{"pageNumber":"2428","pageRowStart":"60675","pageSize":"25","recordCount":68807,"records":[{"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":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":70176022,"text":"70176022 - 1973 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972","interactions":[],"lastModifiedDate":"2016-08-23T15:26:55","indexId":"70176022","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":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Puente, C., 1973, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1972: Edwards Underground Water District Bulletin 31, 8 p.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327747,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dde4b03fd6b7df2cfd","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":646810,"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":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":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":70010157,"text":"70010157 - 1973 - Extraction and concentration of organic solutes from water","interactions":[],"lastModifiedDate":"2023-03-17T16:43:19.525112","indexId":"70010157","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Extraction and concentration of organic solutes from water","docAbstract":"<p>A continuous extraction apparatus is described. It extracts and simultaneously concentrates organic solutes from water. Any immiscible solvent can be used in this apparatus if the solute will partition between the solvent and water. A concentration factor of up to 10<sup>5</sup> is obtained with this technique. The dipole moment difference between the solute and solvent is demonstrated to be an index of the extraction efficiency. Optimum extraction of a given molecular species may be obtained by use of this index.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60323a020","usgsCitation":"Goldberg, M.C., DeLong, L.L., and Sinclair, M., 1973, Extraction and concentration of organic solutes from water: Analytical Chemistry, v. 45, no. 1, p. 89-93, https://doi.org/10.1021/ac60323a020.","productDescription":"5 p.","startPage":"89","endPage":"93","numberOfPages":"5","costCenters":[],"links":[{"id":219434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"1","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a0e5ce4b0c8380cd533f2","contributors":{"authors":[{"text":"Goldberg, Marvin C.","contributorId":26066,"corporation":false,"usgs":true,"family":"Goldberg","given":"Marvin","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLong, Lewis L.","contributorId":91146,"corporation":false,"usgs":true,"family":"DeLong","given":"Lewis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":358150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sinclair, Mark","contributorId":91027,"corporation":false,"usgs":true,"family":"Sinclair","given":"Mark","email":"","affiliations":[],"preferred":false,"id":358151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":70010113,"text":"70010113 - 1973 - Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","interactions":[],"lastModifiedDate":"2020-12-30T15:25:29.654987","indexId":"70010113","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":"Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications","docAbstract":"<p>Deuterium and O<sup>18</sup><span>&nbsp;</span>analyses were made on 25 formation-water samples from Miocene (Temblor Formation) and Eocene (McAdams Formation) reservoir rocks at Kettleman North Dome oil field, California, and on three surface water samples from Reef Ridge located about three miles to the west of the field. The<span>&nbsp;</span><i>δO</i><sup>18</sup><span>&nbsp;</span>values obtained generally increase with depth and most probably are due to temperature controlled exchange reactions with carbonate cement and dissolved carbonate species. The δD values obtained seem to be controlled primarily by the membrane behavior of shales modifying the assumed original values. The contribution of isotopic exchange between water and clays cannot be evaluated at present.</p><p>The isotopic data support the conclusions based on a detailed study of geology, hydrodynamics, and formation water geochemistry (<span class=\"small-caps\">Kharaka</span>, 1971) which indicate that:</p><p>1. The Temblor Formation waters are probably meteoric in origin concentrated chemically and isotopically by shale membranes, and 2. The McAdams Formation waters were most probably obtained by squeezing the original interstitial marine connate waters of deposition from the underlying Mesozoic sediments.