{"pageNumber":"2683","pageRowStart":"67050","pageSize":"25","recordCount":68807,"records":[{"id":1933,"text":"wsp998 - 1947 - Suspended sediment in the Colorado River, 1925-41","interactions":[],"lastModifiedDate":"2017-09-07T13:09:00","indexId":"wsp998","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"998","title":"Suspended sediment in the Colorado River, 1925-41","docAbstract":"<p>This report gives the results of sediment-sampling studies of the Geological Survey in the Colorado River basin for the period from October 1, 1925, to September 30, 1941. Records are given for the entire period for the Grand Canyon gaging station and for shorter periods at other stations in the basin. The results reported consist of the records of the mean daily concentrations.of sediment for all stations, and in addition, the mean daily discharge and daily load of sediment for many of the stations.</p><p>The available records indicate that the runoff of the Colorado near Cisco, Utah, plus the runoff of the Green at Green River, Utah, plus the runoff of the San Juan near Bluff, Utah, amount to about 90 percent of the runoff at the Grand Canyon gaging station, but the sediment loads at the three upper stations amount to only about 60 percent of the sediment load at Grand Canyon. The Little Colorado River and two or three other unsampled tributaries probably are the major sources of the unmeasured sediment</p><p>Information is given concerning the sizes of the particles of the sediment at the Grand Canyon, Willow Beach, and Bluff stations during periods of this investigation.</p><p>The annual load at Grand Canyon during the 16 years ranged from 50,080,000 tons in 1933-34 to 480,000,000 tons in 1928-29, and the mean annual load at that station for the 16-year period was 200,200,000 tons. The mean annual runoff for the Grand Canyon station during the period was 12,640,000 acre-feet</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp998","usgsCitation":"Howard, C.S., 1947, Suspended sediment in the Colorado River, 1925-41: U.S. Geological Survey Water Supply Paper 998, v, 165 p., https://doi.org/10.3133/wsp998.","productDescription":"v, 165 p.","numberOfPages":"175","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":138520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0998/report-thumb.jpg"},{"id":27259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0998/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Colorado River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fd2","contributors":{"authors":[{"text":"Howard, Charles S.","contributorId":15990,"corporation":false,"usgs":true,"family":"Howard","given":"Charles","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":144398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":2080,"text":"wsp968C - 1947 - Topographic characteristics of drainage basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp968C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"968","chapter":"C","title":"Topographic characteristics of drainage basins","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp968C","usgsCitation":"Langbein, W.B., 1947, Topographic characteristics of drainage basins: U.S. Geological Survey Water Supply Paper 968, iii, 125-157 p. :ill., map ;23 cm., https://doi.org/10.3133/wsp968C.","productDescription":"iii, 125-157 p. :ill., map ;23 cm.","costCenters":[],"links":[{"id":138348,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0968c/report-thumb.jpg"},{"id":27640,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0968c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a377","contributors":{"authors":[{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":144648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3015,"text":"wsp920 - 1947 - Utilization of surface-water resources of Sevier Lake Basin, Utah","interactions":[],"lastModifiedDate":"2022-02-18T20:37:28.411999","indexId":"wsp920","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"920","title":"Utilization of surface-water resources of Sevier Lake Basin, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp920","usgsCitation":"Woolley, R., 1947, Utilization of surface-water resources of Sevier Lake Basin, Utah: U.S. Geological Survey Water Supply Paper 920, Report: ix, 393 p.; 7 Plates: 25.00 x 31.35 inches or smaller, 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,{"id":769,"text":"wsp1019 - 1947 - Water levels and artesian pressure in observation wells in the United States, 1944, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"1019","title":"Water levels and artesian pressure in observation wells in the United States, 1944, Part 4, South-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1019","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1947, Water levels and artesian pressure in observation wells in the United States, 1944, Part 4, South-Central States: U.S. Geological Survey Water Supply Paper 1019, iv, 188 p. ;23 cm., https://doi.org/10.3133/wsp1019.","productDescription":"iv, 188 p. ;23 cm.","costCenters":[],"links":[{"id":135982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1019/report-thumb.jpg"},{"id":25336,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa09f","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":527701,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23128,"text":"ofr4737 - 1947 - Ground-water resources of Peeples Valley, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr4737","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"47-37","title":"Ground-water resources