{"pageNumber":"224","pageRowStart":"5575","pageSize":"25","recordCount":36989,"records":[{"id":53815,"text":"ofr20041072 - 2004 - Emergency Assessment of Debris-Flow Hazards from Basins Burned by the Padua Fire of 2003, Southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr20041072","displayToPublicDate":"2004-03-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1072","title":"Emergency Assessment of Debris-Flow Hazards from Basins Burned by the Padua Fire of 2003, Southern California","docAbstract":"Results of a present preliminary assessment of the probability of debris-flow activity and estimates of peak discharges that can potentially be generated by debris flows issuing from basins burned by the Padua Fire of October 2003 in southern California in response to 25-year, 10-year, and 2-year recurrence, 1-hour duration rain storms are presented. The resulting probability maps are based on the application of a logistic multiple-regression model (Cannon and others, 2004) that describes the percent chance of debris-flow production from an individual basin as a function of burned extent, soil properties, basin gradients, and storm rainfall. The resulting peak discharge maps are based on application of a multiple-regression model (Cannon and others, 2004) that can be used to estimate debris-flow peak discharge at a basin outlet as a function of basin gradient, burn extent, and storm rainfall. Probabilities of debris-flow occurrence for the Padua Fire range between 0 and 99% and estimates of debris-flow peak discharges range between 1211 and 6,096 ft3/s (34 to 173 m3/s). These maps are intended to identify those basins that are most prone to the largest debris-flow events and provide information for the preliminary design of mitigation measures and for the planning of evacuation timing and routes.","language":"ENGLISH","doi":"10.3133/ofr20041072","usgsCitation":"Cannon, S.H., Gartner, J.E., Rupert, M.G., and Michael, J.A., 2004, Emergency Assessment of Debris-Flow Hazards from Basins Burned by the Padua Fire of 2003, Southern California (Version 1.0): U.S. Geological Survey Open-File Report 2004-1072, 14 p., https://doi.org/10.3133/ofr20041072.","productDescription":"14 p.","costCenters":[],"links":[{"id":181722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5227,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1072/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6058e2","contributors":{"authors":[{"text":"Cannon, Susan H. cannon@usgs.gov","contributorId":1019,"corporation":false,"usgs":true,"family":"Cannon","given":"Susan","email":"cannon@usgs.gov","middleInitial":"H.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":248423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, Joseph E. jegartner@usgs.gov","contributorId":1876,"corporation":false,"usgs":true,"family":"Gartner","given":"Joseph","email":"jegartner@usgs.gov","middleInitial":"E.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":248425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rupert, Michael G. mgrupert@usgs.gov","contributorId":1194,"corporation":false,"usgs":true,"family":"Rupert","given":"Michael","email":"mgrupert@usgs.gov","middleInitial":"G.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248424,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Michael, John A. jmichael@usgs.gov","contributorId":1877,"corporation":false,"usgs":true,"family":"Michael","given":"John","email":"jmichael@usgs.gov","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":248426,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53443,"text":"ofr20041024 - 2004 - Mineral, Energy, and Fertilizer Resources of the North Coast of Peru: Perspective from the Santa Rita B Archaeological Site","interactions":[],"lastModifiedDate":"2012-02-02T00:11:54","indexId":"ofr20041024","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1024","title":"Mineral, Energy, and Fertilizer Resources of the North Coast of Peru: Perspective from the Santa Rita B Archaeological Site","docAbstract":"The Santa Rita B archaeological site is in the Chao Valley, approximately 65 km southeast of Trujillo, northern Peru. Location of Santa Rita B at the emergence of several drainages from the Andean cordillera is an important factor in the almost continuous occupation of the site over the past 3,000 years. \r\n\r\nMineral resources are abundant throughout the Andes; however, the north coast of Peru was an important center for pre-Columbian mining, metallurgy, and craftsmanship. Success of the Chavin, Moche, Chimu, and other north coast cultures is directly related to the availability and exploitation of mineral and energy resources that include: gold (?silver), as electrum, mainly from placers, and copper from local oxide and carbonate occurrences and from sulfides related to copper porphyry occurrences in the cordillera. An alloy of these three metals is referred to as tumbaga, which is the primary material for Andean metalcraft. \r\n\r\nAnthracite was used for mirrors by north coast cultures and is available near Rio Chicama, Rio Santa, and east of Santa Rita B. These outcrops are a part of the Alto Chicama, Peru's largest coalfield, which extends from Rio Chicama, in the north, for 200 km southward to Rio Santa. Charcoal from the algorrobo tree and llama dung are considered to be the common pre-Columbian energy sources for cooking and metalwork; however, availability and the higher heat content of anthracite indicate that it was used in metallurgical applications. Bitumen is available from petroleum seeps near Talara, north of the study area, and may have been used as glue or as cement. \r\n\r\nHematite, goethite, limonite, and manganese oxides from clay-altered volcanic rock may have provided color and material for ceramics. Guano from the Islas Gua?apes, Chinchas, and Ballestas was used as fertilizer for cotton and other crops.","language":"ENGLISH","doi":"10.3133/ofr20041024","usgsCitation":"Brooks, W.E., Kent, J., and Willett, J.C., 2004, Mineral, Energy, and Fertilizer Resources of the North Coast of Peru: Perspective from the Santa Rita B Archaeological Site: U.S. Geological Survey Open-File Report 2004-1024, online only; 15 figs., https://doi.org/10.3133/ofr20041024.","productDescription":"online only; 15 figs.","costCenters":[],"links":[{"id":175145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5265,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1024/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f4e","contributors":{"authors":[{"text":"Brooks, William E.","contributorId":104061,"corporation":false,"usgs":true,"family":"Brooks","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":247606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kent, Jonathan D.","contributorId":107362,"corporation":false,"usgs":true,"family":"Kent","given":"Jonathan D.","affiliations":[],"preferred":false,"id":247607,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Willett, Jason C. 0000-0002-7598-3174 jwillett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-3174","contributorId":3516,"corporation":false,"usgs":true,"family":"Willett","given":"Jason","email":"jwillett@usgs.gov","middleInitial":"C.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":247605,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53718,"text":"ofr03381 - 2004 - Surficial Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina","interactions":[{"subject":{"id":53718,"text":"ofr03381 - 2004 - Surficial Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina","indexId":"ofr03381","publicationYear":"2004","noYear":false,"title":"Surficial Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"id":1}],"supersededBy":{"id":70040740,"text":"sim2997 - 2012 - Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina","indexId":"sim2997","publicationYear":"2012","noYear":false,"title":"Geologic map of the Great Smoky Mountains National Park region, Tennessee and North Carolina"},"lastModifiedDate":"2016-04-19T12:20:58","indexId":"ofr03381","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-381","title":"Surficial Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina","docAbstract":"<p>The Surficial Geology of the Great Smoky Mountains National Park Region, Tennessee and North Carolina was mapped from 1993 to 2003 under a cooperative agreement between the U.S. Geological Survey (USGS) and the National Park Service (NPS). This 1:100,000-scale digital geologic map was compiled from 2002 to 2003 from unpublished field investigations maps at 1:24,000-scale. The preliminary surficial geologic data and map support cooperative investigations with NPS, the U.S. Natural Resource Conservation Service, and the All Taxa Biodiversity Inventory (http://www.dlia.org/) (Southworth, 2001). Although the focus of our work was within the Park, the geology of the surrounding area is provided for regional context. Surficial deposits document the most recent part of the geologic history of this part of the western Blue Ridge and eastern Tennessee Valley of the Valley and Ridge of the Southern Appalachians. Additionally, there is great variety of surficial materials, which directly affect the different types of soil and associated flora and fauna. The surficial deposits accumulated over tens of millions of years under varied climatic conditions during the Cenozoic era and resulted from a composite of geologic processes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr03381","usgsCitation":"Southworth, S., Schultz, A., Denenny, D., and Triplett, J., 2004, Surficial Geologic Map of the Great Smoky Mountains National Park Region, Tennessee and North Carolina (Version 1.0): U.S. Geological Survey Open-File Report 2003-381, Report: 44 p.; Map: 54 x 30 inches, https://doi.org/10.3133/ofr03381.","productDescription":"Report: 44 p.; Map: 54 x 30 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":177254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110469,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62489.htm","linkFileType":{"id":5,"text":"html"},"description":"62489"},{"id":5060,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/of03-381/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina, Tennessee","otherGeospatial":"Great Smoky Mountains National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84,\n              35.3\n            ],\n            [\n              -84,\n              35.88\n            ],\n            [\n              -83,\n              35.88\n            ],\n            [\n              -83,\n              35.3\n            ],\n            [\n              -84,\n              35.3\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a36b","contributors":{"authors":[{"text":"Southworth, Scott","contributorId":93933,"corporation":false,"usgs":true,"family":"Southworth","given":"Scott","affiliations":[],"preferred":false,"id":248213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schultz, Art","contributorId":44982,"corporation":false,"usgs":true,"family":"Schultz","given":"Art","email":"","affiliations":[],"preferred":false,"id":248210,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denenny, Danielle","contributorId":78804,"corporation":false,"usgs":true,"family":"Denenny","given":"Danielle","affiliations":[],"preferred":false,"id":248211,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Triplett, James","contributorId":93565,"corporation":false,"usgs":true,"family":"Triplett","given":"James","email":"","affiliations":[],"preferred":false,"id":248212,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":53442,"text":"ofr20041023 - 2004 - Update: World Coal Quality Inventory -- Peru","interactions":[],"lastModifiedDate":"2012-02-02T00:11:54","indexId":"ofr20041023","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1023","title":"Update: World Coal Quality Inventory -- Peru","language":"ENGLISH","doi":"10.3133/ofr20041023","usgsCitation":"Brooks, W.E., and Willett, J.C., 2004, Update: World Coal Quality Inventory -- Peru: U.S. Geological Survey Open-File Report 2004-1023, online only; 5 figs, 2 tables, https://doi.org/10.3133/ofr20041023.","productDescription":"online only; 5 figs, 2 tables","costCenters":[],"links":[{"id":175144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5264,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1023/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb31","contributors":{"authors":[{"text":"Brooks, William E.","contributorId":104061,"corporation":false,"usgs":true,"family":"Brooks","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":247604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willett, Jason C. 0000-0002-7598-3174 jwillett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-3174","contributorId":3516,"corporation":false,"usgs":true,"family":"Willett","given":"Jason","email":"jwillett@usgs.gov","middleInitial":"C.