{"pageNumber":"955","pageRowStart":"23850","pageSize":"25","recordCount":46895,"records":[{"id":72483,"text":"sir20055210 - 2005 - Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055210","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5210","title":"Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003","docAbstract":"Winter snow accumulation and summer snow and ice ablation were measured at South Cascade Glacier, Washington, to estimate glacier mass-balance quantities for balance year 2003. The 2003 glacier-average maximum winter snow balance was 2.66 meters water equivalent, which was about equal to the average of such balances for the glacier since balance year 1959. The 2003 glacier summer balance (-4.76 meters water equivalent) was the most negative reported for the glacier, and the 2003 net balance (-2.10 meters water equivalent), was the second-most negative reported. The glacier 2003 annual (water year) balance was -1.89 meters water equivalent. \r\n\r\nThe area of the glacier near the end of the balance year was 1.89 square kilometers, a decrease of 0.03 square kilometer from the previous year. The equilibrium-line altitude was higher than any part of the glacier; however, because snow remained along part of one side of the upper glacier, the accumulation-area ratio was 0.07. During September 13, 2002-September 13, 2003, the glacier terminus retreated at a rate of about 15 meters per year. Average speed of surface ice, computed using a series of vertical aerial photographs dating back to 2001, ranged from 2.2 to 21.8 meters per year. \r\n\r\nRunoff from the subbasin containing the glacier and from an adjacent non-glacierized basin was gaged during part of water year 2003. Air temperature, precipitation, atmospheric water-vapor pressure, wind speed, and incoming solar radiation were measured at selected locations on and near the glacier. Summer 2003 at the glacier was among the warmest for which data are available.","language":"ENGLISH","doi":"10.3133/sir20055210","usgsCitation":"Bidlake, W.R., Josberger, E.G., and Savoca, M.E., 2005, Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003: U.S. Geological Survey Scientific Investigations Report 2005-5210, 60 p., https://doi.org/10.3133/sir20055210.","productDescription":"60 p.","costCenters":[],"links":[{"id":192960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7540,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5210/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489b05","contributors":{"authors":[{"text":"Bidlake, William R. wbidlake@usgs.gov","contributorId":1712,"corporation":false,"usgs":true,"family":"Bidlake","given":"William","email":"wbidlake@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":285725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Josberger, Edward G. ejosberg@usgs.gov","contributorId":1710,"corporation":false,"usgs":true,"family":"Josberger","given":"Edward","email":"ejosberg@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":285724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savoca, Mark E. mesavoca@usgs.gov","contributorId":1961,"corporation":false,"usgs":true,"family":"Savoca","given":"Mark","email":"mesavoca@usgs.gov","middleInitial":"E.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72480,"text":"sir20055147 - 2005 - Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland","interactions":[],"lastModifiedDate":"2017-07-10T10:35:12","indexId":"sir20055147","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5147","title":"Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland","docAbstract":"Natural-stream designs are commonly based on the dimensions of the bankfull channel, which is capable of conveying discharges that transport sediment without excessive erosion or deposition. Regional curves relate bankfull-channel geometry and discharge to drainage area in watersheds with similar runoff characteristics and commonly are utilized by practitioners of natural-stream design to confirm or refute selection of the field-identified bankfull channel. Data collected from 66 streamflow-gaging stations and associated stream reaches between December 1999 and December 2003 were used in one-variable ordinary least-squares regression analyses to develop regional curves relating drainage area to cross-sectional area, discharge, width, and mean depth of the bankfull channel. Watersheds draining to these stations are predominantly within the Piedmont, Ridge and Valley, and Appalachian Plateaus Physiographic Provinces of Pennsylvania and northern Maryland. \r\n\r\nStatistical analyses of physiography, percentage of watershed area underlain by carbonate bedrock, and percentage of watershed area that is glaciated indicate that carbonate bedrock, not physiography or glaciation, has a controlling influence on the slope of regional curves. Regional curves developed from stations in watersheds underlain by 30 percent or less carbonate bedrock generally had steeper slopes than the corresponding relations developed from watersheds underlain by greater than 30 percent carbonate bedrock. In contrast, there is little evidence to suggest that regional curves developed from stations in the Piedmont or Ridge and Valley Physiographic Province are different from the corresponding relations developed from stations in the Appalachian Plateaus Physiographic Province. On the basis of these findings, regional curves are presented to represent two settings that are independent of physiography: (1) noncarbonate settings characterized by watersheds with carbonate bedrock underlying 30 percent or less of watershed area, and (2) carbonate settings characterized by watersheds with carbonate bedrock underlying greater than 30 percent of watershed area. \r\n\r\nAll regional curves presented in this report have slopes that are significantly different from zero and normally distributed residuals that vary randomly with drainage area. Drainage area explains the most variability in bankfull cross-sectional area and bankfull discharge in the noncarbonate setting (R2 = 0.92 for both). Less variability is explained in bankfull width and depth (R2 = 0.81 and 0.72, respectively). Regional curves representing the carbonate setting are generally not as statistically robust as the corresponding noncarbonate relations because there were only 11 stations available to develop these curves and drainage area cannot explain variance resulting from karst features. The carbonate regional curves generally are characterized by less confidence, lower R2 values, and higher residual standard errors. Poor representation by watersheds less than 40 mi2 causes the carbonate regional curves for bankfull discharge, cross-sectional area, and mean depth to be disproportionately influenced by the smallest watershed (values of Cook's Distance range from 3.6 to 8.4). Additional bankfull discharge and channel-geometry data from small watersheds might reduce this influence, increase confidence, and generally improve regional curves representing the carbonate setting. \r\n\r\nLimitations associated with streamflow-gaging station selection and development of the curves result in some constraints for the application of regional curves presented in this report. These curves apply only to streams within the study area in watersheds having land use, streamflow regulation, and drainage areas that are consistent with the criteria used for station selection. Regardless of the setting, the regional curves presented here are not intended for use as the sole method for estimation of bankfull characteristics; however, th","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055147","usgsCitation":"Chaplin, J.J., 2005, Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland: U.S. Geological Survey Scientific Investigations Report 2005-5147, 40 p., https://doi.org/10.3133/sir20055147.","productDescription":"40 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":192903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7538,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5147/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81,39.833333333333336 ], [ -81,42.833333333333336 ], [ -74,42.833333333333336 ], [ -74,39.833333333333336 ], [ -81,39.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de31","contributors":{"authors":[{"text":"Chaplin, Jeffrey J. 0000-0002-0617-5050 jchaplin@usgs.gov","orcid":"https://orcid.org/0000-0002-0617-5050","contributorId":147,"corporation":false,"usgs":true,"family":"Chaplin","given":"Jeffrey","email":"jchaplin@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285721,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70238383,"text":"70238383 - 2005 - Implications for prediction and hazard assessment from the 2004 Parkfield earthquake","interactions":[],"lastModifiedDate":"2022-11-18T18:18:55.697023","indexId":"70238383","displayToPublicDate":"2005-10-13T11:50:53","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Implications for prediction and hazard assessment from the 2004 Parkfield earthquake","docAbstract":"<p><span>Obtaining high-quality measurements close to a large earthquake is not easy: one has to be in the right place at the right time with the right instruments. Such a convergence happened, for the first time, when the 28 September 2004 Parkfield, California, earthquake occurred on the San Andreas fault in the middle of a dense network of instruments designed to record it. The resulting data reveal aspects of the earthquake process never before seen. Here we show what these data, when combined with data from earlier Parkfield earthquakes, tell us about earthquake physics and earthquake prediction. The 2004 Parkfield earthquake, with its lack of obvious precursors, demonstrates that reliable short-term earthquake prediction still is not achievable. To reduce the societal impact of earthquakes now, we should focus on developing the next generation of models that can provide better predictions of the strength and location of damaging ground shaking.</span></p>","language":"English","publisher":"Springer","doi":"10.1038/nature04067","usgsCitation":"Bakun, W.H., Aagaard, B.T., Dost, B., Ellsworth, W.L., Hardebeck, J.L., Harris, R.A., Ji, C., Johnston, M.J., Langbein, J.O., Lienkaemper, J.J., Michael, A.J., Murray, J.R., Nadeau, R., Reasenberg, P., Reichle, M., Roeloffs, E.A., Shakal, A., Simpson, R.W., and Waldhauser, F., 2005, Implications for prediction and hazard assessment from the 2004 Parkfield earthquake: Nature, v. 437, p. 969-974, https://doi.org/10.1038/nature04067.","productDescription":"6 p.","startPage":"969","endPage":"974","costCenters":[],"links":[{"id":477643,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://resolver.caltech.edu/CaltechAUTHORS:20150403-080028282","text":"External Repository"},{"id":409458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Parkfield","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.4537640117938,\n              35.910700976762385\n            ],\n            [\n              -120.4537640117938,\n              35.88567088811958\n            ],\n            [\n              -120.41342358821001,\n              35.88567088811958\n            ],\n            [\n              -120.41342358821001,\n              35.910700976762385\n            ],\n            [\n              -120.4537640117938,\n              35.910700976762385\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"437","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bakun, W. H.","contributorId":67055,"corporation":false,"usgs":true,"family":"Bakun","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":857297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aagaard, Brad T. 0000-0002-8795-9833 baagaard@usgs.gov","orcid":"https://orcid.org/0000-0002-8795-9833","contributorId":192869,"corporation":false,"usgs":true,"family":"Aagaard","given":"Brad","email":"baagaard@usgs.gov","middleInitial":"T.