{"pageNumber":"2646","pageRowStart":"66125","pageSize":"25","recordCount":68827,"records":[{"id":51626,"text":"ofr5440 - 1954 - Water supply in Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr5440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-40","title":"Water supply in Florida","language":"ENGLISH","doi":"10.3133/ofr5440","usgsCitation":"Brown, E., 1954, Water supply in Florida: U.S. Geological Survey Open-File Report 54-40, 15 p., https://doi.org/10.3133/ofr5440.","productDescription":"15 p.","costCenters":[],"links":[{"id":178102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4df","contributors":{"authors":[{"text":"Brown, Eugene","contributorId":15187,"corporation":false,"usgs":true,"family":"Brown","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":244043,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51636,"text":"ofr5462 - 1954 - Progress report of cooperative ground-water investigations for Connecticut for the year ended June 30, 1954","interactions":[],"lastModifiedDate":"2015-10-22T12:58:18","indexId":"ofr5462","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-62","title":"Progress report of cooperative ground-water investigations for Connecticut for the year ended June 30, 1954","docAbstract":"

Ground-water investigations were continued under the Water Commission- U.S. Geological Survey Cooperative Program at four project area in Connecticut during the year ended June 30, 1954. Substantial progress was made in the collection of basic water information in the lower Farmington River basin. Both surface and subsurface geological area were assembled for use by prospective well owners. The preparation of a report on the geology and ground-water resources of the agricultural area of north-central Connecticut was continued during the year. As a continuation of investigations on the ground-water resources of the industrial areas of New Haven and Waterbury, observations of water level and samples of water were taken bi-monthly from 5 well at 5 industrial plants in Waterbury and anaysed for sulfate concentration in order to measure the degree of infiltration of acid-contaminated water to the water-bearing formations.  

","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/ofr5462","usgsCitation":"Cushman, R., 1954, Progress report of cooperative ground-water investigations for Connecticut for the year ended June 30, 1954: U.S. Geological Survey Open-File Report 54-62, 1 p., https://doi.org/10.3133/ofr5462.","productDescription":"1 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5462.jpg"},{"id":310481,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0062/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.64410400390625,\n 40.9964840143779\n ],\n [\n -73.12774658203125,\n 41.155910350545035\n ],\n [\n -72.96844482421875,\n 41.23444575262555\n ],\n [\n -72.63336181640625,\n 41.24890252240322\n ],\n [\n -72.38067626953125,\n 41.25716209782705\n ],\n [\n -72.10601806640625,\n 41.29844430929419\n ],\n [\n -71.87530517578125,\n 41.32320110223851\n ],\n [\n -71.8341064453125,\n 41.32320110223851\n ],\n [\n -71.8231201171875,\n 41.40771586770284\n ],\n [\n -71.806640625,\n 41.44684402008925\n ],\n [\n -71.80389404296875,\n 42.01869237684385\n ],\n [\n -71.80938720703125,\n 42.02889410108475\n ],\n [\n -73.49029541015625,\n 42.05337156043361\n ],\n [\n -73.55621337890625,\n 41.292253642159466\n ],\n [\n -73.49578857421875,\n 41.21791981422843\n ],\n [\n -73.7237548828125,\n 41.104190944576466\n ],\n [\n -73.63311767578125,\n 41.000629848685385\n ],\n [\n -73.64410400390625,\n 40.9964840143779\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df36","contributors":{"authors":[{"text":"Cushman, R.V.","contributorId":28220,"corporation":false,"usgs":true,"family":"Cushman","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":244061,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":51672,"text":"ofr54127 - 1954 - Southern California Water Bulletin for 1953: General review of the water resources of Southern California for the water year of 1952-53 with special reference to the surface runoff for the water year of 1951-52","interactions":[],"lastModifiedDate":"2015-10-01T13:56:56","indexId":"ofr54127","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-127","title":"Southern California Water Bulletin for 1953: General review of the water resources of Southern California for the water year of 1952-53 with special reference to the surface runoff for the water year of 1951-52","docAbstract":"

This WATER BULLETTIN is one of a series issued annually since June 1944. Its main purpose is to present a brief analysis of those phases of the local water supply associated with the work of the Geological Survey. The first part of this review deals with the water resources for the water year ending September 30, 1953. It contains a brief analysis of the annual precipitation, the provisional runoff at a few stations, the changes in water reserves both in surface reservoirs and underground, and the imported waters. It concludes by pointing out the deficiences in the local water reserves. This bulletin has been prepared by the Surface Water Branch; the section on ground-water conditions was prepared chiefly from information supplied by the Ground Hater Branch.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr54127","usgsCitation":"Hofman, W., Briggs, R., and Littlefield, W., 1954, Southern California Water Bulletin for 1953: General review of the water resources of Southern California for the water year of 1952-53 with special reference to the surface runoff for the water year of 1951-52: U.S. Geological Survey Open-File Report 54-127, 30 p., https://doi.org/10.3133/ofr54127.","productDescription":"30 p.","numberOfPages":"37","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":178771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr54127.jpg"},{"id":309421,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0127/report.pdf","text":"Report"}],"country":"United States","state":"California","otherGeospatial":"Southern California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.86035156249999,\n 38.08268954483802\n ],\n [\n -123.06884765625,\n 37.579412513438385\n ],\n [\n -122.25585937500001,\n 36.1822249804225\n ],\n [\n -121.10229492187501,\n 34.6060845921693\n ],\n [\n -120.25634765624999,\n 33.95247360616282\n ],\n [\n -119.036865234375,\n 33.247875947924385\n ],\n [\n -117.94921874999999,\n 32.63012300670739\n ],\n [\n -117.35595703124999,\n 32.55607364492029\n ],\n [\n -116.3671875,\n 32.63012300670739\n ],\n [\n -115.76293945312499,\n 32.722598604044066\n ],\n [\n -114.82910156249999,\n 32.602361666817515\n ],\n [\n -114.444580078125,\n 33.660353121928814\n ],\n [\n -114.224853515625,\n 34.37064492478658\n ],\n [\n -115.367431640625,\n 35.48751102385376\n ],\n [\n -117.5537109375,\n 37.317751851636906\n ],\n [\n -119.608154296875,\n 38.71980474264239\n ],\n [\n -119.86083984375,\n 38.950865400919994\n ],\n [\n -121.86035156249999,\n 38.08268954483802\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7294","contributors":{"authors":[{"text":"Hofman, Walter","contributorId":14496,"corporation":false,"usgs":true,"family":"Hofman","given":"Walter","email":"","affiliations":[],"preferred":false,"id":244117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Briggs, R.C.","contributorId":10022,"corporation":false,"usgs":true,"family":"Briggs","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":244116,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littlefield, W.M.","contributorId":6117,"corporation":false,"usgs":true,"family":"Littlefield","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":244115,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":51630,"text":"ofr5451 - 1954 - Memorandum on ground-water investigations in the Sells area, Papago Indian Reservation, Pima County, Arizona","interactions":[],"lastModifiedDate":"2015-10-22T12:55:47","indexId":"ofr5451","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1954","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":"54-51","title":"Memorandum on ground-water investigations in the Sells area, Papago Indian Reservation, Pima County, Arizona","docAbstract":"

