{"pageNumber":"948","pageRowStart":"23675","pageSize":"25","recordCount":46734,"records":[{"id":72663,"text":"sir20055157 - 2005 - Age and quality of ground water and sources of nitrogen in the surficial aquifers in Pumpkin Creek Valley, western Nebraska, 2000","interactions":[],"lastModifiedDate":"2022-01-05T21:16:12.171314","indexId":"sir20055157","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5157","title":"Age and quality of ground water and sources of nitrogen in the surficial aquifers in Pumpkin Creek Valley, western Nebraska, 2000","docAbstract":"Ground water is the source of drinking water for the residents of Pumpkin Creek Valley, western Nebraska. In this largely agricultural area, shallow aquifers potentially are susceptible to nitrate contamination. During the last 10 years, ground-water levels in the North Platte Natural Resources District have declined and contamination has become a major problem for the district. In 2000, the U.S. Geological Survey and the North Platte Natural Resources District began a cooperative study to determine the age and quality of the ground water and the sources of nitrogen in the aquifers in Pumpkin Creek Valley.\r\n\r\nWater samples were collected from 8 surface-water sites, 2 springs, and 88 ground-water sites during May, July, and August 2000. These samples were analyzed for physical properties, nutrients or nitrate, and hydrogen and oxygen isotopes. In addition, a subset of samples was analyzed for any combination of chlorofluorocarbons, tritium, tritium/helium, sulfur-hexafluoride, carbon-14, and nitrogen-15.\r\n\r\nThe apparent age of ground water in the alluvial aquifer typically varied from about 1980 to modern, whereas ground water in the fractured Brule Formation had a median value in the 1970s. The Brule Formation typically contained ground water that ranged from the 1940s to the 1990s, but low-yield wells had apparent ages of 5,000 to 10,000 years before present. Data for oxygen-18 and deuterium indicated that lake-water samples showed the greatest effects from evaporation. Ground-water data showed no substantial evaporative effects and some ground water became isotopically heavier as the water moved downgradient. In addition, the physical and chemical ground-water data indicate that Pumpkin Creek is a gaining stream because little, if any, of its water is lost to the ground-water system.\r\n\r\nThe water-quality type changed from a sodium calcium bicarbonate type near Pumpkin Creek's headwaters to a calcium sodium bicarbonate type near its mouth. Nitrate concentrations were largest in the alluvial system (median = 5 mg/L) and smallest in the surface-water system (median = 1 mg/L). Most nitrate concentrations exceeding the U.S. Environmental Protection Agency maximum contaminant level for drinking water of 10 mg/L as nitrogen were adjacent to irrigated fields and in areas where alluvial sediments are less than 50 ft thick.\r\n\r\nSources of nitrogen in the ground water of the study area included naturally occurring nitrogen, commercial fertilizer, and animal waste. Based on nitrate concentration and delta nitrogen-15, the nitrogen in 65 percent of the water samples appears to have originated from a mixture of commercial fertilizers and animal waste. Some of the smallest nitrate concentrations in the ground-water samples contained some of the largest delta nitrogen-15 values (greater than 10 per mil), which suggests animal waste as the likely source. Commercial fertilizers were the likely source of most of the nitrogen in water samples with nitrate concentrations that exceeded 10 mg/L. The source of the nitrogen in water samples with nitrate concentrations exceeding 10 mg/L, but with delta nitrogen-15 values close to 10 per mil, could not be determined.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055157","usgsCitation":"Steele, G.V., Cannia, J.C., Sibray, S., and McGuire, V., 2005, Age and quality of ground water and sources of nitrogen in the surficial aquifers in Pumpkin Creek Valley, western Nebraska, 2000: U.S. Geological Survey Scientific Investigations Report 2005-5157, 68 p., https://doi.org/10.3133/sir20055157.","productDescription":"68 p.","costCenters":[],"links":[{"id":192831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393936,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75455.htm"},{"id":7068,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5157/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Pumpkin Creek Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.0525,\n              41.3922\n            ],\n            [\n              -102.9358,\n              41.3922\n            ],\n            [\n              -102.9358,\n              41.8289\n            ],\n            [\n              -104.0525,\n              41.8289\n            ],\n            [\n              -104.0525,\n              41.3922\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689549","contributors":{"authors":[{"text":"Steele, G. V.","contributorId":62543,"corporation":false,"usgs":true,"family":"Steele","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":285838,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cannia, J. C.","contributorId":105258,"corporation":false,"usgs":true,"family":"Cannia","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285841,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sibray, S. S.","contributorId":63048,"corporation":false,"usgs":true,"family":"Sibray","given":"S. S.","affiliations":[],"preferred":false,"id":285839,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGuire, V. L. 0000-0002-3962-4158","orcid":"https://orcid.org/0000-0002-3962-4158","contributorId":94702,"corporation":false,"usgs":true,"family":"McGuire","given":"V. L.","affiliations":[],"preferred":false,"id":285840,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72666,"text":"sir20055221 - 2005 - Baseline water-quality characteristics of the Alaska Army National Guard Stewart River Training Area near Nome, Alaska","interactions":[],"lastModifiedDate":"2016-06-20T15:26:49","indexId":"sir20055221","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5221","title":"Baseline water-quality characteristics of the Alaska Army National Guard Stewart River Training Area near Nome, Alaska","docAbstract":"<p>The Alaska Army National Guard Stewart River Training Area is approximately 23 miles north of Nome on the Seward Peninsula in northwest Alaska. The Stewart River Training Area encompasses much of the Stewart River Basin and a small part of the Snake River Basin. Hydrologic, water-quality, and physical-habitat data were collected at seven surface-water sites within the Stewart River Training Area during the summer runoff months (late-May to early-September) in 2004. Two of the sampling sites selected for this study were on the main stem Stewart River, one at the upstream boundary and one at the downstream boundary of the training area. Continuous hydrologic, precipitation, and water temperature data were collected at these two sites throughout the summer of 2004. Three pond sites, along the upper, middle, and lower reaches of the Stewart River within the training area, were each sampled twice during the summer of 2004 for analysis of water-quality constituents. Two tributaries to the Snake River Basin, Goldbottom Creek and North Fork Snake River, within the Stewart River Training Area boundary, also were sampled twice during the summer of 2004. Water-quality data collected from the Stewart River at the upstream and downstream study sites indicate similar constituent concentrations. Concentrations of most water-quality constituents collected during the summer of 2004 did not exceed standards for drinking water or recreational contact. Analysis of trace-element concentrations in bed sediment samples indicate the threshold effect concentration (below which no adverse effects on organisms is expected) was exceeded for arsenic, chromium, and nickel concentrations at all sample sites within the Stewart River Training Area and cadmium, copper, zinc, and lead concentrations were found to exceed the threshold effect concentration in varying degrees at the sample sites. The probable effect concentration (above which toxic effects on organisms is likely) was exceeded by arsenic concentrations at all sites except the lower pond site. Chromium and nickel concentrations exceeded the probable effect concentration at the upstream Stewart River site and at the North Fork Snake River site.</p>","language":"English","doi":"10.3133/sir20055221","issn":"2328-031X","usgsCitation":"Eash, J.D., 2005, Baseline water-quality characteristics of the Alaska Army National Guard Stewart River Training Area near Nome, Alaska (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5221, 54 p., https://doi.org/10.3133/sir20055221.","productDescription":"54 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":192880,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7070,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5221/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db68774f","contributors":{"authors":[{"text":"Eash, Josh D.","contributorId":100933,"corporation":false,"usgs":true,"family":"Eash","given":"Josh","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285845,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72661,"text":"sim2888 - 2005 - Geologic map of the northern plains of Mars","interactions":[],"lastModifiedDate":"2015-02-09T13:30:19","indexId":"sim2888","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2888","title":"Geologic map of the northern plains of Mars","docAbstract":"<p><span> The northern plains of Mars cover nearly a third of the planet and constitute the planet's broadest region of lowlands. Apparently formed early in Mars' history, the northern lowlands served as a repository both for sediments shed from the adjacent ancient highlands and for volcanic flows and deposits from sources within and near the lowlands. Geomorphic evidence for extensive tectonic deformation and reworking of surface materials through release of volatiles occurs throughout the northern plains. In the polar region, Planum Boreum contains evidence for the accumulation of ice and dust, and surrounding dune fields suggest widespread aeolian transport and erosion. </span></p>\n<p>The most recent regional- and global-scale maps describing the geology of the northern plains are largely based on Viking Orbiter image data (Dial, 1984; Witbeck and Underwood, 1984; Scott and Tanaka, 1986; Greeley and Guest, 1987; Tanaka and Scott, 1987; Tanaka and others, 1992a; Rotto and Tanaka, 1995; Crumpler and others, 2001; McGill, 2002). These maps reveal highland, plains, volcanic, and polar units based on morphologic character, albedo, and relative ages using local stratigraphic relations and crater counts.</p>\n<p><span> This geologic map of the northern plains is the first published map that covers a significant part of Mars using topography and image data from both the Mars Global Surveyor and Mars Odyssey missions. The new data provide a fresh perspective on the geology of the region that reveals many previously unrecognizable units, features, and temporal relations. In addition, we adapted and instituted terrestrial mapping methods and stratigraphic conventions that we think result in a clearer and more objective map. We focus on mapping with the intent of reconstructing the history of geologic activity within the northern plains, including deposition, volcanism, erosion, tectonism, impact cratering, and other processes with the aid of comprehensive crater-density determinations. Mapped areas include all plains regions within the northern hemisphere of Mars, as well as an approximately 300-km-wide strip of cratered highland and volcanic regions, which border the plains. Note that not all of the contiguous northern plains are mapped, because some minor parts of Elysium and Amazonis Planitiae lie south of the equator. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim2888","usgsCitation":"Tanaka, K.L., Skinner, J., and Hare, T.M., 2005, Geologic map of the northern plains of Mars: U.S. Geological Survey Scientific Investigations Map 2888, Map: 57.90 x 42.44 inches; Pamphlet: i, 27 p., https://doi.org/10.3133/sim2888.","productDescription":"Map: 57.90 x 42.44 inches; Pamphlet: i, 27 p.","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":192788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sim2888.jpg"},{"id":297868,"rank":101,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/sim/2005/2888/sim2888.pdf","text":"Map","size":"61.1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Map"},{"id":297869,"rank":102,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/2005/2888/sim2888pamphlet.pdf","text":"Pamphlet","size":"2.