New York–New Jersey Highlands New York–New Jersey Highlands The New York – New Jersey Highlands is a geological formation composed primarily of Precambrian igneous and metamorphic rock running from the Delaware River near Musconetcong Mountain, northeast through the Skylands Region of New Jersey along the Bearfort Ridge and the Ramapo Mountains, Sterling Forest, Harriman and Bear Mountain State Parks in New York, to the Hudson River at Storm King Mountain. The northern region is also known as the Hudson Highlands and the southern as the New Jersey Highlands. A broader definition would extend the region west to Reading, Pennsylvania, and east to the Housatonic
Duane, New York body is Meacham Lake, in the southern part of town. Deer River Flow is located in the northwest. Most of the town is part of the Deer River watershed, a north-flowing tributary of the St. Regis River, which flows to the St. Lawrence River in Canada. The eastern edge of the town is part of the Salmon River watershed, which flows north through Malone and then to the St. Lawrence in Canada. New York State Route 30 is a north-south highway. New York State Route 458 intersects NY-30 at the south town line by Meacham Lake. As of the census