1.12 Shaken and Stirred Flashcards
p waves
short wavelength
travel fast through both solid + liquid
waves push and pull in direction of travel to make compressional and extensional zones
s secondary waves
slower than p waves and can only move through solid
longer wavelength and movement is at right angles to direction of travel
l love waves
slowest but most destructive waves, only move at surface
largest amplitude and shake ground from side to side
what do vertical p waves do
cause the ground to move up and down
what do vertical s waves do
cause the ground to move back and forth
cause the ground to alternate movement from left to right
love wave
stable soil vs liquified soil
loosely packed grains of soil are held together by friction and pore spaces are filled with water, in liquefaction, shaking destabilises the soil , increasing space between grains so soil flows like a liquid
what does crust fracturing do
energy released causes crust to crack and land to displace vertically
secondary effects of earthquakes
landslides when ground shaking dislodges slope material causing it to slide/topple
primary effects
ground shaking or crustal fracturing
aftershocks
smaller earthquakes can occur whilst the fault settles down which can significantly impact response and recovery
prediction of earthquakes
foreshocks can provide warning signs
animal behaviour
p waves trigger early warning systems and aid immediate response