Traditional Knowledge and Norton Sound/Bering Strait Salmon Populations
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Forage Fishes of the Southeastern Bering Sea Conference Proceedings
a OCS Study MMS 87-0017 Forage Fishes of the Southeastern Bering Sea Conference Proceedings 1-1 July 1987 Minerals Management Service Alaska OCS Region OCS Study MMS 87-0017 FORAGE FISHES OF THE SOUTHEASTERN BERING SEA Proceedings of a Conference 4-5 November 1986 Anchorage Hilton Hotel Anchorage, Alaska Prepared f br: U.S. Department of the Interior Minerals Management Service Alaska OCS Region 949 East 36th Avenue, Room 110 Anchorage, Alaska 99508-4302 Under Contract No. 14-12-0001-30297 Logistical Support and Report Preparation By: MBC Applied Environmental Sciences 947 Newhall Street Costa Mesa, California 92627 July 1987 CONTENTS Page ACKNOWLEDGMENTS .............................. iv INTRODUCTION PAPERS Dynamics of the Southeastern Bering Sea Oceanographic Environment - H. Joseph Niebauer .................................. The Bering Sea Ecosystem as a Predation Controlled System - Taivo Laevastu .... Marine Mammals and Forage Fishes in the Southeastern Bering Sea - Kathryn J. Frost and Lloyd Lowry. ............................. Trophic Interactions Between Forage Fish and Seabirds in the Southeastern Bering Sea - Gerald A. Sanger ............................ Demersal Fish Predators of Pelagic Forage Fishes in the Southeastern Bering Sea - M. James Allen ................................ Dynamics of Coastal Salmon in the Southeastern Bering Sea - Donald E. Rogers . Forage Fish Use of Inshore Habitats North of the Alaska Peninsula - Jonathan P. Houghton ................................. Forage Fishes in the Shallow Waters of the North- leut ti an Shelf - Peter Craig ... Population Dynamics of Pacific Herring (Clupea pallasii), Capelin (Mallotus villosus), and Other Coastal Pelagic Fishes in the Eastern Bering Sea - Vidar G. Wespestad The History of Pacific Herring (Clupea pallasii) Fisheries in Alaska - Fritz Funk . Environmental-Dependent Stock-Recruitment Models for Pacific Herring (Clupea pallasii) - Max Stocker. -
Fishery Management Plan for Arctic Grayling Sport Fisheries Along the Nome Road System, 2001–2004
Fishery Management Report No. 02-03 Fishery Management Plan for Arctic Grayling Sport Fisheries along the Nome Road System, 2001–2004 by Fred DeCicco April 2002 Alaska Department of Fish and Game Division of Sport Fish Symbols and Abbreviations The following symbols and abbreviations, and others approved for the Système International d'Unités (SI), are used in Division of Sport Fish Fishery Manuscripts, Fishery Data Series Reports, Fishery Management Reports, and Special Publications without definition. Weights and measures (metric) General Mathematics, statistics, fisheries centimeter cm All commonly accepted e.g., Mr., Mrs., alternate hypothesis HA deciliter dL abbreviations. a.m., p.m., etc. base of natural e gram g All commonly accepted e.g., Dr., Ph.D., logarithm hectare ha professional titles. R.N., etc. catch per unit effort CPUE kilogram kg and & coefficient of variation CV at @ 2 kilometer km common test statistics F, t, , etc. liter L Compass directions: confidence interval C.I. meter m east E correlation coefficient R (multiple) north N metric ton mt correlation coefficient r (simple) milliliter ml south S covariance cov millimeter mm west W degree (angular or ° Copyright temperature) Weights and measures (English) Corporate suffixes: degrees of freedom df cubic feet per second ft3/s Company Co. divided by ÷ or / (in foot ft Corporation Corp. equations) gallon gal Incorporated Inc. equals = inch in Limited Ltd. expected value E mile mi et alii (and other et al. fork length FL ounce oz people) greater than > O pound lb et cetera (and so forth) etc. greater than or equal to quart qt exempli gratia (for e.g., harvest per unit effort HPUE example) yard yd less than < id est (that is) i.e., ? less than or equal to latitude or longitude lat. -
Pamphlet to Accompany Scientific Investigations Map 3131
