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Stalagmites are formed by water (or another liquid) dripping of the ceiling of a cave. When the liquid drips, it picks up minerals. After it reaches the floor, the water eventually evaporates and the mineral in the liquid is left behind. Over millions of years, those little minerals build up, become solid, and form the rocks that you see in caves today.

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What landform is the jenolan caves?

The Jenolan Caves in Australia are an example of karst landforms, formed by the dissolution of limestone over millions of years. These caves showcase unique geological formations such as stalactites, stalagmites, and underground rivers.


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How was Yarrangobilly Caves was formed?

Yarrangobilly Caves were formed by the dissolving of limestone by acidic groundwater over millions of years. The caves contain various formations such as stalactites, stalagmites, and columns created by the deposition of minerals from dripping water. The underground chambers were ultimately carved out by the slow erosion process of water flowing through the limestone bedrock.


How did the caves at ruby falls form?

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Why do people go to the cango caves?

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The Waitomo Caves in New Zealand were formed over millions of years through a combination of underground water flow and the dissolving of limestone rock. As acidic water trickled through the limestone, it created a network of underground tunnels and caverns, eventually forming the intricate caves and spectacular stalactites and stalagmites that we see today.


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Jenolan Caves in New South Wales, Australia, were formed over millions of years through the process of limestone dissolution by underground rivers. As the water seeped through the limestone rock, it slowly carved out the intricate cave systems and left behind the stunning stalactites and stalagmites that we see today. Ongoing geological processes continue to shape and modify the caves.


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