Point Conception
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- Hundreds of Trekkers Missing in Nepal Flooding
Point Conception said:TL;DR: Hundreds of Trekkers Missing in Nepal Flooding
https://www.yahoo.com/news/world/articles/foreign-tourists-missing-nepals-flash-155744585.html.
gmax137 said:The videos are terrifying.
Greg Bernhardt said:The videos are terrifying
https://www.nytimes.com/2026/08/26/world/asia/nepal-flood-glacier-ice-avalanche.html
If the mass of the glacier that fell is estimated to be 5 000 000 000 kg from 1200 m then v =153 m/s. And with KE = 1/2 mv^2 . joules at impact= 58x10^9. The phase change from ice to water=334000 joules/kg. So only about 173,653 kg of ice converted to water at impact.256bits said:
Right. I incorrectly used the Cp for change in degree for water, instead of that for ice.Point Conception said:If the mass of the glacier that fell is estimated to be 5 000 000 000 kg from 1200 m then v =153 m/s. And with KE = 1/2 mv^2 . joules at impact= 58x10^9. The phase change from ice to water=334000 joules. So only about 173,653 kg of ice converted to water at impact.
Greg Bernhardt said:The videos are terrifying
https://www.nytimes.com/2026/08/26/world/asia/nepal-flood-glacier-ice-avalanche.html
Unfortunately I think we'll see more of this with glaciers continuing to melt.
Correction the joules at impact with 5000000000 kg ice falling 1200m: KE = 1/2 mv^2 = mgh = 5.8 x 10^13 joules. So with 334000 joules/kg ice to water phase change. About 176 000,000 kg ice converted to water at 0 degrees C at impact. Out of 5000,000,000 kg ice in glacier. *** Of course all this is kind of hand wavy since the glacier contains other material in the total mass . And some of the kinetic energy at impact is going to displace material at impact locationPoint Conception said:If the mass of the glacier that fell is estimated to be 5 000 000 000 kg from 1200 m then v =153 m/s. And with KE = 1/2 mv^2 . joules at impact= 58x10^9. The phase change from ice to water=334000 joules/kg. So only about 173,653 kg of ice converted to water at impact.
[Mentor Note: Some AI content has been deleted out of this post since the thread is in the technical forums]
Ref: https://en.wikipedia.org/wiki/Nuwakot,_Bagmati_ProvinceNuwakot (Nepali: नुवाकोट) is a town in central Nepal, serving as the namesake of the district of the same name. The town is located on the bank of Trishuli and Tadi Rivers. It is located around 60 kilometres west of Kathmandu, . . .
Ref: https://en.wikipedia.org/wiki/Trishuli_RiverThe Trishuli River (Nepali: त्रिशूली नदी) is one of the major tributaries of the Narayani River basin in central Nepal. The river is formed by the merger of the Gyirong Tsangpo (Kerung Khola) and the Lende Khola (Donglin Tsangpo) originating in Gyirong County of Tibet, which join together near the Rasuwa Gadhi on the Nepal–Tibet border. The valley of the river used to be the traditional trade route between the Kathmandu Valley and Tibet.
https://en.wikipedia.org/wiki/2025_Nepal_floodsRasuwagadhi flood: A severe flash flood on 8 July 2025, caused by monsoon rains and a likely glacial lake outburst, swept away the Friendship Bridge over Nepal’s Trishuli River at Rasuwagadhi.
https://www.itv.com/news/2026-09-01...ses-1000-as-hundreds-still-trapped-in-tunnelsPolice in Kathmandu buried dozens of bodies in multiple trenches as Nepal’s disaster agency said 1,003 deaths had been counted there and 3,916 people still missing, including 583 foreigners.
Chinese authorities reported 16 deaths and 546 missing in their most recent update on Sunday.
The first accounts, including from the U.S. Geological Survey (USGS), indicated the event was a magnitude 4.4 earthquake, which might have shaken rock and ice loose in a landslide that sparked the flood. A dam break was also touted as a possibility. But within 15 minutes of waking up, Cook, who has been conducting research on the Lhende Khola, had downloaded publicly available seismic data from a Nepali station located north of Kathmandu to see for herself. “I could already see that some of the initial attribution was wrong,” she says. Rather than the quick, intense seismic jolt typical of an earthquake, the data showed low-frequency, long-period waves characteristic of prolonged rumblings: a giant landslide, which itself generated the seismic signal.
On the opposite side of the Atlantic Ocean from Cook, Ekström was using data from the Global Seismographic Network, a collection of about 200 seismometers operated by many countries, to come to the same conclusion. He fed the seismic data into algorithms developed at Lamont-Doherty to find that a more accurate magnitude was 5.7—equal to a significant earthquake. It soon became “clear that [the Lhende Khola landslide] was one of the largest in the last decade or two in the world,” he says.
Cook, Ekström, and a smattering of other top natural hazard researchers soon created a Slack group to share data, discuss interpretations, and argue. (As of this publication, the group has more than 85 scientists.) It was here that the next useful observations got shared: satellite imagery from Planet Labs, which takes daily images of Earth’s surface at a resolution of 3 to 5 meters. But there was a problem: In the few available images of the mountains where the seismic signal originated, there were “very strategically placed inconvenient clouds,” Cook says. What could be clearly seen was a sharp edge, at about 5200 meters above sea level, where a glacier that blanketed the mountain had snapped off.
The imagery soon led to reports that the explanation was a glacial collapse: A thick layer of ice had slid off the underlying rock, potentially because of warming at its bottommost layer, until it crashed into the valley below. There, the shattered ice and rock flowed down the Lhende Khola valley at speeds approaching 150 kilometers per hour, kicking off a flood that caused water levels to rise as much as 9 meters in 30 minutes.