Section 19.2 Day 1
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Transcript Section 19.2 Day 1
EXTRA CREDIT
OPPORTUNITY!
1. Attend the musical this
weekend.
2. Get the program signed by a
cast member.
3. Bring it to class next week.
4. Earn 10 EXTRA CREDIT
POINTS!
Thursday, May 6th
Agenda
Collect homework: “High Up in the
Himalayas” worksheet
Quiz over section 19.1
Begin Section 19.2: Earthquakes and
Volcanoes
Movie: “Earthquakes: Our Restless Planet”
Homework: “Plinian Eruptions” Worksheet
We will finish section 19.2 next time…
Section 19.1: Earth’s Interior and Plate
Tectonics Walk/Talk Quiz
Answer only the question that corresponds with
your birthday month.
Once everyone has answered their 1 question,
get up, walk and talk with your classmates to
complete the rest of the quiz.
Don‘t just copy their answer, read the question,
answer it yourself and see if you agree.
If you don’t, discuss it and try to come up with
the correct answer together. Good Luck!
What are Earthquakes?
Earthquakes occur at plate boundaries.
Earthquakes are vibrations resulting from
rocks sliding past each other at a fault
Seismic waves are waves of energy released
during in earthquake
Focus the area along a fault at which the
first motion of an earthquake occurs
Epicenter the point on Earth’s surface
directly above an earthquake’s focus
What are Earthquakes? continued
Energy from earthquakes is transferred by waves.
Earthquakes generate three types of waves:
Longitudinal waves
Transverse waves
Surface waves
Longitudinal waves travel by compressing and
stretching crust, also called primary waves (P
waves)
Transverse waves travel in an up and downward
movement, also called secondary waves (S
waves)
Surface waves seismic waves that can move only
through solids, move in a rolling circular motion
What are Earthquakes? continued
Waves move through Earth and along its
surface.
Both P waves and S waves spread out from
the focus in all directions through the earth.
Surface waves move only on Earth’s
surface.
Measuring Earthquakes
Seismologists detect and measure
earthquakes.
Seismology the study of earthquakes
including their origin, propagation, energy,
and prediction
Seismologists use sensitive equipment called
seismographs to record data about earthquakes.
Measuring Earthquakes, continued
Three seismograph stations are necessary to
locate the epicenter of an earthquake.
There are more than 1000 seismograph
stations across the world.
Because P waves travel faster, the
difference between the arrival of P waves
and the arrival of S waves allows scientists
to calculate how far away the focus is.
Measuring Earthquakes,
continued
Geologists use seismographs to investigate
Earth’s interior.
The way P and S waves travel through Earth’s
interior help scientists make a model of Earth
with layers of different densities.
Measuring Earthquakes,
continued
The Richter scale is a measure of the
magnitude of earthquakes.
Richter scale a scale that expresses the
magnitude of an earthquake
The intensity of an earthquake is measured by
the modified Mercalli scale. Intensity depends
on many factors.
Earthquakes that occur deeper below the
Earth’s surface will not be as intense at the
surface.
The hardness of the rock above and around an
earthquake affects the intensity.
Measuring Earthquakes,
continued
Scientists are trying to predict earthquakes.
Scientists are trying to measure changes in
Earth’s crust that might signal an earthquake.
The ability to predict an earthquake could
save thousands of lives in the future.
Movie:
“Earthquakes: Our Restless Planet”
Homework:
– “Plinian Eruptions” Worksheet
Have a GREAT
weekend!!