{"pageNumber":"625","pageRowStart":"15600","pageSize":"25","recordCount":16495,"records":[{"id":2262,"text":"wsp1839N - 1967 - Hydrologic data for the Oak Ridge area, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1839N","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":"1839","chapter":"N","title":"Hydrologic data for the Oak Ridge area, Tennessee","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1839N","usgsCitation":"McMaster, W.M., 1967, Hydrologic data for the Oak Ridge area, Tennessee: U.S. Geological Survey Water Supply Paper 1839, v, 60 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1839N.","productDescription":"v, 60 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839n/report-thumb.jpg"},{"id":28053,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db608318","contributors":{"authors":[{"text":"McMaster, William M.","contributorId":13597,"corporation":false,"usgs":true,"family":"McMaster","given":"William","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":144914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1204,"text":"wsp1828 - 1967 - Geology and hydrology between Lake McMillan and Carlsbad Springs, Eddy County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1828","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":"1828","title":"Geology and hydrology between Lake McMillan and Carlsbad Springs, Eddy County, New Mexico","docAbstract":"The hydrology of the Pecos River valley between Lake McMillan and Carlsbad Springs, Eddy County, N. Mex., is influenced by facies changes in rocks of Permian age. Water stored for irrigation leaks from Lake McMillan into evaporite rocks, principally gypsum, of the Seven Rivers Formation and from Lake Avalon into carbonate rocks of the Tansill Formation. This leakage returns to the Pecos River at Major Johnson Springs and Carlsbad Springs. The river has perennial flow between Major Johnson Springs and Lake Avalon, but it loses water into evaporite rocks of the Yates Formation in this reach. Ground-water movement is generally toward the Pecos River in aquifers in the Pecos River valley except in the Rustler Formation east of the river where it moves southeastward toward playas east of Lake Avalon. \r\n\r\nThe chloride content of ground and surface waters indicates that surface water moves from some reaches of the Pecos River and from surface-storage reservoirs to aquifers and also indicates the degree of mixing of ground and surface waters. \r\n\r\nAbout 45,000 acre-feet of ground water is stored in highly permeable rocks in a 3-mile wide part of the Seven Rivers Formation between Lake McMillan and Major Johnson Springs. This water in storage comes from leakage from Lake McMillan and from alluvium north of the springs. The flow of Major Johnson Springs is derived from this aquifer. That part of the flow derived from the alluvium north of the springs averaged 13 cfs (cubic feet per second) from 1953 through 1959 ; about 8 cfs of this flow had not been previously measured at gaging stations on the Pecos River and its tributaries. \r\n\r\nThe most favorable plans for increasing terminal storage of the Carlsbad Irrigation District are to construct a dam at the Brantley site (at the downstream end of Major Johnson Springs), or to use underground storage in the permeable Seven Rivers Formation between Lake McMillan and Major Johnson brings in conjunction with surface storage. To avoid excessive leakage from a reservoir at the Brantley site, the dam should be downstream from all sprints in the Major Johnson Springs area but upstream from a point where the river begin losing water to the Yates Formation.","language":"ENGLISH","publisher":"U.S. Govt Print. Off.,","doi":"10.3133/wsp1828","usgsCitation":"Cox, E.R., 1967, Geology and hydrology between Lake McMillan and Carlsbad Springs, Eddy County, New Mexico: U.S. Geological Survey Water Supply Paper 1828, iv, 48 p. :illus., maps (6 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1828.","productDescription":"iv, 48 p. :illus., maps (6 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":138044,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1828/report-thumb.jpg"},{"id":246981,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1828/plate-1.pdf","size":"1092","linkFileType":{"id":1,"text":"pdf"}},{"id":246982,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1828/plate-2.pdf","size":"5458","linkFileType":{"id":1,"text":"pdf"}},{"id":246983,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1828/plate-3.pdf","size":"6241","linkFileType":{"id":1,"text":"pdf"}},{"id":246984,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1828/plate-4.pdf","size":"1900","linkFileType":{"id":1,"text":"pdf"}},{"id":246985,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1828/plate-5.pdf","size":"1891","linkFileType":{"id":1,"text":"pdf"}},{"id":246986,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1828/plate-6.pdf","size":"1285","linkFileType":{"id":1,"text":"pdf"}},{"id":26084,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1828/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db656d40","contributors":{"authors":[{"text":"Cox, Edward