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Lesson 1: Identifying Places Where Earthquakes Occur
Lesson 2: Describing an Earthquake and Its Effect
Lesson 3:Predicting Earthquakes
Prepared by:
Marissa A. Jore
How Earthquakes are
Generated?
• Earth is made up of distinct layers: Crust
(oceanic crust and continental crust),
upper and lower mantle, and outer core
and inner core. Of these layers,
earthquakes occur somewhere in the
crust and lithosphere. The crust is the
outermost solid portion of the Earth that
houses all living things. It is
characterized by various land features
that you are commonly familiar with like
volcanoes, islands, continents, and
mountains.
How Earthquakes are
Generated?
• The lithosphere is a region that
carries the entire crust that
extends down to the upper
portion of the asthenosphere.
The lithosphere, as previously
mentioned, have segments called
tectonic plates or lithospheric
plates. Thus, the lithosphere is a
singular collection of lithospheric
plates.
How Earthquakes are
Generated?
• Each scientists found out that the
lithosphere is “elastic solid” such
that similar to the rocks of Earth’s
crust, the rocks here are elastic
but brittle that they deform or
fracture as they receive and store
stress due to the force rendered
by the movement of rocks in the
asthenosphere below it.
How Earthquakes are
Generated?
• The upper mantle, also known as
the asthenosphere, from the
Greek word asthenes meaning
“weak” and sphere, lies beneath
the lithosphere. It is about 100 –
650km deep and is considered
“plastic solid”. The rocks in the
asthenosphere are partially
molten due to high pressure and
temperature where they exposed.
How Earthquakes are
Generated?
•This characteristic, “plastic solid”
allows the partially molten rocks
to flow in convection pattern in
the asthenosphere. As these rocks
flow, the overriding lithosphere
(or lithospheric plates) that
carries the crust move along with
it.
How Earthquakes are
Generated?
•Scientists believe that this
extremely slow movement or
tectonic force enable lithospheric
plates to collide (caused by
compressional force), separate
(caused by tensional force), or
slide past each other ( caused by
shearing force).
How Earthquakes are
Generated?
•As lithospheric plates and the
crust moves overtime, their rocks
interlock and deform, which
cause stress and friction to build
up. When the amount of stress
and fiction exceeds the strain
threshold of rocks, they fracture
How Earthquakes are
Generated?
Earthquake and Tsunami
Adam lifts a 10 kg mass from the floor
and puts in on a table 5 meter high.
What is the work done?
__________________________
A fourth grade class has 22 students.
Each box of crayons has 24 colors. If
each student brings 2 boxes crayons
for school supplies, how many
crayons is that in all?
PARTS OF AN EARTHQUAKE: FOCUS
AND EPICENTER
How Earthquakes are measured:
Intensity and Magnitude
What is Intensity?
•measures the observed effects of an earthquake
on people, geologic structures, and man – made
structures. Intensity varies from one location to
another. The severity of disaster rendered by an
earthquake on certain location depends on the
design and kind of the construction materials that
were used and the type of ground or soil edifice
where infrastructures are built.
What is Intensity?
• One popular and currently used scale is Modified
Mercalli Intensity
( MMI ) Scale.
• Guiseppe Mercalli, an Italian seismologist, complied
the original scale in 1902.
What is Magnitude?
• pertains to the strength and the “size” of an earthquake.
• It is measured of the amount of energy released by an earthquake at
the epicenter using mathematical formulas and the information from
seismograms.
• measured by the Richter Scale developed by Charles Richter, an
American seismologist in 1935.
Describing an Earthquake and Its
Effects
How underwater Earthquake
Generates Tsunamis
• Tsunami – is a series of huge waves caused by an
earthquake that occurs underneath or near the ocean.
It is a Japanese term that means “ harbor waves “ .
• can also be generated by underwater volcanic
eruptions and landslides and rarely by the impact of
an asteroid or a meteoroid crashing into the ocean
from outer space.
TSUNAMI
• can be very large – their wave height can reach up to 30
feet or more.
• can travel at great speed exceeding 500 miles per hour (
as fast as a jet flies )
• For an underwater earthquake to cause tsunamis, its
magnitude should be over 6.75 on the Richter Scale.
•Earthquake Waves and
the Interior of the Earth
What’s Inside the Earth?
• Comparatively seismic waves move more inward into the crust,
they speed up. This suggests that at the bottom the rocks are
denser. In the uppermost part of the mantle, the waves decrease
down. That means the rocks there are partly melted.
• As the waves enter the core, one variety of seismic waves (s-
waves) disappears. That suggests that the outer core is liquid. At
particular depths, the waves are reflected and refracted (bent).
