May 1954 NAMES and DEFINITIONS of REGIONS, DISTRICTS, and SUBDISTRICTS in ALASKA
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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. -
Spotted Seals, Phoca Largha, in Alaska
Spotted Seals, Phoca largha, in Alaska Item Type article Authors Rugh, David J.; Shelden, Kim E. W.; Withrow, David E. Download date 09/10/2021 03:34:27 Link to Item http://hdl.handle.net/1834/26448 Spotted Seals, Phoca largha, in Alaska DAVID J. RUGH, KIM E. W. SHELDEN, and DAVID E. WITHROW Introduction mine the abundance, distribution, and lar), a 2-month difference in mating sea stock identification of marine mammals sons (effecting reproductive isolation), Under the reauthorization of the Ma that might have been impacted by com the whitish lanugo on newborn P largha rine Mammal Protection Act (MMPA) mercial fisheries in U.S. waters (Bra that is shed in utero in P vitulina, dif in 1988, and after a 5-year interim ex ham and DeMaster1). For spotted seals, ferences in the adult pelage of P largha emption period ending September 1995, Phoca largha, there were insufficient and P vitulina, and some differences in the incidental take of marine mammals data to determine incidental take lev cranial characteristics (Burns et aI., in commercial fisheries was authorized els. Accordingly, as a part of the MMAP, 1984). However, hybridization may if the affected populations were not ad the NMFS National Marine Mammal occur, based on evidence from morpho versely impacted. The Marine Mammal Laboratory (NMML) conducted a study logical intermediates and overlaps in Assessment Program (MMAP) of the of spotted seals in Alaska. The objec range (Bums et aI., 1984). As such, dif National Marine Fisheries Service tives of this study were to: I) provide a ferentiation of these two species in the (NMFS), NOAA, provided funding to review of literature pertaining to man field is very difficult. -
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. -
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 ............... -
Land Cover Mapping of the National Park Service Northwest Alaska Management Area Using Landsat Multispectral and Thematic Mapper Satellite Data
Land Cover Mapping of the National Park Service Northwest Alaska Management Area Using Landsat Multispectral and Thematic Mapper Satellite Data By Carl J. Markon and Sara Wesser Open-File Report 00-51 U.S. Department of the Interior U.S. Geological Survey LAND COVER MAPPING OF THE NATIONAL PARK SERVICE NORTHWEST ALASKA MANAGEMENT AREA USING LANDSAT MULTISPECTRAL AND THEMATIC MAPPER SATELLITE DATA By Carl J. Markon1 and Sara Wesser2 1 Raytheon SIX Corp., USGS EROS Alaska Field Office, 4230 University Drive, Anchorage, AK 99508-4664. E-mail: [email protected]. Work conducted under contract #1434-CR-97-40274 2National Park Service, 2525 Gambell St., Anchorage, AK 99503-2892 Land Cover Mapping of the National Park Service Northwest Alaska Management Area Using Landsat Multispectral Scanner and Thematic Mapper Satellite Data ABSTRACT A land cover map of the National Park Service northwest Alaska management area was produced using digitally processed Landsat data. These and other environmental data were incorporated into a geographic information system to provide baseline information about the nature and extent of resources present in this northwest Alaskan environment. This report details the methodology, depicts vegetation profiles of the surrounding landscape, and describes the different vegetation types mapped. Portions of nine Landsat satellite (multispectral scanner and thematic mapper) scenes were used to produce a land cover map of the Cape Krusenstern National Monument and Noatak National Preserve and to update an existing land cover map of Kobuk Valley National Park Valley National Park. A Bayesian multivariate classifier was applied to the multispectral data sets, followed by the application of ancillary data (elevation, slope, aspect, soils, watersheds, and geology) to enhance the spectral separation of classes into more meaningful vegetation types. -
UNIVERSITY of CALIFORNIA RIVERSIDE a New
