{"pageNumber":"2580","pageRowStart":"64475","pageSize":"25","recordCount":68807,"records":[{"id":68696,"text":"ha47 - 1962 - Floods at Fremont, Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"ha47","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"47","title":"Floods at Fremont, Ohio","language":"ENGLISH","doi":"10.3133/ha47","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Floods at Fremont, Ohio: U.S. Geological Survey Hydrologic Atlas 47, 1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches)), https://doi.org/10.3133/ha47.","productDescription":"1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches))","costCenters":[],"links":[{"id":188097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.18333333333334,41.25 ], [ -83.18333333333334,41.3675 ], [ -83.05,41.3675 ], [ -83.05,41.25 ], [ -83.18333333333334,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7280","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":534516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22804,"text":"ofr6234 - 1962 - Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T15:37:23","indexId":"ofr6234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-34","title":"Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","docAbstract":"This reports evaluates the ground-water resources of about 1,000 square miles in the semiarid uplands south of the Snake River between Bruneau River and Salmon Falls Creek. The outcropping rocks are the Idavada Volcanics of Pliocene age, and the Idaho Group of Pliocene and Plieistocene age, consisting of the Banbury Basalt of middle Pliocene age and overlying predominantly sedimentary deposits of middle Pliocene through middle Pleistocene age. These rocks dip gently northward. The volcanic rocks are the best aquifers, but the yield of water from the sedimentary deposits is adequate for domestic and stock use. About 6,000 acre-feet of water is withdrawn annually from the Idavada Volcanics by 9 irrigation wells to irrigate about 3,000 acres. Only a few tends of acre-feet of water withdrawn from the other formations. The regional dip of the rocks induces weak artesian conditions in the volcanic rocks and somewhat higher artesian head in the sedimentary rocks. Estimated depth to water ranges from less than 250 feet to more than 750 feet, as shown in an accompanying map. The eastern part of the area appears to be more favorable for the development of ground water for irrigation than the western part because of better aquifers at shallower depth.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6234","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Crosthwaite, E., 1962, Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho: U.S. Geological Survey Open-File Report 62-34, Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller, https://doi.org/10.3133/ofr6234.","productDescription":"Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller","numberOfPages":"56","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0034/report-thumb.jpg"},{"id":52232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52233,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52234,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Elmore County;Owyhee County;Twin Falls County","otherGeospatial":"Sailor Creek Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.4626,42.0584 ], [ -116.4626,44.1361 ], [ -112.07,44.1361 ], [ -112.07,42.0584 ], [ -116.4626,42.0584 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0c5","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68665,"text":"ha55 - 1962 - Summary of occurrence of ground water on the Papago Indian Reservation, Arizona","interactions":[],"lastModifiedDate":"2022-09-01T18:49:29.084083","indexId":"ha55","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"55","title":"Summary of occurrence of ground water on the Papago Indian Reservation, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha55","usgsCitation":"Heindl, L., Cosner, O.J., Page, H.G., Armstrong, C.A., and Kister, L., 1962, Summary of occurrence of ground water on the Papago Indian Reservation, Arizona: U.S. Geological Survey Hydrologic Atlas 55, 1 Plate: 39.50 × 30.00 inches, https://doi.org/10.3133/ha55.","productDescription":"1 Plate: 39.50 × 30.00 inches","costCenters":[],"links":[{"id":186049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406085,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15940.htm","linkFileType":{"id":5,"text":"html"}},{"id":90371,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/055/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.708,\n              31.508\n            ],\n            [\n              -111.25,\n              31.508\n            ],\n            [\n              -111.25,\n              32.767\n            ],\n            [\n              -112.708,\n              32.767\n            ],\n            [\n              -112.708,\n              31.508\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6990fa","contributors":{"authors":[{"text":"Heindl, L.A.","contributorId":52150,"corporation":false,"usgs":true,"family":"Heindl","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":278671,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cosner, O. J.","contributorId":19587,"corporation":false,"usgs":true,"family":"Cosner","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278670,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Page, H. G.","contributorId":82775,"corporation":false,"usgs":true,"family":"Page","given":"H.