volcanoes are caused by subduction. it could be an oceanic plate sub-ducting under a continental plate which would result in a coastal volcano or it could be an oceanic plate sub-ducting under another oceanic plate, which would result in a volcanic island.
When an oceanic plate collides with a continental plate, the denser oceanic plate usually subducts beneath the less dense continental plate due to the difference in densities. This can lead to the formation of deep oceanic trenches, volcanic arcs, and mountain ranges on the continental plate due to the intense tectonic forces generated during the collision.
When an oceanic plate collides with a continental plate, the denser oceanic plate is usually subducted beneath the less dense continental plate. This subduction process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding continental plate.
The oceanic plate is denser than the continental plate due to its composition of heavier mafic rock. This density difference causes the oceanic plate to sink below the continental plate in a process known as subduction.
In an oceanic-oceanic subduction boundary, one oceanic plate subducts beneath another oceanic plate. This process can result in volcanic island arcs being formed. In an oceanic-continental subduction boundary, an oceanic plate subducts beneath a continental plate. This can lead to the formation of volcanic mountain ranges on the continental plate.
When an oceanic plate and a continental plate collide, it forms a volcano. The oceanic plate subducts underneath the continental plate. As the oceanic plate slides underneath, a magma chamber is formed. This magma chamber is what feeds the volcano.
Volcanoes cannot be formed at a continental rift, due to the fact that a volcano cannot form between two continental plates: it normally forms when one continental plate and an oceanic plate collide. Normally, a volcano forms when one continental and one oceanic plate collides. The denser oceanic plate
Intraplate volcanism.
volcanoes are caused by subduction. it could be an oceanic plate sub-ducting under a continental plate which would result in a coastal volcano or it could be an oceanic plate sub-ducting under another oceanic plate, which would result in a volcanic island.
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When an oceanic plate collides with a continental plate, the denser oceanic plate usually subducts beneath the less dense continental plate due to the difference in densities. This can lead to the formation of deep oceanic trenches, volcanic arcs, and mountain ranges on the continental plate due to the intense tectonic forces generated during the collision.
When an oceanic plate collides with a continental plate, the denser oceanic plate is usually subducted beneath the less dense continental plate. This subduction process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding continental plate.
It is oceanic
The oceanic plate is denser than the continental plate due to its composition of heavier mafic rock. This density difference causes the oceanic plate to sink below the continental plate in a process known as subduction.
Continental plate.
When oceanic and continental plates collide, the denser oceanic plate subducts beneath the continental plate. This subduction causes melting of the mantle, creating magma that rises to the surface, forming volcanoes on the continental plate. The magma eventually erupts through the volcano, leading to the formation of volcanic islands or mountain ranges.
The three types of convergent boundaries are oceanic-oceanic plate boundary (e.g. Japan Trench), oceanic-continental plate boundary (e.g. Andes Mountains), and continental-continental plate boundary (e.g. Himalayas).