 2000s, and numerous natural springs have stopped flowing. In 1961, the San Gorgonio Pass Water Agency (SGPWA) entered into a contract with the California State Department of Water Resources to receive 17,300 acre-feet per year of water to be delivered by the California State Water Project (SWP) to supplement natural recharge. Currently (2005), a pipeline is delivering SWP water into the area, and the SGPWA is artificially recharging the ground-water system using recharge ponds located along Little San Gorgonio Creek in Cherry Valley with the SWP water. In addition to artificial recharge, SGPWA is considering the direct delivery of SWP water for the irrigation of local golf courses and for agricultural supply in lieu of ground-water pumpage. To better understand the potential hydrologic effects of different water-management alternatives on ground-water levels and movement in the Beaumont and Banning storage units, existing geohydrologic and geochemical data were compiled, new data from a basin-wide ground-water level and water-quality monitoring network were collected, monitoring wells were installed near the Little San Gorgonio Creek recharge ponds, geohydrologic and geochemical analyses were completed, and a ground-water flow simulation model was developed.\r\n\r\nThe San Gorgonio Pass area was divided into several storage units on the basis of mapped or inferred faults. This study addresses primarily the Beaumont and Banning storage units. The geologic units in the study area were generalized into crystalline basement rocks and sedimentary deposits. The younger sedimentary deposits and the surficial deposits are the main water-bearing deposits in the San Gorgonio Pass area. The water-bearing deposits were divided into three aquifers: (1) the perched aquifer, (2) the upper aquifer, and (3) the lower aquifer based on lithologic and downhole geophysical logs.\r\n\r\nNatural recharge in the San Gorgonio Pass area was estimated using INFILv3, a deterministic distributed- parameter precipitation-runoff model. The INFILv3 model simulated that the potential recharge of precipitation and runoff in the Beaumont and Banning storage units was about 3,710 acre-feet per year and that the potential recharge in 28 sub-drainage basins upstream of the storage units was about 6,180 acre-feet per year.\r\n\r\nThe water supply for the Beaumont and Banning storage units is supplied by pumping ground water from wells in the Canyon (Edgar and Banning Canyons), Banning Bench, Beaumont, and Banning storage units. Total annual pumpage from the Beaumont and Banning storage units ranged from about 1,630 acre-feet in 1936 to about 20,000 acre-feet in 2003. Ground-water levels declined by as much as 100 feet in the Beaumont storage unit from 1926-2003 in response to ground-water pumping of about 450,160 acre-feet during this period.\r\n\r\nSince ground-water development began in the San Gorgonio Pass area, there have been several sources of artificial recharge to the basin including return flow from applied water on crops, golf courses, and landscape; septic-tank seepage; and infiltration of storm runoff diversions and imported water into recharge ponds. Return flow from applied water and septic-tank seepage was estimated to reach a maximum of about 8,100 acre-feet per year in 2003. Owing to the great depth of water in much of study area (in excess of 150 feet), the return flow and septic-tank seepage takes years to decades to reach the water table.\r\n\r\nStable-isotope data indicate that the source of ground-water recharge was precipitation from storms passing through the San Gorgonio Pass as opposed to runoff from the higher altitudes of the San Bernar","language":"ENGLISH","doi":"10.3133/sir20065026","usgsCitation":"Rewis, D.L., Christensen, A.H., Matti, J., Hevesi, J.A., Nishikawa, T., and Martin, P., 2006, Geology, ground-water hydrology, geochemistry, and ground-water simulation of the Beaumont and Banning Storage Units, San Gorgonio Pass area, Riverside County, California: U.S. Geological Survey Scientific Investigations Report 2006-5026, 191 p., https://doi.org/10.3133/sir20065026.","productDescription":"191 p.","numberOfPages":"191","onlineOnly":"Y","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":195725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7807,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5026/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c652","contributors":{"authors":[{"text":"Rewis, Diane L. dlrewis@usgs.gov","contributorId":1511,"corporation":false,"usgs":true,"family":"Rewis","given":"Diane","email":"dlrewis@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christensen, Allen H. 0000-0002-7061-5591 ahchrist@usgs.gov","orcid":"https://orcid.org/0000-0002-7061-5591","contributorId":1510,"corporation":false,"usgs":true,"family":"Christensen","given":"Allen","email":"ahchrist@usgs.gov","middleInitial":"H.