This document provides information about earthquakes, including: 1. The key learning objectives are to recognize what earthquakes are, investigate their causes, describe how they are measured, and illustrate prevention methods. 2. Earthquakes are caused by the sudden release of energy from tectonic plate movement along faults in the Earth's crust. They can be measured using seismographs which detect seismic waves. 3. Safety tips during earthquakes include staying away from windows and heavy objects, taking cover under a sturdy table, and staying indoors until the shaking stops.

1. Teacher
Kevin

2. EARTHQUAKE

4. Learning Objectives
1. recognize what is an earthquake;
2. investigate the causes of earthquakes;
3. describe how earthquakes can be
measured; and
4. illustrate on how can they prevent from
an earthquake.
At the end of the lesson, the student/s will be able to:

5. Key Terms
Earthquake – Movement of the earth’s
crust caused by tectonic plate action.
Fault - is a fracture or zone of fractures
between two blocks of rock.
Epicentre – The point on the earths crust
directly above the focus (where most
damage occurs)
Seismograph – An instrument used to
measure the strength of an earthquake
Focus – The point under the crust where
the earthquake occurred.

6. What do you see in the photo shown
above?

7. What are Earthquakes?
• The shaking or trembling caused by the sudden release of
energy.
• Usually associated with faulting or breaking of rocks.
• Continuing adjustment of position results in aftershocks.

8. Faults
■ Faults are blocks of the earth’s crust that meet together.
Scientists identify four types of faults, characterized by the position
of the fault plane, the break in the rock and the movement of the
two rock blocks.
■ Faults lines are under enormous pressure from the two pieces of
the earth’s crust pushing together.
■ The faults will eventually give way to the pressure causing
earthquakes and creating mountain ranges.

9. Types of Faults

10. Types of Faults
Strike-slip fault Normal fault Reverse fault
strike-slip fault - a
fault on which the
two blocks slide
past one
another. The San
Andreas Fault is an
example of a right
lateral fault.
normal fault - a
dip-slip fault in
which the block
above the fault has
moved downward
relative to the block
below.
Reverse Fault -
formed by
compressional
forces that push the
plates towards each
other.

11. Types of Faults observed on a large scale
Strike-slip fault in San
Andreas Fault
Normal fault on the
coast of Somerset,
England
Reverse fault in the
Grands Causses in
Bédarieux, France

12. ACTIVE FAULT LINES
IN THE PHILIPPINES

13. The fault lines in the Philippines
Fault lines Affected areas
1. Central Philippine Fault Entire Ilocos Norte, Aurora, Quezon,
Masbate, Eastern Leyte, Southern
Leyte, Agusan Del Norte, Agusan Del
Sur, Davao Del Norte.
2. Marikina Valley Fault Montalban, San Mateo, Marikina,
Pasig, Taguig, Muntinlupa, San
Pedro,Binan, Carmona, Santa Rosa,
Calamba, Tagaytay, Oriental
Mindoro.
3. Western Philippine Fault Luzon Sea, Mindoro Strait, Panay
Gulf, Sulu Sea.
4. Eastern Philippine Fault Philippine Sea
5. Southern of Mindanao Fault Moro Gulf, Celebes Sea

14. EARTHQUAKE IN THE
PHILIPPINES
Pacific Ring of Fire
- where the Philippines is located and
it is a series of interconnected seismic
plates that cause earthquakes and
volcanic eruptions.
- the country sits on the Philippine
plate, which is sandwiched by the
Pacific Plate and Indian Plate.

15. What Causes
an
Earthquake?

16. When plates collide or rub past each other,
they can cause the Earth to shake.
This is because friction stops them from
moving easily

17. The point inside the crust
where the pressure is
released is called the
focus.
Earthquake energy is released in seismic waves. These waves
spread out from the focus. The waves are felt most strongly at the
epicentre, becoming less strong as they travel further away.
The point on the Earth's
surface above the focus is
called the epicentre.
The most severe damage caused by an earthquake will happen close
to the epicentre.

