{"pageNumber":"2543","pageRowStart":"63550","pageSize":"25","recordCount":184657,"records":[{"id":72422,"text":"fs20053051 - 2005 - Estimated use of water in the United States in 2000","interactions":[],"lastModifiedDate":"2012-02-10T00:11:35","indexId":"fs20053051","displayToPublicDate":"2005-10-05T00:00:00","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":"2005-3051","title":"Estimated use of water in the United States in 2000","language":"ENGLISH","doi":"10.3133/fs20053051","usgsCitation":"Lumia, D.S., Linsey, K.S., and Barber, N.L., 2005, Estimated use of water in the United States in 2000: U.S. Geological Survey Fact Sheet 2005-3051, 2 p., https://doi.org/10.3133/fs20053051.","productDescription":"2 p.","costCenters":[],"links":[{"id":120995,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3051.jpg"},{"id":7445,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3051/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -172.33333333333334,18 ], [ -172.33333333333334,71.83333333333333 ], [ -64.83333333333333,71.83333333333333 ], [ -64.83333333333333,18 ], [ -172.33333333333334,18 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc8d","contributors":{"authors":[{"text":"Lumia, Deborah S.","contributorId":19627,"corporation":false,"usgs":true,"family":"Lumia","given":"Deborah","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linsey, Kristin S. 0000-0001-6492-7639 kslinsey@usgs.gov","orcid":"https://orcid.org/0000-0001-6492-7639","contributorId":3678,"corporation":false,"usgs":true,"family":"Linsey","given":"Kristin","email":"kslinsey@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barber, Nancy L. 0000-0002-2952-5017 nlbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-2952-5017","contributorId":3679,"corporation":false,"usgs":true,"family":"Barber","given":"Nancy","email":"nlbarber@usgs.gov","middleInitial":"L.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true},{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285626,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"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":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"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":70174239,"text":"70174239 - 2005 - Napa-Sonoma marshes pond 3, hydrologic and biotic changes in a salt pond following breaching","interactions":[],"lastModifiedDate":"2017-08-26T13:26:56","indexId":"70174239","displayToPublicDate":"2005-10-04T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Napa-Sonoma marshes pond 3, hydrologic and biotic changes in a salt pond following breaching","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 7th biennial State-of-the-Estuary Conference","conferenceTitle":"7th biennial State-of-the-Estuary Conference","conferenceDate":"October 4-6, 2005","conferenceLocation":"Oakland, California","language":"English","usgsCitation":"Athearn, N., Goodenough, K., Takekawa, J.Y., Miles, A., Saiki, M.K., Spring, S., Mejia, F., Shellenbarger, G., and Schoellhamer, D., 2005, Napa-Sonoma marshes pond 3, hydrologic and biotic changes in a salt pond following breaching, in Proceedings of the 7th biennial State-of-the-Estuary Conference, Oakland, California, October 4-6, 2005, 1 p.","productDescription":"1 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":324764,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"577e2bb1e4b0ef4d2f445a31","contributors":{"authors":[{"text":"Athearn, N.D.","contributorId":86958,"corporation":false,"usgs":true,"family":"Athearn","given":"N.D.","affiliations":[],"preferred":false,"id":641605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodenough, K.","contributorId":172693,"corporation":false,"usgs":false,"family":"Goodenough","given":"K.","affiliations":[],"preferred":false,"id":641606,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":641607,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miles, A.K. 0000-0002-3108-808X","orcid":"https://orcid.org/0000-0002-3108-808X","contributorId":85902,"corporation":false,"usgs":true,"family":"Miles","given":"A.K.","affiliations":[],"preferred":false,"id":641608,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Saiki, M. K.","contributorId":28917,"corporation":false,"usgs":true,"family":"Saiki","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":641609,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Spring, S.","contributorId":14328,"corporation":false,"usgs":true,"family":"Spring","given":"S.","email":"","affiliations":[],"preferred":false,"id":641610,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Mejia, F.","contributorId":73011,"corporation":false,"usgs":true,"family":"Mejia","given":"F.","email":"","affiliations":[],"preferred":false,"id":641611,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Shellenbarger, G.G.","contributorId":12678,"corporation":false,"usgs":true,"family":"Shellenbarger","given":"G.G.","affiliations":[],"preferred":false,"id":641612,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schoellhamer, D. H. 0000-0001-9488-7340","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":85624,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"D. 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The U.S. Geological Survey, in cooperation with the Prairie Island Indian Community and the Minnesota Department of Natural Resources, conducted a study of Sturgeon Lake (a backwater lake in Navigation Pool 3 of the Mississippi River) during 2003-04 to describe the physical, chemical, and biological characteristics of the lake. Riparian and shoreline areas surrounding Sturgeon Lake consist primarily of deciduous tree and shrub cover with minimal amounts of commercial or residential land use. Woody debris and aquatic vegetation are the major types of physical habitat suitable for fish and invertebrates. Among 10 bottom-sediment sampling sites, 24 organic wastewater compounds, 1 organochlorine pesticide metabolite (p,p’DDE), and total polychlorinated biphenyls (PCBs) were detected in the bottom sediments of Sturgeon Lake. The most prevalent class of compounds detected were polyaromatic hydrocarbons. Other classes of compounds detected include sterols, disinfectants, plastic components, alkylphenols, and fragrances. Three compounds detected (bisphenol A, benzo[a]pyrene, and triclosan) are considered endocrine disrupting compounds. Twenty-one and 49 invertebrate taxa were identified from 10 bottom-sediment and 6 woody-debris/vegetation samples, respectively. Most of the taxa were Diptera in the family Chironomidae. The most common invertebrate in terms of density in bottom-sediment samples was the burrowing mayfly (Hexagenia sp.). Trichoptera in the families Hydropsychidae or Polycentropodidae were common in most of the woody-debris samples. The presence of the Hexagenia larvae in samples indicates that the bottom sediments are stable and that dissolved oxygen concentrations in the lake do not drop to acute or sub-lethal anoxic conditions. Backwater lakes such as Sturgeon Lake are important areas of habitat for aquatic organisms along the Mississippi River, and this report provides baseline physical, chemical, and biological information that resource managers can compare with future investigations.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055182","collaboration":"Prepared in cooperation with the Prairie Island Indian Community and Minnesota Department of Natural Resources","usgsCitation":"Lee, K., Sanocki, C.A., and Montz, G.R., 2005, Physical, chemical, and biological characteristics of Sturgeon Lake, Goodhue County, Minnesota, 2003-04: U.S. Geological Survey Scientific Investigations Report 2005-5182, vi, 22 p., https://doi.org/10.3133/sir20055182.","productDescription":"vi, 22 p.","numberOfPages":"31","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319750,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055182.JPG"},{"id":7443,"rank":1,"type":{"id":15,"text":"Index 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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 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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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Alaska","interactions":[],"lastModifiedDate":"2025-08-21T16:57:42.729889","indexId":"ofr20051341","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":"2005-1341","title":"Preliminary integrated geologic map databases for the United States: Digital data for the reconnaissance geologic map of the Yukon-Koyukuk basin, Alaska","docAbstract":"

