نوع مقاله : مقاله پژوهشی
نویسندگان
ندارد
چکیده
کلیدواژهها
عنوان مقاله [English]
نویسندگان [English]
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 are 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.
کلیدواژهها [English]
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