There were multiple other pulses, with an earlier one around 25 minutes after the landslide. Seismic data from KKN station, thanks to the Department of Mines and Geology. The flow is travelling much more slowly than in the Rasuwa disaster, allowing for more evacuation.

Another flow disaster in Nepal, just one catchment to the west of the Trishuli. This one is also caused by a landslide, but with a different mechanism - the landslide dammed the river and an outburst flood followed. Landslide was at 4:22 local time, and the largest flood pulse started around 6 am.

There are reports of more flooding on the Trishuli. The seismic data suggests it started around 8:45 UTC, 2:30 am Nepali time, that the flood is much smaller than the one on Wednesday, and that the flood peak has passed. We need more information to confirm if it's related to the newly formed lakes.

A very nice peek into what we've been up to over the few days!

Yes, checking in from France! I was in the valley several times in the past year though, so this is difficult and terrifying to see.