Wsgs-1916-B-13.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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. -
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 ……………………………………………………………………………………… -
A Preliminary Assessment of Paleontological Resources at Bighorn Canyon National Recreation Area, Montana and Wyoming
A PRELIMINARY ASSESSMENT OF PALEONTOLOGICAL RESOURCES AT BIGHORN CANYON NATIONAL RECREATION AREA, MONTANA AND WYOMING Vincent L. Santucci1, David Hays2, James Staebler2 And Michael Milstein3 1National Park Service, P.O. Box 592, Kemmerer, WY 83101 2Bighorn Canyon National Recreation Area, P.O. Box 7458, Fort Smith, MT 59035 3P.O. Box 821, Cody, WY 82414 ____________________ ABSTRACT - Paleontological resources occur throughout the Paleozoic and Mesozoic formations exposed in Bighorn Canyon National Recreation Area. Isolated research on specific geologic units within Bighorn Canyon has yielded data on a wide diversity of fossil forms. A comprehensive paleonotological survey has not been previously undertaken at Bighorn Canyon. Preliminary paleontologic resource data is presented in this report as an effort to establish baseline data. ____________________ INTRODUCTION ighorn Canyon National Recreation Area (BICA) consists of approximately 120,000 acres within the Bighorn Mountains of north-central Wyoming and south-central Montana B (Figure 1). The northwestern trending Bighorn Mountains consist of over 9,000 feet of sedimentary rock. The predominantly marine and near shore sedimentary units range from the Cambrian through the Lower Cretaceous. Many of these formations are extremely fossiliferous. The Bighorn Mountains were uplifted during the Laramide Orogeny beginning approximately 70 million years ago. Large volumes of sediments, rich in early Tertiary paleontological resources, were deposited in the adjoining basins. This report provides a preliminary assessment of paleontological resources identified at Bighorn Canyon National Recreation Area. STRATIGRAPHY The stratigraphic record at Bighorn Canyon National Recreation Area extends from the Cambrian through the Cretaceous (Figure 2). The only time period during this interval that is not represented is the Silurian. -
Fracture Analysis of Circum-Bighorn Basin Anticlines
FRACTURE ANALYSIS OF CIRCUM-BIGHORN BASIN ANTICLINES, WYOMING-MONTANA by Julian Stahl A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Science MONTANA STATE UNIVERSITY Bozeman, Montana November 2015 ©COPYRIGHT by Julian Stahl 2015 All Rights Reserved ii DEDICATION I dedicate this thesis to my brother, Manuel Stahl, who provided me with the inspiration and drive to pursue a degree that I am truly passionate about. iii ACKNOWLEDGEMENTS The research presented in this document would not have been as thought- provoking and thorough without the help of my mentors and peers. My advisor, Dr. David Lageson helped formulate the project idea and was fundamental throughout the course of my study in leading me in the right direction and always being available to answer questions. I would also like to extend my gratitude to my committee members, Dr. Colin Shaw and Dr. Jean Dixon, for providing me with the necessary assistance and expertise. I would also like to thank my fellow geology peers at Montana State University. Without the constant communication and discussions with Mr. Jacob Thacker, Mr. Travis Corthouts and Mrs. Anita Moore-Nall this project would not have come to fruition. I would also like to offer my sincere appreciation to my two field assistants, Mr. Evan Monroe and Miss Amy Yoder, for taking the time out of their lives to help unravel the geology of the Bighorn Basin in the field. I would like to express my gratitude to my entire family, Dr. Johannes Stahl, Ms. Gabriele Stahl and Mr. -
The First Record of Freshwater Plesiosaurian from the Middle
