{"pageNumber":"645","pageRowStart":"16100","pageSize":"25","recordCount":16440,"records":[{"id":2376,"text":"wsp1475E - 1961 - Ground water in the western part of Cow Creek and Soldier Creek Grazing Units, Malheur County, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:31:43","indexId":"wsp1475E","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":"1475","chapter":"E","title":"Ground water in the western part of Cow Creek and Soldier Creek Grazing Units, Malheur County, Oregon","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1475E","usgsCitation":"Newcomb, R.C., 1961, Ground water in the western part of Cow Creek and Soldier Creek Grazing Units, Malheur County, Oregon: U.S. Geological Survey Water Supply Paper 1475, iii, 159-172 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1475E.","productDescription":"iii, 159-172 p. :ill., map ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":137761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475e/report-thumb.jpg"},{"id":28331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d730","contributors":{"authors":[{"text":"Newcomb, Reuben Clair","contributorId":37712,"corporation":false,"usgs":true,"family":"Newcomb","given":"Reuben","email":"","middleInitial":"Clair","affiliations":[],"preferred":false,"id":145105,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":958,"text":"wsp1608A - 1961 - Effects of phosphate mining on the ground water of Anguar, Palau Islands, Trust Territory of the Pacific Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1608A","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":"1608","chapter":"A","title":"Effects of phosphate mining on the ground water of Anguar, Palau Islands, Trust Territory of the Pacific Islands","docAbstract":"Mining of phosphate ore on Angaur Island by mechanized methods created large water-table lakes, which became filled with brackish or saline water. A hydrologic investigation was started in 1949 to determine whether the saline water in the lakes would spread to surrounding areas and cause damage to agricultural lands and the water supply. \r\n\r\nAngaur, which is in the Palau Islands in the southwestern part of Micronesia, is administered as part of the Trust Territory of the Pacific Islands, under a trusteeship granted to the United States by the United Nations. The island has an area of 3.2 square miles and has a maximum altitude of about 150 feet. The climate is tropical oceanic. The average annual temperature is 82 ? F; the average annual rainfall is about 125 inches; and the average relative humidity is about 80 percent. \r\n\r\nThe northwestern third of Angaur (province A) consists topographically of a series of concentric ridges and depressions which are underlain largely by well-cemented coralline limestone of Pliocene, Pleistocene, and Recent ages. The remaining two-thirds of Angaur (province B} is a low plain underlain in the northern and central parts by a low platform of coralline rubble of Pleistocene and Recent age and in the southern part by sandy and rubbly beach deposits of Recent age. Province A contained extensive phosphate deposits of which more than 3 million tons were mined in 1909-55. \r\n\r\nWeekly water-level measurements at 35 wells, test holes, and lakes indicate that the water table averages about 2 feet above mean sea level in the beach deposits, about half a foot above mean sea level in the rubble deposits, and about 1.35 feet above mean sea level in the coralline limestone. Water samples obtained weekly at the observation sites indicate that the ground water in province A is not of uniform quality, as large variations in salinity occur throughout the area. In contrast, the ground water in province B is of relatively uniform quality, and contains less than 1,000 ppm (parts per million) of chloride in most places. \r\n\r\nIn province A removal of earthy phosphate which had acted as a seal allowed the infiltration of saline water through solution channels exposed at the bottom of several of the lakes. The sampling program showed no indication of large-scale movement of saline water out of the lakes into adjacent ground water. Provinces A and B apparently function as independent ground-water units, and the quality of the ground water in province B has not been noticeably affected by mining activities in province A. \r\n\r\nThe lakes were backfilled with limestone rubble to reduce the possibility of underground movement of saline water out of the lakes. The gross permeability of the backfill material is less than that of the surrounding limestone in province A, and, as the rate of influx of saline water was curtailed, the recharge of fresh water from rainfall tended to reduce the salinity of the ground water in the fill. In parts of the backfilled area the salinity of the water at the water table decreased rapidly in less than 1 year, as a layer of fresh water was built up at the water table.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608A","usgsCitation":"Arnow, T., 1961, Effects of phosphate mining on the ground water of Anguar, Palau Islands, Trust Territory of the Pacific Islands: U.S. Geological Survey Water Supply Paper 1608, iv, 39 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1608A.","productDescription":"iv, 39 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608a/report-thumb.jpg"},{"id":25481,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611a74","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":142917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1761,"text":"wsp1532A - 1961 - Hydrologic effects of water spreading in Box Creek basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1532A","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":"1532","chapter":"A","title":"Hydrologic effects of water spreading in Box Creek basin, Wyoming","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1532A","usgsCitation":"Hadley, R.F., and McQueen, I., 1961, Hydrologic effects of water spreading in Box Creek basin, Wyoming: U.S. Geological Survey Water Supply Paper 1532, iv, 47, [1] p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1532A.","productDescription":"iv, 