Textbook Notes (378,268)
CA (167,148)
UTSC (19,205)
EESA06H3 (240)
Nick Eyles (207)
Chapter 3

# Chapter 3 notes

5 Pages
94 Views

Department
Environmental Science
Course Code
EESA06H3
Professor
Nick Eyles

This preview shows pages 1-2. Sign up to view the full 5 pages of the document.
Chapter 3 Earthquakes
What causes earthquakes?
An earthquake is a trembling or shaking of the ground caused by the sudden release of energy stored in the
rocks beneath Earths surface.
Great forces acting deep in the earth may put a stress on the rock, which may bend or change in shape (strain) –
the rock can only deform so far before it breaks, waves of energy are released and send out through the Earth
Seismic waves = waves of energy produced by an earthquake. It is the seismic waves that cause the ground to
tremble and shake during an earthquake
Fault = the break between the 2 rock masses as they move past each other
Classic explanation of why earthquakes take place is called the elastic rebound theory = sudden release of
progressively stored elastic strain energy in rocks, causing movement along a fault. Eventually the stored energy
in the rock exceeds the breaking strength, rock breaks causing and earthquake
Brittle behaviour of breaking rock is only in rock near Earths surface. Rocks at depth are subjective to increase
temperature and pressure = less brittle.
Why do earthquakes cause so much damage?
The point within the earth where seismic waves first originate is called the focus (or hypocentre) of the
earthquakes – this is the centre of the earthquake, the point of initial breakage and movement on a fault
The point on the Earths surface directly above the focus is the epicenter
2 types of seismic waves are generated during earthquakes:
obody waves – are seismic waves that ravel through the Earths interior, spreading outward from the focus
in all directions
osurface waves – seismic waves that travel on Earths surface away from the epicenter (like water moving
when throwing pebble)
FIG 3.5 page 73 – diagram that explains the waves
Body Waves
2 types of body waves:
oP wave – a compressional or longitudinal wave in which rock vibrates back and forth parallel to the
direction of wave propagation
Very fast wave, 4-7kn per second
First to arrive at a recoding station following an earthquake
oS wav e – secondary wave, slower transverse wave that ravels through near-surface rocks at 2-5km per
second
Characterized by shearing motion (i.e. shaken rope), the rock vibrates perpendicular to the
direction of wave propagation
Both waves pass easily through solid rock. P wave can also pass through fluid (gas or liquid) but S wave cant
Surface Waves
Slowest waves set off by earthquakes, but cause more property damage than body waves because they produce
more ground movement and takes longer to pass
2 types:
oLove waves – similar to S waves that have no vertical displacement. The ground moves side to side in a
horizontal plate that is perpendicular to the direction of the wave travelling or propagating
Do not travel through fluid
Due to horizontal movement, love waves tend to knock buildings off their foundation and destroy
highway bridge support
www.notesolution.com
oRayleigh waves – behave like rolling ocean waves, it causes the ground to move in a elliptical path
opposite to the direction the wave passes
Incredibly destructive to buildings because they produce more ground movement and takes
longer to pass
How do we know where earthquakes occur?
Instrument we use to measure seismic waves is a seismometer
oThe principle of the seismometer is to keep a heavy suspended mass as motionless as possible
suspending it by springs or hanging it as a pendulum from the frame of the instrument
oWhen the ground moves, the frame of the instrument moves with it, heavy mass suspended act as a point
of reference in determining ground motion
oMeasure axis, X, Y and Z (3Dimensions)
A seismogram is a recording device that produces a permanent record of Earth motion detected by a
seismometer, in digital format
Because of different types of waves that travel at different speeds, they arrive in seismograph stations in a
definite order:
oFirst P waves
oS-waves
oFinally surface waves
By analyzing seismograms, can learn about location, and size
Determining the Location of an Earthquake
P and S waves start from the focus of an earthquake at essentially the same time. As they travel away from the
quake, the 2 kinds of body waves gradually separate because they travel in different speeds
The farther the seismic waves travel (from focus to seismograph station) the longer the time interval between the
arrival of P and S waves and more they are separated on the seismograms
oThis time interval can be used to determine the distance form the seismograph station to a quake
oThe increase in P-S interval is regular with increasing distance fro several thousands km and can be
graphed in a travel-time curve = plots seismic wave arrival time against distance
Analyses of seismogram can also indicate at what depth beneath the surface the quake occurred, most quakes
occur near the surface
oThe maximum depth of focus – the distance between focus and epicenter for quakes is about 670km
oQuakes can be classified into 3 group according to their depth of focus:
Shallow focus (0-70km deep) = most common 85% of total quake energy release
Intermediate focus (70-350km deep) = 12%
Deep focus (350-670km deep) = 3%
Measuring the size of an earthquake
Size of earthquake can be measured in 2 ways:
oIntensity – find out how much and what kind of damage the quake has causes. Measure of an
earthquakes effect on people and buildings
Intensity is expressed in roman numerals from I to XII on the modified Mercalli scale (high
number = greater damage)
Limitations in using intensity as a measure of earthquake strength:
Damage lessens with distance intensities for same earthquake
Damage to buildings and other structures depend on type of geological material it was
built on
Damage estimates are also subjective
www.notesolution.com

#### Loved by over 2.2 million students

Over 90% improved by at least one letter grade.

OneClass has been such a huge help in my studies at UofT especially since I am a transfer student. OneClass is the study buddy I never had before and definitely gives me the extra push to get from a B to an A!

Leah — University of Toronto

Balancing social life With academics can be difficult, that is why I'm so glad that OneClass is out there where I can find the top notes for all of my classes. Now I can be the all-star student I want to be.