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287742,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Matti, Jonathan","contributorId":32225,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","affiliations":[],"preferred":false,"id":287745,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hevesi, Joseph A. 0000-0003-2898-1800 jhevesi@usgs.gov","orcid":"https://orcid.org/0000-0003-2898-1800","contributorId":1507,"corporation":false,"usgs":true,"family":"Hevesi","given":"Joseph","email":"jhevesi@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287741,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nishikawa, Tracy 0000-0002-7348-3838 tnish@usgs.gov","orcid":"https://orcid.org/0000-0002-7348-3838","contributorId":1515,"corporation":false,"usgs":true,"family":"Nishikawa","given":"Tracy","email":"tnish@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287744,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Martin, Peter pmmartin@usgs.gov","contributorId":799,"corporation":false,"usgs":true,"family":"Martin","given":"Peter","email":"pmmartin@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287740,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":76735,"text":"ofr20051452 - 2006 - Approach to an assessment of volatile organic compounds in the nation's ground water and drinking-water supply wells","interactions":[],"lastModifiedDate":"2012-02-02T00:14:11","indexId":"ofr20051452","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2005-1452","title":"Approach to an assessment of volatile organic compounds in the nation's ground water and drinking-water supply wells","docAbstract":"The National Water-Quality Assessment (NAWQA) Program of the U.S. Geological Survey (USGS) developed an approach for a national assessment of the occurrence, status, and distribution of volatile organic compounds (VOCs) in samples of ground water from aquifer studies and in samples from drinking-water supply wells, specifically domestic and public wells. Data on VOCs in samples from aquifers and from domestic and public wells had three sources: (1) NAWQA sampling of ground water in aquifer studies and of shallow ground water in areas of agricultural or urban land use from 1993-2002, (2) retrospective data from other Federal, State, and local agencies that sampled ground water in aquifer studies from 1985-1997, and (3) sampling of ground water from public wells used as a source of drinking water from 1999-2000 (source-water survey).\r\n\r\nData for assessing VOCs in ground water came from the NAWQA sampling of aquifers and from retrospective data (1 and 2). Domestic wells were the most commonly sampled well type in these aquifer studies. Data for assessing VOCs in domestic well samples came from the NAWQA sampling of aquifers and shallow ground water and from retrospective data (1 and 2). Data for assessing VOCs in public well samples came from NAWQA sampling of aquifers and shallow ground water and from the source-water survey (1, 2, and 3).\r\n\r\nFifty-five VOCs were included in the national assessment. All ground-water samples were collected using consistent, prescribed field protocols and were analyzed using approved analytical methods. All ground-water collection activities and laboratory procedures included the collection of various quality-control samples in order to ensure the quality of the data.\r\n\r\nComparisons of detection frequencies and detected concentrations among individual VOCs, groups of VOCs, aquifer studies, and data sets were performed using two assessment levels: (1) an assessment level of 0.2 microgram per liter (?g/L), and (2) an assessment level of 0.02 ?g/L. Selection of the 0.2-?g/L assessment level was based on historical laboratory reporting levels of VOCs used by the USGS National Water-Quality Laboratory (NWQL) prior to April 1996, and selection of the 0.02-?g/L assessment level was based on a new, low-level analytical method developed by the NWQL and used since April 1996.\r\n\r\nRelational analyses using multivariate logistic regression were performed on VOC data from aquifers, domestic wells, and public wells to better understand the natural and anthropogenic factors that control or influence the occurrence of VOCs. Ancillary data used in the relational analyses represent a variety of anthropogenic and hydrogeologic controls on the occurrence of VOCs. For aquifers, relational analyses were performed only on NAWQA data analyzed using the new low-level analytical method for 10 frequently detected VOCs. For domestic wells, relational analyses were performed at assessment levels of 0.2 ?g/L and 0.02 ?g/L for 6 and 10 frequently detected VOCs at these levels. For public wells, relational analyses were performed at an assessment level of 0.2 ?g/L for nine frequently detected VOCs.","language":"ENGLISH","doi":"10.3133/ofr20051452","usgsCitation":"Moran, M.J., Zogorski, J.S., and Rowe, B.L., 2006, Approach to an assessment of volatile organic compounds in the nation's ground water and drinking-water supply wells: U.S. Geological Survey Open-File Report 2005-1452, viii, 36 p., https://doi.org/10.3133/ofr20051452.","productDescription":"viii, 36 p.","numberOfPages":"44","costCenters":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"links":[{"id":7818,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1452/","linkFileType":{"id":5,"text":"html"}},{"id":192433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667de9","contributors":{"authors":[{"text":"Moran, Michael J. mjmoran@usgs.gov","contributorId":1047,"corporation":false,"usgs":true,"family":"Moran","given":"Michael","email":"mjmoran@usgs.gov","middleInitial":"J.