{"pageNumber":"258","pageRowStart":"6425","pageSize":"25","recordCount":36989,"records":[{"id":44282,"text":"ofr0278 - 2002 - Abstracts of the annual Planetary Geologic Mappers Meeting, June 18-19, 2001, Albuquerque, New Mexico","interactions":[],"lastModifiedDate":"2018-10-22T19:19:27","indexId":"ofr0278","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-78","title":"Abstracts of the annual Planetary Geologic Mappers Meeting, June 18-19, 2001, Albuquerque, New Mexico","docAbstract":"

The annual Planetary Geologic Mappers Meeting serves two purposes. In addition to giving mappers the opportunity to exchange ideas, experiences, victories, and problems with others, presentations are reviewed by the Geologic Mapping Subcommittee (GeMS) to provide input to the Planetary Geology and Geophysics Mapping Program review panel’s consideration of new proposals and progress reports that include mapping tasks. Funded mappers bring both oral presentation materials (slides or viewgraphs) and map products to post for review by GeMS and fellow mappers. Additionally, the annual meetings typically feature optional field trips offering earth analogs and parallels to planetary mapping problems.

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The 2001 Mappers Meeting, June 18-19, was convened by Tim Parker, Dave Senske, and Ken Tanaka and was hosted by Larry Crumpler and Jayne Aubele of the New Mexico Museum of Natural History and Science in Albuquerque, New Mexico. Oral presentations were given in the Museum’s Honeywell Auditorium, and maps were posted in the Sandia Room. In addition to active mappers, guests included local science teachers who had successfully competed for the right to attend and listen to the reports. It was a unique pleasure for mappers to have the opportunity to interact with and provide information to teachers responding so enthusiastically to the meeting presentation.

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On Sunday, June 17, Larry and Jayne conducted an optional pre-meeting field trip. The flanks of Rio Grande Rift, east and west of Albuquerque and Valles Caldera north of town presented tectonic, volcanic, and sedimentary examples of the Rift and adjoining areas analogous to observed features on Mars and Venus. The arid but volcanically and tectonically active environment of New Mexico’s rift valley enables focus on features that appear morphologically young and spectacular in satellite images and digital relief models. The theme of the trip was to see what, at orbiter resolution, \"obvious\" geologic features look like at lander (outcrop) scales. Trips to the top of the rift-flanking mountains (Sandia Peak, 10,600 ft) and the Valles Caldera, as well as various active spring deposits highlighted the day.

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After welcoming remarks from the host, Larry Crumpler, opening remarks by Tim Parker and Dave Senske and a report on mapping program status by Ken Tanaka, the mappers’ oral presentations began the morning of June 18, with a session on Venus Geologic Mapping. The afternoon continued with an exciting USGS Planetary GIS on the Web (PIGWAD) demonstration and ended with an open discussion of issues in planetary mapping. Posted maps of Venus quadrangles were viewed during the morning break.

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Tuesday’s Mars Geologic Mapping session began with a pep talk from Tim Parker encouraging mapping community input to the MER landing site selection committee and continued with Steve Saunders describing the potential contribution of Odyssey Mission data to the geologic mapping of Mars. A Mars map poster session was held during the morning break, and the meeting was adjourned mid-afternoon.

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After the mappers meeting on Tuesday, attendants were treated to a \"Field trip to Mars.\" The Institute of Meteoritics at the University of New Mexico houses an outstanding collection of meteorites, including those that have been identified as originating from Mars. The Institute tour featured examples of most of the different lithologies exhibited by martian meteorites identified to date, as well as some of the analytical tests (scanning electron microscope) they are conducting on specimens from ALH84001.

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Wednesday, June 20, featured an optional post-meeting field trip to see a travertine quarry and nearby sites of travertine deposition, the Very Large Array near Socorro, and other volcanic features within the Rio Grande Rift.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0278","usgsCitation":"Tanaka, K.L., and Senske, D.A., 2002, Abstracts of the annual Planetary Geologic Mappers Meeting, June 18-19, 2001, Albuquerque, New Mexico: U.S. Geological Survey Open-File Report 2002-78, 27 p., https://doi.org/10.3133/ofr0278.","productDescription":"27 p.","numberOfPages":"27","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":173256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr0278.jpg"},{"id":283406,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0078/pdf/of02-078.pdf"},{"id":3707,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0078/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Rio Grande Rift;Mars;Valles Caldera;Venus","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a38f1","contributors":{"editors":[{"text":"Parker, Thomas J. tparker@usgs.gov","contributorId":2908,"corporation":false,"usgs":true,"family":"Parker","given":"Thomas","email":"tparker@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":749308,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":229469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senske, David A.","contributorId":32975,"corporation":false,"usgs":true,"family":"Senske","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229470,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32941,"text":"ofr02203 - 2002 - Borehole velocity measurements at five sites that recorded the Cape Mendocino, California earthquake of 25 April, 1992","interactions":[],"lastModifiedDate":"2014-03-10T14:44:55","indexId":"ofr02203","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-203","title":"Borehole velocity measurements at five sites that recorded the Cape Mendocino, California earthquake of 25 April, 1992","docAbstract":"The U.S. Geological Survey (USGS), as part of an ongoing program to acquire seismic velocity and geologic data at locations that recorded strong-ground motions during earthquakes, has investigated five sites in the Fortuna, California region (Figure 1). We selected drill sites at strong-motion stations that recorded high accelerations (Table 1) from the Cape Mendocino earthquake (M 7.0) of 25 April 1992 (Oppenheimer et al., 1993). The boreholes were drilled to a nominal depth of 95 meters (310 ft) and cased with schedule 80 pvc-casing grouted in place at each location. S-wave and P-wave data were acquired at each site using a surface source and a borehole three-component geophone. This report contains the velocity models interpreted from the borehole data and gives reference to locations and peak accelerations at the selected strong-motion stations.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02203","usgsCitation":"Gibbs, J., Tinsley, J., and Boore, D.M., 2002, Borehole velocity measurements at five sites that recorded the Cape Mendocino, California earthquake of 25 April, 1992: U.S. Geological Survey Open-File Report 2002-203, 48 p., https://doi.org/10.3133/ofr02203.","productDescription":"48 p.","additionalOnlineFiles":"N","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":3111,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0203/","linkFileType":{"id":5,"text":"html"}},{"id":164373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0203/report-thumb.jpg"},{"id":60847,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0203/pdf/of02-203.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.40655,40.283417 ], [ -124.40655,40.345413 ], [ -124.266993,40.345413 ], [ -124.266993,40.283417 ], [ -124.40655,40.283417 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6029bc","contributors":{"authors":[{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":209487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tinsley, John C. III jtinsley@usgs.gov","contributorId":3266,"corporation":false,"usgs":true,"family":"Tinsley","given":"John C.","suffix":"III","email":"jtinsley@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":209486,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boore, David M. boore@usgs.gov","contributorId":2509,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":209485,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":32937,"text":"ofr02180 - 2002 - Evaluation of economically extractable coal resources in the Gillette coal field, Powder River basin, Wyoming","interactions":[],"lastModifiedDate":"2017-03-07T15:08:50","indexId":"ofr02180","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-180","title":"Evaluation of economically extractable coal resources in the Gillette coal field, Powder River basin, Wyoming","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02180","usgsCitation":"Ellis, M.S., Molnia, C.L., Osmonson, L.M., Ochs, A.M., Rohrbacher, T.J., Mercier, T.J., and Roberts, L.N., 2002, Evaluation of economically extractable coal resources in the Gillette coal field, Powder River basin, Wyoming: U.S. Geological Survey Open-File Report 2002-180, 48 p., https://doi.org/10.3133/ofr02180.","productDescription":"48 p.","costCenters":[],"links":[{"id":163082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3100,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0180/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wyoming ","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae09","contributors":{"authors":[{"text":"Ellis, Margaret S. mellis@usgs.gov","contributorId":198,"corporation":false,"usgs":true,"family":"Ellis","given":"Margaret","email":"mellis@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":209471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Molnia, Carol L.","contributorId":62238,"corporation":false,"usgs":true,"family":"Molnia","given":"Carol","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":209475,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Osmonson, Lee M.","contributorId":33322,"corporation":false,"usgs":false,"family":"Osmonson","given":"Lee","email":"","middleInitial":"M.","affiliations":[{"id":6676,"text":"USGS (retired)","active":true,"usgs":false}],"preferred":false,"id":209473,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ochs, Allan M.","contributorId":57513,"corporation":false,"usgs":true,"family":"Ochs","given":"Allan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":209474,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rohrbacher, Timothy J.","contributorId":20355,"corporation":false,"usgs":true,"family":"Rohrbacher","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":209472,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mercier, Tracy J. 0000-0002-8232-525X","orcid":"https://orcid.org/0000-0002-8232-525X","contributorId":79529,"corporation":false,"usgs":true,"family":"Mercier","given":"Tracy","email":"","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":209476,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roberts, Laura N.R.","contributorId":79530,"corporation":false,"usgs":true,"family":"Roberts","given":"Laura","email":"","middleInitial":"N.R.","affiliations":[],"preferred":false,"id":209477,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":32940,"text":"ofr02196 - 2002 - Bedrock and soil geochemistry from Voyageurs National Park, Minnesota","interactions":[],"lastModifiedDate":"2018-10-18T14:07:33","indexId":"ofr02196","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-196","title":"Bedrock and soil geochemistry from Voyageurs National Park, Minnesota","docAbstract":"