47, [1] p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532a/report-thumb.jpg"},{"id":26874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606e92","contributors":{"authors":[{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":144100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McQueen, I.S.","contributorId":59774,"corporation":false,"usgs":true,"family":"McQueen","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":144101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2662,"text":"wsp1602 - 1961 - Effect of reforestation on streamflow in central New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1602","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":"1602","title":"Effect of reforestation on streamflow in central New York","docAbstract":"Hydrologic data have been collected since 1932 in central New York State to determine the effect of reforestation on streamflow. Data are available for three small partly reforested areas and for one nonreforested control area. From 35 to 58 percent of the 3 areas were reforested, mostly with species of pine and spruce. The trees were allowed to grow without thinning or cutting, and by 1958 these reforested areas had developed into dense coniferous woodlots. \r\n\r\nIntensive statistical analyses of the data from the four study areas were made in 1958. Analyses were made for three hydrologic periods: the dormant season represented by the 6-month period ending April 30, the growing season represented by the 6-month period ending October 31, and the year represented by the 12-month period ending April 30. Analyses of the hydrologic data using multiple correlation with time as a variable and analyses of covariance between early and late periods of record indicated that several significant changes had occurred in the streamflow from the partly reforested study areas. Based on correlation with precipitation, total runoff for the dormant season from the 3 study areas was reduced by annual rates of 0.17 to 0.29 inches per year. Based on correlations with streamflow from a control area, total runoff from the partly reforested Shackham Brook area was reduced by average rates of 0.14 inches per growing season, 0.23 inches per dormant season, and 0.36 inches per hydrologic year. Peak discharges on Shackham Brook during the dormant season were reduced by 1958 by an average of 41 percent for the season, with reductions ranging from an average of 66 percent for November to an average of 16 percent for April. No significant changes were found in the peak discharges for the growing season, rates of base-flow recession, volumes of direct runoff, or annual low flows of streams in the three partly reforested areas. \r\n\r\nThe significant reductions in total runoff are attributed to increases in interception and transpiration in the reforested areas. The reductions in peak discharges during the dormant period are attributed largely to increased interception and sublimation of snowfall, and a gradual desynchronization of snowmelt runoff from the wooded and open areas of partly reforested watersheds. The changes in streamflow occurred gradually over the years; it could not be determined from the data whether changes in streamflow were still occurring in 1958, or whether they had reached a maximum.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1602","usgsCitation":"Schneider, W.J., and Ayer, G.R., 1961, Effect of reforestation on streamflow in central New York: U.S. Geological Survey Water Supply Paper 1602, v, 61 p. :maps, diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1602.","productDescription":"v, 61 p. :maps, diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138228,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1602/report-thumb.jpg"},{"id":28999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1602/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f8680","contributors":{"authors":[{"text":"Schneider, William Joseph","contributorId":104466,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ayer, Gordon Roundy","contributorId":52950,"corporation":false,"usgs":true,"family":"Ayer","given":"Gordon","email":"","middleInitial":"Roundy","affiliations":[],"preferred":false,"id":145572,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2372,"text":"wsp1587 - 1961 - Water resources of the Raft River basin, Idaho-Utah","interactions":[{"subject":{"id":51728,"text":"ofr54219 - 1954 - Ground-water resources of the Raft River basin, Cassia County, Idaho - a summary of unpublished data","indexId":"ofr54219","publicationYear":"1954","noYear":false,"title":"Ground-water resources of the Raft River basin, Cassia County, Idaho - a summary of unpublished data"},"predicate":"SUPERSEDED_BY","object":{"id":2372,"text":"wsp1587 - 1961 - Water resources of the Raft River basin, Idaho-Utah","indexId":"wsp1587","publicationYear":"1961","noYear":false,"title":"Water resources of the Raft River basin, Idaho-Utah"},"id":1}],"lastModifiedDate":"2022-12-19T21:20:39.37645","indexId":"wsp1587","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":"1587","title":"Water resources of the Raft River basin, Idaho-Utah","docAbstract":"<p>Much arable land in the Raft River basin of Idaho lacks water for irrigation, and the potentially irrigable acreage far exceeds the amount that could be irrigated with the estimated total supply of water. Therefore, the amount of uncommitted water that could be intercepted and used within the basin is the limiting factor in further development of its native water supply. Water for additional irrigation might be obtained by constructing surface-storage works, by pumping ground water, or by importing surface water. Additional groundwater development is feasible. As an aid to orderly development and use of the water supplies, the report summarizes available geologic and hydrologic data and, by analysis and interpretation, derives an estimate of the recoverable water yield of the basin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1587","collaboration":"Prepared in cooperation with the Idaho Department of Reclamation","usgsCitation":"Nace, R.L., 1961, Water resources of the Raft River basin, Idaho-Utah: U.S. Geological Survey Water Supply Paper 1587, Report: vi, 138 p.; 6 Plates: 29.00 x 60.00 inches or smaller, https://doi.org/10.3133/wsp1587.","productDescription":"Report: vi, 138 p.; 6 Plates: 29.00 x 60.00 inches or