Quiz Chapter 11 Flashcards
Earthquake
ground shaking caused by the sudden and rapid movement of one block of rock sliding past one another
Faults
rocks sliding past one another along fractures in the crust
focus or hypocenter
where the rock slippage of the Earthquake originates in the ground
Seismic waves
stored up energy released in all directions from the focus
epicenter
point on the ground surface directly about the focus
Causes of Earthquakes
Massive landslides, meteorites, and volcanic eruptions, plate movement
elastic rebound
deformed rocks “snap back” to their original position in this process
aftershocks
small earthquakes that follow major earthquakes
foreshocks
minor earthquakes that sometimes precede a major earthquake by days, weeks, or months
Three major types of faults
Normal, Reverse and thrust, and Strike-slip faults
Normal Fault
associated with divergent plate boundaries
Reverse and thrust
associated with convergent plate boundaries
Megathrust fault: in a subduction zone, the boundary between the subducting and overlying plate
Strike-slip
large faults associated with divergent plate boundaries
Small strike-slip faults associated with divergent plate boundaries
Types of Faults
Some portions exhibit slow, gradual displacement known as fault creep
Other segments regularly slip, producing small earthquakes, others remain stuck and store elastic energy
Fault slip
the amount of displacement on the fault surface