{"pageNumber":"1820","pageRowStart":"45475","pageSize":"25","recordCount":46618,"records":[{"id":70011497,"text":"70011497 - 1968 - Determination of palladium, platinum and rhodium in geologic materials by fire assay and emission spectrography","interactions":[],"lastModifiedDate":"2020-11-29T16:50:51.898381","indexId":"70011497","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Determination of palladium, platinum and rhodium in geologic materials by fire assay and emission spectrography","docAbstract":"<div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>A method is described for the determination of palladium down to 4ppb (parts per billion, 10<sup>9</sup>), platinum down to 10 ppb and rhodium down to 5 ppb in 15 g of sample. Fire-assay techniques are used to preconcentrate the platinum metals into a gold bead, then the bead is dissolved in<span>&nbsp;</span><i>aqua regia</i><span>&nbsp;</span>and diluted to volume with 1<i>M</i><span>&nbsp;</span>hydrochloric acid. The solution is analysed by optical emission spectrography of the residue from 200 μl of it evaporated on a pair of flat-top graphite electrodes. This method requires much less sample handling than most published methods for these elements. Data are presented for G-1, W-1, and six new standard rocks of the U.S. Geological Survey. The values for palladium in W-1 are in reasonable agreement with previously published data.</p></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0039-9140(68)80014-1","issn":"00399140","usgsCitation":"Hapfty, J., and Riley, L., 1968, Determination of palladium, platinum and rhodium in geologic materials by fire assay and emission spectrography: Talanta, v. 15, no. 1, p. 111-117, https://doi.org/10.1016/0039-9140(68)80014-1.","productDescription":"7 p.","startPage":"111","endPage":"117","numberOfPages":"7","costCenters":[],"links":[{"id":221174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ffbbe4b0c8380cd4f379","contributors":{"authors":[{"text":"Hapfty, J.","contributorId":33056,"corporation":false,"usgs":true,"family":"Hapfty","given":"J.","email":"","affiliations":[],"preferred":false,"id":361264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riley, L.B.","contributorId":15994,"corporation":false,"usgs":true,"family":"Riley","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":361263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70190818,"text":"70190818 - 1968 - Selected hydrologic data, San Pitch River drainage basin, Utah","interactions":[],"lastModifiedDate":"2017-09-14T17:03:21","indexId":"70190818","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"14","title":"Selected hydrologic data, San Pitch River drainage basin, Utah","docAbstract":"<p>The u.s. Geological Survey investigated the ground-water resources of the San Pitch River drainage basin during the period 1964- 67. The investigation was a cooperative project, financed equally by the Utah Department of Natural Resources, Division of Water Rights, and the Federal Government, and was a part of an investigation of the groundwater resources of the entire Sevier River drainage system.</p><p>This report is intended to serve two purposes: (1) To make available to the public basic water-resources data useful in planning and studying development of water resources and (2) to supplement an interpretive report that will be published later. Included in the release are data collected by the Geological Survey since 1930.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Robinson, G., 1968, Selected hydrologic data, San Pitch River drainage basin, Utah: Utah Basic-Data Release 14, 44 p.","productDescription":"44 p.","numberOfPages":"49","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345793,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-270&Title=Basic+Data+Report+14"}],"country":"United States","state":"Utah","otherGeospatial":"San Pitch River drainage basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb9538e4b091459a578210","contributors":{"authors":[{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":710545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16369,"text":"ofr68310 - 1968 - Alaska Railroad Terminal Reserve, Anchorage, soil-stability study: Stability in the vicinity of boring lines 1 and 2","interactions":[{"subject":{"id":16369,"text":"ofr68310 - 1968 - Alaska Railroad Terminal Reserve, Anchorage, soil-stability study: Stability in the vicinity of boring lines 1 and 2","indexId":"ofr68310","publicationYear":"1968","noYear":false,"title":"Alaska Railroad Terminal Reserve, Anchorage, soil-stability study: Stability in the vicinity of boring lines 1 and 2"},"predicate":"SUPERSEDED_BY","object":{"id":36081,"text":"b1258D - 1969 - Stability of the west slope of Government Hill Port area of Anchorage, Alaska","indexId":"b1258D","publicationYear":"1969","noYear":false,"chapter":"D","title":"Stability of the west slope of Government Hill Port area of Anchorage, Alaska"},"id":1}],"supersededBy":{"id":36081,"text":"b1258D - 1969 - Stability of the west slope of Government Hill Port area of Anchorage, Alaska","indexId":"b1258D","publicationYear":"1969","noYear":false,"title":"Stability of the west slope of Government Hill Port area of Anchorage, Alaska"},"lastModifiedDate":"2024-05-20T18:21:05.848196","indexId":"ofr68310","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","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":"68-310","title":"Alaska Railroad Terminal Reserve, Anchorage, soil-stability study: Stability in the vicinity of boring lines 1 and 2","docAbstract":"<p>This report has been prepared in response to a request dated April 22, 1966, from the General Manager of The Alaska Railroad to the Director, U.S. Geological Survey, for an evaluation of the propriety of continued industrial expansion on land contained within The Alaska Railroad Terminal Reserve and nearby. It is based on field examination June 8-12, 1966, in company with Messrs. E. B. Eckel and E. G. Dobrovolny, field work September 19-October 3, 1966, and May 1-June 4, 1967, on discussions with the staff of The Alaska Railroad, my colleagues, and Professor H. B. Seed of the University of California, and on review of published and unpublished material pertinent to the area and its problems.</p><p>During the fall of 1966 a detailed topographic map of the port area was prepared for The Alaska Railroad by Jay Whiteford and Associates. During late 1966 and early 1967 a drilling, sampling and soils testing program in an area of immediate interest along Boring Lines 1 and 2 was made by Adams, Corthell, Lee, Wince, and Associates (ACLW), a consultant engineering firm, under contract to The Alaska Railroad. Most of the basic data used in this report for stability analyses, such as the geometry of the ground surface and the physical properties of the materials, was derived from the Whiteford map and the ACLW investigations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr68310","usgsCitation":"Varnes, D., 1968, Alaska Railroad Terminal Reserve, Anchorage, soil-stability study: Stability in the vicinity of boring lines 1 and 2: U.S. Geological Survey Open-File Report 68-310, Report: 40 p.; 27 Plates: 69.58 x 24.31 inches or smaller, https://doi.org/10.3133/ofr68310.","productDescription":"Report: 40 p.; 27 Plates: 69.58 x 24.31 inches or smaller","costCenters":[],"links":[{"id":428909,"rank":30,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428908,"rank":29,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428907,"rank":28,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428906,"rank":27,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428905,"rank":26,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428904,"rank":25,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428903,"rank":24,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428902,"rank":23,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428901,"rank":22,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428900,"rank":21,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428899,"rank":20,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428898,"rank":19,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428897,"rank":18,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428896,"rank":17,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-22.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428895,"rank":16,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-23.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428894,"rank":15,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-24.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428893,"rank":14,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-25.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428892,"rank":13,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428891,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-31.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428890,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-32.