smaller","numberOfPages":"144","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":410736,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24773.htm","linkFileType":{"id":5,"text":"html"}},{"id":28323,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Provisional water-yield map of the Raft River basin, Idaho-Utah"},{"id":28322,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Provisional isohyetal map of the Raft River basin, Idaho-Utah"},{"id":28321,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Generalized geologic map of Raft River basin, Idaho-Utah"},{"id":28327,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1587/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1587/report-thumb.jpg"},{"id":28326,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Pumping rates, in cubic feet per second, of irrigation wells in the Raft River valley, Idaho"},{"id":28325,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Water table contours in the Raft River valley and northern plains section, October-November 1952"},{"id":28324,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Location of wells and stream-measuring stations in the Raft River basin, Idaho-Utah"}],"country":"United States","state":"Idaho, Utah","otherGeospatial":"Raft River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113,\n              42.683\n            ],\n            [\n              -113.844,\n              42.683\n            ],\n            [\n              -113.844,\n              41.76\n            ],\n            [\n              -113,\n              41.76\n            ],\n            [\n              -113,\n              42.683\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fab62","contributors":{"authors":[{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4923,"text":"pp424D - 1961 - Short papers in the geologic and hydrologic sciences, articles 293-435","interactions":[],"lastModifiedDate":"2024-11-15T16:17:42.029637","indexId":"pp424D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"424","chapter":"D","title":"Short papers in the geologic and hydrologic sciences, articles 293-435","docAbstract":"<p>The scientific and economic results of work by the United States Geological Survey during the fiscal year 1961, the 12 months ending June 30, 1961, are summarized in 4 volumes. This volume includes 143 short papers on subjects in the fields of geology, hydrology, and related sciences, prepared by members of the Geologic, Water Resources, and Conservation Divisions of the Survey. Some are announcements of new discoveries or observations on problems of limited scope, which may or may not be described in greater detail subsequently. Others summarize conclusions drawn from more extensive or continuing investigations, which in large part will be described in greater detail in reports to be published at a later date</p><p>Professional Paper 424-A provides a synopsis of the more important new findings resulting from work during the fiscal year. 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,{"id":38969,"text":"pp424A - 1961 - Synopsis of geologic and hydrologic results: Chapter A in <i>Geological Survey research 1961</i>","interactions":[],"lastModifiedDate":"2017-09-07T10:37:44","indexId":"pp424A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"424","chapter":"A","title":"Synopsis of geologic and hydrologic results: Chapter A in <i>Geological Survey research 1961</i>","docAbstract":"<p>The Geological Survey is engaged in many different kinds of investigations in the fields of geology and hydrology. These investigations may be grouped into several broad, inter-related categories as follows:</p><p>(a) Economic geology, including engineering geology</p><p>(b) Regional geologic mapping, including detailed mapping and stratigraphic studies</p><p>(c) Resource and topical studies</p><p>(d) Ground-water studies</p><p>(e) Surface-water studies</p><p>(f) Quality-of-water studies</p><p>(g) Field and laboratory research on geologic and hydrologic processes and principles.</p><p>The Geological Survey also carries on investigations in its fields of competence for other Federal agencies that do not have the required specialized staffs or scientific facilities.</p><p>Nearly all the Geological Survey's activities yield new data and principles of value in the development or application of the geologic and hydrologic sciences. The purpose of this report, which consists of 4 chapters, is to present as promptly as possible findings that have come to the fore during the fiscal year 1961 the 12 months ending June 30, 1961.</p><p>The present volume, chapter A, is a synopsis of the highlights of recent findings of scientific and economic interest. Some of these findings have been published or placed on open file during the year; some are presented in chapters B, C, and D; still others have not been published previously. Only part of the scientific and economic results developed during the year can be presented in this synopsis. Readers who wish more complete or more detailed information should consult the bibliography of reports beginning on page A-156 of this volume, and the collection of short articles presented in the companion chapters as follows:</p><p>Prof. Paper 424-B Articles 1 to 146</p><p>Prof. Paper 424-C Articles 147 to 292</p><p>Prof. Paper 424-D Articles 293 to 435</p><p>A list of investigations in progress in the Geologic and Water Resources Divisions with the names and addresses of the project leaders is given on pages A-110 to A-155 for those interested in work in progress in various areas or on special topics.</p><p>During the fiscal year 1961, the services of the Geologic and Water Resources Divisions were utilized, or supported financially in part, by the many Federal and State agencies listed on pages A-106 to A-109. The Geological Survey has also cooperated from time to time with other agencies, and some of the work described in these chapters stems from work of previous years in cooperation with agencies not shown on the list. All cooperating agencies are identified where appropriate in the individual short articles in chapters B, C, and D, and they are mentioned in connection with some of the larger programs summarized in chapter A; because of space limitations, however, their contributions are mentioned in many of the short summary paragraphs contained in chapter A.