Geology of the Whetstone Ridge Area, Meagher County, Montana

Total Page:16

File Type:pdf, Size:1020Kb

Geology of the Whetstone Ridge Area, Meagher County, Montana AN ABSTRACT OF THE THESIS OF RICHARD MICHAEL GLASHEEN for theMASTER OF SCIENCE (Name) (Degree) in GEOLOGY presented on L&1j (Major) (Data Title: GEOLOGY OF THE WHETSTONERIDGE AREA, MAGHER COUNTY, MONTANA Abstract approved: Redacted for privacy David A. Bostwick The thesis area consists of 65square miles located in the southeastern part of Meagher County,MontanaRanging in age from Precambrian to Quaternary,the strata exposed in the area have a total thickness of about 11, 100 feet. Low grade metamorphic rocks, mainly slates,and limestones represent the estimated 2, 000 foot thick Precambrianunit.Paleo- zoic rocks, about ,600 feet in thickness, consist mainlyof carbon- ates but include marine sandstones,some of which were meta- morphosed into quartzites.Ordovician, Silurian, and Permian strata are absent. The Mesozoic rocks are dominantly marine,continental, and lacustrjne sandstones, siltstones, andshales. Rocks of Triassic age are not present in this 6, 500 foot thicksequence of sedimentary rocks. Intrusiveandextrusive igneous rocks, glacial deposits, and unconsolidated alluvium represent the Cenozoic Period. The major structures in the thesisarea are the result of the Lararnide Revolution and date from Late Cretaceousto Early Tertiary. Geology of the Whetstone Ridge Area, Meagher County, Montaxia by Richard Michael Glasheen A THESIS bmRtd to Oregon State Untverstty in partial fulfillment of the requirements for the degree of Master of Science June 1969 APPROVED: Redacted for privacy Ffofessor ofeology in charge of major Redacted for privacy/ Ciai1 of Geology 'Department Redacted for privacy Dean of Graduate School Date thesis is presented I27 /Y 9 Typed by Donna L. Olson for Richard Michael Glasheen ACKNOWLEDGMENTS The writer wishes to express his gratitude for financial assistance given by Amerada Petroleum Corporation. Special acknowledgment is due Dr. David A, Bostwick for his guidance and critical reading of this manuscript. I am also indebted to the following people of the Castle Mountain area in central Montana for allowing me free access to I their properties and aiding materially in my comfort in the field: Mrs. PauUneHereim, Mr. Andy Grande, Mr. Paul Grande, Voidseth Ranch, Mr. Arliss Berg, Mr. James Berg, Mr. and Mrs. Harold Bonnet, and Margaret Engen, all of Lennep; Bair Company and Marion Coates of Martinsdale. A very special thanks to my parents, Rose and Larry, whose encouragement helped make this thesis a reality. The warmest gratitude to my wife, Nelda, for her under stand- ing and patience during the preparation of the thesis. TABLE OF CONTENTS INTRODUCTION 1 Location and Accessibility 1 Purposes and Methods of Investigation 1 Previous Work 3 Climate 4 Vtation 5 STRATIGRAPHY 6 Precambrian System 6 Belt Series 6 Cambrian System 11 Flathead Formation 11 Distribution and Physiographic Expression lz Lithology and Thickness 'a Age and Fossils 13 Source and Depositional Environment 14 Cambrian Undivided 14 Pilgrim Formation 16 Distribution and Physiographic Expression 17 Lithology and Thickness 17 Age and Fossils 19 Source and Deposi.tional Environment ao Devonian System a' Jefferson Formation Distribution and Physiographic Expression 22 Lithology and Thickness 22 Age and Fossils 23 Source and Depositional Environment 23 Mississippian System 24 Madison Group 24 Lodgepole Formation 25 Distribution and Physiographic Expression 25 Lithology and Thickness 25 Age and Fossils 28 Source and Depositional Environment 28 Mission Canyon Formation 28 Distribution and Physiographic Expression 29 Page Lithology and Thickness 29 Age and Fossils 31 Source and Depositional Environment 31 Big Snowy