An Analysis of Factors Affecting Flowslide Deposit Morphology Using Taguchi Method

Figure 9

Topography of typical flowslides. (a) and (b) located in Folkestone Warren (51°05′03″ N 1°20′36″ E), (c) and (d) located Dover, Kent (51°07′53″ N 1°20′36″ E). Source from Hutchinson [36].

(a)

(b)

(c)

(d)