Title: GEOS 112 Lecture Topics 2303
1GEOS 112 Lecture Topics 2/3/03
- Earthquake Basics
- Tectonics and EQ Distribution
- USGS-NEIC website ? real-time EQ info
(http//wwwneic.cr.usgs.gov)
Read Chapter 16 (Earthquakes) EQ links on
GEOS112 homepage
2Earthquakes
3Elastic Rebound Theory of EQs
Figure 16.2
4Basic Definitions and Concepts
Figure 16.4
5Types of Seismic Waves
2-3 km/s
Body waves (4-6 km/s)
P and S waves travel through Earths interior ?
info about the mantle and core (density,
composition) Surfaces waves (Love, Rayleigh)
travel through the crust ? info about the crust
6Body Wave Motions
P-wave (primary)
S-wave (secondary)
vertical shearing motion perpendicular to
direction of wave propagation
compression/expansion in same direction of wave
propagation
Figure 16.5
7Surface Wave Motions
Love wave
Rayleigh wave
complex, orbital, water wave motion
horizontal shearing motion perpendicular to
direction of wave propagation
Figure 16.5
8Recording EQs on Seismograms
vertical ground motion
horizontal ground motion
Figure 16.6
9Recording EQs on Seismograms
analog recording
Figure 16.7
digital recording
10GEOS 112 Lecture Topics 2/6/03
- Earthquake Basics
- Tectonics and EQ Distribution
- Destructive Effects - Loma Prieta Movie
- USGS-NEIC website ? real-time EQ info
(http//wwwneic.cr.usgs.gov)
Read Chapter 16 (Earthquakes) EQ links on
GEOS112 homepage
11Mercalli Intensity Scale
- Numeric scale from I (smallest) to XII (largest)
- Based on amount of damage subjective human
assesment
- Used primarily for estimate of pre-seismogram
EQs (before early 1900s)
12Richter Earthquake Magnitude Scale
1 mm M 5
10 mm M 6
- Richter scale (M -2 to infinity) EQ range from
2 to 9.5. Largest EQ recorded Chile, 1960, M
9.5
- Based on maximum amplitude of seismogram recording
- Log10 scale every 1 increment increase on scale
is 10x the amplitude on the seismogram. (e.g.,
M 6 is 10x amplitude than M 5).
13Frequency, Magnitude, and Comparative Energy
Release
14GEOS 112 Lecture Topics 2/6/03
- Earthquake Basics
- Tectonics and EQ Distribution
- Destructive Effects - Loma Prieta Movie
- USGS-NEIC website ? real-time EQ info
(http//wwwneic.cr.usgs.gov)
Read Chapter 16 (Earthquakes) EQ links on
GEOS112 homepage
15EQ Distribution
Figure 16.22
16Divergent and Transform Boundary EQs
Maximum Magnitudes divergent (M7) transform (M
8)
Depths usually lt25 km
17Convergent Boundary - Subduction Zone EQs
Maximum Magnitudes (M 9.5) largest on Earth!!
Depth ranges from 0 to 700 km
18EQ Distribution and Depth
19Convergent Boundary - Collision Zone EQs
Figure 16.28
Maximum Magnitudes (M 8.0)
Depth usually lt80 km
20Intraplate EQs
21Large, Historic EQs in New England
1783 Mfa 5.3 New York City
22New Jersey Seismicity (1952 1971)
all M lt 3.5
Ramapo Fault
Large, inactive fault related to the initial
rifting of the Atlantic Ocean 200 m.y. ago
23GEOS 112 Lecture Topics 2/6/03
- Earthquake Basics
- Tectonics and EQ Distribution
- Destructive Effects - Loma Prieta Movie
- USGS-NEIC website ? real-time EQ info
(http//wwwneic.cr.usgs.gov)
Read Chapter 16 (Earthquakes) EQ links on
GEOS112 homepage
24Ground Motion (Shaking)
25- Factors that Affect Amount of Ground Motion
- EQ magnitude
- distance to the EQ focus
- local geology (material amplification)
26Liquefaction
27Liquefaction Damage
Great Alaskan EQ (1964 M 9.2)
- National Geophysical Data Center/NOAA
28Fires
Broken gas lines ignite
Fires burn uncontrolled
29Landslides
30Figure 16.19
Tsunami harbor wave in Japanese
31Fig. 10.34b
32Fig. 10.34a
Figure 16.20
- Cecilio Licos, Yasuki Arakaki Collection/Pacific
Tsunami Museum
33Fig. 10.34c
34Travel Times for Tsunami