Mauch Chunk Ridge (on older USGS Maps) or Mauch Chunk Mountain is a historically important barrier ridgeline paralleling Pisgah Ridge in the ridge and valley formation of the Anthracite coal bearing Appalachian formations of Northeastern Pennsylvania. The northslopes of the long series of worn peaks feed the minor tributary Mauch Chunk Creek's mouth which opens out easterly into the Lehigh River, and where from ca. 1792 on, enabled the earliest mines of the southern Anthracite region at Summit Hill, Pennsylvania to be conveyed to the water transport available on the Lehigh River at what is now Packerton, Pennsylvania. A number of early pack mule routes traveled in part along the north faces of the mountain's long ridgeline (12.5 miles (20.1 km)) from Summit Hill and points west.
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