Four basalt samples for whole-rock K-Ar dating were analyzed with an electron microprobe to locate potassium concentrations. Highest concentrations of potassium were found in those mineral phases which were the last to crystallize. The two reliable samples had potassium concentrated in fine-grained interstitial feldspar and along grain boundaries of earlier formed plagioclase crystals. The two unreliable samples had potassium concentrated in the glassy matrix, demonstrating the ineffectiveness of basaltic glass as a retainer of radiogenic argon. In selecting basalt samples for whole-rock K-Ar dating, particular emphasis should be placed on determining the nature and condition of the fine-grained interstitial phases.
Biscalitheca suzanneana, n. sp., is described from specimens found in an uppermost Pennsylvanian deposit in north-central Texas. The genus was identified primarily on the basis of impressions of the unique sporangial annuli. The occurrence establishes for Biscalitheca a stratigraphic range equivalent to nearly the entire Upper Pennsylvanian Series.
The San Andreas fault is viewed, according to the concepts of seafloor spreading and plate tectonics, as a transform fault that separates the Pacific and North American plates and along which relative movements of 2 to 6 cm/year have been taking place. The resulting strain can be released by creep, by earthquakes of moderate size, or (as near San Francisco and Los Angeles) by great earthquakes. Microearthquakes, as mapped by a dense seismograph network in central California, generally coincide with zones of the San Andreas fault system that are creeping. Microearthquakes are few and scattered in zones where elastic energy is being stored. Changes in the rate of strain, as recorded by tiltmeter arrays, have been observed before several earthquakes of about magnitude 4. Changes in fluid pressure may control timing of seismic activity and make it possible to control natural earthquakes by controlling variations in fluid pressure in fault zones. An experiment in earthquake control is underway at the Rangely oil field in Colorado, where the rates of fluid injection and withdrawal in experimental wells are being controlled.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(72)90080-7","issn":"00401951","usgsCitation":"Healy, J.H., Lee, W., Pakiser, L.C., Raleigh, C., and Wood, M., 1972, Prospects for earthquake prediction and control: Tectonophysics, v. 14, no. 3-4, p. 319-332, https://doi.org/10.1016/0040-1951(72)90080-7.","productDescription":"14 p.","startPage":"319","endPage":"332","numberOfPages":"14","costCenters":[],"links":[{"id":219297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.29980468749999,\n 35.06597313798418\n ],\n [\n -117.24609374999999,\n 35.06597313798418\n ],\n [\n -117.24609374999999,\n 42.13082130188811\n ],\n [\n -122.29980468749999,\n 42.13082130188811\n ],\n [\n -122.29980468749999,\n 35.06597313798418\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"14","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8f57e4b0c8380cd7f6e6","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":358553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, W.H.K.","contributorId":35303,"corporation":false,"usgs":true,"family":"Lee","given":"W.H.K.","affiliations":[],"preferred":false,"id":358551,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":358555,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Raleigh, C.B.","contributorId":40219,"corporation":false,"usgs":true,"family":"Raleigh","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":358552,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wood, M.D.","contributorId":63930,"corporation":false,"usgs":true,"family":"Wood","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":358554,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70010094,"text":"70010094 - 1972 - Differentiation and volcanism in the lunar highlands: Photogeologic evidence and Apollo 16 implications","interactions":[],"lastModifiedDate":"2020-12-23T20:47:47.740182","indexId":"70010094","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Differentiation and volcanism in the lunar highlands: Photogeologic evidence and Apollo 16 implications","docAbstract":"Materials of possible volcanic origin in the lunar highlands include (1) highland plains materials, (2) materials forming closely spaced hills in which summit furrows and chains of craters are common and (3) materials forming closely spaced hills (some of which parallel the lunar grid) on which summit furrows and chain craters are rare. The highland plains materials probably are basaltic lavas with less Fe and Ti than the mare plains materials. The two hilly units appear to consist of materials that, if volcanic, were more viscous in the molten state than any of the lunar plains units; thus these materials may be significantly enriched in felsic components. Most of the highland materials of possible volcanic origin formed after the Imbrium multi-ring basin but before mare material completed flooding parts of the moon; they therefore postdate accretion of the moon and may represent several episodes of premare volcanism.
