Structural Evolution of an Extensional Terrane Margin: Case Studies from the Colorado River Extensional Corridor, Southeastern California, USA
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Southern US 95 & US 93
UNLANDSCAPE ARCHITECTURE & PLANNINGLV RESEARCH CORRIDOR PLAN INCLUDES US 95 SOUTH FROM RAILROAD PASS TO THE CALIFORNIA STATE LINE, US 93 TO Southern US 95 and US 93 HOOVER DAM AND US outhern 95 and 93 95 NORTH OF I-215 TO THE CLARK COUNTY LINE WEST OF INDIAN landscapelandscape andand aestheticsaesthetics corridorcorridor planplan SPRINGS DESIGN WORKSHOP PLACES Sand County Studios JW Zunino & Associates CH2MHill December 15, 2006 Southern US 95 and US 93 corridor plan MESSAGE FROM THE GOVERNOR OF NEVADA MESSAGE FROM THE DIRECTOR OF NEVADA DEPARTMENT OF TRANSPORTATION On June 6, 2002, the Nevada Department of Transportation adopted Landscape and aesthetics are an integral part of the design in as policy, “Pattern and Palette of Place: A Landscape and Aesthetics building and retrofitting our highway system. This Landscape and Master Plan for the Nevada State Highway System.” The second phase Aesthetics Corridor Plan for US 95 and US 93 in Southern Nevada of planning is complete. The Landscape and Aesthetics Corridor helps realize our vision for the future appearance of our highways. Plan represents a significant step forward for the Landscape and The plan will provide the guidance for our own design teams, and Aesthetics program created by the Master Plan because it involves it will help Nevada’s citizens participate in formulating context- local public agencies and citizens in the planning process. Now, sensitive solutions for today’s transportation needs. Together, Nevada’s highways truly represent the State and its people. The we will ensure our highways reflect Nevada’s distinctive heritage, Corridor Plan will be the primary management tool for use in landscape, and culture. -
Utah Geological Association Publication 30.Pub
Utah Geological Association Publication 30 - Pacific Section American Association of Petroleum Geologists Publication GB78 239 CENOZOIC EVOLUTION OF THE NORTHERN COLORADO RIVER EXTEN- SIONAL CORRIDOR, SOUTHERN NEVADA AND NORTHWEST ARIZONA JAMES E. FAULDS1, DANIEL L. FEUERBACH2*, CALVIN F. MILLER3, 4 AND EUGENE I. SMITH 1Nevada Bureau of Mines and Geology, University of Nevada, Mail Stop 178, Reno, NV 89557 2Department of Geology, University of Iowa, Iowa City, IA 52242 *Now at Exxon Mobil Development Company, 16825 Northchase Drive, Houston, TX 77060 3Department of Geology, Vanderbilt University, Nashville, TN 37235 4Department of Geoscience, University of Nevada, Las Vegas, NV 89154 ABSTRACT The northern Colorado River extensional corridor is a 70- to 100-km-wide region of moderately to highly extended crust along the eastern margin of the Basin and Range province in southern Nevada and northwestern Arizona. It has occupied a criti- cal structural position in the western Cordillera since Mesozoic time. In the Cretaceous through early Tertiary, it stood just east and north of major fold and thrust belts and also marked the northern end of a broad, gently (~15o) north-plunging uplift (Kingman arch) that extended southeastward through much of central Arizona. Mesozoic and Paleozoic strata were stripped from the arch by northeast-flowing streams. Peraluminous 65 to 73 Ma granites were emplaced at depths of at least 10 km and exposed in the core of the arch by earliest Miocene time. Calc-alkaline magmatism swept northward through the northern Colorado River extensional corridor during early to middle Miocene time, beginning at ~22 Ma in the south and ~12 Ma in the north. -
Mojave National Preserve Management Plan for Developed