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Pamphlet"},{"id":7066,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2888/","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8493","contributors":{"authors":[{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, James A. 0000-0002-3644-7010 jskinner@usgs.gov","orcid":"https://orcid.org/0000-0002-3644-7010","contributorId":3187,"corporation":false,"usgs":true,"family":"Skinner","given":"James A.","email":"jskinner@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hare, Trent M. 0000-0001-8842-389X thare@usgs.gov","orcid":"https://orcid.org/0000-0001-8842-389X","contributorId":3188,"corporation":false,"usgs":true,"family":"Hare","given":"Trent","email":"thare@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285834,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72665,"text":"sir20055212 - 2005 - Instream flow characterization of upper Salmon River basin streams, central Idaho, 2004","interactions":[],"lastModifiedDate":"2014-05-05T14:43:08","indexId":"sir20055212","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5212","title":"Instream flow characterization of upper Salmon River basin streams, central Idaho, 2004","docAbstract":"<p>Anadromous fish populations in the Columbia River Basin have plummeted in the last 100 years. This severe decline led to Federal listing of Chinook salmon (Oncorhynchus tshawytscha) and steelhead trout (Oncorhynchus mykiss) stocks as endangered or threatened under the Endangered Species Act (ESA) in the 1990s. Historically, the upper Salmon River Basin (upstream of the confluence with the Pahsimeroi River) in Idaho provided migration corridors and significant habitat for these ESA-listed species, in addition to the ESA-listed bull trout (Salvelinus confluentus). Human development has modified the original streamflow conditions in many streams in the upper Salmon River Basin. Summer streamflow modifications resulting from irrigation practices, have directly affected quantity and quality of fish habitat and also have affected migration and (or) access to suitable spawning and rearing habitat for these fish.</p>\n<br>\n<p>As a result of these ESA listings and Action 149 of the Federal Columbia River Power System Biological Opinion of 2000, the Bureau of Reclamation was tasked to conduct streamflow characterization studies in the upper Salmon River Basin to clearly define habitat requirements for effective species management and habitat restoration. These studies include collection of habitat and streamflow information for the Physical Habitat Simulation System model, a widely applied method to determine relations between habitat and discharge requirements for various fish species and life stages. Model results can be used by resource managers to guide habitat restoration efforts by evaluating potential fish habitat and passage improvements by increasing streamflow.</p>\n<br>\n<p>In 2004, instream flow characterization studies were completed on Salmon River and Beaver, Pole, Champion, Iron, Thompson, and Squaw Creeks. Continuous streamflow data were recorded upstream of all diversions on Salmon River and Pole, Iron, Thompson, and Squaw Creeks. In addition, natural summer streamflows were estimated for each study site using regional regression equations.</p> \n<br>\n<p>This report describes Physical Habitat Simulation System modeling results for bull trout, Chinook salmon, and steelhead trout during summer streamflows. Habitat/discharge relations were summarized for adult and spawning life stages at each study site. Adult fish passage and discharge relations were evaluated at specific transects identified as a potential low-streamflow passage barrier at each study site.</p> \n<br>\n<p>Continuous summer water temperature data for selected study sites were summarized and compared with Idaho Water Quality Standards and various water temperature requirements of targeted fish species. Continuous summer water temperature data recorded in 2003 and streamflow relations were evaluated for Fourth of July Creek using the Stream Segment Temperature model that simulates mean and maximum daily water temperatures with changes in streamflow.</p>\n<br>\n<p>Results of these habitat studies can be used to prioritize and direct cost-effective actions to improve fish habitat for ESA-listed anadromous and native fish species in the basin. These actions may include acquiring water during critical low-flow periods by leasing or modifying irrigation delivery systems to minimize out-of-stream diversions.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055212","collaboration":"Prepared in cooperation with the Bureau of Reclamation","usgsCitation":"Maret, T.R., Hortness, J., and Ott, D.S., 2005, Instream flow characterization of upper Salmon River basin streams, central Idaho, 2004: U.S. Geological Survey Scientific Investigations Report 2005-5212, Report: ix, 122 p.; Data files, https://doi.org/10.3133/sir20055212.","productDescription":"Report: ix, 122 p.; Data files","numberOfPages":"135","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":192832,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055212.PNG"},{"id":7069,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5212/","linkFileType":{"id":5,"text":"html"}},{"id":286895,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5212/pdf/sir20055212.pdf"},{"id":286896,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/sir/2005/5212/data/"}],"scale":"40000","projection":"Transverse Mercator Projection","country":"United States","state":"Idaho","otherGeospatial":"Salmon River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0,44.0 ], [ -115.0,44.75 ], [ -114.0,44.75 ], [ -114.0,44.0 ], [ -115.0,44.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db69148f","contributors":{"authors":[{"text":"Maret, Terry R. trmaret@usgs.gov","contributorId":953,"corporation":false,"usgs":true,"family":"Maret","given":"Terry","email":"trmaret@usgs.gov","middleInitial":"R.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":285844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ott, Douglas S. dott@usgs.gov","contributorId":3552,"corporation":false,"usgs":true,"family":"Ott","given":"Douglas","email":"dott@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":285843,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72662,"text":"sir20055100 - 2005 - Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 6 in the Southern Tier of New York","interactions":[],"lastModifiedDate":"2017-04-14T13:11:32","indexId":"sir20055100","displayToPublicDate":"2005-11-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5100","title":"Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 6 in the Southern Tier of New York","docAbstract":"<p>Equations that relate bankfull discharge and channel characteristics (width, depth, and cross-sectional area) to drainage-area size at gaged sites are needed to define bankfull discharge and channel dimensions at ungaged sites and to provide information for watershed assessments, stream-channel classification, and the design of stream-restoration projects. Such equations are most accurate if derived from streams within an area of uniform hydrologic, climatic, and physiographic conditions and applied only within that region. In New York State, eight hydrologic regions were previously defined on the basis of similar high-flow (flood) characteristics. This report presents drainage areas and associated bankfull characteristics (discharge and channel dimensions) for surveyed streams in southwestern New York (Region 6).</p><p>Stream-survey data and discharge records from 11 active (currently gaged) sites and 3 inactive (discontinued) sites were used in regression analyses to relate bankfull discharge and bankfull channel width, depth, and cross-sectional area to the size of the drainage area. The resulting equations are:</p><p>(1) bankfull discharge, in cubic feet per second = 48.0*(drainage area, in square miles)<sup>0.842</sup>;</p><p>(2) bankfull channel width, in feet = 16.9*(drainage area, in square miles)<sup>0.419</sup>;</p><p>(3) bankfull channel depth, in feet = 1.04*(drainage area, in square miles)<sup>0.244</sup>; and</p><p>(4) bankfull channel cross-sectional area, in square feet = 17.6*(drainage area, in square miles)<sup>0.662</sup>.</p><p>The coefficient of determination (R<sup>2</sup>) for these four equations were 0.90, 0.79, 0.64, and 0.89, respectively. The high correlation coefficients for bankfull discharge and cross-sectional area indicate that much of the variation in these variables is explained by the size of the drainage area. The smaller correlation coefficients for bankfull channel width and depth indicate that other factors also affect these relations. Recurrence intervals for the estimated bankfull discharge of each stream ranged from 1.01 to 2.35 years; the mean recurrence interval was 1.54 years. The 14 surveyed streams were classified by Rosgen stream type; most were C-type reaches, with occasional B-type reaches. The Region 6 equation (curve) for bankfull discharge was compared with equations previously developed for four other large areas in New York State and southeastern Pennsylvania. The differences among results indicate that, although the equations need to be refined by region before being applied by water-resources managers to local planning and design efforts, similar regions have similar relations between bankfull discharge and channel characteristics.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055100","collaboration":"Prepared in cooperation with the New York State Department of Environmental Conservation, New York State Department of Transportation, and New York City Department of Environmental Protection","usgsCitation":"Mulvihill, C., Ernst, A., and Baldigo, B.P., 2005, Regionalized equations for bankfull-discharge and channel characteristics of streams in New York State—Hydrologic Region 6 in the Southern Tier of New York: U.S. Geological Survey Scientific Investigations Report 2005-5100, iv, 14 p., https://doi.org/10.3133/sir20055100.","productDescription":"iv, 14 p.","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":339596,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20075189","text":"Scientific Investigations Report 2007-5189","linkHelpText":"- Regionalized Equations for Bankfull Discharge and Channel Characteristics of Streams in New York State—Hydrologic Regions 1 and 2 in the Adirondack Region of Northern New York"},{"id":339126,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20065075","text":"Scientific Investigations Report 2006-5075","linkHelpText":"- Regionalized Equations for Bankfull-Discharge and Channel Characteristics of Streams in New York State—Hydrologic Region 7 in Western New York"},{"id":339594,"rank":7,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20095144","text":"Scientific Investigations Report 2009-5144","linkHelpText":"- Bankfull Discharge and Channel Characteristics of Streams in New York State"},{"id":339595,"rank":6,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20075227","text":"Scientific Investigations Report 2007-5227","linkHelpText":"- Regionalized Equations for Bankfull-Discharge and Channel Characteristics of Streams in New York State—Hydrologic Region 3 East of the Hudson River"},{"id":339597,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/sir20045247 ","text":"Scientific Investigations Report 2004-5247","linkHelpText":"-  Regionalized Equations for Bankfull-Discharge and Channel Characteristics of Streams in New York State—Hydrologic Region 5 in Central New York"},{"id":192789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/sir/2005/5100/coverthb.jpg"},{"id":7067,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5100/pdf/sir2005-5100.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"contact":"<p>Director, New York Water Science Center<br> U.S. Geological Survey<br> 425 Jordan Rd<br> Troy, NY 12180<br> (518) 285-5695 <br> <a href=\"http://ny.water.usgs.gov\" data-mce-href=\"http://ny.water.usgs.gov\">http://ny.water.usgs.gov</a></p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Methods</li><li>Regional Equations for Bankfull Discharge and Channel Characteristics of Streams</li><li>Limitations of This Study</li><li>Summary and Conclusions</li><li>Acknowledgments</li><li>References Cited</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689eea","contributors":{"authors":[{"text":"Mulvihill, Christiane I.","contributorId":31821,"corporation":false,"usgs":true,"family":"Mulvihill","given":"Christiane I.","affiliations":[],"preferred":false,"id":285836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ernst, Anne G.","contributorId":37825,"corporation":false,"usgs":true,"family":"Ernst","given":"Anne G.","affiliations":[],"preferred":false,"id":285837,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baldigo, Barry P. 0000-0002-9862-9119 bbaldigo@usgs.gov","orcid":"https://orcid.org/0000-0002-9862-9119","contributorId":1234,"corporation":false,"usgs":true,"family":"Baldigo","given":"Barry","email":"bbaldigo@usgs.gov","middleInitial":"P.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285835,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207845,"text":"70207845 - 2005 - Historical development of the gravity method in exploration","interactions":[],"lastModifiedDate":"2020-01-15T15:45:05","indexId":"70207845","displayToPublicDate":"2005-11-03T15:33:05","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Historical development of the gravity method in exploration","docAbstract":"<p>The gravity method was the first geophysical technique to be used in oil and gas exploration. Despite being eclipsed by seismology, it has continued to be an important and sometimes crucial constraint in a number of exploration areas. In oil exploration the gravity method is particularly applicable in salt provinces, overthrust and foothills belts, underexplored basins, and targets of interest that underlie high-velocity zones. The gravity method is used frequently in mining applications to map subsurface geology and to directly calculate ore reserves for some massive sulfide orebodies. There is also a modest increase in the use of gravity techniques in specialized investigations for shallow targets.