Sarangani (Mindanao)
Strongest Philippine earthquake since the 1976 Moro Gulf event; on the Cotabato Trench. Uplifted ~100 km of coastline by up to 2 m.
The Philippines sits on the Pacific Ring of Fire — wrapped by trenches and threaded with active faults. This is an interactive look at where the ground moves, how often, and how hard. Magnitudes follow PHIVOLCS where curated; the map runs on open data.
Watch six decades of Philippine earthquakes unfold.
02 · The data story
Every recorded M4.5+ earthquake in the Philippines since 1960. Read the right charts and a few counter-intuitive truths emerge — chiefly that depth, not magnitude alone, decides how deadly a quake is.
Each dot is a notable quake — magnitude up the side, depth across. Bubble size and warmth grow with the death toll. The deadliest events cluster shallow-left, not high-magnitude.
Cebu 2025 (M6.9, ~5 km) killed 79. Hinatuan 2023 was far bigger (M7.6) but ~32 km deep — and killed 3.
Count by magnitude on a log scale — a near-straight fall-off (Gutenberg–Richter).
~9,690 M4.5–4.9 events vs only 46 at M7+ — each step up is roughly 10× rarer.
Yearly M4.5+ counts. Early decades undercount — global detection improved over time.
Peak year: 2023 (678 events). The upward drift is mostly better detection, not more earthquakes.
Curated-event deaths by primary cause. The shaking is often not the deadliest part.
Tsunami (Moro Gulf 1976) and landslides (Negros, Cotabato) drive the toll — the secondary hazard is frequently the real killer.
All 13,872 events by depth band — and shallow is the dangerous band.
75% of PH quakes are shallow (<70 km) — close to the surface, where they do the most damage.
03 · The Big One
The West Valley Fault — about 100 km of right-lateral strike-slip fault — runs straight through the most densely populated region in the country. PHIVOLCS models a potential ~M7.2 movement, the scenario popularly known as "The Big One." It is the crimson line on the map above.
Official baseline: the Metro Manila Earthquake Impact Reduction Study (MMEIRS), JICA / PHIVOLCS / MMDA, 2004, plus secondary liquefaction, fire, and landslide effects. A later World Bank study sketches an upper-range scenario of roughly ~48,000 deaths and ~$48 billion in losses — cited here only as an upper bound, not the central estimate.
The fault crosses Bulacan, Rizal, several Metro Manila cities, Cavite, and Laguna — passing under homes, schools, and expressways.
The fault last moved in a major way in 1658, roughly 367 years ago. Trenching studies put its recurrence interval at about 400–600 years.
2058 is a reference point, not a prediction. In PHIVOLCS' own words, a movement "may happen within our lifetime" — Director Renato Solidum / OIC Teresito Bacolcol have repeatedly stressed that no one can predict the date. We deliberately do not call the fault "overdue."
Myth-bust A large earthquake elsewhere in the Philippines does not "trigger" or "release pressure" on the West Valley Fault — they belong to different fault systems hundreds of kilometres apart. Per PHIVOLCS, recent Mindanao or Cebu events tell us nothing about the timing of the Big One.
04 · Risk lookup
Enter a Philippine city — or use your location — to see the nearest active fault and how far away it is, how much historical activity surrounds you, and your distance to the West Valley Fault. For awareness, not an official hazard assessment.
Loading fault & historical data…
For awareness only — distances are computed from open fault traces and are not a hazard assessment. For authoritative ground-shaking, liquefaction, and fault-trace maps, use PHIVOLCS (e.g. the HazardHunterPH and FaultFinder tools).
05 · Notable quakes
A curated, verified set of the most consequential events — most recent first. Magnitudes lead with PHIVOLCS; where USGS diverges, its value is shown in parentheses.
Strongest Philippine earthquake since the 1976 Moro Gulf event; on the Cotabato Trench. Uplifted ~100 km of coastline by up to 2 m.
Twin earthquakes off Davao Oriental with a minor tsunami; roughly 1.5 million people affected.
Twin events: M7.4 followed by M6.7.
Attributed to the newly identified Bogo Bay Fault; its very shallow depth made it deadly in northern Cebu.
Near the Philippine Trench; its depth kept the toll low despite the high magnitude. A minor tsunami was recorded.
PHIVOLCS M7.4; USGS Mww 7.6.
First M7 on or near the Philippine Fault since 1990; landslides and damage across Abra and the Ilocos region.
M7.0; PHIVOLCS initial estimate was Ms 7.3.
An earthquake swarm in Cotabato; massive landslides struck Makilala and Tulunan.
Swarm of strong shocks over weeks: M6.3 (Oct 16), M6.6 (Oct 29), M6.5 (Oct 31), M6.1 (Dec 15). Date shown is the M6.5 representative shock.
Shallow event near Surigao City; 522 houses destroyed.
Ruptured the previously unmapped North Bohol Fault; centuries-old heritage churches were destroyed.
Shallow event triggering deadly landslides in Guihulngan and La Libertad.
Produced a ~125 km ground rupture along the Philippine Fault; the Hyatt Terraces hotel in Baguio collapsed.
Deadliest tsunami in Philippine history; roughly 85% of deaths were caused by the tsunami, not the shaking.
M8.0; USGS surface-wave Ms 7.9.
06 · Preparedness
Awareness only matters if it changes what you do. Here is the official protocol from PHIVOLCS and NDRRMC — practise it before you need it.
Then evacuate calmly via the stairs (never lifts) and gather at your designated open-space meeting point.
Enough to be self-sufficient for at least three days:
The Nationwide Simultaneous Earthquake Drill (NSED) — the "shake drill" — runs several times a year and rehearses exactly the M7.2 West Valley Fault scenario. Schools, offices, and barangays practise Duck-Cover-Hold and evacuation together.
Participate when your workplace or barangay runs one — muscle memory is what keeps you safe when the ground actually moves.