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Title

EVIDENCES OF PLEISTOCENE GLACIAL GEOMORPHOLOGY IN THE NORTHERN SLOPE OF KHASHCHAL MOUNTAIN (WESTERN ALBORZ)

Pages

 Start Page 51 | End Page 67

Abstract

 Identification and study of geomorphological heritage an important role to represent the trend of last climate chamges in a region. In this research using, topograph, geology maps and field evidences of glacial geomorphology in KHASHCHAL MOUNTAIN northern slope is detected. Detecd evidence is Glacial erasionablation landform like, glacial cirques, glacial valley and Glacial deposits Include glacial moraine. Result show during PLEISTOCENE period, climate in northern slope of KHASHCHAL MOUNTAIN had lower temperature and probably with more precipitation in compare to recent climate. Erasion and morphogenes glacial processes have been active. While nowdays evidence showing because of high evelation and precipitation and temperature situation in region, subglacial morphogenes process (freezing and melting) dominate in the region.

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