Geographic Distribution, Depth Range, and Description of Atka Mackerel Pleurogrammus Monopterygius Nesting Habitat in Alaska
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Alaska Region Revised 2020
Smithsonian Institution, National Museum of Natural History Repatriation Office Case Report Summaries Alaska Region Revised 2020 Alaska Alutiiq, Koniag, 1991 LARSEN BAY, KODIAK ISLAND Yu'pik In September 1991, the NMNH repatriated the human remains of approximately 1000 individuals from the Uyak (KOD-145) archaeological site to the Alaska Native village of Larsen Bay, and 144 funerary objects were repatriated in January 1992. The museum had received a request to repatriate these remains and artifacts in 1987, and a series of communications between the village and the Smithsonian resulted in the decision to repatriate the remains as culturally affiliated with the present day people of Larsen Bay. The burials had been excavated by a Smithsonian curator, Ales Hrdlicka, during a series of excavations in the 1930s, and dated from around 1000 B.C. to post-contact times. No report is available, but information on the site and the repatriation may be found in the following book: Reckoning With the Dead: the Larsen Bay Repatriation and the Smithsonian Institution. Edited by Tamara L. Bray and Thomas W. Killion. Published in 1994 by the Smithsonian Institution Press, Washington, D.C. Alaska Inupiat, Yu'pik, 1994 INVENTORY AND ASSESSMENT OF HUMAN REMAINS AND NANA Regional ASSOCIATED FUNERARY OBJECTS FROM NORTHEAST NORTON Corporation SOUND, BERING STRAITS NATIVE CORPORATION, ALASKA IN THE NATIONAL MUSEUM OF NATURAL HISTORY This report provides a partial inventory and assessment of the cultural affiliation of the human remains and funerary objects in the National Museum of Natural History (NMNH) from within the territorial boundaries of the Bering Strait Native Corporation. -
Miles, A.K., M.A. Ricca, R.G. Anthony, and J.A. Estes. 2009
Environmental Toxicology and Chemistry, Vol. 28, No. 8, pp. 1643–1654, 2009 ᭧ 2009 SETAC Printed in the USA 0730-7268/09 $12.00 ϩ .00 ORGANOCHLORINE CONTAMINANTS IN FISHES FROM COASTAL WATERS WEST OF AMUKTA PASS, ALEUTIAN ISLANDS, ALASKA, USA A. KEITH MILES,*† MARK A. RICCA,† ROBERT G. ANTHONY,‡ and JAMES A. ESTES§ †U.S. Geological Survey, Western Ecological Research Center, Davis Field Station, 1 Shields Avenue, University of California, Davis, California 95616 ‡U.S. Geological Survey, Oregon Cooperative Fish and Wildlife Research Unit, 104 Nash Hall, Oregon State University, Corvallis, Oregon 97331 §Department of Ecology and Evolutionary Biology, Center for Ocean Health, 100 Schaffer Road, University of California, Santa Cruz, California 95060, USA (Received 2 October 2008; Accepted 6 March 2009) Abstract—Organochlorines were examined in liver and stable isotopes in muscle of fishes from the western Aleutian Islands, Alaska, in relation to islands or locations affected by military occupation. Pacific cod (Gadus macrocephalus), Pacific halibut (Hippoglossus stenolepis), and rock greenling (Hexagrammos lagocephalus) were collected from nearshore waters at contemporary (decommissioned) and historical (World War II) military locations, as well as at reference locations. Total (⌺) polychlorinated biphenyls (PCBs) dominated the suite of organochlorine groups (⌺DDTs, ⌺chlordane cyclodienes, ⌺other cyclodienes, and ⌺chlo- rinated benzenes and cyclohexanes) detected in fishes at all locations, followed by ⌺DDTs and ⌺chlordanes; dichlorodiphenyldi- chloroethylene (p,pЈDDE) composed 52 to 66% of ⌺DDTs by species. Organochlorine concentrations were higher or similar in cod compared to halibut and lowest in greenling; they were among the highest for fishes in Arctic or near Arctic waters. Organ- ochlorine group concentrations varied among species and locations, but ⌺PCB concentrations in all species were consistently higher at military locations than at reference locations. -
The Exchange of Water Between Prince William Sound and the Gulf of Alaska Recommended
