The hydrology and water quality of an urbanized reach of Little Cottonwood Creek near Salt Lake City, Utah, were examined as part of the Great Salt Lake Basins study, part of the U.S. Geological Survey National Water-Quality Assessment program. Physical and chemical properties of the stream were referenced to established aquatic-life criteria as available. Two fixed sampling sites were established on Little Cottonwood Creek with the purpose of determining the influence of urbanization on the water quality of the stream. The fixed-site assessment is a component of the National Water-Quality Assessment surface-water study design used to assess the spatial and temporal distribution of selected water-quality constituents.
The occurrence and distribution of major ions, nutrients, trace elements, dissolved and suspended organic carbon, pesticides, volatile organic compounds, and suspended sediment were monitored during this study. From October 1998 to September 2000, stream samples were collected at regular intervals at the two fixed sites. Additional samples were collected at these sites during periods of high flow, which included runoff from snowmelt in the headwaters and seasonal thunderstorms in the lower basin.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/wri024276","usgsCitation":"Gerner, S.J., and Waddell, K.M., 2003, Hydrology and water quality of an urban stream reach in the Great Basin — Little Cottonwood Creek near Salt Lake City, Utah, water years 1999–2000: U.S. Geological Survey Water-Resources Investigations Report 2002-4276, viii, 46 p., https://doi.org/10.3133/wri024276.","productDescription":"viii, 46 p.","numberOfPages":"57","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":170379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394839,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54626.htm"},{"id":4089,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri024276/","linkFileType":{"id":5,"text":"html"}},{"id":334636,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/wri024276/pdf/WRI024276.pdf"}],"country":"United States","state":"Utah","city":"Salt Lake City","otherGeospatial":"Little Cottonwood Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.9451904296875,\n 40.55085246740427\n ],\n [\n -111.9451904296875,\n 40.6504293761137\n ],\n [\n -111.76391601562499,\n 40.6504293761137\n ],\n [\n -111.76391601562499,\n 40.55085246740427\n ],\n [\n -111.9451904296875,\n 40.55085246740427\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"National Water-Quality Assessment Program","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604bf4","contributors":{"authors":[{"text":"Gerner, Steven J. 0000-0002-5701-1304 sjgerner@usgs.gov","orcid":"https://orcid.org/0000-0002-5701-1304","contributorId":972,"corporation":false,"usgs":true,"family":"Gerner","given":"Steven","email":"sjgerner@usgs.gov","middleInitial":"J.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":236182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":236183,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50081,"text":"fs10102 - 2003 - \"Hot Water\" in Lassen Volcanic National Park: Fumaroles, steaming ground, and boiling mudpots","interactions":[],"lastModifiedDate":"2022-10-13T20:57:47.086335","indexId":"fs10102","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"101-02","title":"\"Hot Water\" in Lassen Volcanic National Park: Fumaroles, steaming ground, and boiling mudpots","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs10102","usgsCitation":"Clynne, M.A., Janik, C.J., and Muffler, L.J., 2003, \"Hot Water\" in Lassen Volcanic National Park: Fumaroles, steaming ground, and boiling mudpots: U.S. Geological Survey Fact Sheet 101-02, 4 p., https://doi.org/10.3133/fs10102.","productDescription":"4 p.","costCenters":[],"links":[{"id":120697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_101_02.bmp"},{"id":408294,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54608.htm","linkFileType":{"id":5,"text":"html"}},{"id":4264,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2002/fs101-02/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"Lassen Volcanic National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.5703,\n 40.4067\n ],\n [\n -121.3625,\n 40.4067\n ],\n [\n -121.3625,\n 40.4833\n ],\n [\n -121.5703,\n 40.4833\n ],\n [\n -121.5703,\n 40.4067\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4900e4b0b290850eecc2","contributors":{"authors":[{"text":"Clynne, Michael A. 0000-0002-4220-2968 mclynne@usgs.gov","orcid":"https://orcid.org/0000-0002-4220-2968","contributorId":2032,"corporation":false,"usgs":true,"family":"Clynne","given":"Michael","email":"mclynne@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":240738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janik, Cathy J.","contributorId":87090,"corporation":false,"usgs":true,"family":"Janik","given":"Cathy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":240740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muffler, Leroy J. Patrick","contributorId":16409,"corporation":false,"usgs":true,"family":"Muffler","given":"Leroy","email":"","middleInitial":"J. Patrick","affiliations":[],"preferred":false,"id":240739,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":47826,"text":"fs01303 - 2003 - Water-quality assessment of the central Nebraska basins — Entering a new decade","interactions":[],"lastModifiedDate":"2021-12-27T21:02:35.530419","indexId":"fs01303","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"013-03","title":"Water-quality assessment of the central Nebraska basins — Entering a new decade","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs01303","usgsCitation":"Zelt, R.B., and Frankforter, J.D., 2003, Water-quality assessment of the central Nebraska basins — Entering a new decade: U.S. Geological Survey Fact Sheet 013-03, HTML Document, https://doi.org/10.3133/fs01303.","productDescription":"HTML Document","costCenters":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":120220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_013_03.bmp"},{"id":393470,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54648.htm"},{"id":4032,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs-013-03/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.3,\n 40.4444\n ],\n [\n -95.8667,\n 40.4444\n ],\n [\n -95.8667,\n 42.5278\n ],\n [\n -102.3,\n 42.5278\n ],\n [\n -102.3,\n 40.4444\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6e03","contributors":{"authors":[{"text":"Zelt, Ronald B. 0000-0001-9024-855X rbzelt@usgs.gov","orcid":"https://orcid.org/0000-0001-9024-855X","contributorId":300,"corporation":false,"usgs":true,"family":"Zelt","given":"Ronald","email":"rbzelt@usgs.gov","middleInitial":"B.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":236321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frankforter, Jill D. 0000-0003-0371-2313 jdfrankf@usgs.gov","orcid":"https://orcid.org/0000-0003-0371-2313","contributorId":1739,"corporation":false,"usgs":true,"family":"Frankforter","given":"Jill","email":"jdfrankf@usgs.gov","middleInitial":"D.