The Alaska Volcano Observatory (AVO), a cooperative program of the U.S. Geological Survey, the Geophysical Institute of the University of Alaska Fairbanks, and the Alaska Division of Geological and Geophysical Surveys, has maintained seismic monitoring networks at historically active volcanoes in Alaska since 1988 (Power and others, 1993; Jolly and others, 1996; Jolly and others, 2001; Dixon and others, 2002). The primary objectives of this program are the seismic monitoring of active, potentially hazardous, Alaskan volcanoes and the investigation of seismic processes associated with active volcanism. This catalog presents the basic seismic data and changes in the seismic monitoring program for the period January 1, 2002 through December 31, 2002. Appendix G contains a list of publications pertaining to seismicity of Alaskan volcanoes based on these and previously recorded data. The AVO seismic network was used to monitor twenty-four volcanoes in real time in 2002. These include Mount Wrangell, Mount Spurr, Redoubt Volcano, Iliamna Volcano, Augustine Volcano, Katmai Volcanic Group (Snowy Mountain, Mount Griggs, Mount Katmai, Novarupta, Trident Volcano, Mount Mageik, Mount Martin), Aniakchak Crater, Mount Veniaminof, Pavlof Volcano, Mount Dutton, Isanotski Peaks, Shishaldin Volcano, Fisher Caldera, Westdahl Peak, Akutan Peak, Makushin Volcano, Great Sitkin Volcano, and Kanaga Volcano (Figure 1). Monitoring highlights in 2002 include an earthquake swarm at Great Sitkin Volcano in May-June; an earthquake swarm near Snowy Mountain in July-September; low frequency (1-3 Hz) tremor and long-period events at Mount Veniaminof in September-October and in December; and continuing volcanogenic seismic swarms at Shishaldin Volcano throughout the year. Instrumentation and data acquisition highlights in 2002 were the installation of a subnetwork on Okmok Volcano, the establishment of telemetry for the Mount Veniaminof subnetwork, and the change in the data acquisition system to an EARTHWORM detection system. AVO located 7430 earthquakes during 2002 in the vicinity of the monitored volcanoes. This catalog includes: (1) a description of instruments deployed in the field and their locations; (2) a description of earthquake detection, recording, analysis, and data archival systems; (3) a description of velocity models used for earthquake locations; (4) a summary of earthquakes located in 2002; and (5) an accompanying UNIX tar-file with a summary of earthquake origin times, hypocenters, magnitudes, and location quality statistics; daily station usage statistics; and all HYPOELLIPSE files used to determine the earthquake locations in 2002.
The AVO seismic network was used to monitor twenty-four volcanoes in real time in 2002. These include Mount Wrangell, Mount Spurr, Redoubt Volcano, Iliamna Volcano, Augustine Volcano, Katmai Volcanic Group (Snowy Mountain, Mount Griggs, Mount Katmai, Novarupta, Trident Volcano, Mount Mageik, Mount Martin), Aniakchak Crater, Mount Veniaminof, Pavlof Volcano, Mount Dutton, Isanotski Peaks, Shishaldin Volcano, Fisher Caldera, Westdahl Peak, Akutan Peak, Makushin Volcano, Great Sitkin Volcano, and Kanaga Volcano (Figure 1). Monitoring highlights in 2002 include an earthquake swarm at Great Sitkin Volcano in May-June; an earthquake swarm near Snowy Mountain in July-September; low frequency (1-3 Hz) tremor and long-period events at Mount Veniaminof in September-October and in December; and continuing volcanogenic seismic swarms at Shishaldin Volcano throughout the year. Instrumentation and data acquisition highlights in 2002 were the installation of a subnetwork on Okmok Volcano, the establishment of telemetry for the Mount Veniaminof subnetwork, and the change in the data acquisition system to an EARTHWORM detection system. AVO located 7430 earthquakes during 2002 in the vicinity of the monitored volcanoes.
This catalog includes: (1) a description of instruments deployed in the field and their locations; (2) a description of earthquake detection, recording, analysis, and data archival systems; (3) a description of velocity models used for earthquake locations; (4) a summary of earthquakes located in 2002; and (5) an accompanying UNIX tar-file with a summary of earthquake origin times, hypocenters, magnitudes, and location quality statistics; daily station usage statistics; and all HYPOELLIPSE files used to determine the earthquake locations in 2002.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03267","usgsCitation":"Dixon, J.P., Stihler, S.D., Power, J.A., Tytgat, G., Moran, S.C., Sánchez, J., Estes, S., McNutt, S.R., and Paskievitch, J., 2003, Catalog of earthquake hypocenters at Alaskan volcanoes: January 1 through December 31, 2002: U.S. Geological Survey Open-File Report 2003-267, Report: 58 p.; Appendix F; Data, https://doi.org/10.3133/ofr03267.","productDescription":"Report: 58 p.; Appendix F; Data","numberOfPages":"58","temporalStart":"2002-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":176326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03267.jpg"},{"id":4546,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0267/","linkFileType":{"id":5,"text":"html"}},{"id":285716,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0267/pdf/of03-267.pdf","text":"Report","size":"7.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":285717,"type":{"id":3,"text":"Appendix"},"url":"https://pubs.usgs.gov/of/2003/0267/pdf/appendixf.pdf","text":"Appendix F","size":"724 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Appendix F"},{"id":285718,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0267/2002AVOEarthquakeCatalog.tar.Z","text":"Data File","size":"13 MB","description":"Data File"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -178.90136718749997,\n 50.792047064406844\n ],\n [\n -180,\n 52\n ],\n [\n -170.33203125,\n 61.33353967329142\n ],\n [\n -153.45703125,\n 65.47650756256367\n ],\n [\n -141.15234374999997,\n 66.26685631430843\n ],\n [\n -141.15234374999997,\n 59.88893689676585\n ],\n [\n -153.8525390625,\n 53.69670647530323\n ],\n [\n -178.90136718749997,\n 50.792047064406844\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efa8d","contributors":{"authors":[{"text":"Dixon, James P. 0000-0002-8478-9971 jpdixon@usgs.gov","orcid":"https://orcid.org/0000-0002-8478-9971","contributorId":3163,"corporation":false,"usgs":true,"family":"Dixon","given":"James","email":"jpdixon@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":243839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stihler, Scott D.","contributorId":31373,"corporation":false,"usgs":true,"family":"Stihler","given":"Scott","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":243840,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Power, John A. 0000-0002-7233-4398 jpower@usgs.gov","orcid":"https://orcid.org/0000-0002-7233-4398","contributorId":2768,"corporation":false,"usgs":true,"family":"Power","given":"John","email":"jpower@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":243838,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tytgat, Guy","contributorId":71152,"corporation":false,"usgs":true,"family":"Tytgat","given":"Guy","email":"","affiliations":[],"preferred":false,"id":243843,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moran, Seth C. 0000-0001-7308-9649 smoran@usgs.gov","orcid":"https://orcid.org/0000-0001-7308-9649","contributorId":548,"corporation":false,"usgs":true,"family":"Moran","given":"Seth","email":"smoran@usgs.gov","middleInitial":"C.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":243837,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sánchez, John","contributorId":72056,"corporation":false,"usgs":true,"family":"Sánchez","given":"John","affiliations":[],"preferred":false,"id":243844,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Estes, Steve","contributorId":55881,"corporation":false,"usgs":true,"family":"Estes","given":"Steve","email":"","affiliations":[],"preferred":false,"id":243842,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"McNutt, Stephen R.","contributorId":38133,"corporation":false,"usgs":true,"family":"McNutt","given":"Stephen","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":243841,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Paskievitch, John","contributorId":74050,"corporation":false,"usgs":true,"family":"Paskievitch","given":"John","affiliations":[],"preferred":false,"id":243845,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}} ,{"id":51525,"text":"ofr03281 - 2003 - Preliminary geologic map of the Elsinore 7.5' quadrangle, Riverside County, California","interactions":[],"lastModifiedDate":"2023-06-22T16:56:22.422239","indexId":"ofr03281","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-281","title":"Preliminary geologic map of the Elsinore 7.5' quadrangle, Riverside County, California","docAbstract":"Open-File Report 03-281 contains a digital geologic map database of the Elsinore 7.5’ quadrangle, Riverside County, California that includes:
\n1. ARC/INFO (Environmental Systems Research Institute, http://www.esri.com) version 7.2.1 coverages of the various elements of the geologic map.
\n2. A Postscript file to plot the geologic map on a topographic base, and containing a Correlation of Map Units diagram (CMU), a Description of Map Units (DMU), and an index map.
\n3. Portable Document Format (.pdf) files of:
\na. This Readme; includes in Appendix I, data contained in els_met.txt
\nb. The same graphic as plotted in 2 above. Test plots have not produced precise 1:24,000-scale map sheets. Adobe Acrobat page size setting influences map scale.
