Evidence For Explosive Volcanism On Mars May Rewrite Its Ancient History

Was this type of explosive activity once seen on Mars? NurPhoto/Getty Images
Robin Andrews 15 Jun 2016, 15:20

As far as we can tell, there is no longer any volcanic activity on Mars, but there are plenty of tell-tale signs showing that it once happened. One recent study, for example, revealed that Mars was tipped over by as much as 20° by a profuse period of volcanism that forced much of its deeper mantle up onto the crust.

Now, the intrepid Curiosity rover has managed to detect the presence of tridymite within the Gale Crater, hinting at the presence of powerful, explosive volcanism on the ancient Martian surface. Writing in the Proceedings of the National Academy of Science, the research team led by both NASA and the California Institute of Technology imply that the ancient history of Mars needs to be partly rewritten thanks to this discovery.

“It's really nifty, but we were shocked,” Richard Morris, the NASA scientist who led the study, told CBC News. “Something is going on on Mars that we don't fully appreciate.”

content-1465990318-tridymite-tabulars-ocAncient volcanism on Mars is generally considered to have been mostly effusive, calm, and prolonged, which tends to form shield volcanoes, like Olympus Mons. Thanks to Mars’ low atmospheric pressure, it’s likely that any fire fountaining out of one would have reached considerable heights compared to their terrestrial equivalents, but this doesn’t count as explosive volcanism.

For volcanism to be defined as “explosive,” the magma must be thick, gloopy (“viscous”), and full of gas. These two traits, generally speaking, will produce greater depressurization events when the eruptions occur, and will thereby produce more violent and sometimes cataclysmic eruptions. More viscous magma is typically associated with stratovolcanoes on Earth, such as Mount Fuji or Mount St. Helens.

In addition, plate tectonics are required to produce volcanic eruptions that are conventionally explosive; without this mechanism, viscous, silica-rich magma – the type that may feature minerals like tridymite – cannot form, and many geologists still consider Mars to have never experienced it.

Image in text: A common form of tridymite, from the Eifel region of Germany. Fred Kruijen/Wikimedia Commons; CC BY-SA 3.0 nl

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