{"pageNumber":"2413","pageRowStart":"60300","pageSize":"25","recordCount":184617,"records":[{"id":77385,"text":"ofr20051427 - 2006 - Extracting shorelines from NASA airborne topographic lidar-derived digital elevation models","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"ofr20051427","displayToPublicDate":"2006-07-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1427","title":"Extracting shorelines from NASA airborne topographic lidar-derived digital elevation models","docAbstract":"This report documents part of the National Park Service (NPS)/U.S. Geological Survey (USGS)/National Aeronautics and Space Administration (NASA) Aerial Data Collection and Creation of Products for Park Vital Signs Project. This report is one in a series that describes methods for extracting topographic features from aerial survey data as part of a joint project among the NPS Inventory and Monitoring (IM) Program, the NASA Observational Sciences Branch, and the USGS Center for Coastal and Watershed Studies (CCWS).","language":"ENGLISH","doi":"10.3133/ofr20051427","collaboration":"Metadata in Appendix 1","usgsCitation":"Harris, M., Brock, J., Nayegandhi, A., and Duffy, M., 2006, Extracting shorelines from NASA airborne topographic lidar-derived digital elevation models (Revised and reprinted): U.S. Geological Survey Open-File Report 2005-1427, iv, 32 p., https://doi.org/10.3133/ofr20051427.","productDescription":"iv, 32 p.","numberOfPages":"36","onlineOnly":"Y","costCenters":[{"id":159,"text":"Center for Coastal and Watershed Studies","active":false,"usgs":true}],"links":[{"id":195557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8360,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1427/","linkFileType":{"id":5,"text":"html"}}],"edition":"Revised and reprinted","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8a0e","contributors":{"authors":[{"text":"Harris, M.","contributorId":28207,"corporation":false,"usgs":true,"family":"Harris","given":"M.","affiliations":[],"preferred":false,"id":288520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brock, J. 0000-0002-5289-9332","orcid":"https://orcid.org/0000-0002-5289-9332","contributorId":71658,"corporation":false,"usgs":true,"family":"Brock","given":"J.","affiliations":[],"preferred":false,"id":288522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nayegandhi, A.","contributorId":95578,"corporation":false,"usgs":true,"family":"Nayegandhi","given":"A.","affiliations":[],"preferred":false,"id":288523,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duffy, M.","contributorId":62702,"corporation":false,"usgs":true,"family":"Duffy","given":"M.","affiliations":[],"preferred":false,"id":288521,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":77386,"text":"fs20063051 - 2006 - Along-Track Reef Imaging System (ATRIS)","interactions":[],"lastModifiedDate":"2014-10-09T13:42:23","indexId":"fs20063051","displayToPublicDate":"2006-07-28T00:00:00","publicationYear":"2006","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":"2006-3051","title":"Along-Track Reef Imaging System (ATRIS)","docAbstract":"\"Along-Track Reef Imaging System (ATRIS)\" describes the U.S. Geological Survey's Along-Track Reef Imaging System, a boat-based sensor package for rapidly mapping shallow water benthic environments. ATRIS acquires high resolution, color digital images that are accurately geo-located in real-time.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20063051","usgsCitation":"Brock, J., and Zawada, D., 2006, Along-Track Reef Imaging System (ATRIS): U.S. Geological Survey Fact Sheet 2006-3051, 4 p., https://doi.org/10.3133/fs20063051.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":159,"text":"Center for Coastal and Watershed Studies","active":false,"usgs":true}],"links":[{"id":120981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3051.jpg"},{"id":8361,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3051/","linkFileType":{"id":5,"text":"html"}},{"id":295169,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2006/3051/fs-2006-3051.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687875","contributors":{"authors":[{"text":"Brock, John","contributorId":39011,"corporation":false,"usgs":true,"family":"Brock","given":"John","affiliations":[],"preferred":false,"id":288524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zawada, Dave","contributorId":98403,"corporation":false,"usgs":true,"family":"Zawada","given":"Dave","email":"","affiliations":[],"preferred":false,"id":288525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":77394,"text":"ds69H4 - 2006 - Chapter 4: The GIS Project for the Geologic Assessment of Undiscovered Oil and Gas in the Upper Cretaceous Navarro and Taylor Groups, Western Gulf Province, Texas","interactions":[],"lastModifiedDate":"2018-08-28T16:43:05","indexId":"ds69H4","displayToPublicDate":"2006-07-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"69-H-4","title":"Chapter 4: The GIS Project for the Geologic Assessment of Undiscovered Oil and Gas in the Upper Cretaceous Navarro and Taylor Groups, Western Gulf Province, Texas","docAbstract":"A geographic information system (GIS) focusing on the Upper Cretaceous Navarro and Taylor Groups in the Gulf Coast region was developed as a visual-analysis tool for the U.S. Geological Survey's 2003 assessment of undiscovered, technically recoverable oil and natural gas resources in the Western Gulf Province. The Central Energy Resources Team of the U.S. Geological Survey has also developed an Internet Map Service to deliver the GIS data to the general public. This mapping tool utilizes information from a database about the oil and natural gas endowment of the United States - including physical locations of geologic and geographic data - and converts the data into visual layers. Portrayal and analysis of geologic features on an interactive map provide an excellent tool for understanding domestic oil and gas resources for strategic planning, formulating economic and energy policies, evaluating lands under the purview of the Federal Government, and developing sound environmental policies. Assessment results can be viewed and analyzed or downloaded from the internet web site.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum Systems and Geologic Assessment of Undiscovered Oil and Gas, Navarro and Taylor Groups, Western Gulf Province, Texas","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds69H4","isbn":"1411309987","usgsCitation":"Biewick, L., 2006, Chapter 4: The GIS Project for the Geologic Assessment of Undiscovered Oil and Gas in the Upper Cretaceous Navarro and Taylor Groups, Western Gulf Province, Texas: U.S. Geological Survey Data Series 69-H-4, Available online and on CD-ROM; GIS/Data/Metadata: 3 p., https://doi.org/10.3133/ds69H4.","productDescription":"Available online and on CD-ROM; GIS/Data/Metadata: 3 p.","numberOfPages":"3","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":174,"text":"Central Region Energy Resources Program","active":false,"usgs":true}],"links":[{"id":194560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11614,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/dds/dds-069/dds-069-h/REPORTS/69_H_CH_4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e69","contributors":{"authors":[{"text":"Biewick, Laura","contributorId":83148,"corporation":false,"usgs":true,"family":"Biewick","given":"Laura","affiliations":[],"preferred":false,"id":288548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":77384,"text":"ofr20051048 - 2006 - Geological interpretation of bathymetric and backscatter imagery of the sea floor off eastern Cape Cod, Massachusetts","interactions":[],"lastModifiedDate":"2025-08-01T13:08:21.938564","indexId":"ofr20051048","displayToPublicDate":"2006-07-28T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-1048","displayTitle":"Geological Interpretation of Bathymetric and Backscatter Imagery of the Sea Floor off Eastern Cape Cod, Massachusetts","title":"Geological interpretation of bathymetric and backscatter imagery of the sea floor off eastern Cape Cod, Massachusetts","docAbstract":"

The imagery, interpretive data layers, and data presented herein were derived from multibeam echo-sounder data collected off Eastern Cape Cod, Massachusetts, and from the stations occupied to verify these acoustic data. The basic data layers show sea-floor topography, sun-illuminated shaded relief, and backscatter intensity; interpretive layers show the distributions of surficial sediment and sedimentary environments. Presented verification data include new and historical sediment grain-size analyses and a gallery of still photographs of the seabed.

The multibeam data, which cover a narrow band of the sea floor extending from Provincetown around the northern tip of Cape Cod and south southeastward to off Monomoy Island, were collected during transits between concurrent mapping projects in the Stellwagen Bank National Marine Sanctuary (Valentine and others, 2001; Butman and others, 2004; and Valentine, 2005) and Great South Channel (Valentine and others, 2003a, b, c, d). Although originally collected to maximize the use of time aboard ship, these data provide a fundamental framework for research and management activities in this part of the Gulf of Maine (Noji and others, 2004), show the composition and terrain of the seabed, and provide information on sediment transport and benthic habitat. These data and interpretations also support ongoing modeling studies of the lower Cape’s aquifer system (Masterson, 2004) and of erosional hotspots along the Cape Cod National Seashore (List and others, 2006).

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051048","isbn":"0607971746","usgsCitation":"Poppe, L.J., Paskevich, V.F., Butman, B., Ackerman, S.D., Danforth, W.W., Foster, D.S., and Blackwood, D.S., 2006, Geological interpretation of bathymetric and backscatter imagery of the sea floor off eastern Cape Cod, Massachusetts: U.S. Geological Survey Open-File Report 2005-1048, HTML Document, https://doi.org/10.3133/ofr20051048.","productDescription":"HTML Document","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":8359,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1048/","text":"Index Page","linkFileType":{"id":5,"text":"html"}},{"id":194609,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"projection":"Mercator WGS 84","country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\"crs\": {\"type\": \"name\", \"properties\": {\"name\": \"urn:ogc:def:crs:OGC:1.3:CRS84\"}}, \"geometry\": {\"type\": \"Polygon\", \"coordinates\": [[[-70.20693076362545, 42.09428635936738], [-70.24006610430234, 42.08205026605975], [-70.24887609148374, 42.0629619605001], [-70.23566111071159, 42.0443630986726], [-70.20727337423807, 42.022338130718914], [-70.18475896255222, 42.01891202459283], [-70.16322343833092, 42.03261644909723], [-70.18035396896153, 42.04534198613719], [-70.15343456368481, 42.04044754881418], [-70.14560346396803, 42.02919034297114], [-70.18573785001684, 41.99933427530071], [-70.2009106057182, 41.99835538783611], [-70.23468222324699, 42.00961259367898], [-70.26258051598818, 42.03065867416801], [-70.30026768337547, 42.07764527246906], [-70.29977823964316, 42.08988136577652], [-70.28166882154801, 42.076666385004486], [-70.25768607866519, 42.10211745908418], [-70.24104499176696, 42.10701189640718], [-70.08344410996568, 42.11337466492704], [-70.06092969827972, 42.11190633373018], [-69.93073766548743, 42.0673669540908], [-70.06141914201214, 42.109459115068645], [-70.19307950600131, 42.105054121478005], [-70.13341631503373, 42.09575469056432], [-70.04874254934543, 42.064430291697036], [-70.0228020315335, 42.04044754881418], [-70.00713983209977, 42.03800033015249], [-69.95330102154651, 41.98367207586717], [-69.93029716612841, 41.93228048397541], [-69.83681341325872, 41.61512094544357], [-69.85834893748, 41.62148371396369], [-69.94850447297, 41.9254282717231], [-69.97836054064038, 41.98611929452846], [-70.05177710048577, 42.05757807944462], [-70.13351420378011, 42.09086025324132], [-70.20693076362545, 42.09428635936738]]]}, \"properties\": {\"extentType\": \"Custom\", \"code\": \"\", \"name\": \"\", \"notes\": \"\", \"promotedForReuse\": false, \"abbreviation\": \"\", \"shortName\": \"\", \"description\": \"\"}, \"bbox\": [-70.30026768337547, 41.61512094544357, -69.83681341325872, 42.11337466492704], \"type\": \"Feature\", \"id\": \"3091871\"}","contact":"

