Wildlife Temporary Special Action WSA19-05 Analysis
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Aleutians PPOR Map 02
Center of map at 54˚ 11.10’ N Lat., 162˚ 59.63’ W Lon. GRS GRS AEA-16 AEA-12 King 35-LII Cove BERING SEA 38-LII Moffet Pt. GRS AEA-15 Amak Is. Cold Bay Kudiakof Islands GRS AEA-16 GRS GRS Fox Is. 37-LII AEA-11 Deer AEA-14 35-LIIGRS38-LII Island AEA-15Cold 36-LII Bay Volcano GRS Bay AEA-14 5 nm 5 nm 5 mi. 5 mi. GRS 5,000 yds. Scale 5,000 yds. Scale Morzhovoi Bay 05-D 57-LI AEA-12 56-LI Cold Bay. Fox Island. King 39-LII Cove False Pass 5 nm GRS GRS 5 mi. 37-LII AEA-11 AEA-12 58-LI Fox Is. 5,000 yds. Scale for Aleutians Subarea Deer False 58-LI Island Pass 57-LI Ikatan Bay Unimak Island Ikatan Bay 03-D 56-LI 03-D 04-D King Cove Otter Cove Unimak Bight (1 nm South) 39-LII 04-D 0.25 nm 0.25 mi. Otter Cove 250 yds. Scale Sanak Island King Cove. False Pass, Otter Cove and Ikatan Bay. 2 nm 2 mi. 2,000 yds. Scale 20 nm r 20 mi. Scale Aleutian Subarea 20,000 yds. Mao p This is not intended for navigational use. Soundings in fathoms t 36-LII a GRS Anchorage # Existing GRS Volcano Bay A# Map c Mooring Fish Hatchery M# Aleutian PPOR o Dock/pier Private Cabins D# L Crane Public Use Cabins Map 02 Volcano Bay. Airport Boat Harbor Legend Potential Places of Refuge Potential NUKA Research & Planning Group, LLC. -
Late-Quaternary Geomorphic Processes: Effects on the Ancient Aleuts of Umnak Island in the Aleutians
Late-Quaternary Geomorphic Processes: Effects on the Ancient Aleuts of Umnak Island in the Aleutians ROBERT F. BLACK1 ABSTRACT. Glaciation, volcanic activity, marine processes and wind action affected in various ways the lives of the ancient Aleuts of Umnak Island, who first settled at Anangula about 8,400 BP following deglaciation some 3,000 years earlier. Expanding alpine glaciers reached the sea in places about 3,000 BP without the nearby peoples being much affected. A catastrophic eruption of Okmok Volcano about 8,250 BP is suggested as the cause of the abandonment of the oldest known siteof Anangula, and subsequentmigration westward into thecentral Aleutians. Cutting of strandflats between 8,250 and 3,000 BP led to the development of a very large, accessible, year- round food resource, and an apparent proliferationof settlements. In marked contrast to other parts of Beringia, Umnak Island became the site most favourable for human settlement. RfiSUMe: Les processus géomorphologiques fini-quaternaires et leurs conséquencespour les anciens Aléoutes de Me d’Umnak dans les Aléoutiennes. La glaciation, l’activite vol- canique, les processus marins et l’actiondu vent ont affect6 de diverses façonsla vie des anciens Aleoutes de l’ile d‘Umnak, qui s’établirent B Anangula vers 8400 AP, soit environ 3000 ans après la deglaciation. Les glaciers alpins en expansion atteignirentla mer par endroit vers 3000 AP sans que les habitants du voisinage soient beaucoup affectes. On suppose qu’une eruption catastrophique du volcan Okmok vers 8250 AP a caud l’abandon du plus vieux site COMU d’Anangula et une migration vers l’ouest jusqu’au centre des A16outiennes. -
Aleuts: an Outline of the Ethnic History
i Aleuts: An Outline of the Ethnic History Roza G. Lyapunova Translated by Richard L. Bland ii As the nation’s principal conservation agency, the Department of the Interior has re- sponsibility for most of our nationally owned public lands and natural and cultural resources. This includes fostering the wisest use of our land and water resources, protecting our fish and wildlife, preserving the environmental and cultural values of our national parks and historical places, and providing for enjoyment of life through outdoor recreation. The Shared Beringian Heritage Program at the National Park Service is an international program that rec- ognizes and celebrates the natural resources and cultural heritage shared by the United States and Russia on both sides of the Bering Strait. The