Caves form because ground water is slightly acidic and in flowing through joints, bedding-planes and faults within limestone or gypsum, dissolves the rock away. The only other rocks soluble in water are Chalk, Dolomite and Salt, but their formations do not normally support cave development - though there are a few caves known in chalk.
Over tens or hundreds of thousands of years, areas with limestone rocks can develop caves.
Caves are formed when carbonic acid in ground water dissolves limestone.
If the water level is lowered, then limestone dissolved from rocks above
the cave is deposited as stalactites and stalagmites.
what happened was:
1. the sea water around the poles used to be heated by the sun but the pole ice never melted.
2. This changed and instead the ice was being heated but the sea water was freezing up.
3. The whole Earth was covered in thick sheets of ice.
4. The ice melted and formed glaciers.
i watched it on a documentry. One comes on every week about the Earth.
The large, pointed objects inside of caves are not icicles. Instead, they are calcium carbonate deposits that have formed from dripping mineralized water. These deposits are called "stalagmites" and "stalactites". Did you know that stalacmites and stalactites sometimes bond together to form a single column? ~Apple Juice
ice caves form when the inside of a glacier melts and the whole gets bigger and bigger
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Limestone
It is called weathering.
It is called weathering.
Mineral deposits which develop upwards from a cave floor are known as stagmites. Deposits which form from the ceiling are stalactites.
caves
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The plural form is CAVES.
The word cave can be a noun and a verb. The noun form is a large cavity formed underground. The verb form means to surrender.
it probably going to be a physical change because when the stalagmites form in the cave its still going to be a cave and nothing really is going to change the cave.
Ellison's Cave is a cave located in Appalachian Plateaus of Northwest Georgia. A cave is formed when limestone is dissolved.
Cave painting
Cave drawings.
A shake-hole, sink-hole or doline. The collapse may also form an entrance to the cave below, if the slumped material has not filled the passage.
The sea attacks cracks in the cliff at an headland. The cracks grow larger and form a cave.
Hanging down from the cave roof are stalactites.
That's extremely variable and specific to each cave, but you have to think in tens or hundreds of thousands of years.