Afault generally occurs at a convergent boundary

A strike-slip fault.  

Explanation:

A strike-slip fault is a type of tectonic movement that follows an occurring fracture in a parallel manner. There are two types of strike-slip faults: dextral (right-lateral) and sinistral (left-lateral). In dextral strike-slip faults, the tectonic movement would move to the right – remember its location is still parallel to the location of the fracture in the earth’s surface. In sinistral strike-slip faults, it would move to the left.  

During an earthquake, under your feet, you might feel it as if the earth is moving towards either the right or the left.  

i would have a lunch. it's one big package of food, making it one food. : p

explanation:

on disadvantage of hydroelectric power is the cost. another disadvantage of using hydroelectric power is finding a water source powerful enough to harvest hydroelectric power.