DOCSLIB.ORG

Archaeological Investigations at the Atigun Site, Central Brooks Range, Alaska

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Archaeological Investigations at the Atigun Site, Central Brooks Range, Alaska ARCHAEOLOGICAL INVESTIGATIONS AT THE ATIGUN SITE, CENTRAL BROOKS RANGE, ALASKA IAN ROBERT WILSON B.A. University of British Columbia 1968 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of Archaeology @ IAN ROBERT WILSON, 1977 SIMON FRASER UNIVERSITY April, 1977 All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without permission of the author. APPROVAL Name: Ian Robert Wilson Degree: Master of Arts (Archaeology) Title of Thesis: Archaeological Investigations at the Atigun Site, Central Brooks Range, Alaska. Examining Committee Chairman: Philip M. Hobler Herbert L. Alexander, Jr. Senior Supervisor Knut R. Fladmark '~enryS. Sharp Assistant Professor External Examiner Department of Sociology and Anthropology Simon Fraser University Date Approved April 12, 1977 PARTIAL COPY RIGHT LICENSE I hereby grant to Simon Fraser University the right to lend my thesis or dissertation (the title of which is shown below) to users of the Simon Fraser University Library, and to make partial or sing1 e copies only for such users or in response to a request from the library of any other university, or other educational institution, on its own behalf or for one of its users. I further agree that permission for mu1 tiple copying of this thesis for scholarly purposes may be granted by me or the Dean of Graduate Studies. It is understood that copying or publication of this thesis for financial gain shall not be allowed wi thout my wri tten permi ssi on, Title of Thesis/Dissertation : Archaeological Investigations at the Atigun Site, Central Brooks Range, Alaska. Author : (signature) Ian Robert Wilson (name) April 12, 1977 (date) ABSTRACT This thesis is an archaeological analysis of the Atigun site and is based on work conducted in 1973 and 1974 on the North Slope of the Central Brooks Range, Alaska. The excava- tions add significant information concerning the later pre- history and subsistence activities of the area. The site consisted of a series of discrete occupation levels containing faunal and lithic debris scattered around a hearth. The primary concern of analysis is the cultural af- filiation of the occupations, and to this end, artifacts, chipping debris and faunal remains are examined. Site activ- ities are discussed in detail using the results of this analysis. Because the site is historically and archaeolog- ically marginal to both Indian and Eskimo territory, ethno- graphic accounts of both groups are given to aid in the identification of its prehistoric inhabitants. Archaeolog- ical comparisons are made with sites in Alaska, the Yukon, the Northwest Territories and B.C. A re-evaluation of the prehistory of the Central Brooks Range is outlined, based on recent archaeological work and the results of the new data reported in this thesis. Conclusions point to a late summer occupation of the site by Athapascans probably seeking ground squirrel hides. The site was occupied seasonally between A.D. 1400-1800, and iii / represents a major late-prehistoric Indian incursion through- out the Brooks Range. This period is defined as the Kavik Phase. Finally, it is suggested that boundaries between Indians and Eskimos in the Central Brooks Range have period- ically shifted through time, largely due to environmental factors. ACKNOWLEDGEMENTS Many people contributed in significant ways to the com- pletion of this thesis. I would first like to thank both the Arctic Institute of North America and the Society of Sigma Xi for providing funds for the fieldwork. Dr. John Cook, Mike Kunz and Dale Slaughter all helped with logistic support, as did the Alyeska Pipeline Service Company. My thanks to Jean Williams for her help with my more difficult faunal identifications. Thanks also to Brian Seymour for his excellent artifact drawings. Dr. H. L. Alexander introduced me to the joys of Arctic fieldwork and goaded me through analysis while serving as my senior supervisor. Dr. Alexander generously granted his per- mission to excavate the Atigun site and allowed me free access to his collections. I would also like to express my apprecia- tion to Dr. K. R. Fladmark for his many insightful suggestions in the preparation of this manuscript. In particular, Dr. Fladmark was very helpful in the editing of this thesis. My appreciation also goes to Dr. R. Casteel who read my chapter on faunal remains and provided critical comments. Finally, I would like to express my gratitude to Jane Warner for her considerable input to this thesis. Jane expertly drafted the illustrations, cut through many knots in my tangled prose and continually forced me to refine my ideas. She sup- plied the encouragement and confidence that allowed the comple- tion of this thesis. v TABLE OF CONTENTS Chapter Page THE CONTEXT OF RESEARCH .......................... Introduction................................... Physiography and Climate ....................... Palaeoenvironment.............................. Flora and Fauna ................................ History of the Area ............................ Ethnography .................................... 1 . Nunamiut ................................. 2 . Kutchin .................................. 3 . Nunamiut-Athapascan Relationships........ Summary of Archaeological Investigations....... The Archaeological Sequence .................... THE SITE ......................................... Location ....................................... ~escription.................................... Previous Archaeological Research ............... Research Aims .................................. Sampling and Excavation Procedure .............. Recording of Cultural Material ................. 3 . EXCAVATION ....................................... Location of Excavation Units ................... Stratigraphy ................................... Soils .......................................... 1 . Physical Tests ........................... 2 . Chemical Tests ........................... Features ....................................... 1 . Frost cracks ............................. 2 . Hearths .................................. 4 . FAUNAL REMAINS ................................... 66 Techniques of Recovery and Analysis ............ 66 1 . Recovery ................................. 66 2 . The Sample ............................... 67 vi Chapter Page 3 . Techniques of Analysis. .................... 67 4 . Aims of Analysis ........................... 69 2' Number of Individuals............................ 70'- Seasonality...................................... 76k Length of Occupation ............................. 79 Bone ~istributions............................... 83 Butchering Patterns.............................. 91 Conclusions ......................................103 5 . CHIPPING DEBRIS ....................................108 /'/ ' Types ............................................ 109" Methodology ......................................111 Results and Discussion........................... 113 1 . Raw Material ...............................113 2 . Unmodified Debitage ........................114" / 3 . Modified Debitage ..........................120 5.- Distributions.................................... 127 Sumary.......................................... 128 6 . TOOLS AND MISCELLANEOUS ITEMS ......................130 Lithic Tools ..................................... 130 A . Formed Unifaces ............................131 k' B . Bifaces .................................... 133 1 . Rough Bifaces ........................ 133 2 . Biface Fragments .....................134 3 . Finished Bifaces .....................139, Bone Tools .......................................14 3 A . Piercing Implements........................ 146 1 . Unbarbed Points ...................... 146 2 . Awls .................................152 3 . Needles ..............................154 B . Miscellaneous Bone Implements.............. 154 1 . Antler Rectangles ....................154 2 . Other ................................155 Miscellaneous Items .............................. 158 . Distribution of Tools ............................158 vii Chapter Page 7 . DISCUSSION ...................................... 163 Nature of the Site ............................ 163 1 . Type of Site ............................ 163+-.v' 2 . Dating the Atigun Locality .............. 166 3 . Similarities Among Occupations .......... 168 Archaeological Comparisons .................... 178t[r'l' 1 . Alaska .................................. 178 2 . Yukon Territory ......................... 182 3 . Northwest Territories ................... 185 4 . British Columbia ........................ 186 5 . Summary ................................. 186 Definition of Kavik ........................... 187 1 . Artifacts.. ............................. 187 2 . Activities .............................. 189 3 . Dating .................................. 190 4 . Cultural Affiliations ................... 192 5 . Conclusions ............................. 194 8 . CONCLUSIONS ..................................... 200 The Archaeological Sequence Re.examined ..... 200 Environmental Effects on Culture ............ 205 Problems for Future Research ................ 208 REFERENCES CITED ........................................ viii LIST OF TABLES Table Page Location of soil samples ......................... 51 Mean. sorting co.efficient. skewness and kurtosis of soil samples ....................... 53 Soil samples : sphericity measures ..............
