{"pageNumber":"2591","pageRowStart":"64750","pageSize":"25","recordCount":68811,"records":[{"id":52198,"text":"ofr61108 - 1961 - Ground-water inventory for 1960, Edwards Air Force Base, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr61108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-108","title":"Ground-water inventory for 1960, Edwards Air Force Base, California","docAbstract":"The Old Speck Mountain quadrangle, Maine (44? 30\u0019 - 44? 45\u0019 N. lat., 70? 45\u0019 - 71? 00\u0019 W. long.), is underlain by Paleozoic metamorphic and intrusive rocks. The metamorphic rocks comprise the Albee formation, the Ammonoosuc volcanics, and the Partridge for","language":"ENGLISH","doi":"10.3133/ofr61108","usgsCitation":"Moyle, W.R., 1961, Ground-water inventory for 1960, Edwards Air Force Base, California: U.S. Geological Survey Open-File Report 61-108, 44 p., https://doi.org/10.3133/ofr61108.","productDescription":"44 p.","costCenters":[],"links":[{"id":175591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0108/report-thumb.jpg"},{"id":86685,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0108/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0108/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668c9d","contributors":{"authors":[{"text":"Moyle, W. R. 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C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":244928,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52183,"text":"ofr6180 - 1961 - Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho","interactions":[],"lastModifiedDate":"2013-11-26T11:28:10","indexId":"ofr6180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-80","title":"Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho","language":"English","doi":"10.3133/ofr6180","usgsCitation":"Jones, P., 1961, Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho: U.S. Geological Survey Open-File Report 61-80, 8 p., https://doi.org/10.3133/ofr6180.","productDescription":"8 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":176727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Idaho","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f22","contributors":{"authors":[{"text":"Jones, P.H.","contributorId":50963,"corporation":false,"usgs":true,"family":"Jones","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":244923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52182,"text":"ofr6179 - 1961 - Basic data, ground-water resources and geology of Washington, D. C., and vicinity","interactions":[{"subject":{"id":52182,"text":"ofr6179 - 1961 - Basic data, ground-water resources and geology of Washington, D. C., and vicinity","indexId":"ofr6179","publicationYear":"1961","noYear":false,"title":"Basic data, ground-water resources and geology of Washington, D. C., and vicinity"},"predicate":"SUPERSEDED_BY","object":{"id":1989,"text":"wsp1776 - 1964 - Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water","indexId":"wsp1776","publicationYear":"1964","noYear":false,"title":"Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water"},"id":1}],"supersededBy":{"id":1989,"text":"wsp1776 - 1964 - Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water","indexId":"wsp1776","publicationYear":"1964","noYear":false,"title":"Geology and ground-water resources of Washington, D.C., and vicinity, with a section on chemical quality of the water"},"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-79","title":"Basic data, ground-water resources and geology of Washington, D. C., and vicinity","language":"ENGLISH","doi":"10.3133/ofr6179","usgsCitation":"Johnston, P., 1961, Basic data, ground-water resources and geology of Washington, D. C., and vicinity: U.S. Geological Survey Open-File Report 61-79, 320 p., https://doi.org/10.3133/ofr6179.","productDescription":"320 p.","costCenters":[],"links":[{"id":175588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640bd6","contributors":{"authors":[{"text":"Johnston, P.M.","contributorId":22024,"corporation":false,"usgs":true,"family":"Johnston","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":244922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52180,"text":"ofr6173 - 1961 - Quality of water considerations, lower Colorado River area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6173","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-73","title":"Quality of water considerations, lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6173","usgsCitation":"Irelan, B., 1961, Quality of water considerations, lower Colorado River area: U.S. Geological Survey Open-File Report 61-73, 7 p., https://doi.org/10.3133/ofr6173.","productDescription":"7 p.","costCenters":[],"links":[{"id":175586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651796","contributors":{"authors":[{"text":"Irelan, Burdge","contributorId":15991,"corporation":false,"usgs":true,"family":"Irelan","given":"Burdge","email":"","affiliations":[],"preferred":false,"id":244920,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52175,"text":"ofr6167 - 1961 - Ground water in the vicinity of Roosevelt, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6167","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-67","title":"Ground water in the vicinity of Roosevelt, Oklahoma","docAbstract":"The principal source of additional ground-water supply in the Roosevelt area of west-central Kiowa County is from alluvial deposits. Ground water can be obtained in varying amounts from the red beds of Permian age, but yields of wells are small and the water is of poor quality at most places.\r\nRoosevelt's municipal water needs are supplied from 9 wells, 2 miles west of town (fig. 1). Eight of these wells obtain water from the red beds. The other well taps an alluvial deposit about 30 feet in thickness. It was reported that test drilling for the town of Roosevelt found this deposit to be 25 to 30 feet in thickness with only the lower few feet saturated. Development of additional water supply from either the red beds or alluvial deposit at this location is unlikely.