Gao et al. Journal of Palaeogeography (2019) 8:27 https://doi.org/10.1186/s42501-019-0043-5 Journal of Palaeogeography ORIGINALARTICLE Open Access The first record of freshwater plesiosaurian from the Middle Jurassic of Gansu, NW China, with its implications to the local palaeobiogeography Ting Gao, Da-Qing Li* , Long-Feng Li and Jing-Tao Yang Abstract Plesiosaurs are one of the common groups of aquatic reptiles in the Mesozoic, which mainly lived in marine environments. Freshwater plesiosaurs are rare in the world, especially from the Jurassic. The present paper reports the first freshwater plesiosaur, represented by four isolated teeth from the Middle Jurassic fluviolacustrine strata of Qingtujing area, Jinchang City, Gansu Province, Northwest China. These teeth are considered to come from one individual. The comparative analysis of the corresponding relationship between the body and tooth sizes of the known freshwater plesiosaur shows that Jinchang teeth represent a small-sized plesiosaurian. Based on the adaptive radiation of plesiosaurs and the palaeobiogeographical context, we propose a scenario of a river leading to the Meso-Tethys in the Late Middle Jurassic in Jinchang area, which may have provided a channel for the seasonal migration of plesiosaurs. Keywords: Freshwater plesiosaur, Middle Jurassic, Jinchang, Gansu Province, Palaeobiogeography 1 Introduction Warren 1980;Satoetal.2003; Kear 2012). Up to now, Plesiosaurs are one of the most familiar groups of Mesozoic the taxonomic affinities of most freshwater plesio- marine reptiles, which mainly lived in marine environ- saurs have remained unclear; some of them are re- ments. The records of plesiosaurs in non-marine deposits ferred to Plesiosauroidea (Cruickshank and Fordyce are sparse in comparison to those from marine sediments. -
CORRELATION of the UPPER CRETACEOUS STRATA of WYOMING Stratigraphic Chart Director and State Geologist Upper Cretaceous Laramie, Wyoming by Ranie M
WYOMING STATE GEOLOGICAL SURVEY Open File Report 2017-3 Thomas A. Drean CORRELATION OF THE UPPER CRETACEOUS STRATA OF WYOMING Stratigraphic Chart Director and State Geologist Upper Cretaceous Laramie, Wyoming by Ranie M. Lynds and Joshua S. Slattery Wyoming Interpreting the past, providing for the future 2017 Western Hanna Laramie Bighorn Denver Greater Green River Basin Wind River Basin Powder River Basin Wyoming Basin Basin Basin Basin A B C D E F G H I J K L M N O P Q R S T U V W X Y Age Period Epoch Stage and Stage Polarity U.S. Western Interior U.S. Western Interior U.S. Western Interior North American U.S. Western Interior Southern Jackson Northwestern Southern Eastern Eastern Atlantic Rocky Point Separation Lost Soldier Tully Rawlins Hanna Laramie Western Southern and Eastern Bighorn Northwestern Salt Creek Southwestern Southeastern Central Northwestern Denver (Ma) Boundary Chron Radiometric Ammonite Inoceramid Land Vertebrate Palynostratigraphic Thrust Belt Hole and Rock Springs Rock Springs Rock Springs Washakie Rim Rim Ranch Draw Basin Basin, Wind River Central Wind Wind River Basin Powder Powder Powder River Black Hills Black Hills Basin (Ma) Age (Ma) Biozone Biozone Age Biozone Hoback Basin Uplift Uplift Uplift Basin Rock River Basin River Basin Basin River Basin River Basin Basin (7, 56, 77) (7, 56, 74) (8, 49, 54, 55, 56, 69, 72) (7, 23, 25, 56, 74) (7, 56, 74) (2, 33, 35, 77) (50) (6, 10, 29, 30, 47, 53, (6, 11, 12, 22, 32, 37, (12, 26, 30, 64, 72, (12, 26, 30, 36, 63, 64, (12, 19, 20, 26, 29, 30, (1, 12, 21, 30, 36, 58, -
A Cladistic Analysis and Taxonomic Revision of the Plesiosauria (Reptilia: Sauropterygia) F
Marshall University Marshall Digital Scholar Biological Sciences Faculty Research Biological Sciences 12-2001 A Cladistic Analysis and Taxonomic Revision of the Plesiosauria (Reptilia: Sauropterygia) F. Robin O’Keefe Marshall University, [email protected] Follow this and additional works at: http://mds.marshall.edu/bio_sciences_faculty Part of the Aquaculture and Fisheries Commons, and the Other Animal Sciences Commons Recommended Citation Frank Robin O’Keefe (2001). A cladistic analysis and taxonomic revision of the Plesiosauria (Reptilia: Sauropterygia). ). Acta Zoologica Fennica 213: 1-63. This Article is brought to you for free and open access by the Biological Sciences at Marshall Digital Scholar. It has been accepted for inclusion in Biological Sciences Faculty Research by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected], [email protected]. Acta Zool. Fennica 213: 1–63 ISBN 951-9481-58-3 ISSN 0001-7299 Helsinki 11 December 2001 © Finnish Zoological and Botanical Publishing Board 2001 A cladistic analysis and taxonomic revision of the Plesiosauria (Reptilia: Sauropterygia) Frank Robin O’Keefe Department of Anatomy, New York College of Osteopathic Medicine, Old Westbury, New York 11568, U.S.A Received 13 February 2001, accepted 17 September 2001 O’Keefe F. R. 2001: A cladistic analysis and taxonomic revision of the Plesio- sauria (Reptilia: Sauropterygia). — Acta Zool. Fennica 213: 1–63. The Plesiosauria (Reptilia: Sauropterygia) is a group of Mesozoic marine reptiles known from abundant material, with specimens described from all continents. The group originated very near the Triassic–Jurassic boundary and persisted to the end- Cretaceous mass extinction. This study describes the results of a specimen-based cladistic study of the Plesiosauria, based on examination of 34 taxa scored for 166 morphological characters. -
