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South Dakota to Nebraska
Geological Society of America Special Paper 325 1998 Lithostratigraphic revision and correlation of the lower part of the White River Group: South Dakota to Nebraska Dennis O. Terry, Jr. Department of Geology, University of Nebraska—Lincoln, Lincoln, Nebraska 68588-0340 ABSTRACT Lithologic correlations between type areas of the White River Group in Nebraska and South Dakota have resulted in a revised lithostratigraphy for the lower part of the White River Group. The following pedostratigraphic and lithostratigraphic units, from oldest to youngest, are newly recognized in northwestern Nebraska and can be correlated with units in the Big Badlands of South Dakota: the Yellow Mounds Pale- osol Equivalent, Interior and Weta Paleosol Equivalents, Chamberlain Pass Forma- tion, and Peanut Peak Member of the Chadron Formation. The term “Interior Paleosol Complex,” used for the brightly colored zone at the base of the White River Group in northwestern Nebraska, is abandoned in favor of a two-part division. The lower part is related to the Yellow Mounds Paleosol Series of South Dakota and rep- resents the pedogenically modified Cretaceous Pierre Shale. The upper part is com- posed of the unconformably overlying, pedogenically modified overbank mudstone facies of the Chamberlain Pass Formation (which contains the Interior and Weta Paleosol Series in South Dakota). Greenish-white channel sandstones at the base of the Chadron Formation in Nebraska (previously correlated to the Ahearn Member of the Chadron Formation in South Dakota) herein are correlated to the channel sand- stone facies of the Chamberlain Pass Formation in South Dakota. The Chamberlain Pass Formation is unconformably overlain by the Chadron Formation in South Dakota and Nebraska. -
Petrology of Sandstones from the Bullion Creek and Sentinel Butte Formations (Paleocene), Little Missouri Badlands, North Dakota Mark A
University of North Dakota UND Scholarly Commons Theses and Dissertations Theses, Dissertations, and Senior Projects 1978 Petrology of sandstones from the Bullion Creek and Sentinel Butte Formations (Paleocene), Little Missouri Badlands, North Dakota Mark A. Steiner University of North Dakota Follow this and additional works at: https://commons.und.edu/theses Part of the Geology Commons Recommended Citation Steiner, Mark A., "Petrology of sandstones from the Bullion Creek and Sentinel Butte Formations (Paleocene), Little iM ssouri Badlands, North Dakota" (1978). Theses and Dissertations. 286. https://commons.und.edu/theses/286 This Thesis is brought to you for free and open access by the Theses, Dissertations, and Senior Projects at UND Scholarly Commons. It has been accepted for inclusion in Theses and Dissertations by an authorized administrator of UND Scholarly Commons. For more information, please contact [email protected]. PETROLOGY OF SANDSTONES FROM THE BULLION CREEK AND SENTINEL BUTTE FORNATIONS (PALEOCENE), LITTLE MISSOURI BADLANDS, NORTH DAKOTA by Mark A. Steiner Bachelor of Arts, College of St. Thomas, 1972 A Thesis Submitted to the Graduate Faculty of the University of North Dakota in partial fulfillment of the requirements for the degree of Master of Arts Grand Forks, North Dakota December 1978 This thesis submitted by Mark A. Steiner in partial fulfillment of the requirements for the Degree of Master of Arts from the University of North Dakota is hereby approved by the Faculty Advisory Committee under whom the work has been done. (Chairman) .// ' (r~· _j {~µ..~ Dean of the Graduate School 11 Permission PETROLOGY OF SANDSTONES FROM THE BULLION CREEK AND SENTINEL BUTTE FORMATIONS (PALEOCENE), Title------------'-'--=----~------------------- LITTLE MISSOURI BADLANDS, NORTH DAKOTA In presenting this thesis in partial fulfillment of the require ments for a graduate degree from the University of North Dakota, I agree that the Library of this University shall make it freely avail able for inspection. -
Basin-Margin Depositional Environments of the Fort Union and Wasatch Formations in the Buffalo-Lake De Smet Area, Johnson County, Wyoming