Bedrock Geologic Map of the Seward Peninsula, Alaska, and Accompanying Conodont Data By Alison B. Till, Julie A. Dumoulin, Melanie B. Werdon, and Heather A. Bleick Pamphlet to accompany Scientific Investigations Map 3131 View of Salmon Lake and the eastern Kigluaik Mountains, central Seward Peninsula 2011 U.S. Department of the Interior U.S. Geological Survey Contents Introduction ....................................................................................................................................................1 Sources of data ....................................................................................................................................1 Components of the map and accompanying materials .................................................................1 Geologic Summary ........................................................................................................................................1 Major geologic components ..............................................................................................................1 York terrane ..................................................................................................................................2 Grantley Harbor Fault Zone and contact between the York terrane and the Nome Complex ..........................................................................................................................3 Nome Complex ............................................................................................................................3 -
Eskimos, Reindeer, and Land
ESKIMOS, REINDEER, AND LAND Richard O. Stern Edward L. Arobio Larry L. Naylor and Wayne C. Thomas* Bulletin 59 December 1980 *Richard O. Stern is formerly a research associate in anthropology at the Institute of Arctic Biology, University of Alaska. Fairbanks. He is currently historian for the Alaska Department of Nat•ural Resources, Division of Forest, Land, and Water Management. Edward L. Arobio is a research associate in economics at the Agricultural Experiment Station, University of Alaska, Fairbanks. Larry L. Naylor is formerly an assistant professor of anthropology at the Department of Anthropology. University of Alaska. Fairbanks. He is currently anthropology director at North Texas State University, Denron. Wayne C. Thomas is an associate professor of economics at the Agricultural Experiment Station. University of Alaska, Fairbanks. TABLE OF CONTENTS Table of Figures Table of Photos Table of Tables Preface Chapter I–Introduction Chapter II – Reindeer Biology and Ecology Reindeer Biology and Life Cycle Forage Requirements and Carrying Capacity Antler Growth and Function Reindeer Ecology Generalized Yearly Herding Activity Chapter III – Introduction of Reindeer Herding in Alaska General Historical Summary Conditions Prior to the Introduction of Reindeer Reindeer Introduction Early Development Chapter IV – Non–Native Ownership of Reindeer: 1914–1940 Lomen and Company Epidemics, Company Herds, and Fairs Reindeer Investigations Reindeer Act of 1937 Chapter V – Native Ownership and the Period of Reconstruction: 1940–1977 The1940s The1950s -
Bottom and Near-Bottom Sediment Dynamics in Norton Sound, Alaska
BOTTOM AND NEAR-BOTTOM SEDIMENT DYNAMICS IN NORTON SOUND, ALASKA by David A. Cacchione and David E. Drake Pacific-Arctic Branch of Marine Geology U.S. Geological Survey 345 Middlefield Road Menlo Park, California 94025 Final Report Outer Continental Shelf Environmental Assessment Program Research Unit 430 April 1979 77 TABLE OF CONTENTS Page I. SUMMARY . 81 A. Overview . 81 B. Results . 81 II. INTRODUCTION . 82 A. General Nature and Scope. 82 B. Specific Objectives . 84 C. Relevance to Problems of Petroleum Development . 84 III. CURRENT STATX! OF KNOWLEDGE . 85 IV. STUDY AREA . 86 V. DATA COLLECTION . 87 VI. RESULTS . 87 A. Suspended Particulate Matter . 87 B. Temporal Variations -GEOPROBE Results . 87 Hourly Average Current Measurements . 88 Burst Data . 90 Other Current Data . 90 VII. DISCUSSION . 92 A. Transport Pathways of Suspended Matter . 92 B. Comparison of1976and 1977 Results . 96 C. Temporal Variability . 