Yes. That is what the asthenosphere is.
bhill
The magma forms sills and magma chambers.
Large underground lava deposits are called magma chambers. These chambers are reservoirs of molten rock beneath the Earth's surface that can feed volcanic eruptions when the magma rises to the surface through volcanic vents.
Magma is less dense than rock and is buoyant due to this density difference. It will seek out any weaknesses in the rock above it to reach the surface.
Yes. That is what the asthenosphere is.
Yes. That is what the asthenosphere is.
No, the asthenosphere is a semi-fluid layer of the Earth's mantle located below the lithosphere. Magma chambers form in the Earth's crust where magma accumulates before rising to the surface as lava during volcanic activity.
Hydrothermal vents: Minerals can form when hot water rich in dissolved minerals rises from beneath the Earth's crust and comes into contact with cold seawater. This rapid cooling causes minerals to precipitate and accumulate around the vent openings. Magma chambers: Minerals can also form when molten rock (magma) cools and solidifies underground in magma chambers. As the magma cools, minerals crystallize out from the molten rock and form distinct mineral formations.
Magma chambers
Magma Chambers allow the oceanic plate to rise in the form of of a volcano with no testicles 8===D
bhill
The magma forms sills and magma chambers.
Large underground lava deposits are called magma chambers. These chambers are reservoirs of molten rock beneath the Earth's surface that can feed volcanic eruptions when the magma rises to the surface through volcanic vents.
Huge magma chambers grow under the earth and cannot be released through volcanic activity, until the pressure is too much and the magma pushes out through the earth's crust.
Magma is less dense than rock and is buoyant due to this density difference. It will seek out any weaknesses in the rock above it to reach the surface.
magma chambers. These reservoirs can hold large volumes of magma and are important in the formation of volcanic eruptions.