Palmer, W.R., 1957, Why <strong>the</strong> North Star stands still and o<strong>the</strong>r Indian legends:Englewood Cliffs, New Jersey, Prentice-Hall, Inc., 118 p.Peterson, F., 1994, Sand dunes, sabkhas, streams, and shallow seas – Jurassicpaleogeography in <strong>the</strong> sou<strong>the</strong>rn part <strong>of</strong> <strong>the</strong> <strong>West</strong>ern Interior basin, in Caputo, M.V.,Peterson, J.A., and Franczyk, K.J., editors, Mesozoic systems <strong>of</strong> <strong>the</strong> RockyMountain region, USA: Denver, Colorado, Rocky Mountain Section <strong>of</strong> <strong>the</strong> Societyfor Sedimentary Geology, p. 233-272.Pipiringos, G.N., and O’Sullivan, R.B., 1978, Principal unconformities in Triassic andJurassic rocks, <strong>West</strong>ern Interior United States – a preliminary survey: U.S.<strong>Geologic</strong>al <strong>Survey</strong> Pr<strong>of</strong>essional Paper 1035-A, 29 p.Pollock, S.L., 1999, Provenance, geometry, lith<strong>of</strong>acies, and age <strong>of</strong> <strong>the</strong> Upper CretaceousWahweap Formation, Cordilleran foreland basin, sou<strong>the</strong>rn <strong>Utah</strong>: Las Cruces,New Mexico State University, 117 p.Rahl, J.M., Reiners, P.W., Campbell, I.H., Nicolescu, S., and Allen, C.M., 2003,Combined single-grain (U-Th)/He and U-Pb dating <strong>of</strong> detrital zircons from <strong>the</strong>Navajo Sandstone, <strong>Utah</strong>: Geology, v. 31, no. 9, p. 761-764.Reiners, P.W., Campbell, I.H., Nicolescu, S., Allen, C.M., Hourigan, J.K., Garver, J.I.,Mattinson, J.M., and Cowan, D.S., 2005, (U-Th)/(He-Pb) double-dating <strong>of</strong> detritalzircons: American Journal <strong>of</strong> Science, v. 305, p. 259-311.Riggs, N.R., Mattinson, J.M., and Busby, C.J., 1993, Correlation <strong>of</strong> Jurassic eolian stratabetween <strong>the</strong> magmatic arc and <strong>the</strong> Colorado Plateau – new U-Pb geochronologicdata from sou<strong>the</strong>rn Arizona: <strong>Geologic</strong>al Society <strong>of</strong> America Bulletin, v. 105, p.1231-1246.Rowley, P.D., 1998, Cenozoic transverse zones and igneous belts in <strong>the</strong> Great Basin,western United States – <strong>the</strong>ir tectonic and economic implications, in Faulds, J.E.,and Stewart, J.H., editors, Accommodation zones and transfer zones − <strong>the</strong>regional segmentation <strong>of</strong> <strong>the</strong> Basin and Range Province: <strong>Geologic</strong>al Society <strong>of</strong>America Special Paper 323, p. 195-228.Rowley, P.D., Anderson, J.J., and Williams, P.L., 1975, A summary <strong>of</strong> Tertiary volcanicstratigraphy <strong>of</strong> <strong>the</strong> southwestern High Plateaus and adjacent Great Basin, <strong>Utah</strong>:U.S. <strong>Geologic</strong>al <strong>Survey</strong> Bulletin, 1405-B, 20 p.Rowley, P.D., and Barker, D.S., 1978, Geology <strong>of</strong> <strong>the</strong> Iron Springs mining district, <strong>Utah</strong>,in Shawe, D.R., and Rowley, P.D., editors, Guidebook to mineral deposits <strong>of</strong>southwestern <strong>Utah</strong>: <strong>Utah</strong> <strong>Geologic</strong>al Association Publication 7, p. 49-58.Rowley, P.D., Cunningham, C.G., Steven, T.A., Mehnert, H.H., and Naeser, C.W., 1998,Cenozoic igneous and tectonic setting <strong>of</strong> <strong>the</strong> Marysvale volcanic field, and its83
