{"pageNumber":"2590","pageRowStart":"64725","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. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":244958,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52187,"text":"ofr6191 - 1961 - Investigation of the water resources of the lower Colorado River area","interactions":[{"subject":{"id":52187,"text":"ofr6191 - 1961 - Investigation of the water resources of the lower Colorado River area","indexId":"ofr6191","publicationYear":"1961","noYear":false,"title":"Investigation of the water resources of the lower Colorado River area"},"predicate":"SUPERSEDED_BY","object":{"id":45731,"text":"pp486A - 1976 - Water resources of lower Colorado River-Salton Sea area as of 1971; summary report","indexId":"pp486A","publicationYear":"1976","noYear":false,"chapter":"A","title":"Water resources of lower Colorado River-Salton Sea area as of 1971; summary report"},"id":1}],"supersededBy":{"id":45731,"text":"pp486A - 1976 - Water resources of lower Colorado River-Salton Sea area as of 1971; summary report","indexId":"pp486A","publicationYear":"1976","noYear":false,"title":"Water resources of lower Colorado River-Salton Sea area as of 1971; summary report"},"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6191","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":"61-91","title":"Investigation of the water resources of the lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6191","usgsCitation":"McDonald, C.C., 1961, Investigation of the water resources of the lower Colorado River area: U.S. Geological Survey Open-File Report 61-91, 5 p., https://doi.org/10.3133/ofr6191.","productDescription":"5 p.","costCenters":[],"links":[{"id":176826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c8e4b07f02db4ab7a8","contributors":{"authors":[{"text":"McDonald, C. 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":3411,"text":"cir439 - 1961 - Time of travel of water in the Ohio River, Pittsburgh to Cincinnati","interactions":[],"lastModifiedDate":"2017-06-09T08:32:55","indexId":"cir439","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"439","title":"Time of travel of water in the Ohio River, Pittsburgh to Cincinnati","docAbstract":"This report presents a procedure for estimating the time of travel of water in the Ohio River from Pittsburgh, Pa., to Cincinnati, Ohio, under various river stage conditions. This information is primarily for use by civil defense officials and by others concerned with problems involving travel time of river water. \r\n\r\nTables and charts are presented to show, for a particular stage or discharge at Cincinnati, the average time it would take for water to travel through the entire reach from Pittsburgh, or through successive intermediate segments of the reach. For example, when the discharge at Cincinnati is 200,000 cfs, travel time from Pittsburgh to Cincinnati, a distance of 470 miles, averages about 7 days; and for discharges of more than 200,000 cfs, the travel time decreases very slowly with increasing discharge. When the discharge is 30,000 cfs, travel time is about 28 days; and for discharges of less than 30,000 cfs, the travel time increases very rapidly with decreasing discharge. Estimates of travel time at low discharge are subject to large errors. Statistical analysis of the possible variations of upstream discharge for a given discharge at Cincinnati indicates that the shortest probable travel time from Pittsburgh to Cincinnati ranges from 56 percent of that under average conditions when the discharge at Cincinnati is 15,000 cfs to 93 percent of that under average conditions when the discharge at Cincinnati is 894,000 cfs. \r\n\r\nA chart showing the time distribution of flow at Cincinnati is presented so that the probable travel time of Ohio River water can be determined for any time of the year. This chart provides information which, when applied to the time-of-travel chart, shows that the most probable travel time of water from Pittsburgh to Cincinnati ranges from 160 hours in February to 1,250 hours in September. Also presented is a flow-duration curve that can be used to predict future discharges and, subsequently, times of travel, for use in long-range planning. The procedure used to compute time of travel is described in sufficient detail to make it usable as a guide for similar studies of other rivers that have deans and pools in the reach being studied. \r\n\r\nThe computations for the time-of-travel charts were made as follows: (a) by dividing the reach between Pittsburgh and Cincinnati into four subreaches with a full-range streamgaging station at or near the ends of each; (b) by computing for each subreach mean velocities corresponding to various discharges at Cincinnati, using data obtained from river survey maps and data available from gaging station operations; (c) by assuming that any mass of contaminated water would travel at a rate equal to that of the mean velocity of the river water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir439","usgsCitation":"Steacy, R.E., 1961, Time of travel of water in the Ohio River, Pittsburgh to Cincinnati: U.S. Geological Survey Circular 439, iii, 14 p. :map, diagrs., tables. ;27cm., https://doi.org/10.3133/cir439.","productDescription":"iii, 14 p. :map, diagrs., tables. ;27cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":30428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0439/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0439/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Ohio River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.957275390625,\n              38.272688535980976\n            ],\n            [\n              -79.8046875,\n              38.272688535980976\n            ],\n            [\n              -79.8046875,\n              40.73893324113601\n            ],\n            [\n              -84.957275390625,\n              40.73893324113601\n            ],\n            [\n              -84.957275390625,\n              38.272688535980976\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b6e4b07f02db533c35","contributors":{"authors":[{"text":"Steacy, Robert