Mojave National Preserve—Management Plan for Developed Water Resources CHAPTER 3: AFFECTED ENVIRONMENT Introduction This chapter describes the unique factors that influence water resource management in the Preserve and the resources that could be affected by the implementation of any of the alternatives described in Chapter 2: Alternatives. The resource descriptions provided in this chapter serve as a baseline to compare the potential effects of the management actions proposed in the alternatives. The following resource topics are described in this chapter: • Environmental Setting • Cultural Resources • Water Resources • Wilderness Character • Wildlife Environmental setting and water resources are important for context and are foundational for water resource management, but are not resources that are analyzed for effects. Resource issues that were considered and dismissed from further analysis are listed in Chapter 1: Purpose of and Need for Action and are not discussed further in this EA. A description of the effects of the proposed alternatives on wildlife, cultural resources, and wilderness character is presented in Chapter 4: Environmental Consequences. Environmental Setting The Preserve includes an ecologically diverse yet fragile desert ecosystem consisting of vegetative attributes that are unique to the Mojave Desert, as well as components of the Great Basin and Sonoran Deserts. Topography The topography of the Preserve is characteristic of the mountain and basin physiographic pattern, with tall mountain ranges separated by corresponding valleys filled with alluvial sediments. Primary mountain ranges in the Preserve, from west to east, include the Granite, Kelso, Providence, Clark, New York, and Piute Mountains. Major alluvial valleys include Soda Lake (dry lake bed), Shadow Valley, Ivanpah Valley, Lanfair Valley, and Fenner Valley. -
Preliminary Geologic Map of the Little Piute Mountains, San Bernardino County, California
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Preliminary Geologic Map of the Little Piute Mountains, San Bernardino County, California by Keith A. Howard1, Michael L. Dennis2, Karl E. Karlstrom3, and Geoffrey A. Phelps1 Open-File Report 95-598 1995 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American stratigraphic code. Any use of trade, product, or firm names is for descriptive purpose only and does not imply endorsement by the U.S. Government. 1 Menlo Park, California 94025 2 Northern Arizona University, Flagstaff, Arizona 86002 3 University of New Mexico, Albuquerque, New Mexico 87131 Mapped 1978-1993 by K. Howard, P. Stone, K. Karlstrom, G. Phelps, M. Dennis, and students from Northern Arizona University. GEOLOGIC SUMMARY Introduction The Little Piute Mountains in the eastern Mojave Desert expose a series of folds and thrust faults involving metamorphosed Paleozoic strata (Miller and others, 1982; Stone and others, 1983). Detailed mapping of these structures was undertaken to help elucidate regional Mesozoic structural evolution. Earlier geologic maps were prepared by Cooksley (1960a,b,c,d, generalized by Bishop, 1964) and Stone and others (1983). Deformed and metamorphosed Paleozoic and Triassic rocks form a stratal succession that was originally deposited in shallow seas on the North American craton. Based on lithologic sequence the units are correlated with unmetamorphosed equivalents 200 km to the northeast in the Grand Canyon, Arizona, and 35-50 km to the west in the Marble, Ship, and Providence Mountains, California (Stone and others, 1983). -
Mojave-Road2.Pdf
Mojave Road Detour over the Piute Range The following road log provides a 14.2 mile detour or "go around" to get over the Piute Range if the old Underground Telephone Cable Road is not practicable or closed. GPS coordinates and elevations are included. Even if the road over the Piute Range is open, this route can serve as a pleasant side trip off the Mojave Road, providing an interesting visit to Leiser Ray Mine, the Signal Mining District, Tungsten Flat, and the old Craig family home site. 0.0 N35° 5.47’ W114° 57.30’ (Elevation 2,473 feet) Begin at Mile 27.0 on page 66 in the 2010 edition of the Mojave Road Guide. Instead of turning right (west) to go over the Piute Range, continue generally south on the Metropolitan Water District (MWD) service road. 2.8 miles to: 2.8 N35° 3.05’ W114° 57.40’ (Elevation 2,723 feet) Turn off the MWD service road, curving right on a dirt “flyover.” Continue on this road in a southwest direction. A BLM carsonite trail sign indicates you are on route NN9108. 1.0 mile to: 3.8 N35° 2.69’ W114° 58.38’ (Elevation 2,861 feet) Come to a "Y." Take the road to the right (straight ahead). A BLM carsonite trail sign indicates route [NN9]108 goes to the right. 0.5 mile to: 4.3 N35° 2.40’ W114° 58.68’ (Elevation 2,908 feet) Turn right, up a wash. 0.0+ mile to: 4.3+ Pass a National Park Service Mojave National Preserve boundary marker. -
