It is Because one can't go inside earth since it is too hot. Hence, one has to use their evidence from rock samples and seismic waves.
the mantle the outer core and the inner core
core, mantle, inner crust, outer crust
Both the crust and inner core are layers of the Earth's structure. They are both part of the Earth's interior and are composed of different materials. The crust is the outermost layer of the Earth, while the inner core is the innermost layer.
The structure of Earth's interior is divided into layers: the crust, mantle, outer core, and inner core. Evidence for this structure comes from seismic waves generated by earthquakes, which travel through the Earth and are detected by seismometers. Variations in the speed and behavior of these waves provide information about the composition and density of the different layers.
Meteorites that originate from the asteroid belt can collide with Earth, carrying evidence of Earth's inner composition. By analyzing these meteorites, scientists can study the interior structure and composition of our planet.
The Inner core, outer core, mantle, and crust.
Rock. Their basic structure is probably similar to that of the Earth.
The Earth has a layered structure consisting of the inner core, outer core, mantle, and crust. The inner core is solid iron, the outer core is liquid iron, the mantle is mostly solid but can flow like a very thick liquid over long timescales, and the crust is the Earth's thin outer shell where we live. This structure is known as the "D-layered Earth model."
The inner core is chiefly formed of an alloy of Iron and Nickel with many many other elements occurring in trace amounts
To be precise, there is actually an outer core and an inner core. You can find the details in the Wikipedia article "Structure of the Earth".
The iron is in a crystalline structure under tremendous pressure.
An onion is a common object with a layered structure. It has concentric layers of skin surrounding the inner flesh of the vegetable.