Two vastly different phenomena, impact and salt diapirism, have been proposed for the origin of Upheaval Dome, southeast Utah. Detailed geologic mapping, seismic refraction data, and the presence of shock metamorphosed rocks indicate that the dome originated by collapse of a transient cavity formed by impact. Evidence is: (1) the occurrence of a lag deposit of rare impactites, (2) fan-tailed fracture surfaces (shatter surfaces) and rare shatter cones are present near the center of the structure, (3) the top of the underlying salt horizon is at least 500 m below the surface at the center of the dome and there are no exposures of salt or associated rocks of the Paradox Formation in the dome to support the possibility that a salt diapir has ascended through it, (4) sedimentary strata in the center of the structure are pervasively imbricated by top-toward-the-center thrust faulting and are complexly folded as well, (5) top-toward-the-center normal faults are found at the perimeter of the structure, and 6) clastic dikes are widespread.
We show that the dome formed mainly by centerward motion of rock units along listric faults. Outcrop-scale folding and upturning of beds, especially common in the center, are largely a consequence of this motion. We have also detected some centerward motion of fault-bounded wedges resulting from displacements on subhorizontal faults that conjoin and die out within horizontal bedding near the perimeter of the structure. The observed deformation corresponds to the central uplift and the encircling ring structural depression seen in complex impact craters.
","language":"English","publisher":"Brigham Young University","usgsCitation":"Kriens, B.J., Shoemaker, E.M., and Herkenhoff, K.E., 1997, Structure and kinematics of a complex impact crater, Upheaval Dome, southeast Utah: Brigham Young University Geology Studies, v. 42, no. 2, p. 19-31.","productDescription":"13 p.","startPage":"19","endPage":"31","costCenters":[],"links":[{"id":394539,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":394538,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://geology.byu.edu/free-articles"}],"country":"United States","state":"Utah","otherGeospatial":"Canyonlands National Park, Upheaval Dome","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.93280410766602,\n 38.43308520470687\n ],\n [\n -109.9317741394043,\n 38.43301797052346\n ],\n [\n -109.92958545684814,\n 38.432480094802344\n ],\n [\n -109.92851257324219,\n 38.43274903316375\n ],\n [\n -109.92666721343993,\n 38.43227839037393\n ],\n [\n -109.92542266845703,\n 38.43301797052346\n ],\n [\n -109.92512226104736,\n 38.43372392632674\n ],\n [\n -109.9243927001953,\n 38.434766038944815\n ],\n [\n -109.9243927001953,\n 38.43527028158593\n ],\n [\n -109.9246072769165,\n 38.43570728902624\n ],\n [\n -109.92456436157227,\n 38.43654768051518\n ],\n [\n -109.92374897003172,\n 38.4371863715042\n ],\n [\n -109.92289066314697,\n 38.43896795334589\n ],\n [\n -109.92301940917969,\n 38.439438552529154\n ],\n [\n -109.92546558380127,\n 38.44108562551085\n ],\n [\n -109.92791175842285,\n 38.440951171982306\n ],\n [\n -109.92924213409424,\n 38.44031251430161\n ],\n [\n -109.92971420288086,\n 38.44014444555175\n ],\n [\n -109.93065834045409,\n 38.44088394512412\n ],\n [\n -109.93198871612549,\n 38.44088394512412\n ],\n [\n -109.93361949920653,\n 38.44058142348745\n ],\n [\n -109.93430614471436,\n 38.440278900582946\n ],\n [\n -109.93340492248535,\n 38.439472166639135\n ],\n [\n -109.93331909179688,\n 38.43883349587289\n ],\n [\n -109.93456363677977,\n 38.43822843414527\n ],\n [\n -109.93387699127197,\n 38.43732083204505\n ],\n [\n -109.93452072143555,\n 38.43614429382134\n ],\n [\n -109.93396282196045,\n 38.43570728902624\n ],\n [\n -109.93422031402588,\n 38.435068584952084\n ],\n [\n -109.93361949920653,\n 38.43406009333086\n ],\n [\n -109.93280410766602,\n 38.43308520470687\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"42","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kriens, Bryan J.","contributorId":210961,"corporation":false,"usgs":false,"family":"Kriens","given":"Bryan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":831169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":831170,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herkenhoff, Kenneth E. 0000-0002-3153-6663 kherkenhoff@usgs.gov","orcid":"https://orcid.org/0000-0002-3153-6663","contributorId":2275,"corporation":false,"usgs":true,"family":"Herkenhoff","given":"Kenneth","email":"kherkenhoff@usgs.gov","middleInitial":"E.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":831171,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70093960,"text":"70093960 - 1997 - Design and implementation of the National Water-Quality Assessment Program: a United States example: understanding the limitations of using compliance-monitoring data to assess the water quality of a large river basin","interactions":[],"lastModifiedDate":"2014-02-14T14:26:00","indexId":"70093960","displayToPublicDate":"1997-01-01T14:15:00","publicationYear":"1997","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Design and implementation of the National Water-Quality Assessment Program: a United States example: understanding the limitations of using compliance-monitoring data to assess the water quality of a large river basin","docAbstract":"In the 1980s it was determined that existing ambient and compliance-monitoring data could not satisfactorily evaluate the results of hundreds of billions of dollars spent for water-pollution abatement in the United States. At the request of the US Congress, a new programme, the National Water-Quality Assessment, was designed and implemented by government agency, the US Geological Survey (USGS). The Assessment has reported status and trends in surface- and ground-water quality at national, regional, and local scales since 1991. The legislative basis for US monitoring and data-sharing policies are identified as well as the successive phases of the design and implementation of the USGS Assessment. Application to the Danube Basin is suggested. Much of the water-quality monitoring conducted in the United States is designed to comply with Federal and State laws mandated primarily by the Clean Water Act of 1987 and the Safe Drinking Water Act of 1986. Monitoring programs generally focus on rivers upstream and downstream of point-source discharges and at water-supply intakes. Few data are available for aquifer systems, and chemical analyses are often limited to those constituents required by law. In most cases, the majority of the available chemical and streamflow data have provided the information necessary to meet the objectives of the compliance-monitoring programs, but do not necessarily provide the information requires for basin-wide assessments of the water quality at the local, regional, or national scale.