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Slope angle accuracy and precision were 0.40° and 0.32°, respectively.
Slope angle per se was not correlated with basal area or AGBM within the residual soils.
Slope angle is an important controlling factor of coseismic landslides.
Slope angle was taken into account when projecting field data onto plots of horizontal orientation.
Slope angle is one of the most important factors on slope instability.
Due to combined loading the lateral load carrying capacity of pile in sloped ground is high in slope angle 1 2.5 and low in slope angle 1 1.5.
Since the transport rate for creep and rain splash is proportional to the slope angle, the slope angle must also increase from the divide, resulting in the slope convexity.
Slopes are then further partitioned based on the alignment between slope angle and dip angle.
Surfaces were also compared in the GIS according to elevation, slope angle, and bedrock lithology.
The temperature, ram speed, slope angle and holding time have more important effects descendingly.
For a 0° slope angle, the hydrodynamic pressure reaches its highest level.
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