The exchange of water between Prince William Sound and the Gulf of Alaska Item Type Thesis Authors Schmidt, George Michael Download date 27/09/2021 18:58:15 Link to Item http://hdl.handle.net/11122/5284 THE EXCHANGE OF WATER BETWEEN PRINCE WILLIAM SOUND AND THE GULF OF ALASKA RECOMMENDED: THE EXCHANGE OF WATER BETWEEN PRIMCE WILLIAM SOUND AND THE GULF OF ALASKA A THESIS Presented to the Faculty of the University of Alaska in partial fulfillment of the Requirements for the Degree of MASTER OF SCIENCE by George Michael Schmidt III, B.E.S. Fairbanks, Alaska May 197 7 ABSTRACT Prince William Sound is a complex fjord-type estuarine system bordering the northern Gulf of Alaska. This study is an analysis of exchange between Prince William Sound and the Gulf of Alaska. Warm, high salinity deep water appears outside the Sound during summer and early autumn. Exchange between this ocean water and fjord water is a combination of deep and intermediate advective intrusions plus deep diffusive mixing. Intermediate exchange appears to be an annual phen omenon occurring throughout the summer. During this season, medium scale parcels of ocean water centered on temperature and NO maxima appear in the intermediate depth fjord water. Deep advective exchange also occurs as a regular annual event through the late summer and early autumn. Deep diffusive exchange probably occurs throughout the year, being more evident during the winter in the absence of advective intrusions. ACKNOWLEDGMENTS Appreciation is extended to Dr. T. C. Royer, Dr. J. M. Colonell, Dr. R. T. Cooney, Dr. R. -
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. -
Bathymetry and Geomorphology of Shelikof Strait and the Western Gulf of Alaska
geosciences Article Bathymetry and Geomorphology of Shelikof Strait and the Western Gulf of Alaska Mark Zimmermann 1,* , Megan M. Prescott 2 and Peter J. Haeussler 3 1 National Marine Fisheries Service, Alaska Fisheries Science Center, National Oceanic and Atmospheric Administration (NOAA), Seattle, WA 98115, USA 2 Lynker Technologies, Under contract to Alaska Fisheries Science Center, Seattle, WA 98115, USA; [email protected] 3 U.S. Geological Survey, 4210 University Dr., Anchorage, AK 99058, USA; [email protected] * Correspondence: [email protected]; Tel.: +1-206-526-4119 Received: 22 May 2019; Accepted: 19 September 2019; Published: 21 September 2019 Abstract: We defined the bathymetry of Shelikof Strait and the western Gulf of Alaska (WGOA) from the edges of the land masses down to about 7000 m deep in the Aleutian Trench. This map was produced by combining soundings from historical National Ocean Service (NOS) smooth sheets (2.7 million soundings); shallow multibeam and LIDAR (light detection and ranging) data sets from the NOS and others (subsampled to 2.6 million soundings); and deep multibeam (subsampled to 3.3 million soundings), single-beam, and underway files from fisheries research cruises (9.1 million soundings). These legacy smooth sheet data, some over a century old, were the best descriptor of much of the shallower and inshore areas, but they are superseded by the newer multibeam and LIDAR, where available. Much of the offshore area is only mapped by non-hydrographic single-beam and underway files. We combined these disparate data sets by proofing them against their source files, where possible, in an attempt to preserve seafloor features for research purposes. -
CCS Study EMS 90-0058 Migration of Northern Fur Seal (Callorhinus
CCS Study EMS 90-0058 Migration of northern fur seal (Callorhinus ursinus) pups in the Bering Sea. Final Report. Timothy J. Ragen and Paul K. Dayton Scripps Institution of Oceanography University of California, San Diego La Jolla, California 92093 September 1990 Minerals Management SeNice Department of the Interior Alaska CCS Region 949 East 366th Avenue Anchorage, Alaska 99508-4302 Purchase Order No. <~ --.