{"pageNumber":"2423","pageRowStart":"60550","pageSize":"25","recordCount":184617,"records":[{"id":70175147,"text":"70175147 - 2006 - USGS, NPS, educate the public on the risks, wonders of Alaska's volcanoes","interactions":[],"lastModifiedDate":"2016-08-01T12:09:32","indexId":"70175147","displayToPublicDate":"2006-05-15T13:15:00","publicationYear":"2006","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3030,"text":"People, Land, and Water","active":true,"publicationSubtype":{"id":10}},"title":"USGS, NPS, educate the public on the risks, wonders of Alaska's volcanoes","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"Adleman, J.N., 2006, USGS, NPS, educate the public on the risks, wonders of Alaska's volcanoes: People, Land, and Water.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":325866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57a072c0e4b060ce18fb2e66","contributors":{"authors":[{"text":"Adleman, Jennifer N.","contributorId":12422,"corporation":false,"usgs":true,"family":"Adleman","given":"Jennifer","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":644093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":76717,"text":"sir20065006 - 2006 - Quantification of mass loading to Strawberry Creek near the Gilt Edge mine, Lawrence County, South Dakota, June 2003","interactions":[],"lastModifiedDate":"2020-01-26T11:14:36","indexId":"sir20065006","displayToPublicDate":"2006-05-15T00:00:00","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":"2006-5006","title":"Quantification of mass loading to Strawberry Creek near the Gilt Edge mine, Lawrence County, South Dakota, June 2003","docAbstract":"Although remedial actions have taken place at the Gilt Edge mine in the Black Hills of South Dakota, questions remain about a possible hydrologic connection along shear zones between some of the pit lakes at the mine site and Strawberry Creek. Spatially detailed chemical sampling of stream and inflow sites occurred during low-flow conditions in June 2003 as part of a mass-loading study by the U.S. Geological Survey to investigate the possible connection of shear zones to the stream. Stream discharge was calculated by tracer dilution; discharge increased by 25.3 liters per second along the study reach, with 9.73 liters per second coming from three tributaries and the remaining increase coming from small springs and dispersed, subsurface inflow. Chemical differences among inflow samples were distinguished by cluster analysis and indicated that inflows ranged from those unaffected by interaction with mine wastes to those that could have been affected by drainage from pit lakes. Mass loading to the stream from several inflows resulted in distinct chemical changes in stream water along the study reach. Mass loading of the mine-related metals, including cadmium, copper, nickel, and zinc, principally occurred from the discharge from the Gilt Edge mine, and those metals were substantially attenuated downstream. Secondary loadings of metals occurred in the vicinity of the Oro Fino shaft and from two more inflows about 200 m downstream from there. These are both locations where shear zones intersect the stream and may indicate loading associatedwith these zones. Loading downstream from the Oro Fino shaft had a unique chemical character, high in base-metal concentrations, that could indicate an association with water in the pit lakes. The loading from these downstream sources, however, is small in comparison to that from the initial mine discharge and does not appear to have a substantial impact on Strawberry Creek.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20065006","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Kimball, B.A., Runkel, R.L., Walton-Day, K., and Williamson, J., 2006, Quantification of mass loading to Strawberry Creek near the Gilt Edge mine, Lawrence County, South Dakota, June 2003: U.S. Geological Survey Scientific Investigations Report 2006-5006, vi, 41 p., https://doi.org/10.3133/sir20065006.","productDescription":"vi, 41 p.","numberOfPages":"51","temporalStart":"2003-06-01","temporalEnd":"2003-06-30","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":192071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7779,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5006/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"South Dakota","county":"Lawrence County","otherGeospatial":"Gilt Edge mine, Strawberry Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.6863899230957,\n 44.305178455794234\n ],\n [\n -103.6863899230957,\n 44.34263451728076\n ],\n [\n -103.60055923461914,\n 44.34263451728076\n ],\n [\n -103.60055923461914,\n 44.305178455794234\n ],\n [\n -103.6863899230957,\n 44.305178455794234\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64dc17","contributors":{"authors":[{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runkel, Robert L. 0000-0003-3220-481X runkel@usgs.gov","orcid":"https://orcid.org/0000-0003-3220-481X","contributorId":685,"corporation":false,"usgs":true,"family":"Runkel","given":"Robert","email":"runkel@usgs.gov","middleInitial":"L.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":287697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walton-Day, Katherine 0000-0002-9146-6193","orcid":"https://orcid.org/0000-0002-9146-6193","contributorId":68339,"corporation":false,"usgs":true,"family":"Walton-Day","given":"Katherine","affiliations":[],"preferred":false,"id":287699,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williamson, Joyce E. jewillia@usgs.gov","contributorId":1964,"corporation":false,"usgs":true,"family":"Williamson","given":"Joyce E.","email":"jewillia@usgs.gov","affiliations":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true}],"preferred":false,"id":287698,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":76716,"text":"ofr20061141 - 2006 - Processed 1938 aerial photography for selected areas of the lower Colorado River, southwestern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:14:07","indexId":"ofr20061141","displayToPublicDate":"2006-05-15T00:00:00","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":"2006-1141","title":"Processed 1938 aerial photography for selected areas of the lower Colorado River, southwestern United States","docAbstract":"The U.S. Geological Survey (USGS) initiated a study of the Lower Colorado River to derive temporal-change characteristics from the predam period to the present. In this report, we present summary information on accomplishments under a USGS task for the Department of the Interior's Landscapes in the West project. We discuss our preliminary results in compiling a digital database of geospatial information on the Lower Colorado River and acquisition of data products, and present a geospatial digital dataset of 1938 aerial photography of the river valley. The U.S. Bureau of Reclamation (BOR)'s, Resources Management Office in Boulder City, Nev., provided historical aerial photographs of the river valley from the Hoover Dam to the United States-Mexican border, with some exclusions. USGS authors scanned and mosaicked the photographs, registered the photo mosaics, and created metadata describing each mosaic series, all 15 of which are presented here.","language":"ENGLISH","doi":"10.3133/ofr20061141","usgsCitation":"Norman, L.M., Gishey, M., Gass, L., Yanites, B., Pfeifer, E., Simms, R., and Ahlbrandt, R., 2006, Processed 1938 aerial photography for selected areas of the lower Colorado River, southwestern United States (Version 1.0): U.S. Geological Survey Open-File Report 2006-1141, 116 p., https://doi.org/10.3133/ofr20061141.","productDescription":"116 p.","numberOfPages":"116","additionalOnlineFiles":"Y","temporalStart":"1938-01-01","temporalEnd":"1938-12-31","costCenters":[{"id":294,"text":"Geography","active":false,"usgs":true}],"links":[{"id":192404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7778,"rank":9999,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1141/version_history.