No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp667","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Paxton quadrangle, Worcester County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 667, 1 Plate: 20.74 x 32.50 inches, https://doi.org/10.3133/gp667.","productDescription":"1 Plate: 20.74 x 32.50 inches","costCenters":[],"links":[{"id":491057,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6034.htm","linkFileType":{"id":5,"text":"html"}},{"id":253631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0667/report-thumb.jpg"},{"id":250131,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0667/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250130,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0667/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Worcester County","otherGeospatial":"Paxton quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.875,\n 42.25\n ],\n [\n -71.875,\n 42.375\n ],\n [\n -72,\n 42.375\n ],\n [\n -72,\n 42.25\n ],\n [\n -71.875,\n 42.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b6a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533330,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14339,"text":"ofr69134 - 1969 - Preliminary geologic interpretation of aeromagnetic data in the Yakutat district, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr69134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-134","title":"Preliminary geologic interpretation of aeromagnetic data in the Yakutat district, Alaska","docAbstract":"An aeromagnetic survey covering portions of the Yakutat Feveland region in south-central Alaska was made to delineate concentrations of magnetic minerals possibly associated with heavy mineral placers in beach sands and raised beach ridges. However, the larger magnetic anomalies do not correlate with the beach placers in the surveyed area. The dominant magnetic feature, a strong linear positive anomaly almost parallel to the coastline, is thought to reflect a bedrock feature, probably a mafic igneous body enclosed within nonmagnetic rocks of the Yakutat group.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr69134","usgsCitation":"Johnson, G.R., and Plafker, G., 1969, Preliminary geologic interpretation of aeromagnetic data in the Yakutat district, Alaska: U.S. Geological Survey Open-File Report 69-134, 13 p. ill., maps (4 folded, col.) ;27 cm., https://doi.org/10.3133/ofr69134.","productDescription":"13 p. ill., maps (4 folded, col.) ;27 cm.","costCenters":[],"links":[{"id":106424,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8364.htm","linkFileType":{"id":5,"text":"html"},"description":"8364"},{"id":148273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0134/report-thumb.jpg"},{"id":43003,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0134/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43004,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0134/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43005,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0134/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43006,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0134/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43007,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c304","contributors":{"authors":[{"text":"Johnson, Gordon R.","contributorId":90725,"corporation":false,"usgs":true,"family":"Johnson","given":"Gordon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":169287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":169286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63875,"text":"gp666 - 1969 - Aeromagnetic map of the North Brookfield quadrangle, Worcester County, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-20T19:02:57.018425","indexId":"gp666","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"666","title":"Aeromagnetic map of the North Brookfield quadrangle, Worcester County, Massachusetts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp666","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the North Brookfield quadrangle, Worcester County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 666, 1 Plate: 21.11 x 31.72 inches, https://doi.org/10.3133/gp666.","productDescription":"1 Plate: 21.11 x 31.72 inches","costCenters":[],"links":[{"id":491056,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6033.htm","linkFileType":{"id":5,"text":"html"}},{"id":250157,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0666/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250156,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0666/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253644,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0666/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Worcester County","otherGeospatial":"North Brookfield quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72,\n 42.25\n ],\n [\n -72,\n 42.375\n ],\n [\n -72.125,\n 42.375\n ],\n [\n -72.125,\n 42.25\n ],\n [\n -72,\n 42.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cad","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2865,"text":"wsp1535N - 1969 - Occurrence and distribution of molybdenum in the surface water of Colorado","interactions":[],"lastModifiedDate":"2024-01-12T19:19:19.414003","indexId":"wsp1535N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1535","chapter":"N","title":"Occurrence and distribution of molybdenum in the surface water of Colorado","docAbstract":"Molybdenum was detected in 89 percent of the samples collected from all the \r\nprincipal Colorado streams and their chief tributaries and from a few reservoirs \r\nand lakes. Amounts detected ranged from 1 to 3,800 micrograms per liter. The \r\ngreatest amounts of molybdenum detected were in samples from the Colorado \r\nRiver at and below Kremmling, the Dillon Reservoir, the Blue River below \r\nDillon Dam, the Eagle River, and Tenmile Creek.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1535N","usgsCitation":"Voegeli, P.T., and King, R.U., 1969, Occurrence and distribution of molybdenum in the surface water of Colorado: U.S. Geological Survey Water Supply Paper 1535, Report: iii, 32 p.; 1 Plate: 35.00 x 27.50 inches, https://doi.org/10.3133/wsp1535N.","productDescription":"Report: iii, 32 p.; 1 Plate: 35.00 x 27.50 inches","costCenters":[],"links":[{"id":29473,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1535n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29474,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535n/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138991,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535n/report-thumb.jpg"},{"id":109973,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24722.htm","linkFileType":{"id":5,"text":"html"},"description":"24722"}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.05973207922999,\n 40.96648042313683\n ],\n [\n -109.05973207922999,\n 36.97701757753603\n ],\n [\n -102.02316861780228,\n 36.97701757753603\n ],\n [\n -102.02316861780228,\n 40.96648042313683\n ],\n [\n -109.05973207922999,\n 40.96648042313683\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696357","contributors":{"authors":[{"text":"Voegeli, Paul Thomas","contributorId":54581,"corporation":false,"usgs":true,"family":"Voegeli","given":"Paul","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":145928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Robert Ugstad","contributorId":45696,"corporation":false,"usgs":true,"family":"King","given":"Robert","email":"","middleInitial":"Ugstad","affiliations":[],"preferred":false,"id":145927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14333,"text":"ofr69133 - 1969 - Bibliography of the geology and mineral industry of Liberia and adjacent countries","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr69133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-133","title":"Bibliography of the geology and mineral industry of