Varkala is the only place in Kerala where cliffs are found adjacent to the Arabian Sea.These Cenozoic sedimentary formation cliffs are a unique geological feature on the otherwise flat Kerala coast, and are known among geologists as Varkala Formation. The cliffs have been declared a national geological monument by the Geological Survey of India for their protection, maintenance, promotion, and the enhancement of geotourism. There are numerous water spouts and spas on the sides of these cliffs. In 2015, the Ministry of Mines, the Government of India, and the Geological Survey of India (GSI) declared Varkala Cliffs a geo-heritage site.Varkala is under Varkala police jurisdiction.
Another major landmark in Varkala is the Sivagiri Mutt, established by the social reformer Sree Narayana Guru.
Varkala is the only place in Kerala where cliffs are found adjacent to the Arabian Sea.These Cenozoic sedimentary formation cliffs are a unique geological feature on the otherwise flat Kerala coast, and are known among geologists as Varkala Formation. The cliffs have been declared a national geological monument by the Geological Survey of India for their protection, maintenance, promotion, and the enhancement of geotourism. There are numerous water spouts and spas on the sides of these cliffs. In 2015, the Ministry of Mines, the Government of India, and the Geological Survey of India (GSI) declared Varkala Cliffs a geo-heritage site. Varkala is under Varkala police jurisdiction.
Varkala is also known for the 2,018-year-old Janardana Swami Temple, which is an important Vaishnavaite shrine in India and is often referred to as Dakshin Kashi (Benares of the South). The temple is located close to Papanasam beach, which is an Ayurveda treatment centre. The temple has an ancient bell removed from a shipwreck, donated by the captain of the Dutch vessel which sank near Varkala without causing any casualties.
Another major landmark in Varkala is the Sivagiri Mutt, established by the social reformer Sree Narayana Guru.
Varkala is an important place as far as geology is concerned as it exposes sedimentary rocks belonging to the Cenozoic age, popularly known in the geological literature as the Warkalli formation. The Warkalli formation, along with the Quilon formation, represent sediments laid down in the Kerala basin that existed during Mio-pliocene times. The Quilon formation of the Miocene age is made up of limestone, and the Warkalli formation is made up of alternating beds of sand and shale exposed along the Varkala cliffs. Thin seams of lignite in the shale of the Warkalli formation suggest good vegetation at the time of deposition of the clay sediments.
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