Determining the Motion and Location of the Frenchman Mountain Fault, Las Vegas, Nevada: a Paired Basin Analysis and Structural Analysis
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GSA ROCKY MOUNTAIN/CORDILLERAN JOINT SECTION MEETING 15–17 May Double Tree by Hilton Hotel and Conference Center, Flagstaff, Arizona, USA
Volume 50, Number 5 GSA ROCKY MOUNTAIN/CORDILLERAN JOINT SECTION MEETING 15–17 May Double Tree by Hilton Hotel and Conference Center, Flagstaff, Arizona, USA www.geosociety.org/rm-mtg Sunset Crater is a cinder cone located north of Flagstaff, Arizona, USA. Program 05-RM-cvr.indd 1 2/27/2018 4:17:06 PM Program Joint Meeting Rocky Mountain Section, 70th Meeting Cordilleran Section, 114th Meeting Flagstaff, Arizona, USA 15–17 May 2018 2018 Meeting Committee General Chair . Paul Umhoefer Rocky Mountain Co-Chair . Dennis Newell Technical Program Co-Chairs . Nancy Riggs, Ryan Crow, David Elliott Field Trip Co-Chairs . Mike Smith, Steven Semken Short Courses, Student Volunteer . Lisa Skinner Exhibits, Sponsorship . Stephen Reynolds GSA Rocky Mountain Section Officers for 2018–2019 Chair . Janet Dewey Vice Chair . Kevin Mahan Past Chair . Amy Ellwein Secretary/Treasurer . Shannon Mahan GSA Cordilleran Section Officers for 2018–2019 Chair . Susan Cashman Vice Chair . Michael Wells Past Chair . Kathleen Surpless Secretary/Treasurer . Calvin Barnes Sponors We thank our sponsors below for their generous support. School of Earth and Space Exploration - Arizona State University College of Engineering, Forestry, and Natural Sciences University of Arizona Geosciences (Arizona LaserChron Laboratory - ALC, Arizona Radiogenic Helium Dating Lab - ARHDL) School of Earth Sciences & Environmental Sustainability - Northern Arizona University Arizona Geological Survey - sponsorship of the banquet Prof . Stephen J Reynolds, author of Exploring Geology, Exploring Earth Science, and Exploring Physical Geography - sponsorship of the banquet NOTICE By registering for this meeting, you have acknowledged that you have read and will comply with the GSA Code of Conduct for Events (full code of conduct listed on page 31) . -
Assembly Committee on Government Affairs-April 4
MINUTES OF THE MEETING OF THE ASSEMBLY COMMITTEE ON GOVERNMENT AFFAIRS Seventy-Ninth Session April 4, 2017 The Committee on Government Affairs was called to order by Chairman Edgar Flores at 8:13 a.m. on Tuesday, April 4, 2017, in Room 3143 of the Legislative Building, 401 South Carson Street, Carson City, Nevada. The meeting was videoconferenced to Room 4404B of the Grant Sawyer State Office Building, 555 East Washington Avenue, Las Vegas, Nevada. Copies of the minutes, including the Agenda (Exhibit A), the Attendance Roster (Exhibit B), and other substantive exhibits, are available and on file in the Research Library of the Legislative Counsel Bureau and on the Nevada Legislature's website at www.leg.state.nv.us/App/NELIS/REL/79th2017. COMMITTEE MEMBERS PRESENT: Assemblyman Edgar Flores, Chairman Assemblywoman Dina Neal, Vice Chairwoman Assemblywoman Shannon Bilbray-Axelrod Assemblyman Chris Brooks Assemblyman Richard Carrillo Assemblyman Skip Daly Assemblyman John Ellison Assemblywoman Amber Joiner Assemblyman Al Kramer Assemblyman Jim Marchant Assemblyman Richard McArthur Assemblyman William McCurdy II Assemblywoman Daniele Monroe-Moreno Assemblywoman Melissa Woodbury COMMITTEE MEMBERS ABSENT: None GUEST LEGISLATORS PRESENT: Assemblywoman Lesley E. Cohen, Assembly District No. 29 Assemblyman Elliot T. Anderson, Assembly District No. 15 Assemblyman James Ohrenschall, Assembly District No. 12 Minutes ID: 655 *CM655* Assembly Committee on Government Affairs April 4, 2017 Page 2 STAFF MEMBERS PRESENT: Jered McDonald, Committee Policy -
Sunrise Mountain Landfill 1999 Administrative Record
SFUND RECORDS CTR 2095573 - FINAL - REGULATORY COMPLIANCE AUDIT REPORT Sunrise Mountain Landfill Las Vegas, Nevada ASI Project Manager C_)JamesD. ShsMer 002541 PREFACE Regulatory Compliance Audits A regulatory compliance audit of a solid waste landfill consists of an examination based on the requirements of Federal regulations 40 CFR Parts 241 and 257, proposed Federal regulations 40 CFR Part 258. and existing State regulations. Conduct of a regulatory compliance audit includes a review of landfill case file records, supporting documents, and landfill operating practices; interviews with individuals familiar with the operation of the landfill; identification of site conditions; a visual inspection of the facility; and a determination of whether or not hazardous wastes have been or are being disposed of in excess of amounts normally found in household wastes. 0025*2 TABLE OF CONTENTS Section Page PREFACE II TABLE OF CONTENTS Ill LIST OF TABLES v LIST OF FIGURES v EXECUTIVE SUMMARY vl 1.0 INTRODUCTION 1 1.1 Program Purpose, Scope, and Objectives 1 1.2 Pre-lnspection Activities 3 1.3 On-Site Audit Activities 4 1.4 Post-Inspection Activities 5 2.0 FACILITY ENVIRONMENTAL PROFILE 6 2.1 Facility Description 6 2.1.1 Facility Location 6 2.1.2 Environmental Information 7 2.1.2.1 Topography 7 2.1.2.2 Land Use 7 2.1.2.3 Climate 9 2.1.2.4 Biological Features 9 2.1.2.5 Surface Water 10 2.1.2.6 Geology 10 2.2 Facility History 16 2.2.1 History of Owners, Lessees, and Operators 16 2.2.2 History of Site Operations 17 2.2.3 Regulatory History 19 in 002543 -