\nThe Correlation of Map Units and Description of Map Units is in the editorial format of USGS Geologic Investigations Series (I-series) maps but has not been edited to comply with I-map standards. Within the geologic map data package, map units are identified by standard geologic map criteria such as formation-name, age, and lithology. Where known, grain size is indicated on the map by a subscripted letter or letters following the unit symbols as follows: lg, large boulders; b, boulder; g, gravel; a, arenaceous; s, silt; c, clay; e.g. Qyfa is a predominantly young alluvial fan deposit that is arenaceous. Multiple letters are used for more specific identification or for mixed units, e.g., Qfysa is a silty sand. In some cases, mixed units are indicated by a compound symbol; e.g., Qyf2sc. Even though this is an Open-File Report and includes the standard USGS Open-File disclaimer, the report closely adheres to the stratigraphic nomenclature of the U.S. Geological Survey. Descriptions of units can be obtained by viewing or plotting the .pdf file (3b above) or plotting the postscript file (2 above).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03281","collaboration":"Prepared in cooperation with the California Geological Survey","usgsCitation":"Morton, D.M., Weber, F.H., Alvarez, R., and Burns, D., 2003, Preliminary geologic map of the Elsinore 7.5' quadrangle, Riverside County, California (Version 1.0): U.S. Geological Survey Open-File Report 2003-281, 1 Plate: 45.50 x 31.56 inches; Readme; Metadata; Database, https://doi.org/10.3133/ofr03281.","productDescription":"1 Plate: 45.50 x 31.56 inches; Readme; Metadata; Database","numberOfPages":"18","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":110441,"rank":9,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2003/0281/pdf/README.pdf","linkFileType":{"id":5,"text":"html"},"description":"58858"},{"id":4527,"rank":8,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0281/","linkFileType":{"id":5,"text":"html"}},{"id":398350,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_58858.htm"},{"id":285730,"rank":6,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2003/0281/README.txt"},{"id":285731,"rank":4,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2003/0281/els_met.txt"},{"id":285732,"rank":3,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/2003/0281/els.tar.gz"},{"id":285733,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0281/pdf/els_map.pdf"},{"id":285734,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0281/els_map.ps.gz"},{"id":179289,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03281.gif"}],"scale":"24000","projection":"Polyconic projection","country":"United States","state":"California","county":"Riverside County","otherGeospatial":"Elsinore quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.375,33.625 ], [ -117.375,33.75 ], [ -117.25,33.75 ], [ -117.25,33.625 ], [ -117.375,33.625 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbe45","contributors":{"authors":[{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":243833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weber, F. Harold Jr.","contributorId":10466,"corporation":false,"usgs":true,"family":"Weber","given":"F.","suffix":"Jr.","email":"","middleInitial":"Harold","affiliations":[],"preferred":false,"id":243834,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alvarez, Rachel M.","contributorId":25078,"corporation":false,"usgs":true,"family":"Alvarez","given":"Rachel M.","affiliations":[],"preferred":false,"id":243836,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burns, Diane","contributorId":16093,"corporation":false,"usgs":true,"family":"Burns","given":"Diane","email":"","affiliations":[],"preferred":false,"id":243835,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":51523,"text":"ofr03293 - 2003 - Preliminary geologic map of the San Bernardino 30' x 60' quadrangle, California (includes preliminary GIS database)","interactions":[],"lastModifiedDate":"2021-09-23T19:57:05.444366","indexId":"ofr03293","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-293","title":"Preliminary geologic map of the San Bernardino 30' x 60' quadrangle, California (includes preliminary GIS database)","docAbstract":"The San Bernardino 30'x60' quadrangle, southern California, is diagonally\r\n bisected by the San Andreas Fault Zone, separating the San Gabriel and San\r\n Bernardino Mountains, major elements of California's east-oriented Transverse\r\n Ranges Province. Included in the southern part of the quadrangle is the northern\r\n part of the Peninsular Ranges Province and the northeastern part of the\r\n oil-producing Los Angeles basin. The northern part of the quadrangle includes\r\n the southern part of the Mojave Desert Province. Pre-Quaternary rocks within the\r\n San Bernardino quadrangle consist of three extensive, well-defined basement rock\r\n assemblages, the San Gabriel Mountains, San Bernardino Mountains, and the\r\n Peninsular Ranges assemblages, and a fourth assemblage restricted to a narrow\r\n block bounded by the active San Andreas Fault and the Mill Creek Fault. Each of\r\n these basement rock assemblages is characterized by a relatively unique suite of\r\n rocks that was amalgamated by the end of the Cretaceous and (or) early Cenozoic.\r\n Some Tertiary sedimentary and volcanic rocks are unique to specific assemblages,\r\n and some overlap adjacent assemblages. A few Miocene and Pliocene units cross\r\n the boundaries of adjacent assemblages, but are dominant in only one. Tectonic\r\n events directly and indirectly related to the San Andreas Fault system have\r\n partly dismembered the basement rocks during the Neogene, forming the modern-day\r\n physiographic provinces.\r\n \r\n Rocks of the four basement rock assemblages are divisible into an older suite of\r\n Late Cretaceous and older rocks and a younger suite of post-Late Cretaceous rocks.\r\n The age span of the older suite varies considerably from assemblage to assemblage,\r\n and the point in time that separates the two suites varies slightly. In the\r\n Peninsular Ranges, the older rocks were formed from the Paleozoic to the end of\r\n Late Cretaceous plutonism, and in the Transverse Ranges over a longer period of\r\n time extending from the Proterozoic to metamorphism at the end of the Cretaceous.\r\n Within the Peninsular Ranges a profound diachronous unconformity marks the\r\n pre-Late Cretaceous-post-Late Cretaceous subdivision, but within the Transverse\r\n Ranges the division appears to be slightly younger, perhaps coinciding with the\r\n end of the Cretaceous or extending into the early Cenozoic. Initial docking of\r\n Peninsular Ranges rocks with Transverse Ranges rocks appears to have occurred at\r\n the terminus of plutonism within the Peninsular Ranges. During the Paleogene\r\n there was apparently discontinuous but widespread deposition on the basement rocks\r\n and little tectonic disruption of the amalgamated older rocks. Dismemberment of\r\n these Paleogene and older rocks by strike-slip, thrust, and reverse faulting began\r\n in the Neogene and is ongoing. The Peninsular Ranges basement rock assemblage is\r\n made up of the Peninsular Ranges batholith and a variety of metasedimentary rocks.\r\n Most of the plutonic rocks of the batholith are granodiorite and tonalite in\r\n composition; primary foliation is common, mainly in the eastern part. Tertiary\r\n sedimentary rocks of the Los Angeles Basin crop out in the Puente and San Jose\r\n Hills along with the spatially associated Glendora Volcanics; both units span the\r\n boundary between the Peninsular Ranges and San Gabriel Mountains basement rock\r\n assemblages.\r\n \r\n The San Gabriel Mountains basement rock assemblage includes two discrete areas,\r\n the high standing San Gabriel Mountains and the relatively low San Bernardino\r\n basin east of the San Jacinto Fault. The basement rock assemblage is\r\n characterized by a unique suite of rocks that include anorthosite, Proterozoic\r\n and Paleozoic gneiss and schist, the Triassic","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03293","usgsCitation":"Morton, D.M., and Miller, F.K., 2003, Preliminary geologic map of the San Bernardino 30' x 60' quadrangle, California (includes preliminary GIS database): U.S. Geological Survey Open-File Report 2003-293, HTML Document, https://doi.org/10.3133/ofr03293.","productDescription":"HTML Document","costCenters":[],"links":[{"id":179112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110443,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_58935.htm","linkFileType":{"id":5,"text":"html"},"description":"58935"},{"id":4526,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-293/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"San Bernardino 30' x 60' quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.0,\n 34\n ],\n [\n -118,\n 34\n ],\n [\n -118,\n 34.5\n ],\n [\n -117.0,\n 34.5\n ],\n [\n -117.0,\n 34\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47e3e4b07f02db4bb30c","contributors":{"authors":[{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":243830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Fred K.","contributorId":89503,"corporation":false,"usgs":true,"family":"Miller","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":243831,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51522,"text":"ofr03314 - 2003 - Preliminary analyses for perchlorate in selected natural materials and their derivative products","interactions":[],"lastModifiedDate":"2023-06-22T16:52:26.05805","indexId":"ofr03314","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-314","title":"Preliminary analyses for perchlorate in selected natural materials and their derivative products","docAbstract":"Increasing concern about sources of perchlorate contamination in ground and surface waters has led to interest in identifying potential sources of natural perchlorate and products derived from these natural sources. To date, most perchlorate found in ground and surface waters has been attributed to its major uses as an oxidizer in solid propellants for rockets, in fireworks and other explosives, and a variety of other uses of man-made perchlorate salts. However, perchlorate found in the soils, surface water, and ground water of some locations cannot be linked to an anthropogenic source. This paper contains preliminary data on the detection and non-detection of perchlorate in a variety of natural materials and their products, including some fertilizer materials. These data were previously presented at two conferences; once in poster session and once orally (Harvey and others, 1999; Orris and others, 2000). Although the results presented here are included in a journal article awaiting publication, the lack of public information on this topic has led to repeated requests for the data used as the basis for our presentations in 1999 and 2000.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03314","usgsCitation":"Orris, G., Harvey, G.J., Tsui, D.T., and Eldrige, J.E., 2003, Preliminary analyses for perchlorate in selected natural materials and their derivative products: U.S. Geological Survey Open-File Report 2003-314, Readme; Report: PDF, 6 p.; Report: TXT, https://doi.org/10.3133/ofr03314.","productDescription":"Readme; Report: PDF, 6 p.; Report: TXT","numberOfPages":"6","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":179111,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03314.jpg"},{"id":285768,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0314/OF03-314.txt"},{"id":285767,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0314/pdf/OF03-314.pdf"},{"id":285766,"rank":4,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2003/0314/readme.txt"},{"id":4525,"rank":5,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0314/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a213","contributors":{"authors":[{"text":"Orris, G. J.","contributorId":80252,"corporation":false,"usgs":true,"family":"Orris","given":"G. J.","affiliations":[],"preferred":false,"id":243829,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harvey, G. J.","contributorId":72984,"corporation":false,"usgs":true,"family":"Harvey","given":"G.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":243828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tsui, D. T.","contributorId":7996,"corporation":false,"usgs":true,"family":"Tsui","given":"D.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":243826,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Eldrige, J. E.","contributorId":46007,"corporation":false,"usgs":true,"family":"Eldrige","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":243827,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":51520,"text":"ofr03302 - 2003 - Geologic map and digital database of the Redlands 7.5' quadrangle, San Bernardino and Riverside Counties, California","interactions":[],"lastModifiedDate":"2023-06-22T16:57:23.554746","indexId":"ofr03302","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-302","title":"Geologic map and digital database of the Redlands 7.5' quadrangle, San Bernardino and Riverside Counties, California","docAbstract":"This geologic database of the Redlands 7.5' quadrangle was prepared by the Southern California Areal Mapping Project (SCAMP), a regional geologic-mapping project sponsored jointly by the U.S. Geological Survey and the California Geological Survey. The database was developed as a contribution to the National Cooperative Geologic Mapping Program's National Geologic Map Database, and is intended to provide a general geologic setting of the Redlands quadrangle. The database and map provide information about earth materials and geologic structures, including faults and folds that have developed in the quadrangle due to complexities in the San Andreas Fault system.
