Abstract
ON the evening of April 25 1974 one of the largest landslides known took place in the Mayunmarca valley (12.6°S, 74.6°W), adjacent to the Mantaro River, in the Peruvian Andes (Fig. 1). A total of 1,000 to 1,300 × 106 m3 of soil and rock was displaced in successive slides, which occurred within a few minutes of each other. Part of the slide material reached the Mantaro canyon, where a gigantic natural dam was formed. The dam was 3.8 km long extending along the axis of the canyon, 2.5 km wide across the river (Fig. 2), 170 m high from the river bed to the lowest point on the crest, and had a volume of 800 × 106 m3. At the time of the slide, the Mantaro River was discharging nearly 150 m3 s−1, and a reservoir was quickly impounded upstream from the dam. At its largest, the reservoir was approximately 32 km long and contained over 670 × 106 m3 of water. After 42 days, the reservoir overtopped the natural dam. The high potential of flood damage was minimised by construction of a controlled spillway across the dam.
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BERROCAL, J., ESPINOSA, A. & GALDOS, J. Seismological and geological aspects of the Mantaro landslide in Peru. Nature 275, 533–536 (1978). https://doi.org/10.1038/275533a0
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DOI: https://doi.org/10.1038/275533a0
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