История развития рельефа бассейна р. Мутновской (Южная Камчатка)
Аннотация
Erosion of an ancient volcanic caldera (Pacific coast of Southern Kamchatka) resulted from climatic changes and the World Ocean level fluctuations. 10 terraces and topographic levels correspond to time intervals favourable for terrace formation, their absolute ages are as follows (thousand years): floodplain, Q24 - 4 to 4,5, 1st terrace, Q14- is to 7,5; II, Q3(1)3 - 25; III, Q33(2) - 35; IV, Q33(1) - 45; V, Q31(3) - 75-80; VI, Q31(2) - 105; VII, Q31(1) - 120-130; VIII level, Q22- 165-190; IX level, Q21 - 200-400.
Рецензия
Для цитирования:
Лукина Н.В. История развития рельефа бассейна р. Мутновской (Южная Камчатка). Геоморфология. 1980;(1):93-97.
For citation:
Lukina N.V. Evolution of the relief of the Mutnovskaya liver basin Southern Kamchatka). Geomorfologiya. 1980;(1):93-97.