E.","contributorId":71162,"corporation":false,"usgs":true,"family":"Steacy","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39144,"text":"pp282F - 1961 - Drainage basins, channels, and flow characteristics of selected streams in central Pennsylvania","interactions":[],"lastModifiedDate":"2025-05-16T19:56:16.98169","indexId":"pp282F","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":"282","chapter":"F","title":"Drainage basins, channels, and flow characteristics of selected streams in central Pennsylvania","docAbstract":"<p>The hydraulic, basin, and geologic characteristics of 16 selected streams in central Pennsylvania were measured for the purpose of studying the relations among these general characteristics and their process of development. The basic parameters which were measured include bankfull width and depth, channel slope, bed material size and shape, length of stream from drainage divide, and size of drainage area. The kinds of bedrock over which the streams flow were noted. In these streams the bankfull channel is filled by flows approximating the 2.3-year flood. By measuring the breadth and mean depth of the channel, it was possible to compute the bankfull mean velocity for each of the 119 sampling stations. These data were then used to compute the downstream changes in hydraulic geometry of the streams studied. This method has been called an indirect computation of the hydraulic geometry. The results obtained by the indirect method are similar to those of the direct method of other workers. The basins were studied by examining the relations of drainage area, discharge, and length of stream from drainage divide. For the streams investigated, excellent correlations were found to exist between drainage area and the 2.3-year flood, as well as between length of stream from the basin divide and drainage area. From these correlations it is possible to predict the discharge for the 2.3-year flood at any arbitrary point along the length of the stream. The long, intermediate, and short axes of pebbles sampled from the bed of the stream were recorded to study both size and sphericity changes along individual streams and among the streams studied. No systematic downstream changes in sphericity were found. Particle size changes are erratic and show no consistent relation to channel slope. Particle size decreases downstream in many streams but remains constant or increases in others. Addition of material by tributaries is one factor affecting particle size and another is the parent material. Wear does not appear to account for some of the changes noted in particle size in a downstream direction. Comparison with laboratory studies indicates that at least in some streams the downstream decrease in size is much greater than would be expected from wear alone. The type of bedrock underlying the channels included in this study appears to affect both channel slope and particle size. For a given length of stream, a stream channel underlain by sandstone tends to have a steeper slope and larger bed material than channels underlain by shale or limestone. Hence, a stream which heads in sandstone and ends in limestone tends to have a more rapid decrease in slope and particle size than a stream heading in limestone and ending in sandstone. The association of steep slopes and small particles for limestone channels implies that slope and particle size may show a vague correlation between lithologic groups although no correlation may exist within a given lithologic type. In addition to the effect of bedrock on slope and particle size, there is some evidence that channels in limestone or dolomite have a slightly smaller cross section at bankfull stage than channels in shale or sandstone. Near the headwaters of many of these streams, a deposit of periglacial rubble affects the slope and bed material size. Some of the debris contains residual boulders which are too large to be moved by ordinary floods and, therefore, impose larger particle sizes in the bed of the stream. The addition of this very coarse debris to the bed material is another example of the influence of geologic factors on stream channels even though the channel consists of unconsolidated debris instead of bedrock. The influence of geologic factors noted in selected streams in central Pennsylvania may not be directly applicable to areas other than the Appalachian Mountains, but the general process is no doubt similar in most areas. In large alluvial valleys bedrock cannot be much of an influencing factor; yet large, thick alluvial deposits and terraces are in a sense \"bedrock\" materials upon which the stream works to form the landscape.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp282F","usgsCitation":"Brush, L.M., 1961, Drainage basins, channels, and flow characteristics of selected streams in central Pennsylvania: U.S. Geological Survey Professional Paper 282, Report: 37 p.; 3 Plates: 10.00 x 24.00 inches or smaller, https://doi.org/10.3133/pp282F.","productDescription":"Report: 37 p.; 3 Plates: 10.00 x 24.00 inches or smaller","startPage":"145","endPage":"181","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":66643,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0282f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66644,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0282f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66645,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0282f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66646,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0282f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119375,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0282f/report-thumb.jpg"},{"id":486127,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4258.