\nThe Redlands 7.5' quadrangle contains earth materials and structures that provide insight into the late Cenozoic geologic evolution of the southern California Inland Empire region. Important stratigraphic and structural elements include (1) the modern trace of the San Andreas and San Jacinto faults and (2) late Tertiary and Quaternary sedimentary materials and geologic structures that formed during the last million years or so and that record complex geologic interactions within the San Andreas Fault system. These materials and the structures that deform them provide the geologic framework for investigations of earthquake hazards and ground-water recharge and subsurface flow. Geologic information contained in the Redlands database is general-purpose data that is applicable to land-related investigations in the earth and biological sciences. The term \"general-purpose\" means that all geologic-feature classes have minimal information content adequate to characterize their general geologic characteristics and to interpret their general geologic history. However, no single feature class has enough information to definitively characterize its properties and origin. For this reason the database cannot be used for site-specific geologic evaluations, although it can be used to plan and guide investigations at the site-specific level.
\nThis summary pamphlet discusses major categories of surficial materials in the Redlands quadrangle, and provides a conceptual framework and basis for how geologicmap units containing such materials are recognized and correlated.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03302","collaboration":"Prepared in cooperation with San Bernardino Vally Municipal Water District and California Geological Survey","usgsCitation":"Matti, J.C., Morton, D.M., Cox, B.F., Kendrick, K.J., Cossette, P.M., Jones, B., and Kennedy, S.A., 2003, Geologic map and digital database of the Redlands 7.5' quadrangle, San Bernardino and Riverside Counties, California (Version 1.0): U.S. Geological Survey Open-File Report 2003-302, Pamphlet: 14 p.; 1 Plate: 44.35 x 31.14 inches; Readme: Metadata; Database, https://doi.org/10.3133/ofr03302.","productDescription":"Pamphlet: 14 p.; 1 Plate: 44.35 x 31.14 inches; Readme: Metadata; Database","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":179213,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03302.gif"},{"id":110445,"rank":11,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2003/0302/pdf/red_readme.pdf","linkFileType":{"id":5,"text":"html"},"description":"58938"},{"id":4524,"rank":10,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0302/","linkFileType":{"id":5,"text":"html"}},{"id":398349,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_58938.htm"},{"id":285762,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0302/pdf/red_map.pdf"},{"id":285759,"rank":7,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2003/0302/red_met.html"},{"id":285763,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0302/pdf/red_pamphlet.pdf"},{"id":285760,"rank":5,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/2003/0302/red.tar.gz"},{"id":285761,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0302/pdf/red_attribute_codes.pdf"},{"id":285764,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0302/red_map.ps.gz"},{"id":285765,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0302/pdf/red_dmu.pdf"}],"scale":"24000","projection":"Polyconic projection","country":"United States","state":"California","county":"Riverside County, San Bernardino County","otherGeospatial":"Redlands quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.25,34.0 ], [ -117.25,34.125 ], [ -117.125,34.125 ], [ -117.125,34.0 ], [ -117.25,34.0 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49be","contributors":{"authors":[{"text":"Matti, Jonathan C. jmatti@usgs.gov","contributorId":3666,"corporation":false,"usgs":true,"family":"Matti","given":"Jonathan","email":"jmatti@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":243819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Douglas M. scamp@usgs.gov","contributorId":4102,"corporation":false,"usgs":true,"family":"Morton","given":"Douglas","email":"scamp@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":243820,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cox, Brett F. bcox@usgs.gov","contributorId":5793,"corporation":false,"usgs":true,"family":"Cox","given":"Brett","email":"bcox@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":243821,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kendrick, Katherine J. 0000-0002-9839-6861 kendrick@usgs.gov","orcid":"https://orcid.org/0000-0002-9839-6861","contributorId":2716,"corporation":false,"usgs":true,"family":"Kendrick","given":"Katherine","email":"kendrick@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":243818,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cossette, Pamela M. 0000-0002-9608-6595 pcossette@usgs.gov","orcid":"https://orcid.org/0000-0002-9608-6595","contributorId":1458,"corporation":false,"usgs":true,"family":"Cossette","given":"Pamela","email":"pcossette@usgs.gov","middleInitial":"M.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":243822,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jones, Bradley","contributorId":140585,"corporation":false,"usgs":true,"family":"Jones","given":"Bradley","email":"","affiliations":[],"preferred":false,"id":243823,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kennedy, Stephen A.","contributorId":140207,"corporation":false,"usgs":true,"family":"Kennedy","given":"Stephen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":243824,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":51518,"text":"ofr03294 - 2003 - Hydrogeologic factors that influence ground water movement in the desert southwest United States","interactions":[],"lastModifiedDate":"2023-06-22T16:55:26.267394","indexId":"ofr03294","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-294","title":"Hydrogeologic factors that influence ground water movement in the desert southwest United States","docAbstract":"A project to study ground-water and surface-water interactions in the desert southwestern United States was initiated in 2001 by the Tucson, Arizona office of the Water Resources Division, U.S. Geological Survey (USGS). One of the goals of the Southwest Ground-water Resources Project was to develop a regional synthesis that includes the use of available digital geologic data, which is growing rapidly due to the increasing use of Geographic Information Systems (GIS). Included in this report are the digital maps and databases of geologic information that should have a direct impact on the studies of ground-water flow and surface-water interaction.
\nGround-water flow is governed by many geologic factors or elements including rock and soil permeability, stratigraphy and structural features. These elements directly influence ground-water flow, which is key to understanding the possible inter-connectivity of aquifer systems in desert basins of the southwestern United States. We derive these elements from the evaluation of regional geology and localized studies of hydrogeologic basins. These elements can then be applied to other unstudied areas throughout the desert southwest. This report presents a regional perspective of the geologic elements controlling ground-water systems in the desert southwest that may eventually lead to greater focus on smaller sub-regions and ultimately, to individual ground-water basins.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03294","usgsCitation":"Chuang, F.C., McKee, E.H., and Howard, K.A., 2003, Hydrogeologic factors that influence ground water movement in the desert southwest United States (Version 1.0): U.S. Geological Survey Open-File Report 2003-294, 37 p., https://doi.org/10.3133/ofr03294.","productDescription":"37 p.","numberOfPages":"38","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":285740,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0294/table1.xls"},{"id":285739,"rank":5,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/2003/0294/of03-294db.zip"},{"id":285737,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0294/pdf/of03-294pdf.zip"},{"id":285738,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2003/0294/eps/of03-294ps.zip"},{"id":285736,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0294/pdf/of03-294.pdf"},{"id":4522,"rank":7,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0294/","linkFileType":{"id":5,"text":"html"}},{"id":178670,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03294.jpg"}],"scale":"2000000","country":"United States","state":"Arizona, California, Colorado, Idaho, Nevada, New Mexico, Oregon, Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.0,30.0 ], [ -123.0,42.0 ], [ -107.0,42.0 ], [ -107.0,30.0 ], [ -123.0,30.0 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6287b6","contributors":{"authors":[{"text":"Chuang, Frank C.","contributorId":35600,"corporation":false,"usgs":true,"family":"Chuang","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":243807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":243806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":243805,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":51514,"text":"ofr03343 - 2003 - Tectonic Summaries for Web-served Earthquake Responses, Southeastern North America","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr03343","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-343","title":"Tectonic Summaries for Web-served Earthquake Responses, Southeastern North America","docAbstract":"This report documents the rationale and strategy used to write short summaries of the seismicity and tectonic settings of domains in southeastern North America. The summaries are used in automated responses to notable earthquakes that occur anywhere east of the Rocky Mountains in the United States or Canada. Specifically, the report describes the geologic and tectonic information, data sources, criteria, and reasoning used to determine the content and format of the summaries, for the benefit of geologists or seismologists who may someday need to revise the summaries or write others. These tectonic summaries are designed to be automatically posted on the World Wide Web as soon as an earthquake?s epicenter is determined. The summaries are part of a larger collection of summaries that is planned to cover the world.","language":"ENGLISH","doi":"10.3133/ofr03343","usgsCitation":"Wheeler, R.L., 2003, Tectonic Summaries for Web-served Earthquake Responses, Southeastern North America (Version 1.0): U.S. Geological Survey Open-File Report 2003-343, 28 p., https://doi.org/10.3133/ofr03343.","productDescription":"28 p.","costCenters":[],"links":[{"id":178558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-343/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685982","contributors":{"authors":[{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":243783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51257,"text":"wri034175 - 2003 - Ground-Water Levels and Water-Quality Data for Wells in the Crumpton Creek Area near Arnold Air Force Base, Tennessee, November 2001 to January 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:31","indexId":"wri034175","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4175","title":"Ground-Water Levels and Water-Quality Data for Wells in the Crumpton Creek Area near Arnold Air Force Base, Tennessee, November 2001 to January 2002","docAbstract":"From November 2001 to January 2002, a study of the ground-water resources in the Crumpton Creek area of Middle Tennessee was conducted to determine whether volatile organic compounds (VOCs) from Arnold Air Force Base (AAFB) have affected local private water supplies and to advance understanding of the