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr6167","usgsCitation":"Hollowell, J., 1961, Ground water in the vicinity of Roosevelt, Oklahoma: U.S. Geological Survey Open-File Report 61-67, 9 p., https://doi.org/10.3133/ofr6167.","productDescription":"9 p.","costCenters":[],"links":[{"id":175476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6c8","contributors":{"authors":[{"text":"Hollowell, J.R.","contributorId":18443,"corporation":false,"usgs":true,"family":"Hollowell","given":"J.R.","affiliations":[],"preferred":false,"id":244913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":727,"text":"wsp1712 - 1961 - Surface water supply of the United States, 1960, Part 8, Western Gulf of Mexico Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1712","title":"Surface water supply of the United States, 1960, Part 8, Western Gulf of Mexico Basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1712","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 8, Western Gulf of Mexico Basins: U.S. Geological Survey Water Supply Paper 1712, xi, 511 p. :tables ;23 cm., https://doi.org/10.3133/wsp1712.","productDescription":"xi, 511 p. :tables ;23 cm.","costCenters":[],"links":[{"id":136295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1712/report-thumb.jpg"},{"id":25290,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1712/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942d2","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142655,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52171,"text":"ofr6161 - 1961 - The surface-water supply of the lower Colorado River area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr6161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-61","title":"The surface-water supply of the lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6161","usgsCitation":"Hely, A., 1961, The surface-water supply of the lower Colorado River area: U.S. Geological Survey Open-File Report 61-61, 16 p., https://doi.org/10.3133/ofr6161.","productDescription":"16 p.","costCenters":[],"links":[{"id":176940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634bd1","contributors":{"authors":[{"text":"Hely, A. G.","contributorId":14401,"corporation":false,"usgs":true,"family":"Hely","given":"A. G.","affiliations":[],"preferred":false,"id":244909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52169,"text":"ofr6159 - 1961 - Ground water in the alluvium of Beaver Creek basin, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:13","indexId":"ofr6159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-59","title":"Ground water in the alluvium of Beaver Creek basin, Oklahoma","docAbstract":"Beaver Creek is an 857 square-mile area in south-central Oklahoma. The tributaries head at an altitude as high as 1,400 feet and the mouth of Beaver Creek is at an altitude of 804 feet. Alluvial material has been deposited along all the major streams in the basin. The alluvium contains a high percentage of clay and fine sand and ranges in thickness from a few inches to 50 feet.\r\nReplenishment of water in the alluvium is from precipitation, lateral seepage and runoff from adjoining areas, and infiltration from the streams during high flows.\r\n\r\nThe town of Ryan and Waurika have constructed municipal water-supply wells topping the alluvium and residents of the town of Sugden have private wells topping the alluvium. The other major use of ground water is transpiration by trees, which are very dense where the alluvial plain is wide.\r\n\r\nIn the northern part of the basin the alluvium is thin and only domestic water supplies are available.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr6159","usgsCitation":"Hart, D., 1961, Ground water in the alluvium of Beaver Creek basin, Oklahoma: U.S. Geological Survey Open-File Report 61-59, 13 p., https://doi.org/10.3133/ofr6159.","productDescription":"13 p.","costCenters":[],"links":[{"id":176938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d79b","contributors":{"authors":[{"text":"Hart, D.L. Jr.","contributorId":49403,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":244907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52161,"text":"ofr6145 - 1961 - Wisconsin River near Dekorra, Wisconsin, flood-flow characteristics at proposed bridge site on the Wisconsin freeway in Columbia County","interactions":[],"lastModifiedDate":"2015-10-13T12:45:23","indexId":"ofr6145","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-45","title":"Wisconsin River near Dekorra, Wisconsin, flood-flow characteristics at proposed bridge site on the Wisconsin freeway in Columbia County","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6145","usgsCitation":"Ericson, D., 1961, Wisconsin River near Dekorra, Wisconsin, flood-flow characteristics at proposed bridge site on the Wisconsin freeway in Columbia County: U.S. Geological Survey Open-File Report 61-45, 13 p., https://doi.org/10.3133/ofr6145.","productDescription":"13 p.","numberOfPages":"13","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":178751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Columbia County","city":"Dekorra","otherGeospatial":"Wisconsin River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.45068359374999,\n 43.498262040099405\n ],\n [\n -89.47952270507812,\n 43.4743490160941\n ],\n [\n -89.52140808105467,\n 43.44893105587766\n ],\n [\n -89.55024719238281,\n 43.428489260910034\n ],\n [\n -89.51385498046874,\n 43.41203109265501\n ],\n [\n -89.42802429199217,\n 43.44394588902309\n ],\n [\n -89.40811157226562,\n 43.46288733737435\n ],\n [\n -89.41291809082031,\n 43.49676775343911\n ],\n [\n -89.42390441894531,\n 43.50523488889796\n ],\n [\n -89.45068359374999,\n 43.498262040099405\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0a6e","contributors":{"authors":[{"text":"Ericson, D.W.","contributorId":80295,"corporation":false,"usgs":true,"family":"Ericson","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":244893,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52156,"text":"ofr6128 - 1961 - Floods in Pennsylvania, frequency and magnitude","interactions":[],"lastModifiedDate":"2016-06-23T10:52:55","indexId":"ofr6128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-28","title":"Floods in Pennsylvania, frequency and magnitude","docAbstract":"

