encounters in avalanche country: a history of survival in the mountain west, 1820-1920

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    With support rom the Center or the Study o the Pacific Northwest at the University o Wash-

    ington, the Sick Series in Western History and Biography eatures scholarly books on the peoples

    and issues that have defined and shaped the American West. Trough intellectual ly challenging

    and engaging books o general interest, the series seeks to deepen and expand our understand-

    ing o the American West as a region and its role in the making o the United States and the

    modern world.

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    Te Great Columbia Plain: A Historical

    Geography, , by Donald W. Meinig

    Mills and Markets: A History of the

    Pacific Coast Lumber Industry to ,

    by Tomas R. Cox

    Radical Heritage: Labor, Socialism, and

    Reform in Washington and British Columbia,

    , by Carlos A. Schwantes

    Te Battle for Butte: Mining and Politics

    on the Northern Frontier, ,

    by Michael P. Malone

    Te Forging of a Black Community: Seattles

    Central District f rom through the Civil

    Rights Era, by Quintard aylor

    Warren G. Magnuson and the Shaping of

    wentieth-Century America, by Shelby Scates

    Te Atomic West, edited by Bruce Hevly and

    John M. Findlay

    Power and Place in the North American West,

    edited by Richard White and John M. Findlay

    Henry M. Jackson: A Life in Politics,

    by Robert G. Kauman

    Parallel Destinies: Canadian-American

    Relations West of the Rockies, edited by

    John M. Findlay and Ken S. Coates

    Nikkei in the Pacific Northwest: Japanese

    Americans and Japanese Canadians in the

    wentieth Century, edited by Louis Fiset and

    Gail M. Nomura

    Bringing Indians to the Book,

    by Albert Furtwangler

    Death of Celilo Falls,by Katrine Barber

    Te Power of Promises: Perspectives on Indian

    reaties of the Pacific Northwest,edited by

    Alexandra Harmon

    Warship under Sail: Te USS Decaturin the

    Pacific West,by Lorraine McConaghy

    Shadow ribe: Te Making of Columbia River

    Indian Identity,by Andrew H. Fisher

    A Home for Every Child: Relinquishment,

    Adoption, and the Washington Childrens HomeSociety, ,by Patricia Susan Hart

    Atomic Frontier Days: Hanford and the

    American West, by John M. Findlay and

    Bruce Hevly

    Te Nature of Borders: Salmon,

    Boundaries, and Bandits on the Salish Sea,

    by Lissa K. Wadewitz

    Encounters in Avalanche Country: A History

    of Survival in the Mountain West, ,

    by Diana L. Di Steano

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    .

    ENCOUNTERS inAVALANCHE COUNTRY

    A History of Survival in the Mountain West, 18201920

    in association with

    Seattle and London

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    2013 by the University o Washington Press

    Printed and bound in the United States o America

    17 16 15 14 13 5 4 3 2 1

    All rights reserved. No part o this publication may be reproduced or transmitted in

    any orm or by any means, electronic or mechanical, including photocopy, recording,

    or any inormation storage or retrieval system, without permission in writing romthe publisher.

    353587, , 98195,

    50096, , 98145,

    www.washington.edu/uwpress

    Library o Congress Cataloging-in-Publication Data

    Di Steano, Diana L.

    Encounters in avalanche country : a history o survival in the Mountain West,

    18201920 / Diana L. Di Steano.

    pages cm. (Emil and Kathleen Sick series in Western history and biography)

    Includes bibliographical reerences and index.

    978-0-295-99314-0 (hardback)

    1. Frontier and pioneer lieWest (U.S.) 2. Frontier and pioneer lieRocky

    Mountains. 3. Mountain lieWest (U.S.). 4. Mountain lieRocky Mountains.

    5. AvalanchesWest (U.S.)History. 6. AvalanchesSocial aspectsWest

    (U.S.)History. 7. AvalanchesRocky MountainsHistory. 8. Avalanches

    Social aspectsRocky MountainsHistory. 9. Human ecologyWest (U.S.)

    History. 10. Human ecologyRocky Mountains RegionHistory. I. itle.

    596.5 2013

    978'.02dc23 2013027325

    Te paper used in this publication is acid-ree and meets the minimum requirementso American National Standard or Inormation SciencesPermanence o Paper or

    Printed Library Materials, 39.48 1984.

