Sailing stones, also known as sliding rocks, rolling stones, and moving rocks, are a geological phenomenon where rocks move and inscribe long tracks along a smooth valley floor without human or animal intervention. Instead, rocks move when large ice sheets a few millimeters thick floating in an ephemeral winter pond start to break up during sunny days. These thin floating ice panels, frozen during cold winter nights, are driven by wind and shove rocks at up to 5 m/min.
Trails of sliding rocks have been observed and studied in various locations, including Little Bonnie Claire Playa in Nevada, and most notably Racetrack Playa, Death Valley National Park, California, where the number and length of tracks are notable.
The Racetrack’s stones speckle the playa floor, predominantly in the southern portion. Historical accounts identify some stones around 100 m (300 ft) from shore, yet most of the stones are found relatively close to their respective originating outcrops. Three lithologic types are identified: (1) syenite, found most abundant on the west side of the playa; (2) dolomite, subrounded blue-gray stones with white bands; and (3) black dolomite, the most common type, found almost always in angular joint blocks or slivers. This dolomite composes nearly all stones found in the southern half of the playa, and originates at a steep promontory, 260 m (850 ft) high, paralleling the east shore at the south end of the playa. Intrusive igneous rock originates from adjacent slopes (most of those being tan-colored feldspar-rich syenite). Tracks are often up to 100 m (330 ft) long, about 8 to 30 cm (3 to 12 in) wide, and typically much less than 2.5 cm (1 in) deep. Most moving stones range from about 6 to 18 in (15 to 46 cm) in diameter.
Stones with rough bottoms leave straight striated tracks, while those with smooth bottoms tend to wander. Stones sometimes turn over, exposing another edge to the ground and leaving a different track in the stone's wake.
Trails differ in both direction and length. Rocks that start next to each other may travel parallel for a time, before one abruptly changes direction to the left, right, or even back to the direction from which it came. Trail length also varies – two similarly sized and shaped rocks may travel uniformly, then one could move ahead or stop in its track.
A balance of very specific conditions is thought to be needed for stones to move:
- A flooded surface
- A thin layer of clay
- Ice floes
- Warming temperatures causing ice breakup
At Racetrack Playa, these tracks have been studied since the early 1900s, yet the origins of stone movement were not confirmed and remained the subject of research for which several hypotheses existed. However, as of August 2014, timelapse video footage of rocks moving has been published, showing the rocks moving at high wind speeds within the flow of thin, melting sheets of ice. The scientists have thus identified the cause of the moving stones to be ice shove.
The first documented account of the sliding rock phenomenon dates to 1915, when a prospector named Joseph Crook from Fallon, Nevada, visited the Racetrack Playa site. In the following years, the Racetrack sparked interest from geologists Jim McAllister and Allen Agnew, who mapped the bedrock of the area in 1948 and published the earliest report about the sliding rocks in a Geologic Society of America Bulletin. Their publication gave a brief description of the playa furrows and scrapers, stating that no exact measurements had been taken and suggesting that furrows were the remnants of scrapers propelled by strong gusts of wind – such as the variable winds that produce dust-devils – over a muddy playa floor. Controversy over the origin of the furrows prompted the search for the occurrence of similar phenomena at other locations. Such a location was found at Little Bonnie Claire Playa in Nye County, Nevada, and the phenomenon was studied there, as well.
Naturalists from the National Park Service later wrote more detailed descriptions and Life magazine featured a set of photographs from the Racetrack. In 1952, a National Park Service Ranger named Louis G. Kirk recorded detailed observations of furrow length, width, and general course. He sought simply to investigate and record evidence of the moving rock phenomenon, not to hypothesize or create an extensive scientific report. Speculation about how the stones move started at this time. Various and sometimes idiosyncratic possible explanations have been put forward over the years that have ranged from the supernatural to the very complex. Most hypotheses favored by interested geologists posit that strong winds when the mud is wet are at least in part responsible. Some stones weigh as much as a human, which some researchers, such as geologist George M. Stanley, who published a paper on the topic in 1955, feel is too heavy for the area's winds to move. After extensive track mapping and research on rotation of the tracks in relation to ice floe rotation, Stanley maintained that ice sheets around the stones either help to catch the wind or that ice floes initiate rock movement.
