{"pageNumber":"3065","pageRowStart":"76600","pageSize":"25","recordCount":184785,"records":[{"id":31367,"text":"ofr01131 - 2001 - Geologic map of the San Bernardino North 7.5' quadrangle, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-06-27T13:08:58.161699","indexId":"ofr01131","displayToPublicDate":"2002-01-01T07:00:00","publicationYear":"2001","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":"2001-131","title":"Geologic map of the San Bernardino North 7.5' quadrangle, San Bernardino County, California","docAbstract":"</br>\n<p>Introduction</p>\n</br>\n<p>Open-File Report OF 01-131 contains a digital geologic map database of the San Bernardino North 7.5’ quadrangle, San Bernardino County, California that includes:</p>\n</br>\n<p>1. ARC/INFO (Environmental Systems Research Institute) version 7.2.1 coverages of the various components of the geologic map</p>\n<p>2. A PostScript file to plot the geologic map on a topographic base, and containing a Correlation of Map Units (CMU) diagram, a Description of Map Units (DMU), an index map, and a regional structure map.</p>\n<p>3. Portable Document Format (.pdf) files of:</p>\n</b>\n<p>a. This Readme; includes an Appendix, containing data found in sbnorth_met.txt .</p>\n</br>\n<p>b. The Description of Map Units identical to that found on the plot of the PostScript file.</p>\n</br>\n<p>c. The same graphic as plotted in 2 above. (Test plots from this .pdf do not produce 1:24,000-scale maps. Use Adobe Acrobat pagesize setting to control map scale.)</p>\n</br>\n<p>The Correlation of Map Units and Description of Map Units is in the editorial format of USGS Miscellaneous Investigations Series (I-series) maps. Within the geologic map data package, map units are identified by standard geologic map criteria such as formation-name, age, and lithology. Even though this is an author-prepared report, every attempt has been made to closely adhere to the stratigraphic nomenclature of the U. S. Geological Survey. Descriptions of units can be obtained by viewing or plotting the .pdf file (3b above) or plotting the postscript file (2 above). If roads in some areas, especially forest roads that parallel topographic contours, do not show well on plots of the geologic map, we recommend use of the USGS San Bernardino North 7.5’ topographic quadrangle in conjunction with the geologic map.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01131","usgsCitation":"Miller, F.K., and Matti, J.C., 2001, Geologic map of the San Bernardino North 7.5' quadrangle, San Bernardino County, California: U.S. Geological Survey Open-File Report 2001-131, 22 p., 1 over-size sheet, https://doi.org/10.3133/ofr01131.","productDescription":"22 p., 1 over-size sheet","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":160837,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3029,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0131/","linkFileType":{"id":5,"text":"html"}},{"id":282080,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0131/pdf/readme.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -17.375,34.125 ], [ -17.375,34.25 ], [ -17.25,34.25 ], [ -17.25,34.125 ], [ -17.375,34.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611464","contributors":{"authors":[{"text":"Miller, F. K.","contributorId":10803,"corporation":false,"usgs":true,"family":"Miller","given":"F.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":205800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matti, J. C.","contributorId":51712,"corporation":false,"usgs":true,"family":"Matti","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52895,"text":"ofr01173 - 2001 - Geologic map of the Devore 7.5' quadrangle, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-06-27T13:32:40.483558","indexId":"ofr01173","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-173","title":"Geologic map of the Devore 7.5' quadrangle, San Bernardino County, California","docAbstract":"This Open-File Report contains a digital geologic map database of the Devore 7.5' quadrangle, San Bernardino County, California, that includes:\n\n1. ARC/INFO (Environmental Systems Research Institute) version 7.2.1 coverages of the various components of the geologic map\n\n2. A PostScript (.ps) file to plot the geologic map on a topographic base, containing a Correlation of Map Units diagram, a Description of Map Units, an index map, and a regional structure map\n\n3. Portable Document Format (.pdf) files of:\n\na. This Readme; includes an Appendix, containing metadata details found in devre_met.txt\n\nb. The same graphic as plotted in 2 above. (Test plots from this .pdf do not produce 1:24,000-scale maps. Adobe Acrobat page-size settings control map scale.)\n\nThe Correlation of Map Units and Description of Map Units are in the editorial format of USGS Miscellaneous Investigations Series maps (I-maps) but have not been edited to comply with I-map standards. Within the geologic-map data package, map units are identified by such standard geologic-map criteria as formation name, age, and lithology. Even though this is an author-prepared report, every attempt has been made to closely adhere to the stratigraphic nomenclature of the U.S. Geological Survey. Descriptions of units can be obtained by viewing or plotting the .pdf file (3b above) or plotting the postscript file (2 above). If roads in some areas, especially forest roads that parallel topographic contours, do not show well on plots of the geologic map, we recommend use of the USGS Devore 7.5’ topographic quadrangle in conjunction with the geologic map.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01173","usgsCitation":"Morton, D.M., and Matti, J.C., 2001, Geologic map of the Devore 7.5' quadrangle, San Bernardino County, California: U.S. Geological Survey Open-File Report 2001-173, Report: 26 p.; 1 Plate: 41.33 x 30.82 inches; Metadata: TXT file; Map: PS.GZ file; Data package: TAR.GZ file, https://doi.org/10.3133/ofr01173.","productDescription":"Report: 26 p.; 1 Plate: 41.33 x 30.82 inches; Metadata: TXT file; Map: PS.GZ file; Data package: TAR.GZ file","numberOfPages":"26","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":177736,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01173.jpg"},{"id":282525,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0173/devre_map.ps.gz","linkFileType":{"id":6,"text":"zip"}},{"id":282526,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0173/devre.tar.gz","linkFileType":{"id":6,"text":"zip"}},{"id":4959,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0173/","linkFileType":{"id":5,"text":"html"}},{"id":282522,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0173/pdf/readme.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282523,"rank":5,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0173/devre_met.txt","linkFileType":{"id":2,"text":"txt"}},{"id":282524,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0173/pdf/of01-173_map.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5,34.125 ], [ -117.5,34.25 ], [ -117.375,34.25 ], [ -117.375,34.125 ], [ -117.5,34.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69866d","contributors":{"authors":[{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":246165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matti, Jonathan C. jmatti@usgs.gov","contributorId":3666,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","email":"jmatti@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":246164,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31365,"text":"ofr2001124 - 2001 - Principal facts for gravity data along the Hayward fault and vicinity, San Francisco Bay area, northern California","interactions":[],"lastModifiedDate":"2023-06-27T12:29:47.914855","indexId":"ofr2001124","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-124","title":"Principal facts for gravity data along the Hayward fault and vicinity, San Francisco Bay area, northern California","docAbstract":"The U.S. Geological Survey (USGS) established over 940 gravity stations along the Hayward fault and vicinity. The Hayward fault, regarded as one of the most hazardous faults in northern California (Working Group on California Earthquake Probabilities, 1999), extends for about 90 km from Fremont in the southeast to San Pablo Bay in the northwest. The Hayward fault is predominantly a right-lateral strike-slip fault that forms the western boundary of the East Bay Hills. These data and associated physical property measurement were collected as part of on-going studies to help determine the earthquake hazard potential of major faults within the San Francisco Bay region. Gravity data were collected between latitude 37°30' and 38°15' N and longitude 121°45' and 122°30' W. Gravity stations were located on the following 7.5 minute quadrangles: Newark, Niles, San Leandro, Hayward, Dublin, Oakland West, Oakland East, Las Trampas Ridge, Diablo, Richmond, Briones Valley, Walnut Creek, and Clayton. All data were ultimately tied to primary gravity base station Menlo Park A, located on the campus of the U.S. Geological Survey in Menlo Park, Calif. (latitude 37°27.34' N, longitude 122°10.18' W, observed gravity value 979944.27 mGal).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2001124","usgsCitation":"Ponce, D.A., 2001, Principal facts for gravity data along the Hayward fault and vicinity, San Francisco Bay area, northern California: U.S. Geological Survey Open-File Report 2001-124, Report: 25 p.; Digital Data; Metadata, https://doi.org/10.3133/ofr2001124.","productDescription":"Report: 25 p.; Digital Data; Metadata","numberOfPages":"27","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":160976,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2001124.jpg"},{"id":12806,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0124/","linkFileType":{"id":5,"text":"html"}},{"id":282083,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0124/of01-124_metadata.met.txt","linkFileType":{"id":2,"text":"txt"}},{"id":282081,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0124/pdf/of01-124.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282082,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0124/of01-124_data.zip","linkFileType":{"id":6,"text":"zip"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,37.5 ], [ -122.5,38.25 ], [ -121.75,38.25 ], [ -121.75,37.5 ], [ -122.5,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668097","contributors":{"authors":[{"text":"Ponce, David A. 0000-0003-4785-7354 ponce@usgs.gov","orcid":"https://orcid.org/0000-0003-4785-7354","contributorId":1049,"corporation":false,"usgs":true,"family":"Ponce","given":"David","email":"ponce@usgs.gov","middleInitial":"A.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":205797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50395,"text":"ofr2001139 - 2001 - Geochemical analysis of soils and sediments, Coeur d'Alene drainage basin, Idaho: sampling, analytical methods, and results","interactions":[],"lastModifiedDate":"2014-07-29T14:42:49","indexId":"ofr2001139","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-139","title":"Geochemical analysis of soils and sediments, Coeur d'Alene drainage basin, Idaho: sampling, analytical methods, and results","docAbstract":"<p>This report presents the locations, descriptions, analytical procedures used, and an inter-lab comparison of over 1100 geochemical analyses of samples of soil and sediment in and downstream of a major lead-zinc-silver mining district in the Coeur d'Alene (CdA) drainage basin of northern Idaho. The samples fall in 3 broad categories: (1) samples from vertical profiles of floodplain soils in the valley of the main stem of the CdA River (767 samples) and of the South Fork of the CdA River (38 samples), (2) size fractionated surficial samples of sediment bedload within the channel of the South Fork of the CdA River (68 samples), and (3) samples from vertical profiles of sediment bedload within the channel of the main stem of the CdA River (260 samples).</p>\n<br>\n<p>Five different laboratories contributed geochemical data for this report. Four of the five laboratories employed analytical methods that require sample dissolution prior to analysis; one laboratory (US Geological Survey) used analytical instrumentation (energy dispersive x-ray fluorescence [EDXRF]) that is applied to pulverized samples. Some dissolution procedures use four acids (hydrochloric, nitric, perchloric, and hydrofluoric; Eastern Washington University [EWU] Geochemical Laboratory and XRAL Laboratories, Inc.), others use two acids (nitric acid and aqua regia; CHEMEX Labs, Inc.), and some use only concentrated nitric acid (ACZ Laboratories, Inc.). Most analyses of dissolved samples were done by Inductively Coupled Plasma - Atomic Emission Spectroscopy (ICP-AES) or by ICP - MS (Mass Spectroscopy). Some analyses for Ag and K were done by Flame Atomic Absorption (FAA).</p>\n<br>\n<p>Inter-laboratory comparisons are made for 6 elements: lead (Pb), zinc (Zn), iron\n(Fe), manganese (Mn), arsenic (As), and cadmium (Cd). In general inter-laboratory correlations are better for samples within the compositional range of the Standard Reference Materials (SRMs) from the National Institute of Standards and Technology (NIST). Analyses by EWU are the most accurate relative to the NIST standards (mean recoveries within 1% for Pb, Fe, Mn, and As, 3% for Zn and 5% for Cd) and are the most precise (within 7% of the mean at the 95% confidence interval). USGS-EDXRF is similarly accurate for Pb and Zn. XRAL and ACZ are relatively accurate for Pb (within 5-8% of certified NIST values), but were considerably less accurate for the other 5 elements of concern (10-25% of NIST values). However, analyses of sample splits by more than one laboratory reveal that, for some elements, XRAL (Pb, Mn, Cd) and ACZ (Pb, Mn, Zn, Fe) analyses were comparable to EWU analyses of the same samples (when values are within the range of NIST SRMs). These results suggest that, for some elements, XRAL and ACZ dissolutions are more effective on the matrix of the CdA samples than on the matrix of the NIST samples (obtained from soils around Butte, Montana). Splits of CdA samples analyzed by CHEMEX were the least accurate, yielding values 10-25% less than those of EWU.