Sedimentary Basins of Offshore Alaska and Adjacent Regions By
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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 ............ -
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. -
THE ALEUTIAN ISLANDS: THEIR PEOPLE and NATURAL HISTORY
SMITHSONIAN INSTITUTION WAR BACKGROUND STUDIES NUMBER TWENTY-ONE THE ALEUTIAN ISLANDS: THEIR PEOPLE and NATURAL HISTORY (With Keys for the Identification of the Birds and Plants) By HENRY B. COLLINS, JR. AUSTIN H. CLARK EGBERT H. WALKER (Publication 3775) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION FEBRUARY 5, 1945 BALTIMORE, MB., U„ 8. A. CONTENTS Page The Islands and Their People, by Henry B. Collins, Jr 1 Introduction 1 Description 3 Geology 6 Discovery and early history 7 Ethnic relationships of the Aleuts 17 The Aleutian land-bridge theory 19 Ethnology 20 Animal Life of the Aleutian Islands, by Austin H. Clark 31 General considerations 31 Birds 32 Mammals 48 Fishes 54 Sea invertebrates 58 Land invertebrates 60 Plants of the Aleutian Islands, by Egbert H. Walker 63 Introduction 63 Principal plant associations 64 Plants of special interest or usefulness 68 The marine algae or seaweeds 70 Bibliography 72 Appendix A. List of mammals 75 B. List of birds 77 C. Keys to the birds 81 D. Systematic list of plants 96 E. Keys to the more common plants 110 ILLUSTRATIONS PLATES Page 1. Kiska Volcano 1 2. Upper, Aerial view of Unimak Island 4 Lower, Aerial view of Akun Head, Akun Island, Krenitzin group 4 3. Upper, U. S. Navy submarine docking at Dutch Harbor 4 Lower, Village of Unalaska 4 4. Upper, Aerial view of Cathedral Rocks, Unalaska Island 4 Lower, Naval air transport plane photographed against peaks of the Islands of Four Mountains 4 5. Upper, Mountain peaks of Kagamil and Uliaga Islands, Four Mountains group 4 Lower, Mount Cleveland, Chuginadak Island, Four Mountains group .. -
199503-81.Pdf
1981 ANNUAL REVIEW OF ACTIVITIES Institute of Ocean Sciences ----. �\�� / 1981 ANNUAL REVIEW OF ACTIVITIES Institute of Ocean Sciences PATRICIA BAY, SIDNEY, B.C. ..... Government Gouvernement I ....,.. of Canada du Canada For additional copies or further information, please write to: Department of Fisheries and Oceans Institute of Ocean Sciences P.O. Box 6000 Sidney, British Columbia, Canada VsL 4B2 Contents DEPARTMENT OF FISHERIES AND OCEANS 7 Director-General's Foreword 9 Hydrography 11 Field Hydrography 13 Chart Production and Distribution 16 Tidal and Current Surveys 18 Engineering Services 20 Oceanography 23 Ocean Physics 25 Coastal Zone Oceanography 26 Frozen Sea Research 32 Offshore Oceanography 36 Numerical Modelling 42 Remote Sensing 44 Computing Services 45 Ocean Chemistry 47 Ocean Ecology . 53 Ocean Information 56 Ships 59 Management Services 63 DEPARTMENT OF THE ENVIRONMENT 67 Atmospheric Environment Service 69 Canadian Wildlife Service 71 DEPARTMENT OF ENERGY, MINES AND RESOURCES 73 Earth Physics Branch & Geological Survey of Canada 75 Chief Scientist's Foreword 75 Seismological Service 76 Earth Structure by Seismic Methods 78 Geothermal Studies 79 Gravity 81 Geodynamics 82 Geomagnetism 83 Geological-Geophysical Studies 86 Paleontology 87 Sedimentology 87 APPENDICES I. Contracts Awarded during 1981/82 93 II. Publications 95 III. Permanent Staff, 1981 103 11 [ II : : ( [I Director-General's Foreword One of the tasks of Ocean Science and Surveys Pacific is to respond to problems arising in the development of natural resources that require hydrographic and oceanographic knowledge for their solution. In 1981 OSS Pacific became involved in two major projects of this type both of which will require substantial effort for the next 3 - 4 years. -
Aleutian Islands and Atka-Amlia Islands Management Areas Salmon Annual Management Report, 2014
