• Speleothems in Miller's Chapel.

    Oregon Caves

    National Monument Oregon

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  • Road Work, Expect Delays

    ODOT will be preparing highway 46 for asphalt patching. Please use caution when traveling between the monument and Grayback Campground. Various work will be from continue until July 31, 2014.

  • Watch for Wildlife

    Please be on the lookout for fawns on the section of Caves Highway around Caves Campground! There is at least one very young one that is using the pavement as his transportation corridor.

Speleogenesis- Creation of Cave

speleogensis

Over several million years, the belt of marble within the Siskiyou Mountain cracked as the land uplifted and folded. At the same time, the top of the mountain weathered and exposed the marble to the surface of the earth. A forest grew over the marble and in the forest soil, fungi, bacteria, and mold decomposed dead plants and animals releasing carbon dioxide. Precipitation percolated through the soil and captured the carbon dioxide to create carbonic acid. This mild acid is the same stuff that gives soda pop its fizz.

The acidic water then chemically weathered the marble bedrock as it traveled downward through the cracks and holes in the rocks. Ground water moved downward until it reached the water table--an area where all available pore space in rocks are filled with water. The greatest amount of marble was dissolved just below the water table where the highest concentration of carbonic acid occurred. Water then spreads sideways along the cracks in the bedrock and the carbonic acid slowly dissolved the marble. Over hundreds of thousands of years, the carbonic acid enlarges small cracks into larger cavities as the marble was carried away (eroded) in solution. The process of dissolving marble and opening up spaces within it is called speleogenesis. Speleogensis is derived from the Greek words "spelaion" (cave) and "genesis" (beginning).

Did You Know?

Waterfall and pool near the entrance to Oregon Caves.

The stream that comes out of the entrance of the cave is a tributary to a watershed that empties into the Pacific Ocean. There are no human-made obstructions that would prevent salmon migration, which makes this the only cave in the National Park Service with an unobstructed link to the ocean.