
Most people
refer to the unique secondary mineral deposits found in caves as "cave
formations." Geologists and cavers however frequently refer to them as
speleothems. You will soon see that a wide variety of speleothems exist in
the Timpanogos cave system. Even here in the entrance room are examples of
flowstone and stalagmites. As its name indicates, flowstone is formed by flowing
water. Stalagmites are formed by dripping water, this one is affectionately
referred to as the "Hershey's Kiss." Can you tell why?