of Peeples Valley, Arizona","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr4737","issn":"0094-9140","usgsCitation":"Babcock, H.M., and Brown, S., 1947, Ground-water resources of Peeples Valley, Arizona: U.S. Geological Survey Open-File Report 47-37, 15 p.; 13 leaves (1 folded) :map ;27 cm., https://doi.org/10.3133/ofr4737.","productDescription":"15 p.; 13 leaves (1 folded) :map ;27 cm.","costCenters":[],"links":[{"id":155692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1947/0037/report-thumb.jpg"},{"id":52494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1947/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae2d3","contributors":{"authors":[{"text":"Babcock, H. M.","contributorId":90698,"corporation":false,"usgs":true,"family":"Babcock","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":189499,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, S.C.","contributorId":53834,"corporation":false,"usgs":true,"family":"Brown","given":"S.C.","affiliations":[],"preferred":false,"id":189498,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":164,"text":"wsp1022 - 1947 - Quality of surface waters of the United States, 1944","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1022","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"1022","title":"Quality of surface waters of the United States, 1944","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1022","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1947, Quality of surface waters of the United States, 1944: U.S. Geological Survey Water Supply Paper 1022, v, 311 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1022.","productDescription":"v, 311 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137269,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1022/report-thumb.jpg"},{"id":24775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1022/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db65498a","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":527207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42832,"text":"ofr477 - 1947 - Preliminary geologic map of the Minot quadrangle, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr477","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"47-7","title":"Preliminary geologic map of the Minot quadrangle, North Dakota","language":"ENGLISH","doi":"10.3133/ofr477","usgsCitation":"Lemke, R., Water Resources Division, U.S. Geological Survey, and Smith, J.H., 1947, Preliminary geologic map of the Minot quadrangle, North Dakota: U.S. Geological Survey Open-File Report 47-7, 1 map :photocopy ;58 x 39 cm., on sheet 74 x 65 cm., https://doi.org/10.3133/ofr477.","productDescription":"1 map :photocopy ;58 x 39 cm., on sheet 74 x 65 cm.","costCenters":[],"links":[{"id":136498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80659,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1947/0007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985ab","contributors":{"authors":[{"text":"Lemke, Richard W.","contributorId":59409,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard W.","affiliations":[],"preferred":false,"id":227218,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, J. Hiram","contributorId":82672,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"Hiram","affiliations":[],"preferred":false,"id":227219,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42422,"text":"ofr4722 - 1947 - Preliminary map showing construction materials in the south one-half of Williams County, North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:11:09","indexId":"ofr4722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"47-22","title":"Preliminary map showing construction materials in the south one-half of Williams County, North Dakota","language":"ENGLISH","doi":"10.3133/ofr4722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1947, Preliminary map showing construction materials in the south one-half of Williams County, North Dakota: U.S. Geological Survey Open-File Report 47-22, 1 map on 2 sheets :photocopy ;70 x 157 cm., sheets 107 x 96 cm. and 107 x 67 cm., https://doi.org/10.3133/ofr4722.","productDescription":"1 map on 2 sheets :photocopy ;70 x 157 cm., sheets 107 x 96 cm. and 107 x 67 cm.","costCenters":[],"links":[{"id":175988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98869,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1947/0022/plate-1.pdf","size":"9194","linkFileType":{"id":1,"text":"pdf"}},{"id":98870,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1947/0022/plate-2.pdf","size":"7148","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6ae","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":530923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55583,"text":"ofr4727A - 1947 - Electrochemical stabilization of clayey ground","interactions":[],"lastModifiedDate":"2014-07-09T11:15:23","indexId":"ofr4727A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"47-27","chapter":"A","title":"Electrochemical stabilization of clayey ground","docAbstract":"<p>Recently developed new methods of stabilization of weak grounds (e.g. the silicate treatment) are based on injection of chemical solutions into the ground. Such methods are applicable accordingly only to the kinds of ground that have the coefficient of filtration higher than 2 meters per 24 hours and permit penetration of the chemical solutions under pressure. This limit, however, as it is shown by our experience in construction, excludes a numerous and an important class of grounds, stabilization of which is indispensable in many instances. For example, digging of trenches and pits in clayey, silty, or sandy ground shows that all these types act like typical \"floaters\" (sluds? -S) in the presence of the ground water pressure. There were several instances in the canalization of the city of Moskow where the laying of trenches below the ground water level has led to extreme difficulties with clayey and silty ground.