• 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.

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?

A ranger in the uniform of the French and Indian War.

... that in the 1750s, the northwest border of New Jersey (now Delaware Water Gap National Recreation Area) was a frontier of the English colonies. In the French & Indian (Seven Years) War, a string of forts protected these settlements. The sites of seven of these outposts are in the park. More...