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":236322,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50747,"text":"ofr03186 - 2003 - Channel-Bank Conditions and Accumulations of Large Woody Debris along White River between Anderson and Indianapolis, Indiana, 2002","interactions":[],"lastModifiedDate":"2016-06-22T11:56:28","indexId":"ofr03186","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2003-186","title":"Channel-Bank Conditions and Accumulations of Large Woody Debris along White River between Anderson and Indianapolis, Indiana, 2002","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr03186","usgsCitation":"Robinson, B.A., 2003, Channel-Bank Conditions and Accumulations of Large Woody Debris along White River between Anderson and Indianapolis, Indiana, 2002: U.S. Geological Survey Open-File Report 2003-186, HTML document, https://doi.org/10.3133/ofr03186.","productDescription":"HTML document","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":175391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4238,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-186/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Indiana","city":"Anderson, Indianapolis","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.54067993164062,\n 39.68922382844214\n ],\n [\n -86.54067993164062,\n 40.1673306817866\n ],\n [\n -85.2374267578125,\n 40.1673306817866\n ],\n [\n -85.2374267578125,\n 39.68922382844214\n ],\n [\n -86.54067993164062,\n 39.68922382844214\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e610a","contributors":{"authors":[{"text":"Robinson, Bret A. barobins@usgs.gov","contributorId":3897,"corporation":false,"usgs":true,"family":"Robinson","given":"Bret","email":"barobins@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":242220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47835,"text":"fs02603 - 2003 - Geologic sequestration of carbon dioxide--An energy resource perspective","interactions":[],"lastModifiedDate":"2012-02-02T00:10:47","indexId":"fs02603","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"026-03","title":"Geologic sequestration of carbon dioxide--An energy resource perspective","language":"ENGLISH","doi":"10.3133/fs02603","usgsCitation":"Burruss, R.A., and Brennan, S.T., 2003, Geologic sequestration of carbon dioxide--An energy resource perspective (Online Version 1.0): U.S. Geological Survey Fact Sheet 026-03, 1 sheet ([2] p.) : col. ill. ; 28 x 18 cm., https://doi.org/10.3133/fs02603.","productDescription":"1 sheet ([2] p.) : col. ill. ; 28 x 18 cm.","costCenters":[],"links":[{"id":122032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_026_03.jpg"},{"id":4040,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/fs026-03/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68832a","contributors":{"authors":[{"text":"Burruss, Robert A. 0000-0001-6827-804X burruss@usgs.gov","orcid":"https://orcid.org/0000-0001-6827-804X","contributorId":558,"corporation":false,"usgs":true,"family":"Burruss","given":"Robert","email":"burruss@usgs.gov","middleInitial":"A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":236345,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, Sean T. 0000-0002-7102-9359 sbrennan@usgs.gov","orcid":"https://orcid.org/0000-0002-7102-9359","contributorId":559,"corporation":false,"usgs":true,"family":"Brennan","given":"Sean","email":"sbrennan@usgs.gov","middleInitial":"T.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":236346,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50759,"text":"wri034074 - 2003 - Estimated flood-inundation maps for Cowskin Creek in western Wichita, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:11:20","indexId":"wri034074","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2003-4074","title":"Estimated flood-inundation maps for Cowskin Creek in western Wichita, Kansas","docAbstract":"The October 31, 1998, flood on Cowskin Creek in western Wichita, Kansas, caused millions of dollars in damages. Emergency management personnel and flood mitigation teams had difficulty in efficiently identifying areas affected by the flooding, and no warning was given to residents because flood-inundation information was not available. \r\n\r\nTo provide detailed information about future flooding on Cowskin Creek, high-resolution estimated flood-inundation maps were developed using geographic information system technology and advanced hydraulic analysis. Two-foot-interval land-surface elevation data from a 1996 flood insurance study were used to create a three-dimensional topographic representation of the study area for hydraulic analysis. The data computed from the hydraulic analyses were converted into geographic information system format with software from the U.S. Army Corps of Engineers' Hydrologic Engineering Center. The results were overlaid on the three-dimensional topographic representation of the study area to produce maps of estimated flood-inundation areas and estimated depths of water in the inundated areas for 1-foot increments on the basis of stream stage at an index streamflow-gaging station. \r\n\r\nA Web site (http://ks.water.usgs.gov/Kansas/cowskin.floodwatch) was developed to provide the public with information pertaining to flooding in the study area. The Web site shows graphs of the real-time streamflow data for U.S. Geological Survey gaging stations in the area and monitors the National Weather Service Arkansas-Red Basin River Forecast Center for Cowskin Creek flood-forecast information. When a flood is forecast for the Cowskin Creek Basin, an estimated flood-inundation map is displayed for the stream stage closest to the National Weather Service's forecasted peak stage. Users of the Web site are able to view the estimated flood-inundation maps for selected stages at any time and to access information about this report and about flooding in general. Flood recovery teams also have the ability to view the estimated flood-inundation map pertaining to the most recent flood. The availability of these maps and the ability to monitor the real-time stream stage through the U.S. Geological Survey Web site provide emergency management personnel and residents with information that is critical for evacuation and rescue efforts in the event of a flood as well as for post-flood recovery efforts.","language":"ENGLISH","doi":"10.3133/wri034074","usgsCitation":"Studley, S.E., 2003, Estimated flood-inundation maps for Cowskin Creek in western Wichita, Kansas: U.S. Geological Survey Water-Resources Investigations Report 2003-4074, iv, 18 p. : col. ill., col. maps ; 28 cm., https://doi.org/10.3133/wri034074.","productDescription":"iv, 18 p. : col. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":4187,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://ks.water.usgs.gov/Kansas/pubs/abstracts/wrir.03-4074.html","linkFileType":{"id":5,"text":"html"}},{"id":124825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2003/4074/report-thumb.jpg"},{"id":86341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2003/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd44b","contributors":{"authors":[{"text":"Studley, Seth E. sstudley@usgs.gov","contributorId":5916,"corporation":false,"usgs":true,"family":"Studley","given":"Seth","email":"sstudley@usgs.gov","middleInitial":"E.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":true,"id":242249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47831,"text":"fs01903 - 2003 - The 1903 and 1993 floods in Kansas: The effects of changing times and technology","interactions":[],"lastModifiedDate":"2024-02-22T22:14:32.092707","indexId":"fs01903","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"019-03","title":"The 1903 and 1993 floods in Kansas: The effects of changing times and technology","docAbstract":"No abstract available.