Riley","contributorId":40966,"corporation":false,"usgs":true,"family":"Cox","given":"Edward","email":"","middleInitial":"Riley","affiliations":[],"preferred":false,"id":143362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3607,"text":"cir536 - 1967 - Are we running out of water?","interactions":[],"lastModifiedDate":"2017-08-27T17:54:58","indexId":"cir536","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"536","title":"Are we running out of water?","docAbstract":"Water supplies are not running out, but time is getting short to stem waste of water and destructive exploitation of the environment before harm is done that may be irreparable. Most of the world's water is oceanic brine. Of the waters on the land, most is frozen in Antarctica and Greenland. Only a small part of continental water is available for use and management. The discharge of rivers to the sea is a close measure of the availability of liquid water, but ground-water reservoirs have important functions as inexpensive equalizers of water supply. Soil moisture is a major factor in the water economy, and its function usually is overlooked in assessments of water use and future water demand. Despite outcries of water shortage, the principal use of water in advanced countries is as a medium for waste disposal. In reality, despite regional maldistribution of water, United States supplies are adequate, given rational management. Also, contrary to common belief, water pollution is primarily a problem of economics, not of health. A paramount problem in most parts of the world is the shortage of water development and management facilities, not a shortage of water. The International Hydrological Decade is a program to awaken people everywhere to the crucial importance of water in man's future and to promote rational approach to water problems.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir536","usgsCitation":"Nace, R.L., 1967, Are we running out of water?: U.S. Geological Survey Circular 536, 7 p. :ill. ;26 cm., https://doi.org/10.3133/cir536.","productDescription":"7 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":138954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1967/0536/report-thumb.jpg"},{"id":30642,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1967/0536/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db674d4e","contributors":{"authors":[{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15273,"text":"ofr67173 - 1967 - Some engineering geology problems at Mammoth Cave National Park, Kentucky","interactions":[],"lastModifiedDate":"2020-10-05T14:27:31.276653","indexId":"ofr67173","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":"67-173","title":"Some engineering geology problems at Mammoth Cave National Park, Kentucky","docAbstract":"<p><span>The U.S. Geological Survey, at the request of the rational Park </span><span>Service, participated in a field symposium May </span><span>22-26, </span><span>1967, at Mammoth </span><span>Cave National Park, Kentucky. This symposium, held by the National </span><span>Park Service, was to determine the applicability of the Wilderness </span><span>Act </span><span>of </span><span>1964 to underground and surface portions of the Park (W. Drew </span><span>Chick, Jr., written communication, 1967). Scientific evidence bearing </span><span>on the relationships between human surface activities and natural </span><span>underground openings was examined and discussed at the symposium. </span><span>This report discusses relations between various types of surface </span><span>activities and physical damage to the cave openings and features. </span><span>Additional interpretive material </span><span>is </span><span>taken from the literature and from </span><span>limited laboratory information. Possible hydrologic and biologic </span><span>effects are not considered here, </span><span>but </span><span>were investigated by other </span><span>members of the symposium. Hydrologic effects are discussed in </span><span>companion report by Robert V. Cushman of the Geological Survey. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67173","usgsCitation":"Osterwald, F.W., 1967, Some engineering geology problems at Mammoth Cave National Park, Kentucky: U.S. Geological Survey Open-File Report 67-173, ii, 29 p., https://doi.org/10.3133/ofr67173.","productDescription":"ii, 29 p.","costCenters":[],"links":[{"id":379039,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0173/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0173/report-thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Mammoth Cave National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.18877410888672,\n              37.13322424999132\n            ],\n            [\n              -86.02809906005858,\n              37.13322424999132\n            ],\n            [\n              -86.02809906005858,\n              37.229781671757344\n            ],\n            [\n              -86.18877410888672,\n              37.229781671757344\n            ],\n            [\n              -86.18877410888672,\n              37.13322424999132\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e91df","contributors":{"authors":[{"text":"Osterwald, Frank W.","contributorId":98301,"corporation":false,"usgs":true,"family":"Osterwald","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52647,"text":"ofr67276 - 1967 - Electric analog model study of the hydrology of the Saginaw Formation in the Lansing, Michigan, area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"ofr67276","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":"67-276","title":"Electric analog model study of the hydrology of the Saginaw Formation in the Lansing, Michigan, area","language":"ENGLISH","doi":"10.3133/ofr67276","usgsCitation":"Wheeler, M., 1967, Electric analog model study of the hydrology of the Saginaw Formation in the Lansing, Michigan, area: U.S. Geological Survey Open-File Report 67-276, 70 p., https://doi.org/10.3133/ofr67276.","productDescription":"70 p.","costCenters":[],"links":[{"id":178647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60edd5","contributors":{"authors":[{"text":"Wheeler, Merlin","contributorId":94736,"corporation":false,"usgs":true,"family":"Wheeler","given":"Merlin","email":"","affiliations":[],"preferred":false,"id":245699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68598,"text":"ha248 - 1967 - Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania","interactions":[{"subject":{"id":52522,"text":"ofr662 - 1966 - Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania","indexId":"ofr662","publicationYear":"1966","noYear":false,"title":"Extent and frequency of inundation of Schuylkill River flood plain from Conshohocken to Philadelphia, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":68598,"text":"ha248 - 1967 - Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania","indexId":"ha248","publicationYear":"1967","noYear":false,"title":"Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania"},"id":1}],"lastModifiedDate":"2022-12-05T20:27:40.654787","indexId":"ha248","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":"248","title":"Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha248","usgsCitation":"Alter, A.T., 1967, Floods on Schuylkill River from Conshohocken to Philadelphia, Pennsylvania: U.S. Geological Survey Hydrologic Atlas 248, 1 Plate: 28.00 × 53.00 inches, https://doi.org/10.3133/ha248.","productDescription":"1 Plate: 28.00 × 53.00 inches","costCenters":[],"links":[{"id":90259,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":190107,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410059,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15614.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"16000","country":"United States","state":"Pennsylvania","city":"Conshocken, Philadelphia","otherGeospatial":"Schuylkill River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.329,\n              40.083\n            ],\n            [\n              -75.329,\n              40\n            ],\n            [\n              -75.183,\n              40\n            ],\n            [\n              -75.183,\n              40.083\n            ],\n            [\n              -75.329,\n              40.083\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df801","contributors":{"authors":[{"text":"Alter, A. T.","contributorId":60711,"corporation":false,"usgs":true,"family":"Alter","given":"A.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":278549,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68194,"text":"ha237 - 1967 - Water resources of the Two Rivers Watershed, Northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:03:34","indexId":"ha237","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":"237","title":"Water resources of the Two Rivers Watershed, Northwestern Minnesota","docAbstract":"<p>The Two Rivers watershed includes two physiographic areas a lake plain and a till plain &ndash; within its 1,232 square miles.</p>\n<p>It lies in parts of Kittson and Roseau counties and includes the drainage basins of the Two Rivers and Joe River. The flat lake plain which extends 15 to 20 miles east of the Red River of the North is extensively cultivated for small grains and sugar beets. The gently undulating till plain is cultivated largely for small grains and hay. The areas not under cultivation support a forest of poplar with some maple and oak. Oak is the predominate tree on the sandy ridges. The large peat areas are covered with brush and marsh grasslands. Outdoor recreational facilities in the watershed consist principally of the Lake Bronson Park, water-fowl hunting in the extensive marshlands, and deer and small game hunting in the forested areas.