Curtains are formed when water containing calcium carbonate drips slowly through the joints and bedding planes of the limestone and comes out through a long crack in the ceiling of the cave . The water evaporates, leaving the calcium carbonate behind .
The Maquoketa caves in Iowa were formed through years of natural non-glacial erosion.
Caves are formed by rainwater dissolving away limestone or sandstone.
Ocean caves are formed from most commonly formed by calcium and magnesium, usually sedimentary rocks. They can also be made of granite.
Caves are formed in many ways but mostly by chemical weathering of the surface rock. Tectonic plates on the other hand are huge slabs of rock that form the Earth's crust. Caves are not formed by tectonic plates, think of caves as tiny boreholes in the very surface of a tectonic plate. I agree
Yes. Underwater caves do exist. Many formed when sea levels were lower than they are now and were flooded when sea levels rose.
Erosional caves are formed by the action of water or wind.
No. Most caves are formed out of limestone making that false.
The Maquoketa caves in Iowa were formed through years of natural non-glacial erosion.
Wookies live in trees, not caves.
The Maquoketa caves in Iowa were formed through years of natural non-glacial erosion.
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Limestone caves are formed through a process called chemical weathering. Rainwater, which is slightly acidic, dissolves the limestone rock over time, creating small cracks. These cracks then widen as more water flows through, eventually forming caves. Additionally, some limestone caves are formed through the erosion of underground rivers.
Erosional caves are formed by the action of water or wind.
They - or it? - are normal karst caves, formed in limestone by its dissolution by water. I believe they still carry a stream: if so they are still forming.
Other way round! Water and/or air are in caves.:-) Most of the world's caves have formed / are forming in limestone.
Karst caves, and it is the majority of caves; formed by acidic ground-water dissolving the limestone.
Cave draperies, also known as cave curtains or soda straws, are thin, hollow formations of minerals that hang like curtains from the ceiling of caves. They are typically composed of materials such as calcite or gypsum deposited by dripping water over thousands of years. These delicate formations are often found in limestone caves and can vary in size and shape.