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428889,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-33.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428888,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428887,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428886,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428885,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428884,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428883,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1968/0310/figure-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":428882,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0310/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420323,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8300.htm","linkFileType":{"id":5,"text":"html"}},{"id":147643,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0310/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Anchorage","otherGeospatial":"Alaska Railroad Terminal Reserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -149.85985198496206,\n              61.2552421724688\n            ],\n            [\n              -149.9056882101855,\n              61.25492604539252\n            ],\n            [\n              -149.90596324341948,\n              61.22157058885071\n            ],\n            [\n              -149.8589747366323,\n              61.2207348631986\n            ],\n            [\n              -149.85985198496206,\n              61.2552421724688\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688509","contributors":{"authors":[{"text":"Varnes, David J.","contributorId":86322,"corporation":false,"usgs":true,"family":"Varnes","given":"David J.","affiliations":[],"preferred":false,"id":172737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011532,"text":"70011532 - 1968 - Activity product constant of cryolite at 25°C and one atmosphere using selective-ion electrodes to estimate sodium and fluoride activities","interactions":[],"lastModifiedDate":"2015-06-15T12:24:32","indexId":"70011532","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Activity product constant of cryolite at 25°C and one atmosphere using selective-ion electrodes to estimate sodium and fluoride activities","docAbstract":"<p id=\"\">The activity product constant of cryolite (Na<sub>3</sub>AlF<sub>6</sub>) at 25&deg;C and 1 atm total pressure was calculated from data for solutions from which synthetic cryolite or mixtures of cryolite and a solid apparently related to ralstonite had precipitated. The activities of fluoride and of sodium were estimated using specific ion electrodes. The activity of Al<sup>3+</sup>&nbsp;was calculated from aluminum concentrations using equations which involve aluminum species existing in water solutions containing fluoride and hydroxide ions.</p>\n<p id=\"\">For the reaction&nbsp;<i>Na</i><sub>3</sub><i>AlF</i><sub>6</sub>(<i>c</i>) = 3<i>Na</i><sub>(<i>aq</i>)</sub><sup>+</sup>&nbsp;+&nbsp;<i>Al</i><sup>3+</sup><sub>(<i>aq</i>)</sub>&nbsp;+ 6<i>E</i><sup>-</sup><sub>(<i>aq</i>)</sub>&nbsp;the activity product constant K<sub>so</sub>&nbsp;is 10<sup>&minus;33.84</sup>, and the standard free energy of formation at 25&deg;C is -745.4&plusmn;1.0 kcal mole<sup>&minus;1</sup>. This latter is identical to a value from the literature which is based on calorimetric data.</p>\n<p id=\"\">Although cryolite and related minerals are easily precipitated in the laboratory, their relative scarcity in nature suggests that the effect of influences, perhaps solutes other than those occurring in the structure, may inhibit or prevent the formation of cryolite.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(68)90033-1","issn":"00167037","usgsCitation":"Roberson, C.E., and Hem, J., 1968, Activity product constant of cryolite at 25°C and one atmosphere using selective-ion electrodes to estimate sodium and fluoride activities: Geochimica et Cosmochimica Acta, v. 32, no. 12, p. 1343-1351, https://doi.org/10.1016/0016-7037(68)90033-1.","productDescription":"9 p.","startPage":"1343","endPage":"1351","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":221761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6d0e4b0c8380cd4764a","contributors":{"authors":[{"text":"Roberson, C. E.","contributorId":40190,"corporation":false,"usgs":true,"family":"Roberson","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":361337,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2345,"text":"wsp1859A - 1968 - Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","interactions":[{"subject":{"id":52612,"text":"ofr67164 - 1967 - Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","indexId":"ofr67164","publicationYear":"1967","noYear":false,"title":"Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California"},"predicate":"SUPERSEDED_BY","object":{"id":2345,"text":"wsp1859A - 1968 - Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","indexId":"wsp1859A","publicationYear":"1968","noYear":false,"chapter":"A","title":"Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California"},"id":1}],"lastModifiedDate":"2023-03-13T20:35:14.098526","indexId":"wsp1859A","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1968","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":"1859","chapter":"A","title":"Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California","docAbstract":"This is the third interpretive report prepared by the U.S. Geological Survey in cooperation with the Santa Barbara County Water Agency on the groundwater resources of areas along the south coast of the county. The two previous reports--one by J. E. Upson in 1951 and another by R. E. Evenson, H. D. Wilson, Jr., and K. S. Muir--were on ground-water conditions in the Goleta and Carpinteria basins. The Santa Barbara-Montecito area is between those two basins-the Goleta basin on the west and the Carpinteria basin on the east. This area of about 30 square miles extends from the Pacific Ocean on the south to the Santa Inez Mountains on the north. The city of Santa Barbara and the towns of Montecito and Summerland are within the area. \r\n\r\nThe Santa Barbara-Montecito area is a low-lying flat section of the coastal plain. Farther inland are highlands of consolidated rock and terrace deposits. The highlands are areas of uplift, folding, and faulting, and the lowlands are structural depressions. Most of the urban development in the area has been in the lowlands. The unconsolidated deposits that have partly filled the structural depressions make up the ground-water reservoir of the Santa Barbara-Montecito area. They include the Santa Barbara Formation of Pliocene and Pleistocene age, the Casitas Formation of Pleistocene age, and the alluvium of late Pleistocene and Recent age. These deposits underlie an area of about 20 square miles \r\nand have a maximum thickness of about 2,000 feet. The consolidated rocks of Tertiary age that underlie and form the boundaries of the ground-water reservoir contain ground water in fractures and in sandstone beds. However, the consolidated rocks are not an important source of ground water. \r\n\r\nIn 1959, a year the ground-water basins were full and ground water in storage was at a maximum, storage in the Santa Barbara area was 184,000 acre-feet, and storage in the Montecito area was 97,000 acre-feet. By 1964, in response to below-average recharge and continued withdrawal by pumping, the quantity of ground water in storage in the Santa Barbara area had decreased to 178,000 acre-feet. Because of a reduction in pumpage, there was little change in storage in the Montecito area between 1959 and 1964. \r\n\r\nDeep percolation of rain, seepage from streams, and subsurface inflow from consolidated rocks are the main sources of recharge to the ground-water reservoir in the Santa Barbara-Montecito area. The most important discharge is by pumping.The long-term perennial yield of the ground-water reservoir of the Santa Barbara area is estimated to be 1,700-2,000 acre-feet. Present data are insufficient to accurately determine the perennial yield of the reservoir in the Montecito area, but it is estimated to be about 2,500 acre-feet. \r\n\r\nMost ground water in the Santa Barbara-Montecito area is suitable for general use. However, ground water in some of the consolidated rocks and in the shallow unconsolidated deposits adjacent to the coast is too saline for most uses. Seawater intrusion has occurred in the Santa Barbara area and the western part of the Montecito area. The intrusion, however, is limited to the upper part of the nearshore shallow alluvial deposits and contaminates only wells which were constructed without a near-surface seal.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1859A","usgsCitation":"Muir, K.S., 1968, Ground-water reconnaissance of the Santa Barbara-Montecito area, Santa Barbara County, California: U.S. Geological Survey Water Supply Paper 1859, iv, 28 p., https://doi.org/10.3133/wsp1859A.