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha237","collaboration":"Prepared in cooperation with the Minnesota Department of Conservation, Division of Waters","usgsCitation":"Maclay, R., Winter, T.C., and Pike, G., 1967, Water resources of the Two Rivers Watershed, Northwestern Minnesota: U.S. Geological Survey Hydrologic Atlas 237, 8 Plates: 40 x 40 inches or smaller, https://doi.org/10.3133/ha237.","productDescription":"8 Plates: 40 x 40 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":68429,"text":"ha246 - 1967 - Floods at Easton, Pennsylvania-Phillipsburg, New Jersey","interactions":[{"subject":{"id":52464,"text":"ofr6557 - 1965 - Extent and frequency of floods in the vicinity of Easton, Pennsylvania-Phillipsburg, New Jersey","indexId":"ofr6557","publicationYear":"1965","noYear":false,"title":"Extent and frequency of floods in the vicinity of Easton, Pennsylvania-Phillipsburg, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":68429,"text":"ha246 - 1967 - Floods at Easton, Pennsylvania-Phillipsburg, New Jersey","indexId":"ha246","publicationYear":"1967","noYear":false,"title":"Floods at Easton, Pennsylvania-Phillipsburg, New Jersey"},"id":1}],"lastModifiedDate":"2023-03-07T22:04:51.913637","indexId":"ha246","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":"246","title":"Floods at Easton, Pennsylvania-Phillipsburg, New Jersey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha246","usgsCitation":"Farlekas, G.M., 1967, Floods at Easton, Pennsylvania-Phillipsburg, New Jersey: U.S. Geological Survey Hydrologic Atlas 246, 1 Plate: 39.50 x 37.00 inches, https://doi.org/10.3133/ha246.","productDescription":"1 Plate: 39.50 x 37.00 inches","costCenters":[],"links":[{"id":186616,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413795,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15612.htm","linkFileType":{"id":5,"text":"html"}},{"id":89955,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/246/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New Jersey, Pennsylvania","city":"Easton, Phillipsburg","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.25,\n              40.583\n            ],\n            [\n              -75.25,\n              40.75\n            ],\n            [\n              -75.125,\n              40.75\n            ],\n            [\n              -75.125,\n              40.583\n            ],\n            [\n              -75.25,\n              40.583\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e725d","contributors":{"authors":[{"text":"Farlekas, George M.","contributorId":44963,"corporation":false,"usgs":true,"family":"Farlekas","given":"George","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":278197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22500,"text":"ofr6718 - 1967 - Hydraulic testing techniques of deep drill holes at Pahute Mesa, Nevada test site","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr6718","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":"67-18","title":"Hydraulic testing techniques of deep drill holes at Pahute Mesa, Nevada test site","docAbstract":"This report describes the testing techniques used by the U. S. Geological Survey to obtain hydrologic data in deep holes drilled in volcanic rocks at Pahute Mesa, Nevada Test Site. The testing program in each hole includes geophysical logging, pumping, and injecting and swabbing between straddle packers. \r\n\r\nRock lithologies and qualitative data on hydrologic conditions in the borehole are obtained from electric, caliper, temperature, and fluid resistivity logs. Quantitative data on major water-yielding intervals in the borehole are obtained from radioactive tracer and spinner surveys. \r\n\r\nPumping tests are made to measure the combined yield of the various aquifers. Injection and swabbing tests are made by adding known volumes of water to, or withdrawing known volumes of water from, straddle-packed intervals and observing the rate of decline or rise in water level resulting from this injection or withdrawal of water. The yield of tested intervals is stated as relative specific capacity, in units of gallons per minute per foot of drawdown.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr6718","issn":"0094-9140","usgsCitation":"Blankennagel, R., 1967, Hydraulic testing techniques of deep drill holes at Pahute Mesa, Nevada test site: U.S. Geological Survey Open-File Report 67-18, ii, 51 p. :ill. ;27 cm., https://doi.org/10.3133/ofr6718.","productDescription":"ii, 51 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":155608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0018/report-thumb.jpg"},{"id":52011,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629885","contributors":{"authors":[{"text":"Blankennagel, R. K.","contributorId":65078,"corporation":false,"usgs":true,"family":"Blankennagel","given":"R. K.","affiliations":[],"preferred":false,"id":188361,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68520,"text":"ha294 - 1967 - Flood of August 1967 at Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha294","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":"294","title":"Flood of August 1967 at Fairbanks, Alaska","language":"ENGLISH","doi":"10.3133/ha294","usgsCitation":"Childers, J.M., and Meckel, J.P., 1967, Flood of August 1967 at Fairbanks, Alaska: U.S. Geological