program seeks local, national, and international participation in the preservation and understanding of natural resources and protected lands and works to sustain and protect the cultural traditions and subsistence lifestyle of the Native peoples of the Beringia region. Aleuts: An Outline of the Ethnic History Author: Roza G. Lyapunova English translation by Richard L. Bland 2017 ISBN-13: 978-0-9965837-1-8 This book’s publication and translations were funded by the National Park Service, Shared Beringian Heritage Program. The book is provided without charge by the National Park Service. To order additional copies, please contact the Shared Beringian Heritage Program ([email protected]). National Park Service Shared Beringian Heritage Program © The Russian text of Aleuts: An Outline of the Ethnic History by Roza G. Lyapunova (Leningrad: Izdatel’stvo “Nauka” leningradskoe otdelenie, 1987), was translated into English by Richard L. -
Die-Off of Common Murres on the Alaska Peninsula and Unimak Island
SHORT COMMUNICATIONS 215 SI~~PSON, S., AND J. J. GALBRAITH. 1905. An inves- WETMORE, A. 1921. A study of the body temper- tigation into the diurnal variation of the body tem- ature of birds. Smithsonian Misc. Coll. 72:1-51. perature of nocturnal and other birds, and a few mammals. J. Physiol., 38:225-238. Accepted for publication 12 July 1971. A NORTHERLY WINTERING RECORD is more than 500 mi. NW of the nearest reported OF THE ELF OWL wintering locality. The bird was mist-netted in second-growth thorn (MICRATHENE WHITNEYI) forest near a harvested corn field. It was retained alive and taken to Tucson, Arizona. It appeared to be in good CHARLES A. ELY health and fed freely on insects given it on the nights Department of Zoology of 12-13 and 13-14 January, but suddenly fell dead Fort Hays Kansas State College Hays, Kansas 67601 from its perch late on the night of 13-14 January. Upon skinning the specimen, Crossin noted a circular AND area about 10 mm in diameter on the lower stomach. RICHARD S. CROSSIN The area was a dark bluish-green in color and resem- bled dermal tissue which has received a severe bruise. Neotropical Ornithological Foundation 1719 North Huachuca The cause of the affliction was not determined, but Tucson, Arizona 85705 may possibly have resulted from the intake of some chemical poisoning during feeding. The owl might Ligon (Misc. Publ., Mus. Zool., Univ. Michigan, No. have been afflicted before its capture, which could 136, 1968) investigated the winter range of the Elf account for its wintering far north of the recorded Owl in Mexico, chiefly by playing sound recordings winter range. -
Groundfish Harvest from Parallel Seasons in the Bering Sea-Aleutian Islands Area
Fishery Management Report No. 08-43 Bering Sea-Aleutian Islands Area State-Waters Groundfish Fisheries and Groundfish Harvest from Parallel Seasons in 2007 by Krista Milani August 2008 Alaska Department of Fish and Game Divisions of Sport Fish and Commercial Fisheries Symbols and Abbreviations The following symbols and abbreviations, and others approved for the Système International d'Unités (SI), are used without definition in the following reports by the Divisions of Sport Fish and of Commercial Fisheries: Fishery Manuscripts, Fishery Data Series Reports, Fishery Management Reports, and Special Publications. All others, including deviations from definitions listed below, are noted in the text at first mention, as well as in the titles or footnotes of tables, and in figure or figure captions. Weights and measures (metric) General Measures (fisheries) centimeter cm Alaska Administrative fork length FL deciliter dL Code AAC mideye to fork MEF gram g all commonly accepted mideye to tail fork METF hectare ha abbreviations e.g., Mr., Mrs., standard length SL kilogram kg AM, PM, etc. total length TL kilometer km all commonly accepted liter L professional titles e.g., Dr., Ph.D., Mathematics, statistics meter m R.N., etc. all standard mathematical milliliter mL at @ signs, symbols and millimeter mm compass directions: abbreviations east E alternate hypothesis HA Weights and measures (English) north N base of natural logarithm e cubic feet per second ft3/s south S catch per unit effort CPUE foot ft west W coefficient of variation CV gallon gal copyright © common test statistics (F, t, χ2, etc.) inch in corporate suffixes: confidence interval CI mile mi Company Co. -
