Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 6.0 | 25 km WSW of Bolitoc, Philippines | 10.0 km | 2003-01-06 23:43:50 UTC | View event → |
| M 5.6 | 62 km SW of Basco, Philippines | 33.0 km | 2003-01-06 14:57:33 UTC | View event → |
| M 5.1 | 41 km N of Pagudpud, Philippines | 33.0 km | 2003-01-13 08:32:06 UTC | View event → |
| M 4.9 | 218 km SE of Pondaguitan, Philippines | 100.0 km | 2003-01-13 23:33:17 UTC | View event → |
| M 4.9 | 13 km SE of Union, Philippines | 33.0 km | 2003-01-09 13:37:02 UTC | View event → |
| M 4.8 | 26 km W of Bani, Philippines | 10.0 km | 2003-01-06 23:48:42 UTC | View event → |
| M 4.7 | 38 km SSE of Sarangani, Philippines | 195.8 km | 2003-01-22 11:06:02 UTC | View event → |
| M 4.7 | 32 km SE of Union, Philippines | 33.0 km | 2003-01-04 18:43:48 UTC | View event → |
| M 4.7 | 37 km ENE of Hinatuan, Philippines | 33.0 km | 2003-01-02 05:01:56 UTC | View event → |
| M 4.6 | 170 km SW of Palimbang, Philippines | 600.0 km | 2003-01-28 11:56:53 UTC | View event → |
| M 4.6 | 130 km ESE of Pondaguitan, Philippines | 225.8 km | 2003-01-22 07:36:54 UTC | View event → |
| M 4.6 | 192 km S of Sarangani, Philippines | 200.0 km | 2003-01-15 19:59:12 UTC | View event → |
| M 4.6 | 23 km SSW of Cabangahan, Philippines | 33.0 km | 2003-01-11 12:22:08 UTC | View event → |
| M 4.6 | 11 km SW of Katubao, Philippines | 33.0 km | 2003-01-11 05:04:31 UTC | View event → |
| M 4.5 | 4 km WNW of San Luis, Philippines | 33.0 km | 2003-01-27 03:58:33 UTC | View event → |
| M 4.5 | 9 km ENE of Santa Maria, Philippines | 88.1 km | 2003-01-13 22:16:25 UTC | View event → |
| M 4.5 | 2 km NNE of San Luis, Philippines | 88.9 km | 2003-01-07 12:39:00 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 →
