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1922 Elizabeth T
co.rYRIG HT, 192' The Moootainetro !scot1oror,d The MOUNTAINEER VOLUME FIFTEEN Number One D EC E M BER 15, 1 9 2 2 ffiount Adams, ffiount St. Helens and the (!oat Rocks I ncoq)Ora,tecl 1913 Organized 190!i EDITORlAL ST AitF 1922 Elizabeth T. Kirk,vood, Eclttor Margaret W. Hazard, Associate Editor· Fairman B. L�e, Publication Manager Arthur L. Loveless Effie L. Chapman Subsc1·iption Price. $2.00 per year. Annual ·(onl�') Se,·ent�·-Five Cents. Published by The Mountaineers lncorJ,orated Seattle, Washington Enlerecl as second-class matter December 15, 19t0. at the Post Office . at . eattle, "\Yash., under the .-\0t of March 3. 1879. .... I MOUNT ADAMS lllobcl Furrs AND REFLEC'rION POOL .. <§rtttings from Aristibes (. Jhoutribes Author of "ll3ith the <6obs on lltount ®l!!mµus" �. • � J� �·,,. ., .. e,..:,L....._d.L.. F_,,,.... cL.. ��-_, _..__ f.. pt",- 1-� r�._ '-';a_ ..ll.-�· t'� 1- tt.. �ti.. ..._.._....L- -.L.--e-- a';. ��c..L. 41- �. C4v(, � � �·,,-- �JL.,�f w/U. J/,--«---fi:( -A- -tr·�� �, : 'JJ! -, Y .,..._, e� .,...,____,� � � t-..__., ,..._ -u..,·,- .,..,_, ;-:.. � --r J /-e,-i L,J i-.,( '"'; 1..........,.- e..r- ,';z__ /-t.-.--,r� ;.,-.,.....__ � � ..-...,.,-<. ,.,.f--· :tL. ��- ''F.....- ,',L � .,.__ � 'f- f-� --"- ��7 � �. � �;')'... f ><- -a.c__ c/ � r v-f'.fl,'7'71.. I /!,,-e..-,K-// ,l...,"4/YL... t:l,._ c.J.� J..,_-...A 'f ',y-r/� �- lL.. ��•-/IC,/ ,V l j I '/ ;· , CONTENTS i Page Greetings .......................................................................tlristicles }!}, Phoiitricles ........ r The Mount Adams, Mount St. Helens, and the Goat Rocks Outing .......................................... B1/.ith Page Bennett 9 1 Selected References from Preceding Mount Adams and Mount St. -
CHILCOTIN CENTRAL COAST DESTINATION DEVELOPMENT STRATEGY APE LAKE Photo: Kari Medig
CHILCOTIN CENTRAL COAST DESTINATION DEVELOPMENT STRATEGY APE LAKE Photo: Kari Medig DESTINATION BC Seppe Mommaerts MANAGER, DESTINATION DEVELOPMENT Jody Young SENIOR PROJECT ADVISOR, DESTINATION DEVELOPMENT [email protected] CARIBOO CHILCOTIN COAST TOURISM ASSOCIATION Amy Thacker CEO 250 392 2226 ext. 200 [email protected] Jolene Lammers DESTINATION DEVELOPMENT COORDINATOR 250 392 2226 ext.209 [email protected] MINISTRY OF TOURISM, ARTS AND CULTURE Amber Mattock DIRECTOR, LEGISLATION AND DESTINATION BC GOVERNANCE 250 356 1489 [email protected] INDIGENOUS TOURISM ASSOCIATION OF BC 604 921 1070 [email protected] CHILCOTIN CENTRAL COAST | 2 TABLE OF CONTENTS EXECUTIVE SUMMARY ...........................................................................1 6. A DISTINCTIVE DIRECTION ..........................................................30 a. Distinctive Destination for the Chilcotin Central Coast a. Vision b. Distinctive Direction for the Chilcotin Central Coast b. Goals c. Guiding Principles for Destination Development II. ACRONYMS ...........................................................................................5 d. Motivating Experiences 1. FOREWORD AND ACKNOWLEDGEMENTS..............................7 e. Development Themes 2. INTRODUCING THE STRATEGY .....................................................9 7. STRATEGY AT A GLANCE ................................................................38 a. Program Vision and Goals 8. STRATEGIC PRIORITIES ................................................................. -
GLACIER MASS-BALANCE MEASUREMENTS a Manual for Field and Office Work O^ O^C
