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.
River Road Closure
Starting on Monday, September 8, River Road will be closed from Park Headquarters to Smithfield Beach while contractors complete pavement repairs. Access to Smithfield Beach will still be possible. More »
Dingmans Falls Area and Road Closed
Dingmans Falls Visitor Center, the boardwalk trail to the falls, and the access road will be closed through September as repairs to the road are made. We anticipate the area reopening in October.
The Water Gap
Resort Point Overlook, Rt. 611 PA GPS 41.978171 -74.138205
Kittatinny Point NJ, off Interstate 80 GPS 40.970188 -75.128242
The Delaware Water Gap is bounded by Mt. Minsi in Pennsylvania and Mt. Tammany in New Jersey. Once touted as a scenic Wonder of the World, it is an impressive site when motoring through on Interstate 80 or viewed from the overlooks along Rt. 611 on the Pennsylvania side.
For a basic explanation, see How the Gap Formed.
For detailed geology, see Advanced Geology Stops on Mt. Tammany.
What's a Water Gap? is a Fun Page for Kids. (pdf file)
Before the Gap formed. Mt. Minsi and Mt. Tammany formed one continuous ridge -- the Kittatinny Ridge, along which the
The Shawangunk Formation is the older of the two and forms the bulk of the mountain. It is composed of three layers -- or members. The top and bottom members are largely sandstone, with little shale. The middle layer has a mix of weaker shales and sandstones, and this is where trees grow.
The Bloomsburg Redbeds are more recent and cover the top of the mountains. They consist of layer upon layer of sand and mud that later became stones and shales of the formation.
Although they now tilt upwards at a precarious angle, the Shawangunk and Bloomsburg Formations were laid down horizontally. When the African Plate collided with the North American Plate 250 million years ago, the force of the collision bent the rock layers into folds, forming the Appalachian Mountain chain. Erosion has removed the rock from what is now the Water Gap.
The Work of Water
There are several explanations of how the Water Gap formed, but essentially, erosion has removed the rock from what is now the Water Gap
Headwater Erosion (and stream-capturing) explains that the folding of the rocks layers resulted in a weakened spot in the ridge. Creeks flowing down the mountain eventually slowly eroded their way back through the ridge until they cut the whole way through and "captured" a river on the other side of the ridge. (See How the Gap Formed.)
Superposition explains that creeks eroded an ever deepening channel; the folding or weakening of the rock is not involved.
Ice Comes and Goes
Glaciers have come to this valley and melted away several times over millions of years, the last (Wisconsin) glaciation having melted away 20,000 years ago.
While glaciers likely carried away rock from the slopes, the Water Gap was already by the time that the glaciers advanced. There are glacial erratics (boulders) and till deposits in the valleys and on the mountains, and glacial striae (scratches) on the walls of the Gap itself. (See Advanced Geology Stops on Mt. Tammanyfor more detailed information.)
A Work in Progress
Though in the human frame of time, the Gap looks "finished," erosion is ongoing. Even if you don't know one rock from another, or one geologic era from another, take a moment to ponder the power of water over immense periods of time -- water is still forming the Gap, drop by drop, as you watch the river flow by today.
Did You Know?
... that hemlock groves in Delaware Water Gap National Recreation Area are threatened by a non-native insect, the hemlock woolly adelgid. Hemlocks provide shade for spectacular rhodondenron, for trout streams, and for native wildflowers. As hemlocks weaken and die, they are cut down for your safety. More...