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Fishing Flies from the Transkei
Location: Enclave, East Cape Province, South Africa Republic of South Africa Government: Self-governing tribal Transvaal homeland Area: 16,910 sq. mi. Swaziland Population: 2,876,122 (1985) Capital: Umtata Orange Natal Free The World’s First Fishing Fly Stamps State Cape Province Lesotho Building a Business in South Africa In 1976, Mr. Barry Kent, his partners, and the Republic of Transkei Development Corporation built a fishing fly manufacturing Eastern Cape plant at Butterworth, Transkei, South Africa. Transkei Western Cape The company, named High Flies Ltd., was one of the most modern fishing-fly manufacturing plants in the world. Pricing, quality and clever product marketing proved to be very successful. By 1979 High Flies was employing more than 350 labor-intensive Transkeians, producing over 1,000 dozen flies each day. These flies are used mainly in fly-fishing for trout and salmon. The entire production was exported to countries where these fish are prolific: America, the British Isles, Australia, Canada, New Zealand, Scandinavia, and other European countries. An idea for promoting other Transkei industries was created by depicting fishing flies on postage stamps. The outcome produced a series of five sheets for each year from 1980 through 1984. Each sheet contains five different fly patterns arranged in se-tenant format. Although the last issue of these stamps appeared in 1984, the factory closed in 1983 due to a corrupt business partner and poor management by the South African/Republic of Transkei Development Corporation bureaucrats. Mr. Kent, along with approximately 390 local workers lost their jobs. Philatelic Specifications Designer: A. H. -
STATE of ALASKA Walter J. Hickel - Governor
STATE OF ALASKA Walter J. Hickel - Governor DEPARTMENT OF NATURAL RESOURCES Thomas E. Kelly - Commissioner DIVISION OF MINES AND MINERALS James A. Williams - Director GEOCHEMICAL REPORT NO. 17 A Geochemical Investigation of the Wood River-Tikchik Lakes Area Southwestern A1 as ka BY Gilbert R. Eakins Col 1ege , A1 as ka May 1968 CONTENTS Page ABSTRACT 1 INTRODUCTION Location and accessibi 1 i ty Climate and vegetation History GENERAL GEOLOGY Previous work Physiography Stratigraphy Structure Mineralization Field observations GEOCHEMICAL INVESTIGATIONS Sampl ing procedure Sample analyses and evaluation Field tests Laboratory analyses Copper Zinc Lead Molybdenum Mercury DISCUSSION OF MERCURY SAMPLING Marsh Mountain Southeast end of Lake Aleknagi k Northwest part of Lake A1 eknagi k Little Togiak Lake, south side Other anomalous mercury samples SUGGESTIONS FOR PROSPECTING REFERENCES ILLUSTRATIONS Page Figure 1. Location map showing mercury mines and prospects 3 2. Geochemical sample locations in the Red Top mine area 9 3. Granite intrusion at the west end of Silver Horn 14 4. Contorted carbonate bed on the south side of Golden Horn 14 5. Copper assay distribution graph 20 6. Zinc Assay distribution graph 21 7. Lead and molybdenum assay distribution graphs 22 8. Mercury assay distribution graph 23 9. Map, Geochemical Sample locations, Wood River-Ti kchick In pocket Lakes area, southwestern A1 aska 10. Map, Geochemical mercury anomalies, Wood River-Tikchick In pocket Lakes area, southwestern Alaska Table I. Generalized stratigraphic sequence of rocks in the Lower Kuskokwim-Bristol Bay region, A1 aska Table 11. Analyses for copper, lead, zinc, molybdenum, mercury and field tests. A GEOCHEMICAL INVESTIGATION OF THE WOOD RIVER-TIKCHIK LAKES AREA SOUTHWESTERN ALASKA By Gilbert R. -
NSF 03-021, Arctic Research in the United States
This document has been archived. Home is Where the Habitat is An Ecosystem Foundation for Wildlife Distribution and Behavior This article was prepared The lands and near-shore waters of Alaska remaining from recent geomorphic activities such by Page Spencer, stretch from 48° to 68° north latitude and from 130° as glaciers, floods, and volcanic eruptions.