97 VIII. CONCLUSIONS . ...102 IX. NEEDS FOR FURTHER STUDY . ...103 X. REFERENCES . ...104 APPENDIXES A. ANew Instrument Systemto Investigate Sediment Dynamics on Continental Shelves (abstract) . ...107 B. Sediment Transport in Norton Sound, Alaska (abstract) . 108 C. Sediment Transport during the Winter on the Yukon Prodelta, Norton Sound, Alaska (abstract) . ...109 D. Storm-Generated Sediment Transport on the Bering Sea Shelf, Alaska (abstract) . ...110 E. Bottom Currents on the Yukon Prodelta, July8- September 25, 1977 . ...111 L SU-MNMRIY A. Overview An investigation of sediment dynamics in Norton Sound and other sections of the northern Bering Sea was conducted to define the principal pathways and mechanisms of bottom and suspended materials transport. A major topic of this research is the complicated interrelationships of sediment movement and hydrodynamic stresses that occur in the marine environment. -
Norton Sound Shaktoolik and Unalakleet Subdistricts Chinook Salmon Stock Status and Action Plan
NORTON SOUND SHAKTOOLIK AND UNALAKLEET SUBDISTRICTS CHINOOK SALMON STOCK STATUS AND ACTION PLAN A Report to the Alaska Board of Fisheries By: Wesley W. Jones Regional Information Report No. 3A03-38 Alaska Department of Fish and Game Division of Commercial Fisheries 333 Raspberry Road Anchorage, Alaska 99518 1 The Regional Information Report Series was established in 1987 to provide an information access system for all unpublished divisional reports. These reports frequently serve diverse ad hoc informational purposes or archive basic uninterpreted data. To accommodate needs for up-to-date information, reports in this series may contain preliminary data; this information may be subsequently finalized and published in the formal literature. Consequently, these reports should not be cited without prior approval of the author of the Division of Commercial Fisheries. AUTHOR Wesley W. Jones is the Assistant Area Management Biologist for the Norton Sound – Port Clarence Area and the Kotzebue Area, Alaska Department of Fish and Game, Division of Commercial Fisheries, P.O. Box 1148, Nome, AK 99762. Office Of Equal Opportunity (OEO) Statement The Alaska Department of Fish and Game 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 Americans with Disabilities Act 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, or if you desire further information please write to ADF&G, P.O. -
Digital Data for the Preliminary Bedrock Geologic Map of The
Open-File Report 2009-1254 U.S. Department of the Interior Sheet 2 of 2 U.S. Geological Survey Pamphlet accompanies map '02°761 '01°761 '00°761 LIST OF METAMORPHIC-TECTONIC ELEMENTS HIGH GRADE METAMORPHIC AND ASSOCIATED O<t Qs Ol Nome Complex, west-central – Weakly foliated metasedimentary O<l O<l IGNEOUS ROCKS – Amphibolite and granulite-facies O<l O<l Ol Ols Ols YORK TERRANE – Late Proterozoic (?) and Paleozoic sedimentary and unfoliated metaigneous rocks that retain relict primary features; and metasedimentary rocks and minor Late Cretaceous tin-bearing mineral assemblages in mafic rocks formed at pumpellyite-actinolite, metamorphic rocks and associated Cretaceous plutons; penetratively Qs greenschist, and blueschist facies (one locality) deformed metasedimentary and metaigneous schist and gneiss with Oal granites; dominantly carbonate and siliciclastic lithologies, in which Oal primary features are generally retained; fine-grained Nome Complex, eastern – Penetratively deformed and complex metamorphic histories; aluminum-rich lithologies show Ol early development of kyanite-stable mineral assemblages succeeded Ol 17 metasedimentary rocks are weakly foliated. Metamorphic and recrystallized schists with ductile fabrics; protolith packages and Ol Ols 165°00' by sillimanite-stable, lower-pressure assemblages. Lithologies rich in O<p Ols thermal history variable from unit to unit, and generally lower grade metamorphic fabrics identical to Nome Complex in central Seward Oal Qs Peninsula; mineral assemblages in most of the area are characteristic iron and aluminum retain early, relatively high pressure Ktg than Nome Complex. Tin granites intruded in shallow crustal Ols Ol aluminosilicate plus orthoamphibole assemblages (>5kb) that are Cape Espenberg settings. The generally brittle shallow and steeply-dipping structures of greenschist facies, but slightly higher grade assemblages occur in Ol the vicinity of Kiwalik Mountain. -