ground-water-flow system in this area. VOC samples were collected from private wells that were not included in previous sampling efforts conducted in the Crumpton Creek area near AAFB. Ground-water-flow directions were investigated by measuring water levels in wells and constructing a potentiometric-surface map of the Manchester aquifer in the study area. Data were collected from a total of 68 private wells, 82 monitoring wells, and 1 cave during the period of study. Ground-water levels were determined for 42 of the private wells and for all 82 monitoring wells. Of the 82 monitoring wells, 81 withdraw water from the Manchester aquifer and 1 well withdraws water from the overlying shallow aquifer. The Manchester aquifer wells range in depth from 20 to 150 feet. Water-level altitudes for the Manchester aquifer ranged from 956 to 1,064 feet above the National Geodetic Vertical Datum of 1929. Water levels ranged from approximately 6 feet above land surface to 94 feet below land surface. Water-quality samples were collected from all 68 private wells, 8 of the monitoring wells, and the 1 cave. \r\n\r\nOf the 55 VOCs analyzed, 42 were not detected. Thirteen VOCs were detected; however, only tetrachloroethylene (PCE), methylene chloride, and toluene were detected at concentrations equal to or above reporting levels for the analytical method used. PCE was detected in water samples from 15 private wells and was the only VOC that exceeded drinking water maximum contaminant levels for public water systems. PCE concentrations in samples from five of the wells were below the reporting level and ranged from estimated concentrations of 0.46 to 0.80 microgram per liter (?g/L). Samples from 10 wells contained concentrations equal to or greater than the analytical reporting level of 1 ?g/L for PCE. Samples from one of these wells contained PCE concentrations (12 ?g/L and 11 ?g/L) exceeding the drinking water maximum contaminant level of 5 ?g/L for PCE. The spatial distribution of PCE detections and the relative concentrations of PCE and trichloroethylene suggest that the PCE detections are associated with a small and localized ground-water contamination plume unrelated to AAFB ground-water contamination.","language":"ENGLISH","doi":"10.3133/wri034175","usgsCitation":"Williams, S.D., 2003, Ground-Water Levels and Water-Quality Data for Wells in the Crumpton Creek Area near Arnold Air Force Base, Tennessee, November 2001 to January 2002: U.S. Geological Survey Water-Resources Investigations Report 2003-4175, 28 p., https://doi.org/10.3133/wri034175.","productDescription":"28 p.","costCenters":[],"links":[{"id":4631,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034175/","linkFileType":{"id":5,"text":"html"}},{"id":178487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d17c","contributors":{"authors":[{"text":"Williams, Shannon D. swilliam@usgs.gov","contributorId":4133,"corporation":false,"usgs":true,"family":"Williams","given":"Shannon","email":"swilliam@usgs.gov","middleInitial":"D.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":243235,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":50707,"text":"ofr02421 - 2003 - Archive of boomer seismic reflection data: Collected during USGS Cruise 97KEY01, upper and middle Florida Keys, 12 October - 1 November, 1997","interactions":[],"lastModifiedDate":"2022-07-13T20:46:16.678995","indexId":"ofr02421","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-421","title":"Archive of boomer seismic reflection data: Collected during USGS Cruise 97KEY01, upper and middle Florida Keys, 12 October - 1 November, 1997","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02421","usgsCitation":"Peery, G.M., Lidz, B.H., and Wiese, D.S., 2003, Archive of boomer seismic reflection data: Collected during USGS Cruise 97KEY01, upper and middle Florida Keys, 12 October - 1 November, 1997: U.S. Geological Survey Open-File Report 2002-421, HTML Document: 1 CD-ROM; 1 DVD-ROM, https://doi.org/10.3133/ofr02421.","productDescription":"HTML Document: 1 CD-ROM; 1 DVD-ROM","costCenters":[],"links":[{"id":176514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403690,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_55001.htm","linkFileType":{"id":5,"text":"html"}},{"id":4202,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-421/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"Florida Keys","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.3917,\n 24.4\n ],\n [\n -80.2667,\n 24.4\n ],\n [\n -80.2667,\n 25.1667\n ],\n [\n -81.3917,\n 25.1667\n ],\n [\n -81.3917,\n 24.4\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679dcd","contributors":{"authors":[{"text":"Peery, Gina M.","contributorId":36621,"corporation":false,"usgs":true,"family":"Peery","given":"Gina","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":242123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lidz, Barbara H. blidz@usgs.gov","contributorId":2475,"corporation":false,"usgs":true,"family":"Lidz","given":"Barbara","email":"blidz@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":242121,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":242122,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53094,"text":"ofr2003408 - 2003 - Maps Showing Inundation Depths, Ice-Rafted Erratics, and Sedimentary Facies of Late Pleistocene Missoula Floods in the Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2015-01-26T08:43:05","indexId":"ofr2003408","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-408","title":"Maps Showing Inundation Depths, Ice-Rafted Erratics, and Sedimentary Facies of Late Pleistocene Missoula Floods in the Willamette Valley, Oregon","docAbstract":"Glacial Lake Missoula, impounded by the Purcell Trench lobe of the late Pleistocene Cordilleran Icesheet, repeatedly breached its ice dam, sending floods as large as 2,500 cubic kilometers racing across the Channeled Scabland and down the Columbia River valley to the Pacific Ocean. Peak discharges for some floods exceeded 20 million cubic meters per second. At valley constrictions along the flood route, floodwaters temporarily ponded behind each narrow zone. One such constriction at Kalama Gap-northwest of Portland-backed water 120-150 meters high in the Portland basin, and backflooded 200 km south into Willamette Valley. Dozens of floods backed up into the Willamette Valley, eroding 'scabland' channels, and depositing giant boulder gravel bars in areas of vigorous currents as well as bedded flood sand and silt in backwater areas. Also, large chunks of ice entrained from the breached glacier dam rafted hundreds of 'erratic' rocks, leaving them scattered among the flanking foothills and valley bottom. From several sources and our own mapping, we have compiled information on many of these features and depict them on physiographic maps derived from digital elevation models of the Portland Basin and Willamette Valley. These maps show maximum flood inundation levels, inundation levels associated with stratigraphic evidence of repeated floodings, distribution of flood deposits, and sites of ice-rafted erratics. Accompanying these maps, a database lists locations, elevations, and descriptions of approximately 400 ice-rafted erratics-most compiled from early 20th-century maps and notes of A.M. Piper and I.S. Allison.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2003408","usgsCitation":"Minervini, J., O’Connor, J.E., and Wells, R., 2003, Maps Showing Inundation Depths, Ice-Rafted Erratics, and Sedimentary Facies of Late Pleistocene Missoula Floods in the Willamette Valley, Oregon: U.S. Geological Survey Open-File Report 2003-408, Map: 55 x 34 inches; ReadMe; Data Files, https://doi.org/10.3133/ofr2003408.","productDescription":"Map: 55 x 34 inches; ReadMe; Data Files","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":180889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2003408.jpg"},{"id":297499,"rank":701,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/of03-408/of03-408.pdf","text":"Maps","size":"31.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Maps"},{"id":297501,"rank":703,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2003/of03-408/OF03_408_GDB.zip","text":"Geodatabase","size":"306 MB","description":"Geodatabase"},{"id":297502,"rank":704,"type":{"id":16,"text":"Metadata"},"url":"https://pubs.usgs.gov/of/2003/of03-408/erraticsmetadata.txt","size":"32 kB","linkFileType":{"id":2,"text":"txt"}},{"id":297503,"rank":705,"type":{"id":23,"text":"Spatial Data"},"url":"https://pubs.usgs.gov/of/2003/of03-408/OF03_408_SHP.zip","text":"Shapefile package","size":"306 MB","description":"Shapefile package"},{"id":110451,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_59381.htm","linkFileType":{"id":5,"text":"html"},"description":"59381"},{"id":9743,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-408/","linkFileType":{"id":5,"text":"html"}},{"id":297500,"rank":702,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/2003/of03-408/OF03408README.pdf","size":"272 kB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.5,44 ], [ -123.5,45.75 ], [ -122.36694444444444,45.75 ], [ -122.36694444444444,44 ], [ -123.5,44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aab7","contributors":{"authors":[{"text":"Minervini, J.M.","contributorId":86041,"corporation":false,"usgs":true,"family":"Minervini","given":"J.M.","affiliations":[],"preferred":false,"id":246627,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connor, J. E.","contributorId":59489,"corporation":false,"usgs":true,"family":"O’Connor","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":246625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wells, R.E. 0000-0002-7796-0160","orcid":"https://orcid.org/0000-0002-7796-0160","contributorId":67537,"corporation":false,"usgs":true,"family":"Wells","given":"R.E.","affiliations":[],"preferred":false,"id":246626,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":53088,"text":"ofr03363 - 2003 - Publications of the Western Earth Surface Processes Team 2002","interactions":[],"lastModifiedDate":"2023-06-22T16:58:33.054297","indexId":"ofr03363","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-363","title":"Publications of the Western Earth Surface Processes Team 2002","docAbstract":"The Western Earth Surface Processes Team (WESPT) of the U.S. Geological Survey (USGS) conducts geologic mapping and related topical earth science studies in the western United States. This work is focused on areas where modern geologic maps and associated earth-science data are needed to address key societal and environmental issues such as ground-water quality, landslides and other potential geologic hazards, and land-use decisions. Areas of primary emphasis in 2001 included southern California, the San Francisco Bay region, the Pacific Northwest, and the Las Vegas urban corridor. The team has its headquarters in Menlo Park, California, and maintains smaller field offices at several other locations in the western United States. The results of research conducted by the WESPT are released to the public as a variety of databases, maps, text reports, and abstracts, both through the internal publication system of the USGS and in diverse external publications such as scientific journals and books. This report lists publications of the WESPT released in 2002 as well as additional 1998 and 2001 publications that were not included in the previous list (USGS Open-File Report 00-215, USGS Open-File Report 01-198, and USGS Open-File Report 02-269). Most of the publications listed were authored or coauthored by WESPT staff. The list also includes some publications authored by non-USGS cooperators with the WESPT, as well as some authored by USGS staff outside the WESPT in cooperation with WESPT projects. Several of the publications listed are available on the World Wide Web; for these, URL addresses are provided. Many of these web publications are USGS open-file reports that contain large digital databases of geologic map and related information. Information on ordering USGS publications can be found on the World Wide Web or by calling 1-888-ASK-USGS. The U.S. Geological Survey’s web server for geologic information in the western United States is located at http://geology.wr.usgs.gov. More information is available about the WESPT is available on-line at the team website.