Group 32 Distribution and Physiographic Expression 33 Lithology and Thickness 33 Age and Fossils 34 Source and Depositional Environment 34 Amsden Formation Distribution and Physiographic Expression 36 Lithology and Thickness 36 Age and Fossils 38 Source and Depositional Environment 39 Pennsylvanian System 39 Quadrant Formation 39 Distribution and Physiographic Expression 40 Lithology and Thickness 40 Age and Fossils 42 Source and Depositional Environment 42 Jurassic System 42 Ellis Group 42 Swift Formation 43 Distribution and Physiographic Expression 43 Lithology and Thickness 44 Age and Fossils 44 Source and Depositional Environment 44 Morrison Formation 45 Distribution and Physiographic Expression 46 Lithology and Thickness 47 Age and Fossils 49 Source and Depositional Environment 50 Cretaceous System 50 Kootenai Formation 52 Distribution and Physiographic Expression 54 Lithology and Thickness 56 Age and Fossils 57 Source and Depositional Environment 58 Colorado Group 59 Distribution and Physiographic Expression 59 Lithology and Thickness 61 Age and Fossils 61 Source and Depositional Environment 62 Page Eagle Sandstone 62 Distribution and Physiographic Expres sion 63 Lithology and Thickness 63 Age and Fossils 66 Source and Depositional Environment 66 Judith River Formation 67 Distribution and Physiographic Expression 67 Lithology and Thickness 68 Age and Fossils 70 Source and Depositional Environment 71 Bearpaw Shale 71 Distribution and Physiographic Expres sion 71 Lithology and Thickness 72 Age and Fossils Source and Depositional Environment 74 Lennep Formation 75 Distribution and Physiographic Expression 75 Lithology and Thickness 75 Age and Fossils Source and Depositional Environment 78 Hell Creek Formation 78 Distribution and Physiographic Expression 78 Lithology and Thickness 79 Age and Fossils 80 Source and Depositional Environment 80 Tertiary System 80 Igneous Rocks 80 Intrusive Rocks 81 Sills 81 Dikes 82 Plugs 82 Extrusive Rocks 83 Flows 83 Age of Igneous Rocks 83 Quaternary System 85 STRUCTURAL GEOLOGY 86 Folds and Associated Faults 88 Flagstaff Anticline 88 Flagstaff Canyon Syncline 89 Checkerboard Anticline 89 Pg Coates Pond Syncline 90 Thorsens PondAnticline 90 Coyote Creek Syndline 91 West Flagstaff Anticline 91 LennepSyncline 92 Corral Creek Anticline 92 Blackhawk Syncline 93 Robinson Anticline 93 Time of Folding 94 GEOMORPHOLOGY 96 Structural and Stratigraphic Control of Topography 96 Stream Erosion 96 Glaciation 98 GEOLOGIC HISTORY 99 ECONOMIC GEOLOGY 103 BIBLIOGRAPHY 104 APPENDIX 110 MEASURED STRATIGRAPHIC SECTIONS 110 LIST OF FIGURES Figure Pge 1. Steeply dipping slates of the Belt Series. 9 2. View to the north of the topography developed on the Belt Series. 9 3. Typical outcrop of the Flathead Formation. 1 5 4, Valley formed on nonresistant Cambrian Un- divided strata. 15 5. Hogback ridge of limestone flat-pebblecon- glomerate of the Pilgrim Formation. 18 6. Typical exposure of shaly limestone of the Lodgepole Formation. 26 1. Good outcrop of massive limestone of the Mission Canyon Formation. 30 8, View to the east showing Whetstone Ridge and limestone bluffs of the Madison Group. 30 9. A red soil zone and limestone developed in the middle part of the Amsden Formation. 37 10, Outcrop of quartzose sancstone of theuadrant Formation. 41 11. Outcrop of worm-mottled siltstones and shales of the Morrison Formation. 48 12. View to the northwest of the topography developed on the Cretaceous rocks. 51 13. Typical Kootenai Formation outcrop. 55 14. View northwest up Bonanza Creek. 60 15. Good outcrop of cross-bedded Eagle Sandstone. 64 Figure !a ge 16. Close-up view of rriolluscan coquina bedin the upper part of thc Judith RiverFormation. 69 1 7. Igneous sills form hogback ridges in the Bearpaw Shale. 73 18. Igneous sill underlain by black carbonaceous Bearpaw shale. 