عنوان مقاله [English]
نویسنده [English]چکیده [English]
Talesh mountains because of being located near caspian sea is one of the humid areas of iran, this charactristic due to the climatic changes followed by predominance of glacial and interglacial periods during the quaternary has led to dominance of different erosion realms in different altitudes of these mountains. The most important legacg of these changes in the Neor trough include :lake terraces, lake sediments ,alluvial fan,and fault trough,which are affected by nivation process during the cold seasons and by are eroded by fluvial during warm seasons.
In this paper we will study the geomorphological evidence for identification and reconstruction of paleoclimate in Neor basin.