Stratigraphy of the Morrison and Related Formations, Colorado Plateau Region a Preliminary Report
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Morrison Formation 37 Cretaceous System 48 Cloverly Formation 48 Sykes Mountain Formation 51 Thermopolis Shale 55 Mowry Shale 56
THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING By CHRISTOPHER JAY CARSON Bachelor of Science Oklahoma State University 1998 Submitted to the Faculty of the Graduate College of the Oklahoma State University in partial fulfillment of the requirements for the Degree of MASTER OF SCIENCE July, 2000 THE STRUCTURAL AND STRATIGRAPHIC FRAMEWORK OF THE WARM SPRINGS RANCH AREA, HOT SPRINGS COUNTY, WYOMING Thesis Approved: Thesis Advisor ~~L. ... ~. ----'-"'-....D~e~e:.-g-e----- II ACKNOWLEDGEMENTS I wish to express appreciation to my advisor Dr. Arthur Cleaves for providing me with the opportunity to compile this thesis, and his help carrying out the fieldwork portion of the thesis. My sincere appreciation is extended to my advisory committee members: Dr. Stan Paxton, Dr. Gary Stewart, and Mr. David Schmude. I wish to thank Mr. Schmude especially for the great deal of personal effort he put forth toward the completion of this thesis. His efforts included financial, and time contributions, along with invaluable injections of enthusiasm, advice, and friendship. I extend my most sincere thank you to Dr. Burkhard Pohl, The Big Hom Basin Foundation, and the Wyoming Dinosaur Center. Without whose input and financial support this thesis would not have been possible. In conjunction I would like to thank the staff of the Wyoming Dinosaur Center for the great deal of help that I received during my stay in Thermopolis. Finally I wish to thank my friends and family. To my friends who have pursued this process before me, and with me; thank you very much. -
The Jackpile Sandstone Member of the Morrison Formation in West
TheJackpile Sandstone Member 0f the MorrisonFormation in west-central New Mexico- a formaldefinition byDonald E. jwen,Consulting Geologist, Tulsa, 0K 74152,and Lester J. Walters,Jr. andRonald G. Beck, ARCO Oil and Gas Co., Dallas, IX75221 The JackpileSandstone Member of the uranium mine. The JackpileSandstone is stonelenses Contactswith the underlying Morrison Formation(Upper Jurassic)in west- typically a whitish, crossbeddedsubarkose Brushy BasinMember of the Morrison For- central New Mexico is named here formallv with clay matrix and interbedded, varie- mation may be gradational, scoured, or from a stratotype near the Jackpile-PaguatL gated, pale-greento red, bentonitic mud- interbedded. The Jackpileextends only a short distancesouth of the stratotvDedue R.5W. to truncation along the basal Dakota un- conformity. However, it extendsnortheast to Lamy, north to near Cuba, and a short distancewest and a longer distancenorth- west into the subsurfaceof the San Juan Basin.Thickness of the Jackpileranges from near zero to 300ft (91 m); at the stratotype it is 100 ft (30 m) thick. Crossbeddingin- dicatesa regional easterlypaleocurrent-flow direction for the braided-streamand distal alluvial-fan complexesin which the Jackpile was deposited. Source areas were to the west and southwest,south of Gallup, and in the Mogollon Highlands. Introduction The Jackpile sandstone of economic usage has been employed informally in strati- graphic nomenclature for a distinctive bed in the uppermost part of the Brushy Basin Member of the Morrison Formation in west- central New Mexico since the Jackpile ura- nium body was discovered in that bed dur- ing 1951.The stratigraphic name fackpile has Alsoin this issue Temperatureof.mineralization in Mogollonmining district p. -
Of Physalis Longifolia in the U.S