elation to o<strong>the</strong>r igneous centers in <strong>Utah</strong> and Nevada, in Friedman, J.D., andHuffman, A.C., Jr., coordinators, Laccolith complexes <strong>of</strong> sou<strong>the</strong>astern <strong>Utah</strong> –time <strong>of</strong> emplacement and tectonic setting – workshop proceedings: U.S.<strong>Geologic</strong>al <strong>Survey</strong> Bulletin 2158, p. 167-202.Rowley, P.D., Cunningham, C.G., Steven, T.A., Workman, J.B., Anderson, J.J., andTheissen, K.M., 2002, <strong>Geologic</strong> map <strong>of</strong> <strong>the</strong> central Marysvale volcanic field,southwestern <strong>Utah</strong>: U.S. <strong>Geologic</strong>al <strong>Survey</strong> <strong>Geologic</strong> Investigations Series <strong>Map</strong>I-2645-A, scale 1:100,000.Rowley, P.D., and Dixon, G.L., 2001, The Cenozoic evolution <strong>of</strong> <strong>the</strong> Great Basin area,U.S.A. – new interpretations based on regional geologic mapping, in Erskine,M.C., Faulds, J.E., Bartley, J.M., and Rowley, P.D., editors, The geologictransition, High Plateaus to Great Basin – a symposium and field guide (TheMackin Volume): <strong>Utah</strong> <strong>Geologic</strong>al Association and Pacific Section <strong>of</strong> <strong>the</strong>American Association <strong>of</strong> Petroleum Geologists, <strong>Utah</strong> <strong>Geologic</strong>al AssociationPublication 30, p. 169-188.Rowley, P.D., Hereford, R., and Williams, V.S., 1987, <strong>Geologic</strong> map <strong>of</strong> <strong>the</strong> AdamsHead-Johns Valley area, sou<strong>the</strong>rn Sevier Plateau, Garfield County, <strong>Utah</strong>: U.S.<strong>Geologic</strong>al <strong>Survey</strong> Miscellaneous Investigations Series <strong>Map</strong> I-1798, 1 plate, scale1:50,000.Rowley, P.D., Mehnert, H.H., Naeser, C.W., Snee, L.W., Cunningham, C.G., Steven,T.A., Anderson, J.J., Sable, E.G., and Anderson, R.E., 1994a, Isotopic ages andstratigraphy <strong>of</strong> Cenozoic rocks <strong>of</strong> <strong>the</strong> Marysvale volcanic field and adjacent areas,west-central <strong>Utah</strong>: U.S. <strong>Geologic</strong>al <strong>Survey</strong> Bulletin 2071, 35 p.Rowley, P.D., Nealey, L.D., Unruh, D.M., Snee, L.W., Mehnert, H.H., Anderson, R.E.,and Gromme, C.S., 1995, Stratigraphy <strong>of</strong> Miocene ash-flow tuffs in and near <strong>the</strong>Caliente caldera complex, sou<strong>the</strong>astern Nevada and southwestern <strong>Utah</strong>, in Scott,R.B., and Swadley, W C, editors, <strong>Geologic</strong> studies in <strong>the</strong> Basin and Range –Colorado Plateau transition in sou<strong>the</strong>astern Nevada, southwestern <strong>Utah</strong>, andnorthwestern Arizona, 1992: U.S. <strong>Geologic</strong>al <strong>Survey</strong> Bulletin 2056, p. 43-88.Rowley, P.D., Sable, E.G., Boswell, J.T., Vice, G.S., Hatfield, S.C., Maxwell, D.J., Lund,W.R., Anderson, J.J., and Biek, R.F., in preparation, <strong>Interim</strong> geologic map <strong>of</strong> <strong>the</strong>Brian Head quadrangle, Iron County, <strong>Utah</strong>: <strong>Utah</strong> <strong>Geologic</strong>al <strong>Survey</strong> Open-FileReport , xx p., 1 plate, scale 1:24,000.Rowley, P.D., Shroba, R.R., Simonds, F.W., Burke, K.J., Axen, G.J., and Olmore, S.D.,1994b, <strong>Geologic</strong> map <strong>of</strong> <strong>the</strong> Chief Mountain quadrangle, Lincoln County,Nevada: U.S. <strong>Geologic</strong>al <strong>Survey</strong> <strong>Geologic</strong> Quadrangle <strong>Map</strong> GQ-1731, scale1:24,000.84
- Page 1 and 2:
! !! !!! ! ! !! ! ! ! !! ! !! !! !
- 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 and 72: Biek, R.F., Rowley, P.D., Hayden, J
- Page 73 and 74: field guide (The Mackin Volume): Ut
- 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: Flagstaff-Green River basins [abs.]
- 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