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Protecting Danube River Basin resources: ensuring access to water quality data and information","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Kluwer Academic Publishers","publisherLocation":"Netherlands","isbn":"0792343824","usgsCitation":"Wangsness, D.J., 1997, Design and implementation of the National Water-Quality Assessment Program: a United States example: understanding the limitations of using compliance-monitoring data to assess the water quality of a large river basin, chap. of Protecting Danube River Basin resources: ensuring access to water quality data and information, v. 24, p. 89-103.","productDescription":"15 p.","startPage":"89","endPage":"103","numberOfPages":"15","costCenters":[],"links":[{"id":282430,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5453e4b0b290850f5a96","contributors":{"authors":[{"text":"Wangsness, David J.","contributorId":81475,"corporation":false,"usgs":true,"family":"Wangsness","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":490410,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70226704,"text":"70226704 - 1997 - Two new species of Scolecopteris (Marattiales), sources of Torispora securis Balme and Thymospora thiessenii (Kosanke) Wilson et Venkatachala","interactions":[],"lastModifiedDate":"2021-12-06T20:06:50.871376","indexId":"70226704","displayToPublicDate":"1997-01-01T14:00:18","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3275,"text":"Review of Palaeobotany and Palynology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Two new species of Scolecopteris (Marattiales), sources of Torispora securis Balme and Thymospora thiessenii (Kosanke) Wilson et Venkatachala","title":"Two new species of Scolecopteris (Marattiales), sources of Torispora securis Balme and Thymospora thiessenii (Kosanke) Wilson et Venkatachala","docAbstract":"Two biostratigraphically significant miospore species, Thymospora thiessenii and Torispora securis, were isolated from marattialean synangia preserved in coal-ball permineralizations from Pennsylvanian strata of the Illinois Basin and Western Interior coal region. Synangia containing Thymospora thiessenii were recovered from the Missourian Parker Coal Member (Patoka Formation) of Indiana and are described here as Scolecopteris parkerensis Lesnikowska et Willard, sp. nov. The uniformly thin outer sporangial walls and broadly enclosing, hirsute pinnule margins place the species in the Latifolia group sensu Millay (1979). It is distinguished from the other species of the group by the size of the synangia, by the size and shape of the pinnules, by features of the pedicel and by the spores. Coal balls from the Desmoinesian Cliffland Coal Member (Kalo Formation) of Iowa yielded synangia producing two different spore types: a peripheral layer of spores with a distinct apical crassitude (Torispora securis) and interior spores assignable to Laevigatosporites globosus. The crassitude of Torispora is shown to be a structure distinct from the main spore body but is enclosed with it by the exine. The fructifications are described as Scolecopteris dispora Lesnikowska et Willard, sp. nov., which belongs to the Oliveri group sensu Millay (1979) on the basis of the uniformly thick outer sporangial wall and downturned, hairless pinnule margins. It is distinguished from the other members of the group by the large size of the synangia, the uniform histology of the outer sporangial walls, features of the pedicel, and by the spores. This is the first reported association of either of these spores with permineralized fructifications from coal.
No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The nature of magmatism in the Appalachian orogen","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-1191-6.181","usgsCitation":"Higgins, M.W., Arth, J.G., Wooden, J., Crawford, T.J., Stern, T.W., and Crawford, R., 1997, Age and origin of the Austell Gneiss, western Georgia Piedmont-Blue Ridge, and its bearing on the ages of orogenic events in the Southern Appalachians, chap. of The nature of magmatism in the Appalachian orogen, v. 191, p. 181-192, https://doi.org/10.1130/0-8137-1191-6.181.","productDescription":"12 p.","startPage":"181","endPage":"192","costCenters":[],"links":[{"id":418717,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"western Georgia Piedmont–Blue Ridge,","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -84.15615917693813,\n 34.87622628806666\n ],\n [\n -85.31372314978024,\n 34.87622628806666\n ],\n [\n -85.31372314978024,\n 34.15055868375474\n ],\n [\n -84.15615917693813,\n 34.15055868375474\n ],\n [\n -84.15615917693813,\n 34.87622628806666\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"191","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Sinha, A. Krishna","contributorId":32998,"corporation":false,"usgs":true,"family":"Sinha","given":"A.","email":"","middleInitial":"Krishna","affiliations":[],"preferred":false,"id":876996,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Whalen, Joseph W.","contributorId":315871,"corporation":false,"usgs":false,"family":"Whalen","given":"Joseph","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":876997,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Hogan, John P.","contributorId":172153,"corporation":false,"usgs":false,"family":"Hogan","given":"John","email":"","middleInitial":"P.","affiliations":[{"id":26996,"text":"Missouri University of Science & Technology","active":true,"usgs":false}],"preferred":false,"id":876998,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Higgins, Michael W.","contributorId":12459,"corporation":false,"usgs":true,"family":"Higgins","given":"Michael","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":876990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arth, Joseph G.","contributorId":104546,"corporation":false,"usgs":true,"family":"Arth","given":"Joseph","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":876991,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wooden, Joseph L.","contributorId":32209,"corporation":false,"usgs":true,"family":"Wooden","given":"Joseph L.","affiliations":[],"preferred":false,"id":876992,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crawford, Thomas J.","contributorId":73640,"corporation":false,"usgs":true,"family":"Crawford","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":876993,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stern, Thomas W.","contributorId":271088,"corporation":false,"usgs":false,"family":"Stern","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":876994,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Crawford, Ralph","contributorId":219872,"corporation":false,"usgs":false,"family":"Crawford","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":876995,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":5485,"text":"5485 - 1997 - Natural disasters: forecasting economic and life losses","interactions":[],"lastModifiedDate":"2014-07-16T12:02:15","indexId":"5485","displayToPublicDate":"1997-01-01T11:50:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":359,"text":"Fact Sheet","active":false,"publicationSubtype":{"id":6}},"title":"Natural disasters: forecasting economic and life losses","docAbstract":"Events such as hurricanes, earthquakes, floods, tsunamis, volcanic eruptions, and tornadoes are natural disasters because they negatively impact society, and so they must be measured and understood in human-related terms. At the U.S. Geological Survey, we have developed a new method to examine fatality and dollar-loss data, and to make probabilistic estimates of the frequency and magnitude of future events. This information is vital to large sectors of society including disaster relief agencies and insurance companies.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/5485","usgsCitation":"Nishenko, S., and Barton, C.C., 1997, Natural disasters: forecasting economic and life losses: Fact Sheet, HTML Document, https://doi.org/10.3133/5485.","productDescription":"HTML Document","onlineOnly":"Y","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":290276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":643,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/natural-disasters/"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f05e4b0194841642479","contributors":{"authors":[{"text":"Nishenko, Stuart P.","contributorId":82219,"corporation":false,"usgs":true,"family":"Nishenko","given":"Stuart P.","affiliations":[],"preferred":false,"id":151070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barton, Christopher C.","contributorId":61901,"corporation":false,"usgs":true,"family":"Barton","given":"Christopher","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":151069,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70094722,"text":"70094722 - 1997 - Tests of ground-penetrating radar and induced polarization for mapping fluvial mine tailings on the floor of the Couer d'Alene River, Idaho","interactions":[],"lastModifiedDate":"2014-02-24T11:42:44","indexId":"70094722","displayToPublicDate":"1997-01-01T11:35:00","publicationYear":"1997","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Tests of ground-penetrating radar and induced polarization for mapping fluvial mine tailings on the floor of the Couer d'Alene River, Idaho","docAbstract":"In order to investigate sequences of toxic mine tailings that have settled in the bed of the Coeur d'Alene River, Idaho, (see figure 1) we improvised ways to make geophysical measurements on the river floor. To make ground penetrating radar (GPR) profiles, we mounted borehole antennas on a skid that was towed along the river bottom. To make induced polarization (IP) profiles, we devised a bottom streamer from a garden hose, lead strips, PVC standoffs, and insulated wire. Each approach worked and provided uniquely different information about the buried toxic sediments. GPR showed shallow stratigraphy, but did not directly detect the presence of contaminating metals. IP showed a zone of high chargeability that is probably due to pockets of relatively higher metal content. Neither method was able to define the base of the fluvial tailings section, at least in part because the IP streamer was deliberately designed to sample only the top three meters of sediments to maximize horizontal resolution.","largerWorkTitle":"Proceedings of the Symposium on the Application of geophysics to engineering and environmental problems: SAGEEP '97","conferenceTitle":"Symposium on the Application of geophysics to engineering and environmental problems: SAGEEP '97","conferenceDate":"1997-03-25T00:00:00","conferenceLocation":"Reno, NV","language":"English","publisher":"Society of Engineering & Mineral Exploration Geophysicists","publisherLocation":"Golden, CO","usgsCitation":"Campbell, D.L., Wynn, J.C., Box, S.E., Bookstrom, A.A., and Horton, R., 1997, Tests of ground-penetrating radar and induced polarization for mapping fluvial mine tailings on the floor of the Couer d'Alene River, Idaho, p. 81-87.","productDescription":"p. 81-87","numberOfPages":"7","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":282674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Couer D'alene River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.800467,47.457941 ], [ -116.800467,47.961781 ], [ -115.925418,47.961781 ], [ -115.925418,47.457941 ], [ -116.800467,47.457941 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd76a5e4b0b2908510b0a8","contributors":{"authors":[{"text":"Campbell, David L.","contributorId":95447,"corporation":false,"usgs":true,"family":"Campbell","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":490841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wynn, Jefferey C.","contributorId":19076,"corporation":false,"usgs":true,"family":"Wynn","given":"Jefferey","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":490840,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Box, Stephen E. 0000-0002-5268-8375 sbox@usgs.gov","orcid":"https://orcid.org/0000-0002-5268-8375","contributorId":1843,"corporation":false,"usgs":true,"family":"Box","given":"Stephen","email":"sbox@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":490839,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bookstrom, Arthur A. 0000-0003-1336-3364 abookstrom@usgs.gov","orcid":"https://orcid.org/0000-0003-1336-3364","contributorId":1542,"corporation":false,"usgs":true,"family":"Bookstrom","given":"Arthur","email":"abookstrom@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":5056,"text":"Office of the AD Energy and Minerals, and Environmental Health","active":true,"usgs":true}],"preferred":true,"id":490838,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Horton, Robert 0000-0001-5578-3733 rhorton@usgs.gov","orcid":"https://orcid.org/0000-0001-5578-3733","contributorId":612,"corporation":false,"usgs":true,"family":"Horton","given":"Robert","email":"rhorton@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":490837,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70074659,"text":"70074659 - 1997 - Interpretive geologic bedrock map of the Tanana B-1 Quadrangle, Central Alaska","interactions":[],"lastModifiedDate":"2014-01-31T11:43:21","indexId":"70074659","displayToPublicDate":"1997-01-01T11:33:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesNumber":"97-15B","title":"Interpretive geologic bedrock map of the Tanana B-1 Quadrangle, Central Alaska","docAbstract":"This report provides detailed (1:63,360-scale) mapping of the Tanana B-1 Quadrangle (250 