USGS Scientific Investigations Map 3236, Pamphlet

Total Page:16

File Type:pdf, Size:1020Kb

USGS Scientific Investigations Map 3236, Pamphlet Geologic Map of the Topock 7.5´ Quadrangle, Arizona and California By Keith A. Howard, Barbara E. John, Jane E. Nielson, Julia M.G. Miller, and Joseph L. Wooden Pamphlet to accompany Scientific Investigations Map 3236 2013 U. S. Department of the Interior U. S. Geological Survey Front cover: View downstream into Topock Gorge (“Head of Mojave Cañon”) as pictured in the Report upon the Colorado River of the West (fig. 16 of Ives, 1861). Miocene rocks on the skyline dip steeply to the right (west) in hanging-wall blocks above the Chemehuevi Detachment Fault and Devils Elbow Fault. Contents Abstract............................................................................................................................................................................................ 1 Introduction ...................................................................................................................................................................................... 1 Acknowledgments........................................................................................................................................................................ 2 Geography ....................................................................................................................................................................................... 2 Historical Significance...................................................................................................................................................................... 4 Previous Geologic Investigations..................................................................................................................................................... 7 Tectonic Block Diagram ................................................................................................................................................................... 8 Proterozoic Rocks.......................................................................................................................................................................... 10 Mesozoic Intrusions ....................................................................................................................................................................... 11 Sub-Miocene Unconformity............................................................................................................................................................ 13 Miocene Rocks Related to Tectonic Extension.............................................................................................................................. 14 Lower Miocene Volcanic and Sedimentary Rocks..................................................................................................................... 14 Miocene Intrusions..................................................................................................................................................................... 15 Synextensional Sedimentary Rocks........................................................................................................................................... 17 Miocene Extensional Structure ...................................................................................................................................................... 19 Low-angle Normal Faults ........................................................................................................................................................... 19 Tilted Fault Blocks and the Transverse Gold Dome Fault Zone ................................................................................................ 20 Other Normal Faults................................................................................................................................................................... 22 Folds .......................................................................................................................................................................................... 22 Intrusion Shape and Dike Orientations ...................................................................................................................................... 23 Post-extension Deposits ................................................................................................................................................................ 23 Deposits Predating the Colorado River...................................................................................................................................... 23 Pliocene to Pre-Late Pleistocene Alluvium and Its Relation to Degradation and Aggradation of the Colorado River ............... 24 Late Pleistocene and Holocene Alluvium and Its Relations to Further Aggradations and Degradation of the Colorado River.. 27 Pliocene and Quaternary Deformation........................................................................................................................................... 30 Paleontology .................................................................................................................................................................................. 31 Mineralization and Mineral Exploration .......................................................................................................................................... 31 Geologic History............................................................................................................................................................................. 33 Description of Map Units................................................................................................................................................................ 36 Sedimentary and Volcanic Rocks and Deposits ........................................................................................................................ 36 Rocks Deposited During Extensional Deformation .................................................................................................................... 43 Intrusive and Metamorphic Rocks.............................................................................................................................................. 47 References Cited ........................................................................................................................................................................... 