{"pageNumber":"2108","pageRowStart":"52675","pageSize":"25","recordCount":184689,"records":[{"id":70160348,"text":"70160348 - 2008 - The ecological future of the North American bison: Conceiving long-term, large-scale conservation of a species","interactions":[],"lastModifiedDate":"2016-02-22T11:42:37","indexId":"70160348","displayToPublicDate":"2015-07-06T08:45:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1321,"text":"Conservation Biology","active":true,"publicationSubtype":{"id":10}},"title":"The ecological future of the North American bison: Conceiving long-term, large-scale conservation of a species","docAbstract":"<p>Many wide-ranging mammal species have experienced significant declines over the last 200 years; restoring these species will require long-term, large-scale recovery efforts. We highlight 5 attributes of a recent range-wide vision-setting exercise for ecological recovery of the North American bison (Bison bison) that are broadly applicable to other species and restoration targets. The result of the exercise, the &ldquo;Vermejo Statement&rdquo; on bison restoration, is explicitly (1) large scale, (2) long term, (3) inclusive, (4) fulfilling of different values, and (5) ambitious. It reads, in part, &ldquo;Over the next century, the ecological recovery of the North American bison will occur when multiple large herds move freely across extensive landscapes within all major habitats of their historic range, interacting in ecologically significant ways with the fullest possible set of other native species, and inspiring, sustaining and connecting human cultures.&rdquo; We refined the vision into a scorecard that illustrates how individual bison herds can contribute to the vision. We also developed a set of maps and analyzed the current and potential future distributions of bison on the basis of expert assessment. Although more than 500,000 bison exist in North America today, we estimated they occupy &lt;1% of their historical range and in no place express the full range of ecological and social values of previous times. By formulating an inclusive, affirmative, and specific vision through consultation with a wide range of stakeholders, we hope to provide a foundation for conservation of bison, and other wide-ranging species, over the next 100 years.</p>","language":"English","publisher":"Society for Conservation Biology","doi":"10.1111/j.1523-1739.2008.00899.x","usgsCitation":"Sanderson, E., Redford, K., Weber, B., Aune, K., Baldes, D., Berger, J., Carter, D., Curtin, C., Derr, J., Dobrott, S., Fearn, E., Fleener, C., Forrest, S.C., Gerlach, C., Gates, C.C., Gross, J., Gogan, P., Grassel, S.M., Hilty, J.A., Jensen, M., Kunkel, K.E., Lammers, D., List, R., Minkowski, K., Olson, T., Pague, C., Robertson, P.B., and Stephenson, B., 2008, The ecological future of the North American bison: Conceiving long-term, large-scale conservation of a species: Conservation Biology, v. 22, no. 2, p. 252-266, https://doi.org/10.1111/j.1523-1739.2008.00899.x.","productDescription":"15 p.","startPage":"252","endPage":"266","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":312487,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"North America","volume":"22","issue":"2","noUsgsAuthors":false,"publicationDate":"2008-04-08","publicationStatus":"PW","scienceBaseUri":"5673eac9e4b0da412f4f826c","contributors":{"authors":[{"text":"Sanderson, E.W.","contributorId":6413,"corporation":false,"usgs":true,"family":"Sanderson","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":582672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redford, Kent","contributorId":93428,"corporation":false,"usgs":false,"family":"Redford","given":"Kent","email":"","affiliations":[{"id":35703,"text":"Archipelago Consulting, Portland, ME, U.S.A.","active":true,"usgs":false}],"preferred":false,"id":582673,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weber, Bill","contributorId":150685,"corporation":false,"usgs":false,"family":"Weber","given":"Bill","email":"","affiliations":[],"preferred":false,"id":582674,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Aune, K.","contributorId":64419,"corporation":false,"usgs":true,"family":"Aune","given":"K.","email":"","affiliations":[],"preferred":false,"id":582675,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baldes, Dick","contributorId":150686,"corporation":false,"usgs":false,"family":"Baldes","given":"Dick","email":"","affiliations":[],"preferred":false,"id":582676,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Berger, J.","contributorId":103010,"corporation":false,"usgs":true,"family":"Berger","given":"J.","email":"","affiliations":[],"preferred":false,"id":582677,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Carter, Dave","contributorId":150687,"corporation":false,"usgs":false,"family":"Carter","given":"Dave","email":"","affiliations":[],"preferred":false,"id":582678,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Curtin, C.","contributorId":39601,"corporation":false,"usgs":true,"family":"Curtin","given":"C.","email":"","affiliations":[],"preferred":false,"id":582679,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Derr, James N.","contributorId":72248,"corporation":false,"usgs":true,"family":"Derr","given":"James N.","affiliations":[],"preferred":false,"id":582687,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Dobrott, S.J.","contributorId":90844,"corporation":false,"usgs":true,"family":"Dobrott","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":582688,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Fearn, Eva","contributorId":150689,"corporation":false,"usgs":false,"family":"Fearn","given":"Eva","email":"","affiliations":[],"preferred":false,"id":582689,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Fleener, Craig","contributorId":150690,"corporation":false,"usgs":false,"family":"Fleener","given":"Craig","email":"","affiliations":[],"preferred":false,"id":582690,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Forrest, Steven C.","contributorId":11518,"corporation":false,"usgs":true,"family":"Forrest","given":"Steven","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":582691,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Gerlach, Craig","contributorId":150691,"corporation":false,"usgs":false,"family":"Gerlach","given":"Craig","email":"","affiliations":[],"preferred":false,"id":582692,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Gates, C. Cormack","contributorId":150647,"corporation":false,"usgs":false,"family":"Gates","given":"C.","email":"","middleInitial":"Cormack","affiliations":[],"preferred":false,"id":582693,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Gross, J.E.","contributorId":95845,"corporation":false,"usgs":true,"family":"Gross","given":"J.E.","affiliations":[],"preferred":false,"id":582694,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Gogan, P.","contributorId":107831,"corporation":false,"usgs":false,"family":"Gogan","given":"P.","affiliations":[],"preferred":false,"id":582695,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Grassel, Shaun M.","contributorId":150648,"corporation":false,"usgs":false,"family":"Grassel","given":"Shaun","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":582696,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Hilty, Jodi A.","contributorId":112149,"corporation":false,"usgs":true,"family":"Hilty","given":"Jodi","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":582697,"contributorType":{"id":1,"text":"Authors"},"rank":19},{"text":"Jensen, Marv","contributorId":150695,"corporation":false,"usgs":false,"family":"Jensen","given":"Marv","email":"","affiliations":[],"preferred":false,"id":582698,"contributorType":{"id":1,"text":"Authors"},"rank":20},{"text":"Kunkel, Kyran E.","contributorId":150649,"corporation":false,"usgs":false,"family":"Kunkel","given":"Kyran","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":582699,"contributorType":{"id":1,"text":"Authors"},"rank":21},{"text":"Lammers, Duane","contributorId":150696,"corporation":false,"usgs":false,"family":"Lammers","given":"Duane","email":"","affiliations":[],"preferred":false,"id":582700,"contributorType":{"id":1,"text":"Authors"},"rank":22},{"text":"List, R.","contributorId":103612,"corporation":false,"usgs":true,"family":"List","given":"R.","email":"","affiliations":[],"preferred":false,"id":582701,"contributorType":{"id":1,"text":"Authors"},"rank":23},{"text":"Minkowski, Karen","contributorId":150697,"corporation":false,"usgs":false,"family":"Minkowski","given":"Karen","email":"","affiliations":[],"preferred":false,"id":582702,"contributorType":{"id":1,"text":"Authors"},"rank":24},{"text":"Olson, Tom","contributorId":150698,"corporation":false,"usgs":false,"family":"Olson","given":"Tom","email":"","affiliations":[],"preferred":false,"id":582703,"contributorType":{"id":1,"text":"Authors"},"rank":25},{"text":"Pague, Chris","contributorId":150245,"corporation":false,"usgs":false,"family":"Pague","given":"Chris","email":"","affiliations":[{"id":7041,"text":"The Nature Conservancy","active":true,"usgs":false}],"preferred":false,"id":582704,"contributorType":{"id":1,"text":"Authors"},"rank":26},{"text":"Robertson, Paul B.","contributorId":150699,"corporation":false,"usgs":false,"family":"Robertson","given":"Paul","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":582705,"contributorType":{"id":1,"text":"Authors"},"rank":27},{"text":"Stephenson, Bob","contributorId":150700,"corporation":false,"usgs":false,"family":"Stephenson","given":"Bob","email":"","affiliations":[],"preferred":false,"id":582706,"contributorType":{"id":1,"text":"Authors"},"rank":28}]}}