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":247603,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53441,"text":"ofr20041022 - 2004 - Update: World Coal Quality Inventory -- Argentina","interactions":[],"lastModifiedDate":"2012-02-02T00:11:54","indexId":"ofr20041022","displayToPublicDate":"2004-02-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1022","title":"Update: World Coal Quality Inventory -- Argentina","language":"ENGLISH","doi":"10.3133/ofr20041022","usgsCitation":"Brooks, W.E., and Willett, J.C., 2004, Update: World Coal Quality Inventory -- Argentina: U.S. Geological Survey Open-File Report 2004-1022, online only; 6 fgis., 2 tables, https://doi.org/10.3133/ofr20041022.","productDescription":"online only; 6 fgis., 2 tables","costCenters":[],"links":[{"id":175143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5263,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1022/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eb76","contributors":{"authors":[{"text":"Brooks, William E.","contributorId":104061,"corporation":false,"usgs":true,"family":"Brooks","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":247602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willett, Jason C. 0000-0002-7598-3174 jwillett@usgs.gov","orcid":"https://orcid.org/0000-0002-7598-3174","contributorId":3516,"corporation":false,"usgs":true,"family":"Willett","given":"Jason","email":"jwillett@usgs.gov","middleInitial":"C.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":true,"id":247601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70044,"text":"ofr20041331 - 2004 - Cabeza Prieta National Wildlife Refuge: A survey of visitor experiences: Report to respondents","interactions":[],"lastModifiedDate":"2016-05-09T13:20:45","indexId":"ofr20041331","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1331","title":"Cabeza Prieta National Wildlife Refuge: A survey of visitor experiences: Report to respondents","docAbstract":"<p>In the fall of 2000, researchers from the Policy Analysis and Science Assistance Program (PASA) of the Fort Collins Science Center (FORT) in the U.S. Geological Survey (USGS) met with the staff of the Cabeza Prieta National Wildlife Refuge (CPNWR) to discuss the issues related to social, economic, and human dimensions of natural resource management as it related to the Comprehensive Conservation Plan (CCP) planning process. As a result of the meeting a research study was designed to better understand how visitors are affected by environmental management decisions and provide information to assist the refuge managers in making decisions regarding public use and recreational management related to the goals of the proposed CCP. More specifically, information was collected to document the type and frequency of visitor use; assess the importance of recreational activities; and to determine visitor attitudes about recreation management decisions within the refuge. To this end, we designed a study to assess the effects of the no-action and alternative management plans for the Refuge visitors&rsquo; perceptions and likely visitation patterns.</p>\n<p>In fall of 2002 a questionnaire was developed in collaboration with the U.S. Fish and Wildlife Service (FWS) and the CCP planning team and mailed to 1090 people who visited the refuge between June 2001 and June 2002. We used standard research methods in designing and administering the questionnaire. Six hundred and eightyfive (685) completed questionnaires (74%) were considered usable. We developed the questionnaire (OMB Control Number 1040-00) to answer the following questions:</p>\n<ul>\n<li>What are the important differences in visitors&rsquo; attitudes and perception regarding recreation and visitor use at CPNWR?</li>\n<li>What are the factors that explain the differences in visitor attitudes and perception regarding recreation and visitor use at CPNWR?</li>\n<li>What are the regional economic impacts of visitor spending?</li>\n</ul>\n<p>In general the respondents indicated support for current management practices of CPNWR. We found that people came to the Refuge to experience a connection with the resource and the environment. More than half of the respondents said that viewing the desert scenery, seeking wilderness solitude and viewing wildlife were the most important reasons for making the visit to the refuge.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041331","usgsCitation":"Ponds, P.D., Burkardt, N., and Koontz, L., 2004, Cabeza Prieta National Wildlife Refuge: A survey of visitor experiences: Report to respondents: U.S. Geological Survey Open-File Report 2004-1331, iii, 26 p., https://doi.org/10.3133/ofr20041331.","productDescription":"iii, 26 p.","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":186507,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041331.PNG"},{"id":320270,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1331/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Cabeza Prieta National Wildlife Refuge","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f98ef","contributors":{"authors":[{"text":"Ponds, Phadrea D.","contributorId":65156,"corporation":false,"usgs":true,"family":"Ponds","given":"Phadrea","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burkardt, Nina 0000-0002-9392-9251 burkardtn@usgs.gov","orcid":"https://orcid.org/0000-0002-9392-9251","contributorId":2781,"corporation":false,"usgs":true,"family":"Burkardt","given":"Nina","email":"burkardtn@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":281747,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koontz, Lynne koontzl@usgs.gov","contributorId":2174,"corporation":false,"usgs":false,"family":"Koontz","given":"Lynne","email":"koontzl@usgs.gov","affiliations":[{"id":7016,"text":"Environmental Quality Division, National Park Service, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":281746,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57975,"text":"ofr20041199 - 2004 - An economic analysis of alternative fertility control and associated management techniques for three BLM wild horse herds","interactions":[],"lastModifiedDate":"2017-12-19T18:44:35","indexId":"ofr20041199","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1199","title":"An economic analysis of alternative fertility control and associated management techniques for three BLM wild horse herds","docAbstract":"<p>Contemporary cost projections were computed for several alternative strategies that could be used by BLM to manage three wild horse populations. The alternatives included existing gather and selective removal methods, combined with potential contraceptive applications of varying duration and other potentially useful management techniques. Costs were projected for a 20-year economic life using the Jenkins wild horse population model and cost estimates from BLM that reflect state-by-state per horse removal, adoption, long-term holding, and contraceptive application expenses. Important findings include:</p>\n<ul>\n<li>Application of currently available 2-year contraceptives appears capable of reducing variable operating costs for wild horse populations by about 21% on average.</li>\n<li>Application of 3-year contraceptives, when fully tested and available, may be capable of reducing variable operating costs by about 27% on average.</li>\n<li>Combining contraceptives with modest changes to herd sex ratio (e.g., 55-60% males) can trim existing costs by about 31%.</li>\n<li>All savings are predicted to increase when contraception is applied in conjunction with the proposed removal policy that targets horses age zero to four, instead of zero to five.</li>\n<li>Reductions in herd size result in greater predicted variation in annual operating expenses for each herd, especially below about 200 animals, but are always at least &plusmn;20%.</li>\n<li>Because the horse program&rsquo;s variable operating costs only make up about one half of the total program costs (which include fixed and sunk costs), even with aggressive contraceptive management, total program costs could only be reduced by about 17%. This would still save about $7.7 million per year.</li>\n<li>None of the contraceptive options examined eliminated the need for long-term holding facilities over the 20-year period simulated, but the number of horses held may be reduced by about 23% with aggressive contraceptive treatment.</li>\n<li>Cost estimates are most sensitive to adoption age and per day holding costs.</li>\n<li>There are opportunities to improve both the population modeling software and the modeling processes used in assembling Herd Management Area environmental assessments.</li>\n</ul>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041199","collaboration":"In cooperation with the Bureau of Land Management","usgsCitation":"Bartholow, J.M., 2004, An economic analysis of alternative fertility control and associated management techniques for three BLM wild horse herds (Revised and reprinted 2004): U.S. Geological Survey Open-File Report 2004-1199, iii, 33 p., https://doi.org/10.3133/ofr20041199.","productDescription":"iii, 33 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":184339,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041199.PNG"},{"id":320274,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1199/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48","edition":"Revised and reprinted 2004","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a81","contributors":{"authors":[{"text":"Bartholow, John M.","contributorId":77598,"corporation":false,"usgs":true,"family":"Bartholow","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":258073,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57985,"text":"ofr20041264 - 2004 - Annual Report for 2003 Wild Horse Research and Field Activities","interactions":[],"lastModifiedDate":"2016-05-23T11:04:19","indexId":"ofr20041264","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1264","title":"Annual Report for 2003 Wild Horse Research and Field Activities","docAbstract":"<p>As stated in the Wild Horse Fertility Control Field Trial Plan, the Bureau of Land Management (BLM) has an immediate need for a safe, effective contraceptive agent to assist in the management of the large number of wild horses on western rangelands. The BLM and the U.S. Geological Survey-Biological Resources Discipline (USGS/BRD) are testing the immunocontraceptive agent Porcine Zonae Pellucida (PZP) in field trials with three free-roaming herds of western wild horses. Extensive research has already been conducted on the safety, efficacy, and duration of PZP applications in both domestic and feral horses on eastern barrier islands and in some select trials I with wild horses in Nevada managed by the BLM. However, significant questions remain concerning the effects of I PZP application at the population level in the wild, as well as effects at the individual level on behavior, social structure, and harem dynamics of free-ranging animals. These questions are best answered with field trials on wild horse herds under a tight research protocol. The ultimate goal is to provide the BLM with the protocols and information necessary to begin using fertility control to regulate population growth rates in wild horse herds on a broader scale. Fertility control is intended to assist the conventional capture, removal, and adoption process as a I means of controlling excess numbers of wild horses and burros, and to greatly reduce the adoption costs and numbers of animals handled. Fertility control is not intended to totally replace the removal and adoption process.