This report outlines a method of determining the magnitude of floods having frequencies up to 50 years for any stream in Pennsylvania except regulated streams and streams whose drainage basins are smaller than 10 square miles. On the main stems of the Schuylkill, Delaware, Susquehanna, and Chemung Rivers the magnitude of floods can be determined for frequencies up to 100 years.

\n

Six composite frequency curves show the relation of the mean annual flood to floods having recurrence interval up to 50 to 100 years. Curves for fourteen hydrologic areas show the variation of mean annual flood with drainage area. This report explains how to select the proper curves for any chosen point in the State and how to compute a flood-frequency curve for that point.

\n

A tabulation of peak gage heights and discharges for most gaging stations in the State is included. In general, the tabulations contain all peaks above a specific base discharge, although for some stations only annual peaks are shown.

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The Mountain Iron-Virginia area is a broad, southwest-trending valley in the central part of the Mesabi Range. The valley, which heads in the Laurentian Divide, and covers about 120 square miles, coincides approximately with a bedrock valley filled with as much as 150 feet of glacial deposits.

\n

A complex sequence of glacioaqueous sediments made up of clay, silt, sand, and gravel was delineated from test holes drilled at 238 sites. These sediments range in thickness from 0 to 125 feet and can be considered a hydrologic unit, bounded below by sandy till or bedrock and above by as much as 60 feet of clayey till. The piezometric surface ranges from 0 to about 70 feet below land surface, thus, the glacioaqueous deposits are not everywhere completely saturated. In places, however, the water is under artesian pressure.

\n

Within the Mountain Iron-Virginia area about 50 square miles are underlain by deposits 20 feet or more in thickness of silt, sand, or gravel that constitute an aquifer that is a large potential source for additional water supplies. Except for iron and manganese, which are present in excessive amounts in some wells, the water meets U.S. Public Health Service standards for municipal supplies. Pumping tests of wells in the permeable sand or gravel deposits at five sites indicate that yields of several hundred gallons per minute and possibly as much as 2,000 gpm (gallons per minute) can be expected.

