is the temperature if the stiffer mantle above or below its melting point
the stiffer mantle's temperature is about from 3,500-5,000 degrees Celsius.
is the temperature if the stiffer mantle above or below its melting point
Below
i don’t know
When the temperature of a rock rises above its melting point it turns into magma, usually found in the mantle (found below the Earth's crust).
Mantle Is The Below Layer Of The Crust In Earth.
The melting point oof salt is far higher then the melting point of acetone.
Partially molten, plastic like, flowing layer located below the solid part of Earth's mantle is the Asthenosphere. The asthenosphere is mechanically weak and ductiley deforming region of the upper mantle.
If we're talking layers of the earth, that would be the upper mantle, below the crust.
is the temperature if the stiffer mantle above or below its melting point
is the temperature if the stiffer mantle above or below its melting point
Pressure from the thousands of miles of rock above.
When the temperature of a rock rises above its melting point it turns into magma, usually found in the mantle (found below the Earth's crust).
The crust is above the mantle and the mantle is below the crust
below because the mantle and crust
crust and upper mantle
The density of Earth's mantle varies depending on its depth. The part right below the crust has a density of about 3.4 grams per cubic centimeter while the lowest part of the mantle is 5.6 grams per cubic centimeter.
Subduction into the upper mantle and melting.
-- pure alcohol at room temperature -- mercury at room temperature -- oxygen below its boiling temperature -- iron above its melting temperature -- nitrogen below its boiling temperature -- salt above its melting temperature -- gold above its melting temperature -- any other element or compound that is not H2O, above its melting temperature and below its boiling temperature
Hot spots originate in the mantle, well below the Earth's surface.
Either the loss of confining pressure causing the melting point of the material to drop below the in-situ temperature or due to the presence of volatiles which enter the mantle where subduction occurs and also lower the melting point of the material.