Valley Fault Image
Coordinates: 14°38′N 121°5′E
Plate: Philippine Sea Plate and Sunda Plate
Status: Active
Earthquakes: 1658, 1771
Type: Strike-slip fault
Movement: Dextral
Age: Gelasian
The Valley Fault System is a dextral strike-slip type fault that traverses primarily in the eastern portion of Metro Manila and other provinces such as Bulacan, Rizal, Cavite, and Laguna that sums up to a total length of 146.71 kilometers. It traverses a densely populated area in southern Luzon piercing through over 90 private villages and subdivisions with over 6,000 buildings on top of the fault line.
The Marikina Valley Fault System, also known as the Valley Fault System (VFS), is a dominantly right-lateral strike-slip[2] fault system in Luzon, Philippines. It extends from Doña Remedios Trinidad, Bulacan in the north and runs through the provinces of Rizal, and the Metro Manila cities of Quezon, Marikina, Pasig, Makati, Taguig and Muntinlupa, and the provinces of Cavite and Laguna that ends in Canlubang.[1]
The fault system consists of two major fault lines that are estimated to move once in every 400 years (+/- 100 years) and is capable of triggering about 7.2 magnitude of earthquake. According to DOST - PHIVOLCS this fault moves every 200 – 400 years and the last time it did was in the year 1658, that was 359 years ago.
West Valley Fault
Running Through Bulacan, Rizal, Metro Manila, Cavite, and Laguna. Those near the West Valley Fault will first feel an up and down motion, followed by a horizontal ground motion. Those farther from the West Valley Fault will only feel a horizontal ground motion. The West Fault is capable of producing large scale earthquakes on its active phases with a magnitude of 7 or higher and moves in a dominantly dextral strike-slip motion
Based on kinematic block models that utilize GPS, actual fault geometry, and earthquake focal mechanisms, the West segment of the Marikina Fault was resolved to be almost fully locked, meaning it is currently accumulating and loading elastic strain, at the rate of 10 to 12 mm/yr. The Marikina Valley Fault System is considered to be almost fully locked, i.e. almost no movement, so the pressure is building all of the time
When the West Valley Fault moved and generated a 7.2 magnitude earthquake, 34,000 people may die and will damage lifelines including water, infrastructure, roads, ports, and telecommunication.
The concentration of population in Metro Manila along with the various non-engineered and non-earthquake resilient infrastructures and buildings are causative factors.
East Valley Fault
The eastern segment, known as East Valley Fault (EVF) moves in an oblique dextral motion.[2] It extends to about 17.24 kilometers (10.71 mi) from Rodriguez to San Mateo in the province of Rizal.[1]
Recorded Earthquakes
In July 1990, the Central Philippine Fault moved and caused the 7.7 magnitude earthquake that wreaked havoc across Luzon.
In February 2006, after a 10-day continuous downpour, a minor movement of the same fault, a 2.6 magnitude earthquake tripped a saturated cliff of a ridge that caused a massive rock slide-debris avalanche burying the entire village of Guinsaugon, a township of St. Bernard in Southern Leyte. More than a thousand death was recorded including the 247 children and 7 teachers who died when a school was entombed by the landslide.
Risks
In a 2011 a report by the Earthquakes and Megacities Initiative ("EMI") estimated that a magnitude 7.2 Richter earthquake occurring within the Marikina Valley Fault System would severely damage 175,000 buildings, cause 33,500 deaths, with 114,000 injured and 3,000,000 needing evacuation due to unsafe buildings. Metro Manila has grown significantly in size since 2011 and a significant portion of that development has been close to the West Valley Fault, so these estimates could possibly be doubled.
Barangays In Taguig Located Near Earthquake Fault
Bagumbayan
Bagong Tanyag
Upper Bicutan
Central Bicutan
Lower Bicutan
Maharlika Village
Pinagsama
North Signal Village
Central Signal Village
South Signal Village
Ususan
South Daang Hari
Subdivisions in Taguig Located Near WVF
Pinagsama
Pinagsama Phase II
Pan-Am Village
North Signal Village
Central Signal Village
South Signal Village
Maharlika Village
Camp Bagong Diwa
Villages traversed by the West Valley Fault in Taguig
Pinagsama Village
Perpetual Village X
Major Roads on the Fault Line
C5 (Near Pembo)
Pres. Manuel Quezon
Areas on the Fault
Sucat Napocor Power Plant