The moon consists of three main layers: the crust, mantle, and core, each with unique properties.
The crust is thin and rocky, varying in thickness from about 30 to 40 kilometers.
Discussing plans can also help prevent potential conflicts over lunar territory and resources.
The moon’s core is believed to be partially molten, which contributes to its magnetic field.
Understanding these layers provides insights into the moon’s formation and geological history.
The moon’s interior is essential for studying how other celestial bodies, including Earth, formed.
Ongoing research and lunar missions continue to uncover more about what’s inside the moon.