The Luna 16 landing site is similar in its geologic setting to Apollos 11 and 12. All three sites are located on basaltic mare fill which occurs mostly within multi-ring basins formed by impact earlier in the moon's history. A regolith developed by impact bombardment is present at each of these sites. The regolith is composed mostly of locally derived volcanic material, but also contains exotic fine fragments that have been ballistically transported into the landing sites by large impact events which formed craters such as Langrenus and Copernicus. These exotic fragments probably consist mostly of earlier reworked multi-ring basin debris and, although not directly traceable to individual sources, they do represent a good statistical sample of the composition of most of the premare terrac regions.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp690","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Stewart, J.H., Poole, F.G., Wilson, R.F., Cadigan, R.A., Thordarson, W., and Albee, H.F., 1972, Stratigraphy and origin of the Chinle Formation and related Upper Triassic strata in the Colorado Plateau region, with a section on sedimentary petrology and a section on conglomerate studies: U.S. Geological Survey Professional Paper 690, Report: vi, 336 p.; 5 Plates: 37.48 x 17.24 inches, https://doi.org/10.3133/pp690.","productDescription":"Report: vi, 336 p.; 5 Plates: 37.48 x 17.24 inches","costCenters":[],"links":[{"id":113665,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0690/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113669,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0690/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113670,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0690/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164638,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0690/report-thumb.jpg"},{"id":113666,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0690/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113667,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0690/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":113668,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0690/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":422853,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5000.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, Colorado, Nevada, New Mexico, Utah","otherGeospatial":"Colorado Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116,\n 41\n ],\n [\n -116,\n 34\n ],\n [\n -105,\n 34\n ],\n [\n -105,\n 41\n ],\n [\n -116,\n 41\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab9e8","contributors":{"authors":[{"text":"Stewart, John Harris","contributorId":63790,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"Harris","affiliations":[],"preferred":false,"id":221680,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Poole, Forrest Graham","contributorId":80332,"corporation":false,"usgs":true,"family":"Poole","given":"Forrest","email":"","middleInitial":"Graham","affiliations":[],"preferred":false,"id":221681,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, Richard Farifield","contributorId":98779,"corporation":false,"usgs":true,"family":"Wilson","given":"Richard","email":"","middleInitial":"Farifield","affiliations":[],"preferred":false,"id":221682,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cadigan, R. A.","contributorId":57844,"corporation":false,"usgs":true,"family":"Cadigan","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":221679,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":221677,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Albee, H. F.","contributorId":28984,"corporation":false,"usgs":true,"family":"Albee","given":"H.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":221678,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":5220085,"text":"5220085 - 1972 - A repellent for protecting corn seed from blackbirds and crows","interactions":[],"lastModifiedDate":"2025-02-21T17:35:25.856939","indexId":"5220085","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A repellent for protecting corn seed from blackbirds and crows","docAbstract":"Methiocarb [4-(methylthio)-3,-5-xylyl N-methylcarbamate] was tested as a seed treatment for repelling blackbirds and crows (Corvus sp.) from sprouting corn in South Carolina. The test was conducted on eight fields within a 0.25-square-mile area. Marked repellency occurred; sprout damage averaged 44 percent in the control fields and 0.3 percent in the fields treated with methiocarb.