That means the Earth must exist layered.

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Earthquake and tsunami

  • 2. Lesson 1: Identifying Places Where Earthquakes Occur Lesson 2: Describing an Earthquake and Its Effect Lesson 3:Predicting Earthquakes Prepared by: Marissa A. Jore
  • 3.
  • 4.
  • 5.
  • 6. How Earthquakes are Generated? • Earth is made up of distinct layers: Crust (oceanic crust and continental crust), upper and lower mantle, and outer core and inner core. Of these layers, earthquakes occur somewhere in the crust and lithosphere. The crust is the outermost solid portion of the Earth that houses all living things. It is characterized by various land features that you are commonly familiar with like volcanoes, islands, continents, and mountains.
  • 7. How Earthquakes are Generated? • The lithosphere is a region that carries the entire crust that extends down to the upper portion of the asthenosphere. The lithosphere, as previously mentioned, have segments called tectonic plates or lithospheric plates. Thus, the lithosphere is a singular collection of lithospheric plates.
  • 8. How Earthquakes are Generated? • Each scientists found out that the lithosphere is “elastic solid” such that similar to the rocks of Earth’s crust, the rocks here are elastic but brittle that they deform or fracture as they receive and store stress due to the force rendered by the movement of rocks in the asthenosphere below it.
  • 9. How Earthquakes are Generated? • The upper mantle, also known as the asthenosphere, from the Greek word asthenes meaning “weak” and sphere, lies beneath the lithosphere. It is about 100 – 650km deep and is considered “plastic solid”. The rocks in the asthenosphere are partially molten due to high pressure and temperature where they exposed.
  • 10. How Earthquakes are Generated? •This characteristic, “plastic solid” allows the partially molten rocks to flow in convection pattern in the asthenosphere. As these rocks flow, the overriding lithosphere (or lithospheric plates) that carries the crust move along with it.
  • 11. How Earthquakes are Generated? •Scientists believe that this extremely slow movement or tectonic force enable lithospheric plates to collide (caused by compressional force), separate (caused by tensional force), or slide past each other ( caused by shearing force).
  • 12. How Earthquakes are Generated? •As lithospheric plates and the crust moves overtime, their rocks interlock and deform, which cause stress and friction to build up. When the amount of stress and fiction exceeds the strain threshold of rocks, they fracture
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  • 20. Adam lifts a 10 kg mass from the floor and puts in on a table 5 meter high. What is the work done? __________________________
  • 21. A fourth grade class has 22 students. Each box of crayons has 24 colors. If each student brings 2 boxes crayons for school supplies, how many crayons is that in all?
  • 22. PARTS OF AN EARTHQUAKE: FOCUS AND EPICENTER
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  • 24. How Earthquakes are measured: Intensity and Magnitude
  • 25. What is Intensity? •measures the observed effects of an earthquake on people, geologic structures, and man – made structures. Intensity varies from one location to another. The severity of disaster rendered by an earthquake on certain location depends on the design and kind of the construction materials that were used and the type of ground or soil edifice where infrastructures are built.
  • 26. What is Intensity? • One popular and currently used scale is Modified Mercalli Intensity ( MMI ) Scale. • Guiseppe Mercalli, an Italian seismologist, complied the original scale in 1902.
  • 27. What is Magnitude? • pertains to the strength and the “size” of an earthquake. • It is measured of the amount of energy released by an earthquake at the epicenter using mathematical formulas and the information from seismograms. • measured by the Richter Scale developed by Charles Richter, an American seismologist in 1935.
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  • 29. Describing an Earthquake and Its Effects
  • 30. How underwater Earthquake Generates Tsunamis • Tsunami – is a series of huge waves caused by an earthquake that occurs underneath or near the ocean. It is a Japanese term that means “ harbor waves “ . • can also be generated by underwater volcanic eruptions and landslides and rarely by the impact of an asteroid or a meteoroid crashing into the ocean from outer space.
  • 31. TSUNAMI • can be very large – their wave height can reach up to 30 feet or more. • can travel at great speed exceeding 500 miles per hour ( as fast as a jet flies ) • For an underwater earthquake to cause tsunamis, its magnitude should be over 6.75 on the Richter Scale.
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  • 34. •Earthquake Waves and the Interior of the Earth
  • 35. What’s Inside the Earth? • Comparatively seismic waves move more inward into the crust, they speed up. This suggests that at the bottom the rocks are denser. In the uppermost part of the mantle, the waves decrease down. That means the rocks there are partly melted. • As the waves enter the core, one variety of seismic waves (s- waves) disappears. That suggests that the outer core is liquid. At particular depths, the waves are reflected and refracted (bent). That means the Earth must exist layered.