{"pageNumber":"1790","pageRowStart":"44725","pageSize":"25","recordCount":46619,"records":[{"id":70175495,"text":"70175495 - 1973 - Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971","interactions":[],"lastModifiedDate":"2016-08-15T14:33:51","indexId":"70175495","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175495","usgsCitation":"Massey, B., 1973, Annual compilation and analysis of hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1971: Open-File Report, 84 p., https://doi.org/10.3133/70175495.","productDescription":"84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326491,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7b2e4b03bcb0102e839","contributors":{"authors":[{"text":"Massey, B.C.","contributorId":102483,"corporation":false,"usgs":true,"family":"Massey","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":645499,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010264,"text":"70010264 - 1973 - Production of superheated steam from vapor-dominated geothermal reservoirs","interactions":[],"lastModifiedDate":"2020-12-29T14:15:38.320431","indexId":"70010264","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1828,"text":"Geothermics","active":true,"publicationSubtype":{"id":10}},"title":"Production of superheated steam from vapor-dominated geothermal reservoirs","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Vapor-dominated geothermal systems such as Larderello, Italy, The Geysers, California, and Matsukawa, Japan yield dry or superheated steam when exploited. Models for these systems are examined along with production data and the thermodynamic properties of water, steam and rock. It is concluded that these systems initially consist of a water and steam filled reservoir, a water-saturated cap rock, and a water or brine-saturated deep reservoir below a water table. Most liquid water in all parts of the system is relatively immobilized in small pores and crevices; steam dominates the large fractures and voids of the reservoir and is the continuous, pressure-controlling phase. With production, the pressure is lowered and the liquid water boils, causing massive transfer of heat from the rock and its eventual drying. Passage of steam through already dried rock produces superheating. After an initial vaporization of liquid water in the reservoir, the decrease in pressure produces increased boiling below the deep water table. With heavy exploitation, boiling extends deeper into hotter rock and the temperature of the steam increases. This model explains most features of the published production behavior of these systems and can be used to guide exploitation policies.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6505(73)90022-9","issn":"03756505","usgsCitation":"Truesdell, A., and White, D., 1973, Production of superheated steam from vapor-dominated geothermal reservoirs: Geothermics, v. 2, no. 3-4, p. 154-173, https://doi.org/10.1016/0375-6505(73)90022-9.","productDescription":"20 p.","startPage":"154","endPage":"173","numberOfPages":"20","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":480661,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://repositorio.unal.edu.co/handle/unal/79530","text":"External Repository"},{"id":218710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8de7e4b0c8380cd7eed4","contributors":{"authors":[{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":358477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, D. E.","contributorId":20729,"corporation":false,"usgs":false,"family":"White","given":"D. E.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":358476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010228,"text":"70010228 - 1973 - Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","interactions":[],"lastModifiedDate":"2025-02-28T16:52:00.529379","indexId":"70010228","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander","docAbstract":"<div class=\"u-margin-s-bottom\">The inorganic chemical investigation added in August 1972 to the Viking Lander scientific package will utilize an energy-dispersive X-ray fluorescence spectrometer in which four sealed, gas-filled proportional counters will detect X-rays emitted from samples of the Martian surface materials irradiated by X-rays from radioisotope sources (<sup>55</sup>Fe and<span>&nbsp;</span><sup>109</sup>Cd). The output of the proportional counters will be subjected to pulse-height analysis by an on-board step-scanning single-channel analyzer with adjustable counting periods. The data will be returned to Earth, via the Viking Orbiter relay system, and the spectra constructed, calibrated, and interpreted here. The instrument is inside the Lander body, and samples are to be delivered to it by the Viking Lander Surface Sampler. Calibration standards are an integral part of the instrument.</div><div class=\"u-margin-s-bottom\">The results of the investigation will characterize the surface materials of Mars as to elemental composition with accuracies ranging from a few tens of parts per million (at the trace-element level) to a few percent (for major elements) depending on the element in question. Elements of atomic number 11 or less are determined only as a group, though useful estimates of their individual abundances maybe achieved by indirect means. The expected radiation environment will not seriously hamper the measurements. Based on the results, inferences can be drawn regarding (1) the surface mineralogy and lithology; (2) the nature of weathering processes, past and present, and the question of equilibrium between the atmosphere and the surface; and (3) the extent and type of differentiation that the planet has undergone.</div><div class=\"u-margin-s-bottom\">The Inorganic Chemical Investigation supports and is supported by most other Viking Science investigations.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(73)90048-1","issn":"00191035","usgsCitation":"Toulmin, P., Baird, A.K., Clark, B.C., Keil, K., and Rose, H.J., 1973, Inorganic chemical investigation by x-ray fluorescence analysis: The Viking Mars Lander: Icarus, v. 20, no. 2, p. 153-178, https://doi.org/10.1016/0019-1035(73)90048-1.","productDescription":"26 p.","startPage":"153","endPage":"178","numberOfPages":"26","costCenters":[],"links":[{"id":219294,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3c08e4b0c8380cd629f4","contributors":{"authors":[{"text":"Toulmin, P. III","contributorId":81244,"corporation":false,"usgs":true,"family":"Toulmin","given":"P.