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","language":"English","publisher":"Elsevier ","usgsCitation":"Barnhart, R., Boyd, M., and Pequegnat, J., The ecology of Humboldt Bay, California, an estuarine profile: U.S. Fish and Wildlife Service Biological Report, v. 1, 121 p. .","productDescription":"121 p. ","numberOfPages":"121","costCenters":[{"id":150,"text":"California Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"links":[{"id":373032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"California ","county":"Humboldt","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.134521484375,\n 41.0565730874647\n ],\n [\n -123.72802734375,\n 41.0565730874647\n ],\n [\n -123.72802734375,\n 41.599013054830216\n ],\n [\n -124.134521484375,\n 41.599013054830216\n ],\n [\n -124.134521484375,\n 41.0565730874647\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Barnhart, R.A.","contributorId":223148,"corporation":false,"usgs":false,"family":"Barnhart","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":784286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyd, M.J.","contributorId":223149,"corporation":false,"usgs":false,"family":"Boyd","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":784287,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pequegnat, J.E.","contributorId":223150,"corporation":false,"usgs":false,"family":"Pequegnat","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":784288,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70206821,"text":"70206821 - null - Using GIS to determine the effects of contaminated sediments on natural resources in an estuary","interactions":[],"lastModifiedDate":"2019-11-22T16:47:23","indexId":"70206821","displayToPublicDate":"1992-12-31T16:33:58","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Using GIS to determine the effects of contaminated sediments on natural resources in an estuary","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the second international US Fish and Wildlife Service geographic information systems workshop","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second International U. S. Fish and Wildlife Service Geographic Information Systems Workshop","conferenceDate":"June 10-13, 1991","conferenceLocation":"Fort Collins, CO","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Roscigno, P., Martin, G.M., Johnston, J.B., and Watzin, M.C., Using GIS to determine the effects of contaminated sediments on natural resources in an estuary, in Proceedings of the second international US Fish and Wildlife Service geographic information systems workshop, Fort Collins, CO, June 10-13, 1991, p. 41-50.","productDescription":"10 p.","startPage":"41","endPage":"50","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":369504,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama","otherGeospatial":"Mobile Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.13232421875,\n 30.548069799103555\n ],\n [\n -88.385009765625,\n 30.479449996609706\n ],\n [\n -88.36029052734375,\n 30.268556249047727\n ],\n [\n -87.62695312499999,\n 30.29701788337205\n ],\n [\n -87.62420654296875,\n 30.510216587229984\n ],\n [\n -87.8302001953125,\n 30.493651170505892\n ],\n [\n -87.791748046875,\n 30.873940237887624\n ],\n [\n -88.10211181640624,\n 30.878654895778272\n ],\n [\n -88.12408447265625,\n 30.786677249436945\n ],\n [\n -88.13232421875,\n 30.548069799103555\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Roscigno, P.F.","contributorId":67628,"corporation":false,"usgs":true,"family":"Roscigno","given":"P.F.","affiliations":[],"preferred":false,"id":775932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, G. M.","contributorId":220843,"corporation":false,"usgs":false,"family":"Martin","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":775933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnston, J. B.","contributorId":220844,"corporation":false,"usgs":false,"family":"Johnston","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":775934,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Watzin, Mary C.","contributorId":214534,"corporation":false,"usgs":false,"family":"Watzin","given":"Mary","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":775935,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70216450,"text":"70216450 - null - Oxidation of hydrocarbons coupled to reduction of inorganic species in groundwater","interactions":[],"lastModifiedDate":"2020-11-18T15:18:47.546496","indexId":"70216450","displayToPublicDate":"1992-11-18T09:17:16","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Oxidation of hydrocarbons coupled to reduction of inorganic species in groundwater","docAbstract":"No abstract available.
