Magma is a product of earth processes. To say it has a purpose may be a subjective statement.
**The first question this raises is: what exactly is this "material from the inside"? On our planet, it's magma, fluid molten rock. This material is partially liquid, partially solid and partially gaseous.
magma production around plate boundaries. This interplatevolcanic activity is caused by unusually hot mantle material forming in the lower mantle and pushing up into the upper mantle. The mantle material, which forms a plume shape that is from 500 to 1000 km wide, wells up to create a hot spot under a particular point on the earth. Because of the unusual heat of this mantle material, it melts, forming magma just under the earth's crust. The hot spot itself is stationary; but as a continental plate moves over the spot, the magma will create a string of volcanoes, which die out once they move past the hot spot. The Hawaii volcanoes were created by such a hot spot, which appears to be at least 70 million years old.
So what happens to the magma formed by these processes? We saw that the magma produced at ocean ridges just hardens to form new crust material, and so doesn't produce spewing land volcanoes. There are a few continental ridge areas, where the magma does spew out onto land; but most land volcanoes are produced by subduction zone volcanism and hot spot volcanism.
When the solid rock changes form to a more liquid rock material, it becomes less dense than the surrounding solid rock. Because of this difference in density, the magma pushes upward with great force (for the same reason the helium in a balloon pushes up through the denser surrounding air and oil pushes upward through denser surrounding water). As it pushes up, its intense heat melts some more rock, adding to the magma mixture.
The magma keeps moving through the crust unless its upward pressure is exceeded by the downward pressure of the surrounding solid rock. At this point, the magma collects in magma chambers below the surface of the earth. If the magma pressure rises to a high enough level,or a crack opens up in the crust, the molten rock will spew out at the earths surface.
basaltic,andesitic,rhyolitic
Magma
Magma Design Automation was created in 1997.
Examples of magma include basaltic magma, andesitic magma, and rhyolitic magma. Basaltic magma is the most common type and is associated with oceanic volcanic activity. Andesitic magma has intermediate silica content and is found at convergent plate boundaries. Rhyolitic magma is highly viscous and contains high amounts of silica, commonly found in continental volcanic regions.
This type of magma is called basaltic magma. It has a lower silica content, which gives it a darker color compared to other types of magma. Basaltic magma is commonly associated with volcanic activity at divergent plate boundaries.
When magma and ash cannot leave the mantle fast enough when it has particularly a lot of pressure, a side vent is an alternative way to let out the magma and ash.
An acid magma or a granitic magma.
There is no purpose to volcanoes. Volcanoes are simply areas where magma from the Earth's core branches out to the crust of the Earth where it is contained before pressure makes it burst. Several volcanoe eruptions have caused islands to form, but this is not the direct purpose of a volcanoe; but rather more an odd occurence.
magma
This is called the magma chamber.
Before lava reaches the surface it is called magma.
basaltic,andesitic,rhyolitic
Molten rock under the surface is called "magma". When magma reaches the surface it is called "lava".
The Magma Rock is unavailable during normal gameplay - it can only be obtained through the use of a cheating device like the Action Replay. If obtained, it does nothing. In Platinum, its purpose is revealed to be similar to the Red Chain's purpose: to control the legendary of Stark Mountain, Heatran.
Magma is molten rock beneath the Earth's surface, while a magma chamber is a reservoir where magma is stored before it rises to the surface as lava. Essentially, magma is the molten rock itself, while a magma chamber is the space within the Earth where magma is stored.
Baslatic magma is hotter.
No. Magma is not alive.