UNIVERSITY OF CALIFORNIA RIVERSIDE A New Species of an Enigmatic Fossil Taxon: Ischadites n. sp., a Middle Ordovician Receptaculitid From the Great Basin, Western USA A Thesis submitted in partial satisfaction of the requirements for the degree of Master of Science in Geological Sciences by Sara E Henry June 2014 Thesis Committee: Dr. Mary L. Droser, Chairperson Dr. Nigel C. Hughes Dr. Richard Minnich Copyright by Sara E Henry 2014 The Thesis of Sara E Henry is approved: Committee Chairperson University of California, Riverside ACKNOWLEDGEMENTS First and foremost, I would like to express my sincere gratitude to my advisor, Dr. Mary L. Droser, for her continuous support throughout my graduate studies, field work, and research. I’d additionally like to thank the rest of my committee: Dr. Nigel C. Hughes and Dr. Richard Minnich for their encouragement, insight, and guidance. Dr. Ganqing Jiang of the University of Nevada, Las Vegas, assisted with stratigraphic measurements and provided valuable consultation on sedimentological interpretation in the field. Illustrations of Ischadites n. sp. were produced by my very talented brother, Mr. Keith R. Henry. Several field assistants allowed for large bulk sampling of fossils over multiple field work excursions: T. Beck, M. Nonu, R. Theroux, and J. Minor. Special thanks to L. Graham and T. Beck for lab work assistance. Field work required for this project was funded by the Geological Society of America, the Society for Sedimentary Geology, and the Gulf Coast Section of the Society for Sedimentary Geology. Lastly, I have to thank my parents, Kim and Susan Henry, for their unwavering support, patience, and encouragement. -
Aleutian Islands
Journal of Global Change Data & Discovery. 2018, 2(1): 109-114 © 2018 GCdataPR DOI:10.3974/geodp.2018.01.18 Global Change Research Data Publishing & Repository www.geodoi.ac.cn Global Change Data Encyclopedia Aleutian Islands Liu, C.1* Yang, A. Q.2 Hu, W. Y.1 Liu, R. G.1 Shi, R. X.1 1. Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; 2. Institute of Remote Sensing and Digital Earth,Chinese Academy of Sciences,Beijing100101,China Keywords: Aleutian Islands; Fox Islands; Four Mountains Islands; Andreanof Islands; Rat Islands; Near Islands; Kommandor Islands; Unimak Island; USA; Russia; data encyclopedia The Aleutian Islands extends latitude from 51°12′35″N to 55°22′14″N and longitude about 32 degrees from 165°45′10″E to 162°21′10″W, it is a chain volcanic islands belonging to both the United States and Russia[1–3] (Figure 1, 2). The islands are formed in the northern part of the Pacific Ring of Fire. They form part of the Aleutian Arc in the Northern Pacific Ocean, extending about 1,900 km westward from the Alaska Peninsula to- ward the Kamchatka Peninsula in Russia, Figure 1 Dataset of Aleutian Islands in .kmz format and mark a dividing line between the Ber- ing Sea to the north and the Pacific Ocean to the south. The islands comprise 6 groups of islands (east to west): the Fox Islands[4–5], islands of Four Mountains[6–7], Andreanof Islands[8–9], Rat Islands[10–11], Near Is- lands[12–13] and Kommandor Islands[14–15]. -
Beaufort Sea: Hypothetical Very Large Oil Spill and Gas Release
OCS Report BOEM 2020-001 BEAUFORT SEA: HYPOTHETICAL VERY LARGE OIL SPILL AND GAS RELEASE U.S. Department of the Interior Bureau of Ocean Energy Management Alaska OCS Region OCS Study BOEM 2020-001 BEAUFORT SEA: HYPOTHETICAL VERY LARGE OIL SPILL AND GAS RELEASE January 2020 Author: Bureau of Ocean Energy Management Alaska OCS Region U.S. Department of the Interior Bureau of Ocean Energy Management Alaska OCS Region REPORT AVAILABILITY To download a PDF file of this report, go to the U.S. Department of the Interior, Bureau of Ocean Energy Management (www.boem.gov/newsroom/library/alaska-scientific-and-technical-publications, and click on 2020). CITATION BOEM, 2020. Beaufort Sea: Hypothetical Very Large Oil Spill and Gas Release. OCS Report BOEM 2020-001 Anchorage, AK: U.S. Department of the Interior, Bureau of Ocean Energy Management, Alaska OCS Region. 151 pp. Beaufort Sea: Hypothetical Very Large Oil Spill and Gas Release BOEM Contents List of Abbreviations and Acronyms ............................................................................................................. vii 1 Introduction ........................................................................................................................................... 1 1.1 What is a VLOS? ......................................................................................................................... 1 1.2 What Could Precipitate a VLOS? ................................................................................................ 1 1.2.1 Historical OCS and Worldwide -
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. -
Straddling the Arctic Circle in the East Central Part of the State, Yukon Flats Is Alaska's Largest Interior Valley
