Because it becomes in contact with oxygen which combines with the original composition. There fore changing the composition and temperature.
The opening in the earth crust which magma rise to the surface are Volcanoes
A hot spot is an area where magma from deep within the mantle rises through the crust in the middle of a tectonic plate, creating volcanic activity and forming a chain of volcanic islands or seamounts. The Hawaiian Islands are a well-known example of hot spot activity.
Magma rises through the crust due to differences in density between the magma and surrounding rock. Magma is less dense than the solid surrounding rock, so it moves upwards through cracks and fractures in the crust. As it rises, magma can also be driven by pressure differences and heat from the Earth's mantle.
Rhyolitic magma typically forms beneath continental crust due to high silica content and low temperature. The silica-rich composition leads to viscous magma, which is more common in continental settings compared to oceanic crust where magma tends to be more basaltic and less viscous.
At ocean-continent plate boundaries, the rising magma can interact with overlying continental crust, which can cause changes in its composition. This interaction can lead to the assimilation of continental rocks by the magma, altering its chemical composition before it reaches the surface. This process can produce volcanic rocks with unique characteristics compared to other types of magma.
The movement of magma through the Earth's crust is known as intrusion.
magma can be classified into two,magma of granitic composition(originates from lower continental crust) and magma of basaltic composition (which originates from upper mantle).Both can form intrusive rocks.
The opening in the earth crust which magma rise to the surface are Volcanoes
Yes. If the magma stops in a magma chamber long enough it can change composition through two mechanisms:fractional crystalization, where minerals with lower melting points crystallize and sink to the bottom og the chamberMelting of srrounding rock, which then become part of the magma.
A hot spot is an area where magma from deep within the mantle rises through the crust in the middle of a tectonic plate, creating volcanic activity and forming a chain of volcanic islands or seamounts. The Hawaiian Islands are a well-known example of hot spot activity.
Magma rises through the crust due to differences in density between the magma and surrounding rock. Magma is less dense than the solid surrounding rock, so it moves upwards through cracks and fractures in the crust. As it rises, magma can also be driven by pressure differences and heat from the Earth's mantle.
Rhyolitic magma typically forms beneath continental crust due to high silica content and low temperature. The silica-rich composition leads to viscous magma, which is more common in continental settings compared to oceanic crust where magma tends to be more basaltic and less viscous.
At ocean-continent plate boundaries, the rising magma can interact with overlying continental crust, which can cause changes in its composition. This interaction can lead to the assimilation of continental rocks by the magma, altering its chemical composition before it reaches the surface. This process can produce volcanic rocks with unique characteristics compared to other types of magma.
magma comes from the outer core and when an earthquake or something happends, a crack froms and the pressure of lava shoots up like a geyser.
Once magma breaks through the earths crust it is called"lava"
lava
lava