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No abstract available.

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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.

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 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.

The 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.

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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 (http://www.discoverlifeinamerica.org/). 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.

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No abstract available.

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0000-0002-0485-6266 pvalentine@usgs.gov","orcid":"https://orcid.org/0000-0002-0485-6266","contributorId":1947,"corporation":false,"usgs":true,"family":"Valentine","given":"Page","email":"pvalentine@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":285538,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Warner, John C. 0000-0002-3734-8903 jcwarner@usgs.gov","orcid":"https://orcid.org/0000-0002-3734-8903","contributorId":2681,"corporation":false,"usgs":true,"family":"Warner","given":"John C.","email":"jcwarner@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":285542,"contributorType":{"id":1,"text":"Authors"},"rank":16}]}} ,{"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":"

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.

","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 Page"},"url":"https://pubs.usgs.gov/sir/2005/5066/","linkFileType":{"id":5,"text":"html"}},{"id":191842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055066.GIF"}],"country":"United States","state":"Indiana","county":"Dubois, Spencer, Warrick","otherGeospatial":"Lincoln Boyhood National Memorial","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.6823,38.5263],[-86.6821,38.4393],[-86.6815,38.4202],[-86.6814,38.3976],[-86.6814,38.3822],[-86.6814,38.3804],[-86.6814,38.3776],[-86.6807,38.3364],[-86.68,38.3097],[-86.68,38.2938],[-86.6799,38.2784],[-86.6799,38.2634],[-86.6799,38.2485],[-86.7936,38.2492],[-86.7934,38.207],[-86.7933,38.1893],[-86.7968,38.1834],[-86.8033,38.1816],[-86.8026,38.1707],[-86.7997,38.1626],[-86.795,38.1572],[-86.7985,38.1526],[-86.8008,38.1499],[-86.8031,38.1472],[-86.8043,38.1458],[-86.8066,38.1431],[-86.8054,38.1417],[-86.8002,38.1395],[-86.7972,38.1304],[-86.7948,38.125],[-86.7925,38.1168],[-86.7883,38.1055],[-86.7848,38.1041],[-86.7813,38.1014],[-86.7789,38.1019],[-86.7772,38.1042],[-86.7731,38.1055],[-86.7696,38.1015],[-86.7696,38.0956],[-86.7695,38.0906],[-86.7695,38.0865],[-86.7725,38.0838],[-86.7806,38.0783],[-86.7783,38.0756],[-86.7747,38.0702],[-86.7718,38.0634],[-86.7654,38.0584],[-86.7741,38.0543],[-86.7799,38.0534],[-86.7823,38.0484],[-86.7805,38.0461],[-86.7793,38.0439],[-86.7799,38.0402],[-86.7799,38.0375],[-86.7799,38.0362],[-86.7769,38.0316],[-86.7751,38.0244],[-86.7739,38.0103],[-86.7716,37.9999],[-86.7727,37.9981],[-86.7756,37.9981],[-86.785,37.9999],[-86.792,38.0058],[-86.8008,38.0089],[-86.8031,38.0057],[-86.8089,38.0007],[-86.8206,37.9984],[-86.8253,37.9975],[-86.8311,37.9957],[-86.8369,37.993],[-86.8445,37.9902],[-86.8496,37.9888],[-86.8599,37.9849],[-86.8818,37.9678],[-86