What we feel as earthquakes are created by sudden shifts in the alignment of rocks. This occurs most often at the margins of tectonic plates - the plates of Earth’s crust that Earth’s surface is fractured into. These blocks of rock naturally move on the semi-molten mantle below. Along the edges, pressure builds as unyielding rocks pushes against unyielding rock until suddenly, there is slippage and the plates move creating an earthquake.










































