{"pageNumber":"6712","pageRowStart":"167775","pageSize":"25","recordCount":184884,"records":[{"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":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":3964,"text":"cir480 - 1963 - Preparation of water samples for carbon-14 dating","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir480","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"480","title":"Preparation of water samples for carbon-14 dating","docAbstract":"For most natural water, a large sample is required to provide the 3 grams of carbon needed for a carbon-14 determination. A field procedure for isolating total dissolved-carbonate species is described. Carbon dioxide gas is evolved by adding sulfuric acid to the water sample; the gas is then collected in a sodium hydroxide trap by recycling in a closed system. The trap is then transported to the dating laboratory where the carbon-14 is counted.","language":"ENGLISH","publisher":"United States Geological Survey,","doi":"10.3133/cir480","usgsCitation":"Feltz, H., and Hanshaw, B.B., 1963, Preparation of water samples for carbon-14 dating: U.S. Geological Survey Circular 480, iii, 3 p. :ill. ;27 cm., https://doi.org/10.3133/cir480.","productDescription":"iii, 3 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":123205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1963/0480/report-thumb.jpg"},{"id":31050,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1963/0480/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658935","contributors":{"authors":[{"text":"Feltz, H.R.","contributorId":49341,"corporation":false,"usgs":true,"family":"Feltz","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":147909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hanshaw, Bruce B.","contributorId":47350,"corporation":false,"usgs":true,"family":"Hanshaw","given":"Bruce","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":147908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4120,"text":"cir476 - 1963 - Principal lakes of the United States","interactions":[],"lastModifiedDate":"2018-02-14T16:18:45","indexId":"cir476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"476","title":"Principal lakes of the United States","docAbstract":"<p>The United States has about 250 fresh-water lakes that are known to have surface areas of 10 square miles or more. Nearly 100 of these are in Alaska, and 100 in Minnesota, Wisconsin, Michigan, New York,, and Maine.</p>\n<p>Thirty-four fresh-water lakes, exclusive of the Great Lakes, are known to have maximum depths of 250 feet or more. Twenty of these are in Alaska, and Alaska undoubtedly has more lakes of that depth which have not been sounded.</p>\n<p>The amount of water stored in natural lakes even exclusive of the Great Lakes is much greater than the amount stored in artificial reservoirs. With the exception of the Great Lakes, however, the economic value of natural lakes is surpassed by that of artificial reservoirs. Natural lakes are best known for the recreational advantages they afford.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir476","usgsCitation":"Bue, C.D., 1963, Principal lakes of the United States: U.S. Geological Survey Circular 476, iii, 22 p., https://doi.org/10.3133/cir476.","productDescription":"iii, 22 p.","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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