Riñihuazo

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The town of Riñihue flooded during the Riñihuazo
The town of Riñihue flooded during the Riñihuazo

The Riñihuazo is the name given to the damming of Riñihue Lake on 22 May 1960, after that during Great Chilean Earthquake a landslide blocked its outflow.

During the Great Chilean Earthquake, several landslides near Tralcan Mountain blocked the outflow of Riñihue Lake by (39°46′43″S, 72°27′03″W). Riñihue Lake is the lowest of the Seven Lakes chain and receives a constant inflow from the Enco River. The blocked San Pedro River, which drains the lake, passes through several towns and the city of Valdivia before finally reaching Corral Bay.

Because the San Pedro River was blocked, the water level of Riñihue Lake started to rise quickly. Each meter the water level rose was equivalent to 20 million cubic meters, which meant that 4800 million cubic meters of water would release into the San Pedro River (easily overpowering its flow capacity of 400 cubic meters per second) if it rose above the final, 24-meter-high dam. This potential disaster would have destroyed all the settlements along the course of the river in less than five hours, and had more dire consequences if the dam broke.

About 100,000 people lived in the affected zone. Plans were made to evacuate the city, and many people left.

Workers digging a dyke in San Pedro River
Workers digging a dyke in San Pedro River

To avoid the destruction of Valdivia, several military units and hundreds of workers from ENDESA, CORFO, and MOP started an effort, called the Riñihuazo, to control the lake. Twenty-seven bulldozers were put into service, but they had severe difficulties moving in the mud near the dams, so dykes had to be constructed with shovels. A proposal by some US military to blow up the dams with missiles from an helicopter was rejected. The work was not restricted to the lake; drainages from other parts of the Seven Lakes were also dammed to minimize the flow into Riñihue Lake. These dams were removed later, with the exception of Calafquén Lake, which still retains its dam.

By 23 May, the main dam had been lowered from 24 to 15 meters, allowing 3000 million cubic meters of water to leave the lake gradually, but still with considerable destructive power. The team led by engineer Raúl Sáez finished two months after beginning the works.

There is evidence that a similar landslide and earthquake occurred in 1575.