Distribution and Seasonal Movements of Bendire's Thrasher in California
WESTERN BIRDS Volume 20, Number 3, 1989 DISTRIBUTION AND SEASONAL MOVEMENTS OF BENDIRE'S THRASHER IN CALIFORNIA A. SIDNEY ENGLAND, Departmentof Wildlifeand FisheriesBiology, University of California, Davis. California 95616 WILLIAM E LAUDENSLAYER,JR., U.S. D. A. ForestService, Forestry Sciences Laboratory,2081 E. SierraAvenue, Fresno, California 93710 The ecology and distribution of Bendire's Thrasher (Toxostorna bendirei)have been little studiedand are poorlyunderstood. Garrett and Dunn (1981:280) classifiedthe speciesas a "fairlycommon but very local summer resident on the Mojave Desert" in southern California. Californiabreeding populations are known primarily from the eastern Mojave Desert and scattered locations in and around Joshua Tree NationalMonument in the southernMojave Desert (Johnson et al. 1948, Miller and Stebbins1964, Garrett and Dunn 1981), areas frequently visitedby bird watchersand naturalists. However, recordsfrom other parts of the Mojave and Colorado deserts suggest that breeding populationsof Bendire'sThrasher may be more widely distributedthan currentlyrecognized. Also, the preferredbreeding habitat in Californiais relativelywidespread. This habitatis typicallydescribed as Mojavedesert scrubwith either JoshuaTrees (Yucca brevifolia), SpanishBayonet (Y. baccata), Mojave Yucca (Y. schidigera), cholla cactus (Opuntia acanthocarpa,O. echinocarpa,or O. rarnosissirna),or other succulents (Grinnelland Miller 1944, Bent 1948, Garrett and Dunn 1981). Remsen(1978) consideredthe total Californiabreeding population of Bendire'sThrasher to be under 200 pairs, and the specieshas been placedon the list of Bird Speciesof SpecialConcern by the California Departmentof Fishand Game (Remsen1978). It was placedon this list becausepopulations are smalland locallydistributed and believedto be threatenedby off-roadvehicle use, overgrazing,and harvestingof Joshua Treesand other speciesof yucca. In this paper, we report the resultsof a 2-year studyof the breeding- season distributionand movement patterns of Bendire's Thrasher in California. -
Mojave National Preserve Management Plan for Developed Water Sources
to Las Vegas to Las Vegas Kin Primm gsto E n S W E H G T G a I sh N G N A M Wilderness H R A L Y N R A I (! (!A A N Clark Mountain )" H #T R D N (! (! G # G (! U (! N R U U IO ") N A 95 O (! Y E Yates Well P O S (! A x N C C I L c M (! F IC G e U H IVANPAH R L l K A E Mojave National Preserve s IL L i R R U o # 15 O A (! LAKE (! C A r A Water Resources Management Plan and Environmental Assessment D M L (dry) c D C i n ash M 164 O e LL W HI n Searchlight R WK o MOHA at o Nipton W he a Mojave National Preserve boundary W d )" P # Nipton Road I Salton # ### 164 U M ## # National Park Service wilderness E I T Sea G N h E s N E R Y a A A W # R L (! E s L S Spring ng A H V ri C IL ES L L p M N A S 127 ll L L )" CIMA ROAD # Ivanpah Road I u L Small game guzzler B A )" (! A E V # )" V Y S T " Big game guzzler T # ## A N (! S # M (! L )" # (!(! # Halloran Springs #Morning U N # L (! I # ## (! # Well H E # Star Mine # O h ##(!# A ## s ## W (! )" A Y (! # T a H i # M (! CASTLE ## P l sh (!# Paved road lo a N W # A w W MOUNTAINS N Willow e U )" # P NATIONAL t SILVER A u Spring O i 15 N MONUMENT LAKE # V (! P Unpaved 2-wheel drive road I A (!# # # M (dry) (! # )" Morning Star Mine Road V (! I (! E Cal Nev Ari # L Kessler Unpaved 4-wheel drive road #(!# T # #### Spring K (!## S CIMA R (! (!# Mine Ro (! (! # rt a # A (! ! O # a d Mojave Road 4-wheel drive road #(!#(! ( Y C h DOME (! !( H # s Deer ( (! W (! a E (!(! Spring #(! N (! )" )" P W# (! Keystone Desert wash (! I NEVADA Baker Kelbaker Rd nk (! (! CALIFORNIA a (! (! U T (!(! # (! (! Spring ck -
Piute Valley Groundwater Basin Bulletin 118
