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
Chautauqua County, New York County, in the southwestern corner of New York State, along the New York-Pennsylvania border, is the westernmost of New York's counties. Chautauqua Lake is located in the center of the county, and Lake Erie is its northern border. Part of the Eastern Continental Divide runs through Chautauqua County. The area that drains into the Conewango Creek (including Chautauqua Lake) eventually empties into the Gulf of Mexico; the rest of the county's watershed empties into Lake Erie and via Lake Ontario and the St. Lawrence Seaway into the North Atlantic Ocean. This divide, known as the Chautauqua Ridge, can be used