From 1950 to the present date the Ground Water Branch, U.S. Geological Survey, has been collecting data about the ground-water supply in the Sells area, at the request of the Bureau of Indian Affairs, Papago Indian Agency.  The purpose of these studies has been to aid in locating and developing additional ground-water supplies for the community of Sells, the agency headquarters.  The work has been financed by and has been in cooperation with the Papago Indian Agency.  In addition to the author of this memorandum, the following personnel aided in collecting data: D. G. Metzger, H. E. Skibitzke, S.F. Turner, H. N. Wolcott, and C. B. Yost, Jr.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5451","usgsCitation":"Coates, D., 1954, Memorandum on ground-water investigations in the Sells area, Papago Indian Reservation, Pima County, Arizona: U.S. Geological Survey Open-File Report 54-51, 10 p., https://doi.org/10.3133/ofr5451.","productDescription":"10 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":178702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5451.jpg"},{"id":310478,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0051/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Pima","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.91909790039062,\n 31.949831760406877\n ],\n [\n -111.84974670410155,\n 31.950123073342215\n ],\n [\n -111.82777404785156,\n 31.878723805312543\n ],\n [\n -111.91978454589842,\n 31.87347596019353\n ],\n [\n -111.93866729736328,\n 31.949540446547825\n ],\n [\n -111.90982818603516,\n 31.949831760406877\n ],\n [\n -111.91909790039062,\n 31.949831760406877\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613dc8","contributors":{"authors":[{"text":"Coates, D.R.","contributorId":39449,"corporation":false,"usgs":true,"family":"Coates","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":244050,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70173589,"text":"70173589 - 1954 - The quality and character of Pacific Northwest waters","interactions":[],"lastModifiedDate":"2016-06-21T14:05:03","indexId":"70173589","displayToPublicDate":"1959-12-31T00:00:00","publicationYear":"1954","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":"The quality and character of Pacific Northwest waters","docAbstract":"

This paper is a general discussion of the quality and chemical character of surface and ground waters in the Pacific Northwest as shown by the available data. Previous quality of water studies reported in the literature are reviewed. The composition of natural waters is considered as to the source and significance of the different mineral constituents. Analytical data are presented showing mineral constituents and physical properties of selected surface and ground waters in the region.

","conferenceTitle":"Pacific Northwest Metals and Minerals Conference, American Mining and Metallurgical Engineers","conferenceDate":"April 30, 1954","conferenceLocation":"Portland, OR","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70173589","usgsCitation":"Swenson, H.A., 1954, The quality and character of Pacific Northwest waters: Open-File Report, 9 p., https://doi.org/10.3133/70173589.","productDescription":"9 p.","numberOfPages":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":323087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173589.jpg"},{"id":324137,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173589/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5757f064e4b04f417c24dd28","contributors":{"authors":[{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":637377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70111703,"text":"tei229 - 1954 - Radioactive deposits in California","interactions":[],"lastModifiedDate":"2014-06-19T06:25:32","indexId":"tei229","displayToPublicDate":"1955-01-01T12:50:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"229","title":"Radioactive deposits in California","docAbstract":"

Reconnaissance examination by Government geologists of many areas, mine properties, and prospects in California during the period between 1948 and 1953 has confirmed the presence of radioactive materials in place at more than 40 localities. Abnormal radioactivity at these localities is due to concentrations of primary and secondary uranium minerals, to radon gas, radium (?), and to thorium minerals. Of the known occurrences only three were thought to contain uranium oxide (uranitite or pitchblende), 4 contained uranium-bearing columbate, tantalate, or titanate minerals, 12 contained secondary uranium minerals, such as autunite, carnotite, and torbernite, one contained radon gas, 7 contained thorium minerals, and, at the remaining 16 localities, the source of the anomalous radiation was not positively determined.

\n
\n

The occurrences in which uranium oxide has been tentatively identified include the Rathgeb mine (Calaveras County), the Yerih group of claims (San Bernardino County), and the Rainbow claim (Madera County). Occurrences of secondary uranium minerals are largely confined to the arid desert regions of south-eastern California including deposits in San Bernardino, Kern, Inyo, and Imperial Counties. Uranium-bearing columbate, tantalate, or titanate minerals have been reported from pegmatite and granitic rock in southeastern and eastern California.

\n
\n

Thorium minerals have been found in vein deposits in eastern San Bernardino County and from pegmatites and granitic rocks in various parts of southeastern California; placer concentrations of thorium minerals are known from nearly all areas in the State that are underlain, in part, by plutonic crystalline rocks.

\n
\n

The primary uranium minerals occur principally as minute accessory crystals in pegmatite or granitic rock, or with base-metal sulfide minerals in veins. Thorium minerals also occur as accessory crystals in pegmatite or granitic rock, in placer deposits derived from such rock, and, at Mountain Pass, in veins containing rare earths. Secondary uranium minerals have been found as fracture coatings and as disseminations in various types of wall rock, although they are largely confined to areas of Tertiary volcanic rocks. Probably the uranium in the uraniferous deposits in California is related genetically to felsic crystalline rocks and felsic volcanic rocks; the present distribution of the secondary uranium minerals has been controlled, in part, by circulating ground waters and probably, in part, by magmatic waters related to the Tertiary volcanic activity. The thorium minerals are genetically related to the intrusion of pegmatite and plutonic crystalline rocks.

