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Boulders Moving in Death Valley: A 70-Year Mystery Solved by Thin Ice and Weak Wind

For more than seven decades, heavy rocks weighing up to 300 kg on Racetrack Playa in Death Valley, United States, have left mysterious trails without explanation. In 2013, researchers first recorded direct movement: a thin layer of ice — formed from rainwater freezing at night — was moved by weak wind (5–10 m/s), pushing the rocks across the slick mud surface. This phenomenon requires a unique combination of temperature, humidity, and topography — explaining why it rarely occurs and is hard to observe.

24 Jun 20264 min read3 viewsBy Redaksi KhatulistiwaKhatulistiwa
NeutralDisemak silang 2 model · 68
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  • Batu-batu di Racetrack Playa, Lembah Kematian, meninggalkan jejak misterius selama lebih 70 tahun.
  • Pada 2013, penyelidik merakam pergerakan batu yang disebabkan oleh lapisan ais nipis dan angin lemah.
  • Fenomena ini memerlukan kombinasi unik suhu, kelembapan, dan topografi yang jarang berlaku.
Boulders Moving in Death Valley: A 70-Year Mystery Solved by Thin Ice and Weak Wind

Image: Imej AI: Alibaba Tongyi Wanxiang (wan2.2-t2i-flash)

Boulders Leaving Trails Without a Trace

In the desolate desert of Death Valley, California, lies a dry flatland called Racetrack Playa. Its surface is flat, cracked, and silent — except for dozens of large rocks scattered there. Some weigh up to 300 kilograms. Each leaves straight or curved tracks stretching from several meters to tens of meters — sometimes turning gently, sometimes as straight as a line on a field. No human or animal footprints. No signs of earthquakes or water flow. No evidence of mechanical activity. Since the first records in the early 20th century, this movement has been an unanswered geological mystery.

Hypotheses abounded: strong winds could move the rocks across the slippery surface; micro-tornadoes caused local air waves; even speculation about electromagnetic fields or extraterrestrial beings appeared in media reports. However, none of these hypotheses could be directly tested — because the movement had never been witnessed, and the trails often looked 'fresh' without any witnesses. More than 70 years passed without a single recording. Until 2011, the mystery remained intact: boulders were moving, but no one knew *how*.

Direct Recording After Two Years of Waiting

In 2011, a combined team of researchers from the Scripps Institution of Oceanography and NASA installed high-precision GPS and time-lapse cameras on 15 rocks at Racetrack Playa. They chose a strategic location: a flat area free of vegetation or obstacles, with active trail records. For two consecutive winters, no movement was recorded. Data showed absolute stability — until December 2013.

Within 48 hours after heavy rain and light snow, the temperature dropped suddenly that night. Water pooled on the playa surface, freezing into a thin layer of ice 2–5 mm thick. The next morning, sunlight softened the ice surface, while a consistent northwest wind blew at 5–10 meters per second. Recordings showed ice chunks breaking off, sticking to the bottom of the rocks, then slowly moving — dragging the rocks along with them across the very slick wet mud. The movement lasted from several minutes to two hours. More than 60 rocks moved simultaneously. Maximum speed: less than 0.5 meters per second. Longest distance: 224 meters.

Simple Physics, Complex Conditions

The final explanation is not an extraordinary process — but a rare combination of physical conditions. First, rain must be sufficient to flood the surface, but not so heavy as to wash away or submerge the rocks. Second, nighttime temperatures must drop below freezing to form a thin layer of ice — not thick, nor just frost. Third, daytime winds must be consistent and strong (around 15 km/h) to move the ice chunks attached to the rocks, but not so strong as to completely break the ice. Fourth, the playa surface must be smooth and uniform — fine mud that dries into a clay mirror — to ensure minimal friction.

This discovery was published in the journal *PLOS ONE* in July 2014. The study not only confirmed the ice-wind hypothesis proposed since the 1950s, but also provided the first empirical evidence. As stated in the research report, "The movement does not require extraordinary force — just precise synchronization between weather, surface, and timing." Further questions remain: why do some rocks move farther or more frequently? The answer likely lies in the shape of the rock base — flat-shaped rocks are easier to be "pulled" by ice — and their relative position to the dominant wind direction.

On Earth and Beyond: Traces That Invite Questions

This phenomenon is not just a local curiosity. Similar trails have been detected in satellite images in polar regions of Mars — particularly in dusty northern plains with seasonal carbon dioxide ice layers. Although the mechanism may differ (CO₂ ice is more fragile than water ice), the basic principle — a frozen layer moved by wind over a slick surface — remains relevant. On Earth, Racetrack Playa becomes a natural laboratory for understanding how microgeological processes can leave macroscopic traces that last for decades.

What is most impressive about the entire story is not its complexity, but its simplicity. A 70-year-old mystery was solved not with a new theory, but with careful observation of three common elements: water, ice, and wind. It reminds us that science often advances not through speculative leaps, but through perseverance in recording what *truly happens* — even if it only occurs once every ten years.