{"pageNumber":"2519","pageRowStart":"62950","pageSize":"25","recordCount":68777,"records":[{"id":48183,"text":"ofr73225 - 1967 - Proposed water resources investigations in Morocco","interactions":[],"lastModifiedDate":"2012-02-02T00:10:46","indexId":"ofr73225","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":"73-225","title":"Proposed water resources investigations in Morocco","language":"ENGLISH","doi":"10.3133/ofr73225","usgsCitation":"Phoenix, D.A., 1967, Proposed water resources investigations in Morocco: U.S. Geological Survey Open-File Report 73-225, 89 p. ill., maps ; 27 cm., https://doi.org/10.3133/ofr73225.","productDescription":"89 p. ill., maps ; 27 cm.","costCenters":[],"links":[{"id":171060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a8e1","contributors":{"authors":[{"text":"Phoenix, David A.","contributorId":79156,"corporation":false,"usgs":true,"family":"Phoenix","given":"David","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":236936,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52611,"text":"ofr67162 - 1967 - Synopsis of ground-water conditions in the vicinity of T.11 S., R. 6 E, Pima County, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr67162","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":"67-162","title":"Synopsis of ground-water conditions in the vicinity of T.11 S., R. 6 E, Pima County, Arizona","language":"ENGLISH","doi":"10.3133/ofr67162","usgsCitation":"Moosburner, O., 1967, Synopsis of ground-water conditions in the vicinity of T.11 S., R. 6 E, Pima County, Arizona: U.S. Geological Survey Open-File Report 67-162, 7 p., https://doi.org/10.3133/ofr67162.","productDescription":"7 p.","costCenters":[],"links":[{"id":177222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687d5c","contributors":{"authors":[{"text":"Moosburner, Otto","contributorId":41822,"corporation":false,"usgs":true,"family":"Moosburner","given":"Otto","email":"","affiliations":[],"preferred":false,"id":245640,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":2380,"text":"wsp1839K - 1967 - Ground-water resources of the Pascagoula River basin, Mississippi and Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1839K","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":"K","title":"Ground-water resources of the Pascagoula River basin, Mississippi and Alabama","docAbstract":"Abundant ground-water resources underlie the Pascagoula River basin. These resources have been developed intensively in only a few places--namely, Hattiesburg, Laurel, Meridian, and Pascagoula. Seepage from the ground water reservoirs sustains the base flows of the Leaf, Chickasawhay, Pascagoula, and Escatawpa Rivers and their tributaries. \r\n\r\nThe fresh-water-bearing section is 300 to 3,500 feet thick and is composed chiefly of sand and clay of Eocene to Recent age. Major rock units represented are the Wilcox, Claiborne, Jackson, and Vicksburg Groups and formations of Miocene and Pliocene ages. \r\n\r\nAquifers in the Claiborne Group provide water for all purposes in the northern third of the basin. The Claiborne is underlain by the potentially important but virtually untapped Wilcox Group. Miocene aquifers are the main source of water supplies in the southern half of the basin, but Pliocene aquifers furnish most supplies in the Jackson County area at the basin's southern extremity. Much of the fresh-water section has undergone no water-supply development because of the great depth of many aquifers and the availability, at shallow depths, of supplies adequate for present needs. However, a large part of any substantial increase in ground-water withdrawal will probably come from wells deeper than those commonly drilled in the region. \r\n\r\nGround-water levels are within 50 feet of the surface in most places, and flowing wells are common in the valleys and near the coast. Water-level declines due to pumping have become serious problems only in a few localities of heavy withdrawal. In most of these places redistribution of pumpage would alleviate the problem of excessive drawdown. \r\n\r\nAlthough few wells in the basin yield more than 500 gallons per minute, yields of 2,000 gallons per minute or more could be reasonably expected from efficiently constructed wells almost anywhere in the region. \r\n\r\nTotal ground-water pumpage is estimated to be about 60 million gallons per day. Potential pumpage is many times that figure. Well fields capable of yielding several million gallons of water per day would be feasible in most places. The ground water is of good to excellent quality. Most of it is a sodium bicarbonate type of water. It usually is soft and has a low to moderate dissolved-solids content. Excessive iron is a problem in places, particularly where water supplies are obtained from shallow aquifers, but at least a part of the excess iron comes from corrosion of well and distribution-line fittings by slightly acidic water. \r\n\r\nSalt-water encroachment is a potential problem in the coastal area, but little increase in salinity has been observed in monitor wells in the period 1960-65. Saline-water resources are available for development at considerable depth in most of the region.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1839K","usgsCitation":"Newcome, R., 1967, Ground-water resources of the Pascagoula River basin, Mississippi and Alabama: U.S. Geological Survey Water Supply Paper 1839, iv, 36 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1839K.","productDescription":"iv, 36 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839k/report-thumb.jpg"},{"id":28339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a70d","contributors":{"authors":[{"text":"Newcome, Roy","contributorId":14796,"corporation":false,"usgs":true,"family":"Newcome","given":"Roy","affiliations":[],"preferred":false,"id":145109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1715,"text":"wsp1608H - 1967 - Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1608H","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":"1608","chapter":"H","title":"Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation","docAbstract":"Rising water tables and the salinization of land as the result of canal irrigation threaten the agricultural economy of the Punjab. Since 1954 the Water and Soils Investigation Division of the West Pakistan Water and Power Development Authority has inventoried the water and soils resources of the Punjab and investigated the relations between irrigation activities, the natural hydrologic factors, and the incidence of waterlogging and subsurface-drainage problems. This report summarizes the findings of the investigation, which was carried out under a cooperative agreement between the Government of Pakistan and the U.S. Agency for International Development, and its predecessor, the U.S. International Cooperation Administration. \r\n\r\nLeakage from the canal systems, some of which have been in operation for more than 100 years, is the principal cause of rising water levels and constitutes the major component of ground-water recharge in the Punjab. Geologic studies have shown that virtually the entire Punjab is underlain to depths of 1,000 feet or more by unconsolidated alluvium, which is saturated to within a few feet of land surface. The alluvium varies in texture from medium sand to silty clay, but sandy sediments predominate. Large capacity wells, yielding 4 cfs or more, can be developed almost everywhere. Ground water occurring within a depth of 500 feet below the surface averages less than 1,000 ppm of dissolved solids throughout approximately two-thirds of the Punjab. It is estimated