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1961 (Professional Paper 424)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp424A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Synopsis of geologic and hydrologic results: Chapter A in <i>Geological Survey research 1961</i>: U.S. Geological Survey Professional Paper 424, xii, 194 p., https://doi.org/10.3133/pp424A.","productDescription":"xii, 194 p.","numberOfPages":"209","costCenters":[],"links":[{"id":336127,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp424D","text":"Chapter D","linkHelpText":"Articles 293-435"},{"id":336125,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp424B","text":"Chapter B","linkHelpText":"Articles 1-146"},{"id":336126,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp424C","text":"Chapter C","linkHelpText":"Articles 147-292"},{"id":120394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0424a/report-thumb.jpg"},{"id":66036,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0424a/report.pdf","text":"Report","size":"6.08 MB","linkFileType":{"id":1,"text":"pdf"}}],"publicComments":"A summary of recent scientific and economic results, accompanied by a list of reports released in fiscal 1961 and a list of investigations in progress.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876de","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":529897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52228,"text":"ofr6228 - 1961 - Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions","interactions":[],"lastModifiedDate":"2018-10-03T09:24:58","indexId":"ofr6228","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":"62-28","title":"Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions","docAbstract":"<p>The Appalachian basin is an elongate depression in the crystalline basement complex which contains a great volume of predominantly sedimentary stratified rocks. As defined in this paper it extends from the Adirondack Mountains in New York to central Alabama. From east to west it extends from the west flank of the Blue Ridge Mountains to the crest of the Findlay and Cincinnati arches and the Nashville dome. It encompasses an area of about 207,000 square miles, including all of West Virginia and parts of New York, New Jersey, Pennsylvania, Ohio, Maryland, Virginia, Kentucky, Tennessee, North Carolina, Georgia, and Alabama.</p><p>The stratified rocks that occupy the basin constitute a wedge-shaped mass whose axis of greatest thickness lies close to and parallel to the east edge of the basin. The maximum thickness of stratified rocks preserved in any one part of the basin today is between 35,000 and 40,000 feet. The volume of the sedimentary rocks is approximately 510,000 cubic miles and of volcanic rocks is a few thousand cubic miles. The sedimentary rocks are predominantly Paleozoic in age, whereas the volcanic rocks are predominantly Late Precambrian.</p><p>On the basis of gross lithology the stratified rocks overlying the crystalline basement complex can be divided into nine vertically sequential units, which are designated \"sequences\" in this report. The boundaries between contiguous sequences do not necessarily coincide with the commonly recognized boundaries between systems or series. All sequences are grossly wedge shaped, being thickest along the eastern margin of the basin and thinnest along the western margin.</p><p>The lowermost unit the Late Precambrian stratified sequence is present only along part of the eastern margin of the basin, where it lies unconformably on the basement complex. It consists largely of volcanic tuffs and flows but contains some interbedded sedimentary rocks. The Late Precambrian sequence is overlain by the Early Cambrian clastic sequence. Where the older sequence is absent, the Early Cambrian sequence rests on the basement complex. Interbedded fine- to coarse-grained noncarbonate detrital rocks comprise the bulk of the sequence, but some volcanic and carbonate rocks are included. Next above is the Cambrian-Ordovician carbonate sequence which consists largely of limestone and dolomite. Some quartzose sandstone is present in the lower part in the western half of the basin, and much shale is present in the upper part in the southeast part of the basin. The next higher sequence is the Late Ordovician clastic sequence, which consists largely of shale, siltstone, and sandstone. Coarse-grained light-gray to red rocks are common in the sequence along the eastern side of the basin, whereas fine-grained dark-gray to black calcareous rocks are common along the west side. The Late Ordovician clastic sequence is overlain unconformably in many places by the&nbsp;Early Silurian clastic sequence. The latter comprises a relatively thin wedge of coarse-grained clastic rocks. Some of the most prolific oil- and gas-producing sandstones in the Appalachian basin are included. Among these are the \"Clinton\" sands of Ohio, the Medina Sandstones of New York and Pennsylvania, and the Keefer or \"Big Six\" Sandstone of West Virginia and Kentucky. Conformably overlying the Early Silurian clastic sequence is the Silurian-Devonian carbonate sequence, which consists predominantly of limestone and dolomite. It also contains a salt-bearing unit in the north-central part of the basin and a thick wedge of coarse-grained red beds in the northeastern part. The sequence is absent in much of the southern part of the basin. Large volumes of gas and much oil are obtained from some of its rocks, especially from the Oriskany Sandstone and the Huntersville Ghert. The Silurian-Devonian carbonate sequence is abruptly overlain by the Devonian clastic sequence a thick succession of interbedded shale, mudrock, siltstone, and sandstone. Colors range from predominantly purple and red in the northeastern part of the basin to predominantly dark gray and black in the southwestern part. Many rocks in the upper part contain hydrocarbons in commercial quantities. The next higher sequence is a heterogeneous succession that comprises most rocks of Mississippian age in the basin. It is composed largely of fine-grained to very coarse-grained noncalcareous clastic rocks in the northern half of the basin, and largely of carbonate rocks in the southern part. Large quantities of oil and gas are produced from the sequence. The youngest sequence consists of coarse-grained clastic rocks largely of Pennsylvanian age. In the center of the basin a relatively small volume of lithologically similar rocks of Permian age are included. The sequence has been intensively mined for coal throughout most of its extent.