The Ice Cave: a lava tube that never warms above 31°F
The Ice Cave is genuinely one of the more remarkable small geological features in the American Southwest — a partially-collapsed lava tube where ice accumulates year-round and never melts, even during peak summer temperatures that routinely exceed 100°F on the surrounding lava fields. The cave's interior temperature typically stays below 31°F throughout the year, with the constant cold maintained by a combination of the lava tube's natural insulation, the trapped cold air that flows down into the cave and cannot escape upward, and the consistent seepage of meltwater from above that refreezes inside the cave.
Descent into the Ice Cave is via a wooden staircase that drops visitors approximately 70 feet below the surrounding ground level. The staircase is solidly constructed, well-maintained, and includes handrails throughout — most visitors with reasonable mobility can complete the descent and ascent without difficulty, though the stairs are steep enough that visitors with significant knee, hip, or balance limitations may find the return climb challenging. There is no elevator alternative.
Inside the cave, the ice floor is approximately 20 feet thick — accumulated across centuries of slow seepage and refreezing — and exhibits a striking blue-green color caused by suspended algae and mineral content. The deepest ice layers are generally dated to several hundred years ago, with some estimates running over 1,000 years for the oldest ice still preserved in the cave's deepest pockets. The light filtering down from the cave entrance produces dramatic photography in mid-morning hours when the sun angle is right for the staircase descent.