Bedrock, forest floor, and mineral soil sampling in Voyageurs National Park (VNP), Minnesota in 2000 and 2001 is part of a multidisciplinary project that includes the U. S. Geological Survey, National Park Service, University of Wisconsin – La Crosse, Minnesota Pollution Control Agency, and the Minnesota Department of Natural Resources. The joint project is examining the distribution of mercury in age-1 perch, lake water, bedrock and soils for eighteen watersheds in the interior of VNP. The purpose of the project was to establish the background and baseline geochemistry for bedrock and soil in the region, and to determine terrestrial mercury sources and sinks in VNP.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ofr02196","usgsCitation":"Woodruff, L.G., Cannon, W.F., Dicken, C.L., and Pimley, S., 2002, Bedrock and soil geochemistry from Voyageurs National Park, Minnesota: U.S. Geological Survey Open-File Report 2002-196, ii, 8 p., https://doi.org/10.3133/ofr02196.","productDescription":"ii, 8 p.","onlineOnly":"N","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":319954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02196.JPG"},{"id":3103,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-196/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Voyageurs National 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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":209482,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":209481,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dicken, Connie L. 0000-0002-1617-8132 cdicken@usgs.gov","orcid":"https://orcid.org/0000-0002-1617-8132","contributorId":57098,"corporation":false,"usgs":true,"family":"Dicken","given":"Connie","email":"cdicken@usgs.gov","middleInitial":"L.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":209483,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pimley, Shana","contributorId":96318,"corporation":false,"usgs":true,"family":"Pimley","given":"Shana","affiliations":[],"preferred":false,"id":209484,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":32935,"text":"ofr02174 - 2002 - Quality of economically extractable coal beds in the Gillette coal field as compared with other Tertiary coal beds in the Powder River basin, Wyoming and Montana","interactions":[],"lastModifiedDate":"2017-02-21T15:33:54","indexId":"ofr02174","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-174","title":"Quality of economically extractable coal beds in the Gillette coal field as compared with other Tertiary coal beds in the Powder River basin, Wyoming and Montana","docAbstract":"The Powder River Basin, and specifically the Gillette coal field, contains large quantities of economically extractable coal resources. These coal resources have low total sulfur content and ash yield, and most of the resources are subbituminous in rank. A recent U.S Geological Survey study of economically extractable coal in the Gillette coal field focused on five coal beds, the Wyodak rider, Upper Wyodak, Canyon, Lower Wyodak-Werner, and Gates/Kennedy. This report compares the coal quality of these economically extractable coal beds to coal in the Wyodak-Anderson coal zone in the Powder River Basin and in the Gillette coal field (Flores and others, 1999) and other produced coal in the Gillette coal field (Glass, 2000). The Upper Wyodak, Canyon, and Lower Wyodak/Werner beds are within the Wyodak-Anderson coal zone. Compared with all coal in the Wyodak-Anderson coal zone, both throughout the Powder River Basin and just within the Gillette coal field; the thick, persistent Upper Wyodak coal bed in the Gillette coal field has higher mean gross calorific value (8,569 Btu/lb), lower mean ash yield (5.8 percent), and lower mean total sulfur content (0.46 percent).","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02174","usgsCitation":"Ellis, M.S., 2002, Quality of economically extractable coal beds in the Gillette coal field as compared with other Tertiary coal beds in the Powder River basin, Wyoming and Montana: U.S. Geological Survey Open-File Report 2002-174, 20 p., https://doi.org/10.3133/ofr02174.","productDescription":"20 p.","costCenters":[],"links":[{"id":163000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3098,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0174/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654f6c","contributors":{"authors":[{"text":"Ellis, Margaret S. mellis@usgs.gov","contributorId":198,"corporation":false,"usgs":true,"family":"Ellis","given":"Margaret","email":"mellis@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":209468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32947,"text":"ofr02144 - 2002 - Methods of installing United States National Seismographic Network (USNSN) stations -- a construction manual","interactions":[],"lastModifiedDate":"2012-02-02T00:09:16","indexId":"ofr02144","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-144","title":"Methods of installing United States National Seismographic Network (USNSN) stations -- a construction manual","language":"ENGLISH","doi":"10.3133/ofr02144","usgsCitation":"McMillan, J.R., 2002, Methods of installing United States National Seismographic Network (USNSN) stations -- a construction manual: U.S. Geological Survey Open-File Report 2002-144, 25 p., https://doi.org/10.3133/ofr02144.","productDescription":"25 p.","costCenters":[],"links":[{"id":3115,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0144/","linkFileType":{"id":5,"text":"html"}},{"id":162989,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62be5b","contributors":{"authors":[{"text":"McMillan, John R.","contributorId":27905,"corporation":false,"usgs":true,"family":"McMillan","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":209497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32934,"text":"ofr02171 - 2002 - User's guide to HYPOINVERSE-2000, a Fortran program to solve for earthquake locations and magnitudes","interactions":[],"lastModifiedDate":"2014-03-07T10:45:40","indexId":"ofr02171","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-171","title":"User's guide to HYPOINVERSE-2000, a Fortran program to solve for earthquake locations and magnitudes","docAbstract":"

Hypoinverse is a computer program that processes files of seismic station data for an earthquake (like p wave arrival times and seismogram amplitudes and durations) into earthquake locations and magnitudes. It is one of a long line of similar USGS programs including HYPOLAYR (Eaton, 1969), HYPO71 (Lee and Lahr, 1972), and HYPOELLIPSE (Lahr, 1980).

\n
\n

If you are new to Hypoinverse, you may want to start by glancing at the section “SOME SIMPLE COMMAND SEQUENCES” to get a feel of some simpler sessions. This document is essentially an advanced user’s guide, and reading it sequentially will probably plow the reader into more detail than he/she needs. Every user must have a crust model, station list and phase data input files, and glancing at these sections is a good place to begin. The program has many options because it has grown over the years to meet the needs of one the largest seismic networks in the world, but small networks with just a few stations do use the program and can ignore most of the options and commands.

\n
\n

History and availability. Hypoinverse was originally written for the Eclipse minicomputer in 1978 (Klein, 1978). A revised version for VAX and Pro-350 computers (Klein, 1985) was later expanded to include multiple crustal models and other capabilities (Klein, 1989). This current report documents the expanded Y2000 version and it supercedes the earlier documents. It serves as a detailed user's guide to the current version running on unix and VAX-alpha computers, and to the version supplied with the Earthworm earthquake digitizing system. Fortran-77 source code (Sun and VAX compatible) and copies of this documentation is available via anonymous ftp from computers in Menlo Park. At present, the computer is swave.wr.usgs.gov and the directory is /ftp/pub/outgoing/klein/hyp2000. If you are running Hypoinverse on one of the Menlo Park EHZ or NCSN unix computers, the executable currently is ~klein/hyp2000/hyp2000.

\n
\n

New features. The Y2000 version of Hypoinverse includes all of the previous capabilities, but adds Y2000 formats to those defined earlier. In most cases, the new formats add 2 digits to the year field to accommodate the century. Other fields are sometimes rearranged or expanded to accommodate a better field order. The Y2000 formats are invoked with the “200” command. When the Y2000 flag is turned on, all files are read and written in the new format and there is no mixing of format types in a single run. Some formats without a date field, like station files, have not changed. A separate program called 2000CONV has been written to convert old formats to new.

\n
\n

Other new features, like expanded station names, calculating amplitude magnitudes from a variety of digital seismometers, station history files, interactive earthquake processing, and locations from CUSP (Caltech USGS Seismic Processing) binary files have been added.

