Vindhya Range

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(vĭn'dyə) pronunciation

A chain of hills in central India extending east-northeast for about 965 km (600 mi) and rising to approximately 915 m (3,000 ft).

Vindhya Range (vĭn'dyə), chain of hills, c.600 mi (970 km) long, rising to c.3,000 ft (910 m), Madhya Pradesh state, central India. The Vindhya Range has been the historic dividing line between N and S India, separating the Sanskrit-speaking Aryan invaders from the Dravidian peoples of the Deccan. The massive sandstone of the range, long an important building material, was used for the famous group of Buddhist stupas at Sanchi (built 3d cent. B.C.-11th cent. A.D.), the 11th-century Jain and Brahman temples at Khajuraho, and the 15th-century palaces of Gwalior.


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Vindhya Range (विन्‍ध्य)
Range
Vindhya Range
Country India
State Uttar Pradesh, Madhya Pradesh
River Kali Sindh, Parbati, Betwa, Ken, Son, Tamsa or Tons
Highest point Amarkantak
 - elevation 1,048 m (3,438 ft)
 - coordinates 22°40′N 81°45′E / 22.67°N 81.75°E / 22.67; 81.75
Topographic map of India showing the range

The Vindhya Range (Sanskrit: विन्‍ध्य) is a range of older rounded mountains and hills in the west-central Indian subcontinent, which geographically separates the Indian subcontinent into northern India (the Indo-Gangetic plain) and Southern India.

Contents

Introduction

The western end of the range is in the state of Gujarat at the eastern side of the Gujarat peninsula, near the border with the modern states of Rajasthan and Madhya Pradesh. Reaching the sub-continent proper, the range runs east and north nearly to the Ganges River at Mirzapur. The area to the north and west of the range are arid and inhospitable, located in the shadow of both the Vindhya and the higher Aravalli range to the south blocking the prevailing winds.

Origin of rivers

The southern slopes of the range are drained by the Narmada River, which proceeds westward to the Arabian Sea in the wide valley between the Vindhya Range and the parallel Satpura Range farther to the south. The northern slopes of the range are drained by tributaries of the Ganges, including the Kali Sindh, Parbati, Betwa, & Ken (both are tributary of the yamuna, ), Son & Tamsa or Tons both are tributary of the Ganges, drains the southern slopes of the range at its eastern end.

Palaeontology

The earliest known multicellular fossils of eukaryotes (filamentous algae) have been discovered from Vindhya basin dating back to 1.6 to 1.7 billion years ago.[1]

The Vindhyan tableland is a plateau that lies to the north of the central part of the range. The cities of Bhopal, the capital of Madhya Pradesh, and Indore lie on the tableland, which rises higher than the Indo-Gangetic plain to its north.

Legend

Hindu legends say that the Vindhya mountains once showed a tendency to grow so high as to obstruct the usual trajectory of the sun. This was accompanied by increasing vanity on the part of that mountain range, which demanded that Surya should circum-ambulate the Vindhyas in the same way as he does Mount Meru. The need arose to subdue, by guile, the Vindhyas, and Agastya was chosen to do that.

Agastya Muni journeyed from north to south, and on the way encountered the now impassible Vindhya mountains. He asked the mountain range to facilitate his passage across to the south. In reverence for Agastya, the Vindhya mountains bent low enough to enable the sage and his family to cross over and enter southern India. The Vindhya range also promised not to increase in height until Agastya Muni and his family returned to the north. Agastya Muni settled permanently in the south, near Nasik by the river Godavari in the beginning & later far south in Tamilnadu, and the Vindhya range, true to its word, never grew further.

References

  • Srivastava, P. and Bali R. 2006. Proterozoic carbonaceous remains from the Chorhat sandstone: oldest fossils of the Vindhyan supergroup. Geobios V. 39, pp. 873-878.
  1. ^ Bengtson, S.; Belivanova, V.; Rasmussen, B.; Whitehouse, M. (May 2009). "The controversial "Cambrian" fossils of the Vindhyan are real but more than a billion years older". Proceedings of the National Academy of Sciences of the United States of America 106 (19): 7729–7734. Bibcode 2009PNAS..106.7729B. doi:10.1073/pnas.0812460106. ISSN 0027-8424. . PMID 19416859. http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=2683128.  edit

Coordinates: 24°37′N 82°00′E / 24.617°N 82°E / 24.617; 82


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