</p>\n<p>The USGSIBRD began assisting the BLM with field trials of immunocontraceptive fertility control of wild horses in early 2001. The first PZP treatments were applied during gathers at the Pryor Mountain Wild Horse Range in September 2001, and the Little Book Cliffs Wild Horse Range, Colorado, in July 2002. At those gathers, 5 horses were treated in the Pryor Mountain WHR, and 23 were treated in the Little Book Cliffs WHR with PZP. These initial treatments were followed by booster injections in 2002. The second injection is required in order to raise, and I maintain, the titer levels of mares high enough to be considered contracepted. By the end of 2002, 13 horses on the Pryor Mountain WHR had received both injections, as had 11 horses in the Little Book Cliffs WHR. In 2003, intensive research efforts were carried out by the USGSIBRD at three field locations; Pryor Mountain WHR, Little I Book Cliffs WHR, and McCullough Peaks Wild Horse Management Area. The work at these sites during this I calendar year included treatment of wild horse mares with PZP in the Pryor herd and Little Book Cliffs herd, development and implementation of behavioral research to investigate potential affects of PZP treatment, continued tracking of demography and foal production in all three herds, and early phases of investigating aerial population estimation survey techniques. Detailed descriptions of these research topics can be found in the Wild Horse and Burro Management Strategic Research Plan and the Wild Horse Fertility Control Field Trial Plan. Field work in 2003 was conducted by USGSIBRD and BLM staff with the assistance of many dedicated individuals. See I Acknowledgments for more details.</p>\n<p>This report is meant to highlight the activities of the 2003 field season, as well as to provide a general overview of the data collected. More in-depth data analysis will be conducted following the conclusion of each I phase of the research project, and in many cases will not be possible until several seasons of data are collected.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041264","collaboration":"In cooperation with the Bureau of Land Management","usgsCitation":"Ransom, J., Singer, F., and Zeigenfuss, L., 2004, Annual Report for 2003 Wild Horse Research and Field Activities: U.S. Geological Survey Open-File Report 2004-1264, iii, 22 p., https://doi.org/10.3133/ofr20041264.","productDescription":"iii, 22 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":185203,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041264.PNG"},{"id":320273,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1264/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bbef","contributors":{"authors":[{"text":"Ransom, Jason","contributorId":15703,"corporation":false,"usgs":true,"family":"Ransom","given":"Jason","affiliations":[],"preferred":false,"id":258100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Singer, Francis J.","contributorId":65528,"corporation":false,"usgs":true,"family":"Singer","given":"Francis J.","affiliations":[],"preferred":false,"id":258101,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zeigenfuss, Linda 0000-0002-6700-8563 linda_zeigenfuss@usgs.gov","orcid":"https://orcid.org/0000-0002-6700-8563","contributorId":2079,"corporation":false,"usgs":true,"family":"Zeigenfuss","given":"Linda","email":"linda_zeigenfuss@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":258099,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53658,"text":"ofr20041010 - 2004 - Effect of structural heterogeneity and slip distribution on coseismic vertical displacement from rupture on the Seattle Fault","interactions":[],"lastModifiedDate":"2019-08-12T10:17:13","indexId":"ofr20041010","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1010","title":"Effect of structural heterogeneity and slip distribution on coseismic vertical displacement from rupture on the Seattle Fault","docAbstract":"Workshops in 2001 and 2002 were convened to determine critical issues in the development of tsunami inundation maps for the Puget Sound region. The Tsunami Inundation Mapping Effort (TIME) is conducted under the multi-agency National Tsunami Hazard Mitigation Program (NTHMP). The Puget Sound Tsunami/Landslide Workshop in 2001 focused on integrated tsunami research involving a wide range of research studies and tsunami hazard mitigation issues. The 2002 Puget Sound Tsunami Sources workshop (González et al., 2003) made specific recommendations for tsunami source modeling and improving our state of knowledge for sources in the Puget Sound region. One of the recommendations stated in González et al. (2003) is \"Develop methods to assess the sensitivity of coastal areas to tsunami inundation, based on multiple simulations that reflect the possible range of variations in the source parameters.\" Tsunami inundation models rely heavily on the imposed initial conditions which, for an earthquake source, is the coseismic vertical displacement field. For example, Koshimura et al. (2002) use the geologic uplift observations (Buknam et al., 1992) to constrain the slip distribution for the event that occurred 1100 years ago, resulting in an average slip of 3.7 m and a magnitude of 7.6. Walsh et al. (2003) develop a tsunami inundation map for Elliot Bay based on a M 7.3 earthquake and the geologic uplift observations from the 1100 y.b.p. event as in Koshimura et al. (2002), though they use a constant fault dip of 60° rather than different dips for deep and shallow segments. The objective of this report is to examine how coseismic vertical displacement from a smaller M 6.5 Seattle Fault earthquake (as in Hartzell et al., 2002) is affected by structural heterogeneity and different slip distribution patterns.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041010","usgsCitation":"Geist, E.L., and Yoshioka, S., 2004, Effect of structural heterogeneity and slip distribution on coseismic vertical displacement from rupture on the Seattle Fault: U.S. Geological Survey Open-File Report 2004-1010, HTML document, https://doi.org/10.3133/ofr20041010.","productDescription":"HTML document","onlineOnly":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":177649,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":292611,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1010/"}],"country":"United States","state":"Washington","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6257d1","contributors":{"authors":[{"text":"Geist, Eric L. 0000-0003-0611-1150 egeist@usgs.gov","orcid":"https://orcid.org/0000-0003-0611-1150","contributorId":1956,"corporation":false,"usgs":true,"family":"Geist","given":"Eric","email":"egeist@usgs.gov","middleInitial":"L.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"preferred":true,"id":511525,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yoshioka, Shoichi","contributorId":7358,"corporation":false,"usgs":true,"family":"Yoshioka","given":"Shoichi","email":"","affiliations":[],"preferred":false,"id":511526,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":74373,"text":"ofr20041350 - 2004 - Pocomoke Sound Sedimentary and Ecosystem History ","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr20041350","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1350","title":"Pocomoke Sound Sedimentary and Ecosystem History ","docAbstract":"Summary of Results: Pocomoke Sound Sediment and Sediment Processes\r\nTransport of sediment from coastal marshes. Analyses of pollen and foraminifera from surface sediments in Pocomoke Sound suggest that neither the upstream forested wetlands nor coastal marshes bordering the sound have contributed appreciably to particulate matter in the 10- to 1000-micron size range that is currently being deposited in the sound. \r\n\r\nSediment processes derived from short-lived isotope. Analyses of beryllium-7, cesium-137 and lead-210 and redox sensitive elements from Pocomoke sediments showed that there has been a significant increase in anthropogenic elements since the late 1940's when the Delmarva Peninsula became more accessible from the Baltimore-Washington region. Cesium-137 was found to be a useful tool to determine changes in sedimentation within the system. Three major stages of sedimentation occurred. Before 1950, the system was equilibrium with the agriculture activity in the watershed, whereas urbanization and agricultural activity changes during and immediately preceding World War II resulted in increased sediment flux. Around 1970, the sediment flux diminished and there was an apparent increase in bank erosion sediment to the deeper parts of the system. \r\n\r\nRates of sediment deposition. Radiocarbon, lead-210, and pollen dating of sediment cores from Pocomoke Sound indicate relatively continuous deposition of fine-grained sediments in the main Pocomoke channel at > ~7 m water depths. Mean sediment accumulation rates during the past few centuries were relatively high (>1 cm yr -1 ). The ages of coarser-grained sediments (sands) blanketing the shallow (< ~ 7 m water depth) flanks of Pocomoke Sound are not well constrained but were probably deposited discontinuously. \r\n\r\nImpacts of land-use on benthic biota. The Pocomoke Sound paleoecological record shows that in the 1940-50s and again in the 1970-80s, the sound experienced unprecedented changes in the benthic assemblages of both ostracodes and foraminifera that can be attributed to degradation in water quality. These changes represent perturbations to the natural variability in faunal assemblages, which are normally driven by climatically influenced changes in salinity regimes. Changes in 20th century benthic communities were characterized by the rise to dominance of facultative anaerobic taxa tolerant of hypoxia and detrital-feeding species, reflecting increased influx of organic matter, and perhaps greater turbidity. Results support the hypothesis of Orth et al. (2002) and Orth and Moore (1983) that unprecedented changes to the bay ecosystem affected submerged aquatic vegetation in the Tangiers-Pocomoke region prior to large-scale monitoring began in the 1970s and 80s. Comparison of Pocomoke paleoecological record with those from the mainstem bay indicate that environmental degradation during the 20th century was nearly synchronous bay-wide within the limits of sediment core chronology (10-20 years). \r\n\r\nStable isotopic evidence for decadal water quality changes. Stable isotopic records from benthic foraminifera in Pocomoke Sound sediment cores, especially oxygen isotopes, document regional decadal and centennial climate processes which influence salinity and water quality over the past few centuries. These results provide indirect evidence for discharge-driven changes in freshwater and presumably river-borne sediment from the watershed to the sound. They are consistent with studies in the mainstem indicating the important influence of climatic and hydrological processes on water quality. \r\n\r\nPollen evidence for high sedimentation and vegetation change during colonial land clearance. Pollen assemblages from sediment cores in Pocomoke Sound document high sedimentation rates (0.7->4.0 cm yr -1 ) at most sites throughout the Sound in post-Colonial time. These results confirm those from other regions of the bay that land-clearance increased the flux of river-borne sediment to certain r","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20041350","usgsCitation":"Cronin, T.M., 2004, Pocomoke Sound Sedimentary and Ecosystem History  (Online only): U.S. Geological Survey Open-File Report 2004-1350, 141 p., https://doi.org/10.3133/ofr20041350.","productDescription":"141 p.","onlineOnly":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7565,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1350/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684ab0","contributors":{"authors":[{"text":"Cronin, Thomas M. 0000-0002-2643-0979 tcronin@usgs.gov","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":2579,"corporation":false,"usgs":true,"family":"Cronin","given":"Thomas","email":"tcronin@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":286591,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53656,"text":"ofr20041001 - 2004 - The National Geochemical Survey: Database and documentation","interactions":[],"lastModifiedDate":"2021-09-15T11:51:33.538663","indexId":"ofr20041001","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1001","title":"The National Geochemical Survey: Database and documentation","docAbstract":"The USGS, in collaboration with other federal and state government agencies, industry, and academia, is conducting the National Geochemical Survey (NGS) to produce a body of geochemical data for the United States based primarily on stream sediments, analyzed using a consistent set of methods.  