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Cerberus Fossae

The Cerberus Fossae are a series of semi-parallel fissures on Mars formed by faults which pulled the crust apart in the Cerberus region. They are 1235 km across and centered at 11.28 °N and 166.37 °E. Their northernmost latitude is 16.16 °N and their southernmost latitude 6.23 °N. Their easternmost and westernmost longitudes are 174.72 °E and 154.43 °E, respectively. They can be seen in the Elysium quadrangle.

Gallery
Image:Cerberus Fossae THEMIS day IR v13.1.jpg|THEMIS mosaic of the Cerberus Fossae region. The Athabasca Valles outflow channels emerge from fissures at lower left. (The large image may be more easily viewed at full resolution with ZoomViewer.) Image:Cerberus Fossae from Themis.JPG|One of the Cerberus Fossae, as seen by THEMIS Image:Cerberus Fossae dark emission.JPG|Wind-blown material darkens areas around a Cerberus Fossae trough (scale bar for HiRISE image is 500 m) Image:Cerberus fossae.jpg|A 3 km section of a Cerberus Fossae fissure, taken by the Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) Image:Angular_Unconformity_in_Cerberus.JPG|Angular unconformity in the Cerberus Fossae, as seen by HiRISE (click on image to see the angles of the layers) Image:Troughs showing blue in Elysium Planitia.JPG|Portion of a trough (fossa) in Elysium, as seen by HiRISE under the HiWish program (blue indicates probably seasonal frost) == See also ==
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