* National Park Service, west to 175° east longitude. The immense size of Ecosystems in Alaska are spread out along Anchorage, Alaska; Alaska is frequently portrayed through its super- three major bioclimatic gradients, represented by Gregory Nowacki, USDA Forest Service; Michael imposition on the continental U.S., stretching from the factors of climate (temperature and precipita- Fleming, U.S. Geological Georgia to California and from Minnesota to tion), vegetation (forested to non-forested), and Survey; Terry Brock, Texas. Within Alaska’s broad geographic extent disturbance regime. When the 32 ecoregions are USDA Forest Service there are widely diverse ecosystems, including arrayed along these gradients, eight large group- (retired); and Torre Arctic deserts, rainforests, boreal forests, alpine ings, or ecological divisions, emerge. In this paper Jorgenson, ABR, Inc. tundra, and impenetrable shrub thickets. This land we describe the eight ecological divisions, with is shaped by storms and waves driven across 8000 details from their component ecoregions and rep- miles of the Pacific Ocean, by huge river systems, resentative photos. by wildfire and permafrost, by volcanoes in the Ecosystem structures and environmental Ring of Fire where the Pacific plate dives beneath processes largely dictate the distribution and the North American plate, by frequent earth- behavior of wildlife species. -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Spokane, Washington
Volume 58 No. 3 March, 2013 Web Page: http://www.ieffc.org Editor: Robert Bates GENERAL MEETING MARCH PROGRAM INLAND EMPIRE FLY FISHING CLUB By Lee Funkhouser MUKOGAWA FORT WRIGHT INSTITUTE COMMONS March 12, 2013 Our speaker for March is Sean Visintainer, owner of the Wet Fly Hour: 5:30 p.m. Silver Bow Fly Shop. He will be speaking about river Dinner: 6:30 p.m. and stream fishing, a topic that he has discussed with many of us on an informal basis at his shop. PRESIDENT’S MESSAGE The Silver Bow Fly Shop's slogan may be “Making Fish By Mike Beasley Nervous Since 1988”, but Sean has been making fish nervous since the day he was born. For the past 18 plus Well another month of winter as gone by..... I hope years he has made fly fishing his passion, lifestyle, and everyone is at the bench preparing for the upcoming business. In 2002 he began working and teaching classes spring thaw with visions of 18 inch Cutts taking down a at the Silver Bow and began managing shortly after. In size 12 renegade or fortunate enough to go somewhere 2005 he purchased the shop and moved it to its current warm and work on your 10 to 2 casting stroke. I location along I-90. recently returned from a couple days down at the family cabin in the Trinity mountains of California with my When Sean is not running the shop or guiding he can be father and my first 2013 Steelhead has been brought to found chasing trout and steelhead on local streams or hand. -
INTRODUCTION by Peter Brigg
INTRODUCTION By Peter Brigg Fly fshing, not just for trout, is a multifaceted sport that will absorb you in its reality, it will take you to places of exceptional beauty, to explore, places to revel in the solitude and endless stimulation. He stands alone in the stream, a silver thread, alive, tumbling and Fly fshing, not just for trout, is a multifaceted sport that will absorb sliding in the soft morning light: around him the sights, sounds you in its reality, it will take you to places of exceptional beauty, to and smells of wilderness. Rod under his arm he carefully picks out explore, places to revel in the solitude and endless stimulation. Or, you a fy from amongst the neat rows, slides the fy box back into its vest can lose yourself between the pages of the vast literature on all facets pocket and ties on the small dry fy. Slowly, with poetic artistry he lifts of fy fshing, get absorbed by the history, the heritage, traditions and the rod and ficks the line out, gently landing the fy upstream of the skills, be transported in thought to wild places, or cast to imaginary diminishing circles of the feeding trout – watching, waiting with taut, fsh and gather knowledge. So often fy fshing is spoken of as an art quiet anticipation as the fy bobs and twirls on the current. form and having passed the half century of experience, I’m not averse to this view, just as I believe that fytying is inextricably linked to fy It is a scene we as fy fshers know well, a fascination and pre-occupation fshing, but is in its own right a craft, a form of artistry. -
Togiak National Wildlife Refuge
TOGIAK NATIONAL WILDLIFE REFUGE Dillingham, Alaska ANNUAL NARRATIVE REPORT Calendar Year 1991 U.S. Department of the Interior Fish and Wildlife Service NATIONAL WILDLIFE REFUGE SYSTEM REVIEW AND APPROVALS REVIEW AND APPROVALS TOGIAK NATIONAL WILDLIFE REFUGE Dillingham, Alaska ANNUAL NARRATIVE REPORT Calendar Year 1991 , N?? Regional Office Approval Date US FISH & WILDLIFE SERVICE--ALASKA Ill~~~~~~~~~~~~~~ 3 4982 00022058 1 INTRODUCfiON Togiak National Wildlife Refuge encompasses 4. 