Considering this, how are earthquakes and volcanoes evidence to support plate tectonics?
Colliding plates
Plates sliding past each other cause friction and heat. Subducting plates melt into the mantle, and diverging plates create new crust material. Subducting plates, where one tectonic plate is being driven under another, are associated with volcanoes and earthquakes.
Additionally, why do we find earthquakes and volcanoes on tectonic plate boundaries? Most earthquakes and volcanoes occur because of the movement of the plates, especially as plates interact at their edges or boundaries. At diverging plate boundaries, earthquakes occur as the plates pull away from each other. First, both volcanoes and earthquakes form where one plate sinks under the other.
Subsequently, one may also ask, how do volcanoes support the theory of plate tectonics?
Most volcanoes form at the boundaries of Earth's tectonic plates. At a divergent boundary, tectonic plates move apart from one another. They never really separate because magma continuously moves up from the mantle into this boundary, building new plate material on both sides of the plate boundary.
Do earthquakes have something to do with tectonic plates?
The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.