Straddling the Arctic Circle in the east central part of the State, Yukon Flats is Alaska's largest Interior valley. The Yukon River, fifth largest in North America and 2,300 miles long from its source in Canada to its mouth in the Bering Sea, bisects the broad, level flood- plain of Yukon Flats for 290 miles. More than 40,000 shallow lakes and ponds averaging 23 acres each dot the floodplain and more than 25,000 miles of streams traverse the lowland regions. Upland terrain, where lakes are few or absent, is the source of drainage systems im- portant to the perpetuation of the adequate processes and wetland ecology of the Flats. More than 10 major streams, including the Porcupine River with its headwaters in Canada, cross the floodplain before discharging into the Yukon River. Extensive flooding of low- land areas plays a dominant role in the ecology of the river as it is the primary source of water for the many lakes and ponds of the Yukon Flats basin. Summer temperatures are higher than at any other place of com- parable latitude in North America, with temperatures frequently reaching into the 80's. Conversely, the protective mountains which make possible the high summer temperatures create a giant natural frost pocket where winter temperatures approach the coldest of any inhabited area. While the growing season is short, averaging about 80 days, long hours of sunlight produce a rich growth of aquatic vegeta- tion in the lakes and ponds. Soils are underlain with permafrost rang- ing from less than a foot to several feet, which contributes to pond permanence as percolation is slight and loss of water is primarily due to transpiration and evaporation. -
2014 Draft Fisheries Monitoring Plan
2014 Draft Fisheries Monitoring Plan TABLE OF CONTENTS EXECUTIVE SUMMARY ....................................................................................................... 1 INTRODUCTION ..................................................................................................................... 2 Continuation Projects in 2014 ................................................................................................. 7 Technical Review Committee Membership .............................................................................. 8 Technical Review Committee, Regional Advisory Council, and Interagency Staff Committee Recommendations .................................................................................................................. 9 Summary of Regional Advisory Council Recommendations and Rationale .............................. 15 NORTHERN REGION OVERVIEW .................................................................................... 19 14-101 - Unalakleet River Chinook Salmon Assessment Continuation .................................... 25 14-102 - Climate change and subsistence fisheries: quantifying the direct effects of climatic warming on arctic fishes and lake ecosystems using whole-lake manipulations on the Alaska North Slope ........................................................................................................................... 27 14-103 - Dispersal patterns and summer ocean distribution of adult Dolly Varden in the Beaufort Sea using satellite telemetry .................................................................................. -
Geothermometry of Selected Montana Hot Spring Waters by Michael
Geothermometry of selected Montana hot spring waters by Michael Bernard Kaczmarek A thesis submitted to the Graduate Faculty in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE with concentration in Geology Montana State University © Copyright by Michael Bernard Kaczmarek (1974) Abstract: The base temperature of hot-water dominated hydro-thermal systems can be quantitatively estimated using two different methods. One method uses the concentration of dissolved silica in the discharge wasters in equilibrium with respect to quarts. The other method is based on the ha, K, and Ca concentrations in the discharge waters in equilibrium with solid mineral phases in the wall rocks. Experimental studies and practical applications of these two hydrogeothermometers have been largely limited to the temperature range of 200 to 360°C. This paper presents some results of application of both methods in the temperature range 15 to 150°C. Dissolved silica calculated base temperatures are reliable for undiluced thermal waters in the temperature range studied. Sources of error are cold water dilution of thermal waters and assimilation of silica from amorphous silica in wall rocks. Base temperatures calculated from Na, K, and Ca concentrations in discharge waters are generally inaccurate. Errors in the calculated temperatures result from the fact that net water/rock reactions in the temperature range 15 to 150°C may be significantly different from those in the range 200 to 360°C, Net water/ rock reactions for the temperature range 15 to 150°C are presented here and the importance of E-mica versus kaolinite mineral phase stability is discussed.