Bedrock Geologic Map of the Southern Brooks Range, Alaska, and Accompanying Conodont Data
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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. -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
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. -
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. -
Geologic Map of Alaska
Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey Front cover. Color shaded relief map of Alaska and surroundings. Sources: 100-meter-resolution natural image of Alaska, http://nationalmap.gov/small_scale/mld/nate100.html; rivers and lakes dataset, http://www.asgdc.state.ak.us/; bathymetry and topography of Russia and Canada, https://www.ngdc.noaa.gov/mgg/global/global.html. Back cover. Previous geologic maps of Alaska: 1906—Brooks, A.H., Abbe, Cleveland, Jr., and Goode, R.U., 1906, The geography and geology of Alaska; a summary of existing knowledge, with a section on climate, and a topographic map and description thereof: U.S. Geological Survey Professional Paper 45, 327 p., 1 sheet. 1939—Smith, P.S., 1939, Areal geology of Alaska: U.S. Geological Survey Professional Paper 192, 100 p., 18 plates. 1957—Dutro, J.T., Jr., and Payne, T.G., 1957, Geologic map of Alaska: U.S. Geological Survey, scale 1:2,500,000. 1980—Beikman, H.M., 1980, Geologic map of Alaska: U.S. Geological Survey Special Map, scale 1:2,500,000, 2 sheets. Geologic Map of Alaska Compiled by Frederic H. Wilson, Chad P. Hults, Charles G. Mull, and Susan M. Karl Pamphlet to accompany Scientific Investigations Map 3340 2015 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Director U.S. -
Accomplish Me Cover Photograph South Sawyer Glacier in Southeastern Alaska
m Accomplish me Cover photograph South Sawyer Glacier in southeastern Alaska. View southeast from head of Tracy Arm. The United States Geological Survey in Alaska: Accomplishments during 1977 Kathleen AA. Johnson, Editor GEOLOGICAL SURVEY CIRCULAR 772-B 1978 United States Department of the Interior CECIL D. ANDRUS, Secretary Geological Survey H. William Menard, Director Free on application to Branch of Distribution, U.S. Geological Survey, 1200 South Eads Street, Arlington, VA 22202 CONTENTS Page Abstract. ___________________________ Bl Northern Alaska Continued Summary of important results _______________! Organic geochemistry of rocks from three Introduction. _______________________! NPRA wells, by Leslie B. Magoon and Statewide projects ____________________! George E. Claypool _____________B25 Mineral resources of Alaska, by Edward H. Release of NPRA (NPR-4) data, by Robert D. Cobb _________________1 Carter ______________________26 Landsat color mosaic of Alaska, by Nairn R. D. Fossil reconnaissance study, eastern NPRA, Albert, Wm. Clinton Steele, and James R. by Charles A. Repenning____________ 27 LeCompte ____________________! Reconnaissance snow survey of NPRA, April Landsat data interpretation of various AM- 1977, by Charles E. Sloan, Dennis Trabant, RAP quadrangles, Alaska by Nairn R. D. Al and William Glude _ ___ ____ ____ 28 bert, Wm. Clinton Steele and James R. Hydrologic reconnaissance of lakes in NPRA, LeCompte ____________________4 1977, by Charles E. Sloan and Richard F. Geochemical exploration studies in Alaska, by Snyder ______________________28 G. C. Curtin, T. D. Hessin, R. M. O'Leary, E. Streamflow in NPRA, 1977, by S. H. Jones _ _ 29 F. Cooley, G. W. Day, and R. B. Tripp _ _ _ 5 Development and operation of gas fields in the Streamflow and channel erosion investigations South Barrow area, by Robert D. -
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. -
North America Summary, 1968