\n
\n

None of the known deposits of radioactive minerals in California contain marketable reserves of uranium or thorium ore under economic conditions existing in 1952. With a favorable local market small lots of uranium ore may be available in the following places: the Rosamund prospect, the Rafferty and Chilson properties, the Lucky Star claim, and the Yerih group. The commercial production of thorium minerals will be possible, in the near future, only if these minerals can be recovered cheaply as a byproduct either from the mining of rare earths minerals at Mountain Pass or as a byproduct of placer mining for gold.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei229","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Walker, G.W., and Lovering, T., 1954, Radioactive deposits in California: U.S. Geological Survey Trace Elements Investigations 229, Report: 69 p.; Plate: 15.74 x 19.77 inches, https://doi.org/10.3133/tei229.","productDescription":"Report: 69 p.; Plate: 15.74 x 19.77 inches","numberOfPages":"78","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":288850,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288848,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0229/plate-1.pdf"},{"id":288849,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0229/report.pdf"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.01 ], [ -114.13,42.01 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae77fde4b0abf75cf2c688","contributors":{"authors":[{"text":"Walker, George W.","contributorId":101308,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":494447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lovering, Tom G.","contributorId":31679,"corporation":false,"usgs":true,"family":"Lovering","given":"Tom G.","affiliations":[],"preferred":false,"id":494446,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206101,"text":"70206101 - 1954 - Caribbean land and sea through the ages ","interactions":[],"lastModifiedDate":"2020-03-19T14:32:06","indexId":"70206101","displayToPublicDate":"1954-10-22T10:21:45","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Caribbean land and sea through the ages ","docAbstract":"

The oldest part of the Caribbean region proper is in northern Central America, where Permian (?) and Lower Permian marine deposits rest on metamorphic rocks of unknown, possibly middle Paleozoic, age. According to present dating, geosynclinal deposition spread eastward in Late Jurassic time to include Cuba, farther eastward and southward in Early Cretaceous time to include Hispaniola and probably Jamaica, and still farther eastward in Late Cretaceous time to include Puerto Rico, the Virgin Islands, and St. Croix. Throughout the Caribbean region, the Cretaceous is characterized by volcanics of great thickness, pyroclastics being more widespread and thicker than flows. These volcanics evidently were derived from lands of unknown size that are now under the waters of the Caribbean Sea. Land still persisted south of eastern Cuba during Eocene time. Thereafter no geological evidence is now available pointing to land in the Caribbean Sea. © 1954, The Geological Society of America, Inc.

","language":"English ","publisher":"Geological Society of America ","doi":"10.1130/0016-7606(1954)65[719:CLASTT]2.0.CO;2","issn":"00167606","usgsCitation":"Woodring, W.P., 1954, Caribbean land and sea through the ages : Geological Society of America Bulletin, v. 65, no. 8, p. 719-732, https://doi.org/10.1130/0016-7606(1954)65[719:CLASTT]2.0.CO;2.","productDescription":"14 p. 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Rico\",\"nation\":\"USA \"}}]}","volume":"65","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Woodring, Wendell Phillips","contributorId":10672,"corporation":false,"usgs":true,"family":"Woodring","given":"Wendell","email":"","middleInitial":"Phillips","affiliations":[],"preferred":false,"id":773576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221463,"text":"70221463 - 1954 - Some notes on the relation of ground‐water levels to pond levels in limestone sinks of southwestern Georgia","interactions":[],"lastModifiedDate":"2021-06-16T16:10:44.71487","indexId":"70221463","displayToPublicDate":"1954-10-01T11:06:47","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Some notes on the relation of ground‐water levels to pond levels in limestone sinks of southwestern Georgia","docAbstract":"

Records of water levels in limesink ponds in southwestern Georgia and of water‐table levels in the vicinity of these ponds are used to demonstrate: (1) some ponds with highly impermeable beds are virtually unaffected by water‐table levels, except when water‐table levels are above the rim of the impervious materials; (2) interchange of water between pond and water table occurs when beds are relatively permeable. Three phases in the relation between pond level and water‐table level are recognized: (1) water‐table level higher than pond level causing ground‐water flow into the pond; (2) ground‐water level below pond level but in direct contact with it and measurably controlling rate of seepage from the pond; (3) ground‐water level below pond level but not in direct contact with it and not appreciably controlling rate of seepage from the pond. In phase (3) the water table has a perceptible mound at a point underneath the pond. 

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR035i005p00796","usgsCitation":"Hendricks, E.L., 1954, Some notes on the relation of ground‐water levels to pond levels in limestone sinks of southwestern Georgia: Eos, Transactions, American Geophysical Union, v. 35, no. 5, p. 796-804, https://doi.org/10.1029/TR035i005p00796.","productDescription":"9 p.","startPage":"796","endPage":"804","costCenters":[],"links":[{"id":386543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"southwestern Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.4521484375,\n 30.713503990354965\n ],\n [\n -80.9033203125,\n 30.713503990354965\n ],\n [\n -80.9033203125,\n 32.95336814579932\n ],\n [\n -83.4521484375,\n 32.95336814579932\n ],\n [\n -83.4521484375,\n 30.713503990354965\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"35","issue":"5","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221459,"text":"70221459 - 1954 - Copper cities copper deposit, Globe-Miami district, Arizona","interactions":[],"lastModifiedDate":"2021-06-16T15:51:39.630777","indexId":"70221459","displayToPublicDate":"1954-06-01T10:42:53","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Copper cities copper deposit, Globe-Miami district, Arizona","docAbstract":"

The Copper Cities copper deposit in the Globe-Miami district, Arizona, is now in process of development. It is of the \"porphyry\" type and occurs in a body of quartz monzonite that has been intruded by smaller masses of granite porphyry. The hypogene sulfides are pyrite, chalcopyrite, and a very little molybdenite. Pyritic mineralization extends over a large area of which only a small portion contains an appreciable amount of chalcopyrite. The outcrop of the copper-bearing rock, roughly 1,800 feet square, is bounded on the west, north, and east sides by fault zones. The south boundary is gradational. The pyrite to chalcopyrite ratio of the protore increases rapidly with depth, whereas the copper content decreases but slightly. The ore body is a shallow chalcocite zone formed by supergene enrichment. Bodies of granite porphyry within the copper-bearing area were not as strongly mineralized by hypogene solutions as the quartz monzonite, and in them the chalcocite zone is thin, undoubtedly because the granite porphyry is less pervious to ground water than the quartz monzonite. 

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.49.4.362","usgsCitation":"Peterson, N.P., 1954, Copper cities copper deposit, Globe-Miami district, Arizona: Economic Geology, v. 49, no. 4, p. 362-377, https://doi.org/10.2113/gsecongeo.49.4.362.","productDescription":"16 p.","startPage":"362","endPage":"377","costCenters":[],"links":[{"id":386539,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","city":"Miami","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.91110229492188,\n 33.354620418436255\n ],\n [\n -110.83694458007811,\n 33.354620418436255\n ],\n [\n -110.83694458007811,\n 33.43144133557529\n ],\n [\n -110.91110229492188,\n 33.43144133557529\n ],\n [\n -110.91110229492188,\n 33.354620418436255\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"49","issue":"4","noUsgsAuthors":false,"publicationDate":"1954-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Peterson, N. P.","contributorId":29827,"corporation":false,"usgs":true,"family":"Peterson","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":817762,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":78587,"text":"tem783 - 1954 - Uranium in natural waters","interactions":[],"lastModifiedDate":"2014-07-17T08:53:04","indexId":"tem783","displayToPublicDate":"1954-06-01T08:52:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"783","title":"Uranium in natural waters","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/tem783","usgsCitation":"Fix, P.F., 1954, Uranium in natural waters: U.S. Geological Survey Trace Elements Memorandum 783, 17 p., https://doi.org/10.3133/tem783.","productDescription":"17 p.","numberOfPages":"17","costCenters":[],"links":[{"id":290342,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7a66e4b0b2908510d77b","contributors":{"authors":[{"text":"Fix, Philip Forsyth","contributorId":53390,"corporation":false,"usgs":true,"family":"Fix","given":"Philip","email":"","middleInitial":"Forsyth","affiliations":[],"preferred":false,"id":288970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221460,"text":"70221460 - 1954 - Sedimentary facies of iron-formation","interactions":[],"lastModifiedDate":"2021-06-16T15:56:48.830475","indexId":"70221460","displayToPublicDate":"1954-05-01T10:54:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Sedimentary facies of iron-formation","docAbstract":"

