The impoundment of water in Quail Creek Reservoir in southwestern Utah began in April 1985. The drainage area for the reservoir is 78.4 square miles, including Quail Creek and Leeds Creek watersheds. Water also is diverted from the Virgin River above Hurricane, Utah, to supplement the filling of the reservoir.
A dike, which is one of the structures impounding water in Quail Creek Reservoir, failed on January 1, 1989. This failure resulted in the release of about 25,000 acre-feet of water into the Virgin River near Hurricane, Utah.
Flooding occurred along the Virgin River flood plain in Utah, Arizona, and Nevada. The previous maximum discharge of record was exceeded at three U.S. Geological Survey streamflow-gaging stations, and the flood discharges exceeded the theoretical 100-year flood discharges. Peak discharge estimates ranged from 60,000 to 66,000 cubic feet per second at the three streamflow-gaging stations.
Damage to roads, bridges, agricultural land, livestock, irrigation structures, businesses, and residences totaled more than $12 million. The greatest damage was to agricultural and public-works facilities. Washington County, which is in southwestern Utah, was declared a disaster area by President George Bush.
","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/wri944159","usgsCitation":"Carlson, D., and Meyer, D.F., 1995, Flood on the Virgin River, January 1989, in Utah, Arizona, and Nevada: U.S. Geological Survey Water-Resources Investigations Report 94-4159, Report: iv, 21 p.; Plate: 28.77 x 17.18 inches, https://doi.org/10.3133/wri944159.","productDescription":"Report: iv, 21 p.; Plate: 28.77 x 17.18 inches","costCenters":[],"links":[{"id":119108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4159/report-thumb.jpg"},{"id":55318,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4159/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359559,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4159/plate-1.pdf"}],"country":"United States","state":"Arizona, Nevada, Utah","otherGeospatial":"Virgin River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.55,\n 36\n ],\n [\n -113.2,\n 36\n ],\n [\n -113.2,\n 37.5\n ],\n [\n -114.55,\n 37.5\n ],\n [\n -114.55,\n 36\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48ade4b07f02db52d50d","contributors":{"authors":[{"text":"Carlson, D.D.","contributorId":10816,"corporation":false,"usgs":true,"family":"Carlson","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":196492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, D. F.","contributorId":21167,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52705,"text":"b1995JK - 1995 - Neogene geohistory analysis of Santa Maria Basin, California, and its relationship to transfer of Central California to the Pacific Plate. Diatom biochronology of the Sisquoc Formation in the Santa Maria Basin, California, and its paleoceanographic and tectonic implications","interactions":[{"subject":{"id":52705,"text":"b1995JK - 1995 - Neogene geohistory analysis of Santa Maria Basin, California, and its relationship to transfer of Central California to the Pacific Plate. Diatom biochronology of the Sisquoc Formation in the Santa Maria Basin, California, and its paleoceanographic and tectonic implications","indexId":"b1995JK","publicationYear":"1995","noYear":false,"chapter":"J,K","title":"Neogene geohistory analysis of Santa Maria Basin, California, and its relationship to transfer of Central California to the Pacific Plate. Diatom biochronology of the Sisquoc Formation in the Santa Maria Basin, California, and its paleoceanographic and tectonic implications"},"predicate":"IS_PART_OF","object":{"id":33200,"text":"b1995 - 1991 - Evolution of sedimentary basins/onshore oil and gas investigations: Santa Maria Province","indexId":"b1995","publicationYear":"1991","noYear":false,"title":"Evolution of sedimentary basins/onshore oil and gas investigations: Santa Maria Province"},"id":1}],"isPartOf":{"id":33200,"text":"b1995 - 1991 - Evolution of sedimentary basins/onshore oil and gas investigations: Santa Maria Province","indexId":"b1995","publicationYear":"1991","noYear":false,"title":"Evolution of sedimentary basins/onshore oil and gas investigations: Santa Maria Province"},"lastModifiedDate":"2022-06-03T20:50:52.793053","indexId":"b1995JK","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1995","chapter":"J,K","title":"Neogene geohistory analysis of Santa Maria Basin, California, and its relationship to transfer of Central California to the Pacific Plate. Diatom biochronology of the Sisquoc Formation in the Santa Maria Basin, California, and its paleoceanographic and tectonic implications","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Evolution of Sedimentary Basins/Offshore Oil and Gas Investigations--Santa Maria Province","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1995JK","usgsCitation":"McCrory, P.A., Wilson, D.S., Ingle, J.C., Stanley, R.G., Dumont, M.P., and