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Carolina\",\"nation\":\"USA \"}}]}","volume":"36","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8437","contributors":{"authors":[{"text":"Stickley, A.R. Jr.","contributorId":14538,"corporation":false,"usgs":true,"family":"Stickley","given":"A.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":331311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guarineo, J.L.","contributorId":90411,"corporation":false,"usgs":true,"family":"Guarineo","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":331312,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":34647,"text":"b1372B - 1972 - Stratigraphic nomenclature of Cambrian and Lower Ordovician rocks of easternmost southern Arizona and adjacent westernmost New Mexico","interactions":[],"lastModifiedDate":"2023-05-05T19:59:59.615516","indexId":"b1372B","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"1372","chapter":"B","title":"Stratigraphic nomenclature of Cambrian and Lower Ordovician rocks of easternmost southern Arizona and adjacent westernmost New Mexico","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1372B","usgsCitation":"Hayes, P.T., 1972, Stratigraphic nomenclature of Cambrian and Lower Ordovician rocks of easternmost southern Arizona and adjacent westernmost New Mexico: U.S. Geological Survey Bulletin 1372, iii, 21 p., https://doi.org/10.3133/b1372B.","productDescription":"iii, 21 p.","costCenters":[],"links":[{"id":416786,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92651.htm","linkFileType":{"id":5,"text":"html"}},{"id":62535,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1372b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167262,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1372b/report-thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111,\n 33.375\n ],\n [\n -111,\n 31.3322\n ],\n [\n -106.375,\n 31.3322\n ],\n [\n -106.375,\n 33.375\n ],\n [\n -111,\n 33.375\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebdd","contributors":{"authors":[{"text":"Hayes, Philip Thayer","contributorId":8071,"corporation":false,"usgs":true,"family":"Hayes","given":"Philip","email":"","middleInitial":"Thayer","affiliations":[],"preferred":false,"id":213326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48075,"text":"ofr72348 - 1972 - Water-resources reconnaissance of Anaktuvuk Pass, Alaska","interactions":[],"lastModifiedDate":"2023-08-29T20:48:49.921019","indexId":"ofr72348","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"72-348","title":"Water-resources reconnaissance of Anaktuvuk Pass, Alaska","docAbstract":"A hydrologic reconnaissance was made of Anaktuvuk pass in the central Brooks Range during the summer of 1971 to help develop a water supply for the village school. Winter icings and summer flow conditions in Contact Creek both indicate that ground water is present beneath the creek bed. A well-site area was selected in the channel of Contact Creek near the school where the prospects of obtaining a suitable ground-water supply seem best. In the event that wells are unsuccessful, water can be hauled from Eleanor Lake to the school. Chemical quality of water at Anaktuvuk Pass is excellent, but any source of water may be subject to bacterial contamination and would require treatment.
A virus disease of juvenile sockeye salmon (Oncorhynchus nerka) has been a problem in Washington hatcheries since first reported by Rucker [9] in 1953. Presumably, the same disease has occurred in Oregon, and it is now referred to as the Oregon, and it is now referred to as the Oregon sockeye disease (OSD) or the sockeye salmon virus (SSV) [8,12]. The primary source of the disease was thought to be from the feeding of raw sockeye salmon viscera, and the incidence decreased when pasteurized diets were used [5]. However, sporadic attacks continue to occur even though pelleted diets containing pasteurized fish products are fed.
","language":"English","publisher":"Taylor & Franics","doi":"10.1577/1548-8640(1972)34[143:SFIHNI]2.0.CO;2","usgsCitation":"Amend, D.F., and Wood, J.W., 1972, Survey for infectious hematopoietic necrosis (IHN) virus in Washington salmon: Progressive Fish-Culturist, v. 34, no. 3, p. 143-147, https://doi.org/10.1577/1548-8640(1972)34[143:SFIHNI]2.0.CO;2.","productDescription":"5 p. ","startPage":"143","endPage":"147","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335526,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a5770de4b057081a24eeca","contributors":{"authors":[{"text":"Amend, Donald F.","contributorId":106543,"corporation":false,"usgs":true,"family":"Amend","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":669324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, James W.","contributorId":181742,"corporation":false,"usgs":false,"family":"Wood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":669325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":48066,"text":"ofr72302 - 1972 - Sediment transport and deposition, Walnut and Pacheco Creeks, Contra Costa County, California, August 1965-April 1970","interactions":[],"lastModifiedDate":"2023-03-16T21:48:31.223206","indexId":"ofr72302","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"72-302","title":"Sediment transport and deposition, Walnut and Pacheco Creeks, Contra Costa County, California, August 1965-April 1970","docAbstract":"Average annual sediment discharge in Pacheco Creek basin, \nContra Costa County, Calif., was larger during August 1965-April 1970 \nthan the historical annual sediment discharge (1909-62) by a factor of \nabout 1.3. This increas in sediment discharge is attributed primarily \nto an increased frequency of peak streamflows and to a larger average \nannual streamflow during the 1965-70 period.