Load more

Recommended publications
  • A Trip to Alaska's Brooks Range Is the Trip of a Lifetime. You’Ll See Herds of Caribou Migrating Like They Have for Thousands of Years
    Hunt ID: AK-GBearMooseCaribou-Rifle-Kotzebue-AKO-Wayne A trip to Alaska's Brooks Range is the trip of a lifetime. You’ll see herds of caribou migrating like they have for thousands of years. If you feel comfortable you can take an outfitted semi-guided Caribou Hunt for the largest member of the caribou family, the barren ground caribou. Grizzly bear are often seen splashing after salmon in the river or foraging for berries on the tundra. Moose and other wildlife, including black bears, wolverine, and wolves are seen not far from camp often. He has been hunting in this area for over 40 years and guiding for over 20 years. His son’s adult sons assist with running the camp and guiding. They have both grown up hunting in the area and pride themselves with providing you a hunt of a life time. The enormous size of the big game animals has much to do with their location so far north they must have hung bulk to withstand the long cold winter. The camp is located above the Arctic Circle, in the Squirrel River Valley of the western Brooks Range. Clients fly into the Inupiaq village of Kotzebue where they board small bush planes for the 80 mile trip to the hunting area. Base camps consist of comfortable free standing Hansen Weatherport tents with cots and heaters, including a shower tent. The main tent is a cooking area and gathering point for discussing the days hunt. Cooking is provided by the staff using a modern 4 burner gas stove with oven.
    [Show full text]
  • New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island Area and Brooks Range, Alaska
    Geologica Acta, Vol.12, Nº 1, March 2014, 29-52 DOI: 10.1344/105.000002074 New Late Carboniferous Heritschioidinae (Rugosa) from the Kuiu Island area and Brooks Range, Alaska J. FEDOROWSKI1 C.H. STEVENS2 E. KATVALA3 1Institute of Geology, Adam Mickiewicz University Makow Polnych 16, PL-61-606, Poznan, Poland. E-mail: [email protected] 2Department of Geology, San Jose Unversity San Jose, California 95192, USA. E-mail: [email protected] 3Department of Geology, University of Calgary Calgary, Canada. E-mail: [email protected] ABS TRACT Three new species of the genus Heritschioides, i.e., H. alaskensis sp. nov., H. kuiuensis sp. nov., and H. splendidus sp. nov., and Kekuphyllum sandoense gen. et sp. nov. from the northeastern Kuiu Island area and nearby islets, part of Alexander terrane in southeastern Alaska, and Heritschioides separatus sp. nov. from the Brooks Range, Alaska, are described and illustrated. The three new fasciculate colonial coral species from the Kuiu Island area, collected from the Moscovian Saginaw Bay Formation, are phylogenetically related to those of probable Bashkirian age in the Brooks Range in northern Alaska as shown by the presence of morphologically similar species of Heritschioides. These corals from both areas also are related to one species in the Quesnel terrane in western Canada. Kekuphyllum sandoense from the Saginaw Bay Formation of the Kuiu Island area is the only cerioid-aphroid species within the Subfamily Heritschioidinae described so far. The complete early ontogeny of a protocorallite is for the first time described here on a basis of H. kuiuensis sp. nov. and compared to the hystero-ontogeny in order to show similarities and differences in those processes.
