• Sun beginning to set at Harpers Ferry, as seen from Maryland Heights. Photo by NPS Volunteer Buddy Secor.

    Harpers Ferry

    National Historical Park WV,VA,MD

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  • Change in Park Hours

    The park is currently open daily from 9 a.m. to 5 p.m. with the last shuttle bus departing Lower Town at 6:45 p.m. More »

  • Murphy Farm Closure Sept 2-4, 2014

    The Murphy Farm will be closed to public access Sept. 2-4, 2014 to allow application of fertilizer to the hayfields. For further information please click on the "More" link or contact the park’s Resource Management Specialist at 304-535-6038. More »

Geologic Activity

watergap from the point

View of the water gap between Maryland and Loudoun Heights from the Point.

NPS photo

The park is located in the Blue RidgeMountain section of the Appalachian Mountain Range. The geological history of the park begins 550 million years ago when this area was covered by a shallow sea. Deposition of sediments such as sand, clay, and limestone, began at this time. When the continent of Africa collided with the continent of North America about 360 million years ago, the Appalachian Mountains rose. Normal compaction along with the heat and pressure generated by this collision changed these sediments into the quartzite (sand), phyllite (clay), and limestone (fossil shells and mud) rock types found in the mountains here today.

As the
Appalachians rose, the sea evaporated and the Potomac River cut through the rock, eventually forming the water gap between MarylandHeights and LoudounHeights. This is considered by many to be the most prominent geological feature in the park. While the Potomac River was cutting through the gap, the Appalachians, which were once taller than the Rocky Mountains are today, were being worn down by rock, wind, rain, and ice. After this erosion, only the roots of the Appalachian Mountains were left. Water running off of the mountains began collecting at their base, forming what is now the ShenandoahRiver. This river flows along the base of the Blue Ridge Mountains until reaching Harpers Ferry, where it joins with the Potomac River and flows east towards the Chesapeake Bay.

Did You Know?

Redman, pictured here, conducts his orchestra.  Photo courtesy of Todd Bolton.

Don Redman, "the little giant of Jazz," graduated from Storer College in 1920. Until his death in 1964, Redman continued to have a profound influence on the evolution, direction and development of this uniquely American art form.