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http://geomaps.wr.usgs.gov/parks/deva/racetrack.pdfThe Racetrack Playa, at an elevation of 1131 m, is a dry lakebed nestled in the Panamint Range in Death Valley National Park, California. Though almost perfectly flat, it shows evidence of dynamic traction (sliding) of boulder-sized and smaller rock fragments that tumble onto it from two abutting cliffs and surrounding alluvial fans (Figure 1). Scars of sliding rock activity in the form of recessed furrows have been noted since the beginning of the twentieth century...yet to date no one has witnessed the actual surface process that causes the rocks to slide. [continued]
[link updated] 6/20/09
New Paper Claims Explanation
https://www.physicsforums.com/showthread.php?t=60676&page=5#90
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