“Earthquakes are created most commonly at the three types of boundaries of lithospheric plates, which are known as convergent or destructive, divergent or constructive, and Trans current or transform” (Wald). Most of the earthquakes around the world occur on these faults many of us have heard of///CONTINUITY/// some an example would be the San Andreas Faults.///SINGULAR/// “Most seismologists agree that the energy necessary to produce a major earthquake is accumulated slowly relative to the time it takes for a rupture to occur” (Mattioli). On the faults///AWK/// since the edges of the plates are rough, they get stuck while the rest of the plate keeps moving and what happens///OMIT/// when the plates have moved far enough, the edges eventually get unstuck on one of the faults and that is when an earthquake occurs. “The energy radiates outward from the fault in all directions in the form of seismic waves like ripples on a pond” (Wald). When this happens basically it is like water, the
“Earthquakes are created most commonly at the three types of boundaries of lithospheric plates, which are known as convergent or destructive, divergent or constructive, and Trans current or transform” (Wald). Most of the earthquakes around the world occur on these faults many of us have heard of///CONTINUITY/// some an example would be the San Andreas Faults.///SINGULAR/// “Most seismologists agree that the energy necessary to produce a major earthquake is accumulated slowly relative to the time it takes for a rupture to occur” (Mattioli). On the faults///AWK/// since the edges of the plates are rough, they get stuck while the rest of the plate keeps moving and what happens///OMIT/// when the plates have moved far enough, the edges eventually get unstuck on one of the faults and that is when an earthquake occurs. “The energy radiates outward from the fault in all directions in the form of seismic waves like ripples on a pond” (Wald). When this happens basically it is like water, the