Saarim — University of Michigan

As a college student living on a college budget, I love how easy it is to earn gift cards just by submitting my notes.

Jenna — University of Wisconsin

OneClass has allowed me to catch up with my most difficult course! #lifesaver

Anne — University of California
Description
Chapter 3 Earthquakes What causes earthquakes? • An earthquake is a trembling or shaking of the ground caused by the sudden release of energy stored in the rocks beneath Earth’s surface. • Great forces acting deep in the earth may put a stress on the rock, which may bend or change in shape (strain) – the rock can only deform so far before it breaks, waves of energy are released and send out through the Earth • Seismic waves = waves of energy produced by an earthquake. It is the seismic waves that cause the ground to tremble and shake during an earthquake • Fault = the break between the 2 rock masses as they move past each other • Classic explanation of why earthquakes take place is called the elastic rebound theory = sudden release of progressively stored elastic strain energy in rocks, causing movement along a fault. Eventually the stored energy in the rock exceeds the breaking strength, rock breaks causing and earthquake • Brittle behaviour of breaking rock is only in rock near Earth’s surface. Rocks at depth are subjective to increase temperature and pressure = less brittle. Why do earthquakes cause so much damage? • The point within the earth where seismic waves first originate is called the focus (or hypocentre) of the earthquakes – this is the centre of the earthquake, the point of initial breakage and movement on a fault • The point on the Earth’s surface directly above the focus is the epicenter • 2 types of seismic waves are generated during earthquakes: o body waves – are seismic waves that ravel through the Earth’s interior, spreading outward from the focus in all directions o surface waves – seismic waves that travel on Earth’s surface away from the epicenter (like water moving when throwing pebble) FIG 3.5 page 73 – diagram that explains the waves Body Waves • 2 types of body waves: o P wave – a compressional or longitudinal wave in which rock vibrates back and forth parallel to the direction of wave propagation Very fast wave, 4-7kn per second First to arrive at a recoding station following an earthquake o S wave – secondary wave, slower transverse wave that ravels through near-surface rocks at 2-5km per second Characterized by shearing motion (i.e. shaken rope), the rock vibrates perpendicular to the direction of wave propagation • Both waves pass easily through solid rock. P wave can also pass through fluid (gas or liquid) but S wave can’t Surface Waves • Slowest waves set off by earthquakes, but cause more property damage than body waves because they produce more ground movement and takes longer to pass • 2 types: o Love waves – similar to S waves that have no vertical displacement. The ground moves side to side in a horizontal plate that is perpendicular to the direction of the wave travelling or propagating Do not travel through fluid Due to horizontal movement, love waves tend to knock buildings off their foundation and destroy highway bridge support www.notesolution.com o Rayleigh waves – behave like rolling ocean waves, it causes the ground to move in a elliptical path opposite to the direction the wave passes Incredibly destructive to buildings because they produce more ground movement and takes longer to pass How do we know where earthquakes occur? • Instrument we use to measure seismic waves is a seismometer o The principle of the seismometer is to keep a heavy suspended mass as motionless as possible – suspending it by springs or hanging it as a pendulum from the frame of the instrument o When the ground moves, the frame of the instrument moves with it, heavy mass suspended act as a point of reference in determining ground motion o Measure axis, X, Y and Z (3Dimensions) • A seismogram is a recording device that produces a permanent record of Earth motion detected by a seismometer, in digital format • Because of different types of waves that travel at different speeds, they arrive in seismograph stations in a definite order: o First P waves o S-waves o Finally surface waves • By analyzing seismograms, can learn about location, and size Determining the Location of an Earthquake • P and S waves start from the focus of an earthquake at essentially the same time. As they travel away from the quake, the 2 kinds of body waves gradually separate because they travel in different speeds • The farther the seismic waves travel (from focus to seismograph station) the longer the time interval between the arrival of P and S waves and more they are separated on the seismograms o This time interval can be used to determine the distance form the seismograph station to a quake o The increase in P-S interval is regular with increasing distance fro several thousands km and can be graphed in a travel-time curve = plots seismic wave arrival time against distance • Analyses of seismogram can also indicate at what depth beneath the surface the quake occurred, most quakes occur near the surface o The maximum depth of focus – the distance between focus and epicenter for quakes is about 670km o Quakes can be classified into 3 group according to their depth of focus: Shallow focus (0-70km deep) = most common 85% of total quake energy release Intermediate focus (70-350km deep) = 12% Deep focus (350-670km deep) = 3% Measuring the size of an earthquake • Size of earthquake can be measured in 2 ways: o Intensity – find out how much and what kind of damage the quake has causes. Measure of an earthquake’s effect on people and buildings Intensity is expressed in roman numerals from I to XII on the modified Mercalli scale (high number = greater damage) Limitations in using intensity as a measure of earthquake strength: • Damage lessens with distance intensities for same earthquake • Damage to buildings and other structures depend on type of geological material it was built on • Damage estimates are also subjective www.notesolution.com Advantage – doesn’t involve instruments o Magnitude – calculate the amount of energy released by the quake. Usually measure the height (amplitude) of one of the wiggles on a seismogram. The larger the quake, the more the ground vibrates, the larger the wiggle Report on
More Less

Only pages 1-2 are available for preview. Some parts have been intentionally blurred.

Unlock Document

Unlock to view full version

Unlock Document
Notes
Practice
Earn
Me

OR

Don't have an account?

Join OneClass

Access over 10 million pages of study
documents for 1.3 million courses.

Join to view

OR

By registering, I agree to the Terms and Privacy Policies
Just a few more details

So we can recommend you notes for your school.