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2001139","usgsCitation":"Box, S.E., Bookstrom, A.A., Ikramuddin, M., and Lindsay, J., 2001, Geochemical analysis of soils and sediments, Coeur d'Alene drainage basin, Idaho: sampling, analytical methods, and results (Online version 1.0): U.S. Geological Survey Open-File Report 2001-139, Report: 70 p.; ReadMe; Complete digital data package; Metadata; 7 Appendices: xls and dbf files, https://doi.org/10.3133/ofr2001139.","productDescription":"Report: 70 p.; ReadMe; Complete digital data package; Metadata; 7 Appendices: xls and dbf files","numberOfPages":"206","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"1993-01-01","temporalEnd":"2000-12-31","costCenters":[{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":175484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2001139.PNG"},{"id":10780,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/of01-139/","linkFileType":{"id":5,"text":"html"}},{"id":291343,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/of01-139/of01-139.pdf"},{"id":291344,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2001/of01-139/readme.txt"},{"id":291345,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/of01-139/of01-139.zip"},{"id":291346,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/of01-139/of01-139.met.txt"}],"country":"United States","state":"Idaho","otherGeospatial":"Coeur D�alene Drainage Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.733333,47.466667 ], [ -116.733333,47.583333 ], [ -115.716667,47.583333 ], [ -115.716667,47.466667 ], [ -116.733333,47.466667 ] ] ] } } ] }","edition":"Online version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487f8","contributors":{"authors":[{"text":"Box, Stephen E. 0000-0002-5268-8375 sbox@usgs.gov","orcid":"https://orcid.org/0000-0002-5268-8375","contributorId":1843,"corporation":false,"usgs":true,"family":"Box","given":"Stephen","email":"sbox@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":241354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bookstrom, Arthur A. 0000-0003-1336-3364 abookstrom@usgs.gov","orcid":"https://orcid.org/0000-0003-1336-3364","contributorId":1542,"corporation":false,"usgs":true,"family":"Bookstrom","given":"Arthur","email":"abookstrom@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":241353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ikramuddin, Mohammed","contributorId":46115,"corporation":false,"usgs":true,"family":"Ikramuddin","given":"Mohammed","email":"","affiliations":[],"preferred":false,"id":241356,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lindsay, James","contributorId":34993,"corporation":false,"usgs":true,"family":"Lindsay","given":"James","affiliations":[],"preferred":false,"id":241355,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31380,"text":"ofr01170 - 2001 - Lead recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:09:18","indexId":"ofr01170","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-170","title":"Lead recycling in the United States in 1998","docAbstract":"This materials flow study includes a description of lead supply and demand factors for the United States to illustrate the extent of lead\r\nrecycling and to identify recycling trends. Understanding the system of materials flow from source to ultimate disposition can assist in\r\nimproving the management of the use of natural resources in a manner that is compatible with sound environmental practices. The quantity\r\nof lead recycled in 1998, as a percentage of apparent lead supply, was estimated to be about 63%, and recycling efficiency, to be 95%.\r\nOf the total lead consumed in products for the U.S. market in 1998, an estimated 10% was consumed in products in which the lead was\r\nnot readily recyclable.","language":"ENGLISH","doi":"10.3133/ofr01170","usgsCitation":"Smith, G.R., 2001, Lead recycling in the United States in 1998: U.S. Geological Survey Open-File Report 2001-170, 12 p., https://doi.org/10.3133/ofr01170.","productDescription":"12 p.","costCenters":[],"links":[{"id":164190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3055,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/openfile/of01-170/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a887d","contributors":{"authors":[{"text":"Smith, Gerald R.","contributorId":36496,"corporation":false,"usgs":true,"family":"Smith","given":"Gerald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":205832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30964,"text":"wri014196 - 2001 - Quality of water on the Prairie Band Potawatomi Reservation, northeastern Kansas, February 1999 through February 2001","interactions":[],"lastModifiedDate":"2019-05-21T15:32:40","indexId":"wri014196","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4196","displayTitle":"Quality of Water on the Prairie Band Potawatomi Reservation, Northeastern Kansas, February 1999 Through February 2001","title":"Quality of water on the Prairie Band Potawatomi Reservation, northeastern Kansas, February 1999 through February 2001","docAbstract":"<p>Water-quality samples were collected from 20 surface-water sites and 7 ground-water sites across the Prairie Band Potawatomi Reservation in northeastern Kansas as part of a water-quality study begun in 1996. Water quality is a very important consideration for the tribe. Three creeks draining the reservation, Soldier, Little Soldier, and South Cedar Creeks, are important tribal resources used for maintaining subsistence fishing and hunting needs for tribal members. Samples were collected twice during June 1999 and June 2000 at all 20 surface-water sites after herbicide application, and nine quarterly samples were collected at 5 of the 20 sampling sites from February 1999 through February 2001. Samples were collected once at six wells and twice at one well from September through December 2000. Surface-water-quality constituents analyzed included nutrients, pesticides, and bacteria. In addition to nutrients, pesticides, and bacteria, ground-water constituents analyzed included major dissolved ions, arsenic, boron, and dissolved iron and manganese. </p><p>The median nitrite plus nitrate concentration was 0.376 mg/L (milligram per liter) for 81 surface-water samples, and the maximum concentration was 4.18 mg/L as nitrogen, which is less than one-half the U.S. Environmental Protection Agency's Maximum Contaminant Level (MCL) for drinking water of 10 mg/L as nitrogen. Fifty-one of the 81 surface-water-quality samples exceeded the U.S. Environmental Protection Agency's recommended goal for total phosphorus of 0.10 mg/L for the protection of aquatic life. </p><p>Triazine concentrations in 26 surface-water-quality samples collected during May and June 1999 and 2000 exceeded 3.0 μg/L (micrograms per liter), the Maximum Contaminant Level established for drinking water by the U.S. Environmental Protection Agency. Triazine herbicide concentrations tended to be highest during late spring runoff after herbicide application. High concentrations of fecal indicator bacteria in surface water are a concern on the reservation with fecal coliform concentrations ranging from 4 to greater than 31,000 colonies per 100 milliliters of water with a median concentration of 570 colonies per 100 milliliters. More than one-half of the surface-water-quality samples exceeded the Kansas Department of Health and Environment contact recreation criteria of 200 and 2,000 colonies per 100 milliliters of water and were collected mostly during the spring and summer. </p><p>Two wells had sodium concentrations of about 10 times the U.S. Environmental Protection Agengy health advisory level (HAL) of 20 mg/L; concentrations ranged from 241 to 336 mg/L. In water from two wells, sulfate concentrations exceeded 800 mg/L, more than three times the U.S. Environmental Protection Agency Secondary Maximum Contaminant Level (SMCL) for drinking water of 250 mg/L. All but two of the eight ground-water-quality samples had dissolved-solids concentrations exceeding the SMCL of 500 mg/L. The highest concentration of 2,010 mg/L was more than four times the SMCL. Dissolved boron concentrations exceeded the U.S. Environmental Protection Agency 600-μg/L HAL in water from two of the seven wells sampled. Because the HAL is for a lifetime of exposure, the anticipated health risk due to dissolved boron is low. Dissolved iron concentrations in ground-water samples exceeded the 300-μg/L SMCL for treated drinking water in three of the seven wells sampled. Dissolved manganese concentrations in water from the same three wells also exceeded the established SMCL of 50 μg/L. Dissolved pesticides were not detected in any of the well samples; however, there were degradation products of the herbicides alachlor and metolachlor in several samples. Insecticides were not detected in any ground-water-quality samples. Low concentrations of E. coli and fecal coliform bacteria were detected in water from two wells, and E. coli was detected in water from one well. Much higher concentrations of E. coli, fecal coliform, and fecal strepto</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014196","collaboration":"Prepared in cooperation with the Prairie Band Potawatomi","usgsCitation":"Trombley, T.J., 2001, Quality of water on the Prairie Band Potawatomi Reservation, northeastern Kansas, February 1999 through February 2001: U.S. Geological Survey Water-Resources Investigations Report 2001-4196, vi, 51 p. , https://doi.org/10.3133/wri014196.","productDescription":"vi, 51 p. 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 \"}}]}","contact":"<p><a href=\"mailto:%20dc_ks@usgs.gov\" data-mce-href=\"mailto:%20dc_ks@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/kswsc\" data-mce-href=\"https://www.usgs.gov/centers/kswsc\">Kansas Water Science Center</a><br>U.S. Geological Survey<br>1217 Biltmore Drive<br>Lawrence, KS 66049</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Surface-Water Quality</li><li>Ground-Water Quality</li><li>Summary</li><li>References</li></ul>","publishingServiceCenter":{"id":4,"text":"Rolla PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686211","contributors":{"authors":[{"text":"Trombley, T. 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,{"id":31405,"text":"ofr01290 - 2001 - Geologic map and digital database of the San Rafael Mtn. 7.5-minute quadrangle, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2023-06-27T13:31:50.152959","indexId":"ofr01290","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-290","title":"Geologic map and digital database of the San Rafael Mtn. 7.5-minute quadrangle, Santa Barbara County, California","docAbstract":"Geologic mapping of the San Rafael Primitive Area (now the San Rafael Wilderness) by Gower and others (1966) and Vedder and others (1967) did not include all of the San Rafael Mtn. quadrangle, and the part that was mapped was done in reconnaissance fashion. To help resolve some of the structural and stratigraphic ambiguities of the earlier mapping and to complete the mapping of the quadrangle, additional field work was done during short intervals in 1980 and 1981 and from 1996 to 1998. Contacts within the belt of Franciscan rocks at the southwestern corner of the quadrangle were generalized from the detailed map by Wahl (1998).\n\nBecause extensive areas were inaccessible owing to impenetrable chaparral, observations from several helicopter overflights (1965, 1980, 1981) and interpretations from aerial photographs were used as compilation aids. Consequently, some of the depicted contacts and faults are highly inferential, particularly within the Upper Cretaceous rocks throughout the middle part of the quadrangle.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01290","usgsCitation":"Vedder, J.G., Stanley, R.G., Graham, S.E., and Valin, Z., 2001, Geologic map and digital database of the San Rafael Mtn. 7.5-minute quadrangle, Santa Barbara County, California: U.S. Geological Survey Open-File Report 2001-290, Report: 22 p.; 1 Plate: 48.00 x 36.00 inches; Metadata, https://doi.org/10.3133/ofr01290.","productDescription":"Report: 22 p.; 1 Plate: 48.00 x 36.00 inches; Metadata","numberOfPages":"22","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":160363,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01290.gif"},{"id":282687,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0290/srm.tar.gz","linkFileType":{"id":6,"text":"zip"}},{"id":282684,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0290/pdf/srm_expl.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282683,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0290/","linkFileType":{"id":5,"text":"html"}},{"id":282686,"rank":6,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0290/srm_met.txt","linkFileType":{"id":2,"text":"txt"}},{"id":282685,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0290/pdf/srm.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391296,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43747.htm","linkFileType":{"id":5,"text":"html"}},{"id":282688,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0290/srm.ps.gz","linkFileType":{"id":6,"text":"zip"}}],"scale":"24000","projection":"Polyconic projection","country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"San Rafael Mtn. 7.5-minute quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.875,34.625 ], [ -119.875,34.75 ], [ -119.75,34.75 ], [ -119.75,34.625 ], [ -119.875,34.