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":137740,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859a/report-thumb.jpg"},{"id":28265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414045,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25079.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"Santa Barbara-Montecito area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.565,\n              34.483\n            ],\n            [\n              -119.77,\n              34.483\n            ],\n            [\n              -119.77,\n              34.397\n            ],\n            [\n              -119.565,\n              34.397\n            ],\n            [\n              -119.565,\n              34.483\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649dde","contributors":{"authors":[{"text":"Muir, K. S.","contributorId":53764,"corporation":false,"usgs":true,"family":"Muir","given":"K.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179724,"text":"70179724 - 1967 - Reconnaissance of the chemical quality of water in western Utah, Part I: Sink Valley area, drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area","interactions":[],"lastModifiedDate":"2017-09-06T17:26:00","indexId":"70179724","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9-I","title":"Reconnaissance of the chemical quality of water in western Utah, Part I: Sink Valley area, drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area","docAbstract":"<p>This report presents data collected during the first part of an investigation that was started in 1963 by the U.S. Geological Survey in cooperation with the Utah Geological and Mineralogical Survey. The investigation has the purpose of providing information about the chemical quality of water in western Utah that will help interested parties to evaluate the suitability of the water for various uses in a broad area of Utah where little information of this type previously has been available. The area studied includes the Sink Valley area, the drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area (fig. 1). Osamu Hattori and G. L. Hewitt started the investigation, and the author completed it and prepared the report.</p>","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, Utah","collaboration":"Prepared in cooperation with the Utah Geological and Mineralogical Survey","usgsCitation":"Waddell, K., 1967, Reconnaissance of the chemical quality of water in western Utah, Part I: Sink Valley area, drainage basins of Skull, Rush, and Government Creek Valleys, and the Dugway Valley-Old River Bed area: Utah Geological and Mineralogical Survey Water-Resources Bulletin 9-I, 15 p.","productDescription":"15 p.","numberOfPages":"23","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333203,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-9.pdf"},{"id":333206,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Dugway Valley-Old River Bed area, Government Creek Valley, Rush Valley, Sink Valley, Skull Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.49426269531249,\n              39.6268459848669\n            ],\n            [\n              -113.49426269531249,\n              41.04207384890103\n            ],\n            [\n              -112.401123046875,\n              41.04207384890103\n            ],\n            [\n              -112.401123046875,\n              39.6268459848669\n            ],\n            [\n              -113.49426269531249,\n              39.6268459848669\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d0","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":658438,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180004,"text":"70180004 - 1967 - Developing a state water plan: Ground-water conditions in Utah, spring of 1967","interactions":[],"lastModifiedDate":"2017-01-23T11:32:48","indexId":"70180004","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"5","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1967","docAbstract":"<p>This report is the fourth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.</p><p>This report, like the others (see references, p. 89), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. It also contains supplementary data that are related to ground-water use in some areas. In reports of this series, the inclusion of such supplementary data as graphs showing chemical quality of water and maps showing water-table configuration is intended only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1966. Water-level fluctuations, however, are described for the period spring 1966 to spring 1967. Many of the data used in the report were collected by the Geological Survey in cooperation with the Utah State Engineer.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Baker, C., Price, D., Butler, R., Mower, R.W., Herbert, L.R., Cordova, R., Bolke, E., Bjorklund, L., Robinson, G., and Sandberg, G.W., 1967, Developing a state water plan: Ground-water conditions in Utah, spring of 1967: Cooperative Investigations Report 5, 89 p.","productDescription":"89 p.","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333672,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333671,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-198"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b6b","contributors":{"authors":[{"text":"Baker, C.H. Jr.","contributorId":67526,"corporation":false,"usgs":true,"family":"Baker","given":"C.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":659690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":659691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659692,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659693,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659694,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659695,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659696,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659697,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":659698,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659699,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":71819,"text":"tei871 - 1967 - Hydrologic and chemical data for wells, springs, and streams in central Nevada, Tps. 1-21 N. and Rs. 41-57 E.","interactions":[],"lastModifiedDate":"2022-05-04T15:11:10.618014","indexId":"tei871","displayToPublicDate":"2013-07-18T08:54:00","publicationYear":"1967","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":"871","title":"Hydrologic and chemical data for wells, springs, and streams in central Nevada, Tps. 1-21 N. and Rs. 41-57 E.","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei871","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Robinson, B., Thordarson, W., and Beetem, W., 1967, Hydrologic and chemical data for wells, springs, and streams in central Nevada, Tps. 1-21 N. and Rs. 41-57 E.: U.S. Geological Survey Trace Elements Investigations 871, Report: 61 p.; 1 Map, https://doi.org/10.3133/tei871.","productDescription":"Report: 61 p.; 1 Map","costCenters":[],"links":[{"id":290413,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":400133,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0190/plate-1.pdf","size":"5,147 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":400132,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0190/report.pdf","size":"1,718 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.01,35.0 ], [ -120.01,42.0 ], [ -114.04,42.0 ], [ -114.04,35.0 ], [ -120.01,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd615ce4b0b290850fd7ad","contributors":{"authors":[{"text":"Robinson, B.P.","contributorId":7685,"corporation":false,"usgs":true,"family":"Robinson","given":"B.P.","email":"","affiliations":[],"preferred":false,"id":284804,"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":284805,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beetem, W. Arthur","contributorId":34831,"corporation":false,"usgs":true,"family":"Beetem","given":"W. Arthur","affiliations":[],"preferred":false,"id":284806,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038400,"text":"wdrCA662 - 1967 - Water Resources Data for California, 1966; Part 2: Water Quality Records","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA662","displayToPublicDate":"2012-05-13T13:58:00","publicationYear":"1967","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":"CA-66-2","title":"Water Resources Data for California, 1966; Part 2: Water Quality Records","docAbstract":"<p>Water-resources investigations of the U.S. Geological Survey include the collection of water-quality data on the chemical and physical characteristics of surface- and ground-water supplies of the Nation. These data for the 1966 water year for the quality of surface waters in California are presented in this report. Data for a few water-quality stations in bordering States are also included. The data were collected by the Water Resources Division of the U.S. Geological Survey under the direction of Walter Hofmann and R. Stanley Lord, successive district chiefs, Menlo Park, Calif.</p>\n<p>Water-quality information is presented for chemical quality, fluvial sediment, and water temperatures. The chemical quality includes concentrations of individual dissolved constituents and certain properties or characteristics such as hardness, sodium-adsorption ratio, specific conductance, and pH. Fluvial-sediment information is given for suspended-sediment discharges and concentrations and for particle-size distribution of suspended sediment and bed material. Water-temperature data represent once-daily observations except for stations where a continuous temperature recorder furnishes information from which daily minimums and maximums are obtained.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA662","usgsCitation":"U.S. Geological Survey, 1967, Water Resources Data for California, 1966; Part 2: Water Quality Records: U.S. Geological Survey Water Data Report CA-66-2, x, 461 p., https://doi.org/10.3133/wdrCA662.","productDescription":"x, 461 p.","costCenters":[],"links":[{"id":256926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/ca-66/WDR-1966-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc493e4b08c986b32b714"}
