Advances in Civil Engineering

Research Article

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

Table 3

Formation mechanisms of debris flows along the Parlung River from Bomi to Suotong (e.g., 1–13 in Figure 1).
NO.12345678910111213
NameBitong gullyDada gullyJiaolong gullyCangguo gullyZhataduo gullyNaha gullyGuxiang gullySuotong gullyQiuzhu gullyChidan gullySongrao gullyMichong gullyDanka gully
Formation mechanismModes I and IIIMode IIIMode IIIMode II—Modes I and IIIModes I and IIIMode IIIMode IIMode IIModes I and IIIMode IIMode II
Data sourceThis studyThis study[16]This study—This study[16][16]This studyThis study[22]This studyThis study
LocationNorth bankSouth bank