BLACKFEET RESERVATION List of Topics
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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. -
Modern Shale Gas Development in the United States: a Primer
U.S. Department of Energy • Office of Fossil Energy National Energy Technology Laboratory April 2009 DISCLAIMER This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe upon privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof. Modern Shale Gas Development in the United States: A Primer Work Performed Under DE-FG26-04NT15455 Prepared for U.S. Department of Energy Office of Fossil Energy and National Energy Technology Laboratory Prepared by Ground Water Protection Council Oklahoma City, OK 73142 405-516-4972 www.gwpc.org and ALL Consulting Tulsa, OK 74119 918-382-7581 www.all-llc.com April 2009 MODERN SHALE GAS DEVELOPMENT IN THE UNITED STATES: A PRIMER ACKNOWLEDGMENTS This material is based upon work supported by the U.S. Department of Energy, Office of Fossil Energy, National Energy Technology Laboratory (NETL) under Award Number DE‐FG26‐ 04NT15455. Mr. Robert Vagnetti and Ms. Sandra McSurdy, NETL Project Managers, provided oversight and technical guidance. -
Bakken – the Biggest Oil Resource in the United States?
Winter 2011 Oil & Natural Gas Program Newsletter Bakken – The Biggest Oil Resource in the United States? The announcement of the acquisition of large acreage positions in the Bakken play has become a fairly regular event. Leasing activity in the Bakken has exploded over the last five years and bonus payments per acre CONTENTS have jumped. Total lease bonus payments exceeded $100 million in 2009 (Figure 1). Bakken – The Biggest Oil Resource in the United States? ...1 The heightened acquisition activity is driven by the Bakken’s immense potential. In 2008, the United States Geological Survey (USGS) estimated Commentary ...................................2 that the U.S. portion of the Bakken formation contains between 3 and 4.3 Successful Oil Production in billion barrels (a mean of 3.63 billion barrels) of undiscovered, recoverable the Bakken Formation .................6 oil, ranking it among the very largest U.S. oil plays. The Bakken—An Unconventional Petroleum The number of producing wells and Reservoir System ................9 and volume of oil production has Crude Souring in the Bakken ....11 grown with the growth in leasing and drilling (Figure 2). Production Geomechanical Study has reached nearly 8 million barrels of the Bakken .................................13 per month from roughly 4500 Bakken Requires Outlet for producing wells. Increased Production ................. 16 E&P Snapshots ............................ 18 The Bakken Formation Upcoming Meetings and The Bakken petroleum system is Presentations ............................... 20 part of a larger depositional system CONTACTS laid down in the Williston Basin during the Phanerozoic period with Roy Long Figure 1: Lease payments in North Dakota’s portion sediments up to 16,000 feet thick. -
Evolution of Oil Production in the Bakken Formation
EvolutionEvolution ofof OilOil ProductionProduction inin thethe BakkenBakken FormationFormation JulieJulie A.A. LeFeverLeFever NorthNorth DakotaDakota GeologicalGeological SurveySurvey PlaysPlays ofof thethe BakkenBakken FormationFormation ¾¾ ConventionalConventional BakkenBakken (pre(pre--1987)1987) ¾¾ CycleCycle 11 –– AntelopeAntelope StructureStructure (1950s(1950s –– 60s)60s) ¾¾ CycleCycle 22 –– DepositionalDepositional EdgeEdge (1970s(1970s –– 80s)80s) ¾¾ HorizontalHorizontal DrillingDrilling ofof thethe BakkenBakken ShaleShale (post(post--1987)1987) ¾¾ HorizontalHorizontal DrillingDrilling ofof thethe BakkenBakken MiddleMiddle MemberMember (2001(2001 toto present)present) ConventionalConventional BakkenBakken CycleCycle 11 –– AntelopeAntelope FieldField ¾¾DiscoveryDiscovery WellWell ¾¾ StanolindStanolind -- #1#1 WoodrowWoodrow StarrStarr ¾¾ InitialInitial PotentialPotential (536(536 BO;BO; 0.10.1 BW)BW) ¾¾ AntelopeAntelope FieldField ¾¾ 5252 wells;wells; 12.512.5 millionmillion BO;BO; 1010 BCFBCF GasGas ¾¾ ““SanishSanish SandSand”” ¾¾ CompletionCompletion MethodMethod Conventional Bakken Exploration between Cycles ¾¾ElkhornElkhorn RanchRanch ¾¾ ShellShell OilOil Co.Co. -- #41X#41X--55--11 GovernmentGovernment ¾¾NessonNesson AnticlineAnticline ¾¾ #1#1 B.E.B.E. HoveHove ¾¾ IPIP -- 756756 BOPD,BOPD, 33 BWPDBWPD ¾¾ CompletionCompletion MethodMethod ConventionalConventional BakkenBakken CycleCycle 22 –– DepositionalDepositional LimitLimit ¾¾StratigraphyStratigraphy && StructureStructure ¾¾ ThinThin BakkenBakken ¾¾ MultipleMultiple PaysPays -