\n
\n

General features. Hypoinverse will locate any number of events in an input file, which can be in one of several different formats. Any or all of printout, summary or archive output may be produced.

\n
\n

Hypoinverse is driven by user commands. The various commands define input and output files, set adjustable parameters, and solve for locations of a file of earthquake data using the parameters and files currently set. It is both interactive and \"batch\" in that commands may be executed either from the keyboard or from a file. You execute the commands in a file by typing @filename at the Hypoinverse prompt. Users may either supply parameters on the command line, or omit them and are prompted interactively. The current parameter values are displayed and may be taken as defaults by pressing just the RETURN key after the prompt. This makes the program very easy to use, providing you can remember the names of the commands. Combining commands with and without their required parameters into a command file permits a variety of customized procedures such as automatic input of crustal model and station data, but prompting for a different phase file each time.

\n
\n

All commands are 3 letters long and most require one or more parameters or file names. If they appear on a line with a command, character strings such as filenames must be enclosed in apostrophes (single quotes). Appendix 1 gives this and other free-format rules for supplying parameters, which are parsed in Fortran. When several parameters are required following a command, any of them may be omitted by replacing them with null fields (see appendix 1). A null field leaves that parameter unchanged from its current or default value. When you start HYPOINVERSE, default values are in effect for all parameters except file names.

\n
\n

Hypoinverse is a complicated program with many features and options. Many of these \"advanced\" or seldom used features are documented here, but are more detailed than a typical user needs to read about when first starting with the program. I have put some of this material in smaller type so that a first time user can concentrate on the more important information.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02171","usgsCitation":"Klein, F.W., 2002, User's guide to HYPOINVERSE-2000, a Fortran program to solve for earthquake locations and magnitudes: U.S. Geological Survey Open-File Report 2002-171, 123 p., https://doi.org/10.3133/ofr02171.","productDescription":"123 p.","numberOfPages":"123","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":162999,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02171.jpg"},{"id":3097,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0171/","linkFileType":{"id":5,"text":"html"}},{"id":283467,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0171/pdf/of02-171.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603e5c","contributors":{"authors":[{"text":"Klein, Fred W. klein@usgs.gov","contributorId":4417,"corporation":false,"usgs":true,"family":"Klein","given":"Fred","email":"klein@usgs.gov","middleInitial":"W.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":209467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32933,"text":"ofr2002165 - 2002 - Molybdenum recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:09:18","indexId":"ofr2002165","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-165","title":"Molybdenum recycling in the United States in 1998","docAbstract":"This report describes the flow of molybdenum in the United States in 1998 with emphasis on the extent to which molybdenum was recycled. Molybdenum was mostly recycled from products of molybdenum-bearing steels and superalloys, with some molybdenum products recovered specifically for their high molybdenum content. In 1998, 8,000 metric tons (t) of molybdenum was estimated to have been recycled, and the recycling rate was calculated to be 33 percent, with recycling efficiency at about 30 percent.","language":"ENGLISH","doi":"10.3133/ofr2002165","usgsCitation":"Blossom, J.W., 2002, Molybdenum recycling in the United States in 1998 (Online version 1.0): U.S. Geological Survey Open-File Report 2002-165, 12 p., https://doi.org/10.3133/ofr2002165.","productDescription":"12 p.","costCenters":[],"links":[{"id":162998,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9156,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-165/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699264","contributors":{"authors":[{"text":"Blossom, John W.","contributorId":85238,"corporation":false,"usgs":true,"family":"Blossom","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":209466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32932,"text":"ofr02149 - 2002 - Asbestos: Geology, Mineralogy, Mining, and Uses","interactions":[],"lastModifiedDate":"2012-02-02T00:09:18","indexId":"ofr02149","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-149","title":"Asbestos: Geology, Mineralogy, Mining, and Uses","docAbstract":"The term asbestos is a generic designation referring usually to six types of naturally occurring mineral fibers that are or have been commercially exploited. These fibers belong to two mineral groups: serpentines and amphiboles. The serpentine group contains a single asbestiform variety: chrysotile; five asbestiform varieties of amphiboles are known: anthophyllite asbestos, grunerite asbestos (amosite), riebeckite asbestos (crocidolite), tremolite asbestos, and actinolite asbestos. These fibrous minerals share several properties which qualify them as asbestiform fibers: they are found in bundles of fibers which can be easily separated from the host matrix or cleaved into thinner fibers; the fibers exhibit high tensile strengths, they show high length: diameter (aspect) ratios, from a minimum of 20 up to greater than 1000; they are sufficiently flexible to be spun; and macroscopically, they resemble organic fibers such as cellulose. Since asbestos fibers are all silicates, they exhibit several other common properties, such as incombustibility, thermal stability, resistance to biodegradation, chemical inertia toward most chemicals, and low electrical conductivity. \r\n\r\nThe term asbestos has traditionally been attributed only to those varieties that are commercially exploited. The industrial applications of asbestos fibers have now shifted almost exclusively to chrysotile. Two types of amphiboles, commonly designated as amosite and crocidolite are no longer mined. The other three amphibole varieties, anthophyllite asbestos, actinolite asbestos, and tremolite asbestos, have no significant industrial applications presently.","language":"ENGLISH","doi":"10.3133/ofr02149","usgsCitation":"Virta, R.L., 2002, Asbestos: Geology, Mineralogy, Mining, and Uses: U.S. Geological Survey Open-File Report 2002-149, 35 p. : ill. ; 28 cm., https://doi.org/10.3133/ofr02149.","productDescription":"35 p. : ill. ; 28 cm.","costCenters":[],"links":[{"id":164391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3096,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-149/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672bbb","contributors":{"authors":[{"text":"Virta, Robert L. rvirta@usgs.gov","contributorId":395,"corporation":false,"usgs":true,"family":"Virta","given":"Robert","email":"rvirta@usgs.gov","middleInitial":"L.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":209465,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32936,"text":"ofr02177 - 2002 - Magnetotelluric data along the Tangle Lakes profile, Alaska","interactions":[],"lastModifiedDate":"2022-08-26T21:05:40.24783","indexId":"ofr02177","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-177","title":"Magnetotelluric data along the Tangle Lakes profile, Alaska","docAbstract":"

