Frequently Asked Questions
Here are answers to the questions visitors most often ask about the Long Valley Caldera.
What is the Long Valley Caldera?
A vast volcanic depression 10 miles wide and 20 miles long in the Eastern Sierra, formed roughly 760,000 years ago when a massive magma chamber erupted and collapsed. It is one of the largest calderas in North America and remains geologically active today.
Is the Long Valley Caldera dangerous?
The caldera is continuously monitored by the U.S. Geological Survey for seismic and volcanic activity. It poses no immediate danger to visitors, though certain areas like the CO2 ghost forest at Horseshoe Lake and active thermal features at Hot Creek require caution and carry posted safety warnings.
Can you see the Long Valley Caldera from Mammoth Lakes?
Yes. The town of Mammoth Lakes sits on the southern rim of the caldera. From elevated vantage points like the Mammoth Mountain summit, the full oval depression of the collapsed magma chamber is clearly visible across the valley floor.
What caused the Long Valley Caldera eruption?
A massive magma chamber beneath the Eastern Sierra erupted approximately 760,000 years ago, ejecting enormous volumes of ash and rock, including the Bishop Tuff ash layer, which blanketed much of the western United States. The ground above it collapsed to form the caldera.
How do I explore the Long Valley Caldera?
Start at Hot Creek for active geothermal features, then visit the Earthquake Fault and Inyo Craters for accessible geological stops. Ride the gondola to the top of Mammoth Mountain for a panoramic view of the entire caldera from above. Mammoth Lakes makes the ideal base for a half-day or full-day caldera itinerary.
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