Survey Hydrologic Atlas 294, 1 map :col. ;46 x 94 cm., on sheet 99 x 104 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/ha294.","productDescription":"1 map :col. ;46 x 94 cm., on sheet 99 x 104 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":185535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90117,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/294/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -15.234722222222222,64.83333333333333 ], [ -15.234722222222222,64.83333333333333 ], [ -15.234722222222222,64.83333333333333 ], [ -15.234722222222222,64.83333333333333 ], [ -15.234722222222222,64.83333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef72","contributors":{"authors":[{"text":"Childers, Joseph M.","contributorId":14379,"corporation":false,"usgs":true,"family":"Childers","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":278387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meckel, James P.","contributorId":54174,"corporation":false,"usgs":true,"family":"Meckel","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":278388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57738,"text":"ofr67285 - 1967 - Ground-water levels in observation wells in Oklahoma, 1965-66","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr67285","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":"67-285","title":"Ground-water levels in observation wells in Oklahoma, 1965-66","docAbstract":"The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies; (2) facilitate the prediction of trends in water levels that will indicate likely changes in storage; (3) aid in the prediction of the base flow of streams; (4) provide information for use in basic research; (5) provide long-time continuous records of fluctuations of water levels in representative wells; and (6) serve as a framework to which other types of hydrologic data my be related.\r\nPrior to 1956, measurements of water levels in observation wells in Oklahoma were included in water-supply papers published annually by the U.S. Geological Survey. Beginning with the 1956 calendar year, however, Geological Survey water-level reports will contain only records of a selected network of observation wells, and will be published at 5-year intervals. The first of this series, for the 1956-59 period was published in 1962.\r\n\r\nThis report has been prepared primarily to present water-level records of wells not included in the Federal network. However, for the sake of completeness it includes water-level records of Federal wells that either have been or will be published in water-supply papers since 1955. This report, which contains water-level records for the 2-year period (1965-66), is the fourth in a series presenting water-level records for all permanent observations wells in Oklahoma. The first report, published in 1963, contains water-level records for the 2-year period of (1961-62); the second report, published in 1964, contains water-level records for the 2-year period (1961-62); and the third report, published in 1965, contains water-level records for the 2-year period (1963-64).\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr67285","usgsCitation":"Hart, D., 1967, Ground-water levels in observation wells in Oklahoma, 1965-66: U.S. Geological Survey Open-File Report 67-285, 61 p., https://doi.org/10.3133/ofr67285.","productDescription":"61 p.","costCenters":[],"links":[{"id":182947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667580","contributors":{"authors":[{"text":"Hart, D.L. Jr.","contributorId":49403,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":257671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52574,"text":"ofr6772 - 1967 - Hydrology problems as related to wilderness management and water supplies for recreational areas at Mammoth Cave National Park, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr6772","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":"67-72","title":"Hydrology problems as related to wilderness management and water supplies for recreational areas at Mammoth Cave National Park, Kentucky","language":"ENGLISH","doi":"10.3133/ofr6772","usgsCitation":"Cushman, R., 1967, Hydrology problems as related to wilderness management and water supplies for recreational areas at Mammoth Cave National Park, Kentucky: U.S. Geological Survey Open-File Report 67-72, 16 p., https://doi.org/10.3133/ofr6772.","productDescription":"16 p.","costCenters":[],"links":[{"id":177409,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc758","contributors":{"authors":[{"text":"Cushman, R.V.","contributorId":28220,"corporation":false,"usgs":true,"family":"Cushman","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":245572,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68431,"text":"ha263 - 1967 - Floods on Delaware River in the vicinity of Belvidere, New Jersey","interactions":[{"subject":{"id":52540,"text":"ofr6643 - 1966 - Extent and frequency of floods on Delaware River in vicinity of Belvidere, New Jersey","indexId":"ofr6643","publicationYear":"1966","noYear":false,"title":"Extent