No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0270","usgsCitation":"Hudson, T.L., and Millholland, M., 2002, Alaska resource data file: Russian Mission quadrangle: U.S. Geological Survey Open-File Report 2002-70, 74 p., https://doi.org/10.3133/ofr0270.","productDescription":"74 p.","costCenters":[],"links":[{"id":493055,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0070/ofr0270.pdf","text":"Report","size":"374 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":160793,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":389312,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_50926.htm"},{"id":2858,"rank":3,"type":{"id":18,"text":"Project Site"},"url":"https://doi.org/10.5066/P96MMRFD","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Russian Mission quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -162,\n 62\n ],\n [\n -159,\n 62\n ],\n [\n -159,\n 61\n ],\n [\n -162,\n 61\n ],\n [\n -162,\n 62\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688e93","contributors":{"authors":[{"text":"Hudson, T. L.","contributorId":13992,"corporation":false,"usgs":true,"family":"Hudson","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":206481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Millholland, M.A.","contributorId":70811,"corporation":false,"usgs":true,"family":"Millholland","given":"M.A.","affiliations":[],"preferred":false,"id":206482,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31587,"text":"ofr0262 - 2002 - Fate of carbon in Alaskan Landscapes Project: Database for soils from eddy covariance tower sites, Delta Junction, AK","interactions":[],"lastModifiedDate":"2022-12-20T23:12:09.952278","indexId":"ofr0262","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-62","title":"Fate of carbon in Alaskan Landscapes Project: Database for soils from eddy covariance tower sites, Delta Junction, AK","docAbstract":"Soils in Alaska, and in high latitude terrestrial ecosystems in general, contain significant amounts of organic carbon, most of which is believed to have accumulated since the start of the Holocene about 10 ky before present. High latitude soils are estimated to contain 30-40% of terrestrial soil carbon (Melillo et al., 1995; McGuire and Hobbie, 1997), or ~ 300-400 Gt C (Gt = 1015 g), which equals about half of the current atmospheric burden of carbon. Boreal forests in particular are estimated to have more soil carbon than any other terrestrial biome (Post et al., 1982; Chapin and Matthews, 1993). The relations among net primary production, soil carbon storage, recurrent fire disturbance, nutrients, the hydrologic cycle, permafrost and geomorphology are poorly understood in boreal forest. Fire disturbance has been suggested to play a key role in the interactions among the complex biogeochemical processes influencing carbon storage in boreal forest soils (Harden et al., 2000; Zhuang et al., 2002). There has been an observed increase in fire disturbance in North American boreal black spruce (Picea mariana) forests in recent decades (Murphy et al., 1999; Kasichke et al., 2000), concurrent with increases in Alaskan boreal and arctic surface temperatures and warming of permafrost (Osterkamp and Romanofsky, 1999). Understanding the role of fire in long term carbon storage and how recent changes in fire frequency and severity may influence future high latitude soil carbon pools is necessary for those working to understand or mitigate the effects of global climate change.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0262","usgsCitation":"King, S., Harden, J., Manies, K.L., Munster, J., and White, L.D., 2002, Fate of carbon in Alaskan Landscapes Project: Database for soils from eddy covariance tower sites, Delta Junction, AK: U.S. Geological Survey Open-File Report 2002-62, Report: ii, 18 p.; 5 Tables, https://doi.org/10.3133/ofr0262.","productDescription":"Report: ii, 18 p.; 5 Tables","numberOfPages":"20","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":160592,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0262.jpg"},{"id":410832,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49805.htm","linkFileType":{"id":5,"text":"html"}},{"id":283403,"rank":1,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/2002/0062/Delta_Tower_Transects.xls","text":"Delta Tower Transects"},{"id":283399,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/2002/0062/pdf/Delta_Tower_Sites.pdf","text":"Delta Tower Sites"},{"id":283401,"rank":2,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/2002/0062/Delta_Tower_Physical.xls","text":"Delta Tower Physical"},{"id":283400,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/2002/0062/Delta_Tower_Field.xls","text":"Delta Tower Field"},{"id":283402,"rank":1,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/2002/0062/Delta_Tower_Chemistry.xls","text":"Delta Tower Chemistry"},{"id":2824,"rank":11,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0062/","linkFileType":{"id":5,"text":"html"}},{"id":283398,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0062/pdf/of02-62.pdf"}],"country":"United States","state":"Alaska","city":"Delta Junction","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -145.8,\n 63.825\n ],\n [\n -145.8,\n 64.0722\n ],\n [\n -145.2,\n 64.0722\n ],\n [\n -145.2,\n 63.825\n ],\n [\n -145.8,\n 63.825\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f7386","contributors":{"authors":[{"text":"King, Stagg","contributorId":79394,"corporation":false,"usgs":true,"family":"King","given":"Stagg","email":"","affiliations":[],"preferred":false,"id":206474,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harden, Jennifer","contributorId":46190,"corporation":false,"usgs":true,"family":"Harden","given":"Jennifer","affiliations":[],"preferred":false,"id":206472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manies, Kristen L. 0000-0003-4941-9657 kmanies@usgs.gov","orcid":"https://orcid.org/0000-0003-4941-9657","contributorId":2136,"corporation":false,"usgs":true,"family":"Manies","given":"Kristen","email":"kmanies@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":206471,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Munster, Jennie","contributorId":107364,"corporation":false,"usgs":true,"family":"Munster","given":"Jennie","email":"","affiliations":[],"preferred":false,"id":206475,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"White, L. Douglas","contributorId":72296,"corporation":false,"usgs":true,"family":"White","given":"L.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":206473,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":31583,"text":"ofr0254 - 2002 - Alaska resource data file: Nulato quadrangle","interactions":[],"lastModifiedDate":"2025-07-28T20:02:29.838903","indexId":"ofr0254","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-54","title":"Alaska resource data file: Nulato quadrangle","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0254","usgsCitation":"Dashevsky, S., 2002, Alaska resource data file: Nulato quadrangle: U.S. Geological Survey Open-File Report 2002-54, 64 p., https://doi.org/10.3133/ofr0254.","productDescription":"64 p.","costCenters":[],"links":[{"id":160588,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2820,"rank":4,"type":{"id":18,"text":"Project Site"},"url":"https://doi.org/10.5066/P96MMRFD","linkFileType":{"id":5,"text":"html"}},{"id":389280,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_50925.htm"},{"id":493047,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0054/ofr0254.pdf","text":"Report","size":"318 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Nulato quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156,\n 65\n ],\n [\n -159,\n 65\n ],\n [\n -159,\n 64\n ],\n [\n -156,\n 64\n ],\n [\n -156,\n 65\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6834c8","contributors":{"authors":[{"text":"Dashevsky, S.S.","contributorId":81955,"corporation":false,"usgs":true,"family":"Dashevsky","given":"S.S.","affiliations":[],"preferred":false,"id":206453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31578,"text":"ofr0230 - 2002 - Surface-water quality-assurance plan for the Wisconsin district of the U. S. Geological Survey, Water Resources Division","interactions":[],"lastModifiedDate":"2015-10-14T13:39:39","indexId":"ofr0230","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-30","title":"Surface-water quality-assurance plan for the Wisconsin district of the U. S. Geological Survey, Water Resources Division","docAbstract":"This surface-water quality-assurance plan documents the standards, policies, and procedures used by the Wisconsin District of the U.S. Geological Survey, Water Resources Division, for activities related to the collection, processing, storage, analysis, management, and publication of surface-water data. The roles and responsibilities of District personnel in following these policies and procedures including those related to safety and training are presented.