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. -
Program Book
ACE 101: Bridging Fundamentals and Innovation In conjunction with: PROGRAM BOOK Download the AAPG Events App! Sign Up for EXPLORER Digital Program Book Sponsored by: and Save 10% Today at the AAPG Center/Bookstore. explorer.aapg.org/register1 2 TABLE OF CONTENTS General Information Technical Program Business Center ........................................................................... 10 Theme Chairs ............................................................................... 41 ACE Service Center ....................................................................... 10 Oral Sessions at a Glance .............................................................. 42 Wi-Fi Hot Spot .............................................................................. 10 Poster Sessions at a Glance .......................................................... 44 Luggage Check ............................................................................. 10 Technical Program Sunday ............................................................ 47 Electronic Capturing ..................................................................... 10 Technical Program Monday ........................................................... 47 Lost and Found ............................................................................. 10 Technical Program Tuesday ........................................................... 59 No Smoking .................................................................................. 10 Technical Program Wednesday ..................................................... -
PDF Linkchapter
Index (Italic page numbers indicate major references) Abalone Cove landslide, California, Badger Spring, Nevada, 92, 94 Black Dyke Formation, Nevada, 69, 179, 180, 181, 183 Badwater turtleback, California, 128, 70, 71 abatement districts, California, 180 132 Black Mountain Basalt, California, Abrigo Limestone, Arizona, 34 Bailey ash, California, 221, 223 135 Acropora, 7 Baked Mountain, Alaska, 430 Black Mountains, California, 121, Adams Argillite, Alaska, 459, 462 Baker’s Beach, California, 267, 268 122, 127, 128, 129 Adobe Range, Nevada, 91 Bald Peter, Oregon, 311 Black Point, California, 165 Adobe Valley, California, 163 Balloon thrust fault, Nevada, 71, 72 Black Prince Limestone, Arizona, 33 Airport Lake, California, 143 Banning fault, California, 191 Black Rapids Glacier, Alaska, 451, Alabama Hills, California, 152, 154 Barrett Canyon, California, 202 454, 455 Alaska Range, Alaska, 442, 444, 445, Barrier, The, British Columbia, 403, Blackhawk Canyon, California, 109, 449, 451 405 111 Aldwell Formation, Washington, 380 Basin and Range Province, 29, 43, Blackhawk landslide, California, 109 algae 48, 51, 53, 73, 75, 77, 83, 121, Blackrock Point, Oregon, 295 Oahu, 6, 7, 8, 10 163 block slide, California, 201 Owens Lake, California, 150 Basin Range fault, California, 236 Blue Lake, Oregon, 329 Searles Valley, California, 142 Beacon Rock, Oregon, 324 Blue Mountains, Oregon, 318 Tatonduk River, Alaska, 459 Bear Meadow, Washington, 336 Blue Mountain unit, Washington, 380 Algodones dunes, California, 101 Bear Mountain fault zone, California, -
Western Earth Surface Processes
U.S. DEPARTMENT OF THE INTERIOR Prepared in cooperation with the OPEN-FILE REPORT 2007-1010 U.S. GEOLOGICAL SURVEY U.S. NATIONAL PARK SERVICE PLATE 3 OF 3 LIST OF MAP UNITS EXPLANATION [Detailed descriptions of map units are in the accompanying pamphlet] Contact Dashed where approximately located, dotted where concealed Strike and dip of bedding SURFICIAL DEPOSITS Horse Spring Formation (middle and lower Miocene and upper Oligocene) MESOZOIC AND PALEOZOIC ROCKS o15 Inclined af Artifical fill and other land disturbances (Holocene) Thu Horse Spring Formation, undivided(middle and lower Miocene and upper Oligocene) Kmg Muscovite granite at Walker Wash (Upper Cretaceous) v Vertical Qa Young alluvium (Holocene) Thl Lovell Wash Member, limestone and sandstone facies (middle Miocene) 22 Foreland basin deposits s Overturned Qct Colluvium and talus (Holocene to Pleistocene) Thlb Lovell Wash Member, interbedded basalt flows and vents (middle Miocene) Baseline Sandstone (Upper? to Lower Cretaceous) Horizontal e Qe Eolian deposits (Holocene to Pleistocene) Thbl Bitter Ridge Limestone and Lovell Wash Members, undivided (middle Miocene) Kbo Overton Conglomerate Member (Upper? to Lower Cretaceous) Igneous foliation Qp Playa deposits (Holocene to Pleistocene) 18 Thblv Bitter Ridge Limestone and Lovell Wash Members, undivided, with intercalated dacite and basalt flows (middle Miocene) Kbr Red sandstone member (Upper? to Lower Cretaceous) ¦ Inclined Q1a Intermediate-age sidestream alluvium (upper to middle Pleistocene) Thb Bitter Ridge Limestone Member -
