The Earth's mantle is a layer of hot, solid rock between the crust and the core. It is composed of silicate minerals rich in iron and magnesium, and is responsible for convection currents that drive plate tectonics. The mantle's temperature and pressure conditions vary with depth, with the upper mantle being cooler and more rigid compared to the lower mantle.
The two main parts of the Earth's mantle are the upper mantle and the lower mantle. The upper mantle sits below the Earth's crust and extends to a depth of about 410 miles, while the lower mantle extends from about 410 miles to 1,800 miles depth.
The three main levels of the Earth are the core, mantle, and crust. The core is divided into the inner core and outer core, the mantle is located between the core and crust, and the crust is the outermost layer where we live.
Mantle is part of the Earth's lithosphere.
Tectonic plates are floating on the magma (semi-molten rocks) of the mantle layer. Therefore, they form the crust layer of the Earth.
If anything is rock-solid, it will result in a flat landscape. This will mean that there will be no plateaus, deep sea trenches, volcanoes or mountains if the mantle were solid rock.
heat and pressure
Crust, mantle, and core
Crust, mantle, and core
Crust, mantle, and inner core.
Crust, mantle, and inner core.
mantle
you will find it in earths mantle because it is a kind of an igneous rock
the earths mantle is very hot were cornstarch is not hot at all
the earths mantle is very hot were cornstarch is not hot at all
The Earth's mantle has two main layers: the upper mantle and the lower mantle. These layers are distinguished by differences in their composition, temperature, and behavior. The upper mantle extends from the crust to a depth of about 410 miles (660 kilometers), while the lower mantle extends from about 410 miles (660 kilometers) to approximately 1,800 miles (2,900 kilometers) below the Earth's surface.
The three parts that make up the Earths mantle are the crust, core, and mantle.
the mantle plume There are two source of heat in the earth's interior. The main two sources are fire and breathing heat.