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278674,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":278673,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kister, L. R.","contributorId":54187,"corporation":false,"usgs":true,"family":"Kister","given":"L. R.","affiliations":[],"preferred":false,"id":278672,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57723,"text":"ofr62162 - 1962 - Surface water of Beaver Creek Basin, in South-Central Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr62162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-162","title":"Surface water of Beaver Creek Basin, in South-Central Oklahoma","docAbstract":"Annual discharge from Beaver Creek basin is estimated to have averaged 217,000 acre-feet during a 19-year base period, water years 1938-56, equivalent to an average annual runoff depth of 4.7 inches over the 857 square-mile drainage area. About 55,000 acre-feet per year comes from Little Beaver Creek basin, a tributary drainage of 195 square miles.\r\nYearly streamflow is highly variable. The discharge of Little Beaver Creek near Duncan during 13-year period of record (water years 1949-61) has ranged from 86,530 acre-feet in calendar year 1957 to 4,880 acre-feet in 1956, a ratio of almost 18 to 1.\r\n\r\nHighest runoff within a year tends to occur in the spring months of May and June, a 2-month period that, on the average, accounts for more than half of the annual discharge of Little Beaver Creek near Duncan. The average monthly runoff during record was lowest in January. Variation in daily streamflow is such that while the average discharge for the 13-year period of record was 50.1 cfs (cubic feet per second), the daily discharge was more than 6 cfs only about half of the time. There was no flow at the site 19 percent of the time during the period.\r\n\r\nSome base runoff usually exists in the headwaters of Beaver and Little Beaver Creeks, and in the lower reaches of Beaver Creek. Low flow in Cow Creek tends to be sustained by waste water from Duncan, where water use in 1961 averaged 4 million gallons per day. In the remainder of the basin, periods of no flow occur in most years.\r\n\r\nThe surface water of Beaver Creek basin is very hard but in general is usable for municipal, agricultural and industrial purposes. The chemical character of the water is predominantly a calcium, magnesium bicarbonate type of water in the lower three quarters of the basin, except in Cow Creek where oil-field brines induce a distinct sodium, calcium chloride characteristic at low and medium flows. A calcium sulfate type of water occurs in most of the northern part of the basin except in headwater areas underlain by the Rush Springs Sandstone, where quality is similar to that in the lower basin.\r\n\r\nThe report gives an estimate of the average discharge at several sites in Beaver Creek basin for a 19-year base period, October 1937 to September 1956. Duration curves of daily discharge for Little Beaver Creek near Duncan and Beaver Creek near Waurika are shown for the period of record. Monthly and annual discharge records for these gaging stations are presented. The results of 52 discharge measurements at 17 other sites in the basin are tabulated, with 5 groups being plotted as discharge profiles. Storage requirements for regulated discharge at the two gaging stations are shown.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr62162","usgsCitation":"Laine, L., and Murphy, J., 1962, Surface water of Beaver Creek Basin, in South-Central Oklahoma: U.S. Geological Survey Open-File Report 62-162, 28 p., https://doi.org/10.3133/ofr62162.","productDescription":"28 p.","costCenters":[],"links":[{"id":184243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698203","contributors":{"authors":[{"text":"Laine, L.L.","contributorId":100464,"corporation":false,"usgs":true,"family":"Laine","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":257642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":257641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71759,"text":"tei805 - 1962 - Geology and ground-water hydrology of the Atlantic and Gulf coastal plain as related to disposal of radioactive wastes","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei805","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"805","title":"Geology and ground-water hydrology of the Atlantic and Gulf coastal plain as related to disposal of radioactive wastes","language":"ENGLISH","doi":"10.3133/tei805","usgsCitation":"LeGrand, H.E., 1962, Geology and ground-water hydrology of the Atlantic and Gulf coastal