The sedimentary iron-formations of Precambrian age in the Lake Superior region can be divided on the basis of the dominant original iron mineral into four principal facies: sulfide, carbonate, oxide, and silicate. As chemical sediments, these rocks reflect certain aspects of the chemistry of the depositional environments. The major control, at least for the sulfide, carbonate, and oxide types, probably was the oxidation potential. The evidence indicates that deposition took place in restricted basins, which were separated from the open sea by thresholds that inhibited free circulation and permitted development of abnormalities in oxidation potential and water composition. The sporadic distribution of metamorphism and of later oxidation permits description of the primary facies on the basis of unoxidized, essentially unmetamorphosed material. The sulfide facies is represented by black slates in which pyrite may make up as much as 40 percent of the rock. The free-carbon content of these rocks typically ranges from 5 to 15 percent, indicating that ultra-stagnant conditions prevailed during deposition. Locally, the pyritic rocks contain layers of iron-rich carbonate. The carbonate facies consists, in its purer form, of interbedded iron-rich carbonate and chert. It is a product of an environment in which oxygen concentration was sufficiently high to destroy most of the organic material but not high enough to permit formation of ferric compounds. The oxide facies is found as two principal types, one characterized by magnetite and the other by hematite. Both minerals appear to be of primary origin. The magnetite-banded rock is one of the dominant lithologies in the region; it consists typically of magnetite interlayered with chert, carbonate, or iron silicate, or combinations of the three. Its mineralogy and association suggest origin under weakly oxidizing to moderately reducing conditions, but the mode of precipitation of magnetite is not clearly understood. The hematite-banded rocks consist of finely crystalline hematite interlayered with chert or jasper. Oolitic structure is common. This facies doubtless accumulated in a strongly oxidizing, probably near-shore, environment similar to that in which younger hema-titic ironstones such as the Clinton oolite were deposited. The silicate facies contains one or more of the hydrous ferrous silicates (greenalite, minnesotaite, stilpnomelane, chlorite) as a major constituent. Granule structure, similar to that of glauconite, is typical of some varieties; others are nongranular and finely laminated. The most common association of the silicate rocks is with either carbonate- or magnetite-bearing rocks, which suggests that the optimum conditions for deposition ranged from slightly oxidizing to slightly reducing. The relationship between the iron-rich rocks and volcanism, stressed by many authors, is considered by the writer to be structural, not chemical: in the Lake Superior region both iron-deposition and volcanism are believed to be related to geosynclinal development during Huronian time. In Michigan, the lower Huronian rocks are iron-poor quartzite and dolomite-typical \"stable-shelf\" deposits; much of the upper Huronian consists of iron-poor graywacke and slate with associated volcanic rocks -a typical \"geosynclinal\" assemblage. Thus the iron-rich beds of the middle Huronian and lower part of the upper Huronian were deposited during a transitional stage in structural history. The major environmental requirement for deposition of iron-formation is the closed or restricted basin; this requirement coincides in time with what would be a normal stage in evolution of the geosyncline: namely, structural development of offshore buckles or swells that subsequently develop into island arcs characterized by volcanism. 

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.49.3.235","usgsCitation":"James, H.L., 1954, Sedimentary facies of iron-formation: Economic Geology, v. 49, no. 3, p. 235-293, https://doi.org/10.2113/gsecongeo.49.3.235.","productDescription":"59 p.","startPage":"235","endPage":"293","costCenters":[],"links":[{"id":386540,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States, Canada","otherGeospatial":"Lake Superior","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.7685546875,\n 46.164614496897094\n ],\n [\n -82.3974609375,\n 46.164614496897094\n ],\n [\n -82.3974609375,\n 50.00773901463687\n ],\n [\n -92.7685546875,\n 50.00773901463687\n ],\n [\n -92.7685546875,\n 46.164614496897094\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"49","issue":"3","noUsgsAuthors":false,"publicationDate":"1954-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"James, H. L.","contributorId":96732,"corporation":false,"usgs":true,"family":"James","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":817763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010706,"text":"70010706 - 1954 - Chemical and physical characteristics of Delaware River water from Trenton, N. J., to Marcus Hook, Pa., 1949-52","interactions":[],"lastModifiedDate":"2026-03-06T15:12:35.466533","indexId":"70010706","displayToPublicDate":"1954-04-30T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Chemical and physical characteristics of Delaware River water from Trenton, N. J., to Marcus Hook, Pa., 1949-52","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3096.613","issn":"00368075","usgsCitation":"Durfor, C., and Keighton, W.B., 1954, Chemical and physical characteristics of Delaware River water from Trenton, N. J., to Marcus Hook, Pa., 1949-52: Science, v. 119, no. 3096, p. 613-614, https://doi.org/10.1126/science.119.3096.613.","productDescription":"2 p.","startPage":"613","endPage":"614","costCenters":[],"links":[{"id":219546,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Delaware River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -75.11855426637116,\n 39.99168534331409\n ],\n [\n -75.48006759342248,\n 39.8267274262501\n ],\n [\n -75.32733757633989,\n 39.792032377028846\n ],\n [\n -74.90974946805811,\n 40.01803129259913\n ],\n [\n -74.74614999739644,\n 40.136415002845574\n ],\n [\n -74.68690762570597,\n 40.22268195502912\n ],\n [\n -74.8061641099804,\n 40.22619737950856\n ],\n [\n -74.8720058656924,\n 40.13752567264328\n ],\n [\n -75.11855426637116,\n 39.99168534331409\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"119","issue":"3096","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f54be4b0c8380cd4c170","contributors":{"authors":[{"text":"Durfor, C.N.","contributorId":10094,"corporation":false,"usgs":true,"family":"Durfor","given":"C.N.","affiliations":[],"preferred":false,"id":359460,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keighton, Walter B.","contributorId":81877,"corporation":false,"usgs":true,"family":"Keighton","given":"Walter","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359461,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011033,"text":"70011033 - 1954 - The chemical quality of surface waters in Devils Lake basin, North Dakota","interactions":[],"lastModifiedDate":"2026-03-06T15:21:48.532678","indexId":"70011033","displayToPublicDate":"1954-04-30T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"The chemical quality of surface waters in Devils Lake basin, North Dakota","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3096.614.a","issn":"00368075","usgsCitation":"Swenson, H.A., and Colby, B.R., 1954, The chemical quality of surface waters in Devils Lake basin, North Dakota: Science, v. 119, no. 3096, p. 614-614, https://doi.org/10.1126/science.119.3096.614.a.","productDescription":"1 p.","startPage":"614","endPage":"614","costCenters":[],"links":[{"id":221799,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Devils Lake basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -99.25806363324698,\n 48.16498780293537\n ],\n [\n -99.25806363324698,\n 47.83293405008746\n ],\n [\n -98.28583590294986,\n 47.83293405008746\n ],\n [\n -98.28583590294986,\n 48.16498780293537\n ],\n [\n -99.25806363324698,\n 48.16498780293537\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"119","issue":"3096","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baa2de4b08c986b322747","contributors":{"authors":[{"text":"Swenson, H. A.","contributorId":58618,"corporation":false,"usgs":true,"family":"Swenson","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colby, B. R.","contributorId":59776,"corporation":false,"usgs":true,"family":"Colby","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":360118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":51631,"text":"ofr5452 - 1954 - Ground-water field trip, Tucson to Nogales, Arizona","interactions":[],"lastModifiedDate":"2015-10-22T12:56:49","indexId":"ofr5452","displayToPublicDate":"1954-04-24T00:00:00","publicationYear":"1954","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":"54-52","title":"Ground-water field trip, Tucson to Nogales, Arizona","docAbstract":"