,{"id":70038399,"text":"wdrCA6612 - 1967 - Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA6612","displayToPublicDate":"2012-05-13T13:40:00","publicationYear":"1967","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":"CA-66-1-2","title":"Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within California are given in this report. For convenience, also included are records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann and R. Stanley Lord, successive district chiefs, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA6612","usgsCitation":"U.S. Geological Survey, 1967, Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-66-1-2, xvii, 514 p., https://doi.org/10.3133/wdrCA6612.","productDescription":"xvii, 514 p.","startPage":"483","endPage":"997","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":256929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256917,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/ca-66/WDR-1966-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Northern Great Basin;Central Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc492e4b08c986b32b70e"}
,{"id":70038398,"text":"wdrCA6611 - 1967 - Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Cenral Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA6611","displayToPublicDate":"2012-05-13T13:27:00","publicationYear":"1967","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":"CA-66-1-1","title":"Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Cenral Valley","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within California are given in this report. For convenience, also included are records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann and R. Stanley Lord, successive district chiefs, Menlo Park, Calif.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA6611","usgsCitation":"U.S. Geological Survey, 1967, Water Resources Data for California, 1966; Part 1: Surface Water Records; Volume 1: Colorado River Basin, Southern Great Basin, and Pacific Slope Basins excluding Cenral Valley: U.S. Geological Survey Water Data Report CA-66-1-1, xviii, 482 p., https://doi.org/10.3133/wdrCA6611.","productDescription":"xviii, 482 p.","startPage":"1","endPage":"482","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":256930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256916,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/ca-66/WDR-1966-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Colorado River Basin;Southern Great Basin;Pacific Slope Basins","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc491e4b08c986b32b708"}
,{"id":70038234,"text":"70038234 - 1967 - Hydrogeologic data for the Shetucket River basin, Connecticut","interactions":[],"lastModifiedDate":"2014-04-09T12:36:03","indexId":"70038234","displayToPublicDate":"2012-04-22T10:17:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"12","title":"Hydrogeologic data for the Shetucket River basin, Connecticut","docAbstract":"This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the Shetucket River basin of Connecticut in cooperation with the Connecticut Water Resources Commission. The Shetucket River basin occupies about 507 square miles in the eastern part of the State, including the towns of Andover, Ashford, Chaplin, Coventry, Mansfield, Scotland, Sprague, Windham, and Willington, and parts of Bolton, Canterbury, Columbia, Eastford, Ellington, Franklin, Lebanon, Lisbon, Hampton, Hebron, Norwich, Pomfret, Stafford, Tolland, Union, Vernon, and Woodstock. A companion interpretive report, Connecticut Water Resources Bulletin ll, (Thomas, and others, 1967), evaluates the water resources of the basin. The data on the following pages serve to document and supplement that report and should be especially useful in planning the development of water resources at specific localities.\nData were collected as part of this investigation during the period July\n1962 through December 1964. Streamflow records from continuous-record gaging\nstations in the basin for this period have been published annually along with data\nfrom other parts of the State in a series of U.S. Geological Survey reports\nentitled \"Surface Water Records of Connecticut.\" Water-level measurements in\nwells throughout the State from 1960 through 1964, including those made as part\nof this investigation, are published in Connecticut Water Resources Bulletin 7\n(Meikle and Baker, 1965). Most other data collected during this investigation\nare tabulated on the following pages. Included are some well records and chemical\nanalyses of water samples collected prior to July 1962 and not previously published.\nThe locations of sites at which data were collected are shown on\nplate A in the pocket at the back of the report. Plate A includes the\nlocations of 98 sites where 2 to 6 miscellaneous measurements of streamflow\nwere made during 1963 and 13 other sites where continuous records are\nmaintained. Data for these sites have already been published in \"Surface\nWater Records of Connecticut\" and are not repeated here.\nData presented~ unless otherwise noted, were collected by U.S.\nGeological Survey personnel.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Thomas, C.E., Bednar, G.A., Thomas, M.P., and Wilson, W.E., 1967, Hydrogeologic data for the Shetucket River basin, Connecticut: Connecticut Water Resources Bulletin 12, Report: 48 p.; 1 Plate: 33.28 x 56.69 inches.","productDescription":"Report: 48 p.; 1 Plate: 33.28 x 56.69 inches","numberOfPages":"54","costCenters":[],"links":[{"id":258793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0012/report.pdf","size":"1843","linkFileType":{"id":1,"text":"pdf"}},{"id":258794,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0012/report-thumb.jpg"},{"id":285974,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70038234/plate-a.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Shetucket River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.45,41.55 ], [ -72.45,42.066667 ], [ -72.016667,42.066667 ], [ -72.016667,41.55 ], [ -72.45,41.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b2e4b0c8380cd5f1bc","contributors":{"authors":[{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463700,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463698,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70038229,"text":"70038229 - 1967 - Water resources inventory of Connecticut Part 2: Shetucket River Basin","interactions":[],"lastModifiedDate":"2014-04-09T12:35:29","indexId":"70038229","displayToPublicDate":"2012-04-22T09:08:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"11","title":"Water resources inventory of Connecticut Part 2: Shetucket River Basin","docAbstract":"The Shetucket River basin has a relatively abundant supply of water of generally good quality which is derived from precipitation that has fallen on the basin. Annual precipitation has ranged from about 30 inches to 75 inches and has averaged about 45 inches over a 35-year period. Approximately 20 inches of water are returned to the atmosphere each year by evaporation and transpiration; the remainder of the annual precipitation either flows overland to streams or percolates downward to the water table and ultimately flows out of the basin in the Shetucket River or as underflow through the deposits beneath. During the autumn and winter months precipitation normally is sufficient to cause a substantial increase in the amount of water stored underground and in surface reservoirs within the basins whereas in the summer most of the precipitation is lost through evaporation and transpiration, resulting in sharply reduced streamflow and lowered groundwater levels. The mean monthly storage of water in the basin on an average is 3.5 inches higher in November than it is in June.\nThe amount of water that flows out of the\nbasin in the Shetucket River represents the total\namount of water potentlally available for use by man.