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Photographer's Note

Great Falls of the Potomac
Many people consider the Great Falls of the Potomac to be the most spectacular natural landmark in the Washington D.C. area. Here, the Potomac River builds up speed and force as it falls over a series of steep, jagged rocks. The falls consist of cascading rapids and several 20 foot waterfalls, with a total 76 foot drop in elevation over a distance of less than a mile.

The geologic history of the falls is an interesting one. After the last ice age, the ocean levels dropped, forcing the Potomac River to carve deeper in its path to the sea. The overlying rock was eroded away exposing a much harder, resistant rock formation. This hard layer is principally made up of metamorphic and igneous rock, and may be seen throughout the park.

Great Falls Park is located along the boundary between the Piedmont Plateau and the Atlantic Coastal Plain, in an area known as the fall zone. Joint fault plains, which are natural fissures in the rock substrata where shifting has occurred, exist in many places in the Piedmont Formation between Chain Bridge and the Great Falls. These areas of faulting have loosened the rock, forming areas of weakness. The force of the Potomac has eroded along these areas, changing the river's course to its current position.

Evidence of the ancient river beds can be seen in well-rounded boulders, smoothed surfaces and grooves, and beautifully formed potholes. The metamorphic rocks provide jagged rocky surfaces and high-walled cliffs, stark and pristine against the crashing waters of the Potomac at the falls and along Mather Gorge.

For another view of the falls see Great Falls Park.

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Additional Photos by Betty Jones (BWJ) Gold Star Critiquer/Gold Note Writer [C: 473 W: 0 N: 919] (3094)
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