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03363","usgsCitation":"Powell, C., and Graymer, R., 2003, Publications of the Western Earth Surface Processes Team 2002: U.S. Geological Survey Open-File Report 2003-363, 22 p., https://doi.org/10.3133/ofr03363.","productDescription":"22 p.","numberOfPages":"23","temporalStart":"2002-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":180791,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03363.jpg"},{"id":5285,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0363/","linkFileType":{"id":5,"text":"html"}},{"id":285787,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0363/pdf/of03-363.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db655e50","contributors":{"authors":[{"text":"Powell, Charles II","contributorId":96362,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","affiliations":[],"preferred":false,"id":246604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Graymer, R. W.","contributorId":21174,"corporation":false,"usgs":true,"family":"Graymer","given":"R. W.","affiliations":[],"preferred":false,"id":246603,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53087,"text":"ofr03360 - 2003 - Shaded relief aeromagnetic map of the Santa Clara Valley and vicinity, California","interactions":[],"lastModifiedDate":"2023-06-22T16:53:43.931696","indexId":"ofr03360","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-360","title":"Shaded relief aeromagnetic map of the Santa Clara Valley and vicinity, California","docAbstract":"This aeromagnetic map covers the southern portion of San Francisco Bay, the Santa Clara Valley and surrounding mountains, part of which has been modelled in threedimensions (Jachens and other, 2001). The magnetic anomaly map has been compiled from existing digital data. Data was obtained from six aeromagnetic surveys that were flown at different times, spacings and elevations. The International Geomagnetic Reference Field (IGRF) for the date of each survey had been removed in the initial processing. The resulting residual magnetic anomalies were analytically continued onto a common surface 305 m (1000 ft) above terrain. Portions of each survey were substantially above the specified flight height listed in the table. The surveys were then merged together using a commercial software package called Oasis Montage. The gray lines on the map indicate the extent of each survey. The program used these regions of overlap to determine the best fit between surveys. Black dots show probable edges of magnetic bodies defined by the maximum horizontal gradient determined using a computer program by Blakely (1995).\n\nCrystalline rocks generally contain sufficient magnetic minerals to cause variations in the Earth’s magnetic field that can be mapped by aeromagnetic surveys. Sedimentary rocks are generally weakly magnetized and consequently have a small effect on the magnetic field: thus a magnetic anomaly map can be used to “see through” the sedimentary rock cover and can convey information on lithologic contrasts and structural trends related to the underlying crystalline basement (see Nettleton,1971; Blakely, 1995). Faults often cut magnetic bodies and offset magnetic anomalies can thus be used to help determine fault motion. Serpentinite, which is highly magnetic, is often found along faults. On this map areas of low magnetic anomalies are shown in blues and green while highs are shown in reds and magentas. Faults are from Brabb and others, 1998a,1998b, Graymer and others 1996, Lienkaemper, 1992 and Wentworth and others 1998.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03360","usgsCitation":"Roberts, C.W., and Jachens, R.C., 2003, Shaded relief aeromagnetic map of the Santa Clara Valley and vicinity, California: U.S. Geological Survey Open-File Report 2003-360, 1 Plate: 36.00 inches x 48.00 inches, https://doi.org/10.3133/ofr03360.","productDescription":"1 Plate: 36.00 inches x 48.00 inches","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":180790,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03360.jpg"},{"id":285817,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0360/pdf/of03-360.pdf"},{"id":285782,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0360/"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.25,37.0000 ], [ -122.25,37.6333 ], [ -121.50,37.6333 ], [ -121.50,37.0000 ], [ -122.25,37.0000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4a24","contributors":{"authors":[{"text":"Roberts, Carter W.","contributorId":45282,"corporation":false,"usgs":true,"family":"Roberts","given":"Carter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":246602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jachens, Robert C. jachens@usgs.gov","contributorId":1180,"corporation":false,"usgs":true,"family":"Jachens","given":"Robert","email":"jachens@usgs.gov","middleInitial":"C.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":246601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53086,"text":"ofr03353 - 2003 - Geochemistry of bedrock and glacial deposits in the vicinity of the Bend massive sulfide deposit, north central Wisconsin","interactions":[],"lastModifiedDate":"2018-11-26T09:30:06","indexId":"ofr03353","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-353","title":"Geochemistry of bedrock and glacial deposits in the vicinity of the Bend massive sulfide deposit, north central Wisconsin","docAbstract":"In 1998 the U.S. Geological Survey (USGS) initiated a study to examine the natural regional environmental impact of sulfide mineralization exposed to episodic weathering and glaciation. The study focused on the Bend copper-gold massive sulfide deposit located in the Medford District of the Chequamegon National Forest in north central Wisconsin. The Bend massive sulfide deposit is a small, metal-rich sulfide body hosted by Paleoproterozoic metavolcanics. The mineralized horizon subcrops beneath 100-120 feet of glacial cover, and consists of massive pyrite and other sulfides. Bedrock and ore geochemistry are well characterized by analyses of diamond drill core provided to the USGS by Sharpe Energy and Resources.
\nIn July 1999, five rotasonic drillholes were completed through the unconsolidated Quaternary sediment, averaging about 100 feet thick, on a transect across the Bend deposit. Nearly continuous core was recovered from the surficial material along with several feet of the underlying bedrock. Samples representing the entire section were analyzed by the USGS to give a two-dimensional representation of element dispersal from the unmineralized bedrock. In addition, one hundred regional till samples were subsampled from the archives of the Quaternary Sediment Laboratory in the University of Wisconsin-Madison Department of Geology and Geophysics. These regional samples were collected mainly from Taylor County, where the Bend deposit is located, as well as contiguous parts of Clark and Marathon Counties.
\nThis open file report presents all of the geochemical data collected for this study. Additional publications describing the data in more detail are being completed.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03353","usgsCitation":"Woodruff, L.G., Attig, J.W., Cannon, W.F., Nicholson, S.W., and Schulz, K., 2003, Geochemistry of bedrock and glacial deposits in the vicinity of the Bend massive sulfide deposit, north central Wisconsin (Version 1.0, Online Only): U.S. Geological Survey Open-File Report 2003-353, HTML Document, https://doi.org/10.3133/ofr03353.","productDescription":"HTML Document","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":180789,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5284,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-353/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.0986328125,\n 45.359865333959746\n ],\n [\n -91.0986328125,\n 45.81348649679971\n ],\n [\n -90.32958984375,\n 45.81348649679971\n ],\n [\n -90.32958984375,\n 45.359865333959746\n ],\n [\n -91.0986328125,\n 45.359865333959746\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0, Online Only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab5bd","contributors":{"authors":[{"text":"Woodruff, Laurel G. 0000-0002-2514-9923 woodruff@usgs.gov","orcid":"https://orcid.org/0000-0002-2514-9923","contributorId":2224,"corporation":false,"usgs":true,"family":"Woodruff","given":"Laurel","email":"woodruff@usgs.gov","middleInitial":"G.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Attig, John W.","contributorId":16832,"corporation":false,"usgs":true,"family":"Attig","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":246599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannon, William F. 0000-0002-2699-8118 wcannon@usgs.gov","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":1883,"corporation":false,"usgs":true,"family":"Cannon","given":"William","email":"wcannon@usgs.gov","middleInitial":"F.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246597,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nicholson, Suzanne W. 0000-0002-9365-1894 swnich@usgs.gov","orcid":"https://orcid.org/0000-0002-9365-1894","contributorId":880,"corporation":false,"usgs":true,"family":"Nicholson","given":"Suzanne","email":"swnich@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":246596,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schulz, Klaus","contributorId":41519,"corporation":false,"usgs":true,"family":"Schulz","given":"Klaus","affiliations":[],"preferred":false,"id":246600,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53085,"text":"ofr03349 - 2003 - Interpreting DNAPL saturations in a laboratory-scale injection with GPR data and direct core measurements","interactions":[],"lastModifiedDate":"2012-02-02T00:11:56","indexId":"ofr03349","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-349","title":"Interpreting DNAPL saturations in a laboratory-scale injection with GPR data and direct core measurements","docAbstract":"Ground penetrating radar (GPR) is used to track a dense non-aqueous phase liquid (DNAPL) injection in a laboratory sand tank. Before data reduction, GPR data provide a qualitative measure of DNAPL saturation and movement. One-dimensional (1D) GPR modeling provides a quantitative interpretation of DNAPL volume within a given thickness during and after the injection. This is confirmed qualitatively by visual inspection of cores and two-dimensional GPR modeling. DNAPL saturation in sub-layers of that thickness could not be quantified because calibration of the 1D GPR model is non-unique when both permittivity and depth of multiple layers are unknown. Accurate quantitative interpretation of DNAPL volumes using 1D GPR modeling requires: 1) identification of a suitable target that produces a strong reflection and is not subject to any multidimensional interference; 2) knowledge of the exact depth of that target; and 3) use of two-way radar-wave travel times through the medium to the target to determine the permittivity of the intervening material, which eliminates reliance upon reflection amplitude. With geologic conditions that are suitable for GPR surveys (i.e., shallow depths and low electrical conductivities), the procedures in this laboratory study can be adapted to a field site to identify DNAPL source zones after a release has occurred.","language":"ENGLISH","doi":"10.3133/ofr03349","usgsCitation":"Johnson, R.H., and