U.S. DEPARTMENT OF INTERIOR GEOLOGICAL SURVEY Basin-Margin Depositional Environments of the Fort Union and Wasatch Formations in the Buffalo-Lake De Smet area, Johnson County, Wyoming By Stanley L. Obernyer Open-File Report 79-712 1979 Contents Page Abstract 1 Introduction 5 Methods of investigation 8 Previ ous work - 9 General geol ogy 10 Acknowledgments 16 Descriptive stratigraphy of the Fort Union and Wasatch Formations 18 Fort Union Formation- 18 Lower member 20 Conglomerate member 21 Wasatch Formation 30 Kingsbury Conglomerate Member 32 Moncrief Member 38 Coal-bearing strata Wasatch Formation 45 Conglomeratic sandstone sequence 46 The Lake De Smet coal bed 53 Very fine to medium-grained sandstone sequence 69 Fossil marker beds 78 Environments of Deposition 79 General 79 Alluvial fan environment 82 Braided stream environments 86 Alluvial valley environments 89 Tectonics and Sedimentation 92 Conglomerates and tectonics- 92 Coals and tectonics 98 Conclusions 108 References 111 11 ILLUSTRATIONS Plates Plate 1. Bedrock geologic map of the Buffalo-Lake De Smet area, Johnson County, Wyoming In pocket 2. Geologic cross sections along the Bighorn Mountain Front, Buffalo-Lake De Smet area, Johnson County, Wyoming In pocket FIGURES Page Figure 1. Location map sh wing the major structural units surround ing the Powder River Basin, Wyoming and Montana 7 2. Composite geologic section of the rocks exposed in in the Buffalo-Lake De Smet area- 11 3. Generalized geologic map of the Powder River Basin 12 4. Isopach map of the Fort Union and Wasatch Formations, Powder River Basin, from Curry (1971) 14 5. Generalized stratigraphic column of the conglomerate sequences 19 6. -
Theodore Roosevelt National Park Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Natural Resource Program Center Theodore Roosevelt National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2007/006 THIS PAGE: The Little Missouri River flows near the Juniper Campground in the North Unit of Theodore Roosevelt NP, ND. ON THE COVER: View from the Oxbow Overlook Theodore Roosevelt NP, ND. Photos by: Dave Krueger Theodore Roosevelt National Park Geologic Resource Evaluation Report Natural Resource Report NPS/WASO/NRPC/GRD—2007/006 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Lakewood, Colorado 80225 June 2007 U.S. Department of the Interior Washington, D.C. The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer- reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly- published newsletters. -
Mannville Group of Saskatchewan
Saskatchewan Report 223 Industry and Resources Saskatchewan Geological Survey Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan J.E. Christopher 2003 19 48 Printed under the authority of the Minister of Industry and Resources Although the Department of Industry and Resources has exercised all reasonable care in the compilation, interpretation, and production of this report, it is not possible to ensure total accuracy, and all persons who rely on the information contained herein do so at their own risk. The Department of Industry and Resources and the Government of Saskatchewan do not accept liability for any errors, omissions or inaccuracies that may be included in, or derived from, this report. Cover: Clearwater River Valley at Contact Rapids (1.5 km south of latitude 56º45'; latitude 109º30'), Saskatchewan. View towards the north. Scarp of Middle Devonian Methy dolomite at right. Dolomite underlies the Lower Cretaceous McMurray Formation outcrops recessed in the valley walls. Photo by J.E. Christopher. Additional copies of this digital report may be obtained by contacting: Saskatchewan Industry and Resources Publications 2101 Scarth Street, 3rd floor Regina, SK S4P 3V7 (306) 787-2528 FAX: (306) 787-2527 E-mail: [email protected] Recommended Citation: Christopher, J.E. (2003): Jura-Cretaceous Success Formation and Lower Cretaceous Mannville Group of Saskatchewan; Sask. Industry and Resources, Report 223, CD-ROM. Editors: C.F. Gilboy C.T. Harper D.F. Paterson RnD Technical Production: E.H. Nickel M.E. Opseth Production Editor: C.L. Brown Saskatchewan Industry and Resources ii Report 223 Foreword This report, the first on CD to be released by the Petroleum Geology Branch, describes the geology of the Success Formation and the Mannville Group wherever these units are present in Saskatchewan. -
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 -
