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dc.contributor.authorScarborough, R.B.
dc.date.accessioned2018-11-10T01:04:57Z
dc.date.available2018-11-10T01:04:57Z
dc.date.issued1981-06-01
dc.identifier.citationScarborough, R.B., 1981, Reconnaissance Geology: Salt River - from Roosevelt Dam to Granite Reef Dam, Central Arizona. Arizona Geological Survey Open File Report, OFR-81-30, 9 map sheet, map scale 1:24,000, 79 p.
dc.identifier.urihttp://hdl.handle.net/10150/630649
dc.descriptionThe accompanying geologic maps depict the general geology of a two-mile wide strip centered about the Salt River, starting just below Roosevelt Dam and extending westward 36 miles to just below Granite Reef Dam. The geology was accomplished from October 1980 through April 1981, with the aid of about 25 hours of helicopter logistical support time. Discussions and/or field assistance by Mike Pryor, Joe Bailey, Dick Raymond, Paul Damon, and Tom McGarvin are greatly appreciated. Geologic Summary The lower Salt River below Roosevelt Dam has cut a gorge which exposes much of the geology of the northern Superstition volcanic field. The silicic field of late Oligocene (?) and Miocene age is one of the half dozen or so found in southern and western Arizona. The volcanics extend continuously from around Apache Lake Resort westward to Stewart Mountain Dam, and discontinuously farther west to the Mt. McDowell area, around Granite Reef Dam. The Superstition volcanics were deposited on Precambrian crystalline rocks, dominated by a biotite quartz monzonite which age dates at about 1400 m.y., and which is probably equivalent to the Ruin and Oracle granites further east and south. The northern Superstition volcanics are dominated by silicic pryoclastics, plugs, ash flows, agglomerates, and late stage intrusive domes. Rocks of andesitic composition are subordinate in volume although important in the eastern part of the area.
dc.language.isoen
dc.publisherArizona Geological Survey (Tucson, AZ)
dc.relation.ispartofseriesOFR-81-30
dc.relation.urlhttps://library.azgs.arizona.edu/
dc.rightsArizona Geological Survey. All rights reserved.
dc.subjectArizona Geological Survey Open File Reports
dc.subjectNeogene
dc.subjectCenozoic
dc.subjectTertiary
dc.subjectProterozoic
dc.subjectQuaternary
dc.subjectSaguaro Lake
dc.subjectMesquite Flat
dc.subjectOrme damsite
dc.subjectGoldfield Mountains
dc.subjectApache Lake
dc.subjectHorse Mesa Dam
dc.subjectMt. McDowell
dc.subjectStewart Mountain Dam
dc.subjectSuperstition Volcanic Field
dc.subjectMormon Flat
dc.subjectGranite Reef Dam
dc.subjectRoosevelt Dam
dc.subjectSalt river
dc.subjectgranite
dc.subjectWhitetail conglomerate
dc.subjectquartz monzonite
dc.subjectreverse fault
dc.subjecthigh angle fault
dc.subjectandesite
dc.subjectdomes
dc.subjectpyroclastics
dc.subjectagglomerate
dc.subjectash flow
dc.subjectvolcanics
dc.subjectbedrock geology
dc.titleReconnaissance Geology: Salt River - from Roosevelt Dam to Granite Reef Dam, Central Arizona
csdgm.bounding.west-111.522
csdgm.bounding.east-110.962
csdgm.bounding.north33.9418
csdgm.bounding.south33.5581
dc.description.collectioninformationDocuments in the AZGS Document Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu.
refterms.dateFOA2018-11-10T01:04:57Z


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