it causes the water to become heated beyond boiling point yet still remain liquid because the magma is under a lot of pressure and there is no opening for the very hot water to turn to steam i am 50% sure
Increasing pressure pushes the magma upwards. This rising pressure can be caused by many different things.
When pressure from rising magma cracks underground rock, it can cause seismic activity and result in earthquakes. The cracks in the rock can create pathways for magma to reach the surface, leading to volcanic eruptions. Additionally, the release of pressure can trigger landslides or avalanches in the surrounding area.
Rock flows at great pressure and temperature Rock flows like putty in this inhospitable environment of great pressure and temperature. Rock that surrounds rising magma deforms, allowing passage of the magma. This partially molten magma eventually rises to the base of the continental crust. The upper continental crust is more rigid than the mantle, so the magma must force its way upward through cracks or by melting surrounding crustal
Yes, rising magma can become less fluid as it decompresses. When magma rises towards the surface, the pressure decreases, which can cause dissolved gases to come out of the magma and create gas bubbles. These gas bubbles can increase the viscosity of the magma, making it less fluid.
As magma rises, the gases contained within expand due to the decrease in pressure on them as they rise. This creates bubbles that float through the magma, Like the sudden decrease in pressure on the gas in a carbonated beverage when opening, it's container releases a mass of rising bubbles.
Increasing pressure pushes the magma upwards. This rising pressure can be caused by many different things.
When pressure from rising magma cracks underground rock, it can cause seismic activity and result in earthquakes. The cracks in the rock can create pathways for magma to reach the surface, leading to volcanic eruptions. Additionally, the release of pressure can trigger landslides or avalanches in the surrounding area.
Rock flows at great pressure and temperature Rock flows like putty in this inhospitable environment of great pressure and temperature. Rock that surrounds rising magma deforms, allowing passage of the magma. This partially molten magma eventually rises to the base of the continental crust. The upper continental crust is more rigid than the mantle, so the magma must force its way upward through cracks or by melting surrounding crustal
Yes, rising magma can become less fluid as it decompresses. When magma rises towards the surface, the pressure decreases, which can cause dissolved gases to come out of the magma and create gas bubbles. These gas bubbles can increase the viscosity of the magma, making it less fluid.
As magma rises, the gases contained within expand due to the decrease in pressure on them as they rise. This creates bubbles that float through the magma, Like the sudden decrease in pressure on the gas in a carbonated beverage when opening, it's container releases a mass of rising bubbles.
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.
As magma rises, the gases contained within expand due to the decrease in pressure on them as they rise. This creates bubbles that float through the magma, Like the sudden decrease in pressure on the gas in a carbonated beverage when opening, it's container releases a mass of rising bubbles.
Sedimentary rocks could become metamorphic rocks if they are exposed to extreme heat and pressure deep in the Earth's crust. The rocks could come to the surface by volcanic activity or rising magma.
Igneous rocks can change into metamorphic rocks from great heat and pressure as all other rocks can, melt into magma, the molten rock, and erode into sediment, which are rock fragments.
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