</p><p>Gravimeters have undergone continuous improvement during the past 25 years, particularly in their ability to function in a dynamic environment. This and the advent of global positioning systems (GPS) have led to a marked improvement in the quality of marine gravity and have transformed airborne gravity from a regional technique to a prospect-level exploration tool that is particularly applicable in remote areas or transition zones that are otherwise inaccessible. Recently, moving-platform gravity gradiometers have become available and promise to play an important role in future exploration.</p><p>Data reduction, filtering, and visualization, together with low-cost, powerful personal computers and color graphics, have transformed the interpretation of gravity data. The state of the art is illustrated with three case histories: 3D modeling of gravity data to map aquifers in the Albuquerque Basin, the use of marine gravity gradiometry combined with 3D seismic data to map salt keels in the Gulf of Mexico, and the use of airborne gravity gradiometry in exploration for kimberlites in Canada.</p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.2133785","usgsCitation":"Nabighian, M., Ander, M.E., Grauch, V.J., LaFehr, T., Li, Y., Pearson, W.C., Peirce, J., Phillips, J., and Ruder, M., 2005, Historical development of the gravity method in exploration: Geophysics, v. 70, no. 6, p. 63ND-89ND, https://doi.org/10.1190/1.2133785.","productDescription":"27 p.","startPage":"63ND","endPage":"89ND","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":371273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"70","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nabighian, M.N.","contributorId":62724,"corporation":false,"usgs":true,"family":"Nabighian","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":779514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ander, M. E.","contributorId":221660,"corporation":false,"usgs":false,"family":"Ander","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":779515,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grauch, V. J. S. 0000-0002-0761-3489 tien@usgs.gov","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":886,"corporation":false,"usgs":true,"family":"Grauch","given":"V.","email":"tien@usgs.gov","middleInitial":"J. S.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":779516,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"LaFehr, T.R.","contributorId":16641,"corporation":false,"usgs":true,"family":"LaFehr","given":"T.R.","affiliations":[],"preferred":false,"id":779517,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Li, Y.","contributorId":221662,"corporation":false,"usgs":false,"family":"Li","given":"Y.","email":"","affiliations":[],"preferred":false,"id":779518,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pearson, W. C.","contributorId":221661,"corporation":false,"usgs":false,"family":"Pearson","given":"W.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":779519,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Peirce, J.W.","contributorId":21756,"corporation":false,"usgs":true,"family":"Peirce","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":779520,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Phillips, J. D. 0000-0002-6459-2821","orcid":"https://orcid.org/0000-0002-6459-2821","contributorId":22366,"corporation":false,"usgs":true,"family":"Phillips","given":"J. D.","affiliations":[],"preferred":false,"id":779521,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ruder, M.E.","contributorId":55634,"corporation":false,"usgs":true,"family":"Ruder","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":779522,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":72657,"text":"ofr20051259 - 2005 - Historical late-winter and spring snowpack depth and equivalent water-content data for Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"ofr20051259","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1259","title":"Historical late-winter and spring snowpack depth and equivalent water-content data for Maine","language":"ENGLISH","doi":"10.3133/ofr20051259","usgsCitation":"Hodgkins, G.A., Dudley, R.W., and Loiselle, M.C., 2005, Historical late-winter and spring snowpack depth and equivalent water-content data for Maine: U.S. Geological Survey Open-File Report 2005-1259, 87 p., https://doi.org/10.3133/ofr20051259.","productDescription":"87 p.","costCenters":[],"links":[{"id":192742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7063,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1259/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62ee12","contributors":{"authors":[{"text":"Hodgkins, Glenn A. 0000-0002-4916-5565 gahodgki@usgs.gov","orcid":"https://orcid.org/0000-0002-4916-5565","contributorId":2020,"corporation":false,"usgs":true,"family":"Hodgkins","given":"Glenn","email":"gahodgki@usgs.gov","middleInitial":"A.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true},{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loiselle, Marc C.","contributorId":90350,"corporation":false,"usgs":true,"family":"Loiselle","given":"Marc","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285818,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72655,"text":"sir20055172 - 2005 - A computer program for predicting recharge with a master recession curve","interactions":[],"lastModifiedDate":"2020-01-26T16:57:19","indexId":"sir20055172","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5172","title":"A computer program for predicting recharge with a master recession curve","docAbstract":"Water-table fluctuations occur in unconfined aquifers owing to ground-water recharge following precipitation and infiltration, and ground-water discharge to streams between storm events. Ground-water recharge can be estimated from well hydrograph data using the water-table fluctuation (WTF) principle, which states that recharge is equal to the product of the water-table rise and the specific yield of the subsurface porous medium. The water-table rise, however, must be expressed relative to the water level that would have occurred in the absence of recharge. This requires a means for estimating the recession pattern of the water-table at the site. For a given site there is often a characteristic relation between the water-table elevation and the water-table decline rate following a recharge event. A computer program was written which extracts the relation between decline rate and water-table elevation from well hydrograph data and uses it to construct a master recession curve (MRC). The MRC is a characteristic water-table recession hydrograph, representing the average behavior for a declining water-table at that site. The program then calculates recharge using the WTF method by comparing the measured well hydrograph with the hydrograph predicted by the MRC and multiplying the difference at each time step by the specific yield. This approach can be used to estimate recharge in a continuous fashion from long-term well records. Presented here is a description of the code including the WTF theory and instructions for running it to estimate recharge with continuous well hydrograph data.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055172","usgsCitation":"Heppner, C.S., and Nimmo, J.R., 2005, A computer program for predicting recharge with a master recession curve: U.S. Geological Survey Scientific Investigations Report 2005-5172, 10 p., https://doi.org/10.3133/sir20055172.","productDescription":"10 p.","onlineOnly":"Y","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":192696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7061,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5172/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624762","contributors":{"authors":[{"text":"Heppner, Christopher S.","contributorId":93776,"corporation":false,"usgs":true,"family":"Heppner","given":"Christopher","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285813,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nimmo, John R. 0000-0001-8191-1727 jrnimmo@usgs.gov","orcid":"https://orcid.org/0000-0001-8191-1727","contributorId":757,"corporation":false,"usgs":true,"family":"Nimmo","given":"John","email":"jrnimmo@usgs.gov","middleInitial":"R.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":285812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72658,"text":"ds143 - 2005 - Bacteriological water quality in the Lake Pontchartrain basin, Louisiana, following Hurricanes Katrina and Rita, September 2005","interactions":[],"lastModifiedDate":"2022-04-07T11:21:22.023313","indexId":"ds143","displayToPublicDate":"2005-11-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"143","title":"Bacteriological water quality in the Lake Pontchartrain basin, Louisiana, following Hurricanes Katrina and Rita, September 2005","docAbstract":"The U.S. Geological Survey (USGS), in collaboration with the Louisiana Department of Environmental Quality, monitored bacteriological quality of water at 22 sites in and around Lake Pontchartrain, La., for three consecutive weeks beginning September 13, 2005, following hurricanes Katrina and Rita and the associated flooding. Samples were collected and analyzed by USGS personnel from the USGS Louisiana Water Science Center and the USGS Ohio Water Microbiology Laboratory. Fecal-indicator bacteria (Escherichia coli, enterococci, and fecal coliform) concentrations ranged from the detection limit to 36,000 colony-forming units per 100 milliliters.  Data are presented in tabular form and as plots of data in the context of available historical data and water-quality standards and criteria for each site sampled.  Quality-control data were reviewed to ensure that methods performed as expected in a mobile laboratory setting.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds143","usgsCitation":"Stoeckel, D.M., Bushon, R.N., Demcheck, D.K., Skrobialowski, S.C., Kephart, C.M., Bertke, E.E., Mailot, B.E., Mize, S.V., and Fendick, R., 2005, Bacteriological water quality in the Lake Pontchartrain basin, Louisiana, following Hurricanes Katrina and Rita, September 2005: U.S. Geological Survey Data Series 143, 21 p., https://doi.org/10.3133/ds143.","productDescription":"21 p.","costCenters":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true},{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":192787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7064,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2005/143/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"Lake Pontchartrain basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.83333333333333,30 ], [ -90.83333333333333,31 ], [ -90.16666666666667,31 ], [ -90.16666666666667,30 ], [ -90.83333333333333,30 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab05","contributors":{"authors":[{"text":"Stoeckel, Donald M.","contributorId":78384,"corporation":false,"usgs":true,"family":"Stoeckel","given":"Donald","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285827,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bushon, Rebecca N. rnbushon@usgs.gov","contributorId":2304,"corporation":false,"usgs":true,"family":"Bushon","given":"Rebecca","email":"rnbushon@usgs.gov","middleInitial":"N.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Demcheck, Dennis K. 0000-0003-2981-078X ddemchec@usgs.gov","orcid":"https://orcid.org/0000-0003-2981-078X","contributorId":3273,"corporation":false,"usgs":true,"family":"Demcheck","given":"Dennis","email":"ddemchec@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":285826,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skrobialowski, Stanley C. 0000-0001-8627-0279 sski@usgs.gov","orcid":"https://orcid.org/0000-0001-8627-0279","contributorId":1402,"corporation":false,"usgs":true,"family":"Skrobialowski","given":"Stanley","email":"sski@usgs.gov","middleInitial":"C.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":285820,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kephart, Christopher M. 0000-0002-3369-5596 ckephart@usgs.gov","orcid":"https://orcid.org/0000-0002-3369-5596","contributorId":1932,"corporation":false,"usgs":true,"family":"Kephart","given":"Christopher","email":"ckephart@usgs.gov","middleInitial":"M.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285821,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bertke, Erin E. eebertke@usgs.gov","contributorId":1934,"corporation":false,"usgs":true,"family":"Bertke","given":"Erin","email":"eebertke@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":285822,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mailot, Brian E. bemailot@usgs.gov","contributorId":2569,"corporation":false,"usgs":true,"family":"Mailot","given":"Brian","email":"bemailot@usgs.gov","middleInitial":"E.