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68751d","contributors":{"authors":[{"text":"Vedder, John G.","contributorId":89553,"corporation":false,"usgs":true,"family":"Vedder","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":205901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanley, Richard G. 0000-0001-6192-8783 rstanley@usgs.gov","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":1832,"corporation":false,"usgs":true,"family":"Stanley","given":"Richard","email":"rstanley@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":205899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graham, S. E.","contributorId":100025,"corporation":false,"usgs":true,"family":"Graham","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":205902,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Valin, Z. C. 0000-0001-6199-6700","orcid":"https://orcid.org/0000-0001-6199-6700","contributorId":75165,"corporation":false,"usgs":true,"family":"Valin","given":"Z. C.","affiliations":[],"preferred":false,"id":205900,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31397,"text":"ofr01249 - 2001 - Log for Joint SEPM-Colorado Scientific Society field trip, September 20-21, 1986: Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range, from Westcliffe to Crestone, Colorado","interactions":[{"subject":{"id":14691,"text":"ofr86452 - 1986 - Log for joint SEPM-Colorado Scientific Society field trip from Westcliffe to Crestone, Colorado, September 20-21, 1986; Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range","indexId":"ofr86452","publicationYear":"1986","noYear":false,"title":"Log for joint SEPM-Colorado Scientific Society field trip from Westcliffe to Crestone, Colorado, September 20-21, 1986; Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range"},"predicate":"SUPERSEDED_BY","object":{"id":31397,"text":"ofr01249 - 2001 - Log for Joint SEPM-Colorado Scientific Society field trip, September 20-21, 1986: Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range, from Westcliffe to Crestone, Colorado","indexId":"ofr01249","publicationYear":"2001","noYear":false,"title":"Log for Joint SEPM-Colorado Scientific Society field trip, September 20-21, 1986: Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range, from Westcliffe to Crestone, Colorado"},"id":1}],"lastModifiedDate":"2022-09-15T19:45:11.772543","indexId":"ofr01249","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-249","title":"Log for Joint SEPM-Colorado Scientific Society field trip, September 20-21, 1986: Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range, from Westcliffe to Crestone, Colorado","docAbstract":"<p>This trip will cross the northern Sangre de Cristo Range, from Westcliffe to Crestone, Colorado, by way of the Hermit Pass Road and the Rito Alto pack trail (Fig. 1 below; road and trail shown on Fig. 2). The traverse is designed to give the geologist a sample of the structure and stratigraphy of this part of the range. Emphasis will be on the relationship between the horst of the Sangre de Cristo Range and adjacent down-dropped valleys, on the Laramide thrusted structure of the range, and on the stratigraphy and depositional environments of Pennsylvanian and Permian sedimentary rocks in the range.</p><p>The northern Sangre de Cristo Range is composed mostly of Early and Middle Proterozoic crystalline rocks and Paleozoic clastic sedimentary rocks (see geologic map, Fig. 2). Proterozoic rocks, mostly gneiss and quartz monzonite, are overlain on the west side of the range by about 100 m of early Paleozoic quartzite, dolomite, limestone, and shale. Early Paleozoic rocks are in turn unconformably overlain by Pennsylvanian and Permian clastic rocks. Southeast of the range, in Huerfano Park, Paleozoic rocks are overlain by Jurassic and Cretaceous rocks of the Raton basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01249","usgsCitation":"Lindsey, D.A., 2001, Log for Joint SEPM-Colorado Scientific Society field trip, September 20-21, 1986: Late Paleozoic sedimentation and Laramide tectonics of the Sangre de Cristo Range, from Westcliffe to Crestone, Colorado: U.S. Geological Survey Open-File Report 2001-249, HTML Document, https://doi.org/10.3133/ofr01249.","productDescription":"HTML Document","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":160688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406784,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_42706.htm","linkFileType":{"id":5,"text":"html"}},{"id":2515,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0249/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","city":"Crestone, Westcliffe","otherGeospatial":"Sangre de Cristo Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.70907592773438,\n              37.9991387373021\n            ],\n            [\n              -105.47080993652344,\n              37.9991387373021\n            ],\n            [\n              -105.47080993652344,\n              38.13428653167246\n            ],\n            [\n              -105.70907592773438,\n              38.13428653167246\n            ],\n            [\n              -105.70907592773438,\n              37.9991387373021\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c057","contributors":{"authors":[{"text":"Lindsey, David A. 0000-0002-9466-0899 dlindsey@usgs.gov","orcid":"https://orcid.org/0000-0002-9466-0899","contributorId":773,"corporation":false,"usgs":true,"family":"Lindsey","given":"David","email":"dlindsey@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":205877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31374,"text":"ofr01153 - 2001 - Heavy minerals from the Palos Verdes margin, southern California: Data and factor analysis","interactions":[],"lastModifiedDate":"2021-09-24T13:52:35.862948","indexId":"ofr01153","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-153","title":"Heavy minerals from the Palos Verdes margin, southern California: Data and factor analysis","docAbstract":"Heavy or high-density minerals in the 63-250-_m (micron) size fraction (very fine and fine sand) were analyzed from 36 beach and offshore sites (38 samples) of the Palos Verdes margin to determine the areal and temporal mineralogic distributions and the relation of those distributions to the deposit affected by material discharged from the Los Angeles County Sanitation District sewage system (Lee, 1994) (Figure 1). Data presented here were tabulated for a report to the Department of Justice (Wong, 1994). The results of the data analysis are discussed in Wong (in press).\n\nThe study of heavy minerals is a common method of determining sources (provenance) and distributions of sediments (e.g., Van Andel and Poole, 1960). The choice of grain size is governed by ease of sample preparation, examination by optical microscopy, and comparability to previous studies. How representative the 63-250-_m heavy minerals are of the whole sample can be approximated by the amount of sand in the sample. Lee and others (1994) mapped a pre-effluent, effluent-affected, and surface layer in the study area off Palos Verdes. The amount of sand in the top and pre-effluent layers ranges from about 20 to 80 percent; in the middle of the effluent body, sand is less than 20 percent (Figure 2; MacArthur and others, 1994). Qualitatively, the 63-250-_m heavy minerals are more representative of the top and pre-effluent layer, but these minerals will also provide useful information about the middle layer.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01153","usgsCitation":"Wong, F.L., 2001, Heavy minerals from the Palos Verdes margin, southern California: Data and factor analysis: U.S. Geological Survey Open-File Report 2001-153, Report: 8 p.; Metadata, https://doi.org/10.3133/ofr01153.","productDescription":"Report: 8 p.; Metadata","numberOfPages":"31","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":164095,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01153.jpg"},{"id":389711,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_42119.htm"},{"id":282449,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0153/minsplsmc.txt"},{"id":282448,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0153/pdf/of01-153.pdf"},{"id":3050,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0153/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Palos Verdes Margin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.433333,34.666667 ], [ -118.433333,34.8 ], [ -118.3,34.8 ], [ -118.3,34.666667 ], [ -118.433333,34.666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c099","contributors":{"authors":[{"text":"Wong, Florence L. 0000-0002-3918-5896 fwong@usgs.gov","orcid":"https://orcid.org/0000-0002-3918-5896","contributorId":1990,"corporation":false,"usgs":true,"family":"Wong","given":"Florence","email":"fwong@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":205815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31377,"text":"ofr01157 - 2001 - Archive of water gun subbottom data collected during USGS cruise SEAX 95007 New York Bight, 7-25, May 1995","interactions":[],"lastModifiedDate":"2021-11-23T21:53:41.193576","indexId":"ofr01157","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-157","title":"Archive of water gun subbottom data collected during USGS cruise SEAX 95007 New York Bight, 7-25, May 1995","docAbstract":"<p>Beginning in 1995, the USGS, in cooperation with the U.S Army Corps of Engineers (USACE), New York District, began a program to generate reconnaissance maps of the sea floor offshore of the New York-New Jersey metropolitan area, one of the most populated coastal regions of the United States. The goal of this mapping program is to provide a regional synthesis of the sea-floor environment, including a description of sedimentary environments, sediment texture, seafloor morphology, and geologic history to aid in understanding the impacts of anthropogenic activities, such as ocean dumping. This mapping effort differs from previous studies of this area by obtaining digital, sidescan sonar images that cover 100 percent of the sea floor.</p><p>This investigation was motivated by the need to develop an environmentally acceptable solution for the disposal of dredged material from the New York - New Jersey Port, by the need to identify potential sources of sand for renourishment of the southern shore of Long island, and by the opportunity to develop a better understanding of the transport and long-term fate of contaminants by investigations of the present distribution of materials discharged into the New York Bight over the last 100+ years (Schwab and others, 1997). Data collected in 1996, USGS cruise SEAX 96004, augments data collected in 1995 with sidescan sonar and seismic reflection data collected within the New York Bight Apex region. This report is an archive of the boomer seismic reflection data collected in 1996.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01157","usgsCitation":"Hill, J.C., Schwab, W.C., and Foster, D., 2001, Archive of water gun subbottom data collected during USGS cruise SEAX 95007 New York Bight, 7-25, May 1995: U.S. Geological Survey Open-File Report 2001-157, HTML Document; DVD-ROM, https://doi.org/10.3133/ofr01157.","productDescription":"HTML Document; DVD-ROM","onlineOnly":"N","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":164098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0157/coverthb.jpg"},{"id":350979,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://woodshole.er.usgs.gov/publications/of01-157/"},{"id":392075,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43238.htm"}],"country":"United States","state":"New Jersey, New York","otherGeospatial":"New York Bight","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.9,40.36 ], [ -73.9,40.58 ], [ -73.49,40.58 ], [ -73.49,40.36 ], [ -73.9,40.36 ] ] ] } } ] }","contact":"<p>Director, <a href=\"https://woodshole.er.usgs.gov/index.html\" data-mce-href=\"https://woodshole.er.usgs.gov/index.html\">Woods Hole Science Center</a><br> 384 Woods Hole Road<br> Quissett Campus<br> Woods Hole, MA 02543</p>","tableOfContents":"<ul><li>Read Me&nbsp;</li><li>Cruise Report</li><li>Equipment</li><li>Seismic Data</li><li>Shotpoint Maps</li><li>Navigation</li><li>Disclaimer</li><li>Pictures</li><li>Contact</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db674fe0","contributors":{"authors":[{"text":"Hill, J. C.","contributorId":100878,"corporation":false,"usgs":true,"family":"Hill","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwab, W. C.","contributorId":78740,"corporation":false,"usgs":true,"family":"Schwab","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205822,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, D.S.","contributorId":30641,"corporation":false,"usgs":true,"family":"Foster","given":"D.S.","email":"","affiliations":[],"preferred":false,"id":205821,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31378,"text":"ofr01161 - 2001 - Baseline geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River from North Fork to Corn Creek, collected prior to the severe wildfires of 2000 in central Idaho","interactions":[{"subject":{"id":31378,"text":"ofr01161 - 2001 - Baseline geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River from North Fork to Corn Creek, collected prior to the severe wildfires of 2000 in central Idaho","indexId":"ofr01161","publicationYear":"2001","noYear":false,"title":"Baseline geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River from North Fork to Corn Creek, collected prior to the severe wildfires of 2000 in central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":51434,"text":"ofr03152 - 2003 - Geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River, collected before and after the Clear Creek, Little Pistol, and Shellrock wildfires of 2000 in central Idaho","indexId":"ofr03152","publicationYear":"2003","noYear":false,"title":"Geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River, collected before and after the Clear Creek, Little Pistol, and Shellrock wildfires of 2000 in central Idaho"},"id":1}],"supersededBy":{"id":51434,"text":"ofr03152 - 2003 - Geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River, collected before and after the Clear Creek, Little Pistol, and Shellrock wildfires of 2000 in central Idaho","indexId":"ofr03152","publicationYear":"2003","noYear":false,"title":"Geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River, collected before and after the Clear Creek, Little Pistol, and Shellrock wildfires of 2000 in central Idaho"},"lastModifiedDate":"2012-02-02T00:09:18","indexId":"ofr01161","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-161","title":"Baseline geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River from North Fork to Corn Creek, collected prior to the severe wildfires of 2000 in central Idaho","docAbstract":"In 1996, the U.S. Geological Survey conducted a reconnaissance baseline geochemical study in central Idaho. The purpose of the baseline study was to establish a 'geochemical snapshot' of the area, as a datum for monitoring future change in the geochemical landscape, whether natural or human-induced. This report presents the methology, analytical results, and sample descriptions for water, sediment, and heavy-mineral concentrate samples collected during this geochemical investigation. In the summer of 2000, the Clear Creek, Little Pistol, and Shellrock wildfires swept across much of the area that was sampled. Thus, these data represent a pre-fire baseline geochemical dataset. A 2001 post- fire study is planned and will involve re-sampling of the pre-fire baseline sites, to allow for pre- and post-fire comparison.","language":"ENGLISH","doi":"10.3133/ofr01161","usgsCitation":"Eppinger, R.G., Briggs, P.H., Brown, Z.A., Crock, J.G., Meier, A., Theodorakos, P.M., and Wilson, S.A., 2001, Baseline geochemical data for stream sediment and surface water samples from Panther Creek, the Middle Fork of the Salmon River, and the Main Salmon River from North Fork to Corn Creek, collected prior to the severe wildfires of 2000 in central Idaho (Version 1.0): U.S. Geological Survey Open-File Report 2001-161, 20 p., https://doi.org/10.3133/ofr01161.","productDescription":"20 p.","costCenters":[],"links":[{"id":164099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3053,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0161/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648853","contributors":{"authors":[{"text":"Eppinger, Robert G. eppinger@usgs.gov","contributorId":849,"corporation":false,"usgs":true,"family":"Eppinger","given":"Robert","email":"eppinger@usgs.gov","middleInitial":"G.