The moving rocks of Racetrack Playa a seasonally dry lake located in the Panamint Mountains Death Valley NationalPark
Tuesday, September 9th, 2008

The moving rocks, also known as sliding rocks or sailing stones, are a geological phenomenon found in Racetrack Playa, a seasonally dry lake (a playa) located in the Panamint Mountains in Death Valley NationalPark, California. The rocks move across the surface of the playa, leaving long tracks behind them as they go, without human or animal intervention. They have never been seen or filmed in motion.
Most of the moving stones originate from an 850 foot (260 m) high hillside made of dark dolomite on the south end of the playa, but some are intrusive igneous rock from adjacent slopes. Tracks are often tens to hundreds of feet (low to high tens of meters) long, a few to 12 inches (8 to 30 cm) wide, and typically less than an inch (2.5 cm) deep.
But both theories don’t explain how two rocks right next to each other could go in two opposite directions or one could stay put while the one three times the size, doesn’t. So far every attempt of explanation has been insufficient and purely assumptive. The mystery of moving rocks is yet to be revealed.









