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":857298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dost, B.","contributorId":299207,"corporation":false,"usgs":false,"family":"Dost","given":"B.","email":"","affiliations":[{"id":16158,"text":"Royal Netherlands Meteorological Institute","active":true,"usgs":false}],"preferred":false,"id":857299,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ellsworth, William L. ellsworth@usgs.gov","contributorId":787,"corporation":false,"usgs":true,"family":"Ellsworth","given":"William","email":"ellsworth@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857300,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hardebeck, Jeanne L. 0000-0002-6737-7780 jhardebeck@usgs.gov","orcid":"https://orcid.org/0000-0002-6737-7780","contributorId":841,"corporation":false,"usgs":true,"family":"Hardebeck","given":"Jeanne","email":"jhardebeck@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":857301,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Harris, Ruth A. 0000-0002-9247-0768 harris@usgs.gov","orcid":"https://orcid.org/0000-0002-9247-0768","contributorId":786,"corporation":false,"usgs":true,"family":"Harris","given":"Ruth","email":"harris@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857302,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ji, C.","contributorId":31093,"corporation":false,"usgs":true,"family":"Ji","given":"C.","email":"","affiliations":[],"preferred":false,"id":857303,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Johnston, Malcolm J. S. 0000-0003-4326-8368 mal@usgs.gov","orcid":"https://orcid.org/0000-0003-4326-8368","contributorId":622,"corporation":false,"usgs":true,"family":"Johnston","given":"Malcolm","email":"mal@usgs.gov","middleInitial":"J. S.","affiliations":[],"preferred":true,"id":857304,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Langbein, John O. 0000-0002-7821-8101 langbein@usgs.gov","orcid":"https://orcid.org/0000-0002-7821-8101","contributorId":3293,"corporation":false,"usgs":true,"family":"Langbein","given":"John","email":"langbein@usgs.gov","middleInitial":"O.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857305,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lienkaemper, James J. 0000-0002-7578-7042 jlienk@usgs.gov","orcid":"https://orcid.org/0000-0002-7578-7042","contributorId":1941,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"James","email":"jlienk@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857306,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Michael, Andrew J. 0000-0002-2403-5019 michael@usgs.gov","orcid":"https://orcid.org/0000-0002-2403-5019","contributorId":1280,"corporation":false,"usgs":true,"family":"Michael","given":"Andrew","email":"michael@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":857307,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Murray, Jessica R. 0000-0002-6144-1681 jrmurray@usgs.gov","orcid":"https://orcid.org/0000-0002-6144-1681","contributorId":2759,"corporation":false,"usgs":true,"family":"Murray","given":"Jessica","email":"jrmurray@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857308,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Nadeau, R.M.","contributorId":93268,"corporation":false,"usgs":true,"family":"Nadeau","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":857309,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Reasenberg, P.A.","contributorId":19959,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":857310,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Reichle, M.S.","contributorId":14845,"corporation":false,"usgs":true,"family":"Reichle","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":857311,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Roeloffs, Evelyn A. 0000-0002-4761-0469 evelynr@usgs.gov","orcid":"https://orcid.org/0000-0002-4761-0469","contributorId":2680,"corporation":false,"usgs":true,"family":"Roeloffs","given":"Evelyn","email":"evelynr@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857312,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Shakal, A.","contributorId":20934,"corporation":false,"usgs":false,"family":"Shakal","given":"A.","email":"","affiliations":[{"id":12640,"text":"California Geological Survey","active":true,"usgs":false}],"preferred":false,"id":857313,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":857314,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Waldhauser, F.","contributorId":31897,"corporation":false,"usgs":true,"family":"Waldhauser","given":"F.","affiliations":[],"preferred":false,"id":857315,"contributorType":{"id":1,"text":"Authors"},"rank":19}]}}
,{"id":72465,"text":"ds137 - 2005 - Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database","interactions":[],"lastModifiedDate":"2022-07-11T19:32:27.803531","indexId":"ds137","displayToPublicDate":"2005-10-12T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"137","title":"Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database","docAbstract":"This digital map database has been prepared by R.W. Tabor from the published Geologic map of the Wenatchee 1:100,000 Quadrangle, Central Washington. Together with the accompanying text files as PDF, it provides information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The authors mapped most of the bedrock geology at 1:100,000 scale, but compiled Quaternary units at 1:24,000 scale. The Quaternary contacts and structural data have been much simplified for the 1:100,000-scale map and database. The spatial resolution (scale) of the database is 1:100,000 or smaller. \r\n\r\nThis database depicts the distribution of geologic materials and structures at a regional (1:100,000) scale. The report is intended to provide geologic information for the regional study of materials properties, earthquake shaking, landslide potential, mineral hazards, seismic velocity, and earthquake faults. In addition, the report contains information and interpretations about the regional geologic history and framework. However, the regional scale of this report does not provide sufficient detail for site development purposes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds137","usgsCitation":"Tabor, R.W., Waitt, R., Frizzell, V.A., Swanson, D.A., Byerly, G.R., and Bentley, R.D., 2005, Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database (Version 1.0): U.S. Geological Survey Data Series 137, HTML Document, https://doi.org/10.3133/ds137.","productDescription":"HTML Document","costCenters":[],"links":[{"id":193165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403430,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73770.htm","linkFileType":{"id":5,"text":"html"}},{"id":7494,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/137/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Wenatchee quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              47\n            ],\n            [\n              -120,\n              47\n            ],\n            [\n              -120,\n              47.5\n            ],\n            [\n              -121,\n              47.5\n            ],\n            [\n              -121,\n              47\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a80ce","contributors":{"authors":[{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waitt, R. B.","contributorId":78766,"corporation":false,"usgs":true,"family":"Waitt","given":"R. B.","affiliations":[],"preferred":false,"id":285695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frizzell, V. A. Jr.","contributorId":39376,"corporation":false,"usgs":true,"family":"Frizzell","given":"V.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285694,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swanson, D. A.","contributorId":34102,"corporation":false,"usgs":true,"family":"Swanson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285693,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Byerly, G. R.","contributorId":6826,"corporation":false,"usgs":true,"family":"Byerly","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285691,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bentley, R. D.","contributorId":85561,"corporation":false,"usgs":true,"family":"Bentley","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285696,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70205941,"text":"70205941 - 2005 - Late Devonian Alamo Impact, southern Nevada, USA: Evidence of size, marine site, and widespread effects","interactions":[],"lastModifiedDate":"2020-05-26T12:41:46.564191","indexId":"70205941","displayToPublicDate":"2005-10-10T14:42:23","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Late Devonian Alamo Impact, southern Nevada, USA: Evidence of size, marine site, and widespread effects","docAbstract":"<p><span>The early Late Devonian (early Frasnian) Alamo Impact targeted an oceanic, off-platform site in southern Nevada, excavating a crater with a final diameter of 44–65 km. The original crater is now dismembered and buried beneath younger rocks. Consequently, its size and site must be deduced through multiple converging lines of geological and paleontological evidence. Previous and new evidence includes the catastrophically emplaced Alamo Breccia, tsunamites, shock-metamorphosed quartz grains, carbonate accretionary lapilli, an iridium anomaly, sub-Breccia clastic injection, deep-water Breccia channels, and ejecta material. We now demonstrate, on the basis of conodont microfossils in carbonate ejecta clasts within lapillistone blocks and widely distributed shocked-quartz and lithic-clast ejecta within the upper part of the Breccia, that the Alamo Impact excavated down at least into Upper Cambrian strata, at a depth of 1.7 km, and possibly into the underlying Proterozoic–Lower Cambrian Prospect Mountain Quartzite, ∼2.5 km beneath the Late Devonian seafloor. Distal tsunamites and probable ejecta are now documented as far north as Devils Gate, northern Nevada, and as far northeast as the Confusion Range, western Utah. A charcoal-bearing, early Frasnian estuarine deposit in the Bighorn Mountains, Wyoming, may provide the first evidence of an Alamo Impact fallout-generated forest fire. Our new data further document the widespread effects and size of the Alamo Impact, and constrain the likely present position of the tectonically transported crater to an area between the Timpahute and Hot Creek Ranges, southern Nevada.