,{"id":70041618,"text":"70041618 - 2008 - Viscoelastic love-type surface waves","interactions":[],"lastModifiedDate":"2015-10-29T09:52:05","indexId":"70041618","displayToPublicDate":"2015-04-06T04:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Viscoelastic love-type surface waves","docAbstract":"<p>The general theoretical solution for Love-Type surface waves in viscoelastic media provides theoreticalexpressions for the physical characteristics of the waves in elastic as well as anelastic media with arbitraryamounts of intrinsic damping. The general solution yields dispersion and absorption-coefficient curves for the waves as a function of frequency and theamount of intrinsic damping for any chosen viscoelastic model.Numerical results valid for a variety of viscoelastic models provide quantitative estimates of the physicalcharacteristics of the waves pertinent to models of Earth materials ranging from small amounts of damping in the Earth&rsquo;s crust to moderate and large amounts of damping in soft soils and water-saturated sediments. Numerical results, presented herein, are valid for a wide range of solids and applications.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"The 14th World Conference on Earthquake Engineering","conferenceTitle":"The 14th World Conference on Earthquake Engineering","conferenceDate":"October 12-17, 2008","conferenceLocation":"Beijing, China","language":"English","usgsCitation":"Borcherdt, R.D., 2008, Viscoelastic love-type surface waves, <i>in</i> The 14th World Conference on Earthquake Engineering, Beijing, China, October 12-17, 2008, 7 p.","productDescription":"7 p.","numberOfPages":"7","onlineOnly":"N","additionalOnlineFiles":"N","ipdsId":"IP-007898","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":310750,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"UNITED STATES","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56334347e4b048076347eef3","contributors":{"authors":[{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":578669,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120735,"text":"70120735 - 2008 - Sediment transport measurements","interactions":[],"lastModifiedDate":"2022-12-29T17:16:00.548615","indexId":"70120735","displayToPublicDate":"2013-08-15T16:18:00","publicationYear":"2008","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"110","chapter":"5","title":"Sediment transport measurements","docAbstract":"<p>Sediment erosion, transport, and deposition in fluvial systems are complex processes that are treated in detail in other sections of this book. Development of methods suitable for the collection of data that contribute to understanding these processes is a still-evolving science. Sediment and ancillary data are fundamental requirements for the proper management of river systems, including the design of structures, the determination of aspects of stream behavior, ascertaining the probable effect of removing an existing structure, estimation of bulk erosion, transport, and sediment delivery to the oceans, ascertaining the long-term usefulness of reservoirs and other public works, tracking movement of solid-phase contaminants, restoration of degraded or otherwise modified streams, and assistance in the calibration and validation of numerical models.</p> <br> <p>This chapter presents techniques for measuring bed-material properties and suspended and bed-load discharges. Well-established and relatively recent, yet adequately tested, sampling equipment and methodologies, with designs that are guided by sound physical and statistical principles, are described. Where appropriate, the theory behind the development of the equipment and guidelines for its use are presented.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sedimentation engineering: Processes, measurements, modeling, and practice","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/9780784408148.ch05","usgsCitation":"Diplas, P., Kuhnle, R., Gray, J., Glysson, D., and Edwards, T., 2008, Sediment transport measurements, chap. 5 <i>of</i> Sedimentation engineering: Processes, measurements, modeling, and practice, p. 307-353, https://doi.org/10.1061/9780784408148.ch05.","productDescription":"47 p.","startPage":"307","endPage":"353","numberOfPages":"47","costCenters":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"links":[{"id":292348,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2013-05-06","publicationStatus":"PW","scienceBaseUri":"53ef1ed8e4b0bfa1f993f015","contributors":{"editors":[{"text":"Garcia, Marcelo H.","contributorId":114196,"corporation":false,"usgs":true,"family":"Garcia","given":"Marcelo","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":509946,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Diplas, P.","contributorId":108411,"corporation":false,"usgs":true,"family":"Diplas","given":"P.","email":"","affiliations":[],"preferred":false,"id":498438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kuhnle, R.","contributorId":71897,"corporation":false,"usgs":true,"family":"Kuhnle","given":"R.","affiliations":[],"preferred":false,"id":498435,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gray, J.","contributorId":100683,"corporation":false,"usgs":true,"family":"Gray","given":"J.","affiliations":[],"preferred":false,"id":498437,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glysson, D.","contributorId":98649,"corporation":false,"usgs":true,"family":"Glysson","given":"D.","email":"","affiliations":[],"preferred":false,"id":498436,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Edwards, T.","contributorId":59743,"corporation":false,"usgs":true,"family":"Edwards","given":"T.","email":"","affiliations":[],"preferred":false,"id":498434,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70120727,"text":"70120727 - 2008 - Estimating sediment discharge: Appendix D","interactions":[],"lastModifiedDate":"2014-08-15T16:25:39","indexId":"70120727","displayToPublicDate":"2013-08-15T16:07:00","publicationYear":"2008","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"110","title":"Estimating sediment discharge: Appendix D","docAbstract":"<p>Sediment-discharge measurements usually are available on a discrete or periodic basis. However, estimates of sediment transport often are needed for unmeasured periods, such as when daily or annual sediment-discharge values are sought, or when estimates of transport rates for unmeasured or hypothetical flows are required. Selected methods for estimating suspended-sediment, bed-load, bed- material-load, and total-load discharges have been presented in some detail elsewhere in this volume. The purposes of this contribution are to present some limitations and potential pitfalls associated with obtaining and using the requisite data and equations to estimate sediment discharges and to provide guidance for selecting appropriate estimating equations.</p> <br> <p> Records of sediment discharge are derived from data collected with sufficient frequency to obtain reliable estimates for the computational interval and period. Most sediment- discharge records are computed at daily or annual intervals based on periodically collected data, although some partial records represent discrete or seasonal intervals such as those for flood periods. The method used to calculate sediment- discharge records is dependent on the types and frequency of available data. Records for suspended-sediment discharge computed by methods described by Porterfield (1972) are most prevalent, in part because measurement protocols and computational techniques are well established and because suspended sediment composes the bulk of sediment dis- charges for many rivers. Discharge records for bed load, total load, or in some cases bed-material load plus wash load are less common.</p> <br> <p> Reliable estimation of sediment discharges presupposes that the data on which the estimates are based are comparable and reliable. Unfortunately, data describing a selected characteristic of sediment were not necessarily derived—collected, processed, analyzed, or interpreted—in a consistent manner. For example, bed-load data collected with different types of bed-load samplers may not be comparable (Gray et al. 1991; Childers 1999; Edwards and Glysson 1999). The total suspended solids (TSS) analytical method tends to produce concentration data from open-channel flows that are biased low with respect to their paired suspended-sediment concentration values, particularly when sand-size material composes more than about a quarter of the material in suspension. Instantaneous sediment-discharge values based on TSS data may differ from the more reliable product of suspended- sediment concentration values and the same water-discharge data by an order of magnitude (Gray et al. 2000; Bent et al. 2001; Glysson et al. 2000; 2001). An assessment of data comparability and reliability is an important first step in the estimation of sediment discharges. </p> <br> <p> There are two approaches to obtaining values describing sediment loads in streams. One is based on direct measurement of the quantities of interest, and the other on relations developed between hydraulic parameters and sediment- transport potential. In the next sections, the most common techniques for both approaches are briefly addressed. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Sedimentation engineering: processes, measurements, modeling, and practice","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"American Society of Civil Engineers","usgsCitation":"Gray, J.R., and Simões, F., 2008, Estimating sediment discharge: Appendix D, chap. <i>of</i> Sedimentation engineering: processes, measurements, modeling, and practice, p. 1065-1086.","productDescription":"22 p.","startPage":"1065","endPage":"1086","costCenters":[],"links":[{"id":292344,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ef1ecee4b0bfa1f993ef48","contributors":{"authors":[{"text":"Gray, John R. 0000-0002-8817-3701 jrgray@usgs.gov","orcid":"https://orcid.org/0000-0002-8817-3701","contributorId":1158,"corporation":false,"usgs":true,"family":"Gray","given":"John","email":"jrgray@usgs.gov","middleInitial":"R.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true}],"preferred":true,"id":498432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simões, Francisco J. M.","contributorId":23855,"corporation":false,"usgs":true,"family":"Simões","given":"Francisco J. M.","affiliations":[],"preferred":false,"id":498433,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047867,"text":"ds383C - 2008 - National Land Cover Database 2001 (NLCD01) Tile 3, Southwest United States: NLCD01_3","interactions":[],"lastModifiedDate":"2013-08-28T13:59:56","indexId":"ds383C","displayToPublicDate":"2013-01-30T13:39:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"383","chapter":"C","title":"National Land Cover Database 2001 (NLCD01) Tile 3, Southwest United States: NLCD01_3","docAbstract":"This 30-meter data set represents land use and land cover for the conterminous United States for the 2001 time period. The data have been arranged into four tiles to facilitate timely display and manipulation within a Geographic Information System (see http://water.usgs.gov/GIS/browse/nlcd01-partition.jpg).The National Land Cover Data Set for 2001 was produced through a cooperative project conducted by the Multi-Resolution Land Characteristics (MRLC) Consortium. The MRLC Consortium is a partnership of Federal agencies (http://www.mrlc.gov), consisting of the U.S. Geological Survey (USGS), the National Oceanic and Atmospheric Administration (NOAA), the U.S. Environmental Protection Agency (USEPA), the U.S. Department of Agriculture (USDA), the U.S. Forest Service (USFS), the National Park Service (NPS), the U.S. Fish and Wildlife Service (USFWS), the Bureau of Land Management (BLM), and the USDA Natural Resources Conservation Service (NRCS). One of the primary goals of the project is to generate a current, consistent, seamless, and accurate National Land Cover Database (NLCD) circa 2001 for the United States at medium spatial resolution. For a detailed definition and discussion on MRLC and the NLCD 2001 products, refer to Homer and others (2004), (see: http://www.mrlc.gov/mrlc2k.asp). The NLCD 2001 was created by partitioning the United States into mapping zones. A total of 68 mapping zones (see http://water.usgs.gov/GIS/browse/nlcd01-mappingzones.jpg), were delineated within the conterminous United States based on ecoregion and geographical characteristics, edge-matching features, and the size requirement of Landsat mosaics. Mapping zones encompass the whole or parts of several states. Questions about the NLCD mapping zones can be directed to the NLCD 2001 Land Cover Mapping Team at the USGS/EROS, Sioux Falls, SD (605) 594-6151 or mrlc@usgs.gov.