Contact Pubs Warehouse

","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fd6","contributors":{"authors":[{"text":"Poppe, Larry J.","contributorId":55913,"corporation":false,"usgs":true,"family":"Poppe","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":288517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Paskevich, Valerie F.","contributorId":81907,"corporation":false,"usgs":true,"family":"Paskevich","given":"Valerie","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":288519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":288513,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ackerman, Seth D. 0000-0003-0945-2794 sackerman@usgs.gov","orcid":"https://orcid.org/0000-0003-0945-2794","contributorId":178676,"corporation":false,"usgs":true,"family":"Ackerman","given":"Seth","email":"sackerman@usgs.gov","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":288516,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Danforth, William W. 0000-0002-6382-9487 bdanforth@usgs.gov","orcid":"https://orcid.org/0000-0002-6382-9487","contributorId":3292,"corporation":false,"usgs":true,"family":"Danforth","given":"William","email":"bdanforth@usgs.gov","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":288515,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Foster, Dave S.","contributorId":80371,"corporation":false,"usgs":true,"family":"Foster","given":"Dave","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":288518,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Blackwood, Dann S. dblackwood@usgs.gov","contributorId":2457,"corporation":false,"usgs":true,"family":"Blackwood","given":"Dann","email":"dblackwood@usgs.gov","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":288514,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":77365,"text":"sim2926 - 2006 - Topographic map of the western region of Dao Vallis in Hellas Planitia, Mars; MTM 500k -40/082E OMKT","interactions":[],"lastModifiedDate":"2019-12-30T16:08:50","indexId":"sim2926","displayToPublicDate":"2006-07-27T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2926","title":"Topographic map of the western region of Dao Vallis in Hellas Planitia, Mars; MTM 500k -40/082E 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. Contours were derived from a digital terrain model (DTM) compiled on a digital photogrammetric workstation using Viking Orbiter stereo image pairs with orientation parameters derived from an analytic aerotriangulation. The image base for this map employs Viking Orbiter images from orbits 406 and 363. An orthophotomosaic was created on the digital photogrammetric workstation using the DTM compiled from stereo models.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim2926","usgsCitation":"Rosiek, M.R., Redding, B.L., and Galuszka, D.M., 2006, Topographic map of the western region of Dao Vallis in Hellas Planitia, Mars; MTM 500k -40/082E OMKT: U.S. Geological Survey Scientific Investigations Map 2926, HTML, https://doi.org/10.3133/sim2926.","productDescription":"HTML","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":192625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8342,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/sim/2006/2926/version_history.txt","linkFileType":{"id":2,"text":"txt"}},{"id":8341,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2006/2926/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f822f","contributors":{"authors":[{"text":"Rosiek, Mark R. mrosiek@usgs.gov","contributorId":824,"corporation":false,"usgs":true,"family":"Rosiek","given":"Mark","email":"mrosiek@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":288494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redding, Bonnie L. 0000-0001-8178-1467 bredding@usgs.gov","orcid":"https://orcid.org/0000-0001-8178-1467","contributorId":4798,"corporation":false,"usgs":true,"family":"Redding","given":"Bonnie","email":"bredding@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":288496,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galuszka, Donna M. 0000-0003-1870-1182 dgaluszka@usgs.gov","orcid":"https://orcid.org/0000-0003-1870-1182","contributorId":3186,"corporation":false,"usgs":true,"family":"Galuszka","given":"Donna","email":"dgaluszka@usgs.gov","middleInitial":"M.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":288495,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":77363,"text":"wdrAK051 - 2006 - Water resources data, Alaska, water year 2005","interactions":[],"lastModifiedDate":"2016-06-09T11:44:43","indexId":"wdrAK051","displayToPublicDate":"2006-07-27T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AK-05-1","title":"Water resources data, Alaska, water year 2005","docAbstract":"

Water resources data for the 2005 water year for Alaska consist of records of stage, discharge, and water quality of streams; stages of lakes; and water levels and water quality of ground water. This volume contains records for water discharge at 114 gaging stations; stage or contents only at 3 gaging stations; water quality at 37 gaging stations; and water levels for 41 observation wells. Also included are data for 55 crest-stage partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements and analyses. Some data collected during 2005 will be published in subsequent reports. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Alaska.

","language":"English","doi":"10.3133/wdrAK051","usgsCitation":"Jackson, M.L., Castor, M., Goetz, J., Solin, G., and Wiles, J., 2006, Water resources data, Alaska, water year 2005: U.S. Geological Survey Water Data Report AK-05-1, 509 p., https://doi.org/10.3133/wdrAK051.","productDescription":"509 p.","numberOfPages":"509","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":190531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8339,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-ak-05-1/index.php","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -179,54.75 ], [ -179,71.35 ], [ -130,71.35 ], [ -130,54.75 ], [ -179,54.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1573","contributors":{"authors":[{"text":"Jackson, Melanie L.","contributorId":34548,"corporation":false,"usgs":true,"family":"Jackson","given":"Melanie","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288484,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Castor, M.E.","contributorId":89611,"corporation":false,"usgs":true,"family":"Castor","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":288486,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goetz, J.M.","contributorId":106206,"corporation":false,"usgs":true,"family":"Goetz","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":288488,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Solin, G. L.","contributorId":106132,"corporation":false,"usgs":true,"family":"Solin","given":"G. L.","affiliations":[],"preferred":false,"id":288487,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wiles, J.M.","contributorId":60720,"corporation":false,"usgs":true,"family":"Wiles","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":288485,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":77366,"text":"wdrFL051A - 2006 - Water resources data, Florida, water year 2005. Volume 1A: northeast Florida - Surface water","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"wdrFL051A","displayToPublicDate":"2006-07-27T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-05-1A","title":"Water resources data, Florida, water year 2005. Volume 1A: northeast Florida - Surface water","docAbstract":"Water resources data for the 2005 water year in Florida consist of continuous or daily discharge for 429 streams, periodic discharge for 9 streams, continuous or daily stage for 218 streams, periodic stage for 5 streams, peak stage and discharge for 28 streams; continuous or daily elevations for 15 lakes, periodic elevations for 23 lakes; continuous ground-water levels for 401 wells, periodic ground-water levels for 1,098 wells; quality-of-water data for 211 surface-water sites and 208 wells.\r\n\r\nThe data for northeast Florida include continuous or daily discharge for 140 streams, periodic discharge for 4 streams, continuous or daily stage for 58 streams, periodic stage for 3 streams; peak stage and discharge for 0 streams; continuous or daily elevations for 10 lakes, periodic elevations for 20 lakes; continuous ground water levels for 45 wells, periodic ground-water levels for 520 wells; quality-of-water data for 40 surface-water sites and 65 wells.\r\n\r\nThese data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State and Federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL051A","usgsCitation":"Nazarian, A., Simonds, E., and Dickerson, S., 2006, Water resources data, Florida, water year 2005. Volume 1A: northeast Florida - Surface water: U.S. Geological Survey Water Data Report FL-05-1A, 419 p., https://doi.org/10.3133/wdrFL051A.","productDescription":"419 p.","numberOfPages":"419","onlineOnly":"Y","temporalStart":"2004-10-01","temporalEnd":"2005-09-30","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":192730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8343,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2005/wdr-fl-05-1a/pdf/volume1a05.pdf","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.63333333333334,24.55 ], [ -87.63333333333334,31 ], [ -80,31 ], [ -80,24.55 ], [ -87.63333333333334,24.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f65f","contributors":{"authors":[{"text":"Nazarian, A.P.","contributorId":32595,"corporation":false,"usgs":true,"family":"Nazarian","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":288499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simonds, E.P.","contributorId":31479,"corporation":false,"usgs":true,"family":"Simonds","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":288498,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dickerson, S.M.","contributorId":26748,"corporation":false,"usgs":true,"family":"Dickerson","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":288497,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":77367,"text":"sir20065119 - 2006 - Organochlorine compounds and current-use pesticides in snow and lake sediment in Rocky Mountain National Park, Colorado, and Glacier National Park, Montana, 2002-03","interactions":[],"lastModifiedDate":"2023-01-12T19:58:54.300184","indexId":"sir20065119","displayToPublicDate":"2006-07-27T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5119","title":"Organochlorine compounds and current-use pesticides in snow and lake sediment in Rocky Mountain National Park, Colorado, and Glacier National Park, Montana, 2002-03","docAbstract":"

Organochlorine compounds and current-use pesticides were measured in snow and lake-sediment samples from Rocky Mountain National Park in Colorado and Glacier National Park in Montana to determine their occurrence and distribution in high-elevation aquatic ecosystems. The U.S. Geological Survey, in cooperation with the National Park Service, collected snow samples at eight sites in Rocky Mountain National Park and at eight sites in Glacier National Park during spring of 2002 and 2003 just prior to the start of snowmelt. Surface sediments were collected from 11 lakes in Rocky Mountain National Park and 10 lakes in Glacier National Park during summer months of 2002 and 2003. Samples were analyzed for organochlorine compounds by gas chromatography with electron-capture detection and current-use pesticides by gas chromatography with electron-impact mass spectrometry. A subset of samples was reanalyzed using a third instrumental technique (gas chromatography with electron-capture negative ion mass spectrometry) to verify detected concentrations in the initial analysis and to investigate the presence of additional compounds.