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","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 7th international symposium on water-rock interaction","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceDate":"July 9-23, 1992","conferenceLocation":"Park City, UT","language":"English","publisher":"U.S. Department of Energy","usgsCitation":"Baedecker, M.J., Cozzarelli, I.M., Evans, J., and Hearn, P., Authigenic mineral formation in aquifers rich in organic material, in Proceedings of the 7th international symposium on water-rock interaction, Park City, UT, July 9-23, 1992, p. 257-261.","productDescription":"5 p.","startPage":"257","endPage":"261","costCenters":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":380598,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":380597,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.osti.gov/biblio/10140738-water-rock-interaction-proceedings-volume-low-temperature-environments"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Baedecker, Mary Jo 0000-0002-4865-1043 mjbaedec@usgs.gov","orcid":"https://orcid.org/0000-0002-4865-1043","contributorId":197793,"corporation":false,"usgs":true,"family":"Baedecker","given":"Mary","email":"mjbaedec@usgs.gov","middleInitial":"Jo","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":805148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cozzarelli, Isabelle M. 0000-0002-5123-1007 icozzare@usgs.gov","orcid":"https://orcid.org/0000-0002-5123-1007","contributorId":1693,"corporation":false,"usgs":true,"family":"Cozzarelli","given":"Isabelle","email":"icozzare@usgs.gov","middleInitial":"M.","affiliations":[{"id":49175,"text":"Geology, Energy & Minerals Science Center","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":805149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, J.R.","contributorId":50526,"corporation":false,"usgs":true,"family":"Evans","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":805150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hearn, P.P.","contributorId":18380,"corporation":false,"usgs":true,"family":"Hearn","given":"P.P.","affiliations":[],"preferred":false,"id":805151,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70269553,"text":"70269553 - null - Solitary cases of duck plague in migratory waterfowl: Evidence of a problem?","interactions":[],"lastModifiedDate":"2025-07-25T14:41:20.327563","indexId":"70269553","displayToPublicDate":"1989-05-01T09:37:37","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":70,"text":"Research Information Bulletin","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"89-41","title":"Solitary cases of duck plague in migratory waterfowl: Evidence of a problem?","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Fish & Wildlife Service","usgsCitation":"Docherty, D., and Brand, C.J., Solitary cases of duck plague in migratory waterfowl: Evidence of a problem?: Research Information Bulletin 89-41, 2 p.","productDescription":"2 p.","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":492909,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"1989-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Docherty, Douglas E.","contributorId":58245,"corporation":false,"usgs":true,"family":"Docherty","given":"Douglas E.","affiliations":[],"preferred":false,"id":944040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brand, Christopher J. cbrand@usgs.gov","contributorId":1186,"corporation":false,"usgs":true,"family":"Brand","given":"Christopher","email":"cbrand@usgs.gov","middleInitial":"J.","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":944041,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70236906,"text":"70236906 - null - Radiation exposure near Chernobyl based on analysis of conifer injury using Thematic Mapper satellite images","interactions":[],"lastModifiedDate":"2022-09-21T14:57:59.249544","indexId":"70236906","displayToPublicDate":"1988-12-31T09:51:28","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Radiation exposure near Chernobyl based on analysis of conifer injury using Thematic Mapper satellite images","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Joint CEC/OECD(NEA) workshop on recent advances in reactor accident consequence assessment","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Joint CEC/OECD(NEA) Workshop on Recent Advances in Reactor Accident Consequence Assessment","conferenceDate":"Jan 25-29, 1988","conferenceLocation":"Rome, Italy","language":"English","publisher":"OECD Nuclear energy Agency","usgsCitation":"Goldman, M., Ustin, S.L., Warman, E.A., and Sadowski, F.G., Radiation exposure near Chernobyl based on analysis of conifer injury using Thematic Mapper satellite images, in Joint CEC/OECD(NEA) workshop on recent advances in reactor accident consequence assessment, Rome, Italy, Jan 25-29, 1988, 10 p.","productDescription":"10 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":407137,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Ukraine","otherGeospatial":"Chernobyl","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 29.729003906249996,\n 51.18106473752023\n ],\n [\n 30.25634765625,\n 51.18106473752023\n ],\n [\n 30.25634765625,\n 51.600959780448626\n ],\n [\n 29.729003906249996,\n 51.600959780448626\n ],\n [\n 29.729003906249996,\n 51.18106473752023\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Goldman, Marvin","contributorId":296884,"corporation":false,"usgs":false,"family":"Goldman","given":"Marvin","email":"","affiliations":[],"preferred":false,"id":852661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ustin, Susan L.","contributorId":52878,"corporation":false,"usgs":false,"family":"Ustin","given":"Susan","email":"","middleInitial":"L.","affiliations":[{"id":7214,"text":"University of California, Davis","active":true,"usgs":false}],"preferred":false,"id":852662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Warman, Edward A.","contributorId":296885,"corporation":false,"usgs":false,"family":"Warman","given":"Edward","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":852663,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sadowski, F. G.","contributorId":91634,"corporation":false,"usgs":true,"family":"Sadowski","given":"F.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":852664,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70209260,"text":"70209260 - null - Storm‐dominated bottom boundary layer dynamics on the Northern California Continental Shelf: Measurements and predictions","interactions":[],"lastModifiedDate":"2020-03-25T14:50:41","indexId":"70209260","displayToPublicDate":"1987-03-25T14:36:27","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2315,"text":"Journal of Geophysical Research C: Oceans","active":true,"publicationSubtype":{"id":10}},"title":"Storm‐dominated bottom boundary layer dynamics on the Northern California Continental Shelf: Measurements and predictions","docAbstract":"Measurements of near‐bottom velocity profiles in 85 m water depth during a storm on the continental shelf off northern California using the GEOPROBE tripod in December 1979 provided estimates of shear velocities, , and roughness lengths, , when the near‐bottom velocity profiles were logarithmic. These estimates agree within 90% confidence intervals with values computed from a simple near‐bottom combined wave‐current model that includes movable bed effects. The reasonably good comparison between model and profile estimates of suggests that such models can be used to predict bed shear stresses (or shear velocities) under combined flows of waves and currents typical of stormy conditions on continental shelves if stratification corrections to the velocity profile resulting from suspended sediment are small. The repeated occurrences of storms of similar intensities and wind velocities during the winter months off northern California suggest that the resultant high bottom stresses due to the combined effects of waves and currents are major factors in controlling the distribution of surficial sediment on the central portion of the northern California shelf.