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Print. Off.,","doi":"10.3133/wsp1703","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 2-A, South Atlantic slope basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1703, viii, 269 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1703.","productDescription":"viii, 269 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1703/report-thumb.jpg"},{"id":27074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1703/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942fa","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144254,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1165,"text":"wsp1593 - 1961 - Simplified methods for computing total sediment discharge with the modified Einstein procedure","interactions":[{"subject":{"id":55755,"text":"ofr5721 - 1957 - Simplified methods for computing total sediment discharge with the modified Einstein procedure","indexId":"ofr5721","publicationYear":"1957","noYear":false,"title":"Simplified methods for computing total sediment discharge with the modified Einstein procedure"},"predicate":"SUPERSEDED_BY","object":{"id":1165,"text":"wsp1593 - 1961 - Simplified methods for computing total sediment discharge with the modified Einstein procedure","indexId":"wsp1593","publicationYear":"1961","noYear":false,"title":"Simplified methods for computing total sediment discharge with the modified Einstein procedure"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1593","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1593","title":"Simplified methods for computing total sediment discharge with the modified Einstein procedure","docAbstract":"A procedure was presented in 1950 by H. A. Einstein for computing the total discharge of sediment particles of sizes that are in appreciable quantities in the stream bed. This procedure was modified by the U.S. Geological Survey and adapted to computing the total sediment discharge of a stream on the basis of samples of bed sediment, depth-integrated samples of suspended sediment, streamflow measurements, and water temperature. This paper gives simplified methods for computing total sediment discharge by the modified Einstein procedure. Each of four homographs appreciably simplifies a major step in the computations. Within the stated limitations, use of the homographs introduces much less error than is present in either the basic data or the theories on which the computations of total sediment discharge are based. The results are nearly as accurate mathematically as those that could be obtained from the longer and more complex arithmetic and algebraic computations of the Einstein procedure.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1593","usgsCitation":"Colby, B.R., and Hubbell, D.W., 1961, Simplified methods for computing total sediment discharge with the modified Einstein procedure: U.S. Geological Survey Water Supply Paper 1593, vi, 17 p. ;24 cm., https://doi.org/10.3133/wsp1593.","productDescription":"vi, 17 p. ;24 cm.","costCenters":[],"links":[{"id":137129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1593/report-thumb.jpg"},{"id":26000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1593/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":264358,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-1.pdf","size":"3161","linkFileType":{"id":1,"text":"pdf"}},{"id":264359,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-2.pdf","size":"2582","linkFileType":{"id":1,"text":"pdf"}},{"id":264360,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-3.pdf","size":"1606","linkFileType":{"id":1,"text":"pdf"}},{"id":264361,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-4.pdf","size":"355","linkFileType":{"id":1,"text":"pdf"}},{"id":264362,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-5.pdf","size":"1808","linkFileType":{"id":1,"text":"pdf"}},{"id":264363,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-6.pdf","size":"1599","linkFileType":{"id":1,"text":"pdf"}},{"id":264364,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-7.pdf","size":"4402","linkFileType":{"id":1,"text":"pdf"}},{"id":264365,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1593/plate-8.pdf","size":"4532","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f38d7","contributors":{"authors":[{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbell, David