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285824,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mize, Scott V. 0000-0001-6751-5568 svmize@usgs.gov","orcid":"https://orcid.org/0000-0001-6751-5568","contributorId":2997,"corporation":false,"usgs":true,"family":"Mize","given":"Scott","email":"svmize@usgs.gov","middleInitial":"V.","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285825,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Fendick, Robert B. Jr. rfendick@usgs.gov","contributorId":1313,"corporation":false,"usgs":true,"family":"Fendick","given":"Robert B.","suffix":"Jr.","email":"rfendick@usgs.gov","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":285819,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70238572,"text":"70238572 - 2005 - Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan","interactions":[],"lastModifiedDate":"2022-11-29T20:27:29.708001","indexId":"70238572","displayToPublicDate":"2005-11-01T14:23:36","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1436,"text":"Earthquake Spectra","active":true,"publicationSubtype":{"id":10}},"title":"Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan","docAbstract":"<p>Three exercises of The Plan to Coordinate NEHRP Post-Earthquake Investigations were developed and implemented in late 2003 and early 2004 in order to test the Plan itself via realistic scenarios, and for the NEHRP agencies to learn how to coordinate post-earthquake investigations. The exercises were selected to cover a range of seismic activity and consequences, and were based on scenario events: (1) a Hayward Fault Mw 7 event without foreshocks; (2) a New Madrid seismic zone Mw 7 event with foreshocks, and (3) a Puerto Rico Mw 8 subduction event on the Puerto Rican Trench accompanied by a tsunami affecting the eastern seaboard of the United States. Each exercise consisted of a four-hour telephone conference call with a Web-based electronic link and post-exercise evaluations fed back to participants. Evaluation of the exercises found the Plan to be adequate, with implementation of the Plan by the NEHRP agencies improving with each exercise. Based on the exercises, recommendations were provided that a Plan coordinator should be designated within USGS, an annual exercise of the Plan should be conducted in different regions of the United States, a permanent NEHRP electronic link should be created, and coordination of post-earthquake data collection, preservation, archiving, and dissemination should be greatly improved.</p>","language":"English","publisher":"SAGE Publishing","doi":"10.1193/1.2087707","usgsCitation":"Holzer, T.L., Scawthorn, C., and Rojahn, C., 2005, Coordinating NEHRP Post-Earthquake Investigations: Exercising the Plan: Earthquake Spectra, v. 21, no. 4, p. 1043-1062, https://doi.org/10.1193/1.2087707.","productDescription":"20 p.","startPage":"1043","endPage":"1062","costCenters":[],"links":[{"id":409815,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"4","noUsgsAuthors":false,"publicationDate":"2005-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Holzer, Thomas L. tholzer@usgs.gov","contributorId":2829,"corporation":false,"usgs":true,"family":"Holzer","given":"Thomas","email":"tholzer@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scawthorn, Charles","contributorId":65755,"corporation":false,"usgs":true,"family":"Scawthorn","given":"Charles","affiliations":[],"preferred":false,"id":857953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojahn, Christopher","contributorId":41482,"corporation":false,"usgs":true,"family":"Rojahn","given":"Christopher","email":"","affiliations":[],"preferred":true,"id":857954,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70164302,"text":"70164302 - 2005 - A multi-disciplinary approach to the removal of emerging contaminants in municipal wastewater treatment plans in New York State, 2003-2004","interactions":[],"lastModifiedDate":"2018-10-22T08:27:26","indexId":"70164302","displayToPublicDate":"2005-11-01T11:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"A multi-disciplinary approach to the removal of emerging contaminants in municipal wastewater treatment plans in New York State, 2003-2004","docAbstract":"<p>Across the United States, there is a rapidly growing awareness of the occurrence and the toxicological impacts of natural and synthetic trace compounds in the environment. These trace compounds, referred to as emerging contaminants (ECs), are reported to cause a range of negative impacts in the environment, such as adverse effects on biota in receiving streams and interference with the normal functions of the endocrine system, which controls growth and development in living organisms.</p>\n<p>Wastewater treatment plants (WWTPs) have been identified as a key collection point for ECs in the water cycle and potentially an ideal location at which to treat to remove them, thereby mitigating their release into the environment (<i>Figure 1</i>). This presents wastewater industry professionals with both a significant opportunity and a tremendous challenge: to identify cost effective treatment processes that can remove or reduce these contaminants before they are released into the environment.</p>\n<p>Although WWTPs have been identified as strategic focal points and potential treatment locations for the removal of ECs from the environment, little is known about the nature, variability, transport and fate of this class of compounds in typical wastewaters and treatment facilities in the United States. Furthermore few studies have been performed to monitor or understand the capability of conventional or innovative wastewater treatment processes to remove or reduce the concentrations of a wide variety of ECs at wastewater facilities.</p>\n<p>This study was designed to provide baseline information on this topic. While other studies have examined the occurrence of a limited number of representative contaminants in the environment (generally five to 10 compounds), this study is unique in that it provides information on a comprehensive list of ECs (63 ECs in total, Contaminant List in Appendix A, not included here) in the wastewater collection and treatment systems for four diverse communities over a two-year period. (It should be noted that the study is ongoing and additional data are pending but only 18 months of data are presented in this paper).</p>\n<p>The study was conducted in two phases. Phase 1 was designed to provide information concerning the general character and concentration of ECs commonly detected in wastewaters, the variability over a prolonged period of time, the transport and fate of ECs through typical wastewater treatment plants operating with a range of conventional technologies and the impact of WWTP discharges on receiving streams. It also provided guidance in understanding the capability of distinct wastewater treatment processes or technologies to reduce or remove ECs.</p>\n<p>The second phase of the study focused on one of the most common wastewater treatment processes operated in the United States, the Activated Sludge process. Using four controlled parallel activated sludge pilots, a more detailed assessment of the impact of Sludge Retention Time (SRT) on the reduction or removal of ECs was performed.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Water Environment Federation’s WEFTEC 78th Annual Technical Exhibition and Conference, conference proceedings","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Water Environment Federation’s WEFTEC 78th Annual Technical Exhibition and Conference","conferenceDate":"Oct. 29 - Nov. 2, 2005","conferenceLocation":"Washington, DC","language":"English","publisher":"Water Environment Federation","publisherLocation":"Washington, DC","doi":"10.1061/40927(243)136","usgsCitation":"Philips, P.J., Stinson, B., Zaugg, S.D., Furlong, E.T., Kolpin, D.W., Esposito, K., Bodniewicz, B., Pape, R., and Anderson, J., 2005, A multi-disciplinary approach to the removal of emerging contaminants in municipal wastewater treatment plans in New York State, 2003-2004, <i>in</i> Water Environment Federation’s WEFTEC 78th Annual Technical Exhibition and Conference, conference proceedings, Washington, DC, Oct. 29 - Nov. 2, 2005, p. 5095-5124, https://doi.org/10.1061/40927(243)136.","productDescription":"30 p.","startPage":"5095","endPage":"5124","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":316356,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New 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Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":596898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stinson, Beverley","contributorId":17105,"corporation":false,"usgs":true,"family":"Stinson","given":"Beverley","email":"","affiliations":[],"preferred":false,"id":596899,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":596900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Furlong, Edward T. 0000-0002-7305-4603 efurlong@usgs.gov","orcid":"https://orcid.org/0000-0002-7305-4603","contributorId":740,"corporation":false,"usgs":true,"family":"Furlong","given":"Edward","email":"efurlong@usgs.gov","middleInitial":"T.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":27111,"text":"National Water Quality Program","active":true,"usgs":true},{"id":5046,"text":"Branch of Analytical Serv (NWQL)","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":596901,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kolpin, Dana W. 0000-0002-3529-6505 dwkolpin@usgs.gov","orcid":"https://orcid.org/0000-0002-3529-6505","contributorId":1239,"corporation":false,"usgs":true,"family":"Kolpin","given":"Dana","email":"dwkolpin@usgs.gov","middleInitial":"W.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":596902,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Esposito, Kathleen","contributorId":21835,"corporation":false,"usgs":true,"family":"Esposito","given":"Kathleen","email":"","affiliations":[],"preferred":false,"id":596903,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bodniewicz, B.","contributorId":152701,"corporation":false,"usgs":false,"family":"Bodniewicz","given":"B.","email":"","affiliations":[],"preferred":false,"id":596904,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pape, R.","contributorId":152702,"corporation":false,"usgs":false,"family":"Pape","given":"R.","email":"","affiliations":[],"preferred":false,"id":596905,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Anderson, J.","contributorId":103437,"corporation":false,"usgs":true,"family":"Anderson","given":"J.","affiliations":[],"preferred":false,"id":596906,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70193171,"text":"70193171 - 2005 - Non-lethal estimation of body composition of Yukon River salmon","interactions":[],"lastModifiedDate":"2021-02-04T16:40:38.592901","indexId":"70193171","displayToPublicDate":"2005-10-31T10:32:49","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":7468,"text":"Final Report","active":true,"publicationSubtype":{"id":9}},"title":"Non-lethal estimation of body composition of Yukon River salmon","docAbstract":"<p>Because of the importance of Chinook salmon to commercial and subsistence fisheries on the Yukon River, further study of the factors that may affect the success of this species and our ability to manage the fisheries is warranted. Critical to these studies is the determination of the amount of lipids (fat) stored and available to the fish as its primary energy source for migration and spawning. Recent developments of Bioelectrical Impedance Analysis (BIA) promise a simple, non-lethal means of estimating proximate composition (e.g. fat, protein, water content) for field applications with fish. The goal of the project was to develop BIA models for Chinook salmon from the Yukon River watershed that would permit the non-lethal estimation of body proximate composition for use in field studies. </p><p>Our results clearly demonstrated that BIA can be used to estimate proximate composition and energy density of salmon. While some minor refinements were suggested, the methodology can be used in a wide variety of field applications. For instance, application of the BIA models to predict energy levels of fish during their migration will allow evaluation of management programs, while also yielding data that can be used to evaluate energy use along the migratory path. Correlations of energy level with ongoing tagging, radio-tracking, and genetic studies also have the potential to allow managers and scientists to understand the relationship between fat content and distance to spawning location. These models have the potential for application to this species in other river systems. They also provide tools for a variety of other scientific investigation such as: 1) differences in energy stores in spawning and recruitment success; 2) effects of global warming on migratory salmonid stocks; and 3) differences in annual flow and temperature regiments upon migratory energy costs and resulting recruitment success.