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836f8","contributors":{"authors":[{"text":"Combs, Lanna J.","contributorId":86411,"corporation":false,"usgs":true,"family":"Combs","given":"Lanna","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":236341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, Charles A. cperry@usgs.gov","contributorId":2093,"corporation":false,"usgs":true,"family":"Perry","given":"Charles","email":"cperry@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":236340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":50806,"text":"ofr200337 - 2003 - The New Albany Shale petroleum system, Illinois basin - Data and map image archive from the material-balance assessment","interactions":[],"lastModifiedDate":"2022-06-29T21:04:56.044969","indexId":"ofr200337","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2003-37","title":"The New Albany Shale petroleum system, Illinois basin - Data and map image archive from the material-balance assessment","docAbstract":"The data files and explanations presented in this report were used to generate published material-balance approach estimates of amounts of petroleum 1) expelled from a source rock, and the sum of 2) petroleum discovered in-place plus that lost due to 3) secondary migration within, or leakage or erosion from a petroleum system. This study includes assessment of cumulative production, known petroleum volume, and original oil in place for hydrocarbons that were generated from the New Albany Shale source rocks. More than 4.00 billion barrels of oil (BBO) have been produced from Pennsylvanian-, Mississippian-, Devonian-, and Silurian-age reservoirs in the New Albany Shale petroleum system. Known petroleum volume is 4.16 BBO; the average recovery factor is 103.9% of the current cumulative production. Known petroleum volume of oil is 36.22% of the total original oil in place of 11.45 BBO. More than 140.4 BBO have been generated from the Upper Devonian and Lower Mississippian New Albany Shale in the Illinois Basin. Approximately 86.29 billion barrels of oil that was trapped south of the Cottage Grove fault system were lost by erosion of reservoir intervals. The remaining 54.15 BBO are 21% of the hydrocarbons that were generated in the basin and are accounted for using production data. Included in this publication are 2D maps that show the distribution of production for different formations versus the Rock-Eval pyrolysis hydrogen-indices (HI) contours, and 3D images that show the close association between burial depth and HI values.The primary vertical migration pathway of oil and gas was through faults and fractures into overlying reservoir strata. About 66% of the produced oil is located within the generative basin, which is outlined by an HI contour of 400. The remaining production is concentrated within 30 miles (50 km) outside the 400 HI contour. The generative basin is subdivided by contours of progressively lower hydrogen indices that represent increased levels of thermal maturity and generative capacity of New Albany Shale source rocks. The generative basin was also divided into seven oil-migration catchments. The catchments were determined using a surface-flow hydrologic model with contoured HI values as input to the model.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr200337","usgsCitation":"Higley, D.K., Henry, M.E., Lewan, M.D., and Pitman, J.K., 2003, The New Albany Shale petroleum system, Illinois basin - Data and map image archive from the material-balance assessment (Supersedes Open-File Report 01-162): U.S. Geological Survey Open-File Report 2003-37, HTML Document, https://doi.org/10.3133/ofr200337.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":178241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402720,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54654.htm","linkFileType":{"id":5,"text":"html"}},{"id":4596,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-037/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Illinois, Indiana","otherGeospatial":"Illinois basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.219970703125,\n 37.75334401310656\n ],\n [\n -86.11083984375,\n 37.75334401310656\n ],\n [\n -86.11083984375,\n 40.84706035607122\n ],\n [\n -89.219970703125,\n 40.84706035607122\n ],\n [\n -89.219970703125,\n 37.75334401310656\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Supersedes Open-File Report 01-162","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad4d","contributors":{"authors":[{"text":"Higley, Debra K. 0000-0001-8024-9954 higley@usgs.gov","orcid":"https://orcid.org/0000-0001-8024-9954","contributorId":152663,"corporation":false,"usgs":true,"family":"Higley","given":"Debra","email":"higley@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":242349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henry, M. E.","contributorId":103734,"corporation":false,"usgs":true,"family":"Henry","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":242352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lewan, M. D.","contributorId":46540,"corporation":false,"usgs":true,"family":"Lewan","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":242350,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pitman, Janet K. 0000-0002-0441-779X jpitman@usgs.gov","orcid":"https://orcid.org/0000-0002-0441-779X","contributorId":767,"corporation":false,"usgs":true,"family":"Pitman","given":"Janet","email":"jpitman@usgs.gov","middleInitial":"K.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":242351,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":47770,"text":"wri024299 - 2003 - Estimating the magnitude of the 100-year peak flow in the Big Lost River at the Idaho National Engineering and Environmental Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-12-06T12:02:45","indexId":"wri024299","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2002-4299","title":"Estimating the magnitude of the 100-year peak flow in the Big Lost River at the Idaho National Engineering and Environmental Laboratory, Idaho","docAbstract":"Accurate estimates of peak flows in the Big\nLost River at the Idaho National Engineering and\nEnvironmental Laboratory (INEEL) are needed to\nassist planners and managers with evaluating possible\neffects of flooding on facilities at the INEEL.\nA large difference of 4,350 cubic feet per second\n(ft3/s) between two previous estimates of the magnitude\nof the 100-year peak flow in the Big Lost\nRiver near the western boundary of the INEEL\nprompted the present study.\nRegression models that compared annual peak\nflows and attenuation of annual peak flows\nbetween successive gaging stations for the same\nflow event were used to estimate the magnitude of\nthe 100-year peak flow in the Big Lost River. The\n100-year peak flow of 4,790 ft3/s at the Howell\nRanch gaging station was used as the starting point\nfor this analysis. This estimate was determined by\nusing a three-parameter log-Pearson Type III distribution\nas outlined in “Guidelines for Determining\nFlood Flow Frequency” (Bulletin 17B by the\nInteragency Advisory Committee on Water Data).\nThe regression models indicated that, in the\nreach of the Big Lost River between Howell Ranch\nand Mackay Reservoir, downstream peak flows are\nlower than upstream peak flows. Peak-flow attenuation\nvalues for this reach of the river decreased\nnonlinearly as the magnitude of the peak flow\nincreased. Extrapolation of the trend resulted in an\nattenuation estimate of 13 percent for this reach\nrelative to the 100-year peak flow at the Howell\nRanch gaging station.\nIn the lower reach of the Big Lost River\nbetween Mackay Reservoir and Arco, downstream\npeak flows are also lower than upstream peak\nflows. However, in contrast to the upper reach,\npeak-flow attenuation values decreased linearly as\nthe magnitude of the peak flow increased. Extrapolation\nof the data indicated that peak-flow attenuations\nin this reach of the river approach zero for\nflows approaching the 100-year peak-flow estimate\nimmediately upstream and downstream from\nMackay Reservoir.