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,{"id":23393,"text":"ofr99211 - 1999 - Stream channel cross sections for a reach of the Boise River in Ada County, Idaho","interactions":[],"lastModifiedDate":"2014-05-05T14:35:06","indexId":"ofr99211","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-211","title":"Stream channel cross sections for a reach of the Boise River in Ada County, Idaho","docAbstract":"The Federal Emergency Management Agency produces maps of areas that are likely to be inundated during major floods, usually the 100-year, or 1-percent probability, flood. The maps, called Flood Insurance Rate Maps, are used to determine flood insurance rates for homes, businesses, or other structures located in flood-prone areas. State and local governments also use these maps for help with, among other things, development planning and disaster mitigation. During the period October 1997 through December 1998, the initial phase of a hydraulic analysis project of the Boise River from Barber Dam to the Ada/Canyon County boundary, the U.S. Geological Survey collected stream channel cross-section data at 238 locations along the river and documented 108 elevation reference marks established for horizontal and vertical control. In the final phase of the project, the Survey will use these data to determine water-surface elevations for the 10-, 50-, 100-, and 500-year floods and to define floodway limits. The Federal Emergency Management Agency will use the results of this hydraulic analysis to update the 100- and 500-year flood boundaries and the floodway limits on their Flood Insurance Rate Maps.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99211","issn":"0094-9140","collaboration":"Prepared in cooperation with Federal Emergency Management Agency, City of Boise, City of Garden City, City of Eagle, and Ada County","usgsCitation":"Hortness, J., and Werner, D.C., 1999, Stream channel cross sections for a reach of the Boise River in Ada County, Idaho: U.S. Geological Survey Open-File Report 99-211, Report: iv, 100 p.; Data files, https://doi.org/10.3133/ofr99211.","productDescription":"Report: iv, 100 p.; Data files","numberOfPages":"104","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":156210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0211/report-thumb.jpg"},{"id":52693,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0211/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":286888,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0211/data/"}],"country":"United States","state":"Idaho","county":"Ada","city":"Boise;Garden City;Eagle","otherGeospatial":"Barber Dam;Eagle Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.5141,43.3963 ], [ -116.5141,43.8075 ], [ -115.9742,43.8075 ], [ -115.9742,43.3963 ], [ -116.5141,43.3963 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50eb","contributors":{"authors":[{"text":"Hortness, Jon 0000-0002-9809-2876 hortness@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-2876","contributorId":3601,"corporation":false,"usgs":true,"family":"Hortness","given":"Jon","email":"hortness@usgs.gov","affiliations":[],"preferred":true,"id":190033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Werner, Douglas C.","contributorId":51783,"corporation":false,"usgs":true,"family":"Werner","given":"Douglas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":190034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23452,"text":"ofr99252 - 1999 - Summary of ground-water data for Tutuila and Aunuu, American Samoa, for October 1987 through September 1997","interactions":[],"lastModifiedDate":"2022-07-20T19:35:17.759622","indexId":"ofr99252","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-252","title":"Summary of ground-water data for Tutuila and Aunuu, American Samoa, for October 1987 through September 1997","docAbstract":"Ground-water and rainfall data for the period October 1987 through September 1997 from Tutuila and Aunuu, American Samoa, are plotted in time-series graphs and summarized. The data include pumpage and chloride concentrations from 53 production wells on Tutuila, including 5 new wells that were put into production between October 1996 and September 1997, 3 production wells on Aunuu, water-level measurements from 16 wells on Tutuila, and rainfall data from 2 gages on Tutuila. \r\n\r\nMean annual rainfall was 164 inches at the gage in Afono and 210 inches at the gage in Aasufou during the period October 1987 through September 1997. Rainfall in the 12-month period from October 1996 through September 1997 totaled 210 inches at the Afono gage and 234 inches at the Aasufou gage. \r\n\r\nIn the Tafuna-Leone Plain, most wells were pumped at rates from 0.2 to 0.5 million gallons per day and had chloride concentrations usually less than 500 milligrams per liter. In the 12-month period ending September 1997, the combined pumpage from wells in the Tafuna-Leone Plain was about 6.3 million gallons per day and the chloride concentrations in most wells remained below 200 milligrams per liter. In Aasufou, wells produced 0.04 to 0.05 million gallons per day and chloride concentrations remained near 15 milligrams per liter. \r\n\r\nMost wells in central and eastern Tutuila were pumped at rates less than 0.1 million gallons per day. Wells in the Fagatogo, Pago Pago, and Aua areas, which averaged more than 0.4 million gallons per day of pumpage, are exceptions. Some wells in central and eastern Tutuila had chloride concentrations that frequently exceeded 500 milligrams per liter. In the 12-month period ending September 1997, chloride concentrations in the production wells in Aua rose to the highest levels on record. In the 12-month period ending September 1997, water levels in Tafunafou, Iliili, Pago Pago, and Laulii remained at about the same elevation above mean sea level as in previous years, water levels in Aua remained below mean sea level as in previous years, and water levels in Malaeimi and Fagaalu declined relative to previous years. \r\n\r\nThe three production wells on Aunuu have been pumped at various rates less than 0.1 million gallons per day and had chloride concentrations usually in excess of 500 and often in excess of 1,000 milligrams per liter.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99252","usgsCitation":"Izuka, S.K., 1999, Summary of ground-water data for Tutuila and Aunuu, American Samoa, for October 1987 through September 1997: U.S. Geological Survey Open-File Report 99-252, v, 34 p., https://doi.org/10.3133/ofr99252.","productDescription":"v, 34 p.","temporalStart":"1987-10-01","temporalEnd":"1997-09-30","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":52772,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0252/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0252/report-thumb.jpg"},{"id":404155,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22523.htm","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"American Samoa, Aunuu, Tutuila","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -170.5400848388672,\n              -14.28235021221402\n            ],\n            [\n              -170.5689239501953,\n              -14.240424693263597\n            ],\n            [\n              -170.694580078125,\n              -14.232437996569354\n            ],\n            [\n              -170.74951171875,\n              -14.28035393582422\n            ],\n            [\n              -170.80993652343747,\n              -14.289004338957369\n            ],\n            [\n              -170.84976196289062,\n              -14.325598515691496\n            ],\n            [\n              -170.7550048828125,\n              -14.382141409410732\n            ],\n            [\n              -170.70213317871094,\n              -14.323602623438505\n            ],\n            [\n              -170.6671142578125,\n              -14.297654409469711\n            ],\n            [\n              -170.55450439453125,\n              -14.294327498647808\n            ],\n            [\n              -170.5400848388672,\n              -14.28235021221402\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699558","contributors":{"authors":[{"text":"Izuka, Scot K. 0000-0002-8758-9414 skizuka@usgs.gov","orcid":"https://orcid.org/0000-0002-8758-9414","contributorId":2645,"corporation":false,"usgs":true,"family":"Izuka","given":"Scot","email":"skizuka@usgs.gov","middleInitial":"K.","affiliations":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":190130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23221,"text":"ofr99207 - 1999 - A plan for assessing the occurrence and distribution of methyl tert-butyl ether and other volatile organic compounds in drinking water and ambient ground water in the Northeast and Mid-Atlantic regions of the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:07:56","indexId":"ofr99207","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-207","title":"A plan for assessing the occurrence and distribution of methyl tert-butyl ether and other volatile organic compounds in drinking water and ambient ground water in the Northeast and Mid-Atlantic regions of the United States","docAbstract":"A plan to assess the occurrence and distribution of methyl tert-butyl ether (MTBE) and other volatile organic compounds (VOCs) in drinking water and ambient ground water in the Northeast and Mid-Atlantic regions of the United States was designed to meet two primary objectives. This study will provide the U.S. Environmental Protection Agency with information on potential human exposure to MTBE and other VOCs from drinking water. In addition, the study will further the goals of the U.S. Geological Survey's (USGS) National Water Quality Assessment Program (NAWQA) by providing additional information on the occurrence and distribution of VOCs in ambient ground water beneath a large, highly urbanized part of the Nation. The study will proceed in two phases-a drinking-water assessment (phase 1) and an ambient ground-water assessment (phase 2). The drinking-water assessment will involve compilation, review, and analysis of available water- quality and ancillary data for approximately 20 percent of the community water systems in 12 States in the Northeast and Mid-Atlantic regions. This effort will summarize the occurrence and distribution of MTBE and other VOCs in drinking water supplied by 2,110 community water systems. The ambient ground-water assessment will involve compilation, review, and analysis of data on MTBE and other VOCs from previous USGS studies in the 12-State area, including regional water-quality assessments conducted for the USGS's NAWQA, plus other available State or local datasets. These data will be related, to the extent allowed by the completeness and quality of the data, to land-use patterns, population density, and other anthropogenic and natural factors using statistical tests. The occurrence and distribution of MTBE and other VOCs in ambient ground water and, to the extent possible, drinking water in relation to such factors, will be evaluated.