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":287760,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, Barbara L. blrowe@usgs.gov","contributorId":2673,"corporation":false,"usgs":true,"family":"Rowe","given":"Barbara","email":"blrowe@usgs.gov","middleInitial":"L.","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287762,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76734,"text":"fs20063047 - 2006 - Data collection for the assessment of aquatic communities in northeastern Wyoming and southeastern Montana, 2005","interactions":[],"lastModifiedDate":"2012-03-08T17:16:19","indexId":"fs20063047","displayToPublicDate":"2006-05-18T00:00:00","publicationYear":"2006","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":"2006-3047","title":"Data collection for the assessment of aquatic communities in northeastern Wyoming and southeastern Montana, 2005","language":"ENGLISH","doi":"10.3133/fs20063047","usgsCitation":"Wright, P., Peterson, D.A., and Hallberg, L.L., 2006, Data collection for the assessment of aquatic communities in northeastern Wyoming and southeastern Montana, 2005: U.S. Geological Survey Fact Sheet 2006-3047, 6 p., https://doi.org/10.3133/fs20063047.","productDescription":"6 p.","numberOfPages":"6","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":684,"text":"Wyoming Water Science Center","active":false,"usgs":true}],"links":[{"id":121334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3047.jpg"},{"id":7817,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3047/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c984","contributors":{"authors":[{"text":"Wright, Peter R. prwright@usgs.gov","contributorId":1828,"corporation":false,"usgs":true,"family":"Wright","given":"Peter R.","email":"prwright@usgs.gov","affiliations":[],"preferred":true,"id":287759,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, David A. davep@usgs.gov","contributorId":1742,"corporation":false,"usgs":true,"family":"Peterson","given":"David","email":"davep@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":287757,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hallberg, Laura L. 0000-0001-9983-8003 lhallber@usgs.gov","orcid":"https://orcid.org/0000-0001-9983-8003","contributorId":1825,"corporation":false,"usgs":true,"family":"Hallberg","given":"Laura","email":"lhallber@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287758,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76724,"text":"ofr20061104 - 2006 - A guide for using the transient ground-water flow model of the Death Valley regional ground-water flow system, Nevada and California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061104","displayToPublicDate":"2006-05-16T00:00:00","publicationYear":"2006","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":"2006-1104","title":"A guide for using the transient ground-water flow model of the Death Valley regional ground-water flow system, Nevada and California","docAbstract":"This report is a guide for executing numerical simulations with the transient ground-water flow model of the Death Valley regional ground-water flow system, Nevada and California using the U.S. Geological Survey modular finite-difference ground-water flow model, MODFLOW-2000. Model inputs, including observations of hydraulic head, discharge, and boundary flows, are summarized. Modification of the DVRFS transient ground-water model is discussed for two common uses of the Death Valley regional ground-water flow system model: predictive pumping scenarios that extend beyond the end of the model simulation period (1998), and model simulations with only steady-state conditions.","language":"ENGLISH","doi":"10.3133/ofr20061104","usgsCitation":"Blainey, J.B., Faunt, C., and Hill, M.C., 2006, A guide for using the transient ground-water flow model of the Death Valley regional ground-water flow system, Nevada and California: U.S. Geological Survey Open-File Report 2006-1104, 36 p., https://doi.org/10.3133/ofr20061104.","productDescription":"36 p.","numberOfPages":"36","costCenters":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"links":[{"id":194504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7790,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1104/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae576","contributors":{"authors":[{"text":"Blainey, Joan B.","contributorId":54284,"corporation":false,"usgs":true,"family":"Blainey","given":"Joan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":287721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faunt, Claudia C. 0000-0001-5659-7529 ccfaunt@usgs.gov","orcid":"https://orcid.org/0000-0001-5659-7529","contributorId":1491,"corporation":false,"usgs":true,"family":"Faunt","given":"Claudia