","doi":"10.1029/JC092iC02p01817","usgsCitation":"Cacchione, D., Grant, W., Drake, D., and Glenn, S., Storm‐dominated bottom boundary layer dynamics on the Northern California Continental Shelf: Measurements and predictions: Journal of Geophysical Research C: Oceans, v. 92, no. C2, p. 1817-1827, https://doi.org/10.1029/JC092iC02p01817.","productDescription":"11 p.","startPage":"1817","endPage":"1827","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":373529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Northern California Continental Shelf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.2718505859375,\n 37.99183365313853\n ],\n [\n -122.7008056640625,\n 37.99183365313853\n ],\n [\n -122.7008056640625,\n 39.00211029922515\n ],\n [\n -124.2718505859375,\n 39.00211029922515\n ],\n [\n -124.2718505859375,\n 37.99183365313853\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"92","issue":"C2","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":785618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, W.D.","contributorId":11764,"corporation":false,"usgs":true,"family":"Grant","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":785619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":785620,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glenn, S.M.","contributorId":223608,"corporation":false,"usgs":false,"family":"Glenn","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":785621,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70204780,"text":"70204780 - null - Summary of the conference and information needs for mitigation in wetlands","interactions":[],"lastModifiedDate":"2019-08-15T12:46:53","indexId":"70204780","displayToPublicDate":"1986-12-31T12:45:27","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"seriesNumber":"86-14","chapter":"8","title":"Summary of the conference and information needs for mitigation in wetlands","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Wetland Functions, Rehabilitation, and Creation in the Pacific Northwest: The State of our Understanding ","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"conferenceDate":"Apr 30-May 2, 1986","conferenceLocation":"Port Townsend, WA","usgsCitation":"Quammen, M.L., Summary of the conference and information needs for mitigation in wetlands, chap. 8 of Wetland Functions, Rehabilitation, and Creation in the Pacific Northwest: The State of our Understanding , p. 151-158.","productDescription":"8 p.","startPage":"151","endPage":"158","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":366573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":366572,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://fortress.wa.gov/ecy/publications/SummaryPages/8614.html"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Quammen, Millicent L.","contributorId":218143,"corporation":false,"usgs":false,"family":"Quammen","given":"Millicent","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":768462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70204765,"text":"70204765 - null - Vegetation pattern on channel features in the Passage Creek Gorge, Virginia","interactions":[],"lastModifiedDate":"2019-08-14T10:53:25","indexId":"70204765","displayToPublicDate":"1983-08-14T10:46:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1195,"text":"Castanea","active":true,"publicationSubtype":{"id":10}},"title":"Vegetation pattern on channel features in the Passage Creek Gorge, Virginia","docAbstract":"Persistent distribution patterns of woody vegetation within the bottomland forest of Passage Creek, Virginia, were related to fluvial landforms, channel geometry, streamflow characteristics, and sediment-size characteristics. Vegetation patterns were determined from species presence as observed in transects and traverses on landforms developed along the stream. Distinct species distributional patterns were found on four common fluvial geomorphic landforms: depositional bar, active-channel shelf, floodplain, and terrace. Independent hydrologic characteristics (flow duration and flood frequency) were determined for each of the landforms. Vegetation data were analyzed by binary discriminant analysis, principal components analysis, and detrended correspondence analysis. Results and related field observations suggest that certain species are significantly associated with specific fluvial landforms. Vegetation patterns appear to develop more as a result of hydrologic processes associated with each fluvial landform rather than from sediment-size characteristics. Flood disturbance may be an important factor in maintaining the vegetation patterns, which may therefore be used as indicators for particular hydrogeomorphic site conditions.