\nA regression model of annual maximum daily\nmean flows between Arco and the INEEL diversion\ndam indicated that the attenuation values in\nthis reach of the river are nearly the same for all\nflows of record. Extrapolation of the linear regression\nof these values resulted in an attenuation estimate\nof 10 percent. Seepage measurements made\nduring 1951–53 also resulted in a loss estimate of\napproximately 10 percent. This attenuation value,\ncombined with the values from analyses of the\nupstream reaches, resulted in an estimate of the\n100-year peak flow for the Big Lost River immediately\nupstream from the INEEL diversion dam of\n3,750 ft3/s; upper and lower 95-percent confidence\nlimits were 6,250 ft3/s and 1,300 ft3/s, respectively.\nLocalized rainfall, even of high intensity, is\nnot likely to produce large peak flows at the\nINEEL because of high loss rates (infiltration,\nbank storage, and channel storage) along much of\nthe stream channel. The relatively short flow durations\nresulting from rainstorms historically have\nnot provided sufficient volumes of water to satisfy\nlocal storage demands (bank and channel storage).\nOnly after these storage demands are met do the\nloss rates decrease enough for significant peak\nflows to reach the INEEL site.\nAn uncertain component of the present analysis\nis the effect of seismic activity on the 100-year\npeak-flow estimate. Analysis of the effect of the\nmagnitude 7.3 Borah Peak earthquake in 1983 on normal flow conditions in the Big Lost River suggests\nthat the joint occurrence of a large earthquake\nand a 100-year peak flow could significantly\nincrease the magnitude of the peak flow at the\nINEEL.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024299","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Hortness, J., and Rousseau, J.P., 2003, Estimating the magnitude of the 100-year peak flow in the Big Lost River at the Idaho National Engineering and Environmental Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 2002-4299, v, 36 p., https://doi.org/10.3133/wri024299.","productDescription":"v, 36 p.","numberOfPages":"41","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":262364,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4299/report.pdf"},{"id":262365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4299/report-thumb.jpg"}],"scale":"100000","country":"United States","state":"Idaho","county":"Custer;Butte;Bingham;Jefferson","city":"Mackay;Leslie;Moore;Arco;Butte City","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.5332,43.3291 ], [ -114.5332,44.2975 ], [ -112.274,44.2975 ], [ -112.274,43.3291 ], [ -114.5332,43.3291 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc32e","contributors":{"authors":[{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":236197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rousseau, Joseph P.","contributorId":22030,"corporation":false,"usgs":true,"family":"Rousseau","given":"Joseph","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":236198,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44601,"text":"wri024084 - 2003 - Occurrence and temporal variability of methyl tert-butyl ether (MTBE) and other volatile organic compounds in select sources of drinking water : results of the focused survey","interactions":[],"lastModifiedDate":"2018-05-16T10:41:55","indexId":"wri024084","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2002-4084","title":"Occurrence and temporal variability of methyl tert-butyl ether (MTBE) and other volatile organic compounds in select sources of drinking water : results of the focused survey","docAbstract":"The large-scale use of the gasoline oxygenate methyl tert-butyl ether (MTBE), and its high solubility, low soil adsorption, and low biodegradability, has resulted in its detection in ground water and surface water in many places throughout the United States. Studies by numerous researchers, as well as many State and local environmental agencies, have discovered high levels of MTBE in soils and ground water at leaking underground gasoline-storage-tank sites and frequent occurrence of low to intermediate levels of MTBE in reservoirs used for both public water supply and recreational boating.
In response to these findings, the American Water Works Association Research Foundation sponsored an investigation of MTBE and other volatile organic compounds (VOCs) in the Nation's sources of drinking water. The goal of the investigation was to provide additional information on the frequency of occurrence, concentration, and temporal variability of MTBE and other VOCs in source water used by community water systems (CWSs). The investigation was completed in two stages: (1) reviews of available literature and (2) the collection of new data. Two surveys were associated with the collection of new data. The first, termed the Random Survey, employed a statistically stratified design for sampling source water from 954 randomly selected CWSs. The second, which is the focus of this report, is termed the Focused Survey, which included samples collected from 134 CWS source waters, including ground water, reservoirs, lakes, rivers, and streams, that were suspected or known to contain MTBE. The general intent of the Focused Survey was to compare results with the Random Survey and provide an improved understanding of the occurrence, concentration, temporal variability, and anthropogenic factors associated with frequently detected VOCs.
Each sample collected was analyzed for 66 VOCs, including MTBE and three other ether gasoline oxygenates (hereafter termed gasoline oxygenates). As part of the Focused Survey, 451 source-water samples and 744 field quality-control (QC) samples were collected from 78 ground-water, 39 reservoir and (or) lake, and 17 river and (or) stream source waters at fixed intervals for a period of 1 year.
Using a common assessment level of 0.2 μg/L (micrograms per liter) (2.0 μg/L for methyl ethyl ketone), 37 of the 66 VOCs analyzed were detected in both surveys. However, VOCs, especially MTBE and other gasoline oxygenates, were detected more frequently in the Focused Survey than in the Random Survey. MTBE was detected in 55.5 percent of the CWSs sampled in the Focused Survey and in 8.7 percent of those sampled in the Random Survey. Little difference in occurrence, however, was observed for trihalomethanes (THMs), which were detected in 16.4 and 14.8 percent of Focused Survey and Random Survey CWSs, respectively. This may indicate a pervasive occurrence of THMs in several source-water types, regardless of CWS size or geographic location.
Using data at or above the method detection limit to assess temporal variability and anthropogenic factors associated with frequent detection of select VOCs, concentrations in the Focused Survey in ground-water, reservoir, and river source waters were typically less than 1 μg/L. Also, at a 95-percent confidence interval, no statistically significant differences were observed in comparing concentrations in the first and second ground-water sample. A weak seasonal pattern was observed in samples collected from reservoirs and lakes where gasoline oxygenates and other gasoline compounds were detected more frequently during spring and summer, presumedly a result of increased use of motorized watercraft during these seasons. In contrast, seasonal patterns were not observed in samples collected from rivers and streams. The lack of seasonal differences in river and stream source waters sampled may indicate a common and continuous source of contamination.
