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Impact of the 2008 Wenchuan earthquake in China on subsequent long-term debris flow activities in the epicentral area
The 2008 Wenchuan earthquake triggered the largest number of landslides among the
recent strong earthquake events around the world. The loose landslide materials were …
recent strong earthquake events around the world. The loose landslide materials were …
An example of a hazard and risk assessment for debris flows—A case study of Niwan Gully, Wudu, China
The highly geologically active, structurally complex Bailongjiang river basin, Longnan City,
Gansu Province hosts many debris-flow gullies. The recent Wenchuan and Jiuzhaigou …
Gansu Province hosts many debris-flow gullies. The recent Wenchuan and Jiuzhaigou …
Evolution of debris flow activities in Gaojiagou Ravine during 2008–2016 after the Wenchuan earthquake
Abstract The 2008 Wenchuan earthquake in Sichuan, China triggered numerous landslides
in the stricken area. The loose landslide materials retained on mountain slopes and in …
in the stricken area. The loose landslide materials retained on mountain slopes and in …
Characteristics of earthquake-and rain-induced landslides near the epicenter of Wenchuan earthquake
Numerous landslides were triggered by the 12 May 2008 Wenchuan earthquake in China,
particularly near the epicenter. During the rainy season in 2010 after the earthquake, much …
particularly near the epicenter. During the rainy season in 2010 after the earthquake, much …
Physical vulnerability models for assessing building damage by debris flows
A catastrophic debris flow occurred in Zhouqu County, Gansu Province, Northwestern
China, at midnight on 7 August 2010, resulting in damage to> 390 buildings. Assessment of …
China, at midnight on 7 August 2010, resulting in damage to> 390 buildings. Assessment of …
EDDA 1.0: integrated simulation of debris flow erosion, deposition and property changes
Debris flow material properties change during the initiation, transportation and deposition
processes, which influences the runout characteristics of the debris flow. A quasi-three …
processes, which influences the runout characteristics of the debris flow. A quasi-three …
Role of vegetation restoration in mitigating hillslope erosion and debris flows
After the 2008 Wenchuan earthquake, a large amount of loose landslide deposits was left in
the stricken region. A heavy storm in 2010 turned numerous deposits into debris flows. After …
the stricken region. A heavy storm in 2010 turned numerous deposits into debris flows. After …
Seismically induced hillslope disturbance, sediment connectivity and mass wasting: Insights from the 2008 Wenchuan earthquake
M Chen, C Tang, M Chang, J **ong - Geomorphology, 2024 - Elsevier
A mega-earthquake in a mountainous region can trigger thousands of landslides.
Subsequently, these loose co-seismic materials will experience the erosion-transport …
Subsequently, these loose co-seismic materials will experience the erosion-transport …
Declining geohazard activity with vegetation recovery during first ten years after the 2008 Wenchuan earthquake
Understanding the evolution of post-seismic geohazards with vegetation recovery is of great
significance for long-term geohazard risk assessment. The Wenchuan earthquake in 2008 …
significance for long-term geohazard risk assessment. The Wenchuan earthquake in 2008 …
Simulation of interactions between debris flow and check dams on three-dimensional terrain
Debris flows are rapid gravity-driven flows of sediment-water mixture, which can be greatly
destructive due to its huge volume, high velocity and large impact force. Check dam is …
destructive due to its huge volume, high velocity and large impact force. Check dam is …