The 13 October 2020 Ranger Station-7 Landslide

LCI : VNM202509011810
Main Information
Landslide Name : The 13 October 2020 Ranger Station-7 Landslide
Latitude : 16:25:59.65 N
Longitude : 107:18:38.61 E
Location
City / District : Phong Xuan
Province : Thua Thien Hue
Country : Việt Nam
Reporter
Reporter 1 : Pham Tien
Reporter 2 : Tien Van
Landslide Type
Material : Debris
Movement : Slide
Velocity (mm/sec) : Extremely Rapid
Depth (m) : Moderate-Shallow
Slope (degree) : Moderate
Volume (m³) : Moderate-Small
Date of Occurence
Date of Occurence : Oct 13, 2020
Other Information
Land Use Source area : Forest
Run-out/deposition area : Road
Other Activity : Active in the past
Triggering Factor : Rainfall
Death(s) & Missing : 13
Houses and other structural damage : 1
Photo of landslide :
Google earth kmz file : Ranger Station-7 Landslide.kmz
Plan of landslide :
Cross section of landslide :
Reference (paper/report) : https://link.springer.com/article/10.1007/s10346-021-01663-z
Testing graph : -
Monitoring graph : -
Video of moving landslides including 3D simulation : -
Description :

At approximately 0:00 AM on 13 October 2020, a rapid rainfall-induced landslide occurred in Phong Xuan commune, Phong Dien district, Thua Thien Hue province, sweeping over Ranger Station No. 7 and claiming the lives of 13 rescue team members, including 11 army officers and 2 district officials. Field evidence and topographic analysis indicate that the Ranger Station No. 7 landslide involved an estimated volume of about 81,550 m³, comprising two distinct blocks in the lower and upper slope parts. The failure initiated in the lower slope section, accompanied by a loud sound, which subsequently triggered the collapse of the upper part. The 13 October event was associated with extreme rainfall, with a cumulative amount of 2,190.2 mm recorded at the A Luoi rainfall station between 6 and 12 October. The landslide mass rapidly moved downslope, destroying the ranger station located 145 m from the landslide toe. The displaced materials not only accumulated on the rupture surface but also extended beyond the toe, spreading into the stream channel and covering a flat downslope area of approximately 2.25 ha.