What makes passages in caves?

The most common way that passages in caves are formed is through the process of dissolution. This occurs when water seeps into the ground and comes into contact with soluble rocks, such as limestone, dolomite, and gypsum. As the water moves through the rock, it dissolves the minerals and carries them away. Over time, this process can create large passages and chambers within the cave.

In addition to dissolution, passages in caves can also be formed by other processes, such as:

* Abrasion: This occurs when water carries sediment and debris through a cave, which can scour the walls and enlarge the passages.

* Collapse: This occurs when the roof of a cave collapses, creating a new passage.

* Fracturing: This occurs when the rock in a cave fractures, creating new pathways for water to flow.

The type of passage that is formed in a cave depends on a number of factors, including the type of rock, the amount of water, and the rate at which the water is flowing.

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