Quiz 5 Flashcards
the place inside Earth’s crust where an earthquake originates
focus
The place on the Earth’s surface directly above the focus
epicenter
Earthquake foci depth on transform, divergent, and convergent plates
1)Transform- Shallow
2)Divergent-Shallow
3)Convergent-Deep
a planar zone of seismicity corresponding with the down-going slab in a subduction zone
Wadati-Benioff zone
Earthquake waves that travel through the body of the Earth
body waves
Earthquake waves that travel along the Earth’s surface
surface waves
P-waves
Type of body waves, primary waves, are compressional waves that move back and forth, similar to the action of an accordion or a slinky. Fastest waves
S-waves
Secondary waves, are shear waves that move material in a direction perpendicular to the direction of travel. S-waves can only travel through solids, and are slower than P-waves. Body waves
Love waves
faster surface waves, and they move material back and forth in a horizontal plane that is perpendicular to the direction of wave travel (see Figure 9.4). Buildings do not handle this type of movement well, and Love waves can also be responsible for considerable damage to structures.
Rayleigh waves
Earth’s surface move in an elliptical motion, similar to the movement in a sea wave. This results in ground movement that is up and down and side-to-side.
Intensity
Qualitative measures of the damage inflicted by an earthquake
magnitude
Quantitative measures of the energy released by an earthquake
quantitative measure of an earthquake’s magnitude using the logarithm of the amplitude, phased out due to inefficiency in large earthquakes
Richter scale
This scale has values that range from Roman numerals I to XII which characterize the damage observed and people’s reactions to it. Data for this scale is often collected right after an earthquake by having the local population answer questions about the damage they see and what happened during the quake. This information can then be pooled to create an intensity map, which creates colored zones based on the information collected
The Modified Mercalli Intensity Scale
estimates the total energy released by an earthquake and can be used to describe the magnitude of any size of earthquake including very large earthquakes. The magnitude is based on the seismic moment (estimated based on ground motions recorded on a seismogram), which is a product of the distance a fault moved and the force required to move it.
Moment Magnitude scale.