Arsia Mons Volcano
This image taken by the High Resolution Stereo Camera (HRSC), shows a zone of collapse features on the southern flank of the giant shield volcano Arsia Mons located at 239° E longitude and 10° S latitude.
The image was taken from an altitude of about 400 kilometres during orbit 263 on 2 April 2004. The original image resolution was 20 metres per pixel, but the version shown here has been reprocessed to reduce the volume of data for use on the internet. The image covers an area of 80 kilometres by 105 kilometres.
The total height difference in the land surfaces in this scene is about 7 kilometres, and some individual collapse pits have a depth of 2 kilometres. The pits probably formed when lava erupted from the side of Arsia Mons. When lava, or molten rock, finds its way to the surface, it produces several veins and chambers. These slowly empty as the lava erupts and runs down the volcano flanks.
Some of the lava reaching the surface cools down and becomes solid, often building a roof over the emptied chamber. The resulting voids collapse due to the weight of the overlying material. At several places, the walls of the pits have been modified by later landslides.The overall trend of the collapse zone runs from the south-west to the north-east, following exactly a giant zone of crustal weakness in the Tharsis region, along which the three large volcanoes Arsia, Pavonis and Ascraeus Montes are aligned.
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