Geology of the Greenwater Range, and the Dawn of Death Valley, California Field Guide for the Death Valley Natural History Conference, 2013

Total Page:16

File Type:pdf, Size:1020Kb

Geology of the Greenwater Range, and the Dawn of Death Valley, California Field Guide for the Death Valley Natural History Conference, 2013 Geology of the Greenwater Range, and the Dawn of Death Valley, California Field Guide for the Death Valley Natural History Conference, 2013 By J.P. Calzia, O.T. Rämö, Robert Jachens, Eugene Smith, and Jeffrey Knott Open-File Report 2016–1064 U.S. Department of the Interior U.S. Geological Survey Cover: Photograph looking north from Dantes View across Death Valley toward the Panamint Range, October, 2015. Photograph by Pietari Skyttä, University of Turku, Finland. U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. Geological Survey, Reston, Virginia: 2016 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov/ or call 1–888–ASK–USGS (1–888–275–8747). For an overview of USGS information products, including maps, imagery, and publications, visit http://store.usgs.gov/. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this information product, for the most part, is in the public domain, it also may contain copyrighted materials as noted in the text. Permission to reproduce copyrighted items must be secured from the copyright owner. Suggested citation: Calzia, J.P., Rämö, O.T., Jachens, Robert, Smith, Eugene, and Knott, Jeffrey, 2016, Geology of the Greenwater Range, and the dawn of Death Valley, California—Field guide for the Death Valley Natural History Conference, 2013: U.S. Geological Survey Open-File Report 2016–1064, 32 p., http://dx.doi.org/10.3133/ofr20161064. ISSN 2331-1258 (online) Contents Introduction .................................................................................................................................................... 1 STOP 1. GEOLOGY OF THE SHOSHONE PLUTON, DEATH VALLEY, CALIFORNIA ............................... 2 Introduction ................................................................................................................................................ 2 Geology...................................................................................................................................................... 3 STOP 2. MORE GEOLOGY, THEN ISOTOPE GEOCHEMISTRY OF THE SHOSHONE PLUTON, DEATH VALLEY, CALIFORNIA .................................................................................................................................. 6 Geology...................................................................................................................................................... 6 Isotope Geochemistry ................................................................................................................................ 6 Conclusions ............................................................................................................................................... 7 STOP 3. GRAVITY FIELD OF GREENWATER VALLEY, GREENWATER RANGE, AND SURROUNDING RANGES, DEATH VALLEY, CALIFORNIA—IMPLICATIONS FOR SUBSURFACE DISTRIBUTION OF NEOGENE VOLCANIC AND PLUTONIC ROCKS ........................................................................................ 9 Introduction ................................................................................................................................................ 9 Purpose and Method ................................................................................................................................ 11 Interpretation ............................................................................................................................................ 12 Discussion................................................................................................................................................ 12 STOP 4. PLIOCENE CRATER OR CALDERA IN THE GREENWATER RANGE ....................................... 15 Introduction .............................................................................................................................................. 15 Geologic Setting of the Greenwater Range .............................................................................................. 15 Basalt and Rhyolite Volcanoes of the Greenwater Range ....................................................................... 17 Evidence for a Crater or Caldera in the Greenwater Range ..................................................................... 20 STOP 5: THE ANCIENT FURNACE CREEK BASIN AT ZABRISKIE POINT .............................................. 22 Introduction .............................................................................................................................................. 22 Furnace Creek Formation ........................................................................................................................ 25 Source of Furnace Creek Formation Sediments ...................................................................................... 26 Interpretations and Conclusions ............................................................................................................... 29 Acknowledgments ....................................................................................................................................... 29 References Cited ......................................................................................................................................... 