\nAnnual runoff from the entire basin above the\nQuinebaug River has ranged from about 13 to 42\ninches since 1929, and has averaged about 23\ninches (300 billion gallons). Although runoff\nindicates the total amount of water potentially\navailable, it is usually not economically or\nlegally feasible for man to use all of it. On\nthe other hand, with increased development, It\nis possible that some water will be reused several\ntimes.\nThe water available may be tapped as it flows\nthrough the area or is temporarily stored in\nstreams, lakes, and aquifers. The amounts that\ncan be developed vary from place to place and\ntime to time, depending on the amount of precipitation,\non the size of drainage area, on the\nthickness, permeability and areal extent of aquifers,\nand on the variations in chemical and\nphysical quality of the water.\nDifferences in streamflow from point to\npoint are due primarily to differences in the\nproportion of stratified drift in the drainage\nbasin above each point, which affect the timing\nof streamflow, and to differences in precipitation,\nwhich affect the amount of streamflow.\nInformation on streamflow from gaging stations\nmay be extended to ungaged sites by accounting\nfor both of these factors ,in calculations.\nFuture floods on the upper Willimantic\nRiver or the Shetucket River are unlikely to\ncause major damage so long as buildings are not\nconstructed below the highest flood elevations to\nbe expected with the present system of reservoirs\nfor flood control.\nGround water can be obtained from wells\nalmost anywhere in the Shetucket River basin, but\nthe amount obtainable from individual wells at\nany particular point depends upon the type and\nwater-bearing properties of the aquifers present.\nFor practical purposes, the earth materials in\nthe basin comprise three aquifers--stratified\ndrift, till, and bedrock,\nStratified drift is the only aquifer generally capable of yielding more than 100 gpm to\nindividual wells. This aquifer covers about 18\npercent of the basin and occurs chiefly In lowlands\nwhere it overlies till or bedrock. Coefficient\nof permeability of the coarse-grained unit\nof stratified drift averages about 1,900 gpd per\nsq ft. Drilled, screened wells tapping this unit,\nare known to yield from 200 to 675 gpm. Dug wells\nin coarse-grained stratified drift should supply\nat least 2 gpm per foot of drawdown over an 8-hour\nperiod. Fine-grained stratified drift has an\naverage coefficient of permeability of about 400\ngpd per sq ft and can usually yield to dug wells\nsupplies sufficient for household use.\nTill and bedrock are widespread in extent but\ncan provide only small to moderate water supplies.\nTill is tapped chiefly by dug wells; permanent\nsupplies of more than 200 gpd can be obtained from\ndug wells at a majority of sites in areas of till,\nbut there are many sites where the till is too\nimpermeable or too thin to provide this much water\nthroughout the year. The coefficient of permeability of till ranges from about 0.2 gpd per sq ft to\n55 gpd per sq it. Bedrock Is tapped chiefly by\ndrilled wells, about 90 percent of which will\nsupply at least 3 gpm. Very few, however, will\nsupply more than 50 gpm.\nThe amount of ground water potentially available\nIn an area depends upon the amount of groundwater\noutflow, the amount of ground water in storage,\nand the quantity of water available by Induced\ninfiltration from streams and lakes. From\ndata on permeability, saturated thickness, recharge,\nyield from aquifer storage, well performance, and\nstreamflow, preliminary estimates of ground-water\navailability can be made for any point in the\nbasin. Long-term yields estimated for 15 areas\nespecially favorable for development of large\nground-water supplies ranged from 1.3 to 61.8 mgd.\nDetailed site studies to determine optimum yields,\ndrawdowns, and spacing of individual wells are\nneeded before major ground-water development is\nundertaken In these or other areas.\nThe chemical quality of water in the Shetucket\nbasin Is generally good to excellent. Samples of\nnaturally occurring surface water collected from\n32 sites contained less than 61 ppm of dissolved\nsolids and less than 32 ppm of hardness. Water\nfrom wells is more highly mineralized than naturally\noccurring water from streams. Even so only\n7 percent of wells sampled yielded water with more\nthan 200 ppm of dissolved sol-ids and only 9 percent\nyielded water with more than 120 ppm of hardness.\nEven in the major rivers, which are used to\ntransport industrial waste, the dissolved mineral\ncontent is less than 100 ppm and hardness rarely\nexceeds 40 ppm. One notable exception occurs in\nthe lower reaches of Little River where an\nexceptional amount of industrial waste is discharged\ninto the river near Versailles. This\nwaste is particularly noticeable during low\nstreamflow.\nIron and manganese In both ground water and\nsurface water are the only constituents whose concentrations\ncommonly exceed recommended limits for\ndomestic and industrial use. Most wells in the\n basin yield clear water with little or no iron or\nmanganese, but distributed among them are wells\nwith ground water that contains enough of these dissolved\nconstituents to be troublesome for most uses.\niron concentrations in naturally occurring\nstream water exceeded 0.3 ppm under tow-flow conditions\nat 20 percent of the sites sampled. Large\nconcentrations of iron in stream water result\nfrom discharge of iron-bearing ground water or\nfrom the discharge of water from swamps. In\nswamps the iron is released largely from decaying\nvegetation.\nGround water more than 30 feet below the\nland surface has a relatively constant temperature,\nusually between 48°F and 50°F. Water\ntemperature in very shallow wells may fluctuate\nfrom about 38°F in February or March to about\n55°F in late summer. Water temperature in the\nlarger streams fluctuates much more widely,\nranging from 32°F at least for brief periods\nin winter, to about 85°F occasionally during\nThe quantity of suspended sediment transported\nby streams in the basin is negligible,\nthough amounts large enough to be troublesome\nmay occur locally at times.\nThe total amount of water used In the\nShetucket Rlver basin for all purposes during\n1961 was about 5,810 million gallons~ which is\nequivalent to 208 gpd per person, Public water\nsystems supplied the domestic needs of nearly\nhalf the population of the basin; 10 systems\nwere sampled, all of which provided water of\nbetter quality than the U.S. Public Health Service\nsuggests for drinking water standards.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resource Commission","usgsCitation":"Thomas, M.P., Bednar, G.A., Thomas, C.E., and Wilson, W.E., 1967, Water resources inventory of Connecticut Part 2: Shetucket River Basin: Connecticut Water Resources Bulletin 11, Report: viii, 96 p.; 4 Plates: 36.00 x 58.00 inches and smaller.","productDescription":"Report: viii, 96 p.; 4 Plates: 36.00 x 58.00 inches and smaller","numberOfPages":"112","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0011/report.pdf","size":"22651","linkFileType":{"id":1,"text":"pdf"}},{"id":258792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0011/report-thumb.jpg"},{"id":285972,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-c.pdf"},{"id":285973,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-d.pdf"},{"id":285970,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-a.pdf"},{"id":285971,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038229/plate-b.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Shetucket River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.466667,41.533333 ], [ -72.466667,42.066667 ], [ -72.0,42.066667 ], [ -72.0,41.533333 ], [ -72.466667,41.533333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb78e4b08c986b32d681","contributors":{"authors":[{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bednar, Gene A.","contributorId":81881,"corporation":false,"usgs":true,"family":"Bednar","given":"Gene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463692,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463690,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463691,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70046324,"text":"wdrNM661 - 1967 - Water resources data for New Mexico, water year 1966; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:52:19","indexId":"wdrNM661","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1967","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":"NM-66-1","title":"Water resources data for New Mexico, water year 1966; Part 1. Surface water records","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of New Mexico are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of W. E. Hale, District Chief, Water Resources Division. This report is the sixth in a series presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951' there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in New Mexico were contained in Parts 7, 8, and 9 of that series. Beginning with the 1961 water year, streamflow records and related data have been released\nby the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. The records will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM661","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Water resources data for New Mexico, water year 1966; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-66-1, 268 p., https://doi.org/10.3133/wdrNM661.","productDescription":"268 p.","costCenters":[],"links":[{"id":273453,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274522,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/nm-66/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300e9e4b01368e589e418","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":535534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5230046,"text":"5230046 - 1967 - Retention of extra-wide, lock-on, and regular bands on waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:15:27","indexId":"5230046","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"108","title":"Retention of extra-wide, lock-on, and regular bands on waterfowl","docAbstract":"In tests of three types of bands -- extra-wide bands, lock-on bands, and regular U.S. Fish and Wildlife Service bands -- little difference was noted in the retention qualities of the three types on waterfowl.  