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":205825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Paul H.","contributorId":30973,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":205829,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Zoe Ann","contributorId":95530,"corporation":false,"usgs":true,"family":"Brown","given":"Zoe","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":205830,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crock, James G. jcrock@usgs.gov","contributorId":200,"corporation":false,"usgs":true,"family":"Crock","given":"James","email":"jcrock@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":205824,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Meier, Allen","contributorId":29037,"corporation":false,"usgs":true,"family":"Meier","given":"Allen","affiliations":[],"preferred":false,"id":205828,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Theodorakos, Peter M. ptheodor@usgs.gov","contributorId":1566,"corporation":false,"usgs":true,"family":"Theodorakos","given":"Peter","email":"ptheodor@usgs.gov","middleInitial":"M.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":205826,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wilson, Stephen A. 0000-0002-9468-0005 swilson@usgs.gov","orcid":"https://orcid.org/0000-0002-9468-0005","contributorId":1617,"corporation":false,"usgs":true,"family":"Wilson","given":"Stephen","email":"swilson@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":205827,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":30963,"text":"wri014193 - 2001 - Detection and measurement of land subsidence using Global Positioning System and interferometric synthetic aperture radar, Coachella Valley, California, 1996-98","interactions":[],"lastModifiedDate":"2019-09-09T10:11:44","indexId":"wri014193","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4193","title":"Detection and measurement of land subsidence using Global Positioning System and interferometric synthetic aperture radar, Coachella Valley, California, 1996-98","docAbstract":"Land subsidence associated with ground-water-level declines has been recognized as a potential problem in Coachella Valley, California. Since the early 1920s, ground water has been a major source of agricultural, municipal, and domestic supply in the valley, resulting in water-level declines as large as 15 meters (50 feet) through the late 1940s. In 1949, the importation of Colorado River water to the lower Coachella Valley began, resulting in a reduction in ground-water pumping and a recovery of water levels from the 1950s through the 1970s. Since the late 1970s, the demand for water in the valley has exceeded the deliveries of imported surface water, again resulting in increased pumping and ground-water-level declines. \n\nThe magnitude and temporal occurrence of land subsidence in the lower Coachella Valley are not well known; data are sparse and accuracy varies. Also, the area is tectonically active and has subsided during the past several million years, which further complicates interpretations of the data. Land-surface-elevation data have been collected by many agencies using various methods and different geographic scales; because of this, the -150 millimeters (-0.5 foot) of subsidence determined for the southern parts of the valley for 1930-96 may have a possible error of plus or minus (?)90 millimeters (?0.3 foot). The location, extent, and magnitude of vertical land-surface changes from 1996 to 1998 were determined using Global Positioning System (GPS) and interferometric synthetic aperture radar (InSAR) methods. GPS measurements for 14 monuments in the lower Coachella Valley indicate that the vertical land-surface changes from 1996 to 1998 ranged from -13 to -67 millimeters ? 40 millimeters (-0.04 to -0.22 foot ?0.13 foot). Changes at seven of the monuments exceeded the measurement error of ?40 millimeters (?0.13 foot), which indicates that small amounts of land subsidence occurred at these monuments between 1996 and 1998. Some of the water levels measured in wells near several of these monuments during 1996-98 were the lowest water levels in the recorded histories of the wells. The possible relation between the stresses caused by historically low water levels and the measured vertical changes in land surface suggests that the preconsolidation stress of the aquifer system may have been exceeded during this period and that subsidence may be permanent. Comparisons of several paired monuments and wells indicated that the relation between short-term ground-water-level changes and vertical changes in land surface in the lower Coachella Valley is not clearly defined.\n\nResults of InSAR measurements made between 1996 and 1998 indicate that vertical changes in land surface, ranging from about -20 to -70 millimeters ? 5-10 millimeters (-0.07 to -0.23 foot ? 0.02-0.03 foot), occurred in three areas of the Coachella Valley--near Palm Desert, Indian Wells, and Lake Cahuilla. The areas of subsidence near Palm Desert and Indian Wells coincide with areas of substantial ground-water production during 1996-98. The Coachella Valley Water District reported that they had no ground-water production wells in the Lake Cahuilla area but that there may be private production wells in the area. Production from these wells or possibly tectonic activity may be contributing to or causing the subsidence. \n\nThe geodetic network used for the GPS measurements described in this report covers the area from the Salton Sea on the south to just northwest of Indio. The maps processed using InSAR overlap the part of the geodetic network west of Coachella and north of Lake Cahuilla, and include the Palm Desert area. Both methods of measuring vertical land-surface changes, GPS and InSAR, were used to characterize vertical land-surface changes from the Palm Desert area to the Salton Sea. Because InSAR produces more spatially detailed data over large areas, it generally was useful where vertical land-surface changes were previously unrecognized, such as the","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014193","usgsCitation":"Sneed, M., Ikehara, M.E., Galloway, D., and Amelung, F., 2001, Detection and measurement of land subsidence using Global Positioning System and interferometric synthetic aperture radar, Coachella Valley, California, 1996-98: U.S. Geological Survey Water-Resources Investigations Report 2001-4193, 31 p., https://doi.org/10.3133/wri014193.","productDescription":"31 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":159944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4193/report-thumb.jpg"},{"id":95889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4193/report.pdf","size":"7591","linkFileType":{"id":1,"text":"pdf"}},{"id":2944,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014193","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Coachella Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.2192153930664,\n              33.574296227998836\n            ],\n            [\n              -116.07707977294922,\n              33.574296227998836\n            ],\n            [\n              -116.07707977294922,\n              33.71263140220726\n            ],\n            [\n              -116.2192153930664,\n              33.71263140220726\n            ],\n            [\n              -116.2192153930664,\n              33.574296227998836\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667a5c","contributors":{"authors":[{"text":"Sneed, Michelle 0000-0002-8180-382X micsneed@usgs.gov","orcid":"https://orcid.org/0000-0002-8180-382X","contributorId":155,"corporation":false,"usgs":true,"family":"Sneed","given":"Michelle","email":"micsneed@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ikehara, Marti E.","contributorId":53757,"corporation":false,"usgs":true,"family":"Ikehara","given":"Marti","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":204469,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, D. L. 0000-0003-0904-5355","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":31383,"corporation":false,"usgs":true,"family":"Galloway","given":"D. L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":204468,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Amelung, Falk","contributorId":83569,"corporation":false,"usgs":true,"family":"Amelung","given":"Falk","affiliations":[],"preferred":false,"id":204470,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31383,"text":"ofr01189 - 2001 - Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 1994 through December 31, 1999","interactions":[],"lastModifiedDate":"2016-09-07T15:11:36","indexId":"ofr01189","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-189","title":"Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 1994 through December 31, 1999","docAbstract":"<p>The Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, the Geophysical Institute of the University of Alaska - Fairbanks, and the Alaska Division of Geological and Geophysical Surveys, has maintained a seismic monitoring program at potentially active volcanoes in Alaska since 1988 (Power and others, 1993; Jolly and others, 1996). The primary objectives of this program are the seismic surveillance of active, potentially hazardous, Alaskan volcanoes and the investigation of seismic processes associated with active volcanism.</p><p>Between 1994 and 1999, the AVO seismic monitoring program underwent significant changes with networks added at new volcanoes during each summer from 1995 through 1999. The existing network at Katmai –Valley of Ten Thousand Smokes (VTTS) was repaired in 1995, and new networks were installed at Makushin (1996), Akutan (1996), Pavlof (1996), Katmai - south (1996), Aniakchak (1997), Shishaldin (1997), Katmai - north (1998), Westdahl, (1998), Great Sitkin (1999) and Kanaga (1999). These networks added to AVO's existing seismograph networks in the Cook Inlet area and increased the number of AVO seismograph stations from 46 sites and 57 components in 1994 to 121 sites and 155 components in 1999. The 1995–1999 seismic network expansion increased the number of volcanoes monitored in real-time from 4 to 22, including Mount Spurr, Redoubt Volcano, Iliamna Volcano, Augustine Volcano, Mount Snowy, Mount Griggs, Mount Katmai, Novarupta, Trident Volcano, Mount Mageik, Mount Martin, Aniakchak Crater, Pavlof Volcano, Mount Dutton, Isanotski volcano, Shisaldin Volcano, Fisher Caldera, Westdahl volcano, Akutan volcano, Makushin Volcano, Great Sitkin volcano, and Kanaga Volcano (see Figures 1-15). The network expansion also increased the number of earthquakes located from about 600 per year in1994 and 1995 to about 3000 per year between 1997 and 1999.</p><p>Highlights of the catalog period include: 1) a large volcanogenic seismic swarm at Akutan volcano in March and April 1996 (Lu and others, 2000); 2) an eruption at Pavlof Volcano in fall 1996 (Garces and others, 2000; McNutt and others, 2000); 3) an earthquake swarm at Iliamna volcano between September and December 1996; 4) an earthquake swarm at Mount Mageik in October 1996 (Jolly and McNutt, 1999); 5) an earthquake swarm located at shallow depth near Strandline Lake; 6) a strong swarm of earthquakes near Becharof Lake; 7) precursory seismicity and an eruption at Shishaldin Volcano in April 1999 that included a 5.2 ML earthquake and aftershock sequence (Moran and others, in press; Thompson and others, in press). The 1996 calendar year is also notable as the seismicity rate was very high, especially in the fall when 3 separate areas (Strandline Lake, Iliamna Volcano, and several of the Katmai volcanoes) experienced high rates of located earthquakes.</p><p>This catalog covers the period from January 1, 1994, through December 31,1999, and includes: 1) earthquake origin times, hypocenters, and magnitudes with summary statistics describing the earthquake location quality; 2) a description of instruments deployed in the field and their locations and magnifications; 3) a description of earthquake detection, recording, analysis, and data archival; 4) velocity models used for earthquake locations; 5) phase arrival times recorded at individual stations; and 6) a summary of daily station usage from throughout the report period. We have made calculated hypocenters, station locations, system magnifications, velocity models, and phase arrival information available for download via computer network as a compressed Unix tar file.