The Northern Plains
The Northern Plains of India, extending over a vast area of approximately 7 lakh square kilometers, are a crucial physiographic division characterized by their fertile alluvial soil. These plains have been formed through the geological processes involving the deposition of sediments from the major river systems: the Indus, Ganga, and Brahmaputra, along with their numerous tributaries. Noteworthy for their agricultural proficiency, these plains sustain a dense population due to the combination of rich soil, favorable water supply, and climate conducive to farming.
The plains can be broadly divided into three sections, including the Punjab Plains (through the Indus system), the Ganga Plain, and the Brahmaputra Plain in the east. Additionally, the Northern Plains exhibit varied relief despite being generally flat. Significant features include the 'bhabhar' region, where rivers deposit pebbles, which transitions into the swampy 'terai' region. The plains are further categorized into zones like 'bhangar' (older alluvium) and 'khadar' (floodplains).
Overall, the Northern Plains play an essential role in India's agriculture and support large populations, demonstrating the significance of geological processes in shaping human settlement and activity.