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Tioga & Glacier Point Roads Closed for the Winter
The Tioga Road (Highway 120 through the park) and Glacier Point Road are closed due to snow. You can check on current road conditions and chain restrictions by calling 209/372-0200 (press 1 then 1). More »
Rockfall
What Is a Rockfall? Rockfalls are a natural and dynamic geologic process. Due to its steep, glacier-carved cliffs, Yosemite Valley experiences many rockfalls each year. Historical records indicate that more than 900 rockfalls have occurred in the park during the past 150 years. Massive piles of "talus" or rock debris at the base of Yosemite Valley's cliffs are reminders of these dramatic events. Natural processes like rockfall help to create the beautiful and changing scenery in Yosemite National Park, but they also present potential hazards. Photo by Amanda Nolan What Causes Rockfall? A number of geologic processes set the stage for rockfall. Glaciation, weathering, and bedrock fractures all play a role in causing rockfall. Tectonic stresses and erosion cause granite rock to fracture. Rockfalls later occur along these fractures. Fractures that develop parallel to the surface are called sheet joints. Sheet joints create large slabs of rock that ultimately fall away in a process known as exfoliation. In Yosemite Valley, Royal Arches and the face of Half Dome are examples of landforms that have resulted from this process. Over long periods, water flowing through fractures weathers the bedrock, loosening bonds that hold rocks in place. This is called weathering. Triggering mechanisms like water, ice, earthquakes, and vegetation create the final forces that cause unstable rocks to fall. If water enters fractures in the bedrock, it lubricates surfaces and can build up pressure behind unstable rocks. Water also may seep into fractures in the rock and freeze, causing the fractures in the rock to expand. This process is called "frost wedging" or "freeze-thaw" and can incrementally lever loose rocks away from cliff faces. Ground shaking during earthquakes can also trigger rockfalls. Additionally, a variety of vegetation-most notably firs, pines, and canyon live oaks-grow into the sheer rock faces where their roots expand and pry apart joints in the granite. Recent research suggests that daily temperature variations can cause rock slabs to become unstable. There is still uncertainty about exactly what triggers rockfall; historical records indicate that more than half of all documented rockfalls were not associated with a recognizable trigger. Most rockfalls in Yosemite occur in the winter and early spring, during periods of intense rainfall, snow melt, and/or subfreezing temperatures, but many large rockfalls have also occurred during periods of warm, stable weather. Predicting actual rockfall events is not yet possible, but understanding the forces that trigger rockfalls is an important step toward this goal. How Does the Park Address Rockfall? The National Park Service is responding to rockfall in a variety of ways. Park scientists, in collaboration with the U.S. Geological Survey (USGS) and academic researchers, are actively studying rockfall through the use of new technology, such as high resolution digital photography and laser mapping of cliffs. These tools offer vast improvement in resolution from previously available data, allowing geologists to accurately map rockfall zones and to study rockfall source areas. Additionally, new computer modeling technology shows promise in simulating future rockfall behavior. The park is also actively investigating possible methods for monitoring rockfall activity. In 2012, the National Park Service produced a report quantifying rockfall hazard and risk in Yosemite Valley to help improve safety and guide future park planning efforts. You can read the report, Quantitative rock-fall hazard and risk assessment for Yosemite Valley, Yosemite National Park, California [8 MB PDF], or watch an hour-long presentation by Greg Stock, the park geologist. Additionally, park rangers have developed emergency plans for rockfall events, and may close trails and post warning signs in particularly hazardous areas. What Should I Do in the Event of a Rockfall?
Photo by Tom Evans Yosemite Rockfall Year in Review: 2012 2012 was a relatively quiet year for rockfalls in Yosemite. The most consequential event occurred at about 11:00 pm on January 22 above the Big Oak Flat Road. A boulder some 250 cubic meters in volume (about 745 tons) fell from a cliff above the road, slid down the slope below the cliff, and struck the Big Oak Flat Road, punching a hole in the eastbound lane, tearing out some of the retaining wall, and severely damaging nearly 30 m (100 feet) of roadway. The road was closed for about six weeks for repairs. In all, there were 43 documented rockfalls in 2012, with an approximate cumulative volume of about 700 cubic meters (about 2,100 tons). Both the number of rockfalls and the cumulative volume for all rockfalls in 2012 are substantially less than that documented in recent years. Although it is not clear exactly why rockfall activity was reduced from previous years, it may relate to the exceptionally dry winter of 2011/2012. Learn More about Yosemite National Park's Geology
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Did You Know?
Yosemite has a full-time sign language interpreter in the park every summer? The Yosemite Deaf Services Program began in 1979 and provides a variety of services to make sure the park is accessible for all of Yosemite's D/deaf and hard of hearing visitors.