During the last ice age, which ended 10 000 years ago, the Shield was repeatedly scoured by advancing glaciers. While in retreat, they blanketed much of the landscape with coarse till released
by torrential meltwater streams. Glaciation also had an important influence on the nature of today's soils, having scraped away much of the preglacial cover, often right down to bedrock. Not only are most soils here relatively thin, they are also high in acidity, low in nutrient availability, and cool.
Organic soils underlying the expansive wetlands of this area further restrict plant growth by being oxygen poor and notoriously soggy. Although all of these qualities put severe restrictions on agriculture, the soils of the Boreal Shield are generally well suited for the growth of coniferous trees, as shown by the vast evergreen forests that now blanket much of this ecozone.
Cool temperatures, a short growing season, frequent forest fires, and acidic soils are among the
many challenges faced by plant life in this ecozone. In spite of this, almost 85% of the ecozone is
forest, of which 70% is considered productive for timber. The forest is dominated by a few highly
adaptable tree species, such as black spruce, white spruce, jack pine, and balsam fir. Black spruce,
the most common species, yields high-quality wood pulp and is therefore a prime species for
Canada's growing paper industry.
Farther south there is a higher proportion of broadleaf trees, such as paper birch, trembling aspen,
and balsam poplar, as well as other conifers, such as white, red, and jack pine. In southeastern parts
of the ecozone, species characteristic of more temperate climates are common, including yellow
birch, sugar maple, black ash, and eastern white cedar.
Throughout the Boreal Shield, these forests are mixed with innumerable bogs, fens, marshes, and
other wetlands. Covering nearly 20% of the ecozone, these wetlands are among its most diverse
and biologically productive ecosystems.
The boreal forest soil is very acidic, because the trees aren't deciduous, so they have no annual leaf fall that decomposes and enriches the soil. Because of that, the undergrowth is not very well developed in some boreal forests.
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Soil in the Canadian Shield is very course. It doesn't hold moisture, but is good for growing trees. Because of there long roots, they can reach more nutrients.
There are quite a few non-living things in the Boreal forest. There are rocks and water in the Boreal forest.
the soil used in construction has been handled by man and the natural soil forms naturally as it is
The boreal forest soil is very acidic, because the trees aren't deciduous, so they have no annual leaf fall that decomposes and enriches the soil. Because of that, the undergrowth is not very well developed in some boreal forests.
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Sunlight,air soil
The soil in the Boreal Forest is more fertile than tundra but more acidic(harsh) which limits the number of plants that can thrive
in the candian shield
Soil in the Canadian Shield is very course. It doesn't hold moisture, but is good for growing trees. Because of there long roots, they can reach more nutrients.
There are quite a few non-living things in the Boreal forest. There are rocks and water in the Boreal forest.
the soil used in construction has been handled by man and the natural soil forms naturally as it is
the nature solute is the solute is natural EX: Soil Soil rocks
Natural soil does not have enough nutriences
No crops are grown in the tiaga or boreal forest. The soil is too thin in that area for any crops to be grown.
any soil