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90148-8","issn":"00167037","usgsCitation":"Kharaka, Y., Berry, F., and Friedman, I., 1973, Isotopic composition of oil-field brines from Kettleman North Dome, California, and their geologic implications: Geochimica et Cosmochimica Acta, v. 37, no. 8, p. 1899-1908, https://doi.org/10.1016/0016-7037(73)90148-8.","productDescription":"10 p.","startPage":"1899","endPage":"1908","numberOfPages":"10","costCenters":[],"links":[{"id":381758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Kettleman North Dome","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.58892822265626,\n              35.980228800645676\n            ],\n            [\n              -119.41177368164061,\n              35.980228800645676\n            ],\n            [\n              -119.41177368164061,\n              36.094609063015085\n            ],\n            [\n              -119.58892822265626,\n              36.094609063015085\n            ],\n            [\n              -119.58892822265626,\n              35.980228800645676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3fa3e4b0c8380cd646aa","contributors":{"authors":[{"text":"Kharaka, Y.K.","contributorId":23568,"corporation":false,"usgs":true,"family":"Kharaka","given":"Y.K.","email":"","affiliations":[],"preferred":false,"id":357954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, F.A.F.","contributorId":15755,"corporation":false,"usgs":true,"family":"Berry","given":"F.A.F.","email":"","affiliations":[],"preferred":false,"id":357953,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":357955,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010146,"text":"70010146 - 1973 - Solubility and occurrence of lead in surface water","interactions":[],"lastModifiedDate":"2025-01-07T16:11:33.867111","indexId":"70010146","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2136,"text":"Journal - American Water Works Association","active":true,"publicationSubtype":{"id":10}},"title":"Solubility and occurrence of lead in surface water","docAbstract":"<p><span>The data in this article suggest methods of reducing the lead content of drinking water at the water-treatment plant.</span></p>","language":"English","publisher":"American Water Works Association","doi":"10.1002/j.1551-8833.1973.tb01896.x","issn":"0003150X","usgsCitation":"Hem, J., and Durum, W.H., 1973, Solubility and occurrence of lead in surface water: Journal - American Water Works Association, v. 65, no. 8, p. 562-568, https://doi.org/10.1002/j.1551-8833.1973.tb01896.x.","productDescription":"7 p.","startPage":"562","endPage":"568","numberOfPages":"7","costCenters":[],"links":[{"id":219352,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9241e4b08c986b319db7","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":358117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":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":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":7000077,"text":"7000077 - 1973 - Permafrost","interactions":[],"lastModifiedDate":"2012-02-02T00:15:08","indexId":"7000077","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Permafrost","language":"ENGLISH","doi":"10.3133/7000077","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Permafrost: General Interest Publication, 15 p. : col. ill., col. map ; 23 x 21 cm. folded to 23 x 11 cm., https://doi.org/10.3133/7000077.","productDescription":"15 p. : col. ill., col. map ; 23 x 21 cm. folded to 23 x 11 cm.","costCenters":[],"links":[{"id":196280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881a8","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7000080,"text":"7000080 - 1973 - Map, line and sinker","interactions":[],"lastModifiedDate":"2012-02-02T00:15:08","indexId":"7000080","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Map, line and sinker","language":"ENGLISH","doi":"10.3133/7000080","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Map, line and sinker: General Interest Publication, 1 sheet : ill. ; 23 x 40 cm. folded to 23 x 10 cm., https://doi.org/10.3133/7000080.","productDescription":"1 sheet : ill. ; 23 x 40 cm. folded to 23 x 10 cm.","costCenters":[],"links":[{"id":196316,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64974c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171174,"text":"70171174 - 1973 - The role of the Bureau of Sport Fisheries and Wildlife in the Great Lakes","interactions":[],"lastModifiedDate":"2016-05-25T11:40:28","indexId":"70171174","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The role of the Bureau of Sport Fisheries and Wildlife in the Great Lakes","docAbstract":"<p><span>Ecological blunders of man, such as timber exploitation, draining of wetlands, construction of canals and dams, and pollution have been mainly responsible for serious environmental degradation and catastrophic losses of fish and wildlife values in the Great Lakes Basin. Consequently, the major emphasis of the Bureau of Sport Fisheries and Wildlife must be on the protection and enhancement of the Great Lakes habitat -- primarily as a single large ecosystem, rather than as a number of political units separated by ecologically meaningless boundaries. By authority of Congress, the Bureau has long been concerned in the Great Lakes region with such diverse activities as establishing refuges for migratory waterfowl, conducting fishery research, evaluating the effects of federally sponsored water resource development projects on fish and wildlife, rearing and stocking of game fish, and assisting the states in fish and wildlife management by giving technical advice and financial assistance. Thus, the Bureau shares a strong common interest with other federal administrative units, as well as with state, interstate, and international agencies, in protecting, enhancing, and ensuring the wise use of fish and wildlife in the Great Lakes Basin.