{"pageNumber":"2148","pageRowStart":"53675","pageSize":"25","recordCount":184617,"records":[{"id":86135,"text":"ofr20081221 - 2008 - Earthquakes in Ohio and Vicinity 1776-2007","interactions":[],"lastModifiedDate":"2012-02-10T00:11:42","indexId":"ofr20081221","displayToPublicDate":"2008-08-23T00:00:00","publicationYear":"2008","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":"2008-1221","title":"Earthquakes in Ohio and Vicinity 1776-2007","docAbstract":"This map summarizes two and a third centuries of earthquake activity. The seismic history consists of letters, journals, diaries, and newspaper and scholarly articles that supplement seismograph recordings (seismograms) dating from the early twentieth century to the present. All of the pre-instrumental (historical) earthquakes were large enough to be felt by people or to cause shaking damage to buildings and their contents. Later, widespread use of seismographs meant that tremors too small or distant to be felt could be detected and accurately located.\r\nEarthquakes are a legitimate concern in Ohio and parts of adjacent States. Ohio has experienced more than 160 felt earthquakes since 1776. Most of these events caused no damage or injuries. However, 15 Ohio earthquakes resulted in property damage and some minor injuries. The largest historic earthquake in the state occurred in 1937. This event had an estimated magnitude of 5.4 and caused considerable damage in the town of Anna and in several other western Ohio communities. The large map shows all historical and instrumentally located earthquakes from 1776 through 2007.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081221","collaboration":"Prepared in cooperation with the Ohio Department of Natural Resources, Division of Geological Survey","usgsCitation":"Dart, R.L., and Hansen, M.C., 2008, Earthquakes in Ohio and Vicinity 1776-2007 (Version 1.0): U.S. Geological Survey Open-File Report 2008-1221, Report: 1 p.; Downloads Directory, https://doi.org/10.3133/ofr20081221.","productDescription":"Report: 1 p.; Downloads Directory","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":194537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11702,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1221/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.5,38 ], [ -85.5,42.5 ], [ -79.75,42.5 ], [ -79.75,38 ], [ -85.5,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db629654","contributors":{"authors":[{"text":"Dart, Richard L. dart@usgs.gov","contributorId":1209,"corporation":false,"usgs":true,"family":"Dart","given":"Richard","email":"dart@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":296916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, Michael C.","contributorId":67612,"corporation":false,"usgs":false,"family":"Hansen","given":"Michael","email":"","middleInitial":"C.","affiliations":[{"id":16232,"text":"Ohio Department of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":296917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86133,"text":"sir20085112 - 2008 - Precipitation-Frequency and Discharge-Frequency Relations for Basins Less than 32 Square Miles in Kansas","interactions":[],"lastModifiedDate":"2012-03-08T17:16:26","indexId":"sir20085112","displayToPublicDate":"2008-08-23T00:00:00","publicationYear":"2008","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":"2008-5112","title":"Precipitation-Frequency and Discharge-Frequency Relations for Basins Less than 32 Square Miles in Kansas","docAbstract":"Precipitation-frequency and discharge-frequency relations for small drainage basins with areas less than 32 square miles in Kansas were evaluated to reduce the uncertainty of discharge-frequency estimates. Gaged-discharge records were used to develop discharge-frequency equations for the ratio of discharge to drainage area (Q/A) values using data from basins with variable soil permeability, channel slope, and mean annual precipitation. Soil permeability and mean annual precipitation are the dominant basin characteristics in the multiple linear regression analyses.\r\n\r\nIn addition, 28 discharge measurements at ungaged sites by indirect surveying methods and by velocity meters also were used in this analysis to relate precipitation-recurrence interval to discharge-recurrence interval. Precipitation-recurrence interval for each of these discharge measurements were estimated from weather-radar estimates of precipitation and from nearby raingages. Time of concentration for each basin for each of the ungaged sites was computed and used to determine the precipitation-recurrence interval based on precipitation depth and duration. The ratio of discharge/drainage area (Q/A) value for each event was then assigned to that precipitation-recurrence interval. \r\n\r\nThe relation between the ratio of discharge/drainage area (Q/A) and precipitation-recurrence interval for all 28 measured events resulted in a correlation coefficient of 0.79. Using basins less than 5.4 mi2 only, the correlation decreases to 0.74. However, when basins greater than 5.4 and less than 32 mi2 are examined the relation improves to a correlation coefficient of 0.95.\r\n\r\nThere were a sufficient number of discharge and radar-measured precipitation events for both the 5-year (8 events) and the 100-year (11 events) recurrence intervals to examine the effect of basin characteristics on the Q/A values for basins less than 32 mi2. At the 5-year precipitation-/discharge-recurrence interval, channel slope was a significant predictor (r=0.99) of Q/A. Permeability (r=0.68) also had a significant effect on Q/A values for the 5-year recurrence interval. At the 100-year recurrence interval, permeability, channel slope, and mean annual precipitation did not have a significant effect on Q/A; however, time of concentration was a significant factor in determining Q/A for the 100-year events with greater times of concentration resulting in lower Q/A values. Additional high-recurrence interval (5-, 10-, 25-, 50-, and 100-year) precipitation/discharge data are needed to confirm these relations suggested above. Discharge data with attendant basin-wide precipitation data from precipitation-radar estimates provides a unique opportunity to study the effects of basin characteristics on the relation between precipitation recurrence interval and discharge-recurrence interval.\r\n\r\nDischarge-frequency values from the Q/A equations, the rational method, and the Kansas discharge-frequency equations (KFFE) were compared to 28 measured weather-radar precipitation-/discharge-frequency values. The association between precipitation frequency from weather-radar estimates and the frequency of the resulting discharge was shown in these comparisons. The measured and Q/A equation computed discharges displayed the best equality from low to high discharges of the three methods. Here the slope of the line was nearly 1:1 (y=0.9844x0.9677). Comparisons with the rational method produced a slope greater than 1:1 (y=0.0722x1.235), and the KFFE equations produced a slope less than 1:1 (y=5.9103x0.7475). The Q/A equation standard error of prediction averaged 0.1346 log units for the 5.4-to 32-square-mile group and 0.0944 log units for the less than 5.4-square mile group. The KFFE standard error averaged 0.2107 log units for the less-than-30-square-mile equations. Using the Q/A equations for determining discharge frequency values for ungaged sites thus appears to be a good alternative to the other two methods because of this s","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20085112","collaboration":"Prepared in cooperation with the Kansas Department of Transportation","usgsCitation":"Perry, C.A., 2008, Precipitation-Frequency and Discharge-Frequency Relations for Basins Less than 32 Square Miles in Kansas: U.S. Geological Survey Scientific Investigations Report 2008-5112, vi, 25 p., https://doi.org/10.3133/sir20085112.","productDescription":"vi, 25 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":195795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11700,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5112/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.08333333333333,37 ], [ -102.08333333333333,40 ], [ -94.58333333333333,40 ], [ -94.58333333333333,37 ], [ -102.08333333333333,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69bae3","contributors":{"authors":[{"text":"Perry, Charles A. cperry@usgs.gov","contributorId":2093,"corporation":false,"usgs":true,"family":"Perry","given":"Charles","email":"cperry@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":296914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86132,"text":"sir20085118 - 2008 - Aquifer Tests and Characterization of Transmissivity, Ada-Vamoosa Aquifer on the Osage Reservation, Osage County, Oklahoma, 2006","interactions":[],"lastModifiedDate":"2012-02-10T00:11:42","indexId":"sir20085118","displayToPublicDate":"2008-08-23T00:00:00","publicationYear":"2008","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":"2008-5118","title":"Aquifer Tests and Characterization of Transmissivity, Ada-Vamoosa Aquifer on the Osage Reservation, Osage County, Oklahoma, 2006","docAbstract":"The Ada-Vamoosa aquifer of northeastern Oklahoma is a sedimentary bedrock aquifer of Pennsylvanian age that crops out over 800 square miles of the Osage Reservation. The Osage Nation needed additional information regarding the production potential of the aquifer to aid them in future development planning. To address this need, the U.S. Geological Survey, in cooperation with the Osage Nation, conducted a study of aquifer properties in the Ada-Vamoosa aquifer. This report presents the results of the aquifer tests from 20 wells in the Ada-Vamoosa aquifer and one well in a minor aquifer east of the Ada-Vamoosa outcrop on the Osage Reservation. Well information for 17 of the 21 wells in this report was obtained from the Indian Health Service. Data collected by the U.S. Geological Survey during this investigation are pumping well data from four domestic wells collected during the summer of 2006. Transmissivity values were calculated from well pumping data or were estimated from specific capacity values depending on the reliability of the data. The estimated transmissivity values are 1.1 to 4.3 times greater than the calculated transmissivity values. The calculated and estimated transmissivity values range from 5 to 1,000 feet squared per day.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20085118","collaboration":"Prepared in cooperation with the Osage Tribal Council","usgsCitation":"Abbott, M.M., and DeHay, K., 2008, Aquifer Tests and Characterization of Transmissivity, Ada-Vamoosa Aquifer on the Osage Reservation, Osage County, Oklahoma, 2006 (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2008-5118, iv, 10 p., https://doi.org/10.3133/sir20085118.","productDescription":"iv, 10 p.","onlineOnly":"Y","temporalStart":"2006-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":121165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5118.jpg"},{"id":11699,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5118/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.16666666666667,36.083333333333336 ], [ -97.16666666666667,37.083333333333336 ], [ -95.91666666666667,37.083333333333336 ], [ -95.91666666666667,36.083333333333336 ], [ -97.16666666666667,36.083333333333336 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a067","contributors":{"authors":[{"text":"Abbott, Marvin M.","contributorId":89106,"corporation":false,"usgs":true,"family":"Abbott","given":"Marvin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":296913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeHay, Kelli","contributorId":14064,"corporation":false,"usgs":true,"family":"DeHay","given":"Kelli","affiliations":[],"preferred":false,"id":296912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86123,"text":"fs20083046 - 2008 - Detecting Evidence of Climate Change in the Forests of the Eastern United States","interactions":[],"lastModifiedDate":"2012-02-10T00:11:42","indexId":"fs20083046","displayToPublicDate":"2008-08-22T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3046","title":"Detecting Evidence of Climate Change in the Forests of the Eastern United States","docAbstract":"Changes in land use or disturbances such as defoliation by insects, disease, or fire all affect the composition and amount of tree canopy in a forest. These changes are easy to detect. Noticing and understanding the complex ways that global or regional-scale climate change combines with these disturbances to affect forest growth patterns and succession is difficult. This is particularly true for regions where changes in climate are not the most extreme, such as the mid-latitude forests of the Eastern United States. If land and water resources are to be managed responsibly, it is important to know how well the impacts of climate change on these forests can be measured in order to provide the best information possible to respond to any future changes. The goal of this study is to test whether climate-induced changes in forests in the Eastern United States can be detected and characterized using satellite imagery.