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A magnitude 5.2 earthquake struck the Dodecanese Islands region of Greece on 2nd July 2026, occurring at a depth of 10 km. The event was recorded by multiple seismic networks across Europe and classified as a shallow earthquake, typical of the tectonic activity along the Hellenic Arc.
The Dodecanese Islands lie near the boundary between the African Plate and the Aegean microplate, a zone known for frequent moderate earthquakes. Shallow events like this can be felt widely across nearby islands and coastal areas.
The Dodecanese (Greek: Δωδεκάνησα) is a group of 15 larger islands and numerous smaller islets in the southeastern Aegean Sea. Key islands include Rhodes, Kos, Kalymnos, and Karpathos. This region is known for:
The earthquake reflects the ongoing subduction of the African Plate beneath the Eurasian Plate, which drives much of the seismic activity in southern Greece. Events of magnitude 5.0–5.5 are common in this region and rarely cause major damage, though they can produce noticeable shaking across nearby islands and coastal cities.
The M5.2 earthquake at 10 km depth highlights the persistent tectonic movement along the Hellenic Arc, which continues to shape the Aegean region. No significant damage or injuries were reported at the time of writing, but the event serves as another reminder of Greece’s dynamic seismic landscape.
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