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INVENTORY of TERMINAL POSITION CHANGES in ALASKAN COASTAL GLACIERS SINCE the 1750'S
INVENTORY OF TEWINAL POSITION CHANGES IN ALASKAN COASTAL GLACIERS SINCE THE 1750's MAYNARD M. MILLER Foundation for Glacier & Environmental Research Pacific Science Center Seattle, WA 98109 Repnnted frum PEmEEDIhGS OF THE? .LmHCAi"; PNfLOXlPNlCAL SOCIETY, Vnl 108, No 3, June, 196-4 INVENTORY OF TERMINAL POSITION CHANGES IN ALASKAN COASTAL GLACIERS SINCE THE 1750's MAYNARD M. MILLER Dep;~rttnerltof Geology, Michigan State Ilniversity, a~idthe Fountlation fnr Glacier Research, Seattle, \Vashingtori THE PROGRAM OF REGIOXAI, GLACIER graphic records at established control stations, a SURVEYS 1 long-negative Zeiss-Ikon camera, a Speed Graphic 'I'ris neetl for a syste~naticand up-to-date in- or a Keystone F10 photogran~metriccamera were \entory of glacier positions in the cordilleran employed. The aerial photographs were taken r:lrlges oi Sot~theril~\laska first became apparent either with a 90 111111. German aerial Handkammer, io lue \vliile participating in two glacial illapping a Fairchild 4 x 5-inch I<-20 camera or the afore- c5sl)ecli tlons to the .ilaskan f-':ui~liandlein 1940 and mentioned F10. More than 2,700 ohlique photo- 1941 (Miller, 1940, 1913). As a result, each graphs and recorded o1)servations on 174 major sulnmer froin 1946 through 1953, I was for- glaciers have been obtained.' tunate enough to be able to undertake a pro- gram of ground and aerial surveys of termini GLACIOLOGICAL PROVINCES IN SOUTH ;untl nCvi.-line positions on Alaskan coastal glaciers COASTAL ALASKA ihlilier. 1947. 1918, 1949. 1954). The project For convenience. southeastern coastal Alaska \\:is further extended by selective photography is divided into seven glaciological provinces de- :~nclniapping carried out in 1954, 1955, 1958, and lineated on the nlap in figure 3. -
Geology and Mineral Deposits Tulsequah Map-Area, British Columbia (104K)
GEOLOGY AND MINERAL DEPOSITS TULSEQUAH MAP-AREA, BRITISH COLUMBIA (104K) 1.(50-1971-6J44 Technical Editor H. M. A. RJCl! Critical Readers J. O. WHUL~R HNll R. B. CAMPBELL Editor D. W>UT1! Text printed OD Georgian Olfset Smooth Finish Set iD Times Roman with 20th Century captioos by CANADIAN GOVEI\NMENT PJuN'TTNG BUReAU Artwork by C,\JlTOCRAPHlC UNIT, GSC 201339 FIGURE 1. View looking 'outhwe'l from the Tohllon Highland ocro" Tohomenie lake to the inner range' of the Coo,1 Mountain<. GEOLOGICAL SURVEY OF CANADA MEMOIR 362 GEOLOGY AND MINERAL DEPOSITS OF TULSEQUAH MAP-AREA, BRITISH COLUMBIA (104K) By J. G. Souther DEPARTMENT OF ENERGY, MINES AND RESOURCES CANADA © Crown Copyrighls reserved AvailabLe by mail from Information Canada, OIlOWO, rrom Geological SOf"ey or Canada. 601 Boolh St., Ollaw" nnd tll the following Jnformalion Canada b()Qk~hops: HALl FA>.' 1735 Barringlon Slreel MONTREAL 1182 SI. Cnlherine SlreeL West OrT,\WA 171 S Ialer Slreel TORONTO '22L Yonge Streel WINNlPEG 393 Ponage Avenue VA1'JCOUV£R 657 GranvilLe Street or through your bookseller A depos\t copy or Ihis publicalion is also 3yailable ror reference in public libraries acros~ Canada Price: $3.00 Calalogue No. M46·362 Price subju.1 to c.hange wilhaut nOlice Tnformiuion Canada Ollawa. 1971 PREFACE Taku River was used as a route to the Yukon during the Klondike gold rush of 1898 and this led to extensive prospecting, but it was not until 1937 that any of the silver-gold showings discovered in the intervening years were brought into production. Declining metal prices resulted in the closure of the last producing mine in 1957, but in recent years extensive geophysical and geochemical surveys have been made by several major exploration com panies and new prospects have been discovered. -
An#Integrated#Assessment#Of#The#Cumulative#Impacts#Of#Climate# Change'and'industrial'development'on'salmon'in'western'bc!! Stiki