The 89 km long Tangle Lakes profile of 14 magnetotelluric (MT) stations begins 4 km south of the confluence of Augustana Creek and the Delta River in south central Alaska. The northernmost station, TLM13, is located just south of the Denali Fault in the rugged Clearwater Mountains. The north-south profile crosses the Ampitheater Mountains northwest of the Tangle Lakes area and continues until it terminates in the flatlands south of the Alphabet Hills. The profile intersects the Denali Highway 32km west of Paxson.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr02177","usgsCitation":"Sampson, J.A., and Rodriguez, B.D., 2002, Magnetotelluric data along the Tangle Lakes profile, Alaska: U.S. Geological Survey Open-File Report 2002-177, 144 p., https://doi.org/10.3133/ofr02177.","productDescription":"144 p.","costCenters":[],"links":[{"id":163001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":405727,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51835.htm","linkFileType":{"id":5,"text":"html"}},{"id":3099,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0177/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Tangle Lakes","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -145.6333,\n 62.5947\n ],\n [\n -146.5833,\n 62.5947\n ],\n [\n -146.5833,\n 63.45\n ],\n [\n -145.6333,\n 63.45\n ],\n [\n -145.6333,\n 62.5947\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649436","contributors":{"authors":[{"text":"Sampson, Jay A.","contributorId":13939,"corporation":false,"usgs":true,"family":"Sampson","given":"Jay","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":209470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodriguez, Brian D. 0000-0002-2263-611X brod@usgs.gov","orcid":"https://orcid.org/0000-0002-2263-611X","contributorId":836,"corporation":false,"usgs":true,"family":"Rodriguez","given":"Brian","email":"brod@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":209469,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32944,"text":"ofr02189 - 2002 - Rare Earth Element Mines, Deposits, and Occurrences","interactions":[],"lastModifiedDate":"2012-02-10T00:10:09","indexId":"ofr02189","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-189","title":"Rare Earth Element Mines, Deposits, and Occurrences","docAbstract":"Data on rare earth (including yttrium) mines, deposits, and occurrences were compiled as part of an effort by the USGS and the University of Arizona Center for Mineral Resources to summarize current knowledge on the supply and demand outlook and related topics for this group of elements. Economic competition and environmental concerns are increasingly constraining the mining and processing of rare earths from the Mountain Pass mine in California. For many years, the deposit at Mountain Pass was the world's dominant source of rare earth elements and the United States was essentially self-sufficient. Starting approximately 10 years ago, the U.S. has become increasingly dependent (> 90 percent of separated rare earths) upon imports from China, now the dominant source of rare earths. A knowledge of the known economic and noneconomic sources of rare earths is basic to evaluating the outlook for rare earth supply and associated issues.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr02189","usgsCitation":"Orris, G.J., and Grauch, R.I., 2002, Rare Earth Element Mines, Deposits, and Occurrences (Version 1.0): U.S. Geological Survey Open-File Report 2002-189, Report: 174 p.; ReadMe; Metadata; Appendix, https://doi.org/10.3133/ofr02189.","productDescription":"Report: 174 p.; ReadMe; Metadata; Appendix","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":162988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":11520,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-189/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -166.5,-41.1 ], [ -166.5,71 ], [ 175.86666666666667,71 ], [ 175.86666666666667,-41.1 ], [ -166.5,-41.1 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684cea","contributors":{"authors":[{"text":"Orris, Greta J. 0000-0002-2340-9955 greta@usgs.gov","orcid":"https://orcid.org/0000-0002-2340-9955","contributorId":3472,"corporation":false,"usgs":true,"family":"Orris","given":"Greta","email":"greta@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":209492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grauch, Richard I. 0000-0002-1763-0813 rgrauch@usgs.gov","orcid":"https://orcid.org/0000-0002-1763-0813","contributorId":1193,"corporation":false,"usgs":true,"family":"Grauch","given":"Richard","email":"rgrauch@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":209491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32980,"text":"ofr02102 - 2002 - Water-quality monitoring and studies of the formation and fate of trihalomethanes during the third injection, storage and recovery test at Lancaster, Antelope Valley, California, March 1998 through April 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:09:17","indexId":"ofr02102","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-102","title":"Water-quality monitoring and studies of the formation and fate of trihalomethanes during the third injection, storage and recovery test at Lancaster, Antelope Valley, California, March 1998 through April 1999","docAbstract":"The U.S. Geological Survey, in cooperation with the Los Angeles County Department of Public Works and the Antelope Valley-East Kern Water Agency, conducted three cycles of injection, storage, and recovery tests to evaluate the feasibility of artificially recharging ground water in the Lancaster area of Antelope Valley, California. During the third cycle (March 1998 through April 1999), the tests included investigations of the formation and fate of trihalomethanes in the aquifer. Trihalomethanes are disinfection by-products formed by reaction between natural dissolved organic carbon that is present in water and chlorine that is added during the drinking-water-treatment process. This report includes a discussion of the design of the investigation; descriptions of the sampling, analytical, and experimental methods used in the investigation; and a presentation of the data collected.\r\n\r\nDuring the third cycle, 60 million gallons of chlorinated water was injected into the aquifer through well 7N/12W-27P2 in the Los Angeles County Department of Public Works well field in Lancaster between April 15 and June 16, 1998. One hundred fifty million gallons of water was extracted from the same well between June 30, 1998, and April 29, 1999. Water-quality samples were collected during the entire cycle from the well and from a nearby set of nested piezometers, and were analyzed for residual chlorine, dissolved organic carbon, trihalomethane, major anion, and dissolved solid concentrations; ultraviolet absorbance spectra; and a number of field water-quality parameters. A statistical analysis was done to evaluate the analytical precision of the residual chlorine, dissolved organic carbon, trihalomethane, and ultraviolet absorbance measurements on these samples. The formation of trihalomethanes in the injection water was examined in laboratory experiments: Trihalomethane concentrations in samples of injection water were monitored during a storage period, and trihalomethane formation potential in the presence of excess chlorine was measured. The role of mixing between injection water and ground water and the conservative or non-conservative behavior of trihalomethanes was studied by adding a conservative tracer, sulfur hexafluoride, to the injection water and monitoring its concentration in the extraction water. The potential for biodegradation of trihalomethanes by aquifer bacteria was assessed in laboratory experiments: Microcosms containing ground water or extraction water and sediment or concentrated bacteria were spiked with trihalomethanes, and the amount of trihalomethanes was monitored during an incubation period. The potential for sorption of trihalomethanes to aquifer sediments was assessed in laboratory experiments: Mixtures of sediment and water were spiked with trihalomethanes, and then the trihalomethane concentrations were measured after an equilibration period.","language":"ENGLISH","doi":"10.3133/ofr02102","usgsCitation":"Fram, M.S., Berghouse, J.K., Bergamaschi, B., Fujii, R., Goodwin, K.D., and Clark, J., 2002, Water-quality monitoring and studies of the formation and fate of trihalomethanes during the third injection, storage and recovery test at Lancaster, Antelope Valley, California, March 1998 through April 1999: U.S. Geological Survey Open-File Report 2002-102, 48 p.; 8 illus.; 27 tables, https://doi.org/10.3133/ofr02102.","productDescription":"48 p.; 8 illus.; 27 tables","costCenters":[],"links":[{"id":163453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3142,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/ofr02102/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5611","contributors":{"authors":[{"text":"Fram, Miranda S. 0000-0002-6337-059X mfram@usgs.gov","orcid":"https://orcid.org/0000-0002-6337-059X","contributorId":1156,"corporation":false,"usgs":true,"family":"Fram","given":"Miranda","email":"mfram@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":209601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berghouse, Joshua K.","contributorId":19990,"corporation":false,"usgs":true,"family":"Berghouse","given":"Joshua","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":209602,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bergamaschi, Brian A. 0000-0002-9610-5581","orcid":"https://orcid.org/0000-0002-9610-5581","contributorId":73241,"corporation":false,"usgs":true,"family":"Bergamaschi","given":"Brian A.","affiliations":[],"preferred":false,"id":209603,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fujii, Roger rfujii@usgs.gov","contributorId":553,"corporation":false,"usgs":true,"family":"Fujii","given":"Roger","email":"rfujii@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":209600,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Goodwin, Kelly D.","contributorId":79934,"corporation":false,"usgs":true,"family":"Goodwin","given":"Kelly","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":209604,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Clark, Jordan F.","contributorId":106177,"corporation":false,"usgs":true,"family":"Clark","given":"Jordan F.","affiliations":[],"preferred":false,"id":209605,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":32943,"text":"ofr02225 - 2002 - Data from theodolite measurements of creep rates on San Francisco Bay region faults, California: 1979-2001","interactions":[{"subject":{"id":32943,"text":"ofr02225 - 2002 - Data from theodolite measurements of creep rates on San Francisco Bay region faults, California: 1979-2001","indexId":"ofr02225","publicationYear":"2002","noYear":false,"title":"Data from theodolite measurements of creep rates on San Francisco Bay region faults, California: 1979-2001"},"predicate":"SUPERSEDED_BY","object":{"id":97671,"text":"ofr20091119 - 2009 - Data from theodolite measurements of creep rates on