• Fulmer Falls at George W. Childs Park

    Delaware Water Gap

    National Recreation Area NJ,PA

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  • Hornbecks Creek Trail Partial Closure

    The trail is closed between the first and second waterfall; a portion of the trail has sloughed off, causing a hazardous condition. The first waterfall is accessible from the 209 trailhead and the second waterfall is accessible from Emory Road.

  • Dingmans Falls Area and Road Closed

    Dingmans Falls Visitor Center, the boardwalk trail to the falls, and the access road are closed through while repairs to the road are made. We anticipate the area reopening in mid-November.

Waterfalls

Raymondskill Falls

Raymondskill Falls

The ravines carved between the ridge tops are partly the result of glaciers moving across the landscape, deepening and widening the path opened up by the creek. When each glacier retreated, the creeks then tumbled over ledges of rock, forming waterfalls.

Where the rock at the top of the waterfall is more resistant to weathering than the rock below the falls, the waterfall is steep. Where the rock at the top of a waterfall is not much harder than the rock at the bottom, more gradual waterfalls can form.

Natural springs, swamp runs, and outlets of natural and artificial lakes drain the mountain sides along the river valley and form part of the Delaware Watershed. The drops of water that you see hurtling over these waterfalls will reach the Delaware River, and, in time, flow into the Atlantic Ocean.

 

Did You Know?

Sketch of a dam with forests on the river banks.

... that the reservoir of the proposed Tocks Island Dam would have inundated 30 miles of the Delaware River and 30,000 acres of its river valley (now part of Delaware Water Gap National Recreation Area.) The defeat of the dam was an early victory of the environmental movement in this country. More...