earthquakes & earth’s interior chapter 8 pg 217. bill nye on earthquakes

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  • Slide 1
  • Earthquakes & Earths Interior Chapter 8 pg 217
  • Slide 2
  • Bill Nye on Earthquakes http://www.youtube.com/watch?v=RwDEysDCsoM http://www.youtube.com/watch?v=RwDEysDCsoM
  • Slide 3
  • A. What is an Earthquake? 1. Earthquakes a. A vibration of Earth produced by rapid release of energy within the lithosphere b. Happen along a fault c. Fault fracture in the crust where movement occurs
  • Slide 4
  • d. Focus 1) Place where earthquake starts 2) Along a fault beneath surface 3) Energy goes out in all directions 4) Energy travels as seismic waves
  • Slide 5
  • e. Epicenter place on surface directly above focus
  • Slide 6
  • f. Faults and change to earths surface 1) Vertical movement a) Known as uplifting b) Fault scarp sharp edge ridge 2) Horizontal - displacement
  • Slide 7
  • Slide 8
  • Imperial fault - displacement
  • Slide 9
  • 2. Cause of Earthquakes (Elastic rebound hypothesis) a. Convection currents move plates on both sides of fault b. Rocks bend and store elastic energy c. Resistance from friction is overcome d. Rocks slip at weakest point (fault)
  • Slide 10
  • e. Causes forces farther up fault resulting in more slippage f. Continues until energy is released and rock returns to previous state
  • Slide 11
  • Elastic Rebound Page 220 figure 4
  • Slide 12
  • g. Aftershocks 1) Smaller than original quake 2) Happen after original quake 3) Caused from additional movements along the fault 4) Cause damage to previously weakened buildings
  • Slide 13
  • Effects of initial earthquake
  • Slide 14
  • h. Foreshocks small quakes before large earthquake i. Fault segments behave differently 1) Fault creep slow gradual movements 2) Regular slippage 3) Stay locked for extended periods of time
  • Slide 15
  • Slide 16
  • B. Measuring Earthquakes 1. Intro a. Seismology study of earthquake waves b. Seismographs record earthquake waves c. Seismogram recorded ground motion
  • Slide 17
  • Slide 18
  • Seismographs ThenNow
  • Slide 19
  • 2. Earthquake waves a. Spread out in all directions b. Surface waves 1) Travel along earths outer layer 2) Up/down & side/side motion 3) Most destructive waves
  • Slide 20
  • 4) Change volume of material temporarily by pushing/pulling 5) Slowest waves 6) Recorded by seismogram
  • Slide 21
  • c. Body waves 1) Travel through earths interior 2) P waves a) Push-pull waves (compress/expand) b) Push/pull rocks in direction wave travels c) Known as compression waves d) Fastest waves
  • Slide 22
  • Slide 23
  • 3) S waves a) Shake particles at right angles to their direction of travel b) Transverse waves c) Change shape of material they pass through temporarily d) Gases and liquids will not transmit them b/c there is no elastic rebound to original shape
  • Slide 24
  • Slide 25
  • Slide 26
  • 3. Locating an Earthquake a. Earthquake distance 1) Find time b/w 1 st P wave and 1 st S wave 2) Use a travel-time graph
  • Slide 27
  • b. Earthquake Direction 1) Need 3 seismic stations 2) Circles are distance of epicenter 3) Intersecting circles shows epicenter
  • Slide 28
  • Slide 29
  • c. Earthquake zones 1) Circum-Pacific belt a) Ring of fire b) Outer edge of Pacific Ocean c) 75% of worlds earthquake activity d) Philippines, Japan, Chile, Alaska 2) Mediterranean-Asian belt 3) Oceanic ridge system
  • Slide 30
  • 4. Measuring Earthquakes a. Intensity measures shaking based on amount of damage b. Magnitude measures seismic waves c. Richter Scale 1) Based on amplitude of largest seismic wave 2) Logarithmic scale
  • Slide 31
  • Richter Scale and Magnitude
  • Slide 32
  • 3) Only useful within 310 miles of epicenter 4) Scientists no longer use it, but the news does
  • Slide 33
  • d. Moment Magnitude 1) More accurate than Richter scale 2) Based on amount of displacement along fault 3) Only scale that estimates energy released by earthquakes
  • Slide 34
  • 4) Calculating: a) Average amount of movement along fault b) Area of surface break c) Strength of broken rock
  • Slide 35
  • C. Destruction from Earthquakes Why does one building have almost no damage to it?