Importance of Groundwater in Propagating
CRevolution 2: Origin and Evolution of the Colorado River System II themed issue Crossey et al. Importance of groundwater in propagating downward integration of the 6–5 Ma Colorado River system: Geochemistry of springs, travertines, and lacustrine carbonates of the Grand Canyon region over the past 12 Ma L.C. Crossey1, K.E. Karlstrom1, R. Dorsey2, J. Pearce3, E. Wan4, L.S. Beard5, Y. Asmerom1, V. Polyak1, R.S. Crow1, A. Cohen6, J. Bright6, and M.E. Pecha6 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico, 87131, USA 2Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403-1272, USA 3U.S. Forest Service, Grand Mesa, Uncompahgre and Gunnison National Forests, Paonia Ranger District, 403 North Rio Grande Avenue, P.O. Box 1030, Paonia, Colorado 81428, USA 4U.S. Geological Survey, 345 Middlefield Road, MS977, Menlo Park, California 94025, USA 5U.S. Geological Survey, 2255 North Gemini Drive, Flagstaff, Arizona 86001, USA 6Department of Geosciences, The University of Arizona, 1040 East 4th Street, Tucson, Arizona 85721, USA ABSTRACT travertines, suggesting a long-lived spring- basins. Bouse carbonates display a southward fed lake/marsh system sourced from western trend toward less radiogenic 87Sr/86Sr values, We applied multiple geochemical tracers Colorado Plateau groundwater. Progressive higher [Sr], and heavier d18O that we attribute (87Sr/86Sr, [Sr], d13C, and d18O) to waters and up-section decrease in 87Sr/86Sr and d13C and to an increased proportion of Colorado River carbonates of the lower Colorado River sys- increase in d18O in the uppermost 50 m of the water through time plus increased evapora- tem to evaluate its paleohydrology over the Hualapai Limestone indicate an increase in tion from north to south. -
Rocks at the GBSSRL Reception Counter
Rocks at the Reception Counter of the Great Basin Science Sample and Records Library All the rocks in the wooden core boxes on the front of the reception counter are from Nevada. They include some geologically and historically significant rocks: the Nevada State Rock (sandstone), one of the oldest rocks in Nevada (2.5-billion-year-old gneiss from Angel Lake), rocks from the “Great Unconformity” separating Precambrian gneiss and Cambrian sandstone (from Frenchman Mountain, where rocks like those at the base of the Grand Canyon are exposed), ore from the Comstock Lode at Virginia City (important in statehood, our nickname, the Silver State, and the motto “Battle Born”), rock from the top of Slide Mountain (which, as measured by high-precision global positioning system instruments, moved up and to the northeast in 2003 in response to probable magma injection at the north end of Lake Tahoe), and some of the youngest rocks in Nevada (caliche from Las Vegas Valley and ferricrete from Geiger Grade). These rocks have been cut to simulate diamond drill core. The Great Basin Science Sample and Records Library houses many boxes of core and cuttings from various mineral, oil, geothermal, and water exploration holes drilled in the State. Slabs of a few different background rocks provide contrast with the Nevada- shaped pieces. The countertop itself is polished Juparana Columbo "granite," which is actually, by geological definitions, a gneiss; it comes from India and looks somewhat like 1.7-billion-year-old gneiss from southern Nevada. Except where noted, the samples were collected by Jon Price, State Geologist and Director of the Nevada Bureau of Mines and Geology. -
Chapter 3 Affected Environment