30 Figures 1–1. Google Earth image showing stop locations. .................................................................................... 2 1–2. Photograph showing quartz monzonite and monzodiorite from the Shoshone Pluton ...................... 3 1–3. Photographs showing contact between Shoshone Pluton and Shoshone Volcanics ........................ 4 2–1. Graphs showing 87Sr/86Sri ratios versus εNdi for samples analyzed from Greenwater Range and vicinity ............................................................................................................................................... 8 3–1. Map showing isostatic residual gravity field of Greenwater province and surrounding areas ......... 10 3–2. Schematic diagram illustrating method used to interpret gravity data ............................................. 11 3–3. Map showing inferred depth to bottom of Cenozoic volcanic rocks of Greenwater province .......... 13 3–4. Map showing inferred depth to bottom of Tertiary granitic pluton beneath Greenwater province ... 14 4–1. Map showing location of Greenwater Range with respect to Greenwater Valley and Furnace Creek Faults .............................................................................................................................................. 16 4–2. Geologic map of Greenwater Range showing Funeral Formation basalt centers and related flows, Greenwater caldera, locations of major rhyolite domes, and Miocene volcanic section ................. 19 iii 4–3. Photograph showing rhyolite and basalt pinch out against borax-bearing sediments of Furnace Creek Formation ............................................................................................................................. 20 4–4. Map showing isostatic gravity survey of eastern Death Valley area ............................................... 21 5–1. Generalized geologic map of northwest-elongated Furnace Creek basin near Zabriskie Point showing major rock groups and geologic structures ....................................................................... 23 5–2. Generalized geologic map of the Zabriskie Point area ................................................................... 24 5–3. Stratigraphic section up Zabriskie Wash showing correlation to magnetic polarity time scale ........ 27 5–4. Block diagrams showing depositional and tectonic setting of Furnace Creek Formation ................ 28 iv Geology of the Greenwater Range, and the Dawn of Death Valley, California Field Guide for the Death Valley Natural History Conference, 2013 By J.P. Calzia,1 O.T. Rämö,2 Robert Jachens,1 Eugene Smith,3 and Jeffrey Knott4 Introduction Much has been written about the age and formation of Death Valley, but that is one—if not the last—chapter in the fascinating geologic history of this area. Igneous and sedimentary rocks in the Greenwater Range, one mountain range east of Death Valley, tell an earlier story that overlaps with the formation of Death Valley proper. This early story has been told by scientists who have studied these rocks for many years and continue to do so. This field guide was prepared for the first Death Valley Natural History Conference and provides an overview of the geology of the Greenwater Range and the early history (10–0 Ma) of Death Valley. 1U.S. Geological Survey 2University of Helsinki 3University of Nevada Las Vegas 4California State University Fullerton STOP 1. GEOLOGY OF THE SHOSHONE PLUTON, DEATH VALLEY, CALIFORNIA By J.P. Calzia,1 O.T. Rämö,2 and Bennie Troxel3 This stop is located at lat 35°58′50.72ʺN., long 116°20ʹ18.20ʺW., the entrance to Death Valley National Park on Highway 178 (fig. 1-1). Introduction The Shoshone Pluton is located at the southern end of the Greenwater Range, approximately 40 kilometers (km) east of Death Valley and 9 km north of Shoshone, California (fig. 1-1). It is one of several granitic bodies that are synchronous with Late Tertiary to Quaternary crustal extension of the Death Valley region. Figure 1–1. Google Earth image
Recommended publications
  • Alluvial Fans in the Death Valley Region California and Nevada
    Alluvial Fans in the Death Valley Region California and Nevada GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 Alluvial Fans in the Death Valley Region California and Nevada By CHARLES S. DENNY GEOLOGICAL SURVEY PROFESSIONAL PAPER 466 A survey and interpretation of some aspects of desert geomorphology UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publications as follows: Denny, Charles Storrow, 1911- Alluvial fans in the Death Valley region, California and Nevada. Washington, U.S. Govt. Print. Off., 1964. iv, 61 p. illus., maps (5 fold. col. in pocket) diagrs., profiles, tables. 30 cm. (U.S. Geological Survey. Professional Paper 466) Bibliography: p. 59. 1. Physical geography California Death Valley region. 2. Physi­ cal geography Nevada Death Valley region. 3. Sedimentation and deposition. 4. Alluvium. I. Title. II. Title: Death Valley region. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C., 20402 CONTENTS Page Page Abstract.. _ ________________ 1 Shadow Mountain fan Continued Introduction. ______________ 2 Origin of the Shadow Mountain fan. 21 Method of study________ 2 Fan east of Alkali Flat- ___-__---.__-_- 25 Definitions and symbols. 6 Fans surrounding hills near Devils Hole_ 25 Geography _________________ 6 Bat Mountain fan___-____-___--___-__ 25 Shadow Mountain fan..______ 7 Fans east of Greenwater Range___ ______ 30 Geology.______________ 9 Fans in Greenwater Valley..-----_____. 32 Death Valley fans.__________--___-__- 32 Geomorpholo gy ______ 9 Characteristics of fans.._______-___-__- 38 Modern washes____.