Eocene Vertebrates, Coprolites, and Plants in the Golden Valley Formation of Western North Dakota
GLENN L. JEPSEN Dept. Geology, Princeton University, Princeton, N. J. Eocene Vertebrates, Coprolites, and Plants in the Golden Valley Formation of Western North Dakota Abstract: An early Eocene date for the origin of this early Tertiary biofacies indicate warm, humid, the Golden Valley Formation in North Dakota is swampy lowlands with subtropical forests bordering confirmed by the discovery of fossil fish, amphib- sluggish streams. Montmorillonite in the formation ians, reptiles, birds, and mammals. Riparian and may represent ash from volcanoes to the west. aquatic animals and plants that were associated in CONTENTS Introduction 673 References cited 683 Acknowledgments 673 Salvinia preauriculata as an index fossil. 675 Figure Age of the Kingsbury Conglomerate. 676 1. Distribution of the Golden Valley Formation Naming of the Golden Valley Formation. 677 in part of Stark County, North Dakota . 674 Fossils of the Golden Valley Formation . 678 Vertebrates 678 Plate Facing Coprolites 680 1. Rocks and fossils of the Golden Valley Forma- Plants 681 tion, Stark County, North Dakota .... 676 "Hard Siliceous" layer 681 2. Vertebrate Coprolites from the Golden Valley Conclusions 682 Formation, Stark County, North Dakota . 677 faculty members and students from universities INTRODUCTION and other schools in Colorado, Connecticut, Recent discoveries of many fossil vertebrates Massachusetts, Montana, New Hampshire, in Stark County, western North Dakota, New Jersey, New York, North Dakota, Ohio, validate an early Eocene (Sparnacian, Wasatch- and South Dakota participated in a program of ian) age for the Golden Valley Formation prospecting for fossils and quarrying in the and extend the known geographic distribution Golden Valley beds on the margins of the of North American, early Eocene land- Little Badlands synclinal basin area southwest vertebrate faunas several hundred miles east- of Dickinson, North Dakota, in the Heart ward. -
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. -
The Stonewall Formation Timothy O
The Stonewall Formation Timothy O. Nesheim Introduction Geology The Stonewall Formation is one of numerous sedimentary strata The Stonewall Formation consists of three carbonate-evaporitic that have commercially produced oil and gas from North Dakota’s cycles deposited during Late Ordovician through Early Silurian subsurface. The Stonewall Formation is also one of many time (fig. 2). The Stonewall Formation is conformably under- geological formations being overshadowed by the prolific Bakken- lain by the Stony Mountain Formation and overlain by the In- Three Forks play. Interestingly, the first successful production terlake Formation. Each Stonewall cycle consists of three gen- test that recovered hydrocarbons (oil and gas) from the eral lithofacies: 1) bioturbated to laminated carbonate mudstone Stonewall Formation took place in 1952, less than a year after the 2) thin greyish green dolomitic and/or shaley, silty to sandy discovery of oil in North Dakota. However, sustained commercial mudstone, and 3) nodular to laminated anhydrite that is some- production from the Stonewall Formation did not take place for times interlaminated to interbedded with dolomite (fig. 3). another 27 years until 1979. Since then, the Stonewall Formation Deposition is interpreted to have taken place within a shallow has produced approximately 10 million barrels of oil equivalent marine (carbonate facies) to hypersaline (anhydrite facies) set- (MBOE) from 65 vertical wells (fig. 1). ting. The shaly sandy mudstone intervals have previously been Figure 1. Map depicting the extent of the Stonewall Formation and Stonewall productive wells in North Dakota (Carlson and Eastwood, 1962). For regulatory reasons the Stonewall Formation has been pooled together with the lower Interlake Formation. -
From Adam to Noah: a Reconsideration of the Antediluvian Patriarchs' Ages