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.5,\n              41.2139\n            ],\n            [\n              -78.5,\n              40.5\n            ],\n            [\n              -77.1372,\n              40.5\n            ],\n            [\n              -77.1372,\n              41.2139\n            ],\n            [\n              -78.5,\n              41.2139\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635dfb","contributors":{"authors":[{"text":"Brush, Lucien M. Jr.","contributorId":107343,"corporation":false,"usgs":true,"family":"Brush","given":"Lucien","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":221035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52163,"text":"ofr6148 - 1961 - Ground-water conditions, Naval Missile Facility, Point Arguello, California","interactions":[{"subject":{"id":52163,"text":"ofr6148 - 1961 - Ground-water conditions, Naval Missile Facility, Point Arguello, California","indexId":"ofr6148","publicationYear":"1961","noYear":false,"title":"Ground-water conditions, Naval Missile Facility, Point Arguello, California"},"predicate":"SUPERSEDED_BY","object":{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","indexId":"wsp1619F","publicationYear":"1963","noYear":false,"chapter":"F","title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California"},"id":1}],"supersededBy":{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","indexId":"wsp1619F","publicationYear":"1963","noYear":false,"title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California"},"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr6148","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":"61-48","title":"Ground-water conditions, Naval Missile Facility, Point Arguello, California","language":"ENGLISH","doi":"10.3133/ofr6148","usgsCitation":"Evenson, R.E., 1961, Ground-water conditions, Naval Missile Facility, Point Arguello, California: U.S. Geological Survey Open-File Report 61-48, 26 p., https://doi.org/10.3133/ofr6148.","productDescription":"26 p.","costCenters":[],"links":[{"id":178852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d08c","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":244895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71101,"text":"wdrWI611 - 1961 - Surface water records of Wisconsin, 1961","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrWI611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-61-1","title":"Surface water records of Wisconsin, 1961","language":"ENGLISH","doi":"10.3133/wdrWI611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of Wisconsin, 1961: U.S. Geological Survey Water Data Report WI-61-1, vi, 143 p., https://doi.org/10.3133/wdrWI611.","productDescription":"vi, 143 p.","numberOfPages":"149","costCenters":[],"links":[{"id":192934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696723","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":534720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52176,"text":"ofr6168 - 1961 - Water wells: Frenchman and Yucca Valleys, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6168","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":"61-68","title":"Water wells: Frenchman and Yucca Valleys, Nevada Test Site, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/ofr6168","usgsCitation":"Hood, J.W., 1961, Water wells: Frenchman and Yucca Valleys, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 61-68, 58 p., https://doi.org/10.3133/ofr6168.","productDescription":"58 p.","costCenters":[],"links":[{"id":175477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd131","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":244914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45134,"text":"pp354JK - 1961 - Lituyapecten (new subgenus of Patinopecten) from Alaska and California; stratigraphic occurrence of Lituyapecten in Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:55","indexId":"pp354JK","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":"354","chapter":"J,K","title":"Lituyapecten (new subgenus of Patinopecten) from Alaska and California; stratigraphic occurrence of Lituyapecten in Alaska","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1959","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp354JK","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Lituyapecten (new subgenus of Patinopecten) from Alaska and California; stratigraphic occurrence of Lituyapecten in Alaska: U.S. Geological Survey Professional Paper 354, 249 p., 43 leaves of plates : ill., map ; 29 cm. , https://doi.org/10.3133/pp354JK.","productDescription":"249 p., 43 leaves of plates : ill., map ; 29 cm. ","costCenters":[],"links":[{"id":168968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0354j-k/report-thumb.jpg"},{"id":82269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0354j-k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635b49","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":531556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":722,"text":"wsp1701 - 1961 - Surface water supply of the United States, 1960, Part 1-A, North Atlantic Slope basins, Maine to Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1701","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":"1701","title":"Surface water supply of the United States, 1960, Part 1-A, North Atlantic Slope basins, Maine to Connecticut","language":"ENGLISH","publisher":"U.S. Govt. Printing Office,","doi":"10.3133/wsp1701","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 1-A, North Atlantic Slope basins, Maine to Connecticut: U.S. Geological Survey Water Supply Paper 1701, v., 286 p. ;23 cm., https://doi.org/10.3133/wsp1701.","productDescription":"v., 286 p. ;23 cm.","costCenters":[],"links":[{"id":136290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1701/report-thumb.jpg"},{"id":25285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1701/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69436e","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":723,"text":"wsp1714 - 1961 - Surface water supply of the United States, 1960, Part 10, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1714","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":"1714","title":"Surface water supply of the United States, 1960, Part 10, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1714","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 10, The Great Basin: U.S. Geological Survey Water Supply Paper 1714, viii, 270 p. :tables ;23 