|
The Southern Arctic Ecozone is a Canadian terrestrial ecozone which spans the northern coast of mainland Northwest Territories, most of northern mainland Nunavut excepting the northeast peninsula, and a portion of northwestern Quebec. Its two constituent territories are interrupted by Hudson Bay. It is sparsely populated, with less than 10,000 inhabitants in 17 major settlements, the largest of which is Rankin Inlet. About 80% of the population is Inuit. It includes Ivvavik National Park and Tuktut Nogait National Park. ==Geography== Its southern boundary demarcates the tree line, and to the north it meets the Northern Arctic terrestrial ecozone and the Arctic Archipelago Marine ecozone. It was formed from glacial deposits left by retreating glaciers about 8,500 years ago, which amassed into moraines cut by long eskers up to 100 km long.〔 〕 The scouring of the land by the 3 km thick glaciers left numerous depressions, some of which contained stray chunks of ice that, upon melting during warmer periods, created kettle lakes and ponds. The Precambrian granite bedrock of the Canadian Shield protrudes to the surface through other sedimentary deposits in some areas. Moreover, glacial erratic chunks of this rock may have been transported to other areas by the ice sheet, sometimes into surroundings with no common elements.〔 Permafrost occurs in a continuous, permanent sheet throughout the zone, which consists primarily of rollings plains.〔 Just a few centimetres from the surface in some parts, it prevents water from penetrating deep into the soil, hence pooling and creating waterlogged soil that freezes regularly.〔 Cyclic freezing and thawing of the soils results in irregular features throughout the terrain, including hummocks and polygonal shapes. The land is characterised by "sprawling shrublands, wet sedge meadows, and cold, clear lakes".〔 〕 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Southern Arctic Ecozone (CEC)」の詳細全文を読む スポンサード リンク
|