The PAYSTREAK Volume 12, No
The PAYSTREAK Volume 12, No. 2, Fall 2010 The Newsletter of the Alaska Mining Hall of Fame Foundation (AMHF) In this issue: AMHF New Inductees Page 1 Induction Ceremony Program Page 2 Introduction and Acknowledgements Page 3 Previous AMHF Inductees Pages 4 - 10 New Inductee Biographies Pages 10 - 23 Distinguished Alaskans Aid Foundation Page 24 Alaska Mining Hall of Fame Directors and Officers Page 24 Alaska Mining Hall of Fame Foundation New Inductees AMHF Honors Pioneers Important to the Seward Peninsula Gold Dredging Industry Nicholas B. and Evinda S. Tweet: It is difficult to name any couple in Alaska mining history that has had more longevity and perseverance than Nicholas B. and Evinda S. Tweet. In marriage, they formed a team that created a remarkably stable, family-owned firm, N.B. Tweet and Sons, which has mined gold in Alaska for 110 years. Nicholas and Evinda mined and lived in several placer mining camps, worked graphite claims, operated gold dredges, and inspired their descendants to continue the placer mining lifestyle. Both Evinda and Nick died at the family mining camp, near Taylor, north of Nome. In 2010, N.B. Tweet and Sons operated the only bucketline stacker gold dredge in North America. Carl S. (left) and Walter A. (right) Glavinovich: Two Croatian (Yugoslavian)-born brothers who, collectively, devoted more than one-hundred years of their lives to the prospecting, deciphering, drilling, thawing, and dredging of the Nome, Alaska, placer gold fields. Most of these years were in the service of one company, the U.S. Smelting, Refining, and Mining Company (USSR&M) or its direct affiliate, the Hammon Consolidated Gold Fields. -
2005 Annual Report
Norton Sound Economic Development Corporation 2005 Annual Report Brevig Mission • Diomede • Elim • Gambell • Golovin • Koyuk • Nome • Saint Michael • Savoonga • Shaktoolik • Stebbins • Teller • Unalakleet • Wales • White Mountain NSEDC MISSION STATEMENT “NSEDC will participate in and encourage the clean harvest of all Bering Sea fisheries to promote and provide economic development through educa- tion, employment, training and financial assistance to member communities and Western Alaska, while protecting subsistence resources.” RUSSIA U.S.A. RUSSIA U.S.A. Big Diomede Little Wales Diomede Brevig Mission Gambell Teller Savoonga BERING SEA Nome White Mountain Eli Koyuk Golovin NORTON SOUND Shaktoolik Unalakleet Stebbins Saint Michael The Year in Review Message From The Chairman projects as they relate to our current Commission took your comments and mission and methods for delivering incorporated them into a formula for benefits to the region. CDQ Program evolution. NSEDC and the other CDQ groups will be working A fundamental part of this process with these ideas to further develop the is to keep looking to the future to program into a form that will bring the anticipate where the company will be regulatory and statutory ability for us in terms of economic and regulatory to advance how we do business in the capability, and to integrate that with region. After amending the laws that hope the Chairman of the NSEDC the major needs of our communities. I govern the CDQ program, the next step Board of Directors never gets tired of NSEDC has been at the forefront of is to examine how NSEDC interacts with delivering the message that NSEDC has the movement to amend the program its communities. -
Special Publication No. SP2012-04