The Ethnobotany and Ethnopharmacology of Wild Tomatillos, Physalis longifolia Nutt., and Related Physalis Species: A Review1 ,2 3 2 2 KELLY KINDSCHER* ,QUINN LONG ,STEVE CORBETT ,KIRSTEN BOSNAK , 2 4 5 HILLARY LORING ,MARK COHEN , AND BARBARA N. TIMMERMANN 2Kansas Biological Survey, University of Kansas, Lawrence, KS, USA 3Missouri Botanical Garden, St. Louis, MO, USA 4Department of Surgery, University of Kansas Medical Center, Kansas City, KS, USA 5Department of Medicinal Chemistry, University of Kansas, Lawrence, KS, USA *Corresponding author; e-mail: [email protected] The Ethnobotany and Ethnopharmacology of Wild Tomatillos, Physalis longifolia Nutt., and Related Physalis Species: A Review. The wild tomatillo, Physalis longifolia Nutt., and related species have been important wild-harvested foods and medicinal plants. This paper reviews their traditional use as food and medicine; it also discusses taxonomic difficulties and provides information on recent medicinal chemistry discoveries within this and related species. Subtle morphological differences recognized by taxonomists to distinguish this species from closely related taxa can be confusing to botanists and ethnobotanists, and many of these differences are not considered to be important by indigenous people. Therefore, the food and medicinal uses reported here include information for P. longifolia, as well as uses for several related taxa found north of Mexico. The importance of wild Physalis species as food is reported by many tribes, and its long history of use is evidenced by frequent discovery in archaeological sites. These plants may have been cultivated, or “tended,” by Pueblo farmers and other tribes. The importance of this plant as medicine is made evident through its historical ethnobotanical use, information in recent literature on Physalis species pharmacology, and our Native Medicinal Plant Research Program’s recent discovery of 14 new natural products, some of which have potent anti-cancer activity. -
A New Microvertebrate Assemblage from the Mussentuchit
A new microvertebrate assemblage from the Mussentuchit Member, Cedar Mountain Formation: insights into the paleobiodiversity and paleobiogeography of early Late Cretaceous ecosystems in western North America Haviv M. Avrahami1,2,3, Terry A. Gates1, Andrew B. Heckert3, Peter J. Makovicky4 and Lindsay E. Zanno1,2 1 Department of Biological Sciences, North Carolina State University, Raleigh, NC, USA 2 North Carolina Museum of Natural Sciences, Raleigh, NC, USA 3 Department of Geological and Environmental Sciences, Appalachian State University, Boone, NC, USA 4 Field Museum of Natural History, Chicago, IL, USA ABSTRACT The vertebrate fauna of the Late Cretaceous Mussentuchit Member of the Cedar Mountain Formation has been studied for nearly three decades, yet the fossil-rich unit continues to produce new information about life in western North America approximately 97 million years ago. Here we report on the composition of the Cliffs of Insanity (COI) microvertebrate locality, a newly sampled site containing perhaps one of the densest concentrations of microvertebrate fossils yet discovered in the Mussentuchit Member. The COI locality preserves osteichthyan, lissamphibian, testudinatan, mesoeucrocodylian, dinosaurian, metatherian, and trace fossil remains and is among the most taxonomically rich microvertebrate localities in the Mussentuchit Submitted 30 May 2018 fi fi Accepted 8 October 2018 Member. To better re ne taxonomic identi cations of isolated theropod dinosaur Published 16 November 2018 teeth, we used quantitative analyses of taxonomically comprehensive databases of Corresponding authors theropod tooth measurements, adding new data on theropod tooth morphodiversity in Haviv M. Avrahami, this poorly understood interval. We further provide the first descriptions of [email protected] tyrannosauroid premaxillary teeth and document the earliest North American record of Lindsay E. -
By HENRY FAIRFIELD OSBORN and CHARL
