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Blister caves are small geological formations created when trapped steam or other gases lift layers of still-molten lava. These cavities are dome-shaped chambers, typically ranging from one to a few meters in diameter, and can be found in large numbers within lava flows rich in volatile components. They are a type of lava cave, distinct from larger lava tubes formed by the draining of molten rock from beneath a solidified crust. Blister caves are primarily found in volcanic regions, with notable occurrences in the Pacific Northwest of the United States and Hawaii.12

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