    [Show full text]
  • Hydrologic Basin Death Valley California
    Hydrologic Basin Death Valley California GEOLOGICAL SURVEY PROFESSIONAL PAPER 494-B Hydrologic Basin Death Valley California By CHARLES B. HUNT, T. W. ROBINSON, WALTER A. BOWLES, and A. L. WASHBURN GENERAL GEOLOGY OF DEATH VALLEY, CALIFORNIA GEOLOGICAL SURVEY PROFESSIONAL PAPER 494-B A! description of the hydrology, geochemistry, and patternedground of the saltpan UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1966 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Page Abstract BI Hydrology-Continued Hydrology, by Charles B. Hunt and T. W. Robinson_ - 3 Descriptions and discharges of springs and of Introduction- 3 marshes-Continued Fieldwork- 3 Discharge of springs in the Furnace Creek fault Climate- 5 zone B35 Rainfall 5 Evapotranspiration discharge from the valley floor Evaporation 7 above the saltpan 37 Temperature- 8 Divisions of the valley according to sources of Humidity- 10 ground water 37 Wind- 11 Possible sources of water at Cottonball Marsh- 37 Rock types in the Death Valley hydrologic basin --- 11 Possible source of water at springs along Fur- Hard-rock formations 12 nace Creek fault zone 38 Unconsolidated Quaternary deposits 13 Geochemistry of the saltpan by Charles B. Hunt 40 Gravel deposits 13 General features 40 Fine-grained alluvial and playa deposits - 15 Fieldwork and acknowledgments 41 Salt deposits and saliferous playa deposits- 15 Geologic
    [Show full text]
  • Death Valley National Park
    COMPLIMENTARY $3.95 2019/2020 YOUR COMPLETE GUIDE TO THE PARKS DEATH VALLEY NATIONAL PARK ACTIVITIES • SIGHTSEEING • DINING • LODGING TRAILS • HISTORY • MAPS • MORE OFFICIAL PARTNERS T:5.375” S:4.75” PLAN YOUR VISIT WELCOME S:7.375” In T:8.375” 1994, Death Valley National SO TASTY EVERYONE WILL WANT A BITE. Monument was expanded by 1.3 million FUN FACTS acres and redesignated a national park by the California Desert Protection Act. Established: Death Valley became a The largest national park below Alaska, national monument in 1933 and is famed this designation helped focus protection for being the hottest, lowest and driest on one the most iconic landscapes in the location in the country. The parched world. In 2018 nearly 1.7 million people landscape rises into snow-capped mountains and is home to the Timbisha visited the park, a new visitation record. Shoshone people. Death Valley is renowned for its colorful Land Area: The park’s 3.4 million acres and complex geology. Its extremes of stretch across two states, California and elevation support a great diversity of life Nevada. and provide a natural geologic museum. Highest Elevation: The top of This region is the ancestral homeland Telescope Peak is 11,049 feet high. The of the Timbisha Shoshone Tribe. The lowest is -282 feet at Badwater Basin. Timbisha established a life in concert Plants and Animals: Death Valley with nature. is home to 51 mammal species, 307 Ninety-three percent of the park is bird species, 36 reptile species, two designated wilderness, providing unique amphibian species and five fish species.
    [Show full text]
  • 5 Day Itinerary
    by a grant from Travel Nevada. Travel from grant a by possible made brochure This JUST 98 MILES NORTH OF LAS VEGAS ON HIGHWAY 95. HIGHWAY ON VEGAS LAS OF NORTH MILES 98 JUST www.beattynevada.org Ph: 1.866.736.3716 Ph: Studio 401 Arts & Salon & Arts 401 Studio Mama’s Sweet Ice Sweet Mama’s Smash Hit Subs Hit Smash VFW Chow VFW Smokin’ J’s BBQ J’s Smokin’ shoot out or two performed by our local cowboys. cowboys. local our by performed two or out shoot Gema’s Café Gema’s historical area you might catch a glimpse of a a of glimpse a catch might you area historical Death Valley Coffee Time Coffee Valley Death of our local eateries. If you are in the downtown downtown the in are you If eateries. local our of Roadhouse 95 Roadhouse After your day trips into the Valley, relax at one one at relax Valley, the into trips day your After Sourdough Saloon & Eatery & Saloon Sourdough lunch at Beatty’s Cottonwood Park. Park. Cottonwood Beatty’s at lunch Hot Stuff Pizza Stuff Hot Store or enjoy walking your dog or having a picnic picnic a having or dog your walking enjoy or Store Mel’s Diner Mel’s Town, the Famous Death Valley Nut and Candy Candy and Nut Valley Death Famous the Town, Happy Burro Chili & Beer & Chili Burro Happy open daily from 10 am to 3 pm, Rhyolite Ghost Ghost Rhyolite pm, 3 to am 10 from daily open The Death Valley Nut & Candy Store Candy & Nut Valley Death The can find in our little town, the Beatty Museum, Museum, Beatty the town, little our in find can LOCAL SHOPS & EATERIES & SHOPS LOCAL Day area, be sure to visit the unique businesses that you you that businesses unique the visit to sure be area, BEATTY Between trips to explore the Death Valley Valley Death the explore to trips Between your plan for each day, and set up a check in time.