The Northern Fur Seal ~/
Wflal~erv:-c;rrc. The Northern Fur Seal ~/ / U IS, S, R, / / Breeding grounds of the northern fur seals: Robben Island (Kaihyoto or Tyuleniy Island) off Sakhalin; the Commandel Islands (Bering Island and Medny or Copper Island) at the Soviet end of the Aleutian chain; and the Pribilof Islands - St. Paul Island, St. George Island, Otter Island, Walrus Island, and Sea Lion Rock. Cover - The Pribilof Islands in Bering Sea are the homeland of the largest fur eal herd in the world. Here the fur seals come ashore to bear their young on the rocks and sands above tidewater. The story behind the restoration and de velopment of the Ala ka fur cal herd is one of adventure and international diplomac}. It i a heartening account of cooperation among nations - an out- tanding example of wildlife conservation. UNITED STATES DEPARTMENT OF THE INTERIOR Walter J. Hickel, Secretary Leslie L. Glasgow, Assistant Secretary f01' Fish and Wildlife, PaTks, and Marine Resources Charles H , Meacham, Commissioner, U,S, FISH AND WILDLIFE SERVICE Philip M, Roedel, Di1'ecto1', BUREAU OF COMMERCIAL FISHERIES The Northern Fur Seal By RALPH C. BAKER, FORD WILKE, and C. HOWARD BALTZ02 Circular 336 Washington, D.C. April 1970 As the Nation's principal conservation agency, the Department of the Interior has basic responsibilities for water, fish, wildlife, mineral, land, park, and recreational resources. Indian and Territorial affairs are other major concerns of America's " Department of Natural Resources." The Department works to assure the wisest choice in managing all our resources so each will make its full contribution to a better United States - now and in the future. -
Grea3tfpermhl RESOURCES of the ALEUTIAN ARC
GrEa3TFPERMhL RESOURCES OF THE ALEUTIAN ARC Wy Roman .I. Mntylcw, RlairB~yA. Lics, Chri~',Boph~r.I. WYC, and Mary A. Moomnsa GEOTHERMAL RESOURCES OF THE ALEUTIAN ARC By Roman J. Motyka, Shirley A. Liss, Christopher J. Nye, and Mary A. Moorman Roman Motyka sampling an upper Glacier Valley hot spring in the Makushin geothermal area. Photo by Shirley Liss. Professional Report 114 Division of Geological & Geophysical Surveys Cover photo: "Old Faithful" of the Geyser Bight geothermal resource area. When- ever it has been observed (1870, 1948, 1980, and 1988),spring G8, Fairbanks, Alaska shown here at maximum activity, has had an eruption cycle of 1993 12 minutes. Photo by Shirley Liss. STATE OF ALASKA Walter J. Hickel, Governor DEPARTMENT OF NATURAL RESOURCES Harry A. Noah, Commissioner DIVISION OF GEOLOGICAL & GEOPHYSICAL SURVEYS Thomas E. Smith, State Geologist Division of Geological & GeophysicalSurveys publications can be inspected at the following locations. Address mail orders to the Fairbanks office. Alaska Division of Geological University of Alaska Anchorage Library & Geophysical Surveys 321 1 Providence Drive 794 University Avenue, Suite 200 Anchorage, Alaska 99508 Fairbanks, Alaska 99709-3645 Elmer E. Rasmuson Library Alaska Resource Library University of Alaska Fairbanks 222 W. 7th Avenue Fairbanks, Alaska 99775-1005 Anchorage, Alaska 995 13-7589 Alaska State Library State Office Building, 8th moor 333 Willoughby Avenue Juneau, Alaska 9981 1-0571 This publication released by the Division of Geological & Geophysical Surveys, was -
Ecoregion-Based Conservation in the Bering Sea