Liberia and adjacent countries","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69133","usgsCitation":"Johnson, D.H., and White, R.W., 1969, Bibliography of the geology and mineral industry of Liberia and adjacent countries: U.S. Geological Survey Open-File Report 69-133, 65 p. ;28 cm., https://doi.org/10.3133/ofr69133.","productDescription":"65 p. ;28 cm.","costCenters":[],"links":[{"id":148250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0133/report-thumb.jpg"},{"id":43001,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0133/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627db3","contributors":{"authors":[{"text":"Johnson, Donald Haskall","contributorId":89543,"corporation":false,"usgs":true,"family":"Johnson","given":"Donald","email":"","middleInitial":"Haskall","affiliations":[],"preferred":false,"id":169279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Richard W.","contributorId":46954,"corporation":false,"usgs":true,"family":"White","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64879,"text":"i599 - 1969 - (RLC-14) Geologic map of the Alphonsus region of the moon","interactions":[],"lastModifiedDate":"2023-03-29T15:43:54.960798","indexId":"i599","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"599","subseriesTitle":"MOON","title":"(RLC-14) Geologic map of the Alphonsus region of the moon","docAbstract":"This 1:250,000- scale geologic map is one of a series prepared largely from photographs transmitted by Ranger IX (reproduced in a report by Jet Propulsion Lab., 1966). It depicts the geology of the crater Alphonsus (in which Ranger IX impacted) and environs. The primary objective of the mapping was to apply extant lunar mapping techniques used on relatively small scale telescopic photographs to the larger scale Ranger photographs, in preparation for extensive analysis of Lunar Orbiter photography in support of the Apollo program. An additional objective was to shed more light on the formation of Alphonsus and its associated features. The map outlines rock units that are inferred from surface features and characteristics, such as topography and albedo. Each rock unit is assigned an age and arranged in the explanation so that the youngest unit are at the top and the oldest at the bottom. The age classification is based on the early work of Shoemaker and Hackman (1962), and subsequent revisions reported by McCauley (1967) and Wilhelms (1966). Geology of the region has been mapped at a scale of 1:1,000,000 on the basis of Earth-based photographs and observations (Howard and Masursky, 1968). A more detailed, 1;50,000-scale map of part of the Alphonsus floor was prepared by McCauley (1969), who used Ranger IX photographs as his source of geologic information.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i599","collaboration":"prepared in cooperation with Jet Propulsion Laboratory, California Institute of Technology National Aeronautics and Space Administration, and the USAF Aeronautical Chart and Information Center","usgsCitation":"Carr, M.H., 1969, (RLC-14) Geologic map of the Alphonsus region of the moon: U.S. Geological Survey IMAP 599, Report; 1 map, https://doi.org/10.3133/i599.","productDescription":"Report; 1 map","costCenters":[],"links":[{"id":486697,"rank":5,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P1RZNFUX","text":"USGS data release","linkHelpText":"Interactive Map: IMAP 599 - (RLC-14) Geologic map of the Alphonsus region of the moon"},{"id":439075,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9WZPPZ8","text":"USGS data release","linkHelpText":"Geologic Map of the Alphonsus Region of the Moon"},{"id":189055,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0599/report-thumb.jpg"},{"id":114855,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0599/plate-1.pdf","size":"8446","linkFileType":{"id":1,"text":"pdf"}},{"id":114854,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0599/report.pdf","size":"47","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","otherGeospatial":"Alphonsus Crater, Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4906e4b0b290850eed1d","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":272304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15892,"text":"ofr69249 - 1969 - Availability of palynological material from Naval Petroleum Reserve No.4, XVII: Sentinel Hill Core Test No. 1","interactions":[],"lastModifiedDate":"2012-02-02T00:07:11","indexId":"ofr69249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-249","title":"Availability of palynological material from Naval Petroleum Reserve No.4, XVII: Sentinel Hill Core Test No. 1","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr69249","usgsCitation":"Scott, R., 1969, Availability of palynological material from Naval Petroleum Reserve No.4, XVII: Sentinel Hill Core Test No. 1: U.S. Geological Survey Open-File Report 69-249, 1 p. ;28 cm., https://doi.org/10.3133/ofr69249.","productDescription":"1 p. ;28 cm.","costCenters":[],"links":[{"id":149425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d7d5","contributors":{"authors":[{"text":"Scott, Richard A.","contributorId":14414,"corporation":false,"usgs":true,"family":"Scott","given":"Richard A.","affiliations":[],"preferred":false,"id":171889,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15658,"text":"ofr69225 - 1969 - Maps showing locations of holes drilled in 1951 to 1953 by U.S. Geological Survey, Spring Creek Mesa and San Miguel bench areas, Uravan district, Montrose County, Colorado","interactions":[],"lastModifiedDate":"2021-11-11T12:01:06.311179","indexId":"ofr69225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-225","title":"Maps showing locations of holes drilled in 1951 to 1953 by U.S. Geological Survey, Spring Creek Mesa and San Miguel bench areas, Uravan district, Montrose County, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69225","usgsCitation":"Roach, C.H., and Alvord, D.C., 1969, Maps showing locations of holes drilled in 1951 to 1953 by U.S. Geological Survey, Spring Creek Mesa and San Miguel bench areas, Uravan district, Montrose County, Colorado: U.S. Geological Survey Open-File Report 69-225, Report 2 p.; 3 Plates: 35.28 × 27.90 inches or smaller, https://doi.org/10.3133/ofr69225.","productDescription":"Report 2 p.; 3 Plates: 35.28 × 27.90 inches or smaller","costCenters":[],"links":[{"id":106440,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8398.htm","linkFileType":{"id":5,"text":"html"},"description":"8398"},{"id":146512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0225/report-thumb.jpg"},{"id":44624,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0225/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0225/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44622,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0225/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44623,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1969/0225/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Montrose County","otherGeospatial":"Spring Creek Mesa and San Miguel bench areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.746,\n 38.363\n ],\n [\n -108.578,\n 38.363\n ],\n [\n -108.578,\n 38.458\n ],\n [\n -108.746,\n 38.458\n ],\n [\n -108.746,\n 38.363\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605b70","contributors":{"authors":[{"text":"Roach, Carl Houston","contributorId":103295,"corporation":false,"usgs":true,"family":"Roach","given":"Carl","email":"","middleInitial":"Houston","affiliations":[],"preferred":false,"id":171508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alvord, Donald Clayton","contributorId":49356,"corporation":false,"usgs":true,"family":"Alvord","given":"Donald","email":"","middleInitial":"Clayton","affiliations":[],"preferred":false,"id":171507,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63884,"text":"gp662 - 1969 - Aeromagnetic map of the Mt. Holyoke quadrangle, Hampshire and Hampden Counties, Massachusetts","interactions":[],"lastModifiedDate":"2025-06-20T18:47:29.059536","indexId":"gp662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"662","title":"Aeromagnetic map of the Mt. Holyoke quadrangle, Hampshire and Hampden Counties, Massachusetts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp662","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Aeromagnetic map of the Mt. Holyoke quadrangle, Hampshire and Hampden Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 662, 1 Plate: 22.49 x 33.78 inches, https://doi.org/10.3133/gp662.","productDescription":"1 Plate: 22.49 x 33.78 inches","costCenters":[],"links":[{"id":253653,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0662/report-thumb.jpg"},{"id":250175,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0662/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250174,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491053,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6029.