Lably
Skip to content

Cheyava Falls

Martian rock noted for its potential life signs

  • 5 min read
  • 4 chapters

Related on Lably

Through Sulfate, Iron and Microorganism

Discovery

An unusual rock, named Cheyava Falls, was found in 2024 by NASA's Perseverance rover in Jezero crater. Cheyava Falls is characterized by large white calcium sulfate veins and bands of reddish material, indicative of hematite, a mineral that gives Mars its rusty color. The veins are "filled with millimeter-size crystals of olivine". The rock features millimeter-sized off-white splotches surrounded by black material, resembling "leopard spots". These spots contain iron and phosphate, elements often associated with microbial life. According to a seven-step scale called Confidence of Life Detection (CoLD) used by NASA astrobiologists, the rock is on Step One, showing "possible signal" of life.

The "arrowhead-shaped rock" was found at the northern edge of Neretva Vallis area, on 18 July 2024, and is 3.2 by 2 feet (0.98 m × 0.61 m). On 21 July 2024, Perseverance took a sample of the rock that became its 22nd core sample that can be delivered to Earth by a future mission. The rover made a "selfie" with a rock on 23 July 2024. The sample from Cheyava Falls is called the "Sapphire Canyon", while the formation where Cheyava Falls were found is called the "Bright Angel", a set of rocky outcrops on the northern and southern edges of Neretva Vallis, an ancient river valley 400 metres (1,300 ft) wide that was carved by water rushing into Jezero crater. The rock was studied by two instruments: the Planetary Instrument for X-Ray Lithochemistry (PIXL) and Scanning Habitable Environments with Raman and Luminescence for Organics and Chemicals (SHERLOC).

Beyond the nickname for a single sampled boulder, mission geologists now use "Cheyava Falls member" for a ~0.5 m-thick mudstone containing rare centimeter-scale olivine-rich horizons. At the northern Bright Angel–Margin-unit contact, it overlies the monomict, matrix-supported olivine granule conglomerate of the Fern Glen Rapids member and is itself overlain by the laminated mudstones of the Walhalla Glades member; the Tuff Cliff base is not exposed at this site.

Sign in to keep reading

3 more chapters are free with a Lably account.

More in Astronomy