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Updated: August 2, 2024
Cook's studies that the deforestation of the Cuzco Basin by the hand of man, and modern methods of tillage on unterraced slopes, have caused an unusual amount of erosion to occur. Landslides are frequent in the rainy season. Opposite Saylla is Mt. Picol, whose twin peaks are the most conspicuous feature on the north side of the basin.
One may imagine the dismay with which the agricultural residents of these ancient houses saw their beautiful fields at the bottom of the hill, covered in a few days, or even hours, by enormous quantities of coarse gravel brought down from the steep slopes of Picol after some driving rainstorm. It may have been some such catastrophe that led them to take up their residence elsewhere.
In one place telephone wires intercept one's view of the beautiful stone facade of an old Jesuit Church, now part of the University of Cuzco. It is built of reddish basalt from the quarries of Huaccoto, near the twin peaks of Mt. Picol.
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