Magma?
less dense than the material of the Earth's mantle
The Lithosphere is the ridged layer of Earth that is about 100 km think and generally less dense than the material below it. This layer is the tectonic plates the move along on the anthesphere.
Because it is less dense than the material that makes up the earth's crust, but more dense than the material that makes up the air.
Convective motion is typically observed in fluids, where warmer, less dense material rises and cooler, denser material sinks. This can occur in various arrangements, such as in a liquid heated from below or in a gas exposed to a temperature gradient. Additionally, convective motion may occur in Earth's mantle due to the heat flow from the core.
Earth is more dense.
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
This process is known as convection, where cooler, denser material sinks while warmer, less dense material rises. This movement of material within the Earth's mantle helps drive the motion of tectonic plates.
Heat from the Earth's core causes material in the mantle to heat up and become less dense. This warm, less dense material rises towards the Earth's surface. As it reaches the top of the mantle, the material cools and becomes denser, causing it to sink back down towards the core. This continuous cycle of rising and sinking material is known as mantle convection.
bends towards the normal.
Actually, heated materials are less dense. When heat is applied to a substance such as liquid, it becomes less dense. It is this less dense and heated material that rises because it weighs less. The part of the mantle that is more dense would be any substance that is cooling and is sinking down.
density is mass per unit volume so the less mass per cubic(what ever measure) the less buoyant.
Yes, that is correct. Magma is less dense than the solid rock around it, causing it to rise towards the surface through cracks and fractures in the Earth's crust. This movement occurs due to the buoyancy of the less dense magma compared to the denser surrounding rock.