'' f1 ^^| Geographisches |^ Institut | "| Universitat NHRI Science Report No. 4 VJ Zurich GLACIER MASS-BALANCE MEASUREMENTS A manual for field and office work o^ O^c G. 0strem and M. Brugman NVE NORWEGIAN WATER RESOURCES AND • <j<L • EnvironmenEnvironi t Environnemant ENERGY ADMINISTRATION •^rB Canada Canada PREFACE During the International Hydrological Decade (1965-1975) it was proposed that the hydrology of selected glaciers should be included in National IHD programs, in addition to various other aspects of hydrology. In Scandinavia it was agreed that Denmark should concentrate on low-land hydrology, including ground water; Sweden should emphasize forested basins, including bogs; and Norwegian hydrologists should study alpine hydrology, including glaciers. Representative, basins were then selected in each country, according to this inter-Scandinavian agreement. In Norway, the selected alpine basins did not comprise glaciers, so some of the already observed glaciers were included in the IHD program. In Canada, the Geographical Branch, within the Department of Mines and Technical Surveys, initiated mass-balance studies on selected glaciers along an east-west profile from the National Hydrology Research Institute Rockies to the Coast Mountains. Inland Waters Directorate Canada, and later Norway, felt that glacier field crews and office technicians Conservation and Protection needed written instructions for their work. This would save time at the start of the Environment Canada EHD program, because new activities were planned at several glaciers almost simultaneously. 11 Innovation Boulevard Therefore, a "cookbook" was prepared in Ottawa by Gunnar 0strem and Alan Saskatoon, Saskatchewan Stanley. This first "Manual for Field Work" was printed in the spring of 1966 for Canada S7N 3H5 use during the following field season. -
Glacier Fluctuations in Garibaldi Provincial Park, Coast Mountains, British Columbia, Canada Johannes Koch,1* Gerald D
The Holocene 17,8 (2007) pp. 1069–1078 Pre-‘Little Ice Age’ glacier fluctuations in Garibaldi Provincial Park, Coast Mountains, British Columbia, Canada Johannes Koch,1* Gerald D. Osborn2 and John J. Clague1 ( 1Department of Earth Sciences, Simon Fraser University, Burnaby, British Columbia V5A 1S6, Canada; 2Department of Geology and Geophysics, University of Calgary, Calgary, Alberta T2N 1N4, Canada) Received 21 July 2006; revised manuscript accepted 10 June 2007 Abstract: Holocene glacier fluctuations prior to the ‘Little Ice Age’ in Garibaldi Provincial Park in the British Columbia Coast Mountains were reconstructed from geomorphic mapping and radiocarbon ages on 37 samples of growth-position and detrital wood from glacier forefields. Glaciers in Garibaldi Park were smaller than at present in the early Holocene, although some evidence exists for minor, short-lived advances at this time. The first well-documented advance dates to 7700–7300 14C yr BP. Subsequent advances date to 6400–5100, 4300, 4100–2900 and 1600–1100 14C yr BP. Some glaciers approached their maximum Holocene limits several times during the past 10 000 years. Periods of advance in Garibaldi Park are broadly synchronous with advances else- where in the Canadian Cordillera, suggesting a common climatic cause. The Garibaldi Park glacier record is also broadly synchronous with the record of Holocene sunspot numbers, supporting previous research that sug- gests solar activity may be an important climate forcing mechanism. Key words: Glacier advances, dendroglaciology, Holocene, solar forcing, Garibaldi Park, Coast Mountains, British Columbia. Introduction The most direct evidence of pre-‘Little Ice Age’ glacier activ- ity is found in glacier forefields and includes in situ tree stumps Recent studies point to significant and rapid fluctuations of climate (Ryder and Thomson, 1986; Luckman et al., 1993; Wiles et al., throughout the Holocene (Bond et al., 2001; Mayewski et al., 1999; Wood and Smith, 2004), detrital logs and branches (Ryder 2004). -
