fig4
![Predictive models for the run-out distance of clay slopes based on material point method](https://image.oaes.cc/b586e73d-4a38-48f2-a563-494bfd5461f2/5908.fig.4.jpg)
Figure 4. (A) The input sinusoidal wave; and the recorded wave velocities at (B) point A1; (C) point A2; (D) point A3; (E) point A4; and (F) point A5, respectively.
Figure 4. (A) The input sinusoidal wave; and the recorded wave velocities at (B) point A1; (C) point A2; (D) point A3; (E) point A4; and (F) point A5, respectively.
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