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Unusual July 10, 1996, rock fall at Happy Isles, Yosemite National Park, California

¹ U.S. Geological Survey, M.S. 955, National Center, Reston, Virginia 20192
² National Park Service, P.O. Box 577, Yosemite National Park, California 95389
³ Cascades Volcano Observatory, U.S. Geological Survey, Vancouver, Washington 98661
⁴ Department of Geology and Geological Engineering, Colorado School of Mines, Golden, Colorado 80401
⁵ Berkeley Seismological Laboratory, University of California, Berkeley, California 94720
⁶ U.S. Geological Survey, M.S. 966, Box 25046, Denver Federal Center, Denver, Colorado 80225
⁷ U.S. Geological Survey, Department of Geophysics, Box 351650, University of Washington, Seattle, Washington 98195
⁸ Department of Geology, State University of New York, Buffalo, New York 14260

Effects of the July 10, 1996, rock fall at Happy Isles in Yosemite National Park, California, were unusual compared to most rock falls. Two main rock masses fell about 14 s apart from a 665-m-high cliff southeast of Glacier Point onto a talus slope above Happy Isles in the eastern part of Yosemite Valley. The two impacts were recorded by seismographs as much as 200 km away. Although the impact area of the rock falls was not particularly large, the falls generated an airblast and an abrasive dense sandy cloud that devastated a larger area downslope of the impact sites toward the Happy Isles Nature Center. Immediately downslope of the impacts, the airblast had velocities exceeding 110 m/s and toppled or snapped about 1000 trees. Even at distances of 0.5 km from impact, wind velocities snapped or toppled large trees, causing one fatality and several serious injuries beyond the Happy Isles Nature Center. A dense sandy cloud trailed the airblast and abraded fallen trunks and trees left standing. The Happy Isles rock fall is one of the few known worldwide to have generated an airblast and abrasive dense sandy cloud. The relatively high velocity of the rock fall at impact, estimated to be 110–120 m/s, influenced the severity and areal extent of the airblast at Happy Isles. Specific geologic and topographic conditions, typical of steep glaciated valleys and mountainous terrain, contributed to the rock-fall release and determined its travel path, resulting in a high velocity at impact that generated the devastating airblast and sandy cloud. The unusual effects of this rock fall emphasize the importance of considering collateral geologic hazards, such as airblasts from rock falls, in hazard assessment and planning development of mountainous areas.

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