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20083046","usgsCitation":"Jones, J., and Osborne, J.D., 2008, Detecting Evidence of Climate Change in the Forests of the Eastern United States: U.S. Geological Survey Fact Sheet 2008-3046, 2 p., https://doi.org/10.3133/fs20083046.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3046.jpg"},{"id":11690,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3046/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79,38 ], [ -79,39 ], [ -78,39 ], [ -78,38 ], [ -79,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667d17","contributors":{"authors":[{"text":"Jones, John 0000-0001-6117-3691 jwjones@usgs.gov","orcid":"https://orcid.org/0000-0001-6117-3691","contributorId":2220,"corporation":false,"usgs":true,"family":"Jones","given":"John","email":"jwjones@usgs.gov","affiliations":[{"id":37786,"text":"WMA - Observing Systems Division","active":true,"usgs":true},{"id":242,"text":"Eastern Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":296885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Osborne, Jesse D.","contributorId":90264,"corporation":false,"usgs":true,"family":"Osborne","given":"Jesse","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":296886,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86130,"text":"sim3002 - 2008 - Geologic Map of the Eastern Three-Quarters of the Cuyama 30' x 60' Quadrangle, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:47","indexId":"sim3002","displayToPublicDate":"2008-08-22T00:00:00","publicationYear":"2008","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":"3002","title":"Geologic Map of the Eastern Three-Quarters of the Cuyama 30' x 60' Quadrangle, California","docAbstract":"The map area encompasses a large part of the western Transverse Ranges\r\nand southern Coast Ranges of southern California.  The San Andreas fault\r\n(SAF) cuts the northern part of the map.  The area south of the SAF, about\r\n80 percent of the map area, encompasses several distinct tectonic blocks\r\nbounded by major thrust or reverse faults, including the Santa Ynez fault,\r\nBig Pine fault (and structurally continuous Pine Mountain fault), Tule Creek\r\nfault, Nacimiento fault, Ozena fault, Munson Creek fault, Morales fault,\r\nand Frazier Mountain Thrust System.  Movement on these faults is as old as\r\nMiocene and some faults may still be active.  In addition, the Paleocene\r\nSawmill Mountain Thrust south of the SAF and the Pastoria Thrust north of\r\nthe SAF place Cretaceous and older crystalline rocks above Pelona Schist\r\n(south of the SAF) and Rand Schist (north of the SAF).\r\n\r\n      South of the SAF, each tectonic block contains a unique stratigraphy,\r\nreflecting either large-scale movement on bounding faults or different\r\ndepositional environments within each block.  On Mount Pinos and Frazier\r\nMountain, intrusive and metamorphic rocks as old as Mesoproterozoic, but\r\nincluding voluminous Cretaceous granitoid rocks, underlie or are thrust\r\nabove non-marine sedimentary rocks as old as Miocene.  Elsewhere, marine\r\nand non-marine sedimentary rocks are as old as Cretaceous, dominated by\r\nthick sequences of both Eocene and Cretaceous marine shales and sandstones.\r\nMiddle Miocene to early Oligocene volcanic rocks crop out in the Caliente\r\nHills (part of Caliente Formation) and south of Mount Pinos (part of the\r\nPlush Ranch Formation). Fault-bounded windows of Jurassic Franciscan\r\nComplex ophiolitic rocks are evident in the southwest corner of the area.\r\n\r\n      North of the SAF, marine and non-marine sedimentary rocks as old as\r\nEocene and Miocene volcanic rocks overlie a crystalline basement complex.\r\nBasement rocks include Cretaceous intrusive rocks that range from\r\nmonzogranite to diorite, and Jurassic to late Paleozoic intrusive and\r\nmetamorphic rocks.  The Jurassic to late Paleozoic intrusive rocks include\r\ndiorite, gabbro, and ultramafic rocks, and the metasedimentary rocks\r\ninclude marble, quartzite, schist, and gneiss.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sim3002","isbn":"9781411320895","collaboration":"Prepared in cooperation with the U.S. Forest Service","usgsCitation":"Kellogg, K., Minor, S.A., and Cossette, P.M., 2008, Geologic Map of the Eastern Three-Quarters of the Cuyama 30' x 60' Quadrangle, California (Version 1.0): U.S. Geological Survey Scientific Investigations Map 3002, Report: iv, 24 p.; 2 Map Sheets: Plate 1 - 39 x 29 inches, Plate 2 - 39 x 33 inches; Downloads Directory, https://doi.org/10.3133/sim3002.","productDescription":"Report: iv, 24 p.; 2 Map Sheets: Plate 1 - 39 x 29 inches, Plate 2 - 39 x 33 inches; Downloads Directory","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":110787,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_84253.htm","linkFileType":{"id":5,"text":"html"},"description":"84253"},{"id":195770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11697,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/3002/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,34.5 ], [ -120,35 ], [ -119,35 ], [ -119,34.5 ], [ -120,34.5 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68888d","contributors":{"authors":[{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":296909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minor, Scott A. 0000-0002-6976-9235 sminor@usgs.gov","orcid":"https://orcid.org/0000-0002-6976-9235","contributorId":765,"corporation":false,"usgs":true,"family":"Minor","given":"Scott","email":"sminor@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":296907,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cossette, Pamela M. 0000-0002-9608-6595 pcossette@usgs.gov","orcid":"https://orcid.org/0000-0002-9608-6595","contributorId":1458,"corporation":false,"usgs":true,"family":"Cossette","given":"Pamela","email":"pcossette@usgs.gov","middleInitial":"M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":296908,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":86126,"text":"ofr20081120 - 2008 - User's Manual for the Object User Interface (OUI): An Environmental Resource Modeling Framework","interactions":[],"lastModifiedDate":"2012-02-02T00:14:26","indexId":"ofr20081120","displayToPublicDate":"2008-08-22T00:00:00","publicationYear":"2008","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":"2008-1120","title":"User's Manual for the Object User Interface (OUI): An Environmental Resource Modeling Framework","docAbstract":"The Object User Interface is a computer application that provides a framework for coupling environmental-resource models and for managing associated temporal and spatial data. The Object User Interface is designed to be easily extensible to incorporate models and data interfaces defined by the user. Additionally, the Object User Interface is highly configurable through the use of a user-modifiable, text-based control file that is written in the eXtensible Markup Language. The Object User Interface user's manual provides (1) installation instructions, (2) an overview of the graphical user interface, (3) a description of the software tools, (4) a project example, and (5) specifications for user configuration and extension.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081120","usgsCitation":"Markstrom, S., and Koczot, K.M., 2008, User's Manual for the Object User Interface (OUI): An Environmental Resource Modeling Framework (Version 1.0): U.S. Geological Survey Open-File Report 2008-1120, vi, 39 p., https://doi.org/10.3133/ofr20081120.","productDescription":"vi, 39 p.","onlineOnly":"Y","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":195549,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11693,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1120/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604012","contributors":{"authors":[{"text":"Markstrom, Steven L. 0000-0001-7630-9547 markstro@usgs.gov","orcid":"https://orcid.org/0000-0001-7630-9547","contributorId":1986,"corporation":false,"usgs":true,"family":"Markstrom","given":"Steven L.","email":"markstro@usgs.gov","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":false,"id":296892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koczot, Kathryn M. 0000-0001-5728-9798 kmkoczot@usgs.gov","orcid":"https://orcid.org/0000-0001-5728-9798","contributorId":2039,"corporation":false,"usgs":true,"family":"Koczot","given":"Kathryn","email":"kmkoczot@usgs.gov","middleInitial":"M.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296893,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86129,"text":"pp1755 - 2008 - Terrestrial Cosmogenic-Nuclide Dating of Alluvial Fans in Death Valley, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:42","indexId":"pp1755","displayToPublicDate":"2008-08-22T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1755","title":"Terrestrial Cosmogenic-Nuclide Dating of Alluvial Fans in Death Valley, California","docAbstract":"We have used terrestrial cosmogenic nuclides (TCN) to establish the age of some of the most extensive Quaternary alluvial fans in Death Valley, California. These intermediate-age alluvial fans are most extensive on the western side of the valley, where tectonic deformation is considerably less pronounced than on the eastern side of the valley. These fans are characterized by a relatively smooth, densely packed desert pavement formed by well-varnished (blackened) clasts. These surfaces have been mapped as the Q2 gravel by previous workers and as unit Qai (intermediate age) by us. However, the intermediate-age gravels probably contain multiple subunits, as evidenced by slight differences in morphologic expression, soil formation, and inset geomorphic relations. The TCN technique used herein sums the cosmogenic 36Cl in approximately 2.5-meter-deep profiles through soil and host alluvium, thus avoiding some of the problems associated with the more typical surface-exposure dating of boulders or smaller clasts.\r\n      Our TCN 36Cl dating of 12 depth profiles indicates that these intermediate-age (Qai) alluvial fans range from about 100 to 40 kilo-annum (ka), with a mean age of about 70 ka. An alternative interpretation is that alluvial unit Qai was deposited in two discrete episodes from 90 to 80 ka and from 60 to 50 ka, before and after MIS (marine oxygen-isotope stage) 4 (respectively). Without an intermediate-age unit, such as MIS 4 lake deposits, we can neither disprove nor prove that Qai was deposited in two discrete intervals or over a longer range of time. Thus, in Death Valley, alluvial unit Qai largely brackets MIS 4, which is not associated with a deep phase of Lake Manly. These Qai fans extend to elevations of about -46 meters (150 feet below sea level) and have not been transgressed by Lake Manly, suggesting that MIS 4 or MIS 2 lakes were rather shallow in Death Valley, perhaps because they lacked inflow from surface runoff of the Sierra Nevada drainages through Panamint Valley and over Wingate Wash.