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,{"id":13902,"text":"ofr6338 - 1963 - Principal facts for gravity stations in the San Francisco Bay area, California","interactions":[{"subject":{"id":13902,"text":"ofr6338 - 1963 - Principal facts for gravity stations in the San Francisco Bay area, California","indexId":"ofr6338","publicationYear":"1963","noYear":false,"title":"Principal facts for gravity stations in the San Francisco Bay area, California"},"predicate":"SUPERSEDED_BY","object":{"id":70046224,"text":"70046224 - 1971 - Principal Facts for Gravity Stations in the San Francisco Bay Area, California","indexId":"70046224","publicationYear":"1971","noYear":false,"title":"Principal Facts for Gravity Stations in the San Francisco Bay Area, California"},"id":1}],"supersededBy":{"id":70046224,"text":"70046224 - 1971 - Principal Facts for Gravity Stations in the San Francisco Bay Area, California","indexId":"70046224","publicationYear":"1971","noYear":false,"title":"Principal Facts for Gravity Stations in the San Francisco Bay Area, California"},"lastModifiedDate":"2019-03-14T13:17:44","indexId":"ofr6338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-38","title":"Principal facts for gravity stations in the San Francisco Bay area, California","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6338","usgsCitation":"Greve, G.M., and Clement, W.G., 1963, Principal facts for gravity stations in the San Francisco Bay area, California: U.S. Geological Survey Open-File Report 63-38, 26 p., https://doi.org/10.3133/ofr6338.","productDescription":"26 p.","costCenters":[],"links":[{"id":145252,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0038/report-thumb.jpg"},{"id":362070,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"San Francisco Bay Area","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667a6c","contributors":{"authors":[{"text":"Greve, Gordon M.","contributorId":7287,"corporation":false,"usgs":true,"family":"Greve","given":"Gordon","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clement, William G.","contributorId":32536,"corporation":false,"usgs":true,"family":"Clement","given":"William","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":168606,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14075,"text":"ofr6345 - 1963 - Preliminary interpretation of an aeromagnetic survey in north-central Iowa","interactions":[],"lastModifiedDate":"2024-07-26T22:16:42.14486","indexId":"ofr6345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-45","title":"Preliminary interpretation of an aeromagnetic survey in north-central Iowa","docAbstract":"<p>Publication of Lyons' gravity map of the United States in 1950 focused attention on a spectacular geophysical feature now generally referred to as the \"midcontinent gravity high.\" This feature, the largest gravity maximum in North America, was discovered and later detailed by geophysicists at the University of Wisconsin (Woollard, 1943, 1951) and Thiel (1956). Their work reveals an essentially continuous large positive gravity anomaly extending southwestward for 800 miles from Lake Superior to the Salina Basin in Kansas. The midcontinent gravity high reaches its maximum intensity in central Iowa where the Bouguer anomaly ranges from -100 to 60 milligals.</p><p>In September-October 1961, the U. S. Geological Survey made a 5,000 square mile aeromagnetic survey in north-central Iowa in cooperation with the Iowa Geological Survey. Objectives of the investigation were to prepare and interpret a detailed aeromagnetic contour map for part of the midcontinent gravity high in Iowa. Analysis of the magnetic data could be expected to yield estimates of local thickness of the Paleozoic-Mesozoic sedimentary section and provide a basis for informed speculation about the character, configuration, and distribution of the Precambrian rocks. Such information would have obvious scientific and possible economic value in an area covered by glacial till and for which little deep subsurface knowledge was available. Interpretation of the Indiana aeromagnetic survey (Henderson and Zietz, 1958) had previously demonstrated that aeromagnetic data from the central stable region of North America would provide a significant amount of geologic information.</p><p>The 5,000 square mile area surveyed in 1961 has been combined with a previously unpublished 600 square mile aeromagnetic survey made in 1953, centered on Manson, Pocahontas Co., Iowa. The combined area is shown as the patterned area in figure 1. The unpatterned area outlined on this same figure is the additional 10,000 square mile cooperative aeromagnetic survey made in the summer of 1962 to complete coverage of the midcontinent gravity high in Iowa.