An#integrated#assessment#of#the#cumulative#impacts#of#climate# change'and'industrial'development'on'salmon'in'Western'BC!! Stikine and Upper Nass Current Social-Ecological Conditions Summary Prepared by: Christina Melymick, Consultant April 2013 The views and conclusions contained in this document are those of the author and should not be interpreted as representing the opinions of the Bulkley Valley Research Centre or the Gordon and Betty Moore Foundation. [email protected] • Box 4274 Smithers, BC V0J 2N0 Canada An#integrated#assessment#of#the#cumulative#impacts#of#climate#change#and#industrial#development#on#salmon#in#Western#BC#! Acknowledgements Thank you to the Gordon and Betty Moore Foundation for supporting this project. Thank you to Jim Pojar for his expansive knowledge and expertise, and for adding to the stack of resources used during research. Thank you to Dave Bustard for taking time from a busy schedule to lend his extensive local knowledge and expertise. Thank you to John Kelson for his eulachon knowledge. Thank you to Richard Overstall for his knowledge and support. Thank you to Rick Budhwa for his support and contribution to the cultural aspects of this report. Thank you to Johanna Pfalz for her support and for providing all the relevant maps. Thank you to Ken Rabnett for support, his breadth of knowledge on the study area. Thank you to Don Morgan for the opportunity to carry out the research and produce this report, and for constant patience, guidance and support through the course of completing this report. Credits Don -
Ring of Fire Proposed RMP and Final EIS- Volume 1 Cover Page
U.S. Department of the Interior Bureau of Land Management N T OF M E TH T E R A IN P T E E D R . I O S R . U M 9 AR 8 4 C H 3, 1 Ring of Fire FINAL Proposed Resource Management Plan and Final Environmental Impact Statement and Final Environmental Impact Statement and Final Environmental Management Plan Resource Proposed Ring of Fire Volume 1: Chapters 1-3 July 2006 Anchorage Field Office, Alaska July 200 U.S. DEPARTMENT OF THE INTERIOR BUREAU OF LAND MANAGEMMENT 6 Volume 1 The Bureau of Land Management Today Our Vision To enhance the quality of life for all citizens through the balanced stewardship of America’s public lands and resources. Our Mission To sustain the health, diversity, and productivity of the public lands for the use and enjoyment of present and future generations. BLM/AK/PL-06/022+1610+040 BLM File Photos: 1. Aerial view of the Chilligan River north of Chakachamna Lake in the northern portion of Neacola Block 2. OHV users on Knik River gravel bar 3. Mountain goat 1 4. Helicopter and raft at Tsirku River 2 3 4 U.S. Department of the Interior Bureau of Land Management Ring of Fire Proposed Resource Management Plan and Final Environmental Impact Statement Prepared By: Anchorage Field Office July 2006 United States Department of the Interior BUREAU OF LAND MANAGEMENT Alaska State Office 222 West Seventh Avenue, #13 Anchorage, Alaska 995 13-7599 http://www.ak.blm.gov Dear Reader: Enclosed for your review is the Proposed Resource Management Plan and Final Environmental Impact Statement (Proposed RMPIFinal EIS) for the lands administered in the Ring of Fire by the Bureau of Land Management's (BLM's) Anchorage Field Office (AFO). -
Alaska Natural Heritage Program Environment and Natural Resources Institute University of Alaska Anchorage 707 a Street Anchorage, Alaska 99501
KLONDIKE GOLD RUSH NATIONAL HISTORICAL PARK VASCULAR PLANT INVENTORY KLONDIKE GOLD RUSH NATIONAL HISTORICAL PARK VASCULAR PLANT INVENTORY FINAL TECHNICAL REPORT Matthew L. Carlson, Michelle Sturdy, Rob Lipkin, & Julie A. Michaelson Alaska Natural Heritage Program Environment and Natural Resources Institute University of Alaska Anchorage 707 A Street Anchorage, Alaska 99501 National Park Service Alaska Region Inventory & Monitoring Program NPS Report : 2nd Edition, December 2004 Cooperative Agreement No. 1443CA991000013 Funding Source: National Park Service, Inventory & Monitoring Program KLONDIKE GOLD RUSH NATIONAL HISTORICAL PARK VASCULAR PLANT INVENTORY ABSTRACT In 2002 and 2003 the University of Alaska Anchorage, Alaska Natural Heritage Program (AKNHP), conducted vascular plant field inventories in Klondike Gold Rush National Historical Park as part of the Inventory and Monitoring Program of the National Park Service. The primary goal was to document greater than 90% of the vascular plant species expected to occur within the park and significantly improve our understanding of current vascular plant species distributions. The inventory targeted diverse habitat types and poorly sampled areas. The AKNHP visited ten diverse eco-geographic regions and sampled intensively within these regions from mid-June to mid-August, 2002 and early July in 2003. A total of 283 specimens were collected, recorded, pressed, and curated. One hundred seventy four individual taxa are represented, 55 are new records for the park, and an additional ten represent verifications of previously unvouchered reports. The percentage of documented taxa increased from 78% to 86% after the 2002 and 2003 field seasons. A number of finds were range extensions or taxa of conservation concern. Collections were made of the state and globally restricted species: Phyllodoce empetriformis (G4- S1S2 rank) and Eleocharis kamtschatica (G4-S2). -