plain as related to disposal of radioactive wastes: U.S. Geological Survey Trace Elements Investigations 805, 170 p., 33 fig. [some missing], https://doi.org/10.3133/tei805.","productDescription":"170 p., 33 fig. [some missing]","costCenters":[],"links":[{"id":191694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/805/report-thumb.jpg"},{"id":90986,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90987,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90988,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90989,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90990,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90991,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90992,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90993,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90994,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90995,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90996,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90997,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90998,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90999,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91000,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91001,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91002,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91003,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91004,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91005,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91006,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91007,"rank":421,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-22.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91008,"rank":422,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-23.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91009,"rank":423,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/805/plate-24.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91010,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/805/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685eaa","contributors":{"authors":[{"text":"LeGrand, Harry E.","contributorId":35824,"corporation":false,"usgs":true,"family":"LeGrand","given":"Harry","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":284719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1809,"text":"wsp1547 - 1962 - Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60","interactions":[],"lastModifiedDate":"2017-09-07T10:08:46","indexId":"wsp1547","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1547","title":"Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60","docAbstract":"<p>This inventory of published and unpublished sediment-load data contains a list of the sediment-transport measurements in the United States and Puerto Rico during October 1950 to September 1960, made by the agencies associated with the Subcommittee on Sedimentation. Some of the agencies have miscellaneous sediment data, such as single observations at scattered stations or observations on very small watersheds, which are not listed in this inventory. Each entry contains the following: drainage area above station, period of record, number or frequency of observations, sampling equipment and method in which it was used, units of expression for load, particle-size analyses, and source of basic data or published results. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1547","collaboration":"Prepared in cooperation with Sub-committee on Sedimentation, Agency Committee on Water Resources","usgsCitation":"Harris, K.F., 1962, Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60: U.S. Geological Survey Water Supply Paper 1547, v, 117 p., https://doi.org/10.3133/wsp1547.","productDescription":"v, 117 p.","numberOfPages":"126","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1547/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1547/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c6e4b07f02db53fe24","contributors":{"authors":[{"text":"Harris, Kerry F.","contributorId":31732,"corporation":false,"usgs":true,"family":"Harris","given":"Kerry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1327,"text":"wsp1475K - 1962 - Ground-Water Reconnaissance at Pinnacles National Monument, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1475K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"K","title":"Ground-Water Reconnaissance at Pinnacles National Monument, California","docAbstract":"Ground-water supplies at Pinnacles National Monument have been obtained from springs that occur in fractures and along bedding planes of volcanic flows and deposits, and from springs discharged from perched water in a sedimentary fanglomerate formation. The spring-water yield is barely adequate to supply existing camp facilities, and therefore a supplemental water supply is necessary before existing campgrounds can be expanded.\r\n\r\nThis supplemental water can be supplied by good-quality ground water obtained from shallow wells drilled in the alluvium of Chalone Creek. The yield of properly constructed wells in this area should exceed 10 gallons per minute.