Ice avalanches in high mountain terrain contribute to the build-up of ice in the accumulation area, as here on Nevado Chacraraju (6172 m), Cordillera Blanca, Peru. JA |
Ice avalanches in high mountain terrain contribute to the build-up of ice in the accumulation area, as here on Nevado Chacraraju (6172 m), Cordillera Blanca, Peru. JA |