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2384-1.259","usgsCitation":"Morrow, J.R., Sandberg, C., and Harris, A.G., 2005, Late Devonian Alamo Impact, southern Nevada, USA: Evidence of size, marine site, and widespread effects: Special Paper of the Geological Society of America, p. 259-280, https://doi.org/10.1130/0-8137-2384-1.259.","productDescription":"22 p.","startPage":"259","endPage":"280","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":368244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.257080078125,\n              37.1165261849112\n            ],\n            [\n              -114.63134765625001,\n              37.1165261849112\n            ],\n            [\n              -114.63134765625001,\n              40.12849105685408\n            ],\n            [\n              -117.257080078125,\n              40.12849105685408\n            ],\n            [\n              -117.257080078125,\n              37.1165261849112\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morrow, Jared R.","contributorId":65934,"corporation":false,"usgs":true,"family":"Morrow","given":"Jared","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":772998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sandberg, Charles sandberg@usgs.gov","contributorId":199124,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":772999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, Anita G.","contributorId":50162,"corporation":false,"usgs":true,"family":"Harris","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":773000,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72436,"text":"ofr20051053 - 2005 - Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: II. diel data, 1999-2001","interactions":[],"lastModifiedDate":"2021-01-15T22:13:30.672116","indexId":"ofr20051053","displayToPublicDate":"2005-10-09T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1053","title":"Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: II. diel data, 1999-2001","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051053","usgsCitation":"Antweiler, R.C., Smith, R.L., Voytek, M.A., and Bohlke, J., 2005, Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: II. diel data, 1999-2001: U.S. Geological Survey Open-File Report 2005-1053, 124 p., https://doi.org/10.3133/ofr20051053.","productDescription":"124 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":191933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":382243,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1053/"},{"id":382171,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1053/pdf/OFR%2020051053.pdf"}],"country":"United States","state":"Indiana, Illinois","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.5,40.666666666666664 ], [ -87.5,40.833333333333336 ], [ -87.41666666666667,40.833333333333336 ], [ -87.41666666666667,40.666666666666664 ], [ -87.5,40.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e57c9","contributors":{"authors":[{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Richard L. 0000-0002-3829-0125 rlsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-3829-0125","contributorId":1592,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rlsmith@usgs.gov","middleInitial":"L.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true}],"preferred":true,"id":285649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voytek, Mary A.","contributorId":91943,"corporation":false,"usgs":true,"family":"Voytek","given":"Mary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285651,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohlke, John Karl 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":66293,"corporation":false,"usgs":true,"family":"Bohlke","given":"John Karl","affiliations":[],"preferred":false,"id":285650,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72435,"text":"sir20055079 - 2005 - Feasibility of using benthic invertebrates as indicators of stream quality in Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055079","displayToPublicDate":"2005-10-09T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5079","title":"Feasibility of using benthic invertebrates as indicators of stream quality in Hawaii","docAbstract":"Macroinvertebrates were collected from 19 sites on 14 streams on the island of Oahu and from 9 sites on 7 streams on the island of Kauai to evaluate associations between macroinvertebrate assemblages and environmental variables and to determine whether or not it would be feasible, in future studies, to develop macroinvertebrate metrics that would indicate stream quality based on the macroinvertebrate assemblages and/or components of the assemblages. The purpose of applying rapid bioassessment techniques is to identify stream quality problems and to document changes in stream quality. Samples were collected at 10 sites in 1999, 3 sites in 2000, and 5 sites in 2003 on Oahu and at 9 sites on Kauai in 2003. Additionally, multiple year and multiple reach samples were collected at 1 site on Oahu. Macroinvertebrates were collected primarily from boulder/cobble riffles or from the fastest flowing habitat when riffles were absent. Although most streams in Hawaii originate in mountainous, forested areas, the lower reaches often drain urban, agricultural, or mixed land-use areas. The macroinvertebrate community data were used to identify metrics that could best differentiate between sites according to levels of environmental impairment. Environmental assessments were conducted using land-use/land-cover data, bed-sediment and fish-tissue contaminant data, and reach-level environmental data using a calibration set of 15 sites. The final scores of the environmental assessments were used to classify the sites into three categories of impairment: mild, moderate or severe. A number of invertebrate metrics were then tested and calibrated to the environmental assessments scores. The individual metrics that were the best at discerning environmental assessments among the sites were combined into a multimetric benthic index of biotic integrity (BIBI). These metrics were: total invertebrate abundance, taxa richness, insect relative abundance, amphipod abundance, crayfish presence or absence, and native mountain shrimp presence or absence. Because this index is in the preliminary stage of development and additional 'pristine' sites need to be sampled and assessed to develop a more robust measure of biotic integrity, the index will be referred to as a Preliminary Hawaiian Benthic Index of Biotic Integrity (P-HBIBI). The P-HBIBI scores were then classified into three categories of impairment: mild, moderate, or severe. The P-HBIBI was then used to assess the remaining sites and classify them into impairment categories. The P-HBIBI was correlated (r2 = 0.72; p < 0.005) with a reduced environmental assessment determined without contaminants data. The results of this study suggest that the development of a reliable Hawaiian benthic index of biotic integrity (HBIBI), based on macroinvertebrate assemblages, is feasible; however, a much larger sample size, including more samples from 'pristine' sites and from the other islands, would be required.","language":"ENGLISH","doi":"10.3133/sir20055079","usgsCitation":"Wolff, R.H., 2005, Feasibility of using benthic invertebrates as indicators of stream quality in Hawaii: U.S. Geological Survey Scientific Investigations Report 2005-5079, viii, 78 p. : ill., https://doi.org/10.3133/sir20055079.","productDescription":"viii, 78 p. : ill.","costCenters":[],"links":[{"id":191878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7456,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5079/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4823e4b07f02db4e2402","contributors":{"authors":[{"text":"Wolff, Reuben H.","contributorId":35020,"corporation":false,"usgs":true,"family":"Wolff","given":"Reuben","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72430,"text":"sir20055052 - 2005 - Hydrology and water quality of lakes and streams in Orange County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055052","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5052","title":"Hydrology and water quality of lakes and streams in Orange County, Florida","docAbstract":"Orange County, Florida, is continuing to experience a large growth in population. In 1920, the population of Orange County was less than 20,000; in 2000, the population was about 896,000. The amount of urban area around Orlando has increased considerably, especially in the northwest part of the County. The eastern one-third of the County, however, had relatively little increase in urbanization from 1977-97. The increase of population, tourism, and industry in Orange County and nearby areas changed land use; land that was once agricultural has become urban, industrial, and major recreation areas. These changes could impact surface-water resources that are important for wildlife habitat, for esthetic reasons, and potentially for public supply. Streamflow characteristics and water quality could be affected in various ways.\r\n\r\nAs a result of changing land use, changes in the hydrology and water quality of Orange County's lakes and streams could occur. Median runoff in 10 selected Orange County streams ranges from about 20 inches per year (in/yr) in the Wekiva River to about 1.1 in/yr in Cypress Creek. The runoff for the Wekiva River is significantly higher than other river basins because of the relatively constant spring discharge that sustains streamflow, even during drought conditions. The low runoff for the Cypress Creek basin results from a lack of sustained inflow from ground water and a relatively large area of lakes within the drainage basin.\r\n\r\nStreamflow characteristics for 13 stations were computed on an annual basis and examined for temporal trends. Results of the trend testing indicate changes in annual mean streamflow, 1-day high streamflow, or 7-day low streamflow at 8 of the 13 stations. However, changes in 7-day low streamflow are more common than changes in annual mean or 1-day high streamflow.\r\n\r\nThere is probably no single reason for the changes in 7-day low streamflows, and for most streams, it is difficult to determine definite reasons for the flow increases. Low flows in the Econlockhatchee River at Chuluota have increased because of discharge of treated wastewater since 1982. However, trends in increasing 7-day low streamflow are evident before 1982, which cannot be attributed to wastewater discharge.\r\n\r\nSome of the increases in 7-day low flows may be related to drainage changes resulting from increased development in Orange County. Development for most purposes, including those as diverse as cattle grazing and residential construction, may involve modification of surface drainage through stream channelization and construction of canals. These changes in land drainage can lower the water table, resulting in reductions of regional evapotranspiration rates and increased streamflow. Another possible cause of increasing low flows in streams is use of water from the Floridan aquifer system for irrigation. Runoff of irrigation water or increased seepage from irrigated areas to streams could increase base streamflow compared to natural conditions.\r\n\r\nWater-level data were analyzed to determine temporal trends from 83 lakes that had more than 15 years of record. There were significant temporal trends in 33 of the 83 lakes (40 percent) over the entire period of record. Of these 33 lakes, 14 had increasing water levels and 19 lakes had decreasing water levels. The downward trends in long-term lake levels could in part be due to high rainfall accumulation in 1960-1961, which included precipitation from Hurricane Donna (September 1960). The high rainfall resulted in historical high-water levels in many lakes in 1960 or 1961.\r\n\r\nA large range of water-quality conditions exists in lakes and streams of Orange County (2000-01). Specific conductance in lake samples ranged from 57 to 1,185 microsiemens per centimeter. Values of pH ranged from 3.2 to 8.7 in stream samples and 4.6 to 9.6 in lake samples. Total nitrogen concentrations ranged from less than 0.2 to 7.1 milligrams per liter (mg/L) as nitrogen in stream samples, and","language":"ENGLISH","doi":"10.3133/sir20055052","usgsCitation":"German, E.R., and Adamski, J.C., 2005, Hydrology and water quality of lakes and streams in Orange County, Florida: U.S. Geological Survey Scientific Investigations Report 2005-5052, 109 p. : ill.; maps, https://doi.org/10.3133/sir20055052.","productDescription":"109 p. : ill.; maps","costCenters":[],"links":[{"id":191874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7452,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5052/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604c05","contributors":{"authors":[{"text":"German, Edward R.","contributorId":85567,"corporation":false,"usgs":true,"family":"German","given":"Edward","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adamski, James C.","contributorId":20316,"corporation":false,"usgs":true,"family":"Adamski","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285639,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72423,"text":"sir20055175 - 2005 - Analysis of ground-water levels and associated trends in Yucca Flat, Nevada Test Site, Nye County, Nevada, 1951-2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055175","displayToPublicDate":"2005-10-05T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5175","title":"Analysis of ground-water levels and associated trends in Yucca Flat, Nevada Test Site, Nye County, Nevada, 1951-2003","docAbstract":"Almost 4,000 water-level measurements in 216 wells in the Yucca Flat area from 1951 to 2003 were quality assured and analyzed. An interpretative database was developed that describes water-level conditions for each water level measured in Yucca Flat. Multiple attributes were assigned to each water-level measurement in the database to describe the hydrologic conditions at the time of measurement. General quality, temporal variability, regional significance, and hydrologic conditions are attributed for each water-level measurement. The database also includes narratives that discuss the water-level history of each well.