Accidents in North American Mountaineering
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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. -
Geomorphic Character, Age and Distribution of Rock Glaciers in the Olympic Mountains, Washington
Portland State University PDXScholar Dissertations and Theses Dissertations and Theses 1987 Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington Steven Paul Welter Portland State University Follow this and additional works at: https://pdxscholar.library.pdx.edu/open_access_etds Part of the Geology Commons, and the Geomorphology Commons Let us know how access to this document benefits ou.y Recommended Citation Welter, Steven Paul, "Geomorphic character, age and distribution of rock glaciers in the Olympic Mountains, Washington" (1987). Dissertations and Theses. Paper 3558. https://doi.org/10.15760/etd.5440 This Thesis is brought to you for free and open access. It has been accepted for inclusion in Dissertations and Theses by an authorized administrator of PDXScholar. For more information, please contact [email protected]. AN ABSTRACT OF THE THESIS OF Steven Paul Welter for the Master of Science in Geography presented August 7, 1987. Title: The Geomorphic Character, Age, and Distribution of Rock Glaciers in the Olympic Mountains, Washington APPROVED BY MEMBERS OF THE THESIS COMMITTEE: Rock glaciers are tongue-shaped or lobate masses of rock debris which occur below cliffs and talus in many alpine regions. They are best developed in continental alpine climates where it is cold enough to preserve a core or matrix of ice within the rock mass but insufficiently snowy to produce true glaciers. Previous reports have identified and briefly described several rock glaciers in the Olympic Mountains, Washington {Long 1975a, pp. 39-41; Nebert 1984), but no detailed integrative study has been made regarding the geomorphic character, age, 2 and distribution of these features. -
GLACIERS Glacial Ice Is One of the Foremost Scenic and Scientific Values of Olympic National Park
OLYMPIC NATIONAL PARK Glaciers MOUNT OLYMPUS GLACIERS Glacial ice is one of the foremost scenic and scientific values of Olympic National Park. There are about sixty glaciers crowning the Olympics peaks; most of them are quite small in contrast to the great rivers of ice in Alaska. The prominent glaciers are those on Mount Olympus covering approximately ten square miles. Beyond the Olympic complex are the glaciers of Mount Carrie, the Bailey Range, Mount Christie, and Mount Anderson. In the company of these glaciers are perpetual snowbanks that have the superficial appearance of glacial ice. Because they are lacking in the criteria below, they are (aerial view) not true glaciers. True glaciers are structurally three layered bodies of frozen water. The top layer is snow; the middle neve, or mixed snow and ice; and the bottom layer is of pure ice, which is quite plastic in nature. Crevasses or deep cracks in the glaciers form as the ice is subjected to uneven flow over alpine terrain. Another structural feature is the bergschrund, which is a prominent crevasse-like opening at the head of the glacier where the ice has been pulled away from the mountain wall. The rate of glacial flow is quite variable, and Olympic glaciers are "slow-moving" in contrast to some in Alaska which occasionally move at the rate of several hundred feet per day for short periods of time. There is no great advance of Olympic glaciers today, but there is not a rapid melting back of the ice either. Forward surges in glacial flow often occur after a number of very heavy winters and cool summers, but such activity has been relatively infrequent with Olympic glaciers in recorded time. -
2018 Basic Alpine Climbing Course Student Handbook
Mountaineers Basic Alpine Climbing Course 2018 Student Handbook 2018 Basic Alpine Climbing Course Student Handbook Allison Swanson [Basic Course Chair] Cebe Wallace [Meet and Greet, Reunion] Diane Gaddis [SIG Organization] Glenn Eades [Graduation] Jan Abendroth [Field Trips] Jeneca Bowe [Lectures] Jared Bowe [Student Tracking] Jim Nelson [Alpine Fashionista, North Cascades Connoisseur] Liana Robertshaw [Basic Climbs] Vineeth Madhusudanan [Enrollment] Fred Beckey, photograph in High Adventure, by Ira Spring, 1951 In loving memory Fred Page Beckey 1 [January 14, 1923 – October 30, 2017] Mountaineers Basic Alpine Climbing Course 2018 Student Handbook 2018 BASIC ALPINE CLIMBING COURSE STUDENT HANDBOOK COURSE OVERVIEW ........................................................................................................................ 