Olivine.
Melts are most likely produced by the adiabatic rise of mantle material at divergent plate boundaries, such as mid-ocean ridges. As mantle material rises due to the reduction in pressure, it undergoes decompression melting, leading to the formation of magma.
A mantle convection current is most likely to move upward at divergent plate boundaries such as mid-ocean ridges. Here, the heat from the Earth's interior causes the mantle material to rise, creating new crust as it cools and solidifies.
The mantle is predominantly composed of silicate minerals rich in magnesium and iron. It is also believed to contain other elements such as oxygen, silicon, and aluminum. The high temperatures and pressure in the mantle result in a semisolid or viscous state known as magma.
The carbon source for these mantle diamonds is most likely carbon trapped.
The carbon source for these mantle diamonds is most likely carbon trapped.
Granite
MANTLE
This material is most often referred to as magma.
you will find it in earths mantle because it is a kind of an igneous rock
Oxygen is not found in large quantities in the Earth's mantle as it is more abundant in the Earth's crust and atmosphere compared to the mantle. The most abundant elements in the Earth's mantle are oxygen, silicon, magnesium, and iron.
plague most likely to be found in Asia, America, Africa
most likely RNA