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GlaciersThe Politics of Ice$
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Jorge Daniel Taillant

Print publication date: 2015

Print ISBN-13: 9780199367252

Published to Oxford Scholarship Online: November 2020

DOI: 10.1093/oso/9780199367252.001.0001

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PRINTED FROM OXFORD SCHOLARSHIP ONLINE (oxford.universitypressscholarship.com). (c) Copyright Oxford University Press, 2021. All Rights Reserved. An individual user may print out a PDF of a single chapter of a monograph in OSO for personal use. date: 27 July 2021

Invisible Glaciers

Invisible Glaciers

Chapter:
(p.88) 4 Invisible Glaciers
Source:
Glaciers
Author(s):

Jorge Daniel Taillant

Publisher:
Oxford University Press
DOI:10.1093/oso/9780199367252.003.0009

Up in the highest reaches of the Central Andes, along the Sierra Nevada in California, along the European Alps, in some of the most unlikely places, including countries like Turkey, Bulgaria, Kosovo, Romania, Montenegro, Armenia, Azerbaijan, Afghanistan, Iran, and China, and in some more likely ones such as Mongolia, Russia, Nepal, Norway, Sweden, Argentina, Chile, and Canada, lie entire swaths of frozen lands containing enormous quantities of invisible water in a solid state, hidden from sight until the surrounding ecosystems call on these lands to provide summer meltwater. As much as 25% of the surface of the Earth’s land experiences these frozen conditions, and more than 9 million people live in such environments. Even more live immediately below these lands, and yet most of us have never even heard of this frozen realm. The Incas and the Aztecs are known to have used this frozen terrain to store and conserve food. I am not talking about the more obviously glaciated regions with visible white cover on high mountaintops (which also act as water towers and basin regulators), but rather of that strip of land that lies somewhere below the lowest limit of the visible glaciers and somewhere above the timber line. No ice or snow may be immediately visible in this region, but, sure enough, the Earth is storing colossal amounts of ice, protected from the warm ambient temperature, for when the environment needs it most. We can think of this invisible frozen region as a buffer or hydrological ice zone that ecosystems call on for steady water all year round. It’s what glaciologists call the periglacial environment. The term itself is somewhat deceiving. Peri suggests “perimeter” or “surrounding,” so we might guess that the periglacial environment is the area surrounding the glacier, a sort of buffer zone around the visible ice where logically some sort of cryogenic activity (freezing activity) is occurring. Although such activity may indeed be occurring around the fringes of any given glacier, this is not the area known as the periglacial environment. Periglacial environments are much more complex than their name might suggest.

Keywords:   Incas, Invisible Glaciers (the Periglacial Environment), Periglacial Environment, Rock Glacier, Salta Province, Solifluction, creeping ground, frost heave, gelifluction, isotherms, mass wasting, thermokarsts

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