\r\n      A remnant of ancient lake shoreline deposits that once extended across the Hanaupah Canyon fan constrains the timing and extent of the last deep cycle of Pleistocene Lake Manly. The lacustrine delta complex yields a 36Cl depth-profile date of 130 ka, which is consistent with deposition during a highstand of Lake Manly at the end of MIS 6. These deposits are presently at an altitude of about 30 meters above sea level (asl), which relates to a lake with a maximum depth of about 115 meters. Remnants of shoreline deposits at higher elevations on the southern margin of the Hanaupah Canyon fan complex are cut across older alluvium (unit Qao) and may be related to an MIS 6 highstand of at least 67 meters asl or, more likely, an older (MIS 8 or earlier) highstand that is poorly preserved and still undated in the valley.\r\n      As part of our work on the west-side fans, we also dated an older phase of alluvial-fan deposits from the Trail Canyon fan complex, which is north of Hanaupah Canyon. A 36Cl depth-profile age of 170 ka suggests alluvial deposition of unit Qaio (older phase of Qao) took place prior to the MIS 6 highstand of Lake Manly.\r\n      Knowing the absolute ages (or range in ages) of the intermediate-age (Qai) surfaces in Death Valley allows us to estimate the following rates of geologic processes: (1) a lateral slip rate of 5 millimeters per year for the northern Death Valley fault zone; (2) uplift of 50 meters in roughly the past 80,000 years for parts of the Mustard Canyon hills in east-central Death Valley; and (3) an estimated 10-40 m of dip-slip thrust movement on the Echo Canyon fault in Furnace Creek Canyon.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/pp1755","isbn":"9781411321878","usgsCitation":"Machette, M., Slate, J.L., and Phillips, F.M., 2008, Terrestrial Cosmogenic-Nuclide Dating of Alluvial Fans in Death Valley, California: U.S. Geological Survey Professional Paper 1755, Report: vi, 45 p.; Appendix 9, https://doi.org/10.3133/pp1755.","productDescription":"Report: vi, 45 p.; Appendix 9","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":190893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp1755.gif"},{"id":11696,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/1755/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.5,35.5 ], [ -117.5,37 ], [ -116.5,37 ], [ -116.5,35.5 ], [ -117.5,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6851be","contributors":{"authors":[{"text":"Machette, Michael N.","contributorId":28963,"corporation":false,"usgs":true,"family":"Machette","given":"Michael N.","affiliations":[],"preferred":false,"id":296905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slate, Janet L. 0000-0002-2870-9068 jslate@usgs.gov","orcid":"https://orcid.org/0000-0002-2870-9068","contributorId":252,"corporation":false,"usgs":true,"family":"Slate","given":"Janet","email":"jslate@usgs.gov","middleInitial":"L.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true}],"preferred":true,"id":296904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Phillips, Fred M.","contributorId":57957,"corporation":false,"usgs":true,"family":"Phillips","given":"Fred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":296906,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":86122,"text":"sir20085110 - 2008 - Assessment of nonpoint source chemical loading potential to watersheds containing uranium waste dumps associated with uranium exploration and mining, San Rafael Swell, Utah","interactions":[],"lastModifiedDate":"2017-01-25T11:57:32","indexId":"sir20085110","displayToPublicDate":"2008-08-22T00:00:00","publicationYear":"2008","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":"2008-5110","title":"Assessment of nonpoint source chemical loading potential to watersheds containing uranium waste dumps associated with uranium exploration and mining, San Rafael Swell, Utah","docAbstract":"During July and August of 2006, 117 solid-phase samples were collected from abandoned uranium waste dumps, geologic background sites, and adjacent streambeds in the San Rafael Swell, in southeastern Utah. The objective of this sampling program was to assess the nonpoint source chemical loading potential to ephemeral and perennial watersheds from uranium waste dumps on Bureau of Land Management property. Uranium waste dump samples were collected using solid-phase sampling protocols. After collection, solid-phase samples were homogenized and extracted in the laboratory using a field leaching procedure. Filtered (0.45 micron) water samples were obtained from the field leaching procedure and were analyzed for Ag, As, Ba, Be, Cd, Cr, Cu, Fe, Mn, Mo, Ni, Pb, Sb, Se, U, V, and Zn at the Inductively Coupled Plasma-Mass Spectrometry Metals Analysis Laboratory at the University of Utah, Salt Lake City, Utah and for Hg at the U.S. Geological Survey National Water Quality Laboratory, Denver, Colorado.\r\nFor the initial ranking of chemical loading potential of suspect uranium waste dumps, leachate analyses were compared with existing aquatic life and drinking-water-quality standards and the ratio of samples that exceeded standards to the total number of samples was determined for each element having a water-quality standard for aquatic life and drinking-water.\r\nApproximately 56 percent (48/85) of the leachate samples extracted from uranium waste dumps had one or more chemical constituents that exceeded aquatic life and drinking-water-quality standards. Most of the uranium waste dump sites with elevated trace-element concentrations in leachates were along Reds Canyon Road between Tomsich Butte and Family Butte. Twelve of the uranium waste dump sites with elevated trace-element concentrations in leachates contained three or more constituents that exceeded drinking-water-quality standards. Eighteen of the uranium waste dump sites had three or more constituents that exceeded trace-element concentrations for aquatic life water-quality standards. The proximity of the uranium waste dumps in the Tomsich Butte area near Muddy Creek, coupled with the elevated concentration of trace elements, increases the offsite impact potential to water resources. Future assessment and remediation priority of these areas may be done by using GIS-based risk-mapping techniques, such as Sensitive Catchment Integrated Mapping and Analysis Project.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20085110","collaboration":"Prepared in cooperation with the Bureau of Land Management","usgsCitation":"Freeman, M.L., Naftz, D.L., Snyder, T., and Johnson, G., 2008, Assessment of nonpoint source chemical loading potential to watersheds containing uranium waste dumps associated with uranium exploration and mining, San Rafael Swell, Utah: U.S. Geological Survey Scientific Investigations Report 2008-5110, vi, 28 p., https://doi.org/10.3133/sir20085110.","productDescription":"vi, 28 p.","temporalStart":"2006-07-01","temporalEnd":"2006-08-31","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":124341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5110.jpg"},{"id":11689,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5110/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"San Rafael Swell","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.16666666666667,38.5 ], [ -111.16666666666667,39.166666666666664 ], [ -110.33333333333333,39.166666666666664 ], [ -110.33333333333333,38.5 ], [ -111.16666666666667,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672901","contributors":{"authors":[{"text":"Freeman, Michael L. mfreeman@usgs.gov","contributorId":1042,"corporation":false,"usgs":true,"family":"Freeman","given":"Michael","email":"mfreeman@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":296882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Naftz, David L. 0000-0003-1130-6892 dlnaftz@usgs.gov","orcid":"https://orcid.org/0000-0003-1130-6892","contributorId":1041,"corporation":false,"usgs":true,"family":"Naftz","given":"David","email":"dlnaftz@usgs.gov","middleInitial":"L.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Snyder, Terry","contributorId":30708,"corporation":false,"usgs":true,"family":"Snyder","given":"Terry","email":"","affiliations":[],"preferred":false,"id":296883,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Greg","contributorId":50240,"corporation":false,"usgs":true,"family":"Johnson","given":"Greg","email":"","affiliations":[],"preferred":false,"id":296884,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":86125,"text":"ofr20081024 - 2008 - A Regional Approach to Wildlife Monitoring Related to Energy Exploration and Development in Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:46","indexId":"ofr20081024","displayToPublicDate":"2008-08-22T00:00:00","publicationYear":"2008","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":"2008-1024","title":"A Regional Approach to Wildlife Monitoring Related to Energy Exploration and Development in Colorado","docAbstract":"The U.S. Bureau of Land Management (BLM) is currently developing a National Monitoring Strategy that will guide efforts to create an efficient and effective process for monitoring land health by BLM. To inform the ongoing development of the national strategy, BLM selected two States (Colorado, Alaska) to serve as focal areas on which to base a flexible framework for developing monitoring programs that evaluate wildlife responses to energy development. \r\nWe developed a three-phase monitoring plan to serve as a template and applied it to the design of a monitoring program for the Colorado focal area (White River and Glenwood Springs Field Offices of the BLM). Phase I is a synthesis and assessment of current conditions that capitalizes on existing but under used data sources. A key component is the use of existing habitat and landscape models to evaluate the cumulative effects of surface disturbance. Phase II is the data collection process that uses information provided in Phase I to refine management objectives and provide a linkage to management decisions. The linkage is established through targeted monitoring, adaptive management, and research. Phase III establishes priorities and strategies for regional and national monitoring, and facilitates coordination among other land management agencies and organizations. The three phases are designed to be flexible and complementary. \r\nThe monitoring plan guides an iterative process that is performed incrementally, beginning with the highest-priority species and management issues, while building on lessons learned and coordination among administrative levels. The activities associated with each phase can be repeated or updated as new information, data, or tools become available. This allows the development of a monitoring program that expands gradually and allows for rapid implementation. \r\nA demonstration application of the three-phase monitoring plan was conducted for a study area encompassing five BLM field offices in Colorado: White River, Glenwood Springs, Kremmling, Grand Junction, and Little Snake. The overall study area was selected to encompass the primary distribution of sagebrush and greater sage-grouse (Centrocercus urophasianus) in Colorado and to provide a larger context for evaluating priority management issues of the White River and Glenwood Springs Field Offices. Within the study area, we selected an additional scale of analysis: the Roan Plateau, an area of increased energy development. We focused our demonstration project on the primary objectives identified by the BLM and other stakeholders: (1) How do we evaluate the cumulative effects of energy development and mitigation activities on species of management interest or concern? (2) How can cumulative effects, including direct and indirect effects, be quantified relative to natural variation? (3) How can we implement compliance and effectiveness monitoring to determine whether lease stipulations are met and restoration/mitigation goals are achieved? \r\nWe targeted greater sage-grouse because this species was identified as a monitoring priority for the White River Field Office. We also evaluated landscape-level indices to address fragmentation resulting from surface disturbance. The primary purpose of this exercise was to highlight the types of analyses and approaches that could be used to evaluate energy development in an application of the three-phase framework. We provide examples of Phase I products that can be used to guide the refinement of management objectives, development of adaptive management and research frameworks, and planning activities in Phase II. Finally, we report on the BLM's National Sage-Grouse Habitat Conservation Strategy as an example of Phase III activities. \r\nThe development of an effective monitoring program is a daunting task, and will be difficult to implement by the BLM independently due to the current work load of staff. However, the scientific expertise and experience for developing cr","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081024","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Kotliar, N.B., Bowen, Z.H., Ouren, D.S., and Farmer, A.H., 2008, A Regional Approach to Wildlife Monitoring Related to Energy Exploration and Development in Colorado (Version 1.0): U.S. Geological Survey Open-File Report 2008-1024, vii, 66 p., https://doi.org/10.3133/ofr20081024.","productDescription":"vii, 66 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11692,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1024/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.08333333333333,38 ], [ -109.08333333333333,41 ], [ -105,41 ], [ -105,38 ], [ -109.08333333333333,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4966e4b0b290850ef20f","contributors":{"authors":[{"text":"Kotliar, Natasha B.","contributorId":23116,"corporation":false,"usgs":true,"family":"Kotliar","given":"Natasha","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":296890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowen, Zachary H. 0000-0002-8656-1831 bowenz@usgs.gov","orcid":"https://orcid.org/0000-0002-8656-1831","contributorId":821,"corporation":false,"usgs":true,"family":"Bowen","given":"Zachary","email":"bowenz@usgs.gov","middleInitial":"H.