The subduction and melting of oceanic crust replaces magma in the earth.
Magma that is low in silica flows readily and produces dark-colored lava. Therefore magma that is low in silica produces Pahoehoe lava. This is called mafic or basaltic magma.
Convergent boundaries produce volcanoes. Volcanoes form when an oceanic plate and a continental plate converge, causing the oceanic plate to subduct. The subduction causes a magma chamber to form which feeds the volcano when it erupts.
subduction, which is when one tectonic plate is pushed down beneath another tectonic plate.
Igneous rock, if heated sufficiently by subduction processes will melt to form magma.
The subduction and melting of oceanic crust replaces magma in the earth.
Andesite can be found around volcanoes with magma of intermediate composition, usually near subduction zones.
Magma that is low in silica flows readily and produces dark-colored lava. Therefore magma that is low in silica produces Pahoehoe lava. This is called mafic or basaltic magma.
magma forms in mantle above slab
Convergent boundaries produce volcanoes. Volcanoes form when an oceanic plate and a continental plate converge, causing the oceanic plate to subduct. The subduction causes a magma chamber to form which feeds the volcano when it erupts.
subduction, which is when one tectonic plate is pushed down beneath another tectonic plate.
Low viscosity mafic magma.
It was liquid rock (magma) which solidified after an extrusion or eruption. Crustal rocks can re-dissolve into magma during subduction of oceanic crust.
not related subduction is when some one sexually seduces you Doh!! Ok wow um your thinking about seduction. This person is asking subduction lol. ok so anyways, convection is when the upper mantle pushes magma through an opening in the crust, which becomes new land on ocean ridges. Subduction is when two plates clash and one slides under the other and turns to magma in the upper mantle.
Igneous rock, if heated sufficiently by subduction processes will melt to form magma.
The transition form magma to rock is a process of cooling.
Rhyolitic magma. Boom! Basaltic magma is its exact opposite, while andesitic magma is in between the two.