NEW ORMOC CITY NATIONAL HIGH SCHOOL
Lesson Plan in Science and Technology 10
Unit I: Earth and Space
Module 2: Earth’s Interior
7:45- 8:45 FIDELITY (M-F)
1:00-2:00 SPA PROBITY (M-F)
Lesson Plan no.
Date: JUNE 22, 2019
11:00-12:00 DEVOTION (M-F)
3:00-4:00 SPS (M-F) 4:00-5:00 SPS (M-F)
GRADE LEVEL
10
CONTENT STANDARD
The learners demonstrate an understanding of the relationship among the locations
of volcanoes, earthquake epicenters, and mountain ranges.
PERFORMANCE STANDARD
The learners shall be able to:
1. demonstrate ways to ensure disaster preparedness during earthquakes, tsunamis,
and volcanic eruptions
2. suggest ways by which he/she can contribute to government efforts in reducing damage
due to earthquakes, tsunamis, and volcanic eruptions
a Describe the internal structure of the Earth. S10ES –Ia-j-36.4
I. LEARNING COMPETENCIES
AND OBJECTIVES
Subtask/s:
1. Describe the different types of seismic waves.
2. Differentiate between body waves and surface waves.
3. Differentiate love and Rayleigh waves and P-waves and S-waves.
Integration of Language Strategy:
1. Describe the different types of seismic waves using taxonomy of words and
metacognition.
II.CONTENT
III. LEARNING RESOURCES
A. TOPIC: S10ES-Ia-j-36.4- Internal Structure of the Earth: Seismic waves
B. TIME FRAME: 2 hours
C. MATERIAL/s: LM, CG, TG, chart, photographs, chalkboard and art materials. Video from
youtube
D. REFERENCES: : LM pp. 39-79, TG pp. 27-51, CG p. xxix
E. Other References: Science Explorer, Prentice Hall, Joseph D. Exline, Ed.D., et.al,
pp. 4-15
www. Youtube.com( Simulation of P,S, love and Rayleigh propagation)
DCCM X: Trade and Industry No. 2 Leyte Geothermal Production Field (LGPF), Tongonan,
Ormoc City
DRRM- Earthquake 2017 (Tongonan)
*Test Item Bank- Quarter I
IV. PROCEDURE
Elicit
A.
- Identify the wave characteristics being shown. Label the figure, use the paper strips provided.
B.
- Name the different layers of the Earth according to composition ( outermost- innermost).
Wavelengt
h
Trough
Crest
111
112
113
Amplitude
-Enumerate the layers of the Earth according to Physical properties.
LAMOI-
C. DEFINITION OF TERMS(:
1. Seismograph - a device that records ground movements caused by seismic waves as they
move through Earth.
2. Wave – a disturbance that repeats regularly in space and time (energy) and that is transmitted
from one place to the next.
3. Wave propagation- is any of the ways in which waves travel.
4. Radiate- emit in the form of rays or waves / spread from or as if from a central point.
Engage
- The viewing deck of EDC- Tongonan Geothermal Power Plant
before and after the 6.5 magnitude earthquake hit Ormoc.
- Impacts of the 06 July 2017 M6.5 Leyte Earthquake.
How did Seismologists measure the magnitude of the Earthquake that hit Brgy. Tongonan?
How did they know that there are layers beneath the earth’s surface?
Why does Earth’s crust move?
Explore
1. Go to your group
2. Read the procedure very carefully
Activity Amazing Waves!
Objectives:
1. Define seismic waves scientifically.
2. Differentiate between body waves and surface waves.
3. Differentiate love and Rayleigh waves and P-waves and S-waves.
4. Demonstrate how each type of seismic wave propagates.
Procedure:
1. Using the given organizer, write the necessary information (word/s or phrase/phrases) to complete the
concept about seismic waves.
Guide questions:
Q1. Using the words you have written in each box construct a sentence/s to describe the characteristic/s
of each type of wave.
Q2. Differentiate surface waves from body waves.
Q3. Differentiate Primary waves from secondary waves.
Q4. Differentiate Love waves from Rayleigh waves.
Q5. Which type of waves do you think were useful to seismologists in their study of the Earth’s interior?
Explain your answer.
Explain
Discuss the following:
Seismic waves – are mechanical vibrations that occur inside the Earth ( along fault lines), which is caused
by the breakage of rocks.
Seismic waves – energy waves within the Earth
that are released when plates move and travels
through the Earth.
Seismic waves are classified as surface waves and
body waves.
Seismic waves from even small earthquakes can
travel around the world.
Surface wave – the types of wave that travels
through the surface of the Earth (crust or
lithosphere): classified as love and rayleigh waves.
Move more slowly than body waves.
Love wave – is the faster type of surface wave that travel along the surface of the Earth from the
point directly above the epicenter.
the type of wave that move the ground in a side to side manner.
Most damaging type, faster than Rayleigh waves.
Named after a mathematician Augustus Edward H. Love who worked on mathematical models to
demonstrate the propagation of surface waves.
Rayleigh wave – the type of surface wave that moves the ground in a circular manner,
combination of a longitudinal compression and dilation that results in an elliptical motion of
points on the surface.
Move in a circular manner similar to rolling on the ground, causes the ground to move up and
down and side to side.
Causes the ground to shake during an earthquake.
spread out most in time, producing a long wave duration on seismograph.
Named after John William Strutt, also known as Lord Rayleigh, whose mathematical modeling
predicted the possibility of this type of waves.
Body wave – type of seismic wave that travel through the inner layers of the Earth: classified as
Primary (P) waves and Secondary (S) waves.
Primary wave or P-wave – type of body wave that move in a back and forth motion.
- The faster body wave, moves at speeds between 1.5 to 8 km/s.
- compressional waves or longitudinal waves.
- The particles vibrate parallel to the direction of wave motion, the particles are compressed
and stretched.
- Can travel through solid, liquid and gas.
Secondary wave or S-wave – type of body wave that move in an up and down motion.
- transverse waves
- the particles vibrate perpendicular to the direction of wave motion
- slower than P-waves and can travel throug solids only.
- Travels 60% to 70% slower than P-waves.
-
Elaborate
Describe the seismic waves.
Differentiate between body waves and surface waves.
Differentiate love and Rayleigh waves and P-waves and S-waves.
How do scientists determine the composition and structure of the Earth’s interior?
Complete the following statements :
Subject Theme: Seismic waves
Metacognition for stating knowledge
My chosen word is_____________
I know that I know something _______________
First I know that _____________________
In addition, I know __________________
Finally I know____________________
Now, you know something that I know ________________
2. Describe the different types of seismic waves in terms of how they propagate from the focus to the
different layers of the Earth through a demonstration.
Evaluate A. Cloze Test
Directions: Fill in the blanks with the correct term that would complete the thought of the paragraph.
During an earthquake energy radiates in all directions from its focus in the form of a wave called
___ (1)____. There are __(2)____ main types of it, as classified according to the earth layer it penetrates.
Both Love and Rayleigh waves are confined to the outer layers of the earth only, thus collectively called
_(3)____ waves. Body waves include __(4)____ wave which reaches the detector first and secondary
wave that cannot travel through any ___(5)____ medium.
B.
Extend
TITLE: JOURNEY WITH SEISMIC WAVES
V. Remarks and Reflection
___________________________________________________ Prepared by:
LIEZL I. MALINAO-FLORES
Subject Teacher
No. of Learners with mastery Level:___________
Checked :
No. of Learners needing remediation:__________
______________ ______________ ______________
Observed:
_____________ _____________ _____________ _____________