No abstract available.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Milankovitch and Climate: Understanding the Response to Astronomical Forcing","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Advanced Research Workshop on Milankovitch and Climate","conferenceDate":"November 30- December 4, 1982","conferenceLocation":"Palisades, New York","language":"English","publisher":"Springer","usgsCitation":"Arthur, M., Dean, W.E., Bottjer, D., and Scholle, P.A., Rhythmic bedding in Mesozoic- Cenozoic pelagic carbonate sequences: The primary and diagenetic origin of Milankovitch-like cycles, in Milankovitch and Climate: Understanding the Response to Astronomical Forcing, v. 1, Palisades, New York, November 30- December 4, 1982, p. 191-222.","productDescription":"32","startPage":"191","endPage":"222","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374584,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Arthur, M.A.","contributorId":24791,"corporation":false,"usgs":true,"family":"Arthur","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":788812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bottjer, D.J.","contributorId":73370,"corporation":false,"usgs":true,"family":"Bottjer","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":788814,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scholle, Peter A.","contributorId":48954,"corporation":false,"usgs":true,"family":"Scholle","given":"Peter","email":"","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":788815,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70207209,"text":"70207209 - null - PIERRE PERRAULT: THE MAN AND HIS CONTRIBUTION TO MODERN HYDROLOGY","interactions":[],"lastModifiedDate":"2019-12-12T09:50:36","indexId":"70207209","displayToPublicDate":"1974-08-31T09:48:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2126,"text":"JAWRA","active":true,"publicationSubtype":{"id":10}},"title":" PIERRE PERRAULT: THE MAN AND HIS CONTRIBUTION TO MODERN HYDROLOGY","docAbstract":"ABSTRACT: Pierre Perrault, member of a bourgeois provincial family whose roots were in the Touraine region of France, grew up in Paris. One of six illustrious Brothers, all characterized by brilliance and diversity, he was educated as a lawyer but turned to finance and rose to a high position under King Louis XIV. Owing to political naivete and financial imprudence, he fell into disgrace and went bankrupt. He then became an amateur scientist and wrote a book on the origin of springs. This book broke almost wholly with the traditional authoritarianism of 2, 000 years'standing, and set hydrology on the modern path of observation and direct experiment, He developed the concept of the hydrological cycle, correctly accounting for the disposition of rainfall by evaporation, transpiration, ground‐water recharge and runoff. Some of his ideas about specific processes were erroneous, but where he was wrong his errors were logically based. Much of his contribution to the foundation of scientific hydrology has been overlooked or distorted by historians and hydrologists alike. Copyright © 1974, Wiley Blackwell. All rights reserved
","language":"English","publisher":"Wiley Blackwell ","doi":"10.1111/j.1752-1688.1974.tb05623.x","issn":"1093474X","usgsCitation":"Nace, R.L., PIERRE PERRAULT: THE MAN AND HIS CONTRIBUTION TO MODERN HYDROLOGY: JAWRA, v. 10, no. 4, p. 633-647, https://doi.org/10.1111/j.1752-1688.1974.tb05623.x.","productDescription":"15 p. ","startPage":"633","endPage":"647","costCenters":[],"links":[{"id":370202,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"4","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":777276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70226540,"text":"70226540 - null - Relations between geological structure and aeromagnetic anomalies in central Nevada","interactions":[],"lastModifiedDate":"2021-11-23T14:52:50.982766","indexId":"70226540","displayToPublicDate":"1970-07-01T08:42:20","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Relations between geological structure and aeromagnetic anomalies in central Nevada","docAbstract":"An aeromagnetic survey of a 6000-km2 area in central Nevada has been complied by the U.S. Geological Survey. An interpretation of the aeromagnetic data is developed to establish relations between near-surface geological features and structure extending to intermediate depths in the crust.
A three-dimensional distribution of magnetized material is described which would reproduce approximately the observed aeromagnetic anomalies. Anomaly sources extend from the surface to depths exceeding 15 km and require values of magnetic moment per unit volume averaging more than 2000 × 10−6 (cgs).
Magnetic anomaly lineations were analyzed by two methods. The first involves digital fan filtering and subsequent autocovariance computations. This method is sensitive to amplitude of linear anomalies, and indicated a dominant north-northwest trend with approximately 80 percent of the anomaly trend power in an azimuth range of northwest to northeast. The second method involves preparation of rosettes from measured lengths and azimuths of lineations indicated by noses and flexures on the contoured map. This method is not sensitive to anomaly amplitude. The dominant N. 10°E. trend determined in this way is indicative of the effect of near-surface geological structure on the magnetic field.
The dominant north-northwest-trending zone of magnetic anomalies is located along an alinement of windows through the Roberts Mountains thrust fault. This suggests that elongate doming of the Paleozoic sedimentary rocks associated with the thrust may be related to emplacement of magnetic anomaly source material, and implies that this has been a zone of recurring tectonic activity since late Paleozoic time. Analysis of stresses possibly associated with forceful injection of magnetic anomaly sources and possible shear deformation along this north-northwest-trending zone suggests that these factors may have had a secondary influence on azimuths of high-angle faults and dikes.