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":358368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baird, A. K.","contributorId":65148,"corporation":false,"usgs":true,"family":"Baird","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":358366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, B. C.","contributorId":39918,"corporation":false,"usgs":true,"family":"Clark","given":"B.","middleInitial":"C.","affiliations":[],"preferred":false,"id":358364,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keil, Klaus","contributorId":55955,"corporation":false,"usgs":true,"family":"Keil","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":358365,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rose, H. J. Jr.","contributorId":79465,"corporation":false,"usgs":true,"family":"Rose","given":"H.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":358367,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70009825,"text":"70009825 - 1973 - Comparison of the magnetic properties of glass from Luna 20 with similar properties of glass from the Apollo missions","interactions":[],"lastModifiedDate":"2020-12-29T20:02:02.886089","indexId":"70009825","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of the magnetic properties of glass from Luna 20 with similar properties of glass from the Apollo missions","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id8\" class=\"abstract author\"><div id=\"aep-abstract-sec-id9\"><p>Magnetic susceptibility measurements have been made on four glass spherules and fragments from the Luna 20 fines; two at 300°K and two from 300°K to 4°K. From these data the magnetic susceptibility extrapolated to infinite field, the magnetization at low fields and also the saturation magnetization at high fields, the Curie constant, the Weiss temperature, and the temperature-independent susceptibility were determined. Using a model previously proposed for the Apollo specimens, the Curie constant of the antiferromagnetic inclusions and a zero field splitting parameter were calculated for the same specimens. The data show the relatively low concentration of iron in all forms in these specimens. In addition, the Weiss temperature is lower than that measured for the Apollo specimens, and can be attributed almost entirely to the ligand field distortion about the Fe<sup>2+</sup><span>&nbsp;</span>ions in the glassy phase. The data further suggest that the Luna 20 specimens cooled more slowly than those of the Apollo missions, and that some of the antiferromagnetic inclusions in the glass may have crystallized from the glass during cooling.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90199-3","issn":"00167037","usgsCitation":"Senftle, F.E., Thorpe, A.N., Alexander, C., and Briggs, C., 1973, Comparison of the magnetic properties of glass from Luna 20 with similar properties of glass from the Apollo missions: Geochimica et Cosmochimica Acta, v. 37, no. 4, p. 1053-1062, https://doi.org/10.1016/0016-7037(73)90199-3.","productDescription":"10 p.","startPage":"1053","endPage":"1062","numberOfPages":"10","costCenters":[],"links":[{"id":219649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f8aee4b0c8380cd4d212","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357234,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorpe, A. N.","contributorId":53504,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":357235,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alexander, C.C.","contributorId":34256,"corporation":false,"usgs":true,"family":"Alexander","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":357233,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Briggs, C.L.","contributorId":33048,"corporation":false,"usgs":true,"family":"Briggs","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":357232,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36282,"text":"b1331C - 1973 - Petrography and stratigraphy of glacial drift, Mesabi-Vermilion Iron Range area, northeastern Minnesota","interactions":[],"lastModifiedDate":"2023-03-15T21:17:09.956941","indexId":"b1331C","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1331","chapter":"C","title":"Petrography and stratigraphy of glacial drift, Mesabi-Vermilion Iron Range area, northeastern Minnesota","docAbstract":"<p>Glacial deposits in the Mesabi-Vermilion Iron Range area consist of four major till units and associated glaciofluvial sediments. Particle-size data and pebble, heavy-mineral, clay-mineral, and percentage-soluble content were used in addition to field description of color and texture to describe and correlate the drift units.</p>\n<p>The lowermost till unit, basal till, occurs in only a small number of mines, but the mines are scattered across the entire Iron Range. The till is dark gray to dark greenish gray and brownish gray, sandy, silty, and calcareous. Pebbles are largely granitic and metamorphic rocks of local origin, but include limestone, dolomite, shale, basalt, felsite, agate, and gabbro. Clay-mineral content is largely illite. The age of the till is probably middle or early Wisconsin but could be pre-Wisconsin.</p>\n<p>The middle till unit, bouldery till, is the thickest and most widespread of the four tills. It is gray, yellow, red, orange, or brown, sandy, silty, noncalcareous and contains abundant cobbles and boulders. Pebbles are largely granitic and metamorphic rocks of local origin, but also include gabbro, basalt, and felsite in minor amounts. Montmorillonite is the most common clay mineral. Colored bouldery till below gray bouldery till may be a separate subunit distinguished largely on particle-size differences, but the overall characteristics are similar to the other bouldery till. The till was deposited by the Rainy lobe, which has a minimum age of 14,000 to 16,000 years before present.</p>\n<p>The uppermost, or surficial, tills were deposited contemporaneously by two minor sublobes of the Des Moines lobe about 12,000 years ago. Brown silty till occurs in the western and north-central part of the study area. It is light to medium brown, sandy, silty, and calcareous. Pebbles are largely granitic and metamorphic rocks of local origin, but include limestone, dolomite, shale, basalt, felsite, and gabbro. Clay-mineral content is largely mixed-layered montmorillonite and illite.</p>\n<p>Red clayey till occurs in the south-central part of the area. It is red to reddish brown, clayey, silty, and calcareous. Pebbles are similar to those in the brown silty till, but contain less limestone than the brown till.