San Francisco Bay region faults, California","indexId":"ofr20091119","publicationYear":"2009","noYear":false,"title":"Data from theodolite measurements of creep rates on San Francisco Bay region faults, California"},"id":1}],"supersededBy":{"id":97671,"text":"ofr20091119 - 2009 - Data from theodolite measurements of creep rates on San Francisco Bay region faults, California","indexId":"ofr20091119","publicationYear":"2009","noYear":false,"title":"Data from theodolite measurements of creep rates on San Francisco Bay region faults, California"},"lastModifiedDate":"2014-03-10T15:30:55","indexId":"ofr02225","displayToPublicDate":"2002-06-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-225","title":"Data from theodolite measurements of creep rates on San Francisco Bay region faults, California: 1979-2001","docAbstract":"My purpose is to make our creep data on San Francisco Bay region active faults available to the scientific research community. My student research assistants and I measured creep (aseismic slip) rates on these faults from 1979 until my retirement from the project in 2001. These data are further described in my final technical report as principal investigator, which summarizes results from 22 September 1979 through 28 February 2001 (Galehouse, 2001). We made over 2,600 creep measurements, about one-third in the ten years prior to the Loma Prieta earthquake (LPEQ) and two-thirds in the 11.4 years following it. The measurements are continuing to be made by members of the Geosciences Department at San Francisco State University (SFSU) under the direction of Karen Grove and John Caskey. A complete analysis of our results obtained on the Hayward fault is presented in Lienkaemper, Galehouse, and Simpson (2001). A formal report based on the entire San Francisco Bay region data set is in preparation.\n\nData sheets for each site along the fault are available for downloading in Excel format to facilitate analysis of the data. They are also available as tab-delimited raw data. The data include all regular measurement sites, SF–1 through SF–34, and the 20 SFSU and U.S. Geological Survey (USGS) afterslip sites on the Hayward fault.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr02225","usgsCitation":"Galehouse, J.S., 2002, Data from theodolite measurements of creep rates on San Francisco Bay region faults, California: 1979-2001: U.S. Geological Survey Open-File Report 2002-225, Report: 94 p.; Haward Fault: 1 XLS file, 1 .GZ file; SF Bay: 1 XLS file, 1 SF .GZ file, https://doi.org/10.3133/ofr02225.","productDescription":"Report: 94 p.; Haward Fault: 1 XLS file, 1 .GZ file; SF Bay: 1 XLS file, 1 SF .GZ file","additionalOnlineFiles":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":164375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr02225.gif"},{"id":3113,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/0225/","linkFileType":{"id":5,"text":"html"}},{"id":283760,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0225/pdf/of02-225.pdf"},{"id":283761,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0225/data_files/HaywardFault.tar.gz"},{"id":283762,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0225/SFBayRegion.xls"},{"id":283763,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/2002/0225/data_files/SFBayRegion.tar.gz"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.9148,36.9192 ], [ -123.9148,39.557 ], [ -120.9814,39.557 ], [ -120.9814,36.9192 ], [ -123.9148,36.9192 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c887","contributors":{"authors":[{"text":"Galehouse, Jon S.","contributorId":57894,"corporation":false,"usgs":true,"family":"Galehouse","given":"Jon","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":209490,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32376,"text":"ofr02161 - 2002 - Thermodynamic data for modeling acid mine drainage problems: compilation and estimation of data for selected soluble iron-sulfate minerals","interactions":[],"lastModifiedDate":"2012-02-02T00:09:22","indexId":"ofr02161","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-161","title":"Thermodynamic data for modeling acid mine drainage problems: compilation and estimation of data for selected soluble iron-sulfate minerals","docAbstract":"Enthalpy of formation, Gibbs energy of formation, and entropy values have been compiled from the literature for the hydrated ferrous sulfate minerals melanterite, rozenite, and szomolnokite, and a variety of other hydrated sulfate compounds. On the basis of this compilation, it appears that there is no evidence for an excess enthalpy of mixing for sulfate-H2O systems, except for the first H2O molecule of crystallization. The enthalpy and Gibbs energy of formation of each H2O molecule of crystallization, except the first, in the iron(II) sulfate - H2O system is -295.15 and -238.0 kJ?mol-1, respectively. The absence of an excess enthalpy of mixing is used as the basis for estimating thermodynamic values for a variety of ferrous, ferric, and mixed-valence sulfate salts of relevance to acid-mine drainage systems.","language":"ENGLISH","doi":"10.3133/ofr02161","usgsCitation":"Hemingway, B.S., Seal, R., and Chou, I., 2002, Thermodynamic data for modeling acid mine drainage problems: compilation and estimation of data for selected soluble iron-sulfate minerals: U.S. Geological Survey Open-File Report 2002-161, 13 p., https://doi.org/10.3133/ofr02161.","productDescription":"13 p.","costCenters":[],"links":[{"id":163573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3361,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/of02-161/ ","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a56e4b07f02db62dc10","contributors":{"authors":[{"text":"Hemingway, Bruch S.","contributorId":19542,"corporation":false,"usgs":true,"family":"Hemingway","given":"Bruch","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":208467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seal, Robert R. II 0000-0003-0901-2529 rseal@usgs.gov","orcid":"https://orcid.org/0000-0003-0901-2529","contributorId":397,"corporation":false,"usgs":true,"family":"Seal","given":"Robert R.","suffix":"II","email":"rseal@usgs.gov","affiliations":[],"preferred":false,"id":208465,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chou, I-Ming 0000-0001-5233-6479 imchou@usgs.gov","orcid":"https://orcid.org/0000-0001-5233-6479","contributorId":882,"corporation":false,"usgs":true,"family":"Chou","given":"I-Ming","email":"imchou@usgs.gov","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":208466,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":32373,"text":"ofr02139 - 2002 - Magnetic susceptibilities measured on rocks of the upper Cook Inlet, Alaska","interactions":[],"lastModifiedDate":"2018-05-20T17:03:08","indexId":"ofr02139","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-139","title":"Magnetic susceptibilities measured on rocks of the upper Cook Inlet, Alaska","docAbstract":"We have measured magnetic susceptibility in the field on most of the geologic rock formations exposed in the upper Cook Inlet near Anchorage and Kenai, Alaska. Measured susceptibilities range from less than our detection limit of 0.01 x 10-3 (SI) to greater than 100 x 10-3 (SI). As expected, mafic igneous rocks have the highest susceptibilities and some sedimentary rocks the lowest. Rocks of the Tertiary Sterling Formation yielded some moderate to high susceptibility values. Although we do not have detailed information on the magnetic mineralogy of the rocks measured here, the higher susceptibilities are sufficient to explain the magnitudes of some short-wavelength aeromagnetic anomalies observed on recent surveys of the upper Cook Inlet.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02139","usgsCitation":"Alstatt, A., Saltus, R.W., Bruhn, R., and Haeussler, P.J., 2002, Magnetic susceptibilities measured on rocks of the upper Cook Inlet, Alaska: U.S. Geological Survey Open-File Report 2002-139, 18 p., https://doi.org/10.3133/ofr02139.","productDescription":"18 p.","costCenters":[],"links":[{"id":163482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3359,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0139/","linkFileType":{"id":5,"text":"html"}}],"country":"United States ","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649365","contributors":{"authors":[{"text":"Alstatt, A.A.","contributorId":36984,"corporation":false,"usgs":true,"family":"Alstatt","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":208453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saltus, R. W.","contributorId":85588,"corporation":false,"usgs":true,"family":"Saltus","given":"R.","middleInitial":"W.","affiliations":[],"preferred":false,"id":208456,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bruhn, R.L.","contributorId":46972,"corporation":false,"usgs":true,"family":"Bruhn","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":208454,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haeussler, Peter J. 0000-0002-1503-6247 pheuslr@usgs.gov","orcid":"https://orcid.org/0000-0002-1503-6247","contributorId":503,"corporation":false,"usgs":true,"family":"Haeussler","given":"Peter","email":"pheuslr@usgs.gov","middleInitial":"J.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":208455,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":32372,"text":"ofr2002136 - 2002 - Preliminary geologic map of the Santa Barbara coastal plain area, Santa Barbara County, California","interactions":[{"subject":{"id":32372,"text":"ofr2002136 - 2002 - Preliminary geologic map of the Santa Barbara coastal plain area, Santa Barbara County, California","indexId":"ofr2002136","publicationYear":"2002","noYear":false,"title":"Preliminary geologic map of the Santa Barbara coastal plain area, Santa Barbara County, California"},"predicate":"SUPERSEDED_BY","object":{"id":97766,"text":"sim3001 - 2009 - Geologic Map of the Santa Barbara Coastal Plain Area, Santa Barbara County, California","indexId":"sim3001","publicationYear":"2009","noYear":false,"title":"Geologic Map of the Santa Barbara Coastal Plain Area, Santa Barbara County, California"},"id":1}],"supersededBy":{"id":97766,"text":"sim3001 - 2009 - Geologic Map of the Santa Barbara Coastal Plain Area, Santa Barbara County, California","indexId":"sim3001","publicationYear":"2009","noYear":false,"title":"Geologic Map of the Santa Barbara Coastal Plain Area, Santa Barbara County, California"},"lastModifiedDate":"2012-02-02T00:09:22","indexId":"ofr2002136","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-136","title":"Preliminary geologic map of the Santa Barbara coastal plain area, Santa Barbara County, California","docAbstract":"This report presents a new geologic digital map of the Santa Barbara coastal plain area at a compilation scale of 1:24,000 (one inch on the map = 2,000 feet on the ground) and with a horizontal positional accuracy of at least 20 m. This preliminary map depicts the distribution of bedrock units and surficial deposits and associated deformation underlying and adjacent to the coastal plain within the contiguous Santa Barbara and