Coach Williams Room 310B. Earthquakes Objectives: 1.Define stress and strain as they apply to...

download Coach Williams Room 310B.  Earthquakes  Objectives: 1.Define stress and strain as they apply to rocks 2.Distinguish among the three types of faults.

If you can't read please download the document

Transcript of Coach Williams Room 310B. Earthquakes Objectives: 1.Define stress and strain as they apply to...

  • Slide 1
  • Coach Williams Room 310B
  • Slide 2
  • Earthquakes
  • Slide 3
  • Objectives: 1.Define stress and strain as they apply to rocks 2.Distinguish among the three types of faults 3.Contrast three types of seismic waves
  • Slide 4
  • Vibrations of ground Caused by movement along fractured crust
  • Slide 5
  • Stress: forces that act on a material Compression: decreases volume of material Tension: pulls material apart Shear: causes materials to twist Strain: deformation of material due to stress
  • Slide 6
  • Fault: fracture in crust; caused by stress Reverse: horizontal compression (pushing together) Normal: horizontal pulling apart Strike-Slip: shear forces (sideways)
  • Slide 7
  • Slide 8
  • Primary (P-waves): rocks move in same direction as waves. Secondary (S-waves): rocks move @ right angles to direction of wave. Surface: rocks move in 2 directions Surface waves stay on surface S/P Waves pass through interior (body waves)
  • Slide 9
  • Slide 10
  • Slide 11
  • Focus: point where Earthquakes start Usually below surface Epicenter: point directly above on surface
  • Slide 12
  • Objectives: 1.Describe how a siesmometer works 2.Explain how seismic waves have been used to determine the structure and composition of Earths interior
  • Slide 13
  • Seismology: study of earthquake waves Surface and interior Seismometer: detects/records seismic waves Seismogram: record of waves
  • Slide 14
  • Slide 15
  • Many earthquakes are charted Shows time an distance from epicenter Determines distance
  • Slide 16
  • Changing speed/direction of waves P-waves diffracted S-waves wont go through liquid
  • Slide 17
  • Slide 18
  • Objectives: 1.Compare/contrast earthquake magnitude and intensity and the scales used to measure each 2.Explain why data from at least three seismic stations are needed to locate an earthquakes epicenter 3.Describe Earths seismic belts
  • Slide 19
  • Magnitude: amount of energy released Depth affects magnitude Richter scale: Measured magnitude Largest wave Power of 10 (8 is 10x larger than 7 & 100x more than 6) Moment Magnitude Scale Fracture length and movement Modified Mercalli Scale Amount of damage (intensity) I-XII
  • Slide 20
  • Slide 21
  • Slide 22
  • Distance from 3 seismic stations Intersecting 3 circles
  • Slide 23
  • Slide 24
  • Plotted earthquakes Regions
  • Slide 25
  • Objectives: 1.Discuss factors that affect eh amount of damage done by an earthquake 2.Explain some of the factors considered in earthquake probability studies 3.Define seismic gaps
  • Slide 26
  • Structure failure Buildings (pancaking), building materials? Land/Soil failure Landslides, soil liquefaction Fault scarps: ground deformations Tsunami: large ocean wave
  • Slide 27
  • Slide 28
  • Slide 29
  • Slide 30
  • Slide 31
  • Slide 32
  • Earthquake history: Intervals (Parkfield, CA- 22years) Seismic gaps: time since last earthquake Strain accumulation: measure of strain