52 Figures Figure 1. Map showing geologic mapping responsibilities in the Topock quadrangle................................................................. 2 Figure 2. Map showing Topock quadrangle geology and major structures................................................................................. 3 Figure 3. Map showing some geographic features in the Topock quadrangle............................................................................ 5 Figure 4. View northeastward up Topock Gorge (Mojave Cañon) from near Devils Elbow ........................................................ 6 Figure 5. Photo showing part of the Mystic Maze (Topock Maze)............................................................................................... 7 Figure 6. Map showing the Topock quadrangle in relation to adjacent geologic map areas and the Colorado River extensional corridor. ................................................................................................................................................... 8 iii Figure 7. A. Interpretive tectonic map of the Topock quadrangle. B. Interpretive tectonic block diagram.................................. 9 Figure 8. Contoured orientation data (poles, lower hemisphere equal-area projection) for areas in the Topock quadrangle... 10 Figure 9. Photo showing view west into the Chemehuevi Mountains in the southwest part of the Topock quadrangle............ 12 Figure 10. A reconstructed pre-extension cross-sectional shape of the Chemehuevi Mountains Plutonic Suite ...................... 13 Figure 11. Conceptual diagram showing stratigraphic relations among Cenozoic sedimentary and volcanic units.................. 14 Figure 12. Photo showing steeply dipping Miocene rocks of the sandstone and conglomerate unit (Ts, here including unlabeled basalt interlayers) in the Gold Dome Mine and The Needles area overlying flows of the lower volcanic sequence (Tv)............................................................................................................................................ 15 Figure 13. A. Photo showing cliff-forming rocks of the Needle Mountain intrusion (Ti) that rise above less resistant rocks of the lower volcanic sequence (Tv) in the foreground. B. Detailed map of the Needle Mountain intrusion (Ti) ............................................................................................ 18 Figure 14. Photo showing bedded mud and sand of the Bouse Formation (Tb) and overlying older piedmont alluvium (QTa1) near Sacramento Wash in the northeast part of the quadrangle................................................................ 25 Figure 15. Photo showing fan dips in fluvial and related deposits of the facies of Santa Fe Railway (Pliocene) ...................... 26 Figure 16. Photo showing boulder conglomerate of Bat Cave Wash (Trbb) resting unconformably on red Miocene gneiss-clast conglomerate (Tcgn)..........................................................................................................................
Recommended publications
  • Wilderness Visitors and Recreation Impacts: Baseline Data Available for Twentieth Century Conditions
    United States Department of Agriculture Wilderness Visitors and Forest Service Recreation Impacts: Baseline Rocky Mountain Research Station Data Available for Twentieth General Technical Report RMRS-GTR-117 Century Conditions September 2003 David N. Cole Vita Wright Abstract __________________________________________ Cole, David N.; Wright, Vita. 2003. Wilderness visitors and recreation impacts: baseline data available for twentieth century conditions. Gen. Tech. Rep. RMRS-GTR-117. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 52 p. This report provides an assessment and compilation of recreation-related monitoring data sources across the National Wilderness Preservation System (NWPS). Telephone interviews with managers of all units of the NWPS and a literature search were conducted to locate studies that provide campsite impact data, trail impact data, and information about visitor characteristics. Of the 628 wildernesses that comprised the NWPS in January 2000, 51 percent had baseline campsite data, 9 percent had trail condition data and 24 percent had data on visitor characteristics. Wildernesses managed by the Forest Service and National Park Service were much more likely to have data than wildernesses managed by the Bureau of Land Management and Fish and Wildlife Service. Both unpublished data collected by the management agencies and data published in reports are included. Extensive appendices provide detailed information about available data for every study that we located. These have been organized by wilderness so that it is easy to locate all the information available for each wilderness in the NWPS. Keywords: campsite condition, monitoring, National Wilderness Preservation System, trail condition, visitor characteristics The Authors _______________________________________ David N.
    [Show full text]
  • Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona
    2.SOB nH in ntoiOGIGM. JAN 3 1 1989 Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona U.S. GEOLOGICAL SURVEY BULLETIN 1701-C Chapter C Mineral Resources of the Harquahala Mountains Wilderness Study Area, La Paz and Maricopa Counties, Arizona By ED DE WITT, S.M. RICHARD, J.R. HASSEMER, and W.F. HANNA U.S. Geological Survey J.R. THOMPSON U.S. Bureau of Mines U.S. GEOLOGICAL SURVEY BULLETIN 1701 MINERAL RESOURCES OF WILDERNESS STUDY AREAS- WEST-CENTRAL ARIZONA AND PART OF SAN BERNARDINO COUNTY, CALIFORNIA U. S. GEOLOGICAL SURVEY Dallas L Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publlcatlon Data Mineral resources of the Harquahala Mountains wilderness study area, La Paz and Maricopa counties, Arizona. (Mineral resources of wilderness study areas west-central Arizona and part of San Bernardino County, California ; ch. C) (U.S. Geological Survey bulletin ; 1701-C) Bibliography: p. Supt. of Docs, no.: I 19.3:1701-C 1. Mines and mineral resources Arizona Harquahala Mountains Wilderness. 2. Harquahala Mountains (Ariz.) I. DeWitt, Ed. II. Series. III. Series: U.S. Geological Survey bulletin ; 1701. QE75.B9 no. 1701-C 557.3 s [553'.09791'72] 88-600012 [TN24.A6] STUDIES RELATED TO WILDERNESS Bureau of Land Management Wilderness Study Areas The Federal Land Policy and Management Act (Public Law 94-579, October 21, 1976) requires the U.S. Geological Survey and the U.S.