7 million acres of land in southwestern Alaska between Kuskokwim Bay and Bristol Bay. The eastern boundary of the refuge is about 400 air miles southwest of Anchorage. The refuge is bordered on the north by Yukon Delta National Wildlife Refuge and on the east by Wood-Tikchik State Park. The refuge contains a variety of landscapes, including tundra, lakes, wetlands, mountains, and rugged cliffs. The Kanektok, Goodnews and Togiak rivers provide habitat necessary for five species of salmon and other fish that spawn in the refuge. More than 30 species of mammals are present including brown bear, moose, caribou, wolves, and wolverine. Sea lions, walrus, and harbor seals inhabit the Pacific coast shoreline. The Refuge's coastal lakes and wetlands are also heavily used by migrating waterfowl. Southwest Alaska, Togiak National Wildlife Refuge is shaded. The former Cape Newenham National Wildlife Refuge (created in 1969) became part of the present Togiak National Wildlife Refuge. The northern 2.3 million acres of the refuge are designated wilderness. Eighty percent of the refuge is located in the Ahklun Mountains, where large expanses of tundra uplands are cut by several broad glacial valleys expanding to the coastal plain. -
Fly Fishing with Spinning Tackle
FLY FISHING WITH SPINNING TACKLE This setup is deadly on trout. It can be fished on the surface or close to the bottom and it works anywhere that you find trout. Fly fishing is divided into 2 categories: Dry fly and wet fly / nymph fishing. # 1. 90 % of the insects that a trout eats are in the form of nymphs. So this is where you should concentrate UNLESS you see trout taking insects from the surface. (see # 2) Fill your water float completely full of water, taking care that there are no air bubbles remaining. Slide your line through starting at the skinny end of the float. Next tie on a # 12 snap swivel. Tie a separate 5 foot leader of 2 - 4 lb. test with one of the following: # 12 Zug Bug, # 8 or # 10 Woolly Bugger / green or black, # 12 Hare's Ear nymph, or a # 12 Prince. Cast out and count. For every second, the water float will sink 1 foot and when it hits the bottom your line will go slack. If you counted to 12, then it is about 12 feet deep. Then reel SLOWLY 1 or 2 cranks and let it sit for 5 seconds and continue this pattern until all the line is in. The next cast you will want to shorten the sinking time by 2 seconds so that the fly covers the next 2 feet up and you continue on each cast to shorten the sinking time until you either catch fish or are at the surface. If you don't catch fish move a little bit down the shoreline and repeat. -
Bedrock Geologic Map of the Northern Alaska Peninsula Area, Southwestern Alaska Compiled by Frederic H
Bedrock Geologic Map of the Northern Alaska Peninsula Area, Southwestern Alaska Compiled by Frederic H. Wilson, Robert B. Blodgett, Charles D. Blome, Solmaz Mohadjer, Cindi C. Preller, Edward P. Klimasauskas, Bruce M. Gamble, and Warren L. Coonrad Pamphlet to accomopany Scientific Investigations Map 2942 2017 U.S. Department of the Interior U.S. Geological Survey Contents Abstract ...........................................................................................................................................................1 Introduction and Previous Work .................................................................................................................1 Geographic, Geologic, and Physiographic Framework ...........................................................................2 Geologic Discussion ......................................................................................................................................3 Ahklun Mountains Province ................................................................................................................4 Lime Hills Province ...............................................................................................................................4 Alaska-Aleutian Range Province .......................................................................................................4 Map Units Not Assigned to a Province .............................................................................................4 Digital Data......................................................................................................................................................5 -
Holocene Glacier Fluctuations in Alaska
