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Mars may one day have rings similar to Saturn's famous halo, new research suggests.
In a few tens of millions of years, the Red Planet may completely crush its innermost moon, Phobos, and form a ring of rocky debris, according to the new work. Phobos is moving closer to Mars every year, meaning the planet's gravitational pull on the satellite is increasing. Some scientists have theorized that Phobos will eventually collide with Mars, but the new research suggests that the small moon may not last that long.
"The main factor affecting whether Phobos will crash into Mars or break apart is its strength," Tushar Mittal, a graduate student at the University of California, Berkeley and one of the authors of the new research paper, told Space.com by email. "If Phobos is too weak to withstand increasing tidal stresses, then we expect it to break apart."
The two moons of Mars, Phobos and Deimos, are named after the children of the god Ares, the Greek counterpart to Mars, the Roman god of war.
The larger, inner moon, Phobos, is only about 14 miles (22 kilometers) wide, and orbits the Red Planet rapidly, rising and setting twice each Martian day. The tiny moon is slowly moving toward its host — drawing closer to Mars by 6.5 feet (2 meters) every century — which may result in a dramatic crash into the Martian surface within 30 million to 50 million years, previous research has shown.
But after simulating the physical stresses that Mars exerts on Phobos, Mittal and co-author Benjamin Black, a postdoctoral researcher at UC Berkeley, see a different fate for Phobos. Their research suggests that instead of going out in a single, enormous impact, the moon will be pulled apart by the Martian gravity.
On Earth, the gravitational pull of the moon causes the rise and fall of ocean tides. Although the moon has no oceans, Earth's gravitational pull is still referred to as "tidal forces."
Phobos and other moons in the solar system also feel tidal stress from their hosts. Black and Mittal studied the "strength" of the Martian satellite, including characteristics like composition and density, to determine how much planetary stress the moon could withstand.
After comparing it to several meteorites on Earth, they concluded that Phobos today is made up of porous, heavily damaged rock and is likely the same throughout its interior.
"The moon is probably neither a complete rubble pile, nor completely rigid," Mittal said. "The porosity of Phobos may have helped it survive."
After simulating the stresses caused by the tidal pull of Mars, the pair found that the moon would break up over the course of 20 million to 40 million years, forming a ring of debris around the planet.