INGV reported that during 30 June-1 July, small landslides occurred on Stromboli's Sciara del Fuoco. A new lava flow that began on 7 July flowed from the high part of Sciara del Fuoco (N2) and followed the path of the previous flows. A hot avalanche occurred at 0733 that reached the coastline and was followed by a lava flow. Two other lava flows began from the same location (N2); one during the afternoon of 9 July that was accompanied by small landslides and another on 10 July.

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)