Las Vegas Disposal Boundary Chapter 3 Chapter 3 Affected Environment Final EIS December 2004 Las Vegas Disposal Boundary Chapter 3 THIS PAGE INTENTIONALLY LEFT BLANK Final EIS December 2004 Las Vegas Disposal Boundary Chapter 3 CHAPTER 3 AFFECTED ENVIRONMENT The affected environment is the baseline from BLM lands within the disposal boundary area. which to identify and evaluate environmental The purpose of the surveys was to identify the changes resulting from the proposed action and presence of sensitive environmental resources and alternatives. This chapter focuses on the human to locate potential hazardous materials sites. Bio- environment that has the potential to be affected logical field surveys covered the desert tortoise by implementing the land sale and land use ac- and sensitive plant species including the Las Ve- tions. The human environment potentially af- gas bearpoppy, Las Vegas buckwheat, and pen- fected is interpreted comprehensively to include stemon. Surveys were also completed to locate the natural and physical resources and the rela- historic sites, archaeological sites, and paleon- tionship of people with those resources [40 Code tological resources, and to identify lands with po- of Federal Regulations (CFR) §1508.14]. The tential hazardous materials present. affected environment discussed in this chapter includes air quality, earth resources, water re- 3.1 AIR QUALITY sources, biological resources, cultural and histori- cal resources, Native American concerns, visual Air resources are characterized by the existing resources, land use, recreation and wilderness re- concentrations of various pollutants and the cli- sources, range resources, hazardous materials, matic and meteorological conditions that influ- social and economic conditions, and environ- ence the quality of the air. -
Kinematic Evolution of a Large-Offset Continental Normal Fault System, South Virgin Mountains, Nevada
Kinematic evolution of a large-offset continental normal fault system, South Virgin Mountains, Nevada Robert Brady* Brian Wernicke Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA Joan Fryxell Department of Geological Sciences, California State University, San Bernardino, California 92407, USA ABSTRACT examination of other areas suggests that the John and Foster, 1993); others may have ini- evolutionary sequence seen in the South tiated with steep dips and remained active as The South Virgin Mountains and Grand Virgin Mountains may, in fact, be widely they tilted to shallow dips. Tilting of these Wash trough comprise a mid-Miocene nor- applicable. faults is probably due to combined domino- mal fault system that de®nes the boundary style tilting and isostatically driven footwall between the unextended Colorado Plateau Keywords: Egan Range, kinematics, Lemi- ¯exure (Fig. 1C). Many gently dipping normal to the east and highly extended crust of the tar Mountains, normal faults, South Virgin faults might be best interpreted this way, rath- central Basin and Range province to the Mountains, Yerington. er than invoking rotation by younger struc- west. In the upper 3 km of the crust, the tures. system developed in subhorizontal cratonic INTRODUCTION Detailed geologic studies were conducted in strata in the foreland of the Cordilleran the South Virgin Mountains of southeastern fold and thrust system. The rugged topog- Geologic mapping in the Basin and Range Nevada and northwestern Arizona (Fig. 2), a raphy and lack of vegetation of the area af- province has shown that gently dipping nor- region well suited for testing existing kine- ford exceptional three-dimensional expo- mal faults are common (e.g., Longwell, 1945; matic models of normal faulting. -
Chapter 4 Affected Environment and Impacts of MSHCP and Alternatives
Clark County MSHCP/EIS 4. Affected Environment/Impacts of MSHCP & Alternatives Chapter 4 Affected Environment and Impacts of MSHCP and Alternatives 4.1 Setting Clark County is located in the southernmost tip of Nevada, as shown in Figure 4-1. It is bordered on the north by Lincoln County, Nevada; on the east by Mojave County, Arizona; on the southwest by San Bernardino and Inyo Counties, California; and on the west by Nye County, Nevada. It covers approximately 7,880 square miles, or about 7 percent of the state’s total area. It is Nevada’s most populated county, with an estimated 1997 population of 1,170,113, or about 67 percent of the state total (Clark County Department of Comprehensive Planning 1997). Elevations within Clark County range from 450 feet above mean sea level along the Colorado River to 11,918 feet at Charleston Peak (see Figure 4-1). Much of the county has features that are characteristic of the Great Basin, such as mountain ranges that extend in a north-south direction and erode laterally to long, narrow desert valleys. The mountain ranges are generally steep and composed primarily of bedrock. Wide alluvial fans or aprons extend from the base of the mountains and level out to basin lowlands. The basin lowlands have been continually filling since the mountains were originally formed and have a surface generally composed of fine sand, silt, and clay. The Las Vegas Valley extends in a northwest-southeast direction with the Spring Mountains to the west; the Pintwater, Desert, Sheep, and Las Vegas Mountains to the north; Frenchman Mountain to the east; and the Bird Spring and McCullough mountain ranges to the south.