Dragon Cliff, Basaltic monolith in Axel Heiberg Island, Nunavut, Canada.
Dragon Cliff is a basalt formation on Axel Heiberg Island that rises steeply above Expedition Fiord. The dark rock walls display distinct vertical column structures that run along the entire cliff face.
The basalt formation developed millions of years ago through repeated lava flows that built up in successive layers. These geological processes created the layered appearance visible on the cliff today.
The cliff stands as a reference point within the traditional territories of Inuit communities who have lived in this region for generations.
Reaching this site requires careful planning since the location in one of North America's most remote regions means visitors need special permits and transportation. It is best to contact experienced guides or outfitters familiar with local conditions.
The cliff contains more than 10 separate flow units of flood basalt, forming part of the extensive High Arctic Large Igneous Province.
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