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr72302","usgsCitation":"Porterfield, G., 1972, Sediment transport and deposition, Walnut and Pacheco Creeks, Contra Costa County, California, August 1965-April 1970: U.S. Geological Survey Open-File Report 72-302, iv, 21 p., https://doi.org/10.3133/ofr72302.","productDescription":"iv, 21 p.","numberOfPages":"24","temporalStart":"1965-08-01","temporalEnd":"1970-04-30","costCenters":[],"links":[{"id":161970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr72302.jpg"},{"id":414312,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_54415.htm","linkFileType":{"id":5,"text":"html"}},{"id":285918,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0302/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Contra Costa County","otherGeospatial":"Pacheco Creek, Walnut Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.9064,\n 37.75\n ],\n [\n -121.9064,\n 38.0458\n ],\n [\n -122.1644,\n 38.0458\n ],\n [\n -122.1644,\n 37.75\n ],\n [\n -121.9064,\n 37.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbfdb","contributors":{"authors":[{"text":"Porterfield, George","contributorId":68719,"corporation":false,"usgs":true,"family":"Porterfield","given":"George","email":"","affiliations":[],"preferred":false,"id":236763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17610,"text":"ofr72325 - 1972 - Reconnaissance geologic map of the Solomon D-6 quadrangle, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2022-08-11T13:04:59.96683","indexId":"ofr72325","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"72-325","title":"Reconnaissance geologic map of the Solomon D-6 quadrangle, Seward Peninsula, Alaska","docAbstract":"The Solomon D-6 15- by 30-minute quadrangle lies 20 miles northeast of Nome, Alaska, and adjoins on the east the Nome D-l quadrangle mapped by Hummel (1962b) and on the west the Solomon D-5 quadrangle mapped by Smith (1910).
Placer gold has been produced from Iron Creek and many of its tributaries, and a small amount of copper was shipped from the Wheeler mine. Many lode prospects contain small amounts of copper in silicified limestone within and near the base of thrust plates of carbonate rocks. Other lodes consist of well-defined veins containing gold and base-metal sulfide minerals, but none has been commercially productive.
Mapped rock units include the \"York Slate,\" of Precambrian age, which consists of a highly deformed and thick sequence of graphitic calcareous siltite, which contains thin limestone beds and intercalated(?) volcaniclastic rocks, and Paleozoic carbonate rocks, which have been converted largely to marble and schistose marble. Along and near the Kigluaik Mountains in the north part of the quadrangle, quartzo-feldspathic gneisses of Precambrian age are intruded by fine-grained granite. A very thick sequence of schistose thin-bedded argillaceous and dolomitic limestone overlies the York Slate and is correlative with a similar rock originally mapped in the York Mountains.
Surficial deposits, consisting principally of moraine and stream-reworked moraine, mantle large parts of the quadrangle.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72325","usgsCitation":"Sainsbury, C., Hudson, T., Ewing, R., and Richards, T., 1972, Reconnaissance geologic map of the Solomon D-6 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Open-File Report 72-325, Report: 17 p.; 1 Plate: 17.71 x 22.79 inches, https://doi.org/10.3133/ofr72325.","productDescription":"Report: 17 p.; 1 Plate: 17.71 x 22.79 inches","costCenters":[],"links":[{"id":150582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0325/report-thumb.jpg"},{"id":46804,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0325/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0325/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404229,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_113150.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"63360","country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula, Solomon D-6 quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -165,\n 64.75\n ],\n [\n -164.5,\n 64.75\n ],\n [\n -164.5,\n 65\n ],\n [\n -165,\n 65\n ],\n [\n -165,\n 64.