</p>\n<p>Glaciofluvial sediments are common between the various till units throughout the area, but are thickest near the east and near the west ends of the Iron Range.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/b1331C","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Winter, T.C., Cotter, R.D., and Young, H.L., 1973, Petrography and stratigraphy of glacial drift, Mesabi-Vermilion Iron Range area, northeastern Minnesota: U.S. Geological Survey Bulletin 1331, Document: iv, 41 p.; 2 Plates: 26.0 x 43.1 inches and 21.5 x 27.0 inches, https://doi.org/10.3133/b1331C.","productDescription":"Document: iv, 41 p.; 2 Plates: 26.0 x 43.1 inches and 21.5 x 27.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":64217,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1331c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1331c/report-thumb.jpg"},{"id":64218,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1331c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64219,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1331c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414263,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21438.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi-Vermilion Iron Range Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.793,\n              47.032\n            ],\n            [\n              -91.793,\n              47.975\n            ],\n            [\n              -93.775,\n              47.975\n            ],\n            [\n              -93.775,\n              47.032\n            ],\n            [\n              -91.793,\n              47.032\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688026","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216065,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":216066,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216064,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175502,"text":"70175502 - 1973 - Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972","interactions":[],"lastModifiedDate":"2016-08-15T14:53:47","indexId":"70175502","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175502","usgsCitation":"Ollman, R., 1973, Time of travel of solutes, field observations of water quality, and suspended-sediment data for stream reaches in the Trinity River Basin, Texas, July 31 to August 14, 1972: Open-File Report, 2 Sheets, https://doi.org/10.3133/70175502.","productDescription":"2 Sheets","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326499,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7cde4b03bcb0102e993","contributors":{"authors":[{"text":"Ollman, R.H.","contributorId":88806,"corporation":false,"usgs":true,"family":"Ollman","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":645511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175496,"text":"70175496 - 1973 - Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971","interactions":[],"lastModifiedDate":"2017-06-14T11:10:34","indexId":"70175496","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70175496","usgsCitation":"Steger, R., 1973, Annual compilation and analysis of hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1971: Open-File Report, 109 p., https://doi.org/10.3133/70175496.","productDescription":"109 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326492,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b2e7b2e4b03bcb0102e83d","contributors":{"authors":[{"text":"Steger, R.D.","contributorId":78008,"corporation":false,"usgs":true,"family":"Steger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":645500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045441,"text":"70045441 - 1973 - Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971","interactions":[],"lastModifiedDate":"2016-08-23T14:00:15","indexId":"70045441","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":128,"text":"Open-File Report","active":false,"publicationSubtype":{"id":2}},"title":"Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971","docAbstract":"<p>The U.S. Geological Survey, in cooperation with the Texas Water Development Board, began hydrologic studies in the Austin urban area in 1954. The objectives of this project are as follows: </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">1. To determine the effects of progressive urbanization on infiltration, rates of peak discharge, and rainfall-runoff relations in the Waller Creek watershed. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">2. To provide rainfall-and-runoff data from the rural Wilbarger Creek watershed to be used for comparative purposes in determining the effects of existing and progressive urbanization in the Waller Creek watershed. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">3. To provide applied research facilities for studies at the University of Texas at Austin. </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">The purpose of this report is to present rainfall-and-runoff data for the Waller Creek and Wilbarger Creek study areas for the 1971 water year (October 1, 1970, to September 30, 1971). </p><p style=\"padding-left: 30px;\" data-mce-style=\"padding-left: 30px;\">To facilitate the publication and distribution of this report at the earliest feasible time, certain material has been included that does not conform to the formal publication standards of the U.S. Geological Survey. </p>","language":"English","publisher":"U.S. Gelogical Survey, Water Resources Division","publisherLocation":"Reston, VA","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Tovar, F., 1973, Annual compilation and analysis of hydrologic data for urban studies  in the Austin, Texas Metropolitan Area, 1971: Open-File Report, iv, 73 p.","productDescription":"iv, 73 p.","numberOfPages":"77","additionalOnlineFiles":"N","temporalStart":"1970-10-01","temporalEnd":"1971-09-30","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":271000,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045441/report-thumb.jpg"},{"id":272734,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045441/report.pdf"}],"country":"United States","state":"Texas","city":"Austin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72dee4b00154e4368b7f","contributors":{"authors":[{"text":"Tovar, F.H.","contributorId":42116,"corporation":false,"usgs":true,"family":"Tovar","given":"F.H.","email":"","affiliations":[],"preferred":false,"id":477505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045438,"text":"70045438 - 1973 - Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range","interactions":[],"lastModifiedDate":"2018-10-30T13:01:07","indexId":"70045438","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range","docAbstract":"<p>Geohydrologic data have been obtained from more than 100 wells and test holes that have been drilled in the Post Headquarters and adjacent areas of White Sands Missile Range. Observation-well data show that, in general, a continuous decline of the water table has occurred in the vicinity of the well field since production began in 1949. Approximately 40,000 acre-feet of water has been produced from the aquifer to date (1972). </p><p>A series of maps are presented which show the changes that have occurred in the well field as the result of development.