THE FOREST ECOSYSTEM of SOUTHEAST ALASKA L.The Setting
1974 USDA FOREST SERVICE GENERAL TECHNICAL REPORT PNW-12 This file was created by scanning the printed publication. Text errors identified by the software have been corrected; however, some errors may remain. THE FOREST ECOSYSTEM OF SOUTHEAST ALASKA l.The Setting Arland S. Harris 0. Keith Hutchison William R. Meehan Douglas N. Swanston Austin E. Helmers John C. Hendee Thomas M. Collins PACIFIC NORTHWEST FOREST AND RANGE EXPERIMENT STATION U.S. DEPARTMENT OF AGRICULTURE FOREST SERVICE PORTLAND, OREGON ABSTRACT A description-of the discovery and exploration of southeast Alaska sets the scene for a discussion of the physical and biological features of this region. Subjects discussed include geography, climate, vegetation types, geology, minerals, forest products, soils, fish, wildlife, water, recreation, and esthetic values. This is the first of a series of publications sumnarizing present knowledge of southeast Alaska's forest resources. Pub1 ications will follow which discuss in detail the subjects mentioned above and how this information can be helpful in managing the resources. Keywords: Forest surveys, Alaska, resource planning, researc h. CONTRIBUTORS FORESTRY SCIENCES LABORATORY , JUNEAU ALASKA Arland S. Harris, Vegetation 0. Keith Hutchison, Wood Industries William R. Meehan, Fish and Vildlife FORESTRY SCIENCES LABORATORY , CORVALLIS, OREGON Douglas N. Swanston, Geology INSTITUTE OF NORTHERN FORESTRY, FAIRBANKS , ALASKA Austin E. Helmers, Discovery and History, Geography, Water MILDLAND RECREATION PROJECT, SEATTLE, WASHINGTON John C. Hendee, Recreation and Esthetics ALASKA REGION, U .S. FOREST SERVICE, JUNEAU, ALASKA Thomas pi. Collins, Soizs and Soil Development PREFACE This, the first in a series of pub1 ications summarizing knowledge about the forest resources of southeast dlaska, describes the physical, biological, and socioeconomic setting of southeast Alaska. -
The Grasslands of British Columbia
The Grasslands of British Columbia The Grasslands of British Columbia Brian Wikeem Sandra Wikeem April 2004 COVER PHOTO Brian Wikeem, Solterra Resources Inc. GRAPHICS, MAPS, FIGURES Donna Falat, formerly Grasslands Conservation Council of B.C., Kamloops, B.C. Ryan Holmes, Grasslands Conservation Council of B.C., Kamloops, B.C. Glenda Mathew, Left Bank Design, Kamloops, B.C. PHOTOS Personal Photos: A. Batke, Andy Bezener, Don Blumenauer, Bruno Delesalle, Craig Delong, Bob Drinkwater, Wayne Erickson, Marylin Fuchs, Perry Grilz, Jared Hobbs, Ryan Holmes, Kristi Iverson, C. Junck, Bob Lincoln, Bob Needham, Paul Sandborn, Jim White, Brian Wikeem. Institutional Photos: Agriculture Agri-Food Canada, BC Archives, BC Ministry of Forests, BC Ministry of Water, Land and Air Protection, and BC Parks. All photographs are the property of the original contributor and can not be reproduced without prior written permission of the owner. All photographs by J. Hobbs are © Jared Hobbs. © Grasslands Conservation Council of British Columbia 954A Laval Crescent Kamloops, B.C. V2C 5P5 http://www.bcgrasslands.org/ All rights reserved. No part of this document or publication may be reproduced in any form without prior written permission of the Grasslands Conservation Council of British Columbia. ii Dedication This book is dedicated to the Dr. Vernon pathfinders of our ecological Brink knowledge and understanding of Dr. Alastair grassland ecosystems in British McLean Columbia. Their vision looked Dr. Edward beyond the dust, cheatgrass and Tisdale grasshoppers, and set the course to Dr. Albert van restoring the biodiversity and beauty Ryswyk of our grasslands to pristine times. Their research, extension and teaching provided the foundation for scientific management of our grasslands. -
Long-Term Nivation Rates, Cathedral Massif, Northwestern British Columbia