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db6411dc","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":177092,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudson, Travis","contributorId":90282,"corporation":false,"usgs":true,"family":"Hudson","given":"Travis","affiliations":[],"preferred":false,"id":177091,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ewing, Rodney","contributorId":106914,"corporation":false,"usgs":true,"family":"Ewing","given":"Rodney","affiliations":[],"preferred":false,"id":177093,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richards, Thomas","contributorId":54622,"corporation":false,"usgs":true,"family":"Richards","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":177090,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":96421,"text":"96421 - 1972 - Highways and their impact on the wildlife in the pinyon-juniper-oak woodland and grassland in north-central Arizona","interactions":[],"lastModifiedDate":"2014-08-15T11:53:28","indexId":"96421","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Highways and their impact on the wildlife in the pinyon-juniper-oak woodland and grassland in north-central Arizona","docAbstract":"No abstract available.","language":"English","publisher":"Prescott College Ecological Survey","usgsCitation":"Douglas, C.L., and Johnson, R., 1972, Highways and their impact on the wildlife in the pinyon-juniper-oak woodland and grassland in north-central Arizona, iv, 109 p.","productDescription":"iv, 109 p.","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":128305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.82,31.33 ], [ -114.82,37.0 ], [ -109.05,37.0 ], [ -109.05,31.33 ], [ -114.82,31.33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6886a2","contributors":{"authors":[{"text":"Douglas, Charles L.","contributorId":10742,"corporation":false,"usgs":true,"family":"Douglas","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":299614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, R. Roy","contributorId":16352,"corporation":false,"usgs":true,"family":"Johnson","given":"R. Roy","affiliations":[],"preferred":false,"id":299615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70190911,"text":"70190911 - 1972 - Water-quality data for the Flaming Gorge Reservoir area, Utah and Wyoming, 1969-72","interactions":[],"lastModifiedDate":"2017-09-17T11:51:43","indexId":"70190911","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5498,"text":"Utah Basic-Data Release","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"Water-quality data for the Flaming Gorge Reservoir area, Utah and Wyoming, 1969-72","docAbstract":"This report presents the basic data that were collected by the U.S. Geological Survey during a study of the chemical quality of water in Flaming Gorge Reservoir. An interpretive report will follow. The basic data were collected from the reservoir during six sampling runs between October 1970 and September 1972. The reservoir was sampled for chemical analyses at 17 sites. Chemical and physical data were measured in situ at 34 sites. The sites are shown in figure 1 and the data are listed in tables 1 and 3-6.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","usgsCitation":"Bolke, E., and Waddell, K., 1972, Water-quality data for the Flaming Gorge Reservoir area, Utah and Wyoming, 1969-72: Utah Basic-Data Release 24, iii, 50 p.","productDescription":"iii, 50 p.","numberOfPages":"56","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345836,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-480&Title=Basic+Data+Report+24"}],"country":"United States","state":"Utah","otherGeospatial":"Flaming Gorge Reservoir","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bf899ce4b091459a5e0889","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":710678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":710679,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66086,"text":"i697 - 1972 - Reconnaissance geologic map of the Cedaredge area, Delta County, Colorado","interactions":[],"lastModifiedDate":"2023-04-03T13:24:45.117427","indexId":"i697","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"697","title":"Reconnaissance geologic map of the Cedaredge area, Delta County, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i697","usgsCitation":"Hail, W., 1972, Reconnaissance geologic map of the Cedaredge area, Delta County, Colorado: U.S. Geological Survey IMAP 697, Report: 1 p.; 1 Plate: 26.48 x 26.63 inches, https://doi.org/10.3133/i697.","productDescription":"Report: 1 p.; 1 Plate: 26.48 x 26.63 inches","costCenters":[],"links":[{"id":415053,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9467.htm","linkFileType":{"id":5,"text":"html"}},{"id":255594,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0697/report-thumb.jpg"},{"id":255593,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0697/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255592,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0697/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Colorado","county":"Delta County","otherGeospatial":"Cedaredge area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.75,\n 38.75\n ],\n [\n -107.75,\n 39\n ],\n [\n -108,\n 39\n ],\n [\n -108,\n 38.75\n ],\n [\n -107.75,\n 38.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a72e4b07f02db64300e","contributors":{"authors":[{"text":"Hail, W. J. Jr.","contributorId":35332,"corporation":false,"usgs":true,"family":"Hail","given":"W. J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":273954,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175672,"text":"70175672 - 1972 - Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971","interactions":[],"lastModifiedDate":"2016-08-17T16:02:33","indexId":"70175672","displayToPublicDate":"1972-01-01T00:00:00","publicationYear":"1972","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":"29","title":"Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971","docAbstract":"No abstract available.