73 19. Well-developed large scale contorted flaggy bedding in the Lennep Formation 76 O. View to the northeast of Miocene basaltflows overlying limestones of the Mission Canyon Formation. 84 LIST OF TABLES Table 1. Generalized stratigraphic section of the Whetstone Ridge area. 7 Z. Regional correlation chart. 8 3. Historical development of stratigraphicterminology of the Upper Cretaceous rocks in theCastle Mountain area. 53 LIST OF PLATES Plate 1. Index map showing location of thesisarea. 2 2. Tectonic sketch map of west-central Montana. 87 3. Geologic map of the Whetstone Ridgearea, Meagher County, Montana. In Pocket GEOLOGY OF THE WHETSTONE RIDGE AREA, MEAGHER COUNTY, MONTANA INTRODUC TION Location and Accessibjlity The thesis area is located in MeagherCounty, Montana, approximately0 miles southeast of White Sulphur Springs (Plate 1). The area includes the easternpart of the Castle Mountains, spec- fically the eastern sections of Ts. 8 and9N., R. 9 E., and the western sections of Ts. 8 and 9 N., R. jOE.Within the area mapped are the small con-munities ofLennep and Checkerboard, now but remnants of once busy miningcenters. Access to the area is excellent.The main approach to the area is from the northwest.U.S. Highway lleads southeast from White Sulphur Springs through thetown of Checicerboarci ard marks the northern boundary of thearea, Montana State Highway 294, an all-weather road that extends west from Martinsdaleand ciosely parallels the Chicago, Milwaukee, St. Paul, andPacific Railroad marks the southern boundary of the thesisarea.In addition, im- proved and unimproved roads provideaccess into the area. Purposes and Methods of Investigation The primary purposes of the thesis problemwere:1) tomap Cascade County MONTANA kungs Hill Lingshire \\ ) I' \\ ,) \ IV1ESGHER COUNTY Broadwater Lounty Checkerboard ( Springs Castle-, TI-ESL I Moui4tains .ennep 10 11 / 0Lebo Ringling \\ I - Gallatjn County Park County 0 5 10 miles PLATE 1.INDEX MAP Highway Secondary Road 3 the surface geology of thearea; 2) to determine the major structures of the area; and 3) tomeasure
Recommended publications
  • Taphonomy of the Sun River Bonebed, Late Cretaceous
    TAPHONOMY OF THE SUN RIVER BONEBED, LATE CRETACEOUS (CAMPANIAN) TWO MEDICINE FORMATION OF MONTANA by Benjamin Andrew Scherzer A thesis submitted in partial fulfillment of the requirements for the degree of Master of Science in Earth Sciences MONTANA STATE UNIVERSITY-BOZEMAN Bozeman, Montana April 2008 © COPYRIGHT by Benjamin Andrew Scherzer 2008 All Rights Reserved ii APPROVAL of a thesis submitted by Benjamin Andrew Scherzer This thesis has been read by each member of the thesis committee and has been found to be satisfactory regarding content, English usage, format, citations, bibliographic style, and consistency, and is ready for submission to the Division of Graduate Education. Dr. David J. Varricchio Approved for the Department of Earth Sciences Dr. Stephan G. Custer Approved for the Division of Graduate Education Dr. Carl A. Fox iii STATEMENT OF PERMISSION TO USE In presenting this thesis in partial fulfillment for the requirements for a master’s degree at Montana State University, I agree that the Library shall make it available to borrowers under rules of the Library. If I have indicated my intention to copyright this thesis by including a copyright notice page, copying is allowed only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Request for permission for extended quotation from or reproduction of this thesis in whole or in parts may be granted only by the copyright holder. Benjamin Andrew Scherzer April 2008 iv ACKNOWLEDGEMENTS This thesis would not have come to completion without the help of each member of my committee: Dave Varricchio, Jack Horner, and Jim Schmitt.
