Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock...

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Rock material at plate boundaries can bend, slide, fracture and hence, generate earthquakes

Transcript of Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock...

Page 1: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

Rock material at plate boundaries can bend, slide, fracture and hence, generate earthquakes

Page 3: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

PNW EQ Sources1. Subduction Zone EQ

Page 4: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

PNW EQ Sources2. Benioff Zone EQs

Earthquakes produced by slip along the subduction thrust fault or by slip on faults within the down-going ocean crust as a result of bending and extension as the plate is pulled into the mantle.

Nisqually EQ was 52.4 km below the surface

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PNW EQ Sources

3. Shallow, Crustal EQs

Page 6: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

EQs due to volcanic activity Mt. Rainier

Mt. Rainier

Page 7: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science
Page 8: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science
Page 9: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

seismometerseismograph

instruments used to record the motion of the ground during an EQ

seismometer is the internal part of the seismograph

seismogram

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The Pacific Northwest Seismic Network

Page 11: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

Richter Magnitude

Page 12: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

Richter Magnitude Length Analogy 1 1 millimeter 2 1 centimeter 3 10 centimeters 4 1 meter 5 10 meters 6 100 meters 7 1 kilometer 8 10 kilometers 9 100 kilometers 10 1000 kilometers

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Richter Magnitude Damage

Magnitude Under 2 "Micro Quake" - Generally not felt.

Magnitude 3 Normally not felt.

Magnitude 4 Often felt. Damage is rare.

Magnitude 5 Felt widely. Normally only slight damage.

Magnitude 6 Poorly constructed buildings are damaged.

Magnitude 7 - 7.8 Very serious damage occurs.

Magnitude 7.8+ "Great Quake" - Tremendous destruction and loss of life.

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The science of seismology is essential for the assessment of earthquake risk. Why?

Page 17: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

The science of seismology is essential for the assessment of earthquake risk. Why?

• locations• depths• magnitudes• frequencies• episodic activity

Seismic monitoring allows seismologists to determine EQ

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How often do earthquakes occur in the Pacific Northwest?

http://www.pnsn.org/INFO_GENERAL/faq.html#1

Over 1000 earthquakes with magnitude 1.0 or greater in Washington and Oregon occur every year. About 25 are large enough to be felt.

Most Recent EQ

In the 20th century, there were about 14 earthquakes of magnitude 5 or greater that have occurred near Puget Sound (most are Benioff):

1904 (M 5.3) 1909 (M 6.0) 1932 (M 5.2) 1939 (M 6.2) 1945 (M 5.9) 1946 (M 6.4) 1949 (M 7.0) 1965 (M 6.5)1990 (M 5.0) crustal (Deming, WA) 1995 (M 5.0) crustal1996 (M 5.3) crustal2001 (M 6.8)2001 (M 5.0)

Location Map

Page 19: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

How often do earthquakes occur in the Pacific Northwest?

http://www.pnsn.org/INFO_GENERAL/faq.html#1

Over 1000 earthquakes with magnitude 1.0 or greater in Washington and Oregon occur every year. About 25 are large enough to be felt.

In the 20th century, there were 13 earthquakes of magnitude 5 or greater that have occurred near Puget Sound (most are Benioff):

1904 (M 5.3) 1909 (M 6.0) 1932 (M 5.2) 1939 (M 6.2) 1945 (M 5.9) 1946 (M 6.4) 1949 (M 7.0) 1965 (M 6.5) 1990 (M 5.0) crustal (Deming, WA)1995 (M 5.0) crustal1996 (M 5.3) crustal2001 (M 6.8)2001 (M 5.0)

What is the return period?

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The last Cascadia subduction zone EQ occurred in 1700

Evidence suggests they occur every 400 to 500 years

Page 21: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

The science of seismology is essential for the assessment of earthquake risk. Why?

• locations• depths• magnitudes• frequencies• episodic activity

Seismic monitoring allows seismologists to determine EQ

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What other geologic research contributes to our understanding of EQs and hence contributes to risk assessment?

• Surface mapping with LiDAR• Monitoring plate movements with GPS• Sea-floor mapping• Mapping

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10m DEM from 1:24K contours

Maple Falls

Kendall

LiDAR survey of Nooksack River revealed Kendall Scarp

(Haugerud et al, 2005)

Page 24: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

What other geologic research contributes to our understanding of EQs and hence contributes to risk assessment?

• Surface mapping with LiDAR• Monitoring plate movements with GPS• Sea-floor mapping• Mapping

Page 25: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

What other geologic research contributes to our understanding of EQs and hence contributes to risk assessment?

• Surface mapping with LiDAR• Monitoring plate movements with GPS• Sea-floor mapping• Mapping

Page 26: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science

What other geologic research contributes to our understanding of EQs and hence contributes to risk assessment?

• Surface mapping with LiDAR• Monitoring plate movements with GPS• Sea-floor mapping• Mapping

Page 27: Rock material at plate boundaries can bend, slide ...geology.wwu.edu/rjmitch/EQ_Sources.pdf · Rock material at plate boundaries can bend, slide, fracture and hence, ... The science