    [Show full text]
  • A Transect Across the Death Valley Extended Terrane, California Michael S
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. B1, 2010, 10.1029/2001JB000239, 2002 Assessing vertical axis rotations in large-magnitude extensional settings: A transect across the Death Valley extended terrane, California Michael S. Petronis and John W. Geissman Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, USA Daniel K. Holm Department of Geology, Kent State University, Kent, Ohio, USA Brian Wernicke and Edwin Schauble Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA Received 11 September 2000; revised 7 May 2001; accepted 14 July 2001; published 18 January 2002. [1] Models for Neogene crustal deformation in the central Death Valley extended terrane, southeastern California, differ markedly in their estimates of upper crustal extension versus shear translations. Documentation of vertical axis rotations of range-scale crustal blocks (or parts thereof) is critical when attempting to reconstruct this highly extended region. To better define the magnitude, aerial extent, and timing of vertical axis rotation that could mark shear translation of the crust in this area, paleomagnetic data were obtained from Tertiary igneous and remagnetized Paleozoic carbonate rocks along a roughly east-west traverse parallel to about 36°N latitude. Sites were established in 7 to 5 Ma volcanic sequences (Greenwater Canyon and Brown’s Peak) and the 10 Ma Chocolate Sundae Mountain granite in the Greenwater Range, 8.5 to 7.5 Ma and 5 to 4 Ma basalts on the east flank of the Black Mountains, the 10.6 Ma Little Chief stock and upper Miocene(?) basalts in the eastern Panamint Mountains, and Paleozoic Pogonip Group carbonate strata in the north central Panamint Mountains.
    [Show full text]
  • Death Valley National Monument
    DEATH VALLEY NATIONAL MONUMENT D/ETT H VALLEY NATIONAL 2 OPEN ALL YEAR o ^^uJv^/nsurty 2! c! Contents 2 w Scenic Attractions 2 2! Suggested Trips in Death Valley 4 H History 7 Indians 8 Wildlife 9 Plants 12 Geology 18 How To Reach Death Valley 23 By Automobile 23 By Airplane, Bus, or Railroad 24 Administration 25 Naturalist Service 25 Free Public Campground 25 Accommodations 25 References 27 UNITED STATES DEPARTMENT OF THE INTERIOR- Harold L. Ickes, Secretary NATIONAL PARK SERVICE Arno B. Cammerer, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON EATH VALLEY National Monument was created by Presidential proclamation on 2February 11), 1933, and enlarged to its present dimensions on March 26, 1937. Embracing 2,981 square miles, or nearly 2 million acres of primitive, unspoiled desert country, it is the second largest area administered by the National Park Service in the United States proper. Famed as the scene of a tragic episode in the gold-rush drama of '49, Death Valley has long been known to scientist and layman alike as a region rich in scientific and human interest. Its distinctive types of scenery, its geological phenomena, its flora, and climate are not duplicated by any other area open to general travel. In all ways it is different and unique. The monument is situated in the rugged desert region lying east of the High Sierra in eastern California and southwestern Nevada. The valley itself is about 140 miles in length, with the forbidding Panamint Range forming the western wall, and the precipitous slopes of the Funeral Range bounding it on the east.