A field excursion following the route described herein was conducted as a part of the curriculum of the 6th Ground Water Short Course, which was held by the Geological Survey at the University of Arizona in April 1954. The route log and descriptive text were designed to provide a general background of the ground-water situation in the Upper Santa Cruz Basin, a few of the geologic features that affect the occurrence of ground water, and some of the historical highlights of the region. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5452","usgsCitation":"Coates, D., and Halpenny, L., 1954, Ground-water field trip, Tucson to Nogales, Arizona: U.S. Geological Survey Open-File Report 54-52, 25 p., https://doi.org/10.3133/ofr5452.","productDescription":"25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":178703,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5452.jpg"},{"id":310479,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1954/0052/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","otherGeospatial":"Santa Cruz Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.05667114257812,\n 31.333698040439433\n ],\n [\n -110.80947875976562,\n 31.33604401284106\n ],\n [\n -110.71746826171875,\n 31.387640604815132\n ],\n [\n -110.65017700195312,\n 31.522361470421437\n ],\n [\n -110.709228515625,\n 31.572685550720422\n ],\n [\n -110.73806762695312,\n 31.59725256170666\n ],\n [\n -110.79025268554686,\n 31.612457465205498\n ],\n [\n -110.87677001953125,\n 31.612457465205498\n ],\n [\n -110.94955444335938,\n 31.615965936476076\n ],\n [\n -111.0498046875,\n 31.615965936476076\n ],\n [\n -111.08551025390624,\n 31.611287945395063\n ],\n [\n -111.1376953125,\n 31.606609719226917\n ],\n [\n -111.16241455078125,\n 31.532896662756986\n ],\n [\n -111.15280151367188,\n 31.44389548193338\n ],\n [\n -111.13082885742188,\n 31.371226579385738\n ],\n [\n -111.0992431640625,\n 31.339562861784987\n ],\n [\n -111.03607177734375,\n 31.333698040439433\n ],\n [\n -111.05667114257812,\n 31.333698040439433\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cde6","contributors":{"authors":[{"text":"Coates, D.R.","contributorId":39449,"corporation":false,"usgs":true,"family":"Coates","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":244051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halpenny, L.C.","contributorId":40967,"corporation":false,"usgs":true,"family":"Halpenny","given":"L.C.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":244052,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011046,"text":"70011046 - 1954 - Water resources of the Louisville area, Kentucky and Indiana","interactions":[],"lastModifiedDate":"2026-03-06T16:40:22.307872","indexId":"70011046","displayToPublicDate":"1954-04-09T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Water resources of the Louisville area, Kentucky and Indiana","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3093.477.a","issn":"00368075","usgsCitation":"Rorabaugh, M.I., Schrader, F.F., and Laird, L., 1954, Water resources of the Louisville area, Kentucky and Indiana: Science, v. 119, no. 3093, p. 477-477, https://doi.org/10.1126/science.119.3093.477.a.","productDescription":"1 p.","startPage":"477","endPage":"477","costCenters":[],"links":[{"id":220812,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana, Kentucky","city":"Louisville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -85.95993444811936,\n 38.395009974436675\n ],\n [\n -85.95993444811936,\n 38.07903267436703\n ],\n [\n -85.47463665670458,\n 38.07903267436703\n ],\n [\n -85.47463665670458,\n 38.395009974436675\n ],\n [\n -85.95993444811936,\n 38.395009974436675\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"119","issue":"3093","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcc0ae4b08c986b32d939","contributors":{"authors":[{"text":"Rorabaugh, M. I.","contributorId":28221,"corporation":false,"usgs":true,"family":"Rorabaugh","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":360152,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schrader, F. F.","contributorId":88082,"corporation":false,"usgs":true,"family":"Schrader","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":360153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Laird, L.B.","contributorId":23522,"corporation":false,"usgs":true,"family":"Laird","given":"L.B.","email":"","affiliations":[],"preferred":false,"id":360151,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010509,"text":"70010509 - 1954 - Ground water in the High Plains of west-central United States","interactions":[],"lastModifiedDate":"2026-03-09T15:08:35.539649","indexId":"70010509","displayToPublicDate":"1954-04-02T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in the High Plains of west-central United States","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3092.446.a","issn":"00368075","usgsCitation":"Lohman, S.W., 1954, Ground water in the High Plains of west-central United States: Science, v. 119, no. 3092, p. 446-446, https://doi.org/10.1126/science.119.3092.446.a.","productDescription":"1 p.","startPage":"446","endPage":"446","costCenters":[],"links":[{"id":219460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"High Plains, west-central United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.15341360416161,\n 38.859268535214454\n ],\n [\n -109.15341360416161,\n 30.670075372843385\n ],\n [\n -93.8596146900224,\n 30.670075372843385\n ],\n [\n -93.8596146900224,\n 38.859268535214454\n ],\n [\n -109.15341360416161,\n 38.859268535214454\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"119","issue":"3092","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2b16e4b0c8380cd5b6c5","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221464,"text":"70221464 - 1954 - Symposium on land erosion: Introduction","interactions":[],"lastModifiedDate":"2021-06-16T16:13:58.901482","indexId":"70221464","displayToPublicDate":"1954-04-01T11:11:23","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Symposium on land erosion: Introduction","docAbstract":"