Chilliwack River - Slesse Creek Area New Westminster Mining Division Southwestern British Columbia
- GEOLOGICAL and DIAMOND DRILLING ASSESSMENT REPORT on the SOUTH SLESSE LIMESTONE QUARRY CHILLIWACK RIVER - SLESSE CREEK AREA NEW WESTMINSTER MINING DIVISION SOUTHWESTERN BRITISH COLUMBIA Longitude- 12 1”42’3VW/Latitude 49”04’35”N NTS 92H/4E - Permit No. NAN-97-07001 10-94, MX-7-114 Prepared for . Machine 86Fibers Ltd. 600-42nd Avenue, S.E. P.O. Box 1325 ? Calgary, Alberta T2P 2L2 *\ ‘/ ‘ ;T<’ Phone: 403-265--6022, Fax: 403-266-264 A ‘.>.a L“: ;” cz! Prepared by ~.,q ,*y ;:cj ‘2. i:ilic;;y>,&_pi J. T. SHEARER, M.Sc., P.Geo. ,..~,, ,- 3 ,;;> “-.> HOMEGGLD RESOURCES LTD. .#:,~,. ~;;1::%,,i g 2; 2 i” ,, % , $ “3 ,“: #5-2330 Tyner St. “.*_&F s” :;22 Port Coquitlam, B.C. “5r;5 v3c 221 ‘“”,:& (5 - ? Phone/Fax: 604-944-6 102 *” .,.I ix “‘2 %i July 15, 1998 P%e ,$ Fieldwork completed between October 4 8e November 25, 1997 ;z 86 March 24 - June 30,199s 1: P TABLE OF CONTENTS !3fs . LIST OF FIGURES and TABLES ................................................................ SUMMARY .............................................................................................. iii _ INTRODUCTION ....................................................................................... 1 LOCATION and ACCESS ........................................................................... 2 CLAIM STATUS ........................................................................................ 4 _ REGIONAL GEOLOGY.. ............................................................................. 5 PROPERTY GEOLOGY and CaC03 RESOURCES ........................................ -
The Photography Issue Tantalus Crossing - Squamish 2 & 3 Bedroom Townhomes from $324,950
WINTER/SPRING 2013 THE PHOTOGRAPHY ISSUE Tantalus Crossing - Squamish 2 & 3 bedroom townhomes from $324,950 MOVE IN SPRING 2013 Voted Best Quality, Best Value and Best Location Phase I sold out. Some great deals still available in Phase Two. Look forward to seeing you here. Come and visit us at the display home on site 40653 Tantalus Rd, Thursday-Sunday 1-4pm For appointment, call Gena Belanger 604-892-4012 [email protected] Target Developments VANCOUVER WHISTLER VILLAGE WHISTLER CREEKSIDE 604 738 3715 604 905 4100 604 905 2444 3rd and Pine St., Kitsilano Marketplace: Beside IGA Innsbruck Rd: Beside Boston Pizza skiisandbiikes.com LFH_2013_Mtn_Life_ad.indd 1 12-10-16 8:20 PM Fornix Helmet Iris 3P Goggle The Fornix helmet combines light weight, Key Features Iris 3P has the unique 3P lens which enables relief Key Features Aramid Bridge adjustable ventilation, size adjustability, and a from excessive reflection without sacrificing the Partially Polarized Adjustable Ventilation NXT Lens unique safety feature called The Aramid Bridge Size Adjustment needed glare to differentiate snow from ice. Thanks Photochromatic to bring you a safe and comfortable helmet. Light weight to the POC Partially Polarized Technology the 3P HCD Filter Optimized fit for The Aramid Bridge is a safety feature that ensures NXT lens optimizes ability to quickly read the snow POC helmets the entire integrity of the helmet is used upon an conditions ahead. The 3P lens is Photochromatic impact, ensuring a high level of energy and also has the patented color vision boosting absorption. The strands of Aramid within the EPS filter HCD (High Chromatic Definition) as well as foam increase the structural stability of the superb olephobic/ hydrophobic treatment and helmet, all while being very light. -
