Storeyed valleys - a paleogeographic paradox of mountain glaciation

Abstract

The notion of "storeyed valleys" was introduced by S.V. Gbruchev. They are formed in mountains on the valley slopes as a result of meltwater flows erosion and are usually represented by narrow gorges and canyons. They are considered to be specific forms due to longitudinal slope erosion, associated with valley glaciers. The problem is discussed using materials obtained from the fonder glaciation of the Khangai Mountains studies.