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0230","usgsCitation":"Garn, H., 2002, Surface-water quality-assurance plan for the Wisconsin district of the U. S. Geological Survey, Water Resources Division: U.S. Geological Survey Open-File Report 2002-30, iv, 52 p., https://doi.org/10.3133/ofr0230.","productDescription":"iv, 52 p.","numberOfPages":"56","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":161420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0030/report-thumb.jpg"},{"id":59809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68ad7c","contributors":{"authors":[{"text":"Garn, H.S.","contributorId":42601,"corporation":false,"usgs":true,"family":"Garn","given":"H.S.","affiliations":[],"preferred":false,"id":206441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31577,"text":"ofr0229 - 2002 - Historical trends in U.S. mineral statistics for selected non-ferrous metals","interactions":[],"lastModifiedDate":"2023-06-27T15:25:03.56907","indexId":"ofr0229","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-29","title":"Historical trends in U.S. mineral statistics for selected non-ferrous metals","docAbstract":"Production figures for selected nonferrous metals-aluminum (including bauxite and alumina), copper, lead, tin, titanium, and zinc-by the United States, as well as other statistics for these commodities, show strong volatility during 20th century. Major shifts were driven by the Great Depression and the two World Wars, but other major temporal changes are also noted that are not directly related to such global crises. For example, the price of tin exhibited a strong maximum in the 1980's, which is unrelated to world production, but rather to failed efforts of the International Tin Council to control price. In the case of copper, U.S. exports have varied throughout the second half of the century, by more than a factor of 5. Such volatility might be explained in part by global economic conditions, at least throughout recent decades. Supporting the interpretation of the importance of foreign pressure on the domestic commodities market is a close correlation between domestic consumption of antimony and its elevated price in the mid 1980's,possibly pushed up mostly by the world dominance in production of this commodity by China. However, only very superficial explanations can be advanced for such relations before we have examined, in concert, information for a much larger suite of commodities.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0229","usgsCitation":"Piper, D.Z., and Nokleberg, W.J., 2002, Historical trends in U.S. mineral statistics for selected non-ferrous metals: U.S. Geological Survey Open-File Report 2002-29, 41 p., https://doi.org/10.3133/ofr0229.","productDescription":"41 p.","numberOfPages":"41","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":283395,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0029/figsandtabs.htm"},{"id":59808,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0029/pdf/of02-29.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2816,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0029/","linkFileType":{"id":5,"text":"html"}},{"id":161148,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0029/report-thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -66.95,71.833333 ], [ -66.95,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c100","contributors":{"authors":[{"text":"Piper, David Z. dzpiper@usgs.gov","contributorId":2452,"corporation":false,"usgs":true,"family":"Piper","given":"David","email":"dzpiper@usgs.gov","middleInitial":"Z.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":206440,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":206439,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31576,"text":"ofr0228 - 2002 - Arsenic in rocks and stream sediments of the central Appalachian Basin, Kentucky","interactions":[],"lastModifiedDate":"2017-03-07T11:36:23","indexId":"ofr0228","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-28","title":"Arsenic in rocks and stream sediments of the central Appalachian Basin, Kentucky","docAbstract":"Arsenic (As) enrichment in coal and stream sediments has been documented in the southern Appalachian basin (see Goldhaber and others, submitted) and is attributed to interaction of rocks and coal with metamorphic fluids generated during the Allegheny Orogeny (late Paleozoic). Similarly derived fluids are expected to affect the coal and in the Kentucky Appalachian Basin to the north as well. In addition, similar processes may have influenced the Devonian oil shale on the western margin of the basin. The major goals of this study are to determine the effect such fluids had on rocks in the Kentucky Appalachian basin (fig. 1), and to understand the geochemical processes that control trace-metal source, residence, and mobility within the basin. This report includes data presented in a poster at the USGS workshop on arsenic (February 21 and 22, 2001), new NURE stream sediment data3 , and field data from a trip in April 2001. Although data for major and minor elements and all detectable trace metals are reported in the Appendices, the narrative of this report primarily focuses on arsenic.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0228","usgsCitation":"Tuttle, M.L., Goldhaber, M.B., Ruppert, L.F., and Hower, J., 2002, Arsenic in rocks and stream sediments of the central Appalachian Basin, Kentucky: U.S. Geological Survey Open-File Report 2002-28, 166 p., https://doi.org/10.3133/ofr0228.","productDescription":"166 p.","costCenters":[],"links":[{"id":161147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2815,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0028/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672d08","contributors":{"authors":[{"text":"Tuttle, Michele L.W. mtuttle@usgs.gov","contributorId":47839,"corporation":false,"usgs":true,"family":"Tuttle","given":"Michele","email":"mtuttle@usgs.gov","middleInitial":"L.W.","affiliations":[],"preferred":false,"id":206438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":206436,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruppert, Leslie F. 0000-0002-7453-1061 lruppert@usgs.gov","orcid":"https://orcid.org/0000-0002-7453-1061","contributorId":660,"corporation":false,"usgs":true,"family":"Ruppert","given":"Leslie","email":"lruppert@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":206435,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hower, James C. 0000-0003-4694-2776","orcid":"https://orcid.org/0000-0003-4694-2776","contributorId":34561,"corporation":false,"usgs":false,"family":"Hower","given":"James C.","affiliations":[{"id":16123,"text":"University of Kentucky, Center for Applied Energy Research, 2540 Research Park Drive, Lexington, KY 40511, United States.","active":true,"usgs":false}],"preferred":false,"id":206437,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":31574,"text":"ofr0221 - 2002 - Geologic map of the Corona South 7.5' quadrangle, Riverside and Orange counties, California","interactions":[],"lastModifiedDate":"2023-06-27T16:02:03.558786","indexId":"ofr0221","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-21","title":"Geologic map of the Corona South 7.5' quadrangle, Riverside and Orange counties, California","docAbstract":"Open-File Report 01-021 contains a digital geologic map database of the Corona South 7.5’ quadrangle, Riverside County, California that includes:
\n1. ARC/INFO (Environmental Systems Research Institute, http://www.esri.com) version 7.2.1 coverages of the various elements of the geologic map.
\n2. A Postscript file to plot the geologic map on a topographic base, and containing a Correlation of Map Units diagram (CMU), a Description of Map Units (DMU), and an index map.
\n3. Portable Document Format (.pdf) files of:
\na. A Readme file; includes in Appendix I, data contained in crs_met.txt
\n\nb. The same graphic as plotted in 2 above. Test plots have not produced 1:24,000-scale map sheets. Adobe Acrobat page size setting influences map scale.
The Correlation of Map Units and Description of Map Units is in the editorial format of USGS Geologic Investigations Series (I-series) maps but has not been edited to comply with I-map standards. Within the geologic map data package, map units are identified by standard geologic map criteria such as formation-name, age, and lithology. Where known, grain size is indicated on the map by a subscripted letter or letters following the unit symbols as follows: lg, large boulders; b, boulder; g, gravel; a, arenaceous; s, silt; c, clay; e.g. Qyfa is a predominantly young alluvial fan deposit that is arenaceous. Multiple letters are used for more specific identification or for mixed units, e.g., Qfysa is a silty sand. In some cases, mixed units are indicated by a compound symbol; e.g., Qyf2sc. Marine deposits are in part overlain by local, mostly alluvial fan, deposits and are labeled Qomf. Grain size follows f.