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ds383C","usgsCitation":"LaMotte, A., 2008, National Land Cover Database 2001 (NLCD01) Tile 3, Southwest United States: NLCD01_3: U.S. Geological Survey Data Series 383, Dataset, https://doi.org/10.3133/ds383C.","productDescription":"Dataset","costCenters":[],"links":[{"id":277112,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277111,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/nlcd01_3.xml"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.305923,22.736542 ], [ -123.305923,39.874012 ], [ -97.818040,39.874012 ], [ -97.818040,22.736542 ], [ -123.305923,22.736542 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521f1beae4b0f8bf2b07614c","contributors":{"authors":[{"text":"LaMotte, Andrew","contributorId":70006,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","affiliations":[],"preferred":false,"id":483179,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70044680,"text":"70044680 - 2008 - The Early Oligocene Copperas Creek Volcano and geology along New Mexico Higway 15 between Sapillo Creek and the Gila Cliff Dwellings National Monument, Grant and Catron Counties, New Mexico","interactions":[],"lastModifiedDate":"2025-09-04T13:43:28.987251","indexId":"70044680","displayToPublicDate":"2013-01-01T15:53:10","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The Early Oligocene Copperas Creek Volcano and geology along New Mexico Higway 15 between Sapillo Creek and the Gila Cliff Dwellings National Monument, Grant and Catron Counties, New Mexico","docAbstract":"The section of New Mexico Highway 15 between the intersection of NM-15 and NM 35 (aka Sapillo junction) at the south and the Gila Cliff Dwellings National Monument at the north end of NM –15 occupies an approximately 18 mile long, mile wide, corridor through the eastern part of the Gila Wilderness (Fig. 1). Whereas most of the Gila Wilderness is dominated by silicic, caldera-forming supervolcanoes of Eocene to Oligocene age, this part of NM-15 traverses a volcanic terrain of similar age, but composed mainly of intermediate composition lava flows and minor associated rhyolitic intrusions and pyroclastic rocks, which are related to the here-named Copperas Creek volcano. This volcanic complex is bounded by Basin and Range structures: on the south by the Sapillo Creek graben, and on the north by the Gila Hot Springs graben, both of which are filled with Gila Conglomerate of late Tertiary to Pleistocene(?) age. Hot springs in the Gila River valley are localized along faults in the deepest part of the Gila Hot Springs graben. The cliff dwellings of the National Monument were constructed in caves in Gila Conglomerate in the western part of the Gila Hot Springs graben. The eastern edge of the Gila Cliff Dwellings caldera is buried by younger rocks east of the cliff dwellings, but spectacular cliffs of Bloodgood Canyon Tuff, which fills the caldera, can be viewed along the West Fork of the Gila River from the trail starting at the cliff dwellings. Although this is not intended as a formal road log, highway mileage markers (MM) will be used to locate geologic features more or less progressively from south to north along NM-15.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"New Mexico Geological Society Fall Field Conference Guidebook 59 Geology of the Gila Wilderness-Silver City area","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"New Mexico Geological Society","doi":"10.56577/FFC-59.129","usgsCitation":"Ratte, J.C., 2008, The Early Oligocene Copperas Creek Volcano and geology along New Mexico Higway 15 between Sapillo Creek and the Gila Cliff Dwellings National Monument, Grant and Catron Counties, New Mexico, <i>in</i> New Mexico Geological Society Fall Field Conference Guidebook 59 Geology of the Gila Wilderness-Silver City area, p. 129-140, https://doi.org/10.56577/FFC-59.129.","productDescription":"12 p.","startPage":"129","endPage":"140","ipdsId":"IP-004856","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":275598,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f8e066e4b0cecbe8fa98bd","contributors":{"editors":[{"text":"Mack, Greg","contributorId":111993,"corporation":false,"usgs":true,"family":"Mack","given":"Greg","email":"","affiliations":[],"preferred":false,"id":509269,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Witcher, James","contributorId":111782,"corporation":false,"usgs":true,"family":"Witcher","given":"James","affiliations":[],"preferred":false,"id":509268,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Lueth, Virgil W.","contributorId":113648,"corporation":false,"usgs":true,"family":"Lueth","given":"Virgil","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":509270,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Ratte, James C.","contributorId":47671,"corporation":false,"usgs":true,"family":"Ratte","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":476224,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045338,"text":"70045338 - 2008 - Geology along the Catwalk National Recreation trail","interactions":[],"lastModifiedDate":"2013-07-30T15:47:41","indexId":"70045338","displayToPublicDate":"2013-01-01T15:44:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geology along the Catwalk National Recreation trail","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"New Mexico Geological Society Fall Field Conference Guidebook_59 Geology of the Gila Wilderness-Silver City area","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"New Mexico Geological Society","usgsCitation":"Ratte, J.C., 2008, Geology along the Catwalk National Recreation trail, <i>in</i> New Mexico Geological Society Fall Field Conference Guidebook_59 Geology of the Gila Wilderness-Silver City area, p. 17-26.","productDescription":"10 p.","startPage":"17","endPage":"26","ipdsId":"IP-004061","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":275595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f8e062e4b0cecbe8fa9875","contributors":{"editors":[{"text":"Mack, Greg","contributorId":111993,"corporation":false,"usgs":true,"family":"Mack","given":"Greg","email":"","affiliations":[],"preferred":false,"id":509283,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Witcher, James","contributorId":111782,"corporation":false,"usgs":true,"family":"Witcher","given":"James","affiliations":[],"preferred":false,"id":509282,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Lueth, Virgil W.","contributorId":113648,"corporation":false,"usgs":true,"family":"Lueth","given":"Virgil","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":509284,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Ratte, James C. jratte@usgs.gov","contributorId":875,"corporation":false,"usgs":true,"family":"Ratte","given":"James","email":"jratte@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":477265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047696,"text":"70047696 - 2008 - Region-wide trends of nesting ospreys in northwestern Mexico: a three-decade perspective","interactions":[{"subject":{"id":80498,"text":"ofr20071298 - 2007 - Population size and trends for nesting ospreys in northwestern Mexico: Region-wide surveys, 1977, 1992/1993 and 2006","indexId":"ofr20071298","publicationYear":"2007","noYear":false,"title":"Population size and trends for nesting ospreys in northwestern Mexico: Region-wide surveys, 1977, 1992/1993 and 2006"},"predicate":"SUPERSEDED_BY","object":{"id":70047696,"text":"70047696 - 2008 - Region-wide trends of nesting ospreys in northwestern Mexico: a three-decade perspective","indexId":"70047696","publicationYear":"2008","noYear":false,"title":"Region-wide trends of nesting ospreys in northwestern Mexico: a three-decade perspective"},"id":1}],"lastModifiedDate":"2013-08-19T14:59:56","indexId":"70047696","displayToPublicDate":"2013-01-01T14:55:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2442,"text":"Journal of Raptor Research","active":true,"publicationSubtype":{"id":10}},"title":"Region-wide trends of nesting ospreys in northwestern Mexico: a three-decade perspective","docAbstract":"We used a double-sampling technique (air plus ground survey) in 2006, with partial double coverage, to estimate the present size of the Osprey (Pandion haliaetus) nesting population in northwestern Mexico (coastal Baja California, islands in the Gulf of California, and coastal Sonora and Sinaloa). With the exception of Natividad, Cedros, and San Benitos islands along the Pacific coast of Baja California (all three excluded from our coverage in 2006 due to fog), this survey was a repeat of previous surveys conducted by us with the same protocol in 1977 and 1992/1993, allowing for estimates of regional population trends. The minimum population estimate for the area we surveyed in 2006 was 1343 nesting pairs, an 81% increase since 1977, but only a 3% increase since 1992/1993. The population on the Gulf side of Baja California generally remained stable during the three surveys (255, 236, and 252 pairs, respectively). The population of the Midriff Islands (Gulf of California in the vicinity of 29°N latitude) remained similar from 1992/1993 (308 pairs) to 2006 (289 pairs), but with notable population changes on the largest two islands (Guardian Angel: 45 to 105 pairs [133% increase]; Tiburón: 164 to 109 pairs [34% decrease]). The minimum estimated Osprey population on the Sonora mainland decreased in a manner similar to adjacent Isla Tiburón, i.e., by 26%, from 214 pairs in 1993 to 158 pairs in 2006. In contrast, the population in coastal Sinaloa, which had increased by 150% between 1977 and 1993, grew again by 58% between 1993 and 2006, from 180 to 285 pairs. Our survey confirmed previously described patterns of rapid population changes at a local level, coupled with apparent shifts in spatial distribution. The large ground-nesting population that until recently nested on two islands in San Ignacio Lagoon ( Pacific Ocean side, Baja California) was no longer present on the islands in 2006, but an equivalent number of pairs were found to the north and south of the lagoon, nesting in small towns and along adjoining overhead electric lines, with no overall change in population size for that general area (198 pairs in 1992; 199 in 2006). Use of artificial nesting structures was 4.3% in 1977 and 6.2% in 1992/1993, but jumped to 26.4% in 2006. Use of poles that support overhead electric lines poses a risk of electrocution to Ospreys and also causes power outages and fires. We recommend modification of these poles to safely accommodate Osprey nests, as has been successfully accomplished in many countries.