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":296888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ouren, Douglas S. ourend@usgs.gov","contributorId":1931,"corporation":false,"usgs":true,"family":"Ouren","given":"Douglas","email":"ourend@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":296889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farmer, Adrian H.","contributorId":107759,"corporation":false,"usgs":true,"family":"Farmer","given":"Adrian","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":296891,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70258394,"text":"70258394 - 2008 - Development of Landsat-5 thematic mapper internal calibrator gain and offset table","interactions":[],"lastModifiedDate":"2024-09-16T16:25:12.563078","indexId":"70258394","displayToPublicDate":"2008-08-20T11:20:30","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Development of Landsat-5 thematic mapper internal calibrator gain and offset table","docAbstract":"<p><span>The National Landsat Archive Production System (NLAPS) has been the primary processing system for Landsat data since U.S. Geological Survey (USGS) Earth Resources Observation and Science Center (EROS) started archiving Landsat data. NLAPS converts raw satellite data into radiometrically and geometrically calibrated products. NLAPS has historically used the Internal Calibrator (IC) to calibrate the reflective bands of the Landsat-5 Thematic Mapper (TM), even though the lamps in the IC were less stable than the TM detectors, as evidenced by vicarious calibration results. In 2003, a major effort was made to model the actual TM gain change and to update NLAPS to use this model rather than the unstable IC data for radiometric calibration. The model coefficients were revised in 2007 to reflect greater understanding of the changes in the TM responsivity. While the calibration updates are important to users with recently processed data, the processing system no longer calculates the original IC gain or offset. For specific applications, it is useful to have a record of the gain and offset actually applied to the older data. Thus, the NLAPS calibration database was used to generate estimated daily values for the radiometric gain and offset that might have been applied to TM data. This paper discusses the need for and generation of the NLAPS IC gain and offset tables. A companion paper covers the application of and errors associated with using these tables.</span></p>","conferenceTitle":"Earth Observing Systems XIII","conferenceDate":"August 11-13, 2008","conferenceLocation":"San Diego, CA","language":"English","publisher":"SPIE","usgsCitation":"Barsi, J.A., Chander, G., Micijevic, E., Markham, B.L., and Haque, O., 2008, Development of Landsat-5 thematic mapper internal calibrator gain and offset table, Earth Observing Systems XIII, v. 7081, San Diego, CA, August 11-13, 2008, 708115.","productDescription":"708115","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":434786,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7081","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Barsi, Julia A.","contributorId":71822,"corporation":false,"usgs":false,"family":"Barsi","given":"Julia","email":"","middleInitial":"A.","affiliations":[{"id":12721,"text":"NASA GSFC SSAI","active":true,"usgs":false}],"preferred":false,"id":913186,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chander, Gyanesh gchander@usgs.gov","contributorId":3013,"corporation":false,"usgs":true,"family":"Chander","given":"Gyanesh","email":"gchander@usgs.gov","affiliations":[],"preferred":true,"id":913187,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Micijevic, Esad 0000-0002-3828-9239 emicijevic@usgs.gov","orcid":"https://orcid.org/0000-0002-3828-9239","contributorId":3075,"corporation":false,"usgs":true,"family":"Micijevic","given":"Esad","email":"emicijevic@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":913188,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Markham, Brian L. 0000-0002-9612-8169","orcid":"https://orcid.org/0000-0002-9612-8169","contributorId":121488,"corporation":false,"usgs":true,"family":"Markham","given":"Brian","email":"","middleInitial":"L.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":913189,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Haque, Obaidul 0000-0002-0914-1446 ohaque@usgs.gov","orcid":"https://orcid.org/0000-0002-0914-1446","contributorId":4691,"corporation":false,"usgs":true,"family":"Haque","given":"Obaidul","email":"ohaque@usgs.gov","affiliations":[{"id":40546,"text":"KBR, Contractor to the USGS Earth Resources Observation and Science (EROS) Center","active":true,"usgs":false}],"preferred":true,"id":913190,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":86120,"text":"fs20083064 - 2008 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008","interactions":[{"subject":{"id":86120,"text":"fs20083064 - 2008 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008","indexId":"fs20083064","publicationYear":"2008","noYear":false,"title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008"},"predicate":"SUPERSEDED_BY","object":{"id":70004633,"text":"fs20113050 - 2011 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010","indexId":"fs20113050","publicationYear":"2011","noYear":false,"title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010"},"id":1}],"supersededBy":{"id":70004633,"text":"fs20113050 - 2011 - Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010","indexId":"fs20113050","publicationYear":"2011","noYear":false,"title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2010"},"lastModifiedDate":"2018-07-31T11:35:50","indexId":"fs20083064","displayToPublicDate":"2008-08-20T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3064","title":"Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008","docAbstract":"The U.S. Geological Survey (USGS) recently assessed the undiscovered oil and gas potential of the West Siberian Basin Province in Russia as part of the USGS Circum-Arctic Resource Appraisal program. This province is the largest petroleum basin in the world and has an areal extent of about 2.2 million square kilometers. It is a large rift-sag feature bounded to the west by the Ural fold belt, to the north by the Novaya Zemlya fold belt and North Siberian Sill, to the south by the Turgay Depression and Altay-Sayan fold belt, and to the east by the Yenisey Ridge, Turukhan-Igarka uplift, Yenisey-Khatanga Basin, and Taimyr High. The West Siberian Basin Province has a total discovered oil and gas volume of more than 360 billion barrels of oil equivalent (Ulmishek, 2000). Exploration has led to the discovery of tens of giant oil and gas fields, including the Urengoy gas field with more than 3500 trillion cubic feet of gas reserves and Samotlar oil field with reserves of nearly 28 billion barrels of oil (Ulmishek, 2003). This report summarizes the results of a reassessment of the undiscovered oil and gas potential of that part of the province north of the Arctic Circle; a previous assessment that included the entire province was completed in 2000 (Ulmishek, 2000). The total petroleum system (TPS) and assessment units (AU) defined by the USGS for the assessments in 2000 were adopted for this assessment. However, only those parts of the Aus lying wholly or partially north of the Arctic Circle were assessed for this study.","language":"English","publisher":"U.S. Geological Survey ","doi":"10.3133/fs20083064","usgsCitation":"Schenk, C.J., Bird, K.J., Charpentier, R., Gautier, D.L., Houseknecht, D.W., Klett, T., Moore, T.E., Pawlewicz, M.J., Pitman, J.K., and Tennyson, M., 2008, Assessment of undiscovered oil and gas resources of the West Siberian Basin Province, Russia, 2008 (Version 1.0): U.S. Geological Survey Fact Sheet 2008-3064, 2 p., https://doi.org/10.3133/fs20083064.","productDescription":"2 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3064.jpg"},{"id":11686,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3064/","linkFileType":{"id":5,"text":"html"}}],"country":"Russia","otherGeospatial":"West Siberian Basin Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 35,50 ], [ 35,80 ], [ 95,80 ], [ 95,50 ], [ 35,50 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67292d","contributors":{"authors":[{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":296874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":296876,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Charpentier, Ronald R. charpentier@usgs.gov","contributorId":934,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","email":"charpentier@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":296875,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gautier, Donald L. gautier@usgs.gov","contributorId":1310,"corporation":false,"usgs":true,"family":"Gautier","given":"Donald","email":"gautier@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":296878,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Houseknecht, David W. 0000-0002-9633-6910 dhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-9633-6910","contributorId":645,"corporation":false,"usgs":true,"family":"Houseknecht","given":"David","email":"dhouse@usgs.gov","middleInitial":"W.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":296870,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":296871,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Moore, Thomas E. 0000-0002-0878-0457 tmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":1033,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas","email":"tmoore@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":296877,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Pawlewicz, Mark J. pawlewicz@usgs.gov","contributorId":752,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"pawlewicz@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science 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,{"id":86119,"text":"ofr20081229 - 2008 - Flood of May 6, 2007, Willow Creek, west-central Iowa","interactions":[],"lastModifiedDate":"2016-01-29T14:08:00","indexId":"ofr20081229","displayToPublicDate":"2008-08-20T00:00:00","publicationYear":"2008","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":"2008-1229","title":"Flood of May 6, 2007, Willow Creek, west-central Iowa","docAbstract":"<p>Major flooding occurred May 6, 2007, in the Willow Creek drainage basin in Harrison County following severe thunderstorm activity over west-central Iowa. More than 7 inches of rain were recorded for the 72-hour period ending 7 a.m., May 6, at the Logan, Iowa weather station. The peak discharge in Willow Creek at Medford Avenue near Missouri Valley, Iowa, was 17,000 cubic feet per second. The recurrence interval of the flood is 160 years, which was estimated using regional regression equations. Information about the basin, the storms, the flooding, and a profile of high-water marks measured at 10 locations along Willow Creek between the mouth at the Boyer River and State Highway 37 in Monona County, a distance of almost 33 river miles, are presented in this report.