\nEven though this is an Open-File Report and includes the standard USGS Open-File disclaimer, the report closely adheres to the stratigraphic nomenclature of the U.S. Geological Survey. Descriptions of units can be obtained by viewing or plotting the .pdf file (3b above) or plotting the postscript file (2 above).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0221","collaboration":"Prepared in cooperation with California Division of Mines and Geology","usgsCitation":"Gray, C.H., Morton, D.M., Weber, F.H., Bovard, K.R., and O'Brien, T., 2002, Geologic map of the Corona South 7.5' quadrangle, Riverside and Orange counties, California: U.S. Geological Survey Open-File Report 2002-21, Map: 52.0 x 34.0 inches; Readme: PDF, 19 p.; Readme: TXT; Metadata; Database, https://doi.org/10.3133/ofr0221.","productDescription":"Map: 52.0 x 34.0 inches; Readme: PDF, 19 p.; Readme: TXT; Metadata; Database","numberOfPages":"19","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":161145,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0221.jpg"},{"id":2813,"rank":9,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0021/","linkFileType":{"id":5,"text":"html"}},{"id":283388,"rank":8,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0021/pdf/README.pdf"},{"id":283389,"rank":7,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2002/0021/README.txt"},{"id":283390,"rank":5,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2002/0021/crs_met.txt"},{"id":283391,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0021/crs.tar.gz"},{"id":283392,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0021/symbols.tar.gz"},{"id":283393,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2002/0021/pdf/crs_map.pdf","text":"Plate 1"},{"id":283394,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0021/crs_map.ps.gz"}],"scale":"24000","projection":"Polyconic projection","country":"United States","state":"California","county":"Orange County, Riverside County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.625,33.75 ], [ -117.625,33.875 ], [ -117.5,33.875 ], [ -117.5,33.75 ], [ -117.625,33.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a141","contributors":{"authors":[{"text":"Gray, C. H. Jr.","contributorId":8901,"corporation":false,"usgs":true,"family":"Gray","given":"C.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":206427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":206426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weber, F. Harold Jr.","contributorId":10466,"corporation":false,"usgs":true,"family":"Weber","given":"F.","suffix":"Jr.","email":"","middleInitial":"Harold","affiliations":[],"preferred":false,"id":206428,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bovard, Kelly R.","contributorId":49009,"corporation":false,"usgs":true,"family":"Bovard","given":"Kelly","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":206430,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"O'Brien, Timothy","contributorId":47838,"corporation":false,"usgs":true,"family":"O'Brien","given":"Timothy","affiliations":[],"preferred":false,"id":206429,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":31005,"text":"wri20014186 - 2002 - Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory--Determination of wastewater compounds by polystyrene-divinylbenzene solid-phase extraction and capillary-column gas chromatography/mass spectrometry","interactions":[],"lastModifiedDate":"2020-02-19T19:39:06","indexId":"wri20014186","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4186","displayTitle":"Methods of Analysis by the U.S. Geological Survey National Water Quality Laboratory - Determination of Wastewater Compounds by Polystyrene-Divinylbenzene Solid-Phase Extraction and Capillary-Column Gas Chromatography/Mass Spectrometry","title":"Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory--Determination of wastewater compounds by polystyrene-divinylbenzene solid-phase extraction and capillary-column gas chromatography/mass spectrometry","docAbstract":"A method for the determination of 67 compounds typically found in domestic and industrial wastewater is described. The method was developed in response to increasing concern over the impact of endocrine-disrupting chemicals in wastewater on aquatic organisms. This method also may be useful for evaluating the impact of combined sanitary and storm-sewer overflow on the water quality of urban streams. The method focuses on the determination of compounds that are an indicator of wastewater or that have been chosen on the basis of their endocrine-disrupting potential or toxicity. These compounds include the alkylphenol ethoxylate nonionic surfactants and their degradates, food additives, fragrances, antioxidants, flame retardants, plasticizers, industrial solvents, disinfectants, fecal sterols, polycyclicaromatic hydrocarbons, and high-use domestic pesticides.\r\n\r\nWater samples are filtered to remove suspended particulate matter and then are extracted by vacuum through disposable solid-phase cartridges that contain polystyrene-divinylbenzene resin. Cartridges are dried with nitrogen gas, and then sorbed compounds are eluted with dichloromethane-diethyl ether (4:1) and determined by capillary-column gas chromatography/mass spectrometry. Recoveries in reagent-water samples fortified at 4 micrograms per liter averaged 74 percent ? 7 percent relative standard deviation for all method compounds. Initial method detection limits for single-component compounds (excluding hormones and sterols) averaged 0.15 microgram per liter. Samples are preserved by filtration, the addition of 60 grams NaCl, and storage at 4 degrees Celsius. The laboratory has established a sample-holding time (prior to sample extraction) of 14 days from the date of sample collection until a statistically accepted method can be used to determine the effectiveness of these sample-preservation procedures.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri20014186","usgsCitation":"Zaugg, S.D., Smith, S.G., Schroeder, M.P., Barber, L.B., and Burkhardt, M.R., 2002, Methods of analysis by the U.S. Geological Survey National Water Quality Laboratory--Determination of wastewater compounds by polystyrene-divinylbenzene solid-phase extraction and capillary-column gas chromatography/mass spectrometry (Version 1.1, Revised 2007): U.S. Geological Survey Water-Resources Investigations Report 2001-4186, vii, 37 p. , https://doi.org/10.3133/wri20014186.","productDescription":"vii, 37 p. ","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":159876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":10343,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri014186/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.1, Revised 2007","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62bb11","contributors":{"authors":[{"text":"Zaugg, Steven D. sdzaugg@usgs.gov","contributorId":768,"corporation":false,"usgs":true,"family":"Zaugg","given":"Steven","email":"sdzaugg@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":204563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Steven G. sgsmith@usgs.gov","contributorId":1560,"corporation":false,"usgs":true,"family":"Smith","given":"Steven","email":"sgsmith@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":204565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schroeder, Michael P.","contributorId":103303,"corporation":false,"usgs":true,"family":"Schroeder","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":204567,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barber, Larry B. 0000-0002-0561-0831 lbbarber@usgs.gov","orcid":"https://orcid.org/0000-0002-0561-0831","contributorId":921,"corporation":false,"usgs":true,"family":"Barber","given":"Larry","email":"lbbarber@usgs.gov","middleInitial":"B.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":204564,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burkhardt, Mark R.","contributorId":27872,"corporation":false,"usgs":true,"family":"Burkhardt","given":"Mark","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":204566,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":31589,"text":"ofr0267 - 2002 - GRA prospectus; optimizing protected areas for conservation, September 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:09:07","indexId":"ofr0267","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-67","title":"GRA prospectus; optimizing protected areas for conservation, September 2001","language":"ENGLISH","doi":"10.3133/ofr0267","usgsCitation":"Halsing, D., and Bernknopf, R., 2002, GRA prospectus; optimizing protected areas for conservation, September 2001: U.S. Geological Survey Open-File Report 2002-67, 11 p., https://doi.org/10.3133/ofr0267.","productDescription":"11 p.","costCenters":[],"links":[{"id":160792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2857,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-067/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1564","contributors":{"authors":[{"text":"Halsing, David","contributorId":75587,"corporation":false,"usgs":true,"family":"Halsing","given":"David","affiliations":[],"preferred":false,"id":206480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernknopf, Richard","contributorId":51701,"corporation":false,"usgs":true,"family":"Bernknopf","given":"Richard","affiliations":[],"preferred":false,"id":206479,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31010,"text":"wri014257 - 2002 - Characteristics of shallow deposits beneath Rillito Creek, Pima County, Arizona","interactions":[],"lastModifiedDate":"2014-06-12T09:26:17","indexId":"wri014257","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4257","title":"Characteristics of shallow deposits beneath Rillito Creek, Pima County, Arizona","docAbstract":"Characteristics of the stream-channel and basin-fill deposits beneath a 12-mile reach of Rillito Creek, Pima County, Arizona, were obtained to describe the geohydrologic system. The findings presented here are part of a larger project to improve the understanding of recharge processes beneath ephemeral streams.
\nThe stream-channel deposits, which range in thickness from 15 to 40 feet, generally are sandy gravels or gravelly sands. On average, the stream-channel deposits are 44 percent gravel, 51 percent sand, 2 percent silt, and 3 percent clay. The underlying basin-fill deposits also are sandy gravels or gravelly sands but have, on average, a larger component of silt and clay than the stream-channel deposits?about 9 percent silt and 6 percent clay.
\nPorosity values for the stream-channel and basin-fill deposits are similar: about 31 and 34 percent on average, respectively. Volumetric moisture content and percent saturation, however, generally were lower in the stream-channel deposits than in the basin-fill deposits. Moisture content in the stream-channel deposits ranged from 2 to 40 percent and averaged about 18 percent, whereas moisture content in the basin-fill deposits ranged from 7 to 47 percent and averaged about 24 percent. Saturation in the stream-channel deposits ranged from 9 to 100 percent and averaged about 58 percent; saturation in the basin-fill deposits ranged from 30 to 100 percent and averaged about 69 percent. Porosity and moisture content correlate with silt and clay content. Cumulative thickness of water in the 100- to 125-foot thick unsaturated zone obtained by integrating the moisture content over depth, ranged from 17.2 to 40.4 feet.
\nMatric potential for saturation levels at the time of sample collection generally was less than -1 bar for deposits that were less than 35 percent saturated. Matric potential generally was greater than -0.1 bar for deposits that were more than 65 percent saturated. Moisture-retention curves are a function of the physical properties, such as porosity and grain size, of the sediments. The shapes and van Genuchten fitting parameters of moisture-retention curves for the stream-channel deposits are different from those of the basin-fill deposits. For instance, the fitting parameter, a, for stream-channel deposits ranged from 4.56 to 1,220 bar-1 and averaged 220 bar-1, whereas a for basin-fill deposits ranged from 4.22 to 67.9 bar-1 and averaged 22.8 bar-1. The residual water content for the basin-fill deposits is greater than that for the stream-channel deposits. Relative hydraulic conductivity of the stream-channel deposits is less than relative hydraulic conductivity of the basin-fill deposits at the same matric potential. Unsaturated hydraulic conductivity for moisture conditions that existed at the time of sample collection typically was more than two orders of magnitude less than saturated hydraulic conductivity.