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Hampden County, Hampshire County","otherGeospatial":"Mt. Holyoke quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.5,\n 42.25\n ],\n [\n -72.5,\n 42.375\n ],\n [\n -72.625,\n 42.375\n ],\n [\n -72.625,\n 42.25\n ],\n [\n -72.5,\n 42.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d22","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2202,"text":"wsp1868 - 1969 - Sediment transport by streams in the Walla Walla River basin, Washington and Oregon, July 1962 - June 1965","interactions":[],"lastModifiedDate":"2021-12-06T21:19:26.174161","indexId":"wsp1868","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1868","title":"Sediment transport by streams in the Walla Walla River basin, Washington and Oregon, July 1962 - June 1965","docAbstract":"The Walla Walla River basin covers about 1,760 square miles in southeastern Washington and northeastern Oregon. From the 6,000-foot crest of the Blue Mountains on the east to the 340-foot altitude of Lake Wallula (Columbia River) on the west, the basin is drained by the Touchet River and Dry Creek, entirely within Washington, and by Mill Creek, North and South Forks Walla Walla River, and Pine Creek-Dry Creek, which all head in Oregon. The central lowland of the basin is bordered on the north by Eureka Flat, Touchet slope, and Skyrocket Hills, on the east by the Blue Mountains, and on the south by the Horse Heaven Hills. \r\n\r\nThe basin is underlain by basalt of the Columbia River Group, which .is the only consolidated rock to crop out in the region. Various unconsolidated fluviatile, lacustrine, and eolian sediments cover the basalt. In the western part of the basin the basalt is overlain by lacustrine deposits of silt and sand which in places are mantled by varying thicknesses of loessal deposits. In the northern and central parts of the basin the loess is at least 100 feet thick. The mountainous eastern part of the basin is underlain at shallow depth by basalt which has a residual soil mantle weathered from the rock. The slopes of the mountains are characterized by alluvial fans and deeply cut stream valleys ,filled with alluvium of sand, gravel, and cobbles. \r\n\r\nAverage annual precipitation in the basin ranges from less than 10 inches in the desert-like areas of the west to more than 45 inches in the timbered mountains of the east; 65 percent of the precipitation occurs from October through March. The average runoff from the basin is about 4.8 inches per year. Most of the runoff occurs during late winter and early spring. Exceptionally high runoff generally results from rainfall and rapid melting of snow on partially frozen ground. \r\n\r\nDuring the study period, July 1964-June 1965, average annual sediment yields in the basin ranged from 420 tons per square mile in the mountainous area to more than 4,000 tons per square mile in the extensively cultivated northern and central parts of the basin, which are drained by the Touchet River and Dry Creek. The Touchet River and Dry Creek transported approximately 80 percent of the total sediment load discharged from the Walla Walla River basin. The highest concentrations were contributed by the loessal deposits in the Dry Creek drainage. Two runoff events resulting from rain and snowmelt on partially frozen ground produced 76 percent of the suspended sediment discharged from the basin during the study period. The maximum concentration measured, 316,000 milligrams per liter, was recorded for Dry Creek at Lowden on December 23. 1964. \r\n\r\nDaily suspended-sediment concentrations for the Walla Walla River near Touchet exceeded 700 milligrams per liter about 10 percent of the time, and 14,000 milligrams per liter about 1 percent of the time. The discharge-weighted mean concentration for the 3-year period of study was 7,000 milligrams per liter. Silt predominates in the suspended sediment transported by all streams in the basin. On the average, sediment from streams draining the Blue Mountains was composed of 20 percent sand, 60 percent silt, and 20 percent clay ; for streams draining the Blue Mountains slope-Horse Heaven Hills area, the percentages are 9, 65, and 26, respectively ; and for those draining the Skyrocket Hills-Touchet slope, the percentages are 5, 75, and 20, respectively. \r\n\r\nThe bedload in the mountain and upland streams was estimated to be about 5-12 percent as much as the suspended load. For the Walla Walla River and its tributaries in the lower basin area, the bedload was estimated to be only about 2-8 percent as much as the suspended load.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1868","usgsCitation":"Mapes, B.E., 1969, Sediment transport by streams in the Walla Walla River basin, Washington and Oregon, July 1962 - June 1965: U.S. Geological Survey Water Supply Paper 1868, Report: iv, 32 p.; 1 Plate: 19.00 × 16.92 inches, https://doi.org/10.3133/wsp1868.","productDescription":"Report: iv, 32 p.; 1 Plate: 19.00 × 16.92 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":392519,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25089.htm"},{"id":27864,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1868/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27863,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1868/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1868/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Walla Walla River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.75,\n 45.775\n ],\n [\n -118.912,\n 45.775\n ],\n [\n -118.912,\n 46.479\n ],\n [\n -117.75,\n 46.479\n ],\n [\n -117.75,\n 45.775\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3fe5","contributors":{"authors":[{"text":"Mapes, B. E.","contributorId":26286,"corporation":false,"usgs":true,"family":"Mapes","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2321,"text":"wsp1870B - 1969 - Floods of April 28, 1966 in the northern part of Dallas, Texas","interactions":[{"subject":{"id":23935,"text":"ofr67157 - 1966 - Floods of April 28, 1966, in the northern part of Dallas, Texas","indexId":"ofr67157","publicationYear":"1966","noYear":false,"title":"Floods of April 28, 1966, in the northern part of Dallas, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":2321,"text":"wsp1870B - 1969 - Floods of April 28, 1966 in the northern part of Dallas, Texas","indexId":"wsp1870B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Floods of April 28, 1966 in the northern part of Dallas, Texas"},"id":1}],"lastModifiedDate":"2016-08-22T11:31:35","indexId":"wsp1870B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1870","chapter":"B","title":"Floods of April 28, 1966 in the northern part of Dallas, Texas","docAbstract":"The floods of April 28, 1966, in the northern part of Dallas, Tex., caused heavy damage to a relatively small area. Flood damage was estimated at $2,500,000; and of this amount, $1,330,000 damage was along Bachman Branch, which has a drainage area of 12.3 square miles. At least seven persons died as a direct result of the floodwaters.