    [Show full text]
  • North-Central Montana
    Petrology of the Eagle Sandstone, Bearpaw Mountains Area, North-Central Montana By DONALD L. GAUTIER INVESTIGATIONS OF SHALLOW GAS RESERVOIRS IN THE NORTHERN GREAT PLAINS GEOLOGICAL SURVEY BULLETIN 1521 Prepared in cooperation with the U. S. Depart1Tl£nt of Energy Composition and burial history of an important conventional shallow methane reservoir in the northern Great Plains UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1981 UNITED STATES DEPARTMENT OF THE INTERIOR JAMES G. WATT, Secretary GEOLOGICAL SURVEY Dallas L. Peck, Director Library of Congress Cataloging in Publication Data . Gautier, Donald L. Petrology of the Eagle Sandstone, Bearpaw Mountains area, north-central Montana. (Investigations of shallow gas reservoirs in the northern Great Plains) (Geological Survey Bulletin 1521) Bibliography: p. 52 1. Sandstone-Montana-Bearpaw Mountains region. 2. Gas, Natural-Geology­ Montana-Bearpaw Mountains region. I. Title. II. Series. III. Series: Geological Survey Bulletin 1521. QE75.B9 no. 1521 [QE471.15.S25] 557.3s 81-607963 [552'.5] AACR2 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Absuact:---------------------------------------------------- 1 In~uction------------------------------------------------- 2 ~~un~--------------------------------------------- 4 Acknowledgments-------------------------------------- 5 Geologic Setting----------------------------------- 6 Hydrocarbons in the Eagle Sandstone------------------------ 8 Lithology----------------------------------------
    [Show full text]
  • Feeding Height Stratification Among the Herbivorous
    Mallon et al. BMC Ecology 2013, 13:14 http://www.biomedcentral.com/1472-6785/13/14 RESEARCH ARTICLE Open Access Feeding height stratification among the herbivorous dinosaurs from the Dinosaur Park Formation (upper Campanian) of Alberta, Canada Jordan C Mallon1,5*, David C Evans2, Michael J Ryan3 and Jason S Anderson4 Abstract Background: Herbivore coexistence on the Late Cretaceous island continent of Laramidia has been a topic of great interest, stemming from the paradoxically high diversity and biomass of these animals in relation to the relatively small landmass available to them. Various hypotheses have been advanced to account for these facts, of which niche partitioning is among the most frequently invoked. However, despite its wide acceptance, this hypothesis has not been rigorously tested. This study uses the fossil assemblage from the Dinosaur Park Formation of Alberta as a model to investigate whether niche partitioning facilitated herbivorous dinosaur coexistence on Laramidia. Specifically, the question of feeding height stratification is examined in light of the role it plays in facilitating modern ungulate coexistence. Results: Most herbivorous dinosaur species from the Dinosaur Park Formation were restricted to feeding no higher than approximately 1 m above the ground. There is minimal evidence for feeding height partitioning at this level, with ceratopsids capable of feeding slightly higher than ankylosaurs, but the ecological significance of this is ambiguous. Hadrosaurids were uniquely capable of feeding up to 2 m quadrupedally, or up to 5 m bipedally. There is no evidence for either feeding height stratification within any of these clades, or for change in these ecological relationships through the approximately 1.5 Ma record of the Dinosaur Park Formation.
    [Show full text]
  • 71St Annual Meeting Society of Vertebrate Paleontology Paris Las Vegas Las Vegas, Nevada, USA November 2 – 5, 2011 SESSION CONCURRENT SESSION CONCURRENT
    ISSN 1937-2809 online Journal of Supplement to the November 2011 Vertebrate Paleontology Vertebrate Society of Vertebrate Paleontology Society of Vertebrate 71st Annual Meeting Paleontology Society of Vertebrate Las Vegas Paris Nevada, USA Las Vegas, November 2 – 5, 2011 Program and Abstracts Society of Vertebrate Paleontology 71st Annual Meeting Program and Abstracts COMMITTEE MEETING ROOM POSTER SESSION/ CONCURRENT CONCURRENT SESSION EXHIBITS SESSION COMMITTEE MEETING ROOMS AUCTION EVENT REGISTRATION, CONCURRENT MERCHANDISE SESSION LOUNGE, EDUCATION & OUTREACH SPEAKER READY COMMITTEE MEETING POSTER SESSION ROOM ROOM SOCIETY OF VERTEBRATE PALEONTOLOGY ABSTRACTS OF PAPERS SEVENTY-FIRST ANNUAL MEETING PARIS LAS VEGAS HOTEL LAS VEGAS, NV, USA NOVEMBER 2–5, 2011 HOST COMMITTEE Stephen Rowland, Co-Chair; Aubrey Bonde, Co-Chair; Joshua Bonde; David Elliott; Lee Hall; Jerry Harris; Andrew Milner; Eric Roberts EXECUTIVE COMMITTEE Philip Currie, President; Blaire Van Valkenburgh, Past President; Catherine Forster, Vice President; Christopher Bell, Secretary; Ted Vlamis, Treasurer; Julia Clarke, Member at Large; Kristina Curry Rogers, Member at Large; Lars Werdelin, Member at Large SYMPOSIUM CONVENORS Roger B.J. Benson, Richard J. Butler, Nadia B. Fröbisch, Hans C.E. Larsson, Mark A. Loewen, Philip D. Mannion, Jim I. Mead, Eric M. Roberts, Scott D. Sampson, Eric D. Scott, Kathleen Springer PROGRAM COMMITTEE Jonathan Bloch, Co-Chair; Anjali Goswami, Co-Chair; Jason Anderson; Paul Barrett; Brian Beatty; Kerin Claeson; Kristina Curry Rogers; Ted Daeschler; David Evans; David Fox; Nadia B. Fröbisch; Christian Kammerer; Johannes Müller; Emily Rayfield; William Sanders; Bruce Shockey; Mary Silcox; Michelle Stocker; Rebecca Terry November 2011—PROGRAM AND ABSTRACTS 1 Members and Friends of the Society of Vertebrate Paleontology, The Host Committee cordially welcomes you to the 71st Annual Meeting of the Society of Vertebrate Paleontology in Las Vegas.
