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Magnitude 6.2 Earthquake Hits Southern Italy Coast

A 6.2 magnitude earthquake struck off Calabria's coast early Monday at 250 kilometers depth, felt across southern Italy but causing no damage or injuries.

Dimitris Papafotis
Dimitris Papafotis Editor in Chief
JUNE 2, 2026 AT 12:09 PM

The seismic event occurred at 12:12 a.m. on June 2 in the Tyrrhenian Sea, with its epicenter located approximately 20 kilometers offshore from Amantea in Cosenza province, according to Brussels Signal.

Italy’s National Institute of Geophysics and Volcanology (INGV) recorded the earthquake and noted that the tremor originated at a considerable depth of roughly 250 kilometers beneath the seafloor. This exceptional depth significantly reduced surface-level impact while allowing the quake to be felt across an unusually wide geographic area.

Residents from Lazio in central Italy all the way south to Sicily reported feeling the earthquake, based on questionnaires collected by INGV. The shaking struck during the early morning hours of June 2, a national public holiday in Italy, prompting many citizens in affected areas to evacuate their homes and seek information from firefighters and regional civil protection services.

Deep Seismic Activity Characteristic of Region

INGV explained that deep earthquakes are a typical phenomenon in the southern Tyrrhenian Sea. The seismic activity results from the geological subduction process, where the Ionian lithosphere is being pushed beneath the Calabrian landmass.

The US Geological Survey classified the surface shaking as light and confirmed that deep-origin earthquakes generally produce weaker surface movements compared to shallow tremors of similar magnitude, though they are felt across far broader territories.

The earthquake’s effects were reported in Naples, Puglia, Basilicata, and throughout the southern Italian regions, despite the significant depth that would normally dampen surface impact.

No Damage or Injuries Reported

Italy’s Civil Protection Department confirmed that no injuries or property damage had been reported and stated that authorities continue to monitor the situation. Officials emphasized that the depth of the earthquake likely prevented the kind of destructive surface damage that shallower tremors of comparable magnitude can produce.

Italy sits on multiple fault lines and experiences regular seismic activity, particularly in its southern regions. The country’s building codes and emergency response systems are designed to handle such events, though deeper earthquakes like this one present different challenges in terms of prediction and public awareness.

With information from Brussels Signal

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Dimitris Papafotis
Dimitris Papafotis

Dimitris Papafotis is the editor-in-chief of NewsFire.GR. He was born and raised in Athens. He studied at the Journalism Workshop (1991-1993). He currently lives in Pyrgos, Ilia, where he has been active in radio and various newspapers, while also maintaining his personal blog, Papafotis.gr.

The seismic event occurred at 12:12 a.m. on June 2 in the Tyrrhenian Sea, with its epicenter located approximately 20 kilometers offshore from Amantea in Cosenza province, according to Brussels Signal.

Italy’s National Institute of Geophysics and Volcanology (INGV) recorded the earthquake and noted that the tremor originated at a considerable depth of roughly 250 kilometers beneath the seafloor. This exceptional depth significantly reduced surface-level impact while allowing the quake to be felt across an unusually wide geographic area.

Residents from Lazio in central Italy all the way south to Sicily reported feeling the earthquake, based on questionnaires collected by INGV. The shaking struck during the early morning hours of June 2, a national public holiday in Italy, prompting many citizens in affected areas to evacuate their homes and seek information from firefighters and regional civil protection services.

Deep Seismic Activity Characteristic of Region

INGV explained that deep earthquakes are a typical phenomenon in the southern Tyrrhenian Sea. The seismic activity results from the geological subduction process, where the Ionian lithosphere is being pushed beneath the Calabrian landmass.

The US Geological Survey classified the surface shaking as light and confirmed that deep-origin earthquakes generally produce weaker surface movements compared to shallow tremors of similar magnitude, though they are felt across far broader territories.

The earthquake’s effects were reported in Naples, Puglia, Basilicata, and throughout the southern Italian regions, despite the significant depth that would normally dampen surface impact.

No Damage or Injuries Reported

Italy’s Civil Protection Department confirmed that no injuries or property damage had been reported and stated that authorities continue to monitor the situation. Officials emphasized that the depth of the earthquake likely prevented the kind of destructive surface damage that shallower tremors of comparable magnitude can produce.

Italy sits on multiple fault lines and experiences regular seismic activity, particularly in its southern regions. The country’s building codes and emergency response systems are designed to handle such events, though deeper earthquakes like this one present different challenges in terms of prediction and public awareness.

With information from Brussels Signal