Download - Earthquake Hazards And Earthquake Risks in the Central US Or, What Keeps Geologists Awake at Night…
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Earthquake HazardsAnd Earthquake Risks in the Central US
Or, What Keeps Geologists
Awake at Night….
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Earthquake Magnitude
• How much energy released
• Logarithmic scale
• M6 = ~30 x M5
• M7 = ~1,000 x M5
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Earthquake Intensity
• How much energy delivered to any one site
• Subjective: depends on felt-reports from each location
• Many different intensities for same earthquake
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Earthquake Depth
• Range from shallow to deep (surface to ~800 km)
• Central US range 0 to 40 km
• Shallow = more energy and intensity at the surface
• Deep = less energy and intensity at the surface
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Earth’s Crust
• Thinner than an apple peel
• Floats on viscous mantle
• Pieces ‘bump and grind’ along plate edges plate tectonics
• Anomaly: Central US & others
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Earthquake Duration
• Felt for a few seconds– small earthquake, near
epicenter
• Felt for several minutes – large earthquake, farther
from epicenter
• Extreme earthquakes ‘ring the earth’ for hours
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Aftershocks & Series• Occur after most larger
earthquakes
• Become smaller and less frequent over time
• Can cause significant damage
• Central US: major earthquakes tend to occur in series
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Did You Feel It?
• April 18, 2008
• 4:36 am (CDT)
• Magnitude 5.4
• Depth ~11 km
• Epicenter near Bellmont, Ill.
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Earthquake Locations
• Need three earthquake recordings (seismograms)
• Measure distance from each recorder
• Common point is approximate epicenter
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Earthquake Locations
• Regional velocity of earthquake waves is known
• Distance from epicenter is estimated
• More recordings = better accuracy
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Mississippi Embayment
• Very clear on maps!
• ‘Bedrock trough’ dips & widens to the SW
• New Madrid fault zone– ‘Bottom’ of trough
– North end of trough
• Filled with sediments
• Mississippi River follows ‘easiest’ route
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New Madrid fault zone• Southeast Missouri &
northeast Arkansas
• Mississippi Embayment
• Old weakness in earth’s crust
• Active for hundreds of millions of years
• Activity continues now– 8-year ‘monitoring’ is
inconsequential
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Central US Earthquakes
• New Madrid FZ– Three ‘dog-legs’
segments
• Wabash Valley FZ
• East Tennessee FZ
• Ste. Genevieve FZ
• ‘Background’ faults everywhere
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New Madrid 1811-12
• Founded 1789; heavy forests
• Largest town between St. Louis & New Orleans
• Frequent floods and swamplands around it
• Heavy forests
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New Madrid Earthquakes
• Winter of 1811-12
• Three earthquakes ~M7+
• 1000s of aftershocks
• Wracked land, choked river
• Most people left the area
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New Madrid Earthquakes
• December 16, 1811– ~mag 7.5
• January 23, 1812– ~mag 7.3
• February 7, 1812– ~mag 7.6
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Eliza Bryan
• Born Pennsylvania 1780
• Arrived New Madrid 1791
• Earthquakes 1811-12
• Chronicled earthquakes 1816
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New Madrid Earthquakes
• Eliza Bryan account– ‘Violent shocks …’
– ‘Continuous agitation …’
– ‘Sand ... from fissures’
– ‘Twenty foot waves …’
• Evidence still visible today
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New Madrid Earthquakes
• River recedes from bank
• 15- to 20-foot waves
• ‘Waters gathered like a mountain …’
• Boats torn from moorings
• ‘Water took groves of cottonwood trees’
• Flooded tributary ¼-mile
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New Madrid Earthquakes
• ‘Retrograde current’– Fault uplifted land
surface downstream– Natural dam– Backflow created
Reelfoot Lake– Channel soon
reclaimed
• Evidence still visible today
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New Madrid Earthquakes
• Probably hundreds died, mostly on the river
• African and Native Americans not counted
• Insurance records (!) show losses of lives and insured cargoes
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Evidence Still Visible Today
• Sandblows
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Evidence Still Visible Today
• Reelfoot Lake
• Northwest Tennessee
• Sunklands
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New Madrid Earthquakes
• Felt area larger than same-size California earthquakes– Rock here is different!
• Aftershocks for years
• What is odd about this map?
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USGS Products
• Detailed hazard maps– Memphis, Tenn.
– Evansville, Ind.
– St. Louis, Mo.
• Groundshaking
• Liquefaction
• Not site-specific!
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US GEOLOGICAL SURVEYCENTRAL US EARTHQUAKE PROGRAM
Phyllis Steckel, RG
Earthquake Insight LLC
Washington, Mo.
In cooperation with the