scholarly journals Birth and evolution of the Virgin River fluvial system: ∼1 km of post–5 Ma uplift of the western Colorado Plateau

Geosphere ◽  
2019 ◽  
Vol 15 (3) ◽  
pp. 759-782 ◽  
Author(s):  
Cory J. Walk ◽  
Karl E. Karlstrom ◽  
Ryan S. Crow ◽  
Matthew T. Heizler
Keyword(s):  
Colorado Plateau ◽  
Fluvial System ◽  
Western Colorado ◽  
Virgin River ◽  
System 1

BIRTH AND EVOLUTION OF THE VIRGIN RIVER: POST 5 MA UPLIFT OF THE WESTERN COLORADO PLATEAU

2018 ◽  
Author(s):  
Cory J. Walk ◽  
◽  
Karl E. Karlstrom ◽  
Ryan S. Crow ◽  
Matthew T. Heizler
Keyword(s):  
Colorado Plateau ◽  
Western Colorado ◽  
Virgin River

scholarly journals Growth faults in the Kaiparowits Basin, Utah, pinpoint initial Laramide deformation in the western Colorado Plateau

Lithosphere ◽  
10.1130/l79.1 ◽  
2010 ◽  
Vol 2 (4) ◽  
pp. 221-231 ◽  
Author(s):  
S.E. Tindall ◽  
L.P. Storm ◽  
T.A. Jenesky ◽  
E.L. Simpson
Keyword(s):  
Colorado Plateau ◽  
Western Colorado

scholarly journals A constraint on post–6 Ma timing of western Grand Canyon (Arizona, USA) incision removed: Local derivation indicated by ca. 5.4 Ma fluvial deposits below Shivwits Plateau basalts north of Grand Canyon

Geosphere ◽  
2021 ◽  
Author(s):  
A.T. Steelquist ◽  
G.E. Hilley ◽  
I. Lucchitta ◽  
R.A. Young
Keyword(s):  
United States ◽  
Detrital Zircon ◽  
Colorado River ◽  
Landscape Evolution ◽  
Colorado Plateau ◽  
Grand Canyon ◽  
River System ◽  
Fluvial Deposits ◽  
Western Colorado ◽  
Rule Out

The timing of integration of the Colorado River system is central to understanding the landscape evolution of much of the southwestern United States. However, the time at which the Colorado River started incising the westernmost Grand Canyon (Arizona) is still an unsettled question, with conflicting interpretations of both geologic and thermochronologic data from western Grand Canyon. Fluvial gravels on the Shivwits Plateau, north of the canyon, have been reported to contain clasts derived from south of the modern canyon, suggesting the absence of western Grand Canyon at the time of their deposition. In this study, we reassess these deposits using modern geochronologic measurements to determine the age of the deposits and the presence or absence of clasts from south of the Grand Canyon. We could not identify southerly derived clasts, so cannot rule out the existence of a major topographic barrier such as Grand Canyon prior to the age of deposition of the gravels. 40Ar/39Ar analysis of a basalt clast entrained in the upper deposit (in combination with prior data) supports a maximum age of deposition of ca. 5.4 Ma, limiting deposition to post-Miocene, a period from which very few diagnostic and dated fluvial deposits remain in the western Colorado Plateau. Analysis of detrital zircon composition of the sand matrix supports interpretation of the deposit as being locally derived and not part of a major throughgoing river. We suggest that the published constraint of <6 Ma timing of Grand Canyon incision may be removed, given that no clasts that must be sourced from south of Grand Canyon were found in the only known outcrop of gravels under the Shivwits Plateau basalts at Grassy Mountain north of Grand Canyon.

scholarly journals Phylogenetic revision of the psammophilic Trogloderus LeConte (Coleoptera: Tenebrionidae), with biogeographic implications for the Intermountain Region

PeerJ ◽  
2019 ◽  
Vol 7 ◽  
pp. e8039 ◽  
Author(s):  
M. Andrew Johnston
Keyword(s):  
New Species ◽  
Great Basin ◽  
Colorado Plateau ◽  
Recent Common Ancestor ◽  
Owens Valley ◽  
Most Recent Common Ancestor ◽  
Western Colorado ◽  
Intermountain Region ◽  
Mohave Desert ◽  
Phylogenetic Revision

The genus Trogloderus LeConte, 1879, which is restricted to dunes and sandy habitats in the western United States, is revised using morphological and molecular information. Six new species are described from desert regions: Trogloderus arcanus New Species (Lahontan Trough); Trogloderus kandai New Species (Owens Valley); Trogloderus major New Species (Mohave Desert); Trogloderus skillmani New Species (eastern Great Basin and Mohave Desert); Trogloderus verpus New Species (eastern Colorado Plateau); and Trogloderus warneri New Species (western Colorado Plateau). A molecular phylogeny is presented for the genus and used to infer its historical biogeography. The most recent common ancestor of Trogloderus is dated to 5.2 mya and is inferred to have inhabited the Colorado Plateau. Current species most likely arose during the mid-Pleistocene where the geographic features of the Lahontan Trough, Bouse Embayment and Kaibab Plateau were significant factors driving speciation.

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