
The Fairfax Stone marks the historical and geographical pivot point where Maryland and West Virginia meet, anchoring a landscape shaped by coal extraction and heavy rail. This high-altitude region is dominated by the industrial infrastructure of the Western Maryland railroad, which follows the winding course of the North Branch Potomac River. The settlement pattern reflects the era's mining economy, with numerous locations marked as Mines, Strip Mine, and Tipple sites near communities like Kempton and Wilsonia.
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