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Classification
Soil Landscape Illustrations of the Northwest Territories
Almost all soil landscapes in the Northwest Territories are
underlain by permafrost with resulting effects on soil development
and the landscape. The development of soils is affected by
cryogenic processes, organisms, parent material, time, weathering
and the translocation of materials. The landscape is dominated by
various permafrost landforms and patterned ground types (e.g.
pingos, palsas, peat plateaus, circles, nets, earth hummocks and
polygons), and is often underlain by thick ground ice. The
landscape is thus very sensitive to natural and man-made
disturbances. North of the arctic tree line these landscapes are
part of the Arctic ecoclimatic zone. Although the northern part of
this zone is sparsely vegetated, the southern part is covered by
shrubby tundra vegetation. South of the arctic tree line the
landscapes are covered by open lichen - coniferous forest
(Subarctic zone) and closed canopy forest (Boreal zone).
Soil landscapes and associated soil profiles
Mesic Organic Cryosol associated with
perennially frozen peatland
 |
Mesic Organic Cryosol profile
 |
Brunisolic Turbic Cryosol associated with
earth-hummock-covered till landscape
 |
Brunisolic Turbic Cryosol profile
 |
Regosolic Turbic Cryosol associated with
colluviated valley
 |
Regosolic Turbic Cryosol profile
 |
Orthic Turbic Cryosol associated with undulating
landscape
 |
Orthic Turbic Cryosol profile
 |
Orthic Turbic Cryosol associated with
bedrock-controlled till landscape
 |
Orthic Turbic Cryosol profile
 |
Degraded Eutric Brunisol associated with level
valley landscape
 |
Degraded Eutric Brunisol profile
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Source: SLC Illustration poster