</p><p>The waste-disposal possibilities of the stratified rocks in the Appalachian basin are considered in terms of the following: 1) gross lithology of the sequences; 2) general lithology of the rock units composing the sequences; and 3) the structural attitudes of the sequences in different parts of the basin. The degree of exploitation of economically significant mineral* resources is considered briefly where such exploitation may affect waste-disposal possibilities. Hydrologic aspects are not in general considered. Based largely on consideration of the above geologic factors the following types of reservoirs associated with particular geologic environments offer some prospects for the disposal of radioactive waste solutions. They are: 1) artificially created cavities in thick salt beds; 2) artificially fractured thin lenticular sandstone bodies isolated in shale or mudrock sequences; 3) portions of thick noncarbonate clastic sequences possessing appreciable natural porosity and permeability; 4) thin clastic units (with natural or artificially created openings) in the plate of a thrust fault overlain by impermeable strata.</p><p>Considered in its entirety the Late Ordovician clastic sequence appears to have a greater number of favorable geologic factors for waste-disposal purposes than the others. The Early Silurian clastic sequence, the Silurian-Devonian carbonate sequence, and the Devonian clastic sequence offer fewer possibilities. The Late Precambrian stratified sequence, Early Cambrian, and the Cambrian-Ordovician carbonate sequence offer few possibilities. The Mississippian and Pennsylvanian sequences appear to be generally unsuitable.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr6228","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Colton, G.W., 1961, Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions: U.S. Geological Survey Open-File Report 62-28, Report: 121 p.; 15 Maps; 1 Illustration, https://doi.org/10.3133/ofr6228.","productDescription":"Report: 121 p.; 15 Maps; 1 Illustration","costCenters":[],"links":[{"id":86729,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86730,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0028/report-thumb.jpg"},{"id":86731,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86732,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86733,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86734,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86735,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86736,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86737,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86738,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86739,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86740,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86741,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86742,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86743,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86744,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.71,35.8 ], [ -84.71,43.91 ], [ -74.13,43.91 ], [ -74.13,35.8 ], [ -84.71,35.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688132","contributors":{"authors":[{"text":"Colton, George Willis","contributorId":12015,"corporation":false,"usgs":true,"family":"Colton","given":"George","email":"","middleInitial":"Willis","affiliations":[],"preferred":false,"id":244999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35357,"text":"b1133A - 1961 - Geology and hydrology of the Piqua area, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"b1133A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1133","chapter":"A","title":"Geology and hydrology of the Piqua area, Ohio","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1133A","usgsCitation":"Norris, S.E., and Spieker, A.M., 1961, Geology and hydrology of the Piqua area, Ohio: U.S. Geological Survey Bulletin 1133, p. A1-A33, ;23 cm., https://doi.org/10.3133/b1133A.","productDescription":"p. A1-A33, ;23 cm.","costCenters":[],"links":[{"id":165591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1133a/report-thumb.jpg"},{"id":63220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1133a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685247","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":214506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spieker, Andrew M.","contributorId":41492,"corporation":false,"usgs":true,"family":"Spieker","given":"Andrew","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":214507,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38970,"text":"pp424B - 1961 - Short papers in the geologic and hydrologic sciences; Articles 1-146","interactions":[],"lastModifiedDate":"2023-09-25T21:08:19.50785","indexId":"pp424B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"424","chapter":"B","title":"Short papers in the geologic and hydrologic sciences; Articles 1-146","docAbstract":"<p>The scientific and economic results of work by the United States Geological Survey during the fiscal year 1961, the 12 months ending June 30, 1961, will be summarized in four volumes of which this is the first. This volume includes 146 short papers on a variety of subjects in the fields of geology, hydrology, and related sciences, prepared by members of the Geologic, Water Resources, and Conservation Divisions of the Survey. These papers are of two kinds. Some are announcements of new discoveries or observations on problems of limited scope, which may or may not be described in greater detail subsequently. Others summarize conclusions drawn from more extensive or continuing investigations, which in large part will be described in greater detail in reports to be published at a· later date.</p><p>Professional Papers 424-C and -D include additional short papers of the same character as those in the present volume. Professional Paper 424-A provides a synopsis of the more important new findings resulting from work during the fiscal year.