\nSaturated vertical hydraulic conductivity of the stream-channel deposits is about an order of magnitude greater than that of the basin-fill deposits. The equivalent hydraulic conductivity of stream-channel deposits ranges from 2 to 7.3 feet per day, and averages about 4 feet per day, whereas the equivalent hydraulic conductivity of the basin-fill deposits ranges from 0.06 to 1.5 feet per day and averages 0.61 foot per day. The equivalent vertical hydraulic conductivity of the entire unsaturated zone cored is 0.75 foot per day. Assuming no vertical to horizontal anisotropy, the equivalent horizontal hydraulic conductivity generally is about two to three times that of the equivalent vertical hydraulic conductivity. The difference between average equivalent vertical and horizontal hydraulic conductivity values results from the differences in methods used to calculate the respective values.
\nElectrical methods were useful in\ndiscriminating between stream-channel deposits\nand basin-fill deposits. In general, electrical\nconductivity of the stream-channel deposits was\nless than 30 millimhos per meter and averaged\n27 millimhos per meter. The conductivity of the\nbasin-fill deposits was greater than that of the\nstream-channel deposits and averaged\n44 millimhos per meter. The greater conductivity\nprobably is related to factors such as greater\nmoisture content and fraction of fine sediments in\nthe basin-fill deposits. Apparent resistivity\nmeasured with two-dimensional resistivity\nsoundings generally decreased with depth.\nThe resistivity values from the near-surface\nmeasurements represent dry stream-channel\ndeposits and averaged 303 ohm meters. The\nresistivity values for basin-fill deposits generally\nwere less than 140 ohm meters and less than\n100 ohm meters when saturated.
\nSeismic-velocity values for the recent alluvium\n(stream-channel and terrace deposits) ranged from\n1,150 to 2,200 feet per second, whereas values for\nbasin-fill deposits ranged from 2,000 to\n11,650 feet per second. The average seismic\nvelocity for the stream-channel deposits\n(1,300 feet per second) was less than that for the\nterrace deposits (1,600 feet per second). Saturated\nbasin-fill deposits had an average velocity of\n7,800 feet per second, whereas unsaturated basin-fill\ndeposits had an average velocity of\n2,750 feet per second.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tucson, AZ","doi":"10.3133/wri014257","collaboration":"Prepared in cooperation with the Arizona Department of Water Resources","usgsCitation":"Hoffmann, J.P., Ripich, M.A., and Ellett, K.M., 2002, Characteristics of shallow deposits beneath Rillito Creek, Pima County, Arizona: U.S. Geological Survey Water-Resources Investigations Report 2001-4257, vii, 42 p., https://doi.org/10.3133/wri014257.","productDescription":"vii, 42 p.","numberOfPages":"53","costCenters":[],"links":[{"id":288434,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288433,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2001/4257/report.pdf"}],"scale":"100000","projection":"Universal Transverse Mercator projection","country":"United States","state":"Arizona","county":"Pima County","otherGeospatial":"Rillito Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.125,32.25 ], [ -111.125,32.333333 ], [ -110.875,32.333333 ], [ -110.875,32.25 ], [ -111.125,32.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545cfc","contributors":{"authors":[{"text":"Hoffmann, John P. jphoffma@usgs.gov","contributorId":1337,"corporation":false,"usgs":true,"family":"Hoffmann","given":"John","email":"jphoffma@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":204578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ripich, Marcella A.","contributorId":73651,"corporation":false,"usgs":true,"family":"Ripich","given":"Marcella","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ellett, Kevin M.","contributorId":68359,"corporation":false,"usgs":true,"family":"Ellett","given":"Kevin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":204579,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31009,"text":"wri014252 - 2002 - Simulation of ground-water flow and potential contaminant transport at Area 6 Landfill, Naval Air Station Whidbey Island, Island County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:09:01","indexId":"wri014252","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2001-4252","title":"Simulation of ground-water flow and potential contaminant transport at Area 6 Landfill, Naval Air Station Whidbey Island, Island County, Washington","docAbstract":"A three-dimensional finite-difference steady-state ground-water flow model was developed to simulate hydraulic conditions at the Area 6 Landfill, Naval Air Station Whidbey Island, near Oak Harbor, Washington. Remediation efforts were started in 1995 in an attempt to contain trichloroethene and other contaminants in the ground water. The model was developed as a tool to test the effectiveness of the pump-and-treat remediation efforts as well as alternative remediation strategies. The model utilized stratigraphic data from approximately 76 Navy and 19 private wells to define the geometry of the shallow, intermediate, and deep aquifers and the intervening confining layers. Initial aquifer parameters and recharge estimates from aquifer tests and published remedial investigation reports were used in the model and then adjusted until simulated water levels closely matched observed water-level data collected prior to the onset of remediation in 1995. The calibrated model was then modified to depict the remedial pump-and-treat system, in which contaminated ground water is extracted, treated, and returned to the ground surface for infiltration. The water levels simulated by the modified model were compared with observed water levels for the 1998 calendar year, during which time the pump-and-treat system was in nearly continuous operation and the ground-water system had equilibrated to steady-state conditions. Although artificial boundaries were used in the model, the choice of model boundary conditions was simulation in the area of primary concern surrounding the western contaminant plume and extraction wells. Particle tracking results indicate that the model can effectively simulate the advective transport of contaminants from the source area to the pumping wells and thus be used to test alternative remedial pumping strategies.","language":"ENGLISH","doi":"10.3133/wri014252","usgsCitation":"Simonds, F.W., 2002, Simulation of ground-water flow and potential contaminant transport at Area 6 Landfill, Naval Air Station Whidbey Island, Island County, Washington: U.S. Geological Survey Water-Resources Investigations Report 2001-4252, 52 p. , https://doi.org/10.3133/wri014252.","productDescription":"52 p. ","costCenters":[],"links":[{"id":159887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3009,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/wri014252/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2b8c","contributors":{"authors":[{"text":"Simonds, F. William","contributorId":61868,"corporation":false,"usgs":true,"family":"Simonds","given":"F.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":204577,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31585,"text":"ofr0259 - 2002 - The road to flamingo: An evaluation of flow pattern alterations and salinity intrusion in the lower glades, Everglades National Park","interactions":[],"lastModifiedDate":"2025-04-18T15:38:16.61772","indexId":"ofr0259","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-59","title":"The road to flamingo: An evaluation of flow pattern alterations and salinity intrusion in the lower glades, Everglades National Park","docAbstract":"This report describes the history of roads through the Lower Glades of Everglades National Park, Florida and their influence on salinity intrusion. The chronology that lead to this work is interesting. The U.S. Geological Survey flew a series of helicopter electromagnetic surveys over portions of Everglades National Park to map saltwater intrusion starting in 1994 (Fitterman et al., 1995; Fitterman, 1996; Fitterman and Deszcz-Pan, 1998, 2002). These surveys identified variations in the electrical resistivity that were associated with changes in ground-water quality. The patterns of ground-water quality have been traced to natural saltwater intrusion, such as the effect of tidal rivers on lowering hydrologic heads far inland, and the influence of man-made structures, such as canals and roadways on surface water flow. These latter effects are of interest as they represent variations from the natural state of affairs in the park.
Previous investigations had been done by Everglades National Park staff on the influence of some roads and canals on the near surface hydrology. This information was scattered through a number of National Park Service publications. In an effort to bring these materials together in an easily located reference, along with new data on flows through culverts beneath the main park road, this report was written.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0259","usgsCitation":"The road to flamingo: An evaluation of flow pattern alterations and salinity intrusion in the lower glades, Everglades National Park; 2002; OFR; 2002-59; Stewart, M. A.; Bhatt, T. N.; Fennema, R. J.; Fitterman, D. V.","productDescription":"36 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":400064,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0059/ofr-02-0059.pdf","text":"Report","size":"1.34 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 2002-0059"},{"id":160590,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0059/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -80.19255002268427,\n 26.455912977980674\n ],\n [\n -81.54181740018961,\n 26.455912977980674\n ],\n [\n -81.54181740018961,\n 25.021398805919503\n ],\n [\n -80.19255002268427,\n 25.021398805919503\n ],\n [\n -80.19255002268427,\n 26.455912977980674\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
The purpose of this study is
\n1. to document the geographic distribution of Holocene (deposited in the last 11,000 years) sedimentary lithologies in and along the Spokane River,
\n2. to document the downstream variation of metal contents (especially lead [Pb] and zinc [Zn] ) by sedimentary lithology, and
\n3. to compare the metal contents of different sedimentary lithologies.
