How the Martian Moon Phobos Got Its Strange Grooves

Mars Moon Got Its Grooves from Rolling Stones

Much of Phobos’ surface is covered with strange linear grooves. New research bolsters that idea the boulders blasted free from Stickney crater (the large depression on the right) carved those iconic grooves. NASA/JPL-Caltech/University of Arizona

A new study bolsters the idea that strange grooves crisscrossing the surface of the Martian moon Phobos were made by rolling boulders blasted free from an ancient asteroid impact.

The research, published in Planetary and Space Science, uses computer models to simulate the movement of debris from Stickney crater, a huge gash on one end of Phobos’ oblong body. The models show that boulders rolling across the surface in the aftermath of the Stickney impact could have created the puzzling patterns of grooves seen on Phobos today.

“These grooves are a distinctive feature of Phobos, and how they formed has been debated by planetary scientists for 40 years,” said Ken Ramsley, a planetary science researcher at Brown University who led the work. “We think this study is another step toward zeroing in on an explanation.”

Phobos’ grooves, which are visible across most of the moon’s surface, were first glimpsed in the 1970s by NASA’s Mariner and Viking missions. Over the years, there has been no shortage of explanations put forward for how they formed. Some scientists have posited that large impacts on Mars have showered the nearby moon with groove-carving debris. Others think that Mars’ gravity is slowly tearing Phobos apart, and the grooves are signs of structural failure.

Rolling Boulder Simulations

Computer models traced the possible paths of Stickney ejecta.

Still, other researchers have made the case that there’s a connection between the grooves and the Stickney impact. In the late 1970s, planetary scientists Lionel Wilson and Jim Head proposed the idea that ejecta — bouncing, sliding, and rolling boulders — from Stickney may have carved the grooves. Head, a professor in Brown’s department of Earth, Environmental and Planetary Sciences, was also a co-author of this new paper.

For a moon the size of the diminutive Phobos (27 kilometers or 17 miles across at its widest point), Stickney is a huge crater at 9 kilometers (5.6 miles) across. The impact that formed it would have blown free tons of giant rocks, making the rolling boulder idea entirely plausible, Ramsley says. But there are also some problems with the idea.

For example, not all of the grooves are aligned radially from Stickney as one might intuitively expect if Stickney ejecta did the carving. And some grooves are superposed on top of each other, which suggests some must have already been there when superposed ones were created. How could there be grooves created at two different times from one single event? What’s more, a few grooves run through Stickney itself, suggesting that the crater must already have been there when the grooves formed. There’s also a conspicuous dead spot on Phobos where there are no grooves at all. Why would all those rolling boulders just skip one particular area?

To explore those questions, Ramsley designed computer models to see if there was any chance that the “rolling boulder model” could recreate these confounding patterns. The models simulate the paths of the boulders ejected from Stickney, taking into account Phobos’ shape and topography, as well as its gravitational environment, rotation, and orbit around Mars.

Ramsley said he had no expectations for what the models might show. He wound up being surprised at how well the model recreated the groove patterns seen on Phobos.

“The model is really just an experiment we run on a laptop,” Ramsley said. “We put all the basic ingredients in, then we press the button and we see what happens.”

The models showed that the boulders tended to align themselves in sets of parallel paths, which jibes with the sets of parallel grooves seen on Phobos. The models also provide a potential explanation for some of the other more puzzling groove patterns.

How Mars Moon Got Its Grooves

The simulations show how boulders take a flying leap over one particular area of Phobos, explaining why it’s devoid of grooves.

The simulations show that because of Phobos’ small size and relatively weak gravity, Stickney stones just keep on rolling, rather than stopping after a kilometer or so like they might on a larger body. In fact, some boulders would have rolled and bounded their way all the way around the tiny moon. That circumnavigation could explain why some grooves aren’t radially aligned to the crater. Boulders that start out rolling across the eastern hemisphere of Phobos produce grooves that appear to be misaligned from the crater when they reach the western hemisphere.

That round-the-globe rolling also explains how some grooves are superposed on top of others. The models show that grooves laid down right after the impact were crossed minutes to hours later by boulders completing their global journeys. In some cases, those globetrotting boulders rolled all the back to where they started — Stickney crater. That explains why Stickney itself has grooves.

Then there’s the dead spot where there are no grooves at all. That area turns out to be a fairly low-elevation area on Phobos surrounded by a higher-elevation lip, Ramsley says. The simulations showed that boulders hit that lip and take a flying leap over the dead spot, before coming down again on the other side.

“It’s like a ski jump,” Ramsley said. “The boulders keep going but suddenly there’s no ground under them. They end up doing this suborbital flight over this zone.”

All told, Ramsley says, the models answer some key questions about how ejecta from Stickney could have been responsible for Phobos’ complicated groove patterns.

“We think this makes a pretty strong case that it was this rolling boulder model accounts for most if not all the grooves on Phobos,” Ramsley said.

Reference: “Origin of Phobos grooves: Testing the Stickney Crater ejecta model” Kenneth R.Ramsley and James W.Head, 16 November 2018, Planetary and Space Science.
DOI: 10.1016/j.pss.2018.11.004

4 Comments on "How the Martian Moon Phobos Got Its Strange Grooves"

  1. Interesting. If you click on the second article under “MORE ON SCITECHDAILY”, The article titled “Mars’ Moon Phobos Shows Signs of Structural Failure”, and look at the comments, I came to the same conclusion about rolling impact debris, back in 2015.

  2. Seems to me they’ve missed the obvious… if the object that impacted Phobos was a conglomeration of smaller boulders, liuke the majority of the asteroids recently observed, then many of the grooves would have been carved by loose material being thrown from the asteroid in the impact, cascading down from the peripheral edges of the asteroid at a shallow angle to Phobos’ surface (the edges of what is now Stickney crater).

    This would also explain why there are grooves on top of other grooves; Boulders thrown from an asteroid would come from the area immediately around the edges of the impacting surface as well as farther back around the asteroid’s sides. Ifthe asteroid were travelling across the face of phobos rather than a dead-aligned hit, then this debris would rain down from a variety of angles, dependent upon the original trajectories of both bodies.

    So, rather than being caused by ejecta from the point of impact, the boulders that created the scars are more likely to be evidence of a cascade of asteroidal debris thrown loose by the impact.

  3. Rocks. Yeah. Rocks. That’ed do it. Except there ain’t no damn rocks. Look.

    Even if there was rocks, you would still have another problem with your explanation, and behind it a third. Friction is going to stop a rock pretty quick, and Phobos escape velocity is 25 mph. If your rock is moving fast enough to do anything it’s moving too fast to do anything. To sum up, the evidence (rocks) that would necessarily have to be on Phobos is not present and you theory is physically impossible, therefore I doubt it.

  4. Instead of spending billions to ruin another planet, lets repair EARTH!

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