VoL. 6, 1920 PALAEONTOLOGY: OSBORN AND MOOK IS RECONSTRUCTION OF THE SKELETON OF THE SAUROPOD DINOSAUR CAMARASA URUS COPE (MOROSA URUS MARSH) By HENRY FAIRFIELD OSBORN AND CHARLES CRAIG MOOK AMERICAN MusEUM or NATURAL HISTORY, NEW YORK CITY Read before the Academy, November 11, 1919 The principles of modern research in vertebrate palaeontology are illustrated in the fifteen years' work resulting in the restoration of the massive sauropod dinosaur known as Camarasaurus, the "chambered saurian.." The animal was found near Canyon City, Colorado, in March, 1877. The first bones were described by Cope, August 23, 1877. The first at- tempted restoration was by Ryder, December 21, 1877. The bones analyzed by this research were found probably to belong to six individuals of Camarasaurus mingled with the remains of some carnivorous dinosaurs, all from the summit of the Morrison formation, now regarded as of Jurassic- Cretaceous age. In these two quarries Cope named nine new genera and fourteen new species of dinosaurs, none of which have found their way into. palaeontologic literature, excepting Camarasaurus. Out of these twenty-three names we unravel three genera, namely: One species of Camarasaurus, identical with Morosaurus Marsh. One species of Amphicaclias, close to Diplodocus Marsh. One species of Epanterias, close to Allosaurus Marsh. The working out of the Camarasaurus skeleton results in both the artica ulated restoration and the restoration of the musculature. The following are the principal characters: The neck is very flexible; anterior vertebrae of the back also freely movable; the division between the latter and the relatively rigid posterior dorsals is sharp. -
Geohydrology of the Westwater Canyon Member, Morrison Formation, of the Southern San Juan Basin, New Mexico Thomas E
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/28 Geohydrology of the Westwater Canyon Member, Morrison Formation, of the southern San Juan Basin, New Mexico Thomas E. Kelly, 1977, pp. 285-290 in: San Juan Basin III (northwestern New Mexico), Fassett, J. F.; James, H. L.; [eds.], New Mexico Geological Society 28th Annual Fall Field Conference Guidebook, 319 p. This is one of many related papers that were included in the 1977 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Stratigraphic Framework of the Cretaceous Mowry Shale, Frontier
Chapter 15 Stratigraphic Framework of the Cretaceous Mowry Shale, Frontier Formation and Adjacent Units, Southwestern Wyoming Province, Volume Title Page Wyoming, Colorado, and Utah By Mark A. Kirschbaum and Laura N.R. Roberts Chapter 15 of Petroleum Systems and Geologic Assessment of Oil and Gas in the Southwestern Wyoming Province, Wyoming, Colorado, and Utah By USGS Southwestern Wyoming Province Assessment Team U.S. Geological Survey Digital Data Series DDS–69–D U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey Charles G. Groat, Director U.S. Geological Survey, Denver, Colorado: Version 1, 2005 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 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 Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Manuscript approved for publication May 10, 2005 ISBN= 0-607-99027-9 Contents Abstract ……………………………………………………………………………………… -
Montana Bureau of Mines and Geology PRELIMINARY
Montana Bureau of Mines and Geology PRELIMINARY GEOLOGIC MAP OF PARADISE VALLEY SOUTH-CENTRAL MONTANA by David A. Lopez and Jon C. Reiten Montana Bureau of Mines and Geology Open File Report MBMG 480 2003 This report has been reviewed for conformity with Montana Bureau of Mines and Geology’s technical and editorial standards. Partial support has been provided by the STATEMAP component of the National Cooperative Geologic Mapping Program of the U.S. Geological Survey under Contract Number: 02HQAG0038. Montana 15 90 Map area 90 15 111° Bozeman Livingston 90 Map area r e 89 v i 45°30' R e n o t s w o l l e Y Emigrant Park Co. Gallatin Co. Pray Chico Miner Corwin Springs Jardine Gardiner YELLOWSTONE NATIONAL PARK 45° MT 3 0 3 6 Miles WY Location of the Paradise Valley map area. 1 CORRELATION OF MAP UNITS Qal Qdf Qrs Qc Qaf Qta Qls Holocene Qat1 Qpg Qgtc Qgoc Qgt Qat2 Qgt8 Qgo8 ? Qat Qat3 Qtr Qat4 QUATERNARY Pleistocene Qat5 Unconformity Qba Unconformity Thr Unconformity Tba Pliocene Tgr Unconformity Ts Miocene Unconformity TERTIARY Thpa Thpb Thpv Td Tdf Tqla Tgcs Tgca Eocene Tslc Tse Unconformity Tft Paleocene Unconformity Kho Kbc Kmi Kcd Unconformity Kls Unconformity Kevt Upper Cretaceous Ke CRETACEOUS Ktc Kco Kcf Kf Km Kmfr Ktf Unconformity Lower Cretaceous Kk Jm Upper Jurassic JURASSIC Je Middle Jurassic JT s R Unconformity TRc Lower Triassic TRIASSIC Unconformity Permi an PERMIAN lPq PMpa PMqa Pennsylvani an PENNSYLVANIAN lPMa Upper Miss. Unconformity MISSISSIPPIAN Mm Lower Miss. Unconformity DOs Dev.