The most frequently detected VOC (MTBE) and the two most frequently occurring subgroups of VOCs (gasoline oxygenates and THMs) detected in CWS source waters were further characterized to evaluate some anthropogenic factors that may better explain their frequent occurrence. Gasoline oxygenates were detected in 73.9 percent of all CWSs sampled. The concentration of gasoline oxygenates was slightly correlated with watercraft use on reservoirs inside MTBE high-use areas (r2=0.3783) but not outside of these areas (r2=0.0242). In general, the concentration of gasoline oxygenates increased as watercraft use increased. THMs were detected in 47.8 percent of the CWSs supplied by surface water. The frequent occurrence of THMs in reservoir source waters was determined to be an artifact of disinfection and the recycling of chlorinated water to these reservoirs. All CWSs with frequent occurrence of THMs served by a reservoir indicated that chlorine was added to waters for various reasons and that the chlorinated water was then released back to,
or upstream of, the reservoir or lake that was sampled.
Director, Dakota Water Science Center, South Dakota Office
U.S. Geological Survey
1608 Mountain View Road
Rapid City, SD 57702
The 13 major south-shore streams in Nassau and Suffolk Counties, Long Island, New York with adequate long-term (1971-97) water-quality records, and 192 south-shore wells with sufficient water-quality data, were selected for analysis of geographic, seasonal, and long-term trends in nitrogen concentration. Annual total nitrogen loads transported to the South Shore Estuary Reserve (SSER) from 11 of these streams were calculated using long-term discharge records. Nitrogen loads from shallow and deep ground water also were calculated using simulated ground-water discharge of 1968-83 hydrologic conditions.
Long-term declines in stream discharge occurred in East Meadow Brook, Bellmore Creek and Massapequa Creek in response to extensive sewering in Nassau County. The smallest longterm annual discharge to the SSER was from the westernmost stream, Pines Brook, which is in an area in which the water table has been lowered by sewers since 1952. The three largest average annual discharges to the SSER were from the Connetquot River, Carlls River, and Carmans River in Suffolk County; the discharges from each of these streams were at least twice those of the other streams considered in this study.
Total nitrogen concentrations in streams show a geographic trend with a general eastward increase in median total nitrogen concentration in Nassau County and a decreasing trend from Massapequa Creek eastward into Suffolk County. Total nitrogen concentrations in streams generally are lowest during summer and highest in winter as a result of seasonal fluctuations in chemical reactions and biological activity. The greatest seasonal difference in median total nitrogen concentration was at Carlls River with values of 3.4 and 4.2 mg/L (milligrams per liter) as N during summer (April through September) and winter (October through March), respectively. Streams affected by the completion of sewer districts show long-term (1971-97) trends of decreasing total nitrogen concentration and streams showing an increase in total nitrogen concentration are in unsewered areas with increased urbanization.
Discharges from shallow ground water (upper glacial aquifer) and deep ground water (upper part of Magothy aquifer) were simulated from a ground-water-flow model calibrated to steadystate (1968-83) conditions. Simulated discharges from shallow-ground-water system in Nassau County were 10,700 Mgal/yr (million gallons per year) or 40,500,000 m3/yr (cubic meters per year), and those from Suffolk County were 52,300 Mgal/yr or 198,000,000 m3/yr. Discharges from deep-ground-water system in Nassau County were 4,900 Mgal/yr or 18,500,000 m3/yr, and those in Suffolk County were 12,700 Mgal/yr or 48,200,000 m3/yr.
Ground-water concentrations of nitrogen decrease with depth and from west to east. The shallow ground water median nitrogen concentration for each county was determined using 1,155 samples collected at 167 shallow wells (125 feet deep or less) within 1 mile of the shore. The deep ground water median nitrate concentration (nitrate represented almost all of the total nitrogen) for each county was determined using 112 samples collected at 25 deep wells (greater than 125 feet deep) within 1 mile of the shore. The median nitrogen concentration for the shallow and median nitrate concentration for the deep ground water in Nassau County were 3.85 and 0.15 mg/L as N, during 1952–97; the corresponding concentrations for Suffolk County were 1.74 and <0.10 (less than 0.10) mg/L as N, during 1952–97.
Nitrogen loads discharged from streams to the SSER for each year during 1972–97 were calculated as the annual total nitrogen concentration multiplied by the annual discharge. These values were calculated only for the seven streams for which sufficient data were available. The largest long-term (1972–97) average annual nitrogen load from Carlls River was 104 ton/yr or 94,300 kg/yr—about twice that of Connetquot River (54 ton/yr or 48,900 kg/yr) and over three times that of Carmans River (33 ton/yr or 29,900 kg/yr). The smallest annual mean nitrogen load was from Pines Brook, which has the lowest annual mean discharge of all streams analyzed.
The nitrogen load carried to the SSER by ground-water discharge in shallow-ground-water system in Nassau and Suffolk Counties was calculated as the simulated discharge for each county multiplied by the respective median nitrogen concentration, and loads from deep-ground-water system were calculated as the simulated discharge for each county multiplied by the respective median nitrate concentration. All discharges were obtained from the U.S. Geological Survey's Long Island ground-water-flow model. The resultant nitrogen loads discharged to the SSER from shallow ground water were 172 ton/yr (156,000 kg/yr) from Nassau County and 380 ton/yr (345,000 kg/yr) from Suffolk County; equaling 552 ton/yr entering the SSER. Those from deep ground water were 3 ton/yr (2,700 kg/yr) from Nassau County and <0.5 ton/yr (480 kg/yr) from Suffolk County; equaling about 3.5 ton/yr entering the SSER.