These data will compose a complete, national-scale geochemical coverage of the US, and will enable construction of geochemical maps, refine estimates of baseline concentrations of chemical elements in the sampled media, and provide context for a wide variety of studies in the geological and environmental sciences.  The goal of the NGS is to analyze at least one stream-sediment sample in every 289 km2 area by a single set of analytical methods across the entire nation, with other solid sample media substituted where necessary. The NGS incorporates geochemical data from a variety of sources, including existing analyses in USGS databases, reanalyses of samples in USGS archives, and analyses of newly collected samples.  At the present time, the NGS includes data covering ~71% of the land area of the US, including samples in all 50 states.\r\nThis version of the online report provides complete access to NGS data, describes the history of the project, the methodology used, and presents preliminary geochemical maps for all analyzed elements. Future editions of this and other related reports will include the results of analysis of variance studies, as well as interpretive products related to the NGS data.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041001","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2004, The National Geochemical Survey: Database and documentation (Version 1.0): U.S. Geological Survey Open-File Report 2004-1001, HTML Document, https://doi.org/10.3133/ofr20041001.","productDescription":"HTML Document","costCenters":[],"links":[{"id":177576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4953,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1001/","linkFileType":{"id":5,"text":"html"}},{"id":389228,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_62308.htm"}],"country":"United States","geographicExtents":"{\n  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,{"id":53657,"text":"ofr20041007 - 2004 - Desert Landforms and Surface Processes in the Mojave National Preserve and Vicinity","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr20041007","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1007","title":"Desert Landforms and Surface Processes in the Mojave National Preserve and Vicinity","docAbstract":"Landscape features in the Mojave National Preserve are a product of ongoing processes involving tectonic forces, weathering, and erosion. Long-term climatic cycles (wet and dry periods) have left a decipherable record preserved as landform features and sedimentary deposits. This website provides and introduction to climate-driven desert processes influencing landscape features including stream channels, alluvial fans, playas (dry lakebeds), dunes, and mountain landscapes. Bedrock characteristics, and the geometry of past and ongoing faulting, fracturing, volcanism, and landscape uplift and subsidence influence the character of processes happening at the surface.","language":"ENGLISH","doi":"10.3133/ofr20041007","usgsCitation":"Stoffer, P.W., 2004, Desert Landforms and Surface Processes in the Mojave National Preserve and Vicinity: U.S. Geological Survey Open-File Report 2004-1007, Online, https://doi.org/10.3133/ofr20041007.","productDescription":"Online","costCenters":[],"links":[{"id":177577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4954,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1007/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f11","contributors":{"authors":[{"text":"Stoffer, Philip W.","contributorId":32559,"corporation":false,"usgs":true,"family":"Stoffer","given":"Philip","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":248027,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72685,"text":"ofr20041337 - 2004 - Bighorn sheep habitat studies, population dynamics, and population modeling in Bighorn Canyon National Recreation Area, Wyoming and Montana, 2000-2003","interactions":[],"lastModifiedDate":"2016-05-09T12:54:47","indexId":"ofr20041337","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1337","title":"Bighorn sheep habitat studies, population dynamics, and population modeling in Bighorn Canyon National Recreation Area, Wyoming and Montana, 2000-2003","docAbstract":"<p>At the request of National Park Service resource managers, we began a study in 2000 to evaluate causes for the decline of the bighorn sheep (Ovis canadensis) population inhabiting Bighorn Canyon National Recreation Area (BICA), the Pryor Mountain Wild Horse Range, and surrounding state and U.S. Forest Service lands in Montana and Wyoming. Our study consisted of radio-collaring adult rams and ewes with mortality sensors to monitor adult mortalities, tracking ewes to determine pregnancy and lambing rates, habitat assessments to determine why the population was not expanding into what had been modeled using GIS methodology as suitable bighorn sheep habitat, measuring ungulate herbaceous consumption rates and herbaceous production to determine plant responses, and aerial and boat surveys to determine bighorn sheep population range and population dynamics (Schoenecker and others, this report). Two habitat suitability models were created and conducted (Gudorf, this report; Wockner and others, this report) using different methodologies, and comparisons made between the two. Herd population dynamics were modeled using the POP-II and POP-III programs (Roelle, this report), and a reassessment of ungulate exclosures that were established 8&ndash;10 years ago was conducted (Gerhardt, this report).</p>\n<p>The bighorn sheep population of the greater Bighorn Canyon National Recreation Area (BICA) was extirpated in the 1800s, and then reintroduced in 1973. The herd increased to a peak population of about 211 animals (Kissell and others, 1996), but then declined sharply in 1995 and 1996. Causes for the decline were unknown. Numbers have remained around 100 &plusmn; 20 animals since 1998. Previous modeling efforts determined what areas were suitable bighorn sheep habitat (Gudorf and others, 1996). We tried to determine why sheep were not using areas that were modeled as suitable or acceptable habitat, and to evaluate population dynamics of the herd.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041337","usgsCitation":"Singer, F.J., and Schoenecker, K.A., 2004, Bighorn sheep habitat studies, population dynamics, and population modeling in Bighorn Canyon National Recreation Area, Wyoming and Montana, 2000-2003: U.S. Geological Survey Open-File Report 2004-1337, xi, 202 p., https://doi.org/10.3133/ofr20041337.","productDescription":"xi, 202 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":193265,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041337.jpg"},{"id":320272,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1337/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Bighorn Canyon national Recreation Area","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db6260da","contributors":{"authors":[{"text":"Singer, Francis J.","contributorId":67026,"corporation":false,"usgs":true,"family":"Singer","given":"Francis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":628944,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoenecker, Kathryn A. 0000-0001-9906-911X schoeneckerk@usgs.gov","orcid":"https://orcid.org/0000-0001-9906-911X","contributorId":2001,"corporation":false,"usgs":true,"family":"Schoenecker","given":"Kathryn","email":"schoeneckerk@usgs.gov","middleInitial":"A.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":285871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53436,"text":"ofr20041017 - 2004 - Invertebrate Paleontology of the Wilson Grove Formation (Late Miocene to Late Pliocene), Sonoma and Marin Counties, California, with some Observations on Its Stratigraphy, Thickness, and Structure","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr20041017","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1017","title":"Invertebrate Paleontology of the Wilson Grove Formation (Late Miocene to Late Pliocene), Sonoma and Marin Counties, California, with some Observations on Its Stratigraphy, Thickness, and Structure","docAbstract":"The Wilson Grove Formation is exposed from Petaluma north to northern Santa Rosa, and from Bennett Valley west to Bodega Bay. A fauna of at least 107 invertebrate taxa consisting of two brachiopods, 95 mollusks (48 bivalves and 46 gastropods), at least eight arthropods, and at least two echinoids have been collected, ranging in age from late Miocene to late Pliocene. Rocks and fossils from the southwest part of the outcrop area, along the Estero de San Antonio, were deposited in a deep-water marine environment. At Meacham Hill, near the Stony Point Rock Quarry, and along the northern margin of the outcrop area at River Road and Wilson Grove, the Wilson Grove Formation was deposited in shallow marine to continental environments. At Meacham Hill, these shallow water deposits represent a brackish bay to continental environment, whereas at River Road and Wilson Grove, fossils suggest normal, euhaline (normal marine salinity) conditions. \r\n\r\nA few taxa from the River Road area suggest water temperatures slightly warmer than along the adjacent coast today because their modern ranges do not extend as far north in latitude as River Road. In addition, fossil collections from along River Road contain the bivalve mollusks Macoma addicotti (Nikas) and Nuttallia jamesii Roth and Naidu, both of which are restricted to the late Pliocene. The late Miocene Roblar tuff of Sarna-Wojcicki (1992) also crops out northeast of the River Road area and underlies the late Pliocene section at Wilson Grove by almost 300 m. Outcrops in the central part of the region are older than those to the northeast, and presumably younger than deposits to the southwest. The Roblar tuff of Sarna-Wojcicki (1992) occurs at Steinbeck Ranch in the central portion of the outcrop area. At Spring Hill, also in the central part of the outcrop area, the sanddollar Scutellaster sp., cf. S. oregonensis (Clark) has been recently collected. This species, questionably identified here, is restricted to the late Miocene from central California through Oregon. Outcrops at Salmon Creek, northeast of Steinbeck Ranch and also in the central part of the outcrop area, contain Aulacofusus? recurva (Gabb) and Turcica brevis Stewart, which are both restricted to the Pliocene, as well as Lirabuccinum portolaensis (Arnold) known from the early Pliocene of central and northern California and into the late Pliocene in southern California. These data suggest an overall pattern of older rocks and deeper water to the south and west, and younger rocks and shallower water to the east and north. Outcrops to the southwest, south of the Bloomfield fault, are not well dated but presumably are older than the late Miocene Roblar tuff of Sarna-Wojcicki (1992). Fossils in this part of the section are rare and are not useful in determining a precise age or environment of deposition for the lower part of the Wilson Grove Formation. However, sedimentary sequences and structures in the rocks here are useful and suggest probable outer shelf and slope water depths. Lituyapecten turneri (Arnold) which occurs in this part of the section has previously been restricted to the Pliocene, but its occurrence below the Roblar tuff of Sarna-Wojcicki (1992) indicates a revised late Miocene age for this taxon.