—Ord. DEV. --ORD Unconformity U & Mid.Cambrian CAMBRIAN Cs Unconformity Early Proterozoic Xmy PRECAMBRIAN Unconformity Archean Ag Anc Aqa Asg Aga As 2 DESCRIPTIONS OF MAP UNITS Qal Alluvium of modern channels and flood plains (Holocene) – Younger alluvium generally confined to the present flood plain developed along active rivers and streams. -
From the Western of the United
from the Western of the United GEOLOGICAL SURVEY P R® BES&lON AL PAPER 1057 Early Triassic Terebratulid Brachiopods from the Western Interior of the United States By PETER R. HOOVER GEOLOGICAL SURVEY PROFESSIONAL PAPER 1057 Description and illustration offive species of terebratulid brachiopods, and discussion of their distribution and developmental and evolutionary history UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1979 UNITED STATES DEPARTMENT OF THE INTERIOR CECIL D. ANDRUS, Secretary GEOLOGICAL SURVEY H. William Menard, Director Library of Congress Cataloging in Publication Data Hoover, Peter R. Early Triassic Terebratulid Brachiopods from the Western Interior of the United States (Geological Survey Professional Paper 1057) Bibliography: p. 19 Includes index Supt. of Docs. No.: I 19:16:1057 1. Terebratulida, Fossil. 2. Paleontology Triassic. 3. Paleontology The West. I. Title. II. Series: United States Geological Survey Professional Paper 1057 QE797.T29H66 564'.8 77-608314 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-03182-5 CONTENTS Page Page Systematic paleontology Continued Abstract ....................... 1 Family Dielasmatidae Continued Introduction .................... 1 Subfamily Dielasmatinae. Previous work................ 1 Rhaetina Waagen ..... Present study ................ 3 Family Terebratulidae ......... 9 Acknowledgments ............ 3 Subfamily Plectoconchiinae. 9 Fossil localities cited in this report. .... 3 Vex, n. gen. ......... 9 Stratigraphic setting of the brachiopods 4 Family Cryptonellidae ......... 11 Faunal relationships. .............. 6 Subfamily Cryptacanthiinae . 11 Biostratigraphic implications........ 6 Obnixia, n. gen. ...... 11 Systematic paleontology............ 7 Family Zeilleriidae ............ 17 Family Dielasmatidae.......... 7 Periallus, n. gen. ......... 17 Subfamily Zugmayeriinae . 7 References cited. ................. 19 Portneufia, n. gen. .... 7 Index ......................... 21 ILLUSTRATIONS [Plates follow index] PLATE 1. -
This Is a Digital Document from the Collections of the Wyoming Water Resources Data System (WRDS) Library
This is a digital document from the collections of the Wyoming Water Resources Data System (WRDS) Library. For additional information about this document and the document conversion process, please contact WRDS at [email protected] and include the phrase “Digital Documents” in your subject heading. To view other documents please visit the WRDS Library online at: http://library.wrds.uwyo.edu Mailing Address: Water Resources Data System University of Wyoming, Dept 3943 1000 E University Avenue Laramie, WY 82071 Physical Address: Wyoming Hall, Room 249 University of Wyoming Laramie, WY 82071 Phone: (307) 766-6651 Fax: (307) 766-3785 Funding for WRDS and the creation of this electronic document was provided by the Wyoming Water Development Commission (http://wwdc.state.wy.us) VOLUME 11-A OCCURRENCE AND CHARACTERISTICS OF GROUND WATER IN THE BIGHORN BASIN, WYOMING Robert Libra, Dale Doremus , Craig Goodwin Project Manager Craig Eisen Water Resources Research Institute University of Wyoming Report to U.S. Environmental Protection Agency Contract Number G 008269-791 Project Officer Paul Osborne June, 1981 INTRODUCTION This report is the second of a series of hydrogeologic basin reports that define the occurrence and chemical quality of ground water within Wyoming. Information presented in this report has been obtained from several sources including available U.S. Geological Survey publications, the Wyoming State Engineer's Office, the Wyoming Geological Survey, and the Wyoming Oil and Gas Conservation Commission. The purpose of this report is to provide background information for implementation of the Underground Injection Control Program (UIC). The UIC program, authorized by the Safe Drinking Water Act (P.L. -
