In the valley of Kashmir, the lake deposits comprise thick deposits of glacial clay and other materials embedded with maintaining, These deposits occur in the valleys within the Himalayan mountain where there was once glacial action and deposition of Morain.

The plain formed between two rivers is known as Doab. It separates two rivers but maintains its uniform character over the whole area. In Punjab, Doabs maintain the physical characteristics of the Punjab plain.

Best Jalandhar Doab
Bari Doab
Chaz Doab
Sind Sagar Doab

The south of Terai is a belt consisting of old and new alluvial deposits known as Bhangar. These areas stand above the level of floodwater and the flood plains. This land is made up of clay pebbles and gravel. In Gangetic plains, these alluvial lands have been formed by the deposition of sandbars by

The northern mountains are young, weak, and flexible and have suffered from folding and deformation. The peninsula contains mostly residual mountains. Here, the river valley is shallow having low gradients. On the other hand, the Himalayas mountains are tectonic and rivers are torrential. The format

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Glacial deposits consists of clay, silt, sand and rocks of various sizes. Such materials deposited directly by the glacier are known as tills. till is deposited as glacial ice melts and drops its load of rock mountains.

Piedmont glaciers occupy broad low lands at the base of steep mountains and form where one or more valley glaciers emerge from the confining walls of mountain valleys.

A drumlin is an oval shaped hill that usually consists of rock debris. Most drumlins occur in clusters called drumlin fields.