that the volume of usable ground water in storage in this part of the alluvial aquifer is on the order of 2 billion acre-feet. In the other one-third of the Punjab, total dissolved solids range from 1,000 to about 20,000 ppm. In about one-half of this area (one-sixth of the area of the Punjab) some ground water can be utilized by diluting with surface water from canals. \r\n\r\nThe ground-water reservoir underlying the Punjab is an unexploited resource of enormous economic value. It is recognized that the scientific management of this ground-water reservoir is the key to permanent irrigation agriculture in the Punjab. The West Pakistan Water .and Power Development Authority has prepared a long-range program for reclaiming the irrigated lands of the Punjab. The essential feature of this program is a proposed network of tubewells (drilled wells) located with an .average density of about one per square mile. Groundwater withdrawals will serve the dual purpose of helping to supply irrigation requirements and of providing subsurface drainage. Despite the feasibility and inherent advantages of tubewell reclamation methods, it is inevitable that just as the superposition of the canal system on the native environment caused undesirable side effects, large-scale ground-water withdrawals again will disturb the hydrologic regimen. The distribtution of withdrawals and maintenance of a favorable salt balance are two distinct, but related aspects of the ground-water budget that present potential hazards that must be considered in the design and management of the tubewell projects. The availability of ground water for irrigation diminishes from northeast to southwest, or downgradient along the doab (an area lying between two rivers) and is negligible in the centers of the lower parts of the doabs, where the ground water is too highly mineralized for use. Ground-water supplies must be developed in areas where they are available and it might become necessary, under a program of maximum exploitation of ground-water resources, to transfer supplies from outside sources to points of use in the lower parts of the doabs. \r\n\r\nSeveral factors inherent in the tubewell system will tend to depreciate the quality of ground water with time. Among these are the addition of salts leached from the soils, increased concentration of salts due .to repeated cycles of recirculation, and the possible lateral and upward encroachment of saline water in response to pumping. It is reasonably ce","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608H","usgsCitation":"Greenman, D., Swarzenski, W., and Bennett, G., 1967, Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation: U.S. Geological Survey Water Supply Paper 1608, iv, 66 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1608H.","productDescription":"iv, 66 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608h/report-thumb.jpg"},{"id":26796,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26797,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26798,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26799,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26790,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26791,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26792,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26793,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26794,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26795,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608h/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668a83","contributors":{"authors":[{"text":"Greenman, D.W.","contributorId":81072,"corporation":false,"usgs":true,"family":"Greenman","given":"D.W.","affiliations":[],"preferred":false,"id":144006,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, W.V.","contributorId":80243,"corporation":false,"usgs":true,"family":"Swarzenski","given":"W.V.","email":"","affiliations":[],"preferred":false,"id":144005,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bennett, G.D.","contributorId":81073,"corporation":false,"usgs":true,"family":"Bennett","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":144007,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42348,"text":"ofr67224 - 1967 - Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California","interactions":[],"lastModifiedDate":"2025-07-24T19:44:54.186569","indexId":"ofr67224","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":"67-224","title":"Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67224","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California: U.S. Geological Survey Open-File Report 67-224, 1 Plate: 29.67 x 42.79 inches, https://doi.org/10.3133/ofr67224.","productDescription":"1 Plate: 29.67 x 42.79 inches","costCenters":[],"links":[{"id":414489,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8179.htm","linkFileType":{"id":5,"text":"html"}},{"id":80114,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0224/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Aurora, Powell Mountain, Huntoon Valley, and Trench Canyon quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119,\n              38.5\n            ],\n            [\n              -119,\n              38\n            ],\n            [\n              -118.5,\n              38\n            ],\n            [\n              -118.5,\n              38.5\n            ],\n            [\n              -119,\n              38.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697271","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":530914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42325,"text":"ofr67248 - 1967 - Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California","interactions":[],"lastModifiedDate":"2022-11-22T21:58:09.747382","indexId":"ofr67248","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":"67-248","title":"Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67248","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles, Nevada-California: U.S. Geological Survey Open-File Report 67-248, 1 Plate: 30.88 × 40.85 inches, https://doi.org/10.3133/ofr67248.","productDescription":"1 Plate: 30.88 × 40.85 inches","costCenters":[],"links":[{"id":409554,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8203.htm","linkFileType":{"id":5,"text":"html"}},{"id":80088,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0248/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Rhyolite Ridge, Silver Peak, Piper Peak, and Lida Wash quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118,\n              38\n            ],\n            [\n              -118,\n              37.5\n            ],\n            [\n              -117.5,\n              37.5\n            ],\n            [\n              -117.5,\n              38\n            ],\n            [\n              -118,\n              38\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a38","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":530904,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1369,"text":"wsp1594E - 1967 - Artificial recharge through a well tapping basalt aquifers at the Dalles, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:33:01","indexId":"wsp1594E","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":"1594","chapter":"E","title":"Artificial recharge through a well tapping basalt aquifers at the Dalles, Oregon","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1594E","usgsCitation":"Foxworthy, B., and Bryant, C.T., 1967, Artificial recharge through a well tapping basalt aquifers at the Dalles, Oregon: U.S. Geological Survey Water Supply Paper 1594, iv, 55 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1594E.","productDescription":"iv, 55 p. :ill. ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":26456,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26457,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1594e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1594e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c13","contributors":{"authors":[{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":143649,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryant, Charles T.","contributorId":8438,"corporation":false,"usgs":true,"family":"Bryant","given":"Charles","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":143648,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3775,"text":"cir537 - 1967 - Effects of the Truckee, California, earthquake of September 12, 1966","interactions":[],"lastModifiedDate":"2017-04-25T14:01:45","indexId":"cir537","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":"537","title":"Effects of the Truckee, California, earthquake of September 12, 1966","docAbstract":"<p>The Truckee, Calif., earthquake of September 12, 1966, had a magnitude of 5.4 on the Richter scale, as reported by the U.S. Coast and Geodetic Survey. It was felt over an area extending from San Francisco eastward to Salt Lake City and from Bakersfield northward beyond Chico, Calif. Ground breakage due to seismic shaking occurred in unconsolidated alluvium along a zone about 10 miles long that trends about N. 30° E. and extends from a point west of Prosser Reservoir, 4 miles northeast of Truckee, to Hoke Valley. The concentration of ground breakage along this zone suggests that it may be related to a subsurface northeastward-trending fault rather than to buried extensions of the northwestward-trending faults that dominate the regional geologic structure.</p><p>Other effects of the earthquake include the following: (1) Damage to Prosser and Boca Dams, (2) minor damage to several bridges on Interstate Highway 80, (3) several earthquake-generated slumps or landslides on Interstate Highway 80 between Boca Dam and the California-Nevada boundary, (4) damage to the caretaker's house at Boca Dam and a lumber shed at Loyalton, (5) damage by falling rocks to the Farad powerhouse, to the wooden flume which supplies water to the powerhouse, and to the Southern Pacific Lines in Truckee Canyon, (6) minor damage to water wells and water distribution systems, particularly at Truckee, and (7) rejuvenation of springs throughout the Truckee-Russel Valley area.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir537","usgsCitation":"Kachadoorian, R., Yerkes, R.F., and Waananen, A.O., 1967, Effects of the Truckee, California, earthquake of September 12, 1966: U.S. Geological Survey Circular 537, Report: iii, 14 p.; 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F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":147579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waananen, Arvi O.","contributorId":34904,"corporation":false,"usgs":true,"family":"Waananen","given":"Arvi","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":147580,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2877,"text":"wsp1330H - 1967 - Water requirements of the iron and steel industry","interactions":[{"subject":{"id":2877,"text":"wsp1330H - 1967 - Water requirements of the iron and steel industry","indexId":"wsp1330H","publicationYear":"1967","noYear":false,"chapter":"H","title":"Water requirements of the iron and steel industry"},"predicate":"IS_PART_OF","object":{"id":70188911,"text":"wsp1330 - 1955 - Water requirements of selected industries","indexId":"wsp1330","publicationYear":"1955","noYear":false,"title":"Water requirements of selected industries"},"id":1}],"isPartOf":{"id":70188911,"text":"wsp1330 - 1955 - Water requirements of selected industries","indexId":"wsp1330","publicationYear":"1955","noYear":false,"title":"Water requirements of selected industries"},"lastModifiedDate":"2017-06-27T14:25:24","indexId":"wsp1330H","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":"1330","chapter":"H","title":"Water requirements of the iron and steel industry","docAbstract":"<p>Twenty-nine steel plants surveyed during 1957 and 1958 withdrew from various sources about 1,400 billion gallons of water annually and produced 40.8 million tons of ingot steel. This is equivalent to about 34,000 gallons of water per ton of steel. Fifteen iron ore mines and fifteen ore concentration plants together withdrew annually about 89,000 million gallons to produce 15 million tons of iron ore concentrate, or 5,900 gallons per ton of concentrate. About 97 percent of the water used in the steel plants came from surface sources, 2.2 percent was reclaimed sewage, and 1.2 percent was ground water. Steel plants supplied about 96 percent of their own water requirements, although only three plants used self-supplied water exclusively. Water used by the iron ore mines and concentration plants was also predominantly self supplied from surface source. </p><p>Water use in the iron and steel industry varied widely and depended on the availability of water, age and condition of plants and equipment, kinds of processes, and plant operating procedures. Gross water use in integrated steel plants ranged from 11,200 to 110,000 gallons per ton of steel ingots, and in steel processing plants it ranged from 4,180 to 26,700 gallons per ton. Water reuse also varied widely from 0 to 18 times in integrated steel plants and from 0 to 44 times in steel processing plants. Availability of water seemed to be the principal factor in determining the rate of reuse. Of the units within steel plants, a typical (median) blast furnace required 20,500 gallons of water per ton of pig iron. At the 1956-60 average rate of pig iron consumption, this amounts to about 13,000 gallons per ton of steel ingots or about 40 percent of that required by a typical integrated steel plant 33,200 gallons per ton. Different processes of iron ore concentration are devised specifically for the various kinds of ore. These processes result in a wide range of water use from 124 to 11,300 gallons of water per ton of iron ore concentrate. Water use in concentration plants is related to the physical state of the ore. The data in this report indicate that grain size of the ore is the most important factor; the very fine grained taconite and jasper required the greatest amount of water. Reuse was not widely practiced in the iron ore industry.</p><p>Consumption of water by integrated steel plants ranged from 0 to 2,010 gallons per ton of ingot steel and by steel processing plants from 120 to 3,420 gallons per ton. Consumption by a typical integrated steel plant was 681 gallons per ton of ingot steel, about 1.8 percent of the intake and about 1 percent of the gross water use. Consumption by a typical steel processing plant was 646 gallons per ton, 18 percent of the intake, and 3.2 percent of the gross water use. </p><p>The quality of available water was found not to be a critical factor in choosing the location of steel plants, although changes in equipment and in operating procedures are necessary when poor-quality water is used. The use of saline water having a concentration of dissolved solids as much as 10,400 ppm (parts per million) was reported. This very saline water was used for cooling furnaces and for quenching slag. In operations such as rolling steel in which the water comes into contact with the steel being processed, better quality water is used, although water containing as much as 3,410 ppm dissolved solids has been used for this purpose. Treatment of water for use in the iron and steel industry was not widely practiced. Disinfection and treatment for scale and corrosion control were the most frequently used treatment methods.