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The Alaska Boundary Dispute
University of Calgary PRISM: University of Calgary's Digital Repository University of Calgary Press University of Calgary Press Open Access Books 2014 A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939 Smith, Gordon W. University of Calgary Press "A historical and legal study of sovereignty in the Canadian north : terrestrial sovereignty, 1870–1939", Gordon W. Smith; edited by P. Whitney Lackenbauer. University of Calgary Press, Calgary, Alberta, 2014 http://hdl.handle.net/1880/50251 book http://creativecommons.org/licenses/by-nc-nd/4.0/ Attribution Non-Commercial No Derivatives 4.0 International Downloaded from PRISM: https://prism.ucalgary.ca A HISTORICAL AND LEGAL STUDY OF SOVEREIGNTY IN THE CANADIAN NORTH: TERRESTRIAL SOVEREIGNTY, 1870–1939 By Gordon W. Smith, Edited by P. Whitney Lackenbauer ISBN 978-1-55238-774-0 THIS BOOK IS AN OPEN ACCESS E-BOOK. It is an electronic version of a book that can be purchased in physical form through any bookseller or on-line retailer, or from our distributors. Please support this open access publication by requesting that your university purchase a print copy of this book, or by purchasing a copy yourself. If you have any questions, please contact us at ucpress@ ucalgary.ca Cover Art: The artwork on the cover of this book is not open access and falls under traditional copyright provisions; it cannot be reproduced in any way without written permission of the artists and their agents. The cover can be displayed as a complete cover image for the purposes of publicizing this work, but the artwork cannot be extracted from the context of the cover of this specificwork without breaching the artist’s copyright. -
Chapter 2 Darkness
Chapter 2 Darkness f all the disconcerting statements in Veniaminov’s great work on the eastern Aleutians—and there are several—few are O more arresting than his assertion that elderly Unanga{ told of famous shamans who, long before the first Russians appeared, said white people would arrive from the sea and afterwards all Unanga{ would come to resemble them and would adopt their customs. These elders also reported that at the time of the Russian arrival the shamans began prophesizing that “in the east, over their islands,” they saw “a brilliant dawn or a great light” inhabited by “many people resembling the newcomers, while in the lower world, of the people whom they had seen there before, very few remained” and “impenetrable darkness set in.”1 This darkness surrounds the earliest history of Biorka, Kashega, and Makushin. Nick Galaktionoff joked that when people asked him where Aleuts came from, he would tell them, “Tomorrow I come from Makushin!” By “tomorrow” he meant “yesterday” or “that time before.” “I was right,” he laughed, “‘cause I was born there.”2 And yet Nick had an older origin story that began when Unanga{ lived on the mainland, a time when ice covered much of the coastline.3 Food became scarce and animals began preying on villages, taking food and attacking people. The chiefs spoke with their people and explained that they would have to go across the ice. They covered the bottoms of their open skin boats with seal skin that still had the fur on it, and this smooth surface allowed the heavily laden boats to be towed. -
Southeast Alaska Sea Cucumber Commercial Fishery Area Rotation
Alaska Department of Fish and Gam e Southeast Alaska Sea Cucumber Open Season Commercial Fishery Area Rotation (October 1 - March 31) Map IV.b. (southern Southeast) ! 