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr99207","issn":"0094-9140","usgsCitation":"Grady, S.J., and Casey, G.D., 1999, A plan for assessing the occurrence and distribution of methyl tert-butyl ether and other volatile organic compounds in drinking water and ambient ground water in the Northeast and Mid-Atlantic regions of the United States: U.S. Geological Survey Open-File Report 99-207, iv, 36 p. :maps ;28 cm., https://doi.org/10.3133/ofr99207.","productDescription":"iv, 36 p. :maps ;28 cm.","costCenters":[],"links":[{"id":154397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0207/report-thumb.jpg"},{"id":52527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab79e","contributors":{"authors":[{"text":"Grady, Stephen J.","contributorId":101636,"corporation":false,"usgs":true,"family":"Grady","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":189666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Casey, George D.","contributorId":105689,"corporation":false,"usgs":true,"family":"Casey","given":"George","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":189667,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23567,"text":"ofr99192 - 1999 - Water-quality and bottom-sediment-chemistry data for Left Hand Valley Reservoir, Boulder County, Colorado, January-August 1998","interactions":[],"lastModifiedDate":"2022-10-07T18:55:08.483236","indexId":"ofr99192","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-192","title":"Water-quality and bottom-sediment-chemistry data for Left Hand Valley Reservoir, Boulder County, Colorado, January-August 1998","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99192","usgsCitation":"Kimbrough, R.A., 1999, Water-quality and bottom-sediment-chemistry data for Left Hand Valley Reservoir, Boulder County, Colorado, January-August 1998: U.S. Geological Survey Open-File Report 99-192, iv, 29 p., https://doi.org/10.3133/ofr99192.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":408103,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19418.htm","linkFileType":{"id":5,"text":"html"}},{"id":52856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0192/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0192/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Boulder County","otherGeospatial":"Left Hand Valley Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.274,\n              40.092\n            ],\n            [\n              -105.258,\n              40.092\n            ],\n            [\n              -105.258,\n              40.108\n            ],\n            [\n              -105.274,\n              40.108\n            ],\n            [\n              -105.274,\n              40.092\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e72a4","contributors":{"authors":[{"text":"Kimbrough, R. A.","contributorId":21150,"corporation":false,"usgs":true,"family":"Kimbrough","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":190329,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24599,"text":"ofr99311 - 1999 - Subduction zone and crustal dynamics of western Washington; a tectonic model for earthquake hazards evaluation","interactions":[],"lastModifiedDate":"2017-03-09T14:50:33","indexId":"ofr99311","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-311","title":"Subduction zone and crustal dynamics of western Washington; a tectonic model for earthquake hazards evaluation","docAbstract":"The Cascadia subduction zone is extremely complex in the western Washington region, involving local deformation of the subducting Juan de Fuca plate and complicated block structures in the crust. It has been postulated that the Cascadia subduction zone could be the source for a large thrust earthquake, possibly as large as M9.0. Large intraplate earthquakes from within the subducting Juan de Fuca plate beneath the Puget Sound region have accounted for most of the energy release in this century and future such large earthquakes are expected. Added to these possible hazards is clear evidence for strong crustal deformation events in the Puget Sound region near faults such as the Seattle fault, which passes through the southern Seattle metropolitan area. In order to understand the nature of these individual earthquake sources and their possible interrelationship, we have conducted an extensive seismotectonic study of the region. We have employed P-wave velocity models developed using local earthquake tomography as a key tool in this research. Other information utilized includes geological, paleoseismic, gravity, magnetic, magnetotelluric, deformation, seismicity, focal mechanism and geodetic data. Neotectonic concepts were tested and augmented through use of anelastic (creep) deformation models based on thin-plate, finite-element techniques developed by Peter Bird, UCLA. These programs model anelastic strain rate, stress, and velocity fields for given rheological parameters, variable crust and lithosphere thicknesses, heat flow, and elevation. Known faults in western Washington and the main Cascadia subduction thrust were incorporated in the modeling process.\r\n\r\nSignificant results from the velocity models include delineation of a previously studied arch in the subducting Juan de Fuca plate. The axis of the arch is oriented in the direction of current subduction and asymmetrically deformed due to the effects of a northern buttress mapped in the velocity models. This buttress occurs under the North Cascades region of Washington and under southern Vancouver Island. We find that regional faults zones such as the Devils Mt. and Darrington zones follow the margin of this buttress and the Olympic-Wallowa lineament forms its southern boundary east of the Puget Lowland. Thick, high-velocity, lower-crustal rocks are interpreted to be a mafic/ultramafic wedge occuring just above the subduction thrust. This mafic wedge appears to be jointly deformed with the arch, suggesting strong coupling between the subducting plate and upper plate crust in the Puget Sound region at depths >30 km. Such tectonic coupling is possible if brittle-ductile transition temperatures for mafic/ultramafic rocks on both sides of the thrust are assumed.\r\n\r\nThe deformation models show that dominant north-south compression in the coast ranges of Washington and Oregon is controlled by a highly mafic crust and low heat flow, allowing efficient transmission of margin-parallel shear from Pacific plate interaction with North America. Complex stress patterns which curve around the Puget Sound region require a concentration of northwest-directed shear in the North Cascades of Washington. The preferred model shows that greatest horizontal shortening occurs across the Devils Mt. fault zone and the east end of the Seattle fault.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99311","issn":"0094-9140","usgsCitation":"Stanley, D., Villasenor, A.H., and Benz, H., 1999, Subduction zone and crustal dynamics of western Washington; a tectonic model for earthquake hazards evaluation: U.S. Geological Survey Open-File Report 99-311, 90 p., https://doi.org/10.3133/ofr99311.","productDescription":"90 p.","costCenters":[],"links":[{"id":155455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0311/report-thumb.jpg"},{"id":53648,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0311/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1631,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/ofr-99-0311/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699bf5","contributors":{"authors":[{"text":"Stanley, Dal","contributorId":71205,"corporation":false,"usgs":true,"family":"Stanley","given":"Dal","email":"","affiliations":[],"preferred":false,"id":192228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Villasenor, Antonio H. 0000-0001-8592-4832","orcid":"https://orcid.org/0000-0001-8592-4832","contributorId":38186,"corporation":false,"usgs":true,"family":"Villasenor","given":"Antonio","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":192227,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benz, Harley","contributorId":91460,"corporation":false,"usgs":true,"family":"Benz","given":"Harley","affiliations":[],"preferred":false,"id":192229,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":22801,"text":"ofr99307 - 1999 - Archive of seismic-reflection data collected aboard RV CORLISS cruise CRLS98014 in the Columbia River estuary, Willapa Bay, and off southern Washington inner continental shelf","interactions":[],"lastModifiedDate":"2017-01-18T10:11:06","indexId":"ofr99307","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-307","title":"Archive of seismic-reflection data collected aboard RV CORLISS cruise CRLS98014 in the Columbia River estuary, Willapa Bay, and off southern Washington inner continental shelf","language":"ENGLISH","publisher":"U.S. Geological Survey, Marine and Coastal Geology Program, Woods Hole Section,","doi":"10.3133/ofr99307","issn":"0094-9140","isbn":"060792831X","usgsCitation":"Cross, V., Twichell, D., and Parolski, K.F., 1999, Archive of seismic-reflection data collected aboard RV CORLISS cruise CRLS98014 in the Columbia River estuary, Willapa Bay, and off southern Washington inner continental shelf: U.S. Geological Survey Open-File Report 99-307, 3 computer optical discs :col. ill., col. ports., col. map ;4 3/4 in., in plastic envelope (13 x 14 cm.), https://doi.org/10.3133/ofr99307.","productDescription":"3 computer optical discs :col. ill., col. ports., col. map ;4 3/4 in., in plastic envelope (13 x 14 cm.)","costCenters":[],"links":[{"id":155690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":333318,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0307/ofr99307_1.zip","text":"Disc 1","linkFileType":{"id":6,"text":"zip"}},{"id":333319,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0307/ofr99307_2.zip","text":"Disc 2","linkFileType":{"id":6,"text":"zip"}},{"id":333320,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0307/ofr99307_3.zip","text":"Disc 3","linkFileType":{"id":6,"text":"zip"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679c8c","contributors":{"authors":[{"text":"Cross, V.A.","contributorId":88687,"corporation":false,"usgs":true,"family":"Cross","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":188898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Twichell, D.C.","contributorId":84304,"corporation":false,"usgs":true,"family":"Twichell","given":"D.C.","affiliations":[],"preferred":false,"id":188897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Parolski, K. F.","contributorId":99173,"corporation":false,"usgs":true,"family":"Parolski","given":"K.