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The Hudson Canyon is a submarine canyon that begins from the shallow outlet of the estuary at the mouth of the Hudson River. It extends out over 640 km (400 mi) seaward across the continental shelf finally connecting to the deep ocean basin at a depth of 3–4 km (1.9–2.5 mi) below sea level .
A 2016 U.S. Army Corps of Engineers map showing New York–New Jersey Harbor Estuary's drainage divide and drainage basin Harrisse/LOC copy of the Manatus Map of 1639 An 1866 map of New York–New Jersey Harbor Estuary A 2011 NASA image of New York–New Jersey Harbor Estuary Population density and elevation above sea level in the New York City metropolitan area as of 2010 An aerial view of ...
A colorized depiction of the Hudson Canyon and the New York Bight area. The New York/New Jersey Bight is the geological identification applied to a roughly triangular indentation, regarded as a bight, along the Atlantic coast of the United States that extends northeasterly from Cape May Inlet in New Jersey to Montauk Point on the eastern tip of Long Island.
A submarine canyon is a steep-sided valley cut into the seabed of the continental slope, sometimes extending well onto the continental shelf, having nearly vertical walls, and occasionally having canyon wall heights of up to 5 km (3 mi), from canyon floor to canyon rim, as with the Great Bahama Canyon. [1]
The main shipping channel through Lower New York Bay is the Ambrose Channel, 2,000 feet (600 meters) wide and dredged to a depth of 40 feet (12 meters). The channel is navigable by ships with up to a 37-foot draft at low tide. [1]
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The Northeast Canyons and Seamounts Marine National Monument is located within the New England and mid-Atlantic regions, 130 miles southeast of Cape Cod. [1] It comprises a total area of 4,913 square miles, [1] and protects four underwater seamounts (Bear, Mytilus, Physalia, and Retriever Seamounts) and three submarine canyons in the edge of the continental shelf (Oceanographer, Lydonia, and ...