Disturbance History of the Tanana River Basin in Alaska: Management Implications
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This Is a List of Material Related to the Gates of the Arctic National Park Resident Zoned Communities Which Are Not Found in the University of Alaska System
This is a list of material related to the Gates of the Arctic National Park resident zoned communities which are not found in the University of Alaska system. This list was compiled in 2008 by park service employees. BOOKS: Douglas, Leonard and Vera Douglas. 2000. Kobuk Human-Land Relationships: Life Histories Volume I. Ambler, Kobuk, Shungnak Woods, Wesley and Josephine Woods. 2000. Kobuk Human-Land Relationships: Life Histories Volume 2. Ambler, Kobuk, Shungnak Kunz, Michael L. 1984. Archeology and History in the Upper Kobuk River Drainage: A Report of Phase I of a Cultural Resources Survey and Inventory. Department of the Interior, National Park Service, Gates of the Arctic National Park and Preserve. Kobuk, Ambler, Shungnak Aigner, Jean S. 1981. Cultural resources at Betty, Etivluk, Galbraith-Mosquito, Itkillik, Kinyksukvik, Swayback, and Tukuto Lakes in the Northern foothills of the Brooks Range, Alaska (incomplete citation, possibly incorrect date). Anaktuvuk Pass Aigner, Jean. 1977. A report on the potential archaeological impact of proposed expansion of the Anaktuvuk Pass airstrip facility by the North Slope Borough. Anaktuvuk Pass Alaska Department of Highways, Planning and Research Division. 1973. City of Huslia, Alaska; population 159. Allakaket, Alaska; population 174. Prepared by the State of Alaska, Department of Highways, Planning and Research Division in cooperation with U.S. Department of Transportation, Federal Highway Administration. Allakaket Alexander, Herbert L., Jr. 1968. Archaeology in the Atigun Valley. Expedition 2(1): 35-37. Anaktuvuk Pass Alexander, Herbert L., Jr. 1967. Alaskan survey. Expedition 9(1): 20-29. Anaktuvuk Pass Amsden, Charles W. 1977. Hard times: a case study from northern Alaska, and implications for Arctic prehistory. -
Willows of Interior Alaska
1 Willows of Interior Alaska Dominique M. Collet US Fish and Wildlife Service 2004 2 Willows of Interior Alaska Acknowledgements The development of this willow guide has been made possible thanks to funding from the U.S. Fish and Wildlife Service- Yukon Flats National Wildlife Refuge - order 70181-12-M692. Funding for printing was made available through a collaborative partnership of Natural Resources, U.S. Army Alaska, Department of Defense; Pacific North- west Research Station, U.S. Forest Service, Department of Agriculture; National Park Service, and Fairbanks Fish and Wildlife Field Office, U.S. Fish and Wildlife Service, Department of the Interior; and Bonanza Creek Long Term Ecological Research Program, University of Alaska Fairbanks. The data for the distribution maps were provided by George Argus, Al Batten, Garry Davies, Rob deVelice, and Carolyn Parker. Carol Griswold, George Argus, Les Viereck and Delia Person provided much improvement to the manuscript by their careful editing and suggestions. I want to thank Delia Person, of the Yukon Flats National Wildlife Refuge, for initiating and following through with the development and printing of this guide. Most of all, I am especially grateful to Pamela Houston whose support made the writing of this guide possible. Any errors or omissions are solely the responsibility of the author. Disclaimer This publication is designed to provide accurate information on willows from interior Alaska. If expert knowledge is required, services of an experienced botanist should be sought. Contents -
Joint Land Use Study
Fairbanks North Star Borough Joint Land Use Study United States Army, Fort Wainwright United States Air Force, Eielson Air Force Base Fairbanks North Star Borough, Planning Department July 2006 Produced by ASCG Incorporated of Alaska Fairbanks North Star Borough Joint Land Use Study Fairbanks Joint Land Use Study This study was prepared under contract with Fairbanks North Star Borough with financial support from the Office of Economic Adjustment, Department of Defense. The content reflects the views of Fairbanks North Star Borough and does not necessarily reflect the views of the Office of Economic Adjustment. Historical Hangar, Fort Wainwright Army Base Eielson Air Force Base i Fairbanks North Star Borough Joint Land Use Study Table of Contents 1.0 Study Purpose and Process................................................................................................. 1 1.1 Introduction....................................................................................................................1 1.2 Study Objectives ............................................................................................................ 2 1.3 Planning Area................................................................................................................. 2 1.4 Participating Stakeholders.............................................................................................. 4 1.5 Public Participation........................................................................................................ 5 1.6 Issue Identification........................................................................................................ -