Paleontological Resources Technical Report Riley Ridge to Natrona Project DECEMBER 2018
U.S. Department of the Interior Bureau of Land Management Paleontological Resources Technical Report Riley Ridge to Natrona Project DECEMBER 2018 Table of Contents 1.0 Introduction ......................................................................................................................................... 1 2.0 Regional Setting .................................................................................................................................. 1 3.0 Inventory Methodology ....................................................................................................................... 1 4.0 Potential Fossil-Bearing Geologic Formations ................................................................................... 4 4.1 Browns Park Formation (PFYC 3) ............................................................................................ 4 4.2 White River Formation or Group (PFYC 5) .............................................................................. 5 4.3 Wind River Formation (PFYC 5) .............................................................................................. 5 4.4 Green River Formation (PFYC 5) ............................................................................................. 5 4.5 Wasatch Formation (PFYC 5) ................................................................................................... 5 4.6 Battle Spring Formation (PFYC 3)............................................................................................ 6 4.7 Bridger Formation -
Yellowstone Paleontological Survey
Yellowstone Paleontological Survey Introduction Stratigraphy Fossil Chronology Taxonomy Localities Vincent L. Santucci Interpretation Paleontological Resource Management Research Collections and Curation Paleontological Resources Near Yellowstone [email protected] Bibliography Yellowstone Center for Resources Appendix A: Yellowstone Paleontological Survey Proposal National Park Service Yellowstone National Park, Wyoming Appendix B: Yellowstone Paleo-Species List YCR-NR-98-1 1998 Appendix C: RMP Paleontological Project Statements Appendix D: Paleontology Researchers at Yellowstone Appendix E: Fossil Specimens in Park Collections Appendix F: Yellowstone Fossils in Outside Repositories Appendix G: GIS Stratigraphy Maps http://www2.nature.nps.gov/geology/paleontology/surveys/yell_survey/index.htm[5/28/2013 2:13:48 PM] Yellowstone Paleo Survey: Introduction Introduction A survey of Yellowstone's fossil resources was initiated in the same spirit of discovery demonstrated by Captain William Raynolds, Henry Washburn, and Ferdinand Hayden. Rumors of marine reptiles, trilobite mass death assemblages, and even dinosaurs in Yellowstone have lured a team of paleontologists in the same way that the legends of "Colter's Hell" and Jim Bridger's "Tall Tales" have attracted many before. Compared to other natural resources at Yellowstone National Park, fossils have received little attention. Except for the research conducted on the petrified forests, Yellowstone's fossils have remained a relative "paleo-incognita" more than 125 years after the park's establishment. As this survey demonstrates, the lack of paleontological research is not due to a lack of significant fossils. Perhaps historian Aubrey Haines provided the best explanation in his comment, "Past administrations preferred that resources not in the public's eye be left alone" (pers. -
Geology and Oil and Coal Eesoueces of the Eegion South of Cody Paek County, Wyoming
