mantle is earth's layers there is 4 important layers crust, mantle, outer and inner core. Yet magma is volcano and more into that (:
Karina:
The mantle is below the plates.
No, solid rock located deep in the mantle is not called magma. Magma is molten rock that is found beneath the Earth's surface in the mantle and crust. Solid rock in the mantle is known as the lithosphere.
Magma is stored in the mantle layer of the Earth, which is located between the crust and the outer core. Magma is formed in the mantle due to the high temperatures and pressures present in this layer. When magma rises towards the Earth's surface, it can lead to volcanic eruptions.
mantle
Igneous rock
The upper mantle is harder than the lower mantle
Yes, the lower mantle is also known as the mesosphere. It is the region of Earth's mantle that lies between the upper mantle and the outer core.
Mantle is part of the Earth's lithosphere.
The mantle is below the plates.
Molten rock in any of Earth's layers is called magma. The mantle is actually composed of solid, but very hot and plastic-like rock.
The melted mineral material in the mantle is called magma.
No, solid rock located deep in the mantle is not called magma. Magma is molten rock that is found beneath the Earth's surface in the mantle and crust. Solid rock in the mantle is known as the lithosphere.
Magma forms in the mantle layer of the Earth. It is a molten rock material that originates from the partial melting of rocks in the upper mantle. Magma can rise to the Earth's surface through volcanic eruptions.
magma comes from volcanoes, water doesnt, unless its volvic
Melted material that rises from the mantle is called magma. Once magma reaches the Earth's surface, it is then referred to as lava.
Magma is stored in the mantle layer of the Earth, which is located between the crust and the outer core. Magma is formed in the mantle due to the high temperatures and pressures present in this layer. When magma rises towards the Earth's surface, it can lead to volcanic eruptions.
Magma comes from the melting of material in the crust or upper mantle.