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01189","usgsCitation":"Jolly, A.D., Stihler, S.D., Power, J.A., Lahr, J.C., Paskievitch, J., Tytgat, G., Estes, S., Lockhart, A., Moran, S.C., McNutt, S.R., and Hammond, W.R., 2001, Catalog of earthquake hypocenters at Alaskan volcanoes: January 1, 1994 through December 31, 1999: U.S. Geological Survey Open-File Report 2001-189, Report: 22 p.; Appendix B; Download: TAR.GZ file, https://doi.org/10.3133/ofr01189.","productDescription":"Report: 22 p.; Appendix B; Download: TAR.GZ file","numberOfPages":"22","temporalStart":"1994-01-01","temporalEnd":"1999-12-31","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":164292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01189.jpg"},{"id":3058,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0189/","linkFileType":{"id":5,"text":"html"}},{"id":282542,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0189/pdf/of01-189.pdf","text":"Report","size":"522 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":282543,"rank":3,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2001/0189/pdf/appendixb.pdf","text":"Appendix B","size":"2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Appendix B"},{"id":282544,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0189/ofr01-189-tar.gz","text":"Data Files","size":"14.5 MB","description":"Data Files"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -178.0,52.0 ], [ -178.0,64.0 ], [ -138.0,64.0 ], [ -138.0,52.0 ], [ -178.0,52.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efb90","contributors":{"authors":[{"text":"Jolly, Arthur D.","contributorId":57913,"corporation":false,"usgs":true,"family":"Jolly","given":"Arthur","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stihler, Scott D.","contributorId":31373,"corporation":false,"usgs":true,"family":"Stihler","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":205843,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Power, John A. 0000-0002-7233-4398 jpower@usgs.gov","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":2768,"corporation":false,"usgs":true,"family":"Power","given":"John","email":"jpower@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":205841,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lahr, John C.","contributorId":20328,"corporation":false,"usgs":true,"family":"Lahr","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205842,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Paskievitch, John","contributorId":74050,"corporation":false,"usgs":true,"family":"Paskievitch","given":"John","affiliations":[],"preferred":false,"id":205848,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tytgat, Guy","contributorId":71152,"corporation":false,"usgs":true,"family":"Tytgat","given":"Guy","email":"","affiliations":[],"preferred":false,"id":205847,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Estes, Steve","contributorId":55881,"corporation":false,"usgs":true,"family":"Estes","given":"Steve","email":"","affiliations":[],"preferred":false,"id":205845,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Lockhart, Andrew B. ablock@usgs.gov","contributorId":632,"corporation":false,"usgs":true,"family":"Lockhart","given":"Andrew B.","email":"ablock@usgs.gov","affiliations":[],"preferred":true,"id":205840,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Moran, Seth C. 0000-0001-7308-9649 smoran@usgs.gov","orcid":"https://orcid.org/0000-0001-7308-9649","contributorId":548,"corporation":false,"usgs":true,"family":"Moran","given":"Seth","email":"smoran@usgs.gov","middleInitial":"C.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":205839,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"McNutt, Stephen R.","contributorId":38133,"corporation":false,"usgs":true,"family":"McNutt","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":205844,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Hammond, William R.","contributorId":76375,"corporation":false,"usgs":true,"family":"Hammond","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":205849,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":31385,"text":"ofr01198 - 2001 - Publications of the Western Earth Surface Processes Team 2000","interactions":[],"lastModifiedDate":"2023-06-27T12:53:50.256124","indexId":"ofr01198","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-198","title":"Publications of the Western Earth Surface Processes Team 2000","docAbstract":"The Western Earth Surface Processes Team (WESP) of the U.S. Geological Survey (USGS) conducts geologic mapping and related topical earth science studies in the western United States. This work is focused on areas where modern geologic maps and associated earth-science data are needed to address key societal and environmental issues such as ground-water quality, potential geologic hazards, and land-use decisions. Areas of primary emphasis in 2000 included southern California, the San Francisco Bay region, the Pacific Northwest, the Las Vegas urban corridor, and selected National Park lands. The team has its headquarters in Menlo Park, California, and maintains smaller field offices at several other locations in the western United States. The results of research conducted by the WESPT are released to the public as a variety of databases, maps, text reports, and abstracts, both through the internal publication system of the USGS and in diverse external publications such as scientific journals and books. This report lists publications of the WESPT released in 2000 as well as additional 1999 publications that were not included in the previous list (USGS Open-file Report 00-215). Most of the publications listed were authored or coauthored by WESPT staff. The list also includes some publications authored by non-USGS cooperators with the WESPT, as well as some authored by USGS staff outside the WESPT in cooperation with WESPT projects. Several of the publications listed are available on the World Wide Web; for these, URL addresses are provided. Many of these Web publications are USGS open-file reports that contain large digital databases of geologic map and related information.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01198","usgsCitation":"Powell, C.L., and Stone, P., 2001, Publications of the Western Earth Surface Processes Team 2000: U.S. Geological Survey Open-File Report 2001-198, 17 p., https://doi.org/10.3133/ofr01198.","productDescription":"17 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":59770,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0198/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":281577,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0198/","linkFileType":{"id":5,"text":"html"}},{"id":163374,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2001/0198/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687d3d","contributors":{"authors":[{"text":"Powell, Charles L. II 0000-0002-1913-555X cpowell@usgs.gov","orcid":"https://orcid.org/0000-0002-1913-555X","contributorId":3243,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","email":"cpowell@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":205854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, Paul 0000-0002-1439-0156 pastone@usgs.gov","orcid":"https://orcid.org/0000-0002-1439-0156","contributorId":273,"corporation":false,"usgs":true,"family":"Stone","given":"Paul","email":"pastone@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":205853,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30961,"text":"wri20014188 - 2001 - Low-Level Volatile Organic Compounds in Active Public Supply Wells as Ground-Water Tracers in the Los Angeles Physiographic Basin, California, 2000","interactions":[],"lastModifiedDate":"2012-02-10T00:10:08","indexId":"wri20014188","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4188","title":"Low-Level Volatile Organic Compounds in Active Public Supply Wells as Ground-Water Tracers in the Los Angeles Physiographic Basin, California, 2000","docAbstract":"Data were collected to evaluate the use of low-level volatile organic compounds (VOC) to assess the vulnerability of public supply wells in the Los Angeles physiographic basin. Samples of untreated ground water from 178 active public supply wells in the Los Angeles physiographic basin show that VOCs were detected in 61 percent of the ground-water samples; most of these detections were low, with only 29 percent above 1 mg/L (microgram per liter). Thirty-nine of the 86 VOCs analyzed were detected in at least one sample, and 11 VOCs were detected in 7 percent or more of the samples. The six most frequently detected VOCs were trichloromethane (chloroform) (46 percent); trichloroethene (TCE) (28 percent); tetrachloro-ethene (PCE) (19 percent); methyl tert-butyl ether (MTBE) (14 percent); 1,1-dichloroethane (11 percent); and 1,1,1-trichloroethane (TCA) (11 percent). These VOCs were also the most frequently detected VOCs in ground water representative of a wide range of hydrologically conditions in urban areas nationwide. Only two VOCs (TCE and PCE) exceeded state and federal primary maximum contaminant levels (MCL) for drinking water in a total of seven samples. Because samples were collected prior to water treatment, sample concentrations do not represent the concentrations entering the drinking-water system.Ground water containing VOCs may be considered to be a tracer of postindustrial-aged water-water that was recharged after the onset of intense urban development. The overall distribution of VOC detections is related to the hydrological and the engineered recharge facilities in the Coastal Los Angeles Basin and the Coastal Santa Ana Basin that comprise the Los Angeles physiographic basin. Most of the ground-water recharge occurs at engineered recharge facilities in the generally coarse-grained northeastern parts of the study area (forebay areas). Ground-water recharge from the land surface is minimal in the southwestern part of the basins, distal from the recharge facilities, where clay layers impede the vertical migration of ground water (pressure areas).VOCs are not uniformly distributed over the study area. Most of the wells with multiple VOC detections, which also have the highest concentrations, are in the forebay areas and are clustered proximal to the recharge facilities. In addition, the number of VOC detections and VOC concentrations decrease beyond about 10-15 kilometers from the recharge facilities. The distribution of individual VOCs is also related to their history of use. MTBE traces ground water recharged during about the last decade and is detected almost exclusively in the forebay areas. Chloroform, which has been used since the 1920s, is more widely distributed and is detected at the greatest distances from the recharge facilities.Downward migration of VOCs from the land surface may be a viable process for VOCs to reach aquifers in parts of the forebay areas, but there is little indication that the same process is active in the pressure area. The lack of contrast in the number of VOC detections between wells of different depths over most of the study area suggests that the downward migration from the land surface is not a dominant pathway for VOCs to travel to the capture zones of public supply wells. Isolated occurrences of multiple VOC detections and high concentrations of VOCs in individual wells may indicate rapid vertical transport from a localized source. Stable isotope data indicate that ground water containing VOCs is a mixture of local precipitation and runoff with water that is isotopically lighter (more negative) than the local sources. The isotopically lighter water could either be Colorado River water or State Water Project water, both of which are imported to the basin and used as a source of recharge to the ground-water flow system. The stable isotope data support the interpretation that VOCs in ground water are associated with the engineered recharge facilities.Two of the most frequently detecte","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri20014188","collaboration":"Prepared in cooperation with the California State Water Resources Control Board","usgsCitation":"Shelton, J.L., Burow, K.R., Belitz, K., Dubrovsky, N.M., Land, M., and Gronberg, J., 2001, Low-Level Volatile Organic Compounds in Active Public Supply Wells as Ground-Water Tracers in the Los Angeles Physiographic Basin, California, 2000: U.S. Geological Survey Water-Resources Investigations Report 2001-4188, 35 p., https://doi.org/10.3133/wri20014188.","productDescription":"35 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":159932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11336,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ca.water.usgs.gov/archive/reports/wrir014188/","linkFileType":{"id":5,"text":"html"}},{"id":21876,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/2001/wri014188/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.66666666666667,33.5 ], [ -118.66666666666667,34.166666666666664 ], [ -117.58333333333333,34.166666666666664 ], [ -117.58333333333333,33.5 ], [ -118.66666666666667,33.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640e46","contributors":{"authors":[{"text":"Shelton, Jennifer L. 0000-0001-8508-0270 jshelton@usgs.gov","orcid":"https://orcid.org/0000-0001-8508-0270","contributorId":1155,"corporation":false,"usgs":true,"family":"Shelton","given":"Jennifer","email":"jshelton@usgs.gov","middleInitial":"L.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burow, Karen R. 0000-0001-6006-6667 krburow@usgs.gov","orcid":"https://orcid.org/0000-0001-6006-6667","contributorId":1504,"corporation":false,"usgs":true,"family":"Burow","given":"Karen","email":"krburow@usgs.gov","middleInitial":"R.