Goleta 7.5' quadrangles. A planned second version will extend the mapping westward into the adjoining Dos Pueblos Canyon quadrangle and eastward into the Carpinteria quadrangle. The mapping presented here results from the collaborative efforts of geologists with the U.S. Geological Survey Southern California Areal Mapping Project (SCAMP) (Minor, Kellogg, Stanley, Stone, and Powell) and the tectonic geomorphology research group at the University of California at Santa Barbara (Gurrola and Selting). C.L. Powell, II, performed all new fossil identifications and interpretations reported herein. T.R. Brandt designed and edited the GIS database,performed GIS database integration and created the digital cartography for the map layout. \r\n\r\n The Santa Barbara coastal plain is located in the western Transverse Ranges physiographic province along a west-trending segment of the southern California coastline about 100 km (62 mi) northwest of Los Angeles. The coastal plain region, which extends from the Santa Ynez Mountains on the north to the Santa Barbara Channel on the south, is underlain by numerous active and potentially active folds and partly buried thrust faults of the Santa Barbara fold and fault belt. Strong earthquakes that occurred in the region in 1925 (6.8 magnitude) and 1978 (5.1 magnitude) are evidence that such structures pose a significant earthquake hazard to the approximately 200,000 people living within the major coastal population centers of Santa Barbara and Goleta. Also, young landslide deposits along the steep lower flank of the Santa Ynez Mountains indicate the potential for continued slope failures and mass movements that may threaten urbanized parts of the coastal plain. Deformed sedimentary rocks in the subsurface of the coastal plain and the adjacent Santa Barbara Channel contain deposits of oil and gas, some of which are currently being extracted. Shallow, localized sedimentary aquifers underlying the coastal plain provide limited amounts of water for the urban areas, but the quality of some of this groundwater is compromised by coastal salt-water contamination. The present map compilation provides a set of uniform geologic digital coverages that can be used for analysis and prediction of these and other geologic hazards and resources in the coastal plain region.\r\n In the map area the oldest stratigraphic units consist of resistant Eocene to Oligocene marine and terrestrial sedimentary rocks that form a mostly southward-dipping and laterally continuous sequence along the south flank of the Santa Ynez Mountains. Less resistant, but more variably deformed, Miocene, Pliocene, and Pleistocene marine sedimentary rocks and deposits are exposed in the lower Santa Ynez foothills and in the coastal hills and sea cliffs farther south. Pleistocene and Holocene surficial alluvial, colluvial, estuarine, and marine-terrace deposits directly underlie much of the low-lying coastal plain area, and similar-aged alluvial and landslide deposits locally mantle the lower flanks of the Santa Ynez Mountains.\r\n Structurally, the Santa Barbara coastal plain area is dominated by the Santa Barbara fold and fault belt, an east-west-trending zone of Quaternary, partly active folds and blind and exposed reverse and thrust faults. The dominant trend of individual structures within the belt is west-northwest -- slightly oblique to the overall trend of the fold and fault belt. A conspicuous exception, however, is the More Ranch fault system, which strikes east-northeast across the fold and f","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr2002136","usgsCitation":"Minor, S.A., Kellogg, K., Stanley, R.G., Stone, P., Powell, C.L., Gurrola, L.D., Selting, A.J., and Brandt, T.R., 2002, Preliminary geologic map of the Santa Barbara coastal plain area, Santa Barbara County, California (Superseded by SIM 3001): U.S. Geological Survey Open-File Report 2002-136, 21 p., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet)., https://doi.org/10.3133/ofr2002136.","productDescription":"21 p., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet).","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":110290,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51443.htm","linkFileType":{"id":5,"text":"html"},"description":"51443"},{"id":163481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8382,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0136/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","edition":"Superseded by SIM 3001","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67abed","contributors":{"authors":[{"text":"Minor, Scott A. 0000-0002-6976-9235 sminor@usgs.gov","orcid":"https://orcid.org/0000-0002-6976-9235","contributorId":765,"corporation":false,"usgs":true,"family":"Minor","given":"Scott","email":"sminor@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":208446,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":208451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stanley, Richard G. 0000-0001-6192-8783 rstanley@usgs.gov","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":1832,"corporation":false,"usgs":true,"family":"Stanley","given":"Richard","email":"rstanley@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":208448,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stone, Paul 0000-0002-1439-0156 pastone@usgs.gov","orcid":"https://orcid.org/0000-0002-1439-0156","contributorId":273,"corporation":false,"usgs":true,"family":"Stone","given":"Paul","email":"pastone@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":208445,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Powell, Charles L. II 0000-0002-1913-555X cpowell@usgs.gov","orcid":"https://orcid.org/0000-0002-1913-555X","contributorId":3243,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","email":"cpowell@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":208449,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gurrola, Larry D.","contributorId":95525,"corporation":false,"usgs":true,"family":"Gurrola","given":"Larry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":208452,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Selting, Amy J.","contributorId":35782,"corporation":false,"usgs":true,"family":"Selting","given":"Amy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":208450,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Brandt, Theodore R. 0000-0002-7862-9082 tbrandt@usgs.gov","orcid":"https://orcid.org/0000-0002-7862-9082","contributorId":1267,"corporation":false,"usgs":true,"family":"Brandt","given":"Theodore","email":"tbrandt@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":208447,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":32374,"text":"ofr02142 - 2002 - Post-glacial inflation-deflation cycles, tilting, and faulting in the Yellowstone Caldera based on Yellowstone Lake shorelines","interactions":[],"lastModifiedDate":"2017-03-07T14:03:14","indexId":"ofr02142","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-142","title":"Post-glacial inflation-deflation cycles, tilting, and faulting in the Yellowstone Caldera based on Yellowstone Lake shorelines","docAbstract":"The Yellowstone caldera, like many other later Quaternary calderas of the world, exhibits dramatic unrest. Between 1923 and 1985, the center of the Yellowstone caldera rose nearly one meter along an axis between its two resurgent domes (Pelton and Smith, 1979, Dzurisin and Yamashita, 1987). From 1985 until 1995-6, it subsided at about two cm/yr (Dzurisin and others, 1990). More recent radar interferometry studies show renewed inflation of the northeastern resurgent dome between 1995 and 1996; this inflation migrated to the southwestern resurgent dome from 1996 to 1997 (Wicks and others, 1998). We extend this record back in time using dated geomorphic evidence of postglacial Yellowstone Lake shorelines around the northern shore, and Yellowstone River levels in the outlet area. We date these shorelines using carbon isotopic and archeological methods. Following Meyer and Locke (1986) and Locke and Meyer (1994), we identify the modern shoreline as S1 (1.9 ? 0.3 m above the lake gage datum), map paleoshoreline terraces S2 to S6, and infer that the prominent shorelines were cut during intracaldera uplift episodes that produced rising water levels. Doming along the caldera axis reduces the gradient of the Yellowstone River from Le Hardys Rapids to the Yellowstone Lake outlet and ultimately causes an increase in lake level. The 1923-1985 doming is part of a longer uplift episode that has reduced the Yellowstone River gradient to a ?pool? with a drop of only 0.25 m over most of this 5 km reach. We also present new evidence that doming has caused submergence of some Holocene lake and river levels. Shoreline S5 is about 14 m above datum and estimated to be ~12.6 ka, because it post-dates a large hydrothermal explosion deposit from the Mary Bay area (MB-II) that occurred ~13 ka. S4 formed about 8 m above datum ~10.7 ka as dated by archeology and 14C, and was accompanied by offset on the Fishing Bridge fault. About 9.7 ka, the Yellowstone River eroded the ?S-meander?, followed by a ~5 m rise in lake level to S2. The lowest generally recognizable shoreline is S2. It is ~5 m above datum (3 m above S1) and is ~8 ka, as dated on both sides of the outlet. Yellowstone Lake and the river near Fishing Bridge were 5-6 m below their present level about 3-4 ka, as indicated by 14C ages from submerged beach deposits, drowned valleys, and submerged Yellowstone River gravels. Thus, the lake in the outlet region has been below or near its present level for about half the time since a 1 km-thick icecap melted from the Yellowstone Lake basin about 16 ka. The amplitude of two rises in lake and river level can be estimated based on the altitude of Le Hardys Rapids, indicators of former lake and river levels, and reconstruction of the river gradient from\r\nthe outlet to Le Hardys Rapids. Both between ~9.5 ka and ~8.5 ka, and after ~3 ka, Le Hardys Rapids (LHR) was uplifted about 8 meters above the outlet, suggesting a cyclic deformation process. Older possible rises in lake level are suggested by locations where the ~10.7 ka S4 truncates older shorelines, and valleys truncated by the ~12.6 ka S5 shoreline. Using these controls, a plot of lake level through time shows 5-7 millennial-scale oscillations since 14.5 ka. Major cycles of inflation and deflation are thousands of years long. Le Hardys Rapids has twice been uplifted ~8 m relative to the lake outlet. These two locations span only the central 25% of the historic caldera doming, so that if we use historic doming as a model, total projected uplift would be ~32 m. This ?heavy breathing? of the central part of the Yellowstone caldera may reflect a combination of several possible processes: magmatic inflation, tectonic stretching and deflation, and hydrothermal fluid sealing and inflation followed by cracking of the seal, pressure release, and deflation. Over the entire postglacial period, subsidence has balanced or slightly exceeded uplift as shown by older shorelines that descend