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Raptor Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"The Raptor Research Foundation","doi":"10.3356/JRR-08-05.1","usgsCitation":"Henny, C.J., Anderson, D.W., Vera, A.C., and Cartron, J.E., 2008, Region-wide trends of nesting ospreys in northwestern Mexico: a three-decade perspective: Journal of Raptor Research, v. 42, no. 4, p. 229-242, https://doi.org/10.3356/JRR-08-05.1.","productDescription":"14 p.","startPage":"229","endPage":"242","costCenters":[{"id":290,"text":"Forest and Rangeland Ecosystem Science Center","active":false,"usgs":true}],"links":[{"id":476457,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3356/jrr-08-05.1","text":"Publisher Index Page"},{"id":276774,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276772,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3356/JRR-08-05.1"}],"volume":"42","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e38e4b0b08f44619921","contributors":{"authors":[{"text":"Henny, Charles J. 0000-0001-7474-350X hennyc@usgs.gov","orcid":"https://orcid.org/0000-0001-7474-350X","contributorId":3461,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"hennyc@usgs.gov","middleInitial":"J.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true}],"preferred":true,"id":482739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Daniel W.","contributorId":74345,"corporation":false,"usgs":false,"family":"Anderson","given":"Daniel","email":"","middleInitial":"W.","affiliations":[{"id":7214,"text":"University of California, Davis","active":true,"usgs":false}],"preferred":false,"id":482740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vera, Aradit Castellanos","contributorId":98824,"corporation":false,"usgs":true,"family":"Vera","given":"Aradit","email":"","middleInitial":"Castellanos","affiliations":[],"preferred":false,"id":482742,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cartron, Jean-Luc E.","contributorId":91012,"corporation":false,"usgs":true,"family":"Cartron","given":"Jean-Luc","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482741,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047162,"text":"70047162 - 2008 - Landslides and engineering geology of the Seattle, Washington, area","interactions":[],"lastModifiedDate":"2019-07-10T13:56:25","indexId":"70047162","displayToPublicDate":"2013-01-01T10:52:00","publicationYear":"2008","noYear":false,"publicationType":{"id":4,"text":"Book"},"seriesNumber":"20","title":"Landslides and engineering geology of the Seattle, Washington, area","docAbstract":"This volume brings together case studies and summary papers describing the application of state-of-the-art engineering geologic methods to landslide hazard analysis for the Seattle, Washington, area. An introductory chapter provides a thorough description of the Quaternary and bedrock geology of Seattle. Nine additional chapters review the history of landslide mapping in Seattle, present case studies of individual landslides, describe the results of spatial assessments of landslide hazard, discuss hydrologic controls on landsliding, and outline an early warning system for rainfall-induced landslides.","language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","usgsCitation":"Baum, R.L., Godt, J.W., and Highland, L.M., 2008, Landslides and engineering geology of the Seattle, Washington, area, v, 181 p.","productDescription":"v, 181 p.","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":363,"text":"Landslide Hazards Program","active":false,"usgs":true}],"links":[{"id":275278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275277,"type":{"id":15,"text":"Index Page"},"url":"https://rock.geosociety.org/Store/detail.aspx?id=REG020"}],"country":"United States","state":"Washington","city":"Seattle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.8534,47.25 ], [ -122.8534,47.9774 ], [ -121.7963,47.9774 ], [ -121.7963,47.25 ], [ -122.8534,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51efa5f2e4b0b09fbe58f195","contributors":{"authors":[{"text":"Baum, Rex L. 0000-0001-5337-1970 baum@usgs.gov","orcid":"https://orcid.org/0000-0001-5337-1970","contributorId":1288,"corporation":false,"usgs":true,"family":"Baum","given":"Rex","email":"baum@usgs.gov","middleInitial":"L.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":481194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Godt, Jonathan W. 0000-0002-8737-2493 jgodt@usgs.gov","orcid":"https://orcid.org/0000-0002-8737-2493","contributorId":1166,"corporation":false,"usgs":true,"family":"Godt","given":"Jonathan","email":"jgodt@usgs.gov","middleInitial":"W.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":481193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Highland, Lynn M. highland@usgs.gov","contributorId":1292,"corporation":false,"usgs":true,"family":"Highland","given":"Lynn","email":"highland@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":481195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047438,"text":"70047438 - 2008 - The Nation's top 25 construction aggregates producers","interactions":[],"lastModifiedDate":"2013-08-06T10:34:26","indexId":"70047438","displayToPublicDate":"2013-01-01T10:33:09","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":674,"text":"Aggregates Manager","active":true,"publicationSubtype":{"id":10}},"title":"The Nation's top 25 construction aggregates producers","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Aggregates Manager","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Randall Reilly Publishing","usgsCitation":"Willett, J., 2008, The Nation's top 25 construction aggregates producers: Aggregates Manager, v. 13, no. 2, p. 50-56.","productDescription":"7 p.","startPage":"50","endPage":"56","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":276101,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021aeae4b0e21cafa49ca6","contributors":{"authors":[{"text":"Willett, Jason Christopher","contributorId":85480,"corporation":false,"usgs":true,"family":"Willett","given":"Jason Christopher","affiliations":[],"preferred":false,"id":482043,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047121,"text":"70047121 - 2008 - High Resolution Imaging Science Experiment (HiRISE) observations of glacial and periglacial morphologies in the circum-Argyre Planitia highlands, Mars","interactions":[],"lastModifiedDate":"2018-11-27T10:37:29","indexId":"70047121","displayToPublicDate":"2013-01-01T08:57:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2317,"text":"Journal of Geophysical Research E: Planets","active":true,"publicationSubtype":{"id":10}},"title":"High Resolution Imaging Science Experiment (HiRISE) observations of glacial and periglacial morphologies in the circum-Argyre Planitia highlands, Mars","docAbstract":"The landscape of the Argyre Planitia and adjoining Charitum and Nereidum Montes in the southern hemisphere of Mars has been heavily modified since formation of the Argyre impact basin. This study examines morphologies in the Argyre region revealed in images acquired by the High Resolution Imaging Science Experiment (HiRISE) camera and discusses the implications for glacial and periglacial processes. Distinctive features such as large grooves, semicircular embayments in high topography, and streamlined hills are interpreted as glacially eroded grooves, cirques, and whalebacks or roche moutonnée, respectively. Large boulders scattered across the floor of a valley may be ground moraine deposited by ice ablation. Glacial interpretations are supported by the association of these features with other landforms typical of glaciated landscapes such as broad valleys with parabolic cross sections and stepped longitudinal profiles, lobate debris aprons interpreted as remnant debris covered glaciers or rock glaciers, and possible hanging valleys. Aligned boulders observed on slopes may also indicate glacial processes such as fluting. Alternatively, boulders aligned on slopes and organized in clumps and polygonal patterns on flatter surfaces may indicate periglacial processes, perhaps postglaciation, that form patterned ground. At least portions of the Argyre region appear to have been modified by processes of ice accumulation, glacial flow, erosion, sediment deposition, ice stagnation and ablation, and perhaps subsequent periglacial processes. The type of bedrock erosion apparent in images suggests that glaciers were, at times, wet based. The number of superposed craters is consistent with geologically recent glacial activity, but may be due to subsequent modification.