You can see Cavell Glacier fairly well in this photograph. Look at the bottom of the mountain; see the inverted cones? Those cones are formed by avalanches from above and accumulate at the bottom of the rock wall.
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You can see Cavell Glacier fairly well in this photograph. Look at the bottom of the mountain; see the inverted cones? Those cones are formed by avalanches from above and accumulate at the bottom of the rock wall.
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