</p>\n<br/>\n<p>Similar examples could be cited in mining, engineering hydrology, and railroad construction. For these reasons, the development of methods of stabilizing such difficult types of ground has become an urgent problem of our day.</p>\n<br/>\n<p>In 1936, the author began his investigations, at the ground Stabilization Laboratory of VODGEO Institute, with direct electrical current as the means of stabilization of grounds. Experiments had shown that a large number of clayey types, following passage of direct electrical current, undergoes a transformation of its physico-chemical properties. It was established that the (apparent -S) density of the ground is substantially increased in consequence of the application of direct electrical current. The ground loses also its capacity to swell and to soften in water. Later, after a more detailed study of the physico-chemical mechanism of the electrical stabilization, it became possible to develop the method so as to make it applicable to sandy and silty as well as to clayey ground. By this time (1941, S.), the method has already been tested in the field, was found satisfactory, and is being introduced into construction practice.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4727A","usgsCitation":"Rzhanitzin, B., and Sokoloff, V., 1947, Electrochemical stabilization of clayey ground: U.S. Geological Survey Open-File Report 47-27, 8 p., https://doi.org/10.3133/ofr4727A.","productDescription":"8 p.","numberOfPages":"14","costCenters":[],"links":[{"id":289624,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289623,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1947/0027-A/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606e09","contributors":{"authors":[{"text":"Rzhanitzin, B.A.","contributorId":16921,"corporation":false,"usgs":true,"family":"Rzhanitzin","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":253757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sokoloff, V.P. (translator)","contributorId":18773,"corporation":false,"usgs":true,"family":"Sokoloff","given":"V.P.","suffix":"(translator)","email":"","affiliations":[],"preferred":false,"id":253758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4574,"text":"wsp1044 - 1947 - Surface water supply of the United States, 1945, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"wsp1044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"1044","title":"Surface water supply of the United States, 1945, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1044","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1947, Surface water supply of the United States, 1945, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1044, vi, 237 p. ;23 cm., https://doi.org/10.3133/wsp1044.","productDescription":"vi, 237 p. ;23 cm.","costCenters":[],"links":[{"id":139906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1044/report-thumb.jpg"},{"id":31631,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e06","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":528269,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4589,"text":"wsp1034 - 1947 - Surface water supply of the United States, 1945, Part IV, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp1034","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"1034","title":"Surface water supply of the United States, 1945, Part IV, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1034","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1947, Surface water supply of the United States, 1945, Part IV, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1034, v, 247 p. ;23 cm., https://doi.org/10.3133/wsp1034.","productDescription":"v, 247 p. ;23 cm.","costCenters":[],"links":[{"id":139633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1034/report-thumb.jpg"},{"id":31646,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697022","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":528284,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1056,"text":"wsp968A - 1947 - Flood runoff in the Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:29:46","indexId":"wsp968A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"968","chapter":"A","title":"Flood runoff in the Willamette Valley, Oregon","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp968A","usgsCitation":"Brands, M., 1947, Flood runoff in the Willamette Valley, Oregon: U.S. Geological Survey Water Supply Paper 968, iv, p. 1-59 : ill., maps ;23 cm., https://doi.org/10.3133/wsp968A.","productDescription":"iv, p. 1-59 : ill., maps ;23 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":137958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0968a/report-thumb.jpg"},{"id":25730,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0968a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e74dd","contributors":{"authors":[{"text":"Brands, M.D.","contributorId":62986,"corporation":false,"usgs":true,"family":"Brands","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":143101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":1240,"text":"wsp816 - 1947 - Major Texas floods of 1936","interactions":[],"lastModifiedDate":"2016-08-22T10:21:05","indexId":"wsp816","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1947","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":"816","title":"Major Texas floods of 1936","docAbstract":"<p>In 1936 floods occurred in parts of Texas during two periods one about July 1 and the other in the later portion of September which were marked by record-breaking or outstanding stages and discharges on some of the larger rivers.