18. What are Seismic Waves?
• Response of material to the arrival of
energy fronts released by rupture
• Two types:
–Body waves
• P and S
–Surface waves
• R and L

19. Body Waves: P and S waves
• Body waves
– P or primary waves
• fastest waves
• travel through solids,
liquids, or gases
• compressional wave,
material movement is in
the same direction as
wave movement
– S or secondary waves
• slower than P waves
• travel through solids only
• shear waves - move
material perpendicular to
wave movement

20. Surface Waves: R and L waves
• Surface Waves
– Travel just below or along the ground’s surface
– Slower than body waves; rolling and side-to-side movement
– Especially damaging to buildings

21. How are the Size and Strength
of an Earthquake Measured?

22. This measures the magnitude of a tremor (how
powerful it is) using an instrument called a
seismograph.
On the Richter Scale, magnitude is expressed in
whole numbers and decimal fractions. Although the
Richter Scale has no upper limit, the largest
earthquake ever recorded was in 1960 in Chile. It
measured 9.5 on the Richter Scale.
It is a logarithmic scale which means that a size ‘6’
on the Richter Scale is 10 times larger than a size
‘5’ and 100 times larger than a size ‘4’.
The Richter Scale

23. Ritcher Scale- designed
by Dr. Charles F.
Ritcher of the
California Institute of
Technology.
- is the best known
logarithmic scale in
measuring the
magnitude( strength of
the shock waves) of
earthquakes.

24. are instruments
used to record the
motion of the
ground during an
earthquake. They
are installed in the
ground throughout
the world and
operated as part of
a seismographic
network.
SEISMOGRAPH
, OR
SEISMOMETER

25. - is a service institute of the Department of
Science and Technology (DOST) that is
principally mandated to mitigate disasters
that may arise from volcanic eruptions,
earthquakes, tsunami and other related
geotectonic phenomena.

26. MODIFIED VERSION OF THE RICHTER SCALE
Magnitude General Description Damage Expected
8 and up National Disaster Complete Destruction
7 to 8 Major Earthquake Major damage to all buildings;
crust’s surface cracks
6 to 7 Destructive earthquake Collapse of some structures
5 to 6 Damaging earthquake Poorly constructed buildings
are damaged
4 to 5 Strong earthquake Trees broken; sleepers are
awakened
3 to 4 Small earthquake Some fragile are broken
0 to 3 Tremor Barely felt, but sound of
tinkling glass can be heard.

27. Analyzing a seismogram
enables seismologist to
determine the time, focus,
and epicenter, as well as
the amount of energy
released by the movement
of the rock masses.

28. Level of
Earthquake
Instrumental
Detected only by
Seismograph
I Instrumental Detected only by seismograph
II Feeble Noticed only by sensitive people
III Slight Resembling vibrations caused by heavy traffic
IV Moderate Felt by people walking; rocking of free-standing
objects
V Rather strong Sleepers awakened and bells ring
VI Strong Trees sway, some damage from overturning and
falling objects
VII Very strong General alarm, cracking of walls

29. Level of
Earthquake
Instrumental Detected only by Seismograph
VIII Destructive Chimneys fall and there is some damage to
buildings
IX Ruinous Ground begins to crack, houses begins to collapse,
and pipes reak
X Disastrous Ground badly cracked and many buildings are
destroyed. There are some landslides.
XI Very disastrous Few buildings remain standing; bridges and
railways destroyed, water, gas, electricity and
telephones out of action
XII Catastrophic Total destruction; objects are thrown into the air,
much heaving, shaking, and distortion of the
ground.

30. Earthquake Safety

31. Family Readiness
•Know the safe spot in each room
•Know the danger spots
•Decide where your family will reunite if separated
•Keep a list of emergency phone numbers
•Develop a survival kit for work, car, and home

32. Home Preparedness
•Learn how to shut off gas, water,
and electricity
•Check chimneys, roofs, and wall
foundations for stability
•Secure heavy furnishings
•Secure water heater and
appliances
•Keep heavy objects on lower
shelves
•Maintain emergency food, water,
medicine, first aid kit, tools, and
clothing

33. During an Earthquake
•Stay away from windows, bookcases, file cabinets, heavy mirrors, and other heavy objects
that could fall
•Duck under a desk or sturdy table
•Watch for falling plaster or ceiling tiles
•Stay undercover until the shaking stops, and hold onto your cover
•If the desk or table you are under moves… move with it
•If in your car, stop, but not on a
bridge, or under trees or a power
line
•If outside, stay outside, and move
to an area clear of overhead trees,
power lines, or objects that could
fall from a structure
•Don’t forget about aftershocks

34. After The Earthquake
•Be prepared for aftershocks, plan for cover when they occur
•Check for injuries, give first aid as necessary
•Remain calm, try to reassure others
•Wear shoes to avoid injury from broken glass
•Check for fire and take appropriate actions
•Check gas, water, and electric lines
•Tune to emergency broadcast system on radio

36. Activity:
Think.Pause.Reflect