Everything about Raccoon Creek New Jersey totally explained
Raccoon Creek (also called the
Raccoon River) is a
tributary of the
Delaware River in southern
New Jersey in the
United States.
It rises to the west of
Glassboro, and flows east, meeting
Cartwheel Brook at Wrights Mill. Just below, it's impounded to form
Gilman Lake. It turns to the north and is again dammed to form
Ewan Lake.
Clems Run and
Miery Run empty into the stream, which is steeply banked on the east side. It flows through
Mullica Hill (formerly the head of navigation), where it's dammed to form
Mullica Hill Pond, and turns east again, flowing through a wide but steep valley. The
South Branch (of the creek) joins it about 1.5 mi (2.4 km) east of the town. Flowing along the north side of
Swedesboro, the creek becomes tidal and passes under the Locke Avenue moveable bridge, marking more recent limits of navigation. (The bridge was last opened in the 1960s.) The creek turns north again and meanders through the marshlands, passing under the (fixed)
Interstate 295 bridge and running along the west side of the
Pureland Industrial Complex, one of the largest
industrial parks in the United States. A tangle of marshy channels leads to the west side of
Bridgeport, where the creek passes under moveable spans of the
Conrail Penns Grove Secondary and
U.S. Route 130. It empties into the Delaware River just south of the
Commodore Barry Bridge where it crosses
Raccoon Island (now connected to the mainland by fill).
Swedish settlers of the 17th century came upstream along Raccoon Creek to settle the communities of Bridgeport and Swedesboro.
Tributaries
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