  • Slide 36
  • 1. Factors a. Intensity b. Duration c. Material used in buildings d. Building design
  • Slide 37
  • 1) Wood and steel frames = more flexible 2) Concrete needs to be reinforced
  • Slide 38
  • e. Liquefaction 1) Happens to loosely packed saturated soils 2) Soil turns into a liquid 3) Buildings settle, underground structures rise http://www.youtube.com/watch?v=4Uwxr42JqYQ
  • Slide 39
  • 2. Tsunamis a. Causes 1) Ocean floor is displaced vertically 2) Underwater landslide
  • Slide 40
  • b. Characteristics 1) Move quickly in open ocean 2) Can go unnoticed 3) Waves slow and increase in size as depth decreases
  • Slide 41
  • c. Warning system 1) Use water levels in tidal gauges 2) Provides about 1 hour warning Importance http://www.youtube.com/watch?v=noq8FYvRqgs
  • Slide 42
  • 3. Other dangers a. Landslides 1) Most damage 2) Landslides, slopes fail, ground collapses, gas and water lines break b. Fire
  • Slide 43
  • 4. Predicting Earthquakes a. Short-range 1) Study uplift, strain in rocks, water levels, pressure in wells, radon gas emission, electromagnetic properties in rocks 2) Hasnt been successful
  • Slide 44
  • b. Long-range 1) Probability of certain magnitude earthquakes happening w/in 30-100+ yrs 2) Important for building codes 3) Based on that earthquakes are cyclical 4) Study seismic gap no activity for long periods of time 5) Limited success
  • Slide 45
  • D. Earths Layered Structure 1. Intro a. We have only drilled 7.5 miles b. How do we know what the inside looks like? - Studying earthquake waves
  • Slide 46
  • c. Waves speed up with depth b/c of pressure d. Pressure causes waves to refract
  • Slide 47
  • 2. Layers by composition a. Crust 1) Oceanic a) 7 km (4mi) b) Igneous rocks (basalt) c) Younger than continentalrocks d) Ave. density 3.0 g/cm 3
  • Slide 48
  • 2) Continental a) 8 75 km (5-47mi) b) Average 40 km c) Older than oceanic crust
  • Slide 49
  • Slide 50
  • b. Mantle 1) Middle layer 2) 1795 miles 3) Density 3.4g/cm3 c. Core 1) Iron-nickel alloy 2) Density 13 g/cm3 3) 2162 miles
  • Slide 51
  • 3. Layers by physical properties 1) Lithosphere a) Rigid shell b) Crust and upper mantle 2) Asthenosphere a) Upper mantle b) Rocks near melting point c) Putty like substance
  • Slide 52
  • Slide 53
  • 3) Lower mantle a) More rigid but still can flow b) Bottom part is much more fluid from heat from core 4) Outer core a) Liquid b) Flowing causes magnetic field 5) Inner core solid from pressure
  • Slide 54
  • Slide 55
  • 4. Discovering layers a. Finding crust/mantle 1) Moho discontinuity place where seismic waves speed up 2) Named after Andrija Mohorovicic
  • Slide 56
  • Slide 57
  • b. Finding outer core (fig 16 pg 236) 1) P waves bend around liquid core 2) Shadow zone p waves arrive minutes slower than expected through outer core 3) S waves cant go through liquid
  • Slide 58
  • Slide 59
  • Slide 60
  • S waves dont go through core
  • Slide 61
  • E. Earthquake Safety 1. Before a. Go over safety until it is instinctive b. Teach everyone c. Have emergency supplies 1) Battery radio 2) Batteries 3) First aid kit 4) Water and food for 2 weeks 5) Blankets
  • Slide 62
  • d. Arrange home for safety 1) Heavy things on bottom shelf 2) Breakables with latched doors 3) Dont hang heavy things (mirrors, pictures, etc.) above where people sleep 4) Anchor heavy appliances 5) Flammable liquids away from ignition sources (water heaters, stoves, furnaces)
  • Slide 63
  • e. Locate main turn-offs (water, gas, and electric) 2. During a. Stay inside b. Move: 1) Under desk or table 2) Interior wall 3) NOT by windows, mirrors, fireplaces, and hanging objects
  • Slide 64
  • c. If cooking turn off stove and take cover d. If outside 1) Move to open area 2) Get away from buildings, power lines, and trees
  • Slide 65
  • e. If driving 1) Stop on side of road 2) Dont stop under bridges and overpasses, power lines, trees, large signs 3) Stay in car
  • Slide 66
  • 3. After a. Check for injuries b. Check for damage to see if you are safe c. Smell gas open windows and get outside d. Smell/see frayed wires turn off electric and get outside
  • Slide 67
  • The New Madrid Fault https://www.youtube.com/watch?v=7kc7pJ8f1aY https://www.youtube.com/watch?v=7kc7pJ8f1aY