2018-19 2019-20 2020-21 South Mitkof and North Zarembo Islands Wrangell Zimovia Strait and Anita Bay ! Stikine Strait and Chichagof Passage Bradfield Canal, Blake Channel and Eastern Passage µ Snow Pass Northern Ernest Sound North Behm Canal Clarence Strait West Behm Canal 101-85 Rudyerd Bay, Southern Ernest Sound East Behm Canal, Thorne Bay and Kasaan Peninsula and Walker Cove George Inlet, SanSan ChristovalChristoval West Behm Canal Cleveland Peninsula Bold Island, Channel,Channel, westernwestern 101-90, 95 San Alberto Bay, and Carroll Inlet San Alberto Bay, Kasaan Bay andand TrocaderoTrocadero BayBay and Skowl Arm Tongass Craig Narrows East Behm Canal ! and Smeaton Bay Clarence Strait ! Ketchikan Revillagigedo Channel, Cholmondeley Thorne Arm, and Sound East Behm Canal West Shore of Bucareli Bay and Gravina Island Port Real Marina Moira Sound Eastern shore Boca de of Dall Island Quadra and Soda Bay Lower Hetta Inlet, Clarence Percy Islands Nutkwa Inlet, Strait and Keete Inlet Long Island and upper Cordova Bay Clarence Strait and Dixon Entrance Tree Point Willard and Revillagigedo Channel Fillmore Inlets and Southern Clarence Strait Revillagigedo Channel and Felice Strait 25 12.5 0 25 50 Nautical Miles Last modified: 10/24/2018 Map Datum and Projection: NAD 83 Alaska 1 State Plane FIPS 5001 (meters) Mike Donnellan. -
Resource Utilization in Unalaska, Aleutian Islands, Alaska
RESOURCE UTILIZATION IN UNALASKA, ALEUTIAN ISLANDS, ALASKA Douglas W. Veltre, Ph. D. Mary J. Veltre, B.A. Technical Paper Number 58 Alaska Department of Fish and Game Division of Subsistence October 23, 1982 Contract 824790 ACKNOWLEDGMENTS This report would not have been possible to produce without the generous support the authors received from many residents of Unalaska. Numerous individuals graciously shared their time and knowledge, and the Ounalashka Corporation,. in particular, deserves special thanks for assistance with housing and transportation. Thanks go too to Linda Ellanna, Deputy Director of the Division of Subsistence, who provided continuing support throughout this project, and to those individuals who offered valuable comments on an earlier draft of this report. ii TABLE OF CONTENTS ACKNOWLEDGMENTS. ii Chapter 1 INTRODUCTION . 1 Purpose ..................... 1 Research objectives ............... 4 Research methods 6 Discussion of rese~r~h'm~tho~oio~y' ........ ...... 8 Organization of the report ........... 10 2 BACKGROUNDON ALEUT RESOURCE UTILIZATION . 11 Introduction ............... 11 Aleut distribuiiin' ............... 11 Precontact resource is: ba;tgr;ls' . 12 The early postcontact period .......... 19 Conclusions ................... 19 3 HISTORICAL BACKGROUND. 23 Introduction ........................... 23 The precontact'plrioi . 23 The Russian period ............... 25 The American period ............... 30 Unalaska community profile. ........... 37 Conclusions ................... 38 4 THE NATURAL SETTING ............... -
Sockeye Salmon, Oncorhynchus Nerka, Catches in Southeast Alaska, Based on Incidence of Allozyme Variants, Freshwater Ages, and a Brain-Tissue Parasite
Stock Composition of Some Sockeye Salmon, Oncorhynchus nerka, Catches in Southeast Alaska, Based on Incidence of Allozyme Variants, Freshwater Ages, and a Brain-Tissue Parasite Item Type monograph Authors Pella, Jerome; Masuda, Michele; Guthrie III, Charles; Kondzela, Christine; Gharrett, Anthony J.; Moles, Adam; Winans, Gary Publisher NOAA/National Marine Fisheries Service Download date 09/10/2021 14:19:18 Link to Item http://hdl.handle.net/1834/20475 NOAA Technical Report NMFS 132 January 1998 Stock Composition of Some Sockeye Salmon, Oncorhynchus nerka, Catches in Southeast Alaska, Based on Incidence of Allozyme Variants, Freshwater Ages, and a Brain-Tissue Parasite Jerome Pella Michele Masuda Charles Guthrie III Christine Kondzela Anthony Gharrett Adam Moles Gary Winans U.S. Department of Commerce u.s. DEPARTMENT OF COMMERCE WILLIAM M. DALEY NOAA SECRETARY National Oceanic and Atmospheric Adn:llnistration Technical D. James Baker Under Secretary for Oceans and Atmosphere Reports NMFS National Marine Fisheries Service Technical Reports of the Fishery Bulletin Rolland A. Schmitten Assistant Administrator for Fisheries Scientific Editor Dr. John B. Pearce Northeast Fisheries Science Center National Marine Fisheries Service, NOAA 166 Water Street Woods Hole, Massachusetts 02543-1097 Editorial Committee Dr. Andrew E. Dizon National Marine Fisheries Service Dr. Linda L. Jones National