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475K","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Evenson, R.E., 1962, Ground-Water Reconnaissance at Pinnacles National Monument, California: U.S. Geological Survey Water Supply Paper 1475, iii, 375-382 p., https://doi.org/10.3133/wsp1475K.","productDescription":"iii, 375-382 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":137990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475k/report-thumb.jpg"},{"id":12513,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-K/","linkFileType":{"id":5,"text":"html"}},{"id":26378,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d538","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1190,"text":"wsp1475J - 1962 - Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","interactions":[{"subject":{"id":51815,"text":"ofr5531 - 1955 - Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","indexId":"ofr5531","publicationYear":"1955","noYear":false,"title":"Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":1190,"text":"wsp1475J - 1962 - Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","indexId":"wsp1475J","publicationYear":"1962","noYear":false,"chapter":"J","title":"Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona"},"id":1}],"lastModifiedDate":"2024-01-10T21:22:09.485848","indexId":"wsp1475J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"J","title":"Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona","docAbstract":"The Wupatki and Sunset Crater National Monuments are 15 and 30 miles, respectively, northeast of Flagstaff on the San Francisco Plateau. They are in the eastern part of the San Francisco volcanic field and on the southwest flank of the Black Mesa basin. The Supai formation, Coconino sandstone, Kaibab limestone, Moenkopi formation, and Chinle formation are overlain in parts of the area by volcanic rocks and alluvium. The regional water table occurs chiefly in the Coconino sandstone at altitudes of about 5,000 feet at Sunset Crater, about 4,075 feet near Wupatki Ruin, and about 4,100 feet near Citadel Ruin. The general movement of the ground water is northeastward. Small supplies of perched water occur in the Moenkopi formation and in the alluvium, and perched water may be present locally in the volcanic rocks. The results of the field investigation indicated that adequate ground-water supplies were available from the Coconino sandstone to meet the needs of the National Monuments, and a well was drilled at the Wupatki Monument headquarters in 1958 to a total depth of 904 feet. It produced 50 gpm (gallons per minute) of water with 45 feet of drawdown from a static water level of 780 feet below land surface.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475J","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Cosner, O.J., 1962, Ground water in the Wupatki and Sunset Crater National Monuments, Coconino County, Arizona: U.S. Geological Survey Water Supply Paper 1475, Report: iv, 15 p.; 2 Plates: 29.25 x 30.88 inches and 14.80 x 9.90 inches, https://doi.org/10.3133/wsp1475J.","productDescription":"Report: iv, 15 p.; 2 Plates: 29.25 x 30.88 inches and 14.80 x 9.90 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":424287,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24413.htm","linkFileType":{"id":5,"text":"html"}},{"id":26053,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137938,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475j/report-thumb.jpg"},{"id":26055,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26054,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475j/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Coconino County","otherGeospatial":"Wupatki and Sunset Crater National Monuments","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n      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,{"id":52240,"text":"ofr6244 - 1962 - Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962","interactions":[{"subject":{"id":52240,"text":"ofr6244 - 1962 - Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962","indexId":"ofr6244","publicationYear":"1962","noYear":false,"title":"Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962"},"predicate":"SUPERSEDED_BY","object":{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","indexId":"wsp1619F","publicationYear":"1963","noYear":false,"chapter":"F","title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California"},"id":1}],"supersededBy":{"id":1325,"text":"wsp1619F - 1963 - Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California","indexId":"wsp1619F","publicationYear":"1963","noYear":false,"title":"Geology and ground-water features of Point Arguello Naval Missile Facility, Santa Barbara County, California"},"lastModifiedDate":"2012-02-02T00:11:46","indexId":"ofr6244","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-44","title":"Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962","language":"ENGLISH","doi":"10.3133/ofr6244","usgsCitation":"Evenson, R.E., 