\r\n\r\nThree possibly new gastropods (Mollusca) are reported here: Calyptraea (Trochita) n. sp. and Nucella sp., aff. N. lamellosa (Gmelin), both from the Bloomfield Quarry area, and Acanthinucella? n. sp. from the River Road area. These species are not described here because this venue is deemed insufficient for the description of new taxa.","language":"ENGLISH","doi":"10.3133/ofr20041017","usgsCitation":"Powell, C.L., Allen, J., and Holland, P.J., 2004, Invertebrate Paleontology of the Wilson Grove Formation (Late Miocene to Late Pliocene), Sonoma and Marin Counties, California, with some Observations on Its Stratigraphy, Thickness, and Structure: U.S. Geological Survey Open-File Report 2004-1017, 105 p.; 2 over-sized sheets, https://doi.org/10.3133/ofr20041017.","productDescription":"105 p.; 2 over-sized sheets","costCenters":[],"links":[{"id":180810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5216,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1017/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b7e4b07f02db534581","contributors":{"authors":[{"text":"Powell, Charles L. II 0000-0002-1913-555X cpowell@usgs.gov","orcid":"https://orcid.org/0000-0002-1913-555X","contributorId":3243,"corporation":false,"usgs":true,"family":"Powell","given":"Charles","suffix":"II","email":"cpowell@usgs.gov","middleInitial":"L.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":247589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, James R.","contributorId":51840,"corporation":false,"usgs":true,"family":"Allen","given":"James R.","affiliations":[],"preferred":false,"id":247590,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holland, Peter J.","contributorId":75220,"corporation":false,"usgs":true,"family":"Holland","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":247591,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70429,"text":"ofr20041418 - 2004 - Chronic wasting disease risk analysis workshop: An integrative approach","interactions":[],"lastModifiedDate":"2016-05-09T12:49:35","indexId":"ofr20041418","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1418","title":"Chronic wasting disease risk analysis workshop: An integrative approach","docAbstract":"<p>Risk analysis tools have been successfully used to determine the potential hazard associated with disease introductions and have facilitated management decisions designed to limit the potential for disease introduction. Chronic Wasting Disease (CWD) poses significant challenges for resource managers due to an incomplete understanding of disease etiology and epidemiology and the complexity of management and political jurisdictions. Tools designed specifically to assess the risk of CWD introduction would be of great value to policy makers in areas where CWD has not been detected.</p>\n<p>To this end, the U.S. Geological Survey (USGS) created a steering committee representing states, native communities, federal, academic, and non-government entities. This committee formulated a collaborative process for the development of CWD risk assessment tools applicable to both free-ranging and captive populations. The committee recommended a workshop be held on the topic and suggested the format, content, and potential participants.</p>\n<p>Identified objectives of the workshop included:</p>\n<p>1. Identify and discuss the needs of various government and non-government groups involved with assessing, managing, and/or preventing CWD.</p>\n<p>2. Identify current gaps in CWD research specifically in relation to information applicable to the risk analysis process.</p>\n<p>3. Construct a general, consensual, framework model (Figure 1) that incorporates all factors identified as potentially associated with the presence or absence of CWD (Table 1).</p>\n<p>The resulting CWD Risk Analysis Workshop was held May 11&ndash;13, 2004 in Fort Collins, Colorado. The workshop was attended by 28 individuals representing a cross-section of management, research, and nongovernment organizations. Experts with experience in a variety of risk analysis approaches and representatives from public and private user groups presented in the plenary session. The remainder of the workshop consisted of facilitated breakout sessions and all-group discussions.</p>\n<p>The framework model (Figure 1) reflects the workshop discussions and subsequent review and comments from workshop participants and steering committee members.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041418","usgsCitation":"Gillette, S., Dein, J., Salman, M., Richards, B., and Duarte, P., 2004, Chronic wasting disease risk analysis workshop: An integrative approach: U.S. Geological Survey Open-File Report 2004-1418, v, 53 p., https://doi.org/10.3133/ofr20041418.","productDescription":"v, 53 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":186181,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041418.PNG"},{"id":320280,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1418/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673637","contributors":{"authors":[{"text":"Gillette, Shana","contributorId":44620,"corporation":false,"usgs":true,"family":"Gillette","given":"Shana","affiliations":[],"preferred":false,"id":282408,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dein, Joshua","contributorId":8558,"corporation":false,"usgs":true,"family":"Dein","given":"Joshua","email":"","affiliations":[],"preferred":false,"id":282405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Salman, Mo","contributorId":30296,"corporation":false,"usgs":true,"family":"Salman","given":"Mo","affiliations":[],"preferred":false,"id":282407,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richards, Bryan","contributorId":56731,"corporation":false,"usgs":true,"family":"Richards","given":"Bryan","affiliations":[],"preferred":false,"id":282409,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Duarte, Paulo","contributorId":9349,"corporation":false,"usgs":true,"family":"Duarte","given":"Paulo","email":"","affiliations":[],"preferred":false,"id":282406,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70023,"text":"ofr20041442 - 2004 - Summary of studies supporting cumulative effects analysis of upper Yellowstone River channel modifications","interactions":[],"lastModifiedDate":"2017-12-19T18:54:33","indexId":"ofr20041442","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1442","title":"Summary of studies supporting cumulative effects analysis of upper Yellowstone River channel modifications","docAbstract":"<p>During the last several decades, portions of the upper Yellowstone River have been modified for flood control and erosion prevention. The U.S. Army Corps of Engineers is responsible for administration of a permit program for evaluating construction activities affecting rivers, streams, and wetlands. The Corps regulates activities under the authority of Section 10 of the Rivers and Harbors Act and Section 404 of the Clean Water Act. Since assumption of jurisdiction in the mid-1970&rsquo;s, the Corps has processed a total of 156 permit actions for the upper Yellowstone River. Over two-thirds of the permit actions occurred during or after two consecutive large floods during 1996 and 1997. In response to concern regarding the potential environmental and ecological consequences of channel modification, the Corps, in conjunction with State and local government agencies, initiated a series of scientific studies to better understand the effects of channel modification in the upper Yellowstone River (Figure 1). These included preparation of wetland and riparian inventory maps (Bon, 2001); hydraulic modeling and flood-plain delineation; watershed land-cover assessment (Pick and Potter, 2003); historic bottomland use analysis (Brelsford and others, 2003); analysis of channel modification effects on fish habitat (Bowen and others, 2003); comparison of juvenile salmonid use of modified and unmodified habitats (Zale and Rider, 2003); analysis of riparian vegetation and flood-plain turnover (Merigliano and Polzin, 2003); study of the relations between riparian habitat and bird communities (Hansen and others, 2003); analyses of geomorphology and historical channel changes (Dalby and Robinson, 2003); socioeconomic assessment (BBC Research and Consulting, 2002); and sediment transport investigations and modeling (Holnbeck, 2003).</p>\n<p>This report is a summary of results from the individual scientific studies as they bear on future programmatic cumulative effects analyses of channel modification of the upper Yellowstone River. We do not attempt a formal, cumulative impact assessment in the sense of evaluating alternatives or future scenarios. The first section presents major findings of the resource studies in terms of temporal comparisons, spatial comparisons, and causal relations. In this section, we present a series of conceptual models or flow diagrams of the major causal pathways of cumulative impacts from channel modification. These represent major pathways of potential impact based on knowledge from other rivers, concerns expressed about the upper Yellowstone, and results from the scientific studies. These diagrams serve to focus interpretation of study results as either supporting or not supporting the importance and magnitude of particular causal relations and to identify key linking variables appearing in multiple causal pathways. These key variables that connect channel&nbsp;modification actions to multiple, valued environmental attributes can serve as the foundation for both projecting and monitoring future responses of the system.&nbsp;</p>\n<p>A section on analytical realities outlines some of the limitations of projecting cumulative impacts from channel modification of the upper Yellowstone River on meaningful spatial and temporal scales and some of the difficulties of interpreting results from studies conducted shortly after two extreme floods and substantial increases in channel modification. A section on classification describes the two primary geomorphic classification systems of the upper Yellowstone River used in the various individual resource studies. Each of these systems has been valuable in supporting field sampling and expressing results concerning patterns of variation. Their integration or revision into a classification system to achieve some new purpose, such as a regulatory program or monitoring system, will depend on a crisp articulation of riverine management or regulatory objectives. A section on key variables identifies those that are central to the causal pathways connecting channel modification to impacts and provides a rationale for key variables as an alternative to other tools such as Proper Functioning Condition (Barrett and others, 1993), Index of Biotic Integrity (Karr, 1981), or the Synoptic Approach (Liebowitz and others, 1992). This section also explains relations among key variable to Hydrogeomorphic (HGM) assessment procedures (Hauer and Smith, 1998; Hauer and others, 2001) and outlines how these 2 variables might be monitored to track cumulative impacts. Examples of how selected key variables can be quantified using Geographic Information System data sets developed from the resource studies are presented for one reach.</p>\n<p>The largest portion of the document is an Appendix that summarizes each of the individual scientific studies in terms of scope and methods, findings, principal variables, and metrics used in the study or suggested by the study results, and important needs for further study.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041442","usgsCitation":"Auble, G.T., Bowen, Z.H., Bovee, K.D., Farmer, A.H., Sexton, N.R., and Waddle, T.J., 2004, Summary of studies supporting cumulative effects analysis of upper Yellowstone River channel modifications (Revised and reprinted 2004): U.S. Geological Survey Open-File Report 2004-1442, v, 60 p., https://doi.org/10.3133/ofr20041442.","productDescription":"v, 60 p.","numberOfPages":"68","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":193276,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041442.PNG"},{"id":320290,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1442/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Yellowstone River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.91934204101562,\n              45.00462215014995\n            ],\n            [\n              -110.91934204101562,\n              45.740693395533064\n            ],\n            [\n              -110.22308349609375,\n              45.740693395533064\n            ],\n            [\n              -110.22308349609375,\n              45.00462215014995\n            ],\n            [\n              -110.91934204101562,\n              45.00462215014995\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Revised and reprinted 2004","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699528","contributors":{"authors":[{"text":"Auble, Gregor T. 0000-0002-0843-2751 aubleg@usgs.gov","orcid":"https://orcid.org/0000-0002-0843-2751","contributorId":2187,"corporation":false,"usgs":true,"family":"Auble","given":"Gregor","email":"aubleg@usgs.gov","middleInitial":"T.