Northern Arctic Ecozone (CEC)

Palaeozoic and Mesozoic sedimentary rock forms the western portion of the ecozone, whereas Precambrian granite is the dominant feature in the east.[3] Broad flat plains are common on the coastlines, and extend inland up to 10 kilometres (6 mi) in some parts.[4] In the east, plateaus and rocky hills merge into the foothills of the Arctic Cordillera.[3] The west is characterised by glacial deposits and "frost-shattered limestone"[4] and sandstone.

A permanent layer of permafrost may be up to one kilometre thick, and lies under a shallow stratum of waterlogged active soils that cyclically freeze and thaw, creating patterned ground.[4] Its features are similar to the badlands found in the southwestern United States.

The region is extremely cold, with temperatures rising above the freezing point only in July and August. Short, cold summers give way to bitterly cold, dark winters with mean January temperatures less than −30 °C in the northern islands.[4] Little precipitation falls here, with a typical annual total of 250 mm, but may exceed 500 mm in its extreme southeastern extent. Snowfall may occur at any time, and snow cover persists from September to June.[4]

Despite the low precipitation, the permafrost's ability to prevent water from draining through the soil, and the abundant snow and ice cover throughout the zone ensure that the climate is usually moist.[4]

The northern waters are permanently frozen, but coastal areas in the south may open in the summer, though numerous large ice floes persist.[3]

A number of protected areas have been established to protect representative and/or significant portions of this ecozone. These include Aulavik National Park, Auyuittuq National Park, Sirmilik National Park, Qausuittuq National Park, Quttinirpaaq National Park, and Ukkusiksalik National Park.