Wellington","contributorId":88330,"corporation":false,"usgs":true,"family":"Hubbell","given":"David","email":"","middleInitial":"Wellington","affiliations":[],"preferred":false,"id":143288,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047695,"text":"70047695 - 1961 - A study of flow in alluvial channels: the effect of large concentrations of fine sediment on the mechanics of flow in a small flume","interactions":[],"lastModifiedDate":"2016-11-09T09:31:38","indexId":"70047695","displayToPublicDate":"1969-01-21T14:54:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"A study of flow in alluvial channels: the effect of large concentrations of fine sediment on the mechanics of flow in a small flume","docAbstract":"A flume study was made using a natural river sand as the bed material, median diameter = 0. 54 millimeters. Clear-water flow was compared with flow containing from 6 1 000 to 65,000 parts per million of fine sediment (bentonite). The study shows that the form of bed roughness could be changed by adding sufficient fine sediment (bentonite) to the clear-water flow. The total bed material transport was decreased by 50 percent with increasing fine sediment\nconcentration with the dune bed form and was increased by as much as 550 percent for the transition, standing wave, and antidune forms of bed roughness. Resistance to flow was less (C/√ g increased by 45 percent) with fine sediment-laden flow than with clear-water flow for the dune, and transition bed forms; and was greater (C/√ g   reduced by 25 percent) for the standing waves and the antidunes. A narrow range of bentonite concentration for each form of bed roughness was established as a limit below which only minor changes in bed form, bed material transport, and resistance to flow occurred. The variation of the liquid properties, specific weight and viscosity, for water-bentonite dispersions were studied and their effect on the properties of the bed material particles measured. The fall velocity of the particles in a dispersion of 100, 000 parts per million fine sediment in water was reduced to about one-half their fall velocity in clear water.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Fort Collins, CO","doi":"10.3133/70047695","usgsCitation":"Haushild, W.L., Simons, D.B., and Richadrson, E.V., 1961, A study of flow in alluvial channels: the effect of large concentrations of fine sediment on the mechanics of flow in a small flume, viii, 44 p., https://doi.org/10.3133/70047695.","productDescription":"viii, 44 p.","numberOfPages":"53","costCenters":[],"links":[{"id":278730,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047695/report.pdf","text":"Report","size":"15.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":276775,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047695/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"527a217be4b051792d0194c0","contributors":{"authors":[{"text":"Haushild, William Leland","contributorId":87447,"corporation":false,"usgs":true,"family":"Haushild","given":"William","email":"","middleInitial":"Leland","affiliations":[],"preferred":false,"id":482737,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simons, Daryl Baldwin","contributorId":98621,"corporation":false,"usgs":true,"family":"Simons","given":"Daryl","email":"","middleInitial":"Baldwin","affiliations":[],"preferred":false,"id":482738,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richadrson, Everett V.","contributorId":75053,"corporation":false,"usgs":true,"family":"Richadrson","given":"Everett","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":482736,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":265,"text":"265 - 1961 - Surface water records of Indiana, 1961","interactions":[],"lastModifiedDate":"2014-05-19T13:33:05","indexId":"265","displayToPublicDate":"1962-01-01T13:18:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of Indiana, 1961","docAbstract":"

