Geography
The Shawangunk Ridge is the northern end of a long ridge within the Appalachian Mountains that begins in Virginia, where it is called North Mountain, continues through Pennsylvania as Blue Mountain, becomes known as the Kittatinny Mountains after it crosses the Delaware Water Gap into New Jersey and becomes the Shawangunks at the New York state line. These mountains mark the western and northern edge of the Great Appalachian Valley.
The ridge is widest (7.5 miles/12 kilometers) near the northern end, narrow in the middle (1.25 miles/under 2 kilometers) with a maximum elevation of 2,289 feet (698 m) near Lake Maratanza on the Shawangunk Ridge. The Ridge rises above a broad, high plain which stretches to the Hudson River to the east. On the west the low foot-hills of the Appalachian Mountains mingle with a low flat made by the Rondout Creek and Sandburgh Creek, the Basher Kill and various small kills as well as the Neversink River and Delaware River at the southern end. These adjacent valleys are underlain by relatively weak sedimentary rock (e.g., sandstone, shale, limestone).
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