.8913,37.9584],[-86.9013,37.9485],[-86.9126,37.9409],[-86.9132,37.9407],[-86.9361,37.935],[-86.9446,37.9346],[-86.9562,37.9341],[-86.9627,37.9336],[-86.9672,37.9329],[-86.9791,37.9304],[-86.986,37.929],[-86.9959,37.9249],[-87.0064,37.9203],[-87.0169,37.9162],[-87.0263,37.9109],[-87.0343,37.9048],[-87.0407,37.8998],[-87.0423,37.8978],[-87.0443,37.8947],[-87.046,37.8901],[-87.0443,37.8814],[-87.0428,37.8743],[-87.0438,37.8679],[-87.0462,37.8597],[-87.0552,37.8288],[-87.057,37.8252],[-87.0658,37.8083],[-87.071,37.8014],[-87.0835,37.7917],[-87.0894,37.789],[-87.0974,37.7853],[-87.1062,37.7834],[-87.107,37.7833],[-87.1241,37.7835],[-87.1283,37.7851],[-87.1288,37.7854],[-87.133,37.7874],[-87.1336,37.788],[-87.139,37.7964],[-87.1407,37.8018],[-87.1425,37.8073],[-87.1443,37.8127],[-87.1457,37.8157],[-87.151,37.8247],[-87.1673,37.8387],[-87.1749,37.8406],[-87.1772,37.8411],[-87.1819,37.8416],[-87.2028,37.8433],[-87.2233,37.8487],[-87.225,37.8494],[-87.232,37.8526],[-87.2342,37.8536],[-87.2414,37.8575],[-87.2472,37.8611],[-87.2561,37.8671],[-87.2649,37.8732],[-87.2684,37.8754],[-87.2767,37.8813],[-87.2884,37.8889],[-87.3002,37.8956],[-87.3027,37.8967],[-87.3058,37.8979],[-87.3205,37.9046],[-87.3312,37.9094],[-87.3374,37.9111],[-87.3434,37.9128],[-87.3668,37.9258],[-87.3759,37.9309],[-87.384,37.9349],[-87.3899,37.9375],[-87.3943,37.9392],[-87.4166,37.9442],[-87.4193,37.9443],[-87.4324,37.9445],[-87.446,37.9416],[-87.4512,37.9394],[-87.4501,38.0373],[-87.4729,38.0371],[-87.4711,38.1242],[-87.4676,38.1242],[-87.4676,38.1655],[-87.4663,38.2035],[-87.3557,38.2048],[-87.317,38.2051],[-87.3167,38.2314],[-87.3169,38.2459],[-87.2981,38.246],[-87.2985,38.2319],[-87.073,38.2323],[-87.0723,38.5147],[-87.0693,38.5129],[-87.0657,38.5047],[-87.0616,38.5007],[-87.0545,38.5025],[-87.0463,38.5107],[-87.0352,38.5126],[-87.0251,38.5072],[-87.0199,38.5076],[-87.0128,38.5122],[-87.0069,38.5086],[-87.0022,38.5086],[-86.994,38.5136],[-86.9869,38.5073],[-86.9781,38.5024],[-86.9681,38.5038],[-86.9645,38.5047],[-86.9563,38.5034],[-86.9563,38.4921],[-86.9498,38.4903],[-86.9404,38.4939],[-86.9398,38.5012],[-86.9358,38.5048],[-86.924,38.5048],[-86.9228,38.4999],[-86.9145,38.4958],[-86.9081,38.4999],[-86.9004,38.5013],[-86.8916,38.4954],[-86.8804,38.4946],[-86.8775,38.4959],[-86.8763,38.5014],[-86.8711,38.5055],[-86.8558,38.5091],[-86.8446,38.5146],[-86.8358,38.5228],[-86.8376,38.526],[-86.8247,38.526],[-86.8106,38.526],[-86.7941,38.5261],[-86.6823,38.5263]]]},\"properties\":{\"name\":\"Dubois\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624c5b","contributors":{"authors":[{"text":"Buszka, Paul M. 0000-0001-8218-826X pmbuszka@usgs.gov","orcid":"https://orcid.org/0000-0001-8218-826X","contributorId":1786,"corporation":false,"usgs":true,"family":"Buszka","given":"Paul","email":"pmbuszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fowler, Kathleen K. 0000-0002-0107-3848 kkfowler@usgs.gov","orcid":"https://orcid.org/0000-0002-0107-3848","contributorId":2439,"corporation":false,"usgs":true,"family":"Fowler","given":"Kathleen","email":"kkfowler@usgs.gov","middleInitial":"K.","affiliations":[{"id":27231,"text":"Indiana-Kentucky Water Science Center","active":true,"usgs":true},{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":"

