[Illustration: FIG. 13.--The larger physiographic divisions of North
America.]
Each of the four physiographic provinces briefly described above is in a
conspicuous manner elongated in a north and south direction. The
mountains, valleys, and plateaus, as well as the controlling lines of
structure in the rocks below the surface, throughout the main body of
the continent coincide in direction more or less nearly with the
parallels of longitude. At the south, however, and crossing the trend of
each of the provinces named above, is the:
Fifth, or Caribbean province, which includes the West Indies, the
southern part of Mexico, and all of Central America. In this
province are the _Antillean Mountains_, now mostly submerged, the
principal axes of which trend east and west.
With this brief outline of the larger physical divisions of North
America in mind, let us endeavour to become acquainted with the leading
characteristics of each of the provinces as they exist to-day, and at
the same time learn something of their long and varied histories.
COASTAL PLAINS AND PLATEAUS
_The Coastal Plains._--From New York to Key West and thence about the
borders of the Gulf of Mexico to the neighbourhood of Vera Cruz, the
border of the present land area of the continent is formed by a low
plain, from 30 to 50 miles broad in New Jersey, but increasing in width
southward to Georgia and Florida, where its somewhat indefinite inland
margin is more than 100 miles from the sea, and reaching its greatest
development in the delta of the Mississippi. Extending southward about
the west coast of the Gulf, it forms the low, featureless eastern border
of Texas, about 50 miles broad, and passes into Mexico, but gradually
narrows as the Pacific Mountains approach the coast, and ends in the
vicinity of Vera Cruz.
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