earthquakes chapter 15 recent quakes (last 7 days) uakes/recenteqsww
TRANSCRIPT
EARTHQUAKES
Chapter 15
Recent quakes (last 7 days)
http://earthquake.usgs.gov/earthquakes/recenteqsww/
LARGEST QUAKES SINCE 1900• Chile 1960 9.5• Alaska 1964 9.2• Alaska 1957 9.1• Sumatra 2004 9.1• Japan 2011 9.0• Chile 2010 8.8
MAJOR RECENT QUAKES
• China 7.9 5/12/08 87,000 • Sumatra 7.0 12/26/04 230,000• Haiti 7.0 1/12/10
316,000• Chile 8.8 2/27/10 810• Japan 9.0 3/11/11 28,000 +• Philippines 6.7 2/6/12 113
Michigan earthquakes
• Year Date Mag. City • 1877 Aug 17 3.2 Greenfield • 1938 Mar 13 3.8 Gibralter • 1938 Mar 14 ? Gibralter• 1947 Aug 10 4.7 Coldwater • 1977 Oct 26 2.7 L Superior • 1980 Apr 29 0.5 L Superior • 1982 Nov 26 2.5 Scotts • 1994 Sep 02 3.4 Central Lansing• 2001 Oct 23 2.9 Prairie L
What is an Earthquake?
• Vibration of earth from rapid release of energy
• Movement at focus
• above focus is the epicenter
Elastic rebound theory
Aftershocks
• “Readjustment” of the plate in it’s new position
• Due to Elastic rebound theory
• Bigger earthquakes= bigger aftershocks
Normal faulttensional stress
footwall
Hanging wall
Reverse (thrust) faultcompressional stress
footwall
Hanging wall
Strike slipshearing stress
San Andreas Fault
EARTHQUAKE WAVES
Measured by a seismograph
P waves
• Primary• travel fastest• travels through liquids and solids• compressional wave
– push/pull
S waves
• Secondary• travels only through solids• shearing wave
– back and forth motion
Surface waves
• Travel on surface• slow• similar to water
waves• Usually cause
most damage
GPS seismometer
Label layers
Seismic wavesS waves do NOT travel through liquids
• Mantle= P + S waves= solid
• Outer core= P waves only= liquid
• Inner core-= solid
Locating an epicenter
• use lag time between P and S waves to calculate the distance the epicenter was from the seismograph
• Doesn’t tell direction
INTENSITY OF QUAKE
• Depends on– energy released (magnitude)– distance from epicenter– rock type (soft=worse)– depth
SCALES
• Mercalli– Created in 1902 (before
seismographs)– measures damage– I- XII– Depends on population, building type
Coldwater, MI 1947
RICHTER SCALE
• Developed by Charles Richter (1935)
• Measures ground shaking- each step is 10x higher wave amplitude
• Each step is 32x more energy- logarithmic
• 4.5 compared to 6.5 energy=
Richter Scale (ML)
• Under 2 not felt by humans
• Designed for California shallow quakes
• Not accurate for large quakes
Moment- Magnitude Scale (Mw)• More accurate than Richter,
especially for large quakes
• Mw= Area of fault’s rupture X slippage X rock resistance
Where do quakes happen?
At plate boundaries (most of the time)
Quakes outline plate boundaries
Depth of quakes
PLATE BOUNDARIES
•Divergent–small–shallow–normal faults
PLATE BOUNDARIES
•CONVERGENT– Most major
quakes– reverse faults– Shallow
through deep
PLATE BOUNDARIES
• INTRAPLATE– asthenospher
e causes vertical movement?
– Ancient faults?
Earthquake hazards
• Structural damage– Most prevalent
• Tsunamis• Fires (electrical lines + gas lines)• landslides
Peru 2007
Pakistan 2005
Chile
• Feb. 27, 2010• 8.8 Mw• Depth 35 km• 486 deaths• Reverse fault• Moved Santiago 11 inches to the west
Alaskan school, Good Friday 1964
Olympia WA, 1949