    [Show full text]
  • History of Moose in Northern Alaska and Adjacent Regions
    History of Moose in Northern Alaska and Adjacent Regions ] OHN W. COADY Alaska Department of Fish and Game, 1300 College Road, Fairbanks, Alaska 99701 Coady, John W. 1980. History of Moose in northern Alaska and adjacent regions. Canadian Field-Naturalist 94(1): 61 - 68. Moose (Alces alces) have occurred in northern Alaska since the late 1800s. Before the 1920s most Moose were probably immigrants from more southern latitudes. Breeding populations became established during the 1920s in the eastern portion of the region, and during the 1950s and 1960s in the western portion. Weather, habitat, and predation were probably not limiting factors to Moose in northern Alaska during the late 1800s and early 1900s. Temporary cessation of most hunting in northern Alaska and growth of Moose populations south of the region by 1920 were probably the most important factors promoting dispersal to, and increase in Moose numbers in, northern Alaska. Key Words: Moose, Alces alces, northern Alaska, historical account. Moose (Alces alces) are holarctic in distribution (Rausch 1963), having emigrated from Siberia across Study Area the Bering land bridge to unglaciated refugia in Northern Alaska is considered here as that portion Alaska during the early Rancholabrean Age (Illinoian of Alaska from the crest of the Brooks Range north to glaciation) (Pewe and Hopkins 1967). Both the pollen the Arctic Ocean (Figure 1). The region is divided into record (Colinvaux 1964) and the boreal nature of three physiographic provinces (Wahrhaftig 1965). mammals dispersing across the Bering land bridge The Brooks Range province consists of rugged moun­ (Repenning 1967) suggest that tundra and open steppe tains from 1200- 1500 m elevation in the west to conditions have prevailed in the Bering Strait region 2100- 2400 m elevation in the east.
    [Show full text]
  • Aerial Moose Survey in Upper Game Management Unit 24, Alaska
    AERIAL MOOSE SURVEY IN UPPER GAME MANAGEMENT UNIT 24, ALASKA, FALL 2004, INCLUDING STATE LAND, AND LANDS ADMINISTERED BY THE BUREAU OF LAND MANAGEMENT, GATES OF THE ARCTIC NATIONAL PARK AND PRESERVE, AND KANUTI NATIONAL WILDLIFE REFUGE Project Report: NPS/AR/NR/TR-2006-55 Prepared by: James P. Lawler, National Park Service Lisa Saperstein, U.S. Fish and Wildlife Service Tim Craig, Bureau of Land Management Glenn Stout, Alaska Department of Fish and Game April 2006 Photo: G. Stout The Alaska Department of Fish and Game, Division of Wildlife Conservation's mission is to conserve and enhance Alaska's wildlife and habitats and provide for a wide range of public uses and benefits. The Division of Wildlife Conservation recognizes wildlife as a public trust belonging to all Alaskans. We respect the diversity of public values associated with wildlife and support uses that reflect public support and sound principles of conservation. We are an organization of individuals committed to interacting professionally with one another and the public and to using scientific data and public input to conserve Alaska's wildlife. The Bureau of Land Management is directed by Congress in the Federal Land Policy and Management Act of 1976 to manage public lands “in a manner that will protect the quality of scientific, scenic, historical, ecological, environmental, air and atmospheric, water resources, and archeological values; that where appropriate, will preserve and protect certain public lands in their natural condition, that will provide food and habitat of fish and wildlife and domestic animals, and that will provide for outdoor recreation and human occupancy and use;” (Sec.101.[43 us.s.c.1701] (a) (8)).
    [Show full text]
  • Late Carboniferous Colonial Rugosa (Anthozoa) from Alaska
    Geologica Acta, Vol.12, Nº 3, September 2014, 239-267 DOI: 10.1344/GeologicaActa2014.12.3.6 Late Carboniferous colonial Rugosa (Anthozoa) from Alaska J. FEDOROWSKI1 and C.H. STEVENS2 1Institute of Geology, Adam Mickiewicz University Maków Polnych 16, PL-61-606, Poznań, Poland. E-mail: [email protected] 2 Department of Geology, San José University San José, California 95192, USA. E-mail: [email protected] ABS TRACT Late Carboniferous colonial corals from the Moscovian Saginaw Bay Formation and the underlying Bashkirian crinoidal limestone exposed on northeastern Kuiu Island and a nearby islet, part of the Alexander terrane in southeastern Alaska, are described and illustrated for the first time, and are supplemented by revision, redescription and reillustration of most Atokan specimens from Brooks Range, northern Alaska, first described by Armstrong (1972). New taxa from the Kuiu Island area include the new species Paraheritschioides katvalae and the new genus and species Arctistrotion variabilis, as well as the new Subfamily Arctistrotioninae. The corals Corwenia jagoensis and Lithostrotionella wahooensis of Armstrong (1972) also are redefined and redescribed. Paraheritschioides jagoensis is based on the holotype of ‘C’. jagoensis. P. compositus sp. nov. is based on a “paratype” of ‘C.’ jagoensis. In addition to a redefinition and redescription of ‘L.’ wahooensis as Arctistrotion wahooense, one “paratype” of that species is described as A. simplex sp. nov. The phylogeny and suspected relationships of some fasciculate Carboniferous Rugosa also are discussed. Based on relationships and similarities within the Late Carboniferous colonial Rugosa from the Brooks Range, Kuiu Island and the eastern Klamath terrane, we conclude that all three areas were geographically close enough at that time so that larvae were occasionally dispersed by oceanic currents.