Fishery Management Report No. 15-02 Aleutian Islands and Atka-Amlia Islands Management Areas Salmon Annual Management Report, 2014 by Dawn M. Wilburn and Matthew D. Keyse January 2015 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 Mathematics, statistics centimeter cm Alaska Administrative all standard mathematical deciliter dL Code AAC signs, symbols and gram g all commonly accepted abbreviations hectare ha abbreviations e.g., Mr., Mrs., alternate hypothesis HA kilogram kg AM, PM, etc. base of natural logarithm e kilometer km all commonly accepted catch per unit effort CPUE liter L professional titles e.g., Dr., Ph.D., coefficient of variation CV meter m R.N., etc. common test statistics (F, t, χ2, etc.) milliliter mL at @ confidence interval CI millimeter mm compass directions: correlation coefficient east E (multiple) R Weights and measures (English) north N correlation coefficient cubic feet per second ft3/s south S (simple) r foot ft west W covariance cov gallon gal copyright degree (angular ) ° inch in corporate suffixes: degrees of freedom df mile mi Company Co. -
ALEUTIAN ISLANDS and ATKA-AMLIA ISLANDS AREAS SALMON MANAGEMENT PLAN, 2003 by Arnold R. Shaul and Joseph J. Dinnocenzo Regional
ALEUTIAN ISLANDS AND ATKA-AMLIA ISLANDS AREAS SALMON MANAGEMENT PLAN, 2003 By Arnold R. Shaul and Joseph J. Dinnocenzo Regional Information Report1 No. 4K03-17 Alaska Department of Fish and Game Division of Commercial Fisheries 211 Mission Road Kodiak, Alaska 99615 April 2003 1The Regional Information Report Series was established in 1987 to provide an information access system for all unpublished division reports. These reports frequently serve diverse ad hoc informational purposes or archive basic uninterpreted data. To accommodate timely reporting of recently collected information, reports in this series undergo only limited internal review and 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 or the Division of Commercial Fisheries. TABLE OF CONTENTS Page LIST OF FIGURES .................................................................................................................. i ABSTRACT.............................................................................................................................. 1 ALEUTIAN ISLANDS AREA.................................................................................................. 2 ATKA-AMLIA AREA.............................................................................................................. 3 GPS COORDINATES AND ENFORCEMENT...................................................................... 4 FIGURES................................................................................................................................. -
Ridge Subduction and Slab Window Magmatism in Western North America
Cenozoic to Recent plate confi gurations in the Pacifi c Basin: Ridge subduction and slab window magmatism in western North America J.K. Madsen*† D.J. Thorkelson* Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada R.M. Friedman* Pacifi c Centre for Isotopic and Geochemical Research, Department of Earth and Ocean Science, University of British Columbia, Vancouver, British Columbia V6T 1Z4, Canada D.D. Marshall* Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada ABSTRACT Keywords: tectonics, magmatism, geochro- and temporally complex and spans Paleocene to nology, forearc, slab window, ridge subduc- Miocene time. The most spatially and tempo- Forearc magmatic rocks were emplaced in tion, western North America, Cordillera. rally coherent portion is the eastward-younging a semicontinuous belt from Alaska to Oregon Sanak-Baranof Belt in southern to southeastern from 62 to 11 Ma. U-Pb and 40Ar-39Ar dating INTRODUCTION Alaska (Bradley et al., 1993; Haeussler et al., indicates that the magmatism was concur- 1995; Bradley et al., 2003). The age progres- rent in widely separated areas. Eight new Forearcs are typically amagmatic with low sion has been attributed to the passage of an conventional isotope dilution–thermal ion- heat fl ow (Gill, 1981); however, subduction of a eastwardly migrating ridge-trench-trench triple ization mass spectrometry (ID-TIMS) U-Pb mid-ocean ridge imparts a thermal pulse into the junction related to the subduction of a mid-ocean zircon ages from forearc intrusions on Van- forearc, which may result in near-trench mag- spreading ridge in Paleocene to middle Eocene couver Island (51.2 ± 0.4, 48.8 ± 0.5 Ma, 38.6 matism (Marshak and Karig, 1977; DeLong et time (Hill et al., 1981; Bradley et al., 1993; Sisson ± 0.1, 38.6 ± 0.2, 37.4 ± 0.2, 36.9 ± 0.2, 35.4 al., 1979; Sisson et al., 2003). -
Reconnaissance Geology of Amlia Island, Aleutian Islands, Alaska