The sum of both stream loads and groundwater loads results in the total load to the SSER. The largest calculated total nitrogen load entering the SSER from both streams and ground water occurred in 1979 with a total load of 1,260 ton/yr (1,140,000 kg/yr). The smallest calculated nitrogen load entering the SSER occurred in 1995 with a total load of 725 ton/yr (658,000 kg/yr).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri024255","collaboration":"Prepared in cooperation with the New York State Department of State","usgsCitation":"Monti, and Scorca, M.P., 2003, Trends in nitrogen concentration and nitrogen loads entering the South Shore Estuary Reserve from streams and ground-water discharge in Nassau and Suffolk counties, Long Island, New York, 1952–97: U.S. Geological Survey Water-Resources Investigations Report 2002-4255, v, 36 p., https://doi.org/10.3133/wri024255.","productDescription":"v, 36 p.","onlineOnly":"N","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":411008,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54607.htm","linkFileType":{"id":5,"text":"html"}},{"id":3694,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/2002/4255/wri20024255.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 2002-4255"},{"id":168541,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/2002/4255/coverthb.jpg"}],"country":"United States","state":"New York","county":"Nassau County, Suffolk County","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -72.5,\n 41.875\n ],\n [\n -73.7625,\n 41.875\n ],\n [\n -73.7625,\n 40.5861\n ],\n [\n -72.5,\n 40.5861\n ],\n [\n -72.5,\n 41.875\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"Director, New York Water Science Center
U.S. Geological Survey
425 Jordan Rd
Troy, NY 12180
(518) 285-5695
http://ny.water.usgs.gov/
As part of a national inventory program funded by the National Park Service, we conducted an inventory of marine and estuarine fishes in Glacier Bay National Park and Preserve, Wrangell-St. Elias National Park and Preserve, Sitka National Historical Park, and Klondike Gold Rush National Historical Park in 2001 and 2002. In addition, marine fish data from a previous project that focused on forage fishes and marine predators during 1999 and 2000 in Glacier Bay proper were compiled for this study. Sampling was conducted with modified herring and Isaacs-Kidd midwater trawls, a plumb staff beam trawl, and beach seines. Species lists of relative abundance were generated for nearshore fishes in all parks, and for demersal and pelagic fishes in Glacier Bay National Park and Preserve and Wrangell-St. Elias National Park and Preserve. With a total sampling effort of 531 sets, we captured 100 species in Glacier Bay National Park and Preserve, 31 species in Wrangell-St. Elias National Park and Preserve, 23 species in Sitka National Historical Park, and 11 species in Klondike Gold Rush National Historical Park. We estimated that between 59 and 85 percent of the total marine fish species present were sampled by us in the various habitat-park units. We also combined these data with historical records and prepared an annotated species list of 160 marine and estuarine fishes known to occur in Glacier Bay National Park and Preserve. Shannon-Wiener diversity index and catch per unit effort were used to assess the effects of depth and latitude (distance from tidewater glaciers) on marine fish community ecology in Glacier Bay proper. Our findings suggest that demersal fishes are more abundant and diverse with increased distance from tidewater glaciers, and that pelagic fishes sampled deeper than 50 m are more abundant in areas closer to tidewater glaciers.
In this article, we summarize our recent InSAR studies of 13 Alaska volcanoes, including New Trident, Okmok, Akutan, Kiska, Augustine, Westdahl, Peulik, Makushin, Seguam, Shishaldin, Pavlof, Cleveland, and Korovin volcanoes.
","language":"English","usgsCitation":"Lu, Z., Wicks, C., Dzurisin, D., Power, J.A., Thatcher, W.R., and Masterlark, T., 2003, Interferometric Synthetic Aperture radar studies of Alaska volcanoes: Earth Observation Magazine, v. 5, p. 8-18.","productDescription":"11 p.","startPage":"8","endPage":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":308200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55fa92bfe4b05d6c4e501a97","contributors":{"authors":[{"text":"Lu, Zhong 0000-0001-9181-1818 lu@usgs.gov","orcid":"https://orcid.org/0000-0001-9181-1818","contributorId":901,"corporation":false,"usgs":true,"family":"Lu","given":"Zhong","email":"lu@usgs.gov","affiliations":[],"preferred":true,"id":571371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wicks, Charles W. Jr.","contributorId":68169,"corporation":false,"usgs":true,"family":"Wicks","given":"Charles W.","suffix":"Jr.","affiliations":[],"preferred":false,"id":571372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":571373,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Power, John A. 0000-0002-7233-4398 jpower@usgs.gov","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":2768,"corporation":false,"usgs":true,"family":"Power","given":"John","email":"jpower@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":571374,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thatcher, Wayne R. 0000-0001-6324-545X thatcher@usgs.gov","orcid":"https://orcid.org/0000-0001-6324-545X","contributorId":2599,"corporation":false,"usgs":true,"family":"Thatcher","given":"Wayne","email":"thatcher@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":571375,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Masterlark, Timothy","contributorId":92829,"corporation":false,"usgs":false,"family":"Masterlark","given":"Timothy","email":"","affiliations":[{"id":35607,"text":"South Dakota School of Mines","active":true,"usgs":false}],"preferred":false,"id":571376,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":47812,"text":"fs15102 - 2003 - Kamchatskaia gruppa reagironvaniia na vulkanicheskie izverzheniia (KVERT) G [The Kamchatkan Volcanic Eruption Response Team (KVERT)]","interactions":[],"lastModifiedDate":"2017-05-19T18:51:32","indexId":"fs15102","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"151-02","title":"Kamchatskaia gruppa reagironvaniia na vulkanicheskie izverzheniia (KVERT) G [The Kamchatkan Volcanic Eruption Response Team (KVERT)]","language":"Russian","doi":"10.3133/fs15102","usgsCitation":"Kirianov, V.Y., Neal, C., Gordeev, E.I., and Miller, T.P., 2003, Kamchatskaia gruppa reagironvaniia na vulkanicheskie izverzheniia (KVERT) G [The Kamchatkan Volcanic Eruption Response Team (KVERT)]: U.S. Geological Survey Fact Sheet 151-02, 1 sheet ([2] p.) : col. ill., col. maps ; 28 cm., https://doi.org/10.3133/fs15102.","productDescription":"1 sheet ([2] p.) : col. ill., col. maps ; 28 cm.","costCenters":[],"links":[{"id":84663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2002/0151/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":125300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2002/0151/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b487f","contributors":{"authors":[{"text":"Kirianov, Vladimir Yu.","contributorId":51343,"corporation":false,"usgs":true,"family":"Kirianov","given":"Vladimir","email":"","middleInitial":"Yu.","affiliations":[],"preferred":false,"id":236288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neal, Christina A. 0000-0002-7697-7825","orcid":"https://orcid.org/0000-0002-7697-7825","contributorId":82660,"corporation":false,"usgs":true,"family":"Neal","given":"Christina A.","affiliations":[],"preferred":false,"id":236289,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gordeev, Evgenii I.","contributorId":36980,"corporation":false,"usgs":true,"family":"Gordeev","given":"Evgenii","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":236287,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":236286,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":50789,"text":"wri034054 - 2003 - Development of health-based screening levels for use in state- or local-scale water-quality assessments","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"wri034054","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2003-4054","title":"Development