    [Show full text]
  • A Thermal History of Permafrost in Alaska
    Permafrost, Phillips, Springman & Arenson (eds) © 2003 Swets & Zeitlinger, Lisse, ISBN 90 5809 582 7 A thermal history of permafrost in Alaska T.E. Osterkamp Geophysical Institute, University of Alaska, Fairbanks, Alaska, USA ABSTRACT: There has been a widespread warming of air temperatures in Alaska since 1977 and some warm- ing of permafrost. Constant or cooling permafrost temperatures followed this in the early 1980s, probably due to thin snow covers and a short cooling trend. Permafrost temperatures along a north south transect from Prudhoe Bay to Gulkana and at other sites have generally warmed since the late 1980s, initially in response to thicker snow covers. The warming north of the Brooks Range is comparable in magnitude to the century long warming there (2 to 4°C). The trend has not been followed at Eagle and the Yukon River bridge. Warming of the discontinuous permafrost is typically ½ to 1½°C. Thin discontinuous permafrost is thawing at the base at a rate of 0.04 m per year at one site. New thermokarst and thawing permafrost have been observed at several sites. 1 INTRODUCTION the permafrost thus implicating changes in snow cover or perhaps an earlier warming. Current information on permafrost suggests that, dur- Some evidence indicates that the discontinuous per- ing the last ice age, the occurrence, distribution and mafrost in Alaska warmed coincident with warming air thickness of terrestrial permafrost increased and, with temperatures since the “little ice age”. Air temperatures low sea levels, thick permafrost formed in the exposed at stations throughout mainland Alaska are correlated continental shelves of the Arctic and Antarctic Oceans.
    [Show full text]
  • Environmental and Cultural Overview of the Yukon Flats Region Prepared By: Kevin Bailey, USFWS Archaeologist Date: 2/12/2015 In
    Environmental and Cultural Overview of the Yukon Flats Region Prepared by: Kevin Bailey, USFWS Archaeologist Date: 2/12/2015 Introduction With a substantial population of Native people residing in their traditional homeland and living a modern traditional lifestyle, the Yukon Flats Refuge and all of the Alaskan Interior is a dynamic and living cultural landscape. The land, people, and wildlife form a tight, interrelated web of relationships extending thousands of years into the past. Natural features and human created “sites” form a landscape of meaning to the modern residents. The places and their meanings are highly relevant to modern residents, not just for people and culture but for the land. To many Gwich’in people culture is not distinct from their homeland. Although only minimally discussed in this overview, this dynamic living cultural landscape should be considered and discussed when writing about this area. Environmental Setting Containing the largest interior basin in Alaska, the Yukon Flats Refuge encompasses over 11 million acres of land in east central Alaska. Extending roughly 220 miles east-west along the Arctic Circle, the refuge lies between the Brooks Range to the north, and the White-Crazy Mountains to the south. The pipeline corridor runs along the refuge’s western boundary while the eastern boundary extends within 30 miles of the Canadian border. The Yukon River bisects the refuge, creating the dominant terrain. As many as 40,000 lakes, ponds, and streams may occur on the refuge, most concentrated in the flood plain along the Yukon and other rivers. Upland terrain, where lakes are less abundant, is the source of important drainage systems.