Barron, J.A., 1995, Neogene geohistory analysis of Santa Maria Basin, California, and its relationship to transfer of Central California to the Pacific Plate. Diatom biochronology of the Sisquoc Formation in the Santa Maria Basin, California, and its paleoceanographic and tectonic implications: U.S. Geological Survey Bulletin 1995, 55 p., https://doi.org/10.3133/b1995JK.","productDescription":"55 p.","costCenters":[],"links":[{"id":181384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1995j-k/report-thumb.jpg"},{"id":87032,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1995j-k/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401722,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22231.htm"}],"country":"United States","state":"California","otherGeospatial":"Santa Maria Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122,\n 34\n ],\n [\n -119,\n 34\n ],\n [\n -119,\n 36\n ],\n [\n -122,\n 36\n ],\n [\n -122,\n 34\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47efe4b07f02db4c19b1","contributors":{"authors":[{"text":"McCrory, Patricia A. 0000-0003-2471-0018 pmccrory@usgs.gov","orcid":"https://orcid.org/0000-0003-2471-0018","contributorId":2728,"corporation":false,"usgs":true,"family":"McCrory","given":"Patricia","email":"pmccrory@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":245870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Douglas S.","contributorId":68782,"corporation":false,"usgs":true,"family":"Wilson","given":"Douglas","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":245872,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingle, James C. Jr.","contributorId":75809,"corporation":false,"usgs":false,"family":"Ingle","given":"James","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[{"id":7033,"text":"School of Earth Sciences, Stanford University","active":true,"usgs":false}],"preferred":false,"id":245873,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stanley, Richard G. 0000-0001-6192-8783 rstanley@usgs.gov","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":1832,"corporation":false,"usgs":true,"family":"Stanley","given":"Richard","email":"rstanley@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":245868,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Dumont, Michael P.","contributorId":47239,"corporation":false,"usgs":true,"family":"Dumont","given":"Michael","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":245871,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barron, John A. 0000-0002-9309-1145 jbarron@usgs.gov","orcid":"https://orcid.org/0000-0002-9309-1145","contributorId":2222,"corporation":false,"usgs":true,"family":"Barron","given":"John","email":"jbarron@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":245869,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":24415,"text":"ofr95644 - 1995 - Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr95644","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-644","title":"Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Idaho","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95644","issn":"0094-9140","usgsCitation":"Ryder, J.L., 1995, Active-, inactive-, and abandoned-mine information and selected geochemical data for the State of Idaho: U.S. Geological Survey Open-File Report 95-644, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr95644.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":157092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1759,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/ofr-95-0644/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a34d5","contributors":{"authors":[{"text":"Ryder, Jean L.","contributorId":80709,"corporation":false,"usgs":true,"family":"Ryder","given":"Jean","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18789,"text":"ofr95269 - 1995 - Merging of analog and digital data in the Northern California Seismic Network, and characteristics of the principal seismic systems it employs","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr95269","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-269","title":"Merging of analog and digital data in the Northern California Seismic Network, and characteristics of the principal seismic systems it employs","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95269","usgsCitation":"Eaton, J.P., 1995, Merging of analog and digital data in the Northern California Seismic Network, and characteristics of the principal seismic systems it employs: U.S. Geological Survey Open-File Report 95-269, 28 p. ill. ;28 cm., https://doi.org/10.3133/ofr95269.","productDescription":"28 p. ill. ;28 cm.","costCenters":[],"links":[{"id":152512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0269/report-thumb.jpg"},{"id":48159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0269/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624ee1","contributors":{"authors":[{"text":"Eaton, Jerry