The surface-water records for the 1961 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Malcolm D. Hale, district engineer, Surface Water Branch.

\n
\n

This report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Indiana were contained in Parts 3A, 4 and 5 of that series.

\n
\n

Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of coterminous United States will be further subdivided.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/265","issn":"0565-5986","collaboration":"Prepared under the direction of Malcolm D. Hale, District Engineer, Surface Water Branch, in cooperation with the State of Indiana and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of Indiana, 1961, vii, 185 p., https://doi.org/10.3133/265.","productDescription":"vii, 185 p.","numberOfPages":"194","temporalStart":"1960-10-01","temporalEnd":"1961-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/265.jpg"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b2807e4b0929ba496abb8","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":527264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206836,"text":"70206836 - 1961 - Origin of Pennsylvanian underclay and related seat rocks","interactions":[],"lastModifiedDate":"2019-11-25T06:51:24","indexId":"70206836","displayToPublicDate":"1961-12-31T20:19:59","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Origin of Pennsylvanian underclay and related seat rocks","docAbstract":"

Seat rocks, including underclay, underlie coal beds and show features such as roots, profiles similar to water-logged soils, lack of bedding, soil-like fracture, and gradation into normally bedded sedimentary rocks indicating that they were once soils. Coarse-grained seat rocks range from argillaceous to nearly pure quartz sandstone (ganister). Seat rocks composed of clay-sized particles (underclays) range from mixtures of illite, mixed-layer clay, and kaolinite to essentially pure kaolinite. Variations in the quartz or kaolinite content suggest that there are degrees of alteration in the formation of a seat rock and that all kinds of seat rock were formed by leaching of the substratum in a swamp. The increasing crystallinity of the clay minerals from plastic underclays to semiflint clay to flint clay and the corresponding increase in titanium support this conclusion. These two features suggest strongly that flint clays formed in place in an acidic swamp environment. The Olive Hill clay shows residual acidity. Seat rocks are affected by the chemical environments in the swamp before peat accumulation, during peat accumulation, and during coalification. Kaolinite is forming in present-day swamps and in wet acidic soils in Hawaii and probably formed in late Paleozoic swamps. The facts can be interpreted to show that all kinds of seat rocks could have formed in Pennsylvanian swamps and probably most did. 

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1643:OOPUAR]2.0.CO;2","issn":"00167606","usgsCitation":"Huddle, J.W., and Patterson, S.H., 1961, Origin of Pennsylvanian underclay and related seat rocks: Geological Society of America Bulletin, v. 72, no. 11, p. 1643-1660 , https://doi.org/10.1130/0016-7606(1961)72[1643:OOPUAR]2.0.CO;2.","productDescription":"18 p. ","startPage":"1643","endPage":"1660 ","costCenters":[],"links":[{"id":369520,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huddle, J. W.","contributorId":29043,"corporation":false,"usgs":true,"family":"Huddle","given":"J.","middleInitial":"W.","affiliations":[],"preferred":false,"id":775998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patterson, S. H.","contributorId":85232,"corporation":false,"usgs":true,"family":"Patterson","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":775999,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220644,"text":"70220644 - 1961 - Paleoecology of an early oligocene biota from Douglass Creek Basin, Montana","interactions":[],"lastModifiedDate":"2021-05-21T19:16:21.510182","indexId":"70220644","displayToPublicDate":"1961-12-31T14:08:45","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Paleoecology of an early oligocene biota from Douglass Creek Basin, Montana","docAbstract":"

Douglass Creek basin lies west of the Continental Divide in the northern part of the Rocky Mountain physiographic province. Numerous minor environmental differences exist between the Douglass Creek area and the Pipestone Springs and Canyon Ferry areas east of the Divide. In the 19th century, however, the three areas had identical mammalian species representation, although not equally dense populations. Fossils of an early Oligocene biota have been collected from the Douglass Creek basin. Presence of all but one of the Douglass Creek mammalian species in the Pipestone Springs-Canyon Ferry early Oligocene fauna suggests that the three ancient ecosystems resembled each other in much the same way as the 19th century systems. The early Oligocene deposits and biota of the Douglass Creek basin indicate a moist, temperate climate with seasonal variations. Sediment size and distribution suggest that the cross-valley relief was no greater than it is now. The fish and invertebrate faunas show that a shallow, hard-water lake existed in the area. The flora included a lowland, lake-border association and an upland coniferous forest. Although the ancient Douglass Creek biota doubtless included many species not represented in the fossil collections, most of the mammalian species are probably represented in the combined Douglass Creek, Pipestone Springs, and Canyon Ferry fossil assemblages. If so, the number of mammalian species was about the same as in the 19th century ecosystem.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1633:POAEOB]2.0.CO;2","usgsCitation":"Konizeski, R.L., 1961, Paleoecology of an early oligocene biota from Douglass Creek Basin, Montana: Geological Society of America Bulletin, v. 72, no. 11, p. 1633-1642, https://doi.org/10.1130/0016-7606(1961)72[1633:POAEOB]2.0.CO;2.","productDescription":"10 p.","startPage":"1633","endPage":"1642","costCenters":[],"links":[{"id":385864,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Douglas Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.06510925292969,\n 46.584350070440536\n ],\n [\n -112.91130065917969,\n 46.584350070440536\n ],\n [\n -112.91130065917969,\n 46.62963563393178\n ],\n [\n -113.06510925292969,\n 46.62963563393178\n ],\n [\n -113.06510925292969,\n 46.584350070440536\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"72","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Konizeski, Richard L.","contributorId":80248,"corporation":false,"usgs":true,"family":"Konizeski","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207362,"text":"70207362 - 1961 - Recent chemical analyses of waters from several closed-basin lakes and their tributaries in the western United States","interactions":[],"lastModifiedDate":"2019-12-18T11:09:00","indexId":"70207362","displayToPublicDate":"1961-12-31T11:04:45","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Recent chemical analyses of waters from several closed-basin lakes and their tributaries in the western United States","docAbstract":"