</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Albuquerque, NM","doi":"10.3133/70045438","collaboration":"Prepared in cooperation with White Sands Missile Range","usgsCitation":"Kelly, T.E., 1973, Summary of ground-water data, Post Headquarters and adjacent areas, White Sands Missile Range: Open-File Report, Report: 66 p.; 4 Plates: 28.47 x 46.17 inches or smaller, https://doi.org/10.3133/70045438.","productDescription":"Report: 66 p.; 4 Plates: 28.47 x 46.17 inches or smaller","numberOfPages":"68","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":272733,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045438/report.pdf"},{"id":270992,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045438/report-thumb.jpg"},{"id":358953,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-30.pdf","text":"Figure 30","linkFileType":{"id":1,"text":"pdf"}},{"id":358954,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-31.pdf","text":"Figure 31","linkFileType":{"id":1,"text":"pdf"}},{"id":358955,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-32.pdf","text":"Figure 32","linkFileType":{"id":1,"text":"pdf"}},{"id":358956,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70045438/figure-33.pdf","text":"Figure 33","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.61666667,\n              32.13333333\n            ],\n            [\n              -106.28333333,\n              32.13333333\n            ],\n            [\n              -106.28333333,\n              32.58333333\n            ],\n            [\n              -106.61666667,\n              32.58333333\n            ],\n            [\n              -106.61666667,\n              32.13333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516e72efe4b00154e4368c48","contributors":{"authors":[{"text":"Kelly, T. E.","contributorId":63824,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":477500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159811,"text":"70159811 - 1973 - New data on cuprobismutite","interactions":[],"lastModifiedDate":"2015-11-25T12:59:59","indexId":"70159811","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"New data on cuprobismutite","docAbstract":"<p>Cuprobismutite from Tunnel Extension Number Two&nbsp;mine, Ohio mining district, Utah, was chemically analyzed using the<br />electron microprobe. &nbsp;Its empirical formula was determined to be&nbsp;Cu<sub>20.8</sub> Ag<sub>0.97</sub> Pb<sub>0.35</sub> Mn<sub>0.22</sub> Bi<sub>26.7</sub>Sb<sub>0.06</sub> Te<sub>0.05</sub> Se<sub>0.55</sub> S<sub>50.4. &nbsp;</sub>The tentative conclusion is that unsubstituted cuprobismutite has the&nbsp;chemical formula 6Cu<sub>2</sub>S*6Bi<sub>2</sub>S<sub>3</sub> rather than the previously ascribed&nbsp;formula 6Cu<sub>2</sub>S*6Bi<sub>2</sub>S<sub>3</sub>&nbsp;and that cuprobismutite is therefore not&nbsp;dimorphous with emplectite.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Taylor, C.M., Radtke, A.S., and Christ, C., 1973, New data on cuprobismutite: Journal of Research of the U.S. Geological Survey, v. 1, no. 1, p. 99-103.","productDescription":"5 pg","startPage":"99","endPage":"103","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":311710,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue1/report.pdf","text":"Report","size":"22.2 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States of America","state":"Utah","otherGeospatial":"Tunnel Extension Number Two Mine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.27787017822266,\n              38.37288556789897\n            ],\n            [\n              -112.36061096191406,\n              38.38553501423449\n            ],\n            [\n              -112.39185333251953,\n              38.4291182807668\n            ],\n            [\n              -112.35923767089844,\n              38.480738480909324\n            ],\n            [\n              -112.32181549072266,\n              38.49095060018781\n            ],\n            [\n              -112.26585388183594,\n              38.49444388772503\n            ],\n            [\n              -112.20817565917967,\n              38.48046972138692\n            ],\n            [\n              -112.1982192993164,\n              38.42965618153018\n            ],\n            [\n              -112.20920562744139,\n              38.396029684120315\n            ],\n            [\n              -112.27787017822266,\n              38.37288556789897\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5656e9bbe4b071e7ea53eeca","contributors":{"authors":[{"text":"Taylor, Charles M.","contributorId":150037,"corporation":false,"usgs":false,"family":"Taylor","given":"Charles","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":580563,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radtke, Arthur S.","contributorId":63795,"corporation":false,"usgs":true,"family":"Radtke","given":"Arthur","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":580564,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Christ, C. L.","contributorId":53906,"corporation":false,"usgs":true,"family":"Christ","given":"C. L.","affiliations":[],"preferred":false,"id":580565,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70156956,"text":"70156956 - 1973 - Biochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, August 1973","interactions":[],"lastModifiedDate":"2019-11-13T14:57:32","indexId":"70156956","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Biochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, August 1973","docAbstract":"<p>Radiochemical data from the Amchitka Island study area were obtained from water samples collected by the U.S. Geological Survey during August 1973. Tritium determinations were made on 86 samples collected and gross alpha and gross beta/gamma determinations were made on 38 samples. The range of data for these samples was equal or less than the range of values obtained before the Cannikin event.