Interim Geologic Map of the West Part of - Utah Geological Survey

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Bowers, W.E., 1990, Geologic map of Bryce Canyon National Park and vicinity,southwestern Utah: U.S. Geological Survey Miscellaneous Investigations SeriesMap I-2108, 15 p., 1 plate, scale 1:24,000.Bown, T.M., Hasiotis, S.T., Genise, J.F., Maldonado, F., and Bowers, E.M., 1997, Tracefossils of Hymenoptera and other insects, and paleoenvironments of the ClaronFormation (Paleocene and Eocene), southwestern Utah, in Maldonado, F., andNealey, L.D., editors, Geologic studies in the Basin and Range-Colorado Plateautransition zone in southeastern Nevada, southwestern Utah, and northwesternArizona, 1995: U.S. Geological Survey Bulletin 2153, p. 43-58.Bullock, K.C., 1970, Iron deposits of Utah: Utah Geological and Mineralogical SurveyBulletin 88, 101 p.Callaghan, E., 1938, Preliminary report on the alunite deposits of the Marysvale region,Utah: U.S. Geological Survey Bulletin 886-D, p. 91-131.Canaday, T.W., 2001, High-altitude archaeological investigations at Cedar BreaksNational Monument, Utah, with contributions by Bakewell, E.F., Chengyu W.,Corson, P.L., Ferris, D.E., Elias, S.A., Funkhouser, G.S., Hughes, R.E., Jackson,S.T., Madsen, D.B., Perry, L., Sarna-Wojciki, A., and Thompson, R.S.: NationalPark Service, Intermountain region, Cultural Resource Selections No. 17, 203 p.Cashion, W.B., 1961, Geology and fuels resources of the Orderville-Glendale area, KaneCounty, Utah: U.S. Geological Survey Coal Investigations Map C-49, scale 1:62,500.Christiansen, R.L., and Lipman, P.W., 1972, Cenozoic volcanism and plate tectonicevolution of the western United States – II. Late Cenozoic: Royal Society ofLondon Philosophical Transactions (A), v. 271, p. 249-284.Cifelli, R.L., Kirkland, J.I., Weil, A., Deinos, A.R., and Kowallis, B.J., 1997, Highprecision40 Ar/ 39 Ar geochronology and the advent of North America’s LateCretaceous terrestrial fauna: Proceedings National Academy of Science USA, v.94, p. 11163-11167.Cook, E.F., 1960, Geologic atlas of Utah, Washington County: Utah Geological andMineralogical Survey Bulletin 70, 119 p., scale 1:125,000.Cook, K.L., and Hardman, E., 1967, Regional gravity survey of the Hurricane fault areaand Iron Springs district, Utah: Geological Society of America Bulletin, v. 78, p.1063-1076.Cornell, D., Butler, T., Holm, D., Hacker, D., and Spell, T., 2001, Stratigraphy and Ar/Arages of volcanic rocks of the Pinto quadrangle, Colorado Plateau transition zone,SW Utah [abs.], in Erskine, M.C., Faulds, J.E., Bartley, J.M., and Rowley, P.D.,editors, The geologic transition, High Plateaus to Great Basin—A symposium and71
field guide (The Mackin Volume): Utah Geological Association and PacificSection of the American Association of Petroleum Geologists: Utah GeologicalAssociation Publication 30, p. 420-421.Currey, D.R., Mulvey, W.E., and Lindsay, L.M.W., 1986, Markagunt Plateau, Utah –southern margin of late Wisconsinan montane glaciation in the great Basin [abs.]:American Quaternary Association Program and Abstracts, v. 35, no 9, p. 126.Davis, G.H., 1999, Structural geology of the Colorado Plateau region of southern Utah,with special emphasis on deformation bands: Geological Society of AmericaSpecial Paper 342, 157 p.Davis, G.H., and Krantz, R.W., 1986, Post-Laramide thrust faults in the ClaronFormation, Bryce Canyon National Park, Utah [abs.]: Geological Society ofAmerica Abstracts with programs, v. 18, p. 98.Davis, G.H., and Rowley, P.D., 1993, Miocene thrusting, gravity sliding, and nearsurfacebatholithic emplacement, Marysvale volcanic field, southwestern Utah[abs.]: Eos (Transactions, American Geophysical Union), v. 74, no. 43, p. 647.Dickinson, W.R., and Gehrels, G.E., 2003, U-Pb ages of detrital zircons from Permianand Jurassic eolian sandstones of the