","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Puente, C., 1972, Ground-water discharge from the Edwards and associated limestones, San Antonio area, Texas, 1971: Edwards Underground Water District Bulletin 29, 8 p.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326771,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad1e4b03bcb0104bbca","contributors":{"authors":[{"text":"Puente, Celso","contributorId":36140,"corporation":false,"usgs":true,"family":"Puente","given":"Celso","email":"","affiliations":[],"preferred":false,"id":645992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207484,"text":"70207484 - 1972 - Foreign literature and translations in earth science","interactions":[],"lastModifiedDate":"2019-12-20T09:22:11","indexId":"70207484","displayToPublicDate":"1971-12-31T09:16:29","publicationYear":"1972","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Foreign literature and translations in earth science","docAbstract":"More than 50 percent of the total abstracted geologic literature is in Russian, followed by English at about 30 percent, and French, German, and Japanese from about 8 to 2 percent. Communist Chinese publications ceased as a result of the Cultural Revolution and have not resumed. Less than 2 percent of American earth scientists read and use Russian literature in the original to any significant extent. About 30 percent know some French, German, and Spanish, but only a much smaller proportion uses these languages in practice. The most important sources of knowledge about foreign work are translation journals, almost exclusively from Russian, and foreign scientists who write in American and international journals. Less than 0.5 percent of Russian earth science books are translated or known in the United States. Scientific provincialism is strong and increasing in the United States, owing to or demonstrated by the publications explosion and squeeze on libraries and scientists, weakening or abandonment of language requirements in universities, and cessation of all broad earth science abstracting services in English. Suggestions for improving communication of foreign literature include earlier exposure to languages in schools and stress on critical use rather than perfunctory examinations. A \"critical mass\" of linguistically competent and active scientists is necessary to find the important, not merely important-sounding, titles in the literature morass and introduce them into widely read earth science media.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Toward the development of a geoscience information system : a symposium : proceedings of the Sixth Annual Meeting of the Geoscience Information Society, November 1, 1971, Washington, D.C.","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Sixth Annual Meeting of the Geoscience Information Society","conferenceDate":"November 1, 1971","conferenceLocation":"Washington, DC","language":"English","publisher":"Geoscience Information Society","usgsCitation":"Manheim, F.T., 1972, Foreign literature and translations in earth science, in Toward the development of a geoscience information system : a symposium : proceedings of the Sixth Annual Meeting of the Geoscience Information Society, November 1, 1971, Washington, D.C., v. 2, Washington, DC, November 1, 1971, p. 11-52.","productDescription":"42 p.","startPage":"11","endPage":"52","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":370544,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70048669,"text":"70048669 - 1972 - Determination of channel capacity of the Mokelumne River downstream from Camanche Dam, San Joaquin and Sacramento Counties, California","interactions":[],"lastModifiedDate":"2013-11-22T09:41:28","indexId":"70048669","displayToPublicDate":"1969-10-29T09:24:00","publicationYear":"1972","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}},"title":"Determination of channel capacity of the Mokelumne River downstream from Camanche Dam, San Joaquin and Sacramento Counties, California","docAbstract":"This study evaluates the adequacy of a 39-mile reach of the Mokelumne River in San Joaquin and Sacramento Counties, California, to carry planned flood releases between Camanche Reservoir and the Bensons Ferry Bridge near Thornton. The flood releases from Camanche Reservoir are to be restricted, insofar as possible, so that the flows in the Mokelumne River will not exceed 5,000 cfs (cubic feet per second) as measured at the gaging station below Camanche Dam.
\nAreas of inundation and computed floodwater profiles are based on channel conditions in late 1970 and on observed water-surface profiles during flood releases of about 5,000 cfs in January 1969 and January 1970. The inundated area shown on the maps (appendix A) and the water-surface elevations indicated on the cross sections (appendix G) are for the flood releases of those dates.
\nThe following conclusions are contingent on there being no levee failures during periods of high flow and no significant channel changes since the flood release of January 1970.
\n1. High tides in San Francisco Bay and, to a greater degree, flood stages on the Cosumnes River, cause backwater in the study reach. Severe backwater conditions occurring simultaneously with a flow of 5,000 cfs in the Mokelumne River can increase the flood stage 4 to 6 feet at Bensons Ferry Bridge (cross section 1). Backwater effects decrease in an upstream direction and are less than 0.5 foot at cross section 35, a river distance of 8.6 miles upstream from cross section 1, and 1.5 miles downstream from the Peltier Road bridge.
\n2. In the reach between cross sections 1 and 35, a 5,000 cfs release from Camanche Reservoir with maximum backwater effect (measured at cross section 1 at the mouth of the Cosumnes River) is confined within the natural or leveed banks except on the right bank flood plain between cross sections 12 and 19.
