Effects of Glacier and Geomorphology on the Mechanism Difference of Glacier-Related Debris Flow on the South and North Banks of Parlung Zangbo River, Southeastern Tibetan Plateau

<div>Debris flow events from investigation in the field. (a) Bitong debris flow in 2016; (b) Dada debris flow in 2017. (c) Guxiang debris flow in 2020. (d) Jiaolong debris flow in 2016; (e) Chidan debris flow in 2016. (f) Songrao debris flow in 2018).</div>

Advances in Civil Engineering

fig3

Figure 3

Figure 3: Effects of Glacier and Geomorphology on the Mechanism Difference of Glacier-Related Debris Flow on the South and North Banks of Parlung Zangbo River, Southeastern Tibetan Plateau 

Figure 3 | Effects of Glacier and Geomorphology on the Mechanism Difference of Glacier-Related Debris Flow on the South and North Banks of Parlung Zangbo River, Southeastern Tibetan Plateau 