UNITED STATES DEPARTMENT OF THE INTERIOR Harold L. Ickes, Secretary GEOLOGICAL SURVEY W. C. Mendenhall, Director Bulletin 921-B GEOLOGY AND OIL AND COAL EESOUECES OF THE EEGION SOUTH OF CODY PAEK COUNTY, WYOMING BY W. G. PIERCE AND D. A. ANDREWS Contributions to economic geology, 1940 (Pages 99-180) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1941 For sale by the Superintendent of Documents, Washington, D. C. -.-.------ Price $1.00 CONTENTS Fag« Abstract.--------------------I---------------------- ........ 99 Introduction _-__.. __-__-..-_-.-----_._-_-_..-.....___.-._.__... 101 Location and extent of the area.-__--__.-_-_____________________- 101 Previous investigations and publications.._____._._._____.___._.._ 101 Field work and acknowledgments_---.-__.____._________....... 103 Geography. ________________....^.-----___________._______._..__._. 104 Climate and vegetation_._..__..___.....____-.-_.___-..__._... 104 Drainage and water supply.....______--_--_.-__.__^___-_._.._.- 106 Transportation and settlement...-.-..--_-_____-______--......._ 107 Sedimentary rocks.__-_----------.-----_---_______-_-_--_____-____- 108 General features.---_--------------_-_-____-__--_-___.___-....- 108 Rocks not exposed...---.--.----------___-_-__-___-_---_--...._ 109 Rocks exposed---_----___-_-.---------__-_-__----____----____- 110 Triassic system._--.-_-_-----_-_-__-___-__-_______--______- 110 Chugwater formation------____-_____________----______ 110 Jurassic system..--_......--_-_._._______*.________-.__...- Ill Upper Jurassic series-----.---.---.____________---___._- Ill Sundance-formation... ... _._._____________.___.._._ Ill Morrison formation._______________________________ 113 Cretaceous system.".....-.-.-_._.___..._.__.___.._____._.._ 116 Lower Cretaceous series._____.___..._______._._...___. -
Western Interior Seaway
() . Paleogeo.graphy of the Late Cretaceous of the Western Interior otMfddle North America+ j?'oal .Blstribution anct,Sedimen~cumulation By Laura N. Robinson Roberts and Mark A. Kirschbaum U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1561 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY Gordon P. Eaton, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center Denver, CO 80225 Any use of trade, product, or finn names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government Library of Congress Cataloging-in-Publication Data Roberts, Laura N. Robinson. Paleogeography of the Late Cretaceous of the western interior of middle North America : coal distribution and sediment accumulation I by Laura N. Robinson Roberts and Mark A. Kirschbaum. p. em.- (U.S. Geological Survey professional paper ; 1561) Includes bibliographical references. Supt. of Docs. no.: I 19.16: 1561 1. Paleogeography-Cretaceous. 2. Paleogeography-West (U.S.). 3. Coal Geology-West (U.S.). I. Kirschbaum, Mark A. II. Title. III. Series. QE50 1.4.P3R63 1995 553.2'1'0978-dc20 94-39032 CIP CONTENTS Abstract........................................................................................................................... 1" Introduction ................................................................................................................... Western Interior Seaway ... .. ... ... ... .. .. .. -
Wsgs-2014-Ofr-03.Pdf
TO ACCOMPANY OPEN FILE REPORT 14-3 WYOMING STATE GEOLOGICAL SURVEY P.O. BOX 1347, LARAMIE, WY 82073 307-766-2286 • 307-766-2605 (fax) [email protected] • www.wsgs.uwyo.edu Director & State Geologist Thomas A. Drean ══════════════════════════════ Preliminary Geologic Map of the North Ridge Quadrangle Johnson County, Wyoming by Ranie M. Lynds, Erin A. Campbell-Stone, and Rachel N. Toner ══════════════════════════════ Open File Report 14-3 Laramie, Wyoming September 12, 2014 Prepared in cooperation with and research supported by the U.S. Geological Survey, National Cooperative Geologic Mapping Program, under USGS award number G13AC000243. The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government. This report is preliminary and has not been reviewed for conformity with Wyoming State Geological Survey editorial standards or with the North American Stratigraphic Code. Contents Introduction ..................................................................................................................................... 2 Location ........................................................................................................................................... 2 Geologic Setting ............................................................................................................................... 2 Structure .........................................................................................................................................