</p>","language":"English","publisher":"Arctic-Yukon-Kuskokwim Sustainable Salmon Initiative","usgsCitation":"Margraf, F.J., Hartman, K.J., and Cox, M.K., 2005, Non-lethal estimation of body composition of Yukon River salmon: Final Report, iv, 23 p.","productDescription":"iv, 23 p.","ipdsId":"IP-007579","costCenters":[{"id":199,"text":"Coop Res Unit Leetown","active":true,"usgs":true}],"links":[{"id":382963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":382962,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.aykssi.org/project/energy-content-of-yukon-river-chinook-salmon/"}],"country":"Canada, United States","state":"Alaska, Yukon","otherGeospatial":"Yukon River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -132.93457031249997,\n              59.712097173322924\n            ],\n            [\n              -139.4384765625,\n              64.62387720204688\n            ],\n            [\n              -144.53613281249997,\n              66.9816661111497\n            ],\n            [\n              -159.521484375,\n              65.34851379240024\n            ],\n            [\n              -161.1474609375,\n              62.512317938386914\n            ],\n            [\n              -163.0810546875,\n              62.91523303947614\n            ],\n            [\n              -165.0146484375,\n              63.29293924364835\n            ],\n            [\n              -164.7509765625,\n              62.08331486294795\n            ],\n            [\n              -161.8505859375,\n              61.33353967329144\n            ],\n            [\n              -159.1259765625,\n              61.75233128411639\n            ],\n            [\n              -157.2802734375,\n              64.14895190024562\n            ],\n            [\n              -149.85351562499997,\n              65.09064558256851\n            ],\n            [\n              -146.07421875,\n              66.19600891267761\n            ],\n            [\n              -142.8662109375,\n              64.64270382119375\n            ],\n            [\n              -140.44921875,\n              63.25341156651705\n            ],\n            [\n              -136.8896484375,\n              61.079544234557304\n            ],\n            [\n              -134.47265625,\n              59.512029386502704\n            ],\n            [\n              -132.93457031249997,\n              59.712097173322924\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","publishingServiceCenter":{"id":9,"text":"Reston PSC"},"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Margraf, F. 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,{"id":70258619,"text":"70258619 - 2005 - Establishing an analytical framework for calculating consistent and sensitive measures of the rate of biodiversity change","interactions":[],"lastModifiedDate":"2024-09-18T16:52:24.800011","indexId":"70258619","displayToPublicDate":"2005-10-27T11:23:51","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Establishing an analytical framework for calculating consistent and sensitive measures of the rate of biodiversity change","docAbstract":"<p>The Convention on Biological Diversity’s (CBD) VIth Conference of the Parties (COP) and the World Summit on Sustainable Development agreed to a target to achieve a significant reduction of the rate of biodiversity loss by 2010. The VIIth COP adopted a conceptual framework to facilitate the assessment of global progress toward 2010 and to encourage national and regional targets and indicators. However, most of the indicators identified are not and will not be adequately quantified at desired accuracy and with desired frequency by 2010. What is possible is the establishment of an analytic framework that can provide guidelines and baselines for biodiversity estimates that can steadily improve with time. </p><p>A judicious combination of remotely sensed data, Geographic Information System data, ground samples, and expert knowledge of species trends and species’ use of habitats form a solid basis for assessing biodiversity. National development of sensitive, consistent, and affordable indicators that can contribute to the CBD global indicators requires access to a baseline set of global ecosystem, climate, topography, land cover, and human impact information. Fortunately, over the last ten years, a number of relevant information sources have become available. Such information, as well as appropriate methods for use, should be promoted and made highly accessible to countries and organizations that support the CBD. </p><p>The NASA-Non-Governmental Organization (NGO) Conservation Working Group is collaborating to evaluate and demonstrate the meaningful role remote sensing can play in developing biodiversity indicators to meet the targets specified. The Working Group members are evaluating indicators across a range of biomes and scales. The results are being synthesized in a handbook describing the use of remote sensing for monitoring the 2010 target to be published in 2006. </p>","conferenceTitle":"16th William T. Pecora Memorial Symposium on Remote Sensing","conferenceDate":"October 23–27, 2005","conferenceLocation":"Sioux Falls, SD","language":"English","publisher":"ASPRS","usgsCitation":"Fosnight, E.A., Strand, H., and White, B., 2005, Establishing an analytical framework for calculating consistent and sensitive measures of the rate of biodiversity change, 16th William T. Pecora Memorial Symposium on Remote Sensing, Sioux Falls, SD, October 23–27, 2005, 11 p.","productDescription":"11 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":437794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fosnight, Eugene A. 0000-0002-8557-3697 fosnight@usgs.gov","orcid":"https://orcid.org/0000-0002-8557-3697","contributorId":2961,"corporation":false,"usgs":true,"family":"Fosnight","given":"Eugene","email":"fosnight@usgs.gov","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":913404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strand, H.","contributorId":182516,"corporation":false,"usgs":false,"family":"Strand","given":"H.","email":"","affiliations":[],"preferred":false,"id":913405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Benjamin","contributorId":344301,"corporation":false,"usgs":false,"family":"White","given":"Benjamin","email":"","affiliations":[{"id":81104,"text":"Institute for Advanced Computer Studies, University of Maryland College Park","active":true,"usgs":false}],"preferred":false,"id":913406,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72649,"text":"ofr20051197 - 2005 - Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: III. biweekly data, 2000-2002","interactions":[],"lastModifiedDate":"2021-01-15T22:14:32.296403","indexId":"ofr20051197","displayToPublicDate":"2005-10-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1197","title":"Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: III. biweekly data, 2000-2002","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051197","usgsCitation":"Antweiler, R.C., Smith, R.L., Voytek, M.A., Bohlke, J., and Dupre, D.H., 2005, Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: III. biweekly data, 2000-2002: U.S. Geological Survey Open-File Report 2005-1197, 74 p., https://doi.org/10.3133/ofr20051197.","productDescription":"74 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":192689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":382244,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1197/"},{"id":7022,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1197/ofr20051197.pdf","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Indiana, Illinois","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.75,40.5 ], [ -87.75,41.25 ], [ -87,41.25 ], [ -87,40.5 ], [ -87.75,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c89","contributors":{"authors":[{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Richard L. 0000-0002-3829-0125 rlsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-3829-0125","contributorId":1592,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rlsmith@usgs.gov","middleInitial":"L.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true}],"preferred":true,"id":285804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voytek, Mary A.","contributorId":91943,"corporation":false,"usgs":true,"family":"Voytek","given":"Mary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285807,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohlke, John Karl 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":66293,"corporation":false,"usgs":true,"family":"Bohlke","given":"John Karl","affiliations":[],"preferred":false,"id":285806,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dupre, David H. dhdupre@usgs.gov","contributorId":2782,"corporation":false,"usgs":true,"family":"Dupre","given":"David","email":"dhdupre@usgs.gov","middleInitial":"H.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285805,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72648,"text":"ofr20051380 - 2005 - Water-quality data, Huron County, Michigan 2004","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"ofr20051380","displayToPublicDate":"2005-10-27T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1380","title":"Water-quality data, Huron County, Michigan 2004","language":"ENGLISH","doi":"10.3133/ofr20051380","usgsCitation":"Duris, J.W., and Haack, S.K., 2005, Water-quality data, Huron County, Michigan 2004: U.S. Geological Survey Open-File Report 2005-1380, 38 p., https://doi.org/10.3133/ofr20051380.","productDescription":"38 p.","costCenters":[],"links":[{"id":192688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7021,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1380/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.83333333333333,42.416666666666664 ], [ -83.83333333333333,43.416666666666664 ], [ -83.25,43.416666666666664 ], [ -83.25,42.416666666666664 ], [ -83.83333333333333,42.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5636","contributors":{"authors":[{"text":"Duris, Joseph W. 0000-0002-8669-8109 jwduris@usgs.gov","orcid":"https://orcid.org/0000-0002-8669-8109","contributorId":1981,"corporation":false,"usgs":true,"family":"Duris","given":"Joseph","email":"jwduris@usgs.gov","middleInitial":"W.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":false,"id":285801,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haack, Sheridan K. skhaack@usgs.gov","contributorId":1982,"corporation":false,"usgs":true,"family":"Haack","given":"Sheridan","email":"skhaack@usgs.gov","middleInitial":"K.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285802,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72646,"text":"wdrWI041 - 2005 - Water resources data - Wisconsin, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"wdrWI041","displayToPublicDate":"2005-10-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-04-1","title":"Water resources data - Wisconsin, water year 2004","language":"ENGLISH","doi":"10.3133/wdrWI041","issn":"07408803","usgsCitation":"Waschbusch, R., Olson, D., Marsh, S., and Stark, P., 2005, Water resources data - Wisconsin, water year 2004: U.S. Geological Survey Water Data Report WI-04-1, 990 p., https://doi.org/10.3133/wdrWI041.","productDescription":"990 p.","numberOfPages":"990","costCenters":[],"links":[{"id":192641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7020,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-wi-04-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8861","contributors":{"authors":[{"text":"Waschbusch, R.J.","contributorId":107307,"corporation":false,"usgs":true,"family":"Waschbusch","given":"R.J.","affiliations":[],"preferred":false,"id":285800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, D.L.","contributorId":34943,"corporation":false,"usgs":true,"family":"Olson","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":285797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marsh, S.B.","contributorId":105329,"corporation":false,"usgs":true,"family":"Marsh","given":"S.B.","email":"","affiliations":[],"preferred":false,"id":285799,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stark, P.A.","contributorId":39850,"corporation":false,"usgs":true,"family":"Stark","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":285798,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72645,"text":"ofr20051286 - 2005 - Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, January-December 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"ofr20051286","displayToPublicDate":"2005-10-25T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1286","title":"Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, January-December 2003","language":"ENGLISH","doi":"10.3133/ofr20051286","usgsCitation":"La Camera, R.J., Locke, G.L., and Habte, A.M., 2005, Selected ground-water data for Yucca Mountain region, southern Nevada and eastern California, January-December 2003: U.S. Geological Survey Open-File Report 2005-1286, 82 p., https://doi.org/10.3133/ofr20051286.","productDescription":"82 p.","costCenters":[],"links":[{"id":192640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7019,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1286/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9ff8","contributors":{"authors":[{"text":"La Camera, Richard J.","contributorId":52212,"corporation":false,"usgs":true,"family":"La Camera","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Locke, Glenn L. gllocke@usgs.gov","contributorId":2479,"corporation":false,"usgs":true,"family":"Locke","given":"Glenn","email":"gllocke@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":285794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Habte, Aron M.","contributorId":108206,"corporation":false,"usgs":true,"family":"Habte","given":"Aron","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285796,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72642,"text":"sir20055166 - 2005 - Hydrogeologic setting, ground-water flow, and ground-water quality at the Lake Wheeler Road research station, 2001-03 : North Carolina Piedmont and Mountains Resource Evaluation Program","interactions":[],"lastModifiedDate":"2022-02-18T22:33:14.349836","indexId":"sir20055166","displayToPublicDate":"2005-10-22T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5166","title":"Hydrogeologic setting, ground-water flow, and ground-water quality at the Lake Wheeler Road research station, 2001-03 : North Carolina Piedmont and Mountains Resource Evaluation Program","docAbstract":"Results of a 2-year field study of the regolith-fractured bedrock ground-water system at the Lake Wheeler Road research station in Wake County, North Carolina, indicate both disconnection and interaction among components of the ground-water system. The three components of the ground-water system include (1) shallow, porous regolith; (2) a transition zone, including partially weathered rock, having both secondary (fractures) and primary porosity; and (3) deeper, fractured bedrock that has little, if any, primary porosity and is dominated by secondary fractures. The research station includes 15 wells (including a well transect from topographic high to low settings) completed in the three major components of the ground-water-flow system and a surface-water gaging station on an unnamed tributary.