Poeter, E.P., 2003, Interpreting DNAPL saturations in a laboratory-scale injection with GPR data and direct core measurements (Version 1.0): U.S. Geological Survey Open-File Report 2003-349, 39 p., https://doi.org/10.3133/ofr03349.","productDescription":"39 p.","costCenters":[],"links":[{"id":182030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5283,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-349/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e02ee","contributors":{"authors":[{"text":"Johnson, Raymond H. rhjohnso@usgs.gov","contributorId":707,"corporation":false,"usgs":true,"family":"Johnson","given":"Raymond","email":"rhjohnso@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":246594,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poeter, Eileen P.","contributorId":78805,"corporation":false,"usgs":true,"family":"Poeter","given":"Eileen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":246595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53081,"text":"ofr03330 - 2003 - North Alaska petroleum system analysis: The regional map compilation","interactions":[],"lastModifiedDate":"2022-01-07T21:13:49.976535","indexId":"ofr03330","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-330","title":"North Alaska petroleum system analysis: The regional map compilation","docAbstract":"The U.S. Geological Survey initiated an effort to model north Alaskan petroleum systems. The geographic and geologic basis for modeling systems is provided by a set of regional digital maps that allow evaluation of the widest possible extent of each system. Accordingly, we laid out a rectangular map grid 1300 km (800 miles) east-west and 600 km (375 miles) north-south. The resulting map area extends from the Yukon Territory of Canada on the east to the Russian-U.S. Chukchi Sea on the west and from the Brooks Range on the south to the Canada basin-Chukchi borderland on the north. Within this map region, we combined disparate types of publicly available data to produce structure contour maps. Data types range from seismic-based mapping as in the National Petroleum Reserve to well penetrations in areas of little or no seismic data where extrapolation was required. With these types of data, we produced structure contour maps on three horizons: top of pre-Mississippian (basement), top of Triassic (Ellesmerian sequence), and top of Neocomian (Beaufortian sequence). These horizons, when combined with present-day topography and bathymetry, provide the bounding structural/stratigraphic surfaces of the north Alaskan petroleum province that mark major defining moments of the region's geologic history and allow regional portrayal of preserved sediment accumulations.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03330","usgsCitation":"Saltus, R.W., and Bird, K.J., 2003, North Alaska petroleum system analysis: The regional map compilation: U.S. Geological Survey Open-File Report 2003-330, 1 Plate: 93.75 x 37.50 inches, https://doi.org/10.3133/ofr03330.","productDescription":"1 Plate: 93.75 x 37.50 inches","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":182126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03330.jpg"},{"id":5257,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0330/","linkFileType":{"id":5,"text":"html"}},{"id":110447,"rank":700,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0330/pdf/of03-330.pdf","linkFileType":{"id":1,"text":"pdf"},"description":"59087"},{"id":394064,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_59087.htm"}],"country":"Canada, United States","state":"Alaska, Yukon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -172,\n 68\n ],\n [\n -135,\n 68\n ],\n [\n -135,\n 73\n ],\n [\n -172,\n 73\n ],\n [\n -172,\n 68\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696dce","contributors":{"authors":[{"text":"Saltus, Richard W. saltus@usgs.gov","contributorId":777,"corporation":false,"usgs":true,"family":"Saltus","given":"Richard","email":"saltus@usgs.gov","middleInitial":"W.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":246582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":246583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53080,"text":"ofr2003329 - 2003 - Sandstone and shale compaction curves derived from sonic and gamma ray logs in offshore wells, North Slope, Alaska– Parameters for basin modeling","interactions":[],"lastModifiedDate":"2021-12-14T19:25:39.950653","indexId":"ofr2003329","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-329","title":"Sandstone and shale compaction curves derived from sonic and gamma ray logs in offshore wells, North Slope, Alaska– Parameters for basin modeling","docAbstract":"Representative compaction curves for the principle lithologies are essential input for reliable models of basin history. Compaction curves influence estimates of maximum burial and erosion. Different compaction curves may produce significantly different thermal histories. Default compaction curves provided by basin modeling packages may or may not be a good proxy for the compaction properties in a given area. Compaction curves in the published literature span a wide range, even within one lithology, e.g., sandstone (see Panel 3). An abundance of geophysical well data for the North Slope, from both government and private sources, provides us with an unusually good opportunity to develop compaction curves for the Cretaceous-Tertiary Brookian sandstones, siltstones, and shales. We examined the sonic and gamma ray logs from 19 offshore wells (see map), where significant erosion is least likely to have occurred. Our data are primarily from the Cretaceous-Tertiary Brookian sequence and are less complete for older sequences. \r\n\r\nFor each well, the fraction of shale (Vsh) at a given depth was estimated from the gamma ray log, and porosity was computed from sonic travel time. By compositing porosities for the near-pure sand (Vsh<1%) and shale (Vsh>99%)from many individual wells we obtained data over sufficient depth intervals to define sandstone and shale 'master' compaction curves. A siltstone curve was defined using the sonic-derived porosities for Vsh values of 50%. These compaction curves generally match most of the sonic porosities with an error of 5% or less. \r\n\r\nOnshore, the curves are used to estimate the depth of maximum burial at the end of Brookian sedimentation. The depth of sonic-derived porosity profiles is adjusted to give the best match with the 'master' compaction curves. The amount of the depth adjustment is the erosion estimate. Using our compaction curves, erosion estimates on the North Slope range from zero in much of the offshore, to as much as 1500 ft along the coast, and to more than 10,000 ft in the foothills (Panel 3). Compaction curves provide an alternative to vitrinite reflectance for estimating erosion. Vitrinite reflectance data are often very sparse in contrast to well log data and are subject to inconsistencies when measurements are made by different labs. The phenomenon of 'recycling' can also make the reflectance values of dispersed vitrinite problematic for quantifying erosion. Recycling is suspected in dispersed vitrinite in North Slope rocks, particularly in the younger, Cretaceous-Tertiary section. The compaction curves defined here are being integrated into our burial history and thermal models to determine the timing of source rock maturation. An example on Panel 3 shows the results of calculating the maturity of the Shublik Fm. at the Tulaga well using two different sets of shale and siltstone compaction curves. Finally, accurate compaction curves improve a model's ability to realistically simulate the pressure regime during burial, including overpressures.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2003329","usgsCitation":"Rowan, E.L., Hayba, D.O., Nelson, P.H., Burns, W.M., and Houseknecht, D.W., 2003, Sandstone and shale compaction curves derived from sonic and gamma ray logs in offshore wells, North Slope, Alaska– Parameters for basin modeling: U.S. Geological Survey Open-File Report 2003-329, HTML Document, https://doi.org/10.3133/ofr2003329.","productDescription":"HTML Document","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":647,"text":"Western Earth Surface Processes","active":false,"usgs":true}],"links":[{"id":182041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8872,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-329/","linkFileType":{"id":5,"text":"html"}},{"id":392867,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_59088.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -167,\n 68.8333\n ],\n [\n -148,\n 68.8333\n ],\n [\n -148,\n 71.4167\n ],\n [\n -167,\n 71.4167\n ],\n [\n -167,\n 68.8333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdcd7","contributors":{"authors":[{"text":"Rowan, Elisabeth L. 0000-0001-5753-6189 erowan@usgs.gov","orcid":"https://orcid.org/0000-0001-5753-6189","contributorId":2075,"corporation":false,"usgs":true,"family":"Rowan","given":"Elisabeth","email":"erowan@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayba, Daniel O. 0000-0003-4092-1894 dhayba@usgs.gov","orcid":"https://orcid.org/0000-0003-4092-1894","contributorId":396,"corporation":false,"usgs":true,"family":"Hayba","given":"Daniel","email":"dhayba@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":246577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Philip H. pnelson@usgs.gov","contributorId":862,"corporation":false,"usgs":true,"family":"Nelson","given":"Philip","email":"pnelson@usgs.gov","middleInitial":"H.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246579,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burns, W. Matthew","contributorId":56742,"corporation":false,"usgs":true,"family":"Burns","given":"W.","email":"","middleInitial":"Matthew","affiliations":[],"preferred":false,"id":246581,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Houseknecht, David W. 0000-0002-9633-6910 dhouse@usgs.gov","orcid":"https://orcid.org/0000-0002-9633-6910","contributorId":645,"corporation":false,"usgs":true,"family":"Houseknecht","given":"David","email":"dhouse@usgs.gov","middleInitial":"W.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246578,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53079,"text":"ofr03328 - 2003 - Distribution, richness, quality, and thermal maturity of source rock units on the North Slope of Alaska","interactions":[],"lastModifiedDate":"2018-08-31T13:36:46","indexId":"ofr03328","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-328","title":"Distribution, richness, quality, and thermal maturity of source rock units on the North Slope of Alaska","docAbstract":"Four source rock units on the North Slope were identified, characterized, and mapped to better understand the origin of petroleum in the area: Hue-gamma ray zone (Hue-GRZ), pebble shale unit, Kingak Shale, and Shublik Formation. Rock-Eval pyrolysis, total organic carbon analysis, and well logs were used to map the present-day thickness, organic quantity (TOC), quality (hydrogen index, HI), and thermal maturity (Tmax) of each unit. To map these units, we screened all available geochemical data for wells in the study area and assumed that the top and bottom of the oil window occur at Tmax of ~440° and 470°C, respectively. Based on several assumptions related to carbon mass balance and regional distributions of TOC, the present-day source rock quantity and quality maps were used to determine the extent of fractional conversion of the kerogen to petroleum and to map the original organic richness prior to thermal maturation.