and frequency of floods on Delaware River in vicinity of Belvidere, New Jersey"},"predicate":"SUPERSEDED_BY","object":{"id":68431,"text":"ha263 - 1967 - Floods on Delaware River in the vicinity of Belvidere, New Jersey","indexId":"ha263","publicationYear":"1967","noYear":false,"title":"Floods on Delaware River in the vicinity of Belvidere, New Jersey"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha263","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":"263","title":"Floods on Delaware River in the vicinity of Belvidere, New Jersey","language":"ENGLISH","doi":"10.3133/ha263","usgsCitation":"Farlekas, G.M., 1967, Floods on Delaware River in the vicinity of Belvidere, New Jersey: U.S. Geological Survey Hydrologic Atlas 263, 1 map., https://doi.org/10.3133/ha263.","productDescription":"1 map.","costCenters":[],"links":[{"id":186679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89957,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/263/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.20083333333334,40.75 ], [ -75.20083333333334,40.86666666666667 ], [ -75.03416666666666,40.86666666666667 ], [ -75.03416666666666,40.75 ], [ -75.20083333333334,40.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df853","contributors":{"authors":[{"text":"Farlekas, George M.","contributorId":44963,"corporation":false,"usgs":true,"family":"Farlekas","given":"George","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":278199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67900,"text":"ha264 - 1967 - Water-bearing characteristics and occurrence of aquifers in Martin County, North Carolina","interactions":[],"lastModifiedDate":"2016-12-07T12:24:49","indexId":"ha264","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":"264","title":"Water-bearing characteristics and occurrence of aquifers in Martin County, North Carolina","language":"ENGLISH","doi":"10.3133/ha264","usgsCitation":"Wyrick, G.G., 1967, Water-bearing characteristics and occurrence of aquifers in Martin County, North Carolina: U.S. Geological Survey Hydrologic Atlas 264, 1 map., https://doi.org/10.3133/ha264.","productDescription":"1 map.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":89063,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/264/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89064,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/264/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.25,35.75 ], [ -77.25,36 ], [ -77,36 ], [ -77,35.75 ], [ -77.25,35.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7df","contributors":{"authors":[{"text":"Wyrick, Granville G.","contributorId":67493,"corporation":false,"usgs":true,"family":"Wyrick","given":"Granville","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":52640,"text":"ofr67267 - 1967 - Hydrology and chloride contamination of the principal artesian aquifer in Glynn County, Georgia","interactions":[{"subject":{"id":52640,"text":"ofr67267 - 1967 - Hydrology and chloride contamination of the principal artesian aquifer in Glynn County, Georgia","indexId":"ofr67267","publicationYear":"1967","noYear":false,"title":"Hydrology and chloride contamination of the principal artesian aquifer in Glynn County, Georgia"},"predicate":"SUPERSEDED_BY","object":{"id":1720,"text":"wsp2029D - 1974 - Geologic and hydrologic control of chloride contamination in aquifers at Brunswick, Glynn County, Georgia","indexId":"wsp2029D","publicationYear":"1974","noYear":false,"chapter":"D","title":"Geologic and hydrologic control of chloride contamination in aquifers at Brunswick, Glynn County, Georgia"},"id":1}],"supersededBy":{"id":1720,"text":"wsp2029D - 1974 - Geologic and hydrologic control of chloride contamination in aquifers at Brunswick, Glynn County, Georgia","indexId":"wsp2029D","publicationYear":"1974","noYear":false,"title":"Geologic and hydrologic control of chloride contamination in aquifers at Brunswick, Glynn County, Georgia"},"lastModifiedDate":"2016-12-14T08:41:00","indexId":"ofr67267","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":"67-267","title":"Hydrology and chloride contamination of the principal artesian aquifer in Glynn County, Georgia","language":"ENGLISH","doi":"10.3133/ofr67267","usgsCitation":"Wait, R.L., and Gregg, D.O., 1967, Hydrology and chloride contamination of the principal artesian aquifer in Glynn County, Georgia: U.S. Geological Survey Open-File Report 67-267, 199 p., https://doi.org/10.3133/ofr67267.","productDescription":"199 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":178542,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United 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,{"id":67898,"text":"ha250 - 1967 - Availability of ground water in Texas County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"ha250","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":"250","title":"Availability of ground water in Texas County, Oklahoma","language":"ENGLISH","doi":"10.3133/ha250","usgsCitation":"Wood, P.R., and Hart, D., 1967, Availability of ground water