Mountain Hazards
Where can Dho Tarap safely build?
A road is reaching Dho Tarap, and a town is planned once it arrives. Where the new houses go will be fixed for decades, and the flattest, sunniest land, the alluvial fans below the side valleys, is where debris flows run out. Mapping the hazards before the building starts costs a fraction of moving buildings after a disaster.
- Debris flows from steep side torrents onto the fans where people farm and build, set off by short storms, rain on snow and fast melt.
- Earthquake shaking: western Nepal sits in a seismic gap, and concrete built the lowland way does badly in both cold and earthquakes.
- River flooding and bank erosion along the Tarap Khola, where the road and bridges go.
- Glacial lake floods look less likely here than in eastern Nepal, but have not been checked for the valley.
From the U.S. Geological Survey's catalogue: magnitude 4 and above, past year.
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Source: U.S. Geological Survey, Earthquake Hazards Program · Public domain.
Borders: Natural Earth, public domain.
Maps and warnings, made with the people who live there
Hazard maps from satellite imagery and field survey; small monitoring stations on a few of the torrents, feeding a debris-flow warning the community runs; and plain guidance on where and how to build. People in Dho Tarap know which slopes move and when, and that knowledge shapes the maps and the warnings rather than being checked against them. All the data will be published openly.
→ Buildings at Altitude, the work already under way in the same valley.
Planned. This is a research concept, and we are raising the funding to start it.