</p><p>The primary purpose of this report is to make the 1953 and 1961 aeromagnetic data available to the public in advance of more formal publication. Only salient magnetic features are discussed in this preliminary presentation and in a second report on results obtained during the 1962 flying. A more complete interpretation of the entire aeromagnetic survey will be prepared.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6345","collaboration":"Prepared in cooperation with the Iowa Geological Survey","usgsCitation":"Henderson, J.R., White, W., and Zietz, I., 1963, Preliminary interpretation of an aeromagnetic survey in north-central Iowa: U.S. Geological Survey Open-File Report 63-45, Report: 27 p.; 4 Figures: 36.03 x 23.90 inches or smaller, https://doi.org/10.3133/ofr6345.","productDescription":"Report: 27 p.; 4 Figures: 36.03 x 23.90 inches or smaller","costCenters":[],"links":[{"id":431530,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431529,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431528,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431527,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0045/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431526,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410197,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8045.htm","linkFileType":{"id":5,"text":"html"}},{"id":146687,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0045/report-thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"north-central Iowa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -95,\n              43.5\n            ],\n            [\n              -95,\n              42.333\n            ],\n            [\n              -92.5,\n              42.333\n            ],\n            [\n              -92.5,\n              43.5\n            ],\n            [\n              -95,\n              43.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69742d","contributors":{"authors":[{"text":"Henderson, John Richard","contributorId":52975,"corporation":false,"usgs":true,"family":"Henderson","given":"John","email":"","middleInitial":"Richard","affiliations":[],"preferred":false,"id":168890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Walter S.","contributorId":34492,"corporation":false,"usgs":true,"family":"White","given":"Walter S.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":168889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":168891,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14039,"text":"ofr6344 - 1963 - Geology of the Pikes Peak Granite and associated ore deposits, Lake George beryllium area, Park County, Colorado","interactions":[],"lastModifiedDate":"2025-06-06T16:38:32.726154","indexId":"ofr6344","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-44","title":"Geology of the Pikes Peak Granite and associated ore deposits, Lake George beryllium area, Park County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6344","usgsCitation":"Hawley, C.C., 1963, Geology of the Pikes Peak Granite and associated ore deposits, Lake George beryllium area, Park County, Colorado: U.S. Geological Survey Open-File Report 63-44, Report: iii, 291 p.; 12 Plates: 38.87 x 28.12 inches or smaller, https://doi.org/10.3133/ofr6344.","productDescription":"Report: iii, 291 p.; 12 Plates: 38.87 x 28.12 inches or 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C.","contributorId":102070,"corporation":false,"usgs":true,"family":"Hawley","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":168835,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24763,"text":"ofr63128 - 1963 - Water for the proposed West Side Campground site, Rocky Mountain National Park, Colorado","interactions":[],"lastModifiedDate":"2025-03-20T19:46:49.821101","indexId":"ofr63128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-128","title":"Water for the proposed West Side Campground site, Rocky Mountain National Park, Colorado","docAbstract":"<p>At the request of the U.S. National Park Service, the U S. Geological Survey investigated the possibility of obtaining a water supply at the proposed West Side Campground Site in the western part of Rocky Mountain Park (fig. 1).</p><p>The first field investigation of the site, made July 24, 1962, revealed two possibilities for obtaining a water supply: a well or wells tapping terrace deposits or diverting part of the flow of the North Fork of the Colorado River Each possibility was investigated considering the location of the source with respect to the proposed point or points of use, adequacy of quantity and chemical quality of water, reliability as a perennial source, and problems of development involving topography and earth materials. Because a ground-water source was preferred by Park Service officials and the ground-water possibilities seemed to be promising, the remaining study effort was devoted entirely to the appraisal of the ground-water potential. Work in and near the proposed campground site consisted of field observation and mapping of surface geologic and hydrologic features, selection of a drilling site for a test well, supervision of the drilling of the test well, and testing the yield of the well.