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Geophysical Research E: Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGU","doi":"10.1029/2007JE002994","usgsCitation":"Banks, M.E., McEwen, A.S., Kargel, J.S., Baker, V., Strom, R.G., Mellon, M.T., Gulick, V.C., Keszthelyi, L., Herkenhoff, K.E., Pelletier, J.D., and Jaeger, W.L., 2008, High Resolution Imaging Science Experiment (HiRISE) observations of glacial and periglacial morphologies in the circum-Argyre Planitia highlands, Mars: Journal of Geophysical Research E: Planets, v. 113, no. E12, E12015; 20 p., https://doi.org/10.1029/2007JE002994.","productDescription":"E12015; 20 p.","ipdsId":"IP-007300","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":275168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Mars","volume":"113","issue":"E12","noUsgsAuthors":false,"publicationDate":"2008-12-31","publicationStatus":"PW","scienceBaseUri":"51ea8703e4b03397884d3994","contributors":{"authors":[{"text":"Banks, Maria E.","contributorId":80914,"corporation":false,"usgs":true,"family":"Banks","given":"Maria","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":481126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McEwen, Alfred S.","contributorId":61657,"corporation":false,"usgs":false,"family":"McEwen","given":"Alfred","email":"","middleInitial":"S.","affiliations":[{"id":7042,"text":"University of Arizona","active":true,"usgs":false}],"preferred":false,"id":481123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kargel, Jeffrey S.","contributorId":76601,"corporation":false,"usgs":true,"family":"Kargel","given":"Jeffrey","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":481125,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, Victor R.","contributorId":6931,"corporation":false,"usgs":true,"family":"Baker","given":"Victor R.","affiliations":[],"preferred":false,"id":481118,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Strom, Robert G.","contributorId":20350,"corporation":false,"usgs":true,"family":"Strom","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":481120,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mellon, Michael T.","contributorId":8603,"corporation":false,"usgs":false,"family":"Mellon","given":"Michael","email":"","middleInitial":"T.","affiliations":[{"id":7037,"text":"Southwest Research Institute, Boulder, Colorado","active":true,"usgs":false}],"preferred":false,"id":481119,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gulick, Virginia C.","contributorId":52443,"corporation":false,"usgs":true,"family":"Gulick","given":"Virginia","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":481122,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Keszthelyi, Laszlo P. 0000-0003-1879-4331 laz@usgs.gov","orcid":"https://orcid.org/0000-0003-1879-4331","contributorId":52802,"corporation":false,"usgs":true,"family":"Keszthelyi","given":"Laszlo P.","email":"laz@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":481127,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"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":481117,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Pelletier, Jon D.","contributorId":22657,"corporation":false,"usgs":false,"family":"Pelletier","given":"Jon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":481121,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Jaeger, Windy L.","contributorId":61679,"corporation":false,"usgs":true,"family":"Jaeger","given":"Windy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":481124,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70045925,"text":"70045925 - 2008 - Mineral resource of the month: iron oxide pigments","interactions":[],"lastModifiedDate":"2013-05-08T20:36:46","indexId":"70045925","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: iron oxide pigments","docAbstract":"The article discusses iron oxide pigments, which have been used as colorants since human began painting as they resist color change due to sunlight exposure, have good chemical resistance and are stable under normal ambient conditions. Cyprus, Italy and Spain are among the countries that are known for the production of iron oxide pigments. Granular forms of iron oxides and nano-sized materials are cited as developments in the synthetic iron oxide pigment industry which are being used in computer disk drives and nuclear magnetic resonance imaging.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2008, Mineral resource of the month: iron oxide pigments: Earth, v. 53, no. 12, p. 25-25.","productDescription":"1 p.","startPage":"25","endPage":"25","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272110,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73eee4b0037667dbc86d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045708,"text":"70045708 - 2008 - Low prevalence of avian influenza virus in shorebirds on the Pacific coast of North America","interactions":[],"lastModifiedDate":"2017-08-23T09:24:35","indexId":"70045708","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3731,"text":"Waterbirds","onlineIssn":"19385390","printIssn":"15244695","active":true,"publicationSubtype":{"id":10}},"title":"Low prevalence of avian influenza virus in shorebirds on the Pacific coast of North America","docAbstract":"The emergence of highly pathogenic avian influenza (HPAI) H5N1 has elevated concerns about wild birds as virus hosts; however, little is known about the ecological and epidemiological factors of transmission by shorebirds. Here we summarize results for 2,773 shorebirds that were live-trapped on the Pacific coast of the United States during 2006-2007 and tested for avian influenza virus using real-time reverse transcriptase-polymerase chain reaction (RT-PCR) and virus isolation. As was the case throughout North America, HPAI H5N1 was not detected in shorebirds during this interval. Contrary to other wild bird groups, most notably waterfowl, the prevalence of even low pathogenicity virus among shorebirds in our study areas in California, Washington, and Alaska was extremely low (0.5%). Virus was detected by RT-PCR from four different species, including, Dunlin (Calidris alpina; N = 3), Western Sandpiper (C. mauri; N = 8), Long-billed Dowitcher (Limnodromus scolopaceus; N = 1), and American Avocet (Recurvirostra americana; N = 1), with the detections in the latter three constituting the first published records for these birds. Based on studies in the eastern United States, we expected, but did not detect (H<sub>1</sub> = 1.6, P = 0.21) elevated avian influenza prevalence among shorebirds during spring migration. Diagnostic tests, which were designed to evaluate testing and sampling methods, indicated poor functioning of traditional virus isolation methods and no improvement in detection likelihood by collecting oropharyngeal swabs in addition to cloacal swab samples for low pathogenicity viruses (Z<sub>1</sub> = 0.7, P = 0.48).","language":"English","publisher":"The Waterbird Society","doi":"10.1675/1524-4695-31.4.602","usgsCitation":"Iverson, S.A., Takekawa, J.Y., Schwarzbach, S., Cardona, C.J., Warnock, N., Bishop, M.A., Schirato, G.A., Paroulek, S., Ackerman, J., Ip, S., and Boyce, W.M., 2008, Low prevalence of avian influenza virus in shorebirds on the Pacific coast of North America: Waterbirds, v. 31, no. 4, p. 602-610, https://doi.org/10.1675/1524-4695-31.4.602.","productDescription":"9 p.","startPage":"602","endPage":"610","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":271653,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271651,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1675/1524-4695-31.4.602"}],"volume":"31","issue":"4","noUsgsAuthors":false,"publicationDate":"2008-12-01","publicationStatus":"PW","scienceBaseUri":"5180e7e6e4b0df838b924d67","contributors":{"authors":[{"text":"Iverson, Samuel A.","contributorId":52308,"corporation":false,"usgs":false,"family":"Iverson","given":"Samuel","email":"","middleInitial":"A.","affiliations":[{"id":12437,"text":"Simon Fraser University, Centre for Wildlife Ecology","active":true,"usgs":false}],"preferred":false,"id":478136,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":478133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schwarzbach, Steven","contributorId":88038,"corporation":false,"usgs":true,"family":"Schwarzbach","given":"Steven","affiliations":[],"preferred":false,"id":478141,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cardona, Carol J.","contributorId":10536,"corporation":false,"usgs":true,"family":"Cardona","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":478134,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Warnock, Nils","contributorId":64534,"corporation":false,"usgs":false,"family":"Warnock","given":"Nils","email":"","affiliations":[],"preferred":false,"id":478137,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bishop, Mary Anne","contributorId":10698,"corporation":false,"usgs":true,"family":"Bishop","given":"Mary","email":"","middleInitial":"Anne","affiliations":[],"preferred":false,"id":478135,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schirato, Greg A.","contributorId":68627,"corporation":false,"usgs":true,"family":"Schirato","given":"Greg","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":478138,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Paroulek, Sara","contributorId":75041,"corporation":false,"usgs":true,"family":"Paroulek","given":"Sara","email":"","affiliations":[],"preferred":false,"id":478139,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Ackerman, Joshua T. 0000-0002-3074-8322 jackerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3074-8322","contributorId":147078,"corporation":false,"usgs":true,"family":"Ackerman","given":"Joshua T.","email":"jackerman@usgs.gov","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":478143,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Ip, S. 0000-0003-4844-7533 hip@usgs.gov","orcid":"https://orcid.org/0000-0003-4844-7533","contributorId":727,"corporation":false,"usgs":true,"family":"Ip","given":"S.","email":"hip@usgs.gov","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":478142,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Boyce, Walter M.","contributorId":75671,"corporation":false,"usgs":true,"family":"Boyce","given":"Walter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":478140,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}}
