It depends on the cave. Since many caves are limestone (water carves it nicely), you usually find limestone. But granite is common in New Hampshire & Vermont.
hard basalt rock of deccan trap
Dacite does not have habitat because it is not a living thing; it is a kind of rock. Specifically, dacite is a volcanic rock, so it will be found on and near volcanoes, typically stratovolcanoes.
The world heritage site located in Gharapuri (Mumbai Harbour) is the Elephanta Caves. These ancient rock-cut caves date back to between the 5th and 8th centuries and are renowned for their intricate sculptures and carvings, particularly those dedicated to the Hindu god Shiva. The site includes a large sculpture of Trimurti, a depiction of a three-headed Shiva. Elephanta Caves was designated a UNESCO World Heritage Site in 1987.
Stalactites hang down from the ceilings of caves.
No every rock is able to change into anther
The Elephanta Caves are made out of basalt rock, which is a type of volcanic rock. Basalt is known for its strength and durability, making it an ideal material for creating caves and structures.
igneous rock
into the caves near castle rock
Mostly caves and rock shelters.
They lived in caves and rock shelters.
Mostly caves and rock shelters.
into the caves near castle rock
Caves wouldn't have much soil. It would mostly be a rock floor with fallen rocks, stones, pebbles from above.
The caves of Ajanta are located in India in the Aurangabad district of Maharashtra. The caves have monuments of Buddha which were carved beginning in the 2nd century BCE.
The Lascaux Caves (Apex)
The Ellora Caves are primarily made up of basalt rock, which is a dark-colored volcanic rock formed from lava flows. This type of rock is relatively soft when first cut but hardens over time, providing a durable material for the intricate carvings and structures found in the caves.
Stalactites in caves are typically formed from minerals such as calcite or aragonite, which are deposited by dripping water containing dissolved minerals. These minerals precipitate out of the water over time, creating the elongated formations we see in caves.