P.","contributorId":22341,"corporation":false,"usgs":true,"family":"Eaton","given":"Jerry","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":179746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70018866,"text":"70018866 - 1995 - Radiocarbon evidence for extensive plate-boundary rupture about 300 years ago at the Cascadia subduction zone","interactions":[],"lastModifiedDate":"2025-05-27T16:37:39.450074","indexId":"70018866","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon evidence for extensive plate-boundary rupture about 300 years ago at the Cascadia subduction zone","docAbstract":"The Cascadia subduction zone, a region of converging tectonic plates along the Pacific coast of North America, has a geological history of very large plate-boundary earthquakes1,2, but no such earthquakes have struck this region since Euro-American settlement about 150 years ago. Geophysical estimates of the moment magnitudes (Mw) of the largest such earthquakes range from 8 (ref. 3).to 91/2 (ref. 4). Radiocarbon dating of earthquake-killed vegetation can set upper bounds on earthquake size by constraining the length of plate boundary that ruptured in individual earthquakes. Such dating has shown that the most recent rupture, or series of ruptures, extended at least 55 km along the Washington coast within a period of a few decades about 300 years ago5. Here we report 85 new 14C ages, which suggest that this most recent rupture (or series) extended at least 900 km between southern British Columbia and northern California. By comparing the 14C ages with written records of the past 150 years, we conclude that a single magnitude 9 earthquake, or a series of lesser earthquakes, ruptured most of the length of the Cascadia subduction zone between the late 1600s and early 1800s, and probably in the early 1700s.
","language":"English","publisher":"Springer Nature","doi":"10.1038/378371a0","issn":"00280836","usgsCitation":"Nelson, A., Atwater, B., Bobrowsky, P., Bradley, L.A., Clague, J.J., Carver, G.A., Darienzo, M., Grant, W., Krueger, H., Sparks, R., Stafford, T.W., and Stuiver, M., 1995, Radiocarbon evidence for extensive plate-boundary rupture about 300 years ago at the Cascadia subduction zone: Nature, v. 378, no. 6555, p. 371-374, https://doi.org/10.1038/378371a0.","productDescription":"4 p.","startPage":"371","endPage":"374","costCenters":[],"links":[{"id":226391,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"California, Oregon, Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -130.7513282764907,\n 51.07766511771612\n ],\n [\n -130.7513282764907,\n 40.97954953268206\n ],\n [\n -123.40724172427474,\n 40.97954953268206\n ],\n [\n -123.40724172427474,\n 51.07766511771612\n ],\n [\n -130.7513282764907,\n 51.07766511771612\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"378","issue":"6555","noUsgsAuthors":false,"publicationDate":"1995-11-01","publicationStatus":"PW","scienceBaseUri":"505a93e4e4b0c8380cd810b6","contributors":{"authors":[{"text":"Nelson, A.R. 0000-0001-7117-7098","orcid":"https://orcid.org/0000-0001-7117-7098","contributorId":55078,"corporation":false,"usgs":true,"family":"Nelson","given":"A.R.","affiliations":[],"preferred":false,"id":380970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atwater, B.F. 0000-0003-1155-2815","orcid":"https://orcid.org/0000-0003-1155-2815","contributorId":14006,"corporation":false,"usgs":true,"family":"Atwater","given":"B.F.","affiliations":[],"preferred":false,"id":380964,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bobrowsky, P.T.","contributorId":69722,"corporation":false,"usgs":true,"family":"Bobrowsky","given":"P.T.","affiliations":[],"preferred":false,"id":380971,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bradley, L. A.","contributorId":35738,"corporation":false,"usgs":true,"family":"Bradley","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380967,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clague, J. J.","contributorId":36306,"corporation":false,"usgs":false,"family":"Clague","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":380968,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carver, G. A.","contributorId":80762,"corporation":false,"usgs":false,"family":"Carver","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":380972,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Darienzo, M.E.","contributorId":90048,"corporation":false,"usgs":true,"family":"Darienzo","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":380974,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Grant, W.C.","contributorId":86908,"corporation":false,"usgs":true,"family":"Grant","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":380973,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Krueger, H.W.","contributorId":16993,"corporation":false,"usgs":true,"family":"Krueger","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":380965,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sparks, R.","contributorId":10939,"corporation":false,"usgs":true,"family":"Sparks","given":"R.","affiliations":[],"preferred":false,"id":380963,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Stafford, Thomas