towards the caldera axis. We","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/ofr02142","usgsCitation":"Pierce, K.L., Cannon, K.P., Meyer, G.A., Trebesch, M.J., and Watts, R.D., 2002, Post-glacial inflation-deflation cycles, tilting, and faulting in the Yellowstone Caldera based on Yellowstone Lake shorelines: U.S. Geological Survey Open-File Report 2002-142, 30 p., https://doi.org/10.3133/ofr02142.","productDescription":"30 p.","costCenters":[],"links":[{"id":163483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3360,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0142/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683ada","contributors":{"authors":[{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":208457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cannon, Kenneth P.","contributorId":14472,"corporation":false,"usgs":false,"family":"Cannon","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":12462,"text":"U.S. Department of the Interior, National Park Service","active":true,"usgs":false}],"preferred":false,"id":208458,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, Grant A.","contributorId":26340,"corporation":false,"usgs":false,"family":"Meyer","given":"Grant","email":"","middleInitial":"A.","affiliations":[{"id":7164,"text":"Department of Biology, University of New Mexico, Albuquerque, NM 87131 USA","active":true,"usgs":false}],"preferred":false,"id":208459,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Trebesch, Matthew J.","contributorId":48227,"corporation":false,"usgs":true,"family":"Trebesch","given":"Matthew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":208460,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Watts, Raymond D.","contributorId":105713,"corporation":false,"usgs":true,"family":"Watts","given":"Raymond","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":208461,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":32364,"text":"ofr0261 - 2002 - Digital inventory of landslides and related deposits in Honduras triggered by Hurricane Mitch","interactions":[],"lastModifiedDate":"2017-03-07T13:26:24","indexId":"ofr0261","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-61","title":"Digital inventory of landslides and related deposits in Honduras triggered by Hurricane Mitch","docAbstract":"Intense rainfall from Hurricane Mitch from October 27-31, 1998, exceeded 900 mm in places in Honduras and triggered in excess of 500,000 landslides throughout the country. Landslides damaged an estimated 70% of the road network in Honduras based on estimates by the U. S Army Corps of Engineers. Numbers of fatalities due to landslides are not accurately known due to the fact that numerous small villages throughout Honduras lost residents to landslides without an official count being recorded. A conservative estimate would place the number at near 1,000. Debris flows accounted for over 95% of the landslides and ranged in thickness from 1 to 15 m. Flow path lengths of these failures ranged from several meters to 7.5 km. The highest concentrations of debris flows occurred in the mountains near the town of Choluteca where over 900 mm of rain fell in three days. Although landslides other than debris flows were few, several deep-seated landslides in the city of Tegucigalpa severely impacted people and property. The 'El Berrinche' rotational slump/earth flow of approximately six million cubic meters volume destroyed the entire neighborhood of Colonia Soto near the center of the city. The landslide also dammed the Rio Choluteca and created a lagoon behind the landslide dam, which immediately posed a health problem for the city, because raw, untreated sewage was emptying into the Rio Choluteca. Several areas of highly concentrated landslides have been responsible for much of the flooding problem\r\nas well. Huge sediment influxes from landslide source areas near La Ceiba, La Libertad, Marale, and in several arms of El Cajon Reservoir have reduced stream capacities to practically nothing and have exacerbated flooding conditions in even the moderate rainfall seasons since Hurricane Mitch. The ongoing hazard to communities from landslides triggered during Hurricane Mitch are being analyzed\r\nusing aerial photography taken by the U.S. Air Force and by supplemental photography taken by local contractors. Through the use of digital elevation models derived from 1:50,000-scale topographic maps and geologic maps, landslide susceptibility maps will be derived to aid land-use planning and relocation\r\nefforts.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr0261","usgsCitation":"Harp, E.L., Hagaman, K.W., Held, M.D., and McKenna, J., 2002, Digital inventory of landslides and related deposits in Honduras triggered by Hurricane Mitch: U.S. Geological Survey Open-File Report 2002-61, 15 p., https://doi.org/10.3133/ofr0261.","productDescription":"15 p.","costCenters":[],"links":[{"id":163930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3345,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0061/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65aa5e","contributors":{"authors":[{"text":"Harp, Edwin L. harp@usgs.gov","contributorId":1290,"corporation":false,"usgs":true,"family":"Harp","given":"Edwin","email":"harp@usgs.gov","middleInitial":"L.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":208421,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hagaman, Kirk W.","contributorId":13673,"corporation":false,"usgs":true,"family":"Hagaman","given":"Kirk","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":208423,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Held, Matthew D.","contributorId":37384,"corporation":false,"usgs":true,"family":"Held","given":"Matthew","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":208424,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKenna, Jonathan P.","contributorId":6915,"corporation":false,"usgs":true,"family":"McKenna","given":"Jonathan P.","affiliations":[],"preferred":false,"id":208422,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":32360,"text":"ofr0225 - 2002 - Digital archive; Report upon the Colorado River of the West explored in 1857 and 1858 by Lieutenant Joseph C. Ives, geological report with maps by John S. Newberry","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"ofr0225","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-25","title":"Digital archive; Report upon the Colorado River of the West explored in 1857 and 1858 by Lieutenant Joseph C. Ives, geological report with maps by John S. Newberry","language":"ENGLISH","doi":"10.3133/ofr0225","isbn":"0607984511","usgsCitation":"McKinney, K.C., 2002, Digital archive; Report upon the Colorado River of the West explored in 1857 and 1858 by Lieutenant Joseph C. Ives, geological report with maps by John S. Newberry (Version 1.0): U.S. Geological Survey Open-File Report 2002-25, 1 CD-ROM : ill., maps ; 4 3/4 in., https://doi.org/10.3133/ofr0225.","productDescription":"1 CD-ROM : ill., maps ; 4 3/4 in.","costCenters":[],"links":[{"id":161365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4617","contributors":{"authors":[{"text":"McKinney, Kevin C. kcmckinney@usgs.gov","contributorId":3406,"corporation":false,"usgs":true,"family":"McKinney","given":"Kevin","email":"kcmckinney@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":208411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32370,"text":"ofr02129 - 2002 - Leveling, EDM, and crack-monitoring networks in the Koa'e fault system, Kilauea Volcano, Hawai'i","interactions":[],"lastModifiedDate":"2012-02-02T00:09:22","indexId":"ofr02129","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-129","title":"Leveling, EDM, and crack-monitoring networks in the Koa'e fault system, Kilauea Volcano, Hawai'i","language":"ENGLISH","doi":"10.3133/ofr02129","usgsCitation":"Avery, V., Fiske, R., and Swanson, D., 2002, Leveling, EDM, and crack-monitoring networks in the Koa'e fault system, Kilauea Volcano, Hawai'i: U.S. Geological Survey Open-File Report 2002-129, iv, 44 leaves : ill., maps ; 28 cm. , https://doi.org/10.3133/ofr02129.","productDescription":"iv, 44 leaves : ill., maps ; 28 cm. ","costCenters":[],"links":[{"id":163402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0129/report-thumb.jpg"},{"id":60358,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5585","contributors":{"authors":[{"text":"Avery, V.F.","contributorId":51811,"corporation":false,"usgs":true,"family":"Avery","given":"V.F.","email":"","affiliations":[],"preferred":false,"id":208442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fiske, R.S.","contributorId":47783,"corporation":false,"usgs":true,"family":"Fiske","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":208441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swanson, Donald","contributorId":47430,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald","email":"","affiliations":[],"preferred":false,"id":208440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":32367,"text":"ofr02101 - 2002 - Helicopter electromagnetic data from Everglades National Park and surrounding areas, Florida: Collected 9-14 December 1994","interactions":[],"lastModifiedDate":"2025-04-18T15:36:17.301756","indexId":"ofr02101","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-101","title":"Helicopter electromagnetic data from Everglades National Park and surrounding areas, Florida: Collected 9-14 December 1994","docAbstract":"This report describes helicopter electromagnetic (HEM) data that were collected over portion of Everglades National Park and surrounding areas in south Florida. The survey was flown 9-14 December 1994. The original data set processed by the contractor, Dighem, are provided as an ASCII, xyz flight-line file. Apparent resistivity grids of the generated from the original data set and JPEG images of these grids are also provided. The data have been corrected by the U.S. Geological Survey to remove the effects of calibration errors and bird-height uncertainty. The corrected data set is included in this report as flight-line data only.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr02101","usgsCitation":"Helicopter electromagnetic data from Everglades National Park and surrounding areas, Florida: Collected 9-14 December 1994; 2002; OFR; 2002-101; Fitterman, David V.; Deszcz-Pan, Maria","productDescription":"HTML Document: 1 CD-ROM","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":3355,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-101/index.html","linkFileType":{"id":5,"text":"html"}},{"id":163853,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-101/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades National Park and surrounding areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.09479583359331,\n 26.643885296477606\n ],\n [\n -82.09479583359331,\n 24.327972112803963\n ],\n [\n -80.11513304200784,\n 24.327972112803963\n ],\n [\n -80.11513304200784,\n 26.643885296477606\n ],\n [\n -82.09479583359331,\n 26.643885296477606\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","contact":"

Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314

Contact Pubs Warehouse

","publishedDate":"2002-05-01","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635dce","contributors":{"authors":[{"text":"Fitterman, David V. dfitterman@usgs.gov","contributorId":1106,"corporation":false,"usgs":true,"family":"Fitterman","given":"David","email":"dfitterman@usgs.gov","middleInitial":"V.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":208429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Deszcz-Pan, Maria 0000-0002-6298-5314 maryla@usgs.gov","orcid":"https://orcid.org/0000-0002-6298-5314","contributorId":1263,"corporation":false,"usgs":true,"family":"Deszcz-Pan","given":"Maria","email":"maryla@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":208430,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32342,"text":"ofr98799 - 2002 - Composition of crude oil and natural gas produced from 10 wells in the Lower Silurian \"Clinton\" Sands, Trumbull County, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"ofr98799","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"98-799","title":"Composition of crude oil and natural gas produced from 10 wells in the Lower Silurian \"Clinton\" Sands, Trumbull County, Ohio","language":"ENGLISH","doi":"10.3133/ofr98799","usgsCitation":"Burruss, R.C., and Ryder, R., 2002, Composition of crude oil and natural gas produced from 10 wells in the Lower Silurian \"Clinton\" Sands, Trumbull County, Ohio: U.S. Geological Survey Open-File Report 98-799, iv, 50 leaves : ill., maps ; 28 cm., https://doi.org/10.3133/ofr98799.","productDescription":"iv, 50 leaves : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":161187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1998/0799/report-thumb.jpg"},{"id":60353,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0799/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a80f0","contributors":{"authors":[{"text":"Burruss, Robert Carlton","contributorId":40253,"corporation":false,"usgs":true,"family":"Burruss","given":"Robert","email":"","middleInitial":"Carlton","affiliations":[],"preferred":false,"id":208312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryder, Robert T.","contributorId":77918,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert T.","affiliations":[],"preferred":false,"id":208313,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":32362,"text":"ofr0246 - 2002 - Large-scale cycles of Holocene deposition and erosion at the entrance to Willapa Bay, Washington: Implications for future land loss and coastal change","interactions":[],"lastModifiedDate":"2022-08-09T20:31:21.664571","indexId":"ofr0246","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-46","title":"Large-scale cycles of Holocene deposition and erosion at the entrance to Willapa Bay, Washington: Implications for future land loss and coastal change","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr0246","usgsCitation":"Morton, R., Purcell, N.A., and Peterson, R.L., 2002, Large-scale cycles of Holocene deposition and erosion at the entrance to Willapa Bay, Washington: Implications for future land loss and coastal change: U.S. Geological Survey Open-File Report 2002-46, iv, 96 p., https://doi.org/10.3133/ofr0246.","productDescription":"iv, 96 p.","costCenters":[],"links":[{"id":405049,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_51452.htm","linkFileType":{"id":5,"text":"html"}},{"id":60356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2002/0046/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2002/0046/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Willapa Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.08782958984375,\n 46.66734468444288\n ],\n [\n -123.96286010742188,\n 46.66734468444288\n ],\n [\n -123.96286010742188,\n 46.73986059969267\n ],\n [\n -124.08782958984375,\n 46.73986059969267\n ],\n [\n -124.08782958984375,\n 46.66734468444288\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8f83","contributors":{"authors":[{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":208416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purcell, Noreen A.","contributorId":92714,"corporation":false,"usgs":true,"family":"Purcell","given":"Noreen","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":208417,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peterson, Russell L.","contributorId":55045,"corporation":false,"usgs":true,"family":"Peterson","given":"Russell","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208415,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":32366,"text":"ofr0292 - 2002 - Technical guidelines for the implementation of the Advanced National Seismic System","interactions":[],"lastModifiedDate":"2017-03-07T13:45:17","indexId":"ofr0292","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-92","title":"Technical guidelines for the implementation of the Advanced National Seismic System","docAbstract":"

The Advanced National Seismic System (ANSS) is a major national initiative led by the US Geological Survey that serves the needs of the earthquake monitoring, engineering, and research communities as well as national, state, and local governments, emergency response organizations, and the general public. Legislation authorizing the ANSS was passed in 2000, and low levels of funding for planning and initial purchases of new seismic instrumentation have been appropriated beginning in FY2000. When fully operational, the ANSS will be an advanced monitoring system (modern digital seismographs and accelerographs, communications networks, data collection and processing centers, and well-trained personnel) distributed across the United States that operates with high performance standards, gathers critical technical data, and effectively provides timely and reliable earthquake products, information, and services to meet the Nation’s needs. The ANSS will automatically broadcast timely and authoritative products describing the occurrence of earthquakes, earthquake source properties, the distribution of ground shaking, and, where feasible, broadcast early warnings and alerts for the onset of strong ground shaking. Most importantly, the ANSS will provide earthquake data, derived products, and information to the public, emergency responders, officials, engineers, educators, researchers, and other ANSS partners rapidly and in forms that are useful for their needs.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr0292","usgsCitation":"Committee, A.T., 2002, Technical guidelines for the implementation of the Advanced National Seismic System: U.S. Geological Survey Open-File Report 2002-92, 92 p., https://doi.org/10.3133/ofr0292.","productDescription":"92 p.","costCenters":[],"links":[{"id":163852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3354,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0092/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6864c4","contributors":{"authors":[{"text":"Committee, ANSS Technical Integration","contributorId":24826,"corporation":false,"usgs":true,"family":"Committee","given":"ANSS","email":"","middleInitial":"Technical Integration","affiliations":[],"preferred":false,"id":208428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32363,"text":"ofr0249 - 2002 - Aeromagnetic survey of Medina and Uvalde counties, Texas","interactions":[],"lastModifiedDate":"2025-05-14T18:58:14.876635","indexId":"ofr0249","displayToPublicDate":"2002-05-01T00:00:00","publicationYear":"2002","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2002-49","title":"Aeromagnetic survey of Medina and Uvalde counties, Texas","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr0249","usgsCitation":"Smith, D.V., Smith, B.D., and Hill, P.L., 2002, Aeromagnetic survey of Medina and Uvalde counties, Texas: U.S. Geological Survey Open-File Report 2002-49, https://doi.org/10.3133/ofr0249.","costCenters":[],"links":[{"id":163929,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":3344,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2002/ofr-02-0049/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","county":"Medina, Uvalde","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d38","contributors":{"authors":[{"text":"Smith, David V. 0000-0003-0426-4401 dvsmith@usgs.gov","orcid":"https://orcid.org/0000-0003-0426-4401","contributorId":1306,"corporation":false,"usgs":true,"family":"Smith","given":"David","email":"dvsmith@usgs.gov","middleInitial":"V.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":208419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Bruce D. 0000-0002-1643-2997 bsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-1643-2997","contributorId":845,"corporation":false,"usgs":true,"family":"Smith","given":"Bruce","email":"bsmith@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":208418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hill, Pat L.","contributorId":35784,"corporation":false,"usgs":true,"family":"Hill","given":"Pat","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":208420,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}