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":281694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowen, Zachary H. 0000-0002-8656-1831 bowenz@usgs.gov","orcid":"https://orcid.org/0000-0002-8656-1831","contributorId":821,"corporation":false,"usgs":true,"family":"Bowen","given":"Zachary","email":"bowenz@usgs.gov","middleInitial":"H.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":281693,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bovee, Ken D.","contributorId":100447,"corporation":false,"usgs":true,"family":"Bovee","given":"Ken","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281697,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farmer, Adrian H.","contributorId":107759,"corporation":false,"usgs":true,"family":"Farmer","given":"Adrian","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":281698,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sexton, Natalie R.","contributorId":82750,"corporation":false,"usgs":true,"family":"Sexton","given":"Natalie","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":281696,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Waddle, Terry J.","contributorId":43430,"corporation":false,"usgs":true,"family":"Waddle","given":"Terry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281695,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":53204,"text":"ofr03469 - 2004 - Photomosaics and logs of trenches on the San Andreas Fault at Mill Canyon near Watsonville, California","interactions":[],"lastModifiedDate":"2023-06-22T16:37:40.670524","indexId":"ofr03469","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-469","title":"Photomosaics and logs of trenches on the San Andreas Fault at Mill Canyon near Watsonville, California","docAbstract":"<p>We present photomosaics and logs of the walls of trenches excavated for a paleoseismic study at Mill Canyon, one of two sites along the San Andreas fault in the Santa Cruz Mtns. on the Kelley-Thompson Ranch. This site was a part of Rancho Salsipuedes beginning in 1834. It was purchased by the present owner’s family in 1851. Remnants of a cabin/mill operations still exist up the canyon dating from 1908 when the area was logged. At this location, faulting has moved a shutter ridge across the mouth of Mill Canyon ponding Holocene sediment. Recent faulting is confined to a narrow zone near the break in slope.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03469","usgsCitation":"Fumal, T.E., Dawson, T.E., Flowers, R., Hamilton, J.C., Heingartner, G.F., Kessler, J., and Samrad, L., 2004, Photomosaics and logs of trenches on the San Andreas Fault at Mill Canyon near Watsonville, California: U.S. Geological Survey Open-File Report 2003-469, 1 Plate: 67.65 x 35.18 inches, https://doi.org/10.3133/ofr03469.","productDescription":"1 Plate: 67.65 x 35.18 inches","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":177134,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03469.jpg"},{"id":283966,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0469/pdf/of03-469.pdf"},{"id":4831,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0469/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"Watsonville","otherGeospatial":"Mill Canyon, San Andreas Fault","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.022445,36.858232 ], [ -122.022445,37.08012 ], [ -121.566315,37.08012 ], [ -121.566315,36.858232 ], [ -122.022445,36.858232 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685dd8","contributors":{"authors":[{"text":"Fumal, Thomas E.","contributorId":67882,"corporation":false,"usgs":true,"family":"Fumal","given":"Thomas","email":"","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":246905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dawson, Timothy E.","contributorId":24429,"corporation":false,"usgs":false,"family":"Dawson","given":"Timothy","email":"","middleInitial":"E.","affiliations":[{"id":7099,"text":"Calif. Geol. Survey","active":true,"usgs":false}],"preferred":false,"id":246904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flowers, Rebecca","contributorId":73269,"corporation":false,"usgs":true,"family":"Flowers","given":"Rebecca","email":"","affiliations":[],"preferred":false,"id":246906,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hamilton, John C. jhamilton@usgs.gov","contributorId":4202,"corporation":false,"usgs":true,"family":"Hamilton","given":"John","email":"jhamilton@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":246901,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Heingartner, Gordon F.","contributorId":11275,"corporation":false,"usgs":true,"family":"Heingartner","given":"Gordon","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":246902,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kessler, James","contributorId":21629,"corporation":false,"usgs":true,"family":"Kessler","given":"James","affiliations":[],"preferred":false,"id":246903,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Samrad, Laura","contributorId":83997,"corporation":false,"usgs":true,"family":"Samrad","given":"Laura","email":"","affiliations":[],"preferred":false,"id":246907,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":53434,"text":"ofr20041011 - 2004 - Emergency assessment of debris-flow hazards from basins burned by the Cedar and Paradise Fires of 2003, southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr20041011","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1011","title":"Emergency assessment of debris-flow hazards from basins burned by the Cedar and Paradise Fires of 2003, southern California","docAbstract":"These maps present preliminary assessments of the probability of debris-flow activity and estimates of peak discharges that can potentially be generated by debris flows issuing from basins burned by the Cedar and Paradise Fires of October 2003 in southern California in response to 25-year, 10-year, and 2-year recurrence, 1-hour duration rain storms. The probability maps are based on the application of a logistic multiple regression model that describes the percent chance of debris-flow production from an individual basin as a function of burned extent, soil properties, basin gradients, and storm rainfall. The peak-discharge maps are based on application of a multiple-regression model that can be used to estimate debris-flow peak discharge at a basin outlet as a function of basin gradient, burn extent, and storm rainfall. Probabilities of debris-flow occurrence for the Cedar Fire range between 0 and 98% and estimates of debris-flow peak discharges range between 893 and 5,987 ft3/s (25 to 170 m3/s). Basins burned by the Paradise Fire show probabilities for debris-flow occurrence between 2 and 98%, and peak discharge estimates between 1,814 and 5,980 ft3/s (51 and 169 m3/s). These maps are intended to identify those basins that are most prone to the largest debris-flow events and provide information for the preliminary design of mitigation measures and for the planning of evacuation timing and routes.","language":"ENGLISH","doi":"10.3133/ofr20041011","usgsCitation":"Cannon, S.H., Gartner, J.E., Rupert, M.G., and Michael, J.A., 2004, Emergency assessment of debris-flow hazards from basins burned by the Cedar and Paradise Fires of 2003, southern California (Version 1.0): U.S. Geological Survey Open-File Report 2004-1011, 90 by 36 inch map, https://doi.org/10.3133/ofr20041011.","productDescription":"90 by 36 inch map","costCenters":[],"links":[{"id":180808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5214,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1011/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604766","contributors":{"authors":[{"text":"Cannon, Susan H. cannon@usgs.gov","contributorId":1019,"corporation":false,"usgs":true,"family":"Cannon","given":"Susan","email":"cannon@usgs.gov","middleInitial":"H.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":247578,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, Joseph E. jegartner@usgs.gov","contributorId":1876,"corporation":false,"usgs":true,"family":"Gartner","given":"Joseph","email":"jegartner@usgs.gov","middleInitial":"E.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":247580,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rupert, Michael G. mgrupert@usgs.gov","contributorId":1194,"corporation":false,"usgs":true,"family":"Rupert","given":"Michael","email":"mgrupert@usgs.gov","middleInitial":"G.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":247579,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Michael, John A. jmichael@usgs.gov","contributorId":1877,"corporation":false,"usgs":true,"family":"Michael","given":"John","email":"jmichael@usgs.gov","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":247581,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":56776,"text":"ofr2003445 - 2004 - Wilderness experience in Rocky Mountain National Park 2002: Report to RMNP","interactions":[],"lastModifiedDate":"2016-05-23T15:09:21","indexId":"ofr2003445","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-445","title":"Wilderness experience in Rocky Mountain National Park 2002: Report to RMNP","docAbstract":"<p>Approximately 250,000 acres of backcountry in Rocky Mountain National Park (RMNP or the Park) may be designated as wilderness use areas in the coming years. Currently, over 3 million people visit RMNP each year; many drive through the park on Trail Ridge Road, camp in designated campgrounds, or hike in front-country areas. However, visitors also report much use of backcountry areas that are not easily accessible by roads or trails. Use of the backcountry is growing at RMNP and is accompanied by changing visitor expectations and preferences for wilderness management. For these reasons it is of great importance for the Park to periodically assess what types of environments and conditions wilderness users seek, to help them facilitate a quality wilderness experience.</p>\n<p>To assist in this effort, the Political Analysis and Science Assistance [PASA] program / Fort Collins Science Center / U.S. Geological Survey, in close collaboration with personnel and volunteers from RMNP and in cooperation with the Natural Resource Recreation and Tourism [NRRT] Department at CSU, and launched a research effort in the summer of 2002 to investigate visitor numbers, wilderness experiences, and management preferences in the Park.</p>\n<p>Specifically, the purposes of the research reported here are: (1) To determine what constitutes a wilderness experience; (2) To identify important places, visual features, and sounds essential to a quality wilderness experience and; (3) To determine what aspects may detract from wilderness experience in RMNP. Thus, answers to these questions should provide insight for Park managers about visitors' expectations for wilderness recreation and the conditions they seek for quality wilderness experiences. Ultimately, this information can be used to support wilderness management decisions within RMNP.</p>\n<p>The social science technique of Visitor Employed Photography [VEP] was used to obtain information from visitors about wilderness experiences. Visitors were selected at random from Park-designated wilderness trails, in proportion to their use, and asked to participate in the survey. Respondents were given single-use, 10-exposure cameras and photo-log diaries to record experiences. A total of 293 cameras were distributed, with a response rate of 87%. Following the development of the photos, a copy of the photos, two pertinent pages from the photo-log, and a follow-up survey were mailed to respondents. Fifty six percent of the follow-up surveys were returned. Findings from the two surveys were analyzed and compared.