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Belitz, Kenneth 0000-0003-4481-2345 kbelitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4481-2345","contributorId":442,"corporation":false,"usgs":true,"family":"Belitz","given":"Kenneth","email":"kbelitz@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204456,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dubrovsky, Neil M. 0000-0001-7786-1149 nmdubrov@usgs.gov","orcid":"https://orcid.org/0000-0001-7786-1149","contributorId":1799,"corporation":false,"usgs":true,"family":"Dubrovsky","given":"Neil","email":"nmdubrov@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204459,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Land, Michael 0000-0001-5141-0307","orcid":"https://orcid.org/0000-0001-5141-0307","contributorId":56613,"corporation":false,"usgs":true,"family":"Land","given":"Michael","affiliations":[],"preferred":false,"id":204461,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gronberg, JoAnn","contributorId":41866,"corporation":false,"usgs":true,"family":"Gronberg","given":"JoAnn","affiliations":[],"preferred":false,"id":204460,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":31386,"text":"ofr01199 - 2001 - Preliminary Precambrian basement map showing geologic-geophysical domains, Wyoming","interactions":[],"lastModifiedDate":"2021-11-03T18:25:18.129346","indexId":"ofr01199","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-199","title":"Preliminary Precambrian basement map showing geologic-geophysical domains, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01199","usgsCitation":"Sims, P., Finn, C., and Rystrom, V., 2001, Preliminary Precambrian basement map showing geologic-geophysical domains, Wyoming: U.S. Geological Survey Open-File Report 2001-199, HTML Document, https://doi.org/10.3133/ofr01199.","productDescription":"HTML Document","costCenters":[],"links":[{"id":163375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110199,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_42121.htm","linkFileType":{"id":5,"text":"html"},"description":"42121"},{"id":3060,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr-01-0199/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.0498046875,\n              41.0130657870063\n            ],\n            [\n              -104.0625,\n              41.02964338716638\n            ],\n            [\n              -104.051513671875,\n              45.01141864227728\n            ],\n            [\n              -111.082763671875,\n              45.00365115687186\n            ],\n            [\n              -111.0498046875,\n              41.0130657870063\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e496","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":205855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Finn, C. A. 0000-0002-6178-0405","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":93917,"corporation":false,"usgs":true,"family":"Finn","given":"C. A.","affiliations":[],"preferred":false,"id":205857,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rystrom, V. L.","contributorId":41484,"corporation":false,"usgs":true,"family":"Rystrom","given":"V. L.","affiliations":[],"preferred":false,"id":205856,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30960,"text":"wri014184 - 2001 - Occurrence and distribution of organochlorine pesticides, polychlorinated biphenyls, and trace elements in fish tissue in the lower Tennessee River basin, 1980-98","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"wri014184","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4184","title":"Occurrence and distribution of organochlorine pesticides, polychlorinated biphenyls, and trace elements in fish tissue in the lower Tennessee River basin, 1980-98","docAbstract":"The U.S. Geological Survey, as part of the National Water-Quality Assessment Program, evaluated the occurrence and distribution of organochlorine pesticides, polychlorinated biphenyls, and trace elements in fish tissue in samples collected in the lower Tennessee River Basin study unit. Fish tissue analysis provides a time-averaged measurement of contaminants as well as a direct measurement of the contaminants that bioaccumulate in fish tissue. Bioaccumulation of contaminants in fish tissue may result in concentrations that can affect human, wildlife, or aquatic health. Data for two types of tissue analyses were evaluated to assess the occurrence and distribution of contaminants: whole fish for organochlorine pesticides and polychlorinated biphenyls and fish fillets for organochlorine pesticides, polychlorinated biphenyls, and trace elements. The fish tissue data analyzed for this study cover an 18-year span including data collected in 1998 by the U.S. Geological Survey as part of the National Water-Quality Assessment Program; data collected from 1980 through 1997 by the Tennessee Valley Authority; and data collected from 1992 through 1997 by the Tennessee Department of Environment and Conservation. Concentration data for constituents that are on the U.S. Environmental Protection Agency Priority Pollutant List were summarized and compared against existing action levels or guidelines.From the list of organochlorine pesticide compounds analyzed, p,p'-dichlorodiphenyldichloroethylene (p,p'-DDE), a breakdown product of dichlorodiphenyltrichloroethane (DDT), was the most commonly detected compound with detections at 83 percent of the sites sampled. Eleven p,p'-DDE samples exceeded action levels or guidelines with concentrations ranging from 0.20 to 12.8 milligrams per kilogram. Five other organochlorine compounds, p,p'-dichlorodiphenyldichloroethane (p,p'-DDD), dieldrin, endrin, chlordane, and polychlorinated biphenyls, also exceeded action levels and guidelines, but the detection frequencies at sampling sites generally were less than 70 percent. Mercury, the only trace element to exceed a guideline, was detected at 51 of 102 sites sampled for trace elements. Selenium was detected in fish fillet samples from 70 of 102 sites sampled, which was more sites than for any other trace element; however, selenium did not exceed the 50 micrograms per gram U.S. Environmental Protection Agency screening criteria. Arsenic and cadmium also were detected at 44 and 54 percent of the sampling sites, respectively.","language":"ENGLISH","doi":"10.3133/wri014184","usgsCitation":"Knight, R., and Powell, J., 2001, Occurrence and distribution of organochlorine pesticides, polychlorinated biphenyls, and trace elements in fish tissue in the lower Tennessee River basin, 1980-98: U.S. Geological Survey Water-Resources Investigations Report 2001-4184, 32 p. , https://doi.org/10.3133/wri014184.","productDescription":"32 p. ","costCenters":[],"links":[{"id":2942,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014184","linkFileType":{"id":5,"text":"html"}},{"id":159931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69632e","contributors":{"authors":[{"text":"Knight, R.R.","contributorId":59063,"corporation":false,"usgs":true,"family":"Knight","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":204454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, J.R.","contributorId":85134,"corporation":false,"usgs":true,"family":"Powell","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":204455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30969,"text":"wri014224 - 2001 - Ground-water levels and flow directions in glacial sediments and carbonate bedrock near Tremont City, Ohio, October-November 2000","interactions":[],"lastModifiedDate":"2019-04-22T09:20:55","indexId":"wri014224","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4224","displayTitle":"Ground-Water Levels and Flow Directions in Glacial Sediments and Carbonate Bedrock Near Tremont City, Ohio, October-November 2000","title":"Ground-water levels and flow directions in glacial sediments and carbonate bedrock near Tremont City, Ohio, October-November 2000","docAbstract":"<h1>Introduction</h1><p>During summer 2000, the U.S. Environmental Protection Agency (USEPA) began an investigation of the Tremont City Landfill Site near Tremont City, Ohio. The site is about 1 mile west of Tremont City, just south of the Clark-Champaign County line. The closed site consists of three main areas: an 8.5-acre barrel fill, a 14-acre waste-transfer area, and a 58-acre landfill. The local hydrogeology is complex, and multiple ground-water-flow directions at the site have been described; however, offsite ground-water levels and flow directions were poorly defined, because they were based on static water levels reported over many years by well drillers. In October 2000, the U.S. Geological Survey (USGS), in cooperation with the USEPA, measured water levels in residential and onsite monitoring wells to prepare a map of the potentiometric surface so that directions of regional ground-water flow could be better delineated in the vicinity of the site.</p><p>The topography of the study area (extent of map) is characterized by a nearly level till plain with minor relief along incised streams draining east-southeast to the Mad River. The Tremont City Landfill Site is in an upland area between two east-southeast-trending streams. Storms Creek is about 1 mile north of the site. The southern extent of the landfill is within about 500 feet of Chapman creek.</p><p>The surficial geology of the study area consists of unconsolidated glacial sediments that overlie Silurian-age Lockport Dolomite. These glacial sediments consist of fine-grained till interbedded with layers of silt, sands, and gravels. Sand and gravel layers are commonly found just above the bedrock surface. Onsite monitoring wells have been installed into several thin, permeable zones in the glacial sediments. Most residential wells in the area produce sufficient water for residential use (as much as 100 gallons per minute), from either sand and gravel layers in the glacial sediments or from the carbonate bedrock. The most productive aquifer in the area is the highly permeable glacial outwash in the buried bedrock valley beneath the Mad River. These outwash sands and gravels can yield more than 1,000 gallons per minute. If weathered, the Lockport Dolomite can be a productive source of water near the top of the unit.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014224","usgsCitation":"Dumouchelle, D.H., 2001, Ground-water levels and flow directions in glacial sediments and carbonate bedrock near Tremont City, Ohio, October-November 2000: U.S. Geological Survey Water-Resources Investigations Report 2001-4224, Report: 39.28 x 28.99 in., https://doi.org/10.3133/wri014224.","productDescription":"Report: 39.28 x 28.99 in.","costCenters":[],"links":[{"id":2949,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4224/wri20014224.pdf","text":"Report","size":"747 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2001-4224"},{"id":159966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2001/4224/coverthb.jpg"}],"country":"United States","state":"Ohio","otherGeospatial":"Tremont City","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.8446307182312,\n              40.00634956420027\n            ],\n            [\n              -83.82637023925781,\n              40.00634956420027\n            ],\n            [\n              -83.82637023925781,\n              40.01803456129624\n            ],\n            [\n              -83.8446307182312,\n              40.01803456129624\n            ],\n            [\n              -83.8446307182312,\n              40.00634956420027\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"dc_oh@usgs.gov\" data-mce-href=\"dc_oh@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/oki-water/\" data-mce-href=\"https://www.usgs.gov/centers/oki-water/\">Ohio Water Science Center</a><br>U.S. Geological Survey<br>6460 Busch Blvd. <br>Columbus, OH 43229</p>","tableOfContents":"<ul><li>Introduction</li><li>Methods of Investigation</li><li>Ground-Water Levels and Flow Directions</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668b3e","contributors":{"authors":[{"text":"Dumouchelle, Denise H. ddumouch@usgs.gov","contributorId":1847,"corporation":false,"usgs":true,"family":"Dumouchelle","given":"Denise","email":"ddumouch@usgs.gov","middleInitial":"H.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30967,"text":"wri014212 - 2001 - Vertical profiles of streambed hydraulic conductivity determined using slug tests in central and western Nebraska","interactions":[],"lastModifiedDate":"2014-04-09T15:26:43","indexId":"wri014212","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4212","title":"Vertical profiles of streambed hydraulic conductivity determined using slug tests in central and western Nebraska","docAbstract":"Many issues of water-resources management\nrely on modeling of ground-water/surfacewater\ninteractions, and streambed hydraulic\nconductivity is a key parameter controlling the\nwater fluxes across the stream/aquifer interface.\nHowever, in central and western Nebraska, this\nparameter is generally undefined. The U.S.\nGeological Survey, in cooperation with the\nNebraska Platte River Cooperative Hydrology\nStudy Group, performed slug tests at 15 stream\nsites in the Platte, Republican, and Little Blue\nRiver watersheds to determine the hydraulic\nconductivity of streambeds in central and western\nNebraska. Slug tests were completed at several\ndiscrete depth intervals using pneumatic or\nmechanical methods, and the water-level response\nwas monitored on site using a pressure transducer\nand laptop computer. Responses were analyzed\nusing either the Bouwer and Rice or Springer and\nGelhar methods. Vertical profiles of hydraulic\nconductivity with depth were developed and were\ncompared to available information on lithology.