,{"id":70045712,"text":"70045712 - 2008 - Duck migration and past influenza A (H5N1) outbreak areas","interactions":[],"lastModifiedDate":"2017-08-23T09:25:14","indexId":"70045712","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1493,"text":"Emerging Infectious Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Duck migration and past influenza A (H5N1) outbreak areas","docAbstract":"In 2005 and 2006, the highly pathogenic avian influenza (HPAI) virus subtype H5N1 rapidly spread from Asia through Europe, the Middle East, and Africa. Waterbirds are considered the natural reservoir of low pathogenic avian influenza viruses (1), but their potential role in the spread of HPAI (H5N1), along with legal and illegal poultry and wildlife trade (2), is yet to be clarified.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Emerging Infectious Diseases","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"CDC","doi":"10.3201/eid1407.071477","usgsCitation":"Gaidet, N., Newman, S.H., Hagemeijer, W., Dodman, T., Cappelle, J., Hammoumi, S., De Simone, L., and Takekawa, J.Y., 2008, Duck migration and past influenza A (H5N1) outbreak areas: Emerging Infectious Diseases, v. 14, no. 7, p. 1164-1166, https://doi.org/10.3201/eid1407.071477.","productDescription":"3 p.","startPage":"1164","endPage":"1166","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":476460,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3201/eid1407.071477","text":"Publisher Index Page"},{"id":271665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271664,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.3201/eid1407.071477"}],"volume":"14","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5180e7e5e4b0df838b924d5c","contributors":{"authors":[{"text":"Gaidet, Nicolas","contributorId":37601,"corporation":false,"usgs":true,"family":"Gaidet","given":"Nicolas","email":"","affiliations":[],"preferred":false,"id":478156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newman, Scott H.","contributorId":101372,"corporation":false,"usgs":true,"family":"Newman","given":"Scott","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":478162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hagemeijer, Ward","contributorId":96406,"corporation":false,"usgs":true,"family":"Hagemeijer","given":"Ward","email":"","affiliations":[],"preferred":false,"id":478161,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dodman, Tim","contributorId":59706,"corporation":false,"usgs":true,"family":"Dodman","given":"Tim","email":"","affiliations":[],"preferred":false,"id":478159,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cappelle, Julien","contributorId":71440,"corporation":false,"usgs":true,"family":"Cappelle","given":"Julien","email":"","affiliations":[],"preferred":false,"id":478160,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hammoumi, Saliha","contributorId":54486,"corporation":false,"usgs":true,"family":"Hammoumi","given":"Saliha","email":"","affiliations":[],"preferred":false,"id":478158,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"De Simone, Lorenzo","contributorId":42117,"corporation":false,"usgs":true,"family":"De Simone","given":"Lorenzo","email":"","affiliations":[],"preferred":false,"id":478157,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":478155,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70046511,"text":"70046511 - 2008 - Future intrusion of oxygenated glacial meltwaters into the Fennoscandian shield: A possibility to consider in performance assessments for nuclear-waste disposal sites?","interactions":[],"lastModifiedDate":"2022-12-27T17:27:40.28357","indexId":"70046511","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"2008:16","chapter":"6","title":"Future intrusion of oxygenated glacial meltwaters into the Fennoscandian shield: A possibility to consider in performance assessments for nuclear-waste disposal sites?","docAbstract":"Provost et al. (1998) and Glynn and Voss (1999; also published in Glynn et al., 1999) considered the possibility that during future glaciations, oxygenated glacial meltwaters from two- to three-kilometer thick ice sheets could potentially intrude to the 500 m depth of planned nuclear-waste repositories. This possibility has been of concern because of potential negative effects on the stability of the repository engineered environment, and because of the potential mobilization of radionuclides should the oxygenated waters come into contact with the radioactive waste. The above reports argued that given the current state of knowledge, it was hard to discount the possibility that oxygenated waters could penetrate to repository level depth. The reports also suggested that oxidizing conditions might be present in the fractured rock environment for significant amounts of time, on the order of thousands to tens of thousands of years. In some earlier reports, Swedish and Finnish governmental agencies in charge of nuclear-waste disposal had considered the possibility that oxygenated meltwaters might intrude to the repository depth (SKI: 1992; Martinerie et al, 1992; Ahonen and Vieno, 1994). Subsequent to the publication of Provost et al. (1998), Glynn et al. (1999) and Glynn and Voss (1999), the Swedish Nuclear Fuel and Waste Handling Company (SKB) commissioned efforts to examine more thoroughly the possibilities that oxygenated meltwaters might occur under ice-sheet conditions and intrude to the repository depth.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Review of SKB's safety assessment SR-Can: Contributions in support of SKI's and SSI's review by external consultants","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Swedish Nuclear Power Inspectorate (SKI)","publisherLocation":"Stockholm, Sweden","usgsCitation":"Glynn, P., 2008, Future intrusion of oxygenated glacial meltwaters into the Fennoscandian shield: A possibility to consider in performance assessments for nuclear-waste disposal sites?, chap. 6 <i>of</i> Review of SKB's safety assessment SR-Can: Contributions in support of SKI's and SSI's review by external consultants, 15 p.","productDescription":"15 p.","ipdsId":"IP-005604","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"links":[{"id":273820,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":273819,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.stralsakerhetsmyndigheten.se/en/publications/reports/waste-shipments-physical-protection/2008/200816/"}],"country":"Finland, Norway, Russia, Sweden","otherGeospatial":"Fennoscandian Shield","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0.0,54.5 ], [ 0.0,72.0 ], [ 44.0,72.0 ], [ 44.0,54.5 ], [ 0.0,54.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c02feae4b0ee1529ed3cd8","contributors":{"authors":[{"text":"Glynn, Pierre","contributorId":88248,"corporation":false,"usgs":true,"family":"Glynn","given":"Pierre","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":479728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045047,"text":"70045047 - 2008 - Challenges in making a seismic hazard map for Alaska and the Aleutians","interactions":[],"lastModifiedDate":"2013-04-20T20:42:14","indexId":"70045047","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1805,"text":"Geophysical Monograph Series: Active Tectonics and Seismic Potential of Alaska","active":true,"publicationSubtype":{"id":10}},"title":"Challenges in making a seismic hazard map for Alaska and the Aleutians","docAbstract":"We present a summary of the data and analyses leading to the revision of the time-independent probabilistic seismic hazard maps of Alaska and the Aleutians. These maps represent a revision of existing maps based on newly obtained data, and reflect best current judgments about methodology and approach. They have been prepared following the procedures and assumptions made in the preparation of the 2002 National Seismic Hazard Maps for the lower 48 States, and will be proposed for adoption in future revisions to the International Building Code. We present example maps for peak ground acceleration, 0.2 s spectral amplitude (SA), and 1.0 s SA at a probability level of 2% in 50 years (annual probability of 0.000404). In this summary, we emphasize issues encountered in preparation of the maps that motivate or require future investigation and research.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geophysical Monograph Series: Active Tectonics and Seismic Potential of Alaska","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGU","publisherLocation":"Washington, D.C.","doi":"10.1029/179GM22","usgsCitation":"Wesson, R.L., Boyd, O., Mueller, C., and Frankel, A., 2008, Challenges in making a seismic hazard map for Alaska and the Aleutians: Geophysical Monograph Series: Active Tectonics and Seismic Potential of Alaska, v. 179, p. 385-397, https://doi.org/10.1029/179GM22.","productDescription":"13 p.","startPage":"385","endPage":"397","ipdsId":"IP-001717","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":271296,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271295,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/179GM22"}],"country":"United States","state":"Alaska","otherGeospatial":"Aleutian Islands","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,51.2 ], [ 172.5,71.4 ], [ -130.0,71.4 ], [ -130.0,51.2 ], [ 172.5,51.2 ] ] ] } } ] }","volume":"179","noUsgsAuthors":false,"publicationDate":"2013-03-19","publicationStatus":"PW","scienceBaseUri":"5173b8e3e4b0e619a5806ebd","contributors":{"editors":[{"text":"Freymueller, J.T.","contributorId":51482,"corporation":false,"usgs":true,"family":"Freymueller","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":509272,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Wesson, R. L.","contributorId":51752,"corporation":false,"usgs":true,"family":"Wesson","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":476690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyd, O.S.","contributorId":74479,"corporation":false,"usgs":true,"family":"Boyd","given":"O.S.","email":"","affiliations":[],"preferred":false,"id":476692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mueller, C.S.","contributorId":45310,"corporation":false,"usgs":true,"family":"Mueller","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":476689,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frankel, A.D.","contributorId":53828,"corporation":false,"usgs":true,"family":"Frankel","given":"A.D.","email":"","affiliations":[],"preferred":false,"id":476691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70045713,"text":"70045713 - 2008 - [Book Review] Avian influenza","interactions":[],"lastModifiedDate":"2017-08-23T07:49:39","indexId":"70045713","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"[Book Review] Avian influenza","docAbstract":"Review of: Avian Influenza. By David E. Swayne, Blackwell Publishing Ltd., Oxford, UK. 2008. 605 pp. ISBN-13 978-0-8138-2047-7/2008. US $149.99 (hardback).","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Wildlife Diseases","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"WDA","usgsCitation":"Schwarzbach, S., Muzzafar, S., and Takekawa, J.Y., 2008, [Book Review] Avian influenza: Journal of Wildlife Diseases, v. 44, no. 4, p. 1056-1058.","productDescription":"3 p.","startPage":"1056","endPage":"1058","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":271668,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5180e7f1e4b0df838b924de1","contributors":{"authors":[{"text":"Schwarzbach, Steven","contributorId":88038,"corporation":false,"usgs":true,"family":"Schwarzbach","given":"Steven","affiliations":[],"preferred":false,"id":478165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muzzafar, Sabir","contributorId":67785,"corporation":false,"usgs":true,"family":"Muzzafar","given":"Sabir","email":"","affiliations":[],"preferred":false,"id":478164,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Takekawa, John Y. 0000-0003-0217-5907 john_takekawa@usgs.gov","orcid":"https://orcid.org/0000-0003-0217-5907","contributorId":176168,"corporation":false,"usgs":true,"family":"Takekawa","given":"John","email":"john_takekawa@usgs.gov","middleInitial":"Y.