lecture 4: earthquakes our hazardous environment geog 1110 dr. thieme
TRANSCRIPT
Lecture 4: Earthquakes
Our Hazardous Environment
GEOG 1110Dr. Thieme
Earthquake - a vibration produced by the rapid release of stored energy.
The focus is the source of the quake, typically on a fault or plane of slippage in the Earth's crust
The epicenter is the point on the Earth's surface immediately above the focus, determined from the seismic waves generated by the quake.
Shallow-focus (<70 km) earthquakes tend to have the largest magnitude, as large as 8.6 on the Richter scale.Strongest intermediate-focus (70-300 km) earthquakes have magnitudes less than 7.5, and deep-focus (>300 km) do not exceed 6.9 in Richter magnitude.
Earthquake Magnitude• Richter scale (quantitative and based
on amplitude of seismic waves)• Moment - determined from the area
ruptured along the fault plane, more or less equal to the old Richter values
• Mercalli scale (Modified Mercalli Intensity Scale) - semi-quantitative and based on damage caused by the quake.
Earthquake Intensity - Mercalli Scale
J.C. Penney store in Anchorage, AK destroyed by the "Good Friday" earthquake in 1964.
Local uplift of shorelines (up to 1 m)
Twisting of steel framesand disintegration of
concrete blocks
Strike-slip (Transform)fault
Reverse (Thrust)fault
Normalfault
Buried or "Blind" Faults
Epicenter Location
• Measure S-P Interval in mm
• Convert to Distance in km using nomogram
• Triangulate to a point of intersection
• Epicenter is a point on the Earth's surface
directly above the earthquake focus
Earth Surface Material Differences
Seismic shaking is much greater in unconsolidated sediment,in more saturated materials, and in materials with laminar bedding.
Effects of 1989 Loma Prieta earthquakeon the Cypress Freeway in Oakland, CA
Large earthquakes in central Mexico (1985, 2003) occur due totransform motion at a "Triple Junction" situation like that in California.
Mexico City was built on a drained lake basin. Even though the cityis over 400 km east of the epicenter on the west coast, liquefaction
of the lake deposits resulted in subsidence and severe shaking duringthe 1985 event.
Shattered windows causedby twisting motion in a
Mexico City building, 1985
Undamaged buildings withvertical steel frames next to
completely demolished structures.
Buildings vibrated against one another because the seismic waveperiods coincided with the spacing of stories.
"Seismic Retrofit" - University Hall on the University of California, Berkeley, campus - 1997
"Seismic Retrofit" - Tohoku University, Sendai, Japan - 2003
Chemistry Building
Architecture Building
Engineering Building
The earthquake of January, 1995 in Kobe, Japan occurred nearanother "Triple Junction" where transform plate motion
occurs inboard of the plate boundary.
Landslide where faultingdestabilized the hillslope.
Paved roads cracked andoffset several meters.
Offset of agricultural terraces
Suspension Bridge pylon offset a meter.Liquefaction of landfill and
estuarine muds
Cretaceous granites are overlain by theOsaka formation, a Plio-Pleistocene
sedimentary unit consisting of alluviuminterbedded with marine clays.
Fill for the harbor was quarried from granite residuum in the interior.
Intraplate Seismicity (New Madrid Zone)
Prediction based on Past Frequency?
550-1200 years8.0
254-500 years7.0
70-90 years6.0
10-12 years5.0
14 months4.0
Recurrence Interval
Richter Magnitude
Prediction based on "Gaps" with stored energy
Paleoseismology
Figure 2.21