Scary Cave | Exploring | Stalactites and Stalagmites - Educational | We found Spiders and Bats

Описание к видео Scary Cave | Exploring | Stalactites and Stalagmites - Educational | We found Spiders and Bats

Do you like Extreme? Exploring New Places, Dark places like Caves with spiders and bats?
You are Lucky! Today you can explore a very Scary Dark Cave with us!
We went to Indian Echo cavern to explore and find spider and bats.
Very scary and dark was at this cave, had to walk narrow trails with banded back. So many Stalactites and Stalagmites!
And You must wear a heat if you don't want loose your hair or head )) there is water drops everywhere from the ceiling! Also, you will see underground Lake, that around 100-400 million years old.

Do you know what is different from between Stalactites and Stalagmites?
Stalactites hang from the ceiling of a cave while stalagmites grow from the cave floor.
When discussing mineral formations in caves, we often talk about stalactites and stalagmites. A stalactite is an icicle-shaped formation that hangs from the ceiling of a cave, and is produced by precipitation of minerals from water dripping through the cave ceiling. Most stalactites have pointed tips.
A stalagmite is an upward-growing mound of mineral deposits that have precipitated from water dripping onto the floor of a cave. Most stalagmites have rounded or flattened tips.
There are many other types of mineral formations found in caves. For example, flowstones are deposits of minerals from water flowing over the floor or walls of a cave. As layers of flowstone become thicker, their shape becomes rounded. Well-defined crystals growing underwater in cave pools are known as pool spar.

Indian Echo Caverns is a limestone cave. Cut through Beekmantown limestone, which is over 440 million years old, they were formed through the erosive properties of water. As time progressed, geological forces led to an “uplift” of the surrounding limestone, eventually allowing more and more water to flow through the formation. As the water flowed over the limestone, it began to create small crevices, these small crevices led to larger ones, and eventually, over a series of millions of years, it created the caverns as they are today.
The temperature inside the caverns is 52° year around.
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