Explore earthquake activity year by year and month by month using the historical Quake Pulse database.
| Magnitude | Location | Depth | Time | |
|---|---|---|---|---|
| M 5.6 | Southwest Indian Ridge | 10.0 km | 2012-03-26 16:58:10 UTC | View event → |
| M 5.4 | Nicobar Islands, India region | 16.8 km | 2012-03-06 02:52:41 UTC | View event → |
| M 5.3 | Southwest Indian Ridge | 10.0 km | 2012-03-29 00:36:40 UTC | View event → |
| M 5.1 | 11 km SSE of Rohtak, India | 10.0 km | 2012-03-05 07:41:04 UTC | View event → |
| M 5.0 | 17 km W of Kishanganj, India | 28.8 km | 2012-03-27 23:40:12 UTC | View event → |
| M 5.0 | 174 km SE of Port Blair, India | 58.2 km | 2012-03-14 17:41:10 UTC | View event → |
| M 5.0 | Nicobar Islands, India region | 19.8 km | 2012-03-06 02:59:25 UTC | View event → |
| M 4.9 | 252 km SSE of Port Blair, India | 53.1 km | 2012-03-20 10:18:52 UTC | View event → |
| M 4.9 | Andaman Islands, India region | 68.3 km | 2012-03-14 17:01:50 UTC | View event → |
| M 4.8 | 170 km SE of Port Blair, India | 35.0 km | 2012-03-16 07:07:23 UTC | View event → |
| M 4.8 | 145 km N of Bamboo Flat, India | 37.9 km | 2012-03-01 17:52:43 UTC | View event → |
| M 4.7 | Southwest Indian Ridge | 10.0 km | 2012-03-19 12:26:00 UTC | View event → |
| M 4.7 | Nicobar Islands, India region | 61.9 km | 2012-03-10 20:58:09 UTC | View event → |
| M 4.6 | 165 km SE of Port Blair, India | 35.0 km | 2012-03-16 05:58:16 UTC | View event → |
| M 4.6 | 166 km SE of Port Blair, India | 35.0 km | 2012-03-15 20:46:35 UTC | View event → |
| M 4.6 | 167 km SE of Port Blair, India | 35.0 km | 2012-03-15 14:56:00 UTC | View event → |
| M 4.6 | Nicobar Islands, India region | 5.1 km | 2012-03-10 18:06:29 UTC | View event → |
| M 4.5 | Mid-Indian Ridge | 10.0 km | 2012-03-16 08:06:36 UTC | View event → |
| M 4.5 | 76 km WSW of Bamboo Flat, India | 35.0 km | 2012-03-10 12:18:29 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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