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20081229","collaboration":"Prepared in cooperation with the Iowa Department of Transportation and Iowa Highway Research Board (Project HR-140)","usgsCitation":"Fischer, E.E., and Eash, D.A., 2008, Flood of May 6, 2007, Willow Creek, west-central Iowa: U.S. Geological Survey Open-File Report 2008-1229, iv, 12 p., https://doi.org/10.3133/ofr20081229.","productDescription":"iv, 12 p.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2007-05-06","temporalEnd":"2007-05-06","costCenters":[{"id":351,"text":"Iowa Water Science 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daeash@usgs.gov","orcid":"https://orcid.org/0000-0002-2749-8959","contributorId":1887,"corporation":false,"usgs":true,"family":"Eash","given":"David","email":"daeash@usgs.gov","middleInitial":"A.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86121,"text":"sir20085136 - 2008 - Determination of Organic and Inorganic Percentages and Mass of Suspended Material at Four Sites in the Illinois River in Northwestern Arkansas and Northeastern Oklahoma, 2005-07","interactions":[],"lastModifiedDate":"2012-02-10T00:11:46","indexId":"sir20085136","displayToPublicDate":"2008-08-20T00:00:00","publicationYear":"2008","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":"2008-5136","title":"Determination of Organic and Inorganic Percentages and Mass of Suspended Material at Four Sites in the Illinois River in Northwestern Arkansas and Northeastern Oklahoma, 2005-07","docAbstract":"The Illinois River located in northwestern Arkansas and northeastern Oklahoma is influenced by point and nonpoint sources of nutrient enrichment. This has led to increased algal growth within the stream, reducing water clarity. Also, sediment runoff from fields, pastures, construction sites, and other disturbed areas, in addition to frequent streambank failure, has increased sedimentation within the stream and decreased water clarity. A study was conducted by the U.S. Geological Survey in cooperation with the Arkansas Department of Environmental Quality and the U.S. Environmental Protection Agency to characterize the increased turbidity by determining the organic and inorganic composition and mass of suspended material in the Illinois River from August 2005 through July 2007. Water-quality samples were collected at four sites on the Illinois River (listed in downstream order): near Viney Grove, Arkansas; at Savoy, Arkansas; south of Siloam Springs, Arkansas; and near Tahlequah, Oklahoma.\r\nIn general, turbidity, total suspended solids, suspended-sediment concentration, organic material concentration (measured as volatile suspended solids and ash-free dry mass), and chlorophyll a concentration were the greatest in samples collected from the Illinois River at Savoy and the least in samples from the most upstream Illinois River site (near Viney Grove) and the most downstream site (near Tahlequah) from August 2005 through July 2007. For example, the suspended-sediment concentration at the Illinois River at Savoy had a median of 15 milligrams per liter, and the total suspended solids had a median of 12 milligrams per liter. The Illinois River near Tahlequah had the least suspended-sediment concentration with a median of 10 milligrams per liter and the least total suspended solids with a median of 6 milligrams per liter.\r\nThe turbidity, total suspended solids, suspended-sediment concentration, organic material concentration, and chlorophyll a concentration in samples collected during high-flow events were greater than in samples collected during base-flow conditions at the Illinois River at Savoy, south of Siloam Springs, and near Tahlequah. For example, the median turbidity for the Illinois River at Savoy was 3 nephelometric turbidity ratio units during base-flow conditions and 52 nephelometric turbidity ratio units during high-flow conditions.\r\nOrganic material in the Illinois River generally composed between 13 and 47 percent of the total suspended material in samples collected from August 2005 through July 2007. Therefore, most of the suspended material in samples collected from the sites was inorganic material. Overall, the highest percentage of organic material was found at the Illinois River near Viney Grove and at the Illinois River near Tahlequah. The Illinois River south of Siloam Springs had the lowest percentage of organic material among the four sites. In general, the percentage of organic material was greater in samples collected during base-flow conditions compared to samples collected during high-flow conditions.\r\nThe mean seasonal concentrations and percentages of organic material were the least in the fall (September through November) in samples collected from August 2005 to July 2007 from the four Illinois River sites, while the greatest concentrations and percentages of organic material occurred at various times of the year depending on the site. The greatest concentrations of organic material occurred in the summer (June through August) in samples from sites on the Illinois River near Viney Grove, at Savoy and south of Siloam Springs, but in the spring (March through May) in samples from the Illinois River near Tahlequah. The greatest percentages of organic material (least percentages of inorganic material) occurred in the summer in samples from the site near Viney Grove, the winter and summer at the site at Savoy, in the spring, fall, and winter (December through February) at the site south of Siloam Springs, an","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20085136","collaboration":"Prepared in cooperation with the Arkansas Department of Environmental Quality and the U.S. Environmental Protection Agency","usgsCitation":"Galloway, J.M., 2008, Determination of Organic and Inorganic Percentages and Mass of Suspended Material at Four Sites in the Illinois River in Northwestern Arkansas and Northeastern Oklahoma, 2005-07 (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2008-5136, v, 32 p., https://doi.org/10.3133/sir20085136.","productDescription":"v, 32 p.","onlineOnly":"Y","temporalStart":"2005-08-01","temporalEnd":"2007-07-31","costCenters":[{"id":129,"text":"Arkansas Water Science Center","active":true,"usgs":true}],"links":[{"id":121227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2008_5136.jpg"},{"id":11687,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5136/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.16666666666667,35.75 ], [ -95.16666666666667,36.25 ], [ -94.08333333333333,36.25 ], [ -94.08333333333333,35.75 ], [ -95.16666666666667,35.75 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66797d","contributors":{"authors":[{"text":"Galloway, Joel M. 0000-0002-9836-9724 jgallowa@usgs.gov","orcid":"https://orcid.org/0000-0002-9836-9724","contributorId":1562,"corporation":false,"usgs":true,"family":"Galloway","given":"Joel","email":"jgallowa@usgs.gov","middleInitial":"M.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86117,"text":"ofr20081244 - 2008 - User's Guide to Handlens - A Computer Program that Calculates the Chemistry of Minerals in Mixtures","interactions":[],"lastModifiedDate":"2012-02-02T00:14:25","indexId":"ofr20081244","displayToPublicDate":"2008-08-20T00:00:00","publicationYear":"2008","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":"2008-1244","title":"User's Guide to Handlens - A Computer Program that Calculates the Chemistry of Minerals in Mixtures","docAbstract":"HandLens is a computer program, written in Excel macro language, that calculates the chemistry of minerals in mineral mixtures (for example, in rocks, soils and sediments) for related samples from inputs of quantitative mineralogy and chemistry. For best results, the related samples should contain minerals having the same chemical compositions; that is, the samples should differ only in the proportions of minerals present. This manual describes how to use the program, discusses the theory behind its operation, and presents test results of the program's accuracy.\r\nRequired input for HandLens includes quantitative mineralogical data, obtained, for example, by RockJock analysis of X-ray diffraction (XRD) patterns, and quantitative chemical data, obtained, for example, by X-ray florescence (XRF) analysis of the same samples. Other quantitative data, such as sample depth, temperature, surface area, also can be entered. The minerals present in the samples are selected from a list, and the program is started. The results of the calculation include: (1) a table of linear coefficients of determination (r2's) which relate pairs of input data (for example, Si versus quartz weight percents); (2) a utility for plotting all input data, either as pairs of variables, or as sums of up to eight variables; (3) a table that presents the calculated chemical formulae for minerals in the samples; (4) a table that lists the calculated concentrations of major, minor, and trace elements in the various minerals; and (5) a table that presents chemical formulae for the minerals that have been corrected for possible systematic errors in the mineralogical and/or chemical analyses. In addition, the program contains a method for testing the assumption of constant chemistry of the minerals within a sample set.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081244","usgsCitation":"Eberl, D.D., 2008, User's Guide to Handlens - A Computer Program that Calculates the Chemistry of Minerals in Mixtures (Version 1.0): U.S. Geological Survey Open-File Report 2008-1244, viii, 27 p., https://doi.org/10.3133/ofr20081244.","productDescription":"viii, 27 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11682,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1244/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6879a0","contributors":{"authors":[{"text":"Eberl, D. D.","contributorId":66282,"corporation":false,"usgs":true,"family":"Eberl","given":"D.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":296864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86118,"text":"ds270 - 2008 - Digital atlas of the upper Washita River basin, southwestern Oklahoma","interactions":[],"lastModifiedDate":"2017-03-29T11:05:18","indexId":"ds270","displayToPublicDate":"2008-08-20T00:00:00","publicationYear":"2008","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":"270","title":"Digital atlas of the upper Washita River basin, southwestern Oklahoma","docAbstract":"Numerous types of environmental data have been collected in the upper Washita River basin in southwestern Oklahoma. However, to date these data have not been compiled into a format that can be comprehensively queried for the purpose of evaluating the effects of various conservation practices implemented to reduce agricultural runoff and erosion in parts of the upper Washita River basin. This U.S. Geological Survey publication, 'Digital atlas of the upper Washita River basin, southwestern Oklahoma' was created to assist with environmental analysis. This atlas contains 30 spatial data sets that can be used in environmental assessment and decision making for the upper Washita River basin.