</span></p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the First Federal Conference on the Great Lakes","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"First Federal Conference on the Great Lakes","conferenceDate":"December 13-15, 1972","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"National Technical Information Service","usgsCitation":"Hester, F.E., 1973, The role of the Bureau of Sport Fisheries and Wildlife in the Great Lakes, <i>in</i> Proceedings of the First Federal Conference on the Great Lakes, Ann Arbor, MI, December 13-15, 1972, p. 39-43.","productDescription":"5 p.","startPage":"39","endPage":"43","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321616,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccc5e4b07e28b662dd50","contributors":{"authors":[{"text":"Hester, F. Eugene","contributorId":169588,"corporation":false,"usgs":false,"family":"Hester","given":"F.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":630161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":93791,"text":"93791 - 1973 - Duck plague (duck virus enteritis) in wild waterfowl","interactions":[],"lastModifiedDate":"2017-10-20T11:55:26","indexId":"93791","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Duck plague (duck virus enteritis) in wild waterfowl","docAbstract":"<p>No abstract availablie.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/93791","usgsCitation":"Friend, M., and Pearson, G.L., 1973, Duck plague (duck virus enteritis) in wild waterfowl, 16 p., https://doi.org/10.3133/93791.","productDescription":"16 p.","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":292377,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633b3e","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":297927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pearson, Gary L.","contributorId":76676,"corporation":false,"usgs":true,"family":"Pearson","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":297928,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7000078,"text":"7000078 - 1973 - Ferdinand Vandiveer Hayden and the founding of the Yellowstone National Park","interactions":[],"lastModifiedDate":"2016-09-07T12:55:03","indexId":"7000078","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Ferdinand Vandiveer Hayden and the founding of the Yellowstone National Park","docAbstract":"<p>Following the Civil War, the United States intensified the exploration of her western frontiers to gain a measure of the vast lands and natural resources in the region now occupied by our Rocky Mountain States. As part of this effort, the U.S. Geological and Geographical Survey of the Territories was formed and staffed under the leadership of geologist Ferdinand Vandiveer Hayden. Originally organized under the U.S. Public Land Office in 1861, the Hayden Survey (as it was most often identified) was placed under the Secretary of the Interior in 1869 and later, under the newly created U.S. Geological Survey. Its records, maps, and photographs were then transferred to the latter agency. </p><p>In commemorating the centennial of Yellowstone National Park, the U.S. Geological Survey drew upon those items deposited by Hayden to describe the early exploration of the Yellowstone area and to recount events that led to the establishment of Yellowstone as the Nation's first national park.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/7000078","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Ferdinand Vandiveer Hayden and the founding of the Yellowstone National Park (Revised and expanded): General Interest Publication, 45 p., https://doi.org/10.3133/7000078.","productDescription":"45 p.","costCenters":[],"links":[{"id":256842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/7000078/report-thumb.jpg"},{"id":256841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/7000078/report.pdf","text":"Report","size":"18.58 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"edition":"Revised and expanded","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6258eb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":66548,"text":"i767E - 1973 - Ground-water yield potential in Knox County, Tennessee","interactions":[],"lastModifiedDate":"2023-03-24T18:36:23.336346","indexId":"i767E","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"767","chapter":"E","title":"Ground-water