EXTREME SUMMER HEAT
Expect high temperatures of 100 to 120 degrees F on your summer visit to Death Valley. Heat related illness is a real possibility. Drink plenty of water and carry extra. Avoid activity in the heat. Travel prepared to survive. Watch for signs of trouble. More »
Zabriskie Point Rehab Project Delayed Until Further Notice
The popular vista site Zabriskie Point will be closed for major repairs over the 2014/2015 winter and spring seasons, but the exact date has not been determined. The site will remain open until further notice.
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?
The highest mountain in Death Valley National Park is 11,049 foot Telescope Peak. The vertical drop from the peak to the Badwater Basin is twice the depth of Grand Canyon. More...