","usgsCitation":"Robinson, E.S., Relations between geological structure and aeromagnetic anomalies in central Nevada: Bulletin of the Geological Society of America, v. 81, no. 7, p. 2045-2060.","productDescription":"16 p.","startPage":"2045","endPage":"2060","costCenters":[],"links":[{"id":392046,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Elko County, Eureka County, Lander County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.90551757812499,\n 39.29179704377487\n ],\n [\n -115.5706787109375,\n 39.29179704377487\n ],\n [\n -115.5706787109375,\n 40.76806170936614\n ],\n [\n -116.90551757812499,\n 40.76806170936614\n ],\n [\n -116.90551757812499,\n 39.29179704377487\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"81","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Robinson, Edwin S.","contributorId":269498,"corporation":false,"usgs":false,"family":"Robinson","given":"Edwin","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":827287,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206731,"text":"70206731 - null - Xenoliths in the honolulu volcanic series, Hawaii","interactions":[],"lastModifiedDate":"2019-11-19T07:55:53","indexId":"70206731","displayToPublicDate":"1970-06-30T07:53:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Xenoliths in the honolulu volcanic series, Hawaii","docAbstract":"The Pleistocene to Holocene Honolulu Volcanic Series was erupted from about 37 vents scattered over the older Koolau tholeiite shield. The rocks of this series are compositionally zoned with respect to the shield; near the Koolau caldera the predominant rocks are melilitenepheline basalts, but these give way outward to nepheline basalts, and ultimately, at the apron of the shield, to alkalic olivine basalts. The xenoliths in these are likewise zoned: most of those in the caldera area consist of dunite, most of those at intermediate distances of lherzolite, and some of those in the apron of the shield consist of garnet pyroxenite and peridotite. The zoning of the xenoliths, however, does not coincide with that of the enclosing rocks. We believe that copious eruption of Koolau tholeiite produced a lateral and vertical heterogeneity in the mantle beneath Oahu, and that the zoning in both Honolulu lavas and their xenoliths is caused by that heterogeneity. The textures of the xenoliths indicate that the basalts were mainly produced by fractional melting rather than fractional crystallization. There is some evidence that the dunite xenoliths are mantle residua produced during the generation of the tholeiite, and that the Honolulu magmas were generated at greater depths than the Koolau magmas, probably as a result of elastic unloading. © 1970 Oxford University Press.
","language":"English","publisher":"Oxford University Press ","doi":"10.1093/petrology/11.2.405","issn":"00223530","usgsCitation":"Jackson, E.D., and Wright, T.L., Xenoliths in the honolulu volcanic series, Hawaii: Journal of Petrology, v. 11, no. 2, p. 405-433, https://doi.org/10.1093/petrology/11.2.405.","productDescription":"29 p. 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\"}}]}","volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jackson, E. D.","contributorId":120010,"corporation":false,"usgs":true,"family":"Jackson","given":"E.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":775577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, T. L.","contributorId":11188,"corporation":false,"usgs":true,"family":"Wright","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":775578,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70230877,"text":"70230877 - null - Infrared sensing of active geologic processes","interactions":[],"lastModifiedDate":"2022-05-04T15:23:37.922376","indexId":"70230877","displayToPublicDate":"1968-01-01T10:23:09","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Infrared sensing of active geologic processes","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the Fifth Symposium on Remote Sensing of Environment","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Fifth Symposium on Remote Sensing of Environment","conferenceDate":"April 16-18, 1968","conferenceLocation":"Ann Arbor, Michigan","language":"English","publisher":"University of Michigan","usgsCitation":"Friedman, J.D., and Williams, R.S., Infrared sensing of active geologic processes, in Proceedings of the Fifth Symposium on Remote Sensing of Environment, Ann Arbor, Michigan, April 16-18, 1968, p. 787-820.","productDescription":"34 p.","startPage":"787","endPage":"820","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":399758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":399756,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://symposia.org/past_symposia.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Friedman, J. D.","contributorId":99157,"corporation":false,"usgs":true,"family":"Friedman","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":841539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, R. S. Jr.","contributorId":95408,"corporation":false,"usgs":true,"family":"Williams","given":"R.","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":841540,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221063,"text":"70221063 - null - Garnet types from the Cazadero area, California","interactions":[],"lastModifiedDate":"2021-06-01T16:26:08.813129","indexId":"70221063","displayToPublicDate":"1963-01-01T11:19:08","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Garnet types from the Cazadero area, California","docAbstract":"This is the third in a series of papers on glaucophane schists from the Franciscan Formation near Cazadero, California. Previous papers describe three distinct types of glaucophane-bearing Franciscan metamorphic rocks near Cazadero.
The purpose of this study is to investigate the garnets present in metamorphic types III (bedrock schists) and IV (tectonic blocks) as defined by Coleman & Lee (1963). Twenty-four garnet analyses are presented. Sixteen of these are from (aragonite-bearing) type III glaucophane schists, and eight are from type IV glaucophane schists. Type IV rocks include California eclogites.
Type III rocks include metabasalt, metachert, metashale, meta-ironstone, and metacarbonate that were formed under high pressure and relatively low temperature. These rocks contain garnets that display a wide range of composition, but the dominant molecules represented are consistently almandine, spessartine, and grossular.
Type IV rocks are mainly metabasalts that were probably formed under higher temperatures and pressures than type III rocks. There is a distinct difference between garnets from type III rocks and those from type IV (including eclogites); the lattercontain less spessartine and more pyrope, and the dominant molecules are almandine and grossular. The four analyses of garnets from California eclogites have an average pyrope content of about ten molecular per cent, and they extend the range of composition reported for eclogite garnets.