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    To my family and the memory of my mother,

    Joan Elisabeth DiStefano

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    CONTENTS

    Acknowledgments ix

    Map o Avalanche Country Study Areas xi

    Introduction: Arrival in Avalanche Country 3

    1 Survival Strategies: 18201860 9

    2 Mountain Miners, Skiing Mailmen, and

    Itinerant Preachers: 18501895 23

    3 Industrial Mining and Risk 38

    4 Railway Workers and Mountain owns: 18701910 53

    5 Whos to Blame? 75

    6 Disaster in the Cascades 89

    7 opping v. Great NorthernRailway Company 104

    8 Departure rom Avalanche Country 119

    Notes 125

    Bibliography 151

    Index 167

    Illustrations follow page

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    ACKNOWLEDGMENTS

    I

    -

    tors, colleagues, and employers. Donna Krasnows and Bob Walchs teach-

    ing skills gave me the oundation to pursue both history and writing. AnneHyde, Betsy Jameson, and Carol Neel remain valued mentors and riends.

    At the University o Montana, Dan Flores and Dave Emmons inspired my

    intellectual growth. Dan has continued to be an indispensable critic and

    supporter o my work. At the University o Colorado in Boulder, I learned

    about the craf o history rom Virginia Anderson, Bob Ferry, Julie Greene,

    Nan Goodman, Ralph Mann, Mark Pittenger, and Carolyn Ramsey. I owe a

    special debt to Peter Boag, my dissertation adviser. I will always be grateul

    or his insistence on solid evidence, organized writing, and analytical rigor.My amazing cohorts at Colorado, John Enyeart, John Grider, Beth Kovacs,

    Eric Morgan, Wendy Rex-Atzet, Duke Richey, and Allison Wickens, all

    offered insightul input. My colleagues at Pacific Lutheran University, Buck-

    nell University, and University o AlaskaFairbanks offered impromptu

    advice and support. I am grateul or the curiosity and good humor o my

    students at those institutions as well. Parts o the book appeared inJournal

    of Social History and Environmental History,and I thank those publications

    or their permission to rework the material here. Appreciation, too, goes

    to my graduate assistant Matt Robinson and map maker Kerri Crowder. I

    also owe thanks to Laura Avedisian, Lincoln Bramwell, Doug Smith, and

    Leon Unruh; my anonymous reviewers; and my readers at the University o

    Washington Press or their patience looking through my manuscript.

    Tis book was possible due to unding rom the University o Colorado,

    the Charles Redd Center or Western History, and Bucknell University.

    Due to the generosity o these institutions, I was able to pursue research atDenver Public Library, Glenbow Archives, Parks Canada Archives in Rev-

    elstoke, Revelstoke Museum and Archives, Revelstoke Railway Museum,

    Stephen H. Hart Library at the Colorado Historical Society, University o

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    Utah Archives, and Utah Historical Society, Washington State University

    Archives and Special Collections, the Washington State Archives, and the

    Wenatchee Valley Museum and Archives. Gary Krist generously shared

    his sources related to the Wellington slide with me.

    Tis book would not have happened without the emotional, intellec-

    tual, and financial support o my riends and amily. I am privileged to

    have too many riends to list them all by name, but their aith in my work

    has been invaluable. My ather Lews love o the West, a passion he passed

    on to me, inspired this book. My sister Anne Maries excellent editing and

    listening skills motivated me through the difficult times. My loyal canine

    companions, Skaia and Emma, reminded me that walks are important,

    too. Finally, the memory o my mothers resilient spirit has sustained me.

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    Western United States and Canada with study areas in Avalanche Countryshown.

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    ENCOUNTERS IN

    AVALANCHE COUNTR Y

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    3

    INTRODUCTION:

    ARRIVAL IN AVALA NCHE COUNTRY

    D. -tains undamentally strange. A sel-described tenderoot, Gardiner

    arrived in Crested Butte, Colorado, in the 1880s. As he walked toward

    his hotel, the towering mountains, deep snow, thin air, and residents ski-

    ing about made an immediate impression. Ten he heard a distant rum-

    ble that sounded like thunder in the mountains; it grew heavier, the walk

    under . . . [his] . . . eet shook, and then, with a last roar, the sound stopped.

    He remembered, No one on the walk seemed to notice it so I asked a pass-

    ing miner what had happened. Te miner replied, Why, man alive . . .dont you know snowslides when you hear them? Tis first encounter

    with the growl o the mountain giant that strikes terror to those . . . in its

    path reinorced or Gardiner the act that he had come to a place quite

    different rom the home he had lef in New York.

    Over the years Gardiner spent in the Elkhorn Range, he would become

    better acquainted with avalanches, or snowslidesas the miners called

    themand make many adjustments to practice medicine in his new home.

