The average temperature is 5400 ºF (3000ºC),
This is in the mantle or upper mantle.
Mantle plumes are in the mantle, BELOW the Earth's crust. The circulation of heat from the lower mantle to the upper mantle can cause "hot spots" in the overlying crust, heating the magma in the areas.
Lithosphere
The most outer solid portion of the planet Earth is the crust.
Your answer would be melted rock, iron, and nickel
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
Inner Mantle: The average temperature is about 3000ºC Outer Mantle: The average temperature is about 2200ºC
Temperature: The upper mantle is cooler than the lower mantle. Composition: The upper mantle is more silicate-rich and less dense compared to the lower mantle. Physical properties: The upper mantle is more rigid and brittle, while the lower mantle is more ductile and capable of flow.
This is in the mantle or upper mantle.
This is in the mantle or upper mantle.
The average temperature is 5400 ºF (3000ºC),
700 degrees celsius
410km
Temperature ranges from 500 to 900 C, 932 to 1652 F.
The mantle is subdivided into the upper mantle and the lower mantle. The upper mantle is closer to the Earth's surface and consists of solid rock that can flow slowly over long periods of time. The lower mantle is located beneath the upper mantle and is more rigid due to higher pressure and temperature.
The upper mantle is mainly composed of minerals such as olivine, pyroxene, and garnet. These minerals form under high temperature and pressure conditions in the Earth's interior, contributing to the solid composition of the upper mantle.
Yes, the transition zone is a region in the Earth's mantle located between the upper and lower mantle. It is marked by changes in temperature, pressure, and mineral composition.