-J ● Migration of northern fur seal (Callorhinus ursinus) pups in the Bering Sea. Final Report. Timothy J. Ragen and Paul K. Dayton Scripps Institution of Oceanography University of California, San Diego La Jolla, California 92093 September 1990 This study was funded in part by the Alaska Outer Continental Shelf Region of the Minerals Management Service, U.S. Department of the Interior, Washington, D.C., under Purchase Order No. 12523. This report has been reviewed by the Minerals Management Service and has been approved for publication. Approval does not signify that the contents necessarily reflect the view and policies of the Service, nor does mention of trade names or commercial products constitute endorsement or recommendation for use. AUTHORS AND RESPONSIBILITIES This report was written by Timothy J. Ragen, under the supervision of Paul K. Dayton. Dr. Ragen and George A. Antonelisr Jr., National Marine Mammal Laboratory, conducted the field portion of this study. ● Migration of northern fur seal (Callorhinus ursims) pups in the Bering Sea. Final Report. Table of Contents Introduction . 1 Methods . 8 Results . , . , . , . 11 Discussion . 17 Summary . 31 References . 33 MIG~TION OF NORTHERM FUR SEAL ( CALLORHINUS URSINUS) PUPS IN TEE BERING SEA INTRODUCTION The northern fur seal (Callorhinus ursinus) is arguably the most extensively studied marine mammal in the world. -
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 ............ -
Adak Army Base and Adak Naval Operating Base and Or Common Adak Naval Station (Naval Air Station Adak) 2
N?S Ferm 10-900 OMB Mo. 1024-0018 (342) NHL - WWM, PACIFIC Eip. 10-31-84 Uncled States Department off the Interior National Park Service For NPS UM only National Register off Historic Places received Inventory Nomination Form date entered See instructions in How to Complete National Register Forms Type all entries complete applicable sections ' _______ 1. Name__________________ historic Adak Army Base and Adak Naval Operating Base and or common Adak Naval Station (Naval Air Station Adak) 2. Location street & number not (or publication city, town vicinity of state Alaska code 02 county Aleutian Islands code 010 3. Classification Category Ownership Status Present Use __ district X public __ occupied __ agriculture __ museum building(s) private __ unoccupied commercial park structure both work in progress educational private residence X site Public Acquisition Accessible entertainment religious object in process X yes: restricted government __ scientific being considered .. yes: unrestricted industrial transportation __ no ,_X military __ other: 4. Owner off Property name United States Navy street & number Adak Naval Station, U.S. Department of the Navy city, town FPO Seattle vicinity of state Washington 98791 5. Location off Legal Description courthouse, registry of deeds, etc. United States Navy street & number Adak Naval Station. U.S. Department of the Navy city, town FPO Seattle state Washington 98791 6. Representation in Existing Surveys y title None has this property been determined eligible? yes J^L no date federal _ _ state __ county local depository for survey records city, town state 7. Description Condition Check one Check one __ excellent __ deteriorated __ unaltered _K original site __ good X_ ruins _X altered __ moved date _.__._. -
Long-Term Measurements of Flow Near the Aleutian Islands
Journal of Marine Research, 55,565-575,1997 Long-term measurements of flow near the Aleutian Islands by R. K. Reed’ and P. J. Stabenol ABSTRACT In summer1995, the AlaskanStream at 173.5Wwas very intense;the peakgeostrophic speed was -125 cm s-l, and the computedvolume transportabove 1000db, referred to 1000db, was 9 X lo6 m3s-l. Flow north of the central Aleutians was shallow, convoluted and weak (2- 3 X lo6 m3SK’). A sequenceof CTD castsacross Amukta Pass,spaced irregularly in time during 1993-1996,showed a meannorthward (southward) geostrophic transport of 1.0 (0.4) X lo6 m3s-t, for a net flow into the Bering Seaof 0.6 X lo6 m3s-t. The sourceof this flow wasthe Alaskan Stream exceptin 1995,when it wasBering Sea water. Results from two 13-monthcurrent mooringswest and eastof the passwere quite different.To the west,flow wasweak andvariable and appeared to have a barotropiccomponent. To the east,flow wasstronger and unidirectional eastward. 1. Introduction Upper-ocean circulation near the central Aleutian Islands is characterized by the swift, westward flowing Alaskan Stream on the southern side and by a relatively weak, eastward flow on the northern side (Favorite, 1974; Sayles et al., 1979). There is exchange between thesetwo flows, however, through the two deep passesacross the ridge near 180 and 172W (Reed and Stabeno, 1994). One of our objectives was to obtain frequent samplesof the density field acrossthe passnear 172W (Amukta Pass; Fig. l), primarily becauseit is a pathway for relatively warm (>4”C) Alaskan Stream water into the Bering Sea (Reed, 1995). -
