description Endicott Arm Overview
Endicott Arm is a deep, narrow fjord carved by glacial activity in southeastern Alaska’s Prince William Sound. The waterway is characterized by the presence of Dawes Glacier, a substantial tidewater glacier, and frequent iceberg sightings. It serves as an important habitat for harbor seals and provides opportunities for observing dynamic glacial processes. This location is particularly appealing to visitors interested in Alaskan geology, marine wildlife, and glacial landscapes.
help Endicott Arm FAQ
What glacier is located at the end of Endicott Arm?
Endicott Arm is a deep fjord characterized by the presence of the Dawes Glacier. This massive tidewater glacier actively calves enormous icebergs directly into the water.
Where is Endicott Arm located?
The fjord is carved by glacial activity in southeastern Alaska. It is a popular destination for small cruise ships and boat tours navigating the state's famous Inside Passage.
What wildlife is commonly seen in Endicott Arm?
The waterway serves as an important habitat for harbor seals, which frequently rest on the floating icebergs. Visitors also commonly spot bears, bald eagles, and whales along the steep fjord walls.
Why is Endicott Arm filled with so much floating ice?
The constant calving of the Dawes Glacier fills the narrow fjord with thousands of small and large icebergs. This dense ice accumulation makes the waters extremely cold and visually stunning.
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