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The concept of plate tectonics has revolutionized the explanation about how earthquakes occur in Earth Sciences. Plate tectonics tells us that the Earth's rigid outer shell (lithosphere) is broken into a mosaic of oceanic and continental plates which can slide over the plastic aesthenosphere, which is the uppermost layer of the mantle. The plates are in constant motion. Where they interact, along their margins, important geological processes take place, such as the formation of mountain belts, earthquakes, and volcanoes.
the lithoseshere
Chitin
No, the rocks in the earth at that depth are too rigid and plastic-like to store the amount of stress needed for an earthquake to occur.
rotating a given rigid point about x or y axis is called a rotaion in CG.