\r\n\r\nWater levels in 34 wells were analyzed for variability and for statistically significant trends. An attempt was made to identify the cause of many of the water-level fluctuations or trends. Potential causes include equilibration following well construction or development, pumping in the monitoring well, withdrawals from a nearby supply well, recharge from precipitation, earthquakes, underground nuclear tests, land subsidence, barometric pressure, and Earth tides. \r\n\r\nSome of the naturally occurring fluctuations in water levels may result from variations in recharge. The magnitude of the overall water-level change for these fluctuations generally is less than 2 feet. Long-term steady-state hydrographs for most of the wells open to carbonate rock have a very similar pattern. Carbonate-rock wells without the characteristic pattern are directly west of the Yucca and Topgallant faults in the southwestern part of Yucca Flat. Long-term steady-state hydrographs from wells open to volcanic tuffs or the Eleana confining unit have a distinctly different pattern from the general water-level pattern of the carbonate-rock aquifers.\r\n\r\nAnthropogenic water-level fluctuations were caused primarily by water withdrawals and nuclear testing. Nuclear tests affected water levels in many wells. Trends in these wells are attributed to test-cavity infilling or the effects of depressurization following nuclear testing. The magnitude of the overall water-level change for wells with anthropogenic trends can be large, ranging from several feet to hundreds of feet.\r\n\r\nVertical water-level differences at 27 sites in Yucca Flat with multiple open intervals were compared. Large vertical differences were noted in volcanic rocks and in boreholes where water levels were affected by nuclear tests. Small vertical differences were noted within the carbonate-rock and valley-fill aquifers. Vertical hydraulic gradients generally are downward in volcanic rocks and from pre-Tertiary clastic rocks toward volcanic- or carbonate-rock units.","language":"ENGLISH","doi":"10.3133/sir20055175","usgsCitation":"Fenelon, J.M., 2005, Analysis of ground-water levels and associated trends in Yucca Flat, Nevada Test Site, Nye County, Nevada, 1951-2003 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5175, 97 p. [some 11 x 17 in.] : ill.; online databases; maps, https://doi.org/10.3133/sir20055175.","productDescription":"97 p. [some 11 x 17 in.] : ill.; online databases; maps","onlineOnly":"Y","costCenters":[],"links":[{"id":7446,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5175/","linkFileType":{"id":5,"text":"html"}},{"id":191242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6803f0","contributors":{"authors":[{"text":"Fenelon, Joseph M. 0000-0003-4449-245X jfenelon@usgs.gov","orcid":"https://orcid.org/0000-0003-4449-245X","contributorId":2355,"corporation":false,"usgs":true,"family":"Fenelon","given":"Joseph","email":"jfenelon@usgs.gov","middleInitial":"M.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72418,"text":"sir20055193 - 2005 - Comparability of suspended-sediment concentration and total suspended-solids data for two sites on the L'Anguille River, Arkansas, 2001 to 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055193","displayToPublicDate":"2005-10-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5193","title":"Comparability of suspended-sediment concentration and total suspended-solids data for two sites on the L'Anguille River, Arkansas, 2001 to 2003","docAbstract":"Suspended-sediment concentration and total suspended solids data collected with automatic pumping samplers at the L'Anguille River near Colt and the L'Anguille River at Palestine, Arkansas, August 2001 to October 2003 were compared using ordinary least squares regression analyses to determine the relation between the two datasets for each of the two sites. The purpose of this report is to describe the suspended-sediment concentration and total suspended-solids data and examine the comparability of the two datasets for each site. \r\n\r\nSuspended-sediment concentration and total suspended solids data for the L'Anguille River varied spatially and temporally from August 2001 to October 2003. The site at the L'Anguille River at Palestine represents a larger portion of the L'Anguille River Basin than the site near Colt, and generally had higher median suspended-sediment concentration and total suspended solids and greater ranges in values. The differences between suspended-sediment concentration and total suspended solids data for the L'Anguille River near Colt appeared inversely related to streamflow and not related to time. The relation between suspended-sediment concentration and total suspended solids at the L'Anguille River at Palestine was more variable than at Colt and did not appear to have a relation with flow or time. The relation between suspended-sediment concentration and total suspended solids for the L'Anguille River near Colt shows that total suspended solids increased proportionally as suspended-sediment concentration increased. However, the relation between suspended-sediment concentration and total suspended solids for the L'Anguille River at Palestine showed total suspended solids increased less proportionally as suspended-sediment concentration increased compared to the L'Anguille River near Colt. \r\n\r\nDifferences between the two analytical methods may partially explain differences between the suspended-sediment concentration and total suspended solids data at the two sites. Total suspended solids are analyzed by removing an aliquot of the original sample for further analysis, and suspended-sediment concentrations are analyzed using all sediment and the total mass of the sample. At the L'Anguille River at Palestine another source of variability in the two data sets could have been the location of the automatic pumping sampler intake. The intake was located at a point in the stream cross-section that was subject to sedimentation, which may have resulted in positive sample bias.","language":"ENGLISH","doi":"10.3133/sir20055193","usgsCitation":"Galloway, J.M., Evans, D.A., and Green, W.R., 2005, Comparability of suspended-sediment concentration and total suspended-solids data for two sites on the L'Anguille River, Arkansas, 2001 to 2003 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5193, 16 p., https://doi.org/10.3133/sir20055193.","productDescription":"16 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7444,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5193/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db54638f","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":285622,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, Dennis A.","contributorId":82404,"corporation":false,"usgs":true,"family":"Evans","given":"Dennis","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285623,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Green, W. Reed","contributorId":87886,"corporation":false,"usgs":true,"family":"Green","given":"W.","email":"","middleInitial":"Reed","affiliations":[],"preferred":false,"id":285624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72415,"text":"sir20055096 - 2005 - Ground-water movement and nitrate in ground water, East Erda area, Tooele County, Utah, 1997-2000","interactions":[],"lastModifiedDate":"2019-12-30T13:44:33","indexId":"sir20055096","displayToPublicDate":"2005-10-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5096","title":"Ground-water movement and nitrate in ground water, East Erda area, Tooele County, Utah, 1997-2000","docAbstract":"Nitrate was discovered in ground water in the east Erda area of Tooele County, Utah, in 1994. The U.S. Geological Survey, in cooperation with Tooele County, investigated the ground-water flow system and water quality in the eastern part of Tooele Valley to determine (1) the vertical and horizontal distribution of nitrate, (2) the direction of movement of the nitrate contamination, and (3) the source of the nitrate. The potentiometric surface of the upper part of the basin-fill aquifer indicates that the general direction of ground-water flow is to the northwest, the flow system is complex, and there is a ground-water mound probably associated with springs. The spatial distribution of nitrate reflects the flow system with the nitrate contamination split into a north and south part by the ground-water mound. The distribution of dissolved solids and sulfate in ground water varies spatially. Vertical profiles of nitrate in water from selected wells indicate that nitrate contamination generally is in the upper part of the saturated zone and in some wells has moved downward. Septic systems, mining and smelting, agriculture, and natural sources were considered to be possible sources of nitrate contamination in the east Erda area. Septic systems are not the source of nitrate because water from wells drilled upgradient of all septic systems in the area had elevated nitrate concentrations. Mining and smelting activity are a possible source of nitrate contamination but few data are available to link nitrate contamination with mining sites. Natural and agricultural sources of nitrate are present east of the Erda area but few data are available about these sources. The source(s) of nitrate in the east Erda area could not be clearly delineated in spite of considerable effort and expenditure of resources.