    [Show full text]
  • Carboniferous Formations and Faunas of Central Montana
    Carboniferous Formations and Faunas of Central Montana GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 Carboniferous Formations and Faunas of Central Montana By W. H. EASTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 348 A study of the stratigraphic and ecologic associa­ tions and significance offossils from the Big Snowy group of Mississippian and Pennsylvanian rocks UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1962 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U.S. Geological Survey Library has cataloged this publication as follows : Eastern, William Heyden, 1916- Carboniferous formations and faunas of central Montana. Washington, U.S. Govt. Print. Off., 1961. iv, 126 p. illus., diagrs., tables. 29 cm. (U.S. Geological Survey. Professional paper 348) Part of illustrative matter folded in pocket. Bibliography: p. 101-108. 1. Paleontology Montana. 2. Paleontology Carboniferous. 3. Geology, Stratigraphic Carboniferous. I. Title. (Series) For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, B.C. CONTENTS Page Page Abstract-__________________________________________ 1 Faunal analysis Continued Introduction _______________________________________ 1 Faunal relations ______________________________ 22 Purposes of the study_ __________________________ 1 Long-ranging elements...__________________ 22 Organization of present work___ __________________ 3 Elements of Mississippian affinity.._________ 22 Acknowledgments--.-------.- ___________________
    [Show full text]
  • FORT BELKNAP RESERVATION List of Topics
    FORT BELKNAP RESERVATION List of Topics BACKGROUND Reservation Overview Regional Geologic Overview GEOLOGIC OVERVIEW Geologic History Summary of Play Types CONVENTIONAL PLAY TYPES Play 1 - Shallow Cretaceous Biogenic Gas Play Play 2 - Northern Plains Biogenic Gas Play Plays 3,4,5 - Jurassic/Cretaceous and Mississippian Plays UNCONVENTIONAL / HYPOTHETICAL PLAY TYPES Plays 6,7 - Fractured Bakken and Cambrian Sandstone Plays REFERENCES Historical Background of the OVERVIEW (i.e. joint ventures) in contrast to procedures and regulatory minimums imposed Assiniboine and Gros Ventre Tribes at Fort Belknap by the previous 1938 Minerals Leasing Act. The 1982 Act further provides that FORT BELKNAP RESERVATION The Fort Belknap Indian Reservation was created in 1887 as the home for the individual Indian allottees may join agreements negotiated for tribal lands. The Assiniboine and Gros Ventre Tribes Assiniboine and Gros Ventre Indian Tribes. The ancestors of these tribes have section entitled Operating Regulations discusses the procedures for obtaining lived on the northern plains for several centuries. The Assiniboine were allottee participance in the negotiated agreement. recognized by Europeans as part of the great Sioux Nation and speak a Siouan Principal components for the formal corporate proposal should include the TRIBAL HEADQUARTERS: Fort Belknap Agency, Montana language. However, their name is taken from a Chippewa word referring to area(s) of interest, type of contract, elaboration of proposed agreement terms, GEOLOGIC SETTING: Williston Basin "those who cook with stones." At some point in time the Assiniboine bands points of potential negotiation, diligence commitments (i.e. drilling), bonus broke with the traditional Sioux and allied themselves with the Cree.