yield potential in Knox County, Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i767E","usgsCitation":"McMaster, W.H., 1973, Ground-water yield potential in Knox County, Tennessee: U.S. Geological Survey IMAP 767, Report: 1 p.; 1 Plate: 27.89 x 20.63 iinches, https://doi.org/10.3133/i767E.","productDescription":"Report: 1 p.; 1 Plate: 27.89 x 20.63 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,{"id":1003229,"text":"1003229 - 1973 - Dynamics of a salt of (2,4-dichlorophenoxy) acetic acid in fish, water and hydrosol","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"1003229","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2149,"text":"Journal of Agricultural and Food Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Dynamics of a salt of (2,4-dichlorophenoxy) acetic acid in fish, water and hydrosol","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Agricultural and Food Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Schultz, D., 1973, Dynamics of a salt of (2,4-dichlorophenoxy) acetic acid in fish, water and hydrosol: Journal of Agricultural and Food Chemistry, v. 21, no. 2, p. 186-192.","productDescription":"pp. 186-192","startPage":"186","endPage":"192","numberOfPages":"7","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":198335,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62f7d3","contributors":{"authors":[{"text":"Schultz, D.P.","contributorId":106054,"corporation":false,"usgs":true,"family":"Schultz","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":313000,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000029,"text":"2000029 - 1973 - Microbial degradation of the lamprey larvicide 3-trifluoromethyl-4-nitrophenol in sediment-water systems","interactions":[],"lastModifiedDate":"2012-02-02T00:14:56","indexId":"2000029","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"18","title":"Microbial degradation of the lamprey larvicide 3-trifluoromethyl-4-nitrophenol in sediment-water systems","docAbstract":"The selective lampricide 3-trifluoromethyl-4-nitrophenol (TFM), maintained in the water at concentrations of 1 to 6 I?g/ml for several hours, kills larval sea lampreys (Petromyzon marinus) in tributaries of the Great Lakes. Because the fate of TFM in the environment is a matter of concern, the interactions of this chemical with river and lake sediments were studied in laboratory experiments. In mixtures of TFM, water, and sediment held in aquariums, the TFM decreased progressively and nearly or completely disappeared in 1 to 4 weeks; concentrations of the fluoride ion increased; and the systems became nontoxic for sea lamprey larvae and goldfish (Carassius auratus). If the reduction in TFM ceased before all of the chemical had disappeared, the process resumed when nutrient broth was added. Loss of TFM from the systems was prevented by the addition of an antiseptic (phenol) and by heat sterilization. Enrichment cultures of microorganisms isolated from stream and lake sediments degraded TFM in nutrient broths. I conclude that TFM is degraded by microorganisms that live in sediment-water systems.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Kempe, L.L., 1973, Microbial degradation of the lamprey larvicide 3-trifluoromethyl-4-nitrophenol in sediment-water systems: Technical Report 18, 16 p.","productDescription":"16 p.","startPage":"0","endPage":"16","numberOfPages":"16","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr18.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62df9c","contributors":{"authors":[{"text":"Kempe, Lloyd L.","contributorId":55117,"corporation":false,"usgs":true,"family":"Kempe","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":324952,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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. The method also may be of use in interpreting compositions of fluid inclusions.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(73)90060-4","issn":"00167037","usgsCitation":"Fournier, R., and Truesdell, A., 1973, An empirical NaKCa geothermometer for natural waters: Geochimica et Cosmochimica Acta, v. 37, no. 5, p. 1255-1275, https://doi.org/10.1016/0016-7037(73)90060-4.","productDescription":"21 p.","startPage":"1255","endPage":"1275","numberOfPages":"21","costCenters":[],"links":[{"id":219060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.15966796875,\n              43.068887774169625\n            ],\n            [\n              -108.56689453125,\n              43.068887774169625\n            ],\n            [\n              -108.56689453125,\n              45.042478050891546\n            ],\n            [\n              -111.15966796875,\n              45.042478050891546\n            ],\n            [\n              -111.15966796875,\n              