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The Legacy of a Taku River Tlingit Clan
Gágiwdul.àt: Brought Forth to Reconfirm THE LEGACY OF A TAKU RIVER TLINGIT CLAN Gágiwdul.àt: Brought Forth to Reconfirm THE LEGACY OF A TAKURIVER TLINGIT CLAN Elizabeth Nyman and JeffLeer Yukon Native Language Centre and Alaska Native Language Center 1993 lV © 1993, Yukon Native Language Centre, Alaska Native Language Center, and Elizabeth Nyman Printed in the United States of America All rights reserved Library of Congress Cataloging-in-Publication Data Nyman, Elizabeth, 1915- Gágiwdutàt : The Legacy of a Taku River Tlingit Clan / Elizabeth Nyman and Jeff Leer. p. cm. Includes index. ISBN 1-55500-048-7 1. Tlingit Indians-Legends. 2. Tlingit Indians-Social life and customs. 3. Nyman, Elizabeth, 1915- . 4. Tlingit Indians-Biography. 5. Tlingit language-Texts. 1. Leer, Jeff. Il. Title. E99.T6N94 1993 93-17399 398.2'089972-dc20 CIP First Printing, 1993 1,000 copies Cover photo: Yakadlakw Shà 'Scratched-face Mountain' (no English name) and the Taku River near Atlin, by Wayne Towriss for YNLC Cover design and drawing on title pages by Dixon Jones, UAF IMP ACT Yukon Native Language Centre Alaska Native Language Center Yukon College University of Alaska Fairbanks Box 2799 Fairbanks, Alaska 99775-0120 Whitehorse, Yukon Canada YlA 5K4 The printing of this book was made possible in part by a contribution to the Council for Yukon Indians by the Secretary of State for Canada and Aborigi nal Language Services (Government of Yukon). It is the policy of the University of Alaska to provide equal education and employment opportunities and to provide -
FNESS Strategic Plan
Strategic Plan 2013-2015 At a Glance FNESS evolved from the Society of Native Indian Fire Fighters of BC (SNIFF), which was established in 1986. SNIFF’s initial objectives were to help reduce the number of fire-related deaths on First Nations reserves, but it changed its emphasis to incorporate a greater spectrum of emergency services. In 1994, SNIFF changed its name to First Nations’ Emergency Services Society of BC to reflect the growing diversity of services it provides. Today our organization continues to gain recognition and trust within First Nations communities and within Aboriginal Affairs and Northern Development Canada (AANDC) and other organizations. This is reflected in both the growing demand of service requests from First Nations communities and the development of more government-sponsored programs with FNESS. r e v Ri k e s l A Inset 1 Tagish Lake Teslin 1059 Daylu Dena Atlin Lake 501 Taku River Tlingit r e v Liard Atlin Lake i R River ku 504 Dease River K Fort a e Nelson T r t 594 Ts'kw'aylaxw e c iv h R ik River 686 Bonaparte a se a 687 Skeetchestn e D Fort Nelson R i v e First Nations in 543 Fort Nelson Dease r 685 Ashcroft Lake Dease Lake 592 Xaxli'p British Columbia 593 T'it'q'et 544 Prophet River 591 Cayoose Creek 692 Oregon Jack Creek 682 Tahltan er 683 Iskut a Riv kw r s e M u iv R Finlay F R Scale ra e n iv s i er 610 Kwadacha k e i r t 0 75 150 300 Km S 694 Cook's Ferry Thutade R r Tatlatui Lake i e 609 Tsay Keh Dene v Iskut iv 547 Blueberry River e R Lake r 546 Halfway River 548 Doig River 698 Shackan Location -
Geology: Ordovician Paleogeography and the Evolution of the Iapetus Ocean
Ordovician paleogeography and the evolution of the Iapetus ocean Conall Mac Niocaill* Department of Geological Sciences, University of Michigan, 2534 C. C. Little Building, Ben A. van der Pluijm Ann Arbor, Michigan 48109-1063. Rob Van der Voo ABSTRACT thermore, we contend that the combined paleomagnetic and faunal data ar- Paleomagnetic data from northern Appalachian terranes identify gue against a shared Taconic history between North and South America. several arcs within the Iapetus ocean in the Early to Middle Ordovi- cian, including a peri-Laurentian arc at ~10°–20°S, a peri-Avalonian PALEOMAGNETIC DATA FROM IAPETAN TERRANES arc at ~50°–60°S, and an intra-oceanic arc (called the Exploits arc) at Displaced terranes occur along the extent of the Appalachian-Cale- ~30°S. The peri-Avalonian and Exploits arcs are characterized by Are- donian orogen, although reliable Ordovician paleomagnetic data from Ia- nigian to Llanvirnian Celtic fauna that are