Therefore, there appeared to be no advantage in using either the extra-wide or the lock-on type of band rather than the regular band now in use by waterfowl banders on this continent.  Waterfowl banded with two bands provided recovery data that were difficult to analyze but suggested that it might be worthwhile to identify banded birds with another type of mark and evaluate the retention of bands through subsequent recapture of the birds.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Martinson, R.K., and Henny, C.J., 1967, Retention of extra-wide, lock-on, and regular bands on waterfowl: Special Scientific Report  - Wildlife 108, iv, 19.","productDescription":"iv, 19","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":202687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":94681,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785114?urlappend=%3Bseq=5"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60450b","contributors":{"authors":[{"text":"Martinson, R. K.","contributorId":106983,"corporation":false,"usgs":true,"family":"Martinson","given":"R.","middleInitial":"K.","affiliations":[],"preferred":false,"id":343423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":343422,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52592,"text":"ofr67108 - 1967 - Progress report: Radionuclide transport in the Pasco to Vancouver, Washington, reach of the Columbia River, July 1962 to September 1963","interactions":[],"lastModifiedDate":"2018-12-04T14:39:59","indexId":"ofr67108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-108","title":"Progress report: Radionuclide transport in the Pasco to Vancouver, Washington, reach of the Columbia River, July 1962 to September 1963","docAbstract":"<p>The disposition of radionuclides in and along the 380-mile reach of the Columbia River between the Hanford, Wash., Atomic Energy Commission reactors (the major radionuclide source) and the head of the estuary is a first step in understanding the environmental cycling and ultimate fate of the discharged radioactive materials. Preliminary results for the study period, July 1962 to September 1963, are presented for radionuclide, sediment, and water data from stations on the Columbia River and from stations near the mouths of the Snake River, the Willamette River, and other Columbia River tributaries.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67108","usgsCitation":"Haushild, W.L., Perkins, R.W., Stevens, H.H., Dempster, G.R., and Glenn, J.L., 1967, Progress report: Radionuclide transport in the Pasco to Vancouver, Washington, reach of the Columbia River, July 1962 to September 1963: U.S. Geological Survey Open-File Report 67-108, xii, 188 p., https://doi.org/10.3133/ofr67108.","productDescription":"xii, 188 p.","costCenters":[],"links":[{"id":359941,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0108/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177670,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0108/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688313","contributors":{"authors":[{"text":"Haushild, William L.","contributorId":211057,"corporation":false,"usgs":true,"family":"Haushild","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":245600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, Richard W.","contributorId":211058,"corporation":false,"usgs":false,"family":"Perkins","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":245601,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stevens, Herbert H. Jr.","contributorId":211059,"corporation":false,"usgs":true,"family":"Stevens","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":245603,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dempster, George R. Jr.","contributorId":106975,"corporation":false,"usgs":true,"family":"Dempster","given":"George","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":245599,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Glenn, Jerry L.","contributorId":54969,"corporation":false,"usgs":true,"family":"Glenn","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":245602,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":52638,"text":"ofr67256 - 1967 - Hydrologic data, Russian River basin in vicinity of Ukiah, California, Floods of December 1955 and December 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"ofr67256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-256","title":"Hydrologic data, Russian River basin in vicinity of Ukiah, California, Floods of December 1955 and December 1964","language":"ENGLISH","doi":"10.3133/ofr67256","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Hydrologic data, Russian River basin in vicinity of Ukiah, California, Floods of December 1955 and December 1964: U.S. Geological Survey Open-File Report 67-256, 16 p., https://doi.org/10.3133/ofr67256.","productDescription":"16 p.","costCenters":[],"links":[{"id":178540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60717b","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":532150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68020,"text":"ha238 - 1967 - Floods on White Rock Creek at Dallas, Texas in 1962 and 1964","interactions":[{"subject":{"id":23192,"text":"ofr6336 - 1963 - Floods on White Rock Creek above White Rock Lake at Dallas, Texas","indexId":"ofr6336","publicationYear":"1963","noYear":false,"title":"Floods on White Rock Creek above White Rock Lake at Dallas, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":68020,"text":"ha238 - 1967 - Floods on White Rock Creek at Dallas, Texas in 1962 and 1964","indexId":"ha238","publicationYear":"1967","noYear":false,"title":"Floods on White Rock Creek at Dallas, Texas in 1962 and 1964"},"id":1}],"lastModifiedDate":"2017-06-14T14:10:01","indexId":"ha238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"238","title":"Floods on White Rock Creek at Dallas, Texas in 1962 and 1964","docAbstract":"<p>This atlas presents data pertaining to the regimen of flooding along White Rock Creek and its tributaries, Spanky Branch, Floyd Branch, and Cottonwood Creek at Dallas, Texas. The map and flood data were prepared to aid those concerned with, and responsible for, the safe and yet extensive use of the floodplain along White Rock Creek and its tributaries. The flood map is shown in two parts&mdash;A, north half, and B, south half.</p>\n<p>The map shows areas inundated by the flood of September 21, 1964, along White Rock Creek and Spanky Branch and by the flood of October 8, 1962, along Cottonwood Creek and Floyd Branch.</p>\n<p>The flood of September 21, 1964, is known to be the greatest since at least 1886 on White Rock Creek upstream from the Texas and Pacific Railroad (mile 6.6). Downstream from the Texas and Pacific Railroad, White Rock Creek has been subject to inundation from backwater from the Trinity River. The greatest known flood on Trinity River occurred May 25, 1908. Because of extensive flood-control works built since 1908 in the upper Trinity River basin, the degree of flooding resulting from a storm of the magnitude of the 1908 catastrophe probably would be substantially different today. No backwater from Trinity River occurred during the flood of September 21, 1964.</p>\n<p>The greatest flood since at least 1892 on Cottonwood Creek and Floyd Branch occurred June 14, 1949. The storm of October 8, 1962, caused flood heights at Forest Lane to be comparable to those of June 14, 1949, on Cottonwood Creek and about 1 foot lower on Floyd Branch. The greatest flood since at least 1917 on Spanky Branch was that of September 21, 1964. Greater floods than those delineated are possible.