United States

East of the Rockies all climatic boundaries are gradational. None, however, is so important or so imperceptibly subtle as the boundary zone that separates the Humid East from the Dry West and that alternates unpredictably between arid and humid conditions from year to year. Stretching approximately from Texas to North Dakota in an ill-defined band between the 95th and 100th meridians, this transitional region deserves separate recognition, partly because of its great size, and partly because of the fine balance between surplus and deficit rainfall, which produces a unique and valuable combination of soils, flora, and fauna. The native vegetation, insofar as it can be reconstructed, was prairie, the legendary sea of tall, deep-rooted grass now almost entirely tilled and planted to grains. Soils, often of loessial derivation, include the enormously productive chernozem (black earth) in the north, with reddish prairie soils of nearly equal fertility in the south. Throughout the region temperatures are severely continental, with bitterly cold winters in the north and scorching summers everywhere.

The western edge of the prairie fades gradually into the shortgrass steppe of the High Plains, the change a function of diminishing rainfall. The eastern edge, however, represents one of the few major discordances between a climatic and biotic boundary in the United States, for the grassland penetrates the eastern forest in a great salient across humid Illinois and Indiana. Many scholars believe this part of the prairie was artificially induced by repeated burning and consequent destruction of the forest margins by Indians.

The Western mountains

Throughout the Cordillera and Intermontane regions, irregular topography shatters the grand bioclimatic pattern into an intricate mosaic of tiny regions that differ drastically according to elevation and exposure. No small- or medium-scale map can accurately record such complexity, and mountainous parts of the West are said, noncommittally, to have a “mountain climate.” Lowlands are usually dry, but increasing elevation brings lower temperature, decreased evaporation, and—if a slope faces prevailing winds—greater precipitation. Soils vary wildly from place to place, but vegetation is fairly predictable. From the desert or steppe of intermontane valleys, a climber typically ascends into parklike savanna, then through an orderly sequence of increasingly humid and boreal forests until, if the range is high enough, one reaches the timberline and Arctic tundra. The very highest peaks are snow-capped, although permanent glaciers rarely occur outside the cool humid highlands of the Pacific Northwest. Peirce F. Lewis

Plant life

The dominant features of the vegetation are indicated by the terms forest, grassland, desert, and alpine tundra.

A coniferous forest of white and red pine, hemlock, spruce, jack pine, and balsam fir extends interruptedly in a narrow strip near the Canadian border from Maine to Minnesota and southward along the Appalachian Mountains. There may be found smaller stands of tamarack, spruce, paper birch, willow, alder, and aspen or poplar. Southward, a transition zone of mixed conifers and deciduous trees gives way to a hardwood forest of broad-leaved trees. This forest, with varying mixtures of maple, oak, ash, locust, linden, sweet gum, walnut, hickory, sycamore, beech, and the more southerly tulip tree, once extended uninterruptedly from New England to Missouri and eastern Texas. Pines are prominent on the Atlantic and Gulf coastal plain and adjacent uplands, often occurring in nearly pure stands called pine barrens. Pitch, longleaf, slash, shortleaf, Virginia, and loblolly pines are commonest. Hickory and various oaks combine to form a significant part of this forest, with magnolia, white cedar, and ash often seen. In the frequent swamps, bald cypress, tupelo, and white cedar predominate. Pines, palmettos, and live oaks are replaced at the southern tip of Florida by the more tropical royal and thatch palms, figs, satinwood, and mangrove.