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":188899,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":24276,"text":"ofr99201 - 1999 - Plan of study to define hydrogeologic characteristics of the Madera Limestone in the east mountain area of central New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr99201","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-201","title":"Plan of study to define hydrogeologic characteristics of the Madera Limestone in the east mountain area of central New Mexico","docAbstract":"The east mountain area of central New Mexico includes the \r\neastern one-third of Bernalillo County and portions of Sandoval, \r\nSanta Fe, and Torrance Counties. The area covers about 320 square \r\nmiles.\r\n\r\nThe Madera Limestone, the principal aquifer in the east mountain \r\narea, is the sole source of water for domestic, municipal, \r\nindustrial, and agricultural uses for many residents. Some water is \r\nimported from wells near Edgewood by the Entranosa Water \r\nCooperative, which serves a population of approximately 3,300. \r\nThe remaining population is served by small water systems that derive \r\nsupplies locally or by individually owned domestic wells.\r\n\r\nThe population of the east mountain area has increased \r\ndramatically over the past 20 years. In 1970, the population of \r\nthe east mountain area was about 4,000. Demographic projections \r\nsuggest that approximately 1,000 people per year are moving into \r\nthe area, and with a growth rate of 3.0 percent the population will \r\nbe 16,700 in 2000. Consequently, ground-water withdrawals have \r\nincreased substantially over the past 20 years, and will continue \r\nto increase.\r\n\r\nLittle is known about the flow characteristics and hydrogeologic \r\nproperties of the Madera Limestone. This report describes \r\nexisting information about the geologic and hydrologic framework \r\nand flow characteristics of the Madera Limestone, and presents a \r\nplan of study for data-collection activities and interpretive \r\nstudies that could be conducted to better define the hydrogeologic \r\ncharacteristics of the Madera Limestone.\r\n\r\nData-collection activities and interpretive studies related \r\nto the hydrogeologic components of the Madera Limestone are \r\nprioritized. Activities that are necessary to improve the \r\nquantification of a component are prioritized as essential. \r\nActivities that could add additional understanding of a \r\ncomponent, but would not be necessary to improve the \r\nquantification of a component, are prioritized as useful.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr99201","issn":"0094-9140","usgsCitation":"Rankin, D., 1999, Plan of study to define hydrogeologic characteristics of the Madera Limestone in the east mountain area of central New Mexico: U.S. Geological Survey Open-File Report 99-201, v, 44 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr99201.","productDescription":"v, 44 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":155031,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0201/report-thumb.jpg"},{"id":53398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0201/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855f0","contributors":{"authors":[{"text":"Rankin, D.R.","contributorId":28991,"corporation":false,"usgs":true,"family":"Rankin","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":191618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24211,"text":"ofr99247 - 1999 - Data on the crystal growth of calcite from calcium bicarbonate solutions at 34 degrees C and CO<sub>2</sub> partial pressures of 0.101, 0.0156 and 0.00102 atmospheres","interactions":[],"lastModifiedDate":"2020-03-23T19:03:33","indexId":"ofr99247","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-247","title":"Data on the crystal growth of calcite from calcium bicarbonate solutions at 34 degrees C and CO<sub>2</sub> partial pressures of 0.101, 0.0156 and 0.00102 atmospheres","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99247","issn":"0094-9140","usgsCitation":"Plummer, N., and Busenberg, E., 1999, Data on the crystal growth of calcite from calcium bicarbonate solutions at 34 degrees C and CO<sub>2</sub> partial pressures of 0.101, 0.0156 and 0.00102 atmospheres: U.S. Geological Survey Open-File Report 99-247, 13 p. , https://doi.org/10.3133/ofr99247.","productDescription":"13 p. ","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":155542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0247/report-thumb.jpg"},{"id":53350,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7c6","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":191496,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Busenberg, Eurybiades ebusenbe@usgs.gov","contributorId":2271,"corporation":false,"usgs":true,"family":"Busenberg","given":"Eurybiades","email":"ebusenbe@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":191495,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24174,"text":"ofr99310 - 1999 - Thickness of Cenozoic Deposits of Yucca Flat Inferred from Gravity Data, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr99310","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-310","title":"Thickness of Cenozoic Deposits of Yucca Flat Inferred from Gravity Data, Nevada Test Site, Nevada","docAbstract":"The basin-basement contact for Yucca Flat was modeled using isostatic gravity data, a linear density-depth function for the basin deposits, and drill-hole constraints to produce a digital database of both the depth to basement and the gravitational anomaly associated with the basement rocks. The model predicts a depth of roughly 2,500 m in the deepest, southern part of the basin. The model shows offsets in the basement rocks along both the Carpetbag and Yucca faults. The basement rocks of Yucca Flat have a higher gravity anomaly west of the N-S trending Carpetbag fault, suggesting higher density rocks on the west side of the valley.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99310","issn":"0094-9140","usgsCitation":"Phelps, G.A., Langenheim, V., and Jachens, R., 1999, Thickness of Cenozoic Deposits of Yucca Flat Inferred from Gravity Data, Nevada Test Site, Nevada: U.S. Geological Survey Open-File Report 99-310, Report: 33 p.; Data Files, https://doi.org/10.3133/ofr99310.","productDescription":"Report: 33 p.; Data Files","additionalOnlineFiles":"Y","costCenters":[{"id":671,"text":"Western Region Geology and Geophysics Science Center","active":false,"usgs":true}],"links":[{"id":155482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":13133,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/of99-310/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.75,36.5 ], [ -116.75,37.5 ], [ -115.75,37.5 ], [ -115.75,36.5 ], [ -116.75,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4a31","contributors":{"authors":[{"text":"Phelps, G. A.","contributorId":67107,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":191448,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langenheim, V.E. 0000-0003-2170-5213","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":54956,"corporation":false,"usgs":true,"family":"Langenheim","given":"V.E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":191446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jachens, R.C.","contributorId":55433,"corporation":false,"usgs":true,"family":"Jachens","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":191447,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21790,"text":"ofr99304 - 1999 - Gas and Isotope Geochemistry of 81 Steam Samples from Wells in The Geysers Geothermal Field, Sonoma and Lake Counties, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr99304","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-304","title":"Gas and Isotope Geochemistry of 81 Steam Samples from Wells in The Geysers Geothermal Field, Sonoma and Lake Counties, California","docAbstract":"The Geysers geothermal field in northern California,\r\nwith about 2000-MW electrical capacity, is the largest geothermal\r\nfield in the world. Despite its importance as a resource\r\nand as an example of a vapor-dominated reservoir,\r\nvery few complete geochemical analyses of the steam have\r\nbeen published (Allen and Day, 1927; Truesdell and others,\r\n1987). This report presents data from 90 steam, gas, and condensate\r\nsamples from wells in The Geysers geothermal field\r\nin northern California. Samples were collected between 1978\r\nand 1991. Well attributes include sampling date, well name,\r\nlocation, total depth, and the wellhead temperature and pressure\r\nat which the sample was collected. Geochemical characteristics\r\ninclude the steam/gas ratio, composition of noncondensable\r\ngas (relative proportions of CO2, H2S, He, H2,\r\nO2, Ar, N2, CH4, and NH3), and isotopic values for deltaD and\r\ndelta18O of H2O, delta13C of CO2, and delta34S of H2S. The compilation\r\nincludes 81 analyses from 74 different production wells, 9\r\nisotopic analyses of steam condensate pumped into injection\r\nwells, and 5 complete geochemical analyses on gases from\r\nsurface fumaroles and bubbling pools.\r\nMost samples were collected as saturated steam and\r\nplot along the liquid-water/steam boiling curve. Steam-togas\r\nratios are highest in the southeastern part of the geothermal\r\nfield and lowest in the northwest, consistent with other\r\nstudies. Wells in the Northwest Geysers are also enriched in\r\nN2/Ar, CO2 and CH4, deltaD, and delta18O. Well discharges from the\r\nSoutheast Geysers are high in steam/gas and have isotopic\r\ncompositions and N2/Ar ratios consistent with recharge by\r\nlocal meteoric waters. Samples from the Central Geysers\r\nshow characteristics found in both the Southeast and Northwest\r\nGeysers.\r\nGas and steam characteristics of well discharges from\r\nthe Northwest Geysers are consistent with input of components\r\nfrom a high-temperature reservoir containing carbonrich\r\ngases derived from the host Franciscan rocks. Throughout\r\nthe geothermal field, the carbon-isotopic composition of\r\nCO2 is consistent with derivation of carbon from Franciscan\r\nmetasedimentary rocks. NH3 concentrations are high in most\r\nGeysers well fluids, and are 2-3 orders of magnitude greater\r\nthan would be expected in a the gas phase exhibiting homogeneous\r\nequilibrium at normal reservoir temperatures and\r\npressures. Evidently, NH3 is flushed from the Franciscan host\r\nrocks at a rate that exceeds the reaction rate for NH3 breakdown.\r\nMany wells show clear influence by fluids from reinjection\r\nwells where steam condensate has been pumped\r\nback into the geothermal reservoir. Six wells were resampled\r\nover the time period of this study. One of these six wells was\r\nstrongly affected by a nearby injection well. Three of the six\r\nresampled wells showed some signs of decreasing liquid/\r\nsteam within the geothermal reservoir, consistent with 'drying\r\nout' of the reservoir due to steam withdrawal. However,\r\ntwo wells exhibited little change.