SOLAR SYSTEM · 2014-05-22
At the Edge of a Polar Cap
At Mars’s north polar edge, layered terrain and frost create boundaries that can resemble terrestrial geology.

What to observe
- Trace the sharp boundary between light and dark terrain.
- Compare broad layers with the finer surface texture.
Explanation
Mars Reconnaissance Orbiter recorded a chasm at the north polar cap edge, where strong downslope winds help carry sediment toward the Olympia Undae dune field.
Color method
This spacecraft image is processed to make surface structure legible; color should be read as imaging data, not as an unaided-eye view from the ground.
Why it matters
Landforms alone do not identify a world. Instrument, location and scale turn visual similarity into evidence.
Sources and credits
Asset credit: NASA/JPL-Caltech/Univ. of Arizona / JPL