Home » Regions » North America » Tundra » Southern Arctic
Southern Arctic
Page contents
To check where a specific point lies, you can look it up in our Ecoregion Locator.
↑Map Legend & Subregion List
This list will help you navigate the regions in case you have problems with viewing or clicking the interactive map above.
Name | † | Color on Map | CEC Code‡ |
Amundsen Plains | ○ | 2.4.1 | |
Aberdeen Plains | ○ | 2.4.2 | |
Central Ungava Peninsula and Ottawa and Belcher Islands | ○ | 2.4.3 | |
Queen Maud Gulf and Chantrey Inlet Lowlands | ○ | 2.4.4 |
† Status: ✓ = Complete ○ = Needs Image … = Incomplete ∅ = Stub Only
‡ This code refers to the CEC's Level 3 ecoregion codes for North America, see here.
↑Progress
Partially Complete | With Images | Complete w/ Images |
Get involved! You can help our ecoregion articles progress faster. Help us find photos of these regions. Contact us if you have any additions or corrections to any of these articles. You can also donate to support our ongoing work.
↑About the Southern Arctic
The Southern Arctic is classified as a level II ecoregion by the US EPA and an ecozone in Canada. It extends across much of the northernmost part of mainland Canada in two disconnected pieces east and west of the Hudson Bay.This area is covered by continuous permafrost, but summer thaws are longer, deeper, and more consistent than regions farther north.
This region can be seen as a transition between the truly treeless tundra, and the beginning of the Taiga. Numerous woody species survive in this area, but generally grow as dwarf shrubs. Grasses, sedge, and other herbaceous plants, as well as lichens are all abundant in this area. This region is almost entirely covered in vegetation, with growth densest in sheltered areas. Wetlands and ponds are abundant.
To the north lies the more barren Northern Arctic, and to the south, the Taiga Shield over the much of the region, and the Taiga Plain farther west. Following the coastline of the Arctic Ocean to the West, this region is replaced by the Alaska Tundra.