New IR map:
https://volcanoes.usgs.gov/observatories/hvo/maps_uploads/image-488.jpg
https://volcanoes.usgs.gov/observatories/hvo/maps_uploads/image-490.jpg
The Kapoho entry point has moved even further south. On one hand, it's great that the area it's flowing over doesn't have much there. On the other hand, I don't like how resistant it's being to go straight to the sea, as if it's built up somewhat of a barrier for itself. Kind of worries me that if it builds up too much resistance on the southern front, it might choose to flow into the remaining houses on the north side of Kapoho :Þ
No change - neither improvement or worsening - in the health of the flow at the northern branch of the first fork. The partial obstruction that first appeared in the last IR image is still visible.
Resistance in going into sea? What resistance is that? The vast majority of the lava is going into deep sea right now.