</p>","largerWorkTitle":"Water requirements of selected industries","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1330H","usgsCitation":"Walling, F.B., and Otts, L.E., 1967, Water requirements of the iron and steel industry: U.S. Geological Survey Water Supply Paper 1330, Report: iv, 54 p.; Plate: 23.50 x 14.76 inches, https://doi.org/10.3133/wsp1330H.","productDescription":"Report: iv, 54 p.; Plate: 23.50 x 14.76 inches","startPage":"341","endPage":"394","costCenters":[],"links":[{"id":29511,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1330h/plate-1.pdf","text":"Plate 4","size":"1.28 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":29512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1330h/report.pdf","text":"Report","size":"3.61 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":138986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1330h/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f976b","contributors":{"authors":[{"text":"Walling, Faulkner B.","contributorId":84743,"corporation":false,"usgs":true,"family":"Walling","given":"Faulkner","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":145946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Otts, Louis Ethelbert Jr.","contributorId":75904,"corporation":false,"usgs":true,"family":"Otts","given":"Louis","suffix":"Jr.","email":"","middleInitial":"Ethelbert","affiliations":[],"preferred":false,"id":145945,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2984,"text":"wsp1842 - 1967 - Water resources of the Marquette Iron Range area, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T15:26:08","indexId":"wsp1842","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":"1842","title":"Water resources of the Marquette Iron Range area, Michigan","docAbstract":"<p>Large quantities of water are needed in the beneficiation and pelletizing processes by which the ore mined from low-grade iron-formations is upgraded into an excellent raw material for the iron and steel industry. Extensive reserves of low-grade iron-formation available for development herald an intensification of the demands upon the area's water supplies. This study was designed to provide water facts for public and private agencies in planning orderly development and in guiding the management of the water resources to meet existing and new requirements. </p><p>Inland lakes and streams are the best potential sources of water for immediate development. The natural flow available for 90 percent of the time in the Middle and East Branches of the Escanaba River, the Carp River, and the Michigamme River is about 190 cubic feet per second. Potential storage sites are identified, and their complete development could increase the available supply from the above streams to about 450 cubic feet per second. </p><p>Outwash deposits are the best potential sources of ground water. Large supplies could be developed from extensive outwash deposits in the eastern part of the area adjacent to Goose Lake Outlet and the East Branch Escanaba River. Other areas of outwash occur in the vicinity of Humboldt, West Branch Creek, and along the stream valleys. Streamflow data were used to make rough approximations of the ground-water potential in some areas. In general, however, the available data were not sufficient to permit quantitative evaluation of the potential ground-water supplies. </p><p>Chemical quality of the surface and ground waters of the area is generally acceptable for most uses. Suspended sediment in the form of mineral tailings in effluents from ore-processing plants is a potential problem. Existing plants use settling basins to effectively remove most of the suspended material. Available records indicate that suspended-sediment concentrations and loads in the receiving waters have not been significantly increased by these operations. </p><p>Present water use is about 60 cubic feet per second in the area. Thus, available water supplies are believed to be adequate for existing and foreseeable new uses. Water management, rather than water availability, is of prime consideration in this area. Time distribution of available water supplies, distribution of water to points of use, effect of surface-water development upon ground water and vice versa, and possible conflicts with competing uses are some of the management problems that are discussed. The presence of many inland lakes, favorable storage sites on streams, and several promising acquifers provide flexibility in&nbsp;possible water-management operations. A discussion of the interrelationships between surface and ground water and a ground-water budget are presented to render a better understanding of the hydrologic system with which water management will be concerned.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1842","collaboration":"Prepared in cooperation with the State of Michigan","usgsCitation":"Wiitala, S.W., Newport, T.G., and Skinner, E.L., 1967, Water resources of the Marquette Iron Range area, Michigan: U.S. Geological Survey Water Supply Paper 1842, Document: ix, 142 p.; 4 Plates: 30.00 x 20.25 inches or smaller, https://doi.org/10.3133/wsp1842.","productDescription":"Document: ix, 142 p.; 4 Plates: 30.00 x 20.25 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":40716,"text":"ofr672 - 1967 - The geohydrology of Pinnacles National Monument, California","interactions":[],"lastModifiedDate":"2022-11-07T16:26:38.119525","indexId":"ofr672","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":"67-2","title":"The geohydrology of Pinnacles National Monument, California","docAbstract":"<p>Water supplies for Pinnacles National Monument are obtained from a collection gallery in alluvium and from a flowing well which obtains water from fractured breccia and tuff near a fault.</p><p>Rocks other than alluvium, in all but the northern fourth of the monument, are dense igneous or metamorphic types that, unless fractured, have little potential for development of ground water. However, in some areas near faults these rocks probably will yield small supplies of water. The alluvium along Chalone Creek contains water of good chemical quality in quantities sufficient to supply the monument's needs. The Temblor Formation, a fanglomerate in the northeastern part of the monument, seems to be capable of absorbing and transmitting water but has not been drilled. A test well to determine the potential of the Temblor is suggested.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr672","collaboration":"Prepared in cooperation with the National Park Service U.S. Department of the Interior","usgsCitation":"Akers, J.P., 1967, The geohydrology of Pinnacles National Monument, California: U.S. Geological Survey Open-File Report 67-2, Report: iii, 14 p; 1 Plate: 17.28 x 22.78 inches, https://doi.org/10.3133/ofr672.","productDescription":"Report: iii, 14 p; 1 Plate: 17.28 x 22.78 inches","numberOfPages":"17","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":77990,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0002/plate-1.