Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 6.5 | 4 km NW of Can-Avid, Philippines | 35.0 km | 2003-11-18 17:14:22 UTC | View event → |
| M 5.2 | 185 km SE of Sarangani, Philippines | 33.0 km | 2003-11-29 20:17:11 UTC | View event → |
| M 5.0 | 156 km SSW of Sarangani, Philippines | 33.0 km | 2003-11-19 18:21:13 UTC | View event → |
| M 4.9 | 192 km ESE of Sarangani, Philippines | 33.0 km | 2003-11-20 11:14:11 UTC | View event → |
| M 4.9 | 12 km W of Taft, Philippines | 66.3 km | 2003-11-18 17:53:59 UTC | View event → |
| M 4.9 | 25 km ENE of Cabodiongan, Philippines | 33.0 km | 2003-11-03 07:35:50 UTC | View event → |
| M 4.8 | 3 km SW of Balangonan, Philippines | 10.0 km | 2003-11-15 01:19:56 UTC | View event → |
| M 4.8 | 33 km ESE of Union, Philippines | 33.0 km | 2003-11-14 13:23:27 UTC | View event → |
| M 4.7 | 4 km ENE of Limbuhan, Philippines | 33.0 km | 2003-11-05 02:38:30 UTC | View event → |
| M 4.6 | 179 km ESE of Sarangani, Philippines | 33.0 km | 2003-11-23 05:52:15 UTC | View event → |
| M 4.6 | 20 km W of Gadung, Philippines | 600.0 km | 2003-11-07 05:01:37 UTC | View event → |
| M 4.5 | 9 km ESE of Capitan Ramon, Philippines | 88.1 km | 2003-11-27 14:24:27 UTC | View event → |
| M 4.5 | 21 km NW of Balbalan, Philippines | 33.0 km | 2003-11-25 23:38:05 UTC | View event → |
| M 4.5 | 80 km ENE of Aras-asan, Philippines | 33.0 km | 2003-11-16 13:51:42 UTC | View event → |
| M 4.5 | 8 km SE of Sampaloc, Philippines | 137.0 km | 2003-11-09 22:31:33 UTC | View event → |
| M 4.5 | 49 km SSW of Lumatil, Philippines | 100.0 km | 2003-11-06 18:24:16 UTC | View event → |
| M 4.5 | 2 km ESE of Santo Niño, Philippines | 127.4 km | 2003-11-06 11:16:53 UTC | View event → |
| M 4.5 | 11 km NNE of Lubang, Philippines | 84.3 km | 2003-11-02 00:21:45 UTC | View event → |
Historical small-earthquake detection varies through time. Long-term comparisons are most robust at higher magnitude thresholds.
Guides, explainers and practical reading to go beyond the live data.
Magnitude is only one part of the story. Depth, distance, local ground conditions and building vulnerability help explain why shaking can differ so much from one earthquake to another.
Read article →
Earthquake-resistant design is not about making buildings immovable. It is about controlling forces, deformation and failure so people have a much better chance of staying safe.
Read article →
Early-warning systems detect an earthquake after it starts and try to send an alert before the strongest shaking arrives. The difference between warning and prediction matters.
Read article →
