USGS Identifier

Title: Long Valley Observatory

Photos of the Resurgent Dome, Long Valley Caldera

The resurgent dome is a broad area of the central caldera floor that was pushed upward within 100,000 years or less of the caldera-forming eruption 730,000 years ago. This uplift was caused by upward pressure related to the intrusion of molten rock into the magma reservoir beneath the caldera. The resurgent dome is made of layers of lava flows, tephra, and pyroclastic flows that were erupted onto the caldera floor soon after the caldera formed. The uplift arched and faulted these volcanic rocks to form a central highland area about 10 km in diameter and as high as 500 m above the surrounding caldera floor.

Resurgent dome, Long Valley Caldera, California View of the resurgent dome looking east-southeast across the west moat of the Long Valley Caldera.
Resurgent dome, Long Valley Caldera, California View of the resurgent dome looking east-northeast; Town of Mammoth Lakes is in foreground.

See views from atop Mammoth Mountain for other photos of the resurgent dome.

Back to photo gallery introduction

 

| Home | Current Condition | Monitoring Data | Volcano Hazards |
| Photo Gallery | Area Maps | Geologic History | Response Plan |



U.S. Department of the Interior, U.S. Geological Survey, Menlo Park, California, USA
URL http://lvo.wr.usgs.gov/gallery/ResurgentDome_1.html
Contact: Long Valley Web Team
Last modification: 9 October 1999 (SRB)