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This forms a geyser.
If enough water pressure build under the surface of the ground, the water can burst through cracks in the surface forming a geyser.
Geyser
The flow aloft aids the formation of cyclones at the surface by pushing air into the vector. This increases the strength, speed and velocity and builds up the pressure as the cyclone develops.
Because as you get closer to the surface of the earth, the more air that is on top of you. At the top of the atmosphere, there is no air, and everything is a vacuum, where you have no weight. When you get close to the earth, the weight of the air builds until it when you're at the very lowest point of the earths surface, all the air in the atmosphere above you is pressing down.
This forms a geyser.
This forms a geyser.
Geyser
If enough water pressure build under the surface of the ground, the water can burst through cracks in the surface forming a geyser.
Geyser
Geyser
Pressure builds up from under the Earth in the moho or asthenosphere from molten lava and the Earth's crust is pushed and eventually cracks and lava seeps out through the crack therefore forming a volcano.
pressure builds up in the earth and pushes the magma up to the surface.
from being under the mantle the gas pressure builds up and forces magma out forming a hot spot.
Volcanoes are essentially holes in the earths surface through which magma and lava can erupt. when pressure builds up below the earths crust, magma is then forced violently out of the volcanoes.
As the magma approches the surface, has gate trapped below, and pressure builds up. Once the pressure is to great to be contained, there is a violent eruption
no, if by clog up you mean the top of the lava pool has cooled , the hot molten rock underneath it will keep melting the cooled rock in a never ending cycle. ^incorrect. "Volcanic Plugs (aka "volcanic necks" or "lava necks")" do happen (just wiki it...). When magma hardens in the vent of a volcano, it can plug it up. Sometimes pressure builds up under it, resulting in an explosive eruption.