The lava flow immediately south of the current lava delta, flow number 2, has advanced and reached the coast at Playa de Los Guirres. The front of the lava flow is cascading down the cliffs onto the beach below, although this lava is yet to make contact with the sea. The rest of the active lava flows however show minimal progress. The eruptive activity continues to be a mixed strombolian mechanism with more explosive strombolian vents within the main cone, a lava emission vent on the NW flank of the main cone, and occasional phreatomagmatic pulses. The number of earthquakes increased again to 99, being recorded mostly at intermediate (10-15 km) depths with some deeper (35-40 km depth) events too, with the day’s largest earthquake being a mbLg 3.8 event at 38 km depth. This is still lower than the earthquake strength and frequency at points in the previous week.

In terms of lava flows, the eruption continues to be stable, with no new ground being affected by the current active flows, which occupy existing tubes and channels in the centre of the flow field. Flow number 11 to the south of the flow field, which was close to overflowing the LP-2 road used for accessing Puerto Naos, has stopped advancing for now. The most active flow currently is flow 1, which is the original flow feeding the lava delta. The affected area hasn’t changed much, at 984 hectares and up to 3,100m wide. According to the land registry, 1,452 buildings have been impacted, including 1,177 for residential use. The number of earthquakes increased to 75, being recorded mostly at intermediate (10-15 km) depths, with the day’s largest earthquake being a mbLg 3.7 event at 14 km depth. Since last week, this still reflects a decrease in earthquake strength and frequency.

The lava flows generated by the increase in activity on the 6th continue to advance south of the effusive focus to the west, although currently they largely flow over past flows in the centre of the lava flow field, with only occasional overflows of the existing lava tubes and channels. New updates have been published about the damage from the flows, including the destruction of 56 km of roads and 284 hectares of agricultural land including 159 hectares of banana plantations. Seismicity continues to decrease relative to the last week, with 54 earthquakes being recorded mostly at intermediate (10-15 km) depths, with the day’s largest earthquake being a mbLg 4.6 event at 37 km depth. Favourable meteorological conditions for air quality and the operation of the airport continue.

There has been minimal evolution in the last few days with regards to the visible eruptive activity and the progress of the lava flows. The furthest south flow, number 11, is almost inactive, although an increased contribution of lava was seen affecting flow number 3 slightly further north, causing some small overflows of the channel. Additionally, a generally increase of lava emission rate was observed at around 6pm local time. Elsewhere, the appearance of yellow-green sulphur deposits on the main cone has been noted, which have formed because of favourable cooling conditions that produce these deposits.

The eruption continues to show variable strombolian activity, with multiple more explosive vents in the main cone, and a more effusive lava emission vent on the NW flanks of the main cone. The lava flows continue to flow across existing flows in the centre and south of the lava flow field, with minimal new land being affected at this time. Nonetheless, work continues on a second access road to Puerto Naos for large tonnage vehicles in the event the LP-211 road is cut off by lava flows in the south. Seismicity continues to decrease relative to the last week, with 37 earthquakes being recorded mostly at intermediate (10-15 km) depths, with the day’s largest earthquake being a mbLg 3.8 event at 35 km depth. Favourable meteorological conditions for air quality and the operation of the airport continue.

Many active lava flows persist to the south of the lava flow field with a variable contribution from the main cone, although almost all of the flows are contained within previous lava channels or tubes, with only small local overflows of lava. The extent of the lava flows has only grown by 2 hectares since yesterday, and now totals 983 hectares.

The eruption continues to show a mixed strombolian mechanism, with explosive phases producing pyroclastics deposits and more effusive phases producing lava flows, as well as pulses of phreatomagmatic activity. There are multiple active strombolian vents in the main cone, with a lava emission vent being located on the NW flank of the main cone, with the activity of the latter being variable.

ue to the continued ashfall and low-level temperatures inversion causing poor air quality with respect to PM10 on the western side of the island, PEVOLCA have maintained the suspension of schooling in El Paso, Los Llanos de Aridane, Tazacorte, Puntagorda and Tijarafe. They will also continue the distribution of face masks and glasses to the population to mitigate the poor air quality.

Due to the increased ashfall in the north and west of the island with the increased ash emission, which was especially bad in Los Llanos de Aridane, new recommendations were brought in for the town. These are separate from the current lighter recommendations also in place in other ash-affected towns El Paso, Tazacorte, Tijarafe and Puntagorda, and advise the residents to reduce outdoor activities wherever possible, and wear FFP2 masks if they do have to go outside.

In the last 24-48 hours, an intensification has been observed in the eruptive process with increased rates of emission of lava from the NW flank of the main cone, as well as periods of more intense explosive activity and ash emission accompanied with audible explosions and visible shockwaves. Regarding the lava flows, the flow to the south of the lava flow field is currently heading south and not towards the sea for now. The rest of the active lava flows run through previously covered areas in channels, contributing to the thickening of these flows. Some sections of the original flows have been estimated at >30 m thick. Despite the uptick in activity, earthquake activity has decreased relative to previous days and remains at levels similar to the 30th. 99 events were recorded mostly at intermediate depths (10-15 km), although again the day’s most powerful earthquake was deeper, a 5.0 mbLg earthquake, this time at 38 km depth.