If we take the trees as representatives of the flora of North America,
and this seems to be the only practicable method in a general treatise,
we find them growing most densely and presenting at the same time the
greatest variety where the temperature is uniformly high throughout the
year and the rainfall heavy and long-continued. From the torrid lowlands
the forests in general decrease in the variety and number of trees on a
given area, both towards the north, where temperature becomes the
controlling factor, and towards regions of small rainfall, where the
leading adverse condition is deficiency of moisture. In the most highly
favoured localities the struggle for existence between species and
species and individual with individual is intense, exposure to the
life-giving sunlight being the dominant aim of every one of the
contending hosts. As drier or colder regions are approached, but few
species can survive and the forests are characterized by their monotony.
Where the conditions of heat and moisture are such that the existence of
a species is precarious, the balance of power, so to speak, passes to
the secondary conditions; and the texture and composition of the soil,
slight differences in the relief of the land, and consequently in
drainage or in the degree of exposure to light, prevalence of fires,
etc., make themselves prominent and limit distribution.
[Illustration: FIG. 28.--Map showing the distribution of forests in
North America.]
From a geographical point of view, the broadest features in the flora of
North America are the forested and unforested areas. The distribution of
the forests, prairies, and treeless plains as they existed previous to
the coming of Europeans is shown on the accompanying map. For the
portion of the continent to the northward of Mexico the data on
which this map is based are much more abundant than for the southern
portion.
THE FORESTS
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