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Earthquakes occur near faults and near the edges of plates in the earth's crust. Volcanic eruptions occur wherever a volcano is. Volcanic eruptions can occur when magma from below Earth's surface seeps through a weak spot in the crust. Volcanoes occur along plate boundaries, along the edges of plates, so this is where volcanoes occur also.
Tectonic plates can result in a variety of events when altered, however the main 4 are:EarthquakesLandslidesTidal WavesVolcanic Eruptions
volcanic eruptions occur when the tectonic plates are convergent which is when one plate goes under another plate and the magma gets hot orwhen the plates are divergent that's when the plate pulls apart and magma fills the hole.
The most destructive volcanic eruptions typically occur along the edges of tectonic plates, known as convergent plate boundaries. These areas, such as the Ring of Fire in the Pacific Ocean, are prone to explosive volcanic activity due to the collision and subduction of tectonic plates. Examples of destructive eruptions in these regions include Mount St. Helens in the United States and Mount Pinatubo in the Philippines.
Earthquakes and volcanic eruptions often occur in the same area because they are both caused by the movement of tectonic plates. Volcanoes are usually found at plate boundaries where plates either converge or diverge, causing magma to rise to the surface. This movement of magma can also generate seismic activity, leading to earthquakes.
subduction boundary eruption
Earthquakes occur near faults and near the edges of plates in the earth's crust. Volcanic eruptions occur wherever a volcano is. Volcanic eruptions can occur when magma from below Earth's surface seeps through a weak spot in the crust. Volcanoes occur along plate boundaries, along the edges of plates, so this is where volcanoes occur also.
Volcanic eruptions at plate boundaries occur when one plate subducts beneath the other, allowing magma to rise and erupt on the surface. This often leads to explosive eruptions due to the pressure buildup of gases in the magma. Additionally, the melting of the subducted plate can create a magma chamber that fuels volcanic activity.
The theory of plate tectonics helps to explain how earthquakes and volcanic eruptions occur.
Stratovolcanoes are usually found along convergent plate boundaries where an ocean plate is pushed under another ocean plate or a continental plate (subduction zone). If you are referring to convergent boundaries in which neither plate is subducted but both are pushed up to form mountains, then my answer would have to be that it is very rare for a volcano to form at this type of boundary.
Most common would be a fissure eruption of basaltic magma.
Earthquakes occur near faults and near the edges of plates in the earth's crust. Volcanic eruptions occur wherever a volcano is. Volcanic eruptions can occur when magma from below Earth's surface seeps through a weak spot in the crust. Volcanoes occur along plate boundaries, along the edges of plates, so this is where volcanoes occur also.
Tectonic plates can result in a variety of events when altered, however the main 4 are:EarthquakesLandslidesTidal WavesVolcanic Eruptions
The Earth's surface is broken into large pieces called tectonic plates. These plates float on the semi-fluid asthenosphere layer beneath them and interact at plate boundaries, where geological phenomena such as earthquakes and volcanic eruptions occur.
volcanic eruptions occur when the tectonic plates are convergent which is when one plate goes under another plate and the magma gets hot orwhen the plates are divergent that's when the plate pulls apart and magma fills the hole.
If the plates are moving together from opposite directions, the colliding edges will uplift into mountain ranges. If the plates are moving apart, a rift valley will form. If the plates are moving together at oblique angles, a fault zone will occur.
Volcanic eruptions occur only in certain places and do not occur randomly. That's because the Earth's outermost shell -- the lithosphere -- is broken into a series of slabs known as lithospheric ortectonic plates. These plates are rigid, but they float on the hotter, softer layer in the Earth's mantle. There are 16 major plates. As the plates move about, they spread apart, collide, or slide past each other. Volcanoes occur most frequently at plate boundaries.