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha238","collaboration":"Prepared in cooperation with the City of Dallas","usgsCitation":"Ruggles, F.H., and Gilbert, C.R., 1967, Floods on White Rock Creek at Dallas, Texas in 1962 and 1964: U.S. Geological Survey Hydrologic Atlas 238, 36.5 x 51.0 inches, https://doi.org/10.3133/ha238.","productDescription":"36.5 x 51.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326594,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha238.JPG"},{"id":89268,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/238/plate-1.pdf","text":"Plate 1","size":"8.21 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"scale":"24000","country":"United States","state":"Texas","city":"Dallas","otherGeospatial":"White Rock Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.83333333333333,32.700833333333335 ], [ -96.83333333333333,33 ], [ -96.70083333333334,33 ], [ -96.70083333333334,32.700833333333335 ], [ -96.83333333333333,32.700833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df796","contributors":{"authors":[{"text":"Ruggles, F. H.","contributorId":105805,"corporation":false,"usgs":true,"family":"Ruggles","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilbert, Carter R.","contributorId":7667,"corporation":false,"usgs":true,"family":"Gilbert","given":"Carter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":277515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32630,"text":"pp579 - 1967 - The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data","interactions":[],"lastModifiedDate":"2021-10-27T18:21:00.771926","indexId":"pp579","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"579","title":"The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp579","usgsCitation":"Brown, R.D., Vedder, J.G., Wallace, R.E., Roth, E.F., Yerkes, R.F., Castle, R.O., Waananen, A., Page, R.W., and Eaton, J.P., 1967, The Parkfield-Cholame, California, earthquakes of June–August 1966— Surface geologic effects water-resources aspects, and preliminary seismic data: U.S. Geological Survey Professional Paper 579, 66 p., https://doi.org/10.3133/pp579.","productDescription":"66 p.","costCenters":[],"links":[{"id":391020,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4623.htm"},{"id":119203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0579/report-thumb.jpg"},{"id":60504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0579/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.5,\n              35.6667\n            ],\n            [\n              -120.25,\n              35.6667\n            ],\n            [\n              -120.25,\n              36\n            ],\n            [\n              -120.5,\n              36\n            ],\n            [\n              -120.5,\n              35.6667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeb3","contributors":{"authors":[{"text":"Brown, Robert David Jr.","contributorId":18382,"corporation":false,"usgs":true,"family":"Brown","given":"Robert","suffix":"Jr.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":208823,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":208827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":208821,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roth, E. F.","contributorId":6056,"corporation":false,"usgs":true,"family":"Roth","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":208820,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":208824,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Castle, R. O.","contributorId":79880,"corporation":false,"usgs":true,"family":"Castle","given":"R.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":208825,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Waananen, A. O.","contributorId":87121,"corporation":false,"usgs":true,"family":"Waananen","given":"A. O.","affiliations":[],"preferred":false,"id":208826,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":208822,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":208828,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":2329,"text":"wsp1819K - 1967 - Correlation and analysis of water-temperature data for Oregon streams","interactions":[{"subject":{"id":52485,"text":"ofr65112 - 1965 - Correlation and analysis of water-temperature data for Oregon streams","indexId":"ofr65112","publicationYear":"1965","noYear":false,"title":"Correlation and analysis of water-temperature data for Oregon streams"},"predicate":"SUPERSEDED_BY","object":{"id":2329,"text":"wsp1819K - 1967 - Correlation and analysis of water-temperature data for Oregon streams","indexId":"wsp1819K","publicationYear":"1967","noYear":false,"chapter":"K","title":"Correlation and analysis of water-temperature data for Oregon streams"},"id":1}],"lastModifiedDate":"2017-02-03T13:42:02","indexId":"wsp1819K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1819","chapter":"K","title":"Correlation and analysis of water-temperature data for Oregon streams","language":"ENGLISH","publisher":"U.S. Govt. Print. Office,","doi":"10.3133/wsp1819K","usgsCitation":"Moore, A., 1967, Correlation and analysis of water-temperature data for Oregon streams: U.S. Geological Survey Water Supply Paper 1819, iv, 53 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1819K.","productDescription":"iv, 53 p. :ill. ;23 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":137616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819k/report-thumb.jpg"},{"id":28172,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684749","contributors":{"authors":[{"text":"Moore, A.M.","contributorId":87909,"corporation":false,"usgs":true,"family":"Moore","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":145021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52563,"text":"ofr6723 - 1967 - Historic surface faulting in continental United States and adjacent parts of Mexico","interactions":[],"lastModifiedDate":"2026-01-21T17:05:14.535821","indexId":"ofr6723","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-23","title":"Historic surface faulting in continental United States and adjacent parts of Mexico","docAbstract":"This report summarizes geometric aspects of approximately 35 instances of historic faulting of the ground surface in the continental United States and adjacent parts of Mexico. This information is of immediate importance in the selection and evaluation of sites for vital structures such as nuclear power plants. The data are presented in a table and graphs which show the quantitative relations between various aspects of the faulting. Certain items in the table that are uncertain, poorly known, or not in the published literature are briefly described in the text.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr6723","collaboration":"This open-file report is preliminary and has not been edited or reviewed for conformity with Geological Survey Standards","usgsCitation":"Bonilla, M.G., 1967, Historic surface faulting in continental United States and adjacent parts of Mexico: U.S. Geological Survey Open-File Report 67-23, Report: iii, 36 p.; 1 Sheet, https://doi.org/10.3133/ofr6723.","productDescription":"Report: iii, 36 p.; 1 Sheet","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":174699,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"Mexico, United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,25 ], [ -125.1,49.5 ], [ -65,49.5 ], [ -65,25 ], [ -125.1,25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62edb7","contributors":{"authors":[{"text":"Bonilla, M. G.","contributorId":33698,"corporation":false,"usgs":true,"family":"Bonilla","given":"M.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":245553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52565,"text":"ofr6738 - 1967 - Preliminary report on Bureau of Mines Yellow Creek core hole No. 1, Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr6738","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-38","title":"Preliminary report on Bureau of Mines Yellow Creek core hole No. 1, Rio Blanco County, Colorado","docAbstract":"Analysis of geologic, hydrologic , and geophysical data obtained in and around Yellow Creek core hole No. 1, Rio Blanco County, Colorado, indicate a 1,615-foot section of oil shale was penetrated by the hole. Geophysical log data indicate the presence of 25 gallons per ton shale for a thickness of 500 feet my be marginal. The richest section of oil shale is indicated to be centered around a depth of 2,260 feet. Within the oil shale the interval 1,182 to 1,737 feet is indicated to be relatively structurally incompetent and probably permeable. Extension of available regional hydrologic data indicate the oil shale section is probably water bearing and may yield as much as 1,000 gallons per minute. Hydrologic testing in the hole is recommended.","language":"ENGLISH","doi":"10.3133/ofr6738","usgsCitation":"Carroll, R.D., Coffin, D., Ege, J., and Welder, F., 1967, Preliminary report on Bureau of Mines Yellow Creek core hole No. 1, Rio Blanco County, Colorado: U.S. Geological Survey Open-File Report 67-38, 36 p., https://doi.org/10.3133/ofr6738.","productDescription":"36 