Despite attempts, getting through the crust has proven impossible with current economic and technological constraints. Temperatures vary from 900 to 1600 degrees F at the Mohorovicic discontinuity, the boundary between the crust and the upper mantle. And the lithostatic pressure at the line dividing the crust and the mantle is estimated to be up to 116,000 pounds per square inch. It is not surprising that drill bits and shafts would be under tremendously high stresses. Geologists look into the interior by indirect means; examination of deep sourced volcanic material, meteorite and moon material, and behaviors of seismic waves. Much can also be inferred by computer modeling of Earth's gravitational influence and magnetic field.
The structure of the planet cannot be directly observed; the interior structure of the earth includes an outer core of molten liquid that would destroy any probes sent to explore it.
It is difficult to study the structure of the Earth because it is divided by several layers. There are areas which are extremely hot and other areas filled with water.
wee cant dig into the earth very far or go there so we have to rely on indirect methods such as using seismic waves
We can't see earth's interior, making it more difficult to determine.
The Earth's interior cannot be directly observed. Scientists must rely on indirect data to make hypotheses about the interior. Indirect evidences include meteorite composition, volcanic ejecta, intrusive igneous rock exposed through erosion, and the behavior of seismic waves as they travel through the Earth. They porduce youmama and fu yall It is difficult to determine Earth's inner structure because of all the layers. The Earth altogether is made up of seven layers.
It's approximately (3,963)miles down to the earths core.
inner core is the earths center .
The earth's inner core is 3160 kilometers beneath the earths surface. The inner core is a solid ball of nickel-iron alloy.
the inner core
The Earth's interior cannot be directly observed. Scientists must rely on indirect data to make hypotheses about the interior. Indirect evidences include meteorite composition, volcanic ejecta, intrusive igneous rock exposed through erosion, and the behavior of seismic waves as they travel through the Earth. They porduce youmama and fu yall It is difficult to determine Earth's inner structure because of all the layers. The Earth altogether is made up of seven layers.
The inner core is chiefly formed of an alloy of Iron and Nickel with many many other elements occurring in trace amounts
the inner part of earths core
inner core outer core lower mantle upper mantle lithosphere
It's approximately (3,963)miles down to the earths core.
inner core is the earths center .
The radious of the inner core is 1,220km(760miles).
The movements in the liquid inner core.
The earth's inner core is 3160 kilometers beneath the earths surface. The inner core is a solid ball of nickel-iron alloy.
The movements in the liquid inner core.
a solid ball of iron
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