The tremor, which occurred at 14:00:52 UTC, reached a magnitude of 4.8 and was felt across several neighboring islands.
At the time of the event, the local weather featured light rain and a cool ambient temperature of 14.2°C.
While the maritime conditions remained relatively calm, the sudden jolt disrupted the quiet afternoon for those in coastal urban centers.
Geological Analysis
Preliminary data suggests the rupture originated within the Hellenic Arc, a high-activity zone where the African plate subducts beneath the Aegean microplate.
The recorded magnitude 4.8 reflects a significant release of energy typical of this region’s complex crustal dynamics.
Experts note that the depth of the event likely mitigated the intensity of surface vibrations felt by the local population.
As the light rain continues across the Dodecanese, seismic monitoring stations remain on high alert for any subsequent crustal adjustments.
Our editorial team carefully monitors seismic data to provide in-depth analysis. Explore our real-time interactive Live Map for more details.