    [Show full text]
  • Pamphlet SIM 3411: Geologic Map of the Castle Rock 7.5' Quadrangle
    Geologic Map of the Castle Rock 7.5’ Quadrangle, Arizona and California By P. Kyle House, Barbara E. John, Daniel V. Malmon, Debra Block, L. Sue Beard, Tracey J. Felger, Ryan S. Crow, Jonathan E. Schwing, and Colleen E. Cassidy Pamphlet to accompany Scientific Investigations Map 3411 Kayaker's view of Castle Rock (unit Tac) looking north-northeast from Castle Rock Bay, Arizona. The northern Mohave Mountains are visible in left background, and sediments of the Chemehuevi Formation (unit Qch) are seen along right edge of photo. Photograph taken August 27, 2014, by Kyle House, USGS. 2018 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior RYAN K. ZINKE, Secretary U.S. Geological Survey James F. Reilly II, Director U.S. Geological Survey, Reston, Virginia: 2018 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 https://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 https://store.usgs.gov. To order USGS information products, visit https://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: House, P.K., John, B.E., Malmon, D.V., Block, Debra, Beard, L.S., Felger, T.J., Crow, R.S., Schwing, J.E., and Cassidy, C.E., 2018, Geologic map of the Castle Rock 7.5’ quadrangle: U.S.
    [Show full text]
  • Chemehuevi Valley Special Recreation Management Area (SRMA)
    Chemehuevi Valley Special Recreation Management Area (SRMA) The Chemehuevi Valley Viewshed with the Turtle Mountains National Natural Landmark is directly west of the communities of Havasu Landing, California and Lake Havasu City, Arizona. The Turtle Mountains Natural Landmark is an excellent illustration of volcanic phenomena with superimposed sculpturing of mountain landforms. In combination, the eastern and western sections present some of the finest geological formations in the Mohave Desert. The site is of scenic value and interest; it also contains excellent examples of Mohave Desert flora and fauna. From October to April each year hundreds of travelers “snowbirds” from the northeastern United States, Canada and Europe journey to the area to enjoy the mild winter climate seeking new experiences, enjoying vast landscape which have not existed in European Nations for hundreds of years. Visitors participate in backcountry touring adventure and the discovery of new hiking trails, rock hounding sites and camping opportunities. The Chemehuevi Reservation Havasu Landing Resort depends on the naturalness of the Chemehuevi Valley to support the recreation pursuits of their visitors. The Needles Field Office has developed a system of designated trails entitled the Mojave Adventure Routes in regards to the 2002 Northern and Eastern Colorado Desert Coordinated Management Plan item 3.8.7. These routes are an outstanding network of 4x4 vehicle backcountry touring routes for motorized recreation. These routes were developed for the purpose of traveling to areas not often seen by many people. This network is a shared-use trail system providing recreation opportunities for all persons, including those who use street-legal and non-street legal (Green Sticker) vehicles, hikers, bicyclists, and equestrians.
