Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.4 | 54 km N of Namuac, Philippines | 37.8 km | 2011-08-11 02:56:40 UTC | View event → |
| M 5.3 | 12 km SSW of San Teodoro, Philippines | 162.8 km | 2011-08-12 02:29:28 UTC | View event → |
| M 5.0 | 128 km SSE of Sarangani, Philippines | 151.4 km | 2011-08-03 06:11:35 UTC | View event → |
| M 4.9 | Panay, Philippines | 37.8 km | 2011-08-25 02:17:18 UTC | View event → |
| M 4.9 | 56 km NE of Alugan, Philippines | 53.2 km | 2011-08-02 09:00:24 UTC | View event → |
| M 4.8 | 117 km W of Basco, Philippines | 10.0 km | 2011-08-30 16:15:48 UTC | View event → |
| M 4.7 | 119 km E of Basco, Philippines | 34.5 km | 2011-08-31 13:55:35 UTC | View event → |
| M 4.7 | Moro Gulf, Mindanao, Philippines | 605.7 km | 2011-08-29 15:28:33 UTC | View event → |
| M 4.7 | 21 km E of Tinogboc, Philippines | 43.9 km | 2011-08-14 07:38:09 UTC | View event → |
| M 4.6 | 108 km NNW of Davila, Philippines | 35.0 km | 2011-08-14 18:13:32 UTC | View event → |
| M 4.6 | 6 km SSW of Calatagan, Philippines | 136.1 km | 2011-08-09 15:41:33 UTC | View event → |
| M 4.6 | 6 km WSW of Buenavista, Philippines | 116.8 km | 2011-08-06 20:00:26 UTC | View event → |
| M 4.5 | 9 km ESE of Baganga, Philippines | 75.0 km | 2011-08-22 13:39:28 UTC | View event → |
| M 4.5 | 15 km NNW of Cortes, Philippines | 104.4 km | 2011-08-21 02:36:24 UTC | View event → |
| M 4.5 | 21 km W of Balud, Philippines | 60.7 km | 2011-08-13 05:37:14 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 →