\r\nAnalyses of gases from five surface manifestations (fumaroles\r\nand bubbling pools) are roughly similar to the deeper\r\ngeothermal samples in both chemical and isotopic composition,\r\nbut are lower in soluble gases that dissolve in groundwater\r\nduring transit toward the surface.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99304","issn":"0566-8174","usgsCitation":"Lowenstern, J.B., Janik, C.J., Fahlquist, L., and Johnson, L.S., 1999, Gas and Isotope Geochemistry of 81 Steam Samples from Wells in The Geysers Geothermal Field, Sonoma and Lake Counties, California (Version 1.0): U.S. Geological Survey Open-File Report 99-304, Report: 28 p.; Data Tables (xls), https://doi.org/10.3133/ofr99304.","productDescription":"Report: 28 p.; Data Tables (xls)","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":124928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_99_304.jpg"},{"id":13356,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/of99-304/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.91666666666667,38.700833333333335 ], [ -122.91666666666667,38.8675 ], [ -122.66666666666667,38.8675 ], [ -122.66666666666667,38.700833333333335 ], [ -122.91666666666667,38.700833333333335 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1349","contributors":{"authors":[{"text":"Lowenstern, Jacob B. 0000-0003-0464-7779 jlwnstrn@usgs.gov","orcid":"https://orcid.org/0000-0003-0464-7779","contributorId":2755,"corporation":false,"usgs":true,"family":"Lowenstern","given":"Jacob","email":"jlwnstrn@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":185685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janik, Cathy J.","contributorId":87090,"corporation":false,"usgs":true,"family":"Janik","given":"Cathy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":185687,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fahlquist, Lynne","contributorId":8810,"corporation":false,"usgs":true,"family":"Fahlquist","given":"Lynne","affiliations":[],"preferred":false,"id":185686,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, Linda S.","contributorId":94334,"corporation":false,"usgs":true,"family":"Johnson","given":"Linda","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":185688,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":21825,"text":"ofr99136 - 1999 - Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska","interactions":[{"subject":{"id":70180394,"text":"70180394 - 1999 - Geology of Unga Island and the northwestern part of Popof Island: Chapter 2 in <i>A geological and geophysical study of the gold-silver vein system of Unga Island, Southwestern Alaska</i>","indexId":"70180394","publicationYear":"1999","noYear":false,"chapter":"2","title":"Geology of Unga Island and the northwestern part of Popof Island: Chapter 2 in <i>A geological and geophysical study of the gold-silver vein system of Unga Island, Southwestern Alaska</i>"},"predicate":"IS_PART_OF","object":{"id":21825,"text":"ofr99136 - 1999 - Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska","indexId":"ofr99136","publicationYear":"1999","noYear":false,"title":"Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska"},"id":1},{"subject":{"id":70180395,"text":"70180395 - 1999 - Rock, stream sediment, and heavy-mineral concentrate geochemical data from Unga and western Popof Islands, Alaska Peninsula, Alaska: Chapter 6 in <i>A geological and geophysical study of the gold-silver vein system of Unga Island, Southwestern Alaska</i>","indexId":"70180395","publicationYear":"1999","noYear":false,"chapter":"6","title":"Rock, stream sediment, and heavy-mineral concentrate geochemical data from Unga and western Popof Islands, Alaska Peninsula, Alaska: Chapter 6 in <i>A geological and geophysical study of the gold-silver vein system of Unga Island, Southwestern Alaska</i>"},"predicate":"IS_PART_OF","object":{"id":21825,"text":"ofr99136 - 1999 - Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska","indexId":"ofr99136","publicationYear":"1999","noYear":false,"title":"Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska"},"id":2}],"lastModifiedDate":"2021-09-08T21:48:30.180266","indexId":"ofr99136","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-136","title":"Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska","docAbstract":"<p>The topic of this CD-ROM is the geologic framework of gold-silver vein deposits on Unga Island, in the Shumagin Islands, southwestern Alaska. The core of the publication is a new geologic map at a scale of 1:63,360 and aeromagnetic and electromagnetic survey data acquired by industry over the area of mineralization. Both the geologic map as well as a preliminary interpretation of the geophysical data - which are included by permission of the owner - are aimed towards deciphering the relations among volcanism, tectonism, and mineralization. Data and discussions are organized in seven chapters, titles of which are outlined in the table of contents. The chapters consist of viewable text and figure images; postscript versions of the frontispiece figures and all chapter figures are included on the CD-ROM as well. The geologic map is a large viewable figure (Plate 1) that accompanies chapter 2. The map was constructed in ARC and its component coverages are provided in the folder 'Geology' for users who may wish to modify the geologic data or add their own data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Anchorage, AK","doi":"10.3133/ofr99136","issn":"0566-8174","isbn":"0607926546","usgsCitation":"1999, Geological and geophysical setting of the gold-silver vein systems of Unga Island, southwestern Alaska (Version 1.3): U.S. Geological Survey Open-File Report 99-136, 6 p.; CD-ROM, https://doi.org/10.3133/ofr99136.","productDescription":"6 p.; CD-ROM","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334270,"rank":4,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/of/1999/of99-136/version_history.txt"},{"id":334269,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/of99-136/of99-136.pdf","text":"Introduction, with links to chapters","size":"138 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":9306,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/of99-136/","linkFileType":{"id":5,"text":"html"}},{"id":154280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Unga Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -160.90576171875,\n              55.11608453987679\n            ],\n            [\n              -160.44708251953125,\n              55.11608453987679\n            ],\n            [\n              -160.44708251953125,\n              55.41342553237579\n            ],\n            [\n              -160.90576171875,\n              55.41342553237579\n            ],\n            [\n              -160.90576171875,\n              55.11608453987679\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.3","publicComments":"Originally published as a CD-ROM; the files are now available online","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae655","contributors":{"editors":[{"text":"Riehle, James R.","contributorId":70048,"corporation":false,"usgs":true,"family":"Riehle","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":661517,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":21848,"text":"ofr99303 - 1999 - Gravity and magnetic study of the Pahute Mesa and Oasis Valley region, Nye County, Nevada","interactions":[],"lastModifiedDate":"2023-06-15T15:34:31.955449","indexId":"ofr99303","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-303","title":"Gravity and magnetic study of the Pahute Mesa and Oasis Valley region, Nye County, Nevada","docAbstract":"Regional gravity and aeromagnetic maps reveal the existence of deep basins underlying much of the southwestern Nevada volcanic field, approximately 150 km northwest of Las Vegas. These maps also indicate the presence of prominent features (geophysical lineaments) within and beneath the basin fill. Detailed gravity surveys were conducted in order to characterize the nature of the basin boundaries, delineate additional subsurface features, and evaluate their possible influence on the movement of ground-water. Geophysical modeling of gravity and aeromagnetic data indicates that many of the features may be related to processes of caldera formation. Collapse of the various calderas within the volcanic field resulted in dense basement rocks occurring at greater depths within caldera boundaries. Modeling indicates that collapse occurred along faults that are arcuate and steeply dipping. There are indications that the basement in the western Pahute Mesa - Oasis Valley region consists predominantly of granitic and/or fine-grained siliceous sedimentary rocks that may be less permeable to groundwater flow than the predominantly fractured carbonate rock basement to the east and southeast of the study area. The northeast-trending Thirsty Canyon lineament, expressed on gravity and basin thickness maps, separates dense volcanic rocks on the northwest from less dense intracaldera accumulations in the Silent Canyon and Timber Mountain caldera complexes. The source of the lineament is an approximately 2-km wide ring fracture system with step-like differential displacements, perhaps localized on a pre-existing northeast-trending Basin and Range fault. Due to vertical offsets, the Thirsty Canyon fault zone probably juxtaposes rock types of different permeability and, thus, it may act as a barrier to ground-water flow and deflect flow from Pahute Mesa along its flanks toward Oasis Valley. Within the Thirsty Canyon fault zone, highly fractured rocks may serve also as a conduit, depending upon the degree of alteration and its effect on porosity and permeability. In the Oasis Valley region, other structures that may influence ground-water flow include the western and southern boundaries of the Oasis Valley basin, where the basement abruptly shallows.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99303","issn":"0566-8174","collaboration":"Prepared in cooperation with the U.S. Department of Energy Nevada Operations Office (Interagency Agreement DE-AI08-96NV11967)","usgsCitation":"Mankinen, E.A., Hildenbrand, T.G., Dixon, G.L., McKee, E.H., Fridrich, C.J., and Laczniak, R.J., 1999, Gravity and magnetic study of the Pahute Mesa and Oasis Valley region, Nye County, Nevada: U.S. Geological Survey Open-File Report 99-303, 58 p., https://doi.org/10.3133/ofr99303.","productDescription":"58 p.","additionalOnlineFiles":"N","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":51332,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0303/pdf/of99-303.