    [Show full text]
  • TGI Strat Column 2009.Cdr
    STRATIGRAPHIC CORRELATION CHART TGI II: Williston Basin Architecture and Hydrocarbon Potential in Eastern Saskatchewan and Western Manitoba EASTERN MANITOBA PERIOD MANITOBA SUBSURFACE SASKATCHEWAN OUTCROP ERA glacial drift glacial drift glacial drift Quaternary Wood Mountain Formation Peace Garden Peace Garden Member Tertiary Member Ravenscrag Formation CENOZOIC Formation Goodlands Member Formation Goodlands Member Turtle Mountain Turtle Mountain Turtle Frenchman Formation Whitemud Formation Boissevain Formation Boissevain Formation Eastend Formation Coulter Member Coulter Member Bearpaw Formation Odanah Member Belly River “marker” Odanah Member Belly River Formation “lower” Odanah Member Millwood Member Lea Park Formation Millwood Member MONTANA GROUP Pembina Member Pembina Member Pierre Shale Pierre Shale Milk River Formation Gammon Ferruginous Member Gammon Ferruginous Member Niobrara Formation Chalky Unit Boyne Member Boyne Member Boyne Calcareous Shale Unit Member Carlile Morden Member Carlile upper Formation Morden Member Formation Morden Member Carlile Formation Assiniboine Marco Calcarenite Assiniboine Member Member CRETACEOUS Second White Specks Laurier Limestone Beds Favel Favel Keld Keld Member Member Formation Formation Belle Fourche Formation Belle Fourche Member MESOZOIC COLORADO GROUP Belle Fourche Member upper Fish Scale Formation Fish Scale Zone upper Base of Fish Scale marker Base of Fish Scale marker Westgate Formation Westgate Member lower Westgate Member Newcastle Formation Newcastle Member lower Viking Sandstone
    [Show full text]
  • Memorial to W.A. “Bill” Cobban (1916–2015) NEAL L
    Memorial to W.A. “Bill” Cobban (1916–2015) NEAL L. LARSON Larson Paleontology Unlimited, LLC, Keystone, South Dakota 57745, USA; [email protected] NEIL H. LANDMAN American Museum of Natural History, Division of Paleontology (Invertebrates), New York, New York 10024, USA; [email protected] STEPHEN C. HOOK Atarque Geologic Consulting, LLC, Socorro, New Mexico 87810, USA; [email protected] Dr. W.A. “Bill” Cobban, one of the most highly re- spected, honored and published geologist-paleontologists of all time, passed away peacefully in his sleep in the morning of 21 April 2015 at the age of 98 in Lakewood, Colorado. Bill was an extraordinary field collector, geologist, stratigrapher, biostratigrapher, paleontologist, and mapmaker who spent nearly his entire life working for the U.S. Geo- logical Survey (USGS). In a career that spanned almost 75 years, he fundamentally changed our understanding of the Upper Cretaceous Western Interior through its fossils, making it known throughout the world. William Aubrey “Bill” Cobban was born in 1916 near Great Falls, Montana. As a teenager, he discovered a dinosaur in the Kootenai Formation catching the attention of Barnum Brown, premier dinosaur collector at the American Museum of Natural History, where the dinosaur now resides. A few years later, as Bill told, he read about the discovery of fossil bones in Shelby, Montana, during excavation of the Toole County Courthouse. The bones turned out to actually be baculites and other iridescent ammonites. These ammonites made such an impression on Bill they would change his life forever. He attended Montana State University in 1936, where he met a geology professor who encouraged an already developing love for geology and paleontology and received his B.S.
    [Show full text]
  • Williston Basin Project (Targeted Geoscience Initiative II): Summary Report on Paleozoic Stratigraphy, Mapping and Hydrocarbon A
    Williston Basin Project (Targeted Geoscience Initiative II): Summary report on Paleozoic stratigraphy, mapping and GP2008-2 hydrocarbon assessment, southwestern Manitoba By M.P.B. Nicolas and D. Barchyn GEOSCIENTIFIC PAPER Geoscientific Paper GP2008-2 Williston Basin Project (Targeted Geoscience Initiative II): Summary report on Paleozoic stratigraphy, mapping and hydrocarbon assessment, southwestern Manitoba by M.P.B. Nicolas and D. Barchyn Winnipeg, 2008, reprinted with minor revisions January, 2009 Science, Technology, Energy and Mines Mineral Resources Division Hon. Jim Rondeau John Fox Minister Assistant Deputy Minister John Clarkson Manitoba Geological Survey Deputy Minister E.C. Syme Director ©Queen’s Printer for Manitoba, 2008, reprinted with minor revisions, January 2009 Every possible effort is made to ensure the accuracy of the information contained in this report, but Manitoba Science, Technol- ogy, Energy and Mines does not assume any liability for errors that may occur. Source references are included in the report and users should verify critical information. Any digital data and software accompanying this publication are supplied on the understanding that they are for the sole use of the licensee, and will not be redistributed in any form, in whole or in part, to third parties. Any references to proprietary software in the documentation and/or any use of proprietary data formats in this release do not constitute endorsement by Manitoba Science, Technology, Energy and Mines of any manufacturer’s product. When using information from this publication in other publications or presentations, due acknowledgment should be given to the Manitoba Geological Survey. The following reference format is recommended: Nicolas, M.P.B, and Barchyn, D.