of health-based screening levels for use in state- or local-scale water-quality assessments","docAbstract":"The U.S. Geological Survey (USGS) has a need to communicate the significance of the water-quality findings of its National Water-Quality Assessment (NAWQA) Program in a human-health context. Historically, the USGS has assessed water-quality conditions by comparing water concentration\r\ndata against established drinking-water standards and guidelines. However, because drinking-\r\nwater standards and guidelines do not exist for many of the contaminants analyzed by the NAWQA Program and other USGS studies, this approach has proven to be insufficient for placing USGS data in a human-health context. To help meet this need, health-based screening level (HBSL) concentrations or ranges are being determined\r\nfor unregulated compounds (that is, those for which Federal or State drinking-water standards\r\nhave not been established), using a consensus approach that was developed collaboratively by the USGS, U.S. Environmental Protection Agency(USEPA), New Jersey Department of Environmental\r\nProtection, and Oregon Health & Science University. USEPA Office of Water methodologies for calculating Lifetime Health Advisory and Risk-Specific Dose values for drinking water are being used to develop HBSL concentrations (for unregulated noncarcinogens) and HBSL concentration\r\nranges (for most unregulated carcinogens). This report describes the methodologies used to develop HBSL concentrations and ranges for unregulated compounds in State- and local-scale analyses, and discusses how HBSL values can be used as tools in water-quality assessments. Comparisons\r\nof measured water concentrations with Maximum Contaminant Level values and HBSL values require that water-quality data be placed in the proper context, with regard to both hydrology and human health. The use of these HBSL concentrations\r\nand ranges by USGS will increase by 27 percent the number of NAWQA contaminants for which health-based benchmarks are available for comparison with USGS water-quality data. USGS can use HBSL values to assist the USEPA and State and local agencies by providing them with comparisons of measured water concentrations\r\nto scientifically defensible human health-based benchmarks, and by alerting them when measured concentrations approach or exceed these benchmarks.","language":"ENGLISH","doi":"10.3133/wri034054","usgsCitation":"Toccalino, P., Nowell, L., Wilber, W., Zogorski, J.S., Donohue, J., Eiden, C., Krietzman, S., and Post, G., 2003, Development of health-based screening levels for use in state- or local-scale water-quality assessments: U.S. Geological Survey Water-Resources Investigations Report 2003-4054, 31 p., https://doi.org/10.3133/wri034054.","productDescription":"31 p.","costCenters":[],"links":[{"id":4572,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri03-4054/","linkFileType":{"id":5,"text":"html"}},{"id":120599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_2003_4054.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de99","contributors":{"authors":[{"text":"Toccalino, Patricia L. 0000-0003-1066-1702","orcid":"https://orcid.org/0000-0003-1066-1702","contributorId":41089,"corporation":false,"usgs":true,"family":"Toccalino","given":"Patricia L.","affiliations":[{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":242310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowell, Lisa 0000-0001-5417-7264","orcid":"https://orcid.org/0000-0001-5417-7264","contributorId":69417,"corporation":false,"usgs":true,"family":"Nowell","given":"Lisa","affiliations":[],"preferred":false,"id":242314,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilber, William","contributorId":48439,"corporation":false,"usgs":true,"family":"Wilber","given":"William","affiliations":[],"preferred":false,"id":242311,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zogorski, John S. jszogors@usgs.gov","contributorId":189,"corporation":false,"usgs":true,"family":"Zogorski","given":"John","email":"jszogors@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":242307,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Donohue, Joyce","contributorId":7568,"corporation":false,"usgs":true,"family":"Donohue","given":"Joyce","email":"","affiliations":[],"preferred":false,"id":242308,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Eiden, Catherine","contributorId":63429,"corporation":false,"usgs":true,"family":"Eiden","given":"Catherine","email":"","affiliations":[],"preferred":false,"id":242313,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Krietzman, Sandra","contributorId":55276,"corporation":false,"usgs":true,"family":"Krietzman","given":"Sandra","affiliations":[],"preferred":false,"id":242312,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Post, Gloria","contributorId":34384,"corporation":false,"usgs":true,"family":"Post","given":"Gloria","affiliations":[],"preferred":false,"id":242309,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":47457,"text":"wri034042 - 2003 - Determination of upstream boundary points on southeastern Washington streams and rivers under the requirements of the Shoreline Management Act of 1971","interactions":[],"lastModifiedDate":"2012-02-02T00:10:38","indexId":"wri034042","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2003-4042","title":"Determination of upstream boundary points on southeastern Washington streams and rivers under the requirements of the Shoreline Management Act of 1971","docAbstract":"Regulation of the shorelines of the State of Washington, as mandated by the Shoreline Management Act of 1971, requires knowledge of the locations on streams and river reaches where specific regulatory criteria are satisfied. The U.S. Geological Survey conducted a study in 1971 to determine the upstream boundary points of these reaches for many of the State's streams and rivers. Updated upstream boundary points were determined in the current study for all the streams and rivers in southeastern Washington that fall under the jurisdiction of the Shoreline Management Act of 1971. Upstream boundary point locations where the mean annual discharge equals 20 cubic feet per second were determined for 149 streams. In addition, upstream boundary point locations where the mean annual discharge equals 200 cubic feet per second or the drainage area equals 300 square miles were determined for 22 rivers. \r\n\r\nBoundary point locations were determined by application of multiple-linear-regression equations that relate mean annual discharge to drainage area and mean annual precipitation. Southeastern Washington was divided into five hydrologically distinct regions, and a separate regression equation was developed for each region. The regression equations are based on data for gaging stations with at least 10 years of record. The number of stations in the regression analysis for each of the five regions ranged from 5 to 33. The coefficient of determination, R2, of the regression equations ranged from 0.953 to 0.997. The equation for the Upper Yakima region had the lowest standard error, ranging from -7 to +9 percent for a regression estimate of 20 cubic feet per second. The equation for the Columbia Basin to Palouse region had the highest standard error, ranging from -36 to +55 percent for a regression estimate of 20 cubic feet per second. The approximate error in the location of an upstream boundary point can be calculated using the variables mean annual precipitation of the basin upstream from a boundary point and average basin width in the vicinity of the boundary point. The calculation gives only a rough estimate of the error of the boundary point location, because of the uncertainty in estimating average basin width.","language":"ENGLISH","doi":"10.3133/wri034042","usgsCitation":"Higgins, J.L., 2003, Determination of upstream boundary points on southeastern Washington streams and rivers under the requirements of the Shoreline Management Act of 1971: U.S. Geological Survey Water-Resources Investigations Report 2003-4042, 