A relatively stable period in the eruption continues, both in respect to the paths taken by the lava flows and the surface eruptive activity. The lava flows continue to feed the lava delta via lava tubes, and the eruption continues to show a strombolian behaviour...
The two effusive vents that opened a few hundred metres NW of the main cone on the 1st October no longer show any activity, according to PEVOLCA. However, the Strombolian vents in the main cone and those on the flanks of the main cone are...
In the first official assessment of the classification of the eruption based on its size, the authorities have announced that the eruption is a Volcanic Explosivity Index (VEI) 2 eruption. This classification is based solely on the cumulative amount of material emitted by the volcano...
The explosivity of the eruption has increased, with activity being more concentrated in the strombolian vents in the main cone than the vents on the flanks of the main cone. The fumarolic field on the NW flank remains active, and elsewhere, activity from the two...
Based upon improved meteorological conditions and air quality levels, the confinements of parts of El Paso and Los Llanos de Aridane on the evening of the 1st October have been lifted, as well as the confinement of Tazacorte ordered six days ago. The eruption continues...
At 2:30 am local time, two new effusive vents 15 m apart opened approximately 600 m NW of the base of the main cone. These have formed a single fluid lava flow, which is travelling parallel to the existing flows and is expected to join...
The lava delta continues to be fed by the active lava flows, which show some stability in that they are largely confined to within previous lava flows. However, there are also localised breakouts onto previously unaffected land. The lava delta has reached a thickness of...
The active lava flow continues cascade down the cliffs of Playa de Los Guirres to the sea, where a lava delta (also called by the Canarianism “fajana”) is being created. The contact of the lava and seawater are creating gases of vapour, although currently due...
The lava flow began the day approximately 1000 m from the coast, although it advanced quickly throughout the day due to the large volume of fluid lava being emitted from the effusive vent on the northwest sector of the cone. The lava flow crossed to...
The eruption has seen a large variation of activity, with increases and decreases in the intensity of Strombolian activity, as well as pulses of phreatomagmatic activity (characterised by white plumes rich in water vapour) and periods of no strombolian activity from the main cone. The...