Extending the Late Holocene White River Ash Distribution, Northwestern Canada STEPHEN D
ARCTIC VOL. 54, NO. 2 (JUNE 2001) P. 157– 161 Extending the Late Holocene White River Ash Distribution, Northwestern Canada STEPHEN D. ROBINSON1 (Received 30 May 2000; accepted in revised form 25 September 2000) ABSTRACT. Peatlands are a particularly good medium for trapping and preserving tephra, as their surfaces are wet and well vegetated. The extent of tephra-depositing events can often be greatly expanded through the observation of ash in peatlands. This paper uses the presence of the White River tephra layer (1200 B.P.) in peatlands to extend the known distribution of this late Holocene tephra into the Mackenzie Valley, northwestern Canada. The ash has been noted almost to the western shore of Great Slave Lake, over 1300 km from the source in southeastern Alaska. This new distribution covers approximately 540000 km2 with a tephra volume of 27 km3. The short time span and constrained timing of volcanic ash deposition, combined with unique physical and chemical parameters, make tephra layers ideal for use as chronostratigraphic markers. Key words: chronostratigraphy, Mackenzie Valley, peatlands, White River ash RÉSUMÉ. Les tourbières constituent un milieu particulièrement approprié au piégeage et à la conservation de téphra, en raison de l’humidité et de l’abondance de végétation qui règnent en surface. L’observation des cendres contenues dans les tourbières permet souvent d’élargir notablement les limites spatiales connues des épisodes de dépôts de téphra. Cet article recourt à la présence de la couche de téphra de la rivière White (1200 BP) dans les tourbières pour agrandir la distribution connue de ce téphra datant de l’Holocène supérieur dans la vallée du Mackenzie, située dans le Nord-Ouest canadien. -
Big Delta Quadrangle Delta Big 1:250,000 - 3645
Big Delta quadrangle Descriptions of the mineral occurrences shown on the accompanying figure follow. See U.S. Geological Survey (1996) for a description of the information content of each field in the records. The data presented here are maintained as part of a statewide database on mines, prospects and mineral occurrences throughout Alaska. o o o o o o o o Distribution of mineral occurrences in the Big Delta 1:250,000-scale quadrangle, Alaska This and related reports are accessible through the USGS World Wide Web site http://ardf.wr.usgs.gov. Comments or information regarding corrections or missing data, or requests for digital retrievals should be directed to Donald Grybeck, USGS, 4200 Unversity Dr., Anchorage, AK 99508-4667, email [email protected], telephone (907) 786-7424. This compilation is authored by: Cameron Rombach Alaska Division of Geological & Geophysical Surveys 794 University Ave., Suite 200 Fairbanks, AK 99709-3645 Alaska Resource Data File This report is preliminary and has not been reviewed for conformity with U.S. Geologi- cal Survey editorial standards or with the North American Stratigraphic code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. OPEN-FILE REPORT 99-354 Alaska Resource Data File BD001 Site name(s): Banner Creek Site type: Mines ARDF no.: BD001 Latitude: 64.316 Quadrangle: BD B-5 Longitude: 146.346 Location description and accuracy: Banner Creek drains southward into the Tanana River. The approximate center of min- ing activity on Banner Creek is in SW1/4SW1/4 section 10, T. -
Tanana Valley Stocked Lakes Fishing Guide
Tanana Valley Stocked Lakes Fishing Guide Alaska Department of Fish and Game Sport Fish Division April 2017 Table of Contents Tanana River Drainage Stocked Lakes Program .................................................................................................... 1 Fishing Facts and Tips ............................................................................................................................................ 3 Arctic Char (Salvelinus alpinus) ......................................................................................................................... 4 Arctic Grayling (Thymallus arcticus) ................................................................................................................. 5 Burbot (Lota lota) ............................................................................................................................................... 6 King (Chinook) Salmon (Oncorhynchus tshawytscha) and Silver (Coho) Salmon (Oncorhynchus kisutch) .... 7 Lake Trout (Salvelinus namaycush) ................................................................................................................... 8 Northern Pike (Esox lucius) ................................................................................................................................ 9 Rainbow Trout (Oncorhynchus mykiss) ........................................................................................................... 10 Road Guide .......................................................................................................................................................... -