    [Show full text]
  • People of Snowy Mountain, People of the River: a Multi-Agency Ethnographic Overview and Compendium Relating to Tribes Associated with Clark County, Nevada
    Portland State University PDXScholar Anthropology Faculty Publications and Presentations Anthropology 2012 People of Snowy Mountain, People of the River: A Multi-Agency Ethnographic Overview and Compendium Relating to Tribes Associated with Clark County, Nevada Douglas Deur Portland State University, [email protected] Deborah Confer University of Washington Follow this and additional works at: https://pdxscholar.library.pdx.edu/anth_fac Part of the Social and Cultural Anthropology Commons, and the Sustainability Commons Let us know how access to this document benefits ou.y Citation Details Deur, Douglas and Confer, Deborah, "People of Snowy Mountain, People of the River: A Multi-Agency Ethnographic Overview and Compendium Relating to Tribes Associated with Clark County, Nevada" (2012). Anthropology Faculty Publications and Presentations. 98. https://pdxscholar.library.pdx.edu/anth_fac/98 This Report is brought to you for free and open access. It has been accepted for inclusion in Anthropology Faculty Publications and Presentations by an authorized administrator of PDXScholar. Please contact us if we can make this document more accessible: [email protected]. Pacific West Region: Social Science Series National Park Service Publication Number 2012-01 U.S. Department of the Interior PEOPLE OF SNOWY MOUNTAIN, PEOPLE OF THE RIVER: A MULTI-AGENCY ETHNOGRAPHIC OVERVIEW AND COMPENDIUM RELATING TO TRIBES ASSOCIATED WITH CLARK COUNTY, NEVADA 2012 Douglas Deur, Ph.D. and Deborah Confer LAKE MEAD AND BLACK CANYON Doc Searls Photo, Courtesy Wikimedia Commons
    [Show full text]
  • November 17, 2017 David Beaver & Karen Summitt 8226 S Evergreen Dr Mohave Valley, AZ 86440 Re: Purchase and Sale Agreement F
    From: Karen Summitt To: Thomas Buschatzke; Sharon Scantlebury Subject: Fw: Objections to the MVIDD Water Transfer Date: Thursday, November 16, 2017 6:24:42 PM Attachments: ADWR Letter.docx November 17, 2017 David Beaver & Karen Summitt 8226 S Evergreen Dr Mohave Valley, AZ 86440 Re: Purchase and Sale Agreement for CAWCD to Acquire Water Rights and Land in Mohave Valley Irrigation and Drainage District, Mohave County, Arizona Dear Thomas Buschatzkle, I write to advise you that I am opposed to the proposed Central Arizona Water Conservation District (CAWCD) land and water purchase to move Colorado River water, prudently set aside for rural Arizona Colorado River mainstream users, to central Arizona for replenishment. As you may recall, the Mohave County Board of Supervisors passed two resolutions opposing the permanent transfer of any Colorado River Water Rights and Allocations to the Central Arizona Water Conservation District for use in the Central Arizona Groundwater Replenishment District – first as to the Quartzsite transfer and second as to the WPI-WAN transfer in the Mohave Valley Irrigation and Drainage District. Here is why I oppose this purchase and transfer of our water: First, as a matter of public policy, 4th Priority Colorado River water allocated to the users on the mainstream of the River, such as Mohave Valley Irrigation and Drainage District (“MVIDD”) in this case, should not be transferred away from mainstream of the River. This is part of the water that the State of Arizona requested be reserved for municipal and industrial uses along the River. Except for that small reservation of 4th Priority Colorado River water to the users on the mainstream, CAWCD received all of Arizona’s Colorado River entitlement remaining at the time that CAWCD and the United States entered into their initial agreement in 1972.
