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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 -
USGS Scientific Investigations Map 2832, Pamphlet
Geologic Map of Mount Mazama and Crater Lake Caldera, Oregon By Charles R. Bacon Pamphlet to accompany Scientific Investigations Map 2832 View from the south-southwest rim of Crater Lake caldera showing the caldera wall from Hillman Peak on the west to Cleetwood Cove on the north. Crater Lake fills half of the 8- by 10-km-diameter caldera formed during the climactic eruption of Mount Mazama volcano approximately 7,700 years ago. Volcanic rocks exposed in the caldera walls and on the flanks record over 400,000 years of eruptive history. The exposed cinder cone and andesite lava flows on Wizard Island represent only 2 percent of the total volume of postcaldera volcanic rock that is largely covered by Crater Lake. Beyond Wizard Island, the great cliff of Llao Rock, rhyodacite lava emplaced 100–200 years before the caldera-forming eruption, dominates the northwest caldera wall where andesite lava flows at the lakeshore are approximately 150,000 years old. 2008 U.S. Department of the Interior U.S. Geological Survey This page intentionally left blank. CONTENTS Introduction . 1 Physiography and access . 1 Methods . 1 Geologic setting . 4 Eruptive history . 5 Regional volcanism . 6 Pre-Mazama silicic rocks . 6 Mount Mazama . 7 Preclimactic rhyodacites . 9 The climactic eruption . 10 Postcaldera volcanism . .11 Submerged caldera walls and floor . .11 Glaciation . .11 Geothermal phenomena . 12 Hazards . 13 Volcanic hazards . 13 Earthquake hazards . 14 Acknowledgments . 14 Description of map units . 14 Sedimentary deposits . 15 Volcanic rocks . 15 Regional volcanism, northwest . 15 Regional volcanism, southwest . 17 Mount Mazama . 20 Regional volcanism, east . 38 References cited . -
Recognizing Ice-Contact Trachyte-Phonolite Lavas at The
RECOGNIZING ICE-CONTACT TRACHYTE-PHONOLITE LAVAS AT THE MOUNT EDZIZA VOLCANIC COMPLEX, BRITISH COLUMBIA, CANADA by Kristen A. LaMoreaux B.S., Kent State University, 2002 Submitted to the Graduate Faculty of Arts and Sciences in partial fulfillment of the requirements for the degree of Master of Science University of Pittsburgh 2008 UNIVERSITY OF PITTSBURGH ARTS AND SCIENCES This thesis was presented by Kristen A. LaMoreaux It was defended on June 17, 2008 and approved by Dr. Michael Ramsey Dr. Thomas Anderson Thesis Director: Dr. Ian Skilling ii Copyright © by Kristen A. LaMoreaux 2008 iii RECOGNIZING ICE-CONTACT TRACHYTE-PHONOLITE LAVAS AT THE MOUNT EDZIZA VOLCANIC COMPLEX, BRITISH COLUMBIA, CANADA Kristen A. LaMoreaux, M.S. University of Pittsburgh, 2008 Mount Edziza Volcanic Complex (MEVC) lies within the Northern Cordilleran Volcanic Province (NCVP), in northwest British Columbia, Canada. The eruption products have been emplaced in a variety of subaerial, sub-ice and subaqueous environments from about 8Ma to less than 2000 y.b.p. (Souther, 1992). Ice Peak Formation (IPF) trachyte lava flows of approximately 1Ma age (Souther, 1992) are exposed at Ornostay Bluff (OB) and Koosick Bluff (KB). These flows comprise basal flow breccias overlain by massive conchoidally-fractured lava with large, poorly-developed columns, and local flow banding. Edziza Formation (EF) approximately 1Ma (Souther, 1992) phonolite is exposed at Triangle Dome (TD). TD can broadly be divided into an upper and lower zone. The upper zone comprises poorly-developed columns in addition to prominent jointing. In the lower zone the columns are planar and 75cm- 3m-wide in the interior of the complex grading into fan-like and curved subhorizontal columns <75cm-wide in the outer margins of the lower zone. -
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). -
Ni 43-101 Technical Report Snoball Property
NI 43-101 TECHNICAL REPORT ON THE SNOBALL PROPERTY Project Location: Liard Mining Division, British Columbia, Canada Latitude 57° 10’ North, Longitude 130° 30’ West NAD 83, Zone 9N, 409300E, 6336900N NTS Map Sheets 104G/ 1W and 2E Prepared for: Evergold Corp. 729 Okanagan Avenue East Penticton, British Columbia, Canada V2A 3K7 Prepared by: David W. Tupper, P.Geo. Effective Date: May 23, 2019 Page iii ______________________________________________________________________ CERTIFICATE OF QUALIFIED PERSON I, David W. Tupper, am a professional geologist residing at 2-620 West 15th St., North Vancouver, British Columbia, Canada, V7M 1S9, and do hereby certify that: 1. I am the author of the report entitled "NI 43-101 Technical Report on the Snoball Property”, dated May 23, 2019; 2. I am a Registered Professional Geoscientist (P.Geo.), Practising, with the Association of Professional Engineers and Geoscientists of British Columbia (licence # 121813). 3. I graduated from the University of British Columbia, Canada, with a B.Sc. in Geology in 1985; 4. I have practiced my profession continuously since graduation, concentrating in mineral property exploration and Quarternary geology throughout British Columbia, the Yukon and Ontario, Nevada, Alaska, Chile and Asia; 5. I visited the Snoball Property on May 11, 2019; 6. I have had no previous involvement with the Property until contracted to write this Technical Report; 7. I am responsible for all sections of this Report entitled "NI 43-101 Technical Report on the Snoball Property”, dated May 23, 2019; 8. I am independent of Evergold Corp. as independence is described in Section 1.5 of NI 43-101. -
Mountain Goats
Environmental Risk Assessment: Base Line Scenario Mountain Goats Prepared by Brad T. Pollard, R.P.Bio. Acer Resource Consulting Ltd., Terrace, B.C.. March 2003. Table of Contents 1.0 Definitions and Abbreviations..........................................................................4 2.0 Introduction.........................................................................................................5 3.0 Methods ..............................................................................................................6 3.1 General Approach............................................................................................6 3.2 Indicators.........................................................................................................8 3.3 Assumptions.................................................................................................. 10 3.4 Analysis and Models...................................................................................... 11 4.0 Results............................................................................................................... 13 4.1 Indicators....................................................................................................... 13 4.2 Risk Assessment............................................................................................ 15 5.0 Discussion and Conclusions............................................................................... 16 5.1 Indicators...................................................................................................... -
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.