\nThe profiles and corresponding lithology\nshowed that different types of streambeds were\ntested and suggested that some streambeds\ndisplay a large variability in hydraulic conductivity\nwith depth. In some cases, hydraulic\nconductivity values associated with nonstreambed\nmaterials could be identified from nearby\nlithologic descriptions. Seven of 15 sites had\nstreambed values that ranged over more than\n3 orders of magnitude, and that variability\nincreased significantly when the measurements\nconsidered to be from nonstreambed materials\nwere included. Streambed profiles from the Platte\nand South Platte River sites generally were more\nhomogeneous and of larger hydraulic conductivity\nthan the other sites. No restrictive layers\nwere detected at any of the streambed sites on the\nmain stems or the flood plains of the main stems\nof their respective watersheds. Alternatively, the\nprofiles characterized by a restrictive streambed\nlayer at some depth below the streambed surface\nwere all from tributary sites out of the main-stem\nflood plain. These profiles can be used to represent\nthe streambed hydraulic conductivity in\ncentral and western Nebraska in various applications,\nincluding modeling ground-water/surfacewater\ninteractions.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lincoln, NB","doi":"10.3133/wri014212","collaboration":"Prepared in cooperation with the Nebraska Platte River Cooperative Hydrology Study Group","usgsCitation":"Rus, D.L., McGuire, V.L., Zurbuchen, B.R., and Zlotnik, V.A., 2001, Vertical profiles of streambed hydraulic conductivity determined using slug tests in central and western Nebraska: U.S. Geological Survey Water-Resources Investigations Report 2001-4212, iv, 32 p., https://doi.org/10.3133/wri014212.","productDescription":"iv, 32 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":159964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri014212.jpg"},{"id":286071,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4212/report.pdf"}],"scale":"2000000","datum":"North American Datum of 1983","country":"United States","state":"Nebraska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.15,40.15 ], [ -104.15,41.93 ], [ -96.83,41.93 ], [ -96.83,40.15 ], [ -104.15,40.15 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60212a","contributors":{"authors":[{"text":"Rus, David L. 0000-0003-3538-7826 dlrus@usgs.gov","orcid":"https://orcid.org/0000-0003-3538-7826","contributorId":881,"corporation":false,"usgs":true,"family":"Rus","given":"David","email":"dlrus@usgs.gov","middleInitial":"L.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGuire, Virginia L. 0000-0002-3962-4158 vlmcguir@usgs.gov","orcid":"https://orcid.org/0000-0002-3962-4158","contributorId":404,"corporation":false,"usgs":true,"family":"McGuire","given":"Virginia","email":"vlmcguir@usgs.gov","middleInitial":"L.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zurbuchen, Brian R.","contributorId":81531,"corporation":false,"usgs":true,"family":"Zurbuchen","given":"Brian","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":204480,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zlotnik, Vitaly A.","contributorId":19985,"corporation":false,"usgs":true,"family":"Zlotnik","given":"Vitaly","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204479,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31375,"text":"ofr01154 - 2001 - Sea-floor photography from the Continental Margin Program: A pictorial survey of benthic character and habitats along the U.S. East Coast","interactions":[],"lastModifiedDate":"2024-08-20T13:17:46.124221","indexId":"ofr01154","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-154","title":"Sea-floor photography from the Continental Margin Program: A pictorial survey of benthic character and habitats along the U.S. East Coast","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01154","usgsCitation":"Paskevich, V., Poppe, L., Hastings, M., and Hathaway, J., 2001, Sea-floor photography from the Continental Margin Program: A pictorial survey of benthic character and habitats along the U.S. East Coast: U.S. Geological Survey Open-File Report 2001-154, HTML Dcoument, https://doi.org/10.3133/ofr01154.","productDescription":"HTML Dcoument","costCenters":[],"links":[{"id":3051,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/of01-154/","linkFileType":{"id":5,"text":"html"}},{"id":164096,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc579","contributors":{"authors":[{"text":"Paskevich, V.F.","contributorId":96285,"corporation":false,"usgs":true,"family":"Paskevich","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":205819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poppe, L.J.","contributorId":72782,"corporation":false,"usgs":true,"family":"Poppe","given":"L.J.","affiliations":[],"preferred":false,"id":205817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hastings, M. E.","contributorId":72012,"corporation":false,"usgs":true,"family":"Hastings","given":"M. E.","affiliations":[],"preferred":false,"id":205816,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hathaway, J.C.","contributorId":94280,"corporation":false,"usgs":true,"family":"Hathaway","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":205818,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31387,"text":"ofr01217 - 2001 - Mississippi Basin Carbon Project: Upland soil database for sites in Nishnabotna River basin, Iowa","interactions":[],"lastModifiedDate":"2025-01-14T17:14:45.824757","indexId":"ofr01217","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-217","title":"Mississippi Basin Carbon Project: Upland soil database for sites in Nishnabotna River basin, Iowa","docAbstract":"<p>The conversion of land from its native state to an agricultural use commonly results in a significant loss of soil carbon (Mann, 1985; Davidson and Ackerman, 1993). Globally, this loss is estimated to account for as much as 1/3 of the net CO<sub>2</sub> emissions for the period of 1850 to 1980 (Houghton and others, 1983). Roughly 20 to 40 percent of original soil carbon is estimated to be lost as CO<sub>2</sub> as a result of agricultural conversion, or \"decomposition enhancement\". Global models use this estimate along with land conversion data to provide agricultural contributions of CO<sub>2</sub> emissions for global carbon budgets (Houghton and others, 1983; Schimel, 1995).</p>\n<br/>\n<p>Soil erosion rates are significantly (10X) higher on croplands than on their undisturbed equivalents (Dabney and others, 1997). Most of the concern over erosion is related to diminished productivity of the uplands (Stallings, 1957; McGregor and others, 1969; Rhoton, 1990) or to increased hazards and navigability of the lowlands in the late 1800's to early 1900's. Yet because soil carbon is concentrated at the soil surface, with an exponential decline in concentration with depth (Harden et al, 1999), it is clear that changes in erosion rates seen on croplands must also impact soil carbon storage and terrestrial carbon budgets as well.</p>\n<br/>\n<p>As yet, erosional losses of carbon are not included in global carbon budgets explicitly as a factor in land conversion nor implicitly as a portion of the decomposition enhancement. However, recent work by Lal and others (1995) and by Stallard (1998) suggests that significant amounts of eroded soil may be stored in man-made reservoirs and depositional environments as a result of agricultural conversion. Moreover, Stallard points out that eroding soils have the potential for replacing part of the carbon trapped in man-made reservoirs. If true, then the global carbon budget may grossly underestimate or ignore a significant sink term resulting from the burial of eroded soil.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01217","usgsCitation":"Harden, J., Fries, T.L., Haughy, R., Kramer, L., and Zheng, S., 2001, Mississippi Basin Carbon Project: Upland soil database for sites in Nishnabotna River basin, Iowa: U.S. Geological Survey Open-File Report 2001-217, 17 p., https://doi.org/10.3133/ofr01217.","productDescription":"17 p.","numberOfPages":"17","additionalOnlineFiles":"Y","costCenters":[{"id":5055,"text":"Land Change Science","active":true,"usgs":true}],"links":[{"id":466226,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43374.htm","text":"Deep Loess Research Station site near Treynor, Iowa","linkFileType":{"id":5,"text":"html"}},{"id":3061,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0217/","linkFileType":{"id":5,"text":"html"}},{"id":408266,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_43373.htm","text":"Dinesen Prairie site near Harlan, Iowa","linkFileType":{"id":5,"text":"html"}},{"id":282573,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0217/pdf/of01-217text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163376,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"Nishnabotna River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.367,\n              41.6330\n            ],\n            [\n              -95.283,\n              41.6330\n            ],\n            [\n              -95.283,\n              41.667\n            ],\n            [\n              -95.367,\n              41.667\n            ],\n            [\n              -95.367,\n              41.6330\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b85","contributors":{"authors":[{"text":"Harden, J.W. 0000-0002-6570-8259","orcid":"https://orcid.org/0000-0002-6570-8259","contributorId":38585,"corporation":false,"usgs":true,"family":"Harden","given":"J.W.","affiliations":[],"preferred":false,"id":205861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fries, T. L.","contributorId":12053,"corporation":false,"usgs":true,"family":"Fries","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haughy, R.","contributorId":73253,"corporation":false,"usgs":true,"family":"Haughy","given":"R.","email":"","affiliations":[],"preferred":false,"id":205862,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kramer, L.","contributorId":14365,"corporation":false,"usgs":true,"family":"Kramer","given":"L.","affiliations":[],"preferred":false,"id":205859,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zheng, Shuhui","contributorId":29490,"corporation":false,"usgs":true,"family":"Zheng","given":"Shuhui","email":"","affiliations":[],"preferred":false,"id":205860,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":44993,"text":"wri014234 - 2001 - Estimates of evapotranspiration from the Ruby Lake National Wildlife Refuge area, Ruby Valley, northeastern Nevada, May 1999–October 2000","interactions":[],"lastModifiedDate":"2022-01-18T22:27:05.675435","indexId":"wri014234","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4234","title":"Estimates of evapotranspiration from the Ruby Lake National Wildlife Refuge area, Ruby Valley, northeastern Nevada, May 1999–October 2000","docAbstract":"The Ruby Lake National Wildlife Refuge in Ruby Valley, Nevada, contains the largest area of perennial wetlands in northeastern Nevada and provides habitat to a large number of migratory and nesting waterfowl. The long-term preservation of the refuge depends on the availability of sufficient water to maintain optimal habitat conditions. In the Ruby Valley water budget, evapotranspiration (ET) from the refuge is one of the largest components of natural outflow. To help determine the amount of inflow needed to maintain wetland habitat, estimates of ET for May 1999 through October 2000 were made at major habitats throughout the refuge.\r\n\r\nThe Bowen-ratio method was used to estimate daily ET at four sites: over open water, in a moderate-to-dense cover of bulrush marsh, in a moderate cover of mixed phreatophytic shrubs, and in a desert-shrub upland. The eddy-correlation method was used to estimate daily ET for periods of 2 to 12 weeks at a meadow site and at four sites in a sparse-to-moderate cover of phreatophytic shrubs. Daily ET rates ranged from less than 0.010 inch per day at all of the sites to a maximum of 0.464 inch per day at the open-water site. Average daily ET rates estimated for open water and a bulrush marsh were about four to five times greater than in areas of mixed phreatophytic shrubs, where the depth to ground water is less than 5 feet. Based on the seasonal distribution of major habitats in the refuge and on winter and summer ET rates, an estimated total of about 89,000 acre-feet of water was consumed by ET during October 1999-September 2000 (2000 water year). Of this total, about 49,800 acre-feet was consumed by ET in areas of open water and bulrush marsh.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri014234","usgsCitation":"Berger, D.L., Johnson, M.J., Tumbusch, M.L., and Mackay, J., 2001, Estimates of evapotranspiration from the Ruby Lake National Wildlife Refuge area, Ruby Valley, northeastern Nevada, May 1999–October 2000: U.S. Geological Survey Water-Resources Investigations Report 2001-4234, vi, 38 p., https://doi.org/10.3133/wri014234.","productDescription":"vi, 38 p.","costCenters":[],"links":[{"id":162898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3865,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri014234","linkFileType":{"id":5,"text":"html"}},{"id":394482,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_45205.htm"}],"country":"United States","state":"Nevada","otherGeospatial":"Ruby Lake National Wildlife Refuge area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.5370,\n              40.0330\n            ],\n            [\n              -115.25,\n              40.0330\n            ],\n            [\n              -115.25,\n              40.342\n            ],\n            [\n              -115.5370,\n              40.342\n            ],\n            [\n              -115.5370,\n              40.0330\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcafe","contributors":{"authors":[{"text":"Berger, David L. dlberger@usgs.gov","contributorId":1861,"corporation":false,"usgs":true,"family":"Berger","given":"David","email":"dlberger@usgs.gov","middleInitial":"L.