\n3. Upstream from cross section 35, there is overbank flooding at a flow of 5,000 cfs between cross sections 48 and 51, and 62 and 67.5. An increase in flow from 5,000 to 6,000 cfs will cause flooding between cross sections 43 and 47, 52 and 56, and 73 and 85.
\n4. A discharge of 5,000 cfs will pass through all bridge openings in the study reach except that of the Western Pacific Railroad Co. bridge at cross section 4. If large amounts of debris lodge on the railroad bridge when backwater from the Cosumnes River occurs, the debris could cause higher stages and flooding along the right bank between cross sections 5 and 12.
","language":"English","publisher":"U.S. Geological Survey Water Resources Division","publisherLocation":"Menlo Park, CA","doi":"10.3133/70048669","collaboration":"Prepared in cooperation with The Reclamation Board, State of California","usgsCitation":"Simpson, R., 1972, Determination of channel capacity of the Mokelumne River downstream from Camanche Dam, San Joaquin and Sacramento Counties, California: U.S. Geological Survey Open-File Report, iv, 64 p., https://doi.org/10.3133/70048669.","productDescription":"iv, 64 p.","numberOfPages":"68","costCenters":[],"links":[{"id":278502,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70048669.jpg"},{"id":279571,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70048669/report.pdf"}],"scale":"500000","country":"United States","state":"California","county":"Sacramento County;San Joaquin County","otherGeospatial":"Camanche Reservoir;Mokelumne River","geographicExtents":"{ \"type\": 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C.","contributorId":189752,"corporation":false,"usgs":false,"family":"Hopps","given":"Howard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":830409,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Anderson, Barbara M.","contributorId":75155,"corporation":false,"usgs":true,"family":"Anderson","given":"Barbara","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":830407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70227281,"text":"70227281 - 1971 - The Fe-Sb-S system","interactions":[],"lastModifiedDate":"2022-01-06T21:25:40.573564","indexId":"70227281","displayToPublicDate":"2022-01-06T15:21:42","publicationYear":"1971","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":"The Fe-Sb-S system","docAbstract":"The phase relations in the Fe-Sb-S system from 300° to 800° C have been determined using new experimental data on phase assemblages and univariant equilibria in conjunction with information from the literature. Estimates have been made for the standard free energies of formation as a function of temperature for stibnite, berthierite, gudmundite, and FeSb2 . Comparison of calculated mineral stabilities with published information on mineral assemblages suggests that apparently contradictory mineral associations may well represent equilibration at different (but all low) temperatures with subsequent lack of reaction as temperature fell to the temperature of observation. Resolution of the complicated, low-temperature phase relations will require additional thermochemical data of unusually high accuracy that might well be supplemented by careful study of natural materials.
Berthierite, gudmundite, and aurostibite are clearly stable only under conditions of relatively low sulfur activity. FeSb2 requires such low sulfur activity for its stable existence that it is seldom, if ever, to be expected as a mineral. The tendency for the common ore mineral galena to react with berthierite to yield pyrrhotite plus a lead sulfantimonide operates to make berthierite a rather uncommon mineral.
No abstract available.
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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":210377,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":808226,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70180008,"text":"70180008 - 1971 - Developing a state water plan: Ground-water conditions in Utah, spring of 1971","interactions":[],"lastModifiedDate":"2017-01-23T11:34:17","indexId":"70180008","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1971","docAbstract":"This report is the eighth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series are prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources and are designed to provide data to enable interested parties such as legislators, administrators, and planners to keep abreast of changing ground-water conditions.
This report, like the others (see references, p. 21), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. It also contains supplementary data that are related to ground-water use in some areas. In reports of this series, the inclusion of such supplementary data as graphs showing chemical quality of water and maps showing water-table configuration is intended only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.
