Reconciling Channel Formation Processes with the Nature of Elevated

  • HESPERIAN OUTFLOW
  • Published 2009

Abstract

Introduction: Most outflow systems in the southern highlands of Mars head at elevations below the 1500 m level considered to be the uppermost level compatible with aquifer recharge beneath the south polar cap [1-3], and these lower systems are widely interpreted as the products of such recharge [e.g., 2]. However, some outflow systems head at greater… (More)

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