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|Experiment Type:||Tsunami Wave Basin|
|Description:||The landslide tsunami generator (LTG) was deployed in the conical island scenario with a water depth of 0.6 m. The conical island configuration consists of the LTG mounted to a conical section with a base diameter of 10 m and a slope of 1:2 (vertical:horizontal) or α = 27.1˚. Wave gauges were strategically placed in the basin along rays at various angles from the landslide source to describe the tsunami wave angular dependence. A hybrid system of runup wave gauges and camera recordings focused on the runup slope measured the wave runup. The deformable landside material consisted of naturally rounded river cobbles. The landslide surface kinematics were recorded with a stereo particle image velocimetry (PIV) setup. The landslide deposit was scanned with a multi-transducer acoustic (MTA) array.|
|Dates:||August 26, 2011 - August 30, 2011|
|Facility:||Oregon State University, OR, United States|
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