\nThe flood was caused by a 5-hour storm in the early hours of April 28. Antecedent rainfall had so saturated the area that the intense, but relatively low, total rainfall (less than a 50-year return period) caused historical floods to be exceeded at many points. A peak runoff rate of 3,160 cubic feet per second per square mile occurred on a 1.5 square-mile area within the watershed.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1870B","usgsCitation":"Mills, W.B., and Schroeder, E.E., 1969, Floods of April 28, 1966 in the northern part of Dallas, Texas: U.S. Geological Survey Water Supply Paper 1870, Report: iv, 37 p.; 2 Plates: 17.50 x 23.25 inches and 53.25 x 35.50 inches, https://doi.org/10.3133/wsp1870B.","productDescription":"Report: iv, 37 p.; 2 Plates: 17.50 x 23.25 inches and 53.25 x 35.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1870b/report-thumb.jpg"},{"id":28161,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1870b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28162,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1870b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28163,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1870b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0843","contributors":{"authors":[{"text":"Mills, Willard B.","contributorId":29390,"corporation":false,"usgs":true,"family":"Mills","given":"Willard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":145010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroeder, Elmer E.","contributorId":38962,"corporation":false,"usgs":true,"family":"Schroeder","given":"Elmer","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16614,"text":"ofr69323 - 1969 - Paleogene floras from the Gulf of Alaska","interactions":[{"subject":{"id":16614,"text":"ofr69323 - 1969 - Paleogene floras from the Gulf of Alaska","indexId":"ofr69323","publicationYear":"1969","noYear":false,"title":"Paleogene floras from the Gulf of Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":6514,"text":"pp997 - 1977 - Paleogene floras from the Gulf of Alaska region","indexId":"pp997","publicationYear":"1977","noYear":false,"title":"Paleogene floras from the Gulf of Alaska region"},"id":1}],"supersededBy":{"id":6514,"text":"pp997 - 1977 - Paleogene floras from the Gulf of Alaska region","indexId":"pp997","publicationYear":"1977","noYear":false,"title":"Paleogene floras from the Gulf of Alaska region"},"lastModifiedDate":"2023-12-27T23:03:10.110922","indexId":"ofr69323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-323","title":"Paleogene floras from the Gulf of Alaska","docAbstract":"Numerous collections of fossil plants from the Gulf of Alaska region were obtained from rocks that are well dated by marine mollusks. The mollusks indicate that the oldest possible age for the lowest plant assemblage is middle Eocene (Domengine) and that the youngest possible age for the highest Paleogene plant assemblage is middle Oligocene (Lincoln).
Paleobotanical correlations indicate that the lowest plant assemblage is of early late Eocene (early Ravenian) age and the highest plant assemblage is of early Oligocene (Kummerian) age. A new provincial stage--the Angoonian--is proposed, based on assemblages from rocks in southeastern Alaska. The Angoonian is thought to be of late Oligocene (early Blakeley) age. Only one stratigraphically isolated assemblage from the Gulf of Alaska region has been recognized as of Angoonian age. The biostratigraphy of the Gulf of Alaska region and of other regions in Alaska indicates that the Seldovian, Homerian, and Clamgulchian Stages are probably entirely of Neogene age.
The early Ravenian assemblages represent Paratropical Rain forest (that is, similar to vegetation of a narrow region bordering the Tropical Rain forest) based on the physiognomic analysis of foliage; the most diverse families represented are Menispermaceae and Icacinaceae. These are accompanied by palms, Anonaceae, tjristicaceae, Dipterocarpaceae, Barringtoniaceae, and Myrtaceae. A minor element is represented by broad-leaved deciduous plants. The middle Ravenian was somewhat cooler, as indicated by foliar physiognomy, the fewer Tropical Rain forest elements, and the diversity of Lauraceae. The late Ravenian assemblage represents a broad-leaved deciduous forest indicating a temperate climate. The Kummerian assemblages were again dominated by Lauraceae, and the physiognomic characters of the foliage indicate that Subtropical forest was again represented.
The existence of a broad-leaved evergreen forest in Alaska such as that of the early Ravenian indicates that extended periods of darkness could probably not have existed at that time. The Alaskan Paleogene floras, as well as those from other regions, indicate that the earth's axis of rotation may not have had as great an inclination in the past. Strong climatic fluctuations evidenced by foliar physiognomy of Tertiary floras is thought to have been the result of changes in the inclination of the earth's axis.
The history of the development of the Arcto-Tertiary concept is reviewed, and the fundamental lack of evidence for this concept is shown. An alternative, more complex, concept is proposed for the development of the Mixed Mesophytic forest. Paleobotanical evidence indicates that tolerances of many genera have changed during the Tertiary. Many Mixed Mesophytic genera--particularly those that are today temperate outliers of basically tropical groups--may have had a wide distribution in the Paleogene Paratropical Rain and Subtropical forests and have entered the warm temperate forests only during the later Paleogene or Neogene. Some Mixed Mesophytic groups appear to be of later Neogene origin and have been significant members of the warm temperate forests since that time. Some Mixed Mesophytic genera apparently were members of the Paratropical Rain forest only in the earliest Paleogene and became adapted to warm temperate climates by the late Eocene or perhaps even earlier. The Mixed Mesophytic forest may have developed independently in Eurasia, western North America, and eastern North America.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr69323","usgsCitation":"Wolfe, J.A., 1969, Paleogene floras from the Gulf of Alaska: U.S. Geological Survey Open-File Report 69-323, ii, 111 p., https://doi.org/10.3133/ofr69323.","productDescription":"ii, 111 p.","costCenters":[],"links":[{"id":423920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0323/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0323/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -136.15250770661777,\n 56.82863558130717\n ],\n [\n -136.15250770661777,\n 60.5418529177804\n ],\n [\n -157.32762172640042,\n 60.5418529177804\n ],\n [\n -157.32762172640042,\n 56.82863558130717\n ],\n [\n -136.15250770661777,\n 56.82863558130717\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ce0","contributors":{"authors":[{"text":"Wolfe, Jack A.","contributorId":102474,"corporation":false,"usgs":true,"family":"Wolfe","given":"Jack","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":173153,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2228,"text":"wsp1850B - 1969 - Floods of June 1965 in South Platte River basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1850B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1850","chapter":"B","title":"Floods of June 1965 in South Platte River basin, Colorado","docAbstract":"Heavy, intense rains in three areas on three different days caused outstanding floods on many streams in the South Platte River basin from Plum Creek, just south of Denver, downstream to the Colorado-Nebraska State line. The flood-producing storms followed a relatively wet period, and rainfall of as much as 14 inches in a few hours was reported. The storms occurred over the Greeley-Sterling area on June 14-15, over