Reconnaissance geology of Amlia Island, Aleutian Islands, Alaska HUGH McLEAN JAMES R. HEIN } U.S. Geological Survey, 345 Middlefield Road, Menlo Park, California 94025 TRACY L. VALUER) 174° ABSTRACT Amlia Island, located in the central part of the Aleutian Island Atka island chain, exhibits excellent shoreline exposures of Paleogene sedimen- tary and volcanic rocks, which record the earliest observable history of the volcanic arc. Volcaniclastic sedimentary rocks deposited by debris flow, turbidite, and grain-flow processes interfinger with vol- canic flows and breccia. Pillowed flows as well as massive columnar flows ranging in composition from basalt to rhyolite record inter- fingering episodes of submarine and subaerial deposition. The occurrence of Reticulofenestra reticulata and Dictyococ- lOL cites scrippsae in laminated siltstone and sandstone beds indicates Haystack that the rocks on Amlia are late middle Eocene to early Oligocene Rock in age. Whole-rock radiometric ages of 32 and 39 m.y. from igneous rocks that interfinger with the sedimentary rocks corroborate the fossil ages and are correlative in age with the Hidden Bay pluton on 52' Adak Island. Some of the rocks on Amlia Island are only slightly altered and contain authigenic zeolite phases; other rocks are highly altered and contain prehnite, pumpellyite, and laumontite. Areal distribution of 180° 160° highly altered rocks may reflect proximity to shallow-seated plu- u.s.s tons, such as those that crop out on nearby Atka Island, which probably underlie much of Amlia. The island is structurally simple, with dips rarely exceeding 10° or 15°. High-angle faults with small displacement are common, however, and may reflect emplacement of shallow-seated intrusive rocks. -
Alaska Maritime National Wildlife Refuge (AMNWR) Would Not Be Indicative of Weather Patterns for the Entire Complex
ANN UAL I~ARRATI VE REPORT Calendar Year 1982 ALAS KA MARITIME NATIONAL WILDLIF E REFUGE Homer, Alas ka ALEUTIAN ISLANDS UNIT Adak, Alaska ALAS!\.P_ l'tA.RITIME NATIONAL WILDLIFE REFUGE Homer, Alaska ANNUAL NARRATIVE REPORT Calendar Year 1982 library U.S. Fish & Wildlife Service 1011 E. Tudor Road Anchorage, Alaska 99503_ U.S. Department of the Interior Fish and Wildlife Service NATIONAL WILDLIFE REFUGE SYSTEM Refuge Manager John L. Martin Assistant Refuge Manager Tom J. Early Refuge Biologist Edgar P . Bailey - •• I-: f ~ :!-!anager. GS - 13 . EOD 12-21-81, PFT J• Eo~ar P. ba~. Refuge Biologist. GS-ll , EOD 10- 01-81, PFT Review and Approvals 1 TABLE OF CONTENTS Page A. HIGHLIGHTS 4 B. CLIMATIC CONDITIONS 5 C. LAND ACQUISITION 1. Fee Title. .Nothing to Report 2. Easement •• .Nothing to Report 3. Other ••••• • ••••••••••••••••••••••••••••••••••••• 5 D. PLANNING l. Master Plan ............••...............•.........•.•............. 9 2. Management Plan . •••••••••...•••••..•.••.••••...•••.•.••.....•..• 9 3. Public Participation •••••••••••••••••••••••••••• Nothing to Report 4. Compliance with Environmental Mandates •••••••••• Nothing to Report s. Research and Investigations ••••••••••••.•••••••••••••••••••••••• 9 J E. ADMINISTRATION 1. Personnel •••••••••••••••••••••••••••••••••••••••••••••••••••••• l2 2. Youth Programs •••••••••••••••••••••••••••••••••• Nothing to Report 3. Other Manpower Programs ••••••••••••••••••••••••• Nothing to Re·port 4. Volunteers Program •••••••••••••••••••••••••••••• Nothing to Report s. Funding . ..........•.•.••...••...........•••....•...•.•......••. -
Sea Otter Distribution and Abundance in Alaska 2/7/73
•• .. 2/7/73 SEA OTTER DISTRIBUTION AND ABlli'IDA.'lCE IN ALASKA by Karl Schneider Alaska Department of Fish and Game The following description of sea otter distribution and abundance is based on a variety of surveys and other information available as of January 5, 1973. Most population estimates of sea otters have been based on-aerial surveys made from fixed-wing aircraft. Kenyon (The sea otter in the eastern Pacific Ocean, 1969) made estimates based on the assumption that he saw 50 to 75 percent of the sea otters from the air. He used these estimates to provide a comparative picture of the status of sea otter populations throughout Alaska but recognized that the actual numbers might be low. Lensink (J. Ma..mmalogy 41(2):172-182, 1960) made an estimate of the population of P.mchitka Island, based on counts from shore, that were three to four times Kenyon's estimate based on aerial surveys. A recent series of comparative surveys and information gathered during harvests demonstrate that estimates based on aerial surveys are extremely low. Many of the following estimates of tsea otter abundance are based on aerial counts expanded to the level of shore counts with information collected by comparing survey technique. Because all of the sea otters are not seen even on shore counts, some of the following estimates may be somewhat low. The present estimate of sea ~tter in Alaska totals approximately 100,000 to 125,000. Near Islands Sea otters were completely exterminated in the Near Islands. In the late 1950's a few individuals appeared throughout the island group. -