    [Show full text]
  • Arctic Alaska
    Carboniferous Biostratigraphy, Northeastern Brooks Range, Arctic Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 884 Carboniferous Biostratigraphy, Northeastern Brooks Range, Arctic Alaska By AUGUSTUS K. ARMSTRONG, U.S. Geological Survey, and BERNARD L. MAMET, University of Montreal, Montreal, Canada GEOLOGICAL SURVEY PROFESSIONAL PAPER 884 Eleven microfossil assemblage zones are recognized in two sections of Carboniferous rocks in the northeastern Brooks Range, correlated with six other previously described sections, and tied to the Cordilleran and Eurasian standards UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON :1975 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress Cataloging in Publication Data Armstrong, Augustus K. Carboniferous Biostratigraphy, northeastern Brooks Range, Arctic Alaska. (Geological Survey Professional Paper 884) Bibliography: p. 23-25. Includes index. Supt. of Docs. No.: I 19.16:884 1. Geology, Stratigraphic-Carboniferous. 2. Micropaleontology-Alaska-Brooks Range. 3. Stratigraphic correlation­ Alaska-Brooks Range. I. Mamet, Bernard L., joint author. II. Title. III. Series: United States. Geological Survey. Professional Paper 884. QE67l.A7 557.3'08s [551.7'5] 75-619053 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Stock Number 024-001-02667-8 CONTENTS Page Page 1\bstract -------------------------------------------------- 1 Kongakut River section------------------------------------
    [Show full text]
  • Foundation Document Overview, Gates of The
    NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Gates of the Arctic National Park and Preserve Alaska Contact Information For more information about the Gates of the Arctic National Park and Preserve Foundation Document, contact: [email protected] or (907) 457-5752 or write to: Superintendent, Gates of the Arctic National Park and Preserve, 4175 Geist Road, Fairbanks, AK 99709 Purpose Significance and Fundamental Resources and Values Significance statements express why Gates of the Arctic National Park and Preserve resources and values are important enough to merit national park unit designation. Statements of significance describe why an area is important within a global, national, regional, and systemwide context. These statements are linked to the purpose of the park unit, and are supported by data, research, and consensus. Significance statements describe the distinctive nature of the park and inform management decisions, focusing efforts on preserving and protecting the most important resources and values of the park unit. Fundamental resources and values are those features, systems, processes, experiences, stories, scenes, sounds, smells, or other attributes determined to merit primary consideration during planning and management processes because they are essential to achieving the purpose of the park and maintaining its significance. © Carl Johnson Wilderness: Gates of the Arctic National Park and Preserve is acknowledged as the premier wilderness park in the national park system, protecting 8.4 million acres of diverse arctic ecosystems. • Designated Wilderness • Wilderness Character The purpose of Gates of the Arctic • Diverse Arctic Ecosystems National Park and Preserve is to • Science in Wilderness preserve the vast, wild, undeveloped • Unique Geological Features character and environmental integrity • Contiguous Wilderness of Alaska’s central Brooks Range and to provide opportunities for wilderness recreation and traditional subsistence uses.
    [Show full text]
  • Geophysical Characterization of Pre-Cenozoic Basement for Hydrocarbon Assessment, Yukon Flats, Alaska
    U.S. Department of the Interior U.S. Geological Survey Geophysical Characterization of Pre-Cenozoic Basement for Hydrocarbon Assessment, Yukon Flats, Alaska By R.W. Saltus1 ([email protected]), J.D. Phillips1 ([email protected]), R.G. Stanley2 ([email protected]), A. Till3 ([email protected]), and R.L. Morin2 ([email protected]) 1 Denver, Colorado, 2 Menlo Park, California, 3 Anchorage, Alaska Open-File Report 2007-1208 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ 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. This publication has not been reviewed for stratigraphic nomenclature. 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. Suggested citation: Saltus, R.W., Phillips, J.D., Stanley, R.G., Till, A., Morin, R.L., 2007 Geophysical Characterization of Pre-Cenozoic Basement for Hydrocarbon Assessment, Yukon Flats, Alaska: Open-File Report 2007-1208, 1 plate. Abstract The Cenozoic basins of interior Alaska are poorly understood, but may host undiscovered hydrocarbon resources in sufficient quantities to serve remote villages and for possible export. Purported oil seeps and the regional occurrence of potential hydrocarbon source and reservoir rocks fuel an exploration interest in the 46,000 km2 Yukon Flats basin. Whether hydrocarbon source rocks are present in the pre-Cenozoic basement beneath Yukon Flats is difficult to determine because vegetation and surficial deposits obscure the bedrock geology, only limited seismic data are available, and no deep boreholes have been drilled.