JANUARY MEETING Thursday, January 5Th, 7:30 P.M
JANUARY 1989 BOEING EMPLOYEES ALPINE SOCIETY, INC. PresideW;~,.,., ... Ken Johnson .. OU·31 .. 342-3974 Conservation ........ Eric Kasiulis.. 81-16 .. 773-57 42 Vice Pr~llnt;. .... .steveMason.. 97 -1.7 ...237 -5820 Echo Editor......... .Rob Freeman .. 6N -95 ..234-0468 Treas=.......... EIden Altiz.er .. 97-17 ...234'1721 Equipm~nt ........... Gareth Beale .. 7A-35 .. 865-5375 Secre~_ .. , .. _.. _•• JolinSumner.• 2.6-63 ... 655~9882 Librarian ............ Rik Anderson .. 76-15 .. 237 -9645 Past Pmsident..A:mbrose. Bittner.. OT-06 ... 342-5140 Membership.. Richard Babunovic.. 6L-15 .. 235-7085 ·Aeti,:tilts ..........MelissaStorey .. 1R-40... 633-3730 Programs.......... Tim .Backman . .4M-02.. 655-4502 Photo: Nevado Huandoy by Mark Dale D. OTT 5K-25 * FROM: 6L-15 R_BABUNOVIC JANUARY MEETING Thursday, January 5th, 7:30 P.M. Oxbow Rec Center CROSS COUNTRY SKI ROUTES ON MT. HOOD AND CENTRAL OREGON The January meeting will feature a slide presentation by Klindt vielbig, mountaineer as well as skier and author of "Cross Country Ski Routes Of Oregons' Cascades". Klindt will show slides illustrating many of the tours described in his book including Mt. )iood, the Wallowa Mtns., Crater Lake, Broken Top Crater, and Mt. Shasta. The diversity of ski tours makes this program a great aid in learning more about oregon skiing. Additionally, Boealps member Jim Blilie will give a short ~esentation on ice climbing. This is an appetizer to Jim's Feb.4-5 Leavenworth ice climbing/knuckle bashing weekend extravaganza. Belay Stance Well November's powder has yielded to December's thaw. Where has all the snow gone. What had started as a great ski season is now looking somewhat questionable. -
Little Ice Age History of Tzeetsaytsul Glacier, Tweedsmuir Provincial
Document generated on 10/02/2021 5:55 a.m. Géographie physique et Quaternaire Little Ice Age history of Tzeetsaytsul Glacier, Tweedsmuir Provincial Park, British Columbia Évolution du glacier de Tzeetsaytsul, au parc provincial de Tweedsmuir (Colombie-Britannique) au cours du Petit Âge glaciaire Geschichte der kleinen Eiszeit des Tzeetsaytsul-Gletschers im Tweedsmuir Provincial Park, British Columbia Dan J. Smith and Joseph R. Desloges Volume 54, Number 2, 2000 Article abstract This paper describes licheno- metric and dendroglaciological investigations of URI: https://id.erudit.org/iderudit/004870ar Little Ice Age (LIA) deposits at Tzeetsaytsul Glacier, Tweedsmuir Provincial DOI: https://doi.org/10.7202/004870ar Park, British Columbia. The glacier originates from an ice- field on the northeast flank of Tzeetsaytsul Peak and terminates in a moraine-dammed See table of contents lake. A stream draining the lake has incised the moraine dam and flows through nested moraines into a second lake. Two end moraines near the lower lake record separate advances, with numerous morainic ridges found between Publisher(s) the two lakes. A locally calibrated Rhizocarpon geographicum growth curve was constructed and provides relative ages for all the moraines. Absolute dates Les Presses de l'Université de Montréal from wood fragments collected from within the morainic debris were determined by matching their annual growth ring patterns to a local Abies ISSN lasiocarpa tree-ring chronology. The outermost terminal moraine was deposited by a 17th century advance that culminated in ca. 1700. Following 0705-7199 (print) subsequent recession, Tzeetsaytsul Glacier readvanced to build a second 1492-143X (digital) terminal moraine by the mid-1800s. -