JETS 37/2 (June 1994) 161!168 FROM ADAM TO NOAH: A RECONSIDERATION OF THE ANTEDILUVIAN PATRIARCHS' AGES R. K. HARRISON* The narrative material of Gen 5:3!32, which catalogued the ages of the principal descendants of Adam through the line of Seth, has long been a matter for debate, if only because of the apparently exaggerated lifespans attributed to the individuals listed there. Until the rise of rational Biblical criticism in the eighteenth century the lengthy ages were accepted much as they stood, out of deference to the sanc- tity of the divinely!revealed Hebrew tradition. But when literary critics dis- regarded the concepts of revelation and inspiration and began to treat the Hebrew Scriptures as nothing more than a collection of national records, of- ten of uncertain provenance and riddled with mythology, a vastly different set of interpretative criteria came to the forefront. Following certain European principles of literary criticism and influ- enced by the notion of supposed human biological evolution, the hypothe- sis developed by Julius Wellhausen (1844!1918) envisioned the growth of Biblical material from rudimentary beginnings until it attained its climax in the late postexilic period (about the second century BC). As far as the Pentateuch was concerned, this approach was worked out in great and of- ten conflicting detail, resulting in the recognition of four supposed basic literary components.1 The developed hypothesis was entirely subjective in nature and, as was the case with Darwin's evolutionary views, was entirely untroubled by the exercise of any objective control. Nevertheless external data began to ap- pear in the nineteenth century, and when archeological discoveries brought an entirely new perspective to bear upon ancient Near Eastern studies it became possible for literary!critical procedures to be scrutinized rigorously and to be shown to possess serious flaws in important areas. -
Silurian System in Eastern Montana
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1966 Silurian system in eastern Montana Frank Kendall Gibbs The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Gibbs, Frank Kendall, "Silurian system in eastern Montana" (1966). Graduate Student Theses, Dissertations, & Professional Papers. 9265. https://scholarworks.umt.edu/etd/9265 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. THE SILURIAN SYSTEM IN EASTERN MONTANA by Frank Kendall Gibbs Geological Bhgineer Colorado School Of Mines, 1955 Presented in partial fulfillment of the requirements for the degree of Master of Science U niversity of Montana 1966 Approved by: 1 Chairman, Board of Examiners Deary" Graduate School J A r r c '^’^ -7_____________ Date ( i ) UMI Number: EP40067 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. UMT Dissertation PuWisNng UMI EP40067 Published by ProOuest LLC (2013). Copyright in the Dissertation held by the Author. Microform Edition © ProOuest LLC. -
The Global Flood of Noah
THE GLOBAL FLOOD OF NOAH by Bert Thompson, Ph.D. DEDICATION This book is dedicated with deep appreciation to Joe and Beryl Nisbet, two “wee Scots” who, as husband and wife, have devoted their entire adult lives to teaching the Gospel in their native Scot- land and who, through their many personal sacrifices and exemplary conduct on behalf of the Lord and His church, have become such an endearing example for everyone around them. APOLOGETICS PRESS, INC. 230 Landmark Drive Montgomery, Alabama 36117-2752 © Copyright 1986 Revised Editions © Copyright 1999, 2005 ISBN: 0-932859-78-X All rights reserved. No part of this book may be reproduced in any form without permission from the publisher, except in the case of brief quotations embodied in articles or critical reviews. -i- TABLE OF CONTENTS CHAPTER 1 INTRODUCTION......................................................................1 Mankind’s Response to the Genesis Flood .....................................1 CHAPTER 2 THE FLOOD IN SCRIPTURE AND HISTORY....................5 The Importance of the Doctrine of the Global Flood ......................5 The Reason for the Flood................................................................6 Supernatural Elements of the Flood ................................................8 The Ubiquity of Flood Stories.........................................................9 CHAPTER 3 THE GLOBAL FLOOD OF NOAH.......................................11 The Antediluvian World ...............................................................11 The Necessity of Constructing