Vocabulary • 1895 Agreement – in 1895, the Blackfeet Indians and Representatives of the United States Agreed That the United States Could Purchase Land from the Tribe
Vocabulary • 1895 Agreement – In 1895, the Blackfeet Indians and representatives of the United States agreed that the United States could purchase land from the tribe. This agreement was ratified (made official) by Congress in 1896, and the land eventually became the eastern half of Glacier National Park. Not all of the Blackfeet signed the agreement, however, and members of the tribe have disputes with the U.S. government concerning certain provisions (conditions) within the Agreement. See “Ceded Strip.” • Agricultural activities - Related to producing crops or livestock and other domestic animal products for sale or use. • Allotment - Something given out in portions. • Alpine Meadow - Type of habitat above tree line with short summers, long winters, and composed mainly of grasses and wildflowers. • Avalanche - A large mass of snow or ice that suddenly falls from a mountain slope. • Bergschrund - A deep crack near the head of a mountain glacier. • Bison (buffalo) - Bison are part of the family Bovidae, to which Asian buffalo, African buffalo and domestic cattle and goats belong. Because American bison resembled in some ways old world buffalo (Asian and African buffalo), early explorers to North America began to call them buffalo. The name buffalo is still used interchangeably with bison. • Blackfeet – The Blackfeet are a group of tribes in the United States and Canada, including the Piegan/Pikuni, Blood/Kainai, Blackfoot, and Siksika. Today these bands or tribes have reserved lands in Montana and Canada, but recently their historical homeland included northern Montana east of the Continental Divide and south-central Alberta. Many Blackfeet tribal members have been part of Glacier Park’s activities since its beginning. -
Blackfeet Nation Fish and Wildlife
About Us BFW Home Blackfeet Fish and Wildlife Contact Us Directions Free Info Permits Resources 2009 - 2010 RECREATIONAL ACTIVITY Big Game Hunts A. Camping. Camping, other than camping on private lands with the owner or occupant's permission, is permitted only at designated privately owned or tribally owned campsites. The following regulations shall be followed at tribally owned campgrounds: Recreational Activity • Care of Property. The defacement or destruction of signs, tables, or Fishing Regulations improvements is prohibited. • Vehicles. All wheeled vehicles, including trailers, must be kept on Code of Regulations the designated campsite parking areas. • Firewood. Only dead and downed wood in designated areas may Licensed Outfitters be gathered for firewood. Campers should check with the campgound manager to locate these areas. Bundles of firewood may be purchased Non Tribal Members at or near concessionaire facilities. • Disturbance of Plant or Animal Life. Plants or animals shall not be Map of Reservation disturbed in any way. The driving of nails into trees or the stripping of bark, leaves or branches from trees or shrubs is prohibited. Land Use • Digging. The natural terrain shall not be altered in any way. The leveling of the ground or digging for any purpose is prohibited. Fishing Report • Dogs, Cats and Pets. All dogs, cats, or other pets must be kept on a leash or under physical restrictive control at all times while in a Director's Update campgound. • Draining and Refuse from Trailers. Trailer owners must provide Photo Gallery receptacles to contain waste water. Such water shall be disposed of only at public restrooms, at holding tank disposal units in major camgrounds, or at tribally owned disposal units for a fee. -
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---------------------------------------- -
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. -
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. -
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--.-------.- ___________________ -
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. -
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