it is 500-900 drgrees get back to you on the other thang
Its hot
the composition of the mantle is peridotite
The mantle is made of ultramafic igneous rock.
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
Earths mantle is less dense and very hot. The mantle is 2885km thick.
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the composition of the mantle is peridotite
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The temperature of the mantle is greater at Point B than Point A. The temperature of the mantle is determined by its depth which is greater at Point B than Point A. The deeper the mantle the hotter and more pressurized it is and so the temperature at Point B will be greater than at Point A.Temperature can also be affected by other factors such as the composition of the mantle and the presence of radioactive elements. In this case since both points are in the same area and have similar composition the temperature will be determined by the depth.To summarize the temperature of the mantle is greater at Point B than Point A because it is deeper and thus more pressurized and hot.
The mantle is made of ultramafic igneous rock.
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
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peridotite
it is dead bodies
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
describe introduction in a composition
Earths mantle is less dense and very hot. The mantle is 2885km thick.
core mantle crust