This structure is true for most rocky planets in our solar system, including Earth.
Here's a breakdown:
* Crust: The outermost layer, relatively thin and composed of various types of rock.
* Mantle: The thickest layer, mostly solid rock, but can behave like a very viscous fluid over long periods.
* Core: The innermost layer, composed mainly of iron and nickel. The inner core is solid due to immense pressure, while the outer core is liquid.