Animals as erosion agents in the alpine zone: Some data and observations from Canada, Lesotho, and Tibet

Citation
K. Hall et al., Animals as erosion agents in the alpine zone: Some data and observations from Canada, Lesotho, and Tibet, ARCT ANTARC, 31(4), 1999, pp. 436-446
Citations number
61
Categorie Soggetti
Multidisciplinary
Journal title
ARCTIC ANTARCTIC AND ALPINE RESEARCH
ISSN journal
15230430 → ACNP
Volume
31
Issue
4
Year of publication
1999
Pages
436 - 446
Database
ISI
SICI code
1523-0430(199911)31:4<436:AAEAIT>2.0.ZU;2-V
Abstract
Animals can exert a very strong impact on erosion and sediment transport in the alpine. Although the alpine is recognized for its abundance of animals , animal-soil erosion interactions have been poorly studied. Animals exert a direct influence through their burrowing and digging for food and also in directly by opening the ground to climatic and geomorphic influences, e.g. rain splash, needle ice, and wind erosion. It is this synergy that is impor tant for alpine erosion. Because the alpine zone is subject to freezing, fr ost action, and snow melt, exposed sediments and/or the availability of dra inage through burrows can have a marked effect on sediment transport and sl opes. On the steeper, less stable alpine slopes, the effects of loading can cause failure that produces arcuate slip scars, the exposed faces of which can also be exploited by geomorphic processes. In an attempt to study the effect of animals in the alpine zone, measurements of burrowing and digging based on quadrats (5 m x 5 m) along several transects were made in the alp ine zone of the Rocky Mountains of Canada. Results indicated an average of 0.0243 m(3) 25 m(-2) sediment displaced due to digging by rodents and a con servative estimation of sediment removal by rodents varying between 600 and 0.6408 m(3) km(-2) yr(-1). Grizzly bears exerted the greatest erosional im pact with as much as 0.4958 m(3) 25 m(-2) being measured. Observations (and limited measurements) relating to the impact of animals on the landscape w ere also obtained from Lesotho and Tibet. These preliminary findings are pr esented in an attempt to exemplify the various and interrelated effects of animals, climate and geomorphic process for the alpine. It is suggested tha t significantly more studies are urgently needed as the situation may be ex acerbated by climatic warming and/or by the expansion of pastoralism result ing from attempts at sustainable development in developing nations. The imp act of animals is an unquantified factor in many development studies, in ge omorphic studies in polar or high altitude environments, and in management plans for national parks or the exploitation of natural resources (e.g. thr ough logging).