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it depends on the deepth
An erupting volcano is an example of the release of pressure from the earth's interior.
Because of the Earth's intense amount of pressure and heat
Temperature and pressure increase massively from the Earth's surface to the centre of the Earth. At the inner core, the pressure is so great that iron is solid, even at such high temperatures.
Simply because there is no way to analyse or study it directly. Much of what we know about the Earth's core has to be 'guess work' - as the temperature and pressure is far too high for today's technology to provide definitive answers.
the temp gets hotter and the pressure gets greater
Lol, do his homework urself. anywayz its pressure and temperature
it depends on the deepth
The melting temperature of materials is dependent on the pressure that is applied, whereby the higher the pressure, the higher the melting temperature. As such the rocks in the mantle are experiencing such a high pressure, that their melting point is driven up beyond the temperature within the Earth's mantle so they remain solid.
An erupting volcano is an example of the release of pressure from the earth's interior.
Increases with depth
it depends on the deepth
it depends on the deepth
it depends on the deepth
In the interior of stars, where matter is at an extreme temperature and pressure. Also, wherever there are radioactive isotopes - for example, on Earth - these will gradually decay.
Temperature
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.