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New Models Suggest Ancient Mars Was Warm, Wet, and Shaped by Precipitation

Simulations show rain and snow likely formed Martian valleys, but the planet's ancient heat source remains a mystery.

An artist's depiction of water rushing into Mars' Jezero Crater (Credit: NASA/JPL-Caltech)

Overview

  • Recent research published in the Journal of Geophysical Research: Planets supports the theory that rain and snow, rather than ice melt, shaped Mars's valley networks.
  • Digital landscape evolution models show valley head distributions align more closely with precipitation scenarios than ice cap melting models.
  • NASA's Perseverance Rover findings in Jezero Crater, such as large boulders requiring deep flowing water, further bolster the precipitation hypothesis.
  • The study highlights unresolved questions about how Mars maintained sufficient warmth for sustained precipitation under the faint young Sun.
  • Researchers suggest Mars's preserved surface offers insights into early Earth conditions, as both planets may have shared similar environments billions of years ago.