William Mahone McGill has written: 'Caverns of Virginia' -- subject(s): Caves, Description and travel
Some main landforms in Carlsbad Caverns include stalactites, stalagmites, flowstone, columns, and cave popcorn. These formations are created by the deposition of minerals carried by dripping water over thousands of years, and they contribute to the unique beauty of the caverns.
Caverns typically form in bedrock through the process of chemical weathering, where acidic groundwater dissolves the minerals within the rock over a long period of time. As the rock erodes away, it creates larger cavities that eventually form caverns. Additionally, the presence of fractures and faults in the bedrock can also contribute to cavern formation.
Carlsbad Caverns.
Caverns can form in the zone of saturation due to processes such as dissolution, where groundwater dissolves soluble rock (like limestone) to create underground voids. Over time, these voids can enlarge and form caverns as groundwater continues to flow through and erode the rock. Additional factors like the presence of fractures or fault lines can also contribute to cavern formation in the zone of saturation.
Carlsbad Caverns experience physical weathering primarily through frost wedging. This process occurs as water seeps into cracks in the rock, freezes, expands, and causes the rock to break apart over time. Additionally, temperature changes and the expansion and contraction of rock layers due to heating and cooling can also contribute to physical weathering at Carlsbad Caverns.
Caverns can be under water and underground.
Caverns of Minos happened in 2012.
Carlsbad Caverns is located in New Mexico.
Caverns of Xaskazien happened in 1995.
Caverns of Xaskazien was created in 1995.
Caverns of Zoarre happened in 1984.