chapter 19. most earthquakes are the result of movement in the earth’s crust at the tectonic...
TRANSCRIPT
Chapter 19
Most Earthquakes are the result of movement in the Earth’s crust at the tectonic plates.
Rocks in the crust resist movement and build up stress overtime.
Stress is the total force acting on crustal rocks per unit of area. When stress is greater than the strength of the rocks, they slip resulting in an earthquake.
Compression: decreases volume of material
Tension: pulls material apart Shear: twists material When material is subject to stress it
can become deformed; strain. When rocks break due to stress and
strain, it releases massive amounts of energy this usually happens at Faults.
PRIMARY WAVES SECONDARY WAVES
Aka P waves Behave like a
compression wave P waves squeeze and
push rocks in the direction the wave is travelling.
Travel fast!
Aka S waves Behave like a transverse
wave S waves move
perpendicular to the direction of the wave
Travel slower.
Surface waves: the slowest type of waves which only travel along the Earth’s surface, not the interior like the S and P body waves.
Surface waves usually cause the most destruction because they move the ground and take the longest time to pass.
The point where the waves originate is where the rock fails; the focus. The point on the crust above this is the epicenter.
RICHTER SCALE MERCALLI SCALE
A scale that measures the energy of the largest seismic waves (in magnitude) that are produced during an earthquake.
The numbers are determined by the height or amplitude of the waves.
A wave that measures 8 on the Richter scale is 10 times more energy than a 7.
Measures Earthquakes by how much damage they cause.
See table 19.2 p. 540 in the text.
A large ocean wave generated by vertical motions of the seafloor during an earthquake.
Wave spreads from the epicenter much like the seismic waves.