Russian–American Telegraph from Wikipedia, the Free Encyclopedia (Redirected from Western Union Telegraph Expedition)
Russian–American telegraph From Wikipedia, the free encyclopedia (Redirected from Western Union Telegraph Expedition) The Russian American telegraph , also known as the Western Union Telegraph Expedition and the Collins Overland telegraph , was a $3,000,000 undertaking by the Western Union Telegraph Company in 1865-1867, to lay an electric telegraph line from San Francisco, California to Moscow, Russia. The route was intended to travel from California via Oregon, Washington Territory, the Colony of British Columbia and Russian Alaska, under the Bering Sea and across Siberia to Moscow, where lines would communicate with the rest of Europe. It was proposed as an alternate to long, deep underwater cables in the Atlantic. Abandoned in 1867, the Russian American Telegraph was considered an economic failure, but history now deems it a "successful failure" because of the many benefits the exploration brought to the regions that were traversed. Contents ■ 1 Perry Collins and Cyrus West Field ■ 2 Preparations ■ 3 Route through Russian Alaska ■ 4 Route through British Columbia ■ 5 Legacy ■ 6 Places named for the expedition members ■ 7 Books and memoirs written about the expedition ■ 8 Further reading ■ 9 External links ■ 10 Notes Perry Collins and Cyrus West Field By 1861 the Western Union Telegraph Company had linked the eastern United States by electric telegraph all the way to San Francisco. The challenge then remained to connect North America with the rest of the world. [1] Working to meet that challenge was Cyrus West Field's Atlantic Telegraph Company, who in 1858 had laid the first undersea cable across the Atlantic Ocean. However, the cable had broken three weeks afterwards and additional attempts had thus far been unsuccessful. -
Summary Report for the Navigability of the Nabesna River Within the Tanana River Region, Alaska
United States Departmentof the Interior BUREAU OF LAND MANAGEMENT TAKE PRIDE • Alaska State Office '"AMERICA 222 West Seventh Avenue, #13 Anchorage, Alaska 99513-7504 http://www.blm.gov/ak In Reply Refer to: 1864 (AK9410) Memorandum To: File FF-094614 From: Jack Frost, Navigable Waters Specialist (AK9410) Subject: Summary Report for the Navigability of the Nabesna River within the Tanana River Region, Alaska The State of Alaska (State) filed an application, dated October 3, 2005, for a recordable disclaimer of interest (RDI) for lands underlying the Nabesna River "between the ordinary high water lines of the left and right banks from its origins at the Nabesna Glacier within Township 5 North, Ranges 13 and 14 East, Copper River Meridian, Alaska, downstream to its confluence with the Tanana River in Township 15 North, Range 19 East, Copper River Meridian." 1 The State identified the location of its application on two maps entitled "Nabesna River Recordable Disclaimer of Interest Application," dated October 3, 2005. The maps were submitted with the State's application. The State filed an amended RDI application for the Nabesna River, dated September 16, 2015, "to include only the submerged lands underlying the Nabesna River from its mouth to the Black Hills (Sec. 25, TI IN, Rl 7E, and CRM). The State withdraws its request for an RDI on the submerged lands underlying the Nabesna River from Sec. 25, Tl IN, R17E, CRM and the river's source at the Nabesna Glacier." 2 Clarifying its letter from September 16, 2015, the State submitted an email on October 16, 2015 stating that "the State withdraws its request for an RDI on the submerged lands underlying the Nabesna River from its confluence with the Cheslina River in Section 35, Tl2N, RI 7E, CRM upstream to the river's source at the Nabesna Glacier." 3 The State bases its application for a disclaimer of interest on the Equal Footing Doctrine, the Submerged Lands Act of May 22, 1953, the Alaska Statehood Act, the Submerged Lands Act of 1988, and any other legally cognizable reason. -
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. -
Yukon River Nulato Hills Lime Hills Alaska Range Yukon River Lowlands Seward Peninsula Yukon-Kuskokwim Delta Ray Mountains Ahklu