square miles; equivalent to four 7.5 minute quadrangles). The area is part of the Manley Hot Springs-Tofty mining districts and adjacent to the Rampart mining district to the north of the Tanana A-1 and A-2 Quadrangles. This report includes detailed bedrock, structural, stratigraphic, and geochronologic data. Based on the resulting geologic maps, field investigations, and laboratory materials analyses, the project has also generated derivative maps of geologic construction materials and geologic hazards.","language":"English","publisher":"Alaska Division of Geological & Geophysical Surveys","usgsCitation":"Reifenstuh, R.R., Dover, J.H., Newberry, R.J., Calutice, K.H., Liss, S.A., Blodgett, R., Budtzen, T.K., and Weber, F.R., 1997, Interpretive geologic bedrock map of the Tanana B-1 Quadrangle, Central Alaska, Report: ii, 15 p.; 1 Plate: 39.00 x 34.44 inches.","productDescription":"Report: ii, 15 p.; 1 Plate: 39.00 x 34.44 inches","numberOfPages":"17","costCenters":[],"links":[{"id":281820,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"scale":"63360","projection":"Universal Transverse Mercator Projection","datum":"1927 North American Datum","country":"United States","state":"Alaska","otherGeospatial":"Tanana B-1 Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.5,85.25 ], [ -150.5,85.5 ], [ -150.0,85.5 ], [ -150.0,85.25 ], [ -150.5,85.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd62ede4b0b290850fe7d9","contributors":{"authors":[{"text":"Reifenstuh, Rocky R.","contributorId":74294,"corporation":false,"usgs":true,"family":"Reifenstuh","given":"Rocky","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":489713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dover, James H.","contributorId":43382,"corporation":false,"usgs":true,"family":"Dover","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":489711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Newberry, Rainer J.","contributorId":68645,"corporation":false,"usgs":true,"family":"Newberry","given":"Rainer","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":489712,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Calutice, Karen H.","contributorId":42867,"corporation":false,"usgs":true,"family":"Calutice","given":"Karen","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":489710,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Liss, Shirley A.","contributorId":90206,"corporation":false,"usgs":true,"family":"Liss","given":"Shirley","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":489716,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Blodgett, Robert B.","contributorId":89612,"corporation":false,"usgs":true,"family":"Blodgett","given":"Robert B.","affiliations":[],"preferred":false,"id":489715,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Budtzen, Thomas K.","contributorId":83021,"corporation":false,"usgs":true,"family":"Budtzen","given":"Thomas","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":489714,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Weber, Florence R.","contributorId":17621,"corporation":false,"usgs":true,"family":"Weber","given":"Florence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":489709,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":61,"text":"61 - 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Examples of applications of this method to geologic studies are provided.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70220360","usgsCitation":"Dulong, F.T., and Jackson, J.C., 1997, X-ray powder diffraction: Information Handout, 2 p., https://doi.org/10.3133/70220360.","productDescription":"2 p.","costCenters":[],"links":[{"id":385497,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":385496,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/info/diffraction/xrd.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":385495,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/info/diffraction/html/","linkFileType":{"id":5,"text":"html"}},{"id":385494,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/info/diffraction/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dulong, Frank T. 0000-0001-7388-647X fdulong@usgs.gov","orcid":"https://orcid.org/0000-0001-7388-647X","contributorId":650,"corporation":false,"usgs":true,"family":"Dulong","given":"Frank","email":"fdulong@usgs.gov","middleInitial":"T.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":815260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, John C. jjackson@usgs.gov","contributorId":2652,"corporation":false,"usgs":true,"family":"Jackson","given":"John","email":"jjackson@usgs.gov","middleInitial":"C.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":815261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70231436,"text":"70231436 - 1997 - Age and correlation of tephra layers, position of the Matuyama-Brunhes chron boundary, and effects of Bishop Ash eruption on Owens Lake, as determined from drill hole OL-92, Southeast California","interactions":[{"subject":{"id":70231436,"text":"70231436 - 1997 - Age and correlation of tephra layers, position of the Matuyama-Brunhes chron boundary, and effects of Bishop Ash eruption on Owens Lake, as determined from drill hole OL-92, Southeast California","indexId":"70231436","publicationYear":"1997","noYear":false,"title":"Age and correlation of tephra layers, position of the Matuyama-Brunhes chron boundary, and effects of Bishop Ash eruption on Owens Lake, as determined from drill hole OL-92, Southeast California"},"predicate":"IS_PART_OF","object":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"id":1}],"isPartOf":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"lastModifiedDate":"2022-05-10T16:30:17.820787","indexId":"70231436","displayToPublicDate":"1997-01-01T11:25:47","publicationYear":"1997","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Age and correlation of tephra layers, position of the Matuyama-Brunhes chron boundary, and effects of Bishop Ash eruption on Owens Lake, as determined from drill hole OL-92, Southeast California","docAbstract":"Tephra layers in the ~323-m-deep Owens lake drill hole OL-92 correlate to tephra layers that have been identified and dated elsewhere in the western United States. Tephra layers identified are the Bishop ash bed (758 ka) at 309.2–298.6 m; the Dibekulewe (ash) bed (ca. 470 ka to ca. 610 ka) at ~224 m; and one of several ash beds in Walker Lake (ca. 60 ka to ca. 80 ka) at ~50.7 m. Other tephra layers, the ages of which are poorly constrained, have also been identified. Age constraints from a sedimentation-rate curve based on dry bulk density and independently derived magnetostratigraphy provide new age constraints to the undated or poorly dated tephra layers: ca. 740 ka for the ash of Thermal Canyon, and ca. 510 ka for the Dibekulewe (ash) bed.