One of the very obvious geologic phenomena that is continuously in operation throughout the Earth's land surface is erosion, the process of wearing away the soil or the surface mantle. The falling of rain drops on an unprotected slope, the flow of water across land or in a channel, the borings of a rodent, the expansion of a root, the pull of gravity, the gouging of a glacier, or the impinging of wind on an open surface are some of the forces continually at work in this erosion process. The tendency of these forces is to bring everything to a common level and the moment a point of land or a continent rises above its surroundings, gravity, rain, wind, and all the other forces set to work, bringing it back to the level of its nieghbor. The poetic expression “the everlasting hills” is an illusion, for these erosion forces have been operative since the dawn of geologic history and the evidence is conclusive that in this sequence of time numerous generations of hills and mountain ranges have been uplifted and then razed by erosion, the waste and rock debris of one range forming the source material for its successor. We could not have the great deposits of alluvium and the thick beds of conglomerate, sandstones, and shales that occur at present throughout the Earth without erosion to furnish the source material.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR035i002p00243","usgsCitation":"Peterson, H., 1954, Symposium on land erosion: Introduction: Eos, Transactions, American Geophysical Union, v. 35, no. 2, p. 243-244, https://doi.org/10.1029/TR035i002p00243.","productDescription":"2 p.","startPage":"243","endPage":"244","costCenters":[],"links":[{"id":386544,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Peterson, H.V.","contributorId":86007,"corporation":false,"usgs":true,"family":"Peterson","given":"H.V.","email":"","affiliations":[],"preferred":false,"id":817768,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220450,"text":"5220450 - 1954 - Marsh and aquatic weed problems in wildlife habitat","interactions":[],"lastModifiedDate":"2026-03-18T22:43:05.597572","indexId":"5220450","displayToPublicDate":"1954-04-01T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3741,"text":"Weeds","active":true,"publicationSubtype":{"id":10}},"title":"Marsh and aquatic weed problems in wildlife habitat","docAbstract":"

To most people, the word weeds signifies pest plants of the farm, roadside, or other upland areas. However, weeds also occur on, under, or near water. Fifteen million dollars have been spent on a single aquatic nuisance in the South—the prolific water-hyacinth which clogs navigable streams and lakes with its growth. Hundreds of thousands of dollars have also been expended on control of the waterchestnut or water caltrop in the Potomac River. In addition, smaller-scale local campaigns are continuing against cattails, reeds, giant cutgrass, maidencane, alligatorweed, needlerush, lotus, rose-mallows, willows, alders, buttonbush, and similar weeds that interfere with land use for recreation, irrigation, or other purposes. Since control of marsh and aquatic plants in wildlife habitat is an unfamiliar activity to most weed workers, broad aspects of its what, why, and how will be explained briefly.

","language":"English","publisher":"Cambridge University Press","doi":"10.2307/4040041","usgsCitation":"Martin, A.C., 1954, Marsh and aquatic weed problems in wildlife habitat: Weeds, v. 3, no. 2, p. 139-142, https://doi.org/10.2307/4040041.","productDescription":"4 p.","startPage":"139","endPage":"142","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193800,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fbd5","contributors":{"authors":[{"text":"Martin, A. C.","contributorId":33754,"corporation":false,"usgs":true,"family":"Martin","given":"A.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":331833,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011030,"text":"70011030 - 1954 - Ground water in the Navajo country","interactions":[],"lastModifiedDate":"2026-03-09T15:32:32.443091","indexId":"70011030","displayToPublicDate":"1954-03-26T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in the Navajo country","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3091.421.a","issn":"00368075","usgsCitation":"Harshbarger, J.W., 1954, Ground water in the Navajo country: Science, v. 119, no. 3091, p. 421-421, https://doi.org/10.1126/science.119.3091.421.a.","productDescription":"1 p.","startPage":"421","endPage":"421","costCenters":[],"links":[{"id":221796,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico, Utah","otherGeospatial":"Navajo country","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.00125368251301,\n 37.91854878483352\n ],\n [\n -110.61543605858947,\n 35.69793813206712\n ],\n [\n -107.27238503153427,\n 35.69793813206712\n ],\n [\n -107.02596023326518,\n 36.98504887788525\n ],\n [\n -109.01365095325309,\n 36.940976384060356\n ],\n [\n -108.91989415797093,\n 37.87415294775664\n ],\n [\n -111.00125368251301,\n 37.91854878483352\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"119","issue":"3091","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2af6e4b0c8380cd5b5d1","contributors":{"authors":[{"text":"Harshbarger, J. W.","contributorId":22309,"corporation":false,"usgs":true,"family":"Harshbarger","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":360113,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010508,"text":"70010508 - 1954 - Geology and ground water resources of the Matanuska Valley agricultural area, Alaska","interactions":[],"lastModifiedDate":"2026-03-09T22:30:01.435821","indexId":"70010508","displayToPublicDate":"1954-03-12T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground water resources of the Matanuska Valley agricultural area, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3089.356.a","issn":"00368075","usgsCitation":"Trainer, F., 1954, Geology and ground water resources of the Matanuska Valley agricultural area, Alaska: Science, v. 119, no. 3089, p. 356-356, https://doi.org/10.1126/science.119.3089.356.a.","productDescription":"1 p.","startPage":"356","endPage":"356","costCenters":[],"links":[{"id":219459,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Matanuska Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -151.5854954486002,\n 62.208203267165345\n ],\n [\n -151.5854954486002,\n 61.27733469146847\n ],\n [\n -150.0180946058932,\n 61.27733469146847\n ],\n [\n -150.0180946058932,\n 62.208203267165345\n ],\n [\n -151.5854954486002,\n 62.208203267165345\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"119","issue":"3089","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2307e4b0c8380cd57530","contributors":{"authors":[{"text":"Trainer, F.W.","contributorId":26007,"corporation":false,"usgs":true,"family":"Trainer","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":359079,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010510,"text":"70010510 - 1954 - Developed and potential water power of the United States and other countries of the world","interactions":[],"lastModifiedDate":"2026-03-09T23:06:08.947162","indexId":"70010510","displayToPublicDate":"1954-03-05T00:00:00","publicationYear":"1954","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Developed and potential water power of the United States and other countries of the world","docAbstract":"

No abstract available.

