--> Figure 5. Close-up of A from Figure 4 showing syn-sedimentary deformation formed by flattening during deposition of the slump. The more competent mud layers tend to pull apart into boudins whereas the surrounding sandy layers flow to fill the remaining available space.

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Figure 5. Close-up of A from Figure 4 showing syn-sedimentary deformation formed by flattening during deposition of the slump. The more competent mud layers tend to pull apart into boudins whereas the surrounding sandy layers flow to fill the remaining available space.