3 Class Meetings ............................................................................................................................ 3 Field Trips ................................................................................................................................... 4 Small Instructional Group (SIG) ................................................................................................. 5 Skills Practice Nights .................................................................................................................. 5 References ................................................................................................................................... 6 Three additional -
Flow of Blue Glacier, Olympic Mountains, Washington, U.S.A.*
Journa/ DiG/a ciD/OK)', Vol. 13, No. 68,1974 FLOW OF BLUE GLACIER, OLYMPIC MOUNTAINS, WASHINGTON, U.S.A.* By MARK F. MEIER, (U.S. Geological Survey, Tacoma, Washington g8408, U .S.A.) W. BARCLAY KAMB, CLARENCE R . ALLEN and ROBERT P. SHARP (California Institute of Technology, Pasaciena, California gl 109, U.S.A.) ABSTRACT. Velocity and stra in-rate patterns in a small temperate valley glacier display flow effects of channel geometry, ice thickness, surface slope, a nd ablation. Surface velocities of 20- 55 m /year show year to-year fluctuations of I .5- 3 m /year. Tra nsverse profiles of velocity have the form of a higher-order para bola modified by the effects of flow around a broad bend in the cha nnel, which makes the velocity profile asym metric, with maximum velocity displaced toward the outside of the bend. M arginal sliding rates are 5- 22 m/ year against bedrock a nd nil against debris. Velocity vectors diverge from the glacier center-line near the terminus, in response to surface ice loss, but converge toward it near the firn line because of channel narrowing. Plunge of the vectors gives an em ergence fl ow component that falls short of bala ncing ice loss by a bout I m /year. Center-line velocities vary systematically with ice thickness and surface slope. In the upper half of the reach studied , effects of changing thickness a nd slope tend to compensate, a nd velocities are nearly constant; in the lower half; the effects are cumula tive a nd velocities decrease progressively down-stream . -
1967, Al and Frances Randall and Ramona Hammerly
The Mountaineer I L � I The Mountaineer 1968 Cover photo: Mt. Baker from Table Mt. Bob and Ira Spring Entered as second-class matter, April 8, 1922, at Post Office, Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and April by The Mountaineers, P.O. Box 122, Seattle, Washington, 98111. Clubroom is at 719Y2 Pike Street, Seattle. Subscription price monthly Bulletin and Annual, $5.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of North west America; To make expeditions into these regions m fulfill ment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor life. EDITORIAL STAFF Betty Manning, Editor, Geraldine Chybinski, Margaret Fickeisen, Kay Oelhizer, Alice Thorn Material and photographs should be submitted to The Mountaineers, P.O. Box 122, Seattle, Washington 98111, before November 1, 1968, for consideration. Photographs must be 5x7 glossy prints, bearing caption and photographer's name on back. The Mountaineer Climbing Code A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. On crevassed glaciers, two rope teams are recommended. Carry at all times the clothing, food and equipment necessary. Rope up on all exposed places and for all glacier travel. Keep the party together, and obey the leader or majority rule. Never climb beyond your ability and knowledge. -
1976 Bicentennial Mckinley South Buttress Expedition
THE MOUNTAINEER • Cover:Mowich Glacier Art Wolfe The Mountaineer EDITORIAL COMMITTEE Verna Ness, Editor; Herb Belanger, Don Brooks, Garth Ferber. Trudi Ferber, Bill French, Jr., Christa Lewis, Mariann Schmitt, Paul Seeman, Loretta Slater, Roseanne Stukel, Mary Jane Ware. Writing, graphics and photographs should be submitted to the Annual Editor, The Mountaineer, at the address below, before January 15, 1978 for consideration. Photographs should be black and white prints, at least 5 x 7 inches, with caption and photo grapher's name on back. Manuscripts should be typed double· spaced, with at least 1 Y:z inch margins, and include writer's name, address and phone number. Graphics should have caption and artist's name on back. Manuscripts cannot be returned. Properly identified photographs and graphics will be returnedabout June. Copyright © 1977, The Mountaineers. Entered as second·class matter April8, 1922, at Post Office, Seattle, Washington, under the act of March 3, 1879. Published monthly, except July, when semi-monthly, by The Mountaineers, 719 Pike Street,Seattle, Washington 98101. Subscription price, monthly bulletin and annual, $6.00 per year. ISBN 0-916890-52-X 2 THE MOUNTAINEERS PURPOSES To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanentform the history and tra ditions of thisregion; To preserve by the encouragement of protective legislation or otherwise the natural beauty of NorthwestAmerica; To make expeditions into these regions in fulfill ment of the above purposes; To encourage a spirit of good fellowship among all loversof outdoor life. 0 � . �·' ' :···_I·:_ Red Heather ' J BJ. Packard 3 The Mountaineer At FerryBasin B. -
1949 Number 13
- . ' _, .... ,:..,, ,'; - ;,. f ' ; -::; -· � :� "' ·- �- ., � . 'f - l'o--: ouh1IF .... ta1nee._ r M· .. J; . f. - ·. ; �- ..,,- ,. {' ,,,.. .. _, , .. "' ' I l t I! 1 9 4 9 The MOUNTAINEER Volume 40 DECEMBER 15, 1949 Number 13 Organized 1906 Incorporated 1913 Editorial Board 1949 MAROLYN SMITH, Editor CAMERON BECKWJTH MARY T. HALEY Proof readers BETTY MANNING ELLEN MYER:; t VALLIE JOHN!;ON Advertising • MARILYN ADAMS JOHN PUTNAM Mailing MRS. IRVING GAVETT Subscription Price, $2.00 a Year Published and Copyrighted by THE MOUNTAINEERS, INC. j Published monthly, January to November, inclusi\·c. and semi-monthly during December by THE l\IOUNTALNEERS, INC., P. 0. Box 122. Seattle 11, Washington Clubroom.s at 521 Pike Str et Entered as Second Class Matter, April 1 , 1922 at Po. toffice at Seattle, \Vashington, under the Act of :\lach 3, 1879 ., I ; I· I Tarteo f Contents PAGE I Mt. Rainier from the West.. .............................. George R. Senner.... 4 The 43rd Summer Outing.................................. Ellen Walrh............ ................... 8 15 Years of Climbing Classes ............................ H arvey Manning.................. ..... 13 2400 Miles from Home...................................... ]ohn Ebert. ........................................ 17 The 1949 Climbers' Outing .............................. R. Safely ............................................ 18 Presenting The Prince and The Pauper. ........... Ellen Walrh ................................ ....... 20 We Had a Hobby Show at the Banqu<.>t.. ..........Elvera -
Paul Whelan Map 1
CANADA PHOTOGRAPHS of the HOH RAINFOREST WASHINGTON THREE SEASONS OF SELECTED IMAGES THROUGH THE EYES OF A PARK RANGER CARTOGRAPHY BY AND IMAGES FROM PAUL WHELAN One of the few remaining primeval forests, the Hoh Rain Forest offers a perspective on the cycle of life and death through the A FEW WORDS ABOUT THE PARK movement of nutrients from monolithic stands of old growth to wellsprings of nurse logs. Only with the falling of one of these The expanse of Olympic National Park encompasses a host of different landscape types and HOH RIVER TRAIL ELEVATION PROFILE enormous trees is enough sunlight available for new tree growth to occur, as this river valley has rarely seen a fire event. The majestic climatic regimes. Although the mountains are comparatively short when scaled against the Cascade Range, their position affords the peninsula a unique array of 4,300 ft Hoh River offers solace to its visitors and a glimpse at the pre-settlement condition of the unique and spectacular Olympic Peninsula. H O microclimates. On the west side of the park, temperate rainforests abound as the prevailing westerly winds (usually with a southerly 2,450 H L A K E T RA component) sweep moist air off the Pacific Ocean. These I L 600 precipitation rich clouds meet the west face of the 0 4.5 9 13.5 17.4 miles !\C Olympic Range and, via orographic lifting, dump !@ Olympus Guard Station !\B torrential rains on the Hoh, Queets and Quinault 50 Basins. Conversely, the east side of the park Miles O H R I L !@ H V A I exhibits starkly different characteristics. -
Norman Rice a Man of the City Husky Picks for Camping