1962, Ground-water conditions, U. S. Naval Missile Facility, Point Arguello, California, June 1961-June 1962: U.S. Geological Survey Open-File Report 62-44, 22 p., https://doi.org/10.3133/ofr6244.","productDescription":"22 p.","costCenters":[],"links":[{"id":175180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d0b4","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245023,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52299,"text":"ofr62155 - 1962 - Surface waters of Otter Creek basin in southwestern Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-155","title":"Surface waters of Otter Creek basin in southwestern Oklahoma","docAbstract":"Otter Creek had an average annual discharge at the gaging station of 22 cfs (cubic feet per second) or 15,900 acre-feet per year from a drainage area of 132 square miles during a selected 19-year base period, water-years 1938-56.\r\nThe maximum yearly runoff was 43,410 acre-feet for water-year 1957. The maximum monthly runoff was 24,090 acre-feet in May 1957.\r\n\r\nOtter Creek has extended periods of no flow except for about the last 5 miles near the mouth. The most severe droughts occurred in 1938-41 and 1952-56. Periods of no flow have extended as long as 363 days and have exceeded 300 days many times.\r\n\r\nThe usable storage required to provide a regulated discharge equal to about half the average discharge at the gaging station at Snyder Lake during the most deficient period was determined to be 18,000 acre-feet.\r\n\r\nMiscellaneous measurements made at selected sites show that there is no sustained base flow in any of the tributaries and none in the mainstem except for about the last 5 miles near the mouth. A group of measurements made in September 1961, when there was ground-water outflow in all of the main tributaries except Horse Creek, shows that most of the ground-water outflow in the upper part of the basin comes from the tributaries that originate in the Wichita Mountains. Considerable base runoff occurs in the lower part of the basin from large alluvial and terrace deposits.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr62155","usgsCitation":"Westfall, A., 1962, Surface waters of Otter Creek basin in southwestern Oklahoma: U.S. Geological Survey Open-File Report 62-155, 37 p., https://doi.org/10.3133/ofr62155.","productDescription":"37 p.","costCenters":[],"links":[{"id":179583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69795e","contributors":{"authors":[{"text":"Westfall, A.O.","contributorId":85225,"corporation":false,"usgs":true,"family":"Westfall","given":"A.O.","email":"","affiliations":[],"preferred":false,"id":245103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52298,"text":"ofr62154 - 1962 - Surface waters of Elk Creek basin in southwestern Oklahoma","interactions":[{"subject":{"id":52298,"text":"ofr62154 - 1962 - Surface waters of Elk Creek basin in southwestern Oklahoma","indexId":"ofr62154","publicationYear":"1962","noYear":false,"title":"Surface waters of Elk Creek basin in southwestern Oklahoma"},"predicate":"SUPERSEDED_BY","object":{"id":52374,"text":"ofr63138 - 1963 - Surface waters of Elk Creek basin in southwestern Oklahoma","indexId":"ofr63138","publicationYear":"1963","noYear":false,"title":"Surface waters of Elk Creek basin in southwestern Oklahoma"},"id":1}],"supersededBy":{"id":52374,"text":"ofr63138 - 1963 - Surface waters of Elk Creek basin in southwestern Oklahoma","indexId":"ofr63138","publicationYear":"1963","noYear":false,"title":"Surface waters of Elk Creek basin in southwestern Oklahoma"},"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-154","title":"Surface waters of Elk Creek basin in southwestern Oklahoma","language":"ENGLISH","doi":"10.3133/ofr62154","usgsCitation":"Westfall, A., 1962, Surface waters of Elk Creek basin in southwestern Oklahoma: U.S. Geological Survey Open-File Report 62-154, 18 p., https://doi.org/10.3133/ofr62154.","productDescription":"18 p.","costCenters":[],"links":[{"id":179582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691230","contributors":{"authors":[{"text":"Westfall, A.O.","contributorId":85225,"corporation":false,"usgs":true,"family":"Westfall","given":"A.O.","email":"","affiliations":[],"preferred":false,"id":245102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52296,"text":"ofr62152 - 1962 - Ground-water inventory for 1961, Edwards Air Force Base, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-152","title":"Ground-water inventory for 1961, Edwards Air Force Base, California","language":"ENGLISH","doi":"10.3133/ofr62152","usgsCitation":"Weir, J.E., 1962, Ground-water inventory for 1961, Edwards Air Force Base, California: U.S. Geological Survey Open-File Report 62-152, 54 p., https://doi.org/10.3133/ofr62152.","productDescription":"54 p.","costCenters":[],"links":[{"id":179501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0152/report-thumb.jpg"},{"id":86787,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0152/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86788,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0152/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668caa","contributors":{"authors":[{"text":"Weir, J. E. Jr.","contributorId":102476,"corporation":false,"usgs":true,"family":"Weir","given":"J.