At the mid-ocean ridge, two oceanic plates are moving apart. This movement creates a loss of overlying pressure at the rift. With the loss of pressure, hot ductile mantle rock rises to fill the void. As this hot rock rises, it undergoes decompression melting due to the new environment it is encountering. The now liquid rock is even more buoyant than the surrounding rock, and rises toward the surface.
Magma can use cracks that are already there on it way to the surface. If there are no cracks present, the magma can create them.
Liquid magma flows upward through cracks in rock because it is less dense than the surrounding material
Volcanoes erupt when pressure from inside the earth pushes magma through a weakness in the earth's surface. As more and more magma erupts, the volcano is formed and grows.
lava
Through cracks.
Magma can use cracks that are already there on it way to the surface. If there are no cracks present, the magma can create them.
1. Pressure in the magma chamber begins to build up. 2. The pressure forces the magma to go up through the vent. 3. Then it will erupt
Liquid magma flows upward through cracks in rock because it is less dense than the surrounding material
Volcanoes erupt when pressure from inside the earth pushes magma through a weakness in the earth's surface. As more and more magma erupts, the volcano is formed and grows.
lava
Through cracks.
the flow of magma in eath's crust is called lava.
push and a pull
Through cracks, holes or vents in the earths crust.
Pressure inside the earth forces the magma through cracks and other conduits in earth's crust.
A volcano is formed by pressure building up below the Earth's crust. Magma forces it way through weaknesses in the earth's crust. When the magma emerges it is called lava. When it cools, it solidifies into rock,or it may emerge though thin cracks,which are called fissure.Or it may be forced though wider pipes,that starts to build up, to a volcano.
Their source of energy and heat is gotten from molten magma by geothermal reactions. And they both erupt, under increased temperature and pressure through vents, holes, cracks or any other form of outlet or passage into the earth surface.