the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
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.
Most volcanoes form at either convergent or divergent plate boundaries. Volcanoes at convergent plate boundaries form when one plate slides under another, taking seawater with it. This causes the rock in the mantle to melt as the melting point drops. This new magma can rise to form volcanoes.At divergent plate boundaries the crust is thing, which lowers pressure on the mantle, causing some material to melt.
tectonic plates, where magma from the mantle rises to the surface. At convergent boundaries, one plate sinks beneath the other, creating intense heat and pressure that can lead to volcanic activity. At divergent boundaries, plates move apart, allowing magma to well up and form new crust.
i am not sure
Convergent and divergent boundaries melt rock in the upper mantle while transform boundaries do not. Convergent boundaries that involve at least one oceanic plate form subduction zones, where an oceanic plate plunges into the mantle. Volatiles carried into the mantle lower the melting point of the rock there, allowing magma to form.At divergent boundaries the crust becomes thinner. This reduces pressure on the upper mantle, thus lowering melting points and generating magma.Transform boundaries have no such means of producing magma.
Volcanoes form on tectonic plates at plate boundaries where magma from the Earth's mantle can rise to the surface. This typically occurs at divergent or convergent plate boundaries where there is movement and interaction between the plates, leading to volcanic activity.
Rhyolite can form at convergent plate boundaries where magma is generated from the melting of continental crust material being subducted. Subduction zones can provide the necessary conditions for the production of rhyolitic magma, resulting in the formation of rhyolite.
They form on convergent boundaries.