Progress in the 1970s
Bob Sharp and Dwight Carey started a Racetrack stone movement monitoring program in May 1972. Eventually , 30 stones with fresh tracks were labeled and stakes were used to mark their locations. Each stone was given a name and changes in the stones' positions were recorded over a seven-year period. Sharp and Carey also tested the ice floe hypothesis by corralling selected stones. A corral 1.7 m (5.5 ft) in diameter was made around a 3 in (8 cm) wide, 1 lb (0.45 kg) track-making stone with seven rebar segments placed 25 to 30 in (64 to 76 cm) apart. If a sheet of ice around the stones either increased wind-catching surface area or helped move the stones by dragging them along in ice floes, then the rebar should at least slow down and deflect the movement. Neither appeared to occur; the stone barely missed a rebar as it moved 28 ft (8.5 m) to the northwest out of the corral in the first winter. Two heavier stones were placed in the corral at the same time; one moved five years later in the same direction as the first, but its companion did not move during the study period. This indicated that if ice played a part in stone movement, then ice collars around stones must be small.
Ten of the initial 30 stones moved in the first winter with Mary Ann (stone A) covering the longest distance at 212 ft (65 m). Two of the next six monitored winters also had multiple stones move. No stones were confirmed to have moved in the summer, and in some winters, none or only a few stones moved. In the end, all but two of the monitored stones moved during the seven-year study. At 2.5 in (6.4 cm) in diameter, Nancy (stone H) was the smallest monitored stone. It also moved the longest cumulative distance, 860 ft (260 m), and the greatest single winter movement, 659 ft (201 m). The largest stone to move was 80 lb (36 kg).
Karen (stone J) is a 29 by 19 by 20 in (74 by 48 by 51 cm) block of dolomite and weighs an estimated 700 lb (320 kg). Karen did not move during the monitoring period. The stone may have created its 570 ft (170 m) long, straight and old track from momentum gained from its initial fall onto the wet playa. However, Karen disappeared sometime before May 1994, possibly during the unusually wet winter of 1992 to 1993. Removal by artificial means is considered unlikely due to the lack of associated damage to the playa that a truck and winch would have caused. A possible sighting of Karen was made in 1994, 1⁄2 mi (800 m) from the playa. Karen was rediscovered by San Jose geologist Paula Messina in 1996.
Continued research in the 1990s
Professor John Reid led six research students from Hampshire College and the University of Massachusetts Amherst in a follow-up study in 1995. They found highly congruent trails from stones that moved in the late 1980s and during the winter of 1992–93. At least some stones were proved beyond a reasonable doubt to have been moved in ice floes that may be up to 1⁄2 mi (800 m) wide. Physical evidence included swaths of lineated areas that could only have been created by moving thin sheets of ice. Consequently, both wind alone and wind in conjunction with ice floes are thought to be motive forces.
Physicists Bacon et al. studying the phenomenon in 1996, informed by studies in Owens Dry Lake Playa, discovered that winds blowing on playa surfaces can be compressed and intensified because of a playa's smooth, flat surfaces. They also found that boundary layers (the region just above ground where winds are slower due to ground drag) on these surfaces can be as low as 2 in (5 cm). As a result, stones just a few centimeters high feel the full force of ambient winds and their gusts, which can reach 90 mph (140 km/h) in winter storms. Such gusts are thought to be the initiating force, while momentum and sustained winds keep the stones moving, possibly as fast as a moderate run (only half the force required to start a stone sailing is needed to keep it in motion).
Wind and ice both are the favored hypothesis for these sliding rocks. Noted in "Surface Processes and Landforms", Don J. Easterbrook mentions that because of the lack of parallel paths between some rock paths, this could be caused by degenerating ice floes resulting in alternate routes. Though the ice breaks up into smaller blocks, it is still necessary for the rocks to slide.