W. Jr.","contributorId":21283,"corporation":false,"usgs":true,"family":"Stafford","given":"Thomas","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":380966,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Stuiver, M.","contributorId":54730,"corporation":false,"usgs":true,"family":"Stuiver","given":"M.","affiliations":[],"preferred":false,"id":380969,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":26030,"text":"wri944178 - 1995 - Hydrogeology of Cibola County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri944178","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"94-4178","title":"Hydrogeology of Cibola County, New Mexico","docAbstract":"The hydrogeology of Cibola County, New Mexico, was evaluated to \r\ndetermine the occurrence, availability, and quality of ground-water \r\nresources. Rocks of Precambrian through Quaternary age are present in \r\nCibola County. Most rocks are sedimentary in origin except for \r\nPrecambrian igneous and metamorphic rocks exposed in the Zuni Uplift \r\nand Tertiary and Quaternary basalts in northern and central parts of the \r\ncounty. The most productive aquifers in the county include (youngest \r\nto oldest) Quaternary deposits, sandstones in the Mesaverde Group, the \r\nDakota-Zuni-Bluff aquifer, the Westwater Canyon aquifer, the Todilto-\r\nEntrada aquifer, sandstone beds in the Chinle Formation, and the San \r\nAndres-Glorieta aquifer.\r\n\r\n Unconsolidated sand, silt, and gravel form a mantle ranging from \r\na few inches to 150 to 200 feet over much of the bedrock in Cibola County. \r\nWell yields range from 5 to 1,110 gallons per minute. Dissolved-solids \r\nconcentrations of ground water range from 200 to more than 5,200 \r\nmilligrams per liter. Calcium, magnesium, bicarbonate, and sulfate are \r\nthe predominant ions in ground water in alluvial material.\r\n\r\n The Mesaverde Group mainly occurs in three areas of the county. \r\nWell yields range from less than 1 to 12 gallons per minute. The \r\npredominant ions in water from wells in the Mesaverde Group are calcium, \r\nsodium, and bicarbonate. The transition from calcium-predominant to \r\nsodium-predominant water in the southwestern part of the county likely \r\nis a result of ion exchange.\r\n\r\n Wells completed in the Dakota-Zuni-Bluff aquifer yield from 1 to 30 \r\ngallons per minute. Dissolved-solids concentrations range from 220 to \r\n2,000 milligrams per liter in water from 34 wells in the western part of \r\nthe county. Predominant ions in the ground water include calcium, sodium, \r\nsulfate, and bicarbonate. Calcium predominates in areas where the aquifer \r\nis exposed at the surface or is overlain with alluvium.\r\n\r\n Sandstones in the Chinle Formation yield from 10 to 300 gallons per \r\nminute to wells in the Grants-Bluewater area. In the western part of \r\nthe county, sodium and bicarbonate predominate in water from the Chinle \r\nFormation. In the eastern part of the county, water quality is more \r\nvariable than elsewhere and the predominant constituents include \r\ncalcium, sodium, sulfate, and chloride.\r\n\r\n Well yields from the San Andres-Glorieta aquifer in the Grants-\r\nBluewater area are as much as 2,830 gallons per minute, whereas the \r\nmaximum recorded pumping rate from the aquifer in other areas of the \r\ncounty is 88 gallons per minute. Dissolved-solids concentrations of \r\nground-water range from about 130 to 4,200 milligrams per liter, and the \r\nwater generally is a calcium bicarbonate sulfate type.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCan be purchased from U.S.G.S. Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/wri944178","usgsCitation":"Baldwin, J.A., and Rankin, D., 1995, Hydrogeology of Cibola County, New Mexico: U.S. Geological Survey Water-Resources Investigations Report 94-4178, vi, 102 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944178.","productDescription":"vi, 102 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4178/report-thumb.jpg"},{"id":54810,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4178/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91730,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4178/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6251b4","contributors":{"authors":[{"text":"Baldwin, J. A.","contributorId":50941,"corporation":false,"usgs":true,"family":"Baldwin","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rankin, D.R.","contributorId":28991,"corporation":false,"usgs":true,"family":"Rankin","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":195670,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":19683,"text":"ofr95305 - 1995 - Hydrologic data