Lesson 2: Faulting and Seismic Zones in the Philippines Flashcards

1
Q

officially reported to have caused 250,000 deaths of the 750,000 inhabitants

A

Tangshan, China earthquake (1976)

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2
Q

during the Tangshan China earthquake, the city was leveled and over _____ of the city’s 750,000 inhabitants were killed

A

250,000

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3
Q

an earthquake happened on October 15, 2013

A

Bohol earthquake

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4
Q

magnitude of Bohol earthquake

A

M7.2

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5
Q

maximum intensity of Bohol earthquake

A

IX

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6
Q

the epicenter of Bohol earthquake

A

Inabanga, Bohol

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7
Q

damages of an earthquake

A
  • damage to infrastructure
  • damage to government building
  • collapse of residential structure
  • damage to commercial building
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8
Q

the Philippine fault is _____ long

A

1250 km

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9
Q

the Philippine fault is an arc-parallel _____ extending NNW parallel to the Philippine archipelago

A

strike-slip fault

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10
Q

this fault traverses Luzon and Mindanao Islands where most economic and population centers of the country
are located

A

Philippine fault

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11
Q

the _____ on the Philippine fault is interpreted to be a result of oblique subduction of the Philippine sea plate beneath the Sunda plate

A

left-lateral motion

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12
Q

GPS surveys depicted _____ left-lateral motion on the Philippine fault

A

20-30 mm/year

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13
Q

it is seismically active with several surface-rupturing earthquakes in the past 200 years

A

Philippine fault

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14
Q

the PFZ traverses the eastern edge of Masbate parallel to the coastline for a length of _____

A

30 km

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15
Q

the calculated slip rate on Masbate island

A

2 mm/year

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16
Q

magnitude of Masbate earthquake 2003

A

M6.2

17
Q

epicenter of Masbate earthquake 2003

A

Naro Bay

18
Q

three major segments of the central Philippine fault zone (PFZ)

A
  • Guinyangan fault
  • Masbate fault
  • Central Leyte fault
19
Q

the location of large major events that have recurrence intervals as short as 65 years

A

Guinyangan fault

20
Q

a transition zone characterized by large and medium earthquakes accompanied by unusually large ground rupture with post-seismic deformation and possibly slow slip components

A

Masbate fault

21
Q

recurrence intervals along this zone range from 5 to 10 years

A

Masbate fault

22
Q

characterized by creep and by medium-sized events usually with clusters of foreshocks that serve as warning to the impending mainshocks

A

Central Leyte fault (NCLF and SCLF)