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52294,"text":"ofr62147 - 1962 - Preliminary report on ground-water conditions at Homer, Alaska","interactions":[{"subject":{"id":52294,"text":"ofr62147 - 1962 - Preliminary report on ground-water conditions at Homer, Alaska","indexId":"ofr62147","publicationYear":"1962","noYear":false,"title":"Preliminary report on ground-water conditions at Homer, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":67947,"text":"ha187 - 1968 - Water resources and surficial geology of the Homer area, south-central Alaska","indexId":"ha187","publicationYear":"1968","noYear":false,"title":"Water resources and surficial geology of the Homer area, south-central Alaska"},"id":1}],"supersededBy":{"id":67947,"text":"ha187 - 1968 - Water resources and surficial geology of the Homer area, south-central Alaska","indexId":"ha187","publicationYear":"1968","noYear":false,"title":"Water resources and surficial geology of the Homer area, south-central Alaska"},"lastModifiedDate":"2012-02-02T00:11:21","indexId":"ofr62147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-147","title":"Preliminary report on ground-water conditions at Homer, Alaska","language":"ENGLISH","doi":"10.3133/ofr62147","usgsCitation":"Waller, R., 1962, Preliminary report on ground-water conditions at Homer, Alaska: U.S. Geological Survey Open-File Report 62-147, 6 p., https://doi.org/10.3133/ofr62147.","productDescription":"6 p.","costCenters":[],"links":[{"id":179499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":111587,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/10680","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cab1","contributors":{"authors":[{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":245098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52293,"text":"ofr62146 - 1962 - Drainage areas at selected sites on streams in North Carolina","interactions":[],"lastModifiedDate":"2016-12-09T11:16:45","indexId":"ofr62146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-146","title":"Drainage areas at selected sites on streams in North Carolina","language":"ENGLISH","doi":"10.3133/ofr62146","usgsCitation":"Walker, P., 1962, Drainage areas at selected sites on streams in North Carolina: U.S. Geological Survey Open-File Report 62-146, 67 p., https://doi.org/10.3133/ofr62146.","productDescription":"67 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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,{"id":52245,"text":"ofr6256 - 1962 - Bibliography of technical reports, articles, and memoranda published or otherwise released by the Ground Water Branch during the calendar year 1961","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"ofr6256","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-56","title":"Bibliography of technical reports, articles, and memoranda published or otherwise released by the Ground Water Branch during the calendar year 1961","language":"ENGLISH","doi":"10.3133/ofr6256","usgsCitation":"Griffin, M.S., and Clark, E., 1962, Bibliography of technical reports, articles, and memoranda published or otherwise released by the Ground Water Branch during the calendar year 1961: U.S. Geological Survey Open-File Report 62-56, 39 p., https://doi.org/10.3133/ofr6256.","productDescription":"39 p.","costCenters":[],"links":[{"id":175256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627d97","contributors":{"authors":[{"text":"Griffin, M. S.","contributorId":93534,"corporation":false,"usgs":true,"family":"Griffin","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":245033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, E.N.","contributorId":75622,"corporation":false,"usgs":true,"family":"Clark","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":245032,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1082,"text":"wsp1619M - 1962 - Ground-water resources of Cow Valley, Malheur County, Oregon","interactions":[{"subject":{"id":51895,"text":"ofr5617 - 1956 - The ground-water resources of Cow Valley near Ironside, Malheur County, Oregon","indexId":"ofr5617","publicationYear":"1956","noYear":false,"title":"The ground-water resources of Cow Valley near Ironside, Malheur County, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1082,"text":"wsp1619M - 1962 - Ground-water resources of Cow Valley, Malheur County, Oregon","indexId":"wsp1619M","publicationYear":"1962","noYear":false,"chapter":"M","title":"Ground-water resources of Cow Valley, Malheur County, Oregon"},"id":1}],"lastModifiedDate":"2023-03-24T19:34:11.254076","indexId":"wsp1619M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"M","title":"Ground-water resources of Cow Valley, Malheur County, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619M","usgsCitation":"Brown, S.G., and Newcomb, R.C., 1962, Ground-water