Marine Fisheries Service Dr. Richard D. Methot National Marine Fisheries Service Dr. Theodore W. Pietsch University of Washington Dr. Joseph E. Powers National Marine Fisheries Service Dr. Tim. D. Stnith National Marine Fisheries Service Managing Editor Shelley E. Arenas Scientific Publications Office National Marine Fisheries Service, NOAA 7600 Sand Point Way N.E. Seattle, Washington 98115-0070 The NOAA Technical Report NMFS (ISSN 0892-8908) series is published by the Scientific Publications Office, Na tional Marine Fisheries Service, NOAA, 7600 Sand Point Way N.E., Seattle, WA The NOAA Technical Report NMFS series of the Fishery Bulletin carries peer-re 98115-0070. -
Journal of Marine Research, Sears Foundation for Marine Research
The Journal of Marine Research is an online peer-reviewed journal that publishes original research on a broad array of topics in physical, biological, and chemical oceanography. In publication since 1937, it is one of the oldest journals in American marine science and occupies a unique niche within the ocean sciences, with a rich tradition and distinguished history as part of the Sears Foundation for Marine Research at Yale University. Past and current issues are available at journalofmarineresearch.org. Yale University provides access to these materials for educational and research purposes only. Copyright or other proprietary rights to content contained in this document may be held by individuals or entities other than, or in addition to, Yale University. You are solely responsible for determining the ownership of the copyright, and for obtaining permission for your intended use. Yale University makes no warranty that your distribution, reproduction, or other use of these materials will not infringe the rights of third parties. This work is licensed under the Creative Commons Attribution- NonCommercial-ShareAlike 4.0 International License. To view a copy of this license, visit http://creativecommons.org/licenses/by-nc-sa/4.0/ or send a letter to Creative Commons, PO Box 1866, Mountain View, CA 94042, USA. Journal of Marine Research, Sears Foundation for Marine Research, Yale University PO Box 208118, New Haven, CT 06520-8118 USA (203) 432-3154 fax (203) 432-5872 [email protected] www.journalofmarineresearch.org RELATION OF POPULATION SIZE TO MARINE GROWTH AND TIME OF SPAWNING MIGRATION IN THE PINK SALMON ( Oncorhynchus gorbuscha) OF SOUTHEASTERN ALASKA F. -
Preliminary Reconnaissance Geologic Map of the Petersburg and Parts of the Port Alexander and Sumdum 1:250,000 Quadrangles, Southeastern Alaska
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY Preliminary reconnaissance geologic map of the Petersburg and parts of the Port Alexander and Sumdum 1:250,000 quadrangles, southeastern Alaska By David A. Brew , A. Thomas Ovenshine , Susan M. Karl , and Susan J. Hunt* Open-File Report 84-405 This report is preliminary and has not been reviewed for conformity with U.S Geological Survey editorial standards and strati graphic nomenclature. *Menlo Park, California ^Reston, Virginia ^Anchorage, Alaska Preliminary reconnaissance geologic map of the Petersburg and parts of the Port Alexander and Sumdum 1:250,000 quadrangles, southeastern Alaska By David A. Brew, A. T. Ovenshine, Susan M. Karl, and Susan J. Hunt INTRODUCTION This report consists of three main items: (1) the geologic map (sheet 1 of 2), (2) the correlation of map units (sheet 2 of 2), which includes an inset map relating different parts of the map to the correlation of map units and to (3) the description of map units (this pamphlet). The inset map on sheet 2 shows the major geological elements of the map area. They are, from west to east, (1) the Alexander belt, consisting of generally unmetamorphosed Lower Paleozoic through Upper Triassic rocks intruded by scattered mid-Cretaceous plutons, (2) the Gravina belt, consisting of unmetamorphosed to highly metamorphosed, variably deformed Upper Jurassic(?) through mid-Cretaceous flysch and volcanic rocks intruded by both mid- and Upper Cretaceous plutons, and (3) the Mainland belt, consisting of metamorphic rocks intruded by Upper Cretaceous, lower Tertiary, and mid- Tertiary plutons. Younger than almost all parts of all of these belts, and extending from the Alexander belt across the Gravina and onto the mainland belt, is the lower to middle Tertiary Kuiu-Etolin belt that consists largely of varied volcanic rocks, associated plutons, and minor sedimentary rocks. -