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic map of Pinnacles national Monument, California, showing location of wells, favorable areas for ground-water development, and proposed well sites"},{"id":77991,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1967/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1967/0002/report-thumb.jpg"}],"country":"United States","state":"California","county":"Monterey County, San Benito County","otherGeospatial":"Pinnacles National Monument","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.21198654174803,\n              36.448903794892864\n            ],\n            [\n              -121.13285064697266,\n              36.448903794892864\n            ],\n            [\n              -121.13285064697266,\n              36.53681226263767\n            ],\n            [\n              -121.21198654174803,\n              36.53681226263767\n            ],\n            [\n              -121.21198654174803,\n              36.448903794892864\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf08","contributors":{"authors":[{"text":"Akers, J. P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":223844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2533,"text":"wsp1839I - 1967 - Ground-water reconnaissance in the Burnt River Valley area, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:42:36","indexId":"wsp1839I","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":"I","title":"Ground-water reconnaissance in the Burnt River Valley area, Oregon","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1839I","usgsCitation":"Price, D., 1967, Ground-water reconnaissance in the Burnt River Valley area, Oregon: U.S. Geological Survey Water Supply Paper 1839, iii, 27 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1839I.","productDescription":"iii, 27 p. :ill., maps ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":139116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1839i/report-thumb.jpg"},{"id":28759,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1839i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28760,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1839i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667105","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":145357,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40719,"text":"ofr675 - 1967 - Ground-water resources of Island County, Washington, with a section on Quality of the ground water","interactions":[{"subject":{"id":40719,"text":"ofr675 - 1967 - Ground-water resources of Island County, Washington, with a section on Quality of the ground water","indexId":"ofr675","publicationYear":"1967","noYear":false,"title":"Ground-water resources of Island County, Washington, with a section on Quality of the ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70047863,"text":"70047863 - 1968 - Ground-water resources of Island County with a section on quality of the ground water","indexId":"70047863","publicationYear":"1968","noYear":false,"title":"Ground-water resources of Island County with a section on quality of the ground water"},"id":1}],"supersededBy":{"id":70047863,"text":"70047863 - 1968 - Ground-water resources of Island County with a section on quality of the ground water","indexId":"70047863","publicationYear":"1968","noYear":false,"title":"Ground-water resources of Island County with a section on quality of the ground water"},"lastModifiedDate":"2013-08-19T11:58:51","indexId":"ofr675","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":"67-5","title":"Ground-water resources of Island County, Washington, with a section on Quality of the ground water","language":"ENGLISH","doi":"10.3133/ofr675","usgsCitation":"Anderson, H.W., and Van Denburgh, A.S., 1967, Ground-water resources of Island County, Washington, with a section on Quality of the ground water: U.S. Geological Survey Open-File Report 67-5, 254 p., https://doi.org/10.3133/ofr675.","productDescription":"254 p.","costCenters":[],"links":[{"id":171312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d674","contributors":{"authors":[{"text":"Anderson, H. W. Jr.","contributorId":11187,"corporation":false,"usgs":true,"family":"Anderson","given":"H.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":223851,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":223852,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112261,"text":"70112261 - 1967 - Explorers from space","interactions":[],"lastModifiedDate":"2017-03-27T13:46:42","indexId":"70112261","displayToPublicDate":"1990-06-12T10:36:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2307,"text":"Journal of Geological Education","active":true,"publicationSubtype":{"id":10}},"title":"Explorers from space","docAbstract":"<p>The statement that a new era in exploration is opening will almost surely bring to mind the venturing of man into space and the ever more imminent exploration of the moon. The reference here, however, is to exploration of earth itself and to the unique capabilities for study of the earth that space technology will provide. Demands for water, minerals, energy, food, and for working, living and recreational space are outrunning our ability to meet them by traditional methods. In order to satisfy these demands, it is necessary now, just as it has been in the past, to look to the activities, the instruments, and the technologies that in part create the pressures for aid in meeting them. Studies being made at the U.S. Geological Survey and elsewhere of the potential applications of remote sensors in space to earth resources research indicate that now, at last, it will be possible to approach solutions on a regional or global basis. This paper discusses the plans for an Earth Resources Observational Satellites Program which will be designed for that purpose.</p>","language":"English","publisher":"National Association of Geology Teachers","publisherLocation":"Appleton, WI","usgsCitation":"Fary, R.W., 1967, Explorers from space: Journal of Geological Education, v. 15, no. 3, p. 99-104.","productDescription":"6 p.","startPage":"99","endPage":"104","numberOfPages":"6","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288453,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbf7e4b0e83db6d08f23","contributors":{"authors":[{"text":"Fary, Raymond W. Jr.","contributorId":22830,"corporation":false,"usgs":true,"family":"Fary","given":"Raymond","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":494589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174084,"text":"70174084 - 1967 - Availability of ground water in Decatur County, Iowa","interactions":[],"lastModifiedDate":"2025-07-29T19:04:41.331482","indexId":"70174084","displayToPublicDate":"1970-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5106,"text":"Iowa Geological Survey Water Atlas","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Availability of ground water in Decatur County, Iowa","docAbstract":"<p>Decatur County and several other counties in south-central Iowa comprise an area that has been chronically short of good-quality water. &nbsp;Municipalities, industries and rural water users alike have been affected by the water shortage. &nbsp;Municipalities have experienced serious problems in obtaining potable supplies adequate to keep pace with their growth and development: industrial expansion has been hindered and continues to be hindered by the shortage of good-quality water; and rural supplies for domestic and livestock use are difficult to obtain at many places. &nbsp;The increased use of water for all purposes and periodic drought conditions have greatly magnified an already serious problem of water shortage.