43.068887774169625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"37","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea33e4b0c8380cd486d4","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":358512,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"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":358511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1001284,"text":"1001284 - 1973 - Selective predation by mink, Mustela vison, on waterfowl","interactions":[],"lastModifiedDate":"2023-02-15T17:47:19.430685","indexId":"1001284","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":737,"text":"American Midland Naturalist","active":true,"publicationSubtype":{"id":10}},"title":"Selective predation by mink, Mustela vison, on waterfowl","docAbstract":"<p>Predation by mink (<i>Mustela vison</i>) on three types of ducks (captive, pen-reared-released and wild) was documented in two studies at the Northern Prairie Wildlife Research Center, Jamestown, North Dakota. In the first study, 36 of 60 flightless adult and juvenile ducks held on eight 0.1-acre experimental ponds disappeared between 10 July and 4 August 1969. Available evidence indicated that all were killed by a large adult mink. The mink selected recently released incubator-hatched ducklings, females in the process of incubating, and adults and juveniles on a marginal food supply.In the second study, 152 wood duck ducklings (<i>Aix sponsa</i>) were released on a 76-acre marsh during 1971. Half of the ducklings, when 24 to 27 days old, were placed at weekly intervals in four floating pens and allowed to escape after 4 days. Each time birds were placed in the floating pens, a comparable group was placed in a predator-proof shoreline pen. Birds in the shoreline pen escaped as they learned to fly when approximately 60 days old. The shoreline of the marsh was periodically searched, and the remains of 21 (28%) of the floating-pen birds were identified in food remains found at 16 mink dens. No remains of birds from the shoreline pen were found at the dens. Coots (<i>Fulica americana</i>) were also taken commonly. Wild ducklings appeared to have been almost totally consumed, but the legs and feet of the wood ducks were often left uneaten because of bands and tags.</p>","language":"English","publisher":"University of Notre Dame","doi":"10.2307/2424149","usgsCitation":"Sargeant, A.B., Swanson, G.A., and Doty, H.A., 1973, Selective predation by mink, Mustela vison, on waterfowl: American Midland Naturalist, v. 89, no. 1, p. 208-214, https://doi.org/10.2307/2424149.","productDescription":"7 p.","startPage":"208","endPage":"214","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":133311,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c1e","contributors":{"authors":[{"text":"Sargeant, Alan B.","contributorId":89185,"corporation":false,"usgs":true,"family":"Sargeant","given":"Alan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":310802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, George A.","contributorId":49654,"corporation":false,"usgs":true,"family":"Swanson","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doty, Harold A.","contributorId":17565,"corporation":false,"usgs":true,"family":"Doty","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":310803,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41925,"text":"ofr73291 - 1973 - Aeromagnetic map of northern Frederick County, Maryland, and parts of adjacent counties in Maryland and Pennsylvania","interactions":[],"lastModifiedDate":"2022-12-14T20:57:37.664247","indexId":"ofr73291","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-291","title":"Aeromagnetic map of northern Frederick County, Maryland, and parts of adjacent counties in Maryland and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73291","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Aeromagnetic map of northern Frederick County, Maryland, and parts of adjacent counties in Maryland and Pennsylvania: U.S. Geological Survey Open-File Report 73-291, 1 Plate: 43.00 × 41.00 inches, https://doi.org/10.3133/ofr73291.","productDescription":"1 Plate: 43.00 × 41.00 inches","costCenters":[],"links":[{"id":136687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410496,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68260.htm","linkFileType":{"id":5,"text":"html"}},{"id":98723,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Maryland, Pennsylvania","county":"Frederick County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77,\n              39.75\n            ],\n            [\n              -77.75,\n              39.75\n            ],\n            [\n              -77.75,\n              39.3756\n            ],\n            [\n              -77,\n              39.3756\n            ],\n            [\n              -77,\n              39.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697ce7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530706,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}