distinct from similarly aged petan terranes have only been obtained from the Central Mobile belt of the Toquima–Table Head fauna of the Laurentian margin, and peri- northern Appalachians (Table 1). The Central Mobile belt separates the Lau- Laurentian arc. The Precordillera terrane of Argentina is also charac- rentian and Avalonian margins of Iapetus and preserves remnants of the terized by an increasing proportion of Celtic fauna from Arenig to ocean, including arcs, ocean islands, and ophiolite slivers (e.g., Keppie, Llanvirn time, which implies (1) that it was in reproductive communi- 1989). Paleomagnetic results from Arenigian and Llanvirnian volcanic units cation with the peri-Avalonian and Exploits arcs, and (2) that it must of the Moreton’s Harbour Group and the Lawrence Head Formation in cen- have been separate from Laurentia and the peri-Laurentian arc well tral Newfoundland indicate paleolatitudes of 11°S (Table 1), placing them before it collided with Gondwana. -
The Taconic Orogeny in Newfoundland: a Three-Stage Process
atlantic geology . volume 43 . 2007 83 geochronology and isotope geology, indicated that this model was incomplete. We will present new evidence that the Taconic orogeny comprises three separate accretionary events starting in the Late Cambrian and finishing in the Late Ordovician. Taconic 1 is represented by ca. 495 Ma west-directed obduc- tion of the ca. 510 Ma Lushs Bight oceanic Tract onto the peri- Laurentian Dashwoods microcontinent. Subduction is inferred to have initiated at a spreading centre abandoned during an inboard ridge jump responsible for separation of Dashwoods from Laurentia. Partial subduction of the buoyant Dashwoods forced subduction to step back into the Humber seaway, which led to formation of the ca. 490 Ma Baie Verte oceanic tract (BVOT). Dextral oblique closure of the Humber seaway first formed the Notre Dame arc (489–477 Ma) built on Dashwoods and the coeval Snooks Arm arc built on the BVOT, followed by their collision with Laurentia (Taconic 2) and each other. The obliquity of convergence induced large-scale translations of continental ribbons of the Laurentian margin from the lati- tude of Labrador to central Newfoundland. After a magmatic gap of c. 7–10 my, the Notre Dame arc records a voluminous flare-up of predominantly tonalite magmatism (464–459 Ma) during the waning stages of Taconic 2. Magmatism overlaps with strong deformation and comprises both arc and non-arc- like tonalite. We relate this flare-up to break-off of the oceanic lithosphere of the downgoing Laurentian slab. Taconic 3 is rep- resented by 455–450 Ma collision between a peri-Laurentian arc terrane and the peri-Gondwanan Popelogan-Exploits arc and their composite accretion to Laurentia. -
For a Larger Version of the First Nations in British
#! Inset 1 Tagish Lake #! Teslin 502 Liard Atlin Lake #!501 Taku River Tlingit L 594 Ts'kw 'aylaxw iard #! Atlin Lake R 687 Skeetchestn ive #! ! 504 Dease River K r 686 Bonaparte # #! e r t e c iv h R ik #! a se a e D Fort Nelson R ! i # ! 592 Xaxli'p #! 685 Ashcroft v # e 543 Fort Nelson Dease r #! 593 T'it'q'et Lake Dease Lake #! First Nations 591 Cayoose Creek #! 692 Oregon Jack Creek 682 Tahltan #! 544 P rophet River r #! a ive in British Colum bia F R in British Colum bia 683 Iskut r #! kw a r s s e M u e iv r R Finlay R e iv n er i 610 Kw ad acha k Scale i t #! ! S R # 694 Cook's Ferry i v 0 75 150 300 km e r Thutade r e Lake I iv Tatlatui 609 Tsay Keh Dene skut R #! 547 Blueberry River Lake #! 698 Shackan #! #! #! #! 696 Nicom en 546 Halfw ay River 548 Doig River 705 Lytton #! #! Location of First Nation's 699 Nooaitch Main Community #! Williston Fort St John 707 Skuppah #! Lake N Indian Reserve a ! s 542 Saulteau # 706 Siska s #! #! 704 Kanaka Bar #! R Takla i 545 W est Moberly v City or Town e Lake r 532 Kispiox 533 Glen Vow ell 608 Takla 677 Nisga'a Village of New Aiyansh 537 Gitanyow 531 Gitanm aax #! #! Park and Protected Area 679 Nisga'a Village of Gitw inksihlkw #! #!!534 Hagw ilget 678 Nisga'a Village of Laxgalt'sap #!#! # #! 700 Boothroyd ! #! #! 535 Gitsegukla 671 Nisga'a Village of Gingolx#! # ! Babine #! 618 McLeod Lake 536 Gitw ar ngak # e 530 W itset v i Sm ithers 674 Lax Kw 'alaam s R Lake 617 Tl'azt'en ! 701 Boston Bar ! # #! Terrace #!680 Kitselas 728 Yekooche ! # #! # #! 730 Binche W hut'en 673 Metlakatla ena -
