INGV reported that during 30 June-2 July activity at Stromboli was characterized by ongoing low-to-medium intensity Strombolian explosions and degassing from multiple vents within the crater terrace. A high-energy explosion from vent C in Area C-S (South Central crater area) was recorded at 2303 on 25 June. The event lasted for about 28 seconds, ejected material that fell onto most of the crater terrace and into the Valle della Luna, and widened the vent.

Geological Summary. Spectacular incandescent nighttime explosions at Stromboli have long attracted visitors to the "Lighthouse of the Mediterranean" in the NE Aeolian Islands. This volcano has lent its name to the frequent mild explosive activity that has characterized its eruptions throughout much of historical time. The small island is the emergent summit of a volcano that grew in two main eruptive cycles, the last of which formed the western portion of the island. The Neostromboli eruptive period took place between about 13,000 and 5,000 years ago. The active summit vents are located at the head of the Sciara del Fuoco, a prominent scarp that formed about 5,000 years ago due to a series of slope failures which extends to below sea level. The modern volcano has been constructed within this scarp, which funnels pyroclastic ejecta and lava flows to the NW. Essentially continuous mild Strombolian explosions, sometimes accompanied by lava flows, have been recorded for more than a millennium.

Source: Sezione di Catania - Osservatorio Etneo (INGV)