    [Show full text]
  • Groundwater Budgets for Detrital, Hualapai, and Sacramento Valleys, Mohave County, Arizona, 2007–08
    Prepared in cooperation with the Arizona Department of Water Resources Groundwater Budgets for Detrital, Hualapai, and Sacramento Valleys, Mohave County, Arizona, 2007–08 Scientific Investigations Report 2011–5159 U.S. Department of the Interior U.S. Geological Survey COVER: View of August 2010, monsoon thunderstorm over Hualapai Mountains, looking east from Sacramento Valley. Photo by Bradley D. Garner. Prepared in cooperation with the Arizona Department of Water Resources Groundwater Budgets for Detrital, Hualapai, and Sacramento Valleys, Mohave County, Arizona, 2007–08 By Bradley D. Garner and Margot Truini Scientific Investigations Report 2011–5159 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2011 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Suggested citation: Garner, B.D., and Truini, Margot, 2011, Groundwater budgets for Detrital, Hualapai, and Sacramento Valleys, Mohave County, Arizona, 2007–08: U.S. Geological Survey Scientific Investigations Report 2011-5159, 34 p.
    [Show full text]
  • Chemehuevi Valley Groundwater Basin Bulletin 118
    Hydrologic Region Colorado River California’s Groundwater Chemehuevi Valley Groundwater Basin Bulletin 118 Chemehuevi Valley Groundwater Basin • Groundwater Basin Number: 7-43 • County: San Bernardino • Surface Area: 273,000 acres (427 square miles) Basin Boundaries and Hydrology This basin underlies Chemehuevi Valley in eastern San Bernardino County. The basin is bounded by Havasu Lake on the east and by nonwater-bearing rocks of the Sacramento Mountains on the north, of the Chemehuevi Mountains on the northeast, of the Whipple Mountains on the southeast, of the Turtle Mountains on the west and south (Bishop 1963). The valley is drained by Chemehuevi Wash to Havasu Lake. Annual average precipitation ranges from about 4 to 6 inches. Hydrogeologic Information Water Bearing Formations Groundwater in the basin is found in alluvium and the Bouse Formation. Alluvium. Holocene age younger alluvium, which is found in washes and the floodplain of the Colorado River, is composed of sand, silt and gravel (Metzger and Loeltz 1973). Older alluvium consists of unconsolidated, fine- to coarse-grained sand, pebbles, and boulders with variable amounts of silt and clay. Bouse Formation. The Pliocene age Bouse Formation is composed of a basal limestone bed overlain by interbedded clay, silt, and sand. Thickness of the formation reaches 254 feet (Metzger and Loeltz 1973). The formation is underlain by locally derived fanglomerate and overlain by alluviums of the Colorado River and its tributaries. Restrictive Structures An unnamed fault crosses a portion of the southern side of the basin (Bishop 1963), but it is not known whether or not this fault impedes groundwater flow in the basin.
    [Show full text]
  • Creating Memorable Travel Experiences Since 1979 2021
    2021 DREAM BOOK LLC CREATING MEMORABLE TRAVEL EXPERIENCES SINCE 1979 One from the Road… When we returned to the road in August, one of our first trips was By the end of the tour, you feel like you just watched Ellen, Dr. Phil across Nevada to pick up the historic (which later and Saturday Night Live. You have truly met the locals once you Lincoln Highway SUCCESS STORIES—A SpECIAl AdvERTISIng SECTIOn became U.S. 50) and make our way back to Sacramento. Small finish walking among the headstones. towns proved to be a good way to gently try and return to traveling. Sure, we would all I didn’t know Wally would even be in town. Last I heard he was prefer not to have to wear a mask and wash buying a camper and heading out to see the world when he retired. our hands every 20 minutes. But if you love For reasons I’m hopeful I’ll hear about some day, he was back in to travel, right now you have to make a few Eureka. compromises. With any luck, those will be short term and we will be able to travel more It’s possible the folks on the trip may have noticed the tear in my eye freely soon. or the crack in my voice when my friend showed up to say hi. Or when he starting telling a couple members of our group about the Our trip went well. We slipped in and out of a cemetery tour and I broke out laughing really loud.