Conservation Prioritization of Prince of Wales Island
CONSERVATION PRIORITIZATION OF PRINCE OF WALES ISLAND Identifying opportunities for private land conservation Prepared by the Southeast Alaska Land Trust With support from U.S. Fish and Wildlife Service Southeast Alaska Coastal Conservation Program February 2013 Conservation prioritization of Prince of Wales Island Conservation prioritization of Prince of Wales Island IDENTIFYING OPPORTUNITIES FOR PRIVATE LAND CONSERVATION INTRODUCTION The U.S. Fish and Wildlife Service (USFWS) awarded the Southeast Alaska Land Trust (SEAL Trust) a Coastal Grant in 2012. SEAL Trust requested this grant to fund a conservation priority analysis of private property on Prince of Wales Island. This report and an associated Geographic Information Systems (GIS) map are the products of that work. Driving SEAL Trust’s interest in conservation opportunities on Prince of Wales Island is its obligations as an in-lieu fee sponsor for Southeast Alaska, which makes it eligible to receive fees in-lieu of mitigation for wetland impacts. Under its instrument with the U.S. Army Corps of Engineers1, SEAL Trust must give priority to project sites within the same 8-digit Hydrologic Unit (HUC) as the permitted impacts. In the past 10 years, SEAL Trust has received a number of in-lieu fees from wetlands impacted by development on Prince of Wales Island, which, along with its outer islands, is the 8-digit HUC #19010103 (see Map 1). SEAL Trust has no conservation holdings or potential projects on Prince of Wales Island. In an attempt to achieve its conservation goals and compliance with the geographic elements of the Instrument, SEAL Trust wanted to take a strategic approach to exploring preservation possibilities in the Prince of Wales HUC. -
Why Does Canada Have So Many Unresolved Maritime Boundary Disputes? –– Pourquoi Le Canada A-T-Il Autant De Différends Non Résolus Concernant Ses Frontières Maritimes?
Why Does Canada Have So Many Unresolved Maritime Boundary Disputes? –– Pourquoi le Canada a-t-il autant de différends non résolus concernant ses frontières maritimes? michael byers and andreas Østhagen Abstract Résumé Canada has five unresolved maritime Le Canada a cinq frontières maritimes qui boundaries. This might seem like a high n’ont pas encore été délimitées. Ce nom- number, given that Canada has only three bre peut paraitre élevé étant donné que le neighbours: the United States, Denmark Canada n’a que trois voisins: les États-Unis, (Greenland), and France (St. Pierre and le Danemark (Groënland) et la France (St. Miquelon). This article explores why Pierre et Miquelon). Cet article cherche à Canada has so many unresolved maritime découvrir pourquoi le Canada a tant de boundaries. It does so through a compar- frontières maritimes irrésolues. Pour ce ison with Norway, which has settled all of faire, l’article se penche sur le cas de la its maritime boundaries, most notably in Norvège, qui a réussi à délimiter toutes ses the Barents Sea with Russia. This compar- frontières maritimes, y compris dans la mer ison illuminates some of the factors that de Barents avec la Russie. Cette comparai- motivate or impede maritime boundary son met en relief certains des facteurs qui negotiations. It turns out that the status favorisent ou entravent les négociations of each maritime boundary can only be pour la résolution de différends maritimes explained on the basis of its own unique frontaliers. Il s’avère que le statut des fron- geographic, historic, political, and legal tières maritimes ne peut s’expliquer qu’en context. -
