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Gypsum Lava Tube Cave, Idaho

Waking up at 4am to drive to Idaho to visit the second largest lava tube cave on the continental United States. Lava tube caves form differently from limestone solution caves — lava flows cool and harden on the outside while molten rock continues flowing through the interior until the flow stops, leaving a hollow tube that can extend for miles. Gypsum Cave in Idaho may have been near the eruption center given its size. The lower viscosity flows that formed the ceiling created a baseline for the tube near the surface.

 
 
 

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