Application of Slope Radar (S-SAR) in Emergency Monitoring of the “11.03” Baige Landslide

Table 1

Strong deformation area statistical characteristics.

No.	Location	Estimated area (m^2)	Cause of strong deformation
①	K3-2	61000	Shallow residual slope soil and cataclastic rock mass collapse
②	K1	14000	Slope face loose stone fall
③, ④	V-shaped groove area	13200	Top of V-shaped groove and falling blocks on both sides scrape the surface
⑤	Cut the exit	15400	Surface landslide deposits, shallow residual slope soil, and cataclastic rock mass collapse