Crater view from Highway 395
Massive rock composed mostly of obsidian.
Mono Craters
The Mono Craters are the youngest mountain range in North America. They rise to 2,400 feet above the surrounding Mono Basin, just south of Mono Lake and east of the junction of Hwy 395 and Hwy 120. They first erupted about 100,000 years ago. The Mono Craters are not really craters. They consist of 30 or more overlapping rhyolite domes and explosion pits. You'll see large quantities of pumice and obsidian in the area. Local Indians used the obsidian to fashion arrowheads and cutting tools. When the L.A. DWP drilled an 11.5 mile aqueduct tunnel through the Mono Craters in the 1930’s, work crews encountered hot and cold groundwater, deadly carbon dioxide gas, and steam proving that there is still activity within the Mono Craters. Nobody knows when the next eruption will be, but geologic changes occur extremely slowly when compared to the human lifetime. The Mono Craters are not dead. They remain dormant and will almost certainly erupt again in the future.
One of many trails crossing the Mono Craters.
In cooperation with Inyo National Forest