There’s a Strange Cloud on Mars Right Now, and It’s Just Hanging Around

There's a Strange Cloud on Mars Right Now, and It's Just Hanging Around

October 26, 2018 – For more than a month now, a European orbiter circling Mars has been watching a long, plume-like cloud on the Red Planet.


The cloud has remained in place over a mountain called Arsia Mons near the Martian equator since Sept. 13, according to a statement released by the European Space Agency (ESA). But that location is just a coincidence, the agency adds. No volcanic process is producing the cloud — the volcano hasn’t been active in about 50 million years, scientists believe.

Arsia Mons is the southernmost of three volcanoes (collectively known as Tharsis Montes) on the Tharsis bulge near the equator of the planet Mars. To its north is Pavonis Mons, and north of that is Ascraeus Mons. The tallest volcano in the solar system, Olympus Mons, is to its northwest. Its name comes from a corresponding albedo feature on a map by Giovanni Schiaparelli, which he named in turn after the legendary Roman forest of Arsia Silva.

The same spacecraft, called Mars Express, and its predecessors have spotted similar clouds on at least three previous occasions, and those structures formed around the same time in the Martian year. And that’s not a coincidence, the ESA wrote.

There's a Strange Cloud on Mars Right Now, and It's Just Hanging Around

The cloud is full of water ice, the agency continued, created by air flow along the side of the volcano. This means the feature is what scientists call an orographic or lee cloud. That also happens to mean that the cloud changes over the course of the day as atmospheric patterns on Mars change.

Scientists watching the cloud have noticed that it grows over the course of the morning, stretching along the equator. It may also be affected by the dust still in the atmosphere from the massive dust storm that engulfed Mars earlier this year.

The caldera of Arsia Mons was formed when the mountain collapsed in on itself after its reservoir of magma was exhausted. There are many other geologic collapse features on the mountain’s flanks. The caldera floor formed around 150 Mya ago.

The three Tharsis Montes, together with some smaller volcanoes to the north, form a rather straight line. It has been proposed that these are the result of plate tectonics, which on Earth makes chains of “hot spot” volcanoes

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