This mile-long lava tube cave was formed roughly 700,000 years ago by molten rock that erupted from a volcanic vent in nearby Hart Prairie. The top, sides, and bottom of the flow cooled and solidified first, after which the insides of the lava river continued to flow emptying out the present cave.

Ample evidence of how the tube was born is written in the rocks from which it is formed. Small wave-like undulations in the floor are the remains of ripples frozen in the last trickle of molten rock that flowed from the cave. Stone icicles hanging from the ceiling show where a final blast of volcanic heat caused the rock to partially re-liquefy and drip.

Dress appropriately when you come to visit, with warm clothes and sturdy shoes. The cave is as cool as 42° even in summer, and you may even find some ice inside. The rocks are always sharp and slippery, too. Bring two or three sources of light, in case one happens to fail, it can be very dark one mile from the nearest light source.

Portions of the cave which were once defaced by graffiti have been cleaned up. Today’s more environmentally aware visitors take better care of such a unique resource and report vandals when they see them.

Drive 9 miles north of Flagstaff on US-180 and turn west (left) on FR-245 (at milepost 230). Continue 3 miles to FR-171 and turn south 1 mile to where FR-171B turns left a short distance to Lava River Cave.

Though the Lava River Cave is open year-round, FR-245 and/or FR-171 are typically closed due to muddy, snowy conditions. It is approximately a four-mile one-way trip to hike or ski to the cave from US-180.