Canadian Journal of Earth Sciences Long-Term Nivation Rates, Cathedral Massif, Northwestern British Columbia Journal: Canadian Journal of Earth Sciences Manuscript ID cjes-2019-0176.R2 Manuscript Type: Article Date Submitted by the 25-Mar-2020 Author: Complete List of Authors: Nyland, Kelsey; Michigan State University, Department of Geography, Environment, and Spatial Sciences; George Washington University, Geography Department Nelson, Frederick; Michigan State University, Department of Geography, Environment,Draft and Spatial Sciences; Northern Michigan University, Department of Earth, Environmental and Geographical Sciences Periglacial Geomorphology, Nivation, Cryoplanation, UAV Survey, Keyword: Volumetric Erosion Estimation, Denudation Rates Is the invited manuscript for consideration in a Special Not applicable (regular submission) Issue? : https://mc06.manuscriptcentral.com/cjes-pubs Page 1 of 28 Canadian Journal of Earth Sciences 1 2 3 4 5 6 7 8 9 10 11 12 13 LONG-TERM NIVATION RATES, CATHEDRAL MASSIF, 14 NORTHWESTERN BRITISH COLUMBIA 15 16 17 18 Draft 19 Kelsey E. Nyland ([email protected])1,2 Frederick E. Nelson ([email protected])2,3 20 1Department of Geography, The George Washington University, Washington, DC, USA 21 Mailing Address: 2036 H St., NW, Washington, DC, 20052 22 2Department of Geography, Environment, and Spatial Sciences, Michigan State University, East 23 Lansing, Michigan, USA 24 Mailing Address: 673 Auditorium Rd., East Lansing, MI, 48824 25 3Department of Earth, Environment, and Geographical Sciences, Northern Michigan University, 26 Marquette, Michigan, USA 27 28 29 30 Corresponding author: 31 Kelsey E. Nyland, Department of Geography, The George Washington University, 2036 H St., 32 NW, Washington, DC, 20052, USA 33 Telephone: 603-562-7023 34 Fax: 202-994-2484 1 https://mc06.manuscriptcentral.com/cjes-pubs Canadian Journal of Earth Sciences Page 2 of 28 35 Abstract: Cryoplanation terraces (CTs) are large (3000-800,000 m2), erosional landforms found 36 in upland periglacial environments. -
Exploring Juneau from Ice to Estuary: Climatic and Tectonic Controls on South-Eastern Alaskan Landscapes
Exploring Juneau from Ice to Estuary: Climatic and Tectonic Controls on South-eastern Alaskan Landscapes A field guide prepared for the Geological Society of America Penrose Conference on Climatic controls on continental erosion and sediment transport—CLAST2019 4-10 August 2019 © I. Johannsen, Led by Cathy Connor, Sonia Nagorski, and Eran Hood University of Alaska Southeast Wednesday, 7 August 2019 Penrose Conference Conveners Tara N. Jonell Jan H. Blöthe Peter D. Clift Introduction Wednesday, 7 August, 2019 Assembly at BW Baranof Hotel by 7:45 am in the lobby. South-eastern Alaska is considered one of the best natural laboratories on earth to observe the interaction among solid earth and earth surface processes. The broad region of Alaska is one of the most seismically and tectonically active areas in the world, accommodating oblique convergence of the North American plate and Yakutat microplate, with modern convergence rates on par with those in the Himalaya (Yakutat Block is converging 50.3 ± 0.8 mm/yr towards N22.9 ± 70.6˚ W; Elliot et al., 2010). Two coastal mountain ranges dominate the region surrounding Juneau: The Coast Range, trending southeast to the Dixon Entrance and continuing farther south; and the Chugach-St. Elias Range following along the Gulf of Alaska into Cross Sound (Figs. 1 and 2). These ranges are the product of a complex late Cretaceous-Cenozoic accretion of arc terranes and magmatism, overprinted by extensive Late Cenozoic glaciation (Figs. 3-6). The overall cool temperate climate and abundant moisture delivered by the North Pacific Ocean provide the necessary ingredients to develop vigorous glaciomarine systems and maritime rainforest. -
Final-Schaft-Creek-Pea-Dec-2007.Pdf
SE Samuel Engineering, Inc. We Provide Solutions Copper Fox Metals Inc. Canadian NI43-101 Technical Report Preliminary Economic Assessment on the Development of the Schaft Creek Project Located in Northwest British Columbia, Canada Effective Date: December 7, 2007 Prepared By: Qualified Persons: Samuel Engineering, Inc. Matt R. Bender, P.E. Keith McCandlish, P. Geo. 8450 E. Crescent Parkway, Suite 200 Jim Gray, P. Eng. Greenwood Village, CO 80111 Ray Hyyppa, P.E. 303.714.4840 SE Samuel Engineering, Inc. We Provide Solutions SE Samuel Engineering, Inc. We Provide Solutions Table of Contents 1.0 Executive Summary ................................................................................... 