The transition from the tropical rain forest to our own woodlands is one
of the most interesting, as it is certainly the most gradual in nature.
Lack of space prevents our stopping to note those strategic points along
this pathway from a hot, steaming forest to the cool shade of our open
woods, where traveling, in at least a virgin forest, may be done easily
on horseback. As we come northward, and if we could travel continuously
through the forest, we should lose first the epiphytes, then most of the
lianes, and finally all the condition of vegetation crowding into every
inch of space suitable for it. While trees in our virgin forests are as
thick as they can be, the forest floor is open and on it grow only a few
herbs that will stand lack of sunshine.
But the really great difference is the long, unfavorable season in
temperate regions where the forest must drop all its leaves, after, in
at least our own Eastern States, the most gorgeous foliage coloring of
any forest in the world. The winter months when the woody vegetation is
practically fully exposed to the elements, are particularly severe in
their effects. Leaf-fall, which is such a common sight as to arouse
scarcely any interest, is the only device by which the great bulk of our
forest trees survive, and only in the southern part of the region are
there found such woody plants as the mountain laurel, rhododendron,
American holly, and a few others which are evergreen but not
cone-bearing ones, and are the only reminders of the truly evergreen
forests of the tropics. The winter winds farther north and in the
central treeless part of the United States prove too much for many kinds
of trees, for instance, all the oaks and sassafras, none of which go
very far north.
There is sufficient rainfall to produce forests much farther north than
they are found, but lower temperatures prevent trees from growing just
as too little water stops their growth altogether. Toward the northern
limits, or upon high mountains, the upper limits of the forest, we get
the best idea of how persistent woody vegetation is in the general
forest area of the eastern United States. Stunted, wind-swept and
weather-beaten trees are often found only a couple of feet high and over
sixty years old. Sometimes they will be flattened out on the ground or
on bare rock, making great patches of bushy growth quite unlike their
lofty relations in the lowlands. The growth rate for such plants is so
slow that their annual rings are all but obscured. With such persistence
in the production of these elfin forests, high up on mountains under the
most unfavorable conditions, it is little wonder that below this are
trackless woods, and that the northeastern United States has one of the
finest developments of the temperate or summer forest in the world.
Public-domain text, read in full here on John Shaqi.
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