Monarch Mountain, Southwest Face, and Other Ascents
AAC Publications Monarch Mountain, Southwest Face, and Other Ascents Canada, British Columbia, Coast Mountains ON JULY 28, Micha Rinn from Germany and I flew by helicopter to the col between Monarch Mountain and Page Mountain at the head of the Empire Way Glacier, deep in the Coast Mountains. Our objective was the pronounced spur that runs up the center of the unclimbed 1,250m southwest face of Monarch Mountain (3,555m). It was a line that prompted awe and excitement in equal measure—a veritable Walker Spur leading directly to the summit of the peak. How a Scottish-German climbing team came to know about one of the finest unclimbed features in western Canada requires some explanation. My fascination with Monarch, the second-highest massif in the Coast Mountains, began 20 years ago when Dave Hesleden and I traversed the Serra Group after making the first ascent of the southeast ridge of Asperity Mountain in the Waddington Range. [The route referred to in the AAJ report as the south ridge later came to be called the southeast ridge. It faces more or less south-southeast.]As we tussled with the jagged crest of the Serras, reputedly the most difficult summits in the range, Monarch stood out like a sentinel 70 miles to the north. With a prominence of 2,925m, there is no higher peak until you reach Mt. Fairweather, a thousand miles up the spine of the coastal range. I was smitten by Monarch’s dominance and resolved to climb it. The Coast Mountains had got under my skin, and I made two further trips to the Waddington massif, a couple to the Pantheon Spires, and one to the difficult-to-access Mt. -
Legend Leader: Prof
CREVASSE HAZARD MAP AT THE JUNEAU ICEFIELD 134°40'0"W 134°30'0"W 134°20'0"W 134°10'0"W 134°0'0"W 133°50'0"W 133°40'0"W Mount Canning Mount Pullen 59°10'0"N 59°10'0"N Mount Hislop Mount Poletca Mount Service Mount London 59°0'0"N 59°0'0"N Field Glacier Boundary Peak 99 Mount Nesselrode Mount Bressler Boundary Peak 96 Bucher Glacier Mount Ogilvie Gale Peak Antler Glacier Blizzard Peak 58°50'0"N 58°50'0"N Vaughan Lewis Glacier Mammary Peak Elephant Promontory Gilkey Glacier Mount Moore Mount Blachnitzky Picket Gate Crags Avalanche Canyon The Citadel Gisel Peak Spirit Range Dipyramid The Wall Bacon Creek Echo Glacier Mathes Gl aci er Amalga (historical) Centurian Peak Unknown Glacier Devils Paw Batle Gl aci er Berners Peaks Couloir Peak The Tusk Thiel GlacierHorn Spire Glacier King Echo Mountain Icefall SpiresCamp 15 Peak Exploraton Peak Demorest Glacier Mount Adolph Knopf Ivy Ridge Floprock Peak The Horn Peaks 58°40'0"N 58°40'0"N Tricouni Peak West Branch Taku Glacier Knowl Hades Highway Vantage Peak Dike Mountain Carpet Peak Bacon Glacier Snowpatch Crag Nunatak Chalet Mustang Peak Icy BasinWashington Basin Antler Peaks Eagle Glacier The Snow Towers Litle Ma aerhor n Folded TowersJuneau Icefiel d Cathedral Peak Organ Pipes Camp 4 Peak Juncture Peak Twin Glacier Peak Taku Towers Boundary Lake Taku Glacier Hodgkins Peak Taku Range East Twin Glacier Boundary Creek Snowdrif Peak West Twin Glacier Triangle Peak The Dukes Kluchman Mountain Mount Ernest GrueningHerbert Glacier Sitakanay Ri ver Rhino PeakPrincess Peak Columbia Basin (not official) -
MVRD Parks Board Meeting Agenda Package
