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The National Fossil Wood Park, Tiruvakkarai is a notified National Geo-heritage Monument located in the Villupuram District in the Indian state of Tamil Nadu and is maintained by the Geological Survey of India. [1] The park was established in 1940 [2] and is located 1 km east of Thiruvakkarai [3] [4] village on the road between Tindivanam and ...
Petrified wood has also been discovered in Dholavira in Kutch, Gujarat, dating back to 187–176 million years. [24] Japan – there is a fossilized forest preserved at Sendai City Tomizawa Site Museum; Indonesia – petrified wood covers several areas in Banten and also in some part of Mount Halimun Salak National Park.
Amkhoi Fossil Park is a fossil park located near Illambazar in the Birbhum District of West Bengal, India. It contains fossilized wood 15 to 20 million years of age and is officially recognized by the State Forest Department of West Bengal. [1]
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Akal Wood Fossil Park is a National Geological Monument of India located in Jaisalmer district, Rajasthan. [2] It is also a Biodiversity Heritage Site.. It is 21 hectares in extent and is located in Akal village, 17–18 km southeast of Jaisalmer city, and 1 km off the NH-68 Jaisalmer-Barmer road, on a stretch of about 10 km 2 of bare hillside. [3]
National Fossil Wood Park, Sathanur [1] is a National Geo-heritage Monument of India [2] [3] [4] located at Sathanur in Perambalur district, Tamil Nadu.This park is located within Sathanur panchayat and has a fossilized tree trunk, which was discovered in 1940 by the geologist M. S. Krishnan of the Geological Survey of India, who hailed from Tanjore.
Visitors can see petrified wood scattered through the park’s southern end and clustered in five large petrified wood deposits referred to as forests: Rainbow Forest, Crystal Forest Jasper Forest ...
Tree remains that have undergone petrifaction, as seen in Petrified Forest National Park. In geology, petrifaction or petrification (from Ancient Greek πέτρα (pétra) 'rock, stone') is the process by which organic material becomes a fossil through the replacement of the original material and the filling of the original pore spaces with minerals.