for the Usquepaug-Queen River basin, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr95305","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-305","title":"Hydrologic data for the Usquepaug-Queen River basin, Rhode Island","docAbstract":"The Usquepaug-Queen River ground-water reservoir in Rhode Island is part of the stratified-drift aquifer along the Usquepaug-Queen River and its tributaries. The thickest, most permeable parts of the aquifer form the Usquepaug-Queen River ground-water reservoir. The 36.1-square mile study area comprises parts of Washington and Kent counties, and includes parts of the towns of Exeter, North Kingstown, Richmond, South Kingstown, and West Greenwich. The report presents geologic and hydrologic information needed for the prediction and management of hydrologic effects of proposed ground-water development. The report describes aquifer lithology, provides historical data on water-level and aquifer-storage changes, provides information on ground-water quality, and presents natural flow characteristics and water quality of streams in the Usquepaug-Queen River area. The data includes 275 ground-water sites; lithologic logs of 66 ground-water sites; water levels for 43 ground- water sites; chemical analyses of 36 ground-water sites; stream discharge measurements from the continuous-record gaging station on the Usquepaug- Queen River; discharge measurements at 10 partial- record stations in the area; chemical analyses of 17 stream sites; and the data from 14 slug tests conducted at ground-water sites.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S.G.S. Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95305","usgsCitation":"Kliever, J.D., 1995, Hydrologic data for the Usquepaug-Queen River basin, Rhode Island: U.S. Geological Survey Open-File Report 95-305, iv, 68 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr95305.","productDescription":"iv, 68 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":152427,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0305/report-thumb.jpg"},{"id":19361,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1995/0305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0305/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608204","contributors":{"authors":[{"text":"Kliever, John D.","contributorId":46976,"corporation":false,"usgs":true,"family":"Kliever","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":181328,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19941,"text":"ofr94506 - 1995 - Pesticides in the atmosphere; distribution, trends, and governing factors","interactions":[],"lastModifiedDate":"2013-05-22T15:26:15","indexId":"ofr94506","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"94-506","title":"Pesticides in the atmosphere; distribution, trends, and governing factors","docAbstract":"A comprehensive review of existing literature on the occurrence and distribution of pesticides in the atmosphere of the United States and adjoining Canadian provinces showed that the atmosphere is an important part of the hydrologic cycle that acts to distribute and deposit pesticides in areas far removed from their application sites. A compilation of existing data shows that pesticides have been detected in the atmosphere throughout the nation. Most of the available information on pesticides in the atmosphere is from small-scale, short-term studies that seldom lasted more than one year. Only two national-scale, multi-year studies were done since the late 1960's that analyzed for a wide variety of pesticides in air that were in current use at the time. Another large-scale study was done during 1990-91, but was limited to the midwestern and northeastern United States and only analyzed for two classes of herbicides in wet deposition. Most of the pesticides analyzed for were detected in either air or rain, and represent about 25 percent of the total number of insecticides, herbicides, and fungicides in current use. The geographical distribution of studies, and the type of sampling and analysis were highly variable with most of the historical study efforts concentrated in the Great Lakes area and California. Air and rain were the main atmospheric matrices sampled, but pesticides were also detected in fog and snow. Reported pesticide concentrations in air and rain were frequently positively correlated to their regional agricultural use. Deviations from this relation could usually be explained by non-agricultural use of pesticides, sampling and analytical difficulties, and environmental persistence. High concentrations of locally used pesticides were found to occur seasonally, usually in conjunction with spring planting of row crops and warm temperatures, but high concentrations also occurred during winter months in those areas where dormant orchards were sprayed. The environmentally more persistent pesticides were detected in the atmosphere at low concen- trations