cm., https://doi.org/10.3133/wsp1714.","productDescription":"viii, 270 p. :tables ;23 cm.","costCenters":[],"links":[{"id":136291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1714/report-thumb.jpg"},{"id":25286,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1714/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942d6","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1262,"text":"wsp1498C - 1961 - Depth-discharge relations of alluvial streams -- discontinuous rating curves","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1498C","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":"1498","chapter":"C","title":"Depth-discharge relations of alluvial streams -- discontinuous rating curves","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies in flow in alluvial channels","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1498C","usgsCitation":"Dawdy, D., 1961, Depth-discharge relations of alluvial streams -- discontinuous rating curves: U.S. Geological Survey Water Supply Paper 1498, iv, 16 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1498C.","productDescription":"iv, 16 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137432,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1498c/report-thumb.jpg"},{"id":26213,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1498c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66e011","contributors":{"authors":[{"text":"Dawdy, D.R.","contributorId":99956,"corporation":false,"usgs":true,"family":"Dawdy","given":"D.R.","affiliations":[],"preferred":false,"id":143460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68325,"text":"ha42 - 1961 - Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","interactions":[],"lastModifiedDate":"2022-06-03T20:40:02.242302","indexId":"ha42","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":"42","title":"Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha42","usgsCitation":"Herrick, E.H., 1961, Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells: U.S. Geological Survey Hydrologic Atlas 42, 1 Plate: 27.50 × 21.00 inches, https://doi.org/10.3133/ha42.","productDescription":"1 Plate: 27.50 × 21.00 inches","costCenters":[],"links":[{"id":185963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":401720,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15804.htm"},{"id":89786,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"680","country":"United States","state":"New Mexico","county":"Dona Ana County","otherGeospatial":"White Sands Missile Range headquarters area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.622314453125,\n              32.287132632616384\n            ],\n            [\n              -106.383,\n              32.287132632616384\n            ],\n            [\n              -106.383,\n              32.465743313283596\n            ],\n            [\n              -106.622314453125,\n              32.465743313283596\n            ],\n            [\n              -106.622314453125,\n              32.287132632616384\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2aef","contributors":{"authors":[{"text":"Herrick, Eugene H.","contributorId":80360,"corporation":false,"usgs":true,"family":"Herrick","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278031,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":52159,"text":"ofr6143 - 1961 - Ground-water conditions during 1960 at the Marine Corps Base, Twentynine Palms, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr6143","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":"61-43","title":"Ground-water conditions during 1960 at the Marine Corps Base, Twentynine Palms, California","language":"ENGLISH","doi":"10.3133/ofr6143","usgsCitation":"Dyer, H., 1961, Ground-water conditions during 1960 at the Marine Corps Base, Twentynine Palms, California: U.S. Geological Survey Open-File Report 61-43, 32 p., https://doi.org/10.3133/ofr6143.","productDescription":"32 p.","costCenters":[],"links":[{"id":178749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d2c3","contributors":{"authors":[{"text":"Dyer, H.B.","contributorId":86404,"corporation":false,"usgs":true,"family":"Dyer","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":244891,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6084,"text":"pp412 - 1961 - Salinity and hydrology of closed lakes","interactions":[],"lastModifiedDate":"2017-02-22T14:30:23","indexId":"pp412","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":"412","title":"Salinity and hydrology of closed lakes","docAbstract":"<p>Lakes without outlets, called closed lakes, are exclusively features of the arid and semiarid zones where annual evaporation exceeds rainfall. The number of closed lakes increases with aridity, so there are relatively few perennial closed lakes, but \"dry\" lakes that rarely contain water are numerous.</p><p>Closed lakes fluctuate in level to a much greater degree than the open lakes of the humid zone, because variations in inflow can be compensated only by changes in surface area. Since the variability of inflow increases with aridity, it is possible to derive an approximate relationship for the coefficient of variation of lake area in terms of data on&nbsp;rates of evaporation, lake area, lake depth, and drainage area.</p><p>The salinity of closed lakes is highly variable, ranging from less than 1 percent to over 25 percent by weight of salts. Some evidence suggests that the tonnage of salts in a lake solution is substantially less than the total input of salts into the lake over the period of existence of the closed lake. This evidence suggests further that the salts in a lake solution represent a kind of long-term balance between factors of gain and loss of salts from the solution.</p><p>Possible mechanisms for the loss of salts dissolved in the lake include deposition in marginal bays, entrapment in sediments, and removal by wind. Transport of salt from the lake surface in wind spray is also a contributing, but seemingly not major, factor.