Moab/ Westwater - Bike/Raft Sampler 4 Day
Moab/ Westwater - Bike/Raft Sampler 4 Day The Moab mountain biking–Westwater Canyon combination trip brings together two of the most popular activities in Utah. Mountain biking and Moab are nearly synonymous; the former uranium boom town has become a mecca for bikers wanting to swoop, soar, climb, and roll over sandstone and wild desert trails. Follow this up with two days of floating on the Colorado River, splashing through rapids beneath the sheer black walls of Westwater Canyon, falling asleep to the sound of water on rocks: relaxation well deserved. SAMPLE 4-DAY ITINERARY One of the advantages of a bike/river trip is the flexibility of the daily itinerary. It can vary widely from one trip to the next based on group desires and ability level, Mother Nature, and courtesy for other groups in the area. This typical itinerary illustrates a bike trip in the Moab area and raft trip through Westwater Canyon on the Colorado River. Day 1: Meet group at headquarters in Green River, Utah. A one-hour van ride to Moab marks the start of the trip. We will select a base camp on public land outside of town, location to be determined by where we want to ride, weather, and camp availability. We will begin with a warm-up ride, depending on the group's interests and ability level. The Bar M trail network north of Moab provides a number of excellent short beginner and intermediate single-track loops. Options for after lunch include riding the Klondike Bluffs or Magnificent 7 trail networks. Dinner and solar showers await back at base camp. -
The Summerville Formation: Evidence for a Sub-Horizontal Stratigraphic Sequence Below the Post-Rift Nu Conformity in the Middleton Place Summerville Seismic Zone
University of South Carolina Scholar Commons Theses and Dissertations 2017 The ummeS rville Formation: Evidence for a Sub- Horizontal Stratigraphic Sequence below the Post- Rift nconforU mity in the Middleton Place Summerville Seismic Zone Joseph Edward Getz University of South Carolina Follow this and additional works at: https://scholarcommons.sc.edu/etd Part of the Geology Commons Recommended Citation Getz, J. E.(2017). The Summerville Formation: Evidence for a Sub-Horizontal Stratigraphic Sequence below the Post-Rift nU conformity in the Middleton Place Summerville Seismic Zone. (Master's thesis). Retrieved from https://scholarcommons.sc.edu/etd/4177 This Open Access Thesis is brought to you by Scholar Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of Scholar Commons. For more information, please contact [email protected]. THE SUMMERVILLE FORMATION: EVIDENCE FOR A SUB- HORIZONTAL STRATIGRAPHIC SEQUENCE BELOW THE POST-RIFT UNCONFORMITY IN THE MIDDLETON PLACE SUMMERVILLE SEISMIC ZONE By Joseph Edward Getz Bachelor of Arts University of South Carolina, 2013 Submitted in Partial Fulfillment of the Requirements For the Degree of Master of Science in Geological Sciences College of Arts and Sciences University of South Carolina 2017 Accepted by: James H. Knapp, Director of Thesis Camelia C. Knapp, Reader Andrew Leier, Reader Cheryl L. Addy, Vice Provost and Dean of the Graduate School © Copyright by Joseph Edward Getz, 2017 All Rights Reserved. ii DEDICATION I would like to dedicate this to my grandparents and my mother, for without their support none of this would have been possible. iii ACKNOWLEDGEMENTS I would like to give a special thanks my major advisor, Dr.