Hydrologic Region Colorado River California’s Groundwater Piute Valley Groundwater Basin Bulletin 118 Piute Valley Groundwater Basin • Groundwater Basin Number: 7-45 • County: San Bernardino • Surface Area: 176,000 acres (275 square miles) Basin Boundaries and Hydrology This basin underlies a portion of Piute Valley in eastern San Bernardino County. The Piute Valley, and its underlying groundwater basin, extends into southern Nevada (Jennings 1961; Bishop 1963), but this report considers only the portion that lies within California. The basin is bounded by the nonwater-bearing rocks of the Dead Mountains on the east, of the Piute Range and Homer Mountain on the northwest, of the Piute Mountains on the southwest, and of the Sacramento Mountains on the southeast (Bishop 1963). The valley is drained by Piute Wash to the southeastern part of the valley, where the drainage enters the Needles Valley and flows eastward to the Colorado River. Annual average precipitation ranges from about 4 to 8 inches. Hydrogeologic Information Water Bearing Formations Groundwater in the basin is found in younger and older alluvium. Older alluvium of Pleistocene age consists of fine to coarse sand interbedded with gravel, silt, and clay. Younger alluvium of Holocene age consists of poorly sorted gravel, sand, silt, and clay (DWR 1954). Valley fill extends to at least 1,044 feet in the central part of the basin and 920 feet in the southeastern part of the basin. Wells in the basin yield a maximum of 1,500 gpm. Restrictive Structures A fault in this basin may be a barrier to groundwater flow (DWR 1954). -
Pluton Emplacement Along an Active Ductile Thrust Zone, Piute Mountains, Southeastern California: Interaction Between Deformationai and Solidification Processes
Pluton emplacement along an active ductile thrust zone, Piute Mountains, southeastern California: Interaction between deformationai and solidification processes K. E. KARLSTROM University of New Mexico, Albuquerque, New Mexico 87131 C. F. MILLER | Vanderbilt University, Nashville, Tennessee 37235 J. A. KINGSBURY J. L. WOODEN U.S. Geological Survey, Menlo Park, California 94025 ABSTRACT id-state deformationai fabrics and brittle syn- space with regional, as opposed to only em- thetic thrusts that offset the pluton margin placement-related, deformation. Plutons that are emplaced synchronously record sharp temperature decline during and Two end-member models for granitoid as- with regional deformation offer the opportu- after crystallization. cent and emplacement are shown in Figure 1. nity to understand the partitioning of defor- Because plutons crystallize rapidly, they can Although ascent and emplacement may often mation and metamorphism in time and space be used to estimate strain rates during orogeny. involve a combination of mechanisms, exam- during orogeny. The 85 Ma East Piute pluton Thermal modeling suggests that the transition ination of end members highlights some of the of the eastern Mojave Desert is an unusually from rheological liquid to solid in the East Piute controversies surrounding the interpretation dear example of a syntectonic pluton; it was pluton occurred during an interval of about 104 of the relative timing of pluton emplacement emplaced during thrusting in the southern yr. As final increments of ductile deformation and regional deformation. Diapiric ascent is Cordillera. Combined petrologic and struc- coincided with final crystallization of evolved often considered to be linked to models of tural studies lead to empirical models for the compositional units, total strain recorded by forceful emplacement, where buoyancy- dynamic interaction of magmatic and defor- fabric in the pluton apparently accumulated driven ascent of the pluton induces ductile mationai processes during granitoid emplace- during this interval. -
Mojave Road Detour Over the Piute Range