throughout the year. Deposition of airborne pesticides can have significant effects on water quality, but neither the nature of nor the magnitude of these effects can be determined with certainty on the basis of the type of data currently available. The lack of consistent, long-term regional and national monitoring and study of pesticides in atmospheric matrices severely limits assessment capability.","language":"ENGLISH","publisher":"U.S. Geological Survey ;Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94506","usgsCitation":"Majewski, M.S., and Capel, P.D., 1995, Pesticides in the atmosphere; distribution, trends, and governing factors: U.S. Geological Survey Open-File Report 94-506, xiii, 191 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr94506.","productDescription":"xiii, 191 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152407,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0506/report-thumb.jpg"},{"id":272568,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0506/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697904","contributors":{"authors":[{"text":"Majewski, Michael S. majewski@usgs.gov","contributorId":440,"corporation":false,"usgs":true,"family":"Majewski","given":"Michael","email":"majewski@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":181770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Capel, Paul D. 0000-0003-1620-5185 capel@usgs.gov","orcid":"https://orcid.org/0000-0003-1620-5185","contributorId":1002,"corporation":false,"usgs":true,"family":"Capel","given":"Paul","email":"capel@usgs.gov","middleInitial":"D.","affiliations":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":181771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27557,"text":"wri954052 - 1995 - Estimated natural ground-water recharge, discharge, and budget for the Dixie Valley area, west-central Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri954052","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4052","title":"Estimated natural ground-water recharge, discharge, and budget for the Dixie Valley area, west-central Nevada","docAbstract":"The Dixie Valley area includes seven valleys in west-central Nevada (Dixie, Fairview, Stingaree, Cowkick, Eastgate, Pleasant, and Jersey Valleys; total, 2,380 square miles). Dixie Valley receives surface-water and ground-water flow from Stingaree, Cowkick, Eastgate, Pleasant, and Jersey Valleys and subsurface flow from Fairview Valley, which is a topographically closed basin. The relation between precipitation and altitude was re-evaluated for the Dixie Valley area using new data, and empirical estimates of recharge were revised accordingly. The revised estimate of total recharge is 23,000 acre-feet per Re-evaluation of ground-water discharge focused on Dixie Valley as the largest basin in the study area. Phreatophytic vegetation was mapped and partitioned into nine zones on the basis of species composition and foliage density. For woody phreatophytes, annual evapotranspiration rates of 0.7 cubic feet of water per cubic foot of foliage for greasewood and 1.1 cubic feet of water per cubic foot of foliage for rabbitbrush were adapted from lysimeter studies near Winnemucca, Nevada. These rates were multiplied by the foliage density of the respective phreatophytes in each zone to estimate a specific rate for that zone. Rates for salt-grass (0.5 to 0.8 foot per year) and the playa surface (0.1 to 0.3 foot per year) were based on a range of rates. used in other recent studies in western and central Nevada. These rates were multiplied by the areas of the zones to produce estimates of the annual volume of ground water discharged. The discharge estimated for Dixie Valley is between 17,000 and 28,000 acre-feet per year. The revised discharge estimate for the entire Dixie Valley area is between 20,000 and 31,000 acre-feet per year. The revised ground-water budget for the entire Dixie Valley study area has a total recharge of about 23,000 acre-feet per year. This is within the range of estimates of natural discharge--from 20,000 to 31,000 acre-feet per year. For Dixie Valley alone, the total recharge of about 8,900 acre-feet per year and the estimated subsurface inflow from tributary areas of about 11,000 acre-feet per year produce an estimated total inflow of about 20,000 acre-feet per year. This compares with the discharge estimate of 17,000 to 28,000 acre-feet per year.