The inner core is solid due to the immense pressure, despite its high temperature.

The mantle is solid but can flow slowly over geological time, behaving like a viscous fluid.

The Mantle is the thickest layer of the Earth, extending about 2900 km below the crust.

The Earth's crust is solid and is the thinnest layer, unlike the outer core which is in a liquid state.

The Earth's inner core is in a solid state, composed mainly of iron and nickel, despite the high temperature.

The outer core is in a liquid state, not solid, and is responsible for generating the Earth's magnetic field.

T-wave is not a recognized type of seismic wave; the main types are P-waves, S-waves, and surface waves (L-waves).

The Crust is the outermost layer of the Earth, lying above the mantle.

The Outer Core is the only layer that is liquid, composed mainly of molten iron and nickel.

The Mantle, particularly the asthenosphere, is responsible for the movement of tectonic plates due to convection currents.

The Inner Core is solid due to the immense pressure, despite its high temperature.

The Inner Core is the hottest part of the Earth, with temperatures reaching up to 5,700 degrees Celsius.

The mantle is the thickest layer of the Earth, making up about 84% of Earth's total volume.

The mantle is the thickest layer of the Earth, extending about 2900 km.

P-waves (primary waves) can travel through both solid and liquid layers of the Earth.