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7777,"rank":9999,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2006/1141/of2006-1141_imagery.zip"},{"id":7776,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1141/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6602cd","contributors":{"authors":[{"text":"Norman, Laura M. 0000-0002-3696-8406 lnorman@usgs.gov","orcid":"https://orcid.org/0000-0002-3696-8406","contributorId":967,"corporation":false,"usgs":true,"family":"Norman","given":"Laura","email":"lnorman@usgs.gov","middleInitial":"M.","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":287690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gishey, Michael","contributorId":102754,"corporation":false,"usgs":true,"family":"Gishey","given":"Michael","email":"","affiliations":[],"preferred":false,"id":287695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gass, Leila 0000-0002-3436-262X lgass@usgs.gov","orcid":"https://orcid.org/0000-0002-3436-262X","contributorId":3770,"corporation":false,"usgs":true,"family":"Gass","given":"Leila","email":"lgass@usgs.gov","affiliations":[{"id":657,"text":"Western Geographic Science Center","active":true,"usgs":true}],"preferred":true,"id":287691,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yanites, Brian","contributorId":91373,"corporation":false,"usgs":true,"family":"Yanites","given":"Brian","affiliations":[],"preferred":false,"id":287694,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pfeifer, Edwin epfeifer@usgs.gov","contributorId":569,"corporation":false,"usgs":true,"family":"Pfeifer","given":"Edwin","email":"epfeifer@usgs.gov","affiliations":[],"preferred":true,"id":287689,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Simms, Ron","contributorId":19439,"corporation":false,"usgs":true,"family":"Simms","given":"Ron","email":"","affiliations":[],"preferred":false,"id":287692,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ahlbrandt, Ray","contributorId":26935,"corporation":false,"usgs":true,"family":"Ahlbrandt","given":"Ray","email":"","affiliations":[],"preferred":false,"id":287693,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":76719,"text":"ofr20061001 - 2006 - Transport pathways in the lower reaches of Hood Canal","interactions":[],"lastModifiedDate":"2023-02-07T20:02:51.191172","indexId":"ofr20061001","displayToPublicDate":"2006-05-15T00:00:00","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":"2006-1001","title":"Transport pathways in the lower reaches of Hood Canal","docAbstract":"In 2003, studies revealed that the waters in the lower reaches of Hood Canal in Washington State had very low dissolved-oxygen concentrations, low enough to cause some fish kills between June and October of that year. In order to determine the transport patterns and the persistence of the low oxygen level in this portion of the canal, the U. S. Geological Survey deployed two instrumented platforms on the seabed near the head of the canal that measured currents over the whole water column, water level, near-bed temperature, salinity and oxygen for 2 months in the fall of 2004. Tidal currents, the dominant current component in the canal, flowed primarily along the canal axis and had speeds of 15-20 cm/s. There was also a persistent internal seiche that caused currents to flow along the canal axis with speeds of a few cm/s. The seiche, which had a period of a few days, caused currents in the surface layer to flow in an opposite direction to currents in water depths deeper than 15 m. A pool of warmer, saltier and more oxygenated water moved past the measurement sites toward the head of the canal with a speed of 1 cm/s. CTD measurements taken near the 2 measurement sites during the deployment indicated that this more oxygenated layer of water extended from the bed to the thermocline. Oxygen data from the tripods showed that this water remained in the region until at least the end of October 2004, when the tripods were recovered.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061001","usgsCitation":"Noble, M.A., Gartner, A.L., Paulson, A.J., Xu, J., Josberger, E.G., and Curran, C., 2006, Transport pathways in the lower reaches of Hood Canal (Version 1.0): U.S. Geological Survey Open-File Report 2006-1001, 55 p., https://doi.org/10.3133/ofr20061001.","productDescription":"55 p.","numberOfPages":"55","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":193088,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":412820,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76567.htm","linkFileType":{"id":5,"text":"html"}},{"id":7783,"rank":3,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/2006/1001/version_history.txt","linkFileType":{"id":2,"text":"txt"}},{"id":7782,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1001/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Hood Canal","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -123.1359555181476,\n 47.30834939148622\n ],\n [\n -122.74790911503446,\n 47.43744127703286\n ],\n [\n -122.56920353465327,\n 47.546691205897616\n ],\n [\n -122.54197220811939,\n 47.68436632590738\n ],\n [\n -122.56920353465327,\n 47.91416032963039\n ],\n [\n -122.6866386303324,\n 47.96546752833669\n ],\n [\n -122.87895987398048,\n 47.84681373747895\n ],\n [\n -123.04404979109472,\n 47.579995910047444\n ],\n [\n -123.19892796075814,\n 47.37293483446297\n ],\n [\n -123.1359555181476,\n 47.30834939148622\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626c0f","contributors":{"authors":[{"text":"Noble, Marlene A. mnoble@usgs.gov","contributorId":1429,"corporation":false,"usgs":true,"family":"Noble","given":"Marlene","email":"mnoble@usgs.gov","middleInitial":"A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":287702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, Anne L.","contributorId":32620,"corporation":false,"usgs":true,"family":"Gartner","given":"Anne","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Paulson, Anthony J. 0000-0002-2358-8834 apaulson@usgs.gov","orcid":"https://orcid.org/0000-0002-2358-8834","contributorId":5236,"corporation":false,"usgs":true,"family":"Paulson","given":"Anthony","email":"apaulson@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":287705,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Xu, Jingping