    [Show full text]
  • 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.
    [Show full text]
  • Mississippian-Pennsylvanian Boundary Problems in the Rocky Mountain Region
    University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln USGS Staff -- Published Research US Geological Survey 7-1948 Mississippian-Pennsylvanian Boundary Problems In The Rocky Mountain Region James Steele Williams United States Geological Survey Follow this and additional works at: https://digitalcommons.unl.edu/usgsstaffpub Part of the Earth Sciences Commons Williams, James Steele, "Mississippian-Pennsylvanian Boundary Problems In The Rocky Mountain Region" (1948). USGS Staff -- Published Research. 502. https://digitalcommons.unl.edu/usgsstaffpub/502 This Article is brought to you for free and open access by the US Geological Survey at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USGS Staff -- Published Research by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. The Journal of Geology, Vol. 56, No. 4, Jul., 1948 MISSISSIPPIAN-PENNSYLVANIAN BOUNDARY PROBLEMS IN THE ROCKY MOUNTAIN REGION' JAMES STEELE WILLIAMS United States Geological Survey ABSTRACT A variety of paleontologic and stratigraphic problems are presented by rocks near the Mississippian- Pennsylvanian boundary in the central and northern Rocky Mountains. Stratigraphic sections of these rocks show diverse interpretations of fundamental concepts of stratigraphy and paleontology. In many places where Upper Mississippian rocks directly underlie Pennsylvanian rocks it is difficult to determine the precise location of the boundary between these units. Formations that straddle the boundary are very useful and satisfactory over large areas. Most geologists use various types of lithologic criteria to distinguish forma- tions, but some appear to rely mainly on faunal data, unconformities, or attempts to trace prominent beds. More uniformity in criteria than now exists for the delimitation of formations is desirable.
    [Show full text]
  • Cross-Section of Paleozoic Rocks of Western North Dakota
    JolfN P. BLOEMLE N. D. Geological Survey NORTH DAKOTA GEOLOGICAL SURVEY WILSON M. LAIRD, State Geologist Miscel1aneous Series No. 34 CROSS-SECTION OF PALEOZOIC ROCKS OF WESTERN NORTH DAKOTA BY CLARENCE G. CARLSON Reprinted from Stratigraphic Cross Section of Paleozoic Rocks-Oklahoma to Saskatchewan, 1967: The American Association of Petroleum Geologists Cross Section Publication 5, p. 13-15, 1 Plate Grand Forks, North Dakota, 1967 NORTH DAKOTAI (Section E-F. Plate 5) C. G. CARLSON' Grand Forks, North Dakota INTRODUCTION which, in ascending order, are the Black Island, Icebox, The North Dakota segment of the cross section was and Roughlock. The Black Island generally consists of constructed with the base of the Spearfish Formation as clean quartzose sandstone, the Icebox of greenish-gray, noncalcareous shale, and the Roughlock of greenish-gray the datum. However, the Permian-Triassic boundary to brownish-gray, calcareous shale or siltstone. now is thought to be within redbeds of the Spearfish The Black Island and Icebox Formations can be Formation (Dow, 1964). If this interpretation is cor­ traced northward to Saskatchewan, but they have not rect, perhaps as much as 300 ft of Paleozoic rocks in been recognized as formations there and are included in well 3 and smaller thicknesses in wells I, 2, and 4-12 an undivided Winnipeg Formation. The Black Island are excluded from Plate 5. pinches out southwestward because of nondeposition Wells were selected which best illustrate the Paleozo­ along the Cedar Creek anticline, but the Icebox and ic section and its facies changes in the deeper part of Roughlock Formations, although not present on the the Williston basin.
    [Show full text]