Magma is molten or partially molten rock beneath the earth's surface. A magma chamber is a space, often beneath a volcano, where magma collects.
This is called the magma chamber.
A magma chamber.
When the magma chamber is no longer pressurised. Note, this does not mean that the magma chamber can not refill and cause another eruption later. Thus there is a difference between the termination of an eruption and a volcano becoming extinct (ceasing to have any more eruptions ever).
Magma Chamber: underground pocket of molten rock
the difference is that outer magma is outside, and lava is inside.
This is called the magma chamber.
A magma chamber.
When the magma chamber is no longer pressurised. Note, this does not mean that the magma chamber can not refill and cause another eruption later. Thus there is a difference between the termination of an eruption and a volcano becoming extinct (ceasing to have any more eruptions ever).
Most often between 700 and 1300 degrees C..
In a magma chamber
Magma Chamber: underground pocket of molten rock
the difference is that outer magma is outside, and lava is inside.
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.
A crater can also be called a vent, and it is the funnel shaped opening at the top of a volcano which allows magma to escape as lava. The magma chamber is the hollow deep within the volcano which is supposedly linked to the core of the planet, bringing up molten rock from the middle of earth to be taken up the vent tube of the volcano to be released to the air.
A Magma Reservoir is a Magma Chamber so to speak. It is an underground cavity containing molten rock, esp. below a volcano.
A Magma Chamber is a space (that can change size) at a depth below a volcano in which magma can accumulate prior to an eruption. A volcanic vent is a conduit connecting the magma chamber to the surface. It is though this that the magma flows during an eruption.
a magma chamber