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":false,"id":478163,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70045052,"text":"70045052 - 2008 - Landslide risk in the San Francisco Bay region","interactions":[],"lastModifiedDate":"2013-06-20T11:12:20","indexId":"70045052","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Landslide risk in the San Francisco Bay region","docAbstract":"We have used historical records of damaging landslides triggered by rainstorms, and a newly developed Probabilistic Landslide Assessment Cost Estimation System (PLACES), to estimate the numbers and direct costs of future landslides in the San Francisco Bay region. The estimated annual cost of future landslides in the entire region is about US $15 million (year 2000 $). The estimated annual cost is highest for San Mateo County ($3.32 million) and lowest for Solano County ($0.18 million). Normalizing costs by dividing by the percentage of land area with slopes equal or greater than about 10&deg; indicates that San Francisco County will have the highest cost per square km ($7,400), whereas Santa Clara County will have the lowest cost per square km ($230). These results indicate that the San Francisco Bay region has one of the highest levels of landslide risk in the United States. Compared to landslide cost estimates from the rest of the world, the risk level in the Bay region seems high, but not exceptionally high.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Landslides an d Engineered Slopes, From the Past to the Future, Proceedings of the 10th International Symposium on Landslides, June 30-July 4, 2008, Xi'an, China","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Taylor & Francis","publisherLocation":"London, UK","usgsCitation":"Coe, J.A., and Crovelli, R., 2008, Landslide risk in the San Francisco Bay region, <i>in</i> Landslides an d Engineered Slopes, From the Past to the Future, Proceedings of the 10th International Symposium on Landslides, June 30-July 4, 2008, Xi'an, China, v. 2, p. 1899-1904.","productDescription":"6 p.","startPage":"1899","endPage":"1904","ipdsId":"IP-003631","costCenters":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":274024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":274023,"type":{"id":11,"text":"Document"},"url":"https://landslides.usgs.gov/docs/coe/CoeISL2008.pdf"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.6515,37.4277 ], [ -122.6515,38.229 ], [ -121.7531,38.229 ], [ -121.7531,37.4277 ], [ -122.6515,37.4277 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51c42461e4b03c77dce65a5f","contributors":{"authors":[{"text":"Coe, J. A.","contributorId":8867,"corporation":false,"usgs":true,"family":"Coe","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":476696,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crovelli, R. A.","contributorId":40969,"corporation":false,"usgs":true,"family":"Crovelli","given":"R. A.","affiliations":[],"preferred":false,"id":476697,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70045922,"text":"70045922 - 2008 - Mineral resource of the month: cultured quartz crystal","interactions":[],"lastModifiedDate":"2013-05-08T20:27:32","indexId":"70045922","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: cultured quartz crystal","docAbstract":"The article presents information on cultured quartz crystals, a mineral used in mobile phones, computers, clocks and other devices controlled by digital circuits. Cultured quartz, which is synthetically produced in large pressurized vessels known as autoclaves, is useful in electronic circuits for precise filtration, frequency control and timing for consumer and military use. Several ingredients are used in producing cultured quartz, including seed crystals, lascas, a solution of sodium hydroxide or sodium carbonate, lithium salts and deionized water.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2008, Mineral resource of the month: cultured quartz crystal: Earth, v. 53, no. 11, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272107,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73e9e4b0037667dbc82e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045919,"text":"70045919 - 2008 - Mineral resource of the month: antimony","interactions":[],"lastModifiedDate":"2013-05-08T20:05:55","indexId":"70045919","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1419,"text":"Earth","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: antimony","docAbstract":"The article describes the characteristics and industrial uses of antimony. Antimony, which is produced as a byproduct of mining other metals such as gold, lead or silver, is used in everything from flame retardants, batteries, ceramics and glass. It is also used in glass for television picture tubes, computer monitors, pigments and catalysts.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Earth","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2008, Mineral resource of the month: antimony: Earth, v. 53, no. 9, p. 29-29.","productDescription":"1 p.","startPage":"29","endPage":"29","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272102,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518b73e6e4b0037667dbc80a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045836,"text":"70045836 - 2008 - Mineral resource of the month: arsenic","interactions":[],"lastModifiedDate":"2013-05-07T11:17:43","indexId":"70045836","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: arsenic","docAbstract":"Arsenic has a long and varied history: Although it was not isolated as an element until the 13th century, it was known to the ancient Chinese, Egyptians and Greeks in compound form in the minerals arsenopyrite, realgar and orpiment. In the 1400s, “Scheele’s Green” was first used as an arsenic pigment in wallpaper, and leached arsenic from wallpaper may have contributed to Napoleon’s death in 1821. The 1940s play and later movie, Arsenic and Old Lace, dramatizes the metal’s more sinister role. Arsenic continues to be an important mineral commodity with many modern applications.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geotimes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Brooks, W.E., 2008, Mineral resource of the month: arsenic: Geotimes, v. 2008, no. January, HTML Document.","productDescription":"HTML Document","costCenters":[],"links":[{"id":271954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271953,"type":{"id":11,"text":"Document"},"url":"https://www.geotimes.org/jan08/article.html?id=nn_arsenic.html"}],"volume":"2008","issue":"January","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518a226ee4b061e1bd5333e1","contributors":{"authors":[{"text":"Brooks, William E.","contributorId":104061,"corporation":false,"usgs":true,"family":"Brooks","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":478409,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045863,"text":"70045863 - 2008 - Mineral resource of the month: strontium","interactions":[],"lastModifiedDate":"2013-05-07T13:38:26","indexId":"70045863","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: strontium","docAbstract":"Last month as Americans sat transfixed watching fireworks on July 4, they were probably unaware that strontium was responsible for the beautiful reds in the display. Strontium, a soft silver-white or yellowish metallic element that turns yellow when exposed to air (and red when it burns), is prized for its brilliant red flame. Because it reacts with air and water, the metal is only present naturally in compounds, such as celestite and strontianite.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geotimes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Ober, J.A., 2008, Mineral resource of the month: strontium: Geotimes, v. 2008, no. August, HTML Document.","productDescription":"HTML Document","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":272016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":272015,"type":{"id":11,"text":"Document"},"url":"https://www.geotimes.org/aug08/article.html?id=nn_strontium.html"}],"volume":"2008","issue":"August","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518a2275e4b061e1bd533458","contributors":{"authors":[{"text":"Ober, Joyce A. 0000-0003-1608-5611 jober@usgs.gov","orcid":"https://orcid.org/0000-0003-1608-5611","contributorId":394,"corporation":false,"usgs":true,"family":"Ober","given":"Joyce","email":"jober@usgs.gov","middleInitial":"A.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":478453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045849,"text":"70045849 - 2008 - Mineral resource of the month: peat","interactions":[],"lastModifiedDate":"2013-05-07T12:58:44","indexId":"70045849","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"Mineral resource of the month: peat","docAbstract":"Peat is a natural organic material of botanical origin, harvested from deposits in bogs and fens. Commercial deposits form from the incomplete decomposition of plant matter under anaerobic conditions and gradually accumulate to form peat over about a 5,000-year period.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geotimes","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"AGI","usgsCitation":"Jasinski, S.M., 2008, Mineral resource of the month: peat: Geotimes, v. 2008, no. February, HTML Document.","productDescription":"HTML Document","costCenters":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"links":[{"id":271994,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":271993,"type":{"id":11,"text":"Document"},"url":"https://www.geotimes.org/feb08/article.html?id=nn_peat.html"}],"volume":"2008","issue":"February","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"518a2273e4b061e1bd533433","contributors":{"authors":[{"text":"Jasinski, Stephen M. sjasinsk@usgs.gov","contributorId":2735,"corporation":false,"usgs":true,"family":"Jasinski","given":"Stephen","email":"sjasinsk@usgs.gov","middleInitial":"M.