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Information Services [distributor],","doi":"10.3133/wri954052","usgsCitation":"Harrill, J., and Hines, L., 1995, Estimated natural ground-water recharge, discharge, and budget for the Dixie Valley area, west-central Nevada: U.S. Geological Survey Water-Resources Investigations Report 95-4052, iv, 12 p. :ill., col. map ;28 cm., https://doi.org/10.3133/wri954052.","productDescription":"iv, 12 p. :ill., col. map ;28 cm.","costCenters":[],"links":[{"id":123547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4052/report-thumb.jpg"},{"id":56414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0fc","contributors":{"authors":[{"text":"Harrill, J. R.","contributorId":10417,"corporation":false,"usgs":true,"family":"Harrill","given":"J. R.","affiliations":[],"preferred":false,"id":198319,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, L.B.","contributorId":49406,"corporation":false,"usgs":true,"family":"Hines","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":198320,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26188,"text":"wri954087 - 1995 - Transport and sources of sediment in the Missouri River between Garrison Dam and the headwaters of Lake Oahe, North Dakota, May 1988 through April 1991","interactions":[],"lastModifiedDate":"2018-02-14T15:55:12","indexId":"wri954087","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"95-4087","title":"Transport and sources of sediment in the Missouri River between Garrison Dam and the headwaters of Lake Oahe, North Dakota, May 1988 through April 1991","docAbstract":"Sediment data were collected on and along the Missouri River downstream from Garrison Dam during May 1988, May 1989, and April 1991 to characterize sediment transport in the river. Specific study objectives were to (1) identify erosional and depositional reaches during two steady-state low-flow periods and one steady-state high-flow period; (2) determine if the reaches are consistently eroding or depositing, regardless of streamflow; and (3) determine the sources of suspended sediment in the river.
Erosional and depositional reaches differed between the two low-flow periods, indicating that slight changes in the channel configuration between the two periods caused changes in erosional and depositional patterns. Erosional and depositional reaches also differed between the low-flow periods and the high-flow period, indicating that channel changes and increased streamflow velocities affect erosional and depositional reaches.
The significant sources of suspended sediment in the Missouri River are the riverbed and riverbanks. The riverbed contributes to the silt and sand load in the river, and the riverbanks contribute to the clay, silt, and sand load. The contribution from tributaries to the suspendedsediment load in the Missouri River usually is small. Occasionally, during low-flow periods on the Missouri River, the Knife River can contribute significantly to the suspended-sediment load in the Missouri River.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954087","usgsCitation":"Berkas, W.R., 1995, Transport and sources of sediment in the Missouri River between Garrison Dam and the headwaters of Lake Oahe, North Dakota, May 1988 through April 1991: U.S. Geological Survey Water-Resources Investigations Report 95-4087, iv, 26 p., https://doi.org/10.3133/wri954087.","productDescription":"iv, 26 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":157623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4087/report-thumb.jpg"},{"id":54985,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","otherGeospatial":"Lake Oahe, Missouri River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626c29","contributors":{"authors":[{"text":"Berkas, Wayne R. wrberkas@usgs.gov","contributorId":425,"corporation":false,"usgs":true,"family":"Berkas","given":"Wayne","email":"wrberkas@usgs.gov","middleInitial":"R.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17481,"text":"ofr95486 - 1995 - The physical preparation and chemical analysis of NIST SRMs 2786 and 2787, lead paint in soil","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr95486","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"95-486","title":"The physical preparation and chemical analysis of NIST SRMs 2786 and 2787, lead paint in soil","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95486","usgsCitation":"Wilson, S., Briggs, P., Mee, J.S., Hageman, P., Siems, D.F., Malcolm, M., and Curry, J., 1995, The physical preparation and chemical analysis of NIST SRMs 2786 and 2787, lead paint in soil: U.S. Geological Survey Open-File Report 95-486, 24 p. ;28 cm., https://doi.org/10.3133/ofr95486.","productDescription":"24 p. ;28 cm.","costCenters":[],"links":[{"id":150804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0486/report-thumb.jpg"},{"id":46632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64492f","contributors":{"authors":[{"text":"Wilson, S. A. 0000-0002-9468-0005","orcid":"https://orcid.org/0000-0002-9468-0005","contributorId":23561,"corporation":false,"usgs":true,"family":"Wilson","given":"S. A.","affiliations":[],"preferred":false,"id":176536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":176542,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mee, J. S.","contributorId":25168,"corporation":false,"usgs":true,"family":"Mee","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":176537,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hageman, P. L. 