• 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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  • Temporary Suspension of Reference Collection Research

    Due to the park archives and research room/library space move, new public research requests will not be filled until at least June 30th, 2014.

  • 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 »

Environmental Factors

Harpers Ferry watergap

View of the water gap from Bolivar Heights.

NPS photo

Approximately 360 million years ago, when the continent of Africa collided with North America, land comprising the park began to take its current shape. At this time the Appalachian Mountains rose and the Potomac River began cutting through them, forming the water gap we see today between Maryland and LoudounHeights. From numerous places throughout the park, visitors are able to enjoy this and many other scenic vistas Harpers Ferry has to offer.

Large seasonal temperature variations characterize the climate of this region. Highs sometimes reach 100 degrees F in July and August, whereas lows can fall below 15 degrees F in January. On average though, annual high and low temperatures here are 63 and 40 degrees F respectively. The average annual precipitation from thunderstorms, rainshowers, Atlantic coastal storms, and snow combine to equal 38 inches in the park. The month of June typically receives the most precipitation, whereas February receives the least.

Floods reaching heights of 20 feet or more occur about every 5 to 10 years. When floods do occur, they tend to be fairly deep since there is not much room for water to spread out once it overflows its banks. Flooding in the park is caused by many factors including rugged topography, changes in vegetation, and meandering stream courses that cause large volumes of water to slow down in their channels and consequently overflow their banks. Another main flood-causing factor is heavy precipitation that produces rapid runoff, especially during the early months of the year.

Natural sources of water hardness and pollution in
Harpers Ferry are calcium and magnesium. These elements are very common due to the large quantities of limestone in this area. Yet the presence of limestone also helps to buffer river waters against acidic conditions. Sodium, potassium, iron, and manganese are also present in the Potomac and ShenandoahRivers. If large enough amounts are present, iron and manganese can be indicators of acidic water.

Both domestic and industrial wastes are sources of water pollution in the
Harpers Ferry area. Predominantly agricultural practices, including the use of fertilizers and pesticides, and heavy rainfall events have contributed to the contamination of the streams and rivers. The amount of forest cover, land use, and waste from industries each affect sedimentation. Most of the suspended materials in the Potomac and ShenandoahRivers are the products of soil and channel erosion, while some are industrial wastes.

Did You Know?

Intake arches channeled water to power industry on Virginius Island.

Virginius Island was a thriving 19th-century industrial town along the Shenandoah River. By 1859, there were about three dozen buildings there.