p.","costCenters":[],"links":[{"id":177319,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0038/report-thumb.jpg"},{"id":86959,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86956,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0038/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86957,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0038/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86958,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0038/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cbb1","contributors":{"authors":[{"text":"Carroll, R. D.","contributorId":53373,"corporation":false,"usgs":true,"family":"Carroll","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":245556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coffin, D.L.","contributorId":91143,"corporation":false,"usgs":true,"family":"Coffin","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":245557,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ege, J. R.","contributorId":106117,"corporation":false,"usgs":false,"family":"Ege","given":"J. R.","affiliations":[],"preferred":false,"id":245559,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Welder, F.A.","contributorId":104878,"corporation":false,"usgs":true,"family":"Welder","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":245558,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":52585,"text":"ofr6793 - 1967 - Kansas River, Bonner Springs to mouth - Degradation of channel","interactions":[],"lastModifiedDate":"2018-11-07T14:34:47","indexId":"ofr6793","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-93","title":"Kansas River, Bonner Springs to mouth - Degradation of channel","docAbstract":"<p>This report has been prepared at the request of the Kansas Water Resources Board under provisions of a cooperative agreement with the U.S. Geological Survey dated July 1, 1966, for water-resources investigations. </p><p>The Kansas Water Resources Board has been advised of a recent serious degradation of the low-water channel of the lower Kansas River below Bonner Springs and has requested information on the following: (1) magnitude of change in regimen of the stream, (2) causes for the change including sand removal, change in sediment load, or change in the regimen of the Missouri River downstream, and (3) future change. </p><p>The requested information, presented herein, is based on the streamflow, stage, and sediment data collected by the U.S. Geological Survey; stage, sediment, and profile data collected by the U.S. Corps of Engineers; and sand removal data provided by the State of Kansas. -Photographs of the reach are shown in plates 1 and 2, and locations of the various features are shown in figure 1.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6793","usgsCitation":"Furness, L., Albert, C., and Leonard, R.B., 1967, Kansas River, Bonner Springs to mouth - Degradation of channel: U.S. Geological Survey Open-File Report 67-93, 18 p., https://doi.org/10.3133/ofr6793.","productDescription":"18 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":177586,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0093/report-thumb.jpg"},{"id":359283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","otherGeospatial":"Kansas River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.88719940185547,\n              39.0421195689398\n            ],\n            [\n              -94.60739135742188,\n              39.0421195689398\n            ],\n            [\n              -94.60739135742188,\n              39.118341154165186\n            ],\n            [\n              -94.88719940185547,\n              39.118341154165186\n            ],\n            [\n              -94.88719940185547,\n              39.0421195689398\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b486c","contributors":{"authors":[{"text":"Furness, L.W.","contributorId":16908,"corporation":false,"usgs":true,"family":"Furness","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":245586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albert, C.D.","contributorId":23923,"corporation":false,"usgs":true,"family":"Albert","given":"C.D.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":245587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leonard, R. B.","contributorId":32917,"corporation":false,"usgs":true,"family":"Leonard","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":245588,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52610,"text":"ofr67160 - 1967 - Delaware River basin - water data stations, 1967","interactions":[],"lastModifiedDate":"2017-06-21T10:19:32","indexId":"ofr67160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-160","title":"Delaware River basin - water data stations, 1967","docAbstract":"<p>This report presents information on station-type activities for acquiring surface-water, ground-water, and quality of water data in the Delaware River basin. The information was collected in 1966 through field offices of the Water Resources Division, U.S. Geological Survey as part of a pilot study for the Office of Water Data Coordination. </p><p>The cooperation and assistance of various Federal, state, and local agencies (table 1) whose activities are listed is acknowledged with appreciation. No attempt was made during the pilot study to inventory data collected by private industries, but information was available for a number of them. This information is included in the report as an example of the extensive data-collection effort by private groups in the Delaware River basin.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67160","collaboration":"Prepared in cooperation with 31 Federal, state, and local agencies","usgsCitation":"Moody, D., and Shaefer, F., 1967, Delaware River basin - water data stations, 1967: U.S. Geological Survey Open-File Report 67-160, Report: viii, 24 p.; Plate: 15.69 x 33.62 inches, https://doi.org/10.3133/ofr67160.","productDescription":"Report: viii, 24 p.; Plate: 15.69 x 33.62 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":177221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":337184,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0160/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":337185,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0160/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Delaware, Maryland, New Jersey, New York, Pennsylvania","otherGeospatial":"Delaware River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.5,\n              38.5\n            ],\n            [\n              -74,\n              38.5\n            ],\n            [\n              -74,\n              42.5\n            ],\n            [\n              -76.5,\n              42.5\n            ],\n            [\n              -76.5,\n              38.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db67242b","contributors":{"authors":[{"text":"Moody, D.W.","contributorId":54642,"corporation":false,"usgs":true,"family":"Moody","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":245638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaefer, F.L.","contributorId":91169,"corporation":false,"usgs":true,"family":"Shaefer","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":245639,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4701,"text":"twri07A - 1967 - Instructions for using the punchcard system for the storage and retrieval of ground-water data.  (NOTE: This publication is no longer maintained, USGS Library still has a copy)","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri07A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"7","chapter":"A","title":"Instructions for using the punchcard system for the storage and retrieval of ground-water data.  (NOTE: This publication is no longer maintained, USGS Library still has a copy)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/twri07A","issn":"0565-596X","usgsCitation":"Lang, S.M., and Leonard, A.R., 1967, Instructions for using the punchcard system for the storage and retrieval of ground-water data.  (NOTE: This publication is no longer maintained, USGS Library still has a copy) (1967): U.S. Geological Survey Techniques of Water-Resources Investigations 7, 1 v. (various pagings) :ill. ;26 cm. - No longer maintained, Library holds a copy, https://doi.org/10.3133/twri07A.","productDescription":"1 v. (various pagings) :ill. ;26 cm. - No longer maintained, Library holds a copy","costCenters":[],"links":[{"id":139126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"1967","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e58fc","contributors":{"authors":[{"text":"Lang, Solomon Max","contributorId":17471,"corporation":false,"usgs":true,"family":"Lang","given":"Solomon","email":"","middleInitial":"Max","affiliations":[],"preferred":false,"id":149643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, Alvin Riley","contributorId":102048,"corporation":false,"usgs":true,"family":"Leonard","given":"Alvin","email":"","middleInitial":"Riley","affiliations":[],"preferred":false,"id":149644,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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