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":230866,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Michael J. johnsonm@usgs.gov","contributorId":2282,"corporation":false,"usgs":true,"family":"Johnson","given":"Michael","email":"johnsonm@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":230867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tumbusch, Mary L.","contributorId":37377,"corporation":false,"usgs":true,"family":"Tumbusch","given":"Mary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":230869,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mackay, Jeffrey","contributorId":26577,"corporation":false,"usgs":true,"family":"Mackay","given":"Jeffrey","email":"","affiliations":[],"preferred":false,"id":230868,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":31406,"text":"ofr01293 - 2001 - Geologic map of the Telegraph Peak 7.5' quadrangle, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-06-27T13:15:00.600212","indexId":"ofr01293","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-293","title":"Geologic map of the Telegraph Peak 7.5' quadrangle, San Bernardino County, California","docAbstract":"Open-File Report OF 01-293 contains a digital geologic map database of the Telegraph Peak 7.5’ quadrangle, San Bernardino County, California that includes:\n\nARC/INFO (Environmental Systems Research Institute, http://www.esri.com) version 7.2.1 double precision coverages of the various elements of the geologic map.\nA PostScript file to plot the geologic map on a topographic base, and containing a Correlation of Map Units diagram, a Description of Map Units, an index map, and a regional structure map.\nPortable Document Format (.pdf) files of:\na. This Readme; includes in Appendix I, data contained in fif_met.txt\n\nb. The same graphic as plotted in 2 above. Test plots have not produced 1:24,000-scale map sheets. Adobe Acrobat pagesize setting influences map scale.\n\nThe Correlation of Map Units and Description of Map Units is in the editorial format of USGS Miscellaneous Investigations Series (I-series) maps but has not been edited to comply with I-map standards. Within the geologic map data package, map units are identified by standard geologic map criteria such as formation-name, age, and lithology. Even though this is an author-prepared report, every attempt has been made to closely adhere to the stratigraphic nomenclature of the U. S. Geological Survey. Descriptions of units can be obtained by viewing or plotting the .pdf file (3b above) or plotting the postscript file (2 above). If roads in some areas, especially forest roads that parallel topographic contours, do not show well on plots of the geologic map, we recommend use of the USGS Telegraph Peak 7.5’ topographic quadrangle in conjunction with the geologic map.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr01293","usgsCitation":"Morton, D.M., Woodburne, M., Foster, J.H., Morton, G., and Cossette, P., 2001, Geologic map of the Telegraph Peak 7.5' quadrangle, San Bernardino County, California: U.S. Geological Survey Open-File Report 2001-293, Report: 21 p.; 1 Plate: 41.36 x 30.57 inches; Metadata: TXT file; Database: TAR.GZ file; Map: PS.GZ file, https://doi.org/10.3133/ofr01293.","productDescription":"Report: 21 p.; 1 Plate: 41.36 x 30.57 inches; Metadata: TXT file; Database: TAR.GZ file; Map: PS.GZ file","numberOfPages":"21","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":160364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01293.jpg"},{"id":282694,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0293/tel.tar.gz","linkFileType":{"id":6,"text":"zip"}},{"id":282691,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2001/0293/pdf/TelReadme.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282693,"rank":5,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0293/tel_met.txt","linkFileType":{"id":2,"text":"txt"}},{"id":282692,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0293/pdf/tel_map.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2523,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0293/","linkFileType":{"id":5,"text":"html"}},{"id":282695,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0293/tel_map.ps.gz","linkFileType":{"id":6,"text":"zip"}}],"scale":"24000","projection":"Lambert conformal conic projection","country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5,34.125 ], [ -117.5,35.25 ], [ -117.375,35.25 ], [ -117.375,34.125 ], [ -117.5,34.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a19f","contributors":{"authors":[{"text":"Morton, D. M.","contributorId":54608,"corporation":false,"usgs":true,"family":"Morton","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woodburne, M.O.","contributorId":63228,"corporation":false,"usgs":true,"family":"Woodburne","given":"M.O.","affiliations":[],"preferred":false,"id":205906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foster, J. H.","contributorId":52786,"corporation":false,"usgs":true,"family":"Foster","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":205904,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morton, Gregory","contributorId":103356,"corporation":false,"usgs":true,"family":"Morton","given":"Gregory","email":"","affiliations":[],"preferred":false,"id":205907,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cossette, P. M. 0000-0002-9608-6595","orcid":"https://orcid.org/0000-0002-9608-6595","contributorId":36586,"corporation":false,"usgs":true,"family":"Cossette","given":"P. M.","affiliations":[],"preferred":false,"id":205903,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":31409,"text":"ofr01311 - 2001 - Geologic map of the Cucamonga Peak 7.5' quadrangle, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-06-26T19:00:33.990191","indexId":"ofr01311","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","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":"2001-311","title":"Geologic map of the Cucamonga Peak 7.5' quadrangle, San Bernardino County, California","docAbstract":"<p>Open-File Report OF 01-311 contains a digital geologic map database of the Cucamonga Peak 7.5’ quadrangle, San Bernardino County, California that includes:</p>\n<br/>\n<p>1. ARC/INFO (Environmental Systems Research Institute, http://www.esri.com) version 7.2.1 coverages of the various elements of the geologic map<br/>\n2. A PostScript file to plot the geologic map on a topographic base, and containing a Correlation of Map Units diagram, a Description of Map Units, an index map, and a regional structure map<br/>\n3. Portable Document Format (.pdf) files of:<br/>\na. This Readme; includes in Appendix I, data contained in fif_met.txt<br/>\n\nb. The same graphic as plotted in 2 above. (Test plots have not produced 1:24,000-scale map sheets. Adobe Acrobat pagesize setting influences map scale.)</p>\n<br/>\n<p>The Correlation of Map Units and Description of Map Units is in the editorial format of USGS Miscellaneous Investigations Series (I-series) maps but has not been edited to comply with I-map standards. Within the geologic map data package, map units are identified by standard geologic map criteria such as formation-name, age, and lithology. Even though this is an author-prepared report, every attempt has been made to closely adhere to the stratigraphic nomenclature of the U. S. Geological Survey. Descriptions of units can be obtained by viewing or plotting the .pdf file (3b above) or plotting the postscript file (2 above). If roads in some areas, especially forest roads that parallel topographic contours, do not show well on plots of the geologic map, we recommend use of the USGS Cucamonga Peak 7.5’ topographic quadrangle in conjunction with the geologic map.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01311","collaboration":"Prepared in cooperation with the U.S. Forest Service (San Bernardino National Forest) and the California Division of Mines and Geology","usgsCitation":"Morton, D.M., Matti, J.C., Koukladas, C., and Cossette, P., 2001, Geologic map of the Cucamonga Peak 7.5' quadrangle, San Bernardino County, California: U.S. Geological Survey Open-File Report 2001-311, Map: 41.31 x 20.50 inches; Readme: 22 p.; Metadata, Database package; Map: PostScript file, https://doi.org/10.3133/ofr01311.","productDescription":"Map: 41.31 x 20.50 inches; Readme: 22 p.; Metadata, Database package; Map: PostScript file","numberOfPages":"22","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":160380,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr01311.jpg"},{"id":282745,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0311/cuc_map.ps.gz","linkFileType":{"id":4,"text":"shapefile"}},{"id":2525,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/0311/","linkFileType":{"id":5,"text":"html"}},{"id":282741,"rank":6,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2001/0311/pdf/CucReadme.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282744,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2001/0311/pdf/cuc_map.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":282742,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2001/0311/cuc_met.txt","linkFileType":{"id":2,"text":"txt"}},{"id":282743,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2001/0311/cuc.tar.gz","linkFileType":{"id":4,"text":"shapefile"}}],"scale":"24000","projection":"Lambert conformal conic projection","country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Cucamonga Peak","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.625,34.125 ], [ -117.625,34.25 ], [ -117.5,34.25 ], [ -117.5,34.125 ], [ -117.625,34.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69895d","contributors":{"authors":[{"text":"Morton, D. M.","contributorId":54608,"corporation":false,"usgs":true,"family":"Morton","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":205916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matti, J. C.","contributorId":51712,"corporation":false,"usgs":true,"family":"Matti","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":205915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koukladas, Catherine","contributorId":6759,"corporation":false,"usgs":true,"family":"Koukladas","given":"Catherine","email":"","affiliations":[],"preferred":false,"id":205913,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cossette, P. M. 0000-0002-9608-6595","orcid":"https://orcid.org/0000-0002-9608-6595","contributorId":36586,"corporation":false,"usgs":true,"family":"Cossette","given":"P. M.","affiliations":[],"preferred":false,"id":205914,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":30951,"text":"wri014004 - 2001 - Evaluation of borehole geophysical logs and hydraulic tests, phase III, at AIW Frank/Mid-County Mustang Superfund Site, Chester County, Pennsylvania","interactions":[],"lastModifiedDate":"2018-02-26T15:54:57","indexId":"wri014004","displayToPublicDate":"2002-01-01T00:00:00","publicationYear":"2001","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4004","title":"Evaluation of borehole geophysical logs and hydraulic tests, phase III, at AIW Frank/Mid-County Mustang Superfund Site, Chester County, Pennsylvania","docAbstract":"<p>Borehole geophysical logs, heatpulse-flowmeter measurements, and aquifer-isolation tests were used to characterize the ground-water-flow system at the AIW Frank/Mid-County Mustang Superfund Site. The site is underlain by fractured carbonate rocks. Caliper, natural-gamma, single-point-resistance, fluid-resistivity, and fluid-temperature logs were run in six wells, and an acoustic borehole televiewer and borehole deviation log was run in one well. The direction and rate of borehole-fluid movement was measured with a high-resolution heatpulse flowmeter for both nonpumping and pumping conditions in four wells. The heatpulse-flowmeter measurements showed flow within the borehole during nonpumping conditions in three of the four wells tested. Flow rates up to 1.4 gallons per minute were measured. Flow was upward in one well and both upward and downward in two wells. Aquifer-isolation (packer) tests were conducted in four wells to determine depth-discrete specific capacity values, to obtain depth-discrete water samples, and to determine the effect of pumping an individual fracture or fracture zone in one well on water levels in nearby wells. Water-level data collected during aquifer-isolation tests were consistent with and confirmed interpretations of borehole geophysical logs and heatpulse-flowmeter measurements. Seven of the 13 fractures identified as water-producing or water-receiving zones by borehole geophysical methods produced water at a rate equal to or greater than 7.5 gallons per minute when isolated and pumped. The specific capacities of isolated fractures range over three orders of magnitude, from 0.005 to 7.1 gallons per minute per foot. Vertical distribution of specific capacity between land surface and 298 feet below land surface is not related to depth. The four highest specific capacities, in descending order, are at depths of 174-198, 90-92, 118-119, and 34-37 feet below land surface.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri014004","collaboration":"Prepared in cooperation with the Environmental Protection Agency","usgsCitation":"Sloto, R.A., 2001, Evaluation of borehole geophysical logs and hydraulic tests, phase III, at AIW Frank/Mid-County Mustang Superfund Site, Chester County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 2001-4004, vi, 33 p., https://doi.org/10.3133/wri014004.","productDescription":"vi, 33 p.","onlineOnly":"Y","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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href=\"mailto:dc_pa@usgs.gov\" data-mce-href=\"mailto:dc_pa@usgs.gov\">Director</a>, <a href=\"https://pa.water.usgs.gov/\" data-mce-href=\"https://pa.water.usgs.gov/\">Pennsylvania Water Science Center</a><br> U.S. Geological Survey<br> 215 Limekiln Road<br> New Cumberland, PA 17070</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction&nbsp;</li><li>Methods of investigation&nbsp;</li><li>Evaluation of borehole geophysical logs and aquifer-isolation tests</li><li>Evaluation of borehole geophysical logs for well RW-1 (CH-5804)</li><li>Evaluation of borehole geophysical logs for well RW-4 (CH-5807)</li><li>Evaluation of borehole geophysical logs for well OB-5 (CH-5447)&nbsp;</li><li>Summary and conclusions</li><li>References cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60257f","contributors":{"authors":[{"text":"Sloto, Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":204427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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