Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.4 | 21 km SE of Bugasong, Philippines | 29.0 km | 2016-08-15 11:32:02 UTC | View event → |
| M 5.4 | 2 km NE of Alabel, Philippines | 87.8 km | 2016-08-06 09:08:23 UTC | View event → |
| M 5.2 | 29 km SE of Kalbay, Philippines | 127.0 km | 2016-08-10 04:06:58 UTC | View event → |
| M 5.1 | 6 km E of Catmon, Philippines | 30.5 km | 2016-08-13 14:05:04 UTC | View event → |
| M 4.9 | 18 km NW of Santa Monica, Philippines | 95.4 km | 2016-08-26 15:53:25 UTC | View event → |
| M 4.9 | 3 km WNW of Alimodian, Philippines | 26.6 km | 2016-08-15 11:34:38 UTC | View event → |
| M 4.8 | 29 km SE of Caburan, Philippines | 101.0 km | 2016-08-15 05:28:14 UTC | View event → |
| M 4.7 | 21 km NE of Alugan, Philippines | 70.8 km | 2016-08-24 08:03:05 UTC | View event → |
| M 4.7 | 71 km NNW of Claveria, Philippines | 45.8 km | 2016-08-16 18:31:12 UTC | View event → |
| M 4.7 | 11 km NNW of Patnanungan, Philippines | 41.2 km | 2016-08-16 17:38:09 UTC | View event → |
| M 4.7 | 4 km SE of Pangyan, Philippines | 74.3 km | 2016-08-10 08:17:46 UTC | View event → |
| M 4.6 | 106 km ESE of Pondaguitan, Philippines | 109.3 km | 2016-08-18 20:10:15 UTC | View event → |
| M 4.6 | 8 km WSW of Karligan, Philippines | 44.5 km | 2016-08-15 02:50:44 UTC | View event → |
| M 4.6 | 4 km SSW of Balogo, Philippines | 41.2 km | 2016-08-12 10:43:27 UTC | View event → |
| M 4.6 | 169 km ESE of Sarangani, Philippines | 53.0 km | 2016-08-10 20:34:33 UTC | View event → |
| M 4.6 | 11 km ESE of Hukay, Philippines | 72.6 km | 2016-08-10 08:07:05 UTC | View event → |
| M 4.6 | 21 km NW of Binabalian, Philippines | 79.0 km | 2016-08-07 23:43:47 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.
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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.
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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 →
