The Potomac River's journey is a study in directional nuance. Its overall course is southward—from the Allegheny Mountains of West Virginia to the Chesapeake Bay—but the path it takes is anything but a straight line.
The Potomac begins at Fairfax Stone, West Virginia (3,140 ft elevation), where the North and South Branches converge. From there:
The Potomac's northward-to-southeast-to-northeast arc reflects the structural grain of the Appalachians—it follows the Great Valley, then cuts across the Fall Line (where hard bedrock meets coastal plain), then widens into a drowned river valley (ria) as sea level rose after the last glaciation.
"The Nation's River" flows past the capital, Mount Vernon, and countless Civil War sites. It supplies drinking water to 5 million people (D.C. metro area), supports recreation (fishing, paddling, the annual Nation's Triathlon), and remains a contested resource—nutrient pollution, sediment, and interstate water allocation (Maryland vs. Virginia vs. West Virginia) are managed by the Interstate Commission on the Potomac River Basin.
So: the Potomac flows south in the broad sense—but its meanders tell the geologic and human story of the mid-Atlantic.