Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.8 | 39 km ENE of Calama, Chile | 111.0 km | 2013-08-23 08:34:06 UTC | View event → |
| M 5.3 | 118 km NNE of Calama, Chile | 115.8 km | 2013-08-19 19:39:45 UTC | View event → |
| M 5.2 | 34 km WSW of Vallenar, Chile | 54.3 km | 2013-08-16 22:17:30 UTC | View event → |
| M 5.2 | 58 km W of Iquique, Chile | 19.1 km | 2013-08-05 05:40:56 UTC | View event → |
| M 4.9 | 17 km ESE of Rengo, Chile | 111.7 km | 2013-08-30 10:48:13 UTC | View event → |
| M 4.7 | 137 km ESE of Iquique, Chile | 111.4 km | 2013-08-28 17:56:29 UTC | View event → |
| M 4.7 | 148 km WSW of Lebu, Chile | 29.6 km | 2013-08-24 07:00:22 UTC | View event → |
| M 4.7 | 53 km W of La Ligua, Chile | 34.6 km | 2013-08-04 15:27:39 UTC | View event → |
| M 4.7 | West Chile Rise | 15.0 km | 2013-08-03 18:53:46 UTC | View event → |
| M 4.6 | 123 km SE of Arica, Chile | 104.8 km | 2013-08-16 05:22:52 UTC | View event → |
| M 4.6 | 39 km W of La Ligua, Chile | 48.0 km | 2013-08-15 10:26:46 UTC | View event → |
| M 4.6 | 60 km S of Calama, Chile | 103.3 km | 2013-08-11 15:28:42 UTC | View event → |
| M 4.6 | 103 km NE of Iquique, Chile | 96.2 km | 2013-08-05 07:29:39 UTC | View event → |
| M 4.6 | 79 km NW of Coquimbo, Chile | 20.2 km | 2013-08-02 06:13:11 UTC | View event → |
| M 4.5 | 28 km ENE of Taltal, Chile | 33.4 km | 2013-08-21 03:25:13 UTC | View event → |
| M 4.5 | 51 km W of Iquique, Chile | 35.7 km | 2013-08-16 06:51:12 UTC | View event → |
| M 4.5 | 49 km WNW of Coronel, Chile | 28.3 km | 2013-08-15 11:13:50 UTC | View event → |
| M 4.5 | 118 km ENE of Iquique, Chile | 107.6 km | 2013-08-07 08:19:57 UTC | View event → |
| M 4.5 | 31 km ENE of Calama, Chile | 125.1 km | 2013-08-07 07:18:39 UTC | View event → |
| M 4.5 | 45 km S of Tocopilla, Chile | 60.6 km | 2013-08-03 20:44:19 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 →