1-1 1.1 Overview of the Study .....................................................................................................1-1 1.2 Schaft Creek Property Location, Description and History ..........................................1-1 1.3 Geology and Resources..................................................................................................1-4 1.4 Metallurgy .........................................................................................................................1-7 1.5 Process .............................................................................................................................1-9 1.6 Mine Plan.........................................................................................................................1-13 1.7 Operating Costs .............................................................................................................1-16 -
Download The
RECONSTRUCTION OF HOLOCENE ENVIRONMENTAL CHANGES IN NORTHERN BRITISH COLUMBIA USING FOSSIL MIDGES by Erin Mattea Fleming B.Sc., Okanagan University College, 2005 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE in The College of Graduate Studies (Environmental Science) UNIVERSITY OF BRITISH COLUMBIA (Okanagan) August 2008 ©Erin Mattea Fleming, 2008 ABSTRACT Lake sediments contain the remains of midge communities that may be used as biological proxies for inferring past environmental changes. Freshwater midges, including Chironomidae and Chaoboridae, from two alpine tarns (Pyramid Lake and Bullwinkle Lake) in the Cassiar Mountains of northern British Columbia were used to estimate Holocene palaeotemperature changes, and more specifically, to test for the presence of the Milankovitch thermal maximum, an early Holocene warm interval coinciding with peak Holocene summer solar insolation. Mean July air temperatures were reconstructed using midge-inference models developed via weighted averaging- partial least squares (WA-PLS) regression. Cold-tolerant midge taxa dominate the stratigraphies from both Pyramid and Bullwinkle Lakes; however, warm-adapted species are more common in Bullwinkle Lake. Early Holocene warming is apparent at both lakes, however it is unclear whether this is indicative of the Milankovitch thermal maximum. A decrease in temperature occurs from 8,700-7,900 cal. yr BP at Pyramid Lake, around the same time that the 8,200 cal. yr BP cooling event occurred in the northern hemisphere. During the middle Holocene, records from Pyramid Lake indicate an overall decrease in temperature, with a short period of warmer temperatures that peak at 5,100 cal. yr BP. -
Pnw 1978 Clark001.Pdf
1 USDA FOREST SERVICE GENERAL TECHNICAL REPORT PNW-66 THE FOREST ECOSYSTEM OF SOUTHEAST ALASKA 10. Outdoor Recreation and -7 I ROGER N. ROBERT C. PACIFIC NORTHWEST FOREST AND RANGE EXPERIMENT STATION U.S. DEPARTMENT OF AGRICULTURE FOREST SERVICE PORTLAND, OREGON ABSTRACT Southeast Alaska offers a variety of recreational and esthetic or scenic resources not found elsewhere in the United States. Use of these resources for commodity production and recreational purposes is increasing, which often results in conflicts. This report sum- marizes what is known about the recreational and esthetic resources of the region, the present and anticipated recreation uses, and the important issues concerning recreation and esthetics. KEYWORDS: Recreation use, recreation, resources (forest), amenity values (forest), ecosystems, Alaska (southeast). ROGER N. CLARK is Recreation Research Project Leader, Pacific Northwest Forest and Range Experiment Station. ROBERT C. LUCAS is Wilderness Management Research Project Leader, Intermountain Forest and Range Experiment Station. ENGLISH AND METRIC EQUIVALENTS 1 acre = 0.4047 hectare 1 foot = 30.48 centimeters 1 inch = 2.54 centimeters 1 mile = 1.61 kilometers I mile per hour = 1.61 kilometers per hour 1 pound = 0.37324 kilogram 5/9('~-32) = 0C PREFACE This is the tenth and final paper in a series of publications summarizing knowledge about the forest resources of southeast Alaska. Our intent in presenting the information in these publications is to provide managers and users of southeast Alaska's forest resources with the most complete information available for estimating the con- sequences of various management alternatives. In this series of papers, we have summarized published and unpublished reports and data as well as the observations of resource scientists and managers developed over years of experience in south- east Alaska.