in Texas County, Oklahoma: U.S. Geological Survey Hydrologic Atlas 250, 3 col. maps ;44 x 77 cm., https://doi.org/10.3133/ha250.","productDescription":"3 col. maps ;44 x 77 cm.","costCenters":[],"links":[{"id":188812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89055,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/250/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89056,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/250/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89057,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/250/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102,36.5 ], [ -102,36.75 ], [ -101,36.75 ], [ -101,36.5 ], [ -102,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8cf","contributors":{"authors":[{"text":"Wood, Perry Rowley","contributorId":10787,"corporation":false,"usgs":true,"family":"Wood","given":"Perry","email":"","middleInitial":"Rowley","affiliations":[],"preferred":false,"id":277278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, D.L.","contributorId":13239,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","affiliations":[],"preferred":false,"id":277279,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52620,"text":"ofr67190 - 1967 - Hydrologic and chemical data for wells, springs, and streams in Nevada, TPS. 1-21 N., and Rs. 41-57 E","interactions":[],"lastModifiedDate":"2022-05-05T13:43:07.402847","indexId":"ofr67190","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":"67-190","title":"Hydrologic and chemical data for wells, springs, and streams in Nevada, TPS. 1-21 N., and Rs. 41-57 E","docAbstract":"<p>Studies of published and unpublished geologic, hydrologic, and chemical-quality data for ground and surface water in central Nevada, Tps. 1 to 21 N. and Rs. 41 to 57 E., Mount Diablo base and meridian, reveal the following information: Rocks exposed in central Nevada are of sedimentary and igneous origin and range in age from Cambrian to Recent. Rocks of Paleozoic age generally are carbonate or clastic, and rocks of Mesozoic age generally are clastic and granitic. Rocks of Tertiary age principally are volcanic, and the valley fill of Quaternary age is alluvial-fan and lake deposits. The rocks are folded, faulted, and highly fractured. Precipitation is closely related to altitude. In general, as the altitude increases the precipitation increases. Most of the streamflow in the valleys originates as snow in the nearby mountains. The streams generally flow only in response to snowmelt and to flash-flood-producing storms. Important chemical quality characteristics of the ground and surface water in central Nevada are hardness, expressed as CaCO<sub>3</sub>, generally in excess of 120 ppm, and a dissolved-solids content of less than 500 ppm. The principal chemical types of both ground and surface waters are sodium and calcium bicarbonates. The major uses of ground water in central Nevada are for irrigation and stock. Frequency of use of wells in decreasing order is: irrigation, stock, domestic, industrial, municipal, and observation. Of the 606 wells tabulated, 29 have multiple uses. Frequency of use of spring water in decreasing order is: stock, irrigation, domestic, and public facilities. Of the 135 springs tabulated, 5 have multiple uses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67190","usgsCitation":"Robinson, B., Thordarson, W., and Beetam, W.A., 1967, Hydrologic and chemical data for wells, springs, and streams in Nevada, TPS. 1-21 N., and Rs. 41-57 E: U.S. Geological Survey Open-File Report 67-190, Report: i, 61 p.; 1 Plate: 30.69 × 39.57 inches, https://doi.org/10.3133/ofr67190.","productDescription":"Report: i, 61 p.; 1 Plate: 30.69 × 39.57 inches","costCenters":[],"links":[{"id":177439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0190/report-thumb.jpg"},{"id":86990,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0190/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0190/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.0810546875,\n              38.03078569382294\n            ],\n            [\n              -115.00488281250001,\n              38.03078569382294\n            ],\n            [\n              -115.00488281250001,\n              40.413496049701955\n            ],\n            [\n              -118.0810546875,\n              40.413496049701955\n            ],\n            [\n              -118.0810546875,\n              38.03078569382294\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118bd","contributors":{"authors":[{"text":"Robinson, B.P.","contributorId":7685,"corporation":false,"usgs":true,"family":"Robinson","given":"B.P.","email":"","affiliations":[],"preferred":false,"id":245654,"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":245655,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beetam, W. A.","contributorId":64327,"corporation":false,"usgs":true,"family":"Beetam","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245656,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171294,"text":"70171294 - 1967 - Climate and