Earthquakes and volcanoes are closely related to tectonic plate movement. The most accurate statement in the context of their relationship is:
As plates move, they push against each other, causing slipping or vents between plates.
Here's a brief explanation of how this works:
-
Tectonic Plate Movement: The Earth's lithosphere is divided into several large and small tectonic plates that float on the semi-fluid asthenosphere beneath them. These plates are constantly moving, albeit very slowly, due to convection currents in the mantle.
-
Earthquakes: When tectonic plates interact—whether they collide, pull apart, or slide past each other—stress builds up at plate boundaries. When this stress exceeds the strength of the rocks, the rocks rupture, causing an earthquake. This often occurs at fault lines where plates are either converging, diverging, or transforming.
-
Volcanoes: Volcanic activity is primarily associated with divergent (plates moving apart) and convergent (plates coming together) boundaries. At divergent boundaries, magma rises to fill the gap, creating new crust and leading to volcanic eruptions. At convergent boundaries, one plate may subduct (sink) beneath another, melting into magma, which can cause volcanic activity.
In summary, both earthquakes and volcanoes are manifestations of the movement of tectonic plates, but they are the result of different interactions between these plates.