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70156956","usgsCitation":"Ballance, W.C., 1973, Biochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, August 1973, i, 20 p., https://doi.org/10.3133/70156956.","productDescription":"i, 20 p.","numberOfPages":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307872,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/OFR474205.JPG"},{"id":308550,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156956/report.pdf","text":"Report","size":"3,498 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              178.584136963,\n              51.63677159243599\n            ],\n            [\n              178.592376709,\n              51.61290019118336\n            ],\n            [\n              179.21585083,\n              51.3254629443313\n            ],\n            [\n             179.508361816,\n              51.37520943448463\n            ],\n            [\n              179.057922363,\n              51.587309751245456\n            ],\n            [\n              178.628082275,\n              51.67936786087718\n            ],\n            [\n              178.584136963,\n              51.63677159243599\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efb1e4b05d6c4e4fa968","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571245,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009880,"text":"70009880 - 1973 - Mariner 9-Image processing and products","interactions":[],"lastModifiedDate":"2020-12-29T20:38:59.170514","indexId":"70009880","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Mariner 9-Image processing and products","docAbstract":"<p>The purpose of this paper is to describe the system for the display, processing, and production of image-data products created to support the Mariner 9 Television Experiment. Of necessity, the system was large in order to respond to the needs of a large team of scientists with a broad scope of experimental objectives. The desire to generate processed data products as rapidly as possible to take advantage of adaptive planning during the mission, coupled with the complexities introduced by the nature of the vidicon camera, greatly increased the scale of the ground-image processing effort.</p><p>This paper describes the systems that carried out the processes and delivered the products necessary for real-time and near-real-time analyses. References are made to the computer algorithms used for the, different levels of decalibration and analysis.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(73)90174-7","issn":"00191035","usgsCitation":"Levinthal, E., Green, W., Cutts, J., Jahelka, E., Johansen, R., Sander, M., Seidman, J., Young, A., and Soderblom, L., 1973, Mariner 9-Image processing and products: Icarus, v. 18, no. 1, p. 75-101, https://doi.org/10.1016/0019-1035(73)90174-7.","productDescription":"27 p.","startPage":"75","endPage":"101","numberOfPages":"27","costCenters":[],"links":[{"id":219335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a51f8e4b0c8380cd6c07d","contributors":{"authors":[{"text":"Levinthal, E.C.","contributorId":45823,"corporation":false,"usgs":true,"family":"Levinthal","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":357350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, W.B.","contributorId":68027,"corporation":false,"usgs":true,"family":"Green","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":357353,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cutts, J.A.","contributorId":56790,"corporation":false,"usgs":true,"family":"Cutts","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":357351,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jahelka, E.D.","contributorId":98876,"corporation":false,"usgs":true,"family":"Jahelka","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":357355,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Johansen, R.A.","contributorId":16156,"corporation":false,"usgs":true,"family":"Johansen","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":357348,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sander, M.J.","contributorId":93188,"corporation":false,"usgs":true,"family":"Sander","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":357354,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Seidman, J.B.","contributorId":61152,"corporation":false,"usgs":true,"family":"Seidman","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":357352,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Young, A.T.","contributorId":17757,"corporation":false,"usgs":true,"family":"Young","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":357349,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Soderblom, L.A. 0000-0002-0917-853X","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":6139,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.A.","affiliations":[],"preferred":false,"id":357347,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":70010095,"text":"70010095 - 1973 - Radial particle-size segregation during packing of particulates into cylindrical containers","interactions":[],"lastModifiedDate":"2020-12-30T15:10:51.612357","indexId":"70010095","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3107,"text":"Powder Technology","active":true,"publicationSubtype":{"id":10}},"title":"Radial particle-size segregation during packing of particulates into cylindrical containers","docAbstract":"<p>In a series of experiments, soil materials were placed in long cylindrical containers, using various packing procedures. Soil columns produced by deposition and simultaneous vibratory compaction were dense and axially uniform, but showed significant radial segregation of particle sizes. Similar results were obtained with deposition and simultaneous impact-type compaction when the impacts resulted in significant container “bouncing”. The latter procedure, modified to minimize “bouncing” produced dense, uniform soil columns, showing little radial particle-size segregation. Other procedures tested (deposition alone and deposition followed by compaction) did not result in radial segregation, but produced columns showing either relatively low or axially nonuniform densities.</p><p>Current data suggest that radial particle-size segregation is mainly due to vibration-induced particle circulation in which particles of various sizes have different circulation rates and paths.