0000-0002-3440-2150","orcid":"https://orcid.org/0000-0002-3440-2150","contributorId":27459,"corporation":false,"usgs":true,"family":"Hageman","given":"P. L.","affiliations":[],"preferred":false,"id":176538,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Siems, D. F.","contributorId":101239,"corporation":false,"usgs":true,"family":"Siems","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":176541,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Malcolm, M.J.","contributorId":95064,"corporation":false,"usgs":true,"family":"Malcolm","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":176539,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Curry, J.","contributorId":98752,"corporation":false,"usgs":true,"family":"Curry","given":"J.","email":"","affiliations":[],"preferred":false,"id":176540,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":18127,"text":"ofr94702W - 1995 - Hydrologic and ecologic influence of playa basins in the southern High Plains, Texas and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr94702W","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"94-702","chapter":"W","title":"Hydrologic and ecologic influence of playa basins in the southern High Plains, Texas and New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr94702W","usgsCitation":"Bexfield, L.M., 1995, Hydrologic and ecologic influence of playa basins in the southern High Plains, Texas and New Mexico: U.S. Geological Survey Open-File Report 94-702, v, 16 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/ofr94702W.","productDescription":"v, 16 p. :ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":149238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0702w/report-thumb.jpg"},{"id":47482,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0702w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611892","contributors":{"authors":[{"text":"Bexfield, Laura M. 0000-0002-1789-654X bexfield@usgs.gov","orcid":"https://orcid.org/0000-0002-1789-654X","contributorId":1273,"corporation":false,"usgs":true,"family":"Bexfield","given":"Laura","email":"bexfield@usgs.gov","middleInitial":"M.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":true,"id":178597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":38220,"text":"pp1564 - 1995 - Characteristics and petrogenesis of alaskan-type ultramafic-mafic intrusions, Southeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:02","indexId":"pp1564","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"1564","title":"Characteristics and petrogenesis of alaskan-type ultramafic-mafic intrusions, Southeastern Alaska","docAbstract":"Characteristics of alaskan-type ultramafic-mafic intrusions are described and evaluated to determine the origin and emplacement mechanism of these bodies.","language":"ENGLISH","doi":"10.3133/pp1564","usgsCitation":"Himmelberg, G.R., and Loney, R.A., 1995, Characteristics and petrogenesis of alaskan-type ultramafic-mafic intrusions, Southeastern Alaska: U.S. Geological Survey Professional Paper 1564, 47 p., https://doi.org/10.3133/pp1564.","productDescription":"47 p.","costCenters":[],"links":[{"id":119220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1564/report-thumb.jpg"},{"id":64548,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1564/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e53d4","contributors":{"authors":[{"text":"Himmelberg, G. R.","contributorId":27106,"corporation":false,"usgs":true,"family":"Himmelberg","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Loney, R. A.","contributorId":90757,"corporation":false,"usgs":true,"family":"Loney","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":219364,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38221,"text":"pp1566 - 1995 - Geochemistry of minor elements in the Monterey Formation, California; seawater chemistry of deposition","interactions":[],"lastModifiedDate":"2015-07-10T13:17:22","indexId":"pp1566","displayToPublicDate":"1995-11-01T00:00:00","publicationYear":"1995","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":"1566","title":"Geochemistry of minor elements in the Monterey Formation, California; seawater chemistry of deposition","docAbstract":"Approximately 24 samples of the Monterey Formation, Southern California, have been analyzed for their major-element oxide and minor-element content. These analyses allow identification of a detrital fraction, composed of terrigenous quartz, clay minerals, and other Al silicate minerals, and a marine fraction, composed of biogenic silica, calcite, dolomite, organic matter, apatite, and minor amounts of pyrite. The minor-element contents in the marine fraction alone are interpreted to have required, at the time of deposition, a high level of primary productivity in the photic zone and denitrifying bacterial respiration in the bottom water.
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