For the snow samples, the pesticides most frequently detected were endosulfan, dacthal, and chlorothalonil, all of which are chlorinated pesticides that currently are registered for use in North America. Concentrations of these pesticides in snow were very low, ranging from 0.07 to 2.36 nanograms per liter. Of the historical-use pesticides, hexachlorobenzene, dieldrin, and trans-nonachlor were detected in snow but only in one sample each. Annual deposition rates of dacthal, endosulfan, and chlorothalonil were estimated at 0.7 to 3.0 micrograms per square meter. These estimates are likely biased low because they do not account for pesticide deposition during summer months.

For the lake-sediment samples, DDE (p,p’-dichlorodiphenyldichoroethene) and DDD (p,p’-dichlorodiphenyldichoroethane) were the most frequently detected organochlorine compounds. DDE and DDD are degradation products of DDT (p,p’-dichlorodiphenyltrichloroethane), which is a well-documented, persistent organochlorine insecticide that has been banned from use in the United States since 1972. Detected concentrations were very low, ranging from 0.12 to 4.7 micrograms per kilogram, and probably pose little threat to aquatic organisms in park lakes. DDD and DDE concentrations in a sediment core from Mills Lake in Rocky Mountain National Park indicate that atmospheric deposition of DDT and possibly other banned organochlorine compounds to high-elevation parks has been in decline since the 1970s. Commonly detected current-use pesticides in lake sediments included dacthal and endosulfan sulfate, which ranged in concentrations from 0.11 to 0.26 micrograms per kilogram for dacthal and 0.12 to 1.2 micrograms per kilogram for endosulfan sulfate. Both compounds were found in nearly all the snow samples, confirming that some current-use pesticides entering high-elevation aquatic ecosystems through atmospheric deposition are accumulating in lake sediments and potentially in aquatic biota.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065119","usgsCitation":"Mast, M.A., Foreman, W., and Skaates, S.V., 2006, Organochlorine compounds and current-use pesticides in snow and lake sediment in Rocky Mountain National Park, Colorado, and Glacier National Park, Montana, 2002-03: U.S. Geological Survey Scientific Investigations Report 2006-5119, vii, 54 p., https://doi.org/10.3133/sir20065119.","productDescription":"vii, 54 p.","numberOfPages":"61","onlineOnly":"Y","temporalStart":"2002-01-01","temporalEnd":"2003-12-31","costCenters":[],"links":[{"id":192463,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411794,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77301.htm","linkFileType":{"id":5,"text":"html"}},{"id":8345,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5119/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado, Montana","otherGeospatial":"Glacier National Park, Rocky Mountain National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.22256720949133,\n 48.42527317084483\n ],\n [\n -113.60607467424119,\n 48.98767176533735\n ],\n [\n -114.46541547488484,\n 49.00631018985513\n ],\n [\n -114.06770402995883,\n 48.462962021557644\n ],\n [\n -113.8333383570563,\n 48.49121030765991\n ],\n [\n -113.66289059494495,\n 48.32148460342714\n ],\n [\n -113.51374880309766,\n 48.21748443055691\n ],\n [\n -113.23677118966748,\n 48.42527317084483\n ],\n [\n -113.22256720949133,\n 48.42527317084483\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.4967089015192,\n 40.42709838882743\n ],\n [\n -105.52630465803442,\n 40.51920025263945\n ],\n [\n -105.54513832127122,\n 40.50692730356354\n ],\n [\n -105.601639310982,\n 40.535560690296165\n ],\n [\n -105.650068730734,\n 40.535560690296165\n ],\n [\n -105.69580762716637,\n 40.551917133974\n ],\n [\n -105.7549991401968,\n 40.51920025263945\n ],\n [\n -105.8895253061748,\n 40.46395429350568\n ],\n [\n -105.94871681920492,\n 40.43529033632856\n ],\n [\n -105.91912106268971,\n 40.37587611024372\n ],\n [\n -105.87607268957704,\n 40.36767692905849\n ],\n [\n -105.84647693306182,\n 40.30615127622238\n ],\n [\n -105.82495274650532,\n 40.2445695305361\n ],\n [\n -105.82226222318565,\n 40.17470910074675\n ],\n [\n -105.7549991401968,\n 40.127409750014664\n ],\n [\n -105.73347495364031,\n 40.07801879133493\n ],\n [\n -105.59087721770358,\n 40.05125038564955\n ],\n [\n -105.56128146118868,\n 40.08007746379681\n ],\n [\n -105.57742460110582,\n 40.125352509318134\n ],\n [\n -105.54782884459091,\n 40.13358109854124\n ],\n [\n -105.52630465803442,\n 40.2486767249583\n ],\n [\n -105.4967089015192,\n 40.42914646925706\n ],\n [\n -105.4967089015192,\n 40.42709838882743\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a834","contributors":{"authors":[{"text":"Mast, M. Alisa 0000-0001-6253-8162 mamast@usgs.gov","orcid":"https://orcid.org/0000-0001-6253-8162","contributorId":827,"corporation":false,"usgs":true,"family":"Mast","given":"M.","email":"mamast@usgs.gov","middleInitial":"Alisa","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foreman, William T. wforeman@usgs.gov","contributorId":1473,"corporation":false,"usgs":true,"family":"Foreman","given":"William T.","email":"wforeman@usgs.gov","affiliations":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"preferred":false,"id":288501,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Skaates, Serena V.","contributorId":18070,"corporation":false,"usgs":true,"family":"Skaates","given":"Serena","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":288502,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":77383,"text":"ds146 - 2006 - usSEABED: Gulf of Mexico and Caribbean (Puerto Rico and U.S. Virgin Islands) offshore surficial sediment data release","interactions":[],"lastModifiedDate":"2022-12-19T19:23:08.622181","indexId":"ds146","displayToPublicDate":"2006-07-27T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"146","title":"usSEABED: Gulf of Mexico and Caribbean (Puerto Rico and U.S. Virgin Islands) offshore surficial sediment data release","docAbstract":"

Over the past 50 years there has been an explosion in scientific interest, research effort and information gathered on the geologic sedimentary character of the United States continental margin. Data and information from thousands of publications have greatly increased our scientific understanding of the geologic origins of the shelf surface but rarely have those data been combined and integrated.

\n
\n

This publication is the first release of the Gulf of Mexico and Caribbean (Puerto Rico and U.S. Virgin Islands) coastal and offshore data from the usSEABED database. The report contains a compilation of published and previously unpublished sediment texture and other geologic data about the sea floor from diverse sources. usSEABED is an innovative database system developed to bring assorted data together in a unified database. The dbSEABED system is used to process the data. Examples of maps displaying attributes such as grain size and sediment color are included. This database contains information that is a scientific foundation for the USGS Marine Aggregate Resources and Processes Assessment and Benthic Habitats projects, and will be useful to the marine science community for other studies of the Gulf of Mexico and Caribbean continental margins.

