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Earthquakes and Seismic Waves
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Published on Nov 19, 2015
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1.
Earthquakes and Seismic Waves
Chapter 6 Section 2
Photo by
tobo
2.
Wave Demonstration
Photo by
GollyGforce - Living My Worst Nightmare
3.
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
4.
Earthquakes
begin in the lithosphere
start underground at the focus
epicenter is on the surface above the focus
5.
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 !!!
6.
P Waves
first waves to arrive after an earthquake
compress and expand like an accordian
P = primary waves
can travel through liquids and solids
Photo by
Andrew Bartram (WarboysSnapper)
7.
S Waves
vibrate from side to side and up & down
shake the ground back and forth
travel through solids only
S = secondary waves
Photo by
Unhindered by Talent
8.
Surface Waves
when P & S waves reach the surface
move slower than other waves
produce severe ground movements
make ground roll like ocean waves
9.
Wave Diagrams
Photo by
rkramer62
10.
Measuring Earthquakes
Magnitude = size of quake
There are 3 commonly used methods
Mercalli, Richter and Moment Magnitude
Photo by
uair01
11.
Mercalli Scale
rates quakes by level of damage
Photo by
waterdotorg
12.
Richter Scale
rates quakes based on seismic waves
also rates the fault movement that occurs
waves are measured by a seismograph
Photo by
jogales
13.
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
Photo by
UCL Mathematical and Physical Sciences
14.
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
15.
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
16.
Earthquake Safety
Chapter 6 Section 4
17.
Earthquake Risk
determine risk by locating faults
also looks at where past quakes happened
what areas are at highest risk?
18.
How Earthquakes Damage
Shaking
Liquefaction
Aftershocks
Tsunamis
Photo by
Cal OES
19.
Shaking
can trigger avalanches and landslides
damages buildings
loose soil shakes more than solid rock
Photo by
Kariido85
20.
Liquefaction
shaking turns loose, soft soil into liquid mud
happens where soil is full of moisture
the ground gives way
21.
Aftershocks
earthquake that occurs after a larger quake
can happen hours, days, or months later
22.
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
23.
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
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