Book contents
- The Global Cryosphere, Second Edition
- Reviews
- The Global Cryosphere
- Copyright page
- Contents
- Preface
- Acknowledgments
- 1 Introduction
- Part I The terrestrial cryosphere
- 2A Snowfall and snow cover
- 2B Avalanches
- 3 Glaciers and ice caps
- 4 Ice sheets
- 5 Frozen ground and permafrost
- 6 Freshwater ice
- Part II The marine cryosphere
- Part III The cryosphere past and future
- Part IV Applications
- References
- Index
- Plate Section (PDF Only)
2B - Avalanches
from Part I - The terrestrial cryosphere
Published online by Cambridge University Press: 15 April 2022
- The Global Cryosphere, Second Edition
- Reviews
- The Global Cryosphere
- Copyright page
- Contents
- Preface
- Acknowledgments
- 1 Introduction
- Part I The terrestrial cryosphere
- 2A Snowfall and snow cover
- 2B Avalanches
- 3 Glaciers and ice caps
- 4 Ice sheets
- 5 Frozen ground and permafrost
- 6 Freshwater ice
- Part II The marine cryosphere
- Part III The cryosphere past and future
- Part IV Applications
- References
- Index
- Plate Section (PDF Only)
Summary
The word avalanche is derived from the French “avaler” (to swallow). An avalanche involves the rapId flow of a mass of sow down a slope, triggered by either natural processes or human activity. Avalanches have long been feared in Alpine countries. On March 1, 1910, on the Great Northern Railway line thorough the Cascade Range at Stevens Pass, WA, northeast of Seattle, 96 passengers and crew were killed by a massive avalanche that struck a stationary train.
- Type
- Chapter
- Information
- The Global CryospherePast, Present, and Future, pp. 87 - 101Publisher: Cambridge University PressPrint publication year: 2022