West Virginia Geography

West Virginia is bordered by Pennsylvania to the north; by Ohio to the north and west; by Kentucky to the west; by Maryland to the north and east; and by Virginia to the east and south. The Ohio and Potomac rivers form parts of the boundaries.

West Virginia is the only state in the nation located entirely within the Appalachian Mountain range, and in which all areas are mountainous; for this reason it is nicknamed The Mountain State. About 75% of the state is within the Cumberland Plateau and Allegheny Plateau regions. Though the relief is not high, the plateau region is extremely rugged in most areas.

On the eastern state line with Virginia, high peaks in the Monongahela National Forest region give rise to an island of colder climate and ecosystems similar to those of northern New England and eastern Canada. The highest point in the state is atop Spruce Knob, which at 4,863 feet (1,482 m)[1] is covered in a boreal forest of dense spruce trees at altitudes above 4,000 feet (1,220 m). Spruce Knob lies within the Monongahela National Forest and is a part of the Spruce Knob-Seneca Rocks National Recreation Area. [2] A total of six wilderness areas can also be found within the forest. Outside the forest to the south, the New River Gorge is a 1,000 foot (304 m) deep canyon carved by the New River. The National Park Service manages a portion of the gorge and river that has been designated as the New River Gorge National River, one of only 15 rivers in the U.S. with this level of protection.

Other areas under protection and management include:

The native vegetation for most of the state was originally mixed hardwood forest of oak, chestnut, maple, beech, and white pine, with willow and American sycamore along the state's waterways. Many of the areas are rich in biodiversity and scenic beauty, a fact that is appreciated by native West Virginians, who refer to their home as Almost Heaven. Ecologically, most of West Virginia falls into the Appalachian mixed mesophytic forests ecoregion.

The underlying rock strata are sandstones, shales, bituminous coal beds, and limestones laid down in a near shore environment from sediments derived from mountains to the east, in a shallow inland sea on the west. Some beds illustrate a coastal swamp environment, some river delta, some shallow water. Sea level rose and fell many times during the Mississippian and Pennsylvanian eras, giving a variety of rock strata. The Appalachian Mountains are some of the oldest on earth, having formed over 300 million years ago.

Shaded relief map of the Cumberland Plateau and Ridge-and-valley Appalachians.

The summit of Spruce Knob is often covered in clouds.