Quantitative spectrographic determinations of minor elements are listed for each of the garnets described. The values determined for some of the minor elements have a wide range and a capricious distribution over a few feet of outcrop area.
As a group, both the garnets from type III rocks and those from type IV are pyralspites with large contents (as much as 35 molecular per cent) of ugrandite. This unusual admixture of the pyralspite and ugrandite garnet series may have resulted in part from the conditions (high pressures and relatively low temperatures) under which the enclosing rocks were recrystallized.
","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/4.3.460","usgsCitation":"Lee, D.E., Coleman, R.G., and Erd, R.C., Garnet types from the Cazadero area, California: Journal of Petrology, v. 4, no. 3, p. 460-492, https://doi.org/10.1093/petrology/4.3.460.","productDescription":"33 p.","startPage":"460","endPage":"492","costCenters":[],"links":[{"id":386035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Cazadero area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.1787109375,\n 38.44390909175749\n ],\n [\n -122.77084350585938,\n 38.44390909175749\n ],\n [\n -122.77084350585938,\n 38.72623322072787\n ],\n [\n -123.1787109375,\n 38.72623322072787\n ],\n [\n -123.1787109375,\n 38.44390909175749\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lee, D. E.","contributorId":96705,"corporation":false,"usgs":true,"family":"Lee","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":816676,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erd, Richard C.","contributorId":89899,"corporation":false,"usgs":true,"family":"Erd","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816677,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220528,"text":"70220528 - null - Effect on evaporation of releases from reservoirs on Salt River, Arizona","interactions":[],"lastModifiedDate":"2021-05-18T17:05:16.62051","indexId":"70220528","displayToPublicDate":"1960-09-30T11:59:52","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Effect on evaporation of releases from reservoirs on Salt River, Arizona","docAbstract":"By means of the energy-budget method, measurements of evaporation losses from four reservoirs on Salt River, Ariz., were determined to range from 57.5 to 69.9 inches for the 12-month period April 1958 to March 1959. Water is withdrawn from Roosevelt Lake at considerable depth and released through three run-of-the-river reservoirs. Because the water released from Roosevelt Lake is cold, evaporation losses from the downstream reservoirs are considerably lower than those from Roosevelt Lake. Evaporation pan coefficients computed for the various reservoirs ranged from 0.53 to 0.65. A base evaporation rate was computed for each reservoir as the evaporation rate that would have occurred had there been no change in energy storage and the net advected energy equalled zero during the year.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493178","usgsCitation":"Koberg, G., Effect on evaporation of releases from reservoirs on Salt River, Arizona: International Association of Scientific Hydrology - Bulletin , v. 5, no. 3, p. 37-44, https://doi.org/10.1080/02626666009493178.","productDescription":"8 p.","startPage":"37","endPage":"44","costCenters":[],"links":[{"id":480529,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666009493178","text":"Publisher Index Page"},{"id":385715,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Salt River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.2637939453125,\n 33.28921188443142\n ],\n [\n -110.8245849609375,\n 33.28921188443142\n ],\n [\n -110.8245849609375,\n 33.75631505992707\n ],\n [\n -112.2637939453125,\n 33.75631505992707\n ],\n [\n -112.2637939453125,\n 33.28921188443142\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Koberg, G.E.","contributorId":258181,"corporation":false,"usgs":false,"family":"Koberg","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":815905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70205259,"text":"70205259 - null - Field guidebook, June 1959","interactions":[],"lastModifiedDate":"2019-09-12T07:11:19","indexId":"70205259","displayToPublicDate":"1960-09-10T14:00:46","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5716,"text":"Oregon State Department of Geology and Mineral Industries Bulletin","active":true,"publicationSubtype":{"id":2}},"subchapterNumber":"John Day to upper Bear Valley, Field Trip no. 5","title":"Field guidebook, June 1959","docAbstract":"No abstract available.
","usgsCitation":"Wilkinson , W., and Thayer, T.P., Field guidebook, June 1959: Oregon State Department of Geology and Mineral Industries Bulletin, v. 50, 5 p.","productDescription":"5 p.","startPage":"98","endPage":"102","costCenters":[],"links":[{"id":367324,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Oregon ","city":"John Day ","otherGeospatial":"Bear Valley ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.08905029296874,\n 44.178756972181695\n ],\n [\n -118.86177062988281,\n 44.178756972181695\n ],\n [\n -118.86177062988281,\n 44.423482510295\n ],\n [\n -119.08905029296874,\n 44.423482510295\n ],\n [\n -119.08905029296874,\n 44.178756972181695\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"50","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Wilkinson , William Donald ","contributorId":218871,"corporation":false,"usgs":false,"family":"Wilkinson ","given":"William Donald ","affiliations":[{"id":6605,"text":"USGS","active":true,"usgs":false},{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false}],"preferred":false,"id":770588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thayer, Thomas P","contributorId":218870,"corporation":false,"usgs":false,"family":"Thayer","given":"Thomas","email":"","middleInitial":"P","affiliations":[{"id":7198,"text":"Oregon Department Geology and Mineral Industries","active":true,"usgs":false},{"id":6605,"text":"USGS","active":true,"usgs":false}],"preferred":false,"id":770589,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220485,"text":"70220485 - null - Interpretation of potentiometric titration of H-montmorillonite","interactions":[],"lastModifiedDate":"2021-05-17T11:42:56.604558","indexId":"70220485","displayToPublicDate":"1960-02-27T06:40:25","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Interpretation of potentiometric titration of H-montmorillonite","docAbstract":"No abstract available.
