Numerous hot springs occur in a variety of geologic provinces in central and western Alaska. Granitic plutons are common to all the provinces and the hot springs are spatially associated with the contacts of these plutons. Of 23 hot springs whose bedrock geology is known, all occur within 3 miles of a granitic pluton. The occurrence of hot springs, however, appears to be independent of the age, composition, or magmatic history of the pluton.
\nPreliminary chemical and isotopic analyses suggest the hot springs waters belong to two groups. Most of the analyzed hot springs appear to have chemical and Isotopic compositions indicating they were derived from deeply circulating meteoric water. About 25 percent of the analyzed hot springs show a distinct saline character with high concentrations of chloride, sodium, potassium, and calcium indicating either much more complex water rock reactions than occurred in the other hot springs or the addition of another type of water. The present chemical and isotopic data are insufficient to determine the source of the constituents of the saline hot springs.
\nChemical geothermometers suggest subsurface temperatures in the general range of 100°C to 160°C. If the hot spring waters have derived their heat solely from deep circulation, the waters must have reached depths of 9,000 to 15,000 feet, assuming geothermal gradients of 30°C to 50°C/km. If hot magmatic water has been added to the geothermal systems or if dilution or mixing has occurred, temperatures of 100°C to 160°C may be reached at shallower depths.
\nThe geologic and chemical data are too preliminary to make an estimate of the potential of the hot springs as a geothermal resource. The data suggest, however, that most of the hot springs of central and western Alaska have relatively low subsurface temperatures and limited reservoir capacities in comparison with geothermal areas presently being utilized for electrical power generation.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73188","usgsCitation":"Miller, T.P., Barnes, I., and Pattan, W.W., 1973, Geologic setting and chemical characteristics of hot springs in central and western Alaska: U.S. Geological Survey Open-File Report 73-188, Report: 19 p.; 1 Figure; 1 Table (in 2 parts), https://doi.org/10.3133/ofr73188.","productDescription":"Report: 19 p.; 1 Figure; 1 Table (in 2 parts)","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":43825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-1.pdf","text":"Figure 1","size":"688.14 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 1"},{"id":43826,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-2.pdf","text":"Table 1","size":"1.21 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1"},{"id":43827,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0188/plate-3.pdf","text":"Table 1, Part 2","size":"1.29 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Table 1, Part 2"},{"id":43828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0188/report.pdf","text":"Report","size":"589.73 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":148931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0188/report-thumb.jpg"}],"country":"United States","state":"Alaska","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\n ],\n [\n -165,\n 66\n ],\n [\n -150,\n 66\n ],\n [\n -150,\n 64\n ],\n [\n -165,\n 64\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881be","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":170388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":170389,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pattan, William Wallace Jr.","contributorId":61297,"corporation":false,"usgs":true,"family":"Pattan","given":"William","suffix":"Jr.","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":170390,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13959,"text":"ofr7397 - 1973 - Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr7397","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-97","title":"Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia","docAbstract":"This report summarizes the geology of an area of some 6000 square kilometers in the northern part of the Central Cordillera of the Colombian Andes. The area, in north-central Department of Antioquia, was mapped between 1964 and 1968 as part of the Inventario Minero Nacional (IMN) project. Mineral resources are summarized within a larger area, designated as subzone ILK of IMN Zone If, which comprises almost 22,000 sq. kin, including the area mapped geologically by IMN and additional areas mapped by other agencies. \r\n\r\nThe oldest formation is a micaceous paragneiss of early Paleozoic or possibly late Precambrian age. A thick geosynclinal sedimentary series accumulated during the Paleozoic Era and became regionally metamorphosed to greenschist (locally amphibolite) facies during the Permian or early Triassic; these schists and gneisses are designated collectively as the Valdivia Group. The Permian(?) orogenic episode included intrusion of concordant syntectonic plutons, mostly of tonalitic composition. Rocks of unequivocal Triassic or Jurassic age are not recognized.