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03328","usgsCitation":"Peters, K.E., Bird, K.J., Keller, M., Lillis, P., and Magoon, L.B., 2003, Distribution, richness, quality, and thermal maturity of source rock units on the North Slope of Alaska: U.S. Geological Survey Open-File Report 2003-328, 3 Sheets: 96.00 x 36.00 inches, https://doi.org/10.3133/ofr03328.","productDescription":"3 Sheets: 96.00 x 36.00 inches","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":182040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03328.jpg"},{"id":285784,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0328/pdf/sheet2.pdf"},{"id":5256,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0328/","linkFileType":{"id":5,"text":"html"}},{"id":285785,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0328/pdf/sheet3.pdf"},{"id":285783,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0328/pdf/sheet1.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -166.85,68.0 ], [ -166.85,71.39 ], [ -141.0,71.39 ], [ -141.0,68.0 ], [ -166.85,68.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d966","contributors":{"authors":[{"text":"Peters, K. E.","contributorId":17295,"corporation":false,"usgs":true,"family":"Peters","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":246572,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, K. J.","contributorId":57824,"corporation":false,"usgs":false,"family":"Bird","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":246576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keller, M.A.","contributorId":41008,"corporation":false,"usgs":true,"family":"Keller","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":246574,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lillis, P. G. 0000-0002-7508-1699","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":17630,"corporation":false,"usgs":true,"family":"Lillis","given":"P. G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":246573,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Magoon, L. B.","contributorId":44531,"corporation":false,"usgs":true,"family":"Magoon","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":246575,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53078,"text":"ofr03327 - 2003 - Association of deformation and fluid events in the central Brooks Range fold-and-thrust belt, Northern Alaska","interactions":[],"lastModifiedDate":"2018-08-31T13:37:06","indexId":"ofr03327","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-327","title":"Association of deformation and fluid events in the central Brooks Range fold-and-thrust belt, Northern Alaska","docAbstract":"Ocentral Brooks Range consists of two superposed north-directed contractional orogens, one formed between 140-120 Ma and the other at ~60-45 Ma. The older orogen was an arc-continent collisional zone characterized by far-traveled allochthons and relatively low structural relief. The younger orogen is a retroarc thrust belt with relatively low amounts of shortening and high structural relief. Folding and thrusting of the younger episode is superimposed on the thin-skinned deformational wedge of the earlier orogen and also produced a frontal triangle zone in a thick sequence of mid-Cretaceous foreland basin sediments to the north. Stable isotope compositions of calcite and quartz veins indicate two fluid events including: (1) an earlier, higher-temperature (~250-300° C) event that produced veins in deformed Devonian clastic rocks, and (2) a younger, lower-temperature (~150° C) event that deposited veins in deformed Mississippian through Albian strata. The fluids in the first event had variable d18O values, but nearly constant d13C values buffered by limestone lithologies. The vein-forming fluids in the second event had similarly variable d18O values, but with distinctly lower d13C values as a result of oxidation of organic matter and/or methane. Zircon fission track ages demonstrate cooling to temperatures below 200° C between 140-120 Ma for the Devonian rocks, whereas zircon and apatite fission track ages show that Mississippian to Albian rocks were never heated above 200° C and cooled below 110-90° C at ~60-45 Ma. These data are interpreted as indicating that the older, high-temperature fluid event was active during thrusting at 120-140 Ma, and the younger fluid event during deformation at ~60-45 Ma. The data and results presented in this poster will be published in early 2004 in Moore and others (in press).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03327","usgsCitation":"Moore, T.E., Potter, C.J., O'Sullivan, P., Shelton, K.L., and Underwood, M.B., 2003, Association of deformation and fluid events in the central Brooks Range fold-and-thrust belt, Northern Alaska: U.S. Geological Survey Open-File Report 2003-327, Sheet 1: 92.31 x 36.92 inches; Sheet 2: 92.31 x 36.92 inches, https://doi.org/10.3133/ofr03327.","productDescription":"Sheet 1: 92.31 x 36.92 inches; Sheet 2: 92.31 x 36.92 inches","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":182039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03327.jpg"},{"id":5255,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0327/","linkFileType":{"id":5,"text":"html"}},{"id":285780,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0327/pdf/sheet1.pdf"},{"id":285781,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0327/pdf/sheet2.pdf"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165.0,66.0 ], [ -165.0,71.0 ], [ -141.0,71.0 ], [ -141.0,66.0 ], [ -165.0,66.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce36","contributors":{"authors":[{"text":"Moore, Thomas E. 0000-0002-0878-0457 tmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":1033,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas","email":"tmoore@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":246568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, Christopher J. 0000-0002-2300-6670 cpotter@usgs.gov","orcid":"https://orcid.org/0000-0002-2300-6670","contributorId":1026,"corporation":false,"usgs":true,"family":"Potter","given":"Christopher","email":"cpotter@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":246567,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O'Sullivan, Paul B.","contributorId":36627,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Paul B.","affiliations":[],"preferred":false,"id":246570,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shelton, Kevin L.","contributorId":48632,"corporation":false,"usgs":true,"family":"Shelton","given":"Kevin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":246571,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Underwood, Michael B.","contributorId":6844,"corporation":false,"usgs":true,"family":"Underwood","given":"Michael","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":246569,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53077,"text":"ofr03325 - 2003 - Petroleum source potential of the Lower Cretaceous mudstone succession of the NPRA and Colville Delta area, North Slope Alaska, based on sonic and resistivity logs","interactions":[],"lastModifiedDate":"2018-08-31T13:37:25","indexId":"ofr03325","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-325","title":"Petroleum source potential of the Lower Cretaceous mudstone succession of the NPRA and Colville Delta area, North Slope Alaska, based on sonic and resistivity logs","docAbstract":"Resource assessment of the North Slope of Alaska by the U. S. Geological Survey includes evaluation of the petroleum source potential of Mesozoic and Cenozoic rocks using the delta log R technique (Passey and others, 1990). Porosity and resistivity logs are used in combination with thermal maturity data to produce a continuous profile of total organic carbon content in weight % (TOC). From the pattern and amount of TOC in the profile produced, the depositional setting and thus the petroleum source-rock potential (kerogen type) of the organic matter can be inferred and compared to interpretations from other data such as Rock-Eval pyrolysis. TOC profiles determined by this technique for the contiguous interval of pebble shale unit, Hue Shale (including the Gamma Ray Zone or GRZ), and lower part of the Torok Formation indicate important potential for petroleum generation in the Tunalik 1, Inigok 1, N. Inigok 1, Kuyanak 1, Texaco Colville Delta 1, Nechelik 1, and Bergschrund 1 wells of the western North Slope region. TOC profiles suggest that this interval contains both type II and III kerogens – consistent with proposed depositional models -- and is predominantly greater than 2 wt. % TOC (cut-off used for effective source potential). Average TOC for the total effective section of the pebble shale unit + Hue Shale ranges from 2.6 to 4.1 wt % TOC (values predominantly 2-8% TOC) over 192-352 ft. Source potential for the lower Torok Formation, which also has interbedded sandstone and lean mudstone, is good to negligible in these 7 wells.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03325","usgsCitation":"Keller, M.A., and Bird, K.J., 2003, Petroleum source potential of the Lower Cretaceous mudstone succession of the NPRA and Colville Delta area, North Slope Alaska, based on sonic and resistivity logs: U.S. Geological Survey Open-File Report 2003-325, Sheet 1: 96.00 x 48.00 inches; Sheet 2: 96.00 x 48.00 inches, https://doi.org/10.3133/ofr03325.","productDescription":"Sheet 1: 96.00 x 48.00 inches; Sheet 2: 96.00 x 48.00 inches","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":181942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03325.jpg"},{"id":5254,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0325/","linkFileType":{"id":5,"text":"html"}},{"id":285773,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0325/pdf/sheet1.pdf"},{"id":285774,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0325/pdf/sheet2.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"North Slope","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165.0,68.0 ], [ -165.0,72.0 ], [ -140.0,72.0 ], [ -140.0,68.0 ], [ -165.0,68.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687ce8","contributors":{"authors":[{"text":"Keller, Margaret A. mkeller@usgs.gov","contributorId":1017,"corporation":false,"usgs":true,"family":"Keller","given":"Margaret","email":"mkeller@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":246566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bird, Kenneth J. kbird@usgs.gov","contributorId":1015,"corporation":false,"usgs":true,"family":"Bird","given":"Kenneth","email":"kbird@usgs.gov","middleInitial":"J.","affiliations":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":246565,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":53074,"text":"ofr2003319 - 2003 - Aeromagnetic surveys in Yukon Flats Alaska, a website for the distribution of data","interactions":[],"lastModifiedDate":"2022-11-23T22:22:33.290523","indexId":"ofr2003319","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-319","title":"Aeromagnetic surveys in Yukon Flats Alaska, a website for the distribution of data","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2003319","usgsCitation":"Brown, P., 2003, Aeromagnetic surveys in Yukon Flats Alaska, a website for the distribution of data (Version 1.0): U.S. Geological Survey Open-File Report 2003-319, HTML Document, https://doi.org/10.3133/ofr2003319.","productDescription":"HTML Document","costCenters":[],"links":[{"id":181824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":409623,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_59092.htm","linkFileType":{"id":5,"text":"html"}},{"id":5252,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/ofr-03-319/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Yukon Flats","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -141,\n 67.5\n ],\n [\n -147,\n 67.5\n ],\n [\n -147,\n 66\n ],\n [\n -141,\n 66\n ],\n [\n -141,\n 67.