","language":"English","publisher":"Nature","doi":"10.1038/185595a0","usgsCitation":"Pommer, A., and Carroll, D., Interpretation of potentiometric titration of H-montmorillonite: Nature, v. 185, no. 4713, p. 595-596, https://doi.org/10.1038/185595a0.","productDescription":"2 p.","startPage":"595","endPage":"596","costCenters":[],"links":[{"id":385666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"185","issue":"4713","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pommer, A. M.","contributorId":20795,"corporation":false,"usgs":false,"family":"Pommer","given":"A. M.","affiliations":[],"preferred":false,"id":815732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carroll, D.","contributorId":84495,"corporation":false,"usgs":true,"family":"Carroll","given":"D.","email":"","affiliations":[],"preferred":false,"id":815733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70212510,"text":"70212510 - null - Yield of sediment in relation to mean annual precipitation","interactions":[],"lastModifiedDate":"2020-08-18T18:22:07.775793","indexId":"70212510","displayToPublicDate":"1958-08-18T13:05:30","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Yield of sediment in relation to mean annual precipitation","docAbstract":"Effective mean annual precipitation is related to sediment yield from drainage basins throughout the climatic regions of the United States. Sediment yield is a maximum at about 10 to 14 inches of precipitation, decreasing sharply on both sides of this maximum in one case owing to a deficiency of runoff and in the other to increased density of vegetation. Data are presented illustrating the increase in bulk density of vegetation with increased annual precipitation and the relation of relative erosion to vegetative density. It is suggested that the effect of a climatic change on sediment yield depends not only upon direction of climate change, but also on the climate before the change. Sediment concentration in runoff is shown to increase with decreased annual precipitation, suggesting further that a decrease in precipitation will cause stream channel aggradation
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR039i006p01076","usgsCitation":"Langbein, W., and Schumm, S.A., Yield of sediment in relation to mean annual precipitation: Eos, Transactions, American Geophysical Union, v. 39, no. 6, p. 1076-1084, https://doi.org/10.1029/TR039i006p01076.","productDescription":"9 p.","startPage":"1076","endPage":"1084","costCenters":[],"links":[{"id":377629,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, Walter B.","contributorId":98294,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter B.","affiliations":[],"preferred":false,"id":796634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schumm, S. A.","contributorId":71957,"corporation":false,"usgs":true,"family":"Schumm","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":796635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70216123,"text":"70216123 - null - Application of fluorescent x-ray spectroscopy in geochemistry","interactions":[],"lastModifiedDate":"2020-11-05T18:33:18.588376","indexId":"70216123","displayToPublicDate":"1955-11-05T12:11:14","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Application of fluorescent x-ray spectroscopy in geochemistry","docAbstract":"No abstract available.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1955)66[1525:AOFXSI]2.0.CO;2","usgsCitation":"Adler, I., and Axelrod, J.M., Application of fluorescent x-ray spectroscopy in geochemistry: GSA Bulletin, v. 66, no. 12, p. 1525-1640, https://doi.org/10.1130/0016-7606(1955)66[1525:AOFXSI]2.0.CO;2.","productDescription":"16 p.","startPage":"1525","endPage":"1640","costCenters":[],"links":[{"id":380205,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Adler, I.","contributorId":13371,"corporation":false,"usgs":true,"family":"Adler","given":"I.","email":"","affiliations":[],"preferred":false,"id":804194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Axelrod, J. M.","contributorId":29796,"corporation":false,"usgs":true,"family":"Axelrod","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":804195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206627,"text":"70206627 - null - Ocoee series of the southern Appalachians","interactions":[],"lastModifiedDate":"2019-11-14T06:58:02","indexId":"70206627","displayToPublicDate":"1949-12-31T06:50:08","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Ocoee series of the southern Appalachians","title":"Ocoee series of the southern Appalachians","docAbstract":"The Ocoee series is divided into four major units present from northern North Carolina to western Georgia and a fifth, younger, formation present only in southern North Carolina and Georgia. The units recognize dare as follows: The Ocoee series is a broad synclinal belt of resistant Great Smoky quartzite, which forms most of the Great Smoky Mountains and the Bald Mountains, with Nantahala slate and in places the Big Butt quartzite enclosed in synclines; the Hurricane graywacke is on the flanks of the main syncline. In the deeper Murphy syncline the Big Butt quartzite is overlain by the Valleytown formation. The Ocoee series is thrust northwestward on the Great Smoky overthrust over Paleozoic rocks of the Great Valley, and in Tennessee overrides unmetamorphosed sandstone, shale, limestone, and limestone conglomerate which previously were mapped as Wilhite slate and were included in the Ocoee series. These rocks in a few places contain Middle Ordovician fossils and are a newly recognized part of a clastic shore facies equivalent to an expanded Tellico sandstone of undetermined stratigraphic range. This part of the Ordovician shore facies is in the Pulaski block in Tennessee and is exposed also in windows in the Great Smoky overthrust block in Tennessee, North Carolina, and Georgia. The Ocoee series does not resemble the Lower Cambrian Chilhowee group, which it overrides, nor any other Lower Cambrian facies. Lower Cambrian quartzites overlie with erosional unconformity the Catoctin basalt, Swift Run tuff, and Mt. Rogers volcanic series, proving that these volcanic rocks are late pre-Cambrian. The Ocoee series resembles the Lynchburg gneiss, which is equivalent to the late pre-Cambrian Swift Run tuff. The Ocoee series is stratigraphically overlain by the Lower Cambrian Unicoi formation and is late pre-Cambrian. © 1949, The Geological Society of America, Inc.
