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Image of the Sinus Sabaeus Quadrangle (MC-20). Most of the region contains heavily cratered highlands. The northern part includes Schiaparelli Crater.
Image of the Sinus Sabaeus Quadrangle (MC-20). Most of the region contains heavily cratered highlands. The northern part includes Schiaparelli Crater.
Wislicenus Crater Floor, as seen by HiRISE. Erosion on floor has made layers visible.
Wislicenus Crater Floor, as seen by HiRISE. Erosion on floor has made layers visible.
Close up of layers in eroded deposits on the floor of Bouguer Crater, as seen by HiRISE. This image is in a different part of the crater than the prev
Close up of layers in eroded deposits on the floor of Bouguer Crater, as seen by HiRISE. This image is in a different part of the crater than the previous image.
Layers in Monument Valley. These are accepted as being formed, at least in part, by water deposition. Since Mars contains similar layers, water remain
Layers in Monument Valley. These are accepted as being formed, at least in part, by water deposition. Since Mars contains similar layers, water remains as a major cause of layering on Mars.
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Layers in a crater inside the Schiaparelli basin as seen by MGS.
Layers in a crater inside the Schiaparelli basin as seen by MGS.
Layers in a crater inside the Schiaparelli basin, as seen by HiRISE.
Layers in a crater inside the Schiaparelli basin, as seen by HiRISE.
Circular structures on floor of Schiaparelli basin, as seen by HiRISE under HiWish program.
Circular structures on floor of Schiaparelli basin, as seen by HiRISE under HiWish program.
Close-up of circular structure from previous image. Streaks are also visible.
Close-up of circular structure from previous image. Streaks are also visible.