When considering a relatively small object, like a sphere of molten iron the size of a Basketball, there is hardly a density gradient from center to edge. If the size of the object we are considering grows to the scale of our planet, or larger, gravity plays a strong role in the density variation from center to edge.
For instance, it is unknown for certain in what state of the core of Jupiter resides. Jupiter is mostly hydrogen and is the largest planet in our system. Even though it is a gas giant, it is speculated that the core is molten hydrogen, possibly solid at the very center. This is considered because of the tremendous weight present at the center of the huge ball of gas. The Sun takes it a step further. It, too, is mostly hydrogen, but it is such a tremendously large body that the core is under enough pressure to start and sustain nuclear fusion.
Two things play a role in determining the state of matter; temperature and pressure. Scale is what allows us to see density gradients within a volume of the same substance.
The inner planets' surface materials differ from the outer planets because the inner planets have rocky surfaces and the outer planets have gas surfaces.
They have rocky surfaces.
The outer planets are mostly composed of gases and the inner planets are mostly made of rock, metals.
The inner planets are smaller and rockier than the outer planets which are made mostly of gases. Plus they are on different sides of the asteroid belt.
The inner planets are Mercury, Venus, Earth and Mars. The outer planets (they are separated by the asteroid belt) are Jupiter, Saturn, Uranus, and Neptune. The outer planets are different than the inner planets because the outer planets are not solid. They are all made up of gas. However, the inner planets are rocky and hard.
The inner planets' surface materials differ from the outer planets because the inner planets have rocky surfaces and the outer planets have gas surfaces.
the inner mantle is hotter than the outer mantle.
outer core is liquid whereas the inner core is solid
Inner planets
the inner mantle is different than the outer mantle because the inner mantle is hotter than the outer mantle.
They have rocky surfaces.
The outer planets are mostly composed of gases and the inner planets are mostly made of rock, metals.
Inner planets differ from outer planets because they have rocky core (excepting Pluto), and the are much smaller than outer planets, which are bigger and take more time to orbit Sun than inner planets because of their location. Outer planets are farther from the Sun than inner planets.
As the names suggest, the inner planets are closer to the Sun than the outer planets.
The inner planets are smaller and rockier than the outer planets which are made mostly of gases. Plus they are on different sides of the asteroid belt.
The outer skin is called the rind. The inner white material is called the pith.
No because the inner planets are made of rocky and hard substances and the outer planets are made of gassy lighter substances.