New Allakaket !! er !! iv !! H R k a e Alatna o z e l t r l a y g C k I o y n C e H r r e g k n e r Allakaket e k t Cre r e v r e Asiksa e i u e e C H K R k r P k a a a s C h h R n n s u i K v Kotzebue Sound Lowlands z i k e u k o r P e h r r t r k i r k k Selawik National u e k e i e e R ek u v u e H k il r i re Cr l C i C a u G v n u C n k R t i o s e la n k h a e ha r i k h r t il i i C e S g t C in u nu C Wildlife Refuge e h w H a r K r k S a e e l reek k e e o C e e ltlinkh h k Ta k r e S g r k W e k u e C h e e v o i n e r r e l e e e r C S R m l e k v o i C Deering k k r e L C e d x ! c u C r R r ! i o e C o D a r m Kada e k f R e ina C l f s re K Kobuk Ridges and Valleys e e K ek k i t o l p k s l o k S g e a lat p c ta ht a e n o i C u D k t k E r oha Creek na a r Al C C Cre a r e C e k C k e r r k k t e r e e ek e e l ek e o e i e r r v r k v C k k i C W ugh P ry i e R ar all g Slo C te e e le ic Lon s R r R k y i C C r k e C re M v e k e k r k k e a k e Map Area Extenitr B e e e r u r r D C K a i r B C h l e C o l v u k k c o y k i o H r m k g e A n e e a c e a u g H r R tla o e e e n C i o r k l n r a k a u R C n m e re n e a o k e y C o C c w b k o e r i a t a n C r k i r u a P e s I k Ca v o a H K M n h C C k e N d n i r oo e l Bb uckland C k u n ek it r l a e uk a re l o C h k ! C r e y C C e ! e L C ek a ree e r z na o E C u k e o r it a re h k C e z ol N s C y k N n s y e h K e i n e p e r n e ig k t i e y lo n k h s C G i ree e H ra o d M C k e o r l p K t d e n N O um e h k k o e z k J e ee k a ee e r Cr n K C B r e -
Roadside Salmon Fishing in the Tanana River Drainage
oadside Salmon Fishing R in the Tanana River Drainage Table of Contents Welcome to Interior Alaska ..........................................................................1 Salmon Biology ...................................................................................................1 Best Places to Fish for King and Chum Salmon ................................................2 Chena River ...............................................................................................2 Salcha River ...............................................................................................3 Other King and Chum Salmon Fisheries .............................................3 Where Can I Catch Coho Salmon? ...............................................................4 cover and front inside photos by: Reed Morisky & Audra Brase The Alaska Department of Fish and Game (ADF&G) administers all programs and activities free from discrimination based on race, color, national origin, age, sex, religion, marital status, pregnancy, parenthood, or disability. The department administers all programs and activities in compliance with Title VI of the Civil Rights Act of 1964, Section 504 of the Rehabilitation Act of 1973, Title II of the Ameri- cans with Disabilities Act (ADA) of 1990, the Age Discrimination Act of 1975, and Title IX of the Education Amendments of 1972. If you believe you have been discriminated against in any program, activity, or facility please write: ADF&G ADA Coordinator, P.O. Box 115526, Juneau, AK 99811-5526 U.S. Fish -
Resedimentation of the Late Holocene White River Tephra, Yukon Territory and Alaska
Resedimentation of the late Holocene White River tephra, Yukon Territory and Alaska K.D. West1 and J.A. Donaldson2 Carleton University3 West, K.D. and Donaldson, J.A. 2002. Resedimentation of the late Holocene White River tephra, Yukon Territory and Alaska. In: Yukon Exploration and Geology 2002, D.S. Emond, L.H. Weston and L.L. Lewis (eds.), Exploration and Geological Services Division, Yukon Region, Indian and Northern Affairs Canada, p. 239-247. ABSTRACT The Wrangell region of eastern Alaska represents a zone of extensive volcanism marked by intermittent pyroclastic activity during the late Holocene. The most recent and widely dispersed pyroclastic deposit in this area is the White River tephra, a distinct tephra-fall deposit covering 540 000 km2 in Alaska, Yukon, and the Northwest Territories. This deposit is the product of two Plinian eruptions from Mount Churchill, preserved in two distinct lobes, created ca. 1887 years B.P. (northern lobe) and 1147 years B.P. (eastern lobe). The tephra consists of distal primary air-fall deposits and proximal, locally resedimented volcaniclastic deposits. Distinctive layers such as the White River tephra provide important chronostratigraphic control and can be used to interpret the cultural and environmental impact of ancient large magnitude eruptions. The resedimentation of White River tephra has resulted in large-scale terraces, which fl ank the margins of Klutlan Glacier. Preliminary analysis of resedimented deposits demonstrates that the volcanic stratigraphy within individual terraces is complex and unique. RÉSUMÉ Au cours de l’Holocène tardif, des matériaux pyroclastiques ont été projetés lors d’importantes et nombreuses éruptions volcaniques, dans la région de Wrangell de l’est de l’Alaska.