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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) . -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
The Tectonic Evolution of the Madrean Archipelago and Its Impact on the Geoecology of the Sky Islands
The Tectonic Evolution of the Madrean Archipelago and Its Impact on the Geoecology of the Sky Islands David Coblentz Earth and Environmental Sciences Division, Los Alamos National Laboratory, Los Alamos, NM Abstract—While the unique geographic location of the Sky Islands is well recognized as a primary factor for the elevated biodiversity of the region, its unique tectonic history is often overlooked. The mixing of tectonic environments is an important supplement to the mixing of flora and faunal regimes in contributing to the biodiversity of the Madrean Archipelago. The Sky Islands region is located near the actively deforming plate margin of the Western United States that has seen active and diverse tectonics spanning more than 300 million years, many aspects of which are preserved in the present-day geology. This tectonic history has played a fundamental role in the development and nature of the topography, bedrock geology, and soil distribution through the region that in turn are important factors for understanding the biodiversity. Consideration of the geologic and tectonic history of the Sky Islands also provides important insights into the “deep time” factors contributing to present-day biodiversity that fall outside the normal realm of human perception. in the North American Cordillera between the Sierra Madre Introduction Occidental and the Colorado Plateau – Southern Rocky The “Sky Island” region of the Madrean Archipelago (lo- Mountains (figure 1). This part of the Cordillera has been cre- cated between the northern Sierra Madre Occidental in Mexico ated by the interactions between the Pacific, North American, and the Colorado Plateau/Rocky Mountains in the Southwest- Farallon (now entirely subducted under North America) and ern United States) is an area of exceptional biodiversity and has Juan de Fuca plates and is rich in geology features, including become an important study area for geoecology, biology, and major plateaus (The Colorado Plateau), large elevated areas conservation management. -
G17 Laramide and Sevier Orogenies
PLATE TECTONICS 423 g17 Laramide and Sevier orogenies < cratonal uplifts, thin-skinned thrust tectonics > ... mountains were thought of ... as punishments dealt to Earth by a Creator disappointed at the misbehavior of its inhabitants. This “catastrophist” view affected ... 18th and early 19th centuries, well-born ladies making the Grand Tour in Europe would pull down their window shades to avoid viewing the Alps. —Donald Kennedy.1 The fold-thrust belt of the northern Rocky Mountains is a back-arc east of the Cascade volcanic- mountains and sediment-filled trench of the eastward subducting Juan da Fuca oceanic plate. The central Rocky Mountains is earthquake-active. Its scenery is of a maturely dissected broad-uparch that in erosional section and by exhumation exposes features of the once Laramide mountain chain. The Wyoming Basin and southern Rocky Mountains is a region of reactivated Laramide cratonal uplifts. To the west of the southern Rocky Mountains and Colorado Plateau is the Basin and Range physiographic province. Its graben and horst scenery results from ongoing extension that has doubled the width of the region since the middle Cenozoic. Created are large displacements on listric faults that at their surfacing ends are imbricate normal faulted. This mimics in reverse the geometry produced by a former compressive orogeny called the Sevier.2 Laramide orogeny (Paleocene climax, near the end of the Cretaceous inception.) Laramide refers to ore-producing intrusions (as Boulder batholith, Montana), eastward-shed foreland- basin sediments as the E-K boundary containing undeformed Arapahoe Conglomerate fm and the folded Cretaceous Mesa Verde fm, Colorado.3 These strata are disconformable on Late Cretaceous Interior Seaway Laramic fm that is nonconformable on a Precambrian basement complex Laramide folds and faults resulted from block faulting and thrust faulting of this underlying craton. -
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 ..................................................... -
