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MARIKINA VALLEY FAULT SYSTEM PHIVOLS: MARIKINA VALLEY FAULT (RIGHT LATERAL) CAPABLE OF TRIGGERING 7.2 MAGNETUDE EARTHQUAKE •CARBON 14 PALEOSEISMIC STUDY REVEALED 200 – 400 YEARS RECURRENCE INTERVAL OF MOVEMENT AT 6-7 MAGNETUDE • THE LAST EARTHQUAKE WAS 200 YEARS BP • DIGDIG FAULT IN NORTHERN LUZON – 7.8, 1990 • AGLUBANG RIVER FAULT, MINDORO – 7.1, 1994 EARTHQUAKE GEOLOGY – STUDY OF HISTORY, EFFECTS, AND MECHANICS OF EARTHQUAKES ON EARTH’S CRUST; SYNONYMOUS WITH ACTIVE TECTONICS, A TERM USED TO DESCRIBE TECTONIC MOVEMENTS EXPECTED TO OCCUR WITHIN A FUTURE TIME PALEOSEISMOLOGY – TIMING, LOCATION, AND SIZE OF PREHISTORIC EARTHQUAKES • FOCUSES: 1) ON INSTANTANEOUS DEFORMATION OF LANDFORMS & SEDIMENTS DURING INDIVIDUAL EARTHQUAKES; 2) DISTRIBUTION OF EARTHQUAKES IN SPACE & OVER TIME PERIODS OF 100 – 1,000 OF YEARS; 3) HELP UNDERSTAND ASPECTS OF EARTHQUAKE GEOLOGY, SUCH AS REGIONAL PATTERNS OF TECTONIC DEFORMATION & LONG-TERN BEHAVIOR OF SPECIFIC FAULTS – KNOWLEDGE OF WHEN, WHERE, AND HOW OFTEN, LARGE EARTHQUAKES OCCUR STUDY OF THE WALL OF TRENCH ACCROSS STRAND OF FAULT