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    Home»Space»Titanic Asteroid 20x Larger Than Dinosaur-Killer Reshaped Solar System’s Largest Moon
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    Titanic Asteroid 20x Larger Than Dinosaur-Killer Reshaped Solar System’s Largest Moon

    By Kobe UniversitySeptember 3, 2024No Comments5 Mins Read
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    Ganymede Asteroid Impact
    Kobe University Naoyuki Hirata was the first to realize that the location of an asteroid impact on Jupiter’s moon Ganymede is almost precisely on the meridian farthest away from Jupiter. This implied that Ganymede had undergone a reorientation of its rotational axis and allowed Hirata to calculate what kind of impact could have caused this to happen. Credit: Naoyuki Hirata

    A colossal asteroid impact on the Jupiter moon Ganymede not only reshaped its physical landscape but may have also altered its rotation, drawing parallels with cataclysmic events on Earth and Pluto.

    Approximately 4 billion years ago, an asteroid hit Ganymede. Now, a Kobe University researcher has discovered that the Solar system’s biggest moon’s axis shifted as a result of the impact. This confirmed that the asteroid was around 20 times larger than the one that ended the age of the dinosaurs on Earth, and caused one of the biggest impacts with clear traces in the Solar System.

    Ganymede: An Unusual Moon

    Ganymede is the largest moon in the Solar System, bigger even than the planet Mercury, and is also interesting for the liquid water oceans beneath its icy surface. Like the Earth’s moon, it is tidally locked, meaning that it always shows the same side to the planet it is orbiting and thus also has a far side. On large parts of its surface, the moon is covered by furrows that form concentric circles around one specific spot, which led researchers in the 1980s to conclude that they are the results of a major impact event.

    “The Jupiter moons Io, Europa, Ganymede, and Callisto all have interesting individual characteristics, but the one that caught my attention was these furrows on Ganymede,” says the Kobe University planetologist Naoyuki Hirata. He continues, “We know that this feature was created by an asteroid impact about 4 billion years ago, but we were unsure how big this impact was and what effect it had on the moon.”

    Ganymede Major Impact Event
    On large parts of its surface, the Jupiter moon Ganymede is covered by furrows (right) that form concentric circles around one specific spot (left, red cross), which led researchers in the 1980s to conclude that they are the results of a major impact event. Credit: Naoyuki Hirata

    The Enigmatic Furrows of Ganymede

    Data from the remote object is scarce making research very difficult, and so Hirata was the first to realize that the purported location of the impact is almost precisely on the meridian farthest away from Jupiter. Drawing from similarities with an impact event on Pluto that caused the dwarf planet’s rotational axis to shift and that we learned about through the New Horizons space probe, this implied that Ganymede, too, had undergone such a reorientation.

    Because Hirata is a specialist in simulating impact events on moons and asteroids, this realization allowed him to calculate what kind of impact could have caused this reorientation to happen.

    Ganymede Topography Furrow System
    Distribution of furrows and the location of the center of the furrow system shown in the hemisphere that always faces away from Jupiter (top) and the cylindrical projection map of Ganymede (bottom). The gray regions represent geologically young terrain without furrows. Furrows (green lines) exist only on geologically old terrains (black regions). Credit: Naoyuki Hirata

    Unraveling Ancient Impacts

    In the journal Scientific Reports, the Kobe University researcher now published that the asteroid probably had a diameter of around 300 kilometers, about 20 times as large as the one that hit the Earth 65 million years ago and ended the age of the dinosaurs, and created a transient crater between 1,400 and 1,600 kilometers in diameter. (Transient craters, widely used in lab and computational simulations, are the cavities produced directly after the crater excavation and before material settles in and around the crater.)

    According to his simulations, only an impact of this size would make it likely that the change in the distribution of mass could cause the moon’s rotational axis to shift into its current position. This result holds true irrespective of where on the surface the impact occurred.

    Exploring Ganymede’s Mysteries Further

    “I want to understand the origin and evolution of Ganymede and other Jupiter moons. The giant impact must have had a significant impact on the early evolution of Ganymede, but the thermal and structural effects of the impact on the interior of Ganymede have not yet been investigated at all. I believe that further research applying the internal evolution of ice moons could be carried out next,” explains Hirata.

    Interesting for its subsurface oceans, Ganymede is the final destination of ESA’s JUICE space probe. If everything goes well, the spacecraft will enter orbit around the moon in 2034 and will make observations for six months, sending back a wealth of data that will help answer Hirata’s questions.

    Reference: “Giant impact on early Ganymede and its subsequent reorientation” by Naoyuki Hirata, 3 September 2024, Scientific Reports.
    DOI: 10.1038/s41598-024-69914-2

    This research was funded by the Japan Society for the Promotion of Science (grants 20K14538 and 20H04614) and the Hyogo Science and Technology Association.

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