","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.119.3088.328.b","issn":"00368075","usgsCitation":"Jones, B.E., and Young, L., 1954, Developed and potential water power of the United States and other countries of the world: Science, v. 119, no. 3088, p. 328-329, https://doi.org/10.1126/science.119.3088.328.b.","productDescription":"2 p.","startPage":"328","endPage":"329","costCenters":[],"links":[{"id":219461,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"3088","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0005e4b0c8380cd4f53f","contributors":{"authors":[{"text":"Jones, B. E.","contributorId":70787,"corporation":false,"usgs":true,"family":"Jones","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359082,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, L.L.","contributorId":16497,"corporation":false,"usgs":true,"family":"Young","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":359081,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70048221,"text":"tei356 - 1954 - The copper and uranium deposits of the Coyote district, Mora County, New Mexico","interactions":[],"lastModifiedDate":"2013-11-22T09:19:59","indexId":"tei356","displayToPublicDate":"1954-01-20T11:52:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"356","title":"The copper and uranium deposits of the Coyote district, Mora County, New Mexico","docAbstract":"The copper and uranium-vanadium deposits of the Coyote district, Mora County, N. Mec, are confined to the lower 2,000 feet of the Sangre de Gristo formation of Pennsylvanian and Permian age. A narrow belt of deposits in steeply dipping or overturned rocks extends for 7 miles along Coyote Creek south of Guadalupita. Earlier studies showed that the copper deposits contained uranium, but both the reserves and the uranium content of the copper-bearing\nshale are too low to permit the recovery of uranium. However, small, commercial grade uranium deposits have been discovered in sandstone. Small lenses of copper-bearing carbonaceous shale, siltstone, limestone or sandstone, interbedded with predominantly red rocks, are present at intervals at 12 or more stratigraphic levels. The better deposits, in carbonaceous shale, average about 2 percent copper. The copper content of the other rocks is usually lower, but small concentrations may contain 6 percent copper. The principal copper minerals are chalcocite and malachite. Chalcocite replaces wood and forms nodules that contain small, variable amounts of pyrite, bornite, covellite, and rarely, uraninite. The uranium deposits occur as small closely spaced pockets that are commonly localized by sedimentary structures within one or more fluviatile arkosic sandstone beds near the middle of the formation, particularly\" where carbonized wood, clay galls, and rock fragments are abundant. The uraniferous sandstone is commonly stained pink by hematite that probably was introduced with the uranium. The color increases in intensity with the radioactivity. The outcrops of the uranium deposits are typically inconspicuous, but close inspection shows they contain malachite, chalcopyrite, black vanadium minerals of micaceous habit, metatyuyamunite and microscopic\ngrains of an unidentified black uraniferous substance. The proportion of copper, uranium, and vanadium is variable and any metal may be dominant. The metals probably were derived from pre-Cambrian granitic rocks. Copper and minor amounts of uranium were deposited in local stagnant basins by reaction with hydrogen sulfide. and decaying organic material. The uraniferous shales and the copper deposits are believed to be syngenetic, or nearly so, but the uranium deposits in sandstone are epigenetic and probably were deposited from ground waters with a possible hydrothermal admixture. The uranium and vanadium may have been\nreconcentrated from earlier, low-grade, syngenetic deposits.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei356","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Tschanz, C., Laub, D., and Fuller, G., 1954, The copper and uranium deposits of the Coyote district, Mora County, New Mexico: U.S. Geological Survey Trace Elements Investigations 356, Report: 72 p.; Plate 2: 10.93 inches x 21.95 inches; Plate 6: 21.25 inches x 17.23 inches; Plate 8: 23.24 inches x 18.03 inches; Plate 9: 24.22 inches x 19.11 inches; Plate 10: 22.49 inches x 18.28 inches; Plate 12: 18.09 inches x 23.98 inches; Plate 13: 17.43 inches x 17.46 inches, https://doi.org/10.3133/tei356.","productDescription":"Report: 72 p.; Plate 2: 10.93 inches x 21.95 inches; Plate 6: 21.25 inches x 17.23 inches; Plate 8: 23.24 inches x 18.03 inches; Plate 9: 24.22 inches x 19.11 inches; Plate 10: 22.49 inches x 18.28 inches; Plate 12: 18.09 inches x 23.98 inches; Plate 13: 17.43 inches x 17.46 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277745,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/356/report-thumb.jpg"},{"id":279516,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/356/report.pdf"},{"id":279517,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/356/plate-02.pdf"},{"id":279518,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/356/plate-06.pdf"},{"id":279519,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/356/plate-08.pdf"},{"id":279520,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/356/plate-09.pdf"},{"id":279521,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/356/plate-10.pdf"},{"id":279522,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/356/plate-13.pdf"}],"country":"United States","state":"New Mexico","city":"Mora County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.720284,35.755951 ], [ -105.720284,36.262924 ], [ -104.327354,36.262924 ], [ -104.327354,35.755951 ], [ -105.720284,35.755951 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523979fce4b04b9308ae4fb1","contributors":{"authors":[{"text":"Tschanz, C.M.","contributorId":62659,"corporation":false,"usgs":true,"family":"Tschanz","given":"C.M.","affiliations":[],"preferred":false,"id":484029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laub, D.C.","contributorId":29493,"corporation":false,"usgs":true,"family":"Laub","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":484028,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, G.W.","contributorId":95540,"corporation":false,"usgs":true,"family":"Fuller","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":484030,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70113791,"text":"tei463 - 1954 - Uranium-bearing lignite in southwestern North Dakota","interactions":[],"lastModifiedDate":"2014-07-14T14:21:30","indexId":"tei463","displayToPublicDate":"1954-01-01T14:54:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"463","title":"Uranium-bearing lignite in southwestern North Dakota","docAbstract":"