    [Show full text]
  • Sustaining the Legacies: Mining and Death Valley
    Volume 61 Issue 3 Fall 2016 Sustaining the Legacies: Mining and Death Valley eath Valley entered my radar about ive years ago when I By Nathan Francis, Board Chair DVNHA Dmoved to the region to work as land manager for Rio Tinto Minerals (U.S. Borax). Until then, I admit it had not been on my College of Mines and Earth Sciences to show them irst-hand the bucket list of places to visit. But as my knowledge about the area region’s legacy of mining. It is my job at Rio Tinto, speciically, to grew, so did my passion for everything it ofers — including its ensure the company’s mining legacy sites in the area are safe and rich history and culture. sustainable. As this year’s board chair of the Death Valley Natural History Association, I am honored and privileged to broaden that People outside of the mining industry are often surprised at role and my support of this national treasure. how intertwined the company’s history is with that of America’s national parks, and particularly Death Valley. In fact, they are very Certainly, my interest in the Death Valley area goes beyond my closely aligned. professional role. My wife and I often explore the region with our four sons. Some of our favorite spots include Ash Meadows It was in Death Valley that the Paciic Coast Borax Company got National Wildlife Refuge, the mesquite lat dunes, Golden its start in the late 1800s. The company eventually became U.S. Canyon, and the salt lats at Badwater.
    [Show full text]
  • Inventory of Amphibians and Reptiles at Death Valley National Park
    Inventory of Amphibians and Reptiles at Death Valley National Park Final Report Permit # DEVA-2003-SCI-0010 (amphibians) and DEVA-2002-SCI-0010 (reptiles) Accession # DEVA- 2493 (amphibians) and DEVA-2453 (reptiles) Trevor B. Persons and Erika M. Nowak Common Chuckwalla in Greenwater Canyon, Death Valley National Park (TBP photo). USGS Southwest Biological Science Center Colorado Plateau Research Station Box 5614, Northern Arizona University Flagstaff, Arizona 86011 May 2006 Death Valley Amphibians and Reptiles_____________________________________________________ ABSTRACT As part of the National Park Service Inventory and Monitoring Program in the Mojave Network, we conducted an inventory of amphibians and reptiles at Death Valley National Park in 2002- 2004. Objectives for this inventory were to: 1) Inventory and document the occurrence of reptile and amphibian species occurring at DEVA, primarily within priority sampling areas, with the goal of documenting at least 90% of the species present; 2) document (through collection or museum specimen and literature review) one voucher specimen for each species identified; 3) provide a GIS-referenced list of sensitive species that are federally or state listed, rare, or worthy of special consideration that occur within priority sampling locations; 4) describe park-wide distribution of federally- or state-listed, rare, or special concern species; 5) enter all species data into the National Park Service NPSpecies database; and 6) provide all deliverables as outlined in the Mojave Network Biological Inventory Study Plan. Methods included daytime and nighttime visual encounter surveys, road driving, and pitfall trapping. Survey effort was concentrated in predetermined priority sampling areas, as well as in areas with a high potential for detecting undocumented species.
    [Show full text]
  • Geology of the Ash Meadows Quadrangle Nevada-California
    Geology of the Ash Meadows Quadrangle Nevada-California By CHARLES S. DENNY and HARALD DREWES CONTRIBUTIONS TO GENERAL GEOLOGY GEOLOGICAL SURVEY BULLETIN 1181-L The history of a desert basin and its bordering highlands UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library catalog card for this publication appears after page L56. For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract. ______________________________________________________ LI Introduction. ________--__-___-_________-_---------__-_________-__- 2 * Geography. _____________________._.__-_-___--___._________.--- 3 Stratigraphy. ______-__--_______-___-___-_-__-__-___-____________-- 6 Paleozoic rocks _--______________-__---_-_-_--_------_.____-- 6 Rocks of the Resting Spring Range.__-_--___-__-_____-____-_ 7 ** Quartzite of Shadow Mountain...-______________________ 7 Unidentified limestone and dolomite____-__..__.____..._. 7 Rocks of the Devils Hole area_____________________________ 7 Bonanza King Formation__________-_-_--___________-- 8 Nopah Formation.____________________________________ 8 Rocks of the Funeral Mountains.___-______--__-___-_-_____- 9 Hidden Valley Dolomite_____.-____--__-____--__..___- 9 » ' Lost Burro Formation________________________________ 10 Tin Mountain Limestone.______________________________ 10 Perdido (?) Formation....-.--------------.-.---..______
    [Show full text]
  • Dedicated to the Future of the Amargosa Watershed PO Box 63 Shoshone, CA 92384 760.852.4339
    PO Box 63 Shoshone, CA 92384 760.852.4339 www.amargosaconservancy.org February 23, 2015 California Energy Commission Dockets Office, MS-4 Docket No. 09-RENEW EO-01 1516 Ninth Street Sacramento, CA 95814-5512 [email protected] Re: National Conservation Lands and Special Recreation Management Areas in the Amargosa Watershed in the Draft DRECP Please accept these comments regarding potential additions to National Conservation Lands and Special Recreation Management Areas in the DRECP. The Amargosa Watershed is a series of interconnected basins which all drain into the Amargosa River. The Amargosa River is one of only two perennial rivers in the Mojave Desert, and one of the only free flowing desert rivers in the US southwest. 26 miles of the river are protected as a congressionally designated Wild & Scenic River. The 150 mile bi-state river and its spring and stream tributaries support a truly unique and rich riparian and aquatic natural community. The Amargosa Basin contains one of the two largest assemblages of listed, endemic and rare species in North America—desert fish, rare plants, mammals, and birds—that are wholly dependent on perennial sources of water. Perennial surface water is located in isolated small oases, streams, springs, and in very limited stretches of the Amargosa River. Except during occasional intense rainstorms, the perennial flow in the Wild and Scenic section of the Amargosa River is completely supplied by groundwater. Several significant springs emerge along the river corridor between Shoshone and the Amargosa River Canyon south of Tecopa that contribute to the flow of the Amargosa River.
