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Figure 9 | Earth, Planets and Space

Figure 9

From: Numerical simulations to account for boulder movements on Lanyu Island, Taiwan: tsunami or storm?

Figure 9

Computed flow depth and flow depth at different survey lines. (A) Topography of survey lines X-X' and Y-Y'. (B) Difference in topography between X-X' and Y-Y', which is calculated by subtracting the topography of X-X' from that of Y-Y' (Figure 7). (C) Maximum flow depth. No reef is the model with topography the same as X-X' and where the reef width is set to 0. (D) Maximum flow velocity.

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