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The Lagrange equation (7) requires modification for a distant object because in that case the object height h is infinite, and the slope angle u is zero.
The slope angle is 40°.
where α is the slope angle.
α: the slope angle of the sea-bottom surface.
Fig. 5 Thematic map of the slope angle.
Where, θ is the slope angle of the landslide.
Landslide number density values increase with the slope angle.
The landslide number density value increases with the slope angle.
Although tractive resistance increases with the slope angle, the compaction resistance remains largely independent with changes in the slope angle.
The slope angle factor S can be defined as: S=tan alpha (1)in which α is the slope angle of the shallow landslide (Fig. 4).
The slope angle of the sliding path was approximately 18° according to field investigations.
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