Bishop tephra fell into a deep Owens Lake, but the lake shallowed as ash was rapidly reworked by wind and water within the Owens Lake basin. The shallowing of the lake was the result in part to filling with the large volume of ash that was deposited in the basin and then reworked into the lake, but the filling was also an effect of the onset of a moderately warm interstadial period of hemispheric or global extent corresponding to oxygen-isotope stage 19. The lake deepened again as the last several meters of the 10-m-thick, composite ash bed were deposited in the lake. Despite its great thickness, reworking of the light ash must have been rapid.
The position of the Matuyama-Brunhes paleomagnetic boundary is estimated to be between 311.4 m and 314.8 m, and most likely between 311.4 m and 312.9 m, in the core, based on (1) the pattern of magnetic inclinations in the Owens Lake core as compared with those at other sites in the region; (2) estimates of the time elapsed between the magnetic reversal and the deposition of the Bishop ash bed; and (3) the probable range of sediment-deposition rates in Owens Lake during this time.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2317-5.79","usgsCitation":"Sarna-Wojcicki, A.M., Meyer, C.E., and Wan, E., 1997, Age and correlation of tephra layers, position of the Matuyama-Brunhes chron boundary, and effects of Bishop Ash eruption on Owens Lake, as determined from drill hole OL-92, Southeast California, chap. of An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California, v. 317, p. 79-90, https://doi.org/10.1130/0-8137-2317-5.79.","productDescription":"12 p.","startPage":"79","endPage":"90","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":400429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Owens Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.15246582031249,\n 36.27085020723902\n ],\n [\n -117.81463623046875,\n 36.27085020723902\n ],\n [\n -117.81463623046875,\n 36.641977814705946\n ],\n [\n -118.15246582031249,\n 36.641977814705946\n ],\n [\n -118.15246582031249,\n 36.27085020723902\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"317","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":842601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, Charles E.","contributorId":84007,"corporation":false,"usgs":true,"family":"Meyer","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":842602,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wan, Elmira 0000-0002-9255-112X ewan@usgs.gov","orcid":"https://orcid.org/0000-0002-9255-112X","contributorId":3434,"corporation":false,"usgs":true,"family":"Wan","given":"Elmira","email":"ewan@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":842603,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70231435,"text":"70231435 - 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1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"id":2},{"subject":{"id":70231423,"text":"70231423 - 1997 - Responses of sediment geochemistry to climate change in Owens Lake sediment: An 800-k.y. record of saline/fresh cycles in core OL-92","indexId":"70231423","publicationYear":"1997","noYear":false,"title":"Responses of sediment geochemistry to climate change in Owens Lake sediment: An 800-k.y. record of saline/fresh cycles in core OL-92"},"predicate":"IS_PART_OF","object":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"id":3},{"subject":{"id":70231427,"text":"70231427 - 1997 - A time-depth scale for Owens Lake sediments of core OL-92; radiocarbon dates and constant mass-accumulation rate","indexId":"70231427","publicationYear":"1997","noYear":false,"title":"A time-depth scale for Owens Lake sediments of core OL-92; radiocarbon dates and constant mass-accumulation rate"},"predicate":"IS_PART_OF","object":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"id":4},{"subject":{"id":70231429,"text":"70231429 - 1997 - A diatom-based paleohydrologic record of climate change for the past 800 k.y. from Owens Lake, California","indexId":"70231429","publicationYear":"1997","noYear":false,"title":"A diatom-based paleohydrologic record of climate change for the past 800 k.y. from Owens Lake, California"},"predicate":"IS_PART_OF","object":{"id":70231435,"text":"70231435 - 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Jr.","contributorId":257913,"corporation":false,"usgs":true,"family":"Briskey","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":815254,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schruben, Paul G.","contributorId":38974,"corporation":false,"usgs":true,"family":"Schruben","given":"Paul","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":815255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70231434,"text":"70231434 - 1997 - Synthesis of the paleoclimatic record from Owens Lake core OL-92","interactions":[{"subject":{"id":70231434,"text":"70231434 - 1997 - Synthesis of the paleoclimatic record from Owens Lake core OL-92","indexId":"70231434","publicationYear":"1997","noYear":false,"title":"Synthesis of the paleoclimatic record from Owens Lake core OL-92"},"predicate":"IS_PART_OF","object":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"id":1}],"isPartOf":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"lastModifiedDate":"2022-05-10T16:18:53.238498","indexId":"70231434","displayToPublicDate":"1997-01-01T11:08:00","publicationYear":"1997","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Synthesis of the paleoclimatic record from Owens Lake core OL-92","docAbstract":"During much of the late Quaternary, Owens Lake overflowed into one or more of four successively lower-elevation basins. Most of the water came from the high, eastern slopes of the southern Sierra Nevada, and changes in the volumes of that water reflect a dominant climatic cycle of ~100 k.y.
