Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.3 | 19 km SE of Union, Philippines | 69.7 km | 2005-06-22 06:30:18 UTC | View event → |
| M 5.2 | 153 km SSE of Pondaguitan, Philippines | 88.7 km | 2005-06-09 03:45:16 UTC | View event → |
| M 4.9 | 21 km S of Sarangani, Philippines | 100.0 km | 2005-06-02 08:53:08 UTC | View event → |
| M 4.8 | 35 km ENE of Sulangan, Philippines | 38.6 km | 2005-06-24 05:31:33 UTC | View event → |
| M 4.8 | 28 km E of Union, Philippines | 10.0 km | 2005-06-22 06:34:29 UTC | View event → |
| M 4.8 | 14 km ENE of Paluan, Philippines | 61.5 km | 2005-06-04 14:28:37 UTC | View event → |
| M 4.7 | 27 km NNE of Karligan, Philippines | 33.3 km | 2005-06-11 05:06:38 UTC | View event → |
| M 4.7 | 96 km SSE of Pondaguitan, Philippines | 10.0 km | 2005-06-08 23:21:13 UTC | View event → |
| M 4.7 | 52 km WSW of San Nicolas, Philippines | 50.0 km | 2005-06-07 03:23:57 UTC | View event → |
| M 4.7 | 4 km NNW of Kabalen, Philippines | 20.0 km | 2005-06-06 07:49:17 UTC | View event → |
| M 4.6 | 11 km NW of Cabcab, Philippines | 35.0 km | 2005-06-25 19:15:41 UTC | View event → |
| M 4.6 | 24 km SSW of Pondaguitan, Philippines | 185.0 km | 2005-06-19 14:11:22 UTC | View event → |
| M 4.6 | 168 km ESE of Sarangani, Philippines | 20.0 km | 2005-06-13 03:39:08 UTC | View event → |
| M 4.6 | 2 km W of Sugal, Philippines | 70.7 km | 2005-06-08 16:28:56 UTC | View event → |
| M 4.6 | 2 km WNW of Gabao, Philippines | 80.4 km | 2005-06-04 17:33:58 UTC | View event → |
| M 4.5 | 104 km SSW of Malisbeng, Philippines | 526.1 km | 2005-06-15 00:56:51 UTC | View event → |
| M 4.5 | 69 km SE of Sarangani, Philippines | 45.2 km | 2005-06-14 19:34:44 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 →