</p><p>The hypothesis of a long-term balance between input to and losses from the lake solution is checked by deriving a formula for the equilibrium concentration and comparing the results with the salinity data. The results indicate that the reported salinities seemingly can be explained in terms of their geometric properties and hydrologic environment.</p><p>The time for accumulation of salts in the lake solution the ratio between mass of salts in the solution and the annual input may also be estimated from the geometric and hydrologic factors, in the absence of data on the salt content of the lake or of the inflow.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp412","usgsCitation":"Langbein, W.B., 1961, Salinity and hydrology of closed lakes: U.S. Geological Survey Professional Paper 412, iii, 20 p., https://doi.org/10.3133/pp412.","productDescription":"iii, 20 p.","numberOfPages":"25","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":33126,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0412/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0412/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdfa9","contributors":{"authors":[{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":152078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":76867,"text":"wsp1498 - 1961 - Studies in flow in alluvial channels","interactions":[],"lastModifiedDate":"2012-02-02T00:14:18","indexId":"wsp1498","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":"1498","title":"Studies in flow in alluvial channels","language":"ENGLISH","doi":"10.3133/wsp1498","collaboration":"This water-supply paper was printed as seperate chapters","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Studies in flow in alluvial channels: U.S. Geological Survey Water Supply Paper 1498, Chapters A through I, https://doi.org/10.3133/wsp1498.","productDescription":"Chapters A through I","costCenters":[],"links":[{"id":194500,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1498/report-thumb.jpg"},{"id":91195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1498/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a128","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":534794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1510,"text":"wsp1707 - 1961 - Surface water supply of the United States 1960, Part 4, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1707","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":"1707","title":"Surface water supply of the United States 1960, Part 4, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1707","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States 1960, Part 4, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1707, x, 437 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1707.","productDescription":"x, 437 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":136950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1707/report-thumb.jpg"},{"id":26571,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1707/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69807d","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143784,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24836,"text":"ofr61172 - 1961 - Some aspects of the effect of urban and suburban development upon runoff","interactions":[],"lastModifiedDate":"2017-02-06T16:14:36","indexId":"ofr61172","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":"61-172","title":"Some aspects of the effect of urban and suburban development upon runoff","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr61172","issn":"0094-9140","usgsCitation":"Wiitala, S.W., 1961, Some aspects of the effect of urban and suburban development upon runoff: U.S. Geological Survey Open-File Report 61-172, iv, 20 p., https://doi.org/10.3133/ofr61172.","productDescription":"iv, 20 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":157008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e9499","contributors":{"authors":[{"text":"Wiitala, Sulo Werner","contributorId":20315,"corporation":false,"usgs":true,"family":"Wiitala","given":"Sulo","email":"","middleInitial":"Werner","affiliations":[],"preferred":false,"id":192656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3498,"text":"cir444 - 1961 - Availability of ground water in Lyon County, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:09:17","indexId":"cir444","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"444","title":"Availability of ground water in Lyon County, Minnesota","docAbstract":"<p>Lyon County is in southwestern Minnesota, about 150 miles southwest of Minneapolis and St. Paul The basement rocks in the area consist of granite and quartzite of Precambrian age. These materials are in turn overlain by shale and sandstone of Cretaceous age, glacial drift of Pleistocene age, and alluvium of Recent age. Ground water is available primarily from aquifers in Pleistocene and Cretaceous strata from depths ranging from 15 to 500 feet below the land surface.</p>\n<p>The county is divided into areas of ground-water availability based on the quality and quantity of ground water available from the different geologic units. The glacial drift which covers all of the area, yields very hard water from sands and gravels occurring in melt-water channel deposits or as small, isolated melt-water bodies. Wells in the drift commonly yield from 2 to 30 gpm (gallons per minute), but sustained yields of as much as 500 gpm are obtained in areas where thick melt-water channel deposits occur. Cretaceous strata underlie about two-thirds of the county and yield water from poorly consolidated sandstone, The water ranges in hardness from soft to very hard and is sometimes high in chloride content. Wells in Cretaceous strata commonly yield from 2 to 7 gpm; however, in areas where the sandstone is in contact with the underlying weathered granite, sustained yields of as much as 75 gpm are obtained. The geographic and stratigraphic distribution of the geologic units suggests that additional water supplies may be available from Pleistocene and Cretaceous strata in areas not yet fully explored.