Description
The story of Cody Caves began 600 million years ago when the limestone in which the caves later formed was laid down at the bottom of an ancient sea. Then, around 170 million years ago, the limestone beds were thrust upwards. This exposed the rock to the elements, water and carbonic acid, which eventually formed Cody Caves. Approximately 875 yards (800 m) of the Cody Caves passageways are explorable. The caves have several types of calcite formations, such as stalagmites, stalactites, soda straws and flowstone. The boxwork is considered to be among the best in the world, protruding up to 20.3 cm, whereas 2.5 to 5 cm is average. These ancient formations have been growing at an average rate of one cubic centimetre per hundred years.
The Ainsworth Hot Springs originate in the Cody Caves area and are considered to be the best commercial hot springs in British Columbia. The temperatures vary from 40–42 °C (104–108 °F) in the cave to 35–38 °C (95–100 °F) in the pool.
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