Rocks become less dense when they melt
Magma is molten or partially molten rock beneath the earth's surface and is lighter than the surrounding rock so it tends to rise. As it moves upward, the magma encounters colder rock and begins to cool.
The hot plastic-like rocks in the asthenosphere rise towards the Earth's surface due to convection currents within the mantle. As the hotter, less dense material rises, it creates upward movement of magma, which can eventually lead to volcanic activity at the surface. This process is driven by the heat generated from radioactive decay and the heat left over from the formation of the Earth.
The sudden vibration in the plates inside the crust causes the earths crust to rise & fall.
The pressure exerted by rock layers above and below an aquifer that forces water to rise to the Earth's surface is called "hydrostatic pressure." This pressure is a result of the weight of the overlying rock and water, which can lead to artesian flow if the aquifer is confined. In such cases, water can rise spontaneously to the surface through wells or natural springs without the need for pumping.
The rock that churns deep beneath the Earth's surface is called "magma." It is a molten rock material that is located beneath the Earth's crust and can eventually rise to the surface as lava through volcanic eruptions.
What property of magam cause it to rise towaed earths surface?
It is a mountain.
During a volcanic eruption or on a constructive boundary
cuz
Through cracks, holes or vents in the earths crust.
Yes, magma tends to rise towards the earth's surface. It does so because once melted it becomes less dense.
Magma is less dense than the surrounding rock; as such, it will rise toward the surface.
because of the high pressure
Magma is molten or partially molten rock beneath the earth's surface and is lighter than the surrounding rock so it tends to rise. As it moves upward, the magma encounters colder rock and begins to cool.
density
Less/dence material rises
The intrusive granites which contain ores are the product of solidified magmas, most probably ones that have undergone significant magmatic differentiation.