GLACIAR 511

 

Event description

 

On May 31, 1970 the most catastrophic known avalanche in history descended from Nevados Huascaran, the highest peak in the Peruvian Andes. The avalanche caused about 18`000 casaulties. The avalanche was triggered at 3:23 PM by a great earthquake (M=7.7). The avalanche originated from a partially overhanging cliff at 5400-6500 m elevation, where the fractured granitic rock of the peak was covered by a 30-m-thick glacier. The avalanche had a volume of ~ 50-100 million cubic meters and traveled 16 km to Rio Santa with a vertical drop of 4 km.

 

Damage

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The aluvion buried the city of Yungay. 18`000 people died.

 

Data source

 

- Lliboutry, L., Arnao, B. M., Pautre, A., Schneider, B. (1977): Glaciological problems set by the contol of dangerous lakes in Cordillera Blanca, Peru. I. Historical failures of morainic dams, their causes and prevention. Journal of Glaciology, 18 (79), 239 � 254.

- http://www.soest.hawaii.edu/martel/Courses/GG454/GG454_Lec_20.pdf

 

Remarks

 

Mapping after the 1970 event revealed deposits from a substantially larger pre-Columbian (before 1492) avalanche that might have attained average speeds of 315-355 km/hr.