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Long Valley - Mammoth -
Inyo - Mono Vicinity, California


USGS Photo of the Inyo Vicinity, Long Valley, California
Aerial view of the Inyo Vicinity, Long Valley, California


Long Valley Caldera Volcano Information

Link to: Click button to link to Long Valley Observatory Website Long Valley Observatory Website


Long Valley and Vicinity
  • America's Volcanic Past - California
    -- Volcanic Highlights and Features
    Long Valley Caldera
    Mammoth Mountain
    Mono and Inyo Craters
    plus other National Parks and Monuments in California

  • Long Valley Caldera
    About 760,000 years ago a cataclysmic volcanic eruption in the Long Valley, California area blew out 150 cubic miles of magma (molten rock) from a depth of about 4 miles beneath the Earth's surface. Rapidly moving flows of glowing hot ash covered much of east-central California, and airborne ash fell as far east as Nebraska. The Earth's surface sank more than 1 mile into the space once occupied by the erupted magma, forming a large volcanic depression that geologists call a caldera. Today, Long Valley occupies the eastern half of this 10-mile-wide, 20-mile-long caldera. Magma still underlies the caldera and heats underground water. The heated water feeds local hot springs and natural steam vents and drives three geothermal power plants, producing a combined 40 megawatts of electricity. -- Excerpt from: Hill, et.al., 1996, Living With a Restless Caldera -- Long Valley, California: USGS Fact Sheet 196-96

  • Mammoth Mountain
    Long Valley, from the headwaters of Owens River to Lake Crowley, is a giant volcanic caldera. Mammoth Mountain - a massive volcanic dome - has grown on the caldera margin. Mammoth Mountain was built by eruptions between about 200,000 and 50,000 years ago. -- Excerpt from: USGS Long Valley Observatory Website, October 2000 and USGS/NPS Geology in the Parks Website, August 2001

  • Mono and Inyo Craters
    The massive Long Valley eruption (see above) was followed by hundreds of smaller eruptions over the next few hundred thousand years. These eruptions of lava flows, domes, and pyroclastic flows were concentrated in the central and western parts of the caldera. Volcanic activity then moved northward to the Mono Lake area about 35,000 years ago to build the Mono Craters. The most recent eruptions in the area occurred from the Mono and Inyo Craters about 600 years ago, and from Negit Island in Mono Lake about 250 years ago. -- Excerpt from: USGS Long Valley Observatory Website, October 2000


Location Maps
Map, click to enlarge
[Map,20K,InlineGIF]

Major West Coast Volcanoes - Washington, Oregon, and California

Map, click to enlarge
[Map,18K,InlineGIF]

Long Valley Caldera, Mono Crater, and Inyo Craters
-- Modified from: USGS-Menlo Park


Climb A Volcano

Black Point

Just off the north shore of the Mono Lake lies another interesting volcano: Black Point. A low, mesa-like mountain of black ash, Black Point erupted 12,000 years ago following the last ice age, when Mono Lake swelled to five times its current size and nearly ten times its current depth. At that time of its eruption, Black Point was located under water, which probably accounts for its unusual flattened top and the 80' deep, 5' wide cooling fissures that puncture its southwestern face.

The hike to the top of Black Point is not an easy one; consider this an exploration, an adventure! There are no trails or signs to show you where to go. You will be walking through the cinders and ash of the volcano and sometimes progress will be difficult. If you persevere, your discovery of the fissures will seem even more spectacular because their remoteness.

The fissures cut across the cap of Black Point in a roughly north-south direction. The best route of travel is to meander up the contours, walking south and west. From the high point (benchmark triangle on map), the fissures are to the southwest.

Remember, you are hiking at an elevation of nearly 7000 feet. If you come from a lower elevation, you may find the climbing particularly exhausting. Plan to allow ample time to enjoy the walk up (about 45 minutes), to explore the fissures and to return (about 3 hours total). Boots or high topped shoes will increase your comfort by keeping the sand out. Wearing a hat and carrying water are good ideas because you will not find any shade until you reach the fissures.

Please watch your step; there are no guard rails or signs. You can help make this experience pleasurable for others by carrying out your trash and by picking up any you find there.

Excerpts from: U. S. Forest Service Website, Inyo National Forest, 2001



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11/06/01, Lyn Topinka