</p>","language":"English","publisher":"Iowa Geological Survey","usgsCitation":"Cagle, J., and Steinhilber, W.L., 1967, Availability of ground water in Decatur County, Iowa: Iowa Geological Survey Water Atlas 2, v, 28 p.","productDescription":"v, 28 p.","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":324448,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324447,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174084/IGS_Water_Atlas_Number_2.pdf","text":"Report","size":"6.43 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Iowa","county":"Decatur County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.558,40.8985],[-93.5573,40.811],[-93.5566,40.7234],[-93.5565,40.6372],[-93.5565,40.5789],[-93.6866,40.5783],[-93.7784,40.5769],[-93.9589,40.5743],[-94.0182,40.5735],[-94.0169,40.6376],[-94.0163,40.7228],[-94.0163,40.8099],[-94.0151,40.8961],[-93.9014,40.897],[-93.7884,40.8987],[-93.6741,40.8989],[-93.6109,40.8989],[-93.558,40.8985]]]},\"properties\":{\"name\":\"Decatur\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57724e2de4b07657d1a81947","contributors":{"authors":[{"text":"Cagle, J.W.","contributorId":36229,"corporation":false,"usgs":true,"family":"Cagle","given":"J.W.","affiliations":[],"preferred":false,"id":640837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinhilber, W. L.","contributorId":79456,"corporation":false,"usgs":true,"family":"Steinhilber","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":640838,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173977,"text":"70173977 - 1967 - Evaluation of potential sources of water in Crater Lake Natonal Park, Oregon","interactions":[],"lastModifiedDate":"2016-06-21T15:49:21","indexId":"70173977","displayToPublicDate":"1968-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Evaluation of potential sources of water in Crater Lake Natonal Park, Oregon","docAbstract":"<p>Crater Lake National Park, in volcanic terrain at the crest of the southern Cascade Range, is well watered by a 67-inch average annual precipitation, measured at park headquarters. Existing park facilities utilize springs that provide quantities of water adequate for present-day as well as foreseeable future needs.</p>\n<p>Ground water occurs under both perched and water-table conditions in the park. Perched ground-water bodies drain to the numerous springs that issue at various altitudes. Test drilling in the northern part failed to locate perched-water bodies capable of supplying quantities of water adequate for proposed facilities, and established that the regional water table is at an altitude below 4,960 feet.</p>\n<p>Many springs and streams at altitudes below 6,500 feet in the western, southern, and southeastern parts discharge quantities of water adequate for a variety of park facilities. Future park-facility development should take into account where water supplies are available. The western, southern, and southeastern parts of the park are more favorable than the northern part in this respect.</p>\n<p>In the northern part of the park, where there are no springs or streams, artificial catchment aprons and storage facilities could be constructed to provide water to points of use. A 100- by 100-foot catchment apron and suitably sized storage tank could provide as much as 1,850 gallons per day for 120 days.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/70173977","usgsCitation":"Hampton, E.R., 1967, Evaluation of potential sources of water in Crater Lake Natonal Park, Oregon: Open-File Report, Report: i, 16 p.; Figure: 9.86 x 15.92 inches, https://doi.org/10.3133/70173977.","productDescription":"Report: i, 16 p.; Figure: 9.86 x 15.92 inches","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":324034,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173977.jpg"},{"id":324141,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173977/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":324162,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70173977/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Crater Lake National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.29019165039062,\n              42.79741601927622\n            ],\n            [\n              -122.29019165039062,\n              43.08894918346591\n            ],\n            [\n              -121.98257446289062,\n              43.08894918346591\n            ],\n            [\n              -121.98257446289062,\n              42.79741601927622\n            ],\n            [\n              -122.29019165039062,\n              42.79741601927622\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913bae4b07657d19ff04e","contributors":{"authors":[{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":639910,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":70011556,"text":"70011556 - 1967 - Silica in alkaline brines","interactions":[],"lastModifiedDate":"2026-02-06T17:25:28.745288","indexId":"70011556","displayToPublicDate":"1967-12-08T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Silica in alkaline brines","docAbstract":"<p><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\"><span>Analysis of sodium carbonate-bicarbonate brines from closed basins in volcanic terranes of Oregon and Kenya reveals silica contents of up to 2700 parts per million at&nbsp;</span><i>p</i><span>H's higher than 10. These high concentrations of SiO</span><sub>2</sub><span>&nbsp;can be attributed to reaction of waters with silicates, and subsequent evaporative concentration accompanied by a rise in&nbsp;</span><i>p</i><span>H. Supersaturation with respect to amorphous silica may occur and persist for brines that are out of contact with silicate muds and undersaturated with respect to trona; correlation of SiO</span><sub>2</sub><span>&nbsp;with concentration of Na and total CO</span><sub>2</sub><span>&nbsp;support this interpretation. Addition of more-dilute waters to alkaline brines may lower the&nbsp;</span><i>p</i><span>H and cause inorganic precipitation of substantial amounts of silica.</span></span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.158.3806.1310","issn":"00368075","usgsCitation":"Jones, B., Rettig, S., and Eugster, H., 1967, Silica in alkaline brines: Science, v. 158, no. 3806, p. 1310-1314, https://doi.org/10.1126/science.158.3806.1310.","productDescription":"5 p.","startPage":"1310","endPage":"1314","costCenters":[],"links":[{"id":221119,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"158","issue":"3806","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8f32e4b08c986b318da9","contributors":{"authors":[{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":361398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rettig, S.L.","contributorId":42592,"corporation":false,"usgs":true,"family":"Rettig","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":361397,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":361399,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221321,"text":"70221321 - 1967 - Stratigraphy and paleoenvironment of the phosphatic miocene strata of North Carolina","interactions":[],"lastModifiedDate":"2021-06-09T19:09:08.163317","indexId":"70221321","displayToPublicDate":"1967-12-01T14:04:13","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Stratigraphy and paleoenvironment of the phosphatic miocene strata of North Carolina","docAbstract":"<p><span>Foraminifera and Mollusca collected from the&nbsp;</span>phosphatic<span>&nbsp;Pungo River Formation and the overlying Yorktown Formation in eastern&nbsp;</span>North<span>&nbsp;</span>Carolina<span>&nbsp;were analyzed and interpreted for stratigraphic and environmental significance in order to determine optimum depositional sites for primary phosphorite. The Mollusca and benthonic foraminifera of the Pungo River Formation correlate with those of the Calvert Formation of Maryland, and the planktonic foraminifera in both of these formations correlate with the Globigerinatella insueta zone