ROCK-FALL MONITORING IN YOSEMITE NATIONAL PARK
Falling rock in Yosemite Valley continues to pose a serious geologic risk because of high potential for continuing failure from steep cliffs, the location of some facilities near the base of the cliffs outside of the Merced River flood plain, and the nearly 4 million annual visitors to the park. Since 1980, there has been an average of about 10 slope failures documented per year. Despite the detailed monitoring of rock-fall events, it is not possible to predict exactly where, when, and what size rock falls will occur. However, the rock-fall inventory provides information for assessing the potential of slope failures within the valley. Scientists and managers know that rock-fall potential can generally be higher during some seasons, such as winter and spring, or during specific events, such as earthquakes or large storms. The NPS developed a Yosemite Valley Plan in November, 2000 restricting future development in rock-fall talus areas depicted on USGS inventory maps. The USGS and NPS are continuing to work closely together to identify and monitor areas that could be hazardous during and following naturally occurring rock falls and to provide timely public information about any potentially dangerous conditions.