\r\n\r\nThe Lake Wheeler Road research station is considered representative of a felsic gneiss hydrogeologic unit having steeply dipping foliation and a relatively thick overlying regolith. Bedrock foliation generally strikes N. 10? E. to N. 30? E. and N. 20? W. to N. 40? W. to a depth of about 400 feet and dips between 70? and 80? SE. and NE., respectively. From 400 to 600 feet, the foliation generally strikes N. 70? E. to N. 80? E., dipping 70? to 80? SE. Depth to bedrock locally ranges from about 67 to 77 feet below land surface. Fractures in the bedrock generally occur in two primary sets: low dip angle, stress relief fractures that cross cut foliation, and steeply dipping fractures parallel to foliation.\r\n\r\nFindings of this study generally support the conceptual models of ground-water flow from high to low topographic settings developed for the Piedmont and Blue Ridge Provinces in previous investigations, but are considered a refinement of the generalized conceptual model based on a detailed local-scale investigation. Ground water flows toward a surface-water boundary, and hydraulic gradients generally are downward in recharge areas and upward in discharge areas; however, local variations in vertical gradients are apparent.\r\n\r\nWater-quality sampling and monitoring efforts were conducted to characterize the interaction of components of the ground-water system. Elevated nitrate concentrations as high as 22 milligrams per liter were detected in shallow ground water from the regolith at the study site. These elevated nitrate concentrations likely are related to land use, which includes agricultural practices that involve animal feeding operations and crop fertilization. Continuous ground-water-quality data indicate seasonal fluctuations in field water-quality properties, differences with respect to depth, and fluctuations during recharge events. Water-quality properties recorded in the regolith well following rainfall indicate the upwelling of deeper ground water in the discharge area, likely from ground water in the transition-zone fractures. Additionally, interaction with a surface-water boundary appears likely in the ground-water discharge area, as water levels in all three ground-water zones, including the deep bedrock, mimic the surface-water rise during rainfall.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055166","usgsCitation":"Chapman, M.J., Bolich, R.E., and Huffman, B.A., 2005, Hydrogeologic setting, ground-water flow, and ground-water quality at the Lake Wheeler Road research station, 2001-03 : North Carolina Piedmont and Mountains Resource Evaluation Program: U.S. Geological Survey Scientific Investigations Report 2005-5166, 99 p., https://doi.org/10.3133/sir20055166.","productDescription":"99 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":192603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7018,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5166/","linkFileType":{"id":5,"text":"html"}},{"id":396213,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75454.htm"}],"country":"United States","state":"North Carolina","county":"Wake County","otherGeospatial":"Lake Wheeler Road Research Station","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.6731,\n              35.7353\n            ],\n            [\n              -78.6811,\n              35.7353\n            ],\n            [\n              -78.6811,\n              35.7297\n            ],\n            [\n              -78.6731,\n              35.7297\n            ],\n            [\n              -78.6731,\n              35.7353\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db6920ef","contributors":{"authors":[{"text":"Chapman, Melinda J. 0000-0003-4021-0320 mjchap@usgs.gov","orcid":"https://orcid.org/0000-0003-4021-0320","contributorId":1597,"corporation":false,"usgs":true,"family":"Chapman","given":"Melinda","email":"mjchap@usgs.gov","middleInitial":"J.","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":285792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolich, Richard E.","contributorId":89615,"corporation":false,"usgs":true,"family":"Bolich","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":285793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huffman, Brad A. 0000-0003-4025-1325 bahuffma@usgs.gov","orcid":"https://orcid.org/0000-0003-4025-1325","contributorId":1596,"corporation":false,"usgs":true,"family":"Huffman","given":"Brad","email":"bahuffma@usgs.gov","middleInitial":"A.","affiliations":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285791,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72640,"text":"i2600D - 2005 - Coastal-change and glaciological map of the Ronne Ice Shelf area, Antarctica, 1974-2002","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"i2600D","displayToPublicDate":"2005-10-21T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2600","chapter":"D","title":"Coastal-change and glaciological map of the Ronne Ice Shelf area, Antarctica, 1974-2002","docAbstract":"Changes in the area and volume of polar ice sheets are intricately linked to changes in global climate, and the resulting changes in sea level may severely impact the densely populated coastal regions on Earth. Melting of the West Antarctic part alone of the Antarctic ice sheet could cause a sea-level rise of approximately 6 meters (m). The potential sea-level rise after melting of the entire Antarctic ice sheet is estimated to be 65 m (Lythe and others, 2001) to 73 m (Williams and Hall, 1993). In spite of its importance, the mass balance (the net volumetric gain or loss) of the Antarctic ice sheet is poorly known; it is not known for certain whether the ice sheet is growing or shrinking. In a review paper, Rignot and Thomas (2002) concluded that the West Antarctic part of the Antarctic ice sheet is probably becoming thinner overall; although it is thickening in the west, it is thinning in the north. Joughin and Tulaczyk (2002), on the basis of analysis of ice-flow velocities derived from synthetic aperture radar, concluded that most of the Ross ice streams (ice streams on the east side of the Ross Ice Shelf) have a positive mass balance, whereas Rignot and others (in press) infer even larger negative mass balance for glaciers flowing northward into the Amundsen Sea, a trend suggested by Swithinbank and others (2003a,b, 2004). The mass balance of the East Antarctic part of the Antarctic ice sheet is unknown, but thought to be in near equilibrium.\r\n\r\nMeasurement of changes in area and mass balance of the Antarctic ice sheet was given a very high priority in recommendations by the Polar Research Board of the National Research Council (1986), in subsequent recommendations by the Scientific Committee on Antarctic Research (SCAR) (1989, 1993), and by the National Science Foundation's (1990) Division of Polar Pro-grams. On the basis of these recommendations, the U.S. Geo-logical Survey (USGS) decided that the archive of early 1970s Landsat 1, 2, and 3 Multispectral Scanner (MSS) images of Ant-arctica and the subsequent repeat coverage made possible with Landsat and other satellite images provided an excellent means of documenting changes in the coastline of Antarctica (Ferrigno and Gould, 1987). The availability of this information provided the impetus for carrying out a comprehensive analysis of the glaciological features of the coastal regions and changes in ice fronts of Antarctica (Swithinbank, 1988; Williams and Ferrigno, 1988). The project was later modified to include Landsat 4 and 5 MSS and Thematic Mapper (TM) (and in some areas Landsat 7 Enhanced Thematic Mapper Plus (ETM+)), RADARSAT images, and other data where available, to compare changes during a 20- to 25- or 30-year time interval (or longer where data were available, as in the Antarctic Peninsula). The results of the analysis are being used to produce a digital database and a series of USGS Geologic Investigations Series Maps (I-2600) consisting of 23 maps at 1:1,000,000 scale and 1 map at 1:5,000,000 scale, in both paper and digital format (Williams and others, 1995; Williams and Ferrigno, 1998; Ferrigno and others, 2002) (available online at http://www.glaciers.er.usgs.gov).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Coastal-change and glaciological maps of Antarctica","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/i2600D","isbn":"0607964413","usgsCitation":"Ferrigno, J.G., Foley, K., Swithinbank, C., Williams, R., and Dalide, L., 2005, Coastal-change and glaciological map of the Ronne Ice Shelf area, Antarctica, 1974-2002 (Version 1.0): U.S. Geological Survey IMAP 2600, 1 map : col. ; 48 x 56 in. (115 x 100 cm.), on sheet 142 x 104 cm., folded in envelope to 29 x 21 cm. + 1 pamphlet (11 p. : map; 28 cm.), https://doi.org/10.3133/i2600D.","productDescription":"1 map : col. ; 48 x 56 in. (115 x 100 cm.), on sheet 142 x 104 cm., folded in envelope to 29 x 21 cm. + 1 pamphlet (11 p. : map; 28 cm.)","additionalOnlineFiles":"Y","temporalStart":"1974-01-01","temporalEnd":"2002-12-31","costCenters":[],"links":[{"id":192602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8347,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/2600/D/","linkFileType":{"id":5,"text":"html"}},{"id":8348,"rank":9999,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/imap/2600/D/ronne.met.txt","linkFileType":{"id":2,"text":"txt"}},{"id":8349,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/imap/2600/D/i2600d.zip"},{"id":8350,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2600/D/i2600d-pamphlet.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","projection":"Polar stereographic, MSL","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,-84 ], [ -90,-74 ], [ -45,-74 ], [ -45,-84 ], [ -90,-84 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9fd","contributors":{"authors":[{"text":"Ferrigno, Jane G. jferrign@usgs.gov","contributorId":39825,"corporation":false,"usgs":true,"family":"Ferrigno","given":"Jane","email":"jferrign@usgs.gov","middleInitial":"G.