Ecoregion-Based Conservation in the Bering Sea Identifying Important Areas for Biodiversity Conservation Contents Page# PART ONE: INTRODUCTION 3 1.2 Why conduct…. 3 1.3 Description… 4 1.4 Biolog Signif… 4 1.5 Changes…. 4 1.6 Conservation opps.. 5 PART TWO: WORKSHOP REPORT 8 2.1 Methodology: Assessing Biodiversity 8 2.2 Experts Workshop 10 2.3 Selecting Conservation Priorities:The Approach 10 Subregions: Bering Strait Bering Sea Shelf Kamchatka Shelf and Coast Aleutian Islands Aleutian Basin Taxa Birds Mammals Fish Invertebrates 2.4 Threat Assessment Summary 13 2.5 Additional Issues of Concern 16 PART THREE: BEYOND MAPS, TOWARD CONSERVATION 19 3.1 Lessons from Girdwood Workshop 19 3.2 Next Steps 21 Edited by: David Banks, Margaret 3.3 The Nature Conservancy and the Bering Sea 22 Williams John Pearce, Alan Springer, 3.4 WWF and the Bering Sea 22 Randy Hagenstein, and David Olson APPENDIX A: MAPS 2-9 A1 Publication design by Eric Cline 2 Subregions of the Bering Sea A2 3 Priority Bird Areas A3 Maps and GIS Data by: Emma BIRD TABLE A4 Underwood, Jennifer D’Amico, 4 Priority Mammal Areas A5 Carrie Wolfe, and Julie Maier MAMMAL TABLE A6 5 Priority Fish Areas A7 A collaborative effort by the FISH TABLE A8 World Wildlife Fund, 6 Priority Invertebrate Areas A9 The Nature Conservancy of Alaska, INVERT TABLE A10 and Participants in the 7 Overlapping Priority Areas for all Taxa A11 Girdwood Bering Sea Experts 8 Priority Areas for Bering Sea Biodiversity A12 Workshop March 20-23, 1999 9 Existing Protected Areas of the Bering Sea A13 Cover photo of walruses by Kevin APPENDIX B: PRIORITY AREA DESCRIPTIONS B1 Schafer, provided courtesy of the photographer APPENDIX C: LITERATURE CITED IN APP. -
Gulf of Al Aska
274 ¢ U.S. Coast Pilot 9, Chapter 6 Chapter 9, Pilot Coast U.S. 160°W 158°W 156°W 154°W 152°W 150°W Chart Coverage in Coast Pilot 9—Chapter 6 C OOK INLET NOAA’s Online Interactive Chart Catalog has complete chart coverage http://www.charts.noaa.gov/InteractiveCatalog/nrnc.shtml Cape Douglas 166°W 164°W 162°W 16603 AFOGNAK ISLAND I T 58°N 16575 A R T 16576 S BRISTOL BAY F 16570 O ND I K LA L IS E H K S IA A D L O S U K I N N E P 16566 16587 N 16568 A Trinity Islands K S A L A 56°N Semidi Islands 16556 Chirikof Island 16553 16561 PAVLOV BAY 16580 16551 Kupreanof Point ISANOTSKI STRAIT 16549 Shumagin Island Unimak Island 16535 GULF OF ALASKA Sanak Island UNIMAK PASS 16547 54°N 16540 26 SEP2021 26 SEP 2021 U.S. Coast Pilot 9, Chapter 6 ¢ 275 Alaska Peninsula (1) This chapter describes the south coast of the Alaska (7) Peninsula from Cape Douglas to Isanotski Strait as well Local magnetic disturbance as the Semidi Islands, Shumagin Islands, Sanak Islands (8) Differences from the normal variation of as much as and many other smaller off-lying islands that fringe this 14° have been observed along the Alaska Peninsula. part of the coast. Also described are Katmai Bay, Wide (9) Bay, Chignik Bay, Stepovak Bay, Unga Strait, Pavlof Currents Bay, Ikatan Bay, Isanotski Strait and many smaller bays (10) A continual current of considerable strength follows and lagoons, and the fishing communities of Sand Point, the coast all the way from Shelikof Strait to the Aleutian King Cove, Cold Bay and False Pass. -
Geology of Umnak and Bogoslof Islands Aleutian Islands Alaska
Geology of Umnak and Bogoslof Islands Aleutian Islands Alaska By F. M. BYERS, JR. INVESTIGATIONS OF ^ALASKAN VOLCANOES GEOLOGICAL SURVEY BULLETIN 1028-L Prepared in cooperation with the Office, Chief of Engineers, U.S. Army UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington 25, D.C. PEEFACE In October 1945 the War Department (now Department of the Army) requested the Geological Survey to undertake a program of volcano investigations in the Aleutian Islands-Alaska Peninsula area. Field studies under general direction of G. D. Robinson, were begun as soon as weather permitted in the spring of 1946. The results of the first year's field, laboratory, and library work were assembled as two administrative reports. Part of the data was published in 1950 in Geological Survey Bulletin 