Некоторые результаты экспериментального исследования дефлюкции
Аннотация
An account is given of the techniques and results of measurements of the mass movement (defluction) rate on slopes in Armenia. The maximum rate has been recorded on the surface of the soil in subalpine and alpine belts-about 1.5 to 2 cm per year. Rate of stone field’s movement downslope is up to 4 to 5 cm per year.
Рецензия
Для цитирования:
Габриелян Г.К. Некоторые результаты экспериментального исследования дефлюкции. Геоморфология. 1988;(1):48-51.
For citation:
Gabrielyan G.K. Some results of experimental studies of the deduction process. Geomorfologiya. 1988;(1):48-51.
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