Ice pinnacles on the inland-flowing Wright Lower Glacier in the Victoria Land Dry Valleys, formed by differential ablation of ice between patches of wind-blown sand. Saline Lake Brownsworth is in the background. |
Ice pinnacles on the inland-flowing Wright Lower Glacier in the Victoria Land Dry Valleys, formed by differential ablation of ice between patches of wind-blown sand. Saline Lake Brownsworth is in the background. |