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":153182,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0303/report-thumb.jpg"},{"id":1241,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0303/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.1972,35.9618 ], [ -118.1972,39.1634 ], [ -114.999,39.1634 ], [ -114.999,35.9618 ], [ -118.1972,35.9618 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5f18e4b0b290850fc1db","contributors":{"authors":[{"text":"Mankinen, Edward A. 0000-0001-7496-2681 emank@usgs.gov","orcid":"https://orcid.org/0000-0001-7496-2681","contributorId":1054,"corporation":false,"usgs":true,"family":"Mankinen","given":"Edward","email":"emank@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":185954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hildenbrand, Thomas G.","contributorId":61787,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"Thomas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":185958,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dixon, Gary L.","contributorId":23571,"corporation":false,"usgs":true,"family":"Dixon","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":185957,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":185956,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fridrich, Christopher J. 0000-0003-2453-6478 fridrich@usgs.gov","orcid":"https://orcid.org/0000-0003-2453-6478","contributorId":1251,"corporation":false,"usgs":true,"family":"Fridrich","given":"Christopher","email":"fridrich@usgs.gov","middleInitial":"J.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":185955,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Laczniak, Randell J.","contributorId":90687,"corporation":false,"usgs":true,"family":"Laczniak","given":"Randell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":185959,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":21983,"text":"ofr99193 - 1999 - New reporting procedures based on long-term method detection levels and some considerations for interpretations of water-quality data provided by the U.S. Geological Survey National Water Quality Laboratory","interactions":[],"lastModifiedDate":"2021-05-28T16:48:14.195107","indexId":"ofr99193","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-193","title":"New reporting procedures based on long-term method detection levels and some considerations for interpretations of water-quality data provided by the U.S. Geological Survey National Water Quality Laboratory","docAbstract":"<p>This report describes the U.S. Geological Survey National Water Quality Laboratory's approach for determining long-term method detection levels and establishing reporting levels, details relevant new reporting conventions, and provides preliminary guidance on interpreting data reported with the new conventions. At the long-term method detection level concentration, the risk of a false positive detection (analyte reported present at the long-term method detection level when not in sample) is no more than 1 percent. However, at the long-term method detection level, the risk of a false negative occurrence (analyte reported not present when present at the long-term method detection level concentration) is up to 50 percent. Because this false negative rate is too high for use as a default 'less than' reporting level, a more reliable laboratory reporting level is set at twice the determined long-term method detection level. For all methods, concentrations measured between the laboratory reporting level and the long-term method detection level will be reported as estimated concentrations. Non-detections will be censored to the laboratory reporting level. Adoption of the new reporting conventions requires a full understanding of how low-concentration data can be used and interpreted and places responsibility for using and presenting final data with the user rather than with the laboratory. Users must consider that (1) new laboratory reporting levels may differ from previously established minimum reporting levels, (2) long-term method detection levels and laboratory reporting levels may change over time, and (3) estimated concentrations are less certain than concentrations reported above the laboratory reporting level. The availability of uncensored but qualified low-concentration data for interpretation and statistical analysis is a substantial benefit to the user. A decision to censor data after they are reported from the laboratory may still be made by the user, if merited, on the basis of the intended use of the data.</p>","language":"English","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr99193","usgsCitation":"Childress, C., Foreman, W., Connor, B.F., and Maloney, T.J., 1999, New reporting procedures based on long-term method detection levels and some considerations for interpretations of water-quality data provided by the U.S. Geological Survey National Water Quality Laboratory: U.S. Geological Survey Open-File Report 99-193, iv, 19 p., https://doi.org/10.3133/ofr99193.","productDescription":"iv, 19 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":154299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0193/report-thumb.jpg"},{"id":51455,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0193/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":1165,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/owq/OFR_99-193/index.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69752a","contributors":{"authors":[{"text":"Childress, Carolyn J. Oblinger","contributorId":57514,"corporation":false,"usgs":true,"family":"Childress","given":"Carolyn J. Oblinger","affiliations":[],"preferred":false,"id":186548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foreman, William T. wforeman@usgs.gov","contributorId":1473,"corporation":false,"usgs":true,"family":"Foreman","given":"William T.","email":"wforeman@usgs.gov","affiliations":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"preferred":false,"id":186545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connor, Brooke F. bfconnor@usgs.gov","contributorId":3172,"corporation":false,"usgs":true,"family":"Connor","given":"Brooke","email":"bfconnor@usgs.gov","middleInitial":"F.","affiliations":[],"preferred":true,"id":186546,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maloney, Thomas J.","contributorId":35736,"corporation":false,"usgs":true,"family":"Maloney","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":186547,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":22081,"text":"ofr99302 - 1999 - Publications of the Western Geologic Mapping Team 1997-1998","interactions":[],"lastModifiedDate":"2023-06-15T15:35:30.745064","indexId":"ofr99302","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-302","title":"Publications of the Western Geologic Mapping Team 1997-1998","docAbstract":"The Western Geologic Mapping Team (WGMT) of the U.S. Geological Survey, Geologic Division (USGS, GD), conducts geologic mapping and related topical earth-science studies in the western United States. This work is focused on areas where modern geologic maps and associated earth-science data are needed to address key societal and environmental issues such as ground-water quality, potential geologic hazards, and land-use decisions. Areas of primary emphasis currently include southern California, the San Francisco Bay region, the Pacific Northwest, the Las Vegas urban corridor, and selected National Park lands. The team has its headquarters in Menlo Park, California, and maintains smaller field offices at several other locations in the western United States.\n\nThe results of research conducted by the WGMT are released to the public as a variety of databases, maps, text reports, and abstracts, both through the internal publication system of the USGS and in diverse external publications such as scientific journals and books. This report lists publications of the WGMT released in calendar years 1997 and 1998. Most of the publications listed were authored or coauthored by WGMT staff. However, the list also includes some publications authored by formal non-USGS cooperators with the WGMT, as well as some authored by USGS staff outside the WGMT in cooperation with WGMT projects.\n\nSeveral of the publications listed are available on the World Wide Web; for these, URL addresses are provided. Most of these Web publications are USGS open-file reports that contain large digital databases of geologic map and related information. For these, the bibliographic citation refers specifically to an explanatory pamphlet containing information about the content and accessibility of the database, not to the actual map or related information comprising the database itself.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99302","issn":"0094-9140","usgsCitation":"Stone, P., and Powell, C., 1999, Publications of the Western Geologic Mapping Team 1997-1998: U.S. Geological Survey Open-File Report 99-302, 27 p., https://doi.org/10.3133/ofr99302.","productDescription":"27 p.","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":51523,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0302/pdf/of99-302.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0302/report-thumb.jpg"},{"id":1198,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0302/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6e86e4b0b29085105d64","contributors":{"authors":[{"text":"Stone, Paul 0000-0002-1439-0156 pastone@usgs.gov","orcid":"https://orcid.org/0000-0002-1439-0156","contributorId":273,"corporation":false,"usgs":true,"family":"Stone","given":"Paul","email":"pastone@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":186989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, C.L. II","contributorId":93520,"corporation":false,"usgs":true,"family":"Powell","given":"C.L.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":186990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22599,"text":"ofr99189 - 1999 - Summary of suspended-solids concentration data, San Francisco Bay, California, water year 1997","interactions":[],"lastModifiedDate":"2016-07-26T16:36:18","indexId":"ofr99189","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-189","title":"Summary of suspended-solids concentration data, San Francisco Bay, California, water year 1997","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ; Information Services [distributor],","doi":"10.3133/ofr99189","issn":"0094-9140","collaboration":"Prepared in cooperation with the San Francisco Regional Water Quality Control Board, and the U.S. Army Corps of Engineers","usgsCitation":"Buchanan, P.A., and Schoellhamer, D., 1999, Summary of suspended-solids concentration data, San Francisco Bay, California, water year 1997: U.S. Geological Survey Open-File Report 99-189, vi, 52 p. ill., map; 28 cm., https://doi.org/10.3133/ofr99189.","productDescription":"vi, 52 p. ill., map; 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1996-10-01","temporalEnd":"1997-09-30","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":124843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_99_189.bmp"},{"id":14638,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/189/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5486","contributors":{"authors":[{"text":"Buchanan, Paul A. 0000-0002-4796-4734 buchanan@usgs.gov","orcid":"https://orcid.org/0000-0002-4796-4734","contributorId":1018,"corporation":false,"usgs":true,"family":"Buchanan","given":"Paul","email":"buchanan@usgs.gov","middleInitial":"A.