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Grad Students Find Missing Link in Early Martian Water Cycle

  • Researchers Mohammad Afzal Shadab and Eric Hiatt, pursuing their graduate studies at The University of Texas at Austin, have created a model to examine how water moved through early Mars’ surface down to underground aquifers.
  • Their computer model simulates how water took between 50 and 200 years to seep from Mars’ surface down to an aquifer about a mile underground.
  • The findings suggest much of Mars’ ancient water was trapped underground and less was available to replenish surface lakes, lakes, or the atmosphere through evaporation.
  • Their model suggests that the underground water may have formed a reservoir at least 300 feet deep, and Hiatt noted that the water infiltrating the Martian crust was not escaping into space.
  • This research revises Mars’ early hydrology picture, implying limited surface water stability and supporting future missions focused on subsurface water and astrobiology.
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On Mars, each relief, each shade of colour, can revive hypotheses of several decades old. Failing to find rivers or seas there, scientists trace the least clues of a past or present activity of water on Mars, whether in rocks, ice or ground patterns. Among the most intriguing traces, some dark marks observed on the sides of craters have long sown doubt. Behind their apparent fluidity, these formations conceal an unexpected process, much drier th…

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In a new study, led by scientists from the University of Bern and the University of Brown, half a million strange marks were mapped on the surface of Mars, to determine whether water would be a key factor in the appearance of stripes that have intrigued researchers for years. The study, cited by the European Space Agency (ESA), details that a global map with almost 500,000 strip characteristics was generated on the red planet, obtaining the larg…

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Phys.org broke the news in United Kingdom on Monday, May 19, 2025.
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