    [Show full text]
  • The Dalton Highway
    Te DaDallHtt ooi g nnh w a y Visitor Guide Road Conditions . pages 6-7 Points of Interest . .page 8 Bear Safety . .page 16 Contents Ultimate Road Adventure Trip Planning The Dalton Highway is a rough, industrial road that begins 84 miles/134 km north of Fairbanks and ends 414 miles/662 km later in 4 Preparing and Safety Deadhorse, the industrial camp at Prudhoe Bay. It provides a rare 6 Mileage Chart opportunity to traverse a remote, unpopulated part of Alaska to the 11-14 Maps very top of the continent. Traveling this farthest-north road involves real risks and challenges. This publication will help you decide 23 Planning Your Trip whether to make the journey, how to prepare, and how to enjoy your experience. Please read this information carefully. Exploring Know Before You Go 8-11 Points of Interest • There is no public access to the Arctic Ocean from Deadhorse. 15 An Icebound Land You must be on an authorized tour. Call toll-free 1-877-474-3565; 17 Watching Wildlife in Fairbanks, 474-3565. 18 Recreation • There are no medical facilities between Fairbanks and Deadhorse, a distance of 500 miles/800 km. For emergency information, see the back page. Facilities and Services • Food, gas, and vehicle repair service are extremely limited. 5 Visitor Centers See page 5. 18 Campgrounds • There is limited cell phone service and public Internet connection between Fairbanks and Deadhorse. The Dalton Highway BLM Coordinator: Kelly Egger Contributors: Eugene Ervine, Lenore Heppler, Lisa Shon Jodwalis, Craig McCaa, Pam Rice. John Rapphahn, Crystal Glassburn, Jason Oles, Jason Post Produced and Designed by All photos courtesy of the BLM unless otherwise noted.
    [Show full text]
  • Alaska 2020 Peninsula & Brooks Range
    Alaska 2020 Peninsula & Brooks Range Hunting in Alaska A hunt with our Partner Mountain Monarchs of Alaska LLC is a once in a lifetime true Alaska wilderness experience. We will take you to the heart of Big Game Country, where you will stay in remote wilderness camps. Our Partner offer several different hunting experiences including Spring and Fall Brown Bear, Arctic Grizzly, Dall Sheep, Caribou and Moose. There are often opportunities to fish and hunt other game as well. They respect the wildlife, the land, and each other. As a result, we hunt hard, have fun, and enjoy a high hunting success rate. The owner Dave Leonard has over 40 years of guide experience and knowledge of Alaska's diverse species and habitats. He has handpicked each of our Alaska hunting guides to ensure that you have a once in a lifetime Alaska hunting experience. ALASKAN PENINSULA BASED HUNTS David River Bear Camp, Cold Bay, AK How to get there How do I get to David River Camp? (Spring/Fall Brown Bear and Caribou) After arriving in Anchorage, you will most likely spend the night in town and then be flown down the Peninsula the following morning. You will need to head to Merrill Field Airport on the North end of Anchorage and take a Lake Clark Air charter flight to Nelson Lagoon. Once in Nelson Lagoon you will then be driven 18 miles down the Bering Sea beach to our camp. Recommend Accommodations in Anchorage: Lakefront Hotel Hotel Captain Cook Hilton Anchorage Sheraton Anchorage **Arrive at Base Camp 2 days prior to start of hunt (allow for weather) Recommended Brown Bear Hunting Weapons & Rifles: your rifle should be equipped with a weatherproof Caliber 100 yards.
    [Show full text]