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Updated: July 15, 2025
It may be that the Inca Viracocha, an unusually gifted ruler, was particularly interested in ceramics and was responsible for building the temple. If so, it would be natural for people who are devoted to ancestor worship to have here worshiped his memory. Route Map of the Peruvian Expedition of 1912 The Valley of the Huatanay
The ancient buildings have doors, windows, and niches in walls of small stones laid in clay, the lintels having been of wood, now decayed. When we asked the name of these ruins we were told that it was Saylla, although that is the name of a modern village three miles away, down the Huatanay, in the Oropesa Basin. Like Piquillacta, old Saylla has no water supply at present.
When one looks at the great amount of arable slopes on most of the hills of the Cuzco Basin and the unusually extensive flat land near the Huatanay, one readily understands why the heart of Inca Land witnessed a concentration of population very unusual in the Andes.
Accordingly, I believed it preferable to take another geologist, whose independent testimony would give great weight to those conclusions should he find them confirmed by an exhaustive geological study of the Huatanay Valley. I asked Dr. Bowman's colleague, Professor Gregory, to make the necessary studies.
Piquillacta is a large mass, nearly five miles long and two miles wide, rising to a point of 2000 feet above the Huatanay and Vilcanota rivers, it has no streams, brooks, or springs. It is an isolated, extinct volcano surrounded by igneous rocks, lavas, andesites, and basalts.
Its drainage was finally accomplished by the Huatanay cutting down the sandstone hills, near Saylla, and developing the Angostura gorge. In the banks of the Huatanay, a short distance below the city of Cuzco, the stratified beds of the vanished Lake Morkill to-day contain many fossil shells.
The valley of the Huatanay River is divided into three parts, the basins of Lucre, Oropesa, and Cuzco. The basaltic cliffs near Oropesa divide the Lucre Basin from the Oropesa Basin. The pass at Angostura, or "the narrows," is the natural gateway between the Oropesa Basin and the Cuzco Basin. Each basin contains interesting ruins.
From the Oropesa Basin, one enters the Cuzco Basin through an opening in the sandstone cliffs of Angostura near the modern town of San Geronimo. On the slopes above the south bank of the Huatanay, just beyond Angostura, are the ruins of a score or more of gable-roofed houses of characteristic Inca construction.
The valley of the Huatanay is one of many valleys tributary to the Urubamba. It differs from them in having more arable land located under climatic conditions favorable for the raising of the food crops of the ancient Peruvians. Containing an area estimated at less than 160 square miles, it was the heart of the greatest empire that South America has ever seen.
At his request a very careful map of the Huatanay Valley was prepared under the direction of Chief Topographer Albert H. Bumstead. Dr. Eaton, who had had no opportunity of seeing Peru, was invited to accompany us and make a study of the bones of modern Peruvian cattle as well as of any other skeletal remains which might be found.
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