Notes on the Geology of the Alaska Peninsula and Aleutian Islands
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Polystichum Aleuticum) Field Survey at Atka Island, Alaska
U.S. Fish and Wildlife Service INTRA-SERVICE BIOLOGICAL OPINION For 2016 Aleutian Shield Fern (Polystichum aleuticum) Field Survey at Atka Island, Alaska To the Anchorage Fish and Wildlife Field Office Prepared by: Fairbanks Fish and Wildlife Field Office Anchorage, Alaska July 25, 2016 Table of Contents 1. Introduction ............................................................................................................................1 2. Description of the Proposed Action .......................................................................................1 Project Overview ...........................................................................................................1 Minimization Measures .................................................................................................3 Action Area ....................................................................................................................3 5. Status of the Species ..............................................................................................................4 6. Environmental Baseline .........................................................................................................6 7. Effects of the Action on Listed Species .................................................................................7 8. Cumulative Effects .................................................................................................................7 9. Conclusion .............................................................................................................................8 -
Two New Subspecies of Birds from Alaska
May, 1944 121 TWO NEW SUBSPECIES OF BIRDS FROM ALASKA By OLAUS J. MURIE In the preparation of manuscript for a forthcoming publication on the “Fauna of the Aleutian Islands and Alaska Peninsula,” numerous specimens were critically ex- amined at the IJnited States National Museum and the American Museum of Natural History. It became apparent that at least two forms of birds were sufficiently distinct to merit names as subspecies.Because of probable delay in the publication of the entire report, the descriptions of these two new forms are presented herewith. Lagopus mutus gabrielsoni, new subspecies Amchitka Rock Ptarmigan Lagopus rupestrisatHzenGs Turner. Contr. Nat. Hist. Alaska, 1886:155-156,part (Amchitka, plentiful) ; Macoun, Cat. Canadian Birds, 1900:208,part (Amchitka) ; Macoun and Macoun, Cat. Canadian Birds, ed. 2, 1909:227,part (Amchitka). Type.-Adult male, no. 4150 I. N. Gahrielson Collection; Amchitka Island, Aleutian Islands, Alaska, June 28, 1940; collectedby I. N. Gabrielson. Des&&n.--The ground color of the type, representingthe summer plumage, varies from ochraceousbuff to buckthorn brown (of Ridgway), with local areas approaching pale olive buff. The dark bars are relqtively broad and fairly evenly distributed throughout. White spots appear on the throat in moderate number. L. ?IZ.gabrielsoni in summer plumage differs from townsendi (from Kiska Island) in having heavier and darker barring; on the average this heavy barring extends farther down the flanks and back. In other words, coarsebarring is not restrictedto the anterior part of the body as in tounrirendi. The ground color is paler, lessochraceous than in townsendi. L. m. gabrielsoti differs from sanjordi of the islandseast of Amchitka in having more uniformly dark ground color and broad bars. -
Prehistoric Aleut Influence at Port Moller
12 'i1 Pribilof lis. "' Resale for so 100 150 200 ·o oO Miles .,• t? 0 Not Fig. 1. Map of the Alaska Peninsula and Adjacent Areas. The dotted line across the Peninsula represents the Aleut boundary as determined by Petroff. Some of the important archaeological sites are marked as follows: 1) Port Moller, 2) Amaknak Island-Unalaska Bay, 3) Fortress or Split Rock, 4) Chaluka, 5) Chirikof Island, 6) Uyak, 7) Kaflia, 8) Pavik-Naknek Drainage, 9) Togiak, 10) Chagvan Bay, 11) Platinum, 12) Hooper Bay. PREHISTORIC ALEUT INFLUENCES AT PORT MOLLER, ALASKA 1 by Allen P. McCartney Univ. of Wisconsin Introduction Recent mention has been made of the Aleut influences at the large prehistoric site at Port Moller, the only locality known archaeologically on the southwestern half of the Alaska Penin sula. Workman ( 1966a: 145) offers the following summary of the Port Moller cultural affinities: Although available published material from the Aleutians is scarce and the easternmost Aleutians in particular have been sadly neglected, it is my opinion that the strongest affinitiesResale of the Port Moller material lie in this direction. The prevalence of extended burial and burial association with ocher at Port Moller corresponds most closely with the burial practices at the Chaluka site on Umnak Island. Several of the more diagnostic projectile points have Aleutian affinities as do the tanged knives and, possibly,for the side-notched projectile point. Strong points of correspondence, particularly in the burial practices and the stone technology, lead me to believe that a definite Aleut component is represented at the site. Data currently available will not allow any definitive statement as to whether or not there are other components represented at the site as well. -
