Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.1 | 52 km SSE of Atico, Peru | 41.6 km | 2007-01-17 16:08:46 UTC | View event → |
| M 5.0 | 4 km SSE of Quilahuani, Peru | 113.7 km | 2007-01-04 09:27:34 UTC | View event → |
| M 5.0 | 171 km WSW of Paramonga, Peru | 35.0 km | 2007-01-02 17:43:54 UTC | View event → |
| M 4.9 | 154 km SW of Punta de Bombón, Peru | 35.0 km | 2007-01-28 01:11:35 UTC | View event → |
| M 4.9 | 55 km WSW of Yuyapichis, Peru | 15.7 km | 2007-01-23 07:02:07 UTC | View event → |
| M 4.8 | 41 km SW of Yuyapichis, Peru | 41.3 km | 2007-01-20 19:56:12 UTC | View event → |
| M 4.7 | 34 km SW of Atico, Peru | 73.4 km | 2007-01-05 07:24:13 UTC | View event → |
| M 4.6 | 8 km W of Victor Raul, Peru | 76.0 km | 2007-01-27 10:28:14 UTC | View event → |
| M 4.5 | 13 km NNE of Curpahuasi, Peru | 64.4 km | 2007-01-26 10:02:50 UTC | View event → |
| M 4.5 | 47 km NNE of Moyobamba, Peru | 35.0 km | 2007-01-02 02:00:07 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.
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