Meeting 1 of 7 METRO VANCOUVER REGIONAL DISTRICT (MVRD) - PARKS REGULAR BOARD MEETING Friday, February 24, 2017 9:00 A.M. 2nd Floor Boardroom, 4330 Kingsway, Burnaby, British Columbia Membership and Votes A G E N D A1 A. ADOPTION OF THE AGENDA 1. February 24, 2017 Regular (Parks) Meeting Agenda That the MVRD Board adopt the agenda for its regular (Parks) meeting scheduled for February 24, 2017 as circulated. B. ADOPTION OF THE MINUTES 1. October 28, 2016 Regular (Parks) Meeting Minutes That the MVRD Board adopt the minutes for its regular (Parks) meeting held October 28, 2016 as circulated. C. DELEGATIONS D. INVITED PRESENTATIONS E. CONSENT AGENDA Note: Directors may adopt in one motion all recommendations appearing on the Consent Agenda or, prior to the vote, request an item be removed from the Consent Agenda for debate or discussion, voting in opposition to a recommendation, or declaring a conflict of interest with an item. 1. REGIONAL PARKS COMMITTEE REPORTS 1.1 Regional Parks Facilities for Connecting People with Nature Policy That the MVRD Board approve the “Regional Parks Facilities for Connecting People with Nature Policy” as presented in the report dated January 23, 2017, titled “Regional Parks Facilities for Connecting People with Nature Policy”. 1 Note: Recommendation is shown under each item, where applicable. February 15, 2017 Metro Vancouver Regional District - Parks - 1 MVRD Board Agenda - Parks February 24, 2017 Agenda Page 2 of 3 1.2 Widgeon Marsh Regional Park Reserve – Background Information and Public Engagement Development of a Regional Park Management Plan That the MVRD Board: a) authorize staff to undertake public engagement associated with the preparation of a park management plan for Widgeon Marsh Regional Park Reserve; and b) direct staff to report back to the MVRD Board with a summary of the feedback received from the public engagement events and a draft Widgeon March Regional Park Reserve Management Plan. -
Simulating Past and Future Mass Balance of Place Glacier Using a Physically-Based, Distributed Glacier Mass Balance Model
Simulating Past and Future Mass Balance of Place Glacier Using a Physically-Based, Distributed Glacier Mass Balance Model by RaJU Aryal B Sc . Tribhuvan Umvers1ty, Nepal. 1995 M.Sc. Tnbhuvan Unt\ersity. Nepal, 1999 M Sc, Nagoya Unt\ersity. Japan, 2002 THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY IN NATURAL RESOURCES AND ENVIRONMENTAL STUDIES UNIVERSITY OF NORTHERN BRITISH COLUMBIA (Prince George) April2015 © Raju Aryal2015 Abstract The objective of this study is to develop a physically-based distributed glacier mass balance (GMB) model for Place Glacier, Brittsh Columbia, Canada, and apply the model to develop the historic and the future mass balance The model Is forced with climate data from Regional Atmospheric Modelmg System (RAMS) mesoscale atmospheric model output from 1979-2008 for developmg htstonc mass balance on Place Glacter The model IS also run in the future (2009-2040) to develop a proJeCtiOn of mass balance. The model simulated the histone glacter-wtde summer and wmter balance on Place Glacier satisfactorily. For all years, root mean squared error (RMSE) m simulated summer and winter balance are 0.43 m water equivalent (we) and 0.27 m w.e., respectively. Over the period of 29 years, the model simulated a cumulative net mass balance of -33.72 m w.e. The model outperformed both empirical temperature index (TI) and enhanced TI models in simulating summer balance on Place Glacier when forced with the same RAMS variables. A linear regression model based on Singular Value Decomposition (SVD) technique is used for downscaling future climate projections from a suite of Global Climate Models (GCMs).