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| Crosswicks Creek | |
|---|---|
View upstream from I-295 at the mouth of the Crosswicks Creek on the border of Bordentown and Hamilton Township
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| Location | |
| Country | United States |
| State | New Jersey |
| Region | Burlington County Mercer County Monmouth County Ocean County |
| Physical characteristics | |
| Source | |
| • location | Joint Base McGuire–Dix–Lakehurst |
| • coordinates | 40°03′07″N 74°32′41″W / 40.05194°N 74.54472°W / 40.05194; -74.54472[1] |
| Mouth | Delaware River |
• location | Bordentown |
• coordinates | 40°08′57″N 74°43′12″W / 40.14917°N 74.72000°W / 40.14917; -74.72000[1] |
| Basin features | |
| River system | Delaware River |
Crosswicks Creek is a 25.3-mile-long (40.7 km)[2] tributary of the Delaware RiverinBurlington, Mercer, Monmouth and Ocean Counties in central and southern New Jersey.[3]
Crosswicks Creek watershed encompasses portions of four counties in south-central New Jersey. Its headwaters flow from the Fort Dix and McGuire Air Force Base Military Reserves in a northwesterly direction and then turn sharply south where it meets the Delaware RiveratBordentown Township. With jets roaring overhead and shells being test fired, the Crosswicks Creek watershed has a set of unique concerns and is the focus of many protection and restoration activities.
In the mid 1990s, the New Jersey Department of Transportation opened the missing segment of I-295, which has had a significantly impact on the mouth of the Crosswicks. This area, known as the Hamilton Marsh, has had significant portions filled in to make way for the freeway. During construction, new wetlands were also created, but at the expense of established woodlands. There may also be interference with wildlife movement patterns due to the large freeway's presence in the marsh. In light of these activities, there is support for the development of a Hamilton Marsh Greenway.
Although most of the creek does not yield particularly abundant deposits of fossils, fossils from the Pleistocene and Cretaceous eras have been found. There exist patches of particularly fossiliferous deposits among mostly non-fossiliferous deposits throughout the creek's path.[4][5]
40°10′44″N 74°41′46″W / 40.178996°N 74.696174°W / 40.178996; -74.696174