the Plum Creek and Cherry Creek basins on June 16, and over the headwaters of Kiowa and Bijou Creeks on June 17 after heavy rains on June 15. The flood crest did not pass Julesburg, in the northeast corner of Colorado, until June 20. \r\n\r\nPrevious record high discharges on many tributaries with drainage areas on the plains were exceeded, sometimes severalfold. The six principal tributaries carrying snowmelt runoff were contributing, but not significant, factors in the floods. The attenuation of the peak flow by channel storage as the flood passed through Denver was considerable; yet the peak discharge of 40,300 cfs (cubic feet per second) of the South Platte River at Denver was 1.8 times the previously recorded high of 22,000 cfs in a period of record starting in 1889. The 1965 peak would have been still higher except that all flow from Cherry Creek was stored in Cherry Creek Reservoir. \r\n\r\nSix persons were drowned, and two other deaths were attributed to the storms. The total damage amounted to $508.2 million, and about 75 percent of this occurred in the Denver metropolitan area. \r\n\r\nDescriptions of the storms and floods, detailed streamflow records, and information on damages, flood profiles, inundated areas, and flood frequency are included in this report. Several comparisons of the magnitude of the flood are made, and all indicate that an outstanding hydrologic event occurred.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1850B","usgsCitation":"Matthai, H.F., 1969, Floods of June 1965 in South Platte River basin, Colorado: U.S. Geological Survey Water Supply Paper 1850, iv, 64 p., https://doi.org/10.3133/wsp1850B.","productDescription":"iv, 64 p.","costCenters":[],"links":[{"id":137712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1850b/report-thumb.jpg"},{"id":27978,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1850b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27979,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1850b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27980,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1850b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27981,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1850b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1850b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfa4a","contributors":{"authors":[{"text":"Matthai, Howard Frederick","contributorId":100824,"corporation":false,"usgs":true,"family":"Matthai","given":"Howard","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":144854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2196,"text":"wsp1535O - 1969 - Water load of uranium radium, and gross beta activity at selected gaging stations, water year 1960-61","interactions":[],"lastModifiedDate":"2022-10-12T18:24:19.460117","indexId":"wsp1535O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1535","chapter":"O","title":"Water load of uranium radium, and gross beta activity at selected gaging stations, water year 1960-61","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1535O","usgsCitation":"Mallory, E.C., Johnson, J.O., and Scott, R.C., 1969, Water load of uranium radium, and gross beta activity at selected gaging stations, water year 1960-61: U.S. Geological Survey Water Supply Paper 1535, Report: iii, 31 p.; 1 Plate: 41.00 × 29.00 inches, https://doi.org/10.3133/wsp1535O.","productDescription":"Report: iii, 31 p.; 1 Plate: 41.00 × 29.00 inches","costCenters":[],"links":[{"id":27838,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1535o/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535o/report-thumb.jpg"},{"id":27839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535o/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408224,"rank":4,"type":{"id":36,"text":"NGMDB Index 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C.","contributorId":90700,"corporation":false,"usgs":true,"family":"Mallory","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, J. O.","contributorId":97480,"corporation":false,"usgs":true,"family":"Johnson","given":"J.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144810,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, Robert Clyde","contributorId":57440,"corporation":false,"usgs":true,"family":"Scott","given":"Robert","email":"","middleInitial":"Clyde","affiliations":[],"preferred":false,"id":144808,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1130,"text":"wsp1892 - 1969 - Selected techniques in water resources investigations, 1966-67","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1892","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1892","title":"Selected techniques in water resources investigations, 1966-67","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp1892","usgsCitation":"Chase, E.B., and Payne, F.N., 1969, Selected techniques in water resources investigations, 1966-67: U.S. Geological Survey Water Supply Paper 1892, 164 p., https://doi.org/10.3133/wsp1892.","productDescription":"164 p.","costCenters":[],"links":[{"id":137929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1892/report-thumb.jpg"},{"id":25908,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1892/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f8317","contributors":{"authors":[{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":143226,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Payne, Faith N.","contributorId":104875,"corporation":false,"usgs":true,"family":"Payne","given":"Faith","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":143227,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2072,"text":"wsp1879B - 1969 - Water resources of Randolph and Lawrence Counties, Arkansas","interactions":[{"subject":{"id":52603,"text":"ofr67143 - 1967 - Well records and depth-to-water measurements in the vicinity of Randolph and Lawrence Counties, Arkansas","indexId":"ofr67143","publicationYear":"1967","noYear":false,"title":"Well records and depth-to-water measurements in the vicinity of Randolph and Lawrence Counties, Arkansas"},"predicate":"SUPERSEDED_BY","object":{"id":2072,"text":"wsp1879B - 1969 - Water resources of Randolph and Lawrence Counties, Arkansas","indexId":"wsp1879B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Water resources of Randolph and Lawrence Counties, Arkansas"},"id":1},{"subject":{"id":55853,"text":"ofr68164 - 1968 - Water resources of Randolph and Lawrence Counties, Arkansas","indexId":"ofr68164","publicationYear":"1968","noYear":false,"title":"Water resources of Randolph and Lawrence Counties, Arkansas"},"predicate":"SUPERSEDED_BY","object":{"id":2072,"text":"wsp1879B - 1969 - Water resources of Randolph and Lawrence Counties, Arkansas","indexId":"wsp1879B","publicationYear":"1969","noYear":false,"chapter":"B","title":"Water resources of Randolph and Lawrence Counties, Arkansas"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1879B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1879","chapter":"B","title":"Water resources of Randolph and Lawrence Counties, Arkansas","docAbstract":"Water is used at an average rate of almost 27 million gallons per day in Randolph and Lawrence Counties, and quantities sufficient for any foreseeable use are available. Supplies for the large uses--municipal, industrial, and irrigation--can best be obtained from wells in .he Coastal Plain part of the counties and from streams in the Interior Highlands part. \r\n\r\nThe counties have abundant supplies of hard but otherwise good-quality surface water, particularly in the Interior Highlands and along the western boundary of the Coastal Plain. Minimum recorded flows of four streams (Black, Current, Eleven Point, and Spring Rivers) exceeded 200 cubic feet per second, or 129 million gallons per day. Five other streams have flows in excess of 13 cubic feet per second 95 percent of the time. Water supplies can be obtained without storage from the larger streams in the