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Viking mosaic of Planum Boreum and surrounds
Viking mosaic of Planum Boreum and surrounds
False color HiRISE image of a side of the Chasma Boreale, a canyon in the polar ice cap. Light browns are layers of surface dust greys and blues are l
False color HiRISE image of a side of the Chasma Boreale, a canyon in the polar ice cap. Light browns are layers of surface dust greys and blues are layers of water and carbon dioxide ice. Regular geometric cracking is indicative of higher concentrations of water ice.
False color HiRISE view of water ice layers in Olympia Rupes, believed by scientists to be preserving climate conditions of Mars dating back millions
False color HiRISE view of water ice layers in Olympia Rupes, believed by scientists to be preserving climate conditions of Mars dating back millions of years. Depicted width: 1.3 km (3⁄4 mi)
November 27, 2011
November 27, 2011
Vastitas Borealis is the large low elevation area surrounding 70°N.
Vastitas Borealis is the large low elevation area surrounding 70°N.
Surface of Mars, as seen by Phoenix. The ground is shaped into polygons which are common where the ground freezes and thaws.
Surface of Mars, as seen by Phoenix. The ground is shaped into polygons which are common where the ground freezes and thaws.
Olympia Planitia Dunes, as seen by HiRISE. Gypsum has been detected here by MRO.
Olympia Planitia Dunes, as seen by HiRISE. Gypsum has been detected here by MRO.
Patterned ground was once called fingerprint terrain because it looked like giant fingerprints. The dark dots are actually chains of low mounds. The c
Patterned ground was once called fingerprint terrain because it looked like giant fingerprints. The dark dots are actually chains of low mounds. The center circular feature is a ring of dark boulders on the rim of a buried crater. Picture from Mars Global Surveyor.