The quality of cave air is usually good. The air’s often cool temperature gives it a fresh feeling many people enjoy. Doctors in several countries recommend Speleotherapy for several ailments, occasionally prescribing sitting in a cave to breathe the air.
Karst caves formed in carbonate rocks (limestone, dolomite, and marble) occasionally have slightly elevated levels of carbon dioxide in the air. As water and air move down through fractures in the rock into a cave, they carry carbon dioxide generated in the soil and released by plants through their roots. The typical levels of carbon dioxide are low and not noticed by visitors.
The significant presence of other gases in caves is uncommon to rare. Examples include methane from the decomposition of large volumes of organic material which washed into a cave, ammonia from large deposits of bat guano, and a variety of possible gases associated with geothermal areas.
The temperature of a cave is usually close to the average annual temperature for the region where it’s located. For example, caves in Texas can be as warm as 70º F. Caves in Missouri might be between 55º F and 60º F. Caves in Wisconsin might be a chilly 50º F.
Air pressure inside a cave always tries to equalize with the outside air pressure. If air pressure outside the cave is greater, air moves into the cave and vice versa. Also, winter air is colder and thus denser than cave air, moving down cave floors and pushing warmer air out of a cave along with the ceiling.
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