Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.9 | 105 km ESE of Namie, Japan | 33.0 km | 2001-02-24 21:53:54 UTC | View event → |
| M 5.8 | 62 km SSW of Hirara, Japan | 15.7 km | 2001-02-08 05:41:39 UTC | View event → |
| M 5.3 | 105 km ESE of Namie, Japan | 33.0 km | 2001-02-26 06:08:32 UTC | View event → |
| M 5.2 | 57 km WNW of Yonakuni, Japan | 109.4 km | 2001-02-16 23:13:09 UTC | View event → |
| M 5.2 | Izu Islands, Japan region | 384.2 km | 2001-02-14 18:10:01 UTC | View event → |
| M 5.1 | southwestern Ryukyu Islands, Japan | 33.0 km | 2001-02-08 10:01:29 UTC | View event → |
| M 5.0 | 60 km S of Hirara, Japan | 33.0 km | 2001-02-26 23:29:12 UTC | View event → |
| M 4.9 | 135 km SSW of Itoman, Japan | 33.0 km | 2001-02-26 02:22:51 UTC | View event → |
| M 4.9 | 14 km SE of Toyohashi, Japan | 36.5 km | 2001-02-22 22:23:46 UTC | View event → |
| M 4.8 | 53 km NE of Yonakuni, Japan | 33.0 km | 2001-02-20 19:07:11 UTC | View event → |
| M 4.8 | 68 km ENE of Naze, Japan | 33.0 km | 2001-02-13 18:28:09 UTC | View event → |
| M 4.7 | 75 km NW of Nago, Japan | 98.2 km | 2001-02-28 17:07:04 UTC | View event → |
| M 4.7 | 42 km SW of Tateyama, Japan | 33.0 km | 2001-02-25 05:05:31 UTC | View event → |
| M 4.7 | near the south coast of Honshu, Japan | 360.7 km | 2001-02-21 16:59:56 UTC | View event → |
| M 4.6 | 69 km E of ?hara, Japan | 33.0 km | 2001-02-25 05:34:01 UTC | View event → |
| M 4.6 | Izu Islands, Japan region | 44.3 km | 2001-02-18 08:09:25 UTC | View event → |
| M 4.6 | 39 km ESE of Nishinoomote, Japan | 33.0 km | 2001-02-09 21:37:13 UTC | View event → |
| M 4.5 | Izu Islands, Japan region | 33.0 km | 2001-02-12 16:42:56 UTC | View event → |
| M 4.5 | 62 km S of Hirara, Japan | 33.0 km | 2001-02-06 21:57:31 UTC | View event → |
| M 4.5 | Izu Islands, Japan region | 33.0 km | 2001-02-04 15:15:13 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 →