P.~Cific· 'R.I..W; ·Pivl.S1po,:
) I' , ,,' , ' f , • ,O~ " by. N~ Seigel. '. C~ HcEwen , " . NORTHERN BIOMES LTD Environme~tal Servic.s Whitehorse', Yukon" for Department of. FiSl.h,El·l",ies, and. ,Oceans ,P.~cific· 'R.i..W; ·pivl.s1po,: , . • r·',',·". , , ~. , . ~ '. ' June... 1,9'84 i ) ACKNOWLEDGEMENTS This project was funded by the Federal Department of Fisheries and Oceans. Fisheries personnel in Whitehorse, Vancouver and Ottawa were most helpful and we would especially like to thank Michael Hunter, Gordon Zealand, Sandy Johnston, Peter Etherton, Elmer Fast, Tim Young, Obert Sweitzer, and Ciunius Boyle. The help and patience of personnel from the Yukon Archives, Hudson's Bay Arohives, and Publio Archives of Canada, partioularly Bob Armstrong, the arohivist in charge of Fisheries documents, is gratefully acknowledged. Interviews with Yukon residents: G.I. Cameron, Charles "Chappie ft Chapman, Silvester Jack, Dorothy Jackson, Elizabeth Nyman, Angela Sidney, George Simmons, Virginia Smarch, Dora Wedge and Ed Whjtehouse provided information that was otherwise not available. Julie Cruikshank suggested useful reference resouroes for Indian fishing information. Aileen Horler and Tim Osler offered suggestions during the embryonic stage of the study. Valuable editorial comments were provided by Gavin Johnston. Sandy Johnston provided ourrent information on the Canada/U.S. Yukon River salmon negotiations. The report was typed by Norma Felker, Sharilyn Gattie and Kelly Wilkinson. ii SUMMARY Prior to the Klondike Gold Rush of 1898, fishing in the Yukon was primarily done by indigenous peoples for subsistenoe. For a number of Indian bands, fish, and partioularly salmon, was the primary food souroe. Contaot with White furtraders initiated a ohange in the Indian lifestyle. -
Paleozoic 3: Alabama in the Paleozoic
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Paleozoic 3: Alabama in the Paleozoic Instructor: Dr. Douglas W. Haywick Last Time The Paleozoic Part 2 1) Back to Newfoundland 2) Eastern Laurentian Orogenies (Appalachians) 3) Other Laurentian Orogenies (Antler, Ouachita) (web notes 25) Laurentia (Paleozoic North America) Even though this coastline of Laurentia was a passive continental margin, a plate tectonic boundary was rapidly approaching… A B A B Laurentia (Paleozoic North America) The resulting Taconic Orogeny first depressed the seafloor Laurentia (localized transgression) and A Island arc then pushed previously deposited passive continental B margin sediments up into thrust fault mountains. Baltica There was only minimal metamorphism and igneous A intrusions. B Middle Ordovician Laurentia (Paleozoic North America) Laurentia Baltica Middle Ordovician Laurentia (Paleozoic North America) Laurentia Baltica Middle Ordovician Laurentia (Paleozoic North America) The next tectonic event (the Acadian Orogeny) was caused Laurentia by the approach of Baltica A B Baltica A B Baltica Baltica Late Ordovician Laurentia (Paleozoic North America) The Acadian Orogeny was more extensive and more intense (metamorphism and A lots of igneous intrusions) B A B Early Devonian Laurentia (Paleozoic North America) The Acadian Orogeny was more extensive and more intense (metamorphism and lots of igneous intrusions) Early Devonian Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. A B B A B Mississippian Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. A B B A B Pennsylvannian Suture zone Laurentia (Paleozoic North America) Lastly, along comes Gondwanna and…. …well you get the idea. -
Atlin Northern Mountain Caribou Management and Monitoring Framework: Final Report 2011
