Шерлопы - пещеры, колодцы и шахты в трещинах отсекания
Аннотация
Sherlopies are caves, wells and pits formed due to process of slope unloading. Morphologically they are vertical or steep cracks, clefts, horizontal crack-like caves growing in dolomite, limestone, gypsum-aleurolitic rocks, sandstone, aleurolite, trapps, shale. False floor, collapses, and intensive weathering of rocks in upper part of sherlopy are characteristics. By their microclimate sherlopies are divided into warm or cold, static or dynamic.
Рецензия
Для цитирования:
Филиппов А.Г. Шерлопы - пещеры, колодцы и шахты в трещинах отсекания. Геоморфология. 2000;(3):103-111.
For citation:
Philippov A.G. Sherlopies - caves, wells and pits in the unloaded slopes. Geomorfologiya. 2000;(3):103-111.
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