Аннотация
Besides Earth, Mars is the only planet with a record of resurfacing
processes and environmental circumstances that indicate the past
operation of a hydrologic cycle. However the present-day conditions
on Mars are far apart of supporting liquid water on the surface.
Although the large-scale morphology of the Martian channels and valleys
show remarkable similarities with fluid-eroded features on Earth,
there are major differences in their size, small-scale morphology,
inner channel structure and source regions indicating that the erosion
on Mars has its own characteristic genesis and evolution. The different
landforms related to fluvial, glacial and periglacial activities,
their relations with volcanism, and the chronology of water-related
processes, are presented.
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