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]. -
Geology of Little Sitkin Island, Alaska
Geology of Little Sitkin Island By G. L. SNYDER INVESTIGATIONS OF ALASKAN VOLCANOES GEOLOGICAL SURVEY BULLETIN 1028-H Prepared in cooperation with the Departments of the Army, Navy, and Air Force UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1959 UNITED STATES DEPARTMENT OF THE INTERIOR FRED A. SEATON, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director The U. S. Geological Survey Library has cataloged this publication as follows : Snyder, George Leonard, 1927- Geology of Little Sitkin Island, Alaska. Washington, U. S. Govt. Print. Off., 1958. - vi, 169-210 p. illus., 2 maps (1 fold. col. in pocket) tables. 24 cm. (U. S. Geological Survey. Bulletin 1028-H. Investigations of Alas- kan volcanoes) Prepared in cooperation with the Departments of the Army, Navy, and Air Force. "References cited" : p. 206-207. 1. Rocks, Igneous. 2. Petrology Aleutian Islands. 3. Little Sitkin Island. I. Title. (Series: U. S. Geological Survey. Bulletin 1028-H. Series: U. S. Geological Survey. Investigations of Alaskau volcanoes) 557.98 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington 25, D. C. PKEFACE 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. The field studies were made during the years 1946-1954. The results of the first year's field, laboratory, and library work were hastily assembled as two administrative reports, and most of these data have been revised for publication in Geological Survey Bulletin 1028. Part of the early work was published in 1950 in Bulletin 974-B, Volcanic activity in the Aleutian arc, and in 1951 in Bulletin 989-A, Geology of Buldir Island, Aleutian Islands, Alaska, both by Robert R. -
North Pacific Internal Tides from the Aleutian Ridge
Journalof Marine Research, 59, 167–191, 2001 Journal of MARINE RESEARCH Volume59, Number 2 NorthPaci c internaltides fromthe Aleutian Ridge: Altimeterobservations andmodeling byPatrickF. Cummins 1,JosefY. Cherniawsky 1 andMichael G. G.Foreman 1 ABSTRACT Internaltides radiating into the North Paci c fromthe Aleutian Ridge near Amukta Pass are examinedusing 7 yearsof Topex/ Poseidonaltimeter data. The observations show coherent southwardphase propagation at the M2 frequencyover a distanceof atleast1100 km intothe central Pacic. Barotropicand baroclinic models are applied to study this internal tidal signal. Results from thebarotropic model show that the strongest cross-slope volume and energy uxesoccur in the vicinityof Amukta Pass, helping to establish this region as an important site for baroclinic energy conversionalong the eastern half of theridge. Atwo-dimensionalversion of the Princeton Ocean Model is used to simulate internal tide generationand propagation. A comparisonbetween the altimeter data south of the ridge and the sea-surfacesignature of theinternal tide signal of the model shows good agreement for the phase, bothclose to thesourceand well into the far eld.Comparison of thephase between model and data alsoprovides evidence for wave refraction. This occurs due to the slow modulation of wavelength associatedwith the variation in the Coriolis parameter encountered as the internal tide propagates southward.The model results suggest that the net rate of conversion of barotropic to baroclinic energyis about 1.8 GW inthe vicinity of Amukta Pass. This represents about 6% of the local barotropicenergy uxacrossthe ridge and perhaps 1% ofglobalbaroclinic conversion. 1.Introduction Prior tothelaunch of the Topex-Poseidon (T/ P)missionin August,1992, it was widely heldthat oceanic internal tides generally did not propagate more than short distance away from asourceregion before becoming ‘ incoherent,’that is, before losing their phase relationwith the generating surface tide.