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Alan R. Nelson, Stephen F. Personius, Rolly E. Rimando, Raymundo S. Punongbayan, Norman Tungol, Hannah Mirabueno, and Ariel Rasdas
Multiple large earthquakes in the past 1500 years on a fault in metropolitan Manila, the Philippines
Bulletin of the Seismological Society of America (February 2000), 90(1):73-85

Abstract:
The first 14 C-based paleoseismic study of an active fault in the Philippines shows that a right-lateral fault on the northeast edge of metropolitan Manila poses a greater seismic hazard than previously thought. Faulted hillslope colluvium, stream-channel alluvium, and debris-flow deposits exposed in trenches across the northern part of the west Marikina Valley fault record two or three surface-faulting events. Three eroded, clay-rich soil B horizons suggest thousands of years between surface faulting events, whereas 14 C ages on detrital charcoal constrain the entire stratigraphic sequence to the past 1300-1700 years. We rely on the 14 C ages to infer faulting recurrence of hundreds rather than thousands of years. Minimal soil development and modern 14 C ages from colluvium overlying a faulted debris-flow deposit in a nearby stream exposure point to a historic age for a probable third or fourth (most recent) faulting event.

Index Terms/Descriptors:
Asia; C-14; carbon; Cenozoic; earthquakes; Far East; faults; Holocene; isotopes; magnitude; Manila Philippine Islands; Marikina Valley; paleoseismicity; Philippine Islands; Quaternary; radioactive isotopes; seismicity; soils

Latitude & Longitude:
N14°50'00" - N14°50'00" and E120°30'00" - E120°30'00" (Search for maps and images at Alexandria Digital Library)

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