Mojave Road Detour over the Piute Range 33.8 14.2 13.9 13.2 27.0 M O J 0.0 A V E R O A D 11.6 11.3 10.9 10.5 10.2 9.9 2.8 9.7 3.8 9.3 5.1 4.3 5.5 8.9 6.7 8.3 7.9 6.9 7.7 8.5 Leiser Ray Mine 7.5 CHRIS S. ERVIN 2016 Mojave Desert Heritage and Cultural Association 37198 Lanfair Road # G-15 Essex, California 92332 760-733-4482 [email protected] Map and Road Log Revised: 17 January 2017 Mojave Road Detour over the Piute Range The following road log provides a 14.2 mile detour or "go around" to get over the Piute Range if the old Underground Telephone Cable Road is not practicable or closed. GPS coordinates and elevations are included. Even if the road over the Piute Range is open, this route can serve as a pleasant side trip off the Mojave Road, providing an interesting visit to Leiser Ray Mine, the Signal Mining District, Tungsten Flat, and the old Craig family home site. 0.0 N35° 5.47’ W114° 57.30’ (Elevation 2,473 feet) Begin at Mile 27.0 on page 66 in the 2010 edition of the Mojave Road Guide. Instead of turning right (west) to go over the Piute Range, continue generally south on the Metropolitan Water District (MWD) service road. 2.8 miles to: 2.8 N35° 3.05’ W114° 57.40’ (Elevation 2,723 feet) Turn off the MWD service road, curving right on a dirt “flyover.” Continue on this road in a southwest direction. -
Henderson, Nevada
December 2016 Local Foods, Local Places A Community-Driven Action Plan for Henderson, Nevada A technical assistance program of the U.S. Environmental Protection Agency, U.S. Department of Agriculture, U.S. Department of Transportation, Centers for Disease Control and Prevention, Appalachian Regional Commission, and Delta Regional Authority Table of Contents: Local Foods Local Places Program ..................................................................................................... 1 Community Story .............................................................................................................................. 1 Challenges ........................................................................................................................................ 3 Opportunities ................................................................................................................................... 6 Project Assistance ............................................................................................................................ 8 Action Plan ..................................................................................................................................... 12 Vision ............................................................................................................................................................................................... 13 GOAL 1: .......................................................................................................................................................................................... -
Geologic Map of the East of Grotto Hills Quadrangle, California
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE EAST OF GROTTO HILLS QUADRANGLE, CALIFORNIA by Jane E. Nielson1 Open-File Report 98-469 Although here released in the Open File series, this report has been reviewed for conformity with U.S. Geological Survey editorial standards and the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. government. Emeritus, 345 Middlefield Road, Menlo Park, CA, 94025 1998 DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP OF 98-469 U.S. GEOLOGICAL SURVEY GEOLOGIC MAP OF THE EAST OF GROTTO HILLS QUADRANGLE, CALIFORNIA by Jane E. Nielson INTRODUCTION The East of Grotto Hills l:24,000-scale quadrangle of California lies west of the Colorado River about 30 km southwest of Searchlight, Nevada (figs. 1, 2), near the boundary between the northern and southern parts of the Basin and Range Province. The quadrangle includes the eastern margin of Lanfair Valley, the southernmost part of the Castle Mountains, and part of the northwest Piute Range. The generally north-trending Piute Range aligns with the Piute and Dead Mountains of California and the Newberry and Eldorado Mountains and McCullough Range of Nevada (fig. 1). The southern part of the Piute Range adjoins Homer Mountain (Spencer and Turner, 1985) near Civil War-era Fort Piute (fig. 2). Adjacent l:24,000-scale quadrangles include Castle Peaks, Homer Mountain, and Signal Hill, Calif.; also Hart Peak, Tenmile Well, and West of Juniper Mine, Figure 1.