Dragon Cliff

Dragon Cliff[1] is a basaltic monolith located on western Axel Heiberg Island, Nunavut, Canada.

Dragon Cliff is made of flood basalt lava flows that contain more than 10 flow units totalling over 200 m (660 ft) of stratigraphic thickness.

It is part of the Albian Strand Fiord Formation, which in turn forms part of the High Arctic Large Igneous Province.

The Strand Fiord Formation is interpreted to represent the cratonward extension of the Alpha Ridge.

This Qikiqtaaluk Region, Nunavut location article is a stub.