The Medusae Fossae Formation is a broad geological unit of uncertain origin on the planet Mars. It is named for the Medusa of Greek mythology. "Fossae" is Latin for "trenches". Located roughly at 5°S 213°E / 5°S 213°E / -5; 213, it straddles the highland - lowland boundary near the Tharsis and Elysium volcanic areas.
The Medusae Fossae Formation is a soft, easily eroded deposit that extends for nearly 1,000 km along the equator of Mars. Sometimes, the formation appears as a smooth and gently undulating surface, however in places it is wind-sculpted into ridges and grooves. Radar imaging has suggested that the region may contain either extremely porous rock (for example volcanic ash) or deep layers of glacier-like ice deposits amounting to about the same quantity as is stored in Mars' south polar cap. Using a global climate model, a group of researchers headed by Laura Kerber found that the Medusae Fossae Formation could have easily been formed from ash from the volcanoes Apollinaris Mons, Arsia Mons, and possibly Pavonis Mons. Another evidence for a fine-grained composition is that the area gives almost no radar return. For this reason it has been called a "stealth" region. The formation is divided into three subunits (members) that are all considered to be Amazonian age, the youngest era in martian geological history.
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Plateau made up of Medusae Fossae materials and rootless cones, as seen by HiRISE. Rootless cones are caused by lava interacting with water ice. Wakes are caused by lava flowing over a source of steam.
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Layers in lower member of Medusae Fossae Formation, as seen by HiRISE. Location is Aeolis quadrangle.
Read more about Medusae Fossae Formation: Inverted Relief, Yardangs
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