    [Show full text]
  • Scorpiones: Vaejovidae)
    New Species of Vaejovis from the Whetstone Mountains, Southern Arizona (Scorpiones: Vaejovidae) Richard F. Ayrey & Michael E. Soleglad January 2015 — No. 194 Euscorpius Occasional Publications in Scorpiology EDITOR: Victor Fet, Marshall University, ‘[email protected]’ ASSOCIATE EDITOR: Michael E. Soleglad, ‘[email protected]’ Euscorpius is the first research publication completely devoted to scorpions (Arachnida: Scorpiones). Euscorpius takes advantage of the rapidly evolving medium of quick online publication, at the same time maintaining high research standards for the burgeoning field of scorpion science (scorpiology). Euscorpius is an expedient and viable medium for the publication of serious papers in scorpiology, including (but not limited to): systematics, evolution, ecology, biogeography, and general biology of scorpions. Review papers, descriptions of new taxa, faunistic surveys, lists of museum collections, and book reviews are welcome. Derivatio Nominis The name Euscorpius Thorell, 1876 refers to the most common genus of scorpions in the Mediterranean region and southern Europe (family Euscorpiidae). Euscorpius is located at: http://www.science.marshall.edu/fet/Euscorpius (Marshall University, Huntington, West Virginia 25755-2510, USA) ICZN COMPLIANCE OF ELECTRONIC PUBLICATIONS: Electronic (“e-only”) publications are fully compliant with ICZN (International Code of Zoological Nomenclature) (i.e. for the purposes of new names and new nomenclatural acts) when properly archived and registered. All Euscorpius issues starting from No. 156 (2013) are archived in two electronic archives: Biotaxa, http://biotaxa.org/Euscorpius (ICZN-approved and ZooBank-enabled) Marshall Digital Scholar, http://mds.marshall.edu/euscorpius/. (This website also archives all Euscorpius issues previously published on CD-ROMs.) Between 2000 and 2013, ICZN did not accept online texts as "published work" (Article 9.8).
    [Show full text]
  • Family Adventures Easy Trips to Take with the Kids, 15 from a Scenic Drive in Sedona to a Pioneer Museum in Snowflake
    Perkinsville Road — No Yep. Bisbee’s Ballpark Is The Ferocious Nature Guardrails,THE STATE’SNo Problem BESTEven HORSEOlder Than TRAILS. Fenway ofGIDDYUP! the Cactus Wren w MAY 2009 ESCAPE. EXPLORE. EXPERIENCE family adventures Easy Trips to Take With the Kids, 15 From a Scenic Drive in Sedona to a Pioneer Museum in Snowflake Restaurants ARIZONA BY HELICOPTER: The Ultimate Way +to See the State CANOEING THE COLORADO HIKING THE MOGOLLON RIM contents 05.09 features Grand Canyon National Park 14 FAMILY ADVENTURES Williams Topock Gorge Clark Griswold wasn’t worried about finding the Grand Canyon. Jerome “It’s the biggest hole in the world,” he said in Family Vacation. Mogollon Rim Whether you’re loading up the “Family Truckster” for a trip to the world’s Seventh Natural Wonder, or just looking for a quick, PHOENIX economical family adventure all your own, Arizona has some- Tucson thing for every family. BY KELLY KRAMER Bisbee 20 WATER, WATER EVERYWHERE POINTS OF INTEREST IN THIS ISSUE Arizona isn’t exactly known for its water supply. Canyons and cactuses, yes; water, no. Well, like the Arizona Cardinals, who proved that a football team from the desert really could go to the Super Bowl, we’re using this month’s portfolio to prove that Arizona has some of the most spectacular watering holes in the world. BY GARY LADD 30 A BETTER VIEW The Grand Canyon is spectacular no matter where you’re departments standing — on the South Rim, along the river or on the roof of a Winnebago. Those vantage points, however, pale in compari- 2 EDITOR’S LETTER 3 CONTRIBUTORS 4 LETTERS TO THE EDITOR son to the views you’ll get from a Robinson R44 Raven II heli- 5 THE JOURNAL copter.
    [Show full text]
  • 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.
    [Show full text]