Because of the Earth's intense amount of pressure and heat
Volcanoes bring up material from deep within the earth. earth's interior is very hot.
No. Fossils tell us about what was living at or near the earths surface in the past, they do not tell us about the Earth's interior. When studying the Earth's interior, geologists look at micro gravity variations (which tell us about density differences in deep rocks), magnetic variations (which tell us a bit about the deep rocks composition) and most importantly seismic records (which tell us about the physical properties of the deep rocks). We also look for deep rocks that have been brought to the surface during the collision of continents (the roots of mountains) and volcanic events (such as diamond pipes).
no i do not know the answer
the deep crack in the earth's surface is the rift
A deep crack in the earth's surface is called a fault.
Heat from Earth's interior.
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.
Volcanoes bring up material from deep within the earth. earth's interior is very hot.
endogenic forces have their origin deep down in the earth's interior and they work from below
I donno. Your mom?
The Sun and in the case of deep sea vents, the heat and chemicals from Earth's interior.
The Sun and in the case of deep sea vents, the heat and chemicals from Earth's interior.
They can learn about conditions deep inside Earth, where these rocks formed. In addition, forces inside Earth sometimes blast rock to the surface from depths of more than 100 kilometers. These rocks provide clues about the interior.
No. Fossils tell us about what was living at or near the earths surface in the past, they do not tell us about the Earth's interior. When studying the Earth's interior, geologists look at micro gravity variations (which tell us about density differences in deep rocks), magnetic variations (which tell us a bit about the deep rocks composition) and most importantly seismic records (which tell us about the physical properties of the deep rocks). We also look for deep rocks that have been brought to the surface during the collision of continents (the roots of mountains) and volcanic events (such as diamond pipes).
They can learn about conditions deep inside Earth, where these rocks formed. In addition, forces inside Earth sometimes blast rock to the surface from depths of more than 100 kilometers. These rocks provide clues about the interior.
We can't actually visit the deep interior of the Earth, because the temperature and pressure would collapse any tunnel we dig or tube that we might insert.
Nope - it's too hot for anyone to go deep into the earth. Even the deepest mines are only about two miles below the surface.