You've partially answered your own question, so to amplify:
Rainwater acidified by absorbed atmospheric carbon dioxide sinks through the joints and other discontinuities in the limestone upland's mass, dissolving the calcium carbonate that is the rock's main constituent.
Eventually the tiny initial conduits start to join and capture others, and discrete passages develop. The water emerges at a rising, resurgence or spring.
Read more: What_is_the_force_that_carves_out_underground_caves_from_limestone
The vast majority of the world's caves are in limestone, which is soluble in weakly acidic ground-water.
So the conditions for cave and other karst-feature development is the presence of a soluble rock (limestone and its metamorphic form, marble; also gypsum) in upland areas having a suitablly stable combination of geological, hydrological and long-term climate characteristics over the tens or hundreds of thousands of years it takes for caves to develop.
Harrison's Cave was formed by rock
by the limestone in the cave formed by dissolution by the limestone in the cave formed by dissolution
fingals cave is a cave formed by the same geological processes as those at the giants causeway on the other side of the Irish sea. after a volcano erupted 60 million years ago, hexagonal basalt columns formed as the cave cooled. the cave which has been formed by the sea eroding it away is easy to access. it was discovered in 1772 by sir Joseph banks and a visit to the cave by the composer Felix Mendelssohn inspired him to write his 'Hebrides overture''. popularly known as ''fingal's cave''.+++Not quite: the columns formed as the rock cooled. The cave did not exist until long after the island formed, and was then, as you say, cut by erosion. The volcanism was associated with the inception of the Atlantic Ocean.
a cave
When rock above a cave collapses, a sinkhole is formed.
how was the titan cave was formed
Harrison's Cave was formed by rock
Ape cave was formed by a water erosion.
A sinkhole is formed when the roof of a cave collapses.
by the limestone in the cave formed by dissolution by the limestone in the cave formed by dissolution
it is a 'karst' cave, i.e. formed by the action of water on limestone.
stalagmites
Stalactites. You may also notice distinct erosion patterns in many cave ceilings, formed when the passage was filled with water at an earleir stage in the cave's development.
fingals cave is a cave formed by the same geological processes as those at the giants causeway on the other side of the Irish sea. after a volcano erupted 60 million years ago, hexagonal basalt columns formed as the cave cooled. the cave which has been formed by the sea eroding it away is easy to access. it was discovered in 1772 by sir Joseph banks and a visit to the cave by the composer Felix Mendelssohn inspired him to write his 'Hebrides overture''. popularly known as ''fingal's cave''.+++Not quite: the columns formed as the rock cooled. The cave did not exist until long after the island formed, and was then, as you say, cut by erosion. The volcanism was associated with the inception of the Atlantic Ocean.
a cave
A cave entrance is commonly referred to as a cave mouth or cave opening.
Calcite, usually, from the limestone above the cave. (Or gypsum, if the cave is in that rock)