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":188546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoellhamer, David H. 0000-0001-9488-7340 dschoell@usgs.gov","orcid":"https://orcid.org/0000-0001-9488-7340","contributorId":631,"corporation":false,"usgs":true,"family":"Schoellhamer","given":"David H.","email":"dschoell@usgs.gov","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":188545,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22591,"text":"ofr99183 - 1999 - Hydrologic and water-quality data for surface water, ground water, and springs in north-central Park County, Colorado, April 1997–November 1998","interactions":[],"lastModifiedDate":"2022-01-20T19:35:28.83401","indexId":"ofr99183","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-183","title":"Hydrologic and water-quality data for surface water, ground water, and springs in north-central Park County, Colorado, April 1997–November 1998","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99183","issn":"0094-9140","usgsCitation":"Bruce, B.W., and Kimbrough, R.A., 1999, Hydrologic and water-quality data for surface water, ground water, and springs in north-central Park County, Colorado, April 1997–November 1998: U.S. Geological Survey Open-File Report 99-183, iv, 37 p., https://doi.org/10.3133/ofr99183.","productDescription":"iv, 37 p.","costCenters":[],"links":[{"id":394605,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19547.htm"},{"id":52066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0183/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1999/0183/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Park County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.9170,\n              39.1920\n            ],\n            [\n              -105.75,\n              39.1920\n            ],\n            [\n              -105.75,\n              39.4190\n            ],\n            [\n              -105.9170,\n              39.4190\n            ],\n            [\n              -105.9170,\n              39.1920\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db61172f","contributors":{"authors":[{"text":"Bruce, B. W.","contributorId":19577,"corporation":false,"usgs":true,"family":"Bruce","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":188526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimbrough, R. A.","contributorId":21150,"corporation":false,"usgs":true,"family":"Kimbrough","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":188527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22236,"text":"ofr99196 - 1999 - U.S. Geological Survey programs in Florida, 1999","interactions":[],"lastModifiedDate":"2012-02-02T00:08:04","indexId":"ofr99196","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-196","title":"U.S. Geological Survey programs in Florida, 1999","docAbstract":"The safety, health, and economic well-being of Florida?s citizens are important to the U.S. Geological Survey (USGS), which is involved in water-related, geologic, biological, land use, and mapping issues in many parts of the State. The USGS office in Tallahassee acts as the liaison for all studies conducted by USGS scientists in Florida. Water resources activities are conducted not only from the office in Tallahassee, but also from offices in Miami, Tampa, and Altamonte Springs (Orlando). Scientists in these offices investigate surface water, ground water and water quality in Florida, working in cooperation with other Federal, State and local agencies and organizations. \rThe USGS Center for Coastal Geology and Regional Marine Studies was established in St. Petersburg in 1988, in cooperation with the University of South Florida. The Center conducts a wide variety of research on mineral resources and on coastal and regional marine problems, including coastal erosion, climate change, wetlands deterioration, and coastal pollution. A USGS mapping office is located in St. Petersburg. Also, the Earth Science Information Center (ESIC) in Tallahassee provides USGS information to customers and directs inquiries to the appropriate USGS office or State agency on earth science topics, particularly those related to cartography, geography, aerial photography, and digital data. Biologists at the USGS Florida Caribbean Science Center, located in Gainesville, conduct biological and ecosystem studies in Florida, Puerto Rico, and the Virgin Islands. ","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr99196","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1999, U.S. Geological Survey programs in Florida, 1999: U.S. Geological Survey Open-File Report 99-196, 4 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/ofr99196.","productDescription":"4 p. :col. ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":1318,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr99-196","linkFileType":{"id":5,"text":"html"}},{"id":156015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db6121ed","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529096,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22259,"text":"ofr99202 - 1999 - Water quality and habitat conditions in upper Midwest streams relative to riparian vegetation and soil characteristics, August 1997 : study design, methods, and data","interactions":[],"lastModifiedDate":"2016-03-28T14:34:52","indexId":"ofr99202","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-202","title":"Water quality and habitat conditions in upper Midwest streams relative to riparian vegetation and soil characteristics, August 1997 : study design, methods, and data","docAbstract":"<p><span>Water-chemistry, biological, and habitat data were collected from 70 sites on Midwestern streams during August 1997 as part of an integrated, regional water-quality assessment by the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program. The study area includes the Corn Belt region of southern Minnesota, eastern Iowa, and west-central Illinois, one of the most intensive and productive agricultural regions of the world. The focus of the study was to evaluate the condition of woodedriparian zones and the influence of basin soildrainage characteristics on water quality and biological-community responses. This report includes a description of the study design and site-characterization process, sample-collection and processing methods, laboratory methods, quality-assurance procedures, and summaries of data on nutrients, herbicides and metabolites, stream productivity and respiration, biological communities, habitat conditions, and agriculturalchemical and land-use information.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr99202","issn":"0094-9140","usgsCitation":"Sorenson, S.K., Porter, S.D., Akers, K., Harris, M., Kalkhoff, S., Lee, K.E., Roberts, L., and Terrio, P.J., 1999, Water quality and habitat conditions in upper Midwest streams relative to riparian vegetation and soil characteristics, August 1997 : study design, methods, and data: U.S. Geological Survey Open-File Report 99-202, iv, 53 p., https://doi.org/10.3133/ofr99202.","productDescription":"iv, 53 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J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":187823,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, K. E.","contributorId":100014,"corporation":false,"usgs":true,"family":"Lee","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":187824,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roberts, L.","contributorId":113146,"corporation":false,"usgs":true,"family":"Roberts","given":"L.","affiliations":[],"preferred":false,"id":623805,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Terrio, P. J.","contributorId":11645,"corporation":false,"usgs":true,"family":"Terrio","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":623806,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":38096,"text":"ofr99190 - 1999 - Water quality and discharge data for St. Joseph Bay, Florida, 1997-98","interactions":[],"lastModifiedDate":"2023-02-07T20:06:16.497871","indexId":"ofr99190","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","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":"99-190","title":"Water quality and discharge data for St. Joseph Bay, Florida, 1997-98","docAbstract":"Historical data were compiled on water quality and water levels for the St. Joseph Bay area to assess quality of possible sources of land-derived water into the Bay. Ground-water quality data were compiled from Florida Department of Environmental Protection and surface-water quality data were compiled from U.S.Geological Survey files. Water-quality and water-level data were measured during two sample collection periods in October 1997 and March 1998 to determine water-quality and discharge rates in St. Joseph Bay under two sets of flow conditions. Measurements in the Bay included water level, temperature, pH, specific conductance, dissolved oxygen, and turbidity. \rMedian pH in water from the surficial, intermediate and Floridan aquifer systems ranged from 4.8 to 7.8, and median specific conductance values were less than 500 microsiemens per centimeter. Median nutrient concentrations-- nitrate plus nitrite, ammonia and phosphorus--in the three aquifers were less than 0.5 milligrams per liter. The median pH was 7.0 and the median specific conductance was 81 microsiemens per centimeter for two samples from the Chipola River distribution canal. Water level data were obtained for several wells near St. Joseph Bay but only two wells yielded sufficient data to plot hydrographs. \rMeasurements in St. Joseph Bay during the October and March collection periods were similar for pH and turbidity but differed for temperature, specific conductance and dissolved oxygen. The median temperature was 20.6 degrees Celsius in October and 15.4 degrees Celsius in March, median specific conductance was 39,500 microsiemens per centimeter in October and 43,300 microsiemens per centimeter in March, and median dissolved oxygen was 7.6 milligrams per liter in October and 8.3 milligrams per liter in March. The range in water levels over a tidal cycle in St. Joseph Bay on October 29, 1997 was about 1 foot. During a 24-hour tidal cycle on October 29, 1997, estimated hourly discharge varied from about -116,000 cubic feet per second (ft3/s) (into the Bay) to about +110,000 ft3/s (out of the Bay). During a 24-hour tidal cycle on March 3, 1998, the water level change was about 1.3 feet and estimated hourly discharge varied from about -132,000 ft3/s (into the Bay) to about +121,000 ft3/s (out of the Bay).