Geological and geomorphological indications of former glaciations within the middle part of the Kolyma drainage basin

Abstract

Extensive glaciations developed within the middle Kolyma drainage Basin during the Early and Middle Pleistocene. The glaciers type and extension are extablished on the basis of glacial and periglacial deposits distribution, position of glacial troughs and eroded glacial cirques and privation-solifluction hollows. The former glaciers developed under conditions of low' mountain and hilly topography.