jpx@usgs.gov","contributorId":2574,"corporation":false,"usgs":true,"family":"Xu","given":"Jingping","email":"jpx@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":287704,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Josberger, Edward G. ejosberg@usgs.gov","contributorId":1710,"corporation":false,"usgs":true,"family":"Josberger","given":"Edward","email":"ejosberg@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":287703,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Curran, Christopher","contributorId":61114,"corporation":false,"usgs":true,"family":"Curran","given":"Christopher","affiliations":[],"preferred":false,"id":287707,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":76720,"text":"ofr20061068 - 2006 - Conodont and Radiolarian Data from the De Long Mountains Quadrangle and Adjacent Areas, Northern Alaska","interactions":[],"lastModifiedDate":"2018-05-07T21:03:38","indexId":"ofr20061068","displayToPublicDate":"2006-05-15T00:00:00","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":"2006-1068","title":"Conodont and Radiolarian Data from the De Long Mountains Quadrangle and Adjacent Areas, Northern Alaska","docAbstract":"

INTRODUCTION This report presents biostratigraphic data from 289 collections at 189 localities in the De Long Mountains, Misheguk Mountain, and Noatak quadrangles (fig. 1); most of these data have never been previously published. The collections were made during studies of the Red Dog massive sulfide deposit in 1998?2004 and in support of regional mapping projects in 1979, 1981, 1983, and 1997?98. The collections?mostly conodonts and some radiolarians?tightly constrain the age of many stratigraphic units of Devonian through Triassic age exposed within the study area, and provide additional data on the depositional environments and thermal history of these rocks. The data are presented in a series of tables, organized by fossil type, stratigraphic unit, and location. Tables 1?12 contain conodont data, mostly from the De Long Mountains quadrangle. All of these collections were initially examined, or were reevaluated, from 1997 through 2004, and complete faunal lists are given for all samples. Table 13 lists ages and conodont color alteration indices (CAIs) of 27 collections from 24 localities in the Noatak quadrangle; updated faunal lists were not prepared for these samples. Radiolarian data?all from the De Long Mountains quadrangle?are given in table 14; these collections were analyzed between 1998 and 2003. Collection localities are shown in four maps (sheets 1, 2). Map 1 (sheet 1) shows all outcrop samples from the De Long Mountains and western Misheguk Mountain quadrangle (locs. 1-121). Maps 2?4 (sheets 1, 2) show all drill hole sample localities; samples come from the Su-Lik deposit and in and around the Anarraaq deposit (map 2, locs. 122?135), in and adjacent to the Red Dog deposits (Paalaaq, Aqqaluk, Main, and Qanaiyaq) (map 3, locs. 136?158), and from drill holes along the Port Road in the Noatak quadrangle (map 4, locs. 159?160). Map 4 (sheet 2) also shows all outcrop samples from the Noatak quadrangle (locs. 161?189). The text summarizes the lithofacies, age, and biofacies of the Paleozoic and Mesozoic stratigraphic units that produced the fossil collections presented in the tables. Many of the data for the Lisburne Group are taken from Dumoulin and others (2004). Plates 1?4 illustrate important conodonts from the collections listed herein, as well as from coeval collections in the Howard Pass quadrangle; information about the Howard Pass conodonts is given in Table 15.

","language":"English","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20061068","usgsCitation":"Dumoulin, J.A., Harris, A.G., Blome, C.D., and Young, L.E., 2006, Conodont and Radiolarian Data from the De Long Mountains Quadrangle and Adjacent Areas, Northern Alaska (Version 1.0): U.S. Geological Survey Open-File Report 2006-1068, Report: iv, 170 p.; Plates; Sheets; Data Files, https://doi.org/10.3133/ofr20061068.","productDescription":"Report: iv, 170 p.; Plates; Sheets; Data Files","numberOfPages":"174","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":194458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7785,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2006/1068/of2006-1068_plates/","linkFileType":{"id":5,"text":"html"}},{"id":7784,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1068/","linkFileType":{"id":5,"text":"html"}},{"id":7786,"rank":9999,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/of/2006/1068/of2006-1068_sheets/","linkFileType":{"id":5,"text":"html"}}],"scale":"0","projection":"Universal Transverse Mercator","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6993c7","contributors":{"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":287708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, Anita G.","contributorId":50162,"corporation":false,"usgs":true,"family":"Harris","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":287710,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blome, Charles D. 0000-0002-3449-9378 cblome@usgs.gov","orcid":"https://orcid.org/0000-0002-3449-9378","contributorId":1246,"corporation":false,"usgs":true,"family":"Blome","given":"Charles","email":"cblome@usgs.gov","middleInitial":"D.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":287709,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Young, Lorne E.","contributorId":67611,"corporation":false,"usgs":true,"family":"Young","given":"Lorne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":287711,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70178403,"text":"70178403 - 2006 - Groundwater in geologic processes, 2nd edition","interactions":[],"lastModifiedDate":"2019-04-08T09:04:37","indexId":"70178403","displayToPublicDate":"2006-05-15T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Groundwater in geologic processes, 2nd edition","docAbstract":"
Interest in the role of Groundwater in Geologic Processes has increased steadily over the past few decades. Hydrogeologists and geologists are now actively exploring the role of groundwater and other subsurface fluids in such fundamental geologic processes as crustal heat transfer, ore deposition, hydrocarbon migration, earthquakes, tectonic deformation, diagenesis, and metamorphism.

Groundwater in Geologic Processes is the first comprehensive treatment of this body of inquiry. Chapters 1 to 4 develop the basic theories of groundwater motion, hydromechanics, solute transport, and heat transport. Chapter 5 applies these theories to regional groundwater flow systems in a generic sense, and Chapters 6 to 13 focus on particular geologic processes and environments. Relative to the first edition of Groundwater in Geologic Processes , this second edition includes a much more comprehensive treatment of hydromechanics (the coupling of groundwater flow and deformation). It also includes new chapters on \"compaction and diagenesis,\" \"metamorphism,\" and \"subsea hydrogeology.\" Finally, it takes advantage of the substantial body of published research that has appeared since the first edition in 1998.