area. Many of the smaller streams in the Interior Highlands also have large water-supply potential because of the excellent impoundment possibilities. \r\n\r\nMost of the water used in the .two counties is obtained from ground-water reservoirs in the Coastal Plain. Wells that tap alluvial deposits of Quaternary age commonly yield 1,000 gallons per minute. However, the water often is unsuitable for many uses unless treated to remove hardness, iron, and manganese. Water possibly may be obtained in the southeastern part of the area from the Wilcox Group of Tertiary age and the Nacatoch Sand of Cretaceous age, but these formations have not been explored in the report area. \r\n\r\nWells in the Interior Highlands generally are less than 200 feet deep and yield 10 gallons per minute, or less. It may be possible to obtain greater amounts of ground water from two unexplored formations, the Roubidox and the Gunter Sandstone Member of the Van Buren Formation, in the Interior Highlands. Ground water in the Interior Highlands is very hard and is more susceptible to local bacterial contamination than is ground water in the Coastal Plain. However, with proper sanitary safeguards against contamination and with treatment for reduction of hardness, ground water in the Interior Highlands is suitable for most uses.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1879B","usgsCitation":"Lamonds, A.G., Hines, M.S., and Plebuch, R.O., 1969, Water resources of Randolph and Lawrence Counties, Arkansas: U.S. Geological Survey Water Supply Paper 1879, iv, 45 p., https://doi.org/10.3133/wsp1879B.","productDescription":"iv, 45 p.","costCenters":[],"links":[{"id":138567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1879b/report-thumb.jpg"},{"id":27625,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1879b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0292","contributors":{"authors":[{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hines, Marion S.","contributorId":29388,"corporation":false,"usgs":true,"family":"Hines","given":"Marion","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":144640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Plebuch, Raymond O.","contributorId":15177,"corporation":false,"usgs":true,"family":"Plebuch","given":"Raymond","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144639,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2599,"text":"wsp1827C - 1969 - Solubility of aluminum in the presence of hydroxide, fluoride, and sulfate","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1827C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1827","chapter":"C","title":"Solubility of aluminum in the presence of hydroxide, fluoride, and sulfate","docAbstract":"The total concentration of aqueous dissolved species of aluminum that will be present in equilibrium with microcrystalline gibbsite at various levels of complexing ligand concentration are shown graphically. The graphs can be used to estimate aluminum solubility, at 25?C and 1 atmosphere total pressure, when the pH of the solution, its ionic strength, and the total sulfate and fluoride concentrations are known. The standard free energy of formation of cryolite calculated from solubility experiments is --745.4 ? 1.0 kcal per mole at 25?C. Diagrams are included showing the solubility of cryolite in terms of aluminum, fluoride, and sodium concentrations. The stability fields of cryolite and microcrystalline gibbsite and their solubilities also are shown on pH-[F] diagrams.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1827C","usgsCitation":"Roberson, C.E., and Hem, J.D., 1969, Solubility of aluminum in the presence of hydroxide, fluoride, and sulfate: U.S. Geological Survey Water Supply Paper 1827, iv, 37 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1827C.","productDescription":"iv, 37 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1827c/report-thumb.jpg"},{"id":28879,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1827c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5eda3e","contributors":{"authors":[{"text":"Roberson, Charles Elmer","contributorId":79451,"corporation":false,"usgs":true,"family":"Roberson","given":"Charles","email":"","middleInitial":"Elmer","affiliations":[],"preferred":false,"id":145471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":145470,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2040,"text":"wsp1798F - 1969 - Sedimentation in upper Stony Creek basin, eastern flank of the Coast Ranges of northern California","interactions":[],"lastModifiedDate":"2021-12-23T19:46:43.776282","indexId":"wsp1798F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1798","chapter":"F","title":"Sedimentation in upper Stony Creek basin, eastern flank of the Coast Ranges of northern California","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sedimentation in small drainage basins","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1798F","usgsCitation":"Knott, J.M., and Dunnam, C., 1969, Sedimentation in upper Stony Creek basin, eastern flank of the Coast Ranges of northern California: U.S. Geological Survey Water Supply Paper 1798, iv, 35 p., https://doi.org/10.3133/wsp1798F.","productDescription":"iv, 35 p.","costCenters":[],"links":[{"id":388910,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24989.htm"},{"id":137707,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798f/report-thumb.jpg"},{"id":27530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.3330,\n 39.7170\n ],\n [\n -122.8330,\n 39.7170\n ],\n [\n -122.8330,\n 39.2500\n ],\n [\n -122.3330,\n 39.2500\n ],\n [\n -122.3330,\n 39.7170\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66055b","contributors":{"authors":[{"text":"Knott, J. M.","contributorId":77909,"corporation":false,"usgs":true,"family":"Knott","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":144573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunnam, C.A.","contributorId":56200,"corporation":false,"usgs":true,"family":"Dunnam","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":144572,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2716,"text":"wsp1877 - 1969 - Feasibility study of the use of the acoustic velocity meter for measurement of net outflow from the Sacramento-San Joaquin Delta in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1877","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1877","title":"Feasibility study of the use of the acoustic velocity meter for measurement of net outflow from the Sacramento-San Joaquin Delta in California","docAbstract":"A reliable measure of the fresh-water outflow from the Sacramento-San Joaquin delta is needed for the operation of the California Water Project and for the evaluation of the interrelated water problems of the delta and San Francisco Bay regions. The Chipps Island channel, immediately downstream from the confluence of the Sacramento and San Joaquin Rivers, is the most promising site for this flow measurement, but the conventional techniques used for evaluating steady flows cannot be employed there because the channel reach is in the tidal zone, and reversals of flow occur during each tidal cycle. Net outflows, which may be as little-as 2,000 cubic feet per second must necessarily be computed as the difference between the large ebbflow and floodflow volumes that move back and forth between the delta region and San Francisco Bay. Discharges during peak periods of the ebb and flood tidal cycles may exceed 300,000 cubic feet per second. In consequence, a very high degree of precision must be maintained in the gross flow measurements if meaningful computations of net outflow are to be made. \r\n\r\nThis report evaluates the probable accuracies that might be achieved by use of an AVM (acoustic velocity meter), a device which measures the stream velocity along a diagonal line across the channel. The study indicates that this line velocity will provide a stable index of the mean velocity in the channel and that such an index could be used as a primary parameter for the computation of discharge. Therefore, net outflows probably could be computed with the required accuracy by the use of such a device. The significant factors controlling the precision of measurement would be the stability of the channel geometry and streamline orientation, the precision with which the current-meter measurements needed for calibration of the system could be made, the instrumental calibration stability of the AVM system, and the length of period over which net outflows were computed. \r\n\r\nThe AVM system developed by the U.S. Geological Survey in cooperation with the California Department of Water Resources and the U.S. Army Corps of Engineers does not have the required instrumental stability for this precise flow measurement. However, other AVM systems now being produced commercially seem to have the desired error characteristics, and a system probably can be procured that will permit computation of the fresh-water outflow from the delta area.