\r\n\r\nThis digital atlas includes U.S. Geological Survey sampling sites and associated water-quality, biological, water-level, and streamflow data collected from 1903 to 2005. The data were retrieved from the U.S. Geological Survey National Water Information System database on September 29, 2005. Data sets are from the Geology, Geography, and Water disciplines of the U.S. Geological Survey and cover parts of Beckham, Caddo, Canadian, Comanche, Custer, Dewey, Grady, Kiowa, and Washita Counties in southwestern Oklahoma. A bibliography of past reports from the U.S. Geological Survey and other State and Federal agencies from 1949 to 2004 is included in the atlas. Additionally, reports by Becker (2001), Martin (2002), Fairchild and others (2004), and Miller and Stanley (2005) are provided in electronic format.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds270","usgsCitation":"Becker, C., Masoner, J.R., and Scott, J.C., 2008, Digital atlas of the upper Washita River basin, southwestern Oklahoma (Version 1.0): U.S. Geological Survey Data Series 270, Available online and on DVD-ROMs, https://doi.org/10.3133/ds270.","productDescription":"Available online and on DVD-ROMs","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":190663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds270.gif"},{"id":11683,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/270/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a832c","contributors":{"authors":[{"text":"Becker, Carol 0000-0001-6652-4542 cjbecker@usgs.gov","orcid":"https://orcid.org/0000-0001-6652-4542","contributorId":2489,"corporation":false,"usgs":true,"family":"Becker","given":"Carol","email":"cjbecker@usgs.gov","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296865,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Masoner, Jason R. 0000-0002-4829-6379 jmasoner@usgs.gov","orcid":"https://orcid.org/0000-0002-4829-6379","contributorId":3193,"corporation":false,"usgs":true,"family":"Masoner","given":"Jason","email":"jmasoner@usgs.gov","middleInitial":"R.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296866,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, Jonathon C. jcscott@usgs.gov","contributorId":5449,"corporation":false,"usgs":true,"family":"Scott","given":"Jonathon","email":"jcscott@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":296867,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":86113,"text":"ofr20081250 - 2008 - Quality-Assurance Plan for Water-Quality Activities in the USGS Ohio Water Science Center","interactions":[{"subject":{"id":25729,"text":"wri984057 - 1998 - Quality-Assurance/Quality-Control Manual for Collection and Analysis of Water-Quality Data in the Ohio District, US Geological Survey","indexId":"wri984057","publicationYear":"1998","noYear":false,"title":"Quality-Assurance/Quality-Control Manual for Collection and Analysis of Water-Quality Data in the Ohio District, US Geological Survey"},"predicate":"SUPERSEDED_BY","object":{"id":86113,"text":"ofr20081250 - 2008 - Quality-Assurance Plan for Water-Quality Activities in the USGS Ohio Water Science Center","indexId":"ofr20081250","publicationYear":"2008","noYear":false,"title":"Quality-Assurance Plan for Water-Quality Activities in the USGS Ohio Water Science Center"},"id":1}],"lastModifiedDate":"2012-03-08T17:16:22","indexId":"ofr20081250","displayToPublicDate":"2008-08-19T00:00:00","publicationYear":"2008","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":"2008-1250","title":"Quality-Assurance Plan for Water-Quality Activities in the USGS Ohio Water Science Center","docAbstract":"In accordance with guidelines set forth by the Office of Water Quality in the Water Resources Discipline of the U.S. Geological Survey, a quality-assurance plan has been written for use by the Ohio Water Science Center in conducting water-quality activities. This quality-assurance plan documents the standards, policies, and procedures used by the Ohio Water Science Center for activities related to the collection, processing, storage, analysis, and publication of water-quality data. The policies and procedures documented in this quality-assurance plan for water-quality activities are meant to complement the Ohio Water Science Center quality-assurance plans for water-quality monitors, the microbiology laboratory, and surface-water and ground-water activities.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081250","usgsCitation":"Francy, D.S., and Shaffer, K., 2008, Quality-Assurance Plan for Water-Quality Activities in the USGS Ohio Water Science Center (Supersedes WRI 98-4057): U.S. Geological Survey Open-File Report 2008-1250, vi, 73 p., https://doi.org/10.3133/ofr20081250.","productDescription":"vi, 73 p.","onlineOnly":"Y","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":190504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11677,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1250/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.75,38.5 ], [ -84.75,42 ], [ -80.75,42 ], [ -80.75,38.5 ], [ -84.75,38.5 ] ] ] } } ] }","edition":"Supersedes WRI 98-4057","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db6514b1","contributors":{"authors":[{"text":"Francy, Donna S. 0000-0001-9229-3557 dsfrancy@usgs.gov","orcid":"https://orcid.org/0000-0001-9229-3557","contributorId":1853,"corporation":false,"usgs":true,"family":"Francy","given":"Donna","email":"dsfrancy@usgs.gov","middleInitial":"S.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296855,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaffer, Kimberly H.","contributorId":98275,"corporation":false,"usgs":true,"family":"Shaffer","given":"Kimberly H.","affiliations":[],"preferred":false,"id":296856,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":86115,"text":"ofr20081183 - 2008 - View_SPECPR: Software for Plotting Spectra (Installation Manual and User's Guide, Version 1.2)","interactions":[],"lastModifiedDate":"2012-02-02T00:14:30","indexId":"ofr20081183","displayToPublicDate":"2008-08-19T00:00:00","publicationYear":"2008","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":"2008-1183","title":"View_SPECPR: Software for Plotting Spectra (Installation Manual and User's Guide, Version 1.2)","docAbstract":"This document describes procedures for installing and using the 'View_SPECPR' software system to plot spectra stored in SPECPR (SPECtrum Processing Routines) files. The View_SPECPR software is comprised of programs written in IDL (Interactive Data Language) that run within the ENVI (ENvironment for Visualizing Images) image processing system. SPECPR files are used by earth-remote-sensing scientists and planetary scientists for storing spectra collected by laboratory, field, and remote sensing instruments. A widely distributed SPECPR file is the U.S. Geological Survey (USGS) spectral library that contains thousands of spectra of minerals, vegetation, and man-made materials (Clark and others, 2007). SPECPR files contain reflectance data and associated wavelength and spectral resolution data, as well as meta-data on the time and date of collection and spectrometer settings. Furthermore, the SPECPR file automatically tracks changes to data records through its 'history' fields. For more details on the format and content of SPECPR files, see Clark (1993). For more details on ENVI, see ITT (2008). This program has been updated using an ENVI 4.5/IDL7.0 full license operating on a Windows XP operating system and requires the installation of the iTools components of IDL7.0; however, this program should work with full licenses on UNIX/LINUX systems. This software has not been tested with ENVI licenses on Windows Vista or Apple Operating Systems.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20081183","usgsCitation":"Kokaly, R., 2008, View_SPECPR: Software for Plotting Spectra (Installation Manual and User's Guide, Version 1.2) (Version 1.0): U.S. Geological Survey Open-File Report 2008-1183, Report: iv, 26 p.; Downloads Directory, https://doi.org/10.3133/ofr20081183.","productDescription":"Report: iv, 26 p.; Downloads Directory","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":195135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11679,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2008/1183/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685828","contributors":{"authors":[{"text":"Kokaly, Raymond F. 0000-0003-0276-7101","orcid":"https://orcid.org/0000-0003-0276-7101","contributorId":81442,"corporation":false,"usgs":true,"family":"Kokaly","given":"Raymond F.","affiliations":[],"preferred":false,"id":296860,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86116,"text":"sir20085083 - 2008 - Evaluation of acoustic doppler velocity meters to quantify flow from Comal Springs and San Marcos Springs, Texas","interactions":[],"lastModifiedDate":"2016-08-23T13:09:06","indexId":"sir20085083","displayToPublicDate":"2008-08-19T00:00:00","publicationYear":"2008","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":"2008-5083","title":"Evaluation of acoustic doppler velocity meters to quantify flow from Comal Springs and San Marcos Springs, Texas","docAbstract":"<p>Comal Springs and San Marcos Springs are the two largest springs in Texas, are major discharge points for the San Antonio segment of the Edwards aquifer, and provide habitat for several Federally listed endangered species that depend on adequate springflows for survival. It is therefore imperative that the Edwards Aquifer Authority have accurate and timely springflow data to guide resource management. Discharge points for Comal Springs and San Marcos Springs are submerged in Landa Lake and in Spring Lake, respectively. Flows from the springs currently (2008) are estimated by the U.S Geological Survey in real time as surface-water discharge from conventional stage-discharge ratings at sites downstream from each spring. Recent technological advances and availability of acoustic Doppler velocity meters (ADVMs) now provide tools to collect data (stream velocity) related to springflow that could increase accuracy of real-time estimates of the springflows. The U.S. Geological Survey, in cooperation with the Edwards Aquifer Authority, did a study during May 2006 through September 2007 to evaluate ADVMs to quantify flow from Comal and San Marcos Springs. The evaluation was based on two monitoring approaches: (1) placement of ADVMs in important spring orifices - spring run 3 and spring 7 at Comal Springs, and diversion spring at San Marcos Springs; and (2) placement of ADVMs at the nearest flowing streams - Comal River new and old channels for Comal Springs, Spring Lake west and east outflow channels and current (2008) San Marcos River streamflow-gaging site for San Marcos Springs. For Comal Springs, ADVM application at spring run 3 and spring 7 was intended to indicate whether the flows of spring run 3 and spring 7 can be related to total springflow. The findings indicate that velocity data from both discharge features, while reflecting changes in flow, do not reliably show a direct relation to measured streamflow and thus to total Comal Springs flow. ADVMs at the Comal River new channel and old channel sites provide data that potentially could yield more accurate real-time estimates of total Comal Springs flow than streamflow measured at the downstream Comal River site. For San Marcos Springs, the findings indicate shortcomings with ADVM installations at diversion spring and in the west and east outflow channels. However, the accuracy of streamflow measured at the San Marcos River gage as an estimate of real-time San Marcos Springs flow could potentially be increased through use of ADVM data from that site.