This data is used to gain some understanding of the physical and chemical processes that control those metal contents. It is hoped this study can be used to guide potential future remedial actions aimed at reducing the biologic impact of metal-enriched sediments in this area. This work was undertaken in cooperation with the Washington Department of Ecology and the Environmental Protection Agency.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02126","collaboration":"Prepared in cooperation with the Washington Department of Ecology and the Environmental Protection Agency","usgsCitation":"Box, S.E., and Wallis, J., 2002, Surficial geology along the Spokane River, Washington and its relationship to the metal content of sediments (Idaho-Washington stateline to Latah Creek confluence): U.S. Geological Survey Open-File Report 2002-126, Report: 76 p.; Readme; Metadata: Digital package; 5 Shapefiles; Geochemical data, https://doi.org/10.3133/ofr02126.","productDescription":"Report: 76 p.; Readme; Metadata: Digital package; 5 Shapefiles; Geochemical data","numberOfPages":"76","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":160808,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02126.jpg"},{"id":2876,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0126/","linkFileType":{"id":5,"text":"html"}},{"id":110288,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51393.htm","linkFileType":{"id":5,"text":"html"},"description":"51393"},{"id":283459,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0126/pdf/of02-126.PDF","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Spokane River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.5,\n 47.625\n ],\n [\n -116.9,\n 47.625\n ],\n [\n -116.9,\n 47.6917\n ],\n [\n -117.5,\n 47.6917\n ],\n [\n -117.5,\n 47.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bf2","contributors":{"authors":[{"text":"Box, Stephen E. 0000-0002-5268-8375 sbox@usgs.gov","orcid":"https://orcid.org/0000-0002-5268-8375","contributorId":1843,"corporation":false,"usgs":true,"family":"Box","given":"Stephen","email":"sbox@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":206534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallis, John C.","contributorId":45755,"corporation":false,"usgs":true,"family":"Wallis","given":"John C.","affiliations":[],"preferred":false,"id":206535,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61475,"text":"mf2372 - 2002 - Hydrostructural maps of the Death Valley regional flow system, Nevada and California","interactions":[],"lastModifiedDate":"2017-03-07T09:09:37","indexId":"mf2372","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2372","title":"Hydrostructural maps of the Death Valley regional flow system, Nevada and California","docAbstract":"The locations of principal faults and structural zones that may influence ground-water flow were compiled in support of a three-dimensional ground-water model for the Death Valley regional flow system (DVRFS), which covers 80,000 square km in southwestern Nevada and southeastern California. Faults include Neogene extensional and strike-slip faults and pre-Tertiary thrust faults. Emphasis was given to characteristics of faults and deformed zones that may have a high potential for influencing hydraulic conductivity. These include: (1) faulting that results in the juxtaposition of stratigraphic units with contrasting hydrologic properties, which may cause ground-water discharge and other perturbations in the flow system; (2) special physical characteristics of the fault zones, such as brecciation and fracturing, that may cause specific parts of the zone to act either as conduits or as barriers to fluid flow; (3) the presence of a variety of lithologies whose physical and deformational characteristics may serve to impede or enhance flow in fault zones; (4) orientation of a fault with respect to the present-day stress field, possibly influencing hydraulic conductivity along the fault zone; and (5) faults that have been active in late Pleistocene or Holocene time and areas of contemporary seismicity, which may be associated with enhanced permeabilities.\n The faults shown on maps A and B are largely from Workman and others (in press), and fit one or more of the following criteria: (1) faults that are more than 10 km in map length; (2) faults with more than 500 m of displacement; and (3) faults in sets that define a significant structural fabric that characterizes a particular domain of the DVRFS. The following fault types are shown: Neogene normal, Neogene strike-slip, Neogene low-angle normal, pre-Tertiary thrust, and structural boundaries of Miocene calderas. We have highlighted faults that have late Pleistocene to Holocene displacement (Piety, 1996). Areas of thick Neogene basin-fill deposits (thicknesses 1-2 km, 2-3 km, and >3 km) are shown on map A, based on gravity anomalies and depth-to-basement modeling by Blakely and others (1999). We have interpreted the positions of faults in the subsurface, generally following the interpretations of Blakely and others (1999). Where geophysical constraints are not present, the faults beneath late Tertiary and Quaternary cover have been extended based on geologic reasoning. Nearly all of these concealed faults are shown with continuous solid lines on maps A and B, in order to provide continuous structures for incorporation into the hydrogeologic framework model (HFM). Map A also shows the potentiometric surface, regional springs (25-35 degrees Celsius, D'Agnese and others, 1997), and cold springs (Turner and others, 1996).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2372","collaboration":"Prepared in cooperation with the U.S. Department of Energy National Nuclear Security Administration Nevada Operations Office","usgsCitation":"Potter, C., Sweetkind, D.S., Dickerson, R., and Killgore, M., 2002, Hydrostructural maps of the Death Valley regional flow system, Nevada and California: U.S. Geological Survey Miscellaneous Field Studies Map 2372, 2 maps Sheets: 34 x 50 inches; Readme; Metadata; ArcInfo Files, https://doi.org/10.3133/mf2372.","productDescription":"2 maps Sheets: 34 x 50 inches; Readme; Metadata; ArcInfo Files","costCenters":[],"links":[{"id":180436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2372.png"},{"id":6045,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/mf-2372/","linkFileType":{"id":5,"text":"html"}},{"id":110287,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_50573.htm","linkFileType":{"id":5,"text":"html"},"description":"50573"}],"scale":"350000","country":"United States","state":"Nevada;California","otherGeospatial":"Death Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.0,35.0 ], [ -118.0,38.0 ], [ -115.0,38.0 ], [ -115.0,35.0 ], [ -118.0,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc693","contributors":{"authors":[{"text":"Potter, C. J. 0000-0002-2300-6670","orcid":"https://orcid.org/0000-0002-2300-6670","contributorId":89925,"corporation":false,"usgs":true,"family":"Potter","given":"C. J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":265746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sweetkind, D. S.","contributorId":61507,"corporation":false,"usgs":true,"family":"Sweetkind","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":265745,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dickerson, R. P.","contributorId":23968,"corporation":false,"usgs":true,"family":"Dickerson","given":"R. P.","affiliations":[],"preferred":false,"id":265743,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Killgore, M.L.","contributorId":60316,"corporation":false,"usgs":true,"family":"Killgore","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":265744,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":61462,"text":"mf2377 - 2002 - Generalized geologic map of part of the upper Animas River watershed and vicinity, Silverton, Colorado","interactions":[],"lastModifiedDate":"2017-03-07T09:14:08","indexId":"mf2377","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2377","title":"Generalized geologic map of part of the upper Animas River watershed and vicinity, Silverton, Colorado","docAbstract":" This dataset represents geology compiled for the upper Animas River Watershed near Silverton, Colorado. The source data used are derived from 1:24,000, 1:20,000, 1:48,000 and 1:250,000-scale geologic maps by geologists who have worked in this area since the early 1960's.","language":"English","publisher":"U.S. Geological ","doi":"10.3133/mf2377","usgsCitation":"Yager, D., and Bove, D.J., 2002, Generalized geologic map of part of the upper Animas River watershed and vicinity, Silverton, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 2377, Sheet 49 by 30 inches (in color), https://doi.org/10.3133/mf2377.","productDescription":"Sheet 49 by 30 inches (in color)","costCenters":[],"links":[{"id":182487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6033,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/mf/2002/mf-2377/","linkFileType":{"id":5,"text":"html"}},{"id":110286,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_50332.htm","linkFileType":{"id":5,"text":"html"},"description":"50332"}],"scale":"48000","country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.86749999999999,37.75 ], [ -107.86749999999999,38 ], [ -107.5,38 ], [ -107.5,37.75 ], [ -107.86749999999999,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e486de4b07f02db50bd27","contributors":{"authors":[{"text":"Yager, D.B. 0000-0001-5074-4022","orcid":"https://orcid.org/0000-0001-5074-4022","contributorId":107330,"corporation":false,"usgs":true,"family":"Yager","given":"D.B.","affiliations":[],"preferred":false,"id":265698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bove, D. J.","contributorId":70767,"corporation":false,"usgs":true,"family":"Bove","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265697,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31599,"text":"ofr0297 - 2002 - Inventory of Neoproterozoic and Paleozoic strata in Sonora, Mexico","interactions":[],"lastModifiedDate":"2023-06-27T15:11:43.713019","indexId":"ofr0297","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-97","title":"Inventory of Neoproterozoic and Paleozoic strata in Sonora, Mexico","docAbstract":"This compilation is an inventory of all known outcrops of Neoproterozoic and Paleozoic strata in Sonora, Mexico. We have not attempted an interpretation of the regional stratigraphic or structural setting of the strata. Brief summaries of the stratigraphic setting of the Sonora rocks are given in Poole and Hayes (1971), Rangin (1978), Stewart and others (1984, 1990), and Poole and Madrid (1986; 1988b). More specific information on the setting of strata of specific ages are given by Stewart and others (2002) for the Neoproterozoic and Cambrian; by Poole and others (1995a) for Ordovician shelf strata; by Poole and others (1995b) for Ordovician deep-water openbasin strata; by Poole and others (1997, 1998, 2000a) for Silurian strata; and by Poole and others (2000a) for Mississippian strata. Other reports that discuss regional aspects of Paleozoic stratigraphy include López-Ramos (1982), Peiffer-Rangin, (1979, 1988), Pérez-Ramos (1992), and Stewart and others (1997, 1999a).