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0032-5910(73)80079-8","issn":"00325910","usgsCitation":"Ripple, C., James, R., and Rubin, J., 1973, Radial particle-size segregation during packing of particulates into cylindrical containers: Powder Technology, v. 8, no. 3-4, p. 165-175, https://doi.org/10.1016/0032-5910(73)80079-8.","productDescription":"11 p.","startPage":"165","endPage":"175","numberOfPages":"11","costCenters":[],"links":[{"id":219666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9390e4b0c8380cd80ed4","contributors":{"authors":[{"text":"Ripple, C.D.","contributorId":11586,"corporation":false,"usgs":true,"family":"Ripple","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":357883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"James, R.V.","contributorId":106634,"corporation":false,"usgs":true,"family":"James","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":357885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rubin, J.","contributorId":26433,"corporation":false,"usgs":true,"family":"Rubin","given":"J.","email":"","affiliations":[],"preferred":false,"id":357884,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70156968,"text":"70156968 - 1973 - Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, July 1972","interactions":[],"lastModifiedDate":"2019-11-13T15:01:25","indexId":"70156968","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, July 1972","docAbstract":"<p>The U.S. Geological Survey established a sampling program on Amchitka Island in 1967 in cooperation with the U.S . Atomic Energy Commission. Water samples are analyzed routinely for tritium, gross alpha, and gross beta/gamma content, Frequency of sampling was semiannually prior to Cannikin and has been bimonthly since the Cannikin event (November 6, 1971). The sampling frequency will be quarterly for the remainder of the first year (through November 1972). Sampling frequency will be changed to an annual basis approximately 1 1/2 years after the event.</p>\n<p>The techniques and procedures used for sample collection, identification, and analysis are described in Beetem, Washington, Janzer, and Schroder (1971) and in Schroder (1971), Radiochemical data obtained from samples analyzed by the U.S. Geological Survey through November 1970 are reported in Beetem, Washington, Janzer, and Schroder (1971), Radiochemical data obtained from samples analyzed by the U.S. Geological Survey from September 1971 through December 1971 and January 13 through April 5, 1972, are reported in Schroder and Ballance (1972a,b). This report presents the radiochemical data from samples collected during July 1972,</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70156968","usgsCitation":"Ballance, W.C., and Schroder, L., 1973, Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, July 1972, i, 15 p., https://doi.org/10.3133/70156968.","productDescription":"i, 15 p.","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308555,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156968/report.pdf","text":"Report","size":"2,666 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":307885,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr474166.JPG"}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              178.584136963,\n              51.63677159243599\n            ],\n            [\n              178.592376709,\n              51.61290019118336\n            ],\n            [\n              179.21585083,\n              51.3254629443313\n            ],\n            [\n             179.508361816,\n              51.37520943448463\n            ],\n            [\n              179.057922363,\n              51.587309751245456\n            ],\n            [\n              178.628082275,\n              51.67936786087718\n            ],\n            [\n              178.584136963,\n              51.63677159243599\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f7efc0e4b05d6c4e4fa98e","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schroder, L.J.","contributorId":31767,"corporation":false,"usgs":true,"family":"Schroder","given":"L.J.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571270,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001633,"text":"1001633 - 1973 - A method to determine waterfowl shooting distances","interactions":[],"lastModifiedDate":"2017-09-15T10:05:54","indexId":"1001633","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"A method to determine waterfowl shooting distances","docAbstract":"Long-range shooting at ducks and geese frequently results in a high crippling loss, unretrieved birds and frustrated hunters. A principal problem has been the general inability of hunters or observers to properly judge distance of birds. This paper describes a reasonably accurate method developed to determine shooting distances to geese. Two observers utilized transit-mounted 4X hunting scopes to determine angles and elevations to goose hunters and birds. These data were used to set up a series of triangles by which a distance between hunter and birds could be calculated. Known-distance tests indicated an average measurement error of approximately two percent. An average shooting distance of 71 yards was calculated from 175 sightings. The maximum range was 240 yards and the minimum was 24 yards. The relationship of shooting to clean kills and crippling loss is also discussed.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Davenport, D., Sherwood, G., and Murdy, H.W., 1973, A method to determine waterfowl shooting distances: Wildlife Society Bulletin, v. 1, no. 2, p. 101-105.","productDescription":"5 p.","startPage":"101","endPage":"105","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae392","contributors":{"authors":[{"text":"Davenport, D.A.","contributorId":71126,"corporation":false,"usgs":true,"family":"Davenport","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":311393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sherwood, G.A.","contributorId":70331,"corporation":false,"usgs":true,"family":"Sherwood","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":311392,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murdy, H. W.","contributorId":9997,"corporation":false,"usgs":true,"family":"Murdy","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":311391,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1014153,"text":"1014153 - 1973 - Fish viruses: Buffers and methods for plaquing eight agents under normal atmosphere","interactions":[],"lastModifiedDate":"2023-09-13T14:05:39.414095","indexId":"1014153","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":843,"text":"Applied Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Fish viruses: Buffers and methods for plaquing eight