Variations in the inflow to, and outflow from, Owens Lake since ca. 800 ka left biological, chemical, mineralogical, and geophysical evidence in the sediments of those changes. Biological evidence includes fossil ostracodes, diatoms, fish, and mollusks (and δ18O data from their shells) which indicate fresh or brackish lake water on the basis of their modern habitats. Fossil pollens indicate ~20 regional vegetation cycles during the same period. Chemical evidence of high inflow and, commonly, outflow volumes is provided by the low inorganic- and organic-C content of some sediments, reflecting short lake-water residence times; long residence times produced higher and more variable quantities of these components. Mineralogical variations in illite/smectite ratios indicate changes in weathering processes and glacial comminution. High magnetic susceptibility correlates with other criteria that indicate high runoff.
Between 810 ka and 645 ka, Owens Lake was fresh, several meters deep, and depositing silt with a few beds of sand; it supported a flora and fauna now found in fresh, sometimes very cool, waters. (Note that most geologic ages describing the OL-92 chronology have been rounded to the nearest 5 or 10 ka.) A shallow-but-freshwater lake may have been the result of accelerated sedimentation during an earlier (>800 ka) glaciation in the Sierra Nevada, choking the basin with sediment nearly to its spillway level. Between 645 ka and 450 ka, the lake was probably even shallower, depositing beds of coarse to fine sand, but overflowing periodically allowing its water to remain fresh. Between 450 ka and 5 ka, Owens Lake was mostly deep, alternating between spilling and being closed part of the time. It deposited silt and clay on its floor, yet underwent detectable variations in salinity caused by climate changes; this part of the record is the most easily interpreted and constitutes the main basis for comparing this paleoclimatic record with other long records. From 5 ka to A.D. 1913, when the Owens River was diverted into an aqueduct, Owens Lake was shallow (~2 m to ~15 m), moderately saline (~5% to <15% salts), and depositing oolites. After 1913, the lake desiccated.
Comparison of the Owens Lake water-depth record with that of Searles Lake, two-basins downstream during much of late Pleistocene time, shows that they underwent similar responses to climate, but sedimentation changes documenting those responses commenced thousands of years apart, apparently because changes in precipitation volumes occurred gradually. Owens Lake, at the base of high mountains, was the first to reflect increasing amounts of regional precipitation; Searles, in a more arid environment, was the first to reflect decreasing amounts of precipitation.
Devils Hole, 150 km east of Owens Lake, has a well dated isotopic-temperature record that resembles the Owens Lake-depth record. Marine records of Pleistocene glacial fluctuations, which measure high-latitude ice-sheet volumes and thus both precipitation and temperature at those latitudes, also resemble the Owens Lake history. There are, however, differences between the ages of the maxima and minima of climatic events as reconstructed from the Owens Lake core and similar-appearing inflections in the other two records; the differences range from 0 to 33 k.y. and average ~15 k.y.
The question arises whether the differences between those ages are results of errors in the time-scale used for the Owens Lake record, or were there significant differences in the times when atmospheric climate change began to affect its different elements. The three records compared here are measurements of different elements and combinations of elements in two latitude belts: the deep-sea marine records measure combinations of temperature and precipitation that determined global ice volumes (at mostly high latitudes), the Devils Hole record measures atmospheric temperatures (in its mid-latitude region), and the Owens Lake record measures effective precipitation (in the same mid-latitude region).
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2317-5.143","usgsCitation":"Smith, G., Bischoff, J.L., and Bradbury, J.P., 1997, Synthesis of the paleoclimatic record from Owens Lake core OL-92, chap. of An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California, v. 317, p. 143-160, https://doi.org/10.1130/0-8137-2317-5.143.","productDescription":"18 p.","startPage":"143","endPage":"160","costCenters":[],"links":[{"id":400426,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Owens Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.15246582031249,\n 36.27085020723902\n ],\n [\n -117.81463623046875,\n 36.27085020723902\n ],\n [\n -117.81463623046875,\n 36.641977814705946\n ],\n [\n -118.15246582031249,\n 36.641977814705946\n ],\n [\n -118.15246582031249,\n 36.27085020723902\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"317","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, George I.","contributorId":57096,"corporation":false,"usgs":true,"family":"Smith","given":"George I.","affiliations":[],"preferred":false,"id":842596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradbury, J. Platt","contributorId":91106,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.","email":"","middleInitial":"Platt","affiliations":[],"preferred":false,"id":842598,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70229444,"text":"70229444 - 1997 - Climate control","interactions":[],"lastModifiedDate":"2022-03-08T17:06:07.562331","indexId":"70229444","displayToPublicDate":"1997-01-01T10:56:08","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":10268,"text":"Chesapeake Bay Journal","active":true,"publicationSubtype":{"id":10}},"title":"Climate control","docAbstract":"April showers bring May flowers. Well, not always. The climate of the Chesapeake Bay area, as elsewhere, varies from year to year as anyone living in the watershed the last few years can attest.
That variability, though, is more than just a conversation ice-breaker. Fluctuations in seasonal rainfall affect river flows into the Bay and can hinder nutrient reduction efforts aimed at restoring the Chesapeake ecosystem because nutrient flows into the Bay are closely tied to river discharge.