","language":"English ","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1949)60[267:OSOTSA]2.0.CO;2","issn":" 00167606","usgsCitation":"George, W., and Stose, A., Ocoee series of the southern Appalachians: Geological Society of America Bulletin, v. 60 , no. 2, p. 267-320, https://doi.org/10.1130/0016-7606(1949)60[267:OSOTSA]2.0.CO;2.","productDescription":"54 p.","startPage":"267","endPage":"320","costCenters":[],"links":[{"id":369185,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"North Carolina, 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\"}}]}","volume":"60 ","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"George, W.O.","contributorId":41886,"corporation":false,"usgs":true,"family":"George","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":775256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stose, A.J.","contributorId":88808,"corporation":false,"usgs":true,"family":"Stose","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":775257,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206352,"text":"70206352 - null - The problem of the Chelmsford, Massachusetts, Granite","interactions":[],"lastModifiedDate":"2019-10-30T17:56:49","indexId":"70206352","displayToPublicDate":"1937-07-01T17:48:36","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The problem of the Chelmsford, Massachusetts, Granite","docAbstract":"The Chelmsford granite is quarried in and around Oak Hill, about six miles west of Lowell, Massachusetts. The granite‐area is about eight miles long and one to three miles wide, and its longer dimension has a northeast bearing which is parallel with the regional axis of foliation in the country rock. The writer favors a hypothesis that much of the granite represents granitization of biotite schist under hydro‐magmatic invasion, and under stress that was insufficient to deform or distort the preexisting country rock‐structures to any marked degree. Banding of the granite is due chiefly, to variable amounts of biotite. The bands are thin and remarkably uniform. The banding, attitudes of schist inclusions, and distribution of the entire mass con form to the regional structural elements. Lit‐par‐lit injection‐bands are not clearly discernible although many of the light‐colored bands are doubtless of such origin. The absence of flow‐schlieren is noted. Petrographic evidence shows a remarkable amount of metasomatic fabric. Undoubted primary granitic texture is practically wanting. There is a high degree of orientation of biotite, muscovite, and groups of small mosaic quartz‐grains. The contacts of inclusions with adjacent granite‐bands are very irregular and interpenetrative, and granitic material also penetrates intricately along schistosity planes within the inclusions. Large irregular feldspar porphyroblasts and strings of such grains are distributed through the inclusions, generally with decreasing concentration toward the centers. Pegmatite and quartz veins, some of which carry much tourmaline, are abundant in some of the quarries. Crystallization zoning of feldspars is very rare. Feldspars are of three generations: (1) Early polysynthetically twinned porphyroblasts and irregular groundmass grains of oligoclase or albite‐oligoclase; (2) microcline and orthoclase, chiefly as porphyroblasts, and in part replacing the earlier plagioclase; and (3) albite and albite‐oligoclase, untwinned and mottled, as individual crystals, streaks, patches, and porphyroblasts, replacing microcline, quartz, and mica. Incomplete twinning, corrosion‐contacts, optical anomalies, inclusions of minerals, pseudo‐perthitic and myrmekitlc grains are among the diagnostic petrographic features that contribute to the theory of replacement.
","language":"English ","publisher":"Elsevier ","doi":"10.1029/TR018i001p00260","issn":" 00028606","usgsCitation":"Currier, L., The problem of the Chelmsford, Massachusetts, Granite: Eos, Transactions, American Geophysical Union, v. 18, no. 1, p. 260-261, https://doi.org/10.1029/TR018i001p00260.","productDescription":"2 pg. 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