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055096","collaboration":"Prepared in cooperation with Tooele County","usgsCitation":"Susong, D., 2005, Ground-water movement and nitrate in ground water, East Erda area, Tooele County, Utah, 1997-2000 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5096, 4 sheets: 40.00 x 36.00 inches or smaller, https://doi.org/10.3133/sir20055096.","productDescription":"4 sheets: 40.00 x 36.00 inches or smaller","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":334244,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5096/PDF/SIR2005_5096_sheet1.pdf","text":"First part of report","size":"3.5 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":334245,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5096/PDF/SIR2005_5096_sheet2.pdf","text":"Second part of report","size":"2.4 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":334246,"rank":5,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/sir/2005/5096/PDF/SIR2005_5096_sheet3.pdf","text":"First part of Table 1; Table 2","size":"2.6 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":334247,"rank":6,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/sir/2005/5096/PDF/SIR2005_5096_sheet4.pdf","text":"Second part of Table 1","size":"1.5 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":7442,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5096/","linkFileType":{"id":5,"text":"html"}},{"id":191190,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","county":"Tooele County","otherGeospatial":"East Erda area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-112.4938,41.0762],[-112.4784,41.0554],[-112.4404,41.0056],[-112.3975,40.9508],[-112.2611,40.7706],[-112.2258,40.7262],[-112.2033,40.7113],[-112.2009,40.7077],[-112.2002,40.7045],[-112.1978,40.6995],[-112.196,40.6927],[-112.1996,40.6882],[-112.2032,40.6787],[-112.1995,40.6728],[-112.2007,40.6646],[-112.2025,40.6533],[-112.1976,40.6483],[-112.197,40.6433],[-112.1928,40.6397],[-112.1928,40.6383],[-112.194,40.6261],[-112.1933,40.6242],[-112.1927,40.6233],[-112.1879,40.6152],[-112.18,40.6129],[-112.18,40.6088],[-112.1739,40.6039],[-112.1769,40.6021],[-112.1781,40.5943],[-112.1745,40.5857],[-112.1793,40.5785],[-112.1835,40.573],[-112.1805,40.5676],[-112.1817,40.5617],[-112.1762,40.5562],[-112.1774,40.5544],[-112.1822,40.5431],[-112.181,40.5399],[-112.1774,40.5299],[-112.1779,40.5204],[-112.1864,40.514],[-112.1797,40.5018],[-112.1864,40.4964],[-112.1724,40.4846],[-112.1754,40.4814],[-112.17,40.4719],[-112.173,40.4674],[-112.1814,40.4683],[-112.1869,40.4687],[-112.2002,40.4601],[-112.2116,40.4587],[-112.2128,40.4551],[-112.2122,40.4446],[-112.2085,40.4392],[-112.2073,40.4347],[-112.2043,40.4306],[-112.1958,40.4215],[-112.1946,40.4124],[-112.197,40.4047],[-112.1994,40.3948],[-112.2,40.3907],[-112.2,40.3861],[-112.1945,40.3784],[-112.1872,40.3739],[-112.192,40.3621],[-112.1896,40.3567],[-112.183,40.3481],[-112.1781,40.3413],[-112.1769,40.3358],[-112.1901,40.3268],[-112.1949,40.319],[-112.1985,40.3122],[-112.1925,40.3045],[-112.1889,40.2991],[-112.1876,40.2887],[-112.187,40.2787],[-112.1912,40.2687],[-112.1918,40.2664],[-112.1882,40.2619],[-112.1845,40.2574],[-112.1845,40.2542],[-112.1809,40.2497],[-112.1767,40.2424],[-112.1772,40.2388],[-112.1772,40.2338],[-112.1742,40.2306],[-112.1724,40.2279],[-112.17,40.2238],[-112.1652,40.2189],[-112.1549,40.2193],[-112.1513,40.2125],[-112.1597,40.198],[-112.1507,40.198],[-112.1464,40.1903],[-112.1452,40.1744],[-112.1542,40.1694],[-112.1566,40.1667],[-112.1602,40.1622],[-112.1728,40.1567],[-112.1662,40.1459],[-112.1716,40.1399],[-112.1746,40.1354],[-112.174,40.1304],[-112.1728,40.1295],[-112.1674,40.1255],[-112.1625,40.1168],[-112.1511,40.1082],[-112.1589,40.0883],[-112.1727,40.0851],[-112.1739,40.0792],[-112.1732,40.0747],[-112.1714,40.0692],[-112.1792,40.0674],[-112.1804,40.0561],[-112.1738,40.047],[-112.172,40.0416],[-112.1713,40.0361],[-112.1725,40.0275],[-112.1773,40.0112],[-112.2055,40.0016],[-112.2151,39.9993],[-112.221,39.9889],[-112.2282,39.9766],[-112.2366,39.9689],[-112.2348,39.9621],[-112.2341,39.9576],[-112.2473,39.953],[-112.2545,39.9516],[-112.2635,39.9412],[-112.2689,39.9412],[-112.2785,39.9407],[-112.2923,39.9407],[-112.3031,39.9366],[-112.3103,39.9379],[-112.3169,39.9461],[-112.3179,39.9461],[-112.3239,39.9444],[-112.332,39.9526],[-112.3397,39.9442],[-112.3361,39.9261],[-112.3366,39.9206],[-112.3395,39.9134],[-112.3431,39.9106],[-112.3407,39.9057],[-112.3419,39.9038],[-112.3467,39.9047],[-112.3653,39.9042],[-112.3851,39.9046],[-112.4606,39.9044],[-112.4984,39.9038],[-112.5361,39.9041],[-112.5553,39.904],[-112.5739,39.9039],[-112.5937,39.9043],[-112.6117,39.9042],[-112.6381,39.9036],[-112.65,39.904],[-112.6686,39.9039],[-112.6872,39.9038],[-112.7022,39.9037],[-112.7064,39.9037],[-112.725,39.9036],[-112.7496,39.9039],[-112.7993,39.9036],[-112.8185,39.9039],[-112.8383,39.9038],[-112.8641,39.904],[-112.8761,39.9044],[-112.8947,39.9048],[-112.9132,39.9046],[-112.9312,39.9045],[-112.9498,39.9048],[-112.9882,39.9045],[-113.0074,39.9048],[-113.026,39.9047],[-113.0446,39.9049],[-113.0638,39.9048],[-113.1009,39.9049],[-113.1063,39.9049],[-113.1201,39.9052],[-113.1357,39.9046],[-113.1543,39.9049],[-113.1729,39.9052],[-113.2106,39.9053],[-113.2214,39.9052],[-113.2298,39.9051],[-113.2466,39.9049],[-113.2682,39.9047],[-113.2868,39.905],[-113.3246,39.905],[-113.3617,39.9051],[-113.4067,39.9055],[-113.4175,39.9054],[-113.5026,39.9053],[-113.5218,39.9055],[-113.5524,39.9052],[-113.5854,39.9052],[-113.6046,39.9054],[-113.6238,39.9056],[-113.6567,39.9056],[-113.6795,39.9053],[-113.6993,39.9055],[-113.7395,39.9054],[-113.7743,39.9054],[-113.7881,39.9052],[-113.7935,39.9056],[-113.8114,39.9053],[-113.8318,39.9055],[-113.8642,39.9054],[-113.8882,39.9051],[-113.9068,39.9053],[-113.9248,39.9054],[-113.9446,39.9056],[-114.0003,39.9052],[-114.0363,39.905],[-114.0405,39.905],[-114.0474,39.9053],[-114.0476,39.982],[-114.0484,40.1186],[-114.0487,40.1683],[-114.0487,40.2161],[-114.0463,40.4287],[-114.0445,40.5541],[-114.0437,40.603],[-114.0434,40.6253],[-114.0434,40.6315],[-114.0422,40.7055],[-114.0418,40.7315],[-114.0415,40.7509],[-114.041,40.7777],[-114.0406,40.794],[-114.0406,40.7968],[-114.0401,40.9225],[-114.0401,40.937],[-114.04,40.9578],[-114.0399,40.9647],[-114.04,40.9793],[-114.0402,40.9938],[-114.0403,41],[-114.0367,40.9996],[-114.0179,41.0004],[-113.9984,41.0002],[-113.9795,41.0005],[-113.96,41.0008],[-113.9168,41.001],[-113.898,41.0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only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6d0f","contributors":{"authors":[{"text":"Susong, D. D.","contributorId":12868,"corporation":false,"usgs":true,"family":"Susong","given":"D. D.","affiliations":[],"preferred":false,"id":285618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72414,"text":"ofr20051054 - 2005 - Magnetotelluric data across the Pajarito fault, west of Santa Fe, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"ofr20051054","displayToPublicDate":"2005-10-03T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1054","title":"Magnetotelluric data across the Pajarito fault, west of Santa Fe, New Mexico","language":"ENGLISH","doi":"10.3133/ofr20051054","usgsCitation":"Williams, J.M., and Rodriguez, B.D., 2005, Magnetotelluric data across the Pajarito fault, west of Santa Fe, New Mexico (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1054, 174 p., https://doi.org/10.3133/ofr20051054.","productDescription":"174 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7441,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1054/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64942a","contributors":{"authors":[{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285617,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":285616,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72394,"text":"fs20053106 - 2005 - Southern California — Wildfires and debris flows","interactions":[],"lastModifiedDate":"2022-01-26T19:48:23.712313","indexId":"fs20053106","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3106","title":"Southern California — Wildfires and debris flows","docAbstract":"<p class=\"textindent\">Wildland fires are inevitable in the western United States. Expansion of man-made developments into fire-prone wildlands has created situations where wildfires can destroy lives and property, as can the flooding and debris flows that are common in the aftermath of the fires. Fast-moving, highly destructive debris flows triggered by intense rainfall are one of the most dangerous post-fire hazards. Such debris flows are particularly dangerous because they tend to occur with little warning. Their mass and speed make them particularly destructive: debris flows can strip vegetation, block drainages, damage structures, and endanger human life.</p><p class=\"textindent\">The U.S. Geological Survey’s Landslide Hazards Program is participating in a multi-agency cooperative effort to investigate debris flows in burned areas of southern California and other parts of the western United States. Participating agencies are the USDA Forest Service, the Natural Resources Conservation Service, and the California, Colorado, and Montana Geological Surveys. The objective of this project is to develop methods needed to estimate the locations, probability of occurrence, and size of potentially destructive debris flows. Public officials can use this information to plan and execute emergency response and post-fire rehabilitation.</p><p class=\"textindent\">Analysis of data collected from studies of debris flows following wildfires can answer many of the questions fundamental to post-fire hazard assessments— what and why, where, when, how big, and how often?</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053106","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Southern California — Wildfires and debris flows (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3106, 4 p., https://doi.org/10.3133/fs20053106.","productDescription":"4 p.","costCenters":[],"links":[{"id":126266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3106.jpg"},{"id":394899,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73917.htm"},{"id":7396,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3106/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.80639648437499,\n              34.18454183141725\n            ],\n            [\n              -116.8341064453125,\n              34.18454183141725\n            ],\n            [\n              -116.8341064453125,\n              34.44315867450577\n            ],\n            [\n              -117.80639648437499,\n              34.44315867450577\n            ],\n            [\n              -117.80639648437499,\n              34.18454183141725\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e72fb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534744,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72387,"text":"ofr20051325 - 2005 - Preliminary integrated geologic map databases for the United States: Delaware, Maryland, New York, Pennsylvania, and Virginia","interactions":[],"lastModifiedDate":"2021-12-02T22:39:35.853082","indexId":"ofr20051325","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1325","title":"Preliminary integrated geologic map databases for the United States: Delaware, Maryland, New York, Pennsylvania, and Virginia","docAbstract":"<p class=\"style1\">The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. Such maps can be conveniently used to generate derivative maps for purposes including mineral-resource assessment, metallogenic studies, tectonic studies, and environmental research. This Open-File Report is a preliminary version of part of a series of integrated state geologic map databases that cover the entire United States.</p><p class=\"style1\">The only national-scale digital geologic maps that portray most or all of the United States for the conterminous U.S. are the digital version of the King and Beikman (1974a, b) map at a scale of 1:2,500,000, as digitized by Schruben and others (1994) and the generalized digital version (Reed and Bush, 2004) of the Geologic Map of North America (Reed and others, 2005a, b) compiled at a scale of 1:5,000,000. The present series of maps is intended to provide the next step in increased detail. State geologic maps that range in scale from 1:100,000 to 1:1,000,000 are available for most of the country, and digital versions of these state maps are the basis for this product. In a few cases, new digital compilations were prepared (e.g. Ohio, South Carloina, South Dakota) or existing paper maps were digitized (e.g. Kentucky, Texas). Also as part of this series, new regional maps for Alaska and Hawaii are being compiled and ultimately new state maps will be produced.</p><p class=\"style1\">The digital geologic maps are presented in standardized formats as ARC/INFO export (.e00) files and as ArcView shape (.shp) files. Accompanying these spatial databases are a set of five supplemental attribute tables that relate the map units to detailed lithologic and age information. The maps for the CONUS have been fitted to a common set of state boundaries based on the 1:100,000 topographic map series of the United States Geological Survey (USGS). When the individual state maps are merged, the combined attribute tables can be used directly with the merged maps to make derivative maps. No attempt has been made to reconcile differences in mapped geology across state lines.