\r\n\r\nThe Cretaceous is well represented by both igneous and sedimentary assemblages. Eugeosynclinal alpine ophiolites comprising submarine basalt flows and numerous intrusions of gabbro and serpentinite are prominent in the Lower Cretaceous, together with flysch composed of marine shale and lesser sandstone and conglomerate. The Upper Cretaceous is represented along the west border of the mapped area by submarine basalt flows and pyroclastic rocks, locally Interbedded with fine-grained clastic sedimentary beds, and lenses of dark laminated chert, at least part of which is radiolarian. The Late Cretaceous was marked by an orogenic event that profoundly folded and faulted all rocks and in the Central Cordillera caused low-grade metamorphism, the overprint of which is hardly observable in pre-Cretaceous rocks elsewhere. The Late Cretaceous orogeny culminated with discordant intrusion of the epizonal tonalitic Antioquian batholith. Displacement along the great Romeral wrench fault may have begun in the Cretaceous. \r\n\r\nPlutonism continued into the Cenozoic, exemplified by the hornblende-diorite Sabanalarga pluton. Intermontane basins were filled with molasse derived from the erosion of adjacent highlands; Tertiary sedimentation in marshy areas included organic carboniferous matter subsequently converted to lignite or subbituminous coal. The Sabanalarga fault system originated in the Late Tertiary; intermittent displacement continued on the older wrench faults such as the Romeral. Epeirogenic uplift, which probably began in the Pliocene and continued through the Pleistocene and Holocene, brought on renewed erosion which has sculptured the mountains into their present form.\r\n\r\nMineral resources in subzone IIA are varied but not of outstanding importance. Gold and silver mining, significant in past centuries, is minor today. Ferruginous laterite on serpentinite once considered as a potential source of iron ore is not economically exploitable. IMN has explored nickeliferous laterite at the extreme northwest corner of subzone IIA; this is a potential resource, exploitable only after exhaustion of the larger and richer nickel laterite deposit at Cerro Matoso, farther to the north and outside the boundaries of Zone If. Known deposits of mercury, chromium, manganese, and copper are small, with limited economic potential. Nonmetallic resources include raw materials for cement, including portland cement. Saprolite clay is widely used in making common red brick and tile, still a dominant construction material in all but the most modern multistory buildings. Aggregate materials are varied and abundant. Kaolin of good quality near La Union is important as a ceramic raw mineral filler. Tertiary subbituminous coal beds are an important energy resource in western subzone IIA, and have a good potential for greater development. Deposits of sodic feldspar, talc, decorative stone, and silica a","language":"ENGLISH","publisher":"U.S. Geological Survey]","doi":"10.3133/ofr7397","usgsCitation":"Hall, R., Alvarez A., J., and Rico H., H., 1973, Geology and mineral resources of central Antioquia Department (Zone IIA), Colombia: U.S. Geological Survey Open-File Report 73-97, x, 174 p. :maps (3 folded, 1 col.) ;27 cm.; 1 map, scale 1:100,000, https://doi.org/10.3133/ofr7397.","productDescription":"x, 174 p. :maps (3 folded, 1 col.) ;27 cm.; 1 map, scale 1:100,000","costCenters":[],"links":[{"id":95182,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0097/plate-1.pdf","size":"12413","linkFileType":{"id":1,"text":"pdf"}},{"id":147401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0097/report-thumb.jpg"},{"id":42615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46fd","contributors":{"authors":[{"text":"Hall, R.B.","contributorId":17214,"corporation":false,"usgs":true,"family":"Hall","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":168699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alvarez A., Jairo","contributorId":44411,"corporation":false,"usgs":true,"family":"Alvarez A.","given":"Jairo","email":"","affiliations":[],"preferred":false,"id":168701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rico H., Hector","contributorId":42481,"corporation":false,"usgs":true,"family":"Rico H.","given":"Hector","email":"","affiliations":[],"preferred":false,"id":168700,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":12556,"text":"ofr7317 - 1973 - Tabulated gravity data from McGrath and Medfra quadrangles, Alaska","interactions":[],"lastModifiedDate":"2024-04-08T22:07:47.792751","indexId":"ofr7317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"73-17","title":"Tabulated gravity data from McGrath and Medfra quadrangles, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7317","collaboration":"Prepared in cooperation with the State of Alaska Division of Geological & Geophysical Surveys","usgsCitation":"Barnes, D., Olson, R.C., and Rambo, W.L., 1973, Tabulated gravity data from McGrath and Medfra quadrangles, Alaska: U.S. Geological Survey Open-File Report 73-17, Report: 39 p.; 2 Plates: 29.43 x 23.33 inches and 29.91 x 23.44 inches, https://doi.org/10.3133/ofr7317.","productDescription":"Report: 39 p.; 2 Plates: 29.43 x 23.33 inches and 29.91 x 23.44 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A colloidal amorphous product having the composition of halloysite was produced in most solutions. It had a consistent and reversible equilibrium solubility equivalent to a standard free energy of formation of -8974 ? 1.0 kcal per mole for the formula A12Si2O5(OH)4. Some aging times were longer than 4 years, but most solutions gave consistent solubilities after only a few months of aging. Where silica concentrations were below about 10 -4 molar, microcrystalline gibbsite was formed below pH 6.0 and crystalline bayerite above pH 7.0, but only after much longer aging than was required for crystallization in silica-free solutions. \r\n\r\nElectron micrographs and diffraction patterns of the synthesized material indicate some crystallinity in the aluminosilicate, but no X-ray diffraction patterns could be obtained even in the material aged 4 years. \r\n\r\nSolubility relationships for solutions containing fluoride as well as silica and aluminum are explainable by using cryolite stabilities determined in previous work. \r\n\r\nAluminum contents of 51 samples of water analyzed for other purposes are in reasonable agreement with the assumption of equilibrium with amorphous clay mineral species similar to the material synthesized in this work. 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