Magma is more buoyant than lithospheric rock, and as such it will push toward the surface. On the continents, magma in intrusions can follow weaknesses in the crustal rock to reach the surface, or in some cases, simply melt its way through from the heat delivered by the intrusion. At divergent plate boundaries, where the lithospheric plates are pulling apart, hot rock from the mantle rises and melts from decompression melting, filling the space left from the parting plates. At so-called hotspots, such as the Hawaiian volcanic mountain chain, magma plumes are thought to rise up from the mantle-core boundary and burn through the moving lithospheric plates, creating first submarine volcanoes, then islands.
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The magma is under pressure from the surround unmelted rocks due to differences in densities. This pressure forces the magma up through preexisting cracks in the rocks. In many cases though there are no preexisting cracks for the magma to move through. When this happens, if the pressure is greater the the force need to break the rock then the magma will make new cracks and contuie to rise. If the pressure is not great enough then the magma will stop rising and pond to form sills or magma chambers until it completely crystallizes or has enough pressure to rise.
the Earth's mantle. As temperatures increase with depth, rocks partially melt to form magma. This magma can rise towards the surface through volcanic activity.
Magma rises towards the Earth's surface due to differences in density between the magma and surrounding rock, as well as pressure changes. This movement can eventually lead to volcanic eruptions.
The rock that melts underneath the Earth is called magma. Magma is formed from the melting of the Earth's mantle and can rise to the surface to form igneous rocks when it solidifies.
Magma is the name given to molten underground rock. It can be found beneath the Earth's surface in the mantle and can eventually rise to the surface through volcanic activity.
Andesitic magma is typically sourced from the partial melting of subducted oceanic crust and overlying mantle at convergent plate boundaries. This process results in the formation of a magma with intermediate silica content, giving rise to andesitic volcanic rocks.
magma rises up out of a volcano by the build up of pressure
liquid magma is dangerous and tastes bad
magma rises and cools
Magma is less dense than the surrounding rock; as such, it will rise toward the surface.
Because of the asthenosphere.
yes. it goes upward through a 'pipe' that connects to the magma chamber.
Magma rises because it is less dense than the rock around it.
cuz
the Earth's mantle. As temperatures increase with depth, rocks partially melt to form magma. This magma can rise towards the surface through volcanic activity.
Volcanic mountains
During a volcanic eruption or on a constructive boundary
Heated magma rises because it is less dense than the surrounding solid rock. As magma rises to the surface, it can create volcanic eruptions.