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20085083","collaboration":"Prepared in cooperation with the Edwards Aquifer Authority","usgsCitation":"Gary, M.O., Gary, R.H., and Asquith, W.H., 2008, Evaluation of acoustic doppler velocity meters to quantify flow from Comal Springs and San Marcos Springs, Texas (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2008-5083, Report: vi, 37 p.; Appendix 1 Files, https://doi.org/10.3133/sir20085083.","productDescription":"Report: vi, 37 p.; Appendix 1 Files","onlineOnly":"Y","additionalOnlineFiles":"Y","temporalStart":"2006-05-01","temporalEnd":"2007-09-30","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":195009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20085083.gif"},{"id":11680,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2008/5083/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.5,28.75 ], [ -100.5,31 ], [ -97.5,31 ], [ -97.5,28.75 ], [ -100.5,28.75 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb014","contributors":{"authors":[{"text":"Gary, Marcus O.","contributorId":68810,"corporation":false,"usgs":true,"family":"Gary","given":"Marcus","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":296863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gary, Robin H.","contributorId":19246,"corporation":false,"usgs":true,"family":"Gary","given":"Robin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":296862,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Asquith, William H. 0000-0002-7400-1861 wasquith@usgs.gov","orcid":"https://orcid.org/0000-0002-7400-1861","contributorId":1007,"corporation":false,"usgs":true,"family":"Asquith","given":"William","email":"wasquith@usgs.gov","middleInitial":"H.","affiliations":[{"id":48595,"text":"Oklahoma-Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296861,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":86114,"text":"ds355 - 2008 - Oregon magnetic and gravity maps and data: A web site for distribution of data","interactions":[],"lastModifiedDate":"2022-07-05T21:18:30.274078","indexId":"ds355","displayToPublicDate":"2008-08-19T00:00:00","publicationYear":"2008","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":"355","title":"Oregon magnetic and gravity maps and data: A web site for distribution of data","docAbstract":"This web site gives the results of a USGS project to acquire the best available, public-domain, aeromagnetic and gravity data in the United States and merge these data into uniform, composite grids for each State. The results for the State of Oregon are presented here on this site. Files of aeromagnetic and gravity grids and images are available for these States for downloading. In Oregon, 49 magnetic surveys have been knit together to form a single digital grid and map. Also, a complete Bouguer gravity anomaly grid and map was generated from 40,665 gravity station measurements in and adjacent to Oregon. In addition, a map shows the location of the aeromagnetic surveys, color-coded to the survey flight-line spacing. This project was supported by the Mineral Resource Program of the USGS.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds355","usgsCitation":"Roberts, C.W., Kucks, R.P., and Hill, P.L., 2008, Oregon magnetic and gravity maps and data: A web site for distribution of data (Version 1.0): U.S. Geological Survey Data Series 355, HTML Document, https://doi.org/10.3133/ds355.","productDescription":"HTML Document","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":190700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403018,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_84191.htm","linkFileType":{"id":5,"text":"html"}},{"id":11678,"rank":100,"type":{"id":15,"text":"Index 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,{"id":86112,"text":"sir20075115 - 2008 - Streamflow, water quality, and metal loads from chat leachate and mine outflow into Tar Creek, Ottawa County, Oklahoma, 2005","interactions":[],"lastModifiedDate":"2020-02-26T17:03:21","indexId":"sir20075115","displayToPublicDate":"2008-08-16T00:00:00","publicationYear":"2008","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":"2007-5115","displayTitle":"Streamflow, Water Quality, and Metal Loads from Chat Leachate and Mine Outflow into Tar Creek, Ottawa County, Oklahoma, 2005","title":"Streamflow, water quality, and metal loads from chat leachate and mine outflow into Tar Creek, Ottawa County, Oklahoma, 2005","docAbstract":"Picher mining district is an abandoned lead and zinc mining area located in Ottawa County, northeastern Oklahoma. During the first half of the 20th century, the area was a primary producer of lead and zinc in the United States. Large accumulations of mine tailings, locally referred to as chat, produce leachate containing cadmium, iron, lead, and zinc that enter drainages within the mining area. Metals also seep to local ground water and streams from unplugged shafts, vent holes, seeps, and abandoned mine dewatering wells. Streamflow measurements were made and water-quality samples were collected and analyzed from two locations in Picher mining district from August 16 to August 29 following a rain event beginning on August 14, 2005, to determine likely concentrations and loads of metals from tailings and mine outflows in the part of Picher mining district near Tar Creek.\r\n\r\nLocations selected for sampling included a tailings pile with an adjacent mill pond, referred to as the Western location, and a segment of Tar Creek from above the confluence with Lytle Creek to below Douthat bridge, referred to as Tar Creek Study Segment. Measured streamflow was less than 0.01 cubic foot per second at the Western location, with streamflow only being measurable at that site on August 16, 2005. Measured streamflows ranged from <0.01 to 2.62 cubic feet per second at Tar Creek Study Segment.\r\n\r\nOne water-quality sample was collected from runoff at the Western location. Total metals concentrations in that sample were 95.3 micrograms per liter cadmium, 182 micrograms per liter iron, 170 micrograms per liter lead, 1,760 micrograms per liter zinc. Total mean metals concentrations in 29 water-quality samples collected from Tar Creek Study Segment from August 16-29, 2005, were 21.8 micrograms per liter cadmium, 7,924 micrograms per liter iron, 7.68 micrograms per liter lead, and 14,548 micrograms per liter zinc. \r\n\r\nNo metals loading values were calculated for the Western location. Metals loading to Tar Creek Study Segment were calculated based on instantaneous streamflow and metals concentrations. Total metals loading to Tar Creek from chat leachate ranged from 0.062 to 0.212 pound per day of cadmium, <0.001 to 0.814 pound per day of iron, 0.003 to 0.036 pound per day of lead, and 10.6 to 47.9 pounds per day of zinc.\r\n\r\nMetals loading to Tar Creek Study Segment from chat leachate and mine outflow was determined by subtracting values at appropriate upstream and downstream stations. Four sources of calculated metal loads are from Tar Creek and Lytle Creek entering the study segment, from chat pile leachate, and from old Lytle Creek mine outflow. Less than 1 percent of total and dissolved iron loading came from chat leachate, while about 99 percent of total iron loading came from mine outflow. Total and dissolved lead loading percentages from chat leachate were greater than total and dissolved lead loading percentages from mine outflow. About 19 percent of total zinc loading came from chat leachate, about 29 percent of total zinc loading came from mine outflow, and about 52 percent of total zinc loading came from Lytle Creek.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20075115","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Cope, C.C., Becker, M.F., Andrews, W.J., and DeHay, K., 2008, Streamflow, water quality, and metal loads from chat leachate and mine outflow into Tar Creek, Ottawa County, Oklahoma, 2005 (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2007-5115, iv, 24 p., https://doi.org/10.3133/sir20075115.","productDescription":"iv, 24 p.","temporalStart":"2005-08-04","temporalEnd":"2005-08-29","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":124809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2007_5115.jpg"},{"id":11675,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2007/5115/pdf/sir2007-5115.pdf"}],"country":"United States","state":"Oklahoma","county":"Ottawa County","otherGeospatial":"Tar Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.95,36.833333333333336 ], [ -94.95,37.06666666666667 ], [ -94.73333333333333,37.06666666666667 ], [ -94.73333333333333,36.833333333333336 ], [ -94.95,36.833333333333336 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4cf2","contributors":{"authors":[{"text":"Cope, Caleb C.","contributorId":81590,"corporation":false,"usgs":true,"family":"Cope","given":"Caleb","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":296854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Becker, Mark F.","contributorId":40180,"corporation":false,"usgs":true,"family":"Becker","given":"Mark","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":296853,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Andrews, William J. 0000-0003-4780-8835 wandrews@usgs.gov","orcid":"https://orcid.org/0000-0003-4780-8835","contributorId":328,"corporation":false,"usgs":true,"family":"Andrews","given":"William","email":"wandrews@usgs.gov","middleInitial":"J.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"DeHay, Kelli","contributorId":14064,"corporation":false,"usgs":true,"family":"DeHay","given":"Kelli","affiliations":[],"preferred":false,"id":296852,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70159149,"text":"70159149 - 2008 - Google earth mapping of damage from the Nigata-Ken-Chuetsu M6.6 earthquake of 16 July 2007","interactions":[],"lastModifiedDate":"2021-10-21T14:53:21.558084","indexId":"70159149","displayToPublicDate":"2008-08-16T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Google earth mapping of damage from the Nigata-Ken-Chuetsu M6.6 earthquake of 16 July 2007","docAbstract":"<p><span>We describe the use of Google Earth during and after a large damaging earthquake thatstruck the central Japan coast on 16 July 2007 to collect and organize damage information and guide the reconnaissance activities. This software enabled greater real-time collaboration among scientists and engineers. After the field investigation, the Google Earth map is used as a final reporting product that was directly linked to the more traditional research report document. Finally, we analyze the use of the software within the context of a post-disaster reconnaissance investigation, and link it to student use of GoogleEarth in field situations</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"6th International Conference on Case Histories in Geotechnical Engineering","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"6th International Conference on Case Histories in Geotechnical Engineering","conferenceDate":"Auguest 11-16 2008","conferenceLocation":"Arlington, Virginia","language":"English","publisher":"University of Missouri-Rolla","usgsCitation":"Kayen, R., Steele, C., Collins, B., and Walker, K., 2008, Google earth mapping of damage from the Nigata-Ken-Chuetsu M6.6 earthquake of 16 July 2007, <i>in</i> 6th International Conference on Case Histories in Geotechnical Engineering, Arlington, Virginia, Auguest 11-16 2008, 7 p.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-009100","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":309970,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              138.2080078125,\n              37.35269280367274\n            ],\n            [\n              138.80126953125,\n              36.94989178681327\n            ],\n            [\n              139.4384765625,\n              37.21283151445594\n            ],\n            [\n              139.94384765625,\n              37.87485339352928\n            ],\n            [\n              139.3505859375,\n              38.22091976683121\n            ],\n            [\n              138.84521484374997,\n              38.13455657705411\n            ],\n            [\n              138.2080078125,\n              37.35269280367274\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce71e4b06217fc478ae6","contributors":{"authors":[{"text":"Kayen, Robert E. rkayen@usgs.gov","contributorId":2787,"corporation":false,"usgs":true,"family":"Kayen","given":"Robert E.","email":"rkayen@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":577705,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steele, Clint","contributorId":149275,"corporation":false,"usgs":false,"family":"Steele","given":"Clint","email":"","affiliations":[],"preferred":false,"id":577706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collins, Brian","contributorId":149276,"corporation":false,"usgs":false,"family":"Collins","given":"Brian","affiliations":[],"preferred":false,"id":577707,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Walker, Kevin","contributorId":149277,"corporation":false,"usgs":false,"family":"Walker","given":"Kevin","email":"","affiliations":[],"preferred":false,"id":577708,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":86111,"text":"fs20083063 - 2008 - Distribution of Elevated Nitrate Concentrations in Ground Water in Washington State","interactions":[],"lastModifiedDate":"2012-03-08T17:16:25","indexId":"fs20083063","displayToPublicDate":"2008-08-15T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3063","title":"Distribution of Elevated Nitrate Concentrations in Ground Water in Washington State","docAbstract":"More than 60 percent of the population of Washington State uses ground water for their drinking and cooking needs. Nitrate concentrations in ground water are elevated in parts of the State as a result of various land-use practices, including fertilizer application, dairy operations and ranching, and septic-system use. Shallow wells generally are more vulnerable to nitrate contamination than deeper wells (Williamson and others, 1998; Ebbert and others, 2000).