\nStructurally, the major Paleozoic feature of Sonora is the Sonora allochthon, consisting of deep-water (eugeoclinal) strata emplaced in the Permian over shelf (miogeoclinal) deposits (Poole and others, 1995a,b; Poole and Perry, 1997; 1998). The emplacement structure is generally considered to be a major Permian continental margin thrust fault that emplaced the deep-water rocks northward over shelf (miogeoclinal) deposits. An alternate interpretation has been presented by Stewart and others (2002). He proposed that the emplacement of the Sonora allochthon was along a major Permian transpressional structure that was primarily a strike-slip fault with only a minor thrust component .
\nThe Mojave-Sonora megashear has been proposed to disrupt Neoproterozoic and Paleozoic trends in Sonora. This feature is a hypothetical, left-lateral, northwest-striking fault extending across northern Sonora and the southwestern United States (Silver and Anderson, 1974; Anderson and Schmidt, 1983). It is proposed to have Jurassic displacements of about 700-800 km. Current opinion is mixed concerning whether the Mojave-Sonora megashear exists (see discussions and references in Stewart and others, 1990; 1999a).
\nThe inventory presented here is the product of a search of the literature for described Neoproterozoic and Paleozoic localities and our examination of a large number of the outcrops in the field. The individual localities are described by reference letters and numbers, locality name, latitude and longitude, a brief text on the stratigraphy of the strata, and references. Figure 1 is an index showing the location of Sonora and the location of figure 2. The location of a few localites that are outside of figure 2 are also shown on figure 1. We also include a separate description of localities that have been erroneously reported, on the based of our field examinations, to contain Neoproterozoic and Paleozoic rocks. We include a brief description of problematic strata in southern Sonora that have been described as Paleozoic, but may be at least in part Mesozoic. Figures 3-11 show the distribution of Neoproterozoic, Cambrian, Ordovician, Silurian, Devonian, Mississippian, Pennsylvanian, and Permian strata in Sonora.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0297","usgsCitation":"Stewart, J.H., and Poole, F.G., 2002, Inventory of Neoproterozoic and Paleozoic strata in Sonora, Mexico: U.S. Geological Survey Open-File Report 2002-97, 43 p., https://doi.org/10.3133/ofr0297.","productDescription":"43 p.","numberOfPages":"50","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":283409,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0297.jpg"},{"id":59811,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0097/pdf/of02-97.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2865,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0097/","linkFileType":{"id":5,"text":"html"}}],"country":"Mexico","state":"Sonora","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.05,26.15 ], [ -115.05,32.49 ], [ -108.42,32.49 ], [ -108.42,26.15 ], [ -115.05,26.15 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ace4b07f02db5c6565","contributors":{"authors":[{"text":"Stewart, John H.","contributorId":83086,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":206512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poole, Forrest G. 0000-0001-8487-0799 bpoole@usgs.gov","orcid":"https://orcid.org/0000-0001-8487-0799","contributorId":1543,"corporation":false,"usgs":true,"family":"Poole","given":"Forrest","email":"bpoole@usgs.gov","middleInitial":"G.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":206511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70179959,"text":"70179959 - 2002 - Elevated temperature exacerbates Ichthyophonus infections in buffalo sculpin","interactions":[],"lastModifiedDate":"2017-01-20T14:06:18","indexId":"70179959","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1648,"text":"Fish Health Newsletter","active":true,"publicationSubtype":{"id":10}},"title":"Elevated temperature exacerbates Ichthyophonus infections in buffalo sculpin","docAbstract":"High incidences of Ichthyophonus hoferi, a parasite primarily of marine and estuarine fishes, have recently been reported in rockfishes and Pacific herring from the eastern North Pacific (Kent et al 2001, Hershberger et al 2002). Taxonomic position of I. hoferi remains unresolved, but recent phylogenetic studies have grouped the organism with Dermocystidium, Psorospermium, the rosette agent of salmonids, and Rhinosporidium in the Mesomycetozoa, a novel clade of protists near the animal-fungal divergence (Herr et al 1999). Genetic differences among isolates from the east coast of North America indicate that more than one species of Ichthyophonus exist (Rand et al 2000), and different species have likely been assigned the same name based on morphological characteristics. Therefore, hereafter in this manuscript, the organism will be referred to as Ichthyophonus .
","language":"English","publisher":"American fisheries society","usgsCitation":"Halpenny, C., Kocan, R.M., Winton, J., Perry, J., and Hershberger, P., 2002, Elevated temperature exacerbates Ichthyophonus infections in buffalo sculpin: Fish Health Newsletter, p. 17-20.","productDescription":"4 p. ","startPage":"17","endPage":"20","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":333611,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58833027e4b0d002316377c6","contributors":{"authors":[{"text":"Halpenny, C.M.","contributorId":76523,"corporation":false,"usgs":true,"family":"Halpenny","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":659308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kocan, R. M.","contributorId":41783,"corporation":false,"usgs":true,"family":"Kocan","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":659309,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winton, J. R. 0000-0002-3505-5509","orcid":"https://orcid.org/0000-0002-3505-5509","contributorId":82441,"corporation":false,"usgs":true,"family":"Winton","given":"J. R.","affiliations":[],"preferred":false,"id":659310,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perry, J.A.","contributorId":100254,"corporation":false,"usgs":true,"family":"Perry","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":659311,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hershberger, P.K. 0000-0002-2261-7760","orcid":"https://orcid.org/0000-0002-2261-7760","contributorId":58818,"corporation":false,"usgs":true,"family":"Hershberger","given":"P.K.","affiliations":[],"preferred":false,"id":659312,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":33073,"text":"b2185 - 2002 - Response plan for volcano hazards in the Long Valley Caldera and Mono Craters region, California","interactions":[],"lastModifiedDate":"2019-09-10T09:11:16","indexId":"b2185","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","title":"Response plan for volcano hazards in the Long Valley Caldera and Mono Craters region, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/b2185","isbn":"0607984880","usgsCitation":"Hill, D.P., Dzurisin, D., Ellsworth, W.L., Endo, E.T., Galloway, D., Gerlach, T.M., Johnston, M.S., Langbein, J.O., McGee, K.A., Miller, C.D., Oppenheimer, D., and Sorey, M.L., 2002, Response plan for volcano hazards in the Long Valley Caldera and Mono Craters region, California: U.S. Geological Survey Bulletin 2185, 65 p., https://doi.org/10.3133/b2185.","productDescription":"65 p.","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":163991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3277,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2185/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Long Valley Caldera, Mono Craters","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.69030761718749,\n 36.74768773190056\n ],\n [\n -117.16918945312499,\n 36.74768773190056\n ],\n [\n -117.16918945312499,\n 38.453588708941375\n ],\n [\n -120.69030761718749,\n 38.453588708941375\n ],\n [\n -120.69030761718749,\n 36.74768773190056\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db628375","contributors":{"authors":[{"text":"Hill, David P. hill@usgs.gov","contributorId":2600,"corporation":false,"usgs":true,"family":"Hill","given":"David","email":"hill@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":false,"id":209819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dzurisin, Daniel 0000-0002-0138-5067 dzurisin@usgs.gov","orcid":"https://orcid.org/0000-0002-0138-5067","contributorId":538,"corporation":false,"usgs":true,"family":"Dzurisin","given":"Daniel","email":"dzurisin@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":209817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":209818,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Endo, Elliot T.","contributorId":10439,"corporation":false,"usgs":true,"family":"Endo","given":"Elliot","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":209820,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Galloway, D. L. 0000-0003-0904-5355","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":31383,"corporation":false,"usgs":true,"family":"Galloway","given":"D. L.