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr2003445","usgsCitation":"Schuster, E., Johnson, S.S., and Taylor, J.G., 2004, Wilderness experience in Rocky Mountain National Park 2002: Report to RMNP: U.S. Geological Survey Open-File Report 2003-445, vi, 47 p., https://doi.org/10.3133/ofr2003445.","productDescription":"vi, 47 p.","numberOfPages":"104","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2002-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":175027,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr2003445.PNG"},{"id":320289,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2003/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49a0e4b07f02db5bdb71","contributors":{"authors":[{"text":"Schuster, Elke","contributorId":63462,"corporation":false,"usgs":true,"family":"Schuster","given":"Elke","email":"","affiliations":[],"preferred":false,"id":255760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, S. Shea","contributorId":93122,"corporation":false,"usgs":true,"family":"Johnson","given":"S.","email":"","middleInitial":"Shea","affiliations":[],"preferred":false,"id":255758,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Jonathan G.","contributorId":37378,"corporation":false,"usgs":true,"family":"Taylor","given":"Jonathan","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":255759,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57981,"text":"ofr20041306 - 2004 - Quality assurance report - Loch Vale watershed, 1999-2002","interactions":[],"lastModifiedDate":"2022-09-16T20:26:56.802384","indexId":"ofr20041306","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1306","title":"Quality assurance report - Loch Vale watershed, 1999-2002","docAbstract":"<p>The National Park Service initiated the Loch Vale Watershed (LVWS) project in 1980 with funding from the Aquatic Effects Research Program of the National Acid Precipitation Assessment Program. Long-term ecological research and monitoring address watershed-scale ecosystem processes, particularly as they respond to atmospheric deposition and climate variability. Monitoring of meteorological, hydrologic, precipitation chemistry, and surface water quality parameters enable us to use long-term trends to distinguish natural from human-caused disturbances. Research into snow distribution, hydrologic flowpaths, vegetation responses to N deposition, isotopic transformations of N by forest and soil processes, trace metals, and aquatic ecological responses to disturbance enable us to understand processes that influence high elevation ecosystems.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041306","collaboration":"In collaboration with Natural Resource Ecology Laboratory","usgsCitation":"Botte, J.A., and Baron, J., 2004, Quality assurance report - Loch Vale watershed, 1999-2002: U.S. Geological Survey Open-File Report 2004-1306, iii, 17 p., https://doi.org/10.3133/ofr20041306.","productDescription":"iii, 17 p.","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1999-01-01","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":185199,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041306.PNG"},{"id":406883,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_69659.htm","linkFileType":{"id":5,"text":"html"}},{"id":320292,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1306/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Loch Vale watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.6378,\n              40.2828\n            ],\n            [\n              -105.8464,\n              40.2828\n            ],\n            [\n              -105.8464,\n              40.3089\n            ],\n            [\n              -105.6378,\n              40.3089\n            ],\n            [\n              -105.6378,\n              40.2828\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643d2c","contributors":{"authors":[{"text":"Botte, Jorin A.","contributorId":106571,"corporation":false,"usgs":true,"family":"Botte","given":"Jorin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":258090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baron, Jill 0000-0002-5902-6251 jill_baron@usgs.gov","orcid":"https://orcid.org/0000-0002-5902-6251","contributorId":194124,"corporation":false,"usgs":true,"family":"Baron","given":"Jill","email":"jill_baron@usgs.gov","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":258089,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57982,"text":"ofr20041291 - 2004 - Stratton Sagebrush Hydrology Study Area: An annotated bibliography of research conducted 1968-1990","interactions":[],"lastModifiedDate":"2016-05-23T11:41:48","indexId":"ofr20041291","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1291","title":"Stratton Sagebrush Hydrology Study Area: An annotated bibliography of research conducted 1968-1990","docAbstract":"<p>This annotated bibliography provides an overview of research projects conducted on the Stratton Sagebrush Hydrology Study Area (Stratton) since its designation as such in 1967. Sources include the Rocky Mountain Forest and Range Experiment Station records storage room, Laramie, Wyoming, the USGS and USFS online reference libraries, and scientific journal databases at the University of Wyoming and Colorado State University. This annotated bibliography summarizes publications from research conducted at Stratton during the prime of its tenure as a research lab from 1968 to 1990. In addition, an appendix is included that catalogues all data on file at the Rocky Mountain Forest and Range Experiment Station in Laramie, Wyoming. Each file folder was searched and its contents recorded here for the researcher seeking original data sets, charts, photographs and records.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041291","usgsCitation":"Burgess, L.M., and Schoenecker, K.A., 2004, Stratton Sagebrush Hydrology Study Area: An annotated bibliography of research conducted 1968-1990: U.S. Geological Survey Open-File Report 2004-1291, iii, 40 p., https://doi.org/10.3133/ofr20041291.","productDescription":"iii, 40 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":185200,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041291.PNG"},{"id":320291,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1291/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a52b4","contributors":{"authors":[{"text":"Burgess, Leah M.","contributorId":58713,"corporation":false,"usgs":true,"family":"Burgess","given":"Leah","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":258092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoenecker, Kathryn A. 0000-0001-9906-911X schoeneckerk@usgs.gov","orcid":"https://orcid.org/0000-0001-9906-911X","contributorId":2001,"corporation":false,"usgs":true,"family":"Schoenecker","given":"Kathryn","email":"schoeneckerk@usgs.gov","middleInitial":"A.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":258091,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57983,"text":"ofr20041281 - 2004 - Colorado Canyons National Conservation Area 2003 visitor use survey: Completion report","interactions":[],"lastModifiedDate":"2016-05-23T11:11:08","indexId":"ofr20041281","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1281","title":"Colorado Canyons National Conservation Area 2003 visitor use survey: Completion report","docAbstract":"<p>This report represents the analysis of research conducted by the U.S. Geological Survey (USGS) for the Bureau of Land Management (BLM). The purpose is to provide socio-economic and recreational use information that can be used in the development of a Resource Management Plan (RMP) for the Colorado Canyons National Conservation Area (CCNCA). The results reported here deal primarily with recreation-based activities in four areas: Kokopelli Loops, Rabbit Valley, Loma Boat Launch, and Devil&rsquo;s Canyon.</p>\n<p>In the fall of 2002, researchers from the Policy Analysis and Science Assistance Program (PASA) of the Fort Collins Science Center (FORT) in the USGS met with the staff of the CCNCA to discuss the issues related to social, economic, and human dimensions of natural resource management related to the RMP. As a result, a research study was designed to investigate the recreational experiences of visitors and their attitudes toward the management of the conservation area.</p>\n<p>In the spring of 2003, PASA conducted an intercept survey of recreational users at the CCNCA and a mail survey of local residents who were actively involved in decision-making regarding recreation on public lands in Mesa County, Colorado. Two hundred and three (203) mail surveys (66%) were returned and all of them were completed in full and considered usable. The intercept survey had a response rate with a range from 56%&ndash;64% among the four sites that were surveyed. We developed a questionnaire (OMB Control Number: 1040-0001) to answer the following questions:<br /><br /></p>\n<ul>\n<li>What are the important differences in citizens&rsquo; attitudes regarding recreation at the CCNCA?</li>\n<li>What are the factors that explain the differences in attitudes and preferences regarding recreation management of the NCA?</li>\n<li>What are citizens&rsquo; attitudes and preferences regarding their attitudes about paying a fee to visit the CCNCA?</li>\n</ul>\n<p>In general, respondents at all sites reported having an excellent or good recreation experience and almost all indicated that they intended to return. The results from the intercept survey indicated that across four sites 1(Kokopelli Loops, Devil&rsquo;s Canyon, Loma Boat Launch, and Rabbit Valley) respondents reported support for undeveloped use and recreation restrictions to limit resource impacts. Respondents indicated that managing sites for undeveloped use was a good idea.</p>\n<p>The respondents from the mail survey generally had a positive orientation toward current management practices of the CCNCA. According to our surveys, non-motorized trail related activities were among the three most popular activities people engaged in both close to home and while away. These trail-based recreational activities included walking, running, mountain bike riding, and horseback riding. Research has shown that people participate in these activities for many reasons including learning about nature, exercising, to learning about paleontology, escaping for awhile, and socializing with family and friends (Taylor, 2000). National data indicate that larger percentages of the general American population engage in trail activities than in many other traditional outdoor&nbsp;activities (Cordell, 1999). Over 65% of people in the U.S. engage in walking as a recreational activity (Figure 1). We found that people wanted to experience the outdoors and the CCNCA provided a good place to do it.</p>\n<p>Trail activities are often those that people participate in on a regular basis as a way to exercise. This can make trail related activities more attractive from a management standpoint because people who participate in an activity may be more likely to be repeat visitors.