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr99190","usgsCitation":"Berndt, M.P., and Franklin, M., 1999, Water quality and discharge data for St. Joseph Bay, Florida, 1997-98: U.S. Geological Survey Open-File Report 99-190, 20 p., https://doi.org/10.3133/ofr99190.","productDescription":"20 p.","costCenters":[],"links":[{"id":162904,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":412821,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19333.htm","linkFileType":{"id":5,"text":"html"}},{"id":3442,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr99-190","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"St Joseph Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -85.21689363438676,\n              29.875514695904158\n            ],\n            [\n              -85.425,\n              29.875514695904158\n            ],\n            [\n              -85.425,\n              29.64957460709401\n            ],\n            [\n              -85.21689363438676,\n              29.64957460709401\n            ],\n            [\n              -85.21689363438676,\n              29.875514695904158\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa33a","contributors":{"authors":[{"text":"Berndt, M. P.","contributorId":74761,"corporation":false,"usgs":true,"family":"Berndt","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":218878,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Franklin, M.A.","contributorId":13631,"corporation":false,"usgs":true,"family":"Franklin","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":218877,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70021201,"text":"70021201 - 1999 - Modeling the effects of land use and climate change on riverine smallmouth bass","interactions":[],"lastModifiedDate":"2023-12-20T11:53:15.75129","indexId":"70021201","displayToPublicDate":"1999-11-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1450,"text":"Ecological Applications","active":true,"publicationSubtype":{"id":10}},"title":"Modeling the effects of land use and climate change on riverine smallmouth bass","docAbstract":"<p><span>Anthropogenic changes in temperature and stream flow, associated with watershed land use and climate change, are critical influences on the distribution and abundance of riverine fishes. To project the effects of changing land use and climate, we modeled a smallmouth bass (</span><i>Micropterus dolomieu</i><span>) population in a midwestern USA, large river–floodplain ecosystem under historical (1915–1925), present (1977–1990), and future (2060, influenced by climate change) temperature and flow regimes. The age-structured model included parameters for temperature and river discharge during critical seasonal periods, fish population dynamics, and fishing harvest. Model relationships were developed from empirical field data collected over a 13-yr period. Sensitivity analyses indicated that discharge during the spawning/rearing period had a greater effect on adult density and fishing yield than did spawning/rearing temperature or winter discharge. Simulations for 100 years projected a 139% greater mean fish density under a historical flow regime (64.9 fish/ha) than that estimated for the present (27.1 fish/ha) with a sustainable fishing harvest under both flow regimes. Simulations under future climate-change-induced temperature and flow regimes with present land use projected a 69% decrease in mean fish density (8.5 fish/ha) from present and an unstable population that went extinct during 56% of the simulations. However, when simulated under a future climate-altered temperature and flow regime with historical land use, the population increased by 66% (45.0 fish/ha) from present and sustained a harvest. Our findings suggest that land-use changes may be a greater detriment to riverine fishes than projected climate change and that the combined effects of both factors may lead to local species extinction. However, the negative effects of increased temperature and precipitation associated with future global warming could be mitigated by river channel, floodplain, and watershed restoration.</span></p>","language":"English","publisher":"Ecological Society of America","doi":"10.1890/1051-0761(1999)009[1391:MTEOLU]2.0.CO;2","usgsCitation":"Peterson, J., and Kwak, T.J., 1999, Modeling the effects of land use and climate change on riverine smallmouth bass: Ecological Applications, v. 9, no. 4, p. 1391-1404, https://doi.org/10.1890/1051-0761(1999)009[1391:MTEOLU]2.0.CO;2.","productDescription":"14 p.","startPage":"1391","endPage":"1404","numberOfPages":"14","costCenters":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"links":[{"id":229741,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5c41e4b0c8380cd6fb41","contributors":{"authors":[{"text":"Peterson, James T. 0000-0002-7709-8590 james_peterson@usgs.gov","orcid":"https://orcid.org/0000-0002-7709-8590","contributorId":2111,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"james_peterson@usgs.gov","middleInitial":"T.","affiliations":[{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":389042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kwak, Thomas J. 0000-0002-0616-137X tkwak@usgs.gov","orcid":"https://orcid.org/0000-0002-0616-137X","contributorId":834,"corporation":false,"usgs":true,"family":"Kwak","given":"Thomas","email":"tkwak@usgs.gov","middleInitial":"J.","affiliations":[{"id":198,"text":"Coop Res Unit Atlanta","active":true,"usgs":true}],"preferred":true,"id":389043,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206105,"text":"70206105 - 1999 - Nomenclature of the micas","interactions":[],"lastModifiedDate":"2019-10-22T13:14:07","indexId":"70206105","displayToPublicDate":"1999-10-22T12:55:28","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2748,"text":"Mineralogical Magazine","active":true,"publicationSubtype":{"id":10}},"title":"Nomenclature of the micas","docAbstract":"<p><span>End-members and species defined with permissible ranges of composition are presented for the true micas, the brittle micas, and the interlayer-deficient micas. The determination of the crystallochemical formula for different available chemical data is outlined, and a system of modifiers and suffixes is given to allow the expression of unusual chemical substitutions or polytypic stacking arrangements. Tables of mica synonyms, varieties, ill-defined materials, and a list of names formerly or erroneously used for micas are presented. The Mica Subcommittee was appointed by the Commission on New Minerals and Mineral Names of the International Mineralogical Association. The definitions and recommendations presented were approved by the Commission.</span></p>","language":"English ","publisher":"Mineralogical Magazine","doi":"10.1180/minmag.1999.063.2.13","issn":"0026461X","usgsCitation":"Rieder, M., Cavazzini, G., D’yakonov, Y., Frank-Kamenetskii, V., Gottardi, G., Guggenheim, S., Koval, P., Muller, G., Neiva, A., Radoslovich, E., Robert, J., Sassi, F., Takeda, H., and Wones, D.R., 1999, Nomenclature of the micas: Mineralogical Magazine, v. 63, no. 2, p. 267-279, https://doi.org/10.1180/minmag.1999.063.2.13.","productDescription":"13 p. ","startPage":"267","endPage":"279","costCenters":[],"links":[{"id":368496,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"2","noUsgsAuthors":false,"publicationDate":"2018-07-05","publicationStatus":"PW","contributors":{"authors":[{"text":"Rieder, M.","contributorId":200496,"corporation":false,"usgs":false,"family":"Rieder","given":"M.","email":"","affiliations":[],"preferred":false,"id":773592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cavazzini, G","contributorId":219918,"corporation":false,"usgs":true,"family":"Cavazzini","given":"G","email":"","affiliations":[],"preferred":false,"id":773593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"D’yakonov, Y.S.","contributorId":219919,"corporation":false,"usgs":false,"family":"D’yakonov","given":"Y.S.","email":"","affiliations":[],"preferred":false,"id":773594,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frank-Kamenetskii, V.A.","contributorId":219920,"corporation":false,"usgs":false,"family":"Frank-Kamenetskii","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":773595,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gottardi, G","contributorId":219921,"corporation":false,"usgs":false,"family":"Gottardi","given":"G","email":"","affiliations":[],"preferred":false,"id":773596,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Guggenheim, S.","contributorId":219922,"corporation":false,"usgs":false,"family":"Guggenheim","given":"S.","email":"","affiliations":[],"preferred":false,"id":773597,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Koval, P.V.","contributorId":219923,"corporation":false,"usgs":false,"family":"Koval","given":"P.V.","email":"","affiliations":[],"preferred":false,"id":773598,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Muller, G","contributorId":219924,"corporation":false,"usgs":false,"family":"Muller","given":"G","email":"","affiliations":[],"preferred":false,"id":773599,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Neiva, A.M.R.","contributorId":219925,"corporation":false,"usgs":false,"family":"Neiva","given":"A.M.R.","email":"","affiliations":[],"preferred":false,"id":773600,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Radoslovich, E.W.","contributorId":219926,"corporation":false,"usgs":false,"family":"Radoslovich","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":773601,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Robert, J.-L.","contributorId":219927,"corporation":false,"usgs":false,"family":"Robert","given":"J.