Mammoth Mountain was developed over 57,000 years ago from a series of eruptions, located west of a town called Mammoth Lakes, California. Located in the Inyo National Forest, produces hazardous volcanic gases yet is home to the Mammoth Mountain Ski Area. Its skiing popularity has a lot to do with the fact it has an unusually large amount of snow, as compared to the other Eastern Sierra peaks because the mountain lies in a low gap area in the crest.
Skiing gondolas, a way to carry skiers on rides through the mountain for a set price, such as the mountain bikers and tourists searching for the most spectacular view from the mountain. The spectacular view of the Mammoth Mountain and its magmatic system is distinct from the Inyo Craters and the Long Valley caldera.
Inyo Crater Lakes is part of the lakes in Mono county of California, the historical deposits of the Mono Inyo Craters overlap in time and space with the Long Valley caldera with its youngest feature only 600 years old. Their volcanic field has developed over 30-miles along with volcanic cracks or elongated fractures that have produced flows of liquid and ejected pyroclastics, extending northward from the Mountain on its south west rim to Mono Inyo Lake and its craters.
It is easy for tourists and visitors to reach the Mono Inyo Craters and its chain of volcanoes, accessed from the Mammoth Lake and Mono Lake region from Highway 395. Two dirt roads, Deadman Creek Road and Glass Flow Road, lead from Highway 395 to Deadman Dome and Glass Creek Dome at the top of Mammoth Lake. The southern part of the Mono Inyo Craters and its trailhead can be reached by following the Mammoth Lakes Scenic Loop Highway. What an exciting way to ski and enjoy volcanoes at their best!!
