Scotty's Castle Road Construction
Expect 30 minute delays Monday-Saturday on Scotty's Castle Road and Mesquite Springs Campground Road. Caution advised due to unpaved surfaces and sections of one-lane road.
Scotty's Castle Road Closure
The road from Scotty's Castle east to the park boundary will be closed to all traffic from February 10 to April 10, 2014. The Castle can be accessed from the south via CA-190 and Scotty's Castle Road; expect 30 minute delays.
Faulting is the one of the main reasons Death Valley exists. Movement along faults allow the mountains to rise and the valleys to sink. Death Valley is located in the southwestern portion of the Basin and Range geomorphic province. The Basin and Range province has a long and active geologic history, including faulting and regional tectonic movement. Fault-bounded uplifted ranges are separated by down-dropped sedimentary basins.
Most faulting that is presently occurring within Death Valley is strike-slip (transverse) with a component of normal movement (see Figure 1). With faulting comes the possibility of seismic activity, more commonly known as earthquakes. Most earthquakes that occur today are very small and cause no damage to structures or the ground surface. However, at some point in the future (no one knows how long into the future), the major fault systems in Death Valley are almost sure to create a significant seismic event.
Did You Know?
Badwater Basin, in Death Valley National Park, is the lowest place in North America and one of the lowest places in the world at 282 feet below sea level. The Dead Sea, between Israel and Jordan, is the lowest at 1371 feet below sea level.