Inwood Hill Park
Inwood Hill Park - Salt Marshes in New York City Parks
Salt marshes play a critical role in the support of human life, acting as natural filtration systems by trapping pollutants that would otherwise contaminate our bays and oceans. Salt marshes have the ability to absorb fertilizers, improve water quality, and reduce erosion. They are also among the richest wildlife habitats.
Inwood Hill Park, a 196-acre oasis at the northern tip of Manhattan, features the last remnant of the tidal marshes that once surrounded Manhattan Island. The marsh receives a mixture of freshwater flowing from the upper Hudson River and saltwater from the ocean’s tides. The mix of salt and fresh waters, called brackish water, has created an environment unique in the city.
When the last of the glaciers melted 7,000 years ago, the oceans rose to their present levels. Sediments washed from the land were deposited offshore in narrow sandy strips, forming long islands parallel to the shoreline. These barrier beaches received the pounding surf on their ocean side, but had calm, protected bays behind their landward shores. While the waters were calm enough for vegetation to take root, the presence of saltwater made survival difficult. One species, however, saltmarsh cordgrass (Spartina alterniflora), was able to colonize the flat expanses of sand and silt, which were covered twice a day by the ocean’s tides. Today, the grass is still found along the Atlantic coast.
As this specialized grass spreads, its stems trap floating debris. Sediments and particles of decaying matter slowly build up, forming nutrient-rich mud. This mud, called detritus, supports life on the marsh. It is the basis of a complex food web in which energy is passed from one organism to another. The fiddler crab (Uca pugnax) and ribbed mussel (Geukensia demissa) have developed a mutually beneficial relationship with the cordgrass. While the crabs and mussels benefit from feeding on decaying matter trapped within cordgrass roots, cordgrass gains from the fiddler’s burrowing, which aerates the soil, and the mussel’s excretion, which provides necessary nitrogen.
At the end of each season, the cordgrass dies, creating a spongy peat. Each year’s peat layer raises the surface of the marsh, enabling it to colonize new territory. A variety of plants with less salt tolerance can colonize the peat, as it is out of the range of most of the high tides. This causes the formation of two separate plant communities, the intertidal marsh and the salt meadow. A third type of salt marsh community is the mudflat. Each of these communities has its own distinctive vegetation, insects, fish, birds, and mammals that have adapted to survive in a saltwater environment. While salt marshes do not have a very wide variety of species, the volume of life present is remarkable.
In addition to saltmarsh cordgrass, Inwood Hill Park’s low marsh also contains big saltwater cordgrass (Spartina cynosuroides) and two species of bulrush. Between the low marsh and the park path are a number of marsh plants rare elsewhere in the city, including water hemp (Acnida cannabinus) and salt marsh bulrush (Scirpus robustus). Marsh elder (Iva frutescens), swamp rose-mallow (Hibiscus palustris), and groundsel bush (Baccharis halimifolia) also grow here. A broad, expansive mudflat runs from the marsh to the channel of the Harlem River Ship Canal. Great blue herons (Ardea herodias) frequent the flat in the winter. Great (Casmerodius albus) and snowy (Egretta thula) egrets are common visitors from spring through fall. You can often hear the chattering of a belted kingfisher (Ceryle alcyon) as it flies overhead, hovers, and then drops into the water, emerging with a wriggling fish in its oversized bill.
Since industrialization, human activity has destroyed many marshes. Where marshes are disturbed, common reed (Phragmites australis) often grows in place of cordgrass. Since reeds do not decompose into as nutritious a substance as cordgrass, a reed marsh does not contribute as much to coastal ecosystems as a cordgrass marsh. In the last 200 years, humans have also filled over 80 percent of the city’s original salt marshes for construction. While recent conservation efforts have improved the condition of marshes, this valuable ecosystem continues to disappear from the City at an alarming rate.
Directions to Inwood Hill Park
Know Before You Go
There are currently 2 service interruptions affecting access within this park.
Inwood Hill Nature Center
Due to the effects of Hurricane Sandy, this facility is closed until further notice.
Inwood Hill Park
Reconstruction work at the Little League Baseball field will correct existing uneven ball field elevations and will provide a sod infield and outfield. A Scorekeeper’s Box will be installed, player dugout areas will be enlarged and will received new concrete floors, and a clay ‘warning track’ will be installed along the perimeter of the outfield fence to assist playing conditions and maintenance mowing in this area. New bases, clay storage boxes, skinned playing areas and painting and reconstruction of perimeter fencing and backstop areas will also be provided. A metal container will provide secure storage for playing and maintenance equipment with an enclosed player’s warm-up area nearby. New ADA accessible bleachers and an elevated turf viewing area are also being installed to provide seating and viewing areas for the playing field.
Anticipated Completion: Summer 2014
Inwood Hill Park Weather
- This Weekend In Parks: Halloween Edition
- Autumnal Equinox: Parks Foliage Guide
- PARKS HOSTS DRUMS ALONG THE HUDSON AT INWOOD HILL PARK
- Barbecuing Areas
- Baseball Fields
- Basketball Courts
- Dog-friendly Areas
- Fitness Equipment
- Handball Courts
- Hiking Trails
- Kayak/Canoe Launch Sites
- Nature Centers
- Roller Hockey
- Soccer Fields
- Spray Showers
- Tennis Courts
Know when to go:
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Inwood Hill Park