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1961 (Professional Paper 424)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp424B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Short papers in the geologic and hydrologic sciences; Articles 1-146: U.S. Geological Survey Professional Paper 424, viii, 344 p., https://doi.org/10.3133/pp424B.","productDescription":"viii, 344 p.","numberOfPages":"352","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":336128,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.er.usgs.gov/publication/pp424A","text":"Chapter A","linkHelpText":"Synopsis of geologic and hydrologic results"},{"id":113313,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0424b/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":173313,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0424b/report-thumb.jpg"},{"id":336129,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.er.usgs.gov/publication/pp424C","text":"Chapter C","linkHelpText":"Articles 147-292"},{"id":336130,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.er.usgs.gov/publication/pp424D","text":"Chapter D","linkHelpText":"Articles 293-435"},{"id":421142,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28432.htm","linkFileType":{"id":5,"text":"html"}}],"publicComments":"Scientific notes and summaries of investigations prepared by me1nbers of the Geologic, Water Resources, and Conservation Divisions in the fields of geology, hydrology, and allied sciences.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648567","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":529898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52188,"text":"ofr6192 - 1961 - Studies of the hydrology of the lower Colorado River area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6192","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":"61-92","title":"Studies of the hydrology of the lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6192","usgsCitation":"McDonald, C.C., 1961, Studies of the hydrology of the lower Colorado River area: U.S. Geological Survey Open-File Report 61-92, 8 p., https://doi.org/10.3133/ofr6192.","productDescription":"8 p.","costCenters":[],"links":[{"id":176827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dc9","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":244929,"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":68664,"text":"ha11 - 1961 - Precipitation, water loss, and runoff in the Delaware River basin and New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:13:41","indexId":"ha11","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"11","title":"Precipitation, water loss, and runoff in the Delaware River basin and New Jersey","language":"ENGLISH","doi":"10.3133/ha11","usgsCitation":"Hely, A.G., Nordenson, T.J., and and others, 1961, Precipitation, water loss, and runoff in the Delaware River basin and New Jersey: U.S. Geological Survey Hydrologic Atlas 11, 1 map :illus., maps (part col.) ;69 cm., https://doi.org/10.3133/ha11.","productDescription":"1 map :illus., maps (part col.) ;69 cm.","costCenters":[],"links":[{"id":186048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db6808b8","contributors":{"authors":[{"text":"Hely, Allen Grant","contributorId":41902,"corporation":false,"usgs":true,"family":"Hely","given":"Allen","email":"","middleInitial":"Grant","affiliations":[],"preferred":false,"id":278668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordenson, T. J.","contributorId":95116,"corporation":false,"usgs":true,"family":"Nordenson","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":534512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66034,"text":"i330 - 1961 - Geology of the Moses Lake North quadrangle, Washington","interactions":[],"lastModifiedDate":"2013-12-13T16:26:47","indexId":"i330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"330","title":"Geology of the Moses Lake North quadrangle, Washington","docAbstract":"The geology of the Moses Lake North quadrangle was mapped in 1954 and 1958 by the U.S. Geological Survey. Some of the basic hydrologic data has been collected by the Geological Survey during the early investigations of ground-water conditions in the Quincy Basin (Henshaw, written communication, 1917; Schwennesen and Meinzer, 1918). Most of the data, however, were obtained by the Geological Survey since 1941, in cooperation with the U.S. Bureau of Reclamation and the Washington State Department of Conservation under continuing programs in the area of the Columbia Basin Project of the Bureau of Reclamation. Some preliminary geologic field work in the Moses Lake North quadrangle was done by the Geological Survey in 1954 in cooperation with the Washington State Department of Conservation.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i330","collaboration":"Prepared in cooperation with the Washington State Department of Conservation","usgsCitation":"Grolier, M.J., and Foxworthy, B.L., 1961, Geology of the Moses Lake North quadrangle, Washington: U.S. Geological Survey IMAP 330, Plate: 37.73 x 40.60 inches, https://doi.org/10.3133/i330.","productDescription":"Plate: 37.73 x 40.60 inches","costCenters":[],"links":[{"id":102912,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1379.htm","linkFileType":{"id":5,"text":"html"},"description":"1379"},{"id":189540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0330/report-thumb.jpg"},{"id":279958,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0330/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Washington","otherGeospatial":"Moses Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.375,47.125 ], [ -119.375,47.25 ], [ -119.25,47.25 ], [ -119.25,47.125 ], [ -119.375,47.