agents under normal atmosphere","docAbstract":"<p><span>A universal procedure was sought for plaque assay of eight fish viruses (bluegill myxovirus, channel catfish virus, eel virus, Egtved virus, infectious hematopoietic necrosis virus, infectious pancreatic necrosis virus, lymphocystis virus, and the agent of spring viremia of carp (</span><i>Rhabdovirus carpio</i><span>), in dish cultures of various fish cells. Eagle minimal essential medium with sodium bicarbonate-CO</span><sub>2</sub><span>&nbsp;buffer (Earle’s salt solution) was compared with minimal essential medium buffered principally with tris (hydroxymethyl)aminomethane or&nbsp;</span><i>N</i><span>-2-hydroxyethylpiperazine-N′-2′-ethanesulfonic acid at a pH or in the range of 7.6 to 8.0 depending upon temperature. Five fish cell lines collectively capable of replicating all fish viruses thus far isolated were tested and quantitatively found to grow comparably well in the three media. Two-phase (gel-liquid) media incorporating the various buffer systems allowed plaquing at 15 to 33 C either in partial pressures of CO</span><sub>2</sub><span>&nbsp;or in normal atmosphere, but greater efficiency and sensitivity were obtained with the organic buffers, and, overall, the best results were obtained with tris(hydroxymethyl)aminomethane. Epizootiological data, specific fish cell line response, and plaque morphology permit presumptive identification of most of the agents. At proper pH, use of organic buffers obviates the need for CO</span><sub>2</sub><span>&nbsp;incubators.</span></p>","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/am.25.4.659-664.1973","usgsCitation":"Wolf, K., and Quimby, M.C., 1973, Fish viruses: Buffers and methods for plaquing eight agents under normal atmosphere: Applied Microbiology, v. 25, no. 4, p. 659-664, https://doi.org/10.1128/am.25.4.659-664.1973.","productDescription":"6 p.","startPage":"659","endPage":"664","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480662,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/am.25.4.659-664.1973","text":"Publisher Index Page"},{"id":197561,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef553","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quimby, M. C.","contributorId":14334,"corporation":false,"usgs":true,"family":"Quimby","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":319869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010973,"text":"70010973 - 1973 - Simultaneous flow of water and solutes through geological membranes-I. Experimental investigation","interactions":[],"lastModifiedDate":"2020-12-29T14:05:30.568856","indexId":"70010973","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Simultaneous flow of water and solutes through geological membranes-I. Experimental investigation","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><p>The relative retardation by geological membranes of cations and anions generally present in subsurface waters was investigated using a high pressure and high temperature ‘filtration cell’. The solutions were forced through different clays and a disaggregated shale subjected to compaction pressures up to 9500 psi and to temperatures from 20 to 70°C.</p><p>The overall efficiences measured increased with increase of exchange capacity of the material used and with decrease in concentration of the input solution. The efficiency of a given membrane increased with increasing compaction pressure but decreased slightly at higher temperatures for solutions of the same ionic concentration.</p><p>The results further show that geological membranes are specific for different dissolved species. The retardation sequences varied depending on the material used and on experimental conditions. The sequences for monovalent and divalent cations at laboratory temperatures were generally as follows: Li &lt; Na &lt; NH<sub>3</sub><span>&nbsp;</span>&lt; K &lt; Rb &lt; Cs Mg &lt; Ca &lt; Sr &lt; Ba.</p><p>The sequences for anions at room temperature were variable, but at 70°C, the sequence was: HCO<sub>3</sub><span>&nbsp;</span>&lt; I &lt; B &lt; SO<sub>4</sub><span>&nbsp;</span>&lt; Cl &lt; Br.</p><p>Monovalent cations contrary to some field data were generally retarded with respect to divalent cations. The differences in the filtration ratios among the divalent cations were smaller than those between the monovalent cations. The passage rate of B, HCO<sub>3</sub>, I and NH<sub>3</sub><span>&nbsp;</span>was greatly increased at 70°C.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90267-6","issn":"00167037","usgsCitation":"Kharaka, Y., and Berry, F., 1973, Simultaneous flow of water and solutes through geological membranes-I. Experimental investigation: Geochimica et Cosmochimica Acta, v. 37, no. 12, p. 2577-2603, https://doi.org/10.1016/0016-7037(73)90267-6.","productDescription":"27 p.","startPage":"2577","endPage":"2603","numberOfPages":"27","costCenters":[],"links":[{"id":221209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b90d3e4b08c986b31968e","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":360003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, F.A.P.","contributorId":57594,"corporation":false,"usgs":true,"family":"Berry","given":"F.A.P.","email":"","affiliations":[],"preferred":false,"id":360004,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010280,"text":"70010280 - 1973 - An empirical NaKCa geothermometer for natural waters","interactions":[],"lastModifiedDate":"2020-12-29T15:04:56.671286","indexId":"70010280","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"An empirical NaKCa geothermometer for natural waters","docAbstract":"<p>An empirical method of estimating the last temperature of water-rock interaction has been devised. It is based upon molar Na, K and Ca concentrations in natural waters from temperature environments ranging from 4 to 340°C. The data for most geothermal waters cluster near a straight line when plotted as the function<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-1-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>log (</mtext><mtext>Na</mtext><mtext>K</mtext><mtext>) + &amp;#x3B2; log [ &amp;#x221A;</mtext><mtext>(Ca)</mtext><mtext>Na</mtext><mtext>]</mtext></math>\"><span class=\"MJX_Assistive_MathML\">log (NaK) + β log [ √(Ca)Na]</span></span></span><span>&nbsp;</span>vs reciprocal of absolute temperature, where β is either<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-2-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>1</mtext><mtext>3</mtext></math>\"><span