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051325","usgsCitation":"Dicken, C.L., Nicholson, S.W., Horton, J.D., Kinney, S.A., Gunther, G.L., Foose, M.P., and Mueller, J.A., 2005, Preliminary integrated geologic map databases for the United States: Delaware, Maryland, New York, Pennsylvania, and Virginia: U.S. Geological Survey Open-File Report 2005-1325, HTML Document, https://doi.org/10.3133/ofr20051325.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":191326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392420,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73912.htm"},{"id":7389,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1325/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Delaware, Maryland, New York, Pennsylvania, Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.6171875,\n              36.66841891894786\n            ],\n            [\n              -75.41015624999999,\n              36.66841891894786\n            ],\n            [\n              -75.41015624999999,\n              44.213709909702054\n            ],\n            [\n              -82.6171875,\n              44.213709909702054\n            ],\n            [\n              -82.6171875,\n              36.66841891894786\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6732d0","contributors":{"authors":[{"text":"Dicken, Connie L. 0000-0002-1617-8132 cdicken@usgs.gov","orcid":"https://orcid.org/0000-0002-1617-8132","contributorId":57098,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie","email":"cdicken@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":285564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, John D. 0000-0003-2969-9073 jhorton@usgs.gov","orcid":"https://orcid.org/0000-0003-2969-9073","contributorId":1227,"corporation":false,"usgs":true,"family":"Horton","given":"John","email":"jhorton@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285565,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kinney, Scott A. 0000-0001-5008-5813 skinney@usgs.gov","orcid":"https://orcid.org/0000-0001-5008-5813","contributorId":1395,"corporation":false,"usgs":true,"family":"Kinney","given":"Scott","email":"skinney@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285566,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gunther, Gregory L. 0000-0002-1761-1604 ggunther@usgs.gov","orcid":"https://orcid.org/0000-0002-1761-1604","contributorId":1581,"corporation":false,"usgs":true,"family":"Gunther","given":"Gregory","email":"ggunther@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285567,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":285568,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mueller, Julia A. L.","contributorId":43861,"corporation":false,"usgs":true,"family":"Mueller","given":"Julia","email":"","middleInitial":"A. L.","affiliations":[],"preferred":false,"id":285569,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":72390,"text":"ofr20051342 - 2005 - Preliminary integrated geologic map databases for the United States: Digital data for the geology of Wrangell-Saint Elias National Park and Preserve, Alaska","interactions":[],"lastModifiedDate":"2022-05-11T18:21:55.329853","indexId":"ofr20051342","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1342","title":"Preliminary integrated geologic map databases for the United States: Digital data for the geology of Wrangell-Saint Elias National Park and Preserve, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051342","usgsCitation":"Wilson, F.H., Labay, K., Shew, N.B., Preller, C.C., Mohadjer, S., and Richter, D.H., 2005, Preliminary integrated geologic map databases for the United States: Digital data for the geology of Wrangell-Saint Elias National Park and Preserve, Alaska: U.S. Geological Survey Open-File Report 2005-1342, HTML Document, https://doi.org/10.3133/ofr20051342.","productDescription":"HTML Document","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":191792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":400525,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73915.htm"},{"id":7392,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1342/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Wrangell-Saint Elias National Park and Preserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147,\n              59\n            ],\n            [\n              -138,\n              59\n            ],\n            [\n              -138,\n              63\n            ],\n            [\n              -147,\n              63\n            ],\n            [\n              -147,\n              59\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67329a","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":285580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Labay, Keith A. 0000-0002-6763-3190 klabay@usgs.gov","orcid":"https://orcid.org/0000-0002-6763-3190","contributorId":2097,"corporation":false,"usgs":true,"family":"Labay","given":"Keith A.","email":"klabay@usgs.gov","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":false,"id":285585,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shew, Nora B. 0000-0003-0025-7220 nshew@usgs.gov","orcid":"https://orcid.org/0000-0003-0025-7220","contributorId":3382,"corporation":false,"usgs":true,"family":"Shew","given":"Nora","email":"nshew@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":285581,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Preller, Cindi C.","contributorId":55898,"corporation":false,"usgs":true,"family":"Preller","given":"Cindi","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285582,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mohadjer, Solmaz","contributorId":61518,"corporation":false,"usgs":true,"family":"Mohadjer","given":"Solmaz","email":"","affiliations":[],"preferred":false,"id":285584,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Richter, Donald H.","contributorId":61021,"corporation":false,"usgs":true,"family":"Richter","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285583,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":72393,"text":"sir20055006 - 2005 - Questa baseline and premining ground-water quality investigation. 8. Lake-sediment geochemical record from 1960 to 2002, Eagle Rock and Fawn Lakes, Taos County, New Mexico","interactions":[],"lastModifiedDate":"2022-06-28T20:13:26.042792","indexId":"sir20055006","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5006","title":"Questa baseline and premining ground-water quality investigation. 8. Lake-sediment geochemical record from 1960 to 2002, Eagle Rock and Fawn Lakes, Taos County, New Mexico","docAbstract":"<p><span>Geochemical studies of lake sediment from Eagle Rock Lake and upper Fawn Lake were conducted to evaluate the effect of mining at the Molycorp Questa porphyry molybdenum deposit located immediately north of the Red River. Two cores were taken, one from each lake near the outlet where the sediment was thinnest, and they were sampled at 1-cm intervals to provide geochemical data at less than 1-year resolution. Samples from the core intervals were digested and analyzed for 34 elements using ICP–AES (inductively coupled plasma–atomic emission spectrometry). The activity of&nbsp;</span><sup>137</sup><span>Cs has been used to establish the beginning of sedimentation in the two lakes. Correlation of the geochemistry of heavy-mineral suites in the cores from both Fawn and Eagle Rock Lakes has been used to develop a sedimentation model to date the intervals sampled. The core from upper Fawn Lake, located upstream of the deposit, provided an annual sedimentary record of the geochemical baseline for material being transported in the Red River, whereas the core from Eagle Rock Lake, located downstream of the deposit, provided an annual record of the effect of mining at the Questa mine on the sediment in the Red River. Abrupt changes in the concentrations of many lithophile and deposit-related metals occur in the middle of the Eagle Rock Lake core, which we correlate with the major flood-of-record recorded at the Questa gage at Eagle Rock Lake in 1979. Sediment from the Red River collected&nbsp;</span><i>at low flow</i><span>&nbsp;in 2002 is a poor match for the geochemical data from the sediment core in Eagle Rock Lake. The change in sediment geochemistry in Eagle Rock Lake in the post-1979 interval is dramatic and requires that a new source of sediment be identified that has substantially different geochemistry from that in the pre-1979 core interval. Loss of mill tailings from pipeline breaks are most likely responsible for some of the spikes in trace-element concentrations in the Eagle Rock Lake core. Enrichment of Al</span><sub>2</sub><span>O</span><sub>3</sub><span>, Cu, and Zn occurred as a result of chemical precipitation of these metals from ground water upstream in the Red River. Comparisons of the geochemistry of the post-1979 sediment core with both mine wastes and with premining sediment from the vicinity of the Questa mine indicate that both are possible sources for this new component of sediment. Existing data have not resolved this enigma.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055006","usgsCitation":"Church, S.E., Fey, D., and Marot, M.E., 2005, Questa baseline and premining ground-water quality investigation. 8. Lake-sediment geochemical record from 1960 to 2002, Eagle Rock and Fawn Lakes, Taos County, New Mexico (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5006, 47 p., https://doi.org/10.3133/sir20055006.","productDescription":"47 p.","temporalStart":"1960-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":402636,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73907.htm","linkFileType":{"id":5,"text":"html"}},{"id":191893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7395,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5006/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","county":"Taos County","otherGeospatial":"Eagle Rock and Fawn Lakes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.58547973632812,\n              36.6959520787169\n            ],\n            [\n              -105.42823791503906,\n              36.6959520787169\n            ],\n            [\n              -105.42823791503906,\n              36.72842852891896\n            ],\n            [\n              -105.58547973632812,\n              36.72842852891896\n            ],\n            [\n              -105.58547973632812,\n              36.6959520787169\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a06c","contributors":{"authors":[{"text":"Church, S. E.","contributorId":58260,"corporation":false,"usgs":true,"family":"Church","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":285597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":285596,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Marot, M. E.","contributorId":7733,"corporation":false,"usgs":true,"family":"Marot","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":285595,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72382,"text":"ofr20051225 - 2005 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","interactions":[{"subject":{"id":72382,"text":"ofr20051225 - 2005 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"ofr20051225","publicationYear":"2005","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"id":1}],"supersededBy":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"lastModifiedDate":"2016-04-19T12:15:23","indexId":"ofr20051225","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1225","title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","docAbstract":"<p><span>The geology of the Great Smoky Mountain National Park (GSMNP) region of Tennessee and North Carolina was studied from 1993 to 2003 as part of a cooperative investigation with the National Park Service (NPS). This work has been compiled as a 1:100,000-scale map derived from mapping done at 1:24,000 and 1:62,500 scale. The geologic data are intended to support cooperative investigations with NPS, the development of a new soil map by the Natural Resources Conservation Service, and the All Taxa Biodiversity Inventory (</span><a href=\"http://www.discoverlifeinamerica.org/\">http://www.discoverlifeinamerica.org/</a><span>). At the request of NPS, we mapped areas previously not visited, revised the geology where stratigraphic and structural problems existed, and developed a map database for use in interdisciplinary research, land management, and interpretive programs for park visitors.