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A magnitude 4.8 earthquake struck Iceland on 5th October 2026 at 17:28 UTC, according to the European‑Mediterranean Seismological Centre (EMSC). The quake occurred at an extremely shallow depth of 2 km, making it capable of producing noticeable shaking near the epicentre.
The epicentre was recorded at 64.670°N, -17.123°W, placing it 237 km ENE of Reykjavík and 103 km WNW of Höfn, two areas familiar with frequent seismic activity due to Iceland’s tectonic setting.
Although classified as a minor earthquake, shallow events like this often attract attention because they can be felt more strongly at the surface.
Iceland sits directly on the Mid‑Atlantic Ridge, where the North American Plate and Eurasian Plate are pulling apart. This tectonic divergence, combined with the country’s active volcanic systems, creates:
This 4.8 event fits the typical pattern of shallow crustal movement along Iceland’s active seismic zones.
While a magnitude 4.8 is considered light, shallow quakes can produce:
No damage has been reported, and Icelandic authorities have not issued any emergency instructions.
The event was also detected by multiple European seismic agencies, confirming its accuracy and classification.
Based on EMSC and global seismic classifications:
These events are common in Iceland and typically do not pose structural risk.
Iceland has experienced increased seismic activity in recent years, especially around:
This 4.8 quake occurred within one of Iceland’s known active zones, consistent with ongoing tectonic movement.
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