The number of documented caves within the Monument currently exceeds 300 and more are discovered each year. There are 3 main types of caves found here (listed from most numerous to least): lava tubes, fissure caves, and differential weathering caves.
Lava Tube Caves
The vast majority of caves found within the Monument are lava tubes. They formed when the cooling exterior of an active lava flow insulated the molten river within allowing it to continue to flow. In this way lava sometimes flowed for many miles underground until the source was cut off or diverted leaving behind an empty space or “cave.” Indian tunnel (shown in photo) is an excellent example of a lava tube cave. This cave and 3 other lava tube caves are easily accessed along the 7 mile Loop Road along the Caves Trail.
The Virtual Lava Tube
Discovering Caves: Lava Tubes (pdf)
Fissure caves are found within the the deep cracks that make up the Great Rift. Some of these caves are remarkably deep, including one particular fissure that may be passable to a depth of 650 feet (200 meters) from the surface. The King's Bowl area is an excellent place to view fissure caves but access is limited to cavers with the right equipment and knowledge to explore these caves safely.
Differential Weathering Caves
These caves were formed when volcanic material was hollowed out by wind, rain and frost. These caves are relatively rare and difficult to find.
White Nose Syndrome
If the answer to both questions is yes, please bring gear with you which has not been exposed to other
Detailed decontamination procedures have been developed by the U.S. Fish and Wildlife Service.
Did You Know?
Searing lava flows that initially destroyed everything in their path today protect the last refuges of intact sagebrush steppe communities on the Snake River Plain. These islands of vegetation, known as kipukas, provide important examples of what is "natural".