resources of Cow Valley, Malheur County, Oregon: U.S. Geological Survey Water Supply Paper 1619, Report: iv, 38 p.; 1 Plate: 16.00 x 11.50 inches, https://doi.org/10.3133/wsp1619M.","productDescription":"Report: iv, 38 p.; 1 Plate: 16.00 x 11.50 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":414725,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24829.htm","linkFileType":{"id":5,"text":"html"}},{"id":137100,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619m/report-thumb.jpg"},{"id":25798,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619m/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25797,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619m/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Malheur County","otherGeospatial":"Cow Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.933,\n              44.3\n            ],\n            [\n              -117.933,\n              44.164\n            ],\n            [\n              -117.656,\n              44.164\n            ],\n            [\n              -117.656,\n              44.3\n            ],\n            [\n              -117.933,\n              44.3\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d823","contributors":{"authors":[{"text":"Brown, Stuart G.","contributorId":88710,"corporation":false,"usgs":true,"family":"Brown","given":"Stuart","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":143150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newcomb, Reuben Clair","contributorId":37712,"corporation":false,"usgs":true,"family":"Newcomb","given":"Reuben","email":"","middleInitial":"Clair","affiliations":[],"preferred":false,"id":143149,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52237,"text":"ofr6241 - 1962 - Interim geological investigations in the U12e.04 tunnel, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"ofr6241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-41","title":"Interim geological investigations in the U12e.04 tunnel, Nevada Test Site, Nye County, Nevada","docAbstract":"The Ul2e.04 tunnel is a part of the Ul2e tunnel system, which has been driven southwestward beneath Rainier Mesa in the northern part of the Nevada Test Site. The Ul2e.04 tunnel was driven about S. 15? W. in zeolitic tuff of subunits E and F of Tunnel Bed W near the top of the lower member of the Indian Trail Formation (upper Miocene or lower Pliocene). Dolomite of Paleozoic age lies about 915 feet below the end of the tunnel; vertical cover over the end of the tunnel to the surface of Rainier Mesa is about 1,390 feet. The tuffs in the tunnel strike almost north-south and dip to the west. There are several normal northwest-trending faults with vertical to steep dips and small displacements. The predominant joint set strikes northwest and dips mostly vertically or steeply to the northeast. \r\n\r\nPetrographically and chemically the tuffs in the U12e.04 tunnel are similar to other tuffs of the Indian Trail Formation from the Nevada Test Site, The tuffs in the tunnel have an average porosity of 38.6 percent, dry bulk density of 1.46 g/cc (grams per cubic centimeter), grain density of 2.38 g/cc, water content of 20.7 percent by weight. \r\n\r\nShore hardness of 25.1, and unconfined compressive strength of 4,400 psi (pounds per square inch). Separately, the tuffs from the chamber at the end of the tunnel have an average porosity of 36.8 percent, dry bulk density of 1.51 g/cc, grain density of 2.38 g/cc, water content of 20.0 percent by weight, Shore hardness of 27.2 and unconfined compressive strength of 4,500 psi. \r\n\r\nAn NX-size cored hole was drilled from the surface of Rainier Mesa into the Ul2e.04 chamber.","language":"ENGLISH","doi":"10.3133/ofr6241","usgsCitation":"Emerick, W., Dickey, D., and McKeown, F.A., 1962, Interim geological investigations in the U12e.04 tunnel, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 62-41, 27 p., https://doi.org/10.3133/ofr6241.","productDescription":"27 p.","costCenters":[],"links":[{"id":175097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0041/report-thumb.jpg"},{"id":86759,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86760,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d482","contributors":{"authors":[{"text":"Emerick, W.L.","contributorId":64668,"corporation":false,"usgs":true,"family":"Emerick","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":245018,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickey, D.D.","contributorId":15612,"corporation":false,"usgs":true,"family":"Dickey","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":245017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":245019,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52246,"text":"ofr6258 - 1962 - Gravity survey of the Nevada Test Site and vicinity, Nye, Lincoln, and Clark Counties, Nevada--interim report","interactions":[],"lastModifiedDate":"2017-08-29T15:59:33","indexId":"ofr6258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-58","title":"Gravity survey of the Nevada Test Site and vicinity, Nye, Lincoln, and Clark Counties, Nevada--interim report","docAbstract":"<p>The gravity survey of the Nevada Test Site and contiguous areas of southern Nevada and southeastern California (fig. 1) has been made by the U.S. Geological Survey on behalf of the U.S. Atomic Energy Commission.