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e98d","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":273889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foxworthy, Bruce L.","contributorId":88815,"corporation":false,"usgs":true,"family":"Foxworthy","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":273888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70220635,"text":"70220635 - 1961 - Flood frequencies as related to land use","interactions":[],"lastModifiedDate":"2021-05-21T17:41:19.605472","indexId":"70220635","displayToPublicDate":"1961-12-31T12:37:42","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Flood frequencies as related to land use","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666109493241","usgsCitation":"Schneider, W.J., 1961, Flood frequencies as related to land use: International Association of Scientific Hydrology - Bulletin , v. 6, no. 4, p. 36-39, https://doi.org/10.1080/02626666109493241.","productDescription":"4 p.","startPage":"36","endPage":"39","costCenters":[],"links":[{"id":480378,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666109493241","text":"Publisher Index Page"},{"id":385855,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schneider, William J.","contributorId":47349,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":816265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220647,"text":"70220647 - 1961 - Bankfull discharge: An example of its statistical relationships","interactions":[],"lastModifiedDate":"2021-05-21T19:36:53.939689","indexId":"70220647","displayToPublicDate":"1961-09-30T14:30:42","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Bankfull discharge: An example of its statistical relationships","docAbstract":"<p><span>Analysis of data for the White and Wabash Rivers suggests means of determining&nbsp;</span><span class=\"ScopusTermHighlight\">discharge</span><span>&nbsp;at the natural&nbsp;</span><span class=\"ScopusTermHighlight\">bankfull</span><span>&nbsp;stage, despite the effects of artificial embanking and clearance of channels.&nbsp;</span><span class=\"ScopusTermHighlight\">Bankfull</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">discharge</span><span>, and&nbsp;</span><span class=\"ScopusTermHighlight\">discharge</span><span>&nbsp;at mean annual flood, undergo an orderly downstream increase in percentage duration of flow.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666109493230","usgsCitation":"Dury, G., 1961, Bankfull discharge: An example of its statistical relationships: International Association of Scientific Hydrology - Bulletin , v. 6, no. 3, p. 48-55, https://doi.org/10.1080/02626666109493230.","productDescription":"8 p.","startPage":"48","endPage":"55","costCenters":[],"links":[{"id":480379,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666109493230","text":"Publisher Index Page"},{"id":385867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Indiana","otherGeospatial":"White and Wabash Rivers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.506103515625,\n              39.30029918615029\n            ],\n            [\n              -84.957275390625,\n              39.30029918615029\n            ],\n            [\n              -84.957275390625,\n              41.52502957323801\n            ],\n            [\n              -87.506103515625,\n              41.52502957323801\n            ],\n            [\n              -87.506103515625,\n              39.30029918615029\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dury, G.H.","contributorId":93106,"corporation":false,"usgs":true,"family":"Dury","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":816289,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220639,"text":"70220639 - 1961 - Stream-gaging problems in Afghanistan","interactions":[],"lastModifiedDate":"2021-05-21T18:32:44.170274","indexId":"70220639","displayToPublicDate":"1961-09-30T13:27:43","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Stream-gaging problems in Afghanistan","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666109493227","usgsCitation":"Heckmiller, I., 1961, Stream-gaging problems in Afghanistan: International Association of Scientific Hydrology - Bulletin , v. 6, no. 3, p. 35-37, https://doi.org/10.1080/02626666109493227.","productDescription":"3 p.","startPage":"35","endPage":"37","costCenters":[],"links":[{"id":480380,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666109493227","text":"Publisher Index Page"},{"id":385859,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Afghanistan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              59.0625,\n              28.459033019728043\n            ],\n            [\n              74.53125,\n              28.459033019728043\n            ],\n            [\n              74.53125,\n              40.04443758460856\n            ],\n            [\n              59.0625,\n              40.04443758460856\n            ],\n            [\n              59.0625,\n              28.459033019728043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Heckmiller, I.A.","contributorId":258266,"corporation":false,"usgs":false,"family":"Heckmiller","given":"I.A.","email":"","affiliations":[],"preferred":false,"id":816270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010634,"text":"70010634 - 1961 - Dating desert ground water","interactions":[],"lastModifiedDate":"2026-02-25T17:33:14.813335","indexId":"70010634","displayToPublicDate":"1961-07-14T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Dating desert ground water","docAbstract":"Tritium in Arabian rainfall has followed the trend observed in North America with peaks in 1958 and the spring of 1959. These measurements will be useful for future hydrologie studies. Water from wadi gravels averages 10 yr old. Carbon-14 measurements of deep waters indicate ages of several thousand years.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.134.3472.105","issn":"00368075","usgsCitation":"Thatcher, L., Rubin, M., and Brown, G.F., 1961, Dating desert ground water: Science, v. 134, no. 3472, p. 105-106.","productDescription":"2 p.","startPage":"105","endPage":"106","costCenters":[],"links":[{"id":219254,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"134","issue":"3472","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fddee4b0c8380cd4e9a0","contributors":{"authors":[{"text":"Thatcher, L.","contributorId":38708,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","affiliations":[],"preferred":false,"id":359309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, Glen F.","contributorId":23943,"corporation":false,"usgs":true,"family":"Brown","given":"Glen","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":359308,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2980,"text":"wsp1526 - 1961 - Hydraulic and hydrologic aspects