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the mantle plume There are two source of heat in the earth's interior. The main two sources are fire and breathing heat.
Scientists have determined what the interior of the earth is like through analyzing seismic or earthquake wave
Scientists use seismic waves to study Earth's interior. Seismic waves travel through the Earth and can be detected far from their source.
The deep interior of the Earth can be mapped using seismic waves. Natural earthquakes produce seismic signals which penetrate the Earth. Timing the arrival of these waves at various sites round the world, gives indication of the shape and the wave velocity in the Earths interior. Rather similar to the way a CAT scan can reveal the interior of a person.
They drill holes into the earth and collect rock samples.
From radioactivity in the Earth's interior.
no. radioactivity has been around since the earth's beginnings.
The primal heat from the deep interior of the Earth is mainly due to radioactive decay, with a small contribution due to gravity compression.
Mining helps us to understand the interiors of the earth because we can learn about how long the earth has been around and about different kinds of dirt.
The study of the earth's interior is important for man to understand his environment. It also helps to predict events that may occur on the earth's surface.
No. Earth's interior is so hot that you could not even make it through the crust.
Radioactivity within the Earth.
The earth's interior is called the core.
There's a slight chance one day we can, but that won't happen until our technology advances and we understand Earth's interior more.
It Does a man
Both. (the sun & radioactivity).
One thing is that now the correct age of the earth could be calculated. Before radioactivity was discovered the earth was though to have cooled enough to be only about 25 million years old by calculation. The discovery of radioactivity changed all that by increasing the heat the earth could radiate and so increasing the age of the earth dramatically.