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":209822,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gerlach, Terry M.","contributorId":104958,"corporation":false,"usgs":true,"family":"Gerlach","given":"Terry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":209828,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Johnston, Malcolm S.J.","contributorId":55879,"corporation":false,"usgs":true,"family":"Johnston","given":"Malcolm","email":"","middleInitial":"S.J.","affiliations":[],"preferred":false,"id":209825,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Langbein, John O.","contributorId":72438,"corporation":false,"usgs":true,"family":"Langbein","given":"John","middleInitial":"O.","affiliations":[],"preferred":false,"id":209827,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"McGee, Ken A.","contributorId":48613,"corporation":false,"usgs":true,"family":"McGee","given":"Ken","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":209824,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Miller, C. Dan","contributorId":38145,"corporation":false,"usgs":true,"family":"Miller","given":"C.","email":"","middleInitial":"Dan","affiliations":[],"preferred":false,"id":209823,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Oppenheimer, David","contributorId":58323,"corporation":false,"usgs":true,"family":"Oppenheimer","given":"David","affiliations":[],"preferred":false,"id":209826,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Sorey, Michael L.","contributorId":20726,"corporation":false,"usgs":true,"family":"Sorey","given":"Michael","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":209821,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":31580,"text":"ofr0235 - 2002 - Volatile Organic Compounds, Specific Conductance, and Temperature in the Bottom Sediments of Mill Pond, Ashland, Massachusetts, April 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:09:09","indexId":"ofr0235","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-35","title":"Volatile Organic Compounds, Specific Conductance, and Temperature in the Bottom Sediments of Mill Pond, Ashland, Massachusetts, April 2001","docAbstract":"A plume of volatile organic compounds in ground water extends northward from the former Nyanza Property in Ashland, Massachusetts, and discharges into the Sudbury River and the upstream end of Mill Pond. A network of polyethylene-membrane passive-vapor-diffusion samplers was installed in February 2001 to help define the lateral extent of the plume under the pond, including an area vegetated by wetland herbs, sedges, and shrubs. Chlorobenzene and trichloroethene were detected with passive-vapor-diffusion samplers at five locations in the bottom sediments of the southern part of the approximate one acre of vegetated area in Mill Pond. Vapor concentrations of chlorobenzene ranged from 178 to 2,210 parts per billion by volume, and vapor concentrations of trichloroethene ranged from 20 to 96 parts per billion by volume. Chlorobenzene also was detected in one sediment-pore-water sample extracted with a push-point sampler in this area; the concentration was 25 micrograms per liter. Toluene was detected with passive-vapor-diffusion samplers at three sites in the open pond area north of the vegetated areas. Vapor concentrations of toluene ranged from 20 to 90 parts per billion by volume.\r\n\r\n\r\n\r\nSpecific conductance and temperature of sediment-pore waters were measured at selected sampling sites in Mill Pond to examine their possible associations with the presence of volatile organic compounds. Temperature in the sediment-pore water also was measured to convert vapor concentrations of volatile organic compounds collected with diffusion samplers to equivalent water concentrations. These equivalent water concentrations were then to be compared with water concentrations collected with a push-point sampler. Because of the limited detections of volatile organic compounds at sites where water samples were collected and where specific conductance and temperature were measured, these potential associations and conversions could not be assessed.","language":"ENGLISH","doi":"10.3133/ofr0235","usgsCitation":"Church, P.E., Lyford, F.P., and Clifford, S., 2002, Volatile Organic Compounds, Specific Conductance, and Temperature in the Bottom Sediments of Mill Pond, Ashland, Massachusetts, April 2001: U.S. Geological Survey Open-File Report 2002-35, 10 p., https://doi.org/10.3133/ofr0235.","productDescription":"10 p.","costCenters":[],"links":[{"id":2818,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr02035","linkFileType":{"id":5,"text":"html"}},{"id":160578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ace4b07f02db5c6226","contributors":{"authors":[{"text":"Church, Peter E.","contributorId":99178,"corporation":false,"usgs":true,"family":"Church","given":"Peter","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":206447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyford, Forest P.","contributorId":43334,"corporation":false,"usgs":true,"family":"Lyford","given":"Forest","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":206445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clifford, Scott","contributorId":63042,"corporation":false,"usgs":true,"family":"Clifford","given":"Scott","email":"","affiliations":[],"preferred":false,"id":206446,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31588,"text":"ofr0263 - 2002 - Directional borehole radar tests of an oil injection experiment at the Colorado School of Mines, Golden, Colorado","interactions":[],"lastModifiedDate":"2017-03-07T13:29:29","indexId":"ofr0263","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-63","title":"Directional borehole radar tests of an oil injection experiment at the Colorado School of Mines, Golden, Colorado","docAbstract":"In October 2001, the U.S. Geological Survey conducted borehole radar surveys of an oil injection experiment at the Colorado School of Mines (CSM), in Golden Colorado using the prototype U.S. Geological Survey (USGS)-developed directional borehole radar system (DBOR). A explanation of the system can be found in Wright and others (2001). The USGS was invited to the CSM to deploy the prototype directional borehole radar system during an oil injection experiment conducted to investigate the applicability of radar to monitoring formation invasion from a horizontal borehole. This work was conducted by a student at the CSM and is summarized in Moita (2001). The purpose of this report is to release the data and to summarize the experiments conducted with the DBOR system. This report contains, (1) a description of the system as deployed in the experiments, (2) a description of the data collected and data parameters used, (3) a simple display of some of the data collected, and (4) a description of the DBOR data files.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr0263","usgsCitation":"Abraham, J., Moulton, C., and Brown, P.J., 2002, Directional borehole radar tests of an oil injection experiment at the Colorado School of Mines, Golden, Colorado: U.S. Geological Survey Open-File Report 2002-63, https://doi.org/10.3133/ofr0263.","costCenters":[],"links":[{"id":160781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2856,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0063/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab9d","contributors":{"authors":[{"text":"Abraham, Jared D.","contributorId":42630,"corporation":false,"usgs":true,"family":"Abraham","given":"Jared D.","affiliations":[],"preferred":false,"id":206476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moulton, Craig","contributorId":106541,"corporation":false,"usgs":true,"family":"Moulton","given":"Craig","affiliations":[],"preferred":false,"id":206478,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Philip J. II","contributorId":67936,"corporation":false,"usgs":true,"family":"Brown","given":"Philip","suffix":"II","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":206477,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":31570,"text":"ofr01483 - 2002 - Effects of water-management alternatives on streamflow in the Ipswich River basin, Massachusetts","interactions":[],"lastModifiedDate":"2025-07-22T15:11:25.976761","indexId":"ofr01483","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2001-483","title":"Effects of water-management alternatives on streamflow in the Ipswich River basin, Massachusetts","docAbstract":"Management alternatives that could help mitigate the effects of water withdrawals on streamflow in the Ipswich River Basin were evaluated by simulation with a calibrated Hydrologic Simulation Program--Fortran (HSPF) model. The effects of management alternatives on streamflow were simulated for a 35-year period (1961-95). Most alternatives examined increased low flows compared to the base simulation of average 1989-93 withdrawals. Only the simulation of no septic-effluent inflow, and the simulation of a 20-percent increase in withdrawals, further lowered flows or caused the river to stop flowing for longer periods of time than the simulation of average 1989-93 withdrawals. Simulations of reduced seasonal withdrawals by 20 percent, and by 50 percent, resulted in a modest increase in low flow in a critical habitat reach (model reach 8 near the Reading town well field); log-Pearson Type III analysis of simulated daily-mean flow indicated that under these reduced withdrawals, model reach 8 would stop flowing for a period of seven consecutive days about every other year, whereas under average 1989-93 withdrawals this reach would stop flowing for a seven consecutive day period almost every year. Simulations of no seasonal withdrawals, and simulations that stopped streamflow depletion when flow in model reach 19 was below 22 cubic feet per second, indicated flow would be maintained in model reach 8 at all times. Simulations indicated wastewater-return flows would augment low flow in proportion to the rate of return flow. Simulations of a 1.5 million gallons per day return flow rate indicated model reach 8 would stop flowing for a period of seven consecutive days about once every 5 years; simulated return flow rates of 1.1 million gallons per day indicated that model reach 8 would stop flowing for a period of seven consecutive days about every other year. Simulation of reduced seasonal withdrawals, combined with no septic effluent return flow, indicated only a slight increase in low flow compared to low flows simulated under average 1989-93 withdrawals. Simulation of reduced seasonal withdrawal, combined with 2.6 million gallons per day wastewater-return flows, provided more flow in model reach 8 than that simulated under no withdrawals.