\n
\n

This publication is divided into ten sections: Home, Introduction, Content, usSEABED (data), dbSEABED (processing), Data Catalog, References, Contacts, Acknowledgments and Frequently Asked Questions. Use the navigation bar on the left to navigate to specific sections of this report. Underlined topics throughout the publication are links to more information. Links to specific and detailed information on processing and those to pages outside this report will open in a new browser window.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds146","usgsCitation":"Buczkowski, B., Reid, J.A., Jenkins, C.J., Reid, J.M., Williams, S.J., and Flocks, J.G., 2006, usSEABED: Gulf of Mexico and Caribbean (Puerto Rico and U.S. Virgin Islands) offshore surficial sediment data release (Version 1.0): U.S. Geological Survey Data Series 146, Report: 50 p.; Spatial Data, https://doi.org/10.3133/ds146.","productDescription":"Report: 50 p.; Spatial Data","numberOfPages":"50","additionalOnlineFiles":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true},{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":194887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ds146.PNG"},{"id":8354,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ds/2006/146/images/pdf/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":8353,"rank":3,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/ds/2006/146/htmldocs/data_cata.htm","linkFileType":{"id":5,"text":"html"}},{"id":8352,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/2006/146/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Caribbean Sea, Gulf of Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -96.32137114540356,\n 28.69625797863533\n ],\n [\n -96.32137114540356,\n 10.54986233515379\n ],\n [\n -58.46737804409631,\n 10.54986233515379\n ],\n [\n -58.46737804409631,\n 28.69625797863533\n ],\n [\n -96.32137114540356,\n 28.69625797863533\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991c4","contributors":{"authors":[{"text":"Buczkowski, Brian J.","contributorId":40299,"corporation":false,"usgs":true,"family":"Buczkowski","given":"Brian J.","affiliations":[],"preferred":false,"id":288511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reid, Jane A. 0000-0003-1771-3894 jareid@usgs.gov","orcid":"https://orcid.org/0000-0003-1771-3894","contributorId":2826,"corporation":false,"usgs":true,"family":"Reid","given":"Jane","email":"jareid@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":288509,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenkins, Chris J.","contributorId":14066,"corporation":false,"usgs":false,"family":"Jenkins","given":"Chris","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":288510,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reid, Jamey M.","contributorId":68386,"corporation":false,"usgs":true,"family":"Reid","given":"Jamey","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":288512,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Williams, S. Jeffress 0000-0002-1326-7420 jwilliams@usgs.gov","orcid":"https://orcid.org/0000-0002-1326-7420","contributorId":2063,"corporation":false,"usgs":true,"family":"Williams","given":"S.","email":"jwilliams@usgs.gov","middleInitial":"Jeffress","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":288508,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Flocks, James G. 0000-0002-6177-7433 jflocks@usgs.gov","orcid":"https://orcid.org/0000-0002-6177-7433","contributorId":816,"corporation":false,"usgs":true,"family":"Flocks","given":"James","email":"jflocks@usgs.gov","middleInitial":"G.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":288507,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":77374,"text":"sir20065101A - 2006 - Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","interactions":[{"subject":{"id":77374,"text":"sir20065101A - 2006 - Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","indexId":"sir20065101A","publicationYear":"2006","noYear":false,"chapter":"A","title":"Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming"},"predicate":"IS_PART_OF","object":{"id":77374,"text":"sir20065101A - 2006 - Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","indexId":"sir20065101A","publicationYear":"2006","noYear":false,"chapter":"A","title":"Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming"},"id":1},{"subject":{"id":77374,"text":"sir20065101A - 2006 - Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","indexId":"sir20065101A","publicationYear":"2006","noYear":false,"chapter":"A","title":"Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming"},"predicate":"IS_PART_OF","object":{"id":77374,"text":"sir20065101A - 2006 - Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","indexId":"sir20065101A","publicationYear":"2006","noYear":false,"chapter":"A","title":"Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming"},"id":2}],"isPartOf":{"id":77374,"text":"sir20065101A - 2006 - Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","indexId":"sir20065101A","publicationYear":"2006","noYear":false,"title":"Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming"},"lastModifiedDate":"2023-03-20T20:40:45.31808","indexId":"sir20065101A","displayToPublicDate":"2006-07-27T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5101","chapter":"A","title":"Effects of urbanization on stream ecosystems in the South Platte River basin, Colorado and Wyoming","docAbstract":"

This report describes the effects of urbanization on physical, chemical, and biological characteristics of stream ecosystems in 28 basins along an urban land-use gradient in the South Platte River Basin, Colorado and Wyoming, from 2002 through 2003. Study basins were chosen to minimize natural variability among basins due to factors such as geology, elevation, and climate and to maximize coverage of different stages of urban development among basins. Because land use or population density alone often are not a complete measure of urbanization, land use, land cover, infrastructure, and socioeconomic variables were integrated in a multimetric urban intensity index to represent the degree of urban development in each study basin. Physical characteristics studied included stream hydrology, stream temperature, and habitat; chemical characteristics studied included nutrients, pesticides, suspended sediment, sulfate, chloride, and fecal bacteria concentrations; and biological characteristics studied included algae, fish, and invertebrate communities. Semipermeable membrane devices (SPMDs), passive samplers that concentrate trace levels of hydrophobic organic contaminants like polycyclic aromatic hydrocarbons (PAHs) and polychlorinated biphenyls (PCBs), also were used. The objectives of the study were to (1) examine physical, chemical, and biological responses along the gradient of urbanization; (2) determine the major physical, chemical, and landscape variables affecting the structure of aquatic communities; and (3) evaluate the relevance of the results to the management of water resources in the South Platte River Basin. Commonly observed effects of urbanization on instream physical, chemical, and biological characteristics, such as increased flashiness, higher magnitude and more frequent peak flows, increased concentrations of chemicals, and changes in aquatic community structure, generally were not observed in this study. None of the hydrologic, temperature, habitat, or chemical variables were correlated strongly (Spearman's rho greater than or equal to 0.7) with urban intensity, with the exception of some of the SPMD-based toxicity and chemical variables. SPMD-based measures of potential toxicity and PAH concentrations were positively correlated with urban intensity. The PAH concentrations also were positively correlated with measures of road density and negatively correlated with distance to the nearest road, indicating that automobile exhaust is a major source of these compounds in the study area. This source may be localized enough that the transport of PAHs would be minimally affected by water-management practices such as diversion or storage upstream. In contrast, the predominant sources of nutrients, bacteria, suspended sediment, sulfate, chloride, and pesticides may be more dispersed throughout the drainage area and, therefore, their transport to downstream sites may be subject to greater disruption by water regulation. Although no direct link was found between most water-chemistry characteristics and urbanization, invertebrate, algae, and fish-community characteristics were strongly associated with nutrients, pesticides, sulfate, chloride, and suspended sediment. None of the biological community variables were strongly correlated with the urban intensity index. Algal biomass predominantly was associated with total nitrogen concentrations, nitrite-plus-nitrate concentrations, and the duration of high flows. Fish communities predominantly were associated with housing age, the percentage of suspended sediment finer than 0.063 millimeters and chloride concentrations. Invertebrate communities predominantly were associated with the frequency of rising and falling flow events, the duration of high flows, total nitrogen concentrations, nitrite-plus-nitrate concentrations, and total herbicide concentrations. Historical records indicate that aquatic communities in the region may have been altered prior to any substantial urban development by early agricultural and water-management practices. Present-day aquatic communities are composed primarily of tolerant species even in areas of minimal urban development; when development does occur, the communities already may be resistant to disturbance. In addition to the effects of historical stressors on aquatic community structure, it is possible that current water-management practices in the study basins are having an effect. In the absence of natural, unaltered hydrologic conditions, more sensitive taxa may be unable to recolonize urban streams. The movement and storage of water also may lead to a disconnect between the land surface and streams, resulting in instream physical, chemical, and biological characteristics that, to some degree, are independent of land-cover characteristics.

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We present a model of gas exsolution and bubble expansion in a melt supersaturated in response to a sudden pressure drop. In our model, the melt contains a suspension of gas bubbles of identical sizes and is encased in a penny-shaped crack embedded in an elastic solid. The suspension is modeled as a three-dimensional lattice of spherical cells with slight overlap, where each elementary cell consists of a gas bubble surrounded by a shell of volatile-rich melt. The melt is then subjected to a step drop in pressure, which induces gas exsolution and bubble expansion, resulting in the compression of the melt and volumetric expansion of the crack. The dynamics of diffusion-driven bubble growth and volumetric crack expansion span 9 decades in time. The model demonstrates that the speed of the crack response depends strongly on volatile diffusivity in the melt and bubble number density and is markedly sensitive to the ratio of crack thickness to crack radius and initial bubble radius but is relatively insensitive to melt viscosity. The net drop in gas concentration in the melt after pressure recovery represents only a small fraction of the initial concentration prior to the drop, suggesting the melt may undergo numerous pressure transients before becoming significantly depleted of gases. The magnitude of pressure and volume recovery in the crack depends sensitively on the size of the input-pressure transient, becoming relatively larger for smaller-size transients in a melt containing bubbles with initial radii less than 10-5 m. Amplification of the input transient may be large enough to disrupt the crack wall and induce brittle failure in the rock matrix surrounding the crack. Our results provide additional basis for the interpretation of volume changes in the magma conduit under Popocatépetl Volcano during Vulcanian degassing bursts in its eruptive activity in April–May 2000.