C.","email":"ccfaunt@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":287720,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, Mary C. mchill@usgs.gov","contributorId":974,"corporation":false,"usgs":true,"family":"Hill","given":"Mary","email":"mchill@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":287719,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76723,"text":"ofr20061105 - 2006 - Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"ofr20061105","displayToPublicDate":"2006-05-16T00:00:00","publicationYear":"2006","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":"2006-1105","title":"Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2004","docAbstract":"Urbanization has dramatically increased precipitation runoff to the system of drainage channels and natural stream channels in the Albuquerque, New Mexico, metropolitan area. Rainfall and runoff data are important for planning and designing future storm-water conveyance channels in newly developing areas. Storm-water quality also is monitored in accordance with the National Pollutant Discharge Elimination System mandated by the U.S. Environmental Protection Agency. The Albuquerque Metropolitan Arroyo Flood Control Authority, the City of Albuquerque, and the U.S. Geological Survey began a cooperative program to collect hydrologic data to assist in assessing the quality and quantity of surface-water resources in the Albuquerque area. This report presents water-quality, streamflow, and rainfall data collected from October 1, 2003, to September 30, 2004 (water year 2004). Also provided is a station analysis for each of the 18 streamflow-gaging sites and 39 rainfall-gaging sites, which includes a description of monitoring equipment, problems associated with data collection during the year, and other information used to compute streamflow discharges or rainfall records. A hydrographic comparison shows the effects that the largest drainage channel in the metropolitan area, the North Floodway Channel, has on total flow in the Rio Grande.","language":"ENGLISH","doi":"10.3133/ofr20061105","usgsCitation":"Kelly, T., Romero, O., and Jimenez, M., 2006, Rainfall, runoff, and water-quality data for the urban storm-water program in the Albuquerque, New Mexico, metropolitan area, water year 2004: U.S. Geological Survey Open-File Report 2006-1105, 127 p., https://doi.org/10.3133/ofr20061105.","productDescription":"127 p.","numberOfPages":"127","temporalStart":"2003-10-01","temporalEnd":"2004-09-30","costCenters":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"links":[{"id":195724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7789,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1105/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64970c","contributors":{"authors":[{"text":"Kelly, Todd","contributorId":89168,"corporation":false,"usgs":true,"family":"Kelly","given":"Todd","email":"","affiliations":[],"preferred":false,"id":287717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Romero, Orlando","contributorId":92335,"corporation":false,"usgs":true,"family":"Romero","given":"Orlando","affiliations":[],"preferred":false,"id":287718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jimenez, Mike","contributorId":33785,"corporation":false,"usgs":true,"family":"Jimenez","given":"Mike","email":"","affiliations":[],"preferred":false,"id":287716,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76725,"text":"sir20055261 - 2006 - Assessment of hydrologic and water quality data collected in Abbotts Lagoon watershed, Point Reyes National Seashore, California, during water years 1999 and 2000","interactions":[],"lastModifiedDate":"2023-01-13T20:22:07.784196","indexId":"sir20055261","displayToPublicDate":"2006-05-16T00:00:00","publicationYear":"2006","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":"2005-5261","title":"Assessment of hydrologic and water quality data collected in Abbotts Lagoon watershed, Point Reyes National Seashore, California, during water years 1999 and 2000","docAbstract":"Abbotts Lagoon is part of Point Reyes National Seashore, located about 40 miles northwest of San Francisco and about 20 miles south of Bodega Bay. Water-quality samples were collected quarterly during water year 1999 at a site in each of three connected lagoons that make up Abbotts Lagoon and at a site in its most significant tributary. The quarterly samples were analyzed for major ions, nutrients, and chlorophyll-a. A bed-sediment sample was collected in each lagoon during August 1999 and was analyzed for organic carbon, iron, and total phosphorus. Seven tributaries were sampled during a February 1999 storm and four during an April 1999 storm. These samples were analyzed only for nutrients. One storm sample collected in April 1999 from a tributary downstream of the I Ranch dairy was analyzed for a suite of 47 compounds indicative of wastewater. Continuous water-level recorders were installed in the most significant tributary and the two largest lagoons for portions of the study.