

The rock involved in the event was a slab of exfoliated granitic rock roughly the size of a football field that broke off from the top of the cliff near Glacier Point, slid for several hundred feet and then fell 1,800 feet, hitting the floor of the valley at a speed of something over 200 mph. The rocks exploded on impact generating an airblast that toppled 1000+ trees. U.C. Berkeley has an excellent analysis of the slide here, and formal article from the GSA Bulletin can be found here.
Regrowth of trees and shrubs has obscured much of the damage, but the Happy Isles Nature Center has a nice exhibit and viewpoint; walk out the back door of the museum to find it. The slide was not the first in the area. Huge talus piles cling to slopes below the breakaway point, and a much larger prehistoric slide has been mapped beneath the thick forest. It forced the Merced River into a new channel, and contributed to the formation of the marshy area west of the campground.