Tsaoling landslide is the largest and best documented landslide among several large
landslides induced by the 1999 Taiwan Chi-Chi earthquake. Pliocene sedimentary rocks of …

Pliocene sedimentary rocks of about 130 Mm3 in volume slid along bedding planes dipping
by 14°, with an average speed of about 35 m/s, during the Tsaoling landslide. We conducted …

In the village of Tsaoling (in Yunlin County, Taiwan), a major landslide was triggered by the
Chi-Chi earthquake in 1999 with more than 125× 106 m3 of rock displaced. The kinematic …

Friction characteristics on the sliding surface of giant landslide is important for investigating
the triggering, moving, and deposition. In this research, we incorporating a velocity …

Dynamic friction degradation of the sliding surface in large earthquake-triggered landslides
is widely assumed, especially for high-speed and long run-out landslides. But there are few …

The Daguangbao (DGB) landslide which triggered by the 2008 Wenchuan earthquake is
one of the largest earthquake-triggered landslides in the world over the past century. In this …

In reactivated slow-moving landslides, the prediction of velocity and displacement is a
crucial issue for understanding landslide kinematics and realizing warning systems. A …

We performed numerical simulations of the 2011 deep-seated Akatani landslide in central
Japan to understand the dynamic evolution of friction of the landslide. By comparing the …

Tsaoling is located in Southwestern Taiwan, 10 km east of the frontal thrusts of the mountain
belt. Five large historical landslide events were recorded from 1862 to 1999. No details of …

During the 1999 Chi-Chi earthquake, extensive slope failures were triggered by the
earthquake in central Taiwan. Among those, a large-scale dip-slope slide in Tsao-Ling …