The Geology of Quail Creek State Park Itself, the Park Is Surrounded by a Landscape of Enormous Geological and Human Interest
TT HH EE G E O L OO GG Y OO FF Q UU AA II LL C R E E K SS T A TT EE PP A R K T H E G E O L O G Y O F Q U A I L C R E E K S T A T E P A R K T H E GEOLO G Y O F Q UA IL CREEK STAT E PA R K by Robert F. Biek Introduction . 1 Layers of Rock. 3 Regional overview . 3 Moenkopi Formation . 4 Shnabkaib Member . 6 Upper red member . 7 Chinle Formation . 7 Shinarump Conglomerate Member . 7 Petrified Forest Member . 8 Surficial deposits . 9 Talus deposits . 9 Mixed river and slopewash deposits . 9 Landslides. 9 The Big Picture . 10 Geological Highlights . .14 Virgin anticline . .14 Faults . .14 Gypsum . .14 “Picture stone” . .15 Boulders from the Pine Valley Mountains . .16 Catastrophic failure of the Quail Creek south dike . .17 Acknowledgments . .19 References . .19 T H E G E O L O G Y O F Q U A I L C R E E K S T A T E P A R K I N T R O D U C T I O N The first thing most visitors to Quail Creek State Park notice, apart from the improbably blue and refreshing waters of the reservoir itself, are the brightly colored, layered rocks of the surrounding cliffs. In fact, Quail Creek State Park lies astride one of the most remarkable geologic features in southwest- ern Utah. The park lies cradled in the eroded core of the Virgin anticline, a long upwarp of folded rock that trends northeast through south-central Washington County. -
Earliest Jurassic U-Pb Ages from Carbonate Deposits in the Navajo Sandstone, Southeastern Utah, USA Judith Totman Parrish1*, E
https://doi.org/10.1130/G46338.1 Manuscript received 3 April 2019 Revised manuscript received 10 July 2019 Manuscript accepted 11 August 2019 © 2019 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Published online 4 September 2019 Earliest Jurassic U-Pb ages from carbonate deposits in the Navajo Sandstone, southeastern Utah, USA Judith Totman Parrish1*, E. Troy Rasbury2, Marjorie A. Chan3 and Stephen T. Hasiotis4 1 Department of Geological Sciences, University of Idaho, P.O. Box 443022, Moscow, Idaho 83844, USA 2 Department of Geosciences, Stony Brook University, Stony Brook, New York 11794, USA 3 Department of Geology and Geophysics, University of Utah, 115 S 1460 E, Room 383, Salt Lake City, Utah 84112-0102, USA 4 Department of Geology, University of Kansas, 115 Lindley Hall, 1475 Jayhawk Boulevard, Lawrence, Kansas 66045-7594, USA ABSTRACT with the lower part of the Navajo Sandstone New uranium-lead (U-Pb) analyses of carbonate deposits in the Navajo Sandstone in across a broad region from southwestern Utah southeastern Utah (USA) yielded dates of 200.5 ± 1.5 Ma (earliest Jurassic, Hettangian Age) to northeastern Arizona (Blakey, 1989; Hassan and 195.0 ± 7.7 Ma (Early Jurassic, Sinemurian Age). These radioisotopic ages—the first re- et al., 2018). The Glen Canyon Group is under- ported from the Navajo erg and the oldest ages reported for this formation—are critical for lain by the Upper Triassic Chinle Formation, understanding Colorado Plateau stratigraphy because they demonstrate that initial Navajo which includes the Black Ledge sandstone (e.g., Sandstone deposition began just after the Triassic and that the base of the unit is strongly Blakey, 2008; Fig. -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on January 26, 2010 Geological Society of America Bulletin Sevier Orogenic Belt in Nevada and Utah RICHARD LEE ARMSTRONG Geological Society of America Bulletin 1968;79;429-458 doi: 10.1130/0016-7606(1968)79[429:SOBINA]2.0.CO;2 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes Copyright © 1968, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. -
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, -
An Inventory of Trilobites from National Park Service Areas
Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 179 AN INVENTORY OF TRILOBITES FROM NATIONAL PARK SERVICE AREAS MEGAN R. NORR¹, VINCENT L. SANTUCCI1 and JUSTIN S. TWEET2 1National Park Service. 1201 Eye Street NW, Washington, D.C. 20005; -email: [email protected]; 2Tweet Paleo-Consulting. 9149 79th St. S. Cottage Grove. MN 55016; Abstract—Trilobites represent an extinct group of Paleozoic marine invertebrate fossils that have great scientific interest and public appeal. Trilobites exhibit wide taxonomic diversity and are contained within nine orders of the Class Trilobita. A wealth of scientific literature exists regarding trilobites, their morphology, biostratigraphy, indicators of paleoenvironments, behavior, and other research themes. An inventory of National Park Service areas reveals that fossilized remains of trilobites are documented from within at least 33 NPS units, including Death Valley National Park, Grand Canyon National Park, Yellowstone National Park, and Yukon-Charley Rivers National Preserve. More than 120 trilobite hototype specimens are known from National Park Service areas. INTRODUCTION Of the 262 National Park Service areas identified with paleontological resources, 33 of those units have documented trilobite fossils (Fig. 1). More than 120 holotype specimens of trilobites have been found within National Park Service (NPS) units. Once thriving during the Paleozoic Era (between ~520 and 250 million years ago) and becoming extinct at the end of the Permian Period, trilobites were prone to fossilization due to their hard exoskeletons and the sedimentary marine environments they inhabited. While parks such as Death Valley National Park and Yukon-Charley Rivers National Preserve have reported a great abundance of fossilized trilobites, many other national parks also contain a diverse trilobite fauna. -
Regional Stratigraphy of Oligocene and Lower Miocene Strata in the Yucca Mountain Region
* *0Ad REGIONAL STRATIGRAPHY OF OLIGOCENE AND LOWER MIOCENE STRATA IN THE YUCCA MOUNTAIN REGION Prepared for U.S. Nuclear Regulatory Commission Contract NRC-02-97-009 Prepared by Danielle A. Murray John A. Stamatakos Kenneth D. Ridgway Center for Nuclear Waste Regulatory Analyses San Antonio, Texas July 2002 CONTENTS Section Page FIGURES ............... ................ TABLES ................ ................ .vii ACKNOWLEDGMENTS .... ................ ..... ix EXECUTIVE SUMMARY .... ................ ..... xi 1 INTRODUCTION ...... ................ .... 1-1 1.1 Purpose........ ................ .... 1-1 1.2 Scope ......... ................ .... 1-2 2 GEOLOGIC SETTING .. 2-1 OLIGOCENE AND LOWER MIOCENE STRATIGRAPHY ..... 3-1 ...... 3 . 3.1 Outcrop Stratigraphy ............................ 3-1 ...... 3.1.1 Funeral Mountains ....................... ...... 3.1.2 Nevada Test Site ........................ 3-7 ...... 3.1.3 Oligocene and Lower Miocene Lithostratigraphy . ..... 3.2 Subsurface Stratigraphy ......................... 3-12 ..... 3.2.1 Nye County Well NC-EWDP-1 DX ........... 3-13 ..... 3.2.2 Nye County Well NC-EWDP-2DB ........... 3-15 ..... 3.2.3 Nye County Well NC-EWDP-3D ............ ..... 3.3 Correlation of Well Stratigraphy to Outcrop Exposures . ..... 3.3.1 Nye County Well NC-EWDP-2DB ........... ..... 3.3.2 Nye County Well NC-EWDP-1 DX ........... ..... 3.3.3 Nye County Well NC-EWDP-3D ............ ..... 4 CROSS SECTIONS ......................................... ........... 4.1 Regional Cross Section ................................ -
Thesis-Reproduction (Electronic)
A synopsis of the geologic and structural history of the Randsburg Mining District Item Type text; Thesis-Reproduction (electronic) Authors Morehouse, Jeffrey Allen, 1953-1985 Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 27/09/2021 08:53:56 Link to Item http://hdl.handle.net/10150/558085 Call No. BINDING INSTRUCTIONS INTERUBRARY INSTRUCTIONS Dept. E9791 Author: Morehouse, J. 1988 245 Title: RUSH___________________ PERMABIND____________ PAMPHLET._____________ GIFT____________________ COLOR: M,S* POCKET FOR MAP______ COVERS Front_______Both Special Instructions - Bindery or Repair REFERENCE____ i________ O th er--------------------------- 3 /2 /9 0 A SYNOPSIS OF THE GEOLOGIC AND STRUCTURAL HISTORY OF THE RANDSBURG MINING DISTRICT by Jeffrey Allen Morehouse A Thesis Submitted to the Faculty of the DEPARTMENT OF GEOSCIENCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE In the Graduate College THE UNIVERSITY OF ARIZONA 19 8 8 THE UNIVERSITY OF ARIZONA TUCSON, ARIZONA 85721 DEPARTMENT OF GEOSCIENCES BUILDING *77 GOULD-SIMPSON BUILDING TEL (602) 621-6024 To the reader of Jeff Morehouse's thesis: Jeff Morehouse's life was lamentably cut short by a hiking-rock climbing accident in the Santa Catalina Mountains near Tucson, Arizona, on March 24, 1985. Those who knew Jeff will always regret that accident, not only because it abbreviated what would certainly have been an uncommonly productive geological career but also because it snuffed an effervescent, optimistic,, charming personality.