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Leenhouts, J.C. Stromberg, and R.L. Scott.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20063027","collaboration":"Prepared in cooperation with the Bureau of Land Management, Arizona Department of Water Resources, City of Sierra Vista, U.S. Department of Defense, and the U.S. Environmental Protection Agency","usgsCitation":"Leenhouts, J.M., Stromberg, J.C., and Scott, R.L., 2006, Hydrologic Requirements of and Evapotranspiration by Riparian Vegetation along the San Pedro River, Arizona: U.S. Geological Survey Fact Sheet 2006-3027, 4 p., https://doi.org/10.3133/fs20063027.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":122401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3027.bmp"},{"id":8334,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3027/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.25,31 ], [ -110.25,32 ], [ -110.25,32 ], [ -110.25,31 ], [ -110.25,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614478","contributors":{"authors":[{"text":"Leenhouts, James M. 0000-0001-5171-9240 leenhout@usgs.gov","orcid":"https://orcid.org/0000-0001-5171-9240","contributorId":225,"corporation":false,"usgs":true,"family":"Leenhouts","given":"James","email":"leenhout@usgs.gov","middleInitial":"M.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stromberg, Julie C.","contributorId":71657,"corporation":false,"usgs":true,"family":"Stromberg","given":"Julie","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":288467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, Russell L.","contributorId":39875,"corporation":false,"usgs":false,"family":"Scott","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288466,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":77088,"text":"sir20055190 - 2006 - Timing and Duration of Flow in Ephemeral Streams of the Sierra Vista Subwatershed of the Upper San Pedro Basin, Cochise County, Southeastern Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:43","indexId":"sir20055190","displayToPublicDate":"2006-07-25T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5190","title":"Timing and Duration of Flow in Ephemeral Streams of the Sierra Vista Subwatershed of the Upper San Pedro Basin, Cochise County, Southeastern Arizona","docAbstract":"Frequency, timing, and duration of streamflow were monitored in 20 ephemeral-stream channels across the Sierra Vista Subwatershed of the Upper San Pedro Basin, southeastern Arizona, during an 18-month period. One channel (Walnut Gulch) had Agricultural Research Service streamflow-gaging stations in place. The sediments of the remaining 19 ephemeral-stream channels were instrumented with multiple temperature loggers along the channel lengths. A thermograph-interpretation technique was developed in order to determine frequency, timing, and duration of streamflow in these channels. Streamflow onset was characterized by exceedance of a critical minimum drop in temperature within the channel sediments during any 15-minute interval, whereas streamflow cessation was identified by the local temperature minimum that immediately followed the critical temperature drop. All data for the 18-month period from December 1, 2000, to May 31, 2002, were analyzed in terms of monsoon (June 1 to September 19) and nonmonsoon (September 20 to May 31) periods. Nonmonsoon precipitation during the 2000-2002 study period (excludes October and November 2000) was 82 percent and 39 percent of the 30-year average, respectively, whereas monsoon precipitation during 2001 was 99 percent of the 30-year average. Ephemeral streamflow was detected at least once during the monitoring period at 87 percent of the monitoring sites (45 of the 52 sites that returned useful data; includes 4 streamflow-gaging stations). The summer monsoon period accounted for 82 percent of all streamflow events by number and 71 percent of all events by total streamflow duration. Nonmonsoon streamflow events peaked in number, total streamflow duration, and mean streamflow duration midway between the Huachuca Mountains and the San Pedro River on the west side of the subwatershed. These three streamflow parameters dropped off sharply about 10 kilometers from the mountain front. The number and total duration of nonmonsoon streamflows on the east side of the subwatershed trended downward with increased distance from the mountain fronts. Monsoon streamflow events were more evenly distributed across the subwatershed than nonmonsoon events, and the number and duration of streamflows generally trended upward with distance from the mountain fronts. Additional years of data are needed to determine whether these patterns are consistent year to year, or were due to randomness in the spatial distribution of precipitation. Streamflows in three ephemeral-stream channels were analyzed in detail. More than two-thirds of the streamflow events detected in each of these channels occurred at no more than one monitoring site along the channel length. In only one of the three channels-Garden Canyon-was a streamflow event detected at all logger sites along its length. Five temperature loggers provided data from urbanized areas, and these loggers detected streamflow more than 50 percent more often and of a duration nearly three times greater than did temperature loggers across the rural parts of the subwatershed. Because historical records do not indicate that more precipitation occurs in the urbanized area than in the rural areas, the increased frequency of flow detection in the urban area is attributed to an increase in runoff from the impervious surfaces throughout the urbanized area.","language":"ENGLISH","doi":"10.3133/sir20055190","usgsCitation":"Gungle, B., 2006, Timing and Duration of Flow in Ephemeral Streams of the Sierra Vista Subwatershed of the Upper San Pedro Basin, Cochise County, Southeastern Arizona (Version 2.0, revised 2007): U.S. Geological Survey Scientific Investigations Report 2005-5190, vi, 47 p., https://doi.org/10.3133/sir20055190.","productDescription":"vi, 47 p.","numberOfPages":"50","temporalStart":"2000-12-01","temporalEnd":"2002-05-31","costCenters":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"links":[{"id":194552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8333,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5190/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.5,31 ], [ -110.5,31.75 ], [ -110,31.75 ], [ -110,31 ], [ -110.5,31 ] ] ] } } ] }","edition":"Version 2.0, revised 2007","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b4e2","contributors":{"authors":[{"text":"Gungle, Bruce 0000-0001-6406-1206","orcid":"https://orcid.org/0000-0001-6406-1206","contributorId":40176,"corporation":false,"usgs":true,"family":"Gungle","given":"Bruce","affiliations":[],"preferred":false,"id":288464,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179068,"text":"70179068 - 2006 - Aftershock decay, productivity, and stress rates in Hawaii: Indicators of temperature and stress from magma sources","interactions":[],"lastModifiedDate":"2016-12-14T13:51:01","indexId":"70179068","displayToPublicDate":"2006-07-25T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Aftershock decay, productivity, and stress rates in Hawaii: Indicators of temperature and stress from magma sources","docAbstract":"