</p><p>The assistance of Robert Haraden and Dave Spivey, National Park Service, is gratefully acknowledged. Thanks are given to Earl Reaksecker, driller, for his excellent cooperation during the drilling of the test well.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr63128","issn":"0094-9140","collaboration":"Prepared for U.S. National Park Service Administrative Report","usgsCitation":"Voegeli, P.T., 1963, Water for the proposed West Side Campground site, Rocky Mountain National Park, Colorado: U.S. Geological Survey Open-File Report 63-128, Report: iv, 22 p.: 6 Plates: 14.99 x 24.80 inches or smaller, https://doi.org/10.3133/ofr63128.","productDescription":"Report: iv, 22 p.: 6 Plates: 14.99 x 24.80 inches or smaller","costCenters":[],"links":[{"id":483602,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0128/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":483599,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0128/figure-3.pdf","text":"Figure 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,{"id":24759,"text":"ofr63125 - 1963 - Floods of March-May 1963 in Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"ofr63125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-125","title":"Floods of March-May 1963 in Hawaii","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr63125","issn":"0094-9140","usgsCitation":"Vaudrey, W.C., 1963, Floods of March-May 1963 in Hawaii: U.S. Geological Survey Open-File Report 63-125, 65 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr63125.","productDescription":"65 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":158267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfada","contributors":{"authors":[{"text":"Vaudrey, Walter C.","contributorId":24770,"corporation":false,"usgs":true,"family":"Vaudrey","given":"Walter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":192510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52350,"text":"ofr6395 - 1963 - Progress on water resource investigations in the Lower Colorado River area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr6395","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-95","title":"Progress on water resource investigations in the Lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6395","usgsCitation":"McDonald, C.C., 1963, Progress on water resource investigations in the Lower Colorado River area: U.S. Geological Survey Open-File Report 63-95, 4 p., https://doi.org/10.3133/ofr6395.","productDescription":"4 p.","costCenters":[],"links":[{"id":179010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885a5","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":245197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52310,"text":"ofr6317 - 1963 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","interactions":[{"subject":{"id":52310,"text":"ofr6317 - 1963 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","indexId":"ofr6317","publicationYear":"1963","noYear":false,"title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047481,"text":"70047481 - 1964 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","indexId":"70047481","publicationYear":"1964","noYear":false,"title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida"},"id":1}],"supersededBy":{"id":70047481,"text":"70047481 - 1964 - Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","indexId":"70047481","publicationYear":"1964","noYear":false,"title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida"},"lastModifiedDate":"2013-08-07T13:48:17","indexId":"ofr6317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-17","title":"Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr6317","usgsCitation":"Clark, W., Musgrove, R., Menke, C., and Cagle, J., 1963, Water-resources data for Alachua, Bradford, Clay, and Union Counties, Florida: U.S. Geological Survey Open-File Report 63-17, 162 p., https://doi.org/10.3133/ofr6317.","productDescription":"162 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":177943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f82","contributors":{"authors":[{"text":"Clark, W.E.","contributorId":68694,"corporation":false,"usgs":true,"family":"Clark","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":245126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, R.H.","contributorId":31051,"corporation":false,"usgs":true,"family":"Musgrove","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":245124,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, C.G.","contributorId":20823,"corporation":false,"usgs":true,"family":"Menke","given":"C.G.","affiliations":[],"preferred":false,"id":245123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, J.W. Jr.","contributorId":63875,"corporation":false,"usgs":true,"family":"Cagle","given":"J.W.","suffix":"Jr.","affiliations":[],"preferred":false,"id":245125,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":52327,"text":"ofr6343 - 1963 - New advances in water-resources research","interactions":[],"lastModifiedDate":"2012-02-02T00:11:33","indexId":"ofr6343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-43","title":"New advances in water-resources research","language":"ENGLISH","doi":"10.3133/ofr6343","usgsCitation":"Hastings, W., 1963, New advances in water-resources research: U.S. Geological Survey Open-File Report 63-43, 21 p., https://doi.org/10.3133/ofr6343.","productDescription":"21 p.","costCenters":[],"links":[{"id":177596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6977e6","contributors":{"authors":[{"text":"Hastings, W.W.","contributorId":11203,"corporation":false,"usgs":true,"family":"Hastings","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":245167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52328,"text":"ofr6347 - 1963 - Geology of the Terra Bella-Lost Hills Area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2025-02-24T14:51:29.508244","indexId":"ofr6347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-47","title":"Geology of the Terra Bella-Lost Hills Area, San Joaquin Valley, California","docAbstract":"<p>The Terra Bella-Lost Hills area in the southeastern part of the San Joaquin Valley includes about 1,700 square miles of Kings, Tulare and Kern Counties. This part of the San Joaquin Valley has mild winters, long hot summers, and little precipitating, almost all of which occurs during the fall and winter months. The area is a basin of interior drainage and the streams are tributary to Tulare Lake.</p><p>The Terra Bella-Lost Hills area is characterized by dissected uplands, low alluvial plains and fans, river-flood plains and channels, and overflow land. and. lake bottoms.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6347","usgsCitation":"Hilton, G., Klausing, R., and Kunkel, F., 1963, Geology of the Terra Bella-Lost Hills Area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 63-47, Report:158 p.; 28 Plates: 52.98 x 36.93 inches or smaller, https://doi.org/10.3133/ofr6347.","productDescription":"Report:158 p.; 28 Plates: 52.98 x 36.93 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cabd","contributors":{"authors":[{"text":"Hilton, G.S.","contributorId":52652,"corporation":false,"usgs":true,"family":"Hilton","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":245169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klausing, R.L.","contributorId":73205,"corporation":false,"usgs":true,"family":"Klausing","given":"R.L.","affiliations":[],"preferred":false,"id":245170,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":245168,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57724,"text":"ofr63147 - 1963 - Tests of crest-stage gage intakes","interactions":[],"lastModifiedDate":"2026-01-26T16:54:15.528383","indexId":"ofr63147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-147","title":"Tests of crest-stage gage intakes","docAbstract":"<p>Various types of c rest-stage gages have been used by the Geological Survey. Most installations consist of a vertically mounted metal pipe, a wooden rod, an intake device, and a small amount of granulated cork. These gages are placed where elevations of flood crests are desired. Water rising and then falling in the gage leaves a high-water mark of granulated cork on the wooden rod. The elevation of this mark can be determined at a date subsequent to the date of the crest.</p><p>It has been found that the high-water mark left on the rod may not represent the true elevation of the flood crest in the stream at the gage site. The difference between the true elevation of the crest at the gage and the recorded elevation will be designated drawdown if the recorded elevation is less than the true elevation, or pileup if the recorded elevation is greater than the true elevation. Tests of drawdown and pileup effects have been made in the past by Survey personnel and others. (See p. 8.) These investigations have sometimes brought forth conflicting results, probably due to the varied conditions under which the gages were tested.