Uranium-bearing lignite was mapped and sampled in the Bullion Butte, Sentinel Butte, HT Butte, and Chalky Buttes areas in southwestern North Dakota. The uraniferous lignite occurs at several stratigraphic positions in the Sentinel Butte member of the Fort Union formation of Paleocene age. A total of 261 samples were collected for uranium analysis from 85 localities, Lignite contained as much as 0.045 percent uranium, 10.0 percent ash, and 0.45 percent uranium in the ash was found although the average is lower. Inferred reserves for the four areas examined are estimated to be about 27 million tons of lignite in beds about 2 feet thick and containing more than 3000 tons of uranium. The lignite in beds about 2 feet thick and containing more than 3000 tons of uranium. The lignite averages more than 30 percent ash in the surface samples. The principal factor that seems to influence the uranium content of lignite beds is their stratigraphic position below the overlying rocks of the White River group of Oligocene age. All of the uranium-bearing beds closely underlie the base of the White River group. Although this relationship seems to be the controlling factor, the relative concentration of uranium may be modified by other conditions. Beds enclosed in permeable rocks are more uraniferous than beds in impermeable rocks, and thin beds have higher content of uranium than thick beds. In addition, thick lignite beds commonly have a top=preferential distribution of uranium. These and other factors suggest that the uranium is secondary and this it was introduced by ground water which had leached uranium from volcanic ash in the overlying rocks of the White River group. It is thought that the uranium is held in the lignite as part of a metallo-organic compound.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei463","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Moore, G.W., Melin, R.E., and Kepferle, R.C., 1954, Uranium-bearing lignite in southwestern North Dakota: U.S. Geological Survey Trace Elements Investigations 463, Report: 35 p.; 1 Plate: 22.82 x 17.92 inches, https://doi.org/10.3133/tei463.","productDescription":"Report: 35 p.; 1 Plate: 22.82 x 17.92 inches","numberOfPages":"36","costCenters":[],"links":[{"id":289974,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289973,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0463/report.pdf"},{"id":289970,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0463/plate-1.pdf"}],"country":"United States","state":"Montana;North Dakota;South Dakota","otherGeospatial":"Bullion Butte;Chalky Buttes;Ht Butte;Sentinel Butte","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.0299,44.9987 ], [ -105.0299,47.1933 ], [ -102.3265,47.1933 ], [ -102.3265,44.9987 ], [ -105.0299,44.9987 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ae7890e4b0abf75cf2d8ff","contributors":{"authors":[{"text":"Moore, George W.","contributorId":21625,"corporation":false,"usgs":true,"family":"Moore","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495193,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Melin, Robert E.","contributorId":23198,"corporation":false,"usgs":true,"family":"Melin","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":495194,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kepferle, Roy C.","contributorId":103586,"corporation":false,"usgs":true,"family":"Kepferle","given":"Roy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":495195,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":71488,"text":"tei458 - 1954 - Stratigraphy of parts of De Soto and Hardee Counties, Florida","interactions":[],"lastModifiedDate":"2014-05-23T16:05:27","indexId":"tei458","displayToPublicDate":"1954-01-01T10:35:00","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"458","title":"Stratigraphy of parts of De Soto and Hardee Counties, Florida","docAbstract":"

The late Cenozoic stratigraphy of part of central Florida immediately south of the land-pebble phosphate district was studies in detail to determine the southern limit of the economically important Bone Valley formation and its relations with marine rocks of late Miocene and Pliocene age in south-central Florida. In addition a reconnaissance\ntype appraisal of the phosphate and uranium resources of this area was\ndesired. The upper Tertiary and Quaternary rocks were mapped, and the\neconomic geology was studied in a general manner.

\n
\n

The Hawthorn formation of middle Miocene age, is the oldest rock\nExposed. Undifferentiated phosphatic sand and clay may be composed of\nthe Bone Valley formation, of late Miocene to Pliocene age; a combination\nof Bone Valley formation and residuum of weathered Hawthorn formation;\nor Hawthorn residuum alone. The Bone Valley formation and residuum of\nHawthorn formation appear almost identical in cuttings from auger drilling\nin this area. It was not feasible nor practical to map these two\nunits separately. The undifferentiated phosphatic sand and clay interfingers with a marine sand of late Miocene age, The Caloosahatchee marl of Pliocene age, is present in the southeast corner of the area\ninvestigated. It is apparent that the undifferentiated phosphatic sand\nand clay was undergoing subaerial erosion and reworking during deposition\nor the Caloosahatchee marl. Stratified sand and clayey sand containing\nscattered thin lenses of fresh-water limestone and marl of Pleistocene age are either floodplain deposits or subaerial topset beds of a delta\nmade by the Pleistocene Peace River. Sediments of Recent age are local\nstream deposits.

\n
\n

Bars and shoals in the Peace River south of Brownville, De Soto\nCounty, contain appreciable tonnages of low grade \"river-pebble\" phosphate.\nThe phosphate and uranium content of the undifferentiated phosphatic\nsand and clay in Hardee County is too low to be of economic significance.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei458","collaboration":"This report concerns work on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Bergendahl, M.H., 1954, Stratigraphy of parts of De Soto and Hardee Counties, Florida: U.S. Geological Survey Trace Elements Investigations 458, Report: 58 p.; 9 Plates: 17.57 x 23.69 inches and smaller, https://doi.org/10.3133/tei458.","productDescription":"Report: 58 p.; 9 Plates: 17.57 x 23.69 inches and smaller","numberOfPages":"59","costCenters":[],"links":[{"id":284149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei458.jpg"},{"id":285861,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-3.pdf"},{"id":285862,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-4.pdf"},{"id":285863,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-5.pdf"},{"id":285858,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-1.pdf"},{"id":285859,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-2-N.pdf"},{"id":285860,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-2-S.pdf"},{"id":285864,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-6.pdf"},{"id":285865,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-7.pdf"},{"id":285866,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0458/plate-8.pdf"},{"id":285867,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0458/report.pdf"}],"country":"United States","state":"Florida","county":"De Soto County;Hardee County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.0,27.0 ], [ -82.0,27.666667 ], [ -81.666667,27.666667 ], [ -81.666667,27.0 ], [ -82.0,27.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559569e4b0120853e8c224","contributors":{"authors":[{"text":"Bergendahl, Maximilian H.","contributorId":38057,"corporation":false,"usgs":true,"family":"Bergendahl","given":"Maximilian","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":284263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70257007,"text":"70257007 - 1954 - Pumpage and ground-water levels in Arizona in 1953","interactions":[],"lastModifiedDate":"2024-10-22T18:34:56.889248","indexId":"70257007","displayToPublicDate":"1954-01-01T09:45:16","publicationYear":"1954","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Pumpage and ground-water levels in Arizona in 1953","docAbstract":"

No abstract available.

","largerWorkType":{"id":18,"text":"Report"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70257007","collaboration":"Prepared in cooperation with Arizona State Land Department Roger Ernst, Commissioner","usgsCitation":"Halpenny, L.C., 1954, Pumpage and ground-water levels in Arizona in 1953, 27 p., https://doi.org/10.3133/70257007.","productDescription":"27 p.","costCenters":[],"links":[{"id":432274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70257007/report-thumb.jpg"},{"id":463093,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70257007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -115.63744727441635,\n 37.16309386845195\n ],\n [\n -115.63744727441635,\n 31.06456113922806\n ],\n [\n -108.74307003551321,\n 31.06456113922806\n ],\n [\n -108.74307003551321,\n 37.16309386845195\n ],\n [\n -115.63744727441635,\n 37.16309386845195\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Halpenny, L. C.","contributorId":120299,"corporation":false,"usgs":true,"family":"Halpenny","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":909116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}