The systematic presentation of theory and application, and the problem sets that conclude each chapter, make this book ideal for undergraduate- and graduate-level geology courses (assuming that the students have some background in calculus and introductory chemistry). It also serves as an invaluable reference for researchers and other professionals in the field
","language":"English","publisher":"Cambridge University Press","isbn":"9780521603218","usgsCitation":"Ingebritsen, S.E., Sanford, W.E., and Neuzil, C.E., 2006, Groundwater in geologic processes, 2nd edition, 564 p.","productDescription":"564 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":331087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331086,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.cambridge.org/us/academic/subjects/earth-and-environmental-science/hydrology-hydrogeology-and-water-resources/groundwater-geologic-processes-2nd-edition?format=PB"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"582dd8ebe4b04d580bd3fa9d","contributors":{"authors":[{"text":"Ingebritsen, Steven E. 0000-0001-6917-9369 seingebr@usgs.gov","orcid":"https://orcid.org/0000-0001-6917-9369","contributorId":818,"corporation":false,"usgs":true,"family":"Ingebritsen","given":"Steven","email":"seingebr@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":653985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanford, Ward E. 0000-0002-6624-0280 wsanford@usgs.gov","orcid":"https://orcid.org/0000-0002-6624-0280","contributorId":2268,"corporation":false,"usgs":true,"family":"Sanford","given":"Ward","email":"wsanford@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":653986,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neuzil, Christopher E. 0000-0003-2022-4055 ceneuzil@usgs.gov","orcid":"https://orcid.org/0000-0003-2022-4055","contributorId":2322,"corporation":false,"usgs":true,"family":"Neuzil","given":"Christopher","email":"ceneuzil@usgs.gov","middleInitial":"E.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":653987,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":76718,"text":"sir20065097 - 2006 - Ground-water flow model of the Boone formation at the Tar Creek superfund site, Oklahoma and Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:14:21","indexId":"sir20065097","displayToPublicDate":"2006-05-15T00:00:00","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":"2006-5097","title":"Ground-water flow model of the Boone formation at the Tar Creek superfund site, Oklahoma and Kansas","docAbstract":"Extensive mining activities conducted at the Tar Creek Superfund site, one of the largest Superfund sites in the United States, pose substantial health and safety risks. Mining activities removed a total of about 6,000,000 tons of lead and zinc by 1949. To evaluate the effect of this mining on the ground-water flow, a MODFLOW 2000 digital model has been developed to simulate ground-water flow in the carbonate formations of Mississippian age underlying the Tar Creek Superfund site. The model consists of three layers of variable thickness and a grid of 580 rows by 680 columns of cells 164 feet (50 meters) on a side. Model flux boundary conditions are specified for rivers and general head boundaries along the northern boundary of the Boone Formation. Selected cells in layer 1 are simulated as drain cells. Model calibration has been performed to minimize the difference between simulated and observed water levels in the Boone Formation. Hydraulic conductivity values specified during calibration range from 1.3 to 35 feet per day for the Boone Formation with the larger values occurring along the axis of the Miami Syncline where horizontal anisotropy is specified as 10 to 1. Hydraulic conductivity associated with the mine void is set at 50,000 feet per day and a specific yield of 1.0 is specified to represent that the mine void is filled completely with water. Residuals (the difference between measured and simulated ground-water altitudes) has a root-mean-squared value of 8.53 feet and an absolute mean value of 7.29 feet for 17 observed values of water levels in the Boone Formation.\r\n\r\nThe utility of the model for simulating and evaluating the possible consequences of remediation activities has been demonstrated. The model was used to simulate the emplacement of chat (mine waste consisting of fines and fragments of chert) back into the mine. Scenarios using 1,800,000 and 6,500,000 tons of chat were run. Hydraulic conductivity was reduced from 50,000 feet per day to 35 feet per day in the model cells corresponding to chat emplacement locations. A comparison of the simulated baseline conditions and conditions after simulated chat emplacement revealed little change in water levels, drainage and stream flux, and ground-water flow velocity.\r\n\r\nUsing the calibrated flow model, particle tracks were simulated using MODPATH to evaluate the simultaneous movement of particles with water in the vicinity of four potential sites at which various volumes of chat might be emplaced in the underground mine workings as part of potential remediation efforts at the site. Particle tracks were generated to follow the rate and direction of water movement for a simulated period of 100 years. In general, chat emplacement had minimal effect on the direction and rate of movement when compared to baseline (current) flow conditions. Water-level differences between baseline and chat-emplacement scenarios showed declines as much as 2 to 3 feet in areas immediately downgradient from the chat emplacement cells and little or no head change upgradient. Chat emplacements had minimal effect on changes in surfacewater flux with the largest simulated difference in one cell between baseline and chat emplacement scenarios being about 3.5 gallons per minute.","language":"ENGLISH","doi":"10.3133/sir20065097","collaboration":"Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce\r\nany copyrighted materials contained within this report.","usgsCitation":"Reed, T., and Czarnecki, J.B., 2006, Ground-water flow model of the Boone formation at the Tar Creek superfund site, Oklahoma and Kansas: U.S. Geological Survey Scientific Investigations Report 2006-5097, 41 p., https://doi.org/10.3133/sir20065097.","productDescription":"41 p.","numberOfPages":"41","onlineOnly":"Y","costCenters":[],"links":[{"id":194521,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7781,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2006/5097/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669640","contributors":{"authors":[{"text":"Reed, T.B.","contributorId":56658,"corporation":false,"usgs":true,"family":"Reed","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":287701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Czarnecki, John B. jczarnec@usgs.gov","contributorId":2555,"corporation":false,"usgs":true,"family":"Czarnecki","given":"John","email":"jczarnec@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":287700,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":76715,"text":"fs20053110 - 2006 - Imperiled species and communities threatened by invasive species","interactions":[],"lastModifiedDate":"2012-02-02T00:14:18","indexId":"fs20053110","displayToPublicDate":"2006-05-13T00:00:00","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":"2005-3110","title":"Imperiled species and communities threatened by invasive species","language":"ENGLISH","doi":"10.3133/fs20053110","usgsCitation":"Muir, R., and Gross, S., 2006, Imperiled species and communities threatened by invasive species: U.S. Geological Survey Fact Sheet 2005-3110, 2 p., https://doi.org/10.3133/fs20053110.