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr01483","usgsCitation":"Zarriello, P.J., 2002, Effects of water-management alternatives on streamflow in the Ipswich River basin, Massachusetts: U.S. Geological Survey Open-File Report 2001-483, 30 p., https://doi.org/10.3133/ofr01483.","productDescription":"30 p.","costCenters":[],"links":[{"id":2810,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2001/ofr01483/index.html","linkFileType":{"id":5,"text":"html"}},{"id":390452,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51402.htm"},{"id":161109,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Ipswich River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.2167,\n 42.5\n ],\n [\n -71.0203,\n 42.5\n ],\n [\n -71.0203,\n 42.6667\n ],\n [\n -71.2167,\n 42.6667\n ],\n [\n -71.2167,\n 42.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683450","contributors":{"authors":[{"text":"Zarriello, Philip J.","contributorId":21588,"corporation":false,"usgs":false,"family":"Zarriello","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":206419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31581,"text":"ofr0238 - 2002 - Vegetative resistance to flow in South Florida Everglades: Summary of vegetation sampling in Water Conservation Area 2A, September 1999","interactions":[],"lastModifiedDate":"2022-07-07T20:07:09.199871","indexId":"ofr0238","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-38","title":"Vegetative resistance to flow in South Florida Everglades: Summary of vegetation sampling in Water Conservation Area 2A, September 1999","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0238","usgsCitation":"Rybicki, N.B., Reel, J.T., Gammon, P.T., and Garrett, M.K., 2002, Vegetative resistance to flow in South Florida Everglades: Summary of vegetation sampling in Water Conservation Area 2A, September 1999: U.S. Geological Survey Open-File Report 2002-38, vi, 42 p., https://doi.org/10.3133/ofr0238.","productDescription":"vi, 42 p.","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":403226,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51420.htm","linkFileType":{"id":5,"text":"html"}},{"id":59810,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160579,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0038/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Water Conservation Area 2A","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.5682373046875,\n 26.12091815959972\n ],\n [\n -80.255126953125,\n 26.12091815959972\n ],\n [\n -80.255126953125,\n 26.49024045886963\n ],\n [\n -80.5682373046875,\n 26.49024045886963\n ],\n [\n -80.5682373046875,\n 26.12091815959972\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60238d","contributors":{"authors":[{"text":"Rybicki, Nancy B. 0000-0002-2205-7927 nrybicki@usgs.gov","orcid":"https://orcid.org/0000-0002-2205-7927","contributorId":2142,"corporation":false,"usgs":true,"family":"Rybicki","given":"Nancy","email":"nrybicki@usgs.gov","middleInitial":"B.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":206448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reel, Justin T.","contributorId":26324,"corporation":false,"usgs":true,"family":"Reel","given":"Justin","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":206450,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gammon, Patricia T.","contributorId":107251,"corporation":false,"usgs":true,"family":"Gammon","given":"Patricia","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":206451,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Garrett, Mary Keith","contributorId":12082,"corporation":false,"usgs":true,"family":"Garrett","given":"Mary","email":"","middleInitial":"Keith","affiliations":[],"preferred":false,"id":206449,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":31584,"text":"ofr0255 - 2002 - Geologic cross sections showing the concentrations of As, Cd, Co, Cu, Cr, Fe, Mo, Ni, Pb, and Zn in acid-insoluble residues of Paleozoic rocks within the Doniphan/Eleven Point Ranger District of the Mark Twain National Forest, Missouri, USA","interactions":[],"lastModifiedDate":"2017-03-07T13:19:31","indexId":"ofr0255","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-55","title":"Geologic cross sections showing the concentrations of As, Cd, Co, Cu, Cr, Fe, Mo, Ni, Pb, and Zn in acid-insoluble residues of Paleozoic rocks within the Doniphan/Eleven Point Ranger District of the Mark Twain National Forest, Missouri, USA","docAbstract":"This report is a product of a U.S. Geological Survey investigation that is focused on characterizing the potential environmental impacts of lead-zinc mining within the Doniphan/Eleven Point ranger district of the Mark Twain national forest. The elemental concentrations of iron (Fe), arsenic (As), cadmium (Cd), cobalt (Co), copper (Cu), chromium (Cr), nickel (Ni), lead (Pb), and zinc (Zn) in acidinsoluble residues are shown for boreholes along two geologic cross sections within Doniphan/Elevan Point ranger district (Figure 1). The purpose of this report is to characterize, in a general sense, the distribution of economically and environmentally important elements within the rocks and aquifers of the Doniphan/Eleven Point ranger district
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr0255","usgsCitation":"Lee, L., and Goldhaber, M.B., 2002, Geologic cross sections showing the concentrations of As, Cd, Co, Cu, Cr, Fe, Mo, Ni, Pb, and Zn in acid-insoluble residues of Paleozoic rocks within the Doniphan/Eleven Point Ranger District of the Mark Twain National Forest, Missouri, USA: U.S. Geological Survey Open-File Report 2002-55, 24 p., https://doi.org/10.3133/ofr0255.","productDescription":"24 p.","costCenters":[],"links":[{"id":160589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2821,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/publication/ofr0255","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Missouri","otherGeospatial":"Mark Twain National Forest","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a641c","contributors":{"authors":[{"text":"Lee, Lopaka","contributorId":83167,"corporation":false,"usgs":true,"family":"Lee","given":"Lopaka","email":"","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":206455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":206454,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":31575,"text":"ofr0222 - 2002 - Geologic map of the Corona North 7.5' quadrangle, Riverside and San Bernardino Counties, California","interactions":[],"lastModifiedDate":"2023-06-27T15:27:02.520334","indexId":"ofr0222","displayToPublicDate":"2002-04-01T00:00:00","publicationYear":"2002","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":"2002-22","title":"Geologic map of the Corona North 7.5' quadrangle, Riverside and San Bernardino Counties, California","docAbstract":"Open-File Report 02-22 contains a digital geologic map database of the Corona North 7.5’ quadrangle, Riverside and San Bernardino Counties, California that includes:\n\nARC/INFO (Environmental Systems Research Institute, http://www.esri.com) version 7.2.1 coverages of the various elements of the geologic map.\nA Postscript file to plot the geologic map on a topographic base, and containing a Correlation of Map Units diagram (CMU), a Description of Map Units (DMU), and an index map.\nPortable Document Format (.pdf) files of:\na. This Readme; includes in Appendix I, data contained in crn_met.txt\n\nb. The same graphic as plotted in 2 above. Test plots have not produced precise 1:24,000- scale map sheets. Adobe Acrobat page size setting influences map scale.\n\nThe Correlation of Map Units and Description of Map Units is in the editorial format of USGS Geologic Investigations Series (I-series) maps but has not been edited to comply with I-map standards. Within the geologic map data package, map units are identified by standard geologic map criteria such as formation name, age, and lithology. Where known, grain size is indicated on the map by a subscripted letter or letters following the unit symbols as follows: lg, large boulders; b, boulder; g, gravel; a, arenaceous; s, silt; c, clay; e.g. Qyfa is a predominantly young alluvial fan deposit that is arenaceous. Multiple letters are used for more specific identification or for mixed units, e.g., Qfysa is a silty sand. In some cases, mixed units are indicated by a compound symbol; e.g., Qyf2sc. Marine deposits are in part overlain by local, mostly alluvial fan, deposits and are labeled Qomf. Grain size follows f.\n\nEven though this is an Open-File Report and includes the standard USGS Open-File disclaimer, the report closely adheres to the stratigraphic nomenclature of the U.S. Geological Survey. 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