Baratang Island | Limestone Cave| চুনাপাথরের গুহা | Mud volcano | কাদার আগ্নেয়গিরি|Andaman আন্দামান

Limestone Cave Baratang | চুনাপাথরের গুহা | Mud volcano | কাদা আগ্নেয়গিরি | North & Middle Andaman|
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Baratang Island is an island of the Andaman Islands. It belongs to the North and Middle Andaman administrative district, part of the Indian union territory of Andaman and Nicobar Islands.The island lies 150 km (93 mi) north of Port Blair.
Limestone Caves is one of the best as well as unique tourist attractions in the Andaman and Nicobar Islands. These naturally formed caves are a visual treat to nature enthusiasts. Formed at the bottom of the sea, limestone is a sedimentary rock. It takes millions of years when deposits of marine life, corals, shells, and skeletons go through a natural compression in order to form unique shapes within the cave. Holding the secret of a million years of the Andaman Islands, these caves are lined up with stalactites and stalagmites. When travelling to the Andamans, include these caves in your itinerary that are nestled deep within the mangroves and surrounded by the lush rainforest.
Limestone caves are highly impressive and one of a kind natural marvel on earth. The caves feature rare stalactites, stalagmites and rock formations. These are nature’s own architecture as they have been formed naturally in the Andaman Islands. A treat to your eyes, you can take a walk through dense mangrove forests to reach these caves. These have been formed over years of corrosion. Here, you will witness a marvelous texture that is sure to leave you awestruck. The limestone formations emerge from the ceiling as well as the floor. Looking at nature transforming, evolving, and creating beautiful structures would be a miraculous experience.
Mud volcanoes, also called ‘Mud Domes, are formed by the eruption of mud slurries, water, and gases. There are various geological processes involved in the formation of mud volcanoes. But unlike actual ingenious volcanoes, mud volcanoes don’t spit out lava when they erupt. Moreover, their eruption process is not magmatic. The sizes of mud volcanoes lie between one and two meters to 700 meters high and between one and two meters to 10 kilometers wide.
Mud volcanoes stay true to their names, producing mud when they erupt. And this mud is what generally goes into the formation of a hot water spring. When the mud and the water from the springs mix up, they form mud slurries that are thrust upwards through fissures due to the hidden pressure. Most mud volcanoes lie underground. But some of them have also been found on or near land.
The temperatures of mud volcanoes are also usually lower than that of real ingenious volcanoes. They remain steady for the most part, ranging from as little as 2 degrees Celsius, going up to nearly 100 degrees Celsius. All volcanoes release different types of gases, and mud volcanoes are no different. However, a significant portion of the gases released by the formation of mud volcanoes is Methane. At the same time, some part of it also consists of carbon dioxide and other types of gases.