    He would learn to ski, which was the only way to reach patients in the

    wintertime, and to treat maladies like snow blindnesstemporary loss o

    sight caused by the suns reflection off the snow. And like others beore and

    afer him, he would discover that the process o community building in a

    mountainous environment demanded he cope with extremes o climate

    and topography. Gardiner had arrived in what is known today as Ava-

    lanche Country, places where steep slopes and snow converge with deadly

    potential.Te conditions that lead to avalanches begin with snowflake struc-

    ture. Snowflakes orm many shapesthe more complex the shape, the

    more tightly the ice crystals bond together on the ground. emperature,

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    moisture content, wind speed, and melting and rereezing rate also affect

    bonding. Snow alls; layers build. Avalanches occur most ofen on slopes

    between 30 to 60 degrees, when the weight o new snow breaks the bonds

    between the underlying layers.

    wo o the most common types o avalanches are loose snow and slab

    avalanches. A loose snow avalanche begins at a single point at the top o a

    ridge and as it streaks downhill it destabilizes the surace snow in its path,

    which then becomes part o the slide. Tis kind o slide ofen ollows creek

    beds or gullies and tends to recur, ollowing the same path year afer year.

    Slab avalanches begin when a crack, perpendicular to the all line, orms

    between snow layers. Te mass o unstable snow breaks off along the crack

    and moves downhill; slab avalanches can comprise huge amounts o snow,move up to 200 miles per hour, and are less predictable than loose snow

    slides.

    Several actors make regions within the Mountain West particularly

    prone to avalanche activity. In southwestern Colorado, or example, the

    San Juan Mountains are extraordinarily steep and receive a air amount

    o sun in the wintertime. Tis creates particularly hazardous snow condi-

    tions, because the sun melts both surace and subsurace layers o snow,

    which then rereeze at night. Tis cycle produces unstable snow layerswith poor cohesion. As a result, the snow cover o the San Juan region

    has an extremely unstable stratigraphy, which means that the layers are

    more likely to slip off one another on steep slopes, creating an avalanche.

    Te Cascades in Washington also experience requent slides. Tey are

    also steep, but receive massive amounts o wet, heavy snowaveraging

    nearly thirty-eight eet during the winter. Changes in the rate o snowall,

    temperature fluctuations that mean it can rain and snow during the same

    storm, alterations in wind speed, and variations in the density o the snow-

    pack contribute to conditions that increase the likelihood o slides.

    Tose with avalanche experience argue that where slides have allen

    once, they are likely to occur again. Tis belie influences modern ava-

    lanche-control methods on highways and at ski resorts where artillery and

    dynamite are used to stimulate slides beore catastrophic amounts o snow

    have accumulated. Over time, avalanche science has become a respected

    field o study; manuals advise backcountry users how to avoid risk; andtechnological advances like avalanche radio beacons, a device worn by ski-

    ers that emits a tracking signal, improve chances o survival or victims

    buried in slides. Nevertheless, deadly disasters occur every year. Te num-

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    ber o deaths in avalanches has hovered around twenty to thirty a year in

    North America in recent decades. Most who died were recreationists: snow

    machine riders and backcountry skiers.

    In the nineteenth century, well beore mountains became risky places to

    play, Americans saw them as obstacles to western expansion. Exploration

    o the Mountain West by European Americans yielded strong reactions

    that would seem to prohibit settlement. Afer traveling through southwest-

    ern Colorados San Juan Mountains, which included hundreds o peaks

    that tower more than 13,000 eet, John C. Frmont declared the range one

    o the highest, most rugged, and impracticable o all the Rocky Mountain

    ranges, inaccessible to trappers and hunters even in summer.Guidebook

    writer Lansord W. Hastings wrote in 1845 that the Rocky Mountain rangeis usually covered with perpetual snow. Te greatest elevations in all

    Oregon [erritory], are ound in this range, many o which are more than

    25,000 eet above the level o the sea. . . . From the oregoing remarks, and

    rom the well-known act, o the entire sterility o all this range, it will be

    readily seen, that it is no wise, adapted to the support o man or beast.

    Hastings was similarly impressed by the Cascade Range in Washington.

    He estimated they stretched rom twelve to eighteen thousand eet into

    the sky.Te twelve volcanic peaks were ormidable, and wherever youare [in the region], you behold these ancient pyramids o eternal ice and

    snow, . . . amid the howling tempest, the flashing lightnings, and the roar-

    ing thunders above.Perhaps Hastings portrayed the mountains in this

    awe-inspiring way to encourage settlers to hasten toward the coast, but his

    descriptions o eternal snow and extraordinary altitude and sterility

    sent a striking message about the hostility o the western mountains.