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":121237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3110.jpg"},{"id":7770,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3110/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8483","contributors":{"authors":[{"text":"Muir, Rachel rmuir@usgs.gov","contributorId":5823,"corporation":false,"usgs":true,"family":"Muir","given":"Rachel","email":"rmuir@usgs.gov","affiliations":[{"id":506,"text":"Office of the AD Ecosystems","active":true,"usgs":true}],"preferred":true,"id":287687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gross, Sharon","contributorId":80372,"corporation":false,"usgs":true,"family":"Gross","given":"Sharon","email":"","affiliations":[],"preferred":false,"id":287688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":76714,"text":"ofr20061109 - 2006 - Mapa Geologico de Venezuela a Escala 1:750,000","interactions":[],"lastModifiedDate":"2026-01-29T20:59:14.658548","indexId":"ofr20061109","displayToPublicDate":"2006-05-13T00:00:00","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":"2006-1109","title":"Mapa Geologico de Venezuela a Escala 1:750,000","docAbstract":"Se presenta un mapa geologico digital de Venezuela sobre un fondo de relieve sombreado. Los datos geologicos e hidrologicos del norte del rio Orinoco proceden de la digitalizacion de mapas geologicos en papel a escala 1:500.000. Estos datos fueron integrados con el mapa geologico digital del Escudo de Guayana Venezolano, a su vez derivado de hojas en papel a escala 1:500.000. La informacion sobre los tipos de fallas mostrados en el mapa es igual que en las fuentes originales. Los poligonos geologicos fueron atribuidos por edad, litologia y nombre de la unidad siguiendo el Codigo geologico de Venezuela. Se incorporaron revisiones significativas de la geologia de la Cordillera de la Costa a partir de las nuevas hojas integradas a escala 1:25.000. Toda esta informacion geologico-estructural se sobrepuso a una imagen de relieve sombreado, producida por el procesamiento de los datos de radar interferometrico con 90 m (3 arcosegundos) de resolucion espacial obtenidos por la mision topografica de radar del transbordador espacial (SRTM). Las areas de la base de datos del SRTM carentes de informacion fueron llenadas por medio de la interpolacion de los datos de las celdas adyacentes. Para producir la imagen de relieve sombreado se uso una direccion de iluminacion de 315 deg con un angulo de 65 deg sobre el horizonte. La proyeccion usada en el mapa es conica equidistante, con latitudes de 4 y 9 deg norte como paralelos estandar y una longitud de 66 deg al oeste como meridiano central.\r\n\r\nLos datos en el mapa proceden primordialment de hojas a escala 1:500.000 y el producto esta preparado para una impresion optima en escala 1:750.000. Los usuarios pueden obtener ampliaciones mayores, sin embargo no se garantiza la precision del mapa a escalas mas detalladas.\r\n\r\nEspecialmente en la region de Guayana, al sobreponer los mapas geologicos sobre la reciente imagen SRTM, se notan grandes discrepancias no sistematicas tanto en contactos como en fallas. Esto es debido a que los mapas geologicos de Guayana tienen como base topografica las imagenes de radar de vision lateral (SLAR), con muy control de campo de los a?os 1970's. La correccion de estos desfases esta planificada para el futuro.","language":"Spanish","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061109","collaboration":"Spanish language version of OFR 2005-1038","usgsCitation":"Hackley, P.C., Urbani, F., Karlsen, A., and Garrity, C.P., 2006, Mapa Geologico de Venezuela a Escala 1:750,000 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1109, 8 map sheets, sizes vary, https://doi.org/10.3133/ofr20061109.","productDescription":"8 map sheets, sizes vary","onlineOnly":"Y","costCenters":[],"links":[{"id":7769,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1109/","linkFileType":{"id":5,"text":"html"}},{"id":194520,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"750000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ebe","contributors":{"authors":[{"text":"Hackley, Paul C. 0000-0002-5957-2551 phackley@usgs.gov","orcid":"https://orcid.org/0000-0002-5957-2551","contributorId":592,"corporation":false,"usgs":true,"family":"Hackley","given":"Paul","email":"phackley@usgs.gov","middleInitial":"C.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":287683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Urbani, Franco","contributorId":67163,"corporation":false,"usgs":true,"family":"Urbani","given":"Franco","email":"","affiliations":[],"preferred":false,"id":287685,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Karlsen, Alex W.","contributorId":78789,"corporation":false,"usgs":true,"family":"Karlsen","given":"Alex W.","affiliations":[],"preferred":false,"id":287686,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Garrity, Christopher P. 0000-0002-5565-1818 cgarrity@usgs.gov","orcid":"https://orcid.org/0000-0002-5565-1818","contributorId":644,"corporation":false,"usgs":true,"family":"Garrity","given":"Christopher","email":"cgarrity@usgs.gov","middleInitial":"P.","affiliations":[{"id":5061,"text":"National Cooperative Geologic Mapping and Landslide Hazards","active":true,"usgs":true},{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":287684,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":76711,"text":"ofr20061134 - 2006 - Geologic and hydrogeologic framework of the Espa?ola basin -- Proceedings of the 5th annual Espa?ola basin workshop, Santa Fe, New Mexico, March 7-8, 2006","interactions":[],"lastModifiedDate":"2012-02-02T00:14:07","indexId":"ofr20061134","displayToPublicDate":"2006-05-13T00:00:00","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":"2006-1134","title":"Geologic and hydrogeologic framework of the Espa?ola basin -- Proceedings of the 5th annual Espa?ola basin workshop, Santa Fe, New Mexico, March 7-8, 2006","docAbstract":"This report presents abstracts of technical studies that are focused on the hydrogeologic framework of the Espa?ola basin, a major subbasin of the Cenozoic Rio Grande rift. The Rio Grande, Rio Chama, Santa Fe River, and their tributaries carry important surface water in the Espa?ola basin. Sediments and interbedded volcanic rocks fill the Espa?ola basin and form extensive aquifer systems for ground water. Surface and ground water provide the principal sources of water for most residents of the basin, including people in the cities of Santa Fe, Espa?ola, and Los Alamos as well as Native Americans in several Pueblos.\r\n\r\nThe abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the fifth-annual Espa?ola basin workshop, held March 7-8 of 2006 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies.\r\n\r\nThe Espa?ola basin workshop was hosted by the Espa?ola basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and the Water Research Technical Assistance Office of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework.\r\n\r\nAbstracts submitted by U.S. Geological Survey authors in this report have had their technical content peer reviewed before they were included in the report. Technical reviews were not required for abstracts submitted by authors outside the USGS, although most did receive peer reviews within their originating agencies. Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Espa?ola basin.","language":"ENGLISH","doi":"10.3133/ofr20061134","usgsCitation":"McKinney, K.C., 2006, Geologic and hydrogeologic framework of the Espa?ola basin -- Proceedings of the 5th annual Espa?ola basin workshop, Santa Fe, New Mexico, March 7-8, 2006 (Version 1.0): U.S. Geological Survey Open-File Report 2006-1134, 40 p., https://doi.org/10.3133/ofr20061134.","productDescription":"40 p.","numberOfPages":"40","onlineOnly":"Y","temporalStart":"2006-03-07","temporalEnd":"2006-03-08","costCenters":[],"links":[{"id":192367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7766,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1134/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8231","contributors":{"authors":[{"text":"McKinney, Kevin C. kcmckinney@usgs.gov","contributorId":3406,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","email":"kcmckinney@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":287677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":76712,"text":"ofr20061064 - 2006 - Rainfall thresholds for forecasting landslides in the Seattle, Washington, area — Exceedance and probability","interactions":[],"lastModifiedDate":"2022-01-26T19:40:58.839957","indexId":"ofr20061064","displayToPublicDate":"2006-05-13T00:00:00","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":"2006-1064","title":"Rainfall thresholds for forecasting landslides in the Seattle, Washington, area — Exceedance and probability","docAbstract":"

Empirical rainfall thresholds and related information form a basis for forecasting landslides in the Seattle area. A formula for a cumulative rainfall threshold (CT), P3=3.5–0.67P15, defined by rainfall amounts (in inches) during the last 3 days (72 hours), P3, and the previous 15 days (360 hours), P15, was developed from analysis of historical data for 91 landslides that occurred as part of 3-day events of three or more landslides between 1933 and 1997. Comparison with historical records for 577 landslides (including some used in developing the CT) indicates that the CT captures more than 90 percent of historical landslide events of three or more landslides in 1-day and 3-day periods that were recorded from 1978 to 2003. However, the probability of landslide occurrence on a day when the CT is exceeded at any single rain gage (8.4 percent) is low, and additional criteria are needed to confidently forecast landslide occurrence. Exceedance of a rainfall intensity-duration threshold I=3.257D–1.13, for intensity, I, (inch per hour) and duration, D, (hours), corresponds to a higher probability of landslide occurrence (42 percent at any 3 rain gages or 65 percent at any 10 rain gages), but it predicts fewer landslides. Both thresholds must be used in tandem to forecast landslide occurrence in Seattle.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061064","usgsCitation":"Chleborad, A.F., Baum, R.L., and Godt, J.W., 2006, Rainfall thresholds for forecasting landslides in the Seattle, Washington, area — Exceedance and probability (Version 1.0): U.S. Geological Survey Open-File Report 2006-1064, iv, 31 p., https://doi.org/10.3133/ofr20061064.","productDescription":"iv, 31 p.","numberOfPages":"35","onlineOnly":"Y","costCenters":[],"links":[{"id":190807,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394897,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76532.htm"},{"id":7767,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1064/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","city":"Seattle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.42614746093749,\n 47.44666502261753\n ],\n [\n -122.23663330078124,\n 47.44666502261753\n ],\n [\n -122.23663330078124,\n 47.85924575819688\n ],\n [\n -122.42614746093749,\n 47.85924575819688\n ],\n [\n -122.42614746093749,\n 47.44666502261753\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e8f1","contributors":{"authors":[{"text":"Chleborad, Alan F.","contributorId":87578,"corporation":false,"usgs":true,"family":"Chleborad","given":"Alan","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":287680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baum, Rex L. 0000-0001-5337-1970 baum@usgs.gov","orcid":"https://orcid.org/0000-0001-5337-1970","contributorId":1288,"corporation":false,"usgs":true,"family":"Baum","given":"Rex","email":"baum@usgs.gov","middleInitial":"L.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":287679,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Godt, Jonathan W. 0000-0002-8737-2493 jgodt@usgs.gov","orcid":"https://orcid.org/0000-0002-8737-2493","contributorId":1166,"corporation":false,"usgs":true,"family":"Godt","given":"Jonathan","email":"jgodt@usgs.gov","middleInitial":"W.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":287678,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":76713,"text":"ofr20061120 - 2006 - Magnetotelluric data collected near geophysically logged boreholes in the Española and Middle Rio Grande Basins, New Mexico","interactions":[],"lastModifiedDate":"2021-10-14T19:35:27.178391","indexId":"ofr20061120","displayToPublicDate":"2006-05-13T00:00:00","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":"2006-1120","title":"Magnetotelluric data collected near geophysically logged boreholes in the Española and Middle Rio Grande Basins, New Mexico","docAbstract":"

The Santa Fe region is growing rapidly. The Santa Fe Group aquifer in the Española Basin is the main source of municipal water for the region, and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's ground-water resources. An important issue in managing the ground-water resources is a better understanding of the hydrogeology of the Tertiary Santa Fe Group. The Santa Fe Group includes the sedimentary deposits that fill the Rio Grande rift and contain the principal ground-water aquifers. The U.S. Geological Survey (USGS) is conducting a series of multidisciplinary studies of the Española Basin in northern New Mexico. Detailed geologic mapping, high-resolution airborne magnetic surveys, electromagnetic surveys, and hydrologic, lithologic, and hydro-geochemical data are being used to better understand the aquifer systems. Magnetotelluric (MT) surveys were completed as part of these studies. The primary purpose of the MT surveys was to map changes in electrical resistivity with depth that are related to differences in various rock types that help control the properties of aquifers in the region. Resistivity modeling of the MT data can be used to investigate buried structures related to the basic geologic framework of the study area. The purpose of this report is to release MT sounding data collected near geophysically logged boreholes in the study area, including the nearby Middle Rio Grande Basin. This MT data can be used in subsequent resistivity modeling. No interpretation of the data is included in this report.

