how geography influence south Indian history?
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The Geography of South India comprises the diverse topological and
climatic patterns of South India. South India is a peninsula in the
shape of a vast inverted triangle, bounded on the west by the Arabian
Sea, on the east by the Bay of Bengal and on the north by the Vindhya
and Satpura ranges. The line created by the Narmada River and Mahanadi
river is the traditional boundary between northern and southern India.
Technically all Indian territories below the 20th Parallel.
The Satpura ranges define the northern spur of the Deccan plateau, one
of the main geographic features of South India. The Western Ghats, along
the western coast, mark another boundary of the plateau. The narrow
strip of verdant land between the Western Ghats and the Arabian Sea is
the Konkan region; the term encompasses the area south of the Narmada as
far as Goa.
The Western Ghats continue south, forming the Malnad (Canara) region
along the Karnataka coast, and terminate at the Nilgiri mountains, an
inward (easterly) extension of the Western Ghats. The Nilgiris run in a
crescent approximately along the borders of Tamil Nadu with northern
Kerala and Karnataka, encompassing the Palakkad and Wayanad hills, and
the Satyamangalam ranges, and extending on to the relatively low-lying
hills of the Eastern Ghats, on the western portion of the Tamil
Nadu–Andhra Pradesh border. The Tirupati and Anaimalai hills form part
of this range.
The Deccan plateau, covering the major portion of the states of
Maharashtra, Karnataka and Tamil Nadu, is the vast elevated region bound
by the C-shape defined by all these mountain ranges. No major
elevations border the plateau to the east, and it slopes gently from the
Western Ghats to the eastern coast.
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