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c9a","contributors":{"authors":[{"text":"Brown, Philip J.","contributorId":70483,"corporation":false,"usgs":true,"family":"Brown","given":"Philip J.","affiliations":[],"preferred":false,"id":246558,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53072,"text":"ofr03278 - 2003 - Approximate potentiometric surface of the bedrock aquifer at Great Bay, southeastern New Hampshire, 2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr03278","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-278","title":"Approximate potentiometric surface of the bedrock aquifer at Great Bay, southeastern New Hampshire, 2001","docAbstract":"Ground-water elevations (heads) in 265 wells were used to map the potentiometric-head surface in the fractured-bedrock aquifer adjacent to Great Bay, N.H. Remotely sensed data, spring-water temperatures and specific conductances, land-surface elevations, and simulated heads were also used to guide construction of the potentiometric surface. Heads in the bedrock aquifer locally varied more than 20 ft (feet) between adjacent wells as little as 200 ft apart. The depth to water below land surface was greater on the western and northwestern sides of the bay (about 20 ft) than on the southern and eastern sides (about 8 ft). Topography has a greater effect on heads than does temporal variation or measurement accuracy. Head gradients are steeper at the southern side of Great Bay, where the topographic relief is greatest, than at the northwestern and northeastern sides.","language":"ENGLISH","doi":"10.3133/ofr03278","usgsCitation":"Roseen, R.M., Degnan, J., Brannaka, L., Ballestero, T., and Mack, T.J., 2003, Approximate potentiometric surface of the bedrock aquifer at Great Bay, southeastern New Hampshire, 2001: U.S. Geological Survey Open-File Report 2003-278, 1 map ; 56 x 56 cm., on sheet 69 x 81 cm., folded in envelope 24 x 20 cm. , https://doi.org/10.3133/ofr03278.","productDescription":"1 map ; 56 x 56 cm., on sheet 69 x 81 cm., folded in envelope 24 x 20 cm. ","costCenters":[],"links":[{"id":5250,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr03-278/","linkFileType":{"id":5,"text":"html"}},{"id":181103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a24a","contributors":{"authors":[{"text":"Roseen, Robert M.","contributorId":74071,"corporation":false,"usgs":true,"family":"Roseen","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":246554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Degnan, J.R.","contributorId":18423,"corporation":false,"usgs":true,"family":"Degnan","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":246552,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brannaka, L.K.","contributorId":79554,"corporation":false,"usgs":true,"family":"Brannaka","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":246555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ballestero, T.P.","contributorId":14053,"corporation":false,"usgs":true,"family":"Ballestero","given":"T.P.","email":"","affiliations":[],"preferred":false,"id":246551,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mack, Thomas J. 0000-0002-0496-3918","orcid":"https://orcid.org/0000-0002-0496-3918","contributorId":39814,"corporation":false,"usgs":true,"family":"Mack","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":246553,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53071,"text":"ofr2003274 - 2003 - Archive of boomer seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June - August, 2001","interactions":[],"lastModifiedDate":"2021-08-19T20:48:18.236971","indexId":"ofr2003274","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-274","title":"Archive of boomer seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June - August, 2001","docAbstract":"In June, July, and August of 2001, the U.S. Geological Survey (USGS), in cooperation with the University of New Orleans (UNO), the U.S. Army Corps of Engineers, and the Louisiana Department of Natural Resources, conducted a shallow geophysical and sediment core survey of Timbalier Bay and the Gulf of Mexico offshore East Timbalier Island, Louisiana. This report serves as an archive of unprocessed digital seismic reflection data, trackline navigation files, trackline navigation maps, observers' logbooks, Geographic Information Systems (GIS) information, and formal Federal Geographic Data Committee (FGDC) metadata. In addition, a filtered and gained digital Graphics Interchange Format (GIF) image of each seismic profile is provided. Please see Kulp and others (2002), Flocks and others (2003), and Kulp and others (in prep.) for further information about the sediment cores collected and the geophysical results. For convenience, a list of acronyms and abbreviations frequently used in this report is also included.\r\n\r\nThis Digital Versatile Disc (DVD) document is readable on any computing platform that has standard DVD driver software installed. Documentation on this DVD was produced using Hyper Text Markup Language (HTML) utilized by the World Wide Web (WWW) and allows the user to access the information using a web browser (i.e. Netscape, Internet Explorer). To access the information contained on this disc, open the file 'index.htm' located at the top level of the disc using a web browser. This report also contains WWW links to USGS collaborators and other agencies. These links are only accessible if access to the Internet is available while viewing this DVD.\r\n\r\nThe archived boomer seismic reflection data are in standard Society of Exploration Geophysicists (SEG) SEG-Y format (Barry et al., 1975) and may be downloaded for processing with public domain software such as Seismic Unix (SU), currently located at http://www.cwp.mines.edu/cwpcodes/index.html. Examples of SU processing scripts are provided in the BOOM.tar file located in the SU subfolder of the SOFTWARE folder located at the top level of this disc. In-house (USGS) DOS and Microsoft Windows compatible software for viewing SEG-Y headers - DUMPSEGY.EXE (Zihlman, 1992) - is provided in the USGS subfolder of the SOFTWARE folder. Processed profile images, trackline navigation maps, logbooks, and formal metadata may be viewed with a web browser.","language":"English","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr2003274","usgsCitation":"Calderon, K., Dadisman, S.V., Flocks, J.G., Kindinger, J.L., and Wiese, D.S., 2003, Archive of boomer seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June - August, 2001: U.S. Geological Survey Open-File Report 2003-274, HTML Document, https://doi.org/10.3133/ofr2003274.","productDescription":"HTML Document","onlineOnly":"N","additionalOnlineFiles":"Y","temporalStart":"2001-06-30","temporalEnd":"2001-08-18","costCenters":[{"id":159,"text":"Center for Coastal and Watershed Studies","active":false,"usgs":true},{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":181102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":12037,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-274/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"East Timablier Island, Timbalier Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.5,28.916666666666668 ], [ -90.5,29.25 ], [ -90.16666666666667,29.25 ], [ -90.16666666666667,28.916666666666668 ], [ -90.5,28.916666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679df6","contributors":{"authors":[{"text":"Calderon, Karynna","contributorId":92739,"corporation":false,"usgs":true,"family":"Calderon","given":"Karynna","email":"","affiliations":[],"preferred":false,"id":246550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":246548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":246547,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kindinger, Jack L. jkindinger@usgs.gov","contributorId":815,"corporation":false,"usgs":true,"family":"Kindinger","given":"Jack","email":"jkindinger@usgs.gov","middleInitial":"L.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":246546,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wiese, Dana S. dwiese@usgs.gov","contributorId":2476,"corporation":false,"usgs":true,"family":"Wiese","given":"Dana","email":"dwiese@usgs.gov","middleInitial":"S.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":246549,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":53070,"text":"ofr2003271 - 2003 - Archive of chirp seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June 30 - July 9 and August 1 - 12, 2001","interactions":[],"lastModifiedDate":"2022-06-29T21:25:08.550555","indexId":"ofr2003271","displayToPublicDate":"2003-10-01T00:00:00","publicationYear":"2003","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-271","title":"Archive of chirp seismic reflection data collected during USGS cruises 01SCC01 and 01SCC02, Timbalier Bay and offshore East Timbalier Island, Louisiana, June 30 - July 9 and August 1 - 12, 2001","docAbstract":"In June, July, and August of 2001, the U.S. Geological Survey (USGS), in cooperation with the University of New Orleans, the U.S. Army Corps of Engineers, and the Louisiana Department of Natural Resources, conducted a shallow geophysical and sediment core survey of Timbalier Bay and the Gulf of Mexico offshore East Timbalier Island, Louisiana. This report serves as an archive of unprocessed digital seismic reflection data, trackline navigation files, trackline navigation maps, observers' logbooks, Geographic Information Systems (GIS) information, and formal Federal Geographic Data Committee (FGDC) metadata. In addition, a gained digital Graphics Interchange Format (GIF) image of each seismic profile is provided. Please see Kulp and others (2002), Flocks and others (2003), and Kulp and others (in prep.) for further information about the sediment cores collected and the geophysical results. For convenience, a list of acronyms and abbreviations frequently used in this report is also included.\r\n\r\nThis Digital Versatile Disc (DVD) document is readable on any computing platform that has standard DVD driver software installed. Documentation on this DVD was produced using Hyper Text Markup Language (HTML) utilized by the World Wide Web (WWW) and allows the user to access the information using a web browser (i.e. Netscape, Internet Explorer). To access the information contained on these discs, open the file 'index.htm' located at the top level of each disc using a web browser. This report also contains WWW links to USGS collaborators and other agencies. These links are only accessible if access to the internet is available while viewing these DVDs.\r\n\r\nThe archived chirp seismic reflection data are in standard Society of Exploration Geophysicists (SEG) SEG-Y format (Barry et al., 1975) and may be downloaded for processing with public domain software such as Seismic Unix (SU), currently located at http://www.cwp.mines.edu/cwpcodes/index.html. Examples of SU processing scripts are provided in the CHIRP.tar file located in the SU subfolder of the SOFTWARE folder located at the top level of each disc. In-house (USGS) DOS and Microsoft Windows compatible software for viewing SEG-Y headers - DUMPSEGY.EXE (Zihlman, 1992) - is provided in the USGS subfolder of the SOFTWARE folder. 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Two types of mine waste were examined in this study: sintered waste rock and slag. The samples were collected from the Elizabeth and Ely mines in the Vermont copper belt (Besshi-type massive sulfide deposits), from the Copper Basin mining district near Ducktown, Tennessee (Besshi-type massive sulfide deposits), and from the Clayton silver mine in the Bayhorse mining district, Idaho (polymetallic vein and replacement deposits). The data in this report are presented as a compilation with minimal interpretation or discussion. A detailed discussion and interpretation of the slag data are presented in a companion paper. Data collected from sintered waste rock and slag include: (1) bulk rock chemistry, (2) mineralogy, (3) and the distribution of trace elements among phases for the slag samples. 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