-L.","email":"","affiliations":[],"preferred":false,"id":773602,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Sassi, F.P","contributorId":219929,"corporation":false,"usgs":false,"family":"Sassi","given":"F.P","email":"","affiliations":[],"preferred":false,"id":773603,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Takeda, H.","contributorId":90462,"corporation":false,"usgs":true,"family":"Takeda","given":"H.","email":"","affiliations":[],"preferred":false,"id":773604,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Wones, David R.","contributorId":47455,"corporation":false,"usgs":true,"family":"Wones","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":773605,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70169448,"text":"70169448 - 1999 - Effects of sample size and sampling frequency on studies of brown bear home ranges and habitat use","interactions":[],"lastModifiedDate":"2016-03-25T16:16:31","indexId":"70169448","displayToPublicDate":"1999-10-01T17:15:00","publicationYear":"1999","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3671,"text":"Ursus","active":true,"publicationSubtype":{"id":10}},"title":"Effects of sample size and sampling frequency on studies of brown bear home ranges and habitat use","docAbstract":"<p>We equipped 9 brown bears (<i>Ursus arctos</i>) on the Kenai Peninsula, Alaska, with collars containing both conventional very-high-frequency (VHF) transmitters and global positioning system (GPS) receivers programmed to determine an animal's position at 5.75-hr intervals. We calculated minimum convex polygon (MCP) and fixed and adaptive kernel home ranges for randomly-selected subsets of the GPS data to examine the effects of sample size on accuracy and precision of home range estimates. We also compared results obtained by weekly aerial radiotracking versus more frequent GPS locations to test for biases in conventional radiotracking data. Home ranges based on the MCP were 20-606 km<sup>2</sup> (<i>x</i> = 201) for aerial radiotracking data (<i>n</i> = 12-16 locations/bear) and 116-1,505 km<sup>2</sup> (<i>x</i> = 522) for the complete GPS data sets (<i>n</i> = 245-466 locations/bear). Fixed kernel home ranges were 34-955 km<sup>2</sup> (<i>x</i> = 224) for radiotracking data and 16-130 km<sup>2</sup> (<i>x</i> = 60) for the GPS data. Differences between means for radiotracking and GPS data were due primarily to the larger samples provided by the GPS data. Means did not differ between radiotracking data and equivalent-sized subsets of GPS data (P &gt; 0.10). For the MCP, home range area increased and variability decreased asymptotically with number of locations. For the kernel models, both area and variability decreased with increasing sample size. Simulations suggested that the MCP and kernel models required &gt;60 and &gt;80 locations, respectively, for estimates to be both accurate (change in area &lt;1%/additional location) and precise (CV &lt; 50%). Although the radiotracking data appeared unbiased, except for the relationship between area and sample size, these data failed to indicate some areas that likely were important to bears. Our results suggest that the usefulness of conventional radiotracking data may be limited by potential biases and variability due to small samples. Investigators that use home range estimates in statistical tests should consider the effects of variability of those estimates. Use of GPS-equipped collars can facilitate obtaining larger samples of unbiased data and improve accuracy and precision of home range estimates.</p>","language":"English","publisher":"International Association for Bear Research and Management","publisherLocation":"New York, NY","usgsCitation":"Arthur, S.M., and Schwartz, C.C., 1999, Effects of sample size and sampling frequency on studies of brown bear home ranges and habitat use: Ursus, v. 11, p. 139-148.","productDescription":"10 p.","startPage":"139","endPage":"148","numberOfPages":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true}],"links":[{"id":319432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":319431,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.bearbiology.com/fileadmin/tpl/Downloads/URSUS/Vol_11/Arthur_Schwartz_Vol_11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f66155e4b07d796bf77045","contributors":{"authors":[{"text":"Arthur, Steve M.","contributorId":66169,"corporation":false,"usgs":true,"family":"Arthur","given":"Steve","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":624154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schwartz, Charles C.","contributorId":124574,"corporation":false,"usgs":false,"family":"Schwartz","given":"Charles","email":"","middleInitial":"C.","affiliations":[{"id":5119,"text":"Retired from U.S. Geological Survey, Interagency Grizzly Bear Study Team, Northern Rocky Mountain Science Center, 2327 University Way, suite 2, Bozeman, MT 59715","active":true,"usgs":false}],"preferred":false,"id":624155,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32216,"text":"ofr99173 - 1999 - The Washington and Oregon mid-shelf silt deposit and its relation to the late Holocene Columbia River sediment budget","interactions":[],"lastModifiedDate":"2014-03-25T09:35:49","indexId":"ofr99173","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","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":"99-173","title":"The Washington and Oregon mid-shelf silt deposit and its relation to the late Holocene Columbia River sediment budget","docAbstract":"The purpose of this report is to compile and analyze existing data which lend support to the development of a sediment budget for the Columbia River, coastal, and offshore regions of southwest Washington. This will contribute to the construction of a sediment budget model which will reflect sediment sources, depocenters, and the sediment contribution to each region. The Columbia River is the source of modern sediment for the beaches of southwest Washington. Development of the sediment budget is necessary to understand the long term effects that reduction in sediment supply has on present day areas of sediment erosion and accumulation in the region. Figure 1 describes the origin, distribution, and thickness of the Mid-Shelf Silt Deposit (MSSD) based on analysis of seismic data acquired between 1976-1980 (Wolf et al., 1997). Sediment volumes deposited during the past 5000 years were calculated for each of the physiographic areal compartments shown in Figure 2. Table 1 organizes the data from Figures 1 and 2 into tabular form. This table provides a representation of the percent volume and weight of sediment types which contribute to the estimated Columbia River sediment budget. The compartments shown in Figure 2 are color coordinated with Table 1.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr99173","usgsCitation":"Wolf, S.C., Nelson, H., Hamer, M.R., Dunhill, G., and Phillips, R.L., 1999, The Washington and Oregon mid-shelf silt deposit and its relation to the late Holocene Columbia River sediment budget (Version 1.0): U.S. Geological Survey Open-File Report 99-173, Report: 60.00 x 36.00 inches; Report GIF, https://doi.org/10.3133/ofr99173.","productDescription":"Report: 60.00 x 36.00 inches; Report GIF","costCenters":[{"id":641,"text":"Water Science Center Office - Tacoma","active":false,"usgs":true}],"links":[{"id":163255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr99173.jpg"},{"id":3176,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1999/0173/","linkFileType":{"id":5,"text":"html"}},{"id":284650,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1999/0173/images/map.gif"},{"id":284648,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1999/0173/pdf/of99-173.pdf"}],"country":"United States","state":"California;Oregon;Washington","otherGeospatial":"Colombia River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -130.0,40.0 ], [ -130.0,48.0 ], [ -122.0,48.0 ], [ -122.0,40.0 ], [ -130.0,40.0 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd775ee4b0b2908510b7e0","contributors":{"authors":[{"text":"Wolf, Stephen C.","contributorId":38148,"corporation":false,"usgs":true,"family":"Wolf","given":"Stephen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":207993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Hans","contributorId":46942,"corporation":false,"usgs":true,"family":"Nelson","given":"Hans","email":"","affiliations":[],"preferred":false,"id":207994,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hamer, Michael R.","contributorId":10471,"corporation":false,"usgs":true,"family":"Hamer","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":207991,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dunhill, Gita","contributorId":36169,"corporation":false,"usgs":true,"family":"Dunhill","given":"Gita","email":"","affiliations":[],"preferred":false,"id":207992,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Phillips, R. Lawrence","contributorId":81478,"corporation":false,"usgs":true,"family":"Phillips","given":"R.","email":"","middleInitial":"Lawrence","affiliations":[],"preferred":false,"id":207995,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":38260,"text":"pp1650AB - 1999 - Atlas of relations between climatic parameters and distributions of important trees and shrubs in North America","interactions":[],"lastModifiedDate":"2012-02-02T00:10:01","indexId":"pp1650AB","displayToPublicDate":"1999-10-01T00:00:00","publicationYear":"1999","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1650","chapter":"A,B","title":"Atlas of relations between climatic parameters and distributions of important trees and shrubs in North America","docAbstract":"This atlas explores the continental-scale relations between the geographic ranges of woody plant species and climate in North America. A 25-km equal-area grid of modern climatic and bioclimatic parameters was constructed from instrumental weather records. The geographic distributions of selected tree and shrub species were digitized, and the presence or absence of each species was determined for each cell on the 25-km grid, thus providing a basis for comparing climatic data and species distributions. The relations between climate and plant distributions are explored in graphical and tabular form. The results of this effort are primarily intended for use in biogeographic, paleoclimatic, and global-change research.","language":"ENGLISH","doi":"10.3133/pp1650AB","usgsCitation":"Thompson, R.S., Anderson, K.H., and Bartlein, P.J., 1999, Atlas of relations between climatic parameters and distributions of important trees and shrubs in North America (Online Version 1.0, 14 December 1999): U.S. Geological Survey Professional Paper 1650, atlas, https://doi.org/10.3133/pp1650AB.","productDescription":"atlas","costCenters":[],"links":[{"id":3497,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/p1650-a/","linkFileType":{"id":5,"text":"html"}},{"id":162451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1650a-b/report-thumb.jpg"},{"id":64636,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1650a-b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Online Version 1.0, 14 December 1999","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669482","contributors":{"authors":[{"text":"Thompson, Robert S. 0000-0001-9287-2954 rthompson@usgs.gov","orcid":"https://orcid.org/0000-0001-9287-2954","contributorId":891,"corporation":false,"usgs":true,"family":"Thompson","given":"Robert","email":"rthompson@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":219438,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Katherine H. 0000-0003-2677-6109","orcid":"https://orcid.org/0000-0003-2677-6109","contributorId":52556,"corporation":false,"usgs":true,"family":"Anderson","given":"Katherine","email":"","middleInitial":"H.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":false,"id":219439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartlein, Patrick J.","contributorId":106879,"corporation":false,"usgs":true,"family":"Bartlein","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":219440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}