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 ............... -
Resource Utilization in Atka, Aleutian Islands, Alaska
RESOURCEUTILIZATION IN ATKA, ALEUTIAN ISLANDS, ALASKA Douglas W. Veltre, Ph.D. and Mary J. Veltre, B.A. Technical Paper Number 88 Prepared for State of Alaska Department of Fish and Game Division of Subsistence Contract 83-0496 December 1983 ACKNOWLEDGMENTS To the people of Atka, who have shared so much with us over the years, go our sincere thanks for making this report possible. A number of individuals gave generously of their time and knowledge, and the Atx^am Corporation and the Atka Village Council, who assisted us in many ways, deserve particular appreciation. Mr. Moses Dirks, an Aleut language specialist from Atka, kindly helped us with Atkan Aleut terminology and place names, and these contributions are noted throughout this report. Finally, thanks go to Dr. Linda Ellanna, Deputy Director of the Division of Subsistence, for her support for this project, and to her and other individuals who offered valuable comments on an earlier draft of this report. ii TABLE OF CONTENTS ACKNOWLEDGMENTS . e . a . ii Chapter 1 INTRODUCTION . e . 1 Purpose ........................ Research objectives .................. Research methods Discussion of rese~r~h*m~t~odoio~y .................... Organization of the report .............. 2 THE NATURAL SETTING . 10 Introduction ........... 10 Location, geog;aih;,' &d*&oio&’ ........... 10 Climate ........................ 16 Flora ......................... 22 Terrestrial fauna ................... 22 Marine fauna ..................... 23 Birds ......................... 31 Conclusions ...................... 32 3 LITERATURE REVIEW AND HISTORY OF RESEARCH ON ATKA . e . 37 Introduction ..................... 37 Netsvetov .............. ......... 37 Jochelson and HrdliEka ................ 38 Bank ....................... 39 Bergslind . 40 Veltre and'Vll;r;! .................................... 41 Taniisif. ....................... 41 Bilingual materials .................. 41 Conclusions ...................... 42 iii 4 OVERVIEW OF ALEUT RESOURCE UTILIZATION . 43 Introduction ............ -
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. -
Wildlife Protection Guidelines for Alaska
Wildlife Protection Guidelines for Alaska Alaska Regional Response Team, Wildlife Protection Committee Revision 5 – August 2012 2018 Administrative Update Revision 5 – August 2012 Administrative Update: March 2018 1 Table of Contents I. Introduction ........................................................................................................................... G-5 A. Background G-5 B. Objectives ........................................................................................................................... G-5 C. Scope of Wildlife Protection Guidelines for Alaska ............................................................... G-6 1. Geographic Area ............................................................................................................. G-6 2. Wildlife Resources .......................................................................................................... G-8 3. Wildlife Resource Agencies ............................................................................................. G-8 D. Committee Organization and Development of Guidelines ................................................... G-8 1. Committee Organization ................................................................................................. G-8 2. Development of Guidelines ............................................................................................ G-9 E. Relationship to National Planning Requirements and Guidance .......................................... G-9 F. Procedures for Revisions and -
Identifying Nesting Habitat of Kittlitz's
Kenney & Kaler: NestingShort habitat Notes of Kittlitz’s Murrelets 73 IDENTIFYING NESTING HABITAT OF KITTLITZ’S MURRELETS BRACHYRAMPHUS BREVIROSTRIS: OLD NESTS LEAD TO A NEW BREEDING RECORD LEAH A. KENNEY1 & ROBB S.A. KALER2 1Alaska Maritime National Wildlife Refuge, Homer, AK, USA ([email protected]) 2Migratory Bird Management, US Fish and Wildlife Service, Anchorage, AK, USA Received 2 September 2012, accepted 27 December 2012 Kittlitz’s Murrelet (Brachyramphus brevirostris) is one of the rarest Kittlitz’s Murrelets at Agattu Island (hereafter, Agattu). In 2009, the breeding seabirds in the North Pacific and one of the least known second year of the Agattu murrelet study, we revisited all previously in North America. With a patchy distribution in both Alaska and discovered nests and noted that several nest sites had increased the Russian Far East, the Kittlitz’s Murrelet population in Alaska plant cover compared with the surrounding area. Specifically, nest is estimated at 19 578 individuals (range 8 190–36 193; BirdLife scrapes where a murrelet chick survived for at least 10–15 days International 2012). Owing to its small population size, restricted contained dense mosses (Tetraplodon mnioides; a coprophilous moss distribution, and an apparent rapid population decline, the US Fish usually found growing on fecal materials and animal remains) and and Wildlife Service (USFWS) has proposed Kittlitz’s Murrelet as grasses (Poaceae). Kittlitz’s Murrelet adults provision their young a candidate species for listing under the Endangered Species Act with marine fishes at the nest scrape during the 24–40 day nestling (USFWS 2009). period (Day et al. 1999, Kaler et al. -
