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Figure 3 - The December 2012 Mayo River debris flow triggered by Super Typhoon Bopha in Mindanao, Philippines: Lessons learned and questions raised
![Figure 3: Debris-flow deposits in the New Bataan area. A= Boulder in ancient reverse-graded debris-flow deposit. Wellestablished trees indicate an age of some decades prior to the settlement of the town. B= Old debris-flow deposits underlying New Bataan – Andap highway. Boulders are separated from each other by a matrix of finer-grained sediment. For scale, the concrete is 15 centimeters thick. The coarse sediment atop the highway are new debris-flow deposits. C= Boulder-rich deposits of debris](https://www.researchgate.net/profile/Kelvin-Rodolfo/publication/301270759/figure/fig2/AS:361488507260951@1463196984927/Debris-flow-deposits-in-the-New-Bataan-area-A-Boulder-in-ancient-reverse-graded_Q320.jpg)
Debris-flow deposits in the New Bataan area. A= Boulder in ancient reverse-graded debris-flow deposit. Wellestablished trees indicate an age of some decades prior to the settlement of the town. B= Old debris-flow deposits underlying New Bataan – Andap highway. Boulders are separated from each other by a matrix of finer-grained sediment. For scale, the concrete is 15 centimeters thick. The coarse sediment atop the highway are new debris-flow deposits. C= Boulder-rich deposits of debris
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