streamflow of Puerto Rico","interactions":[],"lastModifiedDate":"2017-10-05T11:46:50","indexId":"70171294","displayToPublicDate":"1967-12-31T14:30:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1185,"text":"Caribbean Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Climate and streamflow of Puerto Rico","docAbstract":"<p><span>The presently available data on&nbsp;streamflow, runoff rainfall, and temperature of Puerto&nbsp;Rico&nbsp;are evaluated, although the period of record is very short, with a view to contributing to the knowledge of hydrology of tropical islands. The average annual&nbsp;streamflow&nbsp;in&nbsp;Puerto&nbsp;Rico&nbsp;is&nbsp;45 percent&nbsp;of the annual rainfall, or 15 percent more than in the eastern piedmont of the U.S. where it is 30 percent.&nbsp;Climate&nbsp;is assumed to be responsible for this difference as well as for the differences of the flows of&nbsp;Puerto Rican streams which vary from 15 to 85 percent of the annual rainfall. Variations in the&nbsp;climate&nbsp;of&nbsp;Puerto&nbsp;Rico are shown by Thornthwaite's climatic index on a map of the island, and the variations of the streamflow&nbsp;to rainfall ratios of&nbsp;Puerto&nbsp;Rican streams are shown to be related to Thornthwaite's climatic index.</span></p>","language":"English","publisher":"University of Puerto Rico","usgsCitation":"Giusti, E., and Lopez, M.A., 1967, Climate and streamflow of Puerto Rico: Caribbean Journal of Science, v. 7, no. 3-4, p. 87-93.","productDescription":"7 p.","startPage":"87","endPage":"93","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true}],"links":[{"id":321744,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e2de4b07e28b664db8c","contributors":{"authors":[{"text":"Giusti, E.V.","contributorId":51342,"corporation":false,"usgs":true,"family":"Giusti","given":"E.V.","affiliations":[],"preferred":false,"id":630463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lopez, M. A.","contributorId":12493,"corporation":false,"usgs":true,"family":"Lopez","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":630464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221316,"text":"70221316 - 1967 - Test hold in aquifer with many water-bearing zones at Jacksonville, Florida","interactions":[],"lastModifiedDate":"2021-06-09T18:35:59.361297","indexId":"70221316","displayToPublicDate":"1967-10-01T13:30:27","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Test hold in aquifer with many water-bearing zones at Jacksonville, Florida","docAbstract":"<p><span>One of the deepest&nbsp;</span>water<span>‐exploration wells&nbsp;</span>in<span>&nbsp;the southeastern United States was completed&nbsp;</span>in<span>&nbsp;1966&nbsp;</span>at<span>&nbsp;</span>Jacksonville<span>,&nbsp;</span>Florida<span>. It was drilled to a depth of nearly 2,500 feet to supply geologic and hydrologic information on the deeper unexplored part of the Floridan&nbsp;</span>aquifer<span>. This&nbsp;</span>aquifer<span>&nbsp;consists of a series of&nbsp;</span>water<span>&nbsp;producing&nbsp;</span>zones<span>&nbsp;separated by nonproducing&nbsp;</span>zones<span>. An important new fresh‐</span>water<span>&nbsp;producing&nbsp;</span>zone<span>&nbsp;was found, and the contact between the fresh&nbsp;</span>water<span>&nbsp;and salt&nbsp;</span>water<span>&nbsp;was located. The well was completed&nbsp;</span>in<span>&nbsp;three separate&nbsp;</span>zones<span>&nbsp;so that it could be used to monitor the the deeper part of the&nbsp;</span>aquifer<span>&nbsp;to detect any salt‐</span>water<span>&nbsp;encroachment. This paper describes the objectives, techniques, and results of drilling the&nbsp;</span>test<span>&nbsp;well.</span></p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01621.x","usgsCitation":"Leve, G., and Goolsby, D.A., 1967, Test hold in aquifer with many water-bearing zones at Jacksonville, Florida: Groundwater, v. 5, no. 4, p. 18-22, https://doi.org/10.1111/j.1745-6584.1967.tb01621.x.","productDescription":"5 p.","startPage":"18","endPage":"22","costCenters":[],"links":[{"id":386362,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Florida","city":"Jacksonville","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.1337890625,\n              30.088107753367257\n            ],\n            [\n              -81.2109375,\n              30.088107753367257\n            ],\n            [\n              -81.2109375,\n              30.543338954230222\n            ],\n            [\n              -82.1337890625,\n              30.543338954230222\n            ],\n            [\n              -82.1337890625,\n              30.088107753367257\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"5","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Leve, G.W.","contributorId":64294,"corporation":false,"usgs":true,"family":"Leve","given":"G.W.","affiliations":[],"preferred":false,"id":817292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goolsby, D. A.","contributorId":50508,"corporation":false,"usgs":true,"family":"Goolsby","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}