of Trinidad, postulated as late Aquitanian age. The&nbsp;</span>paleoenvironment<span>&nbsp;of the phosphorite deposition, interpreted primarily from the benthonic foraminifera, was of cool-temperate waters, ranging in depth from 100 to 200 m in the&nbsp;</span>phosphatic<span>&nbsp;beds to less than 70 m in the upper calcareous beds where phosphate is scarce. Phosphorite deposition occurred in an oceanic embayment located south of the Fort Monroe high in southern Virginia and&nbsp;</span>north<span>&nbsp;of a positive feature whose axis lies in the vicinity of New Bern,&nbsp;</span>North<span>&nbsp;</span>Carolina<span>. Cool-temperate waters in this area during Pungo River time indicate that circulation patterns of ocean currents and the resultant faunal provinces were not the same as those at present and later in the&nbsp;</span>Miocene<span>. In the Pungo River and its time equivalents of the Atlantic Coastal Plain, the presence of thick diatomaceous clay units, volcanic ash beds, shards, attapulgite clays, and other minerals probably derived from volcanic rocks, suggests a volcanic source somewhere off the coast during the&nbsp;</span>Miocene<span>. The Yorktown unconformably overlies the Pungo River Formation. The unconformity is marked by channels into the Pungo River, filled with&nbsp;</span>phosphatic<span>&nbsp;pebbles, vertebrate bones, and lower York-town molluscs and microfauna. The coarse-grained&nbsp;</span>phosphatic<span>&nbsp;material is derived from the underlying fine-grained primary phosphorite in the Pungo River and is abundant only in the lower part of the Yorktown Formation. Deposition of the lower part of the Yorktown occurred in waters about 100 m deep. The waters gradually became more shallow as deposition of the formation continued until depths of less than 15 m, and probable brackish conditions, were reached as the uppermost part of the formation was deposited. Temperature of the waters, cool-temperate during lower Yorktown deposition, became warm-temperate to subtropical in later Yorktown time. The faunal patterns suggest that circulation patterns reached their present state during late Yorktown time.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[631:SAPOTP]2.0.CO;2","usgsCitation":"Gibson, T., 1967, Stratigraphy and paleoenvironment of the phosphatic miocene strata of North Carolina: Geological Society of America Bulletin, v. 78, no. 5, p. 631-650, https://doi.org/10.1130/0016-7606(1967)78[631:SAPOTP]2.0.CO;2.","productDescription":"20 p.","startPage":"631","endPage":"650","costCenters":[],"links":[{"id":386367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"North Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.8056640625,\n              36.61552763134925\n            ],\n            [\n              -81.6943359375,\n              36.686041276581925\n            ],\n            [\n              -83.78173828125,\n              35.55010533588552\n            ],\n            [\n              -84.30908203125,\n              35.08395557927643\n            ],\n            [\n              -84.30908203125,\n              34.97600151317588\n            ],\n            [\n              -80.947265625,\n              35.137879119634185\n            ],\n            [\n              -80.70556640625,\n              34.813803317113155\n            ],\n            [\n              -79.6728515625,\n              34.77771580360469\n            ],\n            [\n              -78.5302734375,\n              33.88865750124075\n            ],\n            [\n              -78.0908203125,\n              33.925129700072\n            ],\n            [\n              -76.201171875,\n              34.831841149828655\n            ],\n            [\n              -75.52001953125,\n              35.764343479667176\n            ],\n            [\n              -75.8056640625,\n              36.61552763134925\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"78","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gibson, T. G.","contributorId":103702,"corporation":false,"usgs":true,"family":"Gibson","given":"T. G.","affiliations":[],"preferred":false,"id":817299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221361,"text":"70221361 - 1967 - Rocks of eocene age on fippennies ledge, Gulf of Maine","interactions":[],"lastModifiedDate":"2021-06-11T13:36:14.085543","indexId":"70221361","displayToPublicDate":"1967-12-01T08:32:23","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Rocks of eocene age on fippennies ledge, Gulf of Maine","docAbstract":"<p><span>In August 1965, a scallop dredge from R/V Albatross brought up many pieces of fossiliferous opaline chert or porcellanite of&nbsp;</span>Eocene<span>&nbsp;</span>age<span>&nbsp;from&nbsp;</span>Fippennies<span>&nbsp;</span>Ledge<span>, a bank 70 m deep in the central&nbsp;</span>Gulf<span>&nbsp;of&nbsp;</span>Maine<span>. Their presence in this area supports the idea that part of the&nbsp;</span>Gulf<span>&nbsp;is underlain by sedimentary&nbsp;</span>rocks<span>&nbsp;of Tertiary&nbsp;</span>age<span>. Occurrence in the porcellanite of two identifiable species of Bryozoa (ascophoran Cheilostomata), Kleidionella lobata Canu and Bassler and \"Ocheto-sella\" robusta Canu and Bassler, suggests (1) correlation with the Castle Hayne Limestone of Claiborne to Jackson&nbsp;</span>age<span>; (2) a temperate zone, distinctly American biogeographic provenance; and (3) accumulation in quiet water.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[681:ROEAOF]2.0.CO;2","usgsCitation":"Schlee, J., and Cheetham, A., 1967, Rocks of eocene age on fippennies ledge, Gulf of Maine: Geological Society of America Bulletin, v. 78, no. 5, p. 81-84, https://doi.org/10.1130/0016-7606(1967)78[681:ROEAOF]2.0.CO;2.","productDescription":"4 p.","startPage":"81","endPage":"84","costCenters":[],"links":[{"id":386424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Maine","otherGeospatial":"Gulf of Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -65.55541992187499,\n              43.42100882994726\n            ],\n            [\n              -66.181640625,\n              43.83452678223682\n            ],\n            [\n              -66.236572265625,\n              44.47299117260252\n            ],\n            [\n              -67.467041015625,\n              44.6061127451739\n            ],\n            [\n              -68.873291015625,\n              44.49650533109348\n            ],\n            [\n              -70.059814453125,\n              43.874138181474734\n            ],\n            [\n              -70.59814453125,\n              43.389081939117496\n            ],\n            [\n              -70.894775390625,\n              42.775243380699706\n            ],\n            [\n              -70.587158203125,\n              42.601619944327965\n            ],\n            [\n              -68.73046875,\n              42.22851735620852\n            ],\n            [\n              -65.55541992187499,\n              43.42100882994726\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"78","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schlee, J.","contributorId":45821,"corporation":false,"usgs":true,"family":"Schlee","given":"J.","affiliations":[],"preferred":false,"id":817423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cheetham, A.H.","contributorId":76189,"corporation":false,"usgs":true,"family":"Cheetham","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":817424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70210847,"text":"70210847 - 1967 - Viscosity and finite strength of the mantle as determined from water and ice loads","interactions":[],"lastModifiedDate":"2020-06-29T16:18:51.948045","indexId":"70210847","displayToPublicDate":"1967-11-01T11:07:12","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1803,"text":"Geophysical Journal International","active":true,"publicationSubtype":{"id":10}},"title":"Viscosity and finite strength of the mantle as determined from water and ice loads","docAbstract":"<p class=\"chapter-para\">Some recent examples of transient Earth loads (Lake Bonneville, Utah; Glacier Bay, Alaska; northeast Greenland) indicate that both the viscosity and finite strength of the mantle are lower than is commonly presumed. A time constant (1/<i>e</i>) of 4000 years is estimated for Lake Bonneville, and of 1000 years for northeast Greenland. A strain rate of 10<sup>−14</sup><span>&nbsp;</span>is typical. These figures imply viscosities in a homogeneous half space ranging from 10<sup>20</sup><span>&nbsp;</span>to 10<sup>21</sup><span>&nbsp;</span>poises.