\r\nA water budget analysis for an April 2000 storm indicated that the main tributary accounted for 85 percent of surface inflows to Abbotts Lagoon. The portion of the surface inflow from the main tributary was lower in the February 1999 storms and is a function of upstream storage and vegetative growth in the tributary basins. Another water budget analysis for a period of no surface inflow (June and July 2000) indicated that the net ground-water contribution was an outflow (seepage) from Abbotts Lagoon of about 0.3 ft3/s.\r\nSalinity increased and nutrient concentrations decreased from upstream to downstream in the chain of lagoons. The lower lagoon, nearest the ocean, had less organic carbon and total phosphorus in the bed sediment than the upper lagoons. The two tributaries originating in the I Ranch dairy had the highest concentrations of nutrients in storm runoff, and the highest loading rates and yields of ammonia and phosphorus. These tributaries account for only 10.3 percent of the area drained by the sampled tributaries, but contributed 83 percent of the ammonia load and 79 percent of the orthophosphate load. The basins with the highest nutrient loading rates and yields had the highest percentage of dairy and (or) ranching impacted land use and, to a lesser extent, grazing land use. The ratios of inorganic nitrogen to phosphorus in the lagoons ranged from 0.1 to 9.5 in the upper lagoon, 0.10 to 0.15 in the middle lagoon, and 0.05 to 0.10 in the lower lagoon. Thus, there is an abundance of phosphorus in the lagoons, and nitrogen appears to be limiting the growth of phytoplankton. Two sterols indicative of fecal material were among 11 compounds detected in the sample collected for analysis of wastewater indicators from a tributary downstream of the I Ranch dairy.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055261","usgsCitation":"Kratzer, C.R., Saleh, D.K., and Zamora, C., 2006, Assessment of hydrologic and water quality data collected in Abbotts Lagoon watershed, Point Reyes National Seashore, California, during water years 1999 and 2000: U.S. Geological Survey Scientific Investigations Report 2005-5261, vi, 35 p., https://doi.org/10.3133/sir20055261.","productDescription":"vi, 35 p.","numberOfPages":"45","temporalStart":"1998-10-01","temporalEnd":"2000-09-30","costCenters":[],"links":[{"id":192392,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7791,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5261/","linkFileType":{"id":5,"text":"html"}},{"id":7792,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5261/sir_2005-5261.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411913,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76571.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Abbotts Lagoon watershed, Point Reyes National Seashore","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.93589523456119,\n              38.130419637147554\n            ],\n            [\n              -122.96560632740022,\n              38.130419637147554\n            ],\n            [\n              -122.96560632740022,\n              38.10518637187005\n            ],\n            [\n              -122.93589523456119,\n              38.10518637187005\n            ],\n            [\n              -122.93589523456119,\n              38.130419637147554\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab2e4b07f02db66ec8d","contributors":{"authors":[{"text":"Kratzer, Charles R.","contributorId":30619,"corporation":false,"usgs":true,"family":"Kratzer","given":"Charles","email":"","middleInitial":"R.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":287724,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saleh, Dina K. 0000-0002-1406-9303","orcid":"https://orcid.org/0000-0002-1406-9303","contributorId":24737,"corporation":false,"usgs":false,"family":"Saleh","given":"Dina","email":"","middleInitial":"K.","affiliations":[{"id":16706,"text":"California State University, CA","active":true,"usgs":false}],"preferred":false,"id":287723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zamora, Celia 0000-0003-1456-4360 czamora@usgs.gov","orcid":"https://orcid.org/0000-0003-1456-4360","contributorId":1514,"corporation":false,"usgs":true,"family":"Zamora","given":"Celia","email":"czamora@usgs.gov","affiliations":[{"id":154,"text":"California 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":287722,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76722,"text":"wdrMDDEDC051 - 2006 - Water resources data Maryland, Delaware, and Washington, D.C.,water year 2005, Volume 1. Surface-water data","interactions":[],"lastModifiedDate":"2023-03-10T13:08:03.968924","indexId":"wdrMDDEDC051","displayToPublicDate":"2006-05-16T00:00:00","publicationYear":"2006","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":"MD-DE-DC-05-1","title":"Water resources data Maryland, Delaware, and Washington, D.C.,water year 2005, Volume 1. Surface-water data","docAbstract":"Water resources data for the 2005 water year for Maryland, Delaware, and Washington, D.C. consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs. This volume (Volume 1. Surface-Water Data) contains records for water discharge at 145 gaging stations; stage and contents of 1 reservoir; stage only for 2 tidal gaging station; and water quality at 19 gaging stations. Also included are stage only for 11 tidal crest-stage partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, local, and Federal agencies in Maryland, Delaware, and Washington, D.C.