Закономерности распределения тебелеров Чуйской степи Горного Алтая
Аннотация
«Tebelers» are hummocks due to frost heaving: they are formed by freezing of water-saturated horizons within the lose mantle. They are closely associated in the region with ice-cored pingoes and may be attributed to pressure of ground water of artesian type, probably with additional feeding by fissure water.
Рецензия
Для цитирования:
Лузгин Б.Н. Закономерности распределения тебелеров Чуйской степи Горного Алтая. Геоморфология. 1991;(4):86-90.
For citation:
Luzgin B.N. Spatial pattern of tebelers in the Chuyskaya Steppe, Gorny Altai Mountains. Geomorfologiya. 1991;(4):86-90.
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