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":285787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foley, K.M.","contributorId":41846,"corporation":false,"usgs":true,"family":"Foley","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":285788,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swithinbank, C.","contributorId":47036,"corporation":false,"usgs":true,"family":"Swithinbank","given":"C.","affiliations":[],"preferred":false,"id":285790,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, R.S. Jr.","contributorId":46102,"corporation":false,"usgs":true,"family":"Williams","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":285789,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dalide, L.M.","contributorId":8188,"corporation":false,"usgs":true,"family":"Dalide","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":285786,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72581,"text":"sir20055208 - 2005 - Potentiometric surface of the Ozark aquifer in northern Arkansas, 2004","interactions":[],"lastModifiedDate":"2012-02-10T00:11:36","indexId":"sir20055208","displayToPublicDate":"2005-10-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5208","title":"Potentiometric surface of the Ozark aquifer in northern Arkansas, 2004","docAbstract":"The Ozark aquifer in northern Arkansas comprises dolomites, limestones, sandstones, and shales of Late Cambrian to Middle Devonian age, and ranges in thickness from approximately 1,100 feet to more than 4,000 feet. Hydrologically, the aquifer is complex, characterized by discrete and discontinuous flow components with large variations in permeability. \r\n\r\nThe potentiometric-surface map, based on 59 well and 5 spring water-level measurements collected in 2004 in Arkansas and Missouri, indicates maximum water-level altitudes of about 1,188 feet in Benton County and minimum water-level altitudes of about 116 feet in Randolph County. Regionally, the flow within the aquifer is to the south and southeast in the eastern and central part of the study area and to the northwest and north in the western part of the study area. Comparing the 2004 potentiometric- surface map with a predevelopment potentiometricsurface map indicates general agreement between the two surfaces. Potentiometric-surface differences could be attributed to differences in pumping related to changing population from 1990 to 2000, change in source for public supplies, processes or water use outside the study area, or differences in data-collection or map-construction methods.","language":"ENGLISH","doi":"10.3133/sir20055208","usgsCitation":"Schrader, T., 2005, Potentiometric surface of the Ozark aquifer in northern Arkansas, 2004 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5208, 16 p., https://doi.org/10.3133/sir20055208.","productDescription":"16 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7616,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5208/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95,33 ], [ -95,36.833333333333336 ], [ -89,36.833333333333336 ], [ -89,33 ], [ -95,33 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f38","contributors":{"authors":[{"text":"Schrader, T.P.","contributorId":56300,"corporation":false,"usgs":true,"family":"Schrader","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":285754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72488,"text":"sir20055204 - 2005 - Ground-water availability from surficial aquifers in the Red River of the North Basin, Minnesota","interactions":[],"lastModifiedDate":"2016-04-04T11:10:10","indexId":"sir20055204","displayToPublicDate":"2005-10-17T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5204","title":"Ground-water availability from surficial aquifers in the Red River of the North Basin, Minnesota","docAbstract":"<p>Population growth and commercial and industrial development in the Red River of the North Basin in Minnesota, North Dakota, and South Dakota have prompted the Bureau of Reclamation, U.S. Department of the Interior, to evaluate sources of water to sustain this growth. Nine surficial-glacial (surficial) aquifers (Buffalo, Middle River, Two Rivers, Beach Ridges, Pelican River, Otter Tail, Wadena, Pineland Sands, and Bemidji-Bagley) within the Minnesota part of the basin were identified and evaluated for their ground-water resources. Information was compiled and summarized from published studies to evaluate the availability of ground water. Published information reviewed for each of the aquifers included location and extent, physical characteristics, hydraulic properties, ground-water and surface-water interactions, estimates of water budgets (sources of recharge and discharge) and aquifer storage, theoretical well yields and actual ground-water pumping data, recent (2003) ground-water use data, and baseline ground-water-quality data.</p>\n<p>Water-budget estimates for the aquifers were compiled from steady-state aquifer simulations, precipitation data and hydrograph analysis, and recharge and discharge information. Major sources of recharge to the aquifers are areal recharge, flow from surface water, and flow across aquifer boundaries from adjacent geologic units. Losses of water from the aquifers include evapotranspiration, flow to surface water, flow across aquifer boundaries, and withdrawals by pumping wells. The Bemidji-Bagley, Otter Tail, Pineland Sands, and Wadena surficial aquifers have the highest rates of water inflow and outflow of the nine aquifers in the study area, and the Middle River surficial aquifer has the lowest rates of total water inflow and outflow.</p>\n<p>Maximum storage volumes of five of the surficial aquifers were calculated using areal extent and published saturated thickness and porosity data. Storage estimates from published studies were included for three of the surficial aquifers. Maximum theoretical well yields for the aquifers generally occur in areas with more abundant, well-sorted, coarse-grained sediment. In 2003, 28 billion gallons of ground water were withdrawn from the aquifers, not including water used for private supply. In 2003, the largest volume of ground water was withdrawn from the Otter Tail surficial aquifer, and the smallest volume was withdrawn from the the Middle River surficial aquifer. Agricultural irrigation and public supply totaled 95 percent of the volume of ground water withdrawn from the aquifers in 2003.</p>\n<p>Ground-water-quality data indicate that the Buffalo aquifer contained the largest specific conductance and concentrations of dissolved solids, calcium, magnesium, sodium, sulfate, and iron. Ground water from the Bemidji-Bagley, Otter Tail, Pineland Sands, and Wadena surficial aquifers contained the largest concentrations of nitrate (as nitrogen). In general, the nine aquifers are hydraulically connected to local surface water. Simulations of ground-water development for some of the aquifers describe correlations between increased ground-water withdrawals and declining lake levels and streamflows, lower water-table altitudes, and variations in ground-water quality.</p>\n<p>On the basis of data and methods presented to evaluate ground-water availability, the Otter Tail and Pineland Sands surficial aquifers and Pelican River sand-plain aquifer have the greatest potential for additional development of ground-water resources in the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055204","collaboration":"Prepared in cooperation with the Minnesota Geological Survey and Bureau of Reclamation, U.S. Department of the Interior","usgsCitation":"Reppe, T.H., 2005, Ground-water availability from surficial aquifers in the Red River of the North Basin, Minnesota: U.S. Geological Survey Scientific Investigations Report 2005-5204, viii, 54 p., https://doi.org/10.3133/sir20055204.","productDescription":"viii, 54 p.","numberOfPages":"63","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055204.JPG"},{"id":7542,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5204/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota, North Dakota, South Dakota","otherGeospatial":"Red River of the North Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.4052734375, 49.001843917978526 ], [ -99.99755859375, 48.99463598353408 ], [ -99.964599609375, 48.915279853443806 ], [ -99.755859375, 48.88639177703194 ], [ -99.755859375, 48.719961222646276 ], [ 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,{"id":72480,"text":"sir20055147 - 2005 - Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland","interactions":[],"lastModifiedDate":"2017-07-10T10:35:12","indexId":"sir20055147","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5147","title":"Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland","docAbstract":"Natural-stream designs are commonly based on the dimensions of the bankfull channel, which is capable of conveying discharges that transport sediment without excessive erosion or deposition. Regional curves relate bankfull-channel geometry and discharge to drainage area in watersheds with similar runoff characteristics and commonly are utilized by practitioners of natural-stream design to confirm or refute selection of the field-identified bankfull channel. Data collected from 66 streamflow-gaging stations and associated stream reaches between December 1999 and December 2003 were used in one-variable ordinary least-squares regression analyses to develop regional curves relating drainage area to cross-sectional area, discharge, width, and mean depth of the bankfull channel. Watersheds draining to these stations are predominantly within the Piedmont, Ridge and Valley, and Appalachian Plateaus Physiographic Provinces of Pennsylvania and northern Maryland. \r\n\r\nStatistical analyses of physiography, percentage of watershed area underlain by carbonate bedrock, and percentage of watershed area that is glaciated indicate that carbonate bedrock, not physiography or glaciation, has a controlling influence on the slope of regional curves. Regional curves developed from stations in watersheds underlain by 30 percent or less carbonate bedrock generally had steeper slopes than the corresponding relations developed from watersheds underlain by greater than 30 percent carbonate bedrock. In contrast, there is little evidence to suggest that regional curves developed from stations in the Piedmont or Ridge and Valley Physiographic Province are different from the corresponding relations developed from stations in the Appalachian Plateaus Physiographic Province. On the basis of these findings, regional curves are presented to represent two settings that are independent of physiography: (1) noncarbonate settings characterized by watersheds with carbonate bedrock underlying 30 percent or less of watershed area, and (2) carbonate settings characterized by watersheds with carbonate bedrock underlying greater than 30 percent of watershed area. \r\n\r\nAll regional curves presented in this report have slopes that are significantly different from zero and normally distributed residuals that vary randomly with drainage area. Drainage area explains the most variability in bankfull cross-sectional area and bankfull discharge in the noncarbonate setting (R2 = 0.92 for both). Less variability is explained in bankfull width and depth (R2 = 0.81 and 0.72, respectively). Regional curves representing the carbonate setting are generally not as statistically robust as the corresponding noncarbonate relations because there were only 11 stations available to develop these curves and drainage area cannot explain variance resulting from karst features. The carbonate regional curves generally are characterized by less confidence, lower R2 values, and higher residual standard errors. Poor representation by watersheds less than 40 mi2 causes the carbonate regional curves for bankfull discharge, cross-sectional area, and mean depth to be disproportionately influenced by the smallest watershed (values of Cook's Distance range from 3.6 to 8.4). Additional bankfull discharge and channel-geometry data from small watersheds might reduce this influence, increase confidence, and generally improve regional curves representing the carbonate setting. \r\n\r\nLimitations associated with streamflow-gaging station selection and development of the curves result in some constraints for the application of regional curves presented in this report. These curves apply only to streams within the study area in watersheds having land use, streamflow regulation, and drainage areas that are consistent with the criteria used for station selection. Regardless of the setting, the regional curves presented here are not intended for use as the sole method for estimation of bankfull characteristics; however, th","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055147","usgsCitation":"Chaplin, J.J., 2005, Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland: U.S. Geological Survey Scientific Investigations Report 2005-5147, 40 p., https://doi.org/10.3133/sir20055147.","productDescription":"40 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":192903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7538,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5147/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81,39.833333333333336 ], [ -81,42.833333333333336 ], [ -74,42.833333333333336 ], [ -74,39.833333333333336 ], [ -81,39.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de31","contributors":{"authors":[{"text":"Chaplin, Jeffrey J. 0000-0002-0617-5050 jchaplin@usgs.gov","orcid":"https://orcid.org/0000-0002-0617-5050","contributorId":147,"corporation":false,"usgs":true,"family":"Chaplin","given":"Jeffrey","email":"jchaplin@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285721,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72483,"text":"sir20055210 - 2005 - Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055210","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5210","title":"Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003","docAbstract":"Winter snow accumulation and summer snow and ice ablation were measured at South Cascade Glacier, Washington, to estimate glacier mass-balance quantities for balance year 2003. The 2003 glacier-average maximum winter snow balance was 2.66 meters water equivalent, which was about equal to the average of such balances for the glacier since balance year 1959. The 2003 glacier summer balance (-4.76 meters water equivalent) was the most negative reported for the glacier, and the 2003 net balance (-2.10 meters water equivalent), was the second-most negative reported. The glacier 2003 annual (water year) balance was -1.89 meters water equivalent. \r\n\r\nThe area of the glacier near the end of the balance year was 1.89 square kilometers, a decrease of 0.03 square kilometer from the previous year. The equilibrium-line altitude was higher than any part of the glacier; however, because snow remained along part of one side of the upper glacier, the accumulation-area ratio was 0.07. During September 13, 2002-September 13, 2003, the glacier terminus retreated at a rate of about 15 meters per year. Average speed of surface ice, computed using a series of vertical aerial photographs dating back to 2001, ranged from 2.2 to 21.8 meters per year. \r\n\r\nRunoff from the subbasin containing the glacier and from an adjacent non-glacierized basin was gaged during part of water year 2003. Air temperature, precipitation, atmospheric water-vapor pressure, wind speed, and incoming solar radiation were measured at selected locations on and near the glacier. Summer 2003 at the glacier was among the warmest for which data are available.","language":"ENGLISH","doi":"10.3133/sir20055210","usgsCitation":"Bidlake, W.R., Josberger, E.G., and Savoca, M.E., 2005, Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003: U.S. Geological Survey Scientific Investigations Report 2005-5210, 60 p., https://doi.org/10.3133/sir20055210.","productDescription":"60 p.","costCenters":[],"links":[{"id":192960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7540,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5210/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489b05","contributors":{"authors":[{"text":"Bidlake, William R. wbidlake@usgs.gov","contributorId":1712,"corporation":false,"usgs":true,"family":"Bidlake","given":"William","email":"wbidlake@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":285725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Josberger, Edward G. ejosberg@usgs.gov","contributorId":1710,"corporation":false,"usgs":true,"family":"Josberger","given":"Edward","email":"ejosberg@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":285724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savoca, Mark E. mesavoca@usgs.gov","contributorId":1961,"corporation":false,"usgs":true,"family":"Savoca","given":"Mark","email":"mesavoca@usgs.gov","middleInitial":"E.