ISJS 5.07.Qrk
ISJS Newsletter 34 (1), 2007, pp.21-33 21 The Triassic-Jurassic transition at Kunga Island, Queen Charlotte Islands, British Columbia, Canada Louise M. Longridge1, Elizabeth S. Carter2, James W. Haggart3, Paul L. Smith1 1Department of Earth and Ocean Sciences, University of British Columbia, 6339 Stores Road, Vancouver, British Columbia,V6T 1Z4, Canada; [email protected], [email protected] 2Department of Geology, Portland State University, Portland, Oregon, 97207-0751, USA; [email protected] 3Geological Survey of Canada, Vancouver, British Columbia, V6B 5J3; [email protected] 1. Introduction If radiolarian sequences are not selected as the pri- Several stratigraphic sections in the Queen Charlotte mary standard, then we propose that they should be con- Islands of British Columbia, Canada contain exceptional- sidered as a secondary standard and that the Kunga Island ly well-preserved radiolarian faunas that cross the section be designated as a parastratotype in order to better Triassic-Jurassic boundary (TJB). In particular, a section characterize the Triassic-Jurassic transition. In some cir- at Kunga Island shows a dramatic turnover of radiolarians cles, parastratotypes are also known as auxiliary reference that could be used to define and constrain the TJB to with- sections. In addition to radiolarians, the Kunga Island in one metre, a precision that is greater than any other fos- sequence permits the calibration of time scales based on sil group. The Kunga section was originally proposed as a ammonites, radiometric ages and, indirectly, with the car- GSSP candidate for the base of the Jurassic by Carter & bon isotope curve. The aim of designating any stratotype Tipper (1999) and again by Haggart et al. -
New Paleomagnetic Data from the Central Aleutian Arc: Evidence and Implications for Block Rotations
New Paleomagnetic Data From the Central Aleutian Arc: Evidence and Implications for Block Rotations Lena Krutikov Department of Geology and Geophysics, University of Alaska, Fairbanks, Alaska, USA David B. Stone Geophysical Institute, University of Alaska, Fairbanks, Alaska, USA Pavel Minyuk Northeast Interdisciplinary Research Institute, Magadan, Russia Early paleomagnetic measurements (late 1960s and early 1970s) from the central Aleutian Island Arc produced both scattered and internally consistent results based solely on alternating field demagnetization. Archived core samples collected from Amchitka and Adak islands for these previous paleomagnetic studies were reanalyzed for this study using modern thermal demagnetization techniques. The new measurements from Amchitka Island indicate significant clockwise rotation (R = 54.7 ± 8.0°) between 14 Ma and the present. Adak Island showed no rotation for volcanic rocks of Quaternary age associated with the present volcanic arc, which is consistent with the lack of rotation seen in other young volcanic rocks (<2 Ma) sampled at localities from Unalaska Island in the east to Kanaga Island in the west. The Eocene Andrew Lake Formation shows a clear magnetic overprint that completely masks any information about possible rotations. Other published studies show rotations similar to those seen for Amchitka Island on Umnak, Amlia, Bering, and Medny islands. Models predicting clockwise rotations involve breaking the forearc into discrete blocks and slivers that rotate and/or travel westward along the curve of the arc in response to the arc-parallel component of the Pacific Plate motion. These models have difficulty explaining the large rotations seen in the easternmost islands sampled, where the relative motion of the Pacific Plate is more or less perpendicular to the arc.