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":478421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042764,"text":"pp171312 - 2008 - A four-dimensional petroleum systems model for the San Joaquin Basin Province, California: Chapter 12 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>","interactions":[],"lastModifiedDate":"2018-08-31T11:54:34","indexId":"pp171312","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1713-12","title":"A four-dimensional petroleum systems model for the San Joaquin Basin Province, California: Chapter 12 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>","docAbstract":"A calibrated numerical model depicts the geometry and three-dimensional (3-D) evolution of petroleum systems through time (4-D) in a 249 x 309 km (155 x 192 mi) area covering all of the San Joaquin Basin Province of California. Model input includes 3-D structural and stratigraphic data for key horizons and maps of unit thickness, lithology, paleobathymetry, heat flow, original total organic carbon, and original Rock-Eval pyrolysis hydrogen index for each source rock. The four principal petroleum source rocks in the basin are the Miocene Antelope shale of Graham and Williams (1985; hereafter referred to as Antelope shale), the Eocene Kreyenhagen Formation, the Eocene Tumey formation of Atwill (1935; hereafter referred to as Tumey formation), and the Cretaceous to Paleocene Moreno Formation. Due to limited Rock-Eval/total organic carbon data, the Tumey formation was modeled using constant values of original total organic carbon and original hydrogen index. Maps of original total organic carbon and original hydrogen index were created for the other three source rocks. The Antelope shale was modeled using Type IIS kerogen kinetics, whereas Type II kinetics were used for the other source rocks. Four-dimensional modeling and geologic field evidence indicate that maximum burial of the three principal Cenozoic source rocks occurred in latest Pliocene to Holocene time. For example, a 1-D extraction of burial history from the 4-D model in the Tejon depocenter shows that the bottom of the Antelope shale source rock began expulsion (10 percent transformation ratio) about 4.6 Ma and reached peak expulsion (50 percent transformation ratio) about 3.6 Ma. Except on the west flank of the basin, where steep dips in outcrop and seismic data indicate substantial uplift, little or no section has been eroded. Most petroleum migration occurred during late Cenozoic time in distinct stratigraphic intervals along east-west pathways from pods of active petroleum source rock in the Tejon and Buttonwillow depocenters to updip sandstone reservoirs. Satisfactory runs of the model required about 18 hours of computation time for each simulation using parallel processing on a Linux-based cluster.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California (PP 1713)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp171312","usgsCitation":"Peters, K., Magoon, L.B., Lampe, C., Scheirer, A.H., Lillis, P.G., and Gautier, D.L., 2008, A four-dimensional petroleum systems model for the San Joaquin Basin Province, California: Chapter 12 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>: U.S. Geological Survey Professional Paper 1713-12, Chapter 12: 35 p., https://doi.org/10.3133/pp171312.","productDescription":"Chapter 12: 35 p.","additionalOnlineFiles":"Y","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266301,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1713_12.jpg"},{"id":266299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1713/","text":"Index Page","linkFileType":{"id":5,"text":"html"}},{"id":266300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1713/12/pp1713_ch12.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.75,34.75 ], [ -121.75,38.0 ], [ -118.75,38.0 ], [ -118.75,34.75 ], [ -121.75,34.75 ] ] ] } } ] }","publicComments":"This report is Chapter 12 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>.  Please see <a href=\"http://pubs.er.usgs.gov/publication/pp1713\" target=\"_blank\">Professional Paper 1713</a> for other chapters.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51011472e4b033b1feeb2bdd","contributors":{"authors":[{"text":"Peters, Kenneth E.","contributorId":10897,"corporation":false,"usgs":true,"family":"Peters","given":"Kenneth E.","affiliations":[],"preferred":false,"id":472205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":472204,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lampe, Carolyn","contributorId":21840,"corporation":false,"usgs":true,"family":"Lampe","given":"Carolyn","email":"","affiliations":[],"preferred":false,"id":472206,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scheirer, Allegra Hosford","contributorId":93985,"corporation":false,"usgs":true,"family":"Scheirer","given":"Allegra","email":"","middleInitial":"Hosford","affiliations":[],"preferred":false,"id":472207,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":472203,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gautier, Donald L. gautier@usgs.gov","contributorId":1310,"corporation":false,"usgs":true,"family":"Gautier","given":"Donald","email":"gautier@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":472202,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70042762,"text":"pp171310 - 2008 - Petroleum systems of the San Joaquin Basin Province -- geochemical characteristics of gas types: Chapter 10 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>","interactions":[],"lastModifiedDate":"2018-08-31T13:03:54","indexId":"pp171310","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"2008","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1713-10","title":"Petroleum systems of the San Joaquin Basin Province -- geochemical characteristics of gas types: Chapter 10 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>","docAbstract":"The San Joaquin Basin Province is a petroliferous basin filled with predominantly Late Cretaceous to Pliocene-aged sediments, with organic-rich marine rocks of Late Cretaceous, Eocene, and Miocene age providing the source of most of the oil and gas. Previous geochemical studies have focused on the origin of the oil in the province, but the origin of the natural gas has received little attention. To identify and characterize natural gas types in the San Joaquin Basin, 66 gas samples were analyzed and combined with analyses of 15 gas samples from previous studies. For the purpose of this resource assessment, each gas type was assigned to the most likely petroleum system. Three general gas types are identified on the basis of bulk and stable carbon isotopic composition—thermogenic dry (TD), thermogenic wet (TW) and biogenic (B). The thermogenic gas types are further subdivided on the basis of the δ<sup>13</sup>C values of methane and ethane and nitrogen content into TD-1, TD-2, TD-Mixed, TW-1, TW-2, and TW-Mixed. Gas types TD-1 and TD-Mixed, a mixture of biogenic and TD-1 gases, are produced from gas fields in the northern San Joaquin Basin. Type TD-1 gas most likely originated from the Late Cretaceous to Paleocene Moreno Formation, a gas-prone source rock. The biogenic component of the TD-Mixed gas existed in the trap prior to the influx of thermogenic gas. For the assessment, these gas types were assigned to the Winters- Domengine Total Petroleum System, but subsequent to the assessment were reclassified as part of the Moreno-Nortonville gas system. Dry thermogenic gas produced from oil fields in the southern San Joaquin Basin (TD-2 gas) most likely originated from the oil-prone source rock of Miocene age. These samples have low wetness values due to migration fractionation or biodegradation. The thermogenic wet gas types (TW-1, TW-2, TW-Mixed) are predominantly associated gas produced from oil fields in the southern and central San Joaquin Basin. Type TW-1 gas most likely originates from source rocks within the Eocene Kreyenhagen Formation or the Eocene Tumey formation of Atwill (1935). Type TW-2 gas most likely originates from the Miocene Monterey Formation and equivalents. TW-Mixed gas is likely a mixture of biogenic and wet thermogenic gas (TW-1 or TW-2) derived from source rocks mentioned above. The thermogenic wet gas types are included in the corresponding Eocene or Miocene total petroleum systems. Type B gas is a dry, nonassociated gas produced from the Pliocene San Joaquin Formation in the central and southern San Joaquin Basin. This gas type most likely originated from Pliocene marine source rocks as a product of methanogenesis, and defines the Neogene Nonassociated Gas Total Petroleum System.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California (PP 1713)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/pp171310","usgsCitation":"Lillis, P.G., Warden, A., Claypool, G.E., and Magoon, L.B., 2008, Petroleum systems of the San Joaquin Basin Province -- geochemical characteristics of gas types: Chapter 10 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>: U.S. Geological Survey Professional Paper 1713-10, Chapter 10: 30 p., https://doi.org/10.3133/pp171310.","productDescription":"Chapter 10: 30 p.","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266302,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1713_10.jpg"},{"id":266296,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1713/10/pp1713_ch10.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":266295,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1713/","text":"Index Page","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.75,34.75 ], [ -121.75,38.0 ], [ -118.75,38.0 ], [ -118.75,34.75 ], [ -121.75,34.75 ] ] ] } } ] }","publicComments":"This report is Chapter 10 in <i>Petroleum systems and geologic assessment of oil and gas in the San Joaquin Basin Province, California</i>.  Please see <a href=\"http://pubs.er.usgs.gov/publication/pp1713\" target=\"_blank\">Professional Paper 1713</a> for other chapters.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5101147ae4b033b1feeb2c00","contributors":{"authors":[{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":472195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Warden, Augusta awarden@usgs.gov","contributorId":1774,"corporation":false,"usgs":true,"family":"Warden","given":"Augusta","email":"awarden@usgs.gov","affiliations":[],"preferred":true,"id":472194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Claypool, George E.","contributorId":76312,"corporation":false,"usgs":true,"family":"Claypool","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":472197,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":472196,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}