THE UNIVERSITY OF WASHINGTON ALUMNI MAGAZINE JUNE 17 NORMAN RICE A MAN OF THE CITY HUSKY PICKS FOR CAMPING Husky Hats zhats.com Men’s Therma-FIT Hoodie nike.com How do you create a world of good? Start with the things you hold dear. Your ideas and ideals. Your Washington Frisbee hopes and dreams. With the University of Washington, you can connect your passion with philanthropy. ubookstore.com/thehuskyshop Link arms with the students, faculty and staff who unleash boundless possibilities every day. Men’s ½ Zip Performance Top fanatics.com Folding Chair and Fleece Blanket JOIN US. logobrands.com Tank 85 and Colster Can or Bottle Cooler yeti.com uw.edu/boundless Women’s HUSKIES Joggers and V-Neck Tee ubookstore.com/thehuskyshop Built for the Dawgs Dawg Snacks Sole of a True Fan Shades of Purple Celebrate with icy cold drinks and Peanuts are a no-brainer energy Scream your purple pride when You’ll look good and get good well-preserved food when you food for camping and cheering you lace up your Husky SKICKS. looks in your classic Husky shades. add Yeti’s signature cooler to your on the team. And Husky peanuts Made with quality canvas, With hand polished frames,100% camping and Husky tailgating gear. are the tastiest you’ll fi nd. Tuck breathable vent holes, and comfy UV protection, and spring loaded With specially engineered cold- a can or two of this addictive foam insoles, you can hike the hinges, they’re so comfortable that holding insulation, Yeti takes and high satiety snack in your woods or bleachers with ease! you may forget you have them on! ice retention into overtime. -
1912 the Mountaineers
The Mountaineer. Volume Five Nineteen Hundred Twelve h611, •• , ,, The Mountaineen Sea11le. Wa1hla1100 :J1'.)1'1zec1 bv G oog I e 2,-�a""" ...._� _..,..i..c.. tyJ Vi) Copyright 1912 The Mountaineers Din,tiZ<'d by Google CONTENTS Page Greeting ................... ................................John Muir .......................................... Greeting ..................................................... Enos Mills ........................................ The Higher Functions of a Mountain Club................................................... \ Wm. Frederic Bade.......................... 9 Little Tahoma ............ ............................. .Edmond S. Meany............................ 13 Mountaineer Outing of 1912 on north side of Mt. Rainier....................... Mary Paschall ................................... 14 Itinerary of Outing of 1912................... .Charles S. Gleason........................... 26 The Ascent of Mt. Rainier.................... £. M.Hack ........................................ 28 Grand Park .............................................. 1=dmond S. Meany............................ 36 A New Route up Mt. Rainier.............. 'Jara Keen ........................................ 37 Naches Pass .............................................. Edmond S. Meany....... ,.................... 40 Undescribed Glaciers of Mt. Rainier .. Fran,ois Matthes ............................. 42 Thermal Caves ....................................... J. B. Flett .......................................... 58 Change in Willis -
Development Team
Paper No: 4 Environmental Geology Module: 07 Glaciers Development Team Prof. R.K. Kohli Principal Investigator & Prof. V.K. Garg & Prof. Ashok Dhawan Co- Principal Investigator Central University of Punjab, Bathinda Prof. R. Baskar, Guru Jambheshwar University of Paper Coordinator Science and Technology, Hisar Dr Anita Singh, Central University of Jammu, Jammu Content Writer Dr. Somvir Bajar, Central University of Haryana, Content Reviewer Dr B W Pandey, Department of Geography, Delhi University, Delhi Anchor Institute Central University of Punjab 1 Environmental Geology Environmental Sciences Glaciers Description of Module Subject Name Environmental Sciences Paper Name Environmental Geology Module Glaciers Name/Title Module Id EVS/EG-IV/07 Pre-requisites 1. Understand glacier and differentiate the different types of glaciers 2. Describe glacier formation and glacier movement Objectives 3. Understand glacial budget and mass balance 4. To study different types of glacier landforms Keywords Glacier, Calving, Ablation, Accumulation 2 Environmental Geology Environmental Sciences Glaciers Module 07: Glaciers Objectives 5. Understand glacier and differentiate the different types of glaciers 6. Describe glacier formation and glacier movement 7. Understand glacial budget and mass balance 8. To study different types of glacier landforms 7.1 Glacier Glacier is a mass of surface ice on land and formed by accumulation of snow. Glaciers flow downhill under gravity due to its own weight. Glaciers are maintained by accumulation of now and melting of ice. The melted ice discharged into the lakes or the sea. Glaciers grow and shrink in response to the climate change. Meier (1974) provided a definition of a glacier: “A glacier may be defined as a large mass of perennial ice that originates on land by the recrystallization of snow or other forms of solid precipitation and that shows evidence of past or present flow.