of flood-plain planning","interactions":[],"lastModifiedDate":"2023-04-06T20:29:05.829629","indexId":"wsp1526","displayToPublicDate":"1961-01-01T00:00:00","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":"1526","title":"Hydraulic and hydrologic aspects of flood-plain planning","docAbstract":"<p>The valid incentives compelling occupation of the flood plain, up to and eve n into the stream channel, undoubtedly have contributed greatly to the development of the country. But the result has been a heritage of flood disaster, suffering, and enormous costs. Flood destruction awakened a consciousness toward reduction and elimination of flood hazards, originally manifested in the protection of existing developments. More recently, increased knowledge of the problem has shown the impracticability of permitting development that requires costly flood protect/on. The idea of flood zoning, or flood-plain planning, has received greater impetus as a result of this realization. This study shows how hydraulic and hydrologic data concerning the flood regimen of a stream can be used in appraising its flood potential and the risk inherent in occupation of its flood plain. The approach involves the study of flood magnitudes as recorded or computed; flood frequencies based1 on experience shown by many years of gaging-station record; use of existing or computed stagedischarge relations and flood profiles; and, where required, the preparation of flood-zone maps to show the areas inundated by floods of several magnitudes and frequencies. The planner can delineate areas subject to inundation by floods o* specific recurrence intervals for three conditions: (a) for the immediate vicinity of a gaging station; (b) for a gaged stream at a considerable distance from a gaging station; and (c) for an ungaged stream. The average depth for a flood of specific frequency can be estimated on the basis of simple measurements of area of drainage basin, width of channel, and slope of streambed. This simplified approach should be useful in the initial stages of flood-plain planning. Brief discussions are included on various types of flood hazards, the effects of urbanization on flood runoff, and zoning considerations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1526","usgsCitation":"Wiitala, S., Jetter, K., and Sommerville, A.J., 1961, Hydraulic and hydrologic aspects of flood-plain planning: U.S. Geological Survey Water Supply Paper 1526, Report: v, 69 p.; 4 Plates: 34.50 x 18.50 inches or smaller, https://doi.org/10.3133/wsp1526.","productDescription":"Report: v, 69 p.; 4 Plates: 34.50 x 18.50 inches or smaller","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":415379,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24449.htm"},{"id":247262,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1526/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247261,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1526/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138923,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1526/report-thumb.jpg"},{"id":29736,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1526/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247264,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1526/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247263,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1526/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","city":"Carnegie","otherGeospatial":"Chartiers Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.0714,\n              40.4206\n            ],\n            [\n              -80.1194,\n              40.4206\n            ],\n            [\n              -80.1194,\n              40.3189\n            ],\n            [\n              -80.0714,\n              40.3189\n            ],\n            [\n              -80.0714,\n              40.4206\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a33c","contributors":{"authors":[{"text":"Wiitala, S.W.","contributorId":41806,"corporation":false,"usgs":true,"family":"Wiitala","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":146091,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jetter, K.R.","contributorId":23126,"corporation":false,"usgs":true,"family":"Jetter","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":146090,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sommerville, Alan J.","contributorId":64640,"corporation":false,"usgs":true,"family":"Sommerville","given":"Alan","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146092,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3185,"text":"wsp1531 - 1961 - Hydrology of the upper Cheyenne River basin: Part A. Hydrology of stock-water reservoirs in upper Cheyenne River basin; Part B. Sediment sources and drainage-basin characteristics in upper Cheyenne River basin","interactions":[],"lastModifiedDate":"2024-02-05T20:09:59.224588","indexId":"wsp1531","displayToPublicDate":"1961-01-01T00:00:00","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":"1531","title":"Hydrology of the upper Cheyenne River basin: Part A. Hydrology of stock-water reservoirs in upper Cheyenne River basin; Part B. Sediment sources and drainage-basin characteristics in upper Cheyenne River basin","docAbstract":"<p>The objective of this investigation was to determine the effect on runoff of the many stock reservoirs in the Cheyenne River basin above Angostura Dam. As a first step it was necessary to determine, within reasonable limits of accuracy, the number of reservoirs in the basin, the storage capacity, the drainage area, and the water loss from each. A sampling method was adopted because the size of the basin, 9,100 square miles, prohibited examination of all reservoirs within the drainage area. Forty-nine sample areas of 9 square miles each were selected as a 5-percent sample of the 955 complete quarter townships within the basin above Angostura Dam. All reservoirs located within the sample quarter townships were surveyed.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1531","usgsCitation":"Culler, R.C., Hadley, R.F., and Schumm, S.A., 1961, Hydrology of the upper Cheyenne River basin: Part A. Hydrology of stock-water reservoirs in upper Cheyenne River basin; Part B. 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