Strathcona Fiord

Strathcona Fiord is an Arctic inlet on Ellesmere Island that cuts deep into the landscape, with high walls of rock and soil rising steeply on both sides. The terrain shows evidence of past glacial activity, and a freshwater lake sits at the head where meltwater gathers.

The region contains fossilized remains of a forest from the Eocene epoch roughly 50 million years ago, with preserved stumps and plant materials documenting ancient vegetation. These remains show that the area once experienced a much warmer climate than today.

Archaeological evidence includes stone tent rings near the fjord, while portions of the surrounding land are designated as Inuit Owned Land.

The location is remote and difficult to access, so travel here requires organized expeditions or scientific teams. Visitors should prepare for extreme cold, extended darkness during winter months, and the harsh conditions of the Arctic environment.

The Beaver Pond site nearby holds one of the few known locations for Pliocene vertebrate fossils from the High Arctic. This rare spot records evidence of animal life from an earlier geological period that left almost no other traces in this region.

Location: Nunavut

GPS coordinates: 78.68330,-82.66670

Latest update: December 14, 2025 11:22