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDEDC051","usgsCitation":"Saffer, R.W., Pentz, R.H., and Tallman, A.J., 2006, Water resources data Maryland, Delaware, and Washington, D.C.,water year 2005, Volume 1. Surface-water data: U.S. Geological Survey Water Data Report MD-DE-DC-05-1, 530 p., https://doi.org/10.3133/wdrMDDEDC051.","productDescription":"530 p.","numberOfPages":"530","onlineOnly":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":193089,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7788,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-md-de-dc-05-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69959d","contributors":{"authors":[{"text":"Saffer, Richard W.","contributorId":79951,"corporation":false,"usgs":true,"family":"Saffer","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":287715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pentz, Robert H.","contributorId":15276,"corporation":false,"usgs":true,"family":"Pentz","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":287713,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tallman, Anthony J.","contributorId":56275,"corporation":false,"usgs":true,"family":"Tallman","given":"Anthony","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":287714,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":76721,"text":"ofr20061087 - 2006 - Annual dissolved nitrite plus nitrate and total phosphorous loads for the Susquehanna, St. Lawrence, Mississippi-Atchafalaya, and Columbia River basins, 1968-2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:24","indexId":"ofr20061087","displayToPublicDate":"2006-05-16T00:00:00","publicationYear":"2006","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":"2006-1087","title":"Annual dissolved nitrite plus nitrate and total phosphorous loads for the Susquehanna, St. Lawrence, Mississippi-Atchafalaya, and Columbia River basins, 1968-2004","docAbstract":"Annual stream-water loads were calculated near the outlet of four of the larger river basins (Susquehanna, St. Lawrence, Mississippi-Atchafalaya, and Columbia) in the United States for dissolved nitrite plus nitrate (NO2 + NO3) and total phosphorus using LOADEST load estimation software. Loads were estimated for the period 1968-2004; although loads estimated for individual river basins and chemical constituent combinations typically were for shorter time periods due to limitations in data availability. Stream discharge and water-quality data for load estimates were obtained from the U.S. Geological Survey (USGS) with additional stream discharge data for the Mississippi-Atchafalaya River Basin from the U.S. Army Corps of Engineers. The loads were estimated to support national assessments of changes in stream nutrient loads that are periodically conducted by Federal agencies (for example, U.S. Environmental Protection Agency) and other water- and land-resource organizations. Data, methods, and results of load estimates are summarized herein; including World Wide Web links to electronic ASCII text files containing the raw data. The load estimates are compared to dissolved NO2 + NO3 loads for three of the large river basins from 1971 to 1998 that the USGS provided during 2001 to The H. John Heinz III Center for Science, Economics and the Environment (The Heinz Center) for a report The Heinz Center published during 2002. Differences in the load estimates are the result of using the most up-to-date monitoring data since the 2001 analysis, differences in how concentrations less than the reporting limit were handled by the load estimation models, and some errors and exclusions in the 2001 analysis datasets (which resulted in some inaccurate load estimates).","language":"ENGLISH","doi":"10.3133/ofr20061087","collaboration":"Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report.","usgsCitation":"Aulenbach, B.T., 2006, Annual dissolved nitrite plus nitrate and total phosphorous loads for the Susquehanna, St. Lawrence, Mississippi-Atchafalaya, and Columbia River basins, 1968-2004: U.S. Geological Survey Open-File Report 2006-1087, 16 p., https://doi.org/10.3133/ofr20061087.","productDescription":"16 p.","numberOfPages":"16","temporalStart":"1968-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"links":[{"id":194568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7787,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1087/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bb47","contributors":{"authors":[{"text":"Aulenbach, Brent T. 0000-0003-2863-1288 btaulenb@usgs.gov","orcid":"https://orcid.org/0000-0003-2863-1288","contributorId":3057,"corporation":false,"usgs":true,"family":"Aulenbach","given":"Brent","email":"btaulenb@usgs.gov","middleInitial":"T.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287712,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}