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This has created a need for classifying coastal lands and evaluating storm-hazard vulnerability. Government officials and resource managers responsible for dealing with natural hazards also need accurate assessments of potential storm impacts in order to make informed decisions before, during, and after major storm events. Both economic development and coastal-damage mitigation require integrated models of storm parameters, hazard vulnerability, and expected coastal responses. Thus, storm-hazard vulnerability assessments constitute one of the fundamental components of forecasting storm impacts.\r\n\r\nEach year as many as 10 to 12 hurricanes and tropical storms will be the focus of national attention. Of particular interest are intense hurricanes (Categories 3 to 5 of the Saffir-Simpson Hurricane Scale) that have the potential to cause substantial economic and environmental damage to the Atlantic and Gulf Coasts of the United States. These coastal regions include some of the largest metropolitan areas in the country and they continue to experience rapid population growth. Based on media reports, there is a general lack of public knowledge regarding how different coastal segments will respond to the same storm or how the same coastal segment will respond differently depending on storm conditions.\r\n\r\nA primary purpose of the USGS National Assessment of Coastal Change Project is to provide accurate representations of pre-storm ground conditions for areas that are designated high priority because they have dense populations or valuable resources that are at risk. A secondary purpose is to develop a broad coastal classification that, with only minor modification, can be applied to most coastal regions in the United States.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Coastal Classification Atlas","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20061133","usgsCitation":"Morton, R., and Peterson, R.L., 2006, Coastal classification atlas: South Texas coastal classification maps: Mansfield Channel to the Rio Grande: U.S. Geological Survey Open-File Report 2006-1133, HTML Document, https://doi.org/10.3133/ofr20061133.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":422985,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_76531.htm","linkFileType":{"id":5,"text":"html"}},{"id":192235,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7760,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1133/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","otherGeospatial":"Mansfield Channel, Rio Grande","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -97.44773285969062,\n 26.92200388384326\n ],\n [\n -97.24224431455427,\n 25.99446229085062\n ],\n [\n -97.1335908395723,\n 25.988926377530746\n ],\n [\n -97.20037461674151,\n 26.46008894232383\n ],\n [\n -97.34524404106283,\n 26.909174797589287\n ],\n [\n -97.44773285969062,\n 26.92200388384326\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698651","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":287671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Russell L.","contributorId":55045,"corporation":false,"usgs":true,"family":"Peterson","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":287670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":76710,"text":"cir1196W - 2006 - Aluminum recycling in the United States in 2000","interactions":[{"subject":{"id":71079,"text":"ofr20051051 - 2005 - Aluminum recycling in the United States in 2000","indexId":"ofr20051051","publicationYear":"2005","noYear":false,"title":"Aluminum recycling in the United States in 2000"},"predicate":"SUPERSEDED_BY","object":{"id":76710,"text":"cir1196W - 2006 - Aluminum recycling in the United States in 2000","indexId":"cir1196W","publicationYear":"2006","noYear":false,"chapter":"W","title":"Aluminum recycling in the United States in 2000"},"id":1}],"lastModifiedDate":"2012-02-02T00:14:11","indexId":"cir1196W","displayToPublicDate":"2006-05-12T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1196","chapter":"W","title":"Aluminum recycling in the United States in 2000","docAbstract":"As one of a series of reports on metals recycling, this report discusses the flow of aluminum from production through its uses with particular emphasis on the recycling of industrial scrap (new scrap) and used products (old scrap) in 2000. This materials flow study includes a description of aluminum supply and demand factors for the United States to illustrate the extent of aluminum recycling and to identify recycling trends. Understanding the system of materials flow from source to ultimate disposition can assist in improving the management of natural resources in a manner that is compatible with sound environmental practices. In 2000, the old scrap recycling efficiency for aluminum was estimated to be 42 percent. Almost 60 percent of the aluminum that was recycled in 2000 came from new scrap, and the recycling rate was estimated to be 36 percent. The principal source of old scrap was recycled aluminum beverage cans.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Flow Studies for Recycling Metal Commodities in the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/cir1196W","usgsCitation":"Plunkert, P.A., 2006, Aluminum recycling in the United States in 2000 (Version 1.0): U.S. Geological Survey Circular 1196, 16 p., https://doi.org/10.3133/cir1196W.","productDescription":"16 p.","numberOfPages":"16","onlineOnly":"Y","temporalStart":"2000-01-01","temporalEnd":"2000-12-31","costCenters":[],"links":[{"id":7765,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/c1196w/","linkFileType":{"id":5,"text":"html"}},{"id":192138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686984","contributors":{"authors":[{"text":"Plunkert, Patricia A.","contributorId":34593,"corporation":false,"usgs":true,"family":"Plunkert","given":"Patricia","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287676,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":76708,"text":"fs20063052 - 2006 - Microbial ecology in reef sediments of Biscayne National Park","interactions":[],"lastModifiedDate":"2012-02-02T00:14:23","indexId":"fs20063052","displayToPublicDate":"2006-05-12T00:00:00","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":"2006-3052","title":"Microbial ecology in reef sediments of Biscayne National Park","language":"ENGLISH","doi":"10.3133/fs20063052","usgsCitation":"Lisle, J.T., and Reich, C., 2006, Microbial ecology in reef sediments of Biscayne National Park: U.S. Geological Survey Fact Sheet 2006-3052, 4 p., https://doi.org/10.3133/fs20063052.","productDescription":"4 p.","numberOfPages":"4","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":120721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3052.jpg"},{"id":7764,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3052/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62dfc1","contributors":{"authors":[{"text":"Lisle, John T. 0000-0002-5447-2092 jlisle@usgs.gov","orcid":"https://orcid.org/0000-0002-5447-2092","contributorId":2944,"corporation":false,"usgs":true,"family":"Lisle","given":"John","email":"jlisle@usgs.gov","middleInitial":"T.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":287674,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reich, Chris","contributorId":27953,"corporation":false,"usgs":true,"family":"Reich","given":"Chris","affiliations":[],"preferred":false,"id":287675,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":76707,"text":"fs20063045 - 2006 - Microbiology and public beach safety: integrated science for the protection of public health","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"fs20063045","displayToPublicDate":"2006-05-12T00:00:00","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":"2006-3045","title":"Microbiology and public beach safety: integrated science for the protection of public health","language":"ENGLISH","doi":"10.3133/fs20063045","usgsCitation":"Kellogg, C.A., and Lisle, J.T., 2006, Microbiology and public beach safety: integrated science for the protection of public health: U.S. Geological Survey Fact Sheet 2006-3045, 2 p., https://doi.org/10.3133/fs20063045.