class=\"MJX_Assistive_MathML\">13</span></span></span><span>&nbsp;</span>or<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-3-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>4</mtext><mtext>3</mtext></math>\"><span class=\"MJX_Assistive_MathML\">43</span></span></span><span>&nbsp;</span>depending upon whether the water equilibrated above or below 100°C. For most waters tested, the method gives better results than the<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-4-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Na</mtext><mtext>K</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NaK</span></span></span><span>&nbsp;</span>methods suggested by other workers. The ratio<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-5-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Na</mtext><mtext>K</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NaK</span></span></span><span>&nbsp;</span>should not be used to estimate temperature if<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-6-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>&amp;#x221A; (</mtext><mtext>M</mtext><msub><mi></mi><mn>Ca</mn></msub><mtext>)</mtext><mtext>M</mtext><msub><mi></mi><mn>Na</mn></msub></math>\"><span class=\"MJX_Assistive_MathML\">√ (MCa)MNa</span></span></span><span>&nbsp;</span>is greater than 1. The<span>&nbsp;</span><span class=\"math\"><span id=\"MathJax-Element-7-Frame\" class=\"MathJax_SVG\" data-mathml=\"<math xmlns=&quot;http://www.w3.org/1998/Math/MathML&quot;><mtext>Na</mtext><mtext>K</mtext></math>\"><span class=\"MJX_Assistive_MathML\">NaK</span></span></span><span>&nbsp;</span>values of such waters generally yield calculated temperatures much higher than the actual temperature at which water interacted with the rock.</p><p>A comparison of the composition of boiling hot-spring water with that obtained from a nearby well (170°C) in Yellowstone Park shows that continued water-rock reactions may occur during ascent of water even though that ascent is so rapid that little or no heat is lost to the country rock, i.e. the water cools adiabatically. As a result of such continued reaction, waters which dissolve additional Ca as they ascend from the aquifer to the surface will yield estimated aquifer temperatures that are too low. On the other hand, waters initially having enough Ca to deposit calcium carbonate during ascent may yield estimated aquifer temperatures that are too high if aqueous Na and K are prevented from further reaction with country rock owing to armoring by calcite or silica minerals.</p><p>The Na-K-Ca geothermometer is of particular interest to those prospecting for geothermal energy. 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":147999,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":808230,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180009,"text":"70180009 - 1972 - Developing a state water plan: Ground-water conditions in Utah, spring of 1972","interactions":[],"lastModifiedDate":"2017-01-23T11:34:43","indexId":"70180009","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"10","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1972","docAbstract":"<p>This report is the ninth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.</p><p>This report, like the others (see references, p. 19), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1971. Water-level fluctuations, however, are described for the period spring 1971 to spring 1972. Many of the data used in the report were collected by the Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Sumison, C., Bjorklund, L., McGreevy, L.J., Bolke, E., Mower, R.W., Herbert, L.R., Miller, L.L., Butler, R., Adams, D.B., and Sandberg, G.W., 1972, Developing a state water plan: Ground-water conditions in Utah, spring of 1972: Cooperative Investigations Report 10, viii, 73 p.","productDescription":"viii, 73 p.","numberOfPages":"82","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333682,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333681,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-193"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a13e4b0cad700058b61","contributors":{"authors":[{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659734,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGreevy, L. 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,{"id":70043130,"text":"70043130 - 1972 - Principal facts for gravity stations in the Death Valley region, California","interactions":[{"subject":{"id":52557,"text":"ofr6680 - 1966 - Principal facts for gravity stations in the Death Valley region, California","indexId":"ofr6680","publicationYear":"1966","noYear":false,"title":"Principal facts for gravity stations in the Death Valley region, California"},"predicate":"SUPERSEDED_BY","object":{"id":70043130,"text":"70043130 - 1972 - Principal facts for gravity stations in the Death Valley region, California","indexId":"70043130","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in the Death Valley region, California"},"id":1}],"lastModifiedDate":"2013-02-05T14:23:46","indexId":"70043130","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":360,"text":"Final Report","active":false,"publicationSubtype":{"id":6}},"title":"Principal facts for gravity stations in the Death Valley region, California","docAbstract":"Observed gravity values, station locations, terrain corrections, and Bouguer gravity data are provided in tabular form for approximately 1,500 gravity observations in eastern California. Coverage includes Saline Valley, Panamint Valley, Searles Basin, Death Valley, the southern Amargosa Desert and the enclosed and adjoining highlands. These data were used in preparation of -- Mabey, Don R., 1963, Complete Bouguer anomaly map of the Death Valley region, California: U.S. Geol. Survey Geophys. Inv. Map GP-305.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043130","usgsCitation":"Mabey, D.R., 1972, Principal facts for gravity stations in the Death Valley region, California: Final Report, 49 p., https://doi.org/10.3133/70043130.","productDescription":"49 p.","costCenters":[{"id":671,"text":"Western Region Geology and Geophysics Science Center","active":false,"usgs":true}],"links":[{"id":267035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.0 ], [ -114.13,42.0 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51123844e4b0ebe69d7eb721","contributors":{"authors":[{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":473024,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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