The Arsia Mons Elongated Cloud is a wisp of water ice that appears downwind of the 20-km- (12.4-mile) tall Arsia Mons volcano — the southernmost in a trio of giant Martian shield volcanoes known collectively as Tharsis Montes — in the Martian southern hemisphere’s spring and summer.
The post Giant Martian Cloud May Form Through Physics Never Before Seen in Planetary Atmosphere appeared first on Sci.News: Breaking Science News.