</p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp816","usgsCitation":"Dalrymple, T., 1947, Major Texas floods of 1936: U.S. Geological Survey Water Supply Paper 816, v, 145 p., https://doi.org/10.3133/wsp816.","productDescription":"v, 145 p.","numberOfPages":"160","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":137606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0816/report-thumb.jpg"},{"id":26169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0816/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6496e8","contributors":{"authors":[{"text":"Dalrymple, Tate","contributorId":59420,"corporation":false,"usgs":true,"family":"Dalrymple","given":"Tate","email":"","affiliations":[],"preferred":false,"id":143425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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It is in part an outline of the physiographic history of the Connecticut River, a 'history that is treated in progressively greater detail as it concerns events occurring from Mesozoic time to the present, and in part a discussion of erosional and depositional processes associated with the extraordinary floods of March 1936 and September 1938. \r\n\r\nThe Connecticut River flows southward through Massachusetts in a broad lowland area of more than 400 square miles and is joined in this area by four large tributaries, the Deerfield and Westfield Rivers from the west and the Millers and Chicopee Rivers from the east. The lowland area, or :Connecticut Valley province, is flanked on the west by the Berkshire Hills, a, deeply incised uplifted plateau, and on the east by the central upland, or Worcester .County plateau, a lower upland marked by rolling topography. Most of the broad, relatively flat valley floor is underlain by Triassic sedimentary rocks. Rising above it, however, are the prominent Holyoke-Mount Tom and Deerfield Ranges, which consist in large part of dark-colored igneous rocks, also of Triassic age. \r\n\r\nThere is evidence of several cycles of erosion in central western Massachusetts, the last two of which are of Tertiary age and appear to have reached nature and very youthful stages of topographic development, respectively. Immediately prior to the glacial epoch, therefore, the Connecticut River flowed in a fairly narrow, deep gorge, which it had incised in the rather flat 5ottom of the valley that it had formed at an earlier stage. A Pleistocene crustal subsidence probably of several hundred feet, for which there has been only partial compensation in postglacial time, was responsible for the present position of much of this gorge below sea level. That an estuary does not now occupy the gorge is due to a filling by glacial debris, notably by sediments deposited in late glacial lakes. Following disappearance of the last ice sheet and draining of the associated, lakes, the Connecticut River resumed existence and began a new chapter in its history. \r\n\r\nIn those areas where the river regained its preglacial course, it now flows on sediments considerably above the rock floor of the old gorge. Where the gorge was narrow and deep, the upper parts of its walls have confined the postglacial river within rather narrow limits, as in the northern part of the state. Where it was sufficiently wide to be filled by glacial sediments over large areas, the postglacial river has meandered broadly, as in the area north of the Holyoke-Mount Tom Range. In two areas in Massachusetts and in one immediately south in Connecticut, however, the river was forced from its preglacial gorge, and its new channel has been superimposed on bedrock, with development of rapids and falls. Each of these postglacial rock channels acts as a spillway whose level controls the local base level of the river as far upstream as the next spillway. These spillways are not to be confused with other, more spectacular gorges, which are of preglacial origin and in which the present river does not flow on bedrock. \r\n\r\nThe Recent Connecticut has formed extensive flood plains and terraces through repeated sequences of erosion by lateral corrosion and downward scour, followed by deposition of .silt and sand veneers. These features, although irregular in detail, appear to be assignable to five general levels, whose means are approximately 49, 37, 30, 18, and 10 feet above present mean river level. In addition, an 80-foot terrace in the northern part of the valley was left perched, in its present position when the Connecticut abandoned its course over. a rock barrier near Turners Falls in favor of an adjacent much lower gap. The normal terraces and flood plains, slope very gently away from their riverw","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp996","usgsCitation":"Jahns, R.H., 1947, Geologic features of the Connecticut Valley, Massachusetts as related to recent floods: U.S. Geological Survey Water Supply Paper 996, Report: viii, 158 p.; 20 Plates: 31.00 × 31.00 inches or smaller, https://doi.org/10.3133/wsp996.","productDescription":"Report: viii, 158 p.; 20 Plates: 31.00 × 31.00 inches or 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