18 p., 1 over-size sheet, https://doi.org/10.3133/wri034042.","productDescription":"18 p., 1 over-size sheet","costCenters":[],"links":[{"id":3984,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034042/","linkFileType":{"id":5,"text":"html"}},{"id":173317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db6269ec","contributors":{"authors":[{"text":"Higgins, Johnna L. jhiggins@usgs.gov","contributorId":3091,"corporation":false,"usgs":true,"family":"Higgins","given":"Johnna","email":"jhiggins@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":235420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":69685,"text":"mf2407F - 2003 - Map showing zinc concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada","interactions":[],"lastModifiedDate":"2022-05-09T19:15:22.905263","indexId":"mf2407F","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2407","chapter":"F","title":"Map showing zinc concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2407F","usgsCitation":"Yager, D.B., and Folger, H.W., 2003, Map showing zinc concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2407, 1 Plate: 42.78 × 41.10 inches, https://doi.org/10.3133/mf2407F.","productDescription":"1 Plate: 42.78 × 41.10 inches","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":191756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6354,"rank":300,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2003/mf-2407/MF-2407-F.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110413,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54729.htm","linkFileType":{"id":5,"text":"html"},"description":"54729"}],"scale":"500000","country":"United States","state":"California, Nevada","otherGeospatial":"Humboldt River basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,38 ], [ -120,42 ], [ -114,42 ], [ -114,38 ], [ -120,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69e3d8","contributors":{"authors":[{"text":"Yager, Douglas B. 0000-0001-5074-4022 dyager@usgs.gov","orcid":"https://orcid.org/0000-0001-5074-4022","contributorId":798,"corporation":false,"usgs":true,"family":"Yager","given":"Douglas","email":"dyager@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":280890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Folger, Helen W. 0000-0003-1376-5996 hfolger@usgs.gov","orcid":"https://orcid.org/0000-0003-1376-5996","contributorId":3219,"corporation":false,"usgs":true,"family":"Folger","given":"Helen","email":"hfolger@usgs.gov","middleInitial":"W.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":280891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":69634,"text":"i2785 - 2003 - Topographic map of the northwest Loire Valles region of Mars MTM 500k -15/337E OMKT","interactions":[],"lastModifiedDate":"2019-12-26T06:22:18","indexId":"i2785","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2785","displayTitle":"Topographic Map of the Northwest Loire Valles Region of Mars MTM 500k -15/337E OMKT","title":"Topographic map of the northwest Loire Valles region of Mars MTM 500k -15/337E OMKT","docAbstract":"This map, compiled photogrammetrically from Viking Orbiter stereo image pairs, is part of a series of topographic maps of areas of special scientific interest on Mars. MTM 500k –15/337E OMKT: Abbreviation for Mars Transverse Mercator; 1:500,000 series; center of sheet latitude 15° S., longitude 337.5° E. in planetocentric coordinate system (this corresponds to –15/022; latitude 15° S., longitude 22.5° W. in planetographic coordinate system); orthophotomosaic (OM) with color coded (K) topographic contours and nomenclature (T) [Greeley and Batson, 1990].
\nThe figure of Mars used for the computation of the map projection is an oblate spheroid (flattening of 1/176.875) with an equatorial radius of 3396.0 km and a polar radius of 3376.8 km (Kirk and others, 2000). The datum (the 0–km contour line) for elevations is defined as the equipotential surface (gravitational plus rotational) whose average value at the equator is equal to the mean radius as determined by Mars Orbiter Laser Altimeter (Smith and others, 2001).
\nThe image base for this map employs Viking Orbiter images from orbit 651. An orthophotomosaic was created on the digital photogrammetric workstation using the DTM compiled from stereo models. Integrated Software for Imagers and Spectrometers (ISIS) (Torson and Becker, 1997) provided the software to project the orthophotomosaic into the Transverse Mercator Projection.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i2785","collaboration":"Prepared for The National Aeronautics and Space Administration","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2003, Topographic map of the northwest Loire Valles region of Mars MTM 500k -15/337E OMKT: U.S. Geological Survey IMAP 2785, 1 Plate:: 28.00 x 40.00 inches; HTML, https://doi.org/10.3133/i2785.","productDescription":"1 Plate:: 28.00 x 40.00 inches; HTML","additionalOnlineFiles":"Y","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":191702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6287,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/2785/","linkFileType":{"id":5,"text":"html"}},{"id":280479,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2785/pdf/i2785map.pdf"},{"id":280480,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/imap/2785/pdf/i2785map.eps"}],"scale":"502000","projection":"Transverse Mercator Projection","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629bcc","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":69692,"text":"mf2407M - 2003 - Map showing lead concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada","interactions":[],"lastModifiedDate":"2022-05-09T19:10:57.229198","indexId":"mf2407M","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2407","chapter":"M","title":"Map showing lead concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2407M","usgsCitation":"Yager, D.B., and Folger, H.W., 2003, Map showing lead concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada (Version 1.0): U.S. Geological Survey Miscellaneous Field Studies Map 2407, 1 Plate: 42.78 × 41.33 inches, https://doi.org/10.3133/mf2407M.","productDescription":"1 Plate: 42.78 × 41.33 inches","costCenters":[],"links":[{"id":191924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6365,"rank":300,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2003/mf-2407/MF-2407-M.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110420,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54729.htm","linkFileType":{"id":5,"text":"html"},"description":"54729"}],"scale":"500000","country":"United States","state":"California, Nevada","otherGeospatial":"Humboldt River basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,38 ], [ -120,42 ], [ -114,42 ], [ -114,38 ], [ -120,38 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db65892a","contributors":{"authors":[{"text":"Yager, Douglas B. 0000-0001-5074-4022 dyager@usgs.gov","orcid":"https://orcid.org/0000-0001-5074-4022","contributorId":798,"corporation":false,"usgs":true,"family":"Yager","given":"Douglas","email":"dyager@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":280904,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Folger, Helen W. 0000-0003-1376-5996 hfolger@usgs.gov","orcid":"https://orcid.org/0000-0003-1376-5996","contributorId":3219,"corporation":false,"usgs":true,"family":"Folger","given":"Helen","email":"hfolger@usgs.gov","middleInitial":"W.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":280905,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":69686,"text":"mf2407G - 2003 - Map showing arsenic concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada","interactions":[],"lastModifiedDate":"2022-09-15T19:58:35.090337","indexId":"mf2407G","displayToPublicDate":"2003-05-01T00:00:00","publicationYear":"2003","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":"2407","chapter":"G","title":"Map showing arsenic concentrations from stream sediments and soils throughout the Humboldt River basin and surrounding areas, northern Nevada","docAbstract":"No abstract available.
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