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posted by janrinok on Sunday November 24, @07:12PM   Printer-friendly
from the missed-it-by-that-much dept.

A promising explanation is a near-miss by an asteroid:

Earth and Mars are the only two rocky planets in the solar system to have moons. Based on lunar rock samples and computer simulations, we are fairly certain that our Moon is the result of an early collision between Earth and a Mars-sized protoplanet called Theia. Since we don't have rock samples from either Martian moon, the origins of Deimos and Phobos are less clear. There are two popular models, but new computer simulations point to a compromise solution.

Observations of Deimos and Phobos show that they resemble small asteroids. This is consistent with the idea that the Martian moons were asteroids captured by Mars in its early history. The problem with this idea is that Mars is a small planet with less gravitational pull than Earth or Venus, which have no captured moons. It would be difficult for Mars to capture even one small asteroid, much less two. And captured moons would tend to have more elliptical orbits, not the circular ones of Deimos and Phobos.

An alternative model argues that the Martian moons are the result of an early collision similar to that of Earth and Theia. In this model, an asteroid or comet with about 3% of the mass of Mars impacted the planet. It would not be large enough to have fragmented Mars, but it would have created a large debris ring out of which the two moons could have formed. This would explain the more circular orbits, but the difficulty is that debris rings would tend to form close to the planet. While Phobos, the larger Martian moon, orbits close to Mars, Deimos does not.

This new model proposes an interesting middle way. Rather than an impact or direct capture, the authors propose a near miss by a large asteroid. If an asteroid passed close enough to Mars, the tidal forces of the planet would rip the asteroid apart to create a string of fragments. Many of those fragments would be captured in elliptical orbits around Mars. As computer simulations show, the orbits would shift over time due to the small gravitational tugs of the Sun and other solar system bodies, eventually causing some of the fragments to collide. This would produce a debris ring similar to that of an impact event, but with a greater distance range, better able to account for both Phobos and Deimos.

While this new model appears to be better than the capture and impact models, the only way to resolve this mystery will be to study samples from the Martian moons themselves. Fortunately, in 2026 the Mars Moons eXploration mission (MMX) will launch. It will explore both moons and gather samples from Phobos. So we should finally understand the origin of these enigmatic companions of the Red Planet.

Journal Reference: Kegerreis, Jacob A., et al. "Origin of Mars's moons by disruptive partial capture of an asteroid." Icarus 425 (2025): 116337.


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  • (Score: 3, Interesting) by gznork26 on Sunday November 24, @09:04PM

    by gznork26 (1159) on Sunday November 24, @09:04PM (#1383197) Homepage Journal

    The video shows that at one part of the suggested process there was a disk of fragments orbiting Mars. That sounds like the description of a ring. The ring then gradually coalesced into Phobos and Deimos. So now I'm curious how long ago that would have been, and how long the ring persisted. Imagine living on a planet with a ring that gradually thinned as material built the moons. What sort of mythology might develop in that situation? depending on how long the process takes, it might be something that the people realize when comparing images (however they are made) across time.

    --
    Khipu were Turing complete.
  • (Score: 3, Interesting) by Snotnose on Monday November 25, @01:17AM

    by Snotnose (1623) on Monday November 25, @01:17AM (#1383223)

    One of the first books I remember reading was 2 kids going to Mars' moons, and one was a hollow alien artifact (of the moons smartass). This would have been mid to late 60s. Now that we know how light the smaller moon is I wonder if Georgie boy [wikipedia.org] might of been onto something.

    --
    It's just a fact of life that people with brains the size of grapes have mouths the size of watermelons. -- Aunty Acid
  • (Score: 2) by DannyB on Monday November 25, @05:06PM (1 child)

    by DannyB (5839) Subscriber Badge on Monday November 25, @05:06PM (#1383293) Journal

    From TFA . . .

    While this new model appears to be better than the capture and impact models, the only way to resolve this mystery will be to study samples from the Martian moons themselves. Fortunately, in 2026 the Mars Moons eXploration mission (MMX) will launch. It will explore both moons and gather samples from Phobos.

    From Google . . .

    The largest moon is Phobos and it's gravity is 0.0057 m/s², which means you could throw a rock hard enough for it to escape it's gravity. It's not very dense unfortunately.

    But if you threw that rock, would you still be able to remain standing on that "moon"?

    --
    Santa maintains a database and does double verification of it.
    • (Score: 2) by gznork26 on Tuesday November 26, @05:06PM

      by gznork26 (1159) on Tuesday November 26, @05:06PM (#1383429) Homepage Journal

      I love the visual that made for me. Watching the astronaut kind-a stand on the surface. Bending down to get the rock starts them summersaulting. Then, while slowly spinning over the surface, they do some quick calculations and throw the rock at just the right time. The reaction sends them back to the surface, which they bounce off and float away until the small gravity finally pulls them down, too far away from the landing craft to know which way they went.

      --
      Khipu were Turing complete.
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