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70238383,"text":"70238383 - 2005 - Implications for prediction and hazard assessment from the 2004 Parkfield earthquake","interactions":[],"lastModifiedDate":"2022-11-18T18:18:55.697023","indexId":"70238383","displayToPublicDate":"2005-10-13T11:50:53","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Implications for prediction and hazard assessment from the 2004 Parkfield earthquake","docAbstract":"<p><span>Obtaining high-quality measurements close to a large earthquake is not easy: one has to be in the right place at the right time with the right instruments. Such a convergence happened, for the first time, when the 28 September 2004 Parkfield, California, earthquake occurred on the San Andreas fault in the middle of a dense network of instruments designed to record it. The resulting data reveal aspects of the earthquake process never before seen. Here we show what these data, when combined with data from earlier Parkfield earthquakes, tell us about earthquake physics and earthquake prediction. The 2004 Parkfield earthquake, with its lack of obvious precursors, demonstrates that reliable short-term earthquake prediction still is not achievable. To reduce the societal impact of earthquakes now, we should focus on developing the next generation of models that can provide better predictions of the strength and location of damaging ground shaking.</span></p>","language":"English","publisher":"Springer","doi":"10.1038/nature04067","usgsCitation":"Bakun, W.H., Aagaard, B.T., Dost, B., Ellsworth, W.L., Hardebeck, J.L., Harris, R.A., Ji, C., Johnston, M.J., Langbein, J.O., Lienkaemper, J.J., Michael, A.J., Murray, J.R., Nadeau, R., Reasenberg, P., Reichle, M., Roeloffs, E.A., Shakal, A., Simpson, R.W., and Waldhauser, F., 2005, Implications for prediction and hazard assessment from the 2004 Parkfield earthquake: Nature, v. 437, p. 969-974, https://doi.org/10.1038/nature04067.","productDescription":"6 p.","startPage":"969","endPage":"974","costCenters":[],"links":[{"id":477643,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://resolver.caltech.edu/CaltechAUTHORS:20150403-080028282","text":"External Repository"},{"id":409458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Parkfield","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.4537640117938,\n              35.910700976762385\n            ],\n            [\n              -120.4537640117938,\n              35.88567088811958\n            ],\n            [\n              -120.41342358821001,\n              35.88567088811958\n            ],\n            [\n              -120.41342358821001,\n              35.910700976762385\n            ],\n            [\n              -120.4537640117938,\n              35.910700976762385\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"437","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bakun, W. H.","contributorId":67055,"corporation":false,"usgs":true,"family":"Bakun","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":857297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aagaard, Brad T. 0000-0002-8795-9833 baagaard@usgs.gov","orcid":"https://orcid.org/0000-0002-8795-9833","contributorId":192869,"corporation":false,"usgs":true,"family":"Aagaard","given":"Brad","email":"baagaard@usgs.gov","middleInitial":"T.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":857298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dost, B.","contributorId":299207,"corporation":false,"usgs":false,"family":"Dost","given":"B.","email":"","affiliations":[{"id":16158,"text":"Royal Netherlands Meteorological Institute","active":true,"usgs":false}],"preferred":false,"id":857299,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ellsworth, William L. ellsworth@usgs.gov","contributorId":787,"corporation":false,"usgs":true,"family":"Ellsworth","given":"William","email":"ellsworth@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857300,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hardebeck, Jeanne L. 0000-0002-6737-7780 jhardebeck@usgs.gov","orcid":"https://orcid.org/0000-0002-6737-7780","contributorId":841,"corporation":false,"usgs":true,"family":"Hardebeck","given":"Jeanne","email":"jhardebeck@usgs.gov","middleInitial":"L.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857301,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Harris, Ruth A. 0000-0002-9247-0768 harris@usgs.gov","orcid":"https://orcid.org/0000-0002-9247-0768","contributorId":786,"corporation":false,"usgs":true,"family":"Harris","given":"Ruth","email":"harris@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857302,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ji, C.","contributorId":31093,"corporation":false,"usgs":true,"family":"Ji","given":"C.","email":"","affiliations":[],"preferred":false,"id":857303,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Johnston, Malcolm J. S. 0000-0003-4326-8368 mal@usgs.gov","orcid":"https://orcid.org/0000-0003-4326-8368","contributorId":622,"corporation":false,"usgs":true,"family":"Johnston","given":"Malcolm","email":"mal@usgs.gov","middleInitial":"J. S.","affiliations":[],"preferred":true,"id":857304,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Langbein, John O. 0000-0002-7821-8101 langbein@usgs.gov","orcid":"https://orcid.org/0000-0002-7821-8101","contributorId":3293,"corporation":false,"usgs":true,"family":"Langbein","given":"John","email":"langbein@usgs.gov","middleInitial":"O.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857305,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lienkaemper, James J. 0000-0002-7578-7042 jlienk@usgs.gov","orcid":"https://orcid.org/0000-0002-7578-7042","contributorId":1941,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"James","email":"jlienk@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857306,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Michael, Andrew J. 0000-0002-2403-5019 michael@usgs.gov","orcid":"https://orcid.org/0000-0002-2403-5019","contributorId":1280,"corporation":false,"usgs":true,"family":"Michael","given":"Andrew","email":"michael@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":857307,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Murray, Jessica R. 0000-0002-6144-1681 jrmurray@usgs.gov","orcid":"https://orcid.org/0000-0002-6144-1681","contributorId":2759,"corporation":false,"usgs":true,"family":"Murray","given":"Jessica","email":"jrmurray@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857308,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Nadeau, R.M.","contributorId":93268,"corporation":false,"usgs":true,"family":"Nadeau","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":857309,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Reasenberg, P.A.","contributorId":19959,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":857310,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Reichle, M.S.","contributorId":14845,"corporation":false,"usgs":true,"family":"Reichle","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":857311,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Roeloffs, Evelyn A. 0000-0002-4761-0469 evelynr@usgs.gov","orcid":"https://orcid.org/0000-0002-4761-0469","contributorId":2680,"corporation":false,"usgs":true,"family":"Roeloffs","given":"Evelyn","email":"evelynr@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":857312,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Shakal, A.","contributorId":20934,"corporation":false,"usgs":false,"family":"Shakal","given":"A.","email":"","affiliations":[{"id":12640,"text":"California Geological Survey","active":true,"usgs":false}],"preferred":false,"id":857313,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":857314,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Waldhauser, F.","contributorId":31897,"corporation":false,"usgs":true,"family":"Waldhauser","given":"F.","affiliations":[],"preferred":false,"id":857315,"contributorType":{"id":1,"text":"Authors"},"rank":19}]}}
,{"id":72465,"text":"ds137 - 2005 - Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database","interactions":[],"lastModifiedDate":"2022-07-11T19:32:27.803531","indexId":"ds137","displayToPublicDate":"2005-10-12T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"137","title":"Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database","docAbstract":"This digital map database has been prepared by R.W. Tabor from the published Geologic map of the Wenatchee 1:100,000 Quadrangle, Central Washington. Together with the accompanying text files as PDF, it provides information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The authors mapped most of the bedrock geology at 1:100,000 scale, but compiled Quaternary units at 1:24,000 scale. The Quaternary contacts and structural data have been much simplified for the 1:100,000-scale map and database. The spatial resolution (scale) of the database is 1:100,000 or smaller. \r\n\r\nThis database depicts the distribution of geologic materials and structures at a regional (1:100,000) scale. The report is intended to provide geologic information for the regional study of materials properties, earthquake shaking, landslide potential, mineral hazards, seismic velocity, and earthquake faults. In addition, the report contains information and interpretations about the regional geologic history and framework. However, the regional scale of this report does not provide sufficient detail for site development purposes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds137","usgsCitation":"Tabor, R.W., Waitt, R., Frizzell, V.A., Swanson, D.A., Byerly, G.R., and Bentley, R.D., 2005, Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database (Version 1.0): U.S. Geological Survey Data Series 137, HTML Document, https://doi.org/10.3133/ds137.","productDescription":"HTML Document","costCenters":[],"links":[{"id":193165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403430,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73770.htm","linkFileType":{"id":5,"text":"html"}},{"id":7494,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/137/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Wenatchee quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              47\n            ],\n            [\n              -120,\n              47\n            ],\n            [\n              -120,\n              47.5\n            ],\n            [\n              -121,\n              47.5\n            ],\n            [\n              -121,\n              47\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a80ce","contributors":{"authors":[{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waitt, R. B.","contributorId":78766,"corporation":false,"usgs":true,"family":"Waitt","given":"R. B.","affiliations":[],"preferred":false,"id":285695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frizzell, V. A. Jr.","contributorId":39376,"corporation":false,"usgs":true,"family":"Frizzell","given":"V.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285694,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swanson, D. A.","contributorId":34102,"corporation":false,"usgs":true,"family":"Swanson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285693,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Byerly, G. R.","contributorId":6826,"corporation":false,"usgs":true,"family":"Byerly","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285691,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bentley, R. D.","contributorId":85561,"corporation":false,"usgs":true,"family":"Bentley","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285696,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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