By excavation.
It's not a cave but an underground stone quarry in, I think,the Portland rather than overlying PurbeckFormation, worked in the late 18C to early-19C. It is one of a whole series along the coast between St. Aldhelm's and Durlston Heads.
They should not be confused with the many sea-caves that also perforate these cliffs, and which are all natural.
Tilly Whim "Caves" (there are 2 adjacent galleries) were open to the public until the late 1970s or early '80s, when fears for their stability enforced closure.
The Tilly Whim Caves in Dorset, UK, were formed by the erosive action of the sea on the softer rock layers along the coastal cliffs. Over time, the pounding waves undercut the cliffs and created caves, which were later expanded by human hands for limestone extraction.
The opening is called the cave entrance or cave mouth. It is usually an "exit" formed by flowing water.
When rock above a cave collapses, a sinkhole is formed.
The main parts of a cave include the entrance, passage, chamber, and sometimes a sinkhole or dome. These parts can vary depending on the type of cave and how it was formed.
Ellison Cave was formed by the erosion of the rock by water over millions of years. The cave was created as groundwater seeped through the limestone bedrock, dissolving and creating intricate passageways underground. Over time, the cave continued to grow and develop into its current size and complexity.
They are late 18C stone quarries, last worked in 1812 - they are not natural caves despite the name.
The Tilly Whim Caves in Dorset, UK, were formed by the erosive action of the sea on the softer rock layers along the coastal cliffs. Over time, the pounding waves undercut the cliffs and created caves, which were later expanded by human hands for limestone extraction.
how was the titan cave was formed
It was established by political whim, not by a cartographer or geographer.
yes they are! ++ Note though that they are not "caves" but late 18Cunderground quarries, extracting the Portland Stone beds and closed in 1812.
Ape cave was formed by a water erosion.
It was established by political whim, not by a cartographer or geographer.
A sinkhole is formed when the roof of a cave collapses.
Since late 18C: they are not caves but stone mines last worked c.1810; and part of a series of such workings from St. Alhelm's Head to Durlston Head.
it is a 'karst' cave, i.e. formed by the action of water on limestone.
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.
The opening is called the cave entrance or cave mouth. It is usually an "exit" formed by flowing water.