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  2. Galilean moons - Wikipedia

    en.wikipedia.org/wiki/Galilean_moons

    The moon does not form part of the orbital resonance that affects three inner Galilean satellites and thus does not experience appreciable tidal heating. [47] Callisto is composed of approximately equal amounts of rock and ices , which makes it the least dense of the Galilean moons.

  3. Moons of Jupiter - Wikipedia

    en.wikipedia.org/wiki/Moons_of_Jupiter

    The moons of Jupiter are listed below by orbital period. Moons massive enough for their surfaces to have collapsed into a spheroid are highlighted in bold. These are the four Galilean moons, which are comparable in size to the Moon. The other moons are much smaller.

  4. Exploration of Io - Wikipedia

    en.wikipedia.org/wiki/Exploration_of_Io

    So, the determination of its orbital period, along with those of the other Galilean satellites, was an early focus for astronomers. By June 1611, Galileo himself had determined that Io's orbital period was 42.5 hours long, only 2.5 minutes longer than the modern estimate. [12]

  5. Io (moon) - Wikipedia

    en.wikipedia.org/wiki/Io_(moon)

    Io (/ ˈ aɪ. oʊ /), or Jupiter I, is the innermost and second-smallest of the four Galilean moons of the planet Jupiter.Slightly larger than Earth's moon, Io is the fourth-largest moon in the Solar System, has the highest density of any moon, the strongest surface gravity of any moon, and the lowest amount of water by atomic ratio of any known astronomical object in the Solar System.

  6. Callisto (moon) - Wikipedia

    en.wikipedia.org/wiki/Callisto_(moon)

    Callisto is the outermost of the four Galilean moons of Jupiter. It orbits at a distance of approximately 1,880,000 km (26.3 times the 71,492 km radius of Jupiter itself). [3] This is significantly larger than the orbital radius—1,070,000 km—of the next-closest Galilean satellite, Ganymede.

  7. Europa (moon) - Wikipedia

    en.wikipedia.org/wiki/Europa_(moon)

    The first hints of a subsurface ocean came from theoretical considerations of tidal heating (a consequence of Europa's slightly eccentric orbit and orbital resonance with the other Galilean moons). Galileo imaging team members argue for the existence of a subsurface ocean from analysis of Voyager and Galileo images. [80]

  8. The moon has entered a new epoch, scientists say - AOL

    www.aol.com/moon-entered-geological-period...

    The moon also has features like a delicate exosphere composed of dust and gas and ice inside permanently shadowed areas that are vulnerable and could be disturbed by continued explorations, the ...

  9. Orbital resonance - Wikipedia

    en.wikipedia.org/wiki/Orbital_resonance

    The three-body Laplace resonance exhibited by three of Jupiter's Galilean moons. ... A Laplace resonance is a three-body resonance with a 1:2:4 orbital period ratio ...