Geography
The region's geologic setting and landscape history make the Potomac Highlands one of the most scenic areas within the central Appalachian Mountains. The eastern part of the region is within the Ridge and Valley physiographic province, where long, steep-sided mountain ridges alternate with parallel broad, flat valleys. Water gaps, where rivers or streams have cut through the ridges, are important not only for their dramatic scenery, but also for their utility as easy crossings of these otherwise formidable mountains for roads, railroads, and telephone and telegraph lines. The western portion of the Potomac Highlands is within the Allegheny Plateau, with the Allegheny Front's prominent escarpment providing the boundary between these two areas.
While much of the land in the Potomac Highlands is privately owned, large portions of the area are within the Monongahela National Forest, the George Washington National Forest, or various other kinds of parks, preserves, or other managed wild areas. A group of sites within the Allegheny Highlands has been proposed for inclusion as a new unit within the U.S. National Park System.
The Fairfax Stone, marking the source of the Potomac River, is along the north edge of the Potomac Highlands, just south of the southern tip of western Maryland.
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