240 CLIMBS A~D REGIONAL ?\OTES North America Summary, 1968. Climbing activity in both Alaska and Canada subsided mar kedly from the peak in 1967 when both regions were celebrating their centen nials. The lessened activity seems also to have spread to other sections too for new routes and first ascents were considerably fewer. In Alaska probably the outstanding climb from the standpoint of difficulty was the fourth ascent of Mount Foraker, where a four-man party (Warren Bleser, Alex Birtulis, Hans Baer, Peter Williams) opened a new route up the central rib of the South face. Late in June this party flew in from Talkeetna to the Lacuna glacier. By 11 July they had established their Base Camp at the foot of the South face and started up the rib. This involved 10,000 ft of ice and rotten rock at an angle of 65°. In the next two weeks three camps were estab lished, the highest at 13,000 ft. Here, it was decided to make an all-out push for the summit. On 24 July two of the climbers started ahead to prepare a route. In twenty-eight hours of steady going they finally reached a suitable spot for a bivouac. The other two men who started long after them reached the same place in ten hours of steady going utilising the steps, fixed ropes and pitons left by the first party. After a night in the bivouac, the two groups then contin ued together and reached the summit, 17,300 ft, on 25 July. They were forced to bivouac another night on the return before reaching their high camp. -
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)). -
Significant Metalliferous Lode Deposits and Placer Districts of Alaska
Significant Metalliferous Lode Deposits and Placer Districts of Alaska By WARREN J. NOKLEBERG, THOMAS K. BUNDTZEN, HENRY C. BERG, DAVID A. BREW, DONALD GRYBECK, MARK S. ROBINSON, THOMAS E. SMITH, and WARREN YEEND U.S. GEOLOGICAL SURVEY BULLETIN 1786 DEPARTMENT OF THE INTERIOR DONALD PAUL HODEL, Secretary U.S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1987 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center, Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-PublicationData Significant metalliferous lode deposits and placer districts of Alaska. U.S. Geological Survey Bulletin 1786 Bibliography Supt. of Docs. No.: 1 19.3:1786 1. Placer deposits-Alaska. 2. Ore deposits-Alaska. I. Nokleberg, Warren J. II. Series. QE75.B9 No. 1786 557.3 s 87-600165 [TN24.A4] [553'.13'09798] COVER Mill buildings at Kennecott, Alaska. The Kennecott district Cu-Ag mines in the Wrangell Mountains were some of the principal sources of copper in North America from 1913 to 1938. See deposit description for Kennecott district (number 30 for southern Alaska). Copyrighted drawing used by permission of Gail Niebrugge, artist, Glennallen, Alaska. PREFACE This report is a compilation of the signifi- geology. The unpublished data were contributed cant metalliferous lode deposits and placer by mineral deposit and regional geologists in districts of Alaska, and is a comprehensive data private industry, universities, the U.S. Geo- base for a companion article on the metallogene- logical Survey, the Alaska Division of Geologi- sis and major mineral deposits of Alaska that cal and Geophysical Surveys, the U.S. -
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. -
Subject Index
Subject Index NOTE: This index lists Abrams, Pete 21:3 Lands Conservation Act Aleutian Islands 1:4, 3:2, 21:2, 22:2, 23:2 Barnette, E.T. 22:1 most of the subjects Active, John 6:3 (ANILCA) 8:4, 18:3, 3:4, 5:4, 7:2, 7:3, 9:1, Arctic 3:2, 5:4, 6:2, 7:2, Barren Islands 19:3 Adak Island 7:3, 22:2, 19:3, 20:2, 20:3 10:3, 13:2, 18:2, 18:4, 9:4, 12:1,12:4, 13:2, Barrow 1:1, 5:4, 16:2, and people The Alaska 22:4 Alaska Native Arts and 19:2, 21:1, 21:3, 21:4, 20:3 19:2, 21:3, 25:4 Geographic Society has Admiralty Island 1:3, 5:2, Crafts 6:1, 6:3, 7:3, 8:3, 22:2, 22:4, 24:4, 25:4 Arctic Circle 7:1, 7:2, Barter Island 16:2, 20:3 covered in its first 100 7:2, 8:4, 18:3, 20:2, 9:2, 11:3, 12:3, 16:2, Aleutian Islands National 10:4 Bats 8:2, 19:3 issues. The numbers 20:4 17:3, 17:4, 20:2, 21:2, Wildlife Refuge 22:2 Arctic National Wildlife Bears 1:3, 3:4, 4:3, 8:2, (for example, 21:3) Adney, Edwin Tappan 21:4, 22:2, 23:2 Aleutian Range 9:1 Refuge 4:2, 16:2, 19:2, 9:2, 12:4, 15:3, 15:4, 19:1 Alaska Native Claims Alexandrovski 17:1 20:3, 20:4, 23:3 16:1, 17:3, 18:3, 19:2, refer to the Volume and Afognak (community) Settlement Act Alsek River 2:4, 25:2 Arctic Ocean 5:4, 16:2 19:3, 20:2, 20:3, 20:4, Number of the issue 4:3, 19:3 (ANCSA) 3:2, 4:4, 6:3, Alutiiq 12:3, 21:2, 23:2 Arctic Village 7:1, 20:3 21:1, 21:2, 21 :4, 23:4 containing that subject.