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Prepare the
following:
 Folder
 Fault Model
 Scissors
 Glue
 Ruler
 Colored Paper
(Green, Brown,
and Blue) or
Colors
 Epicenter
• Point directly above the focus
 Hypocenter
• The source from which the
energy is released radiating
from all directions.
 Fault Plane
• The surface along which the plate
breaks and slides
 Fault Zone
• The region with prominent but less
dense fractures and deformations
that mark the end of the fault plane
The large fractures in rocks formed
by shifting or dislodging of parts of
the Earth’s crust, often when
adjacent surfaces moved with
respect to each other.
Two types according to
displacement of the plates
Three types according to
geometry and orientation
 Where earthquakes are most
likely to happen in the future.
 There are recorded seismic
activities in the last 10,000 years
Marikina Valley Fault:
 Montalban
 San Mateo
 Marikina
 Pasig
 Taguig
 Muntinlupa
 San Pedro
 Biñan
 Carmona
 Santa Rosa
 Calamba
 Tagaytay
 Oriental Mindoro
Western Philippine
Fault:
 Luzon Sea
 Mindoro Strait
 Panay Gulf
 Sulu Sea
Eastern Philippine Fault:
 Philippine Sea
Southern of Mindanao
Fault:
 Moro Gulf
 Celebes Sea
Central Philippine Fault:
 Entire Ilocos Norte
 Aurora
 Quezon
 Masbate
 Eastern Leyte
 Southern Leyte
 Agusan Del Norte
 Agusan Del Sur
 Davao del Norte
 There are no seismic activities
in the last 10,000 years
 May possibly generate an
earthquake in the future
http://faultfinder.phivolcs.dost
.gov.ph/
 Dip-Slip Fault (Normal and Reverse)
 Strike-Slip Fault (Left-lateral and Right-lateral)
 Oblique-Slip Fault
Hanging wall movement
determines the geometric
classification of faulting
The hanging wall moved
predominantly up or down relative
to the footwall
• Normal Fault
• Reverse Fault
 The hanging wall
slips down relative
to the footwall
 Happens at
divergent
boundaries
The hanging wall
slides over the
footwall.
Happens at
convergent
boundaries
The motion of
plates are
horizontal
 If the hanging wall moves
to the left, the
earthquake is called
right-lateral strike-slip
fault
 If it moves to the right,
it's called a left-lateral
strike-slip fault
The hanging wall motion
is neither dominantly
vertical nor horizontal,
the motion is called
oblique-slip.
An instrument used to detect and
record seismic waves
SEISMOGRAPH
Seismogram is a record written by a seismograph in
response to ground motions produced by an earthquake

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Types of Faults

  • 1. Prepare the following:  Folder  Fault Model  Scissors  Glue  Ruler  Colored Paper (Green, Brown, and Blue) or Colors
  • 2.
  • 3.
  • 4.
  • 5.  Epicenter • Point directly above the focus  Hypocenter • The source from which the energy is released radiating from all directions.
  • 6.
  • 7.  Fault Plane • The surface along which the plate breaks and slides  Fault Zone • The region with prominent but less dense fractures and deformations that mark the end of the fault plane
  • 8. The large fractures in rocks formed by shifting or dislodging of parts of the Earth’s crust, often when adjacent surfaces moved with respect to each other.
  • 9. Two types according to displacement of the plates Three types according to geometry and orientation
  • 10.  Where earthquakes are most likely to happen in the future.  There are recorded seismic activities in the last 10,000 years
  • 11. Marikina Valley Fault:  Montalban  San Mateo  Marikina  Pasig  Taguig  Muntinlupa  San Pedro  Biñan  Carmona  Santa Rosa  Calamba  Tagaytay  Oriental Mindoro
  • 12. Western Philippine Fault:  Luzon Sea  Mindoro Strait  Panay Gulf  Sulu Sea Eastern Philippine Fault:  Philippine Sea Southern of Mindanao Fault:  Moro Gulf  Celebes Sea
  • 13. Central Philippine Fault:  Entire Ilocos Norte  Aurora  Quezon  Masbate  Eastern Leyte  Southern Leyte  Agusan Del Norte  Agusan Del Sur  Davao del Norte
  • 14.  There are no seismic activities in the last 10,000 years  May possibly generate an earthquake in the future
  • 16.  Dip-Slip Fault (Normal and Reverse)  Strike-Slip Fault (Left-lateral and Right-lateral)  Oblique-Slip Fault
  • 17. Hanging wall movement determines the geometric classification of faulting
  • 18. The hanging wall moved predominantly up or down relative to the footwall • Normal Fault • Reverse Fault
  • 19.  The hanging wall slips down relative to the footwall  Happens at divergent boundaries
  • 20. The hanging wall slides over the footwall. Happens at convergent boundaries
  • 21. The motion of plates are horizontal
  • 22.  If the hanging wall moves to the left, the earthquake is called right-lateral strike-slip fault  If it moves to the right, it's called a left-lateral strike-slip fault
  • 23.
  • 24. The hanging wall motion is neither dominantly vertical nor horizontal, the motion is called oblique-slip.
  • 25.
  • 26. An instrument used to detect and record seismic waves
  • 28. Seismogram is a record written by a seismograph in response to ground motions produced by an earthquake