Endicott Arm is a narrow fjord approximately 50 miles (80 km) southeast of Juneau, Alaska, extending over 30 miles (48 km) with nearly one-fifth of its area covered in ice. At the head of the fjord, glaciers, including the Dawes Glacier that we are heading toward, regularly expel enormous chunks of ice that float along the water surface, from a few inches in size up to three stories wide.
We head out of Ketchikan up to the Endicott Arm, entering early in the morning and cruising up the fjord as the sun rises.
Along the coast on the way up
Making our way up the fjord
Waterfalls and floating ice along the way
Continuing up the fjord
Reaching the Dawes Glacier at the head of the fjord
Turning around and heading back
We spot several large chunks of blue floating ice. This phenomenon occurs when snow falls on a glacier, is compressed, and becomes part of the glacier. During compression, air bubbles are squeezed out and dense ice crystals emerge that absorb other colors more efficiently than blue, leading us to see them as blue.
Blue ice
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