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1877","usgsCitation":"Smith, W., 1969, Feasibility study of the use of the acoustic velocity meter for measurement of net outflow from the Sacramento-San Joaquin Delta in California: U.S. Geological Survey Water Supply Paper 1877, vi, 54 p. :illus., maps. ;23 cm., https://doi.org/10.3133/wsp1877.","productDescription":"vi, 54 p. :illus., maps. ;23 cm.","costCenters":[],"links":[{"id":139018,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1877/report-thumb.jpg"},{"id":29100,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1877/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fad50","contributors":{"authors":[{"text":"Smith, Winchell","contributorId":20311,"corporation":false,"usgs":true,"family":"Smith","given":"Winchell","email":"","affiliations":[],"preferred":false,"id":145657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2820,"text":"wsp1861 - 1969 - Water resources of the Sycamore Creek watershed, Maricopa County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1861","title":"Water resources of the Sycamore Creek watershed, Maricopa County, Arizona","docAbstract":"The Sycamore Creek watershed is representative of many small watersheds in the Southwest where much of the streamflow originates in the mountainous areas and disappears rather quickly into the alluvial deposits adjacent to the mountains. Five years of .streamflow records from the Sycamore Creek watershed show that an average annual water yield of 6,110 acre-feet was obtained from the 165 square miles (105,000 acres) of the upper hard-rock mountain area, which receives an average annual precipitation of about 20 inches. Only a small percentage of the ,annual water yield, however, reaches the Verde River as surface flow over the 9-mile reach of the alluvial channel below the mountain front. Flows must be more ,than 200 cubic feet per second to reach the river; flows less than this rate disappear into the 1,ower alluvial area and are stored temporarily in the ground-Water reservoir : most of this water is released as ground-water discharge to the Verde River at a relatively constant rate of about 4,000 acre-feet per year. Evapotranspiration losses in the lower alluvial area are controlled by the depth of the water table and averaged about 1,500 acre-feet per year.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1861","usgsCitation":"Thomsen, B.W., and Schumann, H.H., 1969, Water resources of the Sycamore Creek watershed, Maricopa County, Arizona: U.S. Geological Survey Water Supply Paper 1861, vii, 53 p. :illus., maps (1 fold. col. in pocket) ;24 cm., https://doi.org/10.3133/wsp1861.","productDescription":"vii, 53 p. :illus., maps (1 fold. col. in pocket) ;24 cm.","costCenters":[],"links":[{"id":138740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1861/report-thumb.jpg"},{"id":29377,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1861/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29378,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1861/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb27c","contributors":{"authors":[{"text":"Thomsen, B. W.","contributorId":39768,"corporation":false,"usgs":true,"family":"Thomsen","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schumann, Herbert H.","contributorId":30964,"corporation":false,"usgs":true,"family":"Schumann","given":"Herbert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145849,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2904,"text":"wsp1873A - 1969 - Factors initiating phytoplankton blooms and resulting effects on dissolved oxygen in Duwamish River estuary, Seattle, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp1873A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1873","chapter":"A","title":"Factors initiating phytoplankton blooms and resulting effects on dissolved oxygen in Duwamish River estuary, Seattle, Washington","docAbstract":"Phytoplankton productivity, standing stock, and related environmental factors were studied during 1964-66 in the Duwamish River estuary, at Seattle, Wash., to ascertain the factors that affect phytoplankton growth in the estuary; a knowledge of these factors in turn permits the detection and evaluation of the influence that effluent nutrients have on phytoplankton production. The factors that control the concentration of dissolved oxygen were also evaluated because of the importance of dissolved oxygen to the salmonid populations that migrate through the estuary. \r\n\r\nPhytoplankton blooms, primarily of diatoms, occurred in the lower estuary during August 1965 and 1966. No bloom occurred during 1964, but the presence of oxygen-supersaturated surface water in August 1963 indicates that a bloom did occur then. \r\n\r\nNutrients probably were not the primary factor controlling the timing of phytoplankton blooms. Ammonia ,and phosphate concentrations increased significantly downstream from the Municipality of Metropolitan Seattle's Renton Treatment Plant outfall after the plant began operation in June 1965, and concentrations of nitrogen and phosphorus were relatively high before operation of the Renton Treatment Plant and during nonbloom periods. The consistent coincidence of blooms with minimum fresh-water discharge and tidal exchange during August throughout the study period indicates that bloom timing probably was controlled mostly by hydrographic factors that determine retention time and stability of the surface-water layer. This control was demonstrated in part by a highly significant correlation of gross productivity with retention time (as indicated by fresh-water discharge) and vertical stability (as indicated by the difference between mean surface and mean bottom temperatures). The failure of a bloom to develop in 1964 is related to a minimum fresh-water discharge that was much greater than normal during that summer. Hydrographic factors are apparently important because, as shown by studies of other estuarine environments by other workers, phytoplankton production increases when the zone of vertical turbulent mixing is not markedly deeper than the compensation depth. \r\n\r\nPhytoplankton cells produced in the surface waters sink, thereby contributing oxidizable organic matter to the bottom saline-water wedge. The maximum BOD (biochemical oxygen demand) in this bottom wedge occurs in the same section of the estuary and ,at the same time as the maximum phytoplankton biomass (as indicated by chlorophyll a) and minimum DO (dissolved oxygen). Other sources of BOD occur in the estuary, and conditions of minimum discharge and tidal exchange assist in reducing DO. Nonetheless, the highly significant correlation of chlorophyll a with BOD throughout the summer indicates that respiration and decomposition of phytoplankton cells is dearly an important contributor of BOD. \r\n\r\nIncreases in the biomass and resultant B0D of blooms because of increased effluent nutrients presumably would further decrease the concentration of DO. This possible effect of effluent nutrients was evaluated by laboratory .bioassays and by a comparison of mean annual biomasses in the estuary. A green algal population in vitro did increase in response to added effluent nutrients; however, the available field data suggest that a 46-percent increase in effluent discharge between 1965 and 1966 did not increase the estuary's phytoplankton biomass significantly.