The new lava flow that emerged on the afternoon of the 23rd continues to flow slowly parallel to the southern limits of the old flows and has been named stream 10 to aid its tracking. Elsewhere, the active flows are largely being fed by lava...
Currently, a period of the redistribution of active lava flows seems to be taking place around the volcano, with the flows affecting La Laguna appearing to have almost stopped and receiving a smaller contribution of lava than previous days. As such, the area affected by...
The front of the active lava flows in La Laguna to the north of the flow field are currently practically stopped, although there still remains a high flux of lava feeding these flows, which is leading to their widening and thickening. Nonetheless, the evacuation ordered...
The two active streams to the north have grown and coalesced and appear to be travelling to the SW of La Laguna Mountain. However, it cannot yet be ruled out that their growth and the changing topography may mean the flow travels northwards in the...
The two active lava flows to the north of the flow field continue to be heavily monitored as they both continue to advance. The further south of the two, which travels to the south of La Laguna Mountain, is only 80 m from the coast,...
The self-protection recommendation announced yesterday for the population of El Paso, in the face of continuing unfavourable air quality with respect to PM10 concentrations, has been maintained. Residents should stay indoors as much as possible, particularly between 2pm-9pm local time, and wear an FFP2 mask...
The eruption continues as in the previous days, with a Strombolian mechanism with a predominant effusive phase and a weaker explosive phase. More explosive activity continues to be concentrated in multiple vents within the main cone, and the effusive outlet is seen as a stepped...
The eruption continues to show a strombolian mechanism with mixed explosive and effusive phases, with the effusive phase remaining the stronger of the two currently. The main active lava flows are the two branches to the north of the original flows. The southern branch of...
Although the effusive phase of the eruption continues to be more powerful currently than the more explosive strombolian phase, the active lava flow fronts are currently barely advancing. This is because of the existence of lava tubes, although the flows continue to widen and grow...
The eruption continues to show a mixed strombolian mechanism, with both explosive and effusive phases, although currently the effusive phase is the more predominant one. This has been observed downstream as an increase in fluidity of the active lava flows as a result of the...