The Appalachian Mountains are the oldest range in North America, extending from Canada to the southern United States.
The Appalachian Mountains of eastern North America comprise a north to south-tending range that extends for 1,600 mile (2,500 kilometer) from the Gaspé Peninsula in Atlantic Maritime Canada to northern Alabama in the United States. Uplifted by the collision of continents ancestral to North America and Africa 270 million years ago, the Appalachian Mountains are the oldest mountain range in North America.
The Appalachian Mountains consist of a range of landforms from 4 physiographic provinces. The New England Province consists of rolling coastal lowlands and rugged interior highlands—like the White Mountains of New Hampshire and Maine and the Green Mountains of Vermont—of northern New England and Canada. The Ridge and Valley Province consists of long linear ridges separated by valleys with trellis drainage patterns. The valleys are rich in limestone that dissolves to produce sinkholes and underground caverns, producing karst topography. The Ridge and Valley Province extends from New York to Alabama. The Blue Ridge Mountain Province extends from south-central Pennsylvania to northern Georgia and is a rugged region of high relief with terrain that ranges from narrow ridges with steep slopes to broad mountains. The Appalachian Plateau (known as the Allegheny Plateau in the north and the Cumberland Plateau in the south) is a well-dissected plateau landscape with deeply eroded, dendritic drainage patterns. The Appalachian Plateau extends from New York to Kentucky. The northern Appalachian region from Canada to portions of northern Pennsylvania and New Jersey was glaciated until 4,000 years Before Common Era
Elevation tends to increase from north to south in the Appalachian Mountains. In the north, the plateaus and low rounded mountains of the Gaspé Peninsula (the Shickshock Range) may exceed 4,000 foot (1,200 meter) in elevation. Seven peaks in New Hampshire’s Presidential Range exceed 5,000 foot (1,500 meter). Mount Washington, at 6,288 foot (1,886 meter), is the second-highest Appalachian peak. Elevation decreases somewhat in the central Appalachians, where ridges and peaks—like the Allegheny Mountains in Pennsylvania and Virginia— generally average 3,000 foot (900 meter). Elevations over 5,000 foot (1,500 meter) begin in the Blue Ridge Mountains of southwestern Virginia, like Mt. Rogers at 5,729 foot (1,718 meter) and Pine Mountain at 1,658 m (5,526 ft) and eventually exceed 5,526 foot (1,800 m ) in the Great Smoky Mountains of eastern Tennessee and western North Carolina. The highest peak in the Appalachians (and the eastern United States) is Mt. Mitchell in the Black Mountains of North Carolina at 6,684 foot (2,037 meter).
The climate of the Appalachian Mountains varies with latitude and elevation. Average annual temperature for Canada’s Gaspé Peninsula is approximately 38 degrees F (3 degrees C). Annual precipitation averages 35 inch (89 centimeter) in inland areas but may exceed 58 inch (147 centimeter) along the coast. In the central and southern Appalachians, average annual temperatures may range from 50 to 64 degrees F (10 to 18 degrees C), respectively. Average annual precipitation ranges from 35 inch (89 centimeter) in valleys of the central Appalachians to over 78 inch (198 centimeter) in the high peaks of the southern Appalachians, the highest precipitation in the eastern United States.
The biological diversity of the Appalachian Mountains is rich and diverse, a product of varied climate, topography, and glacial history. In the Gaspé Peninsula and the high peaks of the Presidential Range, the summits are treeless and the vegetation is alpine, dominated by low-stature perennial herbs, shrubs, and graminoids and numerous lichens and mosses. Boreal species such as caribou occur in Canada’s Shickshock Range and historically occurred in northern New England. Northern Appalachian forests include spruce-fir forests dominated by balsam-fir and red spruce and northern hardwood forests dominated by sugar maple, American beech, and yellow birch. Oak forests, dominated by northern red oak and white oak, become more common in the central Appalachians, particularly on drier slopes. The species-rich mixed mesophytic forest, with over 158 tree species, reaches its greatest development in the southern Appalachians. The southern Appalachians are also the world’s center of diversity for the lungless salamanders, harboring 54 species. Many boreal species, like the northern flying squirrel and red spruce, also occur at high elevations in the southern Appalachians, relict survivors of the glaciation that drove them southward.
The Appalachian Mountains are rich in natural resources, particularly minerals and forest products. Coal, both anthracite and bituminous, is abundant in the Appalachians, particularly in the Appalachian Plateau, where oil and gas production is also centered. Limestone is quarried in the karst landscapes of the Ridge and Valley.
CHARLES E. WILLIAMS
CLARION UNIVERSITY OF PENNSYLVANIA