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.

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.

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.

","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":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":"

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.

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.

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.

","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":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":241,"text":"Eastern 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":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":"

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 137Cs 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 at low flow 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 Al2O3, 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.

","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":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":"

No abstract available.

","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":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","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":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":"

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.

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.

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?

","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":72380,"text":"ofr20041300 - 2005 - Mineral Commodity Profile: Indium","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"ofr20041300","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":"2004-1300","title":"Mineral Commodity Profile: Indium","language":"ENGLISH","doi":"10.3133/ofr20041300","usgsCitation":"Jorgenson, J.D., and George, M.W., 2005, Mineral Commodity Profile: Indium (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2004-1300, 24 p., https://doi.org/10.3133/ofr20041300.","productDescription":"24 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7340,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1300/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6356e3","contributors":{"authors":[{"text":"Jorgenson, John D.","contributorId":74087,"corporation":false,"usgs":true,"family":"Jorgenson","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, Micheal W. mgeorge@usgs.gov","contributorId":3128,"corporation":false,"usgs":true,"family":"George","given":"Micheal","email":"mgeorge@usgs.gov","middleInitial":"W.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":285530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":72378,"text":"ofr02303 - 2005 - Mineral commodity profiles — Gold","interactions":[],"lastModifiedDate":"2022-07-22T19:29:51.944859","indexId":"ofr02303","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":"2002-303","title":"Mineral commodity profiles — Gold","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02303","usgsCitation":"Butterman, W., and Amey, E.B., 2005, Mineral commodity profiles — Gold (Version 1.0): U.S. Geological Survey Open-File Report 2002-303, vi, 66 p., https://doi.org/10.3133/ofr02303.","productDescription":"vi, 66 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":192925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404384,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73807.htm","linkFileType":{"id":5,"text":"html"}},{"id":7338,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-303/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6356f4","contributors":{"authors":[{"text":"Butterman, W. 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No abstract available.

","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing (ASPRS)","usgsCitation":"Kirk, R.L., 2005, Mars: Photogrammetric Engineering and Remote Sensing, v. 71, no. 10, p. 1111-1114.","productDescription":"4 p.","startPage":"1111","endPage":"1114","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":360533,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.asprs.org/asprs-publications/grids-and-datums"},{"id":360535,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"71","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c1a1535e4b0708288c23548","contributors":{"authors":[{"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":754646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206530,"text":"70206530 - 2005 - Interpreting the results from multiple regression and structural equation models","interactions":[],"lastModifiedDate":"2019-11-07T16:52:21","indexId":"70206530","displayToPublicDate":"2005-10-01T16:49:25","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1121,"text":"Bulletin of the Ecological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Interpreting the results from multiple regression and structural equation models","docAbstract":"

No abstract available.

","language":"English","publisher":"Ecological Society of America","doi":"10.1890/0012-9623(2005)86[283:ITRFMR]2.0.CO;2","usgsCitation":"Grace, J.B., and Bollen, K.A., 2005, Interpreting the results from multiple regression and structural equation models: Bulletin of the Ecological Society of America, v. 86, no. 4, p. 283-295, https://doi.org/10.1890/0012-9623(2005)86[283:ITRFMR]2.0.CO;2.","productDescription":"13 p.","startPage":"283","endPage":"295","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":369070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"86","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grace, James B. 0000-0001-6374-4726 gracej@usgs.gov","orcid":"https://orcid.org/0000-0001-6374-4726","contributorId":884,"corporation":false,"usgs":true,"family":"Grace","given":"James","email":"gracej@usgs.gov","middleInitial":"B.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":774895,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bollen, Kenneth A.","contributorId":93989,"corporation":false,"usgs":true,"family":"Bollen","given":"Kenneth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":774896,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":"

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.

","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":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources 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}]}} ]}