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir444","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation and the Marshall Municipal Utilities, Marshall, Minn.","usgsCitation":"Rodis, H.G., 1961, Availability of ground water in Lyon County, Minnesota: U.S. Geological Survey Circular 444, iii, 7 p., https://doi.org/10.3133/cir444.","productDescription":"iii, 7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":30508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0444/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0444/report-thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Lyon County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-96.0914,44.631],[-95.6023,44.6309],[-95.6028,44.5433],[-95.5938,44.5434],[-95.5921,44.1964],[-96.0628,44.1987],[-96.0788,44.1993],[-96.0747,44.5455],[-96.0932,44.5456],[-96.0914,44.631]]]},\"properties\":{\"name\":\"Lyon\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dcb0","contributors":{"authors":[{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2830,"text":"wsp1592A - 1961 - Resistance coefficients and velocity distribution smooth rectangular channel","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1592A","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":"1592","chapter":"A","title":"Resistance coefficients and velocity distribution smooth rectangular channel","docAbstract":"Measurements were made in a smooth rectangular channel to establish the effect of the side walls of the channel on velocity distribution and resistance to flow. The velocity distribution in the central region of a section normal to the channel followed the log arithmetic law. In the vicinity of each wall, at a point in the vertical which varied with distance from the wall, the slope of the vertical velocity curve reversed. The velocity distribution over the entire section has been defined in dimensionless terms. As well, the width-depth ratio for the wall region is expressed as a function of a similar ratio for the channel. \r\n\r\nThe variation of a resistance coefficient computed from the measurements is shown to be a function of the flow Reynolds number. The resistance coefficient, for the same Reynolds number, is slightly greater than for smooth pipe or a smooth channel of infinite width.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1592A","usgsCitation":"Tracy, H., and Lester, C., 1961, Resistance coefficients and velocity distribution smooth rectangular channel: U.S. Geological Survey Water Supply Paper 1592, iv, 18 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1592A.","productDescription":"iv, 18 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1592a/report-thumb.jpg"},{"id":29393,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1592a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ed2","contributors":{"authors":[{"text":"Tracy, Hubert J.","contributorId":25925,"corporation":false,"usgs":true,"family":"Tracy","given":"Hubert J.","affiliations":[],"preferred":false,"id":145868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lester, C.M.","contributorId":67497,"corporation":false,"usgs":true,"family":"Lester","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":145869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2165,"text":"wsp1522 - 1961 - Quality of surface waters of the United States, 1957, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1522","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":"1522","title":"Quality of surface waters of the United States, 1957, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1522","usgsCitation":"Love, S.K., 1961, Quality of surface waters of the United States, 1957, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1522, x, 494 p. :ill. ;25 cm., https://doi.org/10.3133/wsp1522.","productDescription":"x, 494 p. :ill. ;25 cm.","costCenters":[],"links":[{"id":138294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1522/report-thumb.jpg"},{"id":27776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1522/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c65","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52162,"text":"ofr6147 - 1961 - Availability of ground water near Pedernales, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"ofr6147","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":"61-47","title":"Availability of ground water near Pedernales, California","language":"ENGLISH","doi":"10.3133/ofr6147","usgsCitation":"Evenson, R.E., 1961, Availability of ground water near Pedernales, California: U.S. Geological Survey Open-File Report 61-47, 52 p., https://doi.org/10.3133/ofr6147.","productDescription":"52 p.","costCenters":[],"links":[{"id":178851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0047/report-thumb.jpg"},{"id":86674,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86675,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8a5","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":244894,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71755,"text":"tei800 - 1961 - Ground water test well A, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and construction","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei800","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"800","title":"Ground water test well A, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and construction","language":"ENGLISH","doi":"10.3133/tei800","usgsCitation":"Price, C., and Thordarson, W., 1961, Ground water test well A, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and construction: U.S. Geological Survey Trace Elements Investigations 800, 60 p., 4 fig. , https://doi.org/10.3133/tei800.","productDescription":"60 p., 4 fig. ","costCenters":[],"links":[{"id":191641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/800/report-thumb.jpg"},{"id":90983,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/800/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/800/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d703","contributors":{"authors":[{"text":"Price, C.E.","contributorId":19642,"corporation":false,"usgs":true,"family":"Price","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":284712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":284713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}