Understanding the boundaries, dimensions, and underlying basement rock structure of the Indo-Gangetic trough.
- Geosynclinal Depression: The Northern Plain is a structural depression formed as a fore-runner of the Himalayan mountain-building process, later filled by alluvium.
- Geographical Dimensions: The plains stretch approximately 3,200 km from the Indus delta in the west to the Brahmaputra valley in the east, with a width varying between 150 to 300 km.
- Alluvial Depth: Borehole data reveals that the depth of alluvium varies from 1,000 to 2,,000 meters, being deepest near the northern boundary close to the Siwaliks.
- Delhi Ridge: The Delhi Ridge acts as a water divide separating the Indus river system basin from the Ganga river system basin within the plains.
| Belt Name | Location/Width | Key Characteristics |
|---|---|---|
| Bhabhar | Narrow belt parallel to Siwaliks (8-16 km) | Pebble-studded zone; streams disappear underground |
| Terai | South of Bhabhar (15-30 km width) | Marshy, damp tract; re-emerged streams; rich biodiversity |
| Bhangar | Older alluvium upland | Contains calcareous nodules called 'Kankar'; flood-free |
| Khadar | Floodplains of newer alluvium | Enriched by fresh silt every year; highly fertile |