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051225","usgsCitation":"Southworth, S., Schultz, A., and Denenny, D., 2005, Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1225, Report: 117 p. ; Plate: 40.75 x 50 in.; Shapefiles, https://doi.org/10.3133/ofr20051225.","productDescription":"Report: 117 p. ; Plate: 40.75 x 50 in.; Shapefiles","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":191322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7385,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1225/","linkFileType":{"id":5,"text":"html"}},{"id":110579,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73809.htm","linkFileType":{"id":5,"text":"html"},"description":"73809"}],"country":"United States","state":"North Carolina, Tennessee","otherGeospatial":"Great Smoky Mountains National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84,\n              35.3\n            ],\n            [\n              -84,\n              35.88\n            ],\n            [\n              -83,\n              35.88\n            ],\n            [\n              -83,\n              35.3\n            ],\n            [\n              -84,\n              35.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698696","contributors":{"authors":[{"text":"Southworth, Scott","contributorId":93933,"corporation":false,"usgs":true,"family":"Southworth","given":"Scott","affiliations":[],"preferred":false,"id":285534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schultz, Art","contributorId":44982,"corporation":false,"usgs":true,"family":"Schultz","given":"Art","email":"","affiliations":[],"preferred":false,"id":285532,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denenny, Danielle","contributorId":78804,"corporation":false,"usgs":true,"family":"Denenny","given":"Danielle","affiliations":[],"preferred":false,"id":285533,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72392,"text":"sir20055066 - 2005 - Reconnaissance of surface-water and ground-water quality at the Lincoln Boyhood National Memorial near Lincoln City, Indiana, 2001-02","interactions":[],"lastModifiedDate":"2016-05-09T09:53:37","indexId":"sir20055066","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5066","title":"Reconnaissance of surface-water and ground-water quality at the Lincoln Boyhood National Memorial near Lincoln City, Indiana, 2001-02","docAbstract":"<p>In cooperation with the National Park Service, the U.S. Geological Survey investigated water quality of key water bodies at the Lincoln Boyhood National Memorial near Lincoln City in southwestern Indiana. The key water bodies were a stock pond, representing possible nonpoint agricultural effects on water quality; an ephemeral stream, representing the water quality of drainage from forested areas of the park; parking-lot runoff, representing water quality related to roads and parking lots; an unnamed ditch below the parking lot, representing the water quality of drainage from the parking lot and from an adjacent railroad track; and Lincoln Spring, a historical ground-water source representing ground-water conditions near a former diesel-fuel-spill site along a rail line. Water samples were analyzed for pH, temperature, specific conductance, and dissolved oxygen and for concentrations of selected major ions and trace metals, nutrients, organic constituents, and Escherichia coli bacteria. Surface-water-quality data of water samples from the park represent baseline conditions for the area in relation to the data available from previous studies of area streams. Specific-conductance values and concentrations of most major ions and various nutrients in surface-water samples from the park were smaller than those reported for samples collected in other USGS studies in areas adjacent to the park. Water-quality-management issues identified by this investigation include potentially impaired water quality from parking-lot runoff, unknown effects on surface-water quality from adjacent railroads, and the potential impairment of water quality in Lincoln Spring from human influences. Parking-lot runoff is a source of calcium, alkalinity, iron, lead, and organic carbon in the water samples from the unnamed ditch. Detection of small concentrations of petroleum hydrocarbons in water from Lincoln Spring could indicate residual contamination from a 1995 diesel-fuel spill and cleanup. The concentration of nitrite plus nitrate in water from Lincoln Spring was 16.5 milligrams per liter as nitrogen, greater than the State of Indiana standard for nitrate in drinking water (10 milligrams per liter as nitrogen). Lead concentrations in samples from the stock pond, parking-lot runoff, and the unnamed ditch exceeded the Indiana chronic aquatic criteria.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055066","usgsCitation":"Buszka, P.M., and Fowler, K.K., 2005, Reconnaissance of surface-water and ground-water quality at the Lincoln Boyhood National Memorial near Lincoln City, Indiana, 2001-02: U.S. Geological Survey Scientific Investigations Report 2005-5066, 57 p.: ill., https://doi.org/10.3133/sir20055066.","productDescription":"57 p.: ill.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":7394,"rank":100,"type":{"id":15,"text":"Index 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Such maps can be conveniently used to generate derivative maps for purposes including mineral-resource assessment, metallogenic studies, tectonic studies, and environmental research. This Open-File Report is a preliminary version of part of a series of integrated state geologic map databases that cover the entire United States.\r\n\r\nThe only national-scale digital geologic maps that portray most or all of the United States for the conterminous U.S. are the digital version of the King and Beikman (1974a, b) map at a scale of 1:2,500,000, as digitized by Schruben and others (1994) and the digital version of the Geologic Map of North America (Reed and others, 2005a, b) compiled at a scale of 1:5,000,000 which is currently being prepared by the U.S. Geological Survey. The present series of maps is intended to provide the next step in increased detail. State geologic maps that range in scale from 1:100,000 to 1:1,000,000 are available for most of the country, and digital versions of these state maps are the basis of this product. In a few cases, new digital compilations were prepared (e.g. OH, SC, SD) or existing paper maps were digitized (e.g. KY, TX). For Alaska and Hawaii, new regional maps are being compiled and ultimately new state maps will be produced.\r\n\r\nThe digital geologic maps are presented in standardized formats as ARC/INFO (.e00) export files and as ArcView shape (.shp) files. Accompanying these spatial databases are a set of five supplemental data tables that relate the map units to detailed lithologic and age information. The maps for the CONUS have been fitted to a common set of state boundaries based on the 1:100,000 topographic map series of the United States Geological Survey (USGS). When the individual state maps are merged, the combined attribute tables can be used directly with the merged maps to make derivative maps. No attempt has been made to reconcile differences in mapped geology across state lines.\r\n\r\nThis is the first version of this product and it will be subsequently updated to include four additional states (North Dakota, South Dakota, Nebraska, and Iowa)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051351","collaboration":"Version updated 20-Sept-2006","usgsCitation":"Stoeser, D.B., Green, G.N., Morath, L.C., Heran, W.D., Wilson, A.B., Moore, D., and Van Gosen, B.S., 2005, Preliminary integrated geologic map databases for the United States: Central states: Montana, Wyoming, Colorado, New Mexico, North Dakota, South Dakota, Nebraska, Kansas, Oklahoma, Texas, Iowa, Missouri, Arkansas, and Louisiana (Version 1.2: December 2007): U.S. Geological Survey Open-File Report 2005-1351, HTML Document, https://doi.org/10.3133/ofr20051351.","productDescription":"HTML 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,{"id":72385,"text":"ofr20051323 - 2005 - Preliminary integrated geologic map databases for the United States: Alabama, Florida, Georgia, Mississippi, North Carolina, and South Carolina","interactions":[],"lastModifiedDate":"2022-05-11T18:16:22.29721","indexId":"ofr20051323","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1323","title":"Preliminary integrated geologic map databases for the United States: Alabama, Florida, Georgia, Mississippi, North Carolina, and South Carolina","docAbstract":"<p class=\"style1\">The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. 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jhorton@usgs.gov","orcid":"https://orcid.org/0000-0003-2969-9073","contributorId":1227,"corporation":false,"usgs":true,"family":"Horton","given":"John","email":"jhorton@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285554,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":285555,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mueller, Julia A. 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,{"id":72386,"text":"ofr20051324 - 2005 - Preliminary integrated geologic map databases for the United States: Kentucky, Ohio, Tennessee, and West Virginia","interactions":[],"lastModifiedDate":"2021-12-02T22:43:03.19113","indexId":"ofr20051324","displayToPublicDate":"2005-10-02T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1324","title":"Preliminary integrated geologic map databases for the United States: Kentucky, Ohio, Tennessee, and West Virginia","docAbstract":"<p class=\"style1\">The growth in the use of Geographic Information Systems (GIS) has highlighted the need for regional and national digital geologic maps attributed with age and lithology information. 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State geologic maps that range in scale from 1:100,000 to 1:1,000,000 are available for most of the country, and digital versions of these state maps are the basis for this product. In a few cases, new digital compilations were prepared (e.g. Ohio, South Carloina, South Dakota) or existing paper maps were digitized (e.g. Kentucky, Texas). Also as part of this series, new regional maps for Alaska and Hawaii are being compiled and ultimately new state maps will be produced.</p><p class=\"style1\">The digital geologic maps are presented in standardized formats as ARC/INFO export (.e00) files and as ArcView shape (.shp) files. Accompanying these spatial databases are a set of five supplemental attribute tables that relate the map units to detailed lithologic and age information. The maps for the CONUS have been fitted to a common set of state boundaries based on the 1:100,000 topographic map series of the United States Geological Survey (USGS). When the individual state maps are merged, the combined attribute tables can be used directly with the merged maps to make derivative maps. No attempt has been made to reconcile differences in mapped geology across state lines.