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}\n }\n ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cronin, Thomas M. 0000-0002-2643-0979 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":2579,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":837455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70231432,"text":"70231432 - 1997 - An 800,000-year pollen record from Owens Lake, California: Preliminary analyses","interactions":[{"subject":{"id":70231432,"text":"70231432 - 1997 - An 800,000-year pollen record from Owens Lake, California: Preliminary analyses","indexId":"70231432","publicationYear":"1997","noYear":false,"title":"An 800,000-year pollen record from Owens Lake, California: Preliminary analyses"},"predicate":"IS_PART_OF","object":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"id":1}],"isPartOf":{"id":70231435,"text":"70231435 - 1997 - An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","indexId":"70231435","publicationYear":"1997","noYear":false,"title":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California"},"lastModifiedDate":"2022-05-10T16:19:14.09398","indexId":"70231432","displayToPublicDate":"1997-01-01T10:54:14","publicationYear":"1997","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"An 800,000-year pollen record from Owens Lake, California: Preliminary analyses","docAbstract":"A long sequence of fossil palynomorph assemblages from a 323-m-long core taken at Owens Lake has enabled us to evaluate the gross vegetational trends for the Owens Valley region of California over the past ~800,000 years. Shifts in vegetation composition and abundance in the study area during the Pleistocene were indicated in core sediments by marked fluctuations in the pollen frequencies of pines, junipers, and, to a lesser extent, of big sagebrush, composites, and chenopods/amaranths. The modern vegetation distribution and modern pollen rain on the eastern flank of the Sierra Nevada indicate that maximal abundances of these taxa generally characterize higher elevation subalpine and montane coniferous forests, lower elevation coniferous woodland, steppe, and desert scrub environments. Pollen frequencies in the upper part of core OL-92 corroborate vegetational trends documented previously from late Wisconsin and Holocene Neotoma middens in the Great Basin. These trends and evidence from this study suggest that woodland taxa expanded their range down the slope of the eastern flank of the Sierra Nevada and were established in (and immediately adjacent to) Owens Valley during moderated climates of the late Wisconsin, apparently in response to decreases in temperature and increases in precipitation, but retreated upslope toward their present position starting as long ago as ca. 20 ka.
More importantly, pollen evidence from core OL-92 documents that the southern Sierra Nevada has experienced nine major cool-to-warm vegetation shifts (in addition to the late Wisconsin-early Holocene warming) during the time interval spanning the middle Pleistocene to early Holocene (Brunhes Normal Polarity Chron). We believe that at least six consecutive cool-to-warm shifts (the most recent ones) represent transitions from full-glacial to full-interglacial conditions on the basis of the magnitude of vegetation change in this portion of the pollen record. These marked changes in the frequency curves of dominant palynomorph taxa enabled us to identify boundaries that define 19 (?20) pollen zones in OL-92. The excursions of the pollen frequency curves within and across zone boundaries approximate the nature, duration, and timing of the middle and late Pleistocene climatic trends documented by geochemical (δ18O) evidence from OL-92 and from Devils Hole (DH-11) in the Amargosa Desert of Nevada.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2317-5.127","usgsCitation":"Litwin, R.J., Adam, D., Frederiksen, N.O., and Woolfenden, W.B., 1997, An 800,000-year pollen record from Owens Lake, California: Preliminary analyses, chap. of An 800,000-year paleoclimatic record from core OL-92, Owens Lake, Southeast California, v. 317, p. 127-142, https://doi.org/10.1130/0-8137-2317-5.127.","productDescription":"16 p.","startPage":"127","endPage":"142","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":400425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Owens Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.15246582031249,\n 36.27085020723902\n ],\n [\n -117.81463623046875,\n 36.27085020723902\n ],\n [\n -117.81463623046875,\n 36.641977814705946\n ],\n [\n -118.15246582031249,\n 36.641977814705946\n ],\n [\n -118.15246582031249,\n 36.27085020723902\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"317","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Litwin, Ronald J. 0000-0002-8661-1296 rlitwin@usgs.gov","orcid":"https://orcid.org/0000-0002-8661-1296","contributorId":2478,"corporation":false,"usgs":true,"family":"Litwin","given":"Ronald","email":"rlitwin@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":842588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adam, D.P.","contributorId":14815,"corporation":false,"usgs":true,"family":"Adam","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":842589,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frederiksen, N. O.","contributorId":78356,"corporation":false,"usgs":true,"family":"Frederiksen","given":"N.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":842590,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Woolfenden, W. B.","contributorId":291588,"corporation":false,"usgs":false,"family":"Woolfenden","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":842591,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70074731,"text":"70074731 - 1997 - Immunochemical technology for environmental applications","interactions":[],"lastModifiedDate":"2019-12-03T16:22:59","indexId":"70074731","displayToPublicDate":"1997-01-01T10:53:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":612,"text":"ACS Symposium Series","active":true,"publicationSubtype":{"id":10}},"title":"Immunochemical technology for environmental applications","docAbstract":"No abstract available.","language":"English","publisher":"American Chemical Society","doi":"10.1021/bk-1997-0657","usgsCitation":"1997, Immunochemical technology for environmental applications: ACS Symposium Series, v. 657, 233 p., https://doi.org/10.1021/bk-1997-0657.","productDescription":"233 p.","numberOfPages":"233","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":281878,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":281877,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/bk-1997-0657"}],"volume":"657","noUsgsAuthors":false,"publicationDate":"2009-07-23","publicationStatus":"PW","scienceBaseUri":"53cd6206e4b0b290850fde85","contributors":{"editors":[{"text":"Aga, Diana S.","contributorId":112821,"corporation":false,"usgs":true,"family":"Aga","given":"Diana","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":509789,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":509788,"contributorType":{"id":2,"text":"Editors"},"rank":2}]}} ,{"id":70199482,"text":"70199482 - 1997 - In situ and laboratory methods to study subsurface microbial transport","interactions":[],"lastModifiedDate":"2018-09-19T10:55:52","indexId":"70199482","displayToPublicDate":"1997-01-01T10:52:50","publicationYear":"1997","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"In situ and laboratory methods to study subsurface microbial transport","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Manual of environmental microbiology","language":"English","publisher":"American Society of Microbiology Press","publisherLocation":"Washington, D.C.","usgsCitation":"Harvey, R.W., 1997, In situ and laboratory methods to study subsurface microbial transport, chap. of Manual of environmental microbiology, p. 586-599.","productDescription":"14 p.","startPage":"586","endPage":"599","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":357479,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c110669e4b034bf6a80cd53","contributors":{"editors":[{"text":"Hurst, C. J.","contributorId":206942,"corporation":false,"usgs":false,"family":"Hurst","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":745551,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Stetzenbach, L.D.","contributorId":207563,"corporation":false,"usgs":false,"family":"Stetzenbach","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":745552,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Walters, M.","contributorId":105056,"corporation":false,"usgs":false,"family":"Walters","given":"M.","affiliations":[{"id":47618,"text":"Retired Calpine","active":true,"usgs":false}],"preferred":false,"id":745553,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Knudsen, G.R.","contributorId":207998,"corporation":false,"usgs":false,"family":"Knudsen","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":745554,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"McInerney, M.J.","contributorId":99298,"corporation":false,"usgs":true,"family":"McInerney","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":745555,"contributorType":{"id":2,"text":"Editors"},"rank":5}],"authors":[{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":745550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70246544,"text":"70246544 - 1997 - Some comparisons between recent ground-motion relations","interactions":[],"lastModifiedDate":"2023-07-07T15:50:31.009681","indexId":"70246544","displayToPublicDate":"1997-01-01T10:47:49","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3372,"text":"Seismological Research Letters","onlineIssn":"1938-2057","printIssn":"0895-0695","active":true,"publicationSubtype":{"id":10}},"title":"Some comparisons between recent ground-motion relations","docAbstract":"We provide an overview of new ground-motion relations for eastern North America (ENA) developed over the last five years. The empirical-stochastic relations of Atkinson and Boore (1995) are compared to relations developed by the Electric Power Research Institute (EPRI, 1993; also Toro et al., 1994), Frankel et al. (1996), and the consensus ENA ground-motion values as reported by SSHAC (1996). The main difference between our relations and those of EPRI or Frankel is in the low-frequency amplitudes (f < 2 Hz, all magnitudes). We predict lower amplitudes (by more than a factor of two) at 1 Hz, largely due to our use of an empirical source model rather than a single-corner-frequency Brune source model; the use of the empirical source model is motivated by the desire to match the ENA ground-motion database as closely as possible.
We also compare our new ENA relations to empirical relations for California. The comparison is complicated by the need to adjust the ENA hard-rock motions to obtain equivalent motions for typical California soil conditions. Two alternative methods of making this correction lead to somewhat different conclusions. One possible conclusion is that our ENA relations predict similar low-frequency amplitudes to those predicted by Boore et al. (1993, 1994) and Abrahamson and Silva (1996) for California, but our predicted ENA amplitudes are much higher (factor > 2) than California values at high frequencies. The alternative soil correction leads to the conclusion that our ENA relations are moderately lower (factor<2) than the California relations at low frequencies, and moderately higher at high frequencies. Both of these conclusions imply that ground-motion relations or time series for earthquakes in one region cannot be simply modified for use in engineering analyses in another region.
","language":"English","publisher":"Seismological Society of America","doi":"10.1785/gssrl.68.1.24","usgsCitation":"Atkinson, G.M., and Boore, D., 1997, Some comparisons between recent ground-motion relations: Seismological Research Letters, v. 68, no. 1, p. 24-40, https://doi.org/10.1785/gssrl.68.1.24.","productDescription":"17 p.","startPage":"24","endPage":"40","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":418767,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Atkinson, Gail M.","contributorId":60515,"corporation":false,"usgs":false,"family":"Atkinson","given":"Gail","email":"","middleInitial":"M.","affiliations":[{"id":13255,"text":"University of Western Ontario","active":true,"usgs":false}],"preferred":false,"id":877105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boore, David 0000-0002-8605-9673 boore@usgs.gov","orcid":"https://orcid.org/0000-0002-8605-9673","contributorId":140502,"corporation":false,"usgs":true,"family":"Boore","given":"David","email":"boore@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":877106,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1714,"text":"1714 - 1997 - The NASA atlas of the solar system","interactions":[],"lastModifiedDate":"2014-07-14T10:48:58","indexId":"1714","displayToPublicDate":"1997-01-01T10:47:12","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"The NASA atlas of the solar system","docAbstract":"Describes every planet, moon, and body that has been the subject of a NASA mission, including images of 30 solar system objects and maps of 26 objects. The presentation includes geologic history, geologic and reference maps, and shaded relief maps.","language":"English","publisher":"Cambridge University Press","publisherLocation":"Cambridge, England","doi":"10.3133/1714","isbn":"0521561272","usgsCitation":"Greeley, R., and Batson, R.M., 1997, The NASA atlas of the solar system, 369 p., https://doi.org/10.3133/1714.","productDescription":"369 p.","numberOfPages":"369","costCenters":[],"links":[{"id":289879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c4fc83e4b0b58d96eeb63f","contributors":{"authors":[{"text":"Greeley, Ronald","contributorId":20833,"corporation":false,"usgs":true,"family":"Greeley","given":"Ronald","email":"","affiliations":[],"preferred":false,"id":144004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Batson, Raymond M.","contributorId":13989,"corporation":false,"usgs":true,"family":"Batson","given":"Raymond","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":144003,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}