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1873A","usgsCitation":"Welch, E.B., 1969, Factors initiating phytoplankton blooms and resulting effects on dissolved oxygen in Duwamish River estuary, Seattle, Washington: U.S. Geological Survey Water Supply Paper 1873, v, 62 p. :ill. map ;24 cm., https://doi.org/10.3133/wsp1873A.","productDescription":"v, 62 p. :ill. map ;24 cm.","costCenters":[],"links":[{"id":138393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873a/report-thumb.jpg"},{"id":29584,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64964b","contributors":{"authors":[{"text":"Welch, Eugene Brummer","contributorId":48947,"corporation":false,"usgs":true,"family":"Welch","given":"Eugene","email":"","middleInitial":"Brummer","affiliations":[],"preferred":false,"id":145985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3078,"text":"wsp1901 - 1969 - Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 1. Basins from Maine to Connecticut","interactions":[],"lastModifiedDate":"2022-11-02T19:31:35.448472","indexId":"wsp1901","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1901","title":"Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 1. Basins from Maine to Connecticut","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1901","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States, 1961-65: Part 1. North Atlantic slope basins: Volume 1. Basins from Maine to Connecticut: U.S. Geological Survey Water Supply Paper 1901, Report: xi, 1027 p.; 1 Plate: 25.00 × 35.00 inches, https://doi.org/10.3133/wsp1901.","productDescription":"Report: xi, 1027 p.; 1 Plate: 25.00 × 35.00 inches","costCenters":[],"links":[{"id":139416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1901/report-thumb.jpg"},{"id":29950,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1901/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29951,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1901/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409074,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25126.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, Rhode Island, Vermont","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -66.30105327026975,\n 47.52171404918724\n ],\n [\n -73.42461764114435,\n 47.52171404918724\n ],\n [\n -73.42461764114435,\n 41.240450495549254\n ],\n [\n -66.30105327026975,\n 41.240450495549254\n ],\n [\n -66.30105327026975,\n 47.52171404918724\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942ac","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3084,"text":"wsp1917 - 1969 - Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 2. Missouri River basin from Williston, North Dakota to Sioux City, Iowa","interactions":[],"lastModifiedDate":"2022-11-02T19:00:54.010678","indexId":"wsp1917","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1917","title":"Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 2. Missouri River basin from Williston, North Dakota to Sioux City, Iowa","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1917","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States 1961-65: Part 6, Missouri River basin: Volume 2. Missouri River basin from Williston, North Dakota to Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1917, Report: viii, 560 p.; 1 Plate: 23.00 × 22.50 inches, https://doi.org/10.3133/wsp1917.","productDescription":"Report: viii, 560 p.; 1 Plate: 23.00 × 22.50 inches","costCenters":[],"links":[{"id":409071,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25141.htm","linkFileType":{"id":5,"text":"html"}},{"id":29962,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1917/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29961,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1917/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1917/report-thumb.jpg"}],"country":"United States","state":"Iowa, Nebraska, North Dakota, South Dakota","otherGeospatial":"Missouri River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -103.78678268521452,\n 48.142391817720835\n ],\n [\n -103.78678268521452,\n 42.48788765617516\n ],\n [\n -96.32676997197834,\n 42.48788765617516\n ],\n [\n -96.32676997197834,\n 48.142391817720835\n ],\n [\n -103.78678268521452,\n 48.142391817720835\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db6282aa","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3085,"text":"wsp1920 - 1969 - Surface water supply of the United States, 1961-65, Part 7. Lower Mississippi River basin, Volume 1. Lower Mississippi River basin except Arkansas River basin","interactions":[],"lastModifiedDate":"2021-12-03T20:14:45.804805","indexId":"wsp1920","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1920","title":"Surface water supply of the United States, 1961-65, Part 7. Lower Mississippi River basin, Volume 1. Lower Mississippi River basin except Arkansas River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1920","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States, 1961-65, Part 7. Lower Mississippi River basin, Volume 1. Lower Mississippi River basin except Arkansas River basin: U.S. Geological Survey Water Supply Paper 1920, 1103 p., https://doi.org/10.3133/wsp1920.","productDescription":"1103 p.","costCenters":[],"links":[{"id":29963,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1920/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1920/report-thumb.jpg"},{"id":392462,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25144.htm"}],"country":"United States","state":"Arkansas, Illinois, Kansas, Kentucky, Louisiana, Mississippi, Missouri, Oklahoma, Tennessee, Texas","otherGeospatial":"lower Mississippi River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103,\n 29\n ],\n [\n -88.293,\n 29\n ],\n [\n -88.293,\n 38.694\n ],\n [\n -103,\n 38.694\n ],\n [\n -103,\n 29\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692938","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3086,"text":"wsp1921 - 1969 - Surface water supply of the United States 1961-65: Part 7. Lower Mississippi River basin: Volume 2, Arkansas River basin","interactions":[],"lastModifiedDate":"2022-12-09T21:09:10.501404","indexId":"wsp1921","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1921","title":"Surface water supply of the United States 1961-65: Part 7. Lower Mississippi River basin: Volume 2, Arkansas River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1921","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Surface water supply of the United States 1961-65: Part 7. Lower Mississippi River basin: Volume 2, Arkansas River basin: U.S. Geological Survey Water Supply Paper 1921, 878 p., https://doi.org/10.3133/wsp1921.","productDescription":"878 p.","costCenters":[],"links":[{"id":29964,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1921/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410234,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25145.htm","linkFileType":{"id":5,"text":"html"}},{"id":138630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1921/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Arkansas River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106.6,\n 39.367\n ],\n [\n -106.6,\n 34\n ],\n [\n -91.35,\n 34\n ],\n [\n -91.35,\n 39.367\n ],\n [\n -106.6,\n 39.367\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980a3","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}