    [Show full text]
  • Geology of the Funeral Peak Quadrangle, California, on the East Flank of Death Valley
    Geology of the Funeral Peak Quadrangle, California, on the East Flank of Death Valley GEOLOGICAL SURVEY PROFESSIONAL PAPER 413 Geology of the Funeral Peak Quadrangle, California, on the East Flank of Death Valley By HARALD DREWES GEOLOGICAL SURVEY PROFESSIONAL PAPER 413 A description of the structural development of part of a large block including contributions on megabrecciaS) turtlebacks^ and chaotic structure overlying the Amargosa thrust fault UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1963 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. CONTENTS Page Page Abstract_--_--__----_________________________ 1 Tertiary volcanic and sedimentary rocks Continued Introduction --------_-_-______________-______._ 2 Copper Canyon formation Continued Location_ ---------_-____________-________ 2 Fauna__ _ __________________________________ 35 Objectives and methods_-_-_______..________ 2 Age and correlation_________________________ 36 Acknowledgments_ _----_---_______..______ 3 Origin and environment.____________________ 36 General geographic features._________________ 3 Greenwater volcanics-__--_____-_---_----------__ 37 General geologic features- _ ---__-___--_______ 4 General description___-__-________-_-____--_ 37 Precambrian rocks._-----_--_-__________________ 5 Vitrophyre member.________________________ 38 Metasedimentary rocks______________________ 5 Petrology-_________________________________ 41 General description _____________________ 5 Tuff-breccia member____________-______-____ 42 Petrography ___________________________ 6 Age and correlation-__-_---_________-_--_--_ 42 Origin and age _________________________ 7 Origin and environment_______-__----_-___-_ 42 Metadiorite_ _--------__-___________________ 7 Tertiary andesite and basalt-____________________ 42 General description. ____________________ 7 General description.
    [Show full text]
  • Cal Poly Geology Club Death Valley Field Trip – 2004
    Cal Poly Geology Club Death Valley Field Trip – 2004 Guidebook by Don Tarman & Dave Jessey Field Trip Organizers Danielle Wall & Leianna Michalka DEATH VALLEY Introduction Spring 2004 Discussion and Trip Log Welcome to Death Valley and environs. During the next two days we will drive through the southern half of Death Valley and see some of the most spectacular geology and scenery in the United States. A detailed road log with mileages follows this short introductory section. We hope to keep the pace leisurely so that everyone can see as much as possible and have an opportunity to ask questions and enjoy the natural beauty of the region. IMPORTANT: WATER- carry and drink plenty. FUEL- have full tank upon leaving Stovepipe Wells or Furnace Creek (total driving distance approx. 150 miles). Participants must provide for their own breakfasts Saturday morning. Lunches will be prepared at the Stovepipe Wells campground before departing. We will make a brief stop at Furnace Creek visitor’s center and for fuel etc. Meeting Points Saturday morning meet in front at the Chevron station on the north side of the highway a short distance east of the campground (8:30 AM) Sunday morning (tentative- depending upon what our last stop is Saturday) meet at the Charles Brown highway intersection with 127 just at the south side of Shoshone. (8:30 AM). Get fuel before meeting. As you know we will be camping Saturday night between the hamlets of Shoshone and Tecopa. If for some reason you become separated from the main caravan during our journey Saturday – and this would be very difficult to accomplish- simply head for Shoshone/Tecopa.
    [Show full text]