Twenty-first century developments
Further understanding of the geologic processes at work in Racetrack Playa goes hand in hand with technological development. In 2009, development of inexpensive time-lapse digital cameras allowed the capturing of transient meteorological phenomena including dust devils and playa flooding. These cameras were aimed at capturing various stages of the previously mentioned phenomena, though discussion of the sliding stones ensued. The developers of photographic technology describe the difficulty of capturing the Racetrack’s stealthy rocks, as movements only occur about once every three years, and they believed, lasted about 10 seconds. Their next identified advancement was wind-triggered imagery, vastly reducing the ten million seconds of nontransit time they had to sift through.
It was postulated that small rafts of ice form around the rocks and the rocks are buoyantly floated off the soft bed, thus reducing the reaction and friction forces at the bed. Since this effect depends on reducing friction, and not on increasing the wind drag, these ice cakes need not have a particularly large surface area if the ice is adequately thick, as the minimal friction allows the rocks to be moved by arbitrarily light winds.
Reinforcing the "ice raft" theory, a research study pointed out narrowing trails, occurrence of intermittent spring systems, and absence of rocks at the end of the trails. The study identified the Racetrack mountain area that drains water towards the Racetrack Playa, while ice covered the intermittent lake. This suggests that this water buoyantly lifts the icebergs with embedded rocks until friction with the playa bed is reduced sufficiently for wind forces to move them and cause the observed tracks. The study also provides mapping and analysis of the effect of artificial ditch preventing the visitors from driving on the playa and they claim that it may interfere with the sliding rock phenomenon.
Based on a study, news articles reported the mystery solved when researchers observed rock movements using GPS and time-lapse photography. The research team witnessed and documented rock movement on December 20, 2013, that involved more than 60 rocks, with some rocks moving up to 224 m between December 2013 and January 2014 in multiple move events. These observations contradicted earlier hypotheses of winds or thick ice floating rocks off the surface. Instead, rocks move when large ice sheets a few millimeters thick floating in an ephemeral winter pond start to break up during sunny days. These thin floating ice panels, frozen during cold winter nights, are driven by light winds and shove rocks at up to 5 m/min (0.3 km/h). Some GPS-measured moves lasted up to 16 minutes, and a number of stones moved more than five times during the existence of the playa pond in the winter of 2013-14
Ralph Lorenz, a NASA scientist, investigated the phenomenon in 2006. To illustrate the "ice raft" theory, Lorenz developed an experiment using a kitchen-table model using a Tupperware container to show how heavy rocks might glide across the surface of the lake bed. A bed of sand is added to the bottom of the Tupperware, a rock is placed on the sand, and water is added until only a small edge of the rock sticks out. After putting the container in the freezer until the water is frozen, then removing the container and letting the ice begin to melt, Lorenz could end up with a small raft of floating ice with a rock embedded in it. All he had to do was gently blow on the floating ice sheet to get the rock to drag across the sand.
Theft of rocks
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- Reid, J.B., Jr., Bucklin, E.P., Copenagle, L., Kidder, J., Pack, S. M., Polissar, P. J., and Williams, M. L., 1995, Sliding rocks at the Racetrack, Death Valley: What makes them move?. Geology v. 23, pp. 819–822
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|Wikimedia Commons has media related to Sliding rocks of Racetrack Playa.|
- Smithsonian Magazine: "How Do Death Valley’s “Sailing Stones” Move Themselves Across the Desert?" — June 2013 issue.
- National Geographic: "What Drives Death Valley's Roving Rocks?"
- Racetrackplaya.org: The Racetrack Playa Blog — homepage
- SJSU.edu: "The Sliding Rocks of Racetrack Playa" — by Paula Messina.
- Smith.edu: "The Mystery of the Rocks on the Racetrack at Death Valley" — by Lena Fletcher and Anne Nester.
- Physics Forums.com: "The Sliding Rock Phenomenon" — online discussion.
- YouTube: Moving Rocks of Death Valley's Racetrack Playa — video by Brian Dunning.
- Fox News.com: Why Are Death Valley's Rocks Moving Themselves? — by Philip Schewe.
- Plosone.org: "Sliding Rocks on Racetrack Playa, Death Valley National Park: First Observation of Rocks in Motion"