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041281","usgsCitation":"Ponds, P., Gillette, S.C., and Koontz, L., 2004, Colorado Canyons National Conservation Area 2003 visitor use survey: Completion report: U.S. Geological Survey Open-File Report 2004-1281, iii, 68 p., https://doi.org/10.3133/ofr20041281.","productDescription":"iii, 68 p.","numberOfPages":"76","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"2003-01-01","temporalEnd":"2003-12-31","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":185201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041281.PNG"},{"id":320279,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1281/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d48e","contributors":{"authors":[{"text":"Ponds, Phadrea","contributorId":88788,"corporation":false,"usgs":true,"family":"Ponds","given":"Phadrea","affiliations":[],"preferred":false,"id":258095,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gillette, Shana C.","contributorId":9346,"corporation":false,"usgs":true,"family":"Gillette","given":"Shana","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":258094,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koontz, Lynne koontzl@usgs.gov","contributorId":2174,"corporation":false,"usgs":false,"family":"Koontz","given":"Lynne","email":"koontzl@usgs.gov","affiliations":[{"id":7016,"text":"Environmental Quality Division, National Park Service, Fort Collins, Colorado","active":true,"usgs":false}],"preferred":false,"id":258093,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":53435,"text":"ofr20041013 - 2004 - Maps showing the stratigraphic framework of South Carolina's Long Bay from Little River to Winyah Bay","interactions":[],"lastModifiedDate":"2012-02-02T00:11:58","indexId":"ofr20041013","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1013","title":"Maps showing the stratigraphic framework of South Carolina's Long Bay from Little River to Winyah Bay","language":"ENGLISH","doi":"10.3133/ofr20041013","usgsCitation":"Baldwin, W.E., Morton, R., Denny, J.F., Dadisman, S.V., Schwab, W.C., Gayes, P.T., and Driscoll, N.W., 2004, Maps showing the stratigraphic framework of South Carolina's Long Bay from Little River to Winyah Bay: U.S. Geological Survey Open-File Report 2004-1013, 20 figs., https://doi.org/10.3133/ofr20041013.","productDescription":"20 figs.","costCenters":[],"links":[{"id":180809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5215,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1013/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60632c","contributors":{"authors":[{"text":"Baldwin, Wayne E. 0000-0001-5886-0917 wbaldwin@usgs.gov","orcid":"https://orcid.org/0000-0001-5886-0917","contributorId":1321,"corporation":false,"usgs":true,"family":"Baldwin","given":"Wayne","email":"wbaldwin@usgs.gov","middleInitial":"E.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":247584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, Robert A.","contributorId":88333,"corporation":false,"usgs":true,"family":"Morton","given":"Robert A.","affiliations":[],"preferred":false,"id":247588,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denny, Jane F. 0000-0002-3472-618X jdenny@usgs.gov","orcid":"https://orcid.org/0000-0002-3472-618X","contributorId":418,"corporation":false,"usgs":true,"family":"Denny","given":"Jane","email":"jdenny@usgs.gov","middleInitial":"F.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":247583,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dadisman, Shawn V. sdadisman@usgs.gov","contributorId":2207,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","email":"sdadisman@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":true,"id":247585,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schwab, William C. 0000-0001-9274-5154 bschwab@usgs.gov","orcid":"https://orcid.org/0000-0001-9274-5154","contributorId":417,"corporation":false,"usgs":true,"family":"Schwab","given":"William","email":"bschwab@usgs.gov","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":247582,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gayes, Paul T.","contributorId":86466,"corporation":false,"usgs":false,"family":"Gayes","given":"Paul","email":"","middleInitial":"T.","affiliations":[{"id":24750,"text":"Coastal Carolina University","active":true,"usgs":false}],"preferred":false,"id":247587,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Driscoll, Neal W.","contributorId":63266,"corporation":false,"usgs":true,"family":"Driscoll","given":"Neal","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":247586,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70048,"text":"ofr20041305 - 2004 - Economic analysis of alternative bison and elk management practices on the National Elk Refuge and Grand Teton National Park: A comparison of visitor and household responses","interactions":[],"lastModifiedDate":"2016-05-23T10:54:42","indexId":"ofr20041305","displayToPublicDate":"2004-01-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-1305","title":"Economic analysis of alternative bison and elk management practices on the National Elk Refuge and Grand Teton National Park: A comparison of visitor and household responses","docAbstract":"<p>The U.S. Fish and Wildlife Service (FWS) and the National Park Service (NPS) are preparing a management plan for bison and elk inhabiting the National Elk Refuge (NER) and Grand Teton National Park (GTNP). These animals are part of the bison and elk herds in Jackson Hole, one of the largest concentrations of freeranging bison and elk in the world. A range of alternatives for managing the bison and elk herds in the project area will be developed in an Environmental Impact Statement. The EIS will likely include such issues as habitat management, disease management, winter-feeding and hunting programs related to the NER and GTNP. The purposes of this study are to determine how the current management and EIS alternatives for bison and elk inhabiting the NER and GTNP would change:</p>\n<ul>\n<li>Visitor use</li>\n<li>Total visitor expenditures in the local and regional economy</li>\n<li>Local area employment and income in the local and regional economy</li>\n<li>Visitor net economic benefits</li>\n<li>Acceptability of individual elk and bison management practices to visitors and household living in Teton County, rest of Wyoming, and rest of the United States.</li>\n</ul>\n<p>Assessing public attitudes and economic effects for different EIS alternatives can provide managers with valuable information regarding the advantages and disadvantages of these alternatives. Economic issues such as local job and income effects are often raised by interest groups opposed to changes in current agency management actions. Having objective data on what the job and income impacts are can help to defuse that issue. Survey data on visitor and public preferences is also useful to supplement the traditional public involvement process conducted as part of the EIS process. This is because the survey reaches visitors and a broad geographic array of residents who may not typically participate in the traditional EIS public involvement process. That is, the survey reflects the effort of the EIS planning team reaching out to the public, rather than requiring the public to come to the EIS meeting locations. Attendance at public meetings is often inconvenient for occasional visitors to the NER and GTNP who frequently live long distances from the relevant FWS and NPS offices. It is also inconvenient for residents of states outside the state where the resource is located.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041305","usgsCitation":"Loomis, J., and Caughlan, L., 2004, Economic analysis of alternative bison and elk management practices on the National Elk Refuge and Grand Teton National Park: A comparison of visitor and household responses: U.S. Geological Survey Open-File Report 2004-1305, v, 110 p., https://doi.org/10.3133/ofr20041305.","productDescription":"v, 110 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"links":[{"id":191440,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041305.PNG"},{"id":320278,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2004/1305/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Grand Teton National Park, National Elk Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.81497192382812,\n              43.489793926746245\n            ],\n            [\n              -110.81497192382812,\n              44.02837121279199\n            ],\n            [\n              -110.45516967773438,\n              44.02837121279199\n            ],\n            [\n              -110.45516967773438,\n              43.489793926746245\n            ],\n            [\n              -110.81497192382812,\n              43.489793926746245\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625ff9","contributors":{"authors":[{"text":"Loomis, John B.","contributorId":27560,"corporation":false,"usgs":true,"family":"Loomis","given":"John B.","affiliations":[],"preferred":false,"id":281755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Caughlan, Lynne","contributorId":97200,"corporation":false,"usgs":true,"family":"Caughlan","given":"Lynne","email":"","affiliations":[],"preferred":false,"id":281756,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53207,"text":"ofr03450 - 2004 - Photomosaics and logs of trenches on the San Andreas Fault at Arano Flat near Watsonville, California","interactions":[],"lastModifiedDate":"2014-03-13T15:32:33","indexId":"ofr03450","displayToPublicDate":"2003-12-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2003-450","title":"Photomosaics and logs of trenches on the San Andreas Fault at Arano Flat near Watsonville, California","docAbstract":"We present photomosaics and logs of the walls of trenches excavated for a paleoseismic \nstudy at Arano Flat, one of two sites along the San Andreas fault in the Santa Cruz Mountains \non the Kelley-Thompson Ranch. At this location, the fault consists of a narrow \nzone along the northeast side of a low ridge adjacent to a possible sag pond and extends about \n60-70 meters across a broad alluvial flat. This site was a part of Rancho Salsipuedes beginning \nin 1834 and was purchased by the present owner’s family in 1851.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr03450","usgsCitation":"Fumal, T.E., Heingartner, G.F., Samrad, L., Dawson, T.E., Hamilton, J.C., and Baldwin, J.N., 2004, Photomosaics and logs of trenches on the San Andreas Fault at Arano Flat near Watsonville, California: U.S. Geological Survey Open-File Report 2003-450, 3 Plates: 83.52 x 34.55 inches and smaller, https://doi.org/10.3133/ofr03450.","productDescription":"3 Plates: 83.52 x 34.55 inches and smaller","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":177211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr03450.jpg"},{"id":4834,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2003/0450/","linkFileType":{"id":5,"text":"html"}},{"id":283954,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0450/pdf/sheet1.pdf"},{"id":283955,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0450/pdf/sheet2.pdf"},{"id":283956,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2003/0450/pdf/sheet3.pdf"}],"country":"United States","state":"California","city":"Watsonvilles","otherGeospatial":"Arano Flat;San Andreas Fault","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.022445,36.858232 ], [ -122.022445,37.08012 ], [ -121.566315,37.08012 ], [ -121.566315,36.858232 ], [ -122.022445,36.858232 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685e03","contributors":{"authors":[{"text":"Fumal, Thomas E.","contributorId":67882,"corporation":false,"usgs":true,"family":"Fumal","given":"Thomas","email":"","middleInitial":"E.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":246919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heingartner, Gordon F.","contributorId":11275,"corporation":false,"usgs":true,"family":"Heingartner","given":"Gordon","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":246916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Samrad, Laura","contributorId":83997,"corporation":false,"usgs":true,"family":"Samrad","given":"Laura","email":"","affiliations":[],"preferred":false,"id":246920,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dawson, Timothy E.","contributorId":24429,"corporation":false,"usgs":false,"family":"Dawson","given":"Timothy","email":"","middleInitial":"E.","affiliations":[{"id":7099,"text":"Calif. Geol. Survey","active":true,"usgs":false}],"preferred":false,"id":246917,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hamilton, John C. jhamilton@usgs.gov","contributorId":4202,"corporation":false,"usgs":true,"family":"Hamilton","given":"John","email":"jhamilton@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":246915,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Baldwin, John N.","contributorId":58551,"corporation":false,"usgs":true,"family":"Baldwin","given":"John","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":246918,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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