The density of the moon is 3.346 g/cm3
either saturn or jupiter but your best bet is jupiter
Callisto, one of Jupiter's largest moons, has an average density of about 1.83 grams per cubic centimeter. This relatively low density indicates that Callisto is composed primarily of a mix of water ice and rocky material, suggesting a significant amount of its mass is made up of ice. Its density is lower than that of some other moons and planets, reflecting its unique composition and structure.
High crater density is associated with older surfaces
The density of Io, one of Jupiter's moons, is about 3.5 g/cm^3, which is similar to the density of Earth's mantle. This high density suggests that Io is primarily composed of rocky material with little to no ice present on its surface.
Mars has two moons, Phobos and Deimos, that are most similar in character to asteroids. They are irregularly shaped, have low density, and are believed to have been captured by Mars' gravitational pull.
Saturn has the lowest density, but it has more than 31 moons.
either saturn or jupiter but your best bet is jupiter
Yes. The density of the Galilean moons decreases with increasing distance from the planet. This decrease in density is likely due to the higher ice-to-rock ratio in the farther moons.
The greater the crater density, the older the surface must be old.
how is the crater density used in the relative dating
Callisto, one of Jupiter's largest moons, has an average density of about 1.83 grams per cubic centimeter. This relatively low density indicates that Callisto is composed primarily of a mix of water ice and rocky material, suggesting a significant amount of its mass is made up of ice. Its density is lower than that of some other moons and planets, reflecting its unique composition and structure.
High crater density is associated with older surfaces
The density of Io, one of Jupiter's moons, is about 3.5 g/cm^3, which is similar to the density of Earth's mantle. This high density suggests that Io is primarily composed of rocky material with little to no ice present on its surface.
The greater the crater density, the older the surface must be old.
Most but not all larger MOONS (bodies that orbit planets, moons, or asteroids) accreted in the same way that PLANETS did, assuming a variable density and a nearly spherical shape. Very large moons such as Titan have many of the characteristics of planets: vulcanism, atmospheres, and weather. Generally speaking, moons orbit planets in the same way that planets orbit stars.
No, the average density of Earth's Moon is about 3.3 g/cm^3, which is much lower than the average density of Earth's core. The core of the Earth is composed of mainly iron and nickel, giving it a much higher average density compared to the Moon.
Mars has two moons, Phobos and Deimos, that are most similar in character to asteroids. They are irregularly shaped, have low density, and are believed to have been captured by Mars' gravitational pull.