974-B, "Volcanic Activity in the Aleutian Arc", by Robert R. Coats. The rest of the data has been included in Bulletin 1028. The geologic investigations covered by this report were recon naissance. The factual information presented is believed to be accu rate, but many of the tentative interpretations and conclusions will be modified as the investigations continue and knowledge grows. The investigations of 1946 were supported almost entirely by the Military Intelligence Division of the Office, Chief of Engineers, U.S. Army. The Geological Survey is indebted to that Office for its early recognition of the value of geologic studies in the Aleutian region, which made this report possible, and for its continuing support. -
Reconstructing the St . Lawrence Island Kayak
RECONSTRUCTING THE ST. LAWRENCE ISLAND KAYAK: FROM FORGOTTEN WATERCRAFT TO A BERING SEA MARITIME NETWORK Evguenia Anichtchenko Center for Maritime Archaeology, University of Southampton, 7009 Madelynne Way, Anchorage, AK 99504; [email protected] ABSTRACT St. Lawrence Island kayaks are absent in both museum collections and written historical sources. At the same time, the pictorial record, indigenous oral lore, and archaeological data point to uninter- rupted use of kayaks well into the beginning of the twentieth century. Drawing on the analysis of kayak data from four archaeological sites, this article reconstructs structural details and discusses the history of the St. Lawrence kayak over the last millennium; it also analyzes the values of these data for understanding prehistoric maritime networks of the Bering Sea. The Bering Sea has one of the richest and most varied tradi- al Alaska, kayaks were still in use in 1910–1920s, when tions of indigenous kayaks in the entire circumpolar north. their significance for subsistence hunting was challenged Together with the Aleutian chain, the region features eight by easy access to different technologies (Golden 2015:11; ethnographic kayak variants, representing all indigenous Nelson 1969:308). By that time, however, examples of eth- coastal and insular nations with two noticeable excep- nographic kayaks had been acquired by museums around tions: the St. Lawrence and Diomede islanders (Adney the world, and the interest generated sent researchers to and Chapelle 2007:190–202; Zimmerly 2000a:39–62). distant communities to record the extant knowledge of This absence is particularly intriguing in the case of St. boat builders and surviving boat frames. -
Amlia Sill Ocean Or Sea: Bering Sea
INTERNATIONAL HYDROGRAPHIC INTERGOVERNMENTAL OCEANOGRAPHIC ORGANIZATION COMMISSION (of UNESCO) UNDERSEA FEATURE NAME PROPOSAL (See IHO-IOC Publication B-6 and NOTE overleaf) Note: The boxes will expand as you fill the form. Name Proposed: Amlia Sill Ocean or Sea: Bering Sea Geometry that best defines the feature (Yes/No) : Point Line Polygon Multiple points Multiple lines* Multiple Combination of polygons* geometries* Yes Yes No No No No Yes * Geometry should be clearly distinguished when providing the coordinates below. Lat. (e.g. 63°32.6’N) Long. (e.g. 046°21.3’W) Point (173 m) 52° 31.8’N Point (173 m) 173° 26.5’W Line Start (183 m) 52° 28.1’N Line Start (183 m) 173° 35.5’W Line Mid1 (173 m) 52° 31.8’N Line Mid1 (173 m) 173° 26.5’W Coordinates: Line Mid2 (203 m) 52° 34.6’N Line Mid2 (203 m) 173° 14.9’W Line Mid3 (383 m) 52° 35.3’N Line Mid3 (383 m) 173° 10.3’W Line Mid4 (483 m) 52° 36.2’N Line Mid4 (483 m) 172° 54.5’W Line End (185 m) 52° 36.7’N Line End (185 m) 172° 41.3’W Maximum Depth: 1050 m Steepness : 1.1° Feature Minimum Depth : 173 m Shape : elliptical Description: Total Relief : 877 m Dimension/Size : 70000 m long/ ~6000 m wide Associated Features: Umnak canyons, Amlia Canyon Shown Named on Map/Chart: Chart/Map References: Shown Unnamed on Map/Chart: US Nav. Chart 16480 Within Area of Map/Chart: Reason for Choice of Name (if a Amlia Sill partially separates Amlia Basin from the Aleutian Basin.