</p><p>The objective of this study is to delineate and interpret gravity anomalies and regional trends so that the configuration and depth of the buried erosional surface of the Paleozoic rocks may be determined. This buried surface is of utmost importance in understanding the geologic history of the Nevada Test Site region, the thickness and distribution of the overlying volcanic rocks and alluvium, and the movement of ground water. The Paleozoic rocks cause positive gravity anomalies where they outcrop or occur near the surface and negative anomalies where they are buried in valleys or capped by low-density Tertiary volcanic rocks. </p><p>Gravity trends which extend over the entire area provide a basis for computing the regional gravity gradient. The regional gravity gradient must be removed from the data for geologic interpretation of the paleotopographic surface in any limited area. </p><p>Knowledge of the thickness of low-density material overlying the paleotopographic surface is useful in several ways. Proposed&nbsp;underground test sites, such as drill holes and tunnels, may be evaluated in terms of rock unit thickness and alluvial cover requirements. Recent work by the Water Resources Division of the U.S. Geological Survey has demonstrated ground-water movement through the Paleozoic rocks in the vicinity of the Nevada Test Site. Therefore, knowledge of the position of buried Paleozoic rocks is important in evaluating (a) the rate and direction of flow of the ground water, (b) ground-water supplies for domestic and industrial uses, and (c) the possibility of radioactive contamination of ground water. Finally, regional gravity trends and paleotopography are useful in working out the structural history of the area in connection with geologic studies now in progress. </p><p>The purpose of this interim report is to present the major part of the gravity data obtained as of December 31, 1961. The data are presented as a complete Bouguer gravity anomaly map. Although the gravity contours are somewhat generalized because the map has a scale of 1:250,000 and a contour interval of 5 milligals, the largest anomalies are adequately delineated. </p><p>Preliminary results of this gravity survey have been reported by Wilmarth and others, 1960, and by Diment and others, 1959 and 1960.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6258","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission,","usgsCitation":"Healy, D.L., and Miller, C., 1962, Gravity survey of the Nevada Test Site and vicinity, Nye, Lincoln, and Clark Counties, Nevada--interim report: U.S. Geological Survey Open-File Report 62-58, Report: 34 p.; 3 Figures: 19.52 x 25.07 inches or smaller, https://doi.org/10.3133/ofr6258.","productDescription":"Report: 34 p.; 3 Figures: 19.52 x 25.07 inches or smaller","costCenters":[],"links":[{"id":86763,"rank":401,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1962/0058/plate-2.pdf","text":"Figure 3","size":"2.28 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 3"},{"id":86764,"rank":402,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1962/0058/plate-3.pdf","text":"Figure 5","size":"1.60 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 5"},{"id":86765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0058/report.pdf","text":"Report","size":"514.56 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":175257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0058/report-thumb.jpg"},{"id":86762,"rank":400,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1962/0058/plate-1.pdf","text":"Figure 2","size":"3.27 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 2"}],"country":"United States","state":"Nevada","county":"Clark County, Lincoln County, Nye County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.191162109375,\n              36.20882309283712\n            ],\n            [\n              -114.06005859375,\n              36.20882309283712\n            ],\n            [\n              -114.06005859375,\n              38.71123253895224\n            ],\n            [\n              -117.191162109375,\n              38.71123253895224\n            ],\n            [\n              -117.191162109375,\n              36.20882309283712\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671fd1","contributors":{"authors":[{"text":"Healy, D. L.","contributorId":99204,"corporation":false,"usgs":true,"family":"Healy","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":245035,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, C.H.","contributorId":19148,"corporation":false,"usgs":true,"family":"Miller","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":245034,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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