Volcanoes are formed by the movements of tectonic plates, which are the large pieces that make up the Earth's crust. The Earth's crust is divided into several tectonic plates that are constantly moving due to the flow of the underlying semi-fluid layer known as the mantle.
There are three main types of plate boundaries: convergent, divergent, and transform. It is at these plate boundaries where volcanoes are formed.
1. Convergent boundaries: When two tectonic plates move towards each other, it results in a convergent boundary. There are three types of convergent boundaries - oceanic-oceanic, oceanic-continental, and continental-continental. In the case of oceanic-oceanic or oceanic-continental convergence, the denser plate (usually the oceanic plate) subducts or sinks beneath the other plate. As it sinks into the mantle, it begins to melt due to the increased pressure and temperature. This molten rock, known as magma, rises to the surface and results in the formation of a volcano.
2. Divergent boundaries: When two tectonic plates move away from each other, it forms a divergent boundary. As the plates separate, magma from the mantle rises up to fill the gap. This molten rock then solidifies and forms new crust along the boundary, giving rise to volcanoes. The most famous example of this is the Mid-Atlantic Ridge.
3. Transform boundaries: Transform boundaries occur when tectonic plates slide past each other horizontally. While these boundaries do not commonly form volcanoes, volcanic activity can occur in some cases, particularly when the movement of the plates causes the crust to crack and allows magma to reach the surface.
In all these cases, the movement of tectonic plates triggers the formation of magma, which leads to the creation of volcanoes when it reaches the Earth's surface.
how are volcanoes formed by the movements of plates
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