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 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 Coastal Karnataka.
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.
Geological development
India is entirely contained on the Indian Plate, a major tectonic plate that was formed when it split off from the left over land of the ancient continent Gondwanaland. About 91 million years ago, during the late CretaceousPeriod, the Indian Plate began moving north at about 15 cm/yr (6 in/yr).[1]
The vast volcanic basalt beds of the Deccan were laid down in the massive Deccan Traps eruption, which occurred towards the end of the Cretaceous period, between 67 and 66 million years ago. Some paleontologists speculate that this eruption may have accelerated the extinction of the non-avian dinosaurs. Layer after layer was formed by the volcanic activity that lasted many thousands of years, and when the volcanoes became extinct, they left a region of highlands with typically vast stretches of flat areas on top like a table. Hence it is also known as Table Top. The volcanic hotspot that produced the Deccan traps is hypothesized to lie under the present day island of Réunion in the Indian Ocean.
Climate
The region has a tropical climate with the monsoons playing the major part. The southwest monsoon accounts for most of the rainfall in the region and much of it occurs from about June to September. Tamil Nadu and southeast Andhra Pradesh receive rains from the northeast monsoon from about October to January. Much of Andhra Pradesh and Karnataka has a distinct dry season from November until May when there is not much rainfall. This region also experiences cooler nights from October to March while the days are pleasantly warm. In the northern parts of the region temperatures can fall below 10 °C or 50 °F on occasions at night. Days are very hot from March to June when temperatures can surpass 40 °C or 104 °F.
The northern portion of the Western Ghats and Deccan plateau are in the states of Goa and Maharashtra, although these states are often classed in Western India. The official and majority languages in Goa and Maharashtra are Indo-European languages.
The low-lying coral islands of Lakshadweep are off the south-western coast of India. Sri Lanka lies off the south-eastern coast, separated from India by the Palk Strait and the chain of low sandbars and islands known as Rama's Bridge. The Andaman and Nicobar islands lie far off the eastern coast of India, near the Tenasserim coast of Burma. The southernmost tip of mainland India is at Kanyakumari (Cape Comorin) on the Indian Ocean.
Water bodies
Rivers of South India are dependent on the monsoons and shrink during the dry season. The line created by the Narmada River and Mahanadi River is the traditional boundary between northern and southern India. The Narmada flows westwards in the depression between the Vindhya and Satpura ranges. The plateau is watered by the east flowing Godavari and Krishna rivers. The other major rivers of the Deccan plateau are the Pennar and the Tungabhadra, a major tributary of the Krishna.
The river Kaveri rises in the Western Ghats, in the Kodagu district of Karnataka and flows through the fertile Mandya, Mysore, Hassan regions before entering Tamil Nadu, where it forms an extensive and fertile delta on the east coast. The three major river deltas of South India, the Kaveri, the Godavari and the Krishna, are located along the Bay of Bengal. These areas constitute the rice bowls of South India. Rivers that flow westward, from the mountains to the Arabian Sea, include the Periyar River, Netravati River, Mandovi and Tapti River (or Tapi) rivers, and the Narmada at the northern edge of the region.
Kuttanad, also known as The Rice Bowl of Kerala, has the lowest altitude in India, and is also one of the few places in world where cultivation takes place below sea level.[4][5] The country's longest lake Vembanad, dominates the backwaters; it lies between Alappuzha and Kochi and is about 200 km2 (77 sq mi) in area.[6] Around eight percent of India's waterways are found in Kerala.[7] Kerala's 44 rivers include the Periyar; 244 kilometres (152 mi), Bharathapuzha; 209 kilometres (130 mi), Pamba; 176 kilometres (109 mi), Chaliyar; 169 kilometres (105 mi), Kadalundipuzha; 130 kilometres (81 mi), Chalakudipuzha; 130 kilometres (81 mi), Valapattanam; 129 kilometres (80 mi) and the Achankovil River; 128 kilometres (80 mi). The average length of the rivers is 64 kilometres (40 mi). Many of the rivers are small and entirely fed by monsoon rain.[8]
^Inland Waterways Authority of India (IWAI—Ministry of Shipping) (2005). "Introduction to Inland Water Transport". IWAI (Ministry of Shipping). Archived from the original on 4 February 2005. Retrieved 19 January 2006.