Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.3 | 82 km SSE of Sarangani, Philippines | 104.8 km | 2015-03-01 07:01:56 UTC | View event → |
| M 5.0 | 73 km SE of Pondaguitan, Philippines | 77.4 km | 2015-03-26 16:46:47 UTC | View event → |
| M 5.0 | 25 km E of Pilar, Philippines | 70.0 km | 2015-03-02 21:51:58 UTC | View event → |
| M 4.9 | 11 km W of Hinlayagan Ilaud, Philippines | 10.0 km | 2015-03-30 01:47:48 UTC | View event → |
| M 4.9 | 185 km SE of Sarangani, Philippines | 104.5 km | 2015-03-06 06:41:17 UTC | View event → |
| M 4.7 | 52 km E of Sarangani, Philippines | 121.2 km | 2015-03-07 16:39:02 UTC | View event → |
| M 4.6 | 197 km SE of Pondaguitan, Philippines | 96.4 km | 2015-03-28 01:19:31 UTC | View event → |
| M 4.6 | 111 km SE of Pondaguitan, Philippines | 134.4 km | 2015-03-21 15:37:21 UTC | View event → |
| M 4.6 | 154 km WNW of Cabra, Philippines | 39.6 km | 2015-03-16 22:54:50 UTC | View event → |
| M 4.6 | 227 km SE of Sarangani, Philippines | 56.9 km | 2015-03-14 18:39:53 UTC | View event → |
| M 4.6 | 1 km NW of Sugod, Philippines | 47.1 km | 2015-03-07 22:53:04 UTC | View event → |
| M 4.6 | 68 km WSW of Pandan Niog, Philippines | 17.0 km | 2015-03-05 17:36:35 UTC | View event → |
| M 4.6 | 22 km E of Pilar, Philippines | 71.4 km | 2015-03-05 12:11:41 UTC | View event → |
| M 4.6 | Mindanao, Philippines | 148.5 km | 2015-03-04 14:19:52 UTC | View event → |
| M 4.5 | 291 km SSE of Latung, Philippines | 589.7 km | 2015-03-19 06:23:44 UTC | View event → |
| M 4.5 | 45 km N of Buluang, Philippines | 35.0 km | 2015-03-15 08:03:13 UTC | View event → |
| M 4.5 | 4 km WSW of Balaoan, Philippines | 65.7 km | 2015-03-14 14:37:37 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 →
