Exactly how the rocks on the famous Death Valley Racetrack move has been a mystery since the 1940s.
Photo courtesy freenaturephotos.com
Researchers from the led by a paleobiologist from the Scripps Institution of Oceanogrophy at U.C. San Diego has answered a question that has been asked since the 1940s: âHow do the rocks on the famous Death Valley Racetrack move?â
Simply put, the answer is that there is a unique phenomena that occurs when weather conditions are just right and sheets of ice begin to move on the Racetrack Playa.
Littered across the flat, dry surface of the dry lake are hundreds of rocks â some weighing as much as 700 pounds â that seem to have been dragged across the ground, often leaving synchronized trails that can stretch for hundreds of meters.
What powerful force could be moving them? Researchers have investigated this question since the 1940s, but no one has ever seen the process in action â until now.
In a new paper published in the Aug. 27, PLOS ONE, a team led by Scripps Institution of Oceanography, UC San Diego, paleobiologist Richard Norris reports on first-hand observations of the phenomenon.
Because the stones can sit for a decade or more without moving, the researchers did not originally expect to see motion in person. Instead, they decided to monitor the rocks remotely by installing a high-resolution weather station capable of measuring gusts to one second intervals and fitting 15 rocks with custom-built, motion-activated GPS units.
Due to regulations, the National Park Service could not allow the researchers to use native rocks, so the team brought in similar rocks from an outside source.
The experiment was set up in Winter 2011 with permission of the National Park Service. Then â in what Ralph Lorenz of the Applied Physics Laboratory at the Johns Hopkins University, one of the paperâs authors, suspected would be âthe most boring experiment everâ â they waited for something to happen.
But in December 2013, Norris and co-author James Norris (of Interwoof and Richardâs cousin) arrived in Death Valley to discover that the playa was covered with a shallow pond no more than three inches deep. Shortly after, the rocks began moving.Â
âScience sometimes has an element of luck,â Richard Norris said. âWe expected to wait five or 10 years without anything moving, but only two years into the project, we just happened to be there at the right time to see it happen in person.â
Their observations show that moving the rocks requires a rare combination of events. First, the playa fills with water, which must be deep enough to allow formation of floating ice during cold winter nights, but remain shallow enough to expose the rocks. As nighttime temperatures plummet, the pond freezes to form sheets of âwindowpaneâ ice, which must be thin enough to move freely but thick enough to maintain strength. On sunny days, the ice begins to melt and break up into large floating panels, which light winds drive across the playa pool. The ice sheets shove rocks in front of them and the moving stones leave trails in the soft mud bed below the pool surface.
Â âOn Dec. 21, 2013, ice breakup happened just before noon, with popping and cracking sounds coming from all over the frozen pond surface,â said Richard Norris. âI said to Jim, âThis is it!ââ
These observations were surprising in light of previous models, which had proposed hurricane-force winds, dust devils, slick algal films, or thick sheets of ice as likely contributors to rock motion. Instead, rocks moved under light winds of about 10 miles per hour and were driven by ice less than 0.25 inches â too thin to grip large rocks and lift them off the playa, which several papers had proposed as a mechanism to reduce friction.
Further, the rocks moved only a few inches per second (2-6 m/minute), a speed that is almost imperceptible at a distance and without stationary reference points. âItâs possible that tourists have actually seen this happening without realizing it,â said Jim Norris. âIt is really tough to gauge that a rock is in motion if all the rocks around it are also moving.â
Individual rocks remained in motion for anywhere from a few seconds to 16 minutes. In one event, the researchers observed that rocks three football fields apart began moving simultaneously and traveled more than 200 feet before stopping. Rocks often moved multiple times before reaching their final resting place. The researchers also observed rock-less trails formed by grounding ice panels â features that the Park Service had previously suspected were the result of tourists stealing rocks.
âThe last suspected movement was in 2006, and so rocks may move only about one millionth of the time,â said Lorenz. âThere is also evidence that the frequency of rock movement, which seems to require cold nights to form ice, may have declined since the 1970s due to climate change.â
Richard and Jim Norris, and co-author Jib Ray of Interwoof started studying the Racetrackâs moving rocks to solve the âpublic mysteryâ and set up the âSlithering Stones Research Initiativeâ (âScience for the fun of itâ) to engage a wide circle of friends in the effort. They needed the help to repeatedly visit the remote dry lake, quarry rocks for the GPS-instrumented stones, and design the custom-built instrumentation. Lorenz and Brian Jackson (of the Department of Physics, Boise State University), in contrast, started working on the phenomenon to study dust devils and other desert weather features that might have analogs to processes happening on other planets. âWhat is striking about prior research on the Racetrack is that almost everybody was doing the work not to gain fame or fortune, but because it is such a neat problem,â says Jim Norris.
So is the mystery of the sliding rocks finally solved?
âWe documented five move events in the two and a half months the pond existed and some involved hundreds of rocksâ, says Richard Norris, âSo we have seen that even in Death Valley, famous for its heat, floating ice is a powerful force driving rock motion. But we have not seen the really big boys move out there âŠ does that work the same way?â
Death Valley National Park wants to remind people that the Racetrack is located in a remote area of the park and road conditions are variable at best, requiring high clearance vehicles and heavy duty tires. âDo not attempt a trip to the Racetrack without a plenty of fuel and water.Â There is no cell phone service in the area,â a press release from DVNP states.Â âBe prepared for the possibility of spending the night if your vehicle becomes disabled.â
A more easily-accessible location to observe the tracks of sliding stones is the Bonnie Claire playa east of Scottyâs Castle â between the park boundary and Highway 95.Â The south shore of the playa runs right along the north side of Highway 72.Â The area is administered by the Bureau of Land Management. There is abundant evidence of sliding stones at this playa, which is believed to experience the same rock-moving conditions as the Racetrack.