\r\n\r\nIn order to protect public health, the Washington State Department of Health requires that public water systems regularly measure nitrate in their wells. Public water systems serving more than 25 people collect water samples at least annually; systems serving from 2 to 14 people collect water samples at least every 3 years. Private well owners serving one residence may be required to sample when the well is first drilled, but are unregulated after that. As a result, limited information is available to citizens and public health officials about potential exposure to elevated nitrate concentrations for people whose primary drinking-water sources are private wells. The U.S. Geological Survey and Washington State Department of Health collaborated to examine water-quality data from public water systems and develop models that calculate the probability of detecting elevated nitrate concentrations in ground water. Maps were then developed to estimate ground water vulnerability to nitrate in areas where limited data are available.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20083063","usgsCitation":"Frans, L., 2008, Distribution of Elevated Nitrate Concentrations in Ground Water in Washington State: U.S. Geological Survey Fact Sheet 2008-3063, 4 p., https://doi.org/10.3133/fs20083063.","productDescription":"4 p.","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":122353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3063.jpg"},{"id":11674,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2008/3063/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.75,45.5 ], [ -124.75,49 ], [ -116.91666666666667,49 ], [ -116.91666666666667,45.5 ], [ -124.75,45.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635781","contributors":{"authors":[{"text":"Frans, Lonna","contributorId":79577,"corporation":false,"usgs":true,"family":"Frans","given":"Lonna","affiliations":[],"preferred":false,"id":296850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86109,"text":"gip70 - 2008 - The National Streamflow Information Program","interactions":[],"lastModifiedDate":"2012-02-02T00:14:24","indexId":"gip70","displayToPublicDate":"2008-08-14T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":315,"text":"General Information Product","code":"GIP","onlineIssn":"2332-354X","printIssn":"2332-3531","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"70","title":"The National Streamflow Information Program","docAbstract":"Provide the streamflow information and understanding required to meet local, State, regional, and national needs.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/gip70","usgsCitation":"Norris, J.M., 2008, The National Streamflow Information Program: U.S. Geological Survey General Information Product 70, Available online, https://doi.org/10.3133/gip70.","productDescription":"Available online","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":444,"text":"National Streamflow Information Program","active":false,"usgs":true}],"links":[{"id":121220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/gip_70.jpg"},{"id":11672,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/gip/70/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aff2","contributors":{"authors":[{"text":"Norris, J. Michael 0000-0002-7480-0161 mnorris@usgs.gov","orcid":"https://orcid.org/0000-0002-7480-0161","contributorId":1625,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"mnorris@usgs.gov","middleInitial":"Michael","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":86107,"text":"ds354 - 2008 - Algal and water-quality data for Rapid Creek and Canyon Lake near Rapid City, South Dakota, 2007","interactions":[],"lastModifiedDate":"2017-10-14T12:27:06","indexId":"ds354","displayToPublicDate":"2008-08-13T00:00:00","publicationYear":"2008","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":"354","title":"Algal and water-quality data for Rapid Creek and Canyon Lake near Rapid City, South Dakota, 2007","docAbstract":"This report summarizes the results of algae and water-quality sampling on Rapid Creek and Canyon Lake during May and September 2007. The overall purpose of the study was to determine the algal community composition of Rapid Creek and Canyon Lake in relation to organisms that are known producers of unwanted tastes and odors in drinking-water supplies. Algal assemblage structure (phytoplankton and periphyton) was examined at 16 sites on Rapid Creek and Canyon Lake during May and September 2007, and actinomycetes bacteria were sampled at the Rapid City water treatment plant intake in May 2007, to determine if taste-and-odor producing organisms were present. During the May 2007 sampling, 3 Rapid Creek sites and 4 Canyon Lake sites were quantitatively sampled for phytoplankton in the water column, 7 Rapid Creek sites were quantitatively sampled for attached periphyton, and 4 lake and retention pond sites were qualitatively sampled for periphyton. Five Rapid Creek sites were sampled for geosmin and 2-methylisoborneol, two common taste-and-odor causing compounds known to affect water supplies. During the September 2007 sampling, 4 Rapid Creek sites were quantitatively sampled for attached periphyton, and 3 Canyon Lake sites were qualitatively sampled for periphyton. Water temperature, dissolved oxygen, pH, and specific conductance were measured during each sampling event. Methods of collection and sample analysis are presented for the various types of biological and chemical constituent samples.\r\n\r\nDiatoms comprised 91-100 percent of the total algal biovolume in periphyton samples collected during May and September. Cyanobacteria (also called blue-green algae) were detected in 7 of the 11 quantitative periphyton samples and ranged from 0.01 to 2.0 percent of the total biovolume. Cyanobacteria were present in 3 of the 7 phytoplankton samples collected in May, but the relative biovolumes were small (0.01-0.2 percent). Six of seven qualitative samples collected from Canyon Lake and retention ponds during May and September also contained cyanobacteria. Geosmin and 2-methylisoborneol concentrations were less than detection limits (0.005 ug/L) in all five of the Rapid Creek samples collected in May. Actinomycetes bacteria were present at the water treatment plant intake in May 2007, at a concentration of 6 colonies per milliliter. During this study, no taste-and-odor problems with the drinking water within the study area were reported. However, the presence of cyanobacterial taxa known to contain taste-and-odor producing strains (such as Leptolyngbya, Phormidium, and Anabaena) indicates the potential for taste-and-odor problems under certain physical and chemical conditions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds354","collaboration":"Prepared in cooperation with the city of Rapid City","usgsCitation":"Hoogestraat, G., Putnam, L.D., and Graham, J.L., 2008, Algal and water-quality data for Rapid Creek and Canyon Lake near Rapid City, South Dakota, 2007: U.S. Geological Survey Data Series 354, Report: vi, 17 p.; Results (Excel spreadsheets), https://doi.org/10.3133/ds354.","productDescription":"Report: vi, 17 p.; Results (Excel spreadsheets)","additionalOnlineFiles":"Y","temporalStart":"2007-05-01","temporalEnd":"2007-09-30","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":190953,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11671,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/354/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Dakota","city":"Rapid City","otherGeospatial":"Canyon Lake, Rapid Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.5,44 ], [ -103.5,44.15083333333333 ], [ -103.21666666666667,44.15083333333333 ], [ -103.21666666666667,44 ], [ -103.5,44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544315","contributors":{"authors":[{"text":"Hoogestraat, Galen K.","contributorId":22442,"corporation":false,"usgs":true,"family":"Hoogestraat","given":"Galen K.","affiliations":[],"preferred":false,"id":296846,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Putnam, Larry D. ldputnam@usgs.gov","contributorId":990,"corporation":false,"usgs":true,"family":"Putnam","given":"Larry","email":"ldputnam@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":296844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graham, Jennifer L. 0000-0002-6420-9335 jlgraham@usgs.gov","orcid":"https://orcid.org/0000-0002-6420-9335","contributorId":1769,"corporation":false,"usgs":true,"family":"Graham","given":"Jennifer","email":"jlgraham@usgs.gov","middleInitial":"L.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":296845,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":86108,"text":"fs20083050 - 2008 - Assessment of undiscovered oil and gas resources of the Bighorn Basin Province, Wyoming and Montana, 2008","interactions":[],"lastModifiedDate":"2018-09-26T13:00:37","indexId":"fs20083050","displayToPublicDate":"2008-08-13T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2008-3050","title":"Assessment of undiscovered oil and gas resources of the Bighorn Basin Province, Wyoming and Montana, 2008","docAbstract":"Using a geology-based assessment methodology, the U.S. Geological Survey estimated a mean of 989 billion cubic feet of undiscovered natural gas, a mean of 72 million barrels of undiscovered oil, and a mean of 13 million barrels of undiscovered natural gas liquids in the Bighorn Basin Providence of Wyoming and Montana.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20083050","usgsCitation":"Kirschbaum, M., Condon, S.M., Finn, T.M., Johnson, R.C., Lillis, P.G., Nelson, P.H., Roberts, L.N., Roberts, S.B., Charpentier, R., Cook, T., Klett, T.R., Pollastro, R.M., and Schenk, C.J., 2008, Assessment of undiscovered oil and gas resources of the Bighorn Basin Province, Wyoming and Montana, 2008 (Version 1.0): U.S. Geological Survey Fact Sheet 2008-3050, 2 p., https://doi.org/10.3133/fs20083050.","productDescription":"2 p.","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":121215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2008_3050.jpg"},{"id":11798,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2008/3050/","text":"Index 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M.","contributorId":95464,"corporation":false,"usgs":true,"family":"Condon","given":"Steven","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":746368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Finn, Thomas M. 0000-0001-6396-9351 finn@usgs.gov","orcid":"https://orcid.org/0000-0001-6396-9351","contributorId":778,"corporation":false,"usgs":true,"family":"Finn","given":"Thomas","email":"finn@usgs.gov","middleInitial":"M.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":746369,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Ronald C. 0000-0002-6197-5165 rcjohnson@usgs.gov","orcid":"https://orcid.org/0000-0002-6197-5165","contributorId":1550,"corporation":false,"usgs":true,"family":"Johnson","given":"Ronald","email":"rcjohnson@usgs.gov","middleInitial":"C.","affiliations":[{"id":164,"text":"Central Energy Resources Science 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