    Now we know that Hastings was somewhat off the mark; the highest

    peak in the Rocky Mountains, Mount Elbert, stands 14,433 eet. More than

    fify other peaks in Colorado surpass 14,000 eet but reach nowhere near

    the heights he estimated. Te highest mountain in the Cascades is Mount

    Rainier at 14,410 eet, and the highest mountain in the contiguous United

    States, Mount Whitney at 14,505 eet, is in the Sierra Nevada. In spite o

    Hastingss inaccurate estimations, these three towering mountain ranges,

    young in geological terms, lef a mark on the trappers, emigrants, and

    prospectors who traversed them, particularly during the winter season,which could last as long as nine months.

    By the second hal o the nineteenth century the mountains raw mate-

    rialsgold, silver, copper, coal, and timberunded and ueled eastern

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    development.Te mountain ranges had become more than areas to map

    or cross; they became places to build communities. Te search or gold

    and silver, especially, drove people higher into the mountains, and some o

    the most productive mines in the region, such as Leadville, Colorado, sat

    above 10,000 eet.

    Prospecting and placer mining came first, but the real riches lay under-

    ground and demanded capital investment to extract. Rail lines and spur

    routes brought in the equipment or underground mining and provided a

    way to export the ore. Te process o developing corporate mines, which

    depended on the railways, happened at different rates o speed and at di-

    erent times, but by the end o the nineteenth century many sites in the

    West had made the transition to company-run mines that employed doz-ens or even hundreds o workers. In the span o a ew decades, more and

    more people moved into the West; railroads crisscrossed the landscape;

    and industrial mining, logging, arming, and cattle ranching character-

    ized the economy.

    By 1880, the West had become the most urbanized region in the United

    States.Te buffaloa symbol o the American West and the native way

    o liewere almost gone, hunted to near extinction and their bones lef

    to bleach in the sun by market hunters. Livestock owners and bountyhunters had wiped out large numbers o grizzly, black bear, cougar, and

    wol populations, predators that were deemed a threat to cattle and sheep.

    Hydraulic and stream-dredge mining had irreparably altered thousands

    o miles o water systems. Salmon were declining as the canning industry

    processed huge amounts o fish along the Pacific Coast. Overgrazing by

    cattle destroyed thousands o acres o grasslands. Even the once seemingly

    endless orests o the West were shrinking and overcut.

    Americans seemed to have mastered nature in the West, and the min-

    ers and railway workers who made up the industrial workorce poten-

    tially fit Karl Marxs theories on how industrial lie alienated people rom

    their natural world, a process that began when Europeans and Americans

    moved rom an agricultural society to an industrial, urban way o lie. Yet

    a closer look at the lives o Mountain West workers tells a different story.

    Snowslides occurred in all the major ranges o the Mountain West, and the

    population growth that came with the prolieration o industrial jobs putmore people in contact with environmental hazards. Far rom controlling

    nature, people aced continuous threats.Indeed, those in the extractive

    and transportation industries ought constantly against environmental

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    challenges. Blizzards loaded the peaks with snow. Steep mountainsides

    and deep gullies meant that in winter miners and others working on the

    slopes o the mountains are obliged to be continually on the lookout or

    avalanches.

    Tus, workers living in the regions were not alienated rom their sur-

    roundings but rather were orced to build an understanding o the moun-

    tains based on the environmental realities o their work situations. Over

    time, Mountain West workers accumulated a store o knowledge about

    their work and their natural environment that influenced the decisions

    they made as they went about the business o living in Avalanche Coun-

    try. Tat knowledge would ultimately influence the workplace and rescue

    efforts within their communities and would lead to challenges to liabilitylaw that saw avalanches as acts o God.

    Te mountains that acted as the physical boundaries o Avalanche

    Country and the snow that covered its peaks and valleys became actors in

    the theater o western industrialization. Te very substance o the moun-

    tainsthe animal pelts and the gold and silver ound in the streams, soil,

    and rocksdrew European Americans to the area and then propelled the

    economic and social transitions that took place there. Te height, slope,

    cold, ice, and snow o the mountains would shape the experiences o Ava-lanche Country inhabitantsrom the trappers who came in the 1820s to

    the sojourners, miners, and railway workers who ollowed into the West.