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LOCATING AN EARTHQUAKE
& CONTINENTAL DRIFT
THEORY
LESSON 4 and 5
How does a
seismologist determine
the location of the
epicenter of an
earthquake if it is too
far from the seismic
station?
TRIANGULAT
ION METHOD
When an earthquake
occurs, seismic waves
radiate out from the
focus and cause
vibrations on the earth’s
surface.
SPEED
P-waves travel at a rate
of 6km/s while S-waves
travel at 4km/s.
Time Lag
Difference between the arrival of
P-waves and S-waves at the
seismograph station.
D =
𝑻𝒅 (𝒔)
𝟖 𝒔𝒆𝒄𝒐𝒏𝒅𝒔
x 100km
At each station, we can draw a
circle on a map that has a
radius equal to the distance to
the epicenter from each station.
The three circles will intersect at
a point that locates the
epicenter.
PROBLEM SOLVING D =
𝑻𝒅 (𝒔)
𝟖 𝒔𝒆𝒄𝒐𝒏𝒅𝒔
x 100km
Recording Station Time difference Distance of the station to
the epicenter
Puerto Princesa 32 seconds 400km
Batangas 44.8 seconds 560km
Davao 38.4 seconds 480km
Continental
Drift
Theory
Has the Earth always
looked the way it is now?
Evidences of the
continental drift
theory
• THE JIGSAW FIT. Continents
were once one in their
shapes. The edge of the
different continents fit the
edge of another. For instance,
South American and West
African coastlines show the
best jigsaw fit.
• FOSSIL EVIDENCE.
Glossopteris was a woody,
seed-bearing shrub or tree.
Fossils of this plant are found
in Australia, South Africa,
South America, India and
Antarctica.
Evidences of the
continental drift
theory
• ROCK EVIDENCE. The broad
belts of rocks and mountains
of South America and Africa
line up perfectly as if they
were once a long mountain
range.
• COAL DEPOSITS EVIDENCE.
Looking at the current
location of Antarctica, living
things could barely survive
there now. If scientists found
coal deposits there, it could
mean that Antarctica might
have been closer before to
the Equator where it had a
warmer climate and could
sustain life.

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Continental drift.pptx

  • 1. LOCATING AN EARTHQUAKE & CONTINENTAL DRIFT THEORY LESSON 4 and 5
  • 2. How does a seismologist determine the location of the epicenter of an earthquake if it is too far from the seismic station?
  • 3. TRIANGULAT ION METHOD When an earthquake occurs, seismic waves radiate out from the focus and cause vibrations on the earth’s surface.
  • 4. SPEED P-waves travel at a rate of 6km/s while S-waves travel at 4km/s.
  • 5. Time Lag Difference between the arrival of P-waves and S-waves at the seismograph station. D = 𝑻𝒅 (𝒔) 𝟖 𝒔𝒆𝒄𝒐𝒏𝒅𝒔 x 100km At each station, we can draw a circle on a map that has a radius equal to the distance to the epicenter from each station. The three circles will intersect at a point that locates the epicenter.
  • 6. PROBLEM SOLVING D = 𝑻𝒅 (𝒔) 𝟖 𝒔𝒆𝒄𝒐𝒏𝒅𝒔 x 100km Recording Station Time difference Distance of the station to the epicenter Puerto Princesa 32 seconds 400km Batangas 44.8 seconds 560km Davao 38.4 seconds 480km
  • 7. Continental Drift Theory Has the Earth always looked the way it is now?
  • 8. Evidences of the continental drift theory • THE JIGSAW FIT. Continents were once one in their shapes. The edge of the different continents fit the edge of another. For instance, South American and West African coastlines show the best jigsaw fit. • FOSSIL EVIDENCE. Glossopteris was a woody, seed-bearing shrub or tree. Fossils of this plant are found in Australia, South Africa, South America, India and Antarctica.
  • 9. Evidences of the continental drift theory • ROCK EVIDENCE. The broad belts of rocks and mountains of South America and Africa line up perfectly as if they were once a long mountain range. • COAL DEPOSITS EVIDENCE. Looking at the current location of Antarctica, living things could barely survive there now. If scientists found coal deposits there, it could mean that Antarctica might have been closer before to the Equator where it had a warmer climate and could sustain life.