The most widely accepted model of Earth's interior is the layered model, which divides the Earth into several distinct layers: the crust, mantle, outer core, and inner core. The crust is the thin, solid outer layer, while the mantle is a thick, semi-solid layer that flows slowly. Beneath the mantle lies the outer core, which is liquid and composed mainly of iron and nickel, and the inner core, which is solid and extremely hot, also primarily made of iron and nickel. This model is supported by seismic wave data and studies of Earth's magnetic field.
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The outer core
The deepest scientist have been able to study earths interior depth is 12,262 meters
Seismic waves
body waves
Seismic data
The earths interior is cold
The image likely shows the layered model of Earth's interior, consisting of the crust, mantle, outer core, and inner core. This model is based on seismic data and helps in understanding the composition and structure of our planet.
A body wave is a seismic wave that travels through Earths interior.
it depends on the deepth
Volcanoes
Volcanoes
The movements in the liquid inner core.
The movements in the liquid inner core.
isaac newton
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The outer core