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Earthquakes and Seismic Waves

Published on Nov 19, 2015

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PRESENTATION OUTLINE

Earthquakes and Seismic Waves

Chapter 6 Section 2
Photo by tobo

Earthquakes

  • Shaking & trembling from the movement of rock
  • Cause: movement of Earth's plates
  • Plate movements cause stress in the crust
  • Stress increases at fault lines until rock breaks
  • Earthquake releases the energy stored in rocks
Photo by arbyreed

Earthquakes

  • begin in the lithosphere
  • start underground at the focus
  • epicenter is on the surface above the focus

Types of Seismic Waves

  • carries energy away from the focus
  • travels through the Earth's interior
  • travels across the Earth's surface
  • there are 3 types of waves
Photo by Pulpolux !!!

P Waves

  • first waves to arrive after an earthquake
  • compress and expand like an accordian
  • P = primary waves
  • can travel through liquids and solids

S Waves

  • vibrate from side to side and up & down
  • shake the ground back and forth
  • travel through solids only
  • S = secondary waves

Surface Waves

  • when P & S waves reach the surface
  • move slower than other waves
  • produce severe ground movements
  • make ground roll like ocean waves

Wave Diagrams

Photo by rkramer62

Measuring Earthquakes

  • Magnitude = size of quake
  • There are 3 commonly used methods
  • Mercalli, Richter and Moment Magnitude
Photo by uair01

Mercalli Scale

  • rates quakes by level of damage
Photo by waterdotorg

Richter Scale

  • rates quakes based on seismic waves
  • also rates the fault movement that occurs
  • waves are measured by a seismograph
Photo by jogales

Moment Magnitude Scale

  • estimates the total energy released
  • uses seismographs
  • measure how strong the waves are the types
  • used for quakes of all sizes and all in all places
  • more accurate than Richter scale

Comparing Magnitudes

  • 1 point increase is 32 times more energy
  • Below 5 causes little damage
  • 6 and above can cause great damage
  • Chile 1960 & Alaska 1964 mag.over 9

Locating the Epicenter

  • use seismic waves 
  • travel at different speeds
  • measure the difference between arrival times
  • need measurements from 3 locations
  • 3 circles are drawn and the overlap is the epicenter

Earthquake Safety

Chapter 6 Section 4

Earthquake Risk

  • determine risk by locating faults
  • also looks at where past quakes happened
  • what areas are at highest risk?

How Earthquakes Damage

  • Shaking
  • Liquefaction
  • Aftershocks
  • Tsunamis
Photo by Cal OES

Shaking

  • can trigger avalanches and landslides
  • damages buildings
  • loose soil shakes more than solid rock
Photo by Kariido85

Liquefaction

  • shaking turns loose, soft soil into liquid mud
  • happens where soil is full of moisture
  • the ground gives way

Aftershocks

  • earthquake that occurs after a larger quake
  • can happen hours, days, or months later

Tsunamis

  • caused by plate movement on ocean floor
  • ocean floor rises slightly and displaces water
  • large wave is formed
  • height wave is low until it reaches shallow water

Steps to Earthquake Safety

  • drop, cover and hold (protect your head)
  • avoid windows/mirrors/furniture that could fall
  • outdoors - move to an open area and sit down
  • avoid power lines
  • prepare an earthquake kit