The report includes individual discussions of the most important areas of ground-water withdrawal in the State for the calendar year 1970. Water-level fluctuations, however, are described for the period spring 1970 to spring 1971. Many of the data used in the report were collected by the Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Cordova, R., Bjorklund, L., McGreevy, L.J., Bolke, E., Sumison, C., Herbert, L.R., Butler, R., Mower, R.W., Sandberg, G.W., and Adams, D.B., 1971, Developing a state water plan: Ground-water conditions in Utah, spring of 1971: Cooperative Investigations Report 9, viii, 72 p.","productDescription":"viii, 72 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333680,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333679,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-194"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a13e4b0cad700058b63","contributors":{"authors":[{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGreevy, L. J.","contributorId":108124,"corporation":false,"usgs":true,"family":"McGreevy","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":659725,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":659726,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659727,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659728,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659729,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659730,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659731,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Adams, D. B.","contributorId":59030,"corporation":false,"usgs":true,"family":"Adams","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":659732,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70179729,"text":"70179729 - 1971 - Nonthermal springs of Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:22:18","indexId":"70179729","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"16","title":"Nonthermal springs of Utah","docAbstract":"Data are presented for about 4,500 nonthermal springs that discharge in the State of Utah. Most major springs having discharge of several cubic feet per second or more are in or near mountain ranges or plateaus where precipitation is much greater than in other parts of the State. The largest instantaneous discharge observed at any spring was 314 cfs at Mammoth Spring in southwestern Utah. Discharges exceeding 200 cfs have been observed at Swan Creek Spring in extreme northern Utah, and discharges of 200 cfs have been reported for Big Brush Creek Spring in northeastern Utah. Maximum discharges generally are during or within a few weeks after the main period of snowmelt, which is usually from late April to the middle of June.
The largest springs generally discharge form or very near carbonate rocks in which solution channels and fractures are numerous or from areas of porous or fractured volcanic rocks. Most nonthermal springs in Utah probably are variable springs – that is, their variability of discharge exceeds 100 percent.
Most of the major springs discharge water that contains less than 500 ppm (parts per million) of dissolved solids, and most of the water is of the calcium bicarbonate type. Water from springs is used for domestic, municipal, irrigation, livestock, mining, and industrial purposes.
","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah Geological and Mineralogical Survey","usgsCitation":"Mundorff, J.C., 1971, Nonthermal springs of Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 16, iv, 70 p.","productDescription":"iv, 70 p.","numberOfPages":"78","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333216,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333214,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-16.pdf"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ace4b0847d353f44c8","contributors":{"authors":[{"text":"Mundorff, J. 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Its purpose is to present available hydrologic data for Hansel Valley, to provide an evaluation of the potential water-resource development of the valley, and to identify needed studies that would improve understanding of the valley's water supply. Hydrologic data from the northern part of adjacent Rozel Flat were collected to aid in evaluation of southern Hansel Valley, and these data also are included in this report.
","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Hood, J.W., 1971, Hydrologic reconnaissance of Hansel Valley and northern Rozel Flat, Box Elder County, Utah: Technical Publication 33, ii, 41 p.","productDescription":"ii, 41 p.","numberOfPages":"46","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331831,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331829,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-710"},{"id":331830,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920008v.pdf"}],"country":"United States","state":"Utah","county":"Box Elder County","otherGeospatial":"Hansel Valley, Northern Rozel Flat","geographicExtents":" {\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.0438232421875,\n 41.42625319507269\n ],\n [\n -113.0438232421875,\n 41.99624282178583\n ],\n [\n -112.4945068359375,\n 41.99624282178583\n ],\n [\n -112.4945068359375,\n 41.42625319507269\n ],\n [\n -113.0438232421875,\n 41.42625319507269\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"584bd0e2e4b077fc20250e2e","contributors":{"authors":[{"text":"Hood, James W.","contributorId":66115,"corporation":false,"usgs":true,"family":"Hood","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":655413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70178880,"text":"70178880 - 1971 - Ground-water resources of Cache Valley, Utah and Idaho","interactions":[],"lastModifiedDate":"2016-12-09T16:46:22","indexId":"70178880","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"36","title":"Ground-water resources of Cache Valley, Utah and Idaho","docAbstract":"This report is based on a study that was designed to provide information to enable the water managers and users in Cache Valley to develop, conserve, and administer their water resources. The report is primarily about the ground water in the valley, but it also includes a discussion of the relation of ground water to surface water and presents a general water-budget analysis for the valley. The report discusses the effects of climate, geology, and development on the source, occurrence, availability, quantity, movement, and chemical quality of the ground water. Most of the discussion pertains to ground water in the Quaternary valley fill, the principal water-bearing unit in the area, but it also includes some information about ground water in other rocks within the Cache Valley drainage basin.
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