description Western Ghats Escarpment Overview
The Western Ghats Escarpment is a prominent geological fault line and mountain range running parallel to the western coast of India. Recognized as a UNESCO World Heritage site, the escarpment was formed by volcanic activity during the breakup of the supercontinent Gondwana. It acts as a crucial geographical barrier that traps monsoon winds, creating a climate responsible for one of the world's most significant biodiversity hotspots. The area is heavily studied by ecological and geological researchers.
help Western Ghats Escarpment FAQ
Is the entire Western Ghats Escarpment a UNESCO World Heritage Site?
UNESCO's Western Ghats property consists of a series of protected components rather than every kilometre of the mountain chain. It was inscribed on the World Heritage List in 2012 for its biodiversity and evolutionary importance.
Why is the western side of the Western Ghats so steep?
The range forms a major escarpment along the western edge of the Deccan Plateau. Its steep western face rises relatively close to India's Arabian Sea coast, while the land generally slopes more gradually eastward.
How do the Western Ghats affect India's monsoon?
Moist air from the Arabian Sea rises against the escarpment and releases heavy rain on its western slopes. Areas east of the crest receive less moisture and can lie in a pronounced rain shadow.
Which animals are strongly associated with Western Ghats biodiversity?
The region supports endemic and threatened species including the lion-tailed macaque, Nilgiri tahr, and purple frog. Its isolated forests and varied elevations have produced exceptionally high levels of plant, amphibian, and reptile endemism.
explore Explore More
Similar to Western Ghats Escarpment
See all arrow_forward
Reviews & Comments
Write a Review
Be the first to review
Share your thoughts with the community and help others make better decisions.