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051324","usgsCitation":"Nicholson, S.W., Dicken, C.L., Horton, J.D., Labay, K., Foose, M.P., and Mueller, J.A., 2005, Preliminary integrated geologic map databases for the United States: Kentucky, Ohio, Tennessee, and West Virginia: U.S. Geological Survey Open-File Report 2005-1324, HTML Document, https://doi.org/10.3133/ofr20051324.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":191325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":392422,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73911.htm"},{"id":7388,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1324/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky, Ohio, Tennessee, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.3061,\n              34.9864\n            ],\n            [\n              -77.73,\n              34.9864\n            ],\n            [\n              -77.73,\n              41.9778\n            ],\n            [\n              -90.3061,\n              41.9778\n            ],\n            [\n              -90.3061,\n              34.9864\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db67327b","contributors":{"authors":[{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":285558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dicken, Connie L. 0000-0002-1617-8132 cdicken@usgs.gov","orcid":"https://orcid.org/0000-0002-1617-8132","contributorId":57098,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie","email":"cdicken@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285562,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, John D. 0000-0003-2969-9073 jhorton@usgs.gov","orcid":"https://orcid.org/0000-0003-2969-9073","contributorId":1227,"corporation":false,"usgs":true,"family":"Horton","given":"John","email":"jhorton@usgs.gov","middleInitial":"D.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":285559,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Labay, Keith A. 0000-0002-6763-3190 klabay@usgs.gov","orcid":"https://orcid.org/0000-0002-6763-3190","contributorId":2097,"corporation":false,"usgs":true,"family":"Labay","given":"Keith A.","email":"klabay@usgs.gov","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":false,"id":285563,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Foose, Michael P. mfoose@usgs.gov","contributorId":4756,"corporation":false,"usgs":true,"family":"Foose","given":"Michael","email":"mfoose@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":285560,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mueller, Julia A. L.","contributorId":43861,"corporation":false,"usgs":true,"family":"Mueller","given":"Julia","email":"","middleInitial":"A. L.","affiliations":[],"preferred":false,"id":285561,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70203380,"text":"70203380 - 2005 - Hydrothermal vent fluids, siliceous hydrothermal deposits, and hydrothermally altered sediments in Yellowstone Lake","interactions":[],"lastModifiedDate":"2019-05-13T11:48:34","indexId":"70203380","displayToPublicDate":"2005-10-01T14:57:51","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydrothermal vent fluids, siliceous hydrothermal deposits, and hydrothermally altered sediments in Yellowstone Lake","docAbstract":"<p><span>Stable isotopic (dD and d18O) data indicate about 13% total evaporative concentration has occurred in Yellowstone Lake, yet lake waters are enriched in dissolved As, B, Cl, Cs, Ge, Li, Mo, Sb, and W by at least an order-of-magnitude relative to the flow-weighted composition of inflowing streams. We conclude that lake water is a mixture of inflowing surface water and hydrothermal source fluid that is strongly enriched in Cl and other elements. We estimate that ~10% of the total hydrothermal flux in Yellowstone National Park (YNP) occurs in Yellowstone Lake. Geochemical and mineralogical studies of hydrothermal deposits and hydrothermally altered lake sediments (vent muds) from the active or recently active vent sites on the floor of Yellowstone Lake indicate that their formation is due to hydrothermal fluid quenching during flow through shallow conduits, or to mixing upon egress into cold bottom waters. Siliceous precipitates form conduits within the uppermost sediments, tabular deposits along sedimentary layers, and spires up to 8 m tall. These deposits are enriched in As, Cs, Hg, Mo, Sb, Tl and W. Spires, vent deposits, and conduits contain filamentous microstructures that probably represent silicified bacteria. Partly recrystallized and silicified diatoms are abundant in deposits below the sediment-water interface. Vent muds and some outer conduit walls show pervasive leaching of silica, which explains the occurrence of most sublacustrine vents in craters. Systematics of dD and Cl variations, as well as silica and cation geothermometry for hydrothermal fluids, suggest that ascending fluids boil due to depressurization to a temperature of ~220°C and then mix with pore waters prior to venting on the lake bottom. Depositional temperatures for sublacustrine silica deposits, calculated using oxygen isotope fractionation, range from 78°C to 164°C. The amorphous silica-saturated vent fluids precipitate silica to form spires or conduits largely by conductive cooling. Bacterial accumulations may have inhibited the mixing of vent fluids and bottom waters, and provided a site for silica deposition.</span></p>","conferenceTitle":"Thermal Biology Institute Workshop","conferenceDate":"October 2005","conferenceLocation":"Yellowstone National Park, WY","language":"English","publisher":"Montana State University","usgsCitation":"Shanks, W.C., Morgan, L., Balistrieri, L.S., and Alt, J.C., 2005, Hydrothermal vent fluids, siliceous hydrothermal deposits, and hydrothermally altered sediments in Yellowstone Lake, Thermal Biology Institute Workshop, Yellowstone National Park, WY, October 2005, p. 53-72.","productDescription":"20 p.","startPage":"53","endPage":"72","numberOfPages":"20","costCenters":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":363603,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.rcn.montana.edu/Publications/Pdf/2005/1_3Shanks.pdf"},{"id":363604,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.8740234375,\n              44.19402066387343\n            ],\n            [\n              -110.10223388671875,\n              44.19402066387343\n            ],\n            [\n              -110.10223388671875,\n              44.69404054463804\n            ],\n            [\n              -110.8740234375,\n              44.69404054463804\n            ],\n            [\n              -110.8740234375,\n              44.19402066387343\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Shanks, W. C. Pat pshanks@usgs.gov","contributorId":193431,"corporation":false,"usgs":true,"family":"Shanks","given":"W.","email":"pshanks@usgs.gov","middleInitial":"C. Pat","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":762406,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, Lisa","contributorId":57751,"corporation":false,"usgs":true,"family":"Morgan","given":"Lisa","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":762407,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balistrieri, Laurie S. 0000-0002-6359-3849 balistri@usgs.gov","orcid":"https://orcid.org/0000-0002-6359-3849","contributorId":1406,"corporation":false,"usgs":true,"family":"Balistrieri","given":"Laurie","email":"balistri@usgs.gov","middleInitial":"S.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":762408,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Alt, Jeffrey C.","contributorId":70213,"corporation":false,"usgs":true,"family":"Alt","given":"Jeffrey","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":762409,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70201356,"text":"70201356 - 2005 - Utility of Viking Orbiter images and products for Mars mapping","interactions":[],"lastModifiedDate":"2018-12-11T10:10:41","indexId":"70201356","displayToPublicDate":"2005-10-01T10:10:16","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Utility of Viking Orbiter images and products for Mars mapping","docAbstract":"<p><span>This paper reports on mapping procedures developed by the U.S. Geological Survey that use Viking Orbiter imagery and Mars Orbiter Laser Altimeter (MOLA) derived radii to produce topographic data. The use of Mosaiced Digital Image Models (MDIMs), created from Viking Orbiter images, and MOLA data to provide horizontal and vertical control is reviewed. We describe procedures to adapt a commercial digital photogrammetric workstation to work with planetary data.</span></p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","doi":"10.14358/PERS.71.10.1187","usgsCitation":"Rosiek, M.R., Kirk, R.L., Archinal, B.A., Howington-Kraus, E., Hare, T.M., Galuszka, D.M., and Redding, B.L., 2005, Utility of Viking Orbiter images and products for Mars mapping: Photogrammetric Engineering and Remote Sensing, v. 10, p. 1187-1195, https://doi.org/10.14358/PERS.71.10.1187.","productDescription":"9 p.","startPage":"1187","endPage":"1195","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":477646,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.14358/pers.71.10.1187","text":"Publisher Index Page"},{"id":360141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10dadee4b034bf6a7fcc53","contributors":{"authors":[{"text":"Rosiek, Mark R. mrosiek@usgs.gov","contributorId":824,"corporation":false,"usgs":true,"family":"Rosiek","given":"Mark","email":"mrosiek@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":753755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirk, Randolph L. 0000-0003-0842-9226 rkirk@usgs.gov","orcid":"https://orcid.org/0000-0003-0842-9226","contributorId":2765,"corporation":false,"usgs":true,"family":"Kirk","given":"Randolph","email":"rkirk@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753756,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Archinal, Brent A. 0000-0002-6654-0742 barchinal@usgs.gov","orcid":"https://orcid.org/0000-0002-6654-0742","contributorId":2816,"corporation":false,"usgs":true,"family":"Archinal","given":"Brent","email":"barchinal@usgs.gov","middleInitial":"A.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753757,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Howington-Kraus, Elpitha 0000-0001-5787-6554 ahowington@usgs.gov","orcid":"https://orcid.org/0000-0001-5787-6554","contributorId":2815,"corporation":false,"usgs":true,"family":"Howington-Kraus","given":"Elpitha","email":"ahowington@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753758,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hare, Trent M. 0000-0001-8842-389X thare@usgs.gov","orcid":"https://orcid.org/0000-0001-8842-389X","contributorId":3188,"corporation":false,"usgs":true,"family":"Hare","given":"Trent","email":"thare@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753759,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Galuszka, Donna M. 0000-0003-1870-1182 dgaluszka@usgs.gov","orcid":"https://orcid.org/0000-0003-1870-1182","contributorId":3186,"corporation":false,"usgs":true,"family":"Galuszka","given":"Donna","email":"dgaluszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753760,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Redding, Bonnie L. 0000-0001-8178-1467 bredding@usgs.gov","orcid":"https://orcid.org/0000-0001-8178-1467","contributorId":4798,"corporation":false,"usgs":true,"family":"Redding","given":"Bonnie","email":"bredding@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":753761,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
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