</p><p class=\"chapter-para\">An upper limit of finite strength is set by Lake Bonneville at a few times 10<sup>6</sup><span>&nbsp;</span>dyn/cm<sup>2</sup>. If mountain ranges like the Sierra Nevada or Himalaya are regarded as dynamically supported rather than static systems, this low value is not incompatible with other geologic observations.</p>","language":"English","publisher":"Oxford Academic","doi":"10.1111/j.1365-246X.1967.tb06243.x","usgsCitation":"Crittenden, M.D., 1967, Viscosity and finite strength of the mantle as determined from water and ice loads: Geophysical Journal International, v. 14, no. 1-4, p. 261-279, https://doi.org/10.1111/j.1365-246X.1967.tb06243.x.","productDescription":"19 p.","startPage":"261","endPage":"279","costCenters":[],"links":[{"id":480342,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1111/j.1365-246x.1967.tb06243.x","text":"Publisher Index Page"},{"id":375982,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Greenland, United States","state":"Alaska, Utah","otherGeospatial":"Glacier Bay, Lake Bonneville, Mesters Vig","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -24.5159912109375,\n              71.99003064007077\n            ],\n            [\n              -23.52996826171875,\n              71.99003064007077\n            ],\n            [\n              -23.52996826171875,\n              72.36577662200845\n            ],\n            [\n              -24.5159912109375,\n              72.36577662200845\n            ],\n            [\n              -24.5159912109375,\n              71.99003064007077\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -135.087890625,\n              59.567723306212955\n            ],\n            [\n              -137.691650390625,\n              58.802361927759456\n            ],\n            [\n              -136.0546875,\n              57.54531289147553\n            ],\n            [\n              -134.80224609375,\n              56.19448087726972\n            ],\n            [\n              -132.37426757812497,\n              57.00485033534416\n            ],\n            [\n              -133.59375,\n              58.45348121776238\n            ],\n            [\n              -135.087890625,\n              59.361195471124816\n            ],\n            [\n              -135.087890625,\n              59.567723306212955\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.3896484375,\n              39.13006024213511\n            ],\n            [\n              -111.39038085937499,\n              39.13006024213511\n            ],\n            [\n              -111.39038085937499,\n              43.04480541304369\n            ],\n            [\n              -114.3896484375,\n              43.04480541304369\n            ],\n            [\n              -114.3896484375,\n              39.13006024213511\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"14","issue":"1-4","noUsgsAuthors":false,"publicationDate":"2010-01-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Crittenden, Max D. Jr.","contributorId":28951,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":791702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1001583,"text":"1001583 - 1967 - Back-pack unit for capturing waterfowl and upland game by night-lighting","interactions":[],"lastModifiedDate":"2025-02-12T15:45:45.248481","indexId":"1001583","displayToPublicDate":"1967-10-06T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Back-pack unit for capturing waterfowl and upland game by night-lighting","docAbstract":"<p>A night-lighting unit, designed as a light weight back-pack, proved successful for capturing waterfowl pairs, pheasants (<i>Phasianus</i> <i>colchicus</i>), and cottontail rabbits (<i>Sylvilagus floridanus</i>) during the spring and summer when most breeding populations are widely dispersed. Eighty ducks of seven species were captured in 48 hours (1.7 ducks per hour) of night-lighting in marsh habitat. Similarly, 30 pheasants were trapped in 25 hours (1.2 birds per hour) and 63 cottontail rabbits were either observed at close range (6-12 ft) or captured during night-lighting operations in upland habitat. Catch per hour of effort increased for all species as their night habitat requirements and reaction to night-lights became known. The mobile unit proved well suited for intensive use on small areas where other methods of capture were unfeasible and where representative coverage of various habitat types was desired. Besides its utility for capturing animals, the unit provided a method for studying nocturnal movements, behavior, and habitat use of marked animals.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797983","usgsCitation":"Drewien, R., Reeves, H., Springer, P.F., and Kuck, T., 1967, Back-pack unit for capturing waterfowl and upland game by night-lighting: Journal of Wildlife Management, v. 31, no. 4, p. 778-783, https://doi.org/10.2307/3797983.","productDescription":"6 p.","startPage":"778","endPage":"783","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133766,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Day County, Sanborn County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-97.9802,45.5883],[-97.6116,45.5882],[-97.4885,45.5892],[-97.3727,45.5889],[-97.3629,45.5603],[-97.3544,45.5605],[-97.2269,45.5603],[-97.226,45.2996],[-97.2251,45.2118],[-97.226,45.1538],[-97.2396,45.1541],[-97.4951,45.1537],[-97.7403,45.1544],[-97.9809,45.1545],[-97.9803,45.2409],[-97.9802,45.5883]]],[[[-97.8506,44.1964],[-97.8494,43.8505],[-97.9662,43.851],[-98.3266,43.851],[-98.331,43.8502],[-98.332,43.9385],[-98.332,44.1974],[-97.8506,44.1964]]]]},\"properties\":{\"name\":\"Day\",\"state\":\"SD\"}}]}","volume":"31","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adb9","contributors":{"authors":[{"text":"Drewien, Rod C.","contributorId":58594,"corporation":false,"usgs":true,"family":"Drewien","given":"Rod C.","affiliations":[],"preferred":false,"id":311299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, H.M.","contributorId":92634,"corporation":false,"usgs":true,"family":"Reeves","given":"H.M.","email":"","affiliations":[],"preferred":false,"id":311300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Springer, P. F.","contributorId":56590,"corporation":false,"usgs":false,"family":"Springer","given":"P.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":311298,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kuck, T.L.","contributorId":101591,"corporation":false,"usgs":true,"family":"Kuck","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":311301,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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