1 ATLIN NORTHERN MOUNTAIN CARIBOU MANAGEMENT AND MONITORING FRAMEWORK: FINAL REPORT 2011 Project Components 1. Habitat Modeling 2. Cumulative Effects Toolkit 3. Caribou Pregnancy 4. Predator Diet Stable Isotope Analysis 5. Lichen Sampling JUNE 2011 REPORT PREPARED FOR Taku River Tlingit First Nation P.O. Box 132 Atlin, BC V0W 1A0 REPORT BY Jean L. Polfus1 Kimberly S. Heinemeyer1 COVER PHOTO CREDITS Jean Polfus (top left, TRTFN Territory sign, bottom left, bottom middle, middle), Wibke Peters (bottom right), Kevin Cannaday (caribou on road). Drawing of caribou by Jean Polfus. 1 Round River Conservation Studies, 284 West 400 North, Suite 105, Salt Lake City, UT 84103; Jean Polfus: [email protected]; Kimberly Heinemeyer: [email protected] 2 FUNDING Funding for this project was provided by the Habitat Stewardship Program for Species at Risk and the Aboriginal Funds for Species at Risk of Environment Canada, the Taku River Tlingit First Nation, Round River Conservation Studies and the University of Montana. 3 ACKNOWLEDGEMENTS The long-term vision of the Taku River Tlingit First Nation (TRTFN) made this project possible by identifying the need for sustainable management of the wildlife and resources in their traditional territory. Many TRTFN members contributed their ecological knowledge and expertise including Jackie Williams, Bryan Jack, Andrew Williams, Terry Jack, Harry Carlick, Richard Carlick, Greta Thorlakson, Douglas Jack, Rickard Johnson and Peter Kirby. Field research was provided by Myranda Simpson, Morgane Stehelin-Holland, Jerry Jack, Phillip Tizya and Mark Connor. The partnership between the TRTFN and Round River Conservation Studies (RRCS) facilitated the development of funding proposals, project management, reporting and implementation and development of project partnerships. -
Resource Atlas for Planning Under the Atlin-Taku Framework Agreement
RESOURCE ATLAS FOR PLANNING UNDER THE ATLIN-TAKU FRAMEWORK AGREEMENT Version 1.5 August, 2009 Resource Atlas Resource Atlas ACKNOWLEDGEMENTS This Atlas was compiled with contributions from many people. Of particular note, maps were produced by Shawn Reed and Darin Welch with the assistance of Dave Amirault, Integrated Land Management Bureau. Descriptive information was mainly based on the report Atlin-Taku Planning Area Background Report: An Overview of Natural, Cultural, and Socio-Economic Features, Land Uses and Resources Management (Horn and Tamblyn 2002), Government of BC websites, and for wildlife the joint Wildlife Habitat Mapping Information Handout May 2009. Atlin-Taku Framework Agreement Implementation Project Page 3 of 87 Resource Atlas Atlin-Taku Framework Agreement Implementation Project Page 4 of 87 TABLE OF CONTENTS Acknowledgements ....................................................................................................................................... 3 Table of Contents ......................................................................................................................................... 5 Introduction ................................................................................................................................................... 7 General Plan Area Description ................................................................................................................... 7 Map 1: Base Information ............................................................................................................................ -
Geology and Topography of Dutchess County (.Pdf)
Chapter 3: The Geology and Topography of Dutchess County Chapter 3: Geology and Topography of Dutchess County, NY ______________________________________________________________________________ Roy T. Budnik, Jeffery R. Walker, and Kirsten Menking1 May 2010 INTRODUCTION The topography, settlement patterns, and mineral resources of Chapter Contents Dutchess County are all influenced by the underlying geology. Geologic History For example, the highest mountains contain the hardest rocks, Bedrock Formations Structural Geology communities in the county are generally located in areas of Surficial Deposits sand and gravel because of the relatively level terrain and Mineral Resources Topography abundant water supplies they contain, and construction Trends and Changes Over aggregates are mined where suitable deposits are found. Time Implications for Decision- Understanding geologic materials and processes is essential to Making sound resource management because the geology affects the Resources 1 This chapter was written during 2010 by Dr. Roy T. Budnik (President, Roy T. Budnik & Associates), Dr. Jeffrey R. Walker (Professor of Earth Science & Geography, Vassar College), and Dr. Kirsten Menking (Associate Professor of Earth Science and Geography, Vassar College). It is an updated and expanded version of the Hydrology chapter of the 1985 document Natural Resources, Dutchess County, NY (NRI). Natural Resource Inventory of Dutchess County, NY 1 Chapter 3: The Geology and Topography of Dutchess County quality and quantity of groundwater resources, the migration of pollutants, potential hazards to inhabitants, drainage patterns, mineral resources, and soil characteristics. Geology is the study of the earth, including all materials found at and below the earth’s surface. Geologists analyze the composition, origin, and ongoing changes in the rocks and sediments that compose the earth. -