Geology and Mineral Deposits of Jumbo Basin Southeastern Alaska
Geology and Mineral Deposits of Jumbo Basin Southeastern Alaska GEOLOGICAL SURVEY PROFESSIONAL PAPER 251 Geology and Mineral Deposits of Jumbo Basin Southeastern Alaska By GEORGE C. KENNEDY GEOLOGICAL SURVEY PROFESSIONAL PAPER 251 A discussion of the contact metamorphism, geomagnetic surveys, magnetite deposits, and iron ore reserves of part of Prince of Whales Island. UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1953 UNITED STATES DEPARTMENT OF THE INTERIOR Douglas McKay, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. CONTENTS Page Page Abstract. __________________________________________ 1 Contact metamorphism—Continued Introduction ______________________________________ 1 Metamorphism in the vicinity of the Magnetite Cliff Previous work. _ _ _______________________________ 1 bodies—Continued Present work- ________ 1 Metamorphism of the schists.________________ 20 Acknowledgments. ______________ _______________ 2 Metamorphism of the dike rocks._____________ 20 Geography__ _______________________________________ 2 Metamorphism in the vicinity of the upper magnetite Location and accessibility________________________ 2 bodies_ _______________________---_----_-_____ 21 Topography. ____________________________!______ 3 Exomorphism of the marble__________________ 21 Climate, water supply, and vegetation. ____________ 4 Endomorphism of the intrusive rocks__________ 22 History and production______________________________ 4 Metamorphism -
Ketchikan and Prince Rupert Quadrangles, Southeastern Alaska
The Alaska Mineral Resource Assessment Program: Guide to Information about the Geology and Mineral Resources of the Ketchikan and Prince Rupert Quadrangles, Southeastern Alaska By Henry C. Berg GEOLOGICAL SURVEY CIRCULAR 855 United States Department of the Interior JAMES G. WATT, Secretary Geological Survey Dallas L. Peck, Director Library of Congress Cataloging in Publication Data Berg, Henry Clayr 1929- The Alaska Mineral;peswrcer Assessment Program: Guide to information about the geoiogy and mineral resources of the Ketchikan h&.~fince'l?upert quadrangles, southeastern Alaska. 3 (Geological Survey circular ; 8551 Bibliography: p. 21-24 Supt. of Docs. no.: I19.4/2:855 1. Mines and mineral resources--Alaska. 2. Geology-- Alaska. I. Title. 11. Series: United States. Geological Survey. Circular 855. QE75.CS no. 855 622 s 82-600083 CTN24. A41 t557.98'21 AACR2 Free on application to Branch of Distribution, U.S. Geological Sumey 604 South Pickett Street, Alexandria, VA 22304 CONTENTS Page Abstract ............................................................................................ 1 Descriptionsof component mapsand reportsofthe Ketchikan Introduction ...................................................................................... 1 and Prince Rupert quadrangles AMRAP folio Purpose and scope .................................................................. 1 and of subsequent related investigations-Continued Geography and access ............................................................ 1 Tectonostratigraphic terranes and structural -
Dixon Entrance
118 ¢ U.S. Coast Pilot 8, Chapter 4 19 SEP 2021 Chart Coverage in Coast Pilot 8—Chapter 4 131°W 130°W NOAA’s Online Interactive Chart Catalog has complete chart coverage http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml 133°W 132°W UNITEDCANADA ST ATES 17420 17424 56°N A 17422 C L L U A S R N R 17425 E I E N N E V C P I E L L A S D T N G R A I L B A G E E I L E T V A H N E D M A L 17423 C O C M I H C L E S P A B A L R N N I A A N L A N C C D E 17428 O F W 17430 D A 17427 Ketchikan N L A E GRAVINA ISLAND L S A T N I R S N E E O L G T R P A E T A S V S I E L N A L P I A S G S L D I L A G O N E D H D C O I N C 55°N H D A A N L N T E E L L DUKE ISLAND L N I I S L CORDOVA BAY D N A A N L T D R O P C Cape Chacon H A T H A 17437 17433 M S O Cape Muzon U N 17434 D DIXON ENTRANCE Langara Island 17420 54°N GRAHAM ISLAND HECATE STRAIT (Canada) 19 SEP 2021 U.S.