</p><p>The purpose of this investigation was (1) to determine the pileup and drawdown characteristics of the intakes now being used by the Survey and (2) to design a better intake if existing models were found unsuitable. It was further prescribed that any new design that might result should be easily fabricated from standard pipe fittings, and should be unaffected by pileup or drawdown in excess of 0.1 foot for velocities up to about 8 feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr63147","usgsCitation":"Carter, J.R., and Gamble, C.R., 1963, Tests of crest-stage gage intakes: U.S. Geological Survey Open-File Report 63-147, 10 p., https://doi.org/10.3133/ofr63147.","productDescription":"10 p.","numberOfPages":"10","costCenters":[],"links":[{"id":499023,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184244,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0147/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6845d0","contributors":{"authors":[{"text":"Carter, Jack R.","contributorId":71632,"corporation":false,"usgs":true,"family":"Carter","given":"Jack","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":257644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":257643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52347,"text":"ofr6392 - 1963 - Aquifer-test compilation for the Upper Santa Ana Valley area, San Bernardino County, California","interactions":[{"subject":{"id":52347,"text":"ofr6392 - 1963 - Aquifer-test compilation for the Upper Santa Ana Valley area, San Bernardino County, California","indexId":"ofr6392","publicationYear":"1963","noYear":false,"title":"Aquifer-test compilation for the Upper Santa Ana Valley area, San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":57731,"text":"ofr64168 - 1964 - Aquifer-test compilation for the Los Angeles and Santa Ana Regions, California","indexId":"ofr64168","publicationYear":"1964","noYear":false,"title":"Aquifer-test compilation for the Los Angeles and Santa Ana Regions, California"},"id":1}],"supersededBy":{"id":57731,"text":"ofr64168 - 1964 - Aquifer-test compilation for the Los Angeles and Santa Ana Regions, California","indexId":"ofr64168","publicationYear":"1964","noYear":false,"title":"Aquifer-test compilation for the Los Angeles and Santa Ana Regions, California"},"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr6392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-92","title":"Aquifer-test compilation for the Upper Santa Ana Valley area, San Bernardino County, California","language":"ENGLISH","doi":"10.3133/ofr6392","usgsCitation":"McClelland, E., 1963, Aquifer-test compilation for the Upper Santa Ana Valley area, San Bernardino County, California: U.S. Geological Survey Open-File Report 63-92, 28 p., https://doi.org/10.3133/ofr6392.","productDescription":"28 p.","costCenters":[],"links":[{"id":178916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679eb6","contributors":{"authors":[{"text":"McClelland, E.J.","contributorId":54280,"corporation":false,"usgs":true,"family":"McClelland","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":245193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52304,"text":"ofr636 - 1963 - Preliminary report on the geology and hydrology of Mortandad Canyon near Los Alamos, New Mexico, with reference to disposal of liquid low-level radioactive waste","interactions":[],"lastModifiedDate":"2012-02-02T00:11:33","indexId":"ofr636","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"63-6","title":"Preliminary report on the geology and hydrology of Mortandad Canyon near Los Alamos, New Mexico, with reference to disposal of liquid low-level radioactive waste","docAbstract":"The U.S. Geological Survey, in cooperation with the U.S. Atomic Energy Commission and the Los Alamos Scientific Laboratory, selected the upper part of Mortandad Canyon near Los Alamos, New Mexico for a site for disposal of treated liquid low-level radioactive waste. This report summarizes the part of a study of the geology and hydrology that was done from October 1960 through June 1961. Additional work is being continued.\r\n\r\nMortandad Canyon is a narrow east-southeast-trending canyon about 9? miles long that heads on the central part of the Pajarito Plateau at an altitude of about 7,340 feet. The canyon is tributary to the Rio Grande. The drainage area of the part of Mortandad Canyon that was investigated is about 2 square miles, and the total drainage area is about 4.9 square miles.\r\n\r\nThe Pajarito Plateau is capped by the Bandelier Tuff of Pleistocene age. Mortandad Canyon is cut in the Bandelier, and alluvium covers the floor of the canyon to depths ranging from less than 1 foot to as much as 100 feet. The Bandelier is underlain by silt, sand, conglomerate, and interbedded basalt of the Santa Fe Group of Miocene, Pliocene, and Pleistocene(?) age. Some ground water is perched in the alluvium in the canyon; however, the top of the main aquifer is in the Santa Fe Group at a depth of about 990 feet below the canyon floor.\r\n\r\nJoints in the Bandelier Tuff probably were caused by shrinkage of the tuff during cooling. The joints range in width from hairline cracks to fissures several inches wide. Water can infiltrate along the open joints where the Bandelier is at the surface; however, soil, alluvial fill, and autochthonous clay inhibit infiltration on the tops of mesas and probably in the alluvium-floored canyons also.