Moose Hunters in - Southwest Alaska a Better Opportunity to Evaluate Antlers
280 AN EVALUATION OF TROPHY MOOSE MANAGEMENT ON THE ALASKA PENINSULA Christian A. Smith, Alaska Dept. of Fish and Game, King Salmon, Alaska James B. Faro, Alaska Dept. of Fish and Game, Anchorage, Alaska Nicholas C. Steen, Alaska Dept. of Fish and Game, King Salmon, Alaska '" Abstract: an experimental trophy management program was initiated on the Alaska Peninsula in 1976 with the imple mentation of a regulation requiring that all harvested bull moose (AZaes aZaes gigas) have antlers with at least a 50 inch spread. The regulation was designed to protect bulls under 5 years of age, to test the capability of hunters to comply with minimum size requirements, and to determine the potential for maintaining trophy class bulls in the population through this approach. The first two objectives have been accomplished. Nearly 70 - percent of the harvested bulls have been 5 or more years old and only 4 percent of the bulls taken were illegal. Adequate survey data are not available to determine current proportions of trophy bulls in the herd. In view of the declining nature of the population and increasing frequency - of 5 year olds in the kill, however, it seems likely that current harvests may be curtailing recruitment beyond age 5. Although this may not further affect average trophy size, availability of trophy class animals could eventually be - limited to the size of the 5 year old cohort. The moose population of the central Alaska Peninsula, Game Management - Unit 9E, appears to have established via i11111igration southwest from the Naknek River drainage in the early 1930's (Faro 1969). -
Article Is Available On- Rise Derived from Satellite Imagery, Nat
The Cryosphere, 15, 1845–1862, 2021 https://doi.org/10.5194/tc-15-1845-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Spatially and temporally resolved ice loss in High Mountain Asia and the Gulf of Alaska observed by CryoSat-2 swath altimetry between 2010 and 2019 Livia Jakob1, Noel Gourmelen1,2,3, Martin Ewart1, and Stephen Plummer4 1Earthwave Ltd, Edinburgh, EH9 3HJ, UK 2School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 3IPGS UMR 7516, Université de Strasbourg, CNRS, Strasbourg, 67000, France 4European Space Agency, ESA-ESTEC, Noordwijk, 2201 AZ, the Netherlands Correspondence: Livia Jakob ([email protected]) Received: 25 June 2020 – Discussion started: 27 July 2020 Revised: 23 February 2021 – Accepted: 26 February 2021 – Published: 14 April 2021 Abstract. Glaciers are currently the largest contributor to sea HMA ice loss is sustained until 2015–2016, with a slight de- level rise after ocean thermal expansion, contributing ∼ 30 % crease in mass loss from 2016, with some evidence of mass to the sea level budget. Global monitoring of these regions gain locally from 2016–2017 onwards. remains a challenging task since global estimates rely on a variety of observations and models to achieve the required spatial and temporal coverage, and significant differences re- main between current estimates. Here we report the first ap- 1 Introduction plication of a novel approach to retrieve spatially resolved elevation and mass change from radar altimetry over entire Glaciers store less than 1 % of the mass (Farinotti et al., 2019) mountain glaciers areas. We apply interferometric swath al- and occupy just over 4 % of the area (RGI Consortium, 2017) timetry to CryoSat-2 data acquired between 2010 and 2019 of global land ice; however their rapid rate of mass loss has over High Mountain Asia (HMA) and in the Gulf of Alaska accounted for almost a third of the global sea level rise dur- (GoA). -
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. -
Spanning the Bering Strait
National Park service shared beringian heritage Program U.s. Department of the interior Spanning the Bering Strait 20 years of collaborative research s U b s i s t e N c e h UN t e r i N c h UK o t K a , r U s s i a i N t r o DU c t i o N cean Arctic O N O R T H E L A Chu a e S T kchi Se n R A LASKA a SIBERIA er U C h v u B R i k R S otk S a e i a P v I A en r e m in i n USA r y s M l u l g o a a S K S ew la c ard Peninsu r k t e e r Riv n a n z uko i i Y e t R i v e r ering Sea la B u s n i CANADA n e P la u a ns k ni t Pe a ka N h las c A lf of Alaska m u a G K W E 0 250 500 Pacific Ocean miles S USA The Shared Beringian Heritage Program has been fortunate enough to have had a sustained source of funds to support 3 community based projects and research since its creation in 1991. Presidents George H.W. Bush and Mikhail Gorbachev expanded their cooperation in the field of environmental protection and the study of global change to create the Shared Beringian Heritage Program.