Colorado Plateau, USA—paleogeographicimplications: Sedimentary Geology, v. 163, issues 1-2, p. 29-66.Dickinson, W.R., and Gehrels, G.E., 2009a, U-Pb ages of detrital zircons in Jurassiceolian and associated sandstones of the Colorado Plateau – evidence fortranscontinental dispersal and intraregional recycling of sediment: GeologicalSociety of America Bulletin, v. 121, nos. 3 and 4, p. 408-433.Dickinson, W.R., and Gehrels, G.E., 2009b, Insights into North Americanpaleogeography and paleotectonics from U-Pb ages of detrital zircons inMesozoic strata of the Colorado Plateau USA: International Journal EarthScience, DOI 10.1007/s00531-009-0462-0, 19 p.Dickinson, W.R., Stair, K.N., Gehrels, G.E., Peters, L., Kowallis, B.J., Blakey, R.C.,Amar, J.R., and Greenhalgh, B.W., 2009, U-Pb and 40 Ar/ 39 Ar ages for a tephralens in the Middle Jurassic Page Sandstone – first direct isotopic dating of aMesozoic eolianite on the Colorado Plateau: The Journal of Geology, v. 118, p.215-221.Doelling, H.H., 2008, Geologic map of the Kanab 30’x60’ quadrangle, Kane andWashington Counties, Utah, and Coconino and Mohave Counties, Arizona: UtahGeological Survey Miscellaneous Publication MP-08-2DM, scale 1:100,000.Doelling, H.H., and Davis, F.D., 1989, The geology of Kane County, Utah – geology,mineral resources, geologic hazards: Utah Geological and Mineral Survey72
Page 1 and 2:
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Page 3 and 4:
MAP UNIT DESCRIPTIONSQUATERNARYAllu
Page 5 and 6:
Qafc Coalesced fan alluvium of Paro
Page 7 and 8:
glacial deposits and features that
Page 9 and 10:
(Tbhv) and Dakota (Kd and Ktd) Form
Page 11 and 12:
typically mapped where lava flows d
Page 13 and 14:
that range in age from Miocene to H
Page 15 and 16:
fronts (except at Dry Valley, immed
Page 17 and 18:
the quadrangle; no fault that postd
Page 19 and 20:
Qbw, QbwcWater Canyon lava flow and
Page 21 and 22: others, 2007); lava flow is typical
Page 23 and 24: Mahogany Hill, about 500 feet (150
Page 25 and 26: lava flow (Tbbm) that conceal the u
Page 27 and 28: TERTIARYpreserved in down-dropped b
Page 29 and 30: and Rowley and others (in preparati
Page 31 and 32: field (or possibly coeval batholith
Page 33 and 34: hidden by shadow; we tentatively as
Page 35 and 36: esistant crystal-poor rhyolite tuff
Page 37 and 38: thickness uncertain but outcrop pat
Page 39 and 40: divide between Red Creek and Little
Page 41 and 42: pyroxene (5%), and sanidine (trace)
Page 43 and 44: unconformityThe Leach Canyon Format
Page 45 and 46: unconformityMa (Best and others, 19
Page 47 and 48: interval, and a lower limestone int
Page 49 and 50: Figure 3. View northwest to North V
Page 51 and 52: dark-yellowish-orange, grayish-pink
Page 53 and 54: TKgc Grand Castle Formation, undivi
Page 55 and 56: track (the latter found by Eric Rob
Page 57 and 58: noted by Moore and Straub (2001) an
Page 59 and 60: shoreface, beach, lagoonal, and est
Page 61 and 62: water deposits of Cenomanian age (N
Page 63 and 64: 62Figure 7. Cedar Mountain Formatio
Page 65 and 66: leached white under the Cretaceous
Page 67 and 68: ACKNOWLEDGMENTSThis geologic map is
Page 69 and 70: Anderson, R.E., and Christenson, G.
Page 71: Biek, R.F., Rowley, P.D., Hayden, J
Page 75 and 76: 2001, Cretaceous and early Tertiary
Page 77 and 78: Hacker, D.B., Rowley, P.D., Blank,
Page 79 and 80: Kurlich, R.A., III, 1990, Geology o
Page 81 and 82: Maldonado, F., and Moore, R.C., 199
Page 83 and 84: Flagstaff-Green River basins [abs.]
Page 85 and 86: elation to other igneous centers in
Page 87 and 88: Schulman, E., 1956, Dendroclimatic
Page 89: Van Kooten, G.K., 1988, Structure a
Page 92: 113°00'112°00'15BV20R i v e rCCNP
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Interim Geologic Map of the West Part of - Utah Geological Survey

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