Quaternary Science Reviews 28 (2009) 2034–2048 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Holocene glacier fluctuations in Alaska David J. Barclay a,*, Gregory C. Wiles b, Parker E. Calkin c a Geology Department, State University of New York College at Cortland, Cortland, NY 13045, USA b Department of Geology, The College of Wooster, Wooster, OH 44691, USA c Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA article info abstract Article history: This review summarizes forefield and lacustrine records of glacier fluctuations in Alaska during the Received 9 May 2008 Holocene. Following retreat from latest Pleistocene advances, valley glaciers with land-based termini Received in revised form were in retracted positions during the early to middle Holocene. Neoglaciation began in some areas by 15 January 2009 4.0 ka and major advances were underway by 3.0 ka, with perhaps two distinct early Neoglacial Accepted 29 January 2009 expansions centered respectively on 3.3–2.9 and 2.2–2.0 ka. Tree-ring cross-dates of glacially killed trees at two termini in southern Alaska show a major advance in the AD 550s–720s. The subsequent Little Ice Age (LIA) expansion was underway in the AD 1180s–1320s and culminated with two advance phases respectively in the 1540s–1710s and in the 1810s–1880s. The LIA advance was the largest Holocene expansion in southern Alaska, although older late Holocene moraines are preserved on many forefields in northern and interior Alaska. Tidewater glaciers around the rim of the Gulf of Alaska have made major advances throughout the Holocene. -
Alaska Shorebird Conservation Plan Version Ii
ALASKA SHOREBIRD CONSERVATION PLAN VERSION II ALASKA SHOREBIRD GROUP NOVEMBER 2008 CONTRIBUTORS Robert E. Gill, Jr., USGS Alaska Science Center, Anchorage Colleen M. Handel, USGS Alaska Science Center, Anchorage Christopher M. Harwood, U.S. Fish and Wildlife Service, Fairbanks Jim A. Johnson, U.S. Fish and Wildlife Service, Anchorage Steven J. Kendall, U.S. Fish and Wildlife Service, Fairbanks Richard B. Lanctot, U.S. Fish and Wildlife Service, Anchorage Joe Liebezeit, Wildlife Conservation Society, Portland Brian J. McCaffery, U.S. Fish and Wildlife Service, Bethel Julie A. Morse, Equinox Ecological, Fairbanks Debora A. Nigro, Bureau of Land Management, Fairbanks Daniel R. Ruthrauff, USGS Alaska Science Center, Anchorage Audrey R. Taylor, University of Alaska, Fairbanks T. Lee Tibbitts, USGS Alaska Science Center, Anchorage Pavel S. Tomkovich, Moscow State University, Moscow SUGGESTED CITATION Alaska Shorebird Group. 2008. Alaska Shorebird Conservation Plan. Version II. Alaska Shorebird Group, Anchorage, AK. The Alaska Shorebird Conservation Plan and updates can be viewed and downloaded at: http://alaska.fws.gov/mbsp/mbm/shorebirds/plans.htm Cover photo: Rock Sandpipers wintering in Cook Inlet • Robert Gill, Jr. Alaska Shorebird Conservation Plan DEDICATION The Alaska Shorebird Conservation Plan is dedicated to Doug Schamel in appreciation for his contributions to shorebird science, education, and conservation over his 20-year career in Alaska. Doug’s natural curiosity and enthusiasm for all things zoological were unbounded, but he focused his professional research efforts on shorebirds. Somewhat of a nonconformist himself, it is not surprising that Doug gravitated toward study of the polyandrous social system of phalaropes. Along with his wife, Diane Tracy, he authored a dozen phalarope publications, including the species accounts for the Birds of North America series. -
Draft Wild and Scenic River Study December 1983
I vu r 6 1 c tgey draft wild and scenic river study december 1983 ALASKA Publication of this document should not be construed as representing either the approval or disapproval of the secretary of the interior. The purpose of this report is to provide the information and alternatives for further consideration by the National Park Service , secretary of the interior, other federal and state agencies , and the public. Prepared and published by the Denver Service Center DRAFT WILD AND SCENIC RIVER STUDY FOR THE KANEKTOK RIVER , ALASKA Prepared by the U. S. Department of the Interior , National Park Service , in cooperation with the U.S. Fish and Wildlife Service Alaska Department of Fish and Game , Qanirtuuq, Inc., City of Quinhagak , and Calista Corporation. Abstract : This draft wild and scenic river study describes and evaluates two alternatives with respect to possible inclusion of the Kanektok River in Alaska into the National Wild and Scenic Rivers System. Alternative One , No Action , is the preferred alternative . It characterizes the future condition of the river and its immediate environment without federal or state action to designate the Kanektok as a wild river. Alternative 2 would designate as wild the main river upstream from the Qanirtuuq, Inc. land to Kagati Lake. Comments on the draft study should be sent to the following official no later than Regional Director Alaska Regional Office National Park Service 540 West Fifth Avenue Anchorage, Alaska 99501 (907) 271-4691 U.S. Department of the Interior / National Park Service