We examined dozens of aftershock sequences in Hawaii in terms of Gutenberg-Richter and modified Omori law parameters. We studied p, the rate of aftershock decay; Ap, the aftershock productivity, defined as the observed divided by the expected number of aftershocks; and c, the time delay when aftershock rates begin to fall. We found that for earthquakes shallower than 20 km, p values >1.2 are near active magma centers. We associate this high decay rate with higher temperatures and faster stress relaxation near magma reservoirs. Deep earthquakes near Kilauea's inferred magma transport path show a range of p values, suggesting the absence of a large, deep magma reservoir. Aftershock productivity is >4.0 for flank earthquakes known to be triggered by intrusions but is normal (0.25 to 4.0) for isolated main shocks. We infer that continuing, post-main shock stress from the intrusion adds to the main shock's stress step and causes higher Ap. High Ap in other zones suggests less obvious intrusions and pulsing magma pressure near Kilauea's feeding conduit. We calculate stress rates and stress rate changes from pre-main shock and aftershock rates. Stress rate increased after many intrusions but decreased after large M7–8 earthquakes. Stress rates are highest in the seismically active volcano flanks and lowest in areas far from volcanic centers. We found sequences triggered by intrusions tend to have high Ap, high (>0.10 day) c values, a stress rate increase, and sometimes a peak in aftershock rate hours after the main shock. We interpret these values as indicating continuing intrusive stress after the main shock.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2005JB003949","usgsCitation":"Klein, F.W., Wright, T., and Nakata, J., 2006, Aftershock decay, productivity, and stress rates in Hawaii: Indicators of temperature and stress from magma sources: Journal of Geophysical Research B: Solid Earth, v. 111, no. B7, B07307; 26 p., https://doi.org/10.1029/2005JB003949.","productDescription":"B07307; 26 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":477319,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2005jb003949","text":"Publisher Index Page"},{"id":332132,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawai'i","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155.55679321289062, 20.128155311797183 ], [ -155.58425903320312, 20.117839630491634 ], [ -155.64056396484375, 20.153941536577403 ], [ -155.65841674804688, 20.168122145270342 ], [ -155.68862915039062, 20.179723502765153 ], [ -155.73394775390625, 20.204212422008773 ], [ -155.73394775390625, 20.218388457307814 ], [ 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-155.55679321289062, 20.128155311797183 ] ] ] } } ] }\n","volume":"111","issue":"B7","noUsgsAuthors":false,"publicationDate":"2006-07-25","publicationStatus":"PW","scienceBaseUri":"585268e4e4b0e2663625ec9c","contributors":{"authors":[{"text":"Klein, Fred W. klein@usgs.gov","contributorId":4417,"corporation":false,"usgs":true,"family":"Klein","given":"Fred","email":"klein@usgs.gov","middleInitial":"W.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":655914,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, Tom","contributorId":177475,"corporation":false,"usgs":false,"family":"Wright","given":"Tom","email":"","affiliations":[],"preferred":false,"id":655915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nakata, Jennifer","contributorId":41542,"corporation":false,"usgs":true,"family":"Nakata","given":"Jennifer","affiliations":[],"preferred":false,"id":655916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":77085,"text":"fs20053142 - 2006 - Urban seismic hazard mapping for Memphis, Shelby County, Tennessee","interactions":[],"lastModifiedDate":"2019-07-17T17:03:54","indexId":"fs20053142","displayToPublicDate":"2006-07-24T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-3142","title":"Urban seismic hazard mapping for Memphis, Shelby County, Tennessee","docAbstract":"Earthquakes cannot be predicted, but scientists can forecast how strongly the ground is likely to shake as a result of an earthquake. Seismic hazard maps provide one way of conveying such forecasts. The U.S. Geological Survey (USGS), which produces seismic hazard maps for the Nation, is now engaged in developing more detailed maps for vulnerable urban areas. The first set of these maps is now available for Memphis, Tennessee.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs20053142","usgsCitation":"Gomberg, J., 2006, Urban seismic hazard mapping for Memphis, Shelby County, Tennessee (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3142, 4 p., https://doi.org/10.3133/fs20053142.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":120791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3142.jpg"},{"id":8330,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3142/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93,34 ], [ -93,38 ], [ -87,38 ], [ -87,34 ], [ -93,34 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e155c","contributors":{"authors":[{"text":"Gomberg, Joan","contributorId":77919,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","affiliations":[],"preferred":false,"id":288458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":77087,"text":"sir20065133 - 2006 - Hydraulic and field water-chemistry characteristics of piedmont alluvial deposits in the Middle Tyger River near Lyman, Spartanburg County, South Carolina, 2005","interactions":[],"lastModifiedDate":"2017-01-12T10:21:32","indexId":"sir20065133","displayToPublicDate":"2006-07-24T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5133","title":"Hydraulic and field water-chemistry characteristics of piedmont alluvial deposits in the Middle Tyger River near Lyman, Spartanburg County, South Carolina, 2005","docAbstract":"This study explores the possibility of developing a bank-filtration process to improve water quality in which alluvial deposits serve as a natural sand filter to pretreat water to be used as a secondary drinking-water source in a small piedmont reservoir along the Middle Tyger River near Lyman in Spartanburg County, South Carolina. From January 2004 to September 2005, data from 10 auger borings, 2 sediment cores, 29 ground-penetrating radar transects, and 3 temporary observation wells, and field water-chemistry data were collected and analyzed. These data were collected and used to characterize the lithology, geometry, hydraulic properties, yield potential, and water-chemistry characteristics of the alluvial deposits in the channel and on the right bank of the reservoir. The assessment was undertaken to determine if an adequate amount of water could be withdrawn from the alluvial deposits to sustain a bank-filtration process and to characterize the water chemistry of the surface water and pore water.\r\n\r\nThe heterogeneous alluvial and fill material at the study site--clay, silty clay, clayey sand, fine- to coarse-grained sand, and mica--on the right bank of the Middle Tyger River ranges in thickness from 0.6 to 7 meters, has a calculated horizontal hydraulic conductivity of 1 meter per day, and yields approximately 0.07 liter per second of water. The small calculated horizontal hydraulic conductivity and water yield for these deposits restrict the use of the right bank as a potential bank-filtration site.\r\n\r\nThe coarse-grained alluvial sand deposit in the channel of the Middle Tyger River, however, may be used for a limited bank-filtration process. The discharge during pumping of the channel deposit yielded water at the rate of 1.9 liters per second. The coarse-grained channel deposit is approximately 49 meters wide and 3 meters thick near the dam. At approximately 183 meters upstream from the dam, the channel narrows to roughly 9 meters and the channel deposits thin to approximately 0.1 meter. Slug tests conducted in the channel deposits near the dam produced a calculated horizontal hydraulic conductivity of 60 meters per day. The limited thickness and aerial extent of the coarse-grained channel deposits coupled with large horizontal hydraulic conductivity likely would allow rapid transmission of water and may degrade the effectiveness of some water-chemistry improvements typical of a bank-filtration process.\r\n\r\nField water-chemistry data were collected for approximately 1 hour and 45 minutes at 10 to 15 minute intervals to compare the surface-water and pore-water quality in and beneath the channel of the Middle Tyger River. The waterchemistry data indicate that (1) the mean water temperature was higher in surface water (22.5 degrees Celsius) than in pore water (18.5 degrees Celsius), (2) the mean specific conductance was less in surface water (56.9 microsiemens per centimeter at 25 degrees Celsius) than in pore water (125.7 microsiemens per centimeter at 25 degrees Celsius), (3) alkalinity was lower in surface water (22.5 milligrams per liter) than in pore water (44.6 milligrams per liter), and (4) recorded pH values ranged between 6.2 and 6.3 in the surface water and pore water during the sampling period. The flow velocity was orders of magnitude slower in the pore water than in the surface water; therefore, the pore water interacts with the alluvial sediment for a longer period of time producing the variation in water-chemistry data between the two waters.","language":"ENGLISH","doi":"10.3133/sir20065133","usgsCitation":"Harrelson, L.G., and Addison, A.D., 2006, Hydraulic and field water-chemistry characteristics of piedmont alluvial deposits in the Middle Tyger River near Lyman, Spartanburg County, South Carolina, 2005: U.S. Geological Survey Scientific Investigations Report 2006-5133, v, 22 p., https://doi.org/10.3133/sir20065133.","productDescription":"v, 22 p.","numberOfPages":"27","onlineOnly":"Y","temporalStart":"2005-01-01","temporalEnd":"2005-12-31","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":191620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8332,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5133/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Carolina","county":"Spartanburg County","otherGeospatial":"Middle Tyger River","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.9713,35.1876],[-81.9196,35.1857],[-81.8746,35.1841],[-81.8092,35.0631],[-81.8057,35.0559],[-81.8072,35.0359],[-81.7943,35.036],[-81.7932,35.0346],[-81.7719,34.983],[-81.7495,34.93],[-81.736,34.9301],[-81.7303,34.9224],[-81.723,34.9179],[-81.7117,34.913],[-81.7429,34.8819],[-81.7833,34.8372],[-81.8188,34.7006],[-81.8248,34.6802],[-81.8411,34.6428],[-81.854,34.5946],[-81.8595,34.5913],[-81.8622,34.5818],[-81.8752,34.5953],[-81.8797,34.5966],[-81.888,34.5925],[-81.8942,34.6006],[-81.9077,34.6028],[-81.9201,34.614],[-81.9332,34.6335],[-81.9479,34.6483],[-81.9911,34.6639],[-82,34.6638],[-82.0598,34.7019],[-82.0699,34.7036],[-82.0661,34.7132],[-82.069,34.7204],[-82.0768,34.7222],[-82.0856,34.7471],[-82.0979,34.7465],[-82.1053,34.7551],[-82.1092,34.7573],[-82.1136,34.7509],[-82.1279,34.7689],[-82.1325,34.7789],[-82.1432,34.7842],[-82.1664,34.8017],[-82.1592,34.8063],[-82.1716,34.8107],[-82.1932,34.835],[-82.2171,34.8539],[-82.2265,34.8511],[-82.2261,34.8601],[-82.2227,34.9287],[-82.2192,35.0627],[-82.2165,35.1354],[-82.2163,35.1959],[-82.1554,35.1943],[-82.1521,35.1942],[-81.9713,35.1876]]]},\"properties\":{\"name\":\"Spartanburg\",\"state\":\"SC\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a324","contributors":{"authors":[{"text":"Harrelson, Larry G.","contributorId":70059,"corporation":false,"usgs":true,"family":"Harrelson","given":"Larry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":288463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Addison, Adrian D.","contributorId":36234,"corporation":false,"usgs":true,"family":"Addison","given":"Adrian","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":288462,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":77084,"text":"fs20063095 - 2006 - 1976 Big Thompson flood, Colorado — Thirty years later","interactions":[],"lastModifiedDate":"2022-07-22T19:07:44.496318","indexId":"fs20063095","displayToPublicDate":"2006-07-24T00:00:00","publicationYear":"2006","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":"2006-3095","title":"1976 Big Thompson flood, Colorado — Thirty years later","docAbstract":"In the early evening of Saturday, July 31, 1976, a large stationary thunderstorm released as much as 7.5 inches of rainfall in about an hour (about 12 inches in a few hours) in the middle reaches of the Big Thompson River Basin and to a lesser extent in parts of the Cache la Poudre River Basin. In steep mountain terrain with thin or no soil, this large amount of rainfall in such a short period of time produced a flash flood that caught residents and tourists by surprise. The sudden flood that churned down the narrow Big Thompson Canyon scoured the river channel that night, caused over $35 million in damages (1977 dollars) to 418 homes and businesses, many mobile homes, 438 automobiles, numerous bridges, paved and unpaved roads, power and telephone lines, and many other structures. The tragedy claimed the lives of 144 people, including two law enforcement officers trying to evacuate people in danger, and there were 250 reported injuries. Scores of other people narrowly escaped with their lives. More than 800 people were evacuated by helicopter the following morning. This fact sheet presents a summary of the hydrologic conditions of the 1976 flood, describes some of the advances in U.S. Geological Survey (USGS) flood science as a consequence of this disaster, and provides a reminder that extreme floods like the 1976 Big Thompson flood have occurred in other locations in Colorado in the past and will occur again.