Some of the classic closed-basin lakes of the western United States have been resampled, and the waters have been analyzed by modern wet-chemical methods. Included are waters from Borax and Little Borax lakes and Mono Lake in California; Big Soda, Pyramid, and Walker Lakes in Nevada; Abert Lake, Oregon; and Great Salt Lake, Utah. Tributary streams and springs have also been sampled and are reported upon. © 1961, The Geological Society of America, Inc.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1961)72[1421:RCAOWF]2.0.CO;2","issn":"00167606","usgsCitation":"Whitehead, H., and Feth, J.H., 1961, Recent chemical analyses of waters from several closed-basin lakes and their tributaries in the western United States: Geological Society of America Bulletin, v. 72, no. 9, p. 1421-1425, https://doi.org/10.1130/0016-7606(1961)72[1421:RCAOWF]2.0.CO;2.","productDescription":"5 p. ","startPage":"1421","endPage":"1425","costCenters":[],"links":[{"id":370401,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Whitehead, H.C.","contributorId":50134,"corporation":false,"usgs":true,"family":"Whitehead","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":777818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777819,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220596,"text":"70220596 - 1961 - Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 2, Relationship of uranium migration dates, geology, and chemistry of the uranium deposits","interactions":[],"lastModifiedDate":"2021-05-21T14:24:33.414608","indexId":"70220596","displayToPublicDate":"1961-12-01T15:13:27","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 2, Relationship of uranium migration dates, geology, and chemistry of the uranium deposits","docAbstract":"

The time of U migration in deposits in sandstone can be determined by correlating apparent age calculations, based on radiochemical analyses, with the geology of a particular deposit. Data were obtained from U ore samples representing deposits above the water table, deposits just above and below perched water tables, and deposits at least 250 ft. below the water table in the Hulett Creek area, Wyoming. The first U deposition occurred more than 250,000 years ago for the deposits now at or above the water table. Approximately 60,000 to 80,000 years ago these deposits were oxidized, leached, and locally enriched. Accumulation of U in the deposits below the water table probably did not start before 180,000 years ago and has continued to the present.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.56.8.1404","usgsCitation":"Robinson, C.S., and Rosholt, J.N., 1961, Uranium migration and geochemistry of uranium deposits in sandstone above, at, and below the water table; Part 2, Relationship of uranium migration dates, geology, and chemistry of the uranium deposits: Economic Geology, v. 56, no. 8, p. 1404-1420, https://doi.org/10.2113/gsecongeo.56.8.1404.","productDescription":"17 p.","startPage":"1404","endPage":"1420","costCenters":[],"links":[{"id":385812,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.09472656249999,\n 43.83452678223682\n ],\n [\n -103.5791015625,\n 43.83452678223682\n ],\n [\n -103.5791015625,\n 45.36758436884978\n ],\n [\n -107.09472656249999,\n 45.36758436884978\n ],\n [\n -107.09472656249999,\n 43.83452678223682\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"56","issue":"8","noUsgsAuthors":false,"publicationDate":"1961-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Robinson, C. S.","contributorId":23578,"corporation":false,"usgs":true,"family":"Robinson","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":816115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosholt, John Nicholas Jr.","contributorId":26370,"corporation":false,"usgs":true,"family":"Rosholt","given":"John","suffix":"Jr.","email":"","middleInitial":"Nicholas","affiliations":[],"preferred":false,"id":816116,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}