Paleozoic Evolution of the Appalachians
Paleozoic Evolution of the Appalachians: Tectonic Overview Three major tectonic episodes, all involving lateral accretion of terranes: deformation, terrane migration, accretion, and continental convergence 1. Ordovician Taconic Orogeny (~470-440 Ma) • collision of Laurentian margin with one or more magmatic arcs Shelburne Falls arc (475-470 Ma) and Bronson Hill arc (454-442 Ma) • or, continent-continent collision between Laurentia and proto-Andean region of Gondwana • slope & rise sediments thrust westward over shelf deposits 2. Devonian Acadian Orogeny (~420-360 Ma) • accretion of Avalon terrane southward continuation of Silurian Caledonian Orogeny (NW Europe) collision of Baltica with Laurentia to form Laurussia • deformation of Bronson Hill arc and sedimentary basins seaward of BH arc at least 3 pulses of deformation • oblique accretion of Avalon and other terranes(?) much strike-slip displacement but also subduction (coastal volcanics) • large mountains erosion creates thick clastic wedge (Catskills and Poccono Mtns.); thinned westward toward cratonic interior 3. Pennsylvansylvanian-Permian Alleghenian Orogeny (~325- 275 Ma) • collision with Gondwanaland consolidation of supercontinent Pangea • extensive zone of deformation New England - Georgia & Alabama (Appalachian Mtns.) - Oklahoma, Arkansas (Ouachita Mtns.) - Texas (Marathon Mtns.) • side-effects: deep crustal shear in Mass., formation of Narragansett rift basin basement block faulting in western interior, uplift of ancestral Rockies "TECTONIC CYCLES" • recorded by the creation of foreland basins sedimentation in eastern New York • associated with tectonic uplift and deformation due to the accretion of island arcs to the east in Massachusetts (first the Ordovician Taconic Orogeny followed by the Devonian Acadian Orogeny: Ordovician Taconic Orogeny (generalized succession in eastern NY) Age Environment Lithology Formation late Ordovician deltaic and molasse Queenston Fm. -
Southern Lakes Fisheries Angler Education and Outreach Campaign - Spring 2020
Southern Lakes Fisheries Angler Education and Outreach Campaign - Spring 2020 Education and Outreach Focussed on Grayling, Northern Pike and Lake Trout at the Lubbock River, Little Atlin Lake and additional accessible locations in the Southern Lakes. Carcross/Tagish Renewable Resources Council June 2020 Campaign and Outreach Facilitated by: Dennis Zimmermann - Big Fish Little Fish Consultants Overview: Increased fishing pressure in the accessible Southern Lakes was already a concern, prior to covid-19. The concern for vulnerable Lubbock River Grayling and Little Atlin Lake Trout was the impetus for this campaign led by the Carcross/Tagish Renewable Resources Council (C/TRRC). The C/TRRC working with partners Carcross/Tagish First Nation (C/TFN) and the Department of Environment (DOE), hired Dennis Zimmermann with Big Fish Little Fish Consultants to develop an outreach and education campaign in the spring of 2020. The outreach and education campaign featured numerous tactics and means by which various messages could be presented to the licenced Yukon angling public. Tactics included the installation of signage at approximately 11 locations, a press release, social media communications and outreach over four weekends between May and June at the Lubbock River and one weekend at Little Atlin Lake. 1 Feedback from anglers and the public has been positive both on social media, in- person responses, and anecdotally comments from the community. Some of the greatest successes of this campaign include: • facilitating a positively focussed and proactive