\r\n\r\nThirty-three test holes, each less than 100 feet deep, were drilled in 10 lies across Mortandad Canyon from the western margin of the study area to just west of the Los Alamos-Santa Fe County line. Ten of the holes were cased for observation wells to measure water levels and collect water samples from the alluvium. Twenty-three of the holes were cased to seal out water and were used as access tubes to accommodate a neutron-neutron probe for determining the moisture content of the alluvium and tuff.\r\n\r\nThe source of recharge for the perched ground-water body in the alluvium in Mortandad Canyon is the precipitation in the drainage area of the canyon. During the winter of 1960-61, a snowpack 1-2 feet thick accumulated in the narrow shaded upper part of the canyon. The alluvium below the snowpack received some recharge because of diurnal melting during the winter. In March 1961 the snowmelt water saturated most of the thin alluvium in the upper part of the canyon, and a surface stream began to flow on the alluvium. The maximum flow of the stream was about 250 gpm (gallons per minute). Water from the stream infiltrated the alluvium at the front of the stream and in the reach upstream from the front. A ground-water mound was formed beneath the channel by water infiltrating from the stream. The front of the stream and the front of the ground-water mound advanced eastward to about the middle of the area studied. From this point eastward, the alluvium was thick enough to absorb and transmit the amount of flow in 1961. Late in April the front of the stream retreated, and by the first of May the flow stopped. During and after this period the ground-water mound decayed, and ground-water levels declined in the upper part of the canyon as water drained into the channel and downgradient through the alluvium.\r\n\r\nThe amount of recharge was small in the wide lower part of the canyon during the period of study. The rise in ground-water levels and the increase in moisture content of the alluvium in the lower part of the canyon indicate that water moved downgradient by underflow through the alluvium from the recharge area in the upper part of the canyon. Moisture measurements indicate that only a little water moved into the underlyin","language":"ENGLISH","doi":"10.3133/ofr636","usgsCitation":"Baltz, E., Abrahams, J., and Purtyman, W., 1963, Preliminary report on the geology and hydrology of Mortandad Canyon near Los Alamos, New Mexico, with reference to disposal of liquid low-level radioactive waste: U.S. Geological Survey Open-File Report 63-6, 105 p., https://doi.org/10.3133/ofr636.","productDescription":"105 p.","costCenters":[],"links":[{"id":177864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0006/report-thumb.jpg"},{"id":86790,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0006/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86791,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0006/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86792,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0006/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86793,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0006/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86794,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0006/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1963/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c900","contributors":{"authors":[{"text":"Baltz, E.H.","contributorId":67146,"corporation":false,"usgs":true,"family":"Baltz","given":"E.H.","affiliations":[],"preferred":false,"id":245111,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abrahams, J.H. Jr.","contributorId":47022,"corporation":false,"usgs":true,"family":"Abrahams","given":"J.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":245110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Purtyman, W.D.","contributorId":95559,"corporation":false,"usgs":true,"family":"Purtyman","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":245112,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41127,"text":"ofr6328 - 1963 - Preliminary geologic map of part of the Rapid City East quadrangle, South Dakota","interactions":[{"subject":{"id":41127,"text":"ofr6328 - 1963 - Preliminary geologic map of part of the Rapid City East quadrangle, South Dakota","indexId":"ofr6328","publicationYear":"1963","noYear":false,"title":"Preliminary geologic map of part of the Rapid City East quadrangle, South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":63245,"text":"gq986 - 1972 - Geologic map of the Rapid City East quadrangle, Pennington County, South Dakota","indexId":"gq986","publicationYear":"1972","noYear":false,"title":"Geologic map of the Rapid City East quadrangle, Pennington County, South Dakota"},"id":1}],"supersededBy":{"id":63245,"text":"gq986 - 1972 - Geologic map of the Rapid City East quadrangle, Pennington County, South Dakota","indexId":"gq986","publicationYear":"1972","noYear":false,"title":"Geologic map of the Rapid City East quadrangle, Pennington County, South 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