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20063095","usgsCitation":"Jarrett, R.D., and Costa, J.E., 2006, 1976 Big Thompson flood, Colorado — Thirty years later (Version 1.0): U.S. Geological Survey Fact Sheet 2006-3095, 5 p., https://doi.org/10.3133/fs20063095.","productDescription":"5 p.","temporalStart":"1976-07-31","temporalEnd":"1976-07-31","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":121045,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3095.gif"},{"id":8329,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3095/","linkFileType":{"id":5,"text":"html"}},{"id":404381,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_77315.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado","otherGeospatial":"Big Thompson River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.75,\n 40.094882122321145\n ],\n [\n -104.7491455078125,\n 40.094882122321145\n ],\n [\n -104.7491455078125,\n 40.90520969727358\n ],\n [\n -105.75,\n 40.90520969727358\n ],\n [\n -105.75,\n 40.094882122321145\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","publicComments":"See also poster GIP 35","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4911e4b0b290850eedb1","contributors":{"authors":[{"text":"Jarrett, Robert D. rjarrett@usgs.gov","contributorId":2260,"corporation":false,"usgs":true,"family":"Jarrett","given":"Robert","email":"rjarrett@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":288456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Costa, John E.","contributorId":105743,"corporation":false,"usgs":true,"family":"Costa","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":288457,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":77086,"text":"sir20065022 - 2006 - The Laramide Mesa formation and the Ojo de Agua caldera, southeast of the Cananea copper mining district, Sonora, Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:14:19","indexId":"sir20065022","displayToPublicDate":"2006-07-24T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5022","title":"The Laramide Mesa formation and the Ojo de Agua caldera, southeast of the Cananea copper mining district, Sonora, Mexico","docAbstract":"The Mesa Formation extends from Cananea, Mexico, southeast to the Sonora River and is the main host rock of Laramide porphyry copper deposits in the Cananea District and at the Alacran porphyry prospect to the east. The Mesa consists of two members-a lower andesite and an upper dacite. The lowest part of the dacite member is a crystal tuff about 100 m thick. This tuff is the outfall of a caldera centered near the village of Ojo de Agua, dated by 40Ar/39Ar at 65.8 Ma ?0.4. The Ojo de Agua Caldera is about 9 km in diameter and is filled by a light gray biotite dacite tuff with abundant flattened pumice fragments. The volume of the caldera is estimated to be 24 km3.","language":"ENGLISH","doi":"10.3133/sir20065022","usgsCitation":"Cox, D.P., Miller, R.J., and Woodbourne, K.L., 2006, The Laramide Mesa formation and the Ojo de Agua caldera, southeast of the Cananea copper mining district, Sonora, Mexico: U.S. Geological Survey Scientific Investigations Report 2006-5022, iii, 7p., https://doi.org/10.3133/sir20065022.","productDescription":"iii, 7p.","numberOfPages":"10","onlineOnly":"Y","costCenters":[{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":194971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8331,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5022/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfd3","contributors":{"authors":[{"text":"Cox, Dennis P. dcox@usgs.gov","contributorId":2766,"corporation":false,"usgs":true,"family":"Cox","given":"Dennis","email":"dcox@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":288460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Robert J. rjmiller@usgs.gov","contributorId":2516,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"rjmiller@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":288459,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodbourne, Keith L.","contributorId":56326,"corporation":false,"usgs":true,"family":"Woodbourne","given":"Keith","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":288461,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":77083,"text":"fs20063091 - 2006 - Assessment of Undiscovered Gas Resources of the Eastern Oregon and Washington Province, 2006","interactions":[],"lastModifiedDate":"2012-02-02T00:14:21","indexId":"fs20063091","displayToPublicDate":"2006-07-21T00:00:00","publicationYear":"2006","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":"2006-3091","title":"Assessment of Undiscovered Gas Resources of the Eastern Oregon and Washington Province, 2006","docAbstract":"Using a geology-based assessment methodology, the U.S. Geological Survey estimated a mean of 2.4 trillion cubic feet (TCF) of undiscovered natural gas in the Eastern Oregon and Washington Province. More than 90 percent, or 2.1 TCF, of the estimated undiscovered natural gas is continuous gas estimated to be trapped in Tertiary rocks overlain by the Columbia River Basalt Group.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20063091","usgsCitation":"Brownfield, M.E., Tennyson, M., Ahlbrandt, T.S., Charpentier, R., Cook, T.A., Klett, T., Pollastro, R.M., and Schenk, C.J., 2006, Assessment of Undiscovered Gas Resources of the Eastern Oregon and Washington Province, 2006: U.S. Geological Survey Fact Sheet 2006-3091, 2 p., https://doi.org/10.3133/fs20063091.","productDescription":"2 p.","numberOfPages":"2","temporalStart":"2006-01-01","temporalEnd":"2006-12-31","costCenters":[{"id":407,"text":"National Assessment of Oil and Gas Project","active":false,"usgs":true}],"links":[{"id":122445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3091.jpg"},{"id":8327,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3091/","linkFileType":{"id":5,"text":"html"}},{"id":8328,"rank":9999,"type":{"id":18,"text":"Project Site"},"url":"https://energy.cr.usgs.gov/oilgas/noga/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672053","contributors":{"authors":[{"text":"Brownfield, Michael E. 0000-0003-3633-1138 mbrownfield@usgs.gov","orcid":"https://orcid.org/0000-0003-3633-1138","contributorId":1548,"corporation":false,"usgs":true,"family":"Brownfield","given":"Michael","email":"mbrownfield@usgs.gov","middleInitial":"E.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tennyson, Marilyn E. 0000-0002-5166-2421 tennyson@usgs.gov","orcid":"https://orcid.org/0000-0002-5166-2421","contributorId":1433,"corporation":false,"usgs":true,"family":"Tennyson","given":"Marilyn E.","email":"tennyson@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":288451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ahlbrandt, Thomas S.","contributorId":57836,"corporation":false,"usgs":true,"family":"Ahlbrandt","given":"Thomas","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":288455,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Charpentier, Ronald R. charpentier@usgs.gov","contributorId":934,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","email":"charpentier@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":288450,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cook, Troy A.","contributorId":52519,"corporation":false,"usgs":true,"family":"Cook","given":"Troy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":288454,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":288448,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":288453,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":288449,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":77065,"text":"ofr20061191 - 2006 - Soil data at sites near Geneva Lake, Lake Geneva, Wisconsin, and Long Lake, near New Auburn, Wisconsin","interactions":[],"lastModifiedDate":"2012-03-08T17:16:23","indexId":"ofr20061191","displayToPublicDate":"2006-07-20T00:00:00","publicationYear":"2006","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":"2006-1191","title":"Soil data at sites near Geneva Lake, Lake Geneva, Wisconsin, and Long Lake, near New Auburn, Wisconsin","docAbstract":"The goals of this project are to describe how water moves through shallow soil and how vegetated buffers influence this flow. This was accomplished by using a series of soil-moisture probes which track the lateral and vertical movement of water during natural and artificial rainfall/runoff events. The purpose of this report is to summarize soil-moisture data collected at near-shore areas adjacent to two Wisconsin lakes.","language":"ENGLISH","doi":"10.3133/ofr20061191","usgsCitation":"Graczyk, D., and Greb, S.R., 2006, Soil data at sites near Geneva Lake, Lake Geneva, Wisconsin, and Long Lake, near New Auburn, Wisconsin: U.S. Geological Survey Open-File Report 2006-1191, iv, 10 p., https://doi.org/10.3133/ofr20061191.","productDescription":"iv, 10 p.","numberOfPages":"14","onlineOnly":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":194497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8322,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1191/","linkFileType":{"id":5,"text":"html"}},{"id":8323,"rank":9999,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/of/2006/1191/appendixes/OFR2006-1191_Appendixes.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49bfe4b07f02db5d1dc2","contributors":{"authors":[{"text":"Graczyk, David J.","contributorId":107265,"corporation":false,"usgs":true,"family":"Graczyk","given":"David J.","affiliations":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"preferred":false,"id":288439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Greb, Steven R.","contributorId":29010,"corporation":false,"usgs":false,"family":"Greb","given":"Steven","email":"","middleInitial":"R.","affiliations":[{"id":6913,"text":"Wisconsin Department of Natural Resources","active":true,"usgs":false}],"preferred":false,"id":288438,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":77066,"text":"sir20065130 - 2006 - Low-flow, base-flow, and mean-flow regression equations for Pennsylvania streams","interactions":[],"lastModifiedDate":"2017-07-06T15:42:51","indexId":"sir20065130","displayToPublicDate":"2006-07-20T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5130","title":"Low-flow, base-flow, and mean-flow regression equations for Pennsylvania streams","docAbstract":"