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":123017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2006_3045.jpg"},{"id":7763,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2006/3045/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e2cd","contributors":{"authors":[{"text":"Kellogg, Christine A.","contributorId":57965,"corporation":false,"usgs":true,"family":"Kellogg","given":"Christine","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":287673,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lisle, John T. 0000-0002-5447-2092 jlisle@usgs.gov","orcid":"https://orcid.org/0000-0002-5447-2092","contributorId":2944,"corporation":false,"usgs":true,"family":"Lisle","given":"John","email":"jlisle@usgs.gov","middleInitial":"T.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":287672,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":76705,"text":"ofr20061111 - 2006 - Stocks and flows of lead-based wheel weights in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:14:07","indexId":"ofr20061111","displayToPublicDate":"2006-05-11T00:00:00","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":"2006-1111","title":"Stocks and flows of lead-based wheel weights in the United States","docAbstract":"Lead is used in many widely known applications, such as automobile batteries and radiation shielding. Another lesser known, but long-term, use of lead is in automotive vehicle wheel weights. Lead weights have been used to balance\r\nwheels since the 1930s because of its high specific gravity, low relative cost, and its malleability. Out-of-balance tires tend to 'cup' and vibrate and as a result cause excessive wear on tires and vehicle suspension components and result in compromised handling, especially at high speeds. The mass, number, and style of weights needed to balance a wheel depend on the tire's size and weight and on the type and condition of the wheels (rims) on the vehicle. This study addresses an accounting of the stocks and flows of lead contained in lead wheel weights from their manufacture, through use, dissipation, and recycling, and environmental issues associated with the use of lead.","language":"ENGLISH","doi":"10.3133/ofr20061111","usgsCitation":"Bleiwas, D.I., 2006, Stocks and flows of lead-based wheel weights in the United States (Version 1.0): U.S. Geological Survey Open-File Report 2006-1111, 16 p., https://doi.org/10.3133/ofr20061111.","productDescription":"16 p.","numberOfPages":"16","onlineOnly":"Y","costCenters":[],"links":[{"id":192256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7759,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1111/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b463e","contributors":{"authors":[{"text":"Bleiwas, Donald I. bleiwas@usgs.gov","contributorId":1434,"corporation":false,"usgs":true,"family":"Bleiwas","given":"Donald","email":"bleiwas@usgs.gov","middleInitial":"I.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":287669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":76704,"text":"ofr20061073 - 2006 - USGS analysis of the Australian UNCLOS submission","interactions":[],"lastModifiedDate":"2012-02-02T00:14:11","indexId":"ofr20061073","displayToPublicDate":"2006-05-11T00:00:00","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":"2006-1073","title":"USGS analysis of the Australian UNCLOS submission","docAbstract":"In November 2004, the Government of Australia made a submission to the Commission on the Limits of the Continental Shelf (CLCS) for 10 extended continental shelf (ECS) regions, utilizing Article-76 of the United Nations Convention on the Law of the Sea (UNCLOS). With information provided in the Australian Executive Summary, the USGS examined the 10 regions of the submission from geological, morphological, and resource perspectives. By their own request, the Australians asked that CLCS take no action on the Australian-Antarctic Territory. The major limitation in this analysis is that no bathymetric soundings or detailed hydrographic profiles were provided in the Australian Executive Summary that might show why the Foot of the Slope (FOS) was chosen or where the 2,500-m contour is located. This represents a major limitation because more than half of the 4,205 boundary points utilize the bathymetric formula line and more than one-third of them utilize the bathymetric constraint line. CLCS decisions on the components of this submission may set a precedent for how ECSs are treated in future submissions. Some of the key decisions will cover (a) how a 'natural prolongation' of a continental margin is determined, particularly if a bathymetric saddle that appears to determine the prolongation is in deep water and is well outside of the 200-nm limit (Exmouth Plateau), (b) defining to what extent that plateaus, rises, caps, banks and spurs that are formed of oceanic crust and from oceanic processes can be considered to be 'natural prolongations' (Kerguelen Plateau), (c) to what degree UNCLOS recognizes reefs and uninhabited micro-islands (specifically, rocks and/or sand shoals) as islands that can have an EEZ (Middleton and Elizabeth Reefs north of Lord Howe Island), and (d) how the Foot of the Slope (FOS) is chosen (Great Australian Bight). The submission contains situations that are relevant to potential future U.S. submissions and are potentially analogous to certain features of the US margins. The Australian margin has significant geological and morphological variety, similar to the US margin and gives a good idea of the complexity of issues related to the U.S. margin. Decisions about basins and ridges in the Lord Howe Rise and Three Kings Ridge regions will likely bear on the status of ridges in the Arctic, such as Lomonosov Ridge. The Naturaliste Plateau and the South Tasman Rise appear to have parallels with the Chukchi Plateau in the Arctic and the Blake Plateau off the southeastern U.S. The ECS on Macquarie Island/Ridge may determine how boundaries along ridges such as the Mariannas are treated.","language":"ENGLISH","doi":"10.3133/ofr20061073","usgsCitation":"Hutchinson, D.R., and Rowland, R.W., 2006, USGS analysis of the Australian UNCLOS submission: U.S. Geological Survey Open-File Report 2006-1073, 23 p., https://doi.org/10.3133/ofr20061073.","productDescription":"23 p.","numberOfPages":"23","onlineOnly":"Y","costCenters":[],"links":[{"id":7758,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2006/1073/","linkFileType":{"id":5,"text":"html"}},{"id":192137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611600","contributors":{"authors":[{"text":"Hutchinson, Deborah R. 0000-0002-2544-5466 dhutchinson@usgs.gov","orcid":"https://orcid.org/0000-0002-2544-5466","contributorId":521,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Deborah","email":"dhutchinson@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":287667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowland, Robert W.","contributorId":42200,"corporation":false,"usgs":true,"family":"Rowland","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":287668,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":76700,"text":"tm6A20 - 2006 - GoPhast: A graphical user interface for PHAST","interactions":[],"lastModifiedDate":"2020-01-26T16:13:55","indexId":"tm6A20","displayToPublicDate":"2006-05-09T00:00:00","publicationYear":"2006","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"6-A20","title":"GoPhast: A graphical user interface for PHAST","docAbstract":"GoPhast is a graphical user interface (GUI) for the USGS model PHAST. 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