Special Publication No. SP2012-04 Subsistence Wildlife Harvests in Elim, Golovin, Kivalina, Koyuk, Noatak, and Wales, Alaska, 2010–2011 by Nicole M. Braem and Marylynne Kostick May 2014 Alaska Department of Fish and Game Division of Subsistence Symbols and Abbreviations The following symbols and abbreviations, and others approved for the Système International d'Unités (SI), are used without definition in the reports by the Division of Subsistence. 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 Mathematics, statistics centimeter cm Alaska Administrative Code AAC all standard mathematical signs, symbols deciliter dL all commonly-accepted and abbreviations gram g abbreviations e.g., alternate hypothesis HA hectare ha Mr., Mrs., base of natural logarithm e kilogram kg AM, PM, etc. catch per unit effort CPUE kilometer km all commonly-accepted coefficient of variation CV liter L professional titles e.g., Dr., Ph.D., common test statistics (F, t, 2, etc.) meter m R.N., etc. confidence interval CI milliliter mL at @ correlation coefficient (multiple) R millimeter mm compass directions: correlation coefficient (simple) r east E covariance cov Weights and measures (English) north N degree (angular ) ° cubic feet per second ft3/s south S degrees of freedom df foot ft west W expected value E gallon gal copyright greater than > inch in corporate suffixes: greater than or equal to mile mi Company Co. harvest per unit effort HPUE nautical mile nmi Corporation Corp. less than < ounce oz Incorporated Inc. -
Norton Sound Service Area
9 Norton Sound Service Area OVERVIEW Alaska Native 2006 User Population. NORTON SOUND SERVICE AREA 7,406 Norton Sound Health Corporation 7,406 Users are defined as beneficiaries who used a facility that reports through the Indian Health Service data system at least once between 10/1/2003 and 9/30/2006. Environmental Factors. The Norton Sound Service Area covers about 23,088 square miles in Northwestern Alaska on the Seward Peninsula. The area extends into the Bering Sea toward Siberia and includes Little Diomede Island, Gambell and Savoonga on St. Lawrence Island, 13 communities along the Bering Straits-Norton Sound coast and the regional center of Nome. Nome is on the south shore of the peninsula facing Norton Sound, 500 miles northwest of Anchorage. Map 9.1 Most of the Natives of the region are from three distinct language and cultural groups of Eskimos: Inupiaq, Central Yup’ik, St. Lawrence Yup’ik and Cup’ik. Nome contains about 30% of the Native population of the region. The remaining 17 communities vary in size from six summer residents in Council to 655 in Unalakleet. Most of the Native people living in the region’s villages still rely heavily on subsistence harvests of land and sea for their existence. A cool marine climate prevails in the summer, and the winters are cold. The mean January temperature is 4 degrees, with routine winter lows of -20 degrees to -40 degrees. Combined with the persistent year-round breeze, which averages 11 knots, the wind chill factor in the winter can reach -50 to -70 degrees. -
Surface and Subsurface Faulting in Norton Sound And
SURFACE AND SUBSURFACE FAULTING IN NORTON SOUND AND CHIRIKOV BASIN, ALASKA By Janice L. Johnson and Mark L. Holmes SUMMARY Seismic reflection data were obtained in July 1977 by the U. S. Geological Survey aboard R/V SEA SOUNDER along 2800 km of track in Norton Sound and northeaster Chirikov basin. These data and records from several previous surveys were analyzed in order to determine the location, extent, and possible age and activity potential of offshore faulting. Acoustic reflection records were obtained using sparkers (160 and 0.8 kilojoule), Uniboom (1200 joule), and 3.5 Id3z subbottom profiler. Sidescan sonar measurements were made along some of the tracklines when- ever the large sparker was not deployed. Maps showing the distribution of surface, near-surface, and deeper subbottom faults show that faulting occurs most commonly within 50 km of the margins of Norton basin, the deep sedimentary trough which under- lies Norton Sound and Chirikov basin. A smaller number of faults were detected in the central reg%ns of the basin. Surface fault scarps were seen in several places in northern Chirikov basin. These sea-floor offsets rafig~d .in height from 5 to 15 m along several west-trending faults which may be associated with some of the major transcurrent faults in Alaska. The existence of these scarps *. 1 indicates possible disturbance of sedimentary deposits over the fault, although the scarps may have been maintained by non-deposition. Evidence from both onshore and offshore field studies indicate that movement along these faults may have occurred between 12,000-120,000 years ago.