Low-flow, base-flow, and mean-flow characteristics are an important part of assessing water resources in a watershed. These streamflow characteristics can be used by watershed planners and regulators to determine water availability, water-use allocations, assimilative capacities of streams, and aquatic-habitat needs. Streamflow characteristics are commonly predicted by use of regression equations when a nearby streamflow-gaging station is not available.

Regression equations for predicting low-flow, base-flow, and mean-flow characteristics for Pennsylvania streams were developed from data collected at 293 continuous- and partial-record streamflow-gaging stations with flow unaffected by upstream regulation, diversion, or mining. Continuous-record stations used in the regression analysis had 9 years or more of data, and partial-record stations used had seven or more measurements collected during base-flow conditions. The state was divided into five low-flow regions and regional regression equations were developed for the 7-day, 10-year; 7-day, 2-year; 30-day, 10-year; 30-day, 2-year; and 90-day, 10-year low flows using generalized least-squares regression. Statewide regression equations were developed for the 10-year, 25-year, and 50-year base flows using generalized least-squares regression. Statewide regression equations were developed for harmonic mean and mean annual flow using weighted least-squares regression.

Basin characteristics found to be significant explanatory variables at the 95-percent confidence level for one or more regression equations were drainage area, basin slope, thickness of soil, stream density, mean annual precipitation, mean elevation, and the percentage of glaciation, carbonate bedrock, forested area, and urban area within a basin. Standard errors of prediction ranged from 33 to 66 percent for the n-day, T-year low flows; 21 to 23 percent for the base flows; and 12 to 38 percent for the mean annual flow and harmonic mean, respectively. The regression equations are not valid in watersheds with upstream regulation, diversions, or mining activities. Watersheds with karst features need close examination as to the applicability of the regression-equation results.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487e6","contributors":{"authors":[{"text":"Stuckey, Marla H. 0000-0002-5211-8444 mstuckey@usgs.gov","orcid":"https://orcid.org/0000-0002-5211-8444","contributorId":1734,"corporation":false,"usgs":true,"family":"Stuckey","given":"Marla","email":"mstuckey@usgs.gov","middleInitial":"H.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":77067,"text":"sir20065111 - 2006 - Fish communities and related environmental conditions of the lower Boise River, southwestern Idaho, 1974-2004","interactions":[],"lastModifiedDate":"2012-03-08T17:16:20","indexId":"sir20065111","displayToPublicDate":"2006-07-20T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5111","title":"Fish communities and related environmental conditions of the lower Boise River, southwestern Idaho, 1974-2004","docAbstract":"Within the last century, the lower Boise River has been transformed from a meandering, braided, gravel-bed river that supported large runs of salmon to a channelized, regulated, urban river that provides flood control and irrigation water to more than 1,200 square miles of land. An understanding of the current status of the river's fish communities and related environmental conditions is important to support the ongoing management of the Boise River. Therefore, fish community data from the U.S. Geological Survey and the Idaho Department of Fish and Game collected since 1974 were analyzed to describe the status of fish communities in the lower Boise River. Each set of data was collected to address different study objectives, but is combined here to provide an overall distribution of fish in the lower Boise River over the last 30 years. Twenty-two species of fish in 7 families have been identified in the lower Boise River-3 salmonidae, trout and whitefish; 2 cottidae, sculpins; 3 catostomidae, suckers; 7 cyprinidae, minnows; 4 centrarchidae, sunfish; 2 ictaluridae, catfish; and 1 cobitidae, loach.\r\n\r\nAnalysis of fish community data using an Index of Biotic Integrity (IBI) for Northwest rivers shows a decrease in the biotic integrity in a downstream direction, with the lowest IBI near the mouth of the Boise River. The number of tolerant and introduced fish were greater in the lower reaches of the river. Changes in land use, habitat, and water quality, as well as regulated streamflow have affected the lower Boise River fish community. IBI scores were negatively correlated with maximum instantaneous water temperature, specific conductance, and suspended sediment; as well as the basin land-use metrics, area of developed land, impervious surface area, and the number of major diversions upstream of a site. Fish communities in the upstream reaches were dominated by piscivorous fish, whereas the downstream reaches were dominated by tolerant, omnivorous fish. The percentage of sculpin in the river decreased in a downstream direction, and sculpin disappear completely at sites downstream of Glenwood Bridge. The sculpin population increased downstream of the Lander wastewater-treatment facility within the last decade, possibly as a result of improved wastewater treatment. The condition of the mountain whitefish (Prosopium williamsoni) throughout the lower Boise River was good and was similar both to the condition of mountain whitefish from least-disturbed rivers in southern Idaho and to the North American standard weight for mountain whitefish. ","language":"ENGLISH","doi":"10.3133/sir20065111","collaboration":"Figure 1 is interactive in .pdf format","usgsCitation":"MacCoy, D.E., 2006, Fish communities and related environmental conditions of the lower Boise River, southwestern Idaho, 1974-2004: U.S. Geological Survey Scientific Investigations Report 2006-5111, vi, 36 p., https://doi.org/10.3133/sir20065111.","productDescription":"vi, 36 p.","numberOfPages":"42","additionalOnlineFiles":"Y","temporalStart":"1974-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":192300,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8325,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5111/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117,43.25 ], [ -117,43.8675 ], [ -115.86749999999999,43.8675 ], [ -115.86749999999999,43.25 ], [ -117,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f19ef","contributors":{"authors":[{"text":"MacCoy, Dorene E. 0000-0001-6810-4728 demaccoy@usgs.gov","orcid":"https://orcid.org/0000-0001-6810-4728","contributorId":948,"corporation":false,"usgs":true,"family":"MacCoy","given":"Dorene","email":"demaccoy@usgs.gov","middleInitial":"E.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":77064,"text":"sir20065068 - 2006 - Occurrence of trihalomethanes in the nation's ground water and drinking-water supply wells, 1985-2002","interactions":[],"lastModifiedDate":"2017-10-15T11:26:06","indexId":"sir20065068","displayToPublicDate":"2006-07-20T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5068","title":"Occurrence of trihalomethanes in the nation's ground water and drinking-water supply wells, 1985-2002","docAbstract":"This report describes the occurrence of trihalomethanes (THMs) in the Nation's ground water and drinking-water supply wells based on analysis of 5,642 samples of untreated ground water and source water collected or compiled during 1985-2002 by the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program. THMs are a group of volatile organic compounds (VOCs) with natural and anthropogenic sources that are of interest because they are associated with acute and chronic health problems in humans. THMs occur in water primarily from chlorination and are classified as disinfection by-products. In this report, the four THMs are discussed in the order of chloroform, bromodichloromethane, dibromochloromethane, and then bromoform; this sequence corresponds to largest to smallest chlorine content and smallest to largest bromine content.\r\n\r\nFour trihalomethanes were detected in less than 20 percent of samples from studies of (1) aquifers, (2) shallow ground water in agricultural areas, (3) shallow ground water in urban areas, (4) domestic wells, and (5) public wells. Detection frequencies for individual THMs in the five studies ranged from zero for shallow ground water in agricultural areas to 19.5 percent for shallow ground water in urban areas. None of the samples from aquifer studies, domestic wells, or public wells had total THM concentrations (the sum of the concentrations of chloroform, bromodichloromethane, dibromochloromethane, and bromoform) greater than or equal to the U.S. Environmental Protection Agency Maximum Contaminant Level of 80 micrograms per liter (?g/L).\r\n\r\nComparisons of results among studies of aquifers, shallow ground water in agricultural areas, and shallow ground water in urban areas were used to describe the occurrence of the four THMs in ground water for three different land-use settings-mixed, agricultural, and urban, respectively. At the 0.2-?g/L assessment level, one or more of the four THMs were detected in 7.9 percent of the samples from aquifer studies, 2.2 percent of the samples from shallow ground water in agricultural areas, and 19.5 percent of the samples from shallow ground water in urban areas. In general, detection frequencies and concentrations of the four THMs were greater in shallow ground water in urban areas compared to aquifer studies and to shallow ground water in agricultural areas. For all three of these studies, the most common two-THM mixture at the 0.2-?g/L assessment level was chloroform-bromodichloromethane, and this was the only two-THM mixture found in samples of shallow ground water in agricultural areas.\r\n\r\nComparisons of results between studies of domestic wells and public wells were used to describe the occurrence of the four THMs in two different supplies of ground water used for drinking water. At the 0.2-?g/L assessment level, one or more of the four THMs were detected in 5.2 percent of the domestic well samples and in 14.7 percent of the public well samples. In general, detection frequencies and THM concentrations were greater in samples from public wells than from domestic wells. At the 0.2-?g/L assessment level, the six possible two-THM mixtures occurred about six times more frequently in samples from public wells than from domestic wells. One of the most common two-THM mixtures in samples from domestic and public wells was bromodichloromethane-dibromochloromethane.\r\n\r\nDetection frequency is associated with the chlorine content of the THM compound. In general, for each of the five studies, as the chlorine content of the THM compound decreased, the detection frequency at the 0.2-?g/L assessment level also decreased. The exception was the study of public wells in which the detection frequency of the THMs decreased in the following order: chloroform, bromoform, dibromochloromethane, and bromodichloromethane.\r\n\r\nAt the 0.2-?g/L assessment level, the median concentration for one or more of the four THMs ranged from 0.3 ?g/L (shallow ground water in agricultural a","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065068","usgsCitation":"Schaap, B.D., and Zogorski, J.S., 2006, Occurrence of trihalomethanes in the nation's ground water and drinking-water supply wells, 1985-2002: U.S. Geological Survey Scientific Investigations Report 2006-5068, viii, 64 p., https://doi.org/10.3133/sir20065068.","productDescription":"viii, 64 p.","numberOfPages":"72","temporalStart":"1985-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":192781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8321,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5068/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f37e3","contributors":{"authors":[{"text":"Schaap, Bryan D.","contributorId":63438,"corporation":false,"usgs":true,"family":"Schaap","given":"Bryan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":288437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":288436,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":77061,"text":"sir20065132 - 2006 - Reconnaissance-level assessment of water and bottom-sediment quality, including pesticides and mercury, in Yankton Sioux Tribe wetlands, Charles Mix County, South Dakota, June-July 2005","interactions":[],"lastModifiedDate":"2017-10-15T11:27:53","indexId":"sir20065132","displayToPublicDate":"2006-07-20T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2006-5132","title":"Reconnaissance-level assessment of water and bottom-sediment quality, including pesticides and mercury, in Yankton Sioux Tribe wetlands, Charles Mix County, South Dakota, June-July 2005","docAbstract":"During June and July 2005, water and bottom-sediment samples were collected from selected Yankton Sioux Tribe wetlands within the historic Reservation area of eastern Charles Mix County as part of a reconnaissance-level assessment by the U.S. Geological Survey and Yankton Sioux Tribe. The water samples were analyzed for pesticides and mercury species. In addition, the water samples were analyzed for physical properties and chemical constituents that might help further characterize the water quality of the wetlands. The bottom-sediment samples were analyzed for mercury species.\r\n\r\nDuring June 2005, water samples were collected from 19 wetlands and were analyzed for 61 widely used pesticide compounds. Many pesticides were not detected in any of the water samples and many others were detected only at low concentrations in a few of the samples. Thirteen pesticides were detected in water samples from at least one of the wetlands. Atrazine and de-ethyl atrazine were detected at each of the 19 wetlands. The minimum, maximum, and median dissolved atrazine concentrations were 0.056, 0.567, and 0.151 microgram per liter (?g/L), respectively. Four pesticides (alachlor, carbaryl, chlorpyrifos, and dicamba) were detected in only one wetland each. The number of pesticides detected in any of the 19 wetlands ranged from 3 to 8, with a median of 6. In addition to the results for this study, recent previous studies have frequently found atrazine in Lake Andes and the Missouri River, but none of the atrazine concentrations have been greater than 3 ?g/L, the U.S. Environmental Protection Agency's Maximum Contaminant Level for atrazine in drinking water.\r\n\r\nDuring June and July 2005, water and bottom-sediment samples were collected from 10 wetlands. Water samples from each of the wetlands were analyzed for major ions, organic carbon, and mercury species, and bottom-sediment samples were analyzed for mercury species. For the whole-water samples, the total mercury concentrations ranged from 1.11 to 29.65 nanograms per liter (ng/L), with a median of 10.56 ng/L. The methylmercury concentrations ranged from 0.45 to 14.03 ng/L, with a median of 2.28 ng/L. For the bottom-sediment samples, the total mercury concentration ranged from 21.3 to 74.6 nanograms per gram (ng/g), with a median of 54.2 ng/g. The methylmercury concentrations ranged from <0.11 to 2.04 ng/g, with a median of 0.78 ng/g. The total mercury concentrations in the water samples were all much less than 2 ?g/L (2,000 ng/L), the U.S. Environmental Protection Agency's Maximum Contaminant Level for mercury in drinking water. However, water samples from four of the wetlands had concentrations larger than 0.012 ?g/L (12 ng/L), the State of South Dakota's chronic standard for surface waters, including wetlands. Maximum methylmercury concentrations for this study are larger than reported concentrations for wetlands in North Dakota and concentrations reported for the Cheyenne River Indian Reservation in South Dakota.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20065132","collaboration":"Prepared in cooperation with the Yankton Sioux Tribe","usgsCitation":"Schaap, B.D., and Bartholomay, R.C., 2006, Reconnaissance-level assessment of water and bottom-sediment quality, including pesticides and mercury, in Yankton Sioux Tribe wetlands, Charles Mix County, South Dakota, June-July 2005: U.S. Geological Survey Scientific Investigations Report 2006-5132, v, 40 p., https://doi.org/10.3133/sir20065132.","productDescription":"v, 40 p.","numberOfPages":"45","onlineOnly":"Y","temporalStart":"2005-06-01","temporalEnd":"2005-07-31","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":192525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8319,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5132/","linkFileType":{"id":5,"text":"html"}}],"projection":"UTM Zone 14","country":"United States","state":"South Dakota","county":"Charles Mix County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.83333333333333,42.666666666666664 ], [ -98.83333333333333,43.333333333333336 ], [ -98,43.333333333333336 ], [ -98,42.666666666666664 ], [ -98.83333333333333,42.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697491","contributors":{"authors":[{"text":"Schaap, Bryan D.","contributorId":63438,"corporation":false,"usgs":true,"family":"Schaap","given":"Bryan","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":288427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bartholomay, Roy C. 0000-0002-4809-9287 rcbarth@usgs.gov","orcid":"https://orcid.org/0000-0002-4809-9287","contributorId":1131,"corporation":false,"usgs":true,"family":"Bartholomay","given":"Roy","email":"rcbarth@usgs.gov","middleInitial":"C.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":288426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}