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Delaware Water Gap National Recreation Area facts for kids

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Delaware Water Gap National Recreation Area
Silver Thread Falls, the smaller waterfall at the Dingman's Falls site is located near Dingman's Ferry, Pennsylvania.
Delaware Water Gap National Recreation Area is located in New Jersey
Delaware Water Gap National Recreation Area
Delaware Water Gap National Recreation Area
Location in New Jersey
Delaware Water Gap National Recreation Area is located in the United States
Delaware Water Gap National Recreation Area
Delaware Water Gap National Recreation Area
Location in the United States
Location New Jersey & Pennsylvania, United States
Nearest city Stroudsburg, Pennsylvania,
Port Jervis, New York
Area 66,741 acres (270.09 km2)
Established September 1, 1965 (1965-September-01)
Visitors 4,986,700 (in 2011)
Governing body National Park Service
Website Delaware Water Gap National Recreation Area

The Delaware Water Gap National Recreation Area is a 70,000 acres (28,000 ha) national recreation area along the middle section of the Delaware River in New Jersey and Pennsylvania stretching from the Delaware Water Gap northward in New Jersey to the state line near Port Jervis, New York, and in Pennsylvania to the outskirts of Milford. A 40-mile (64 km) section of the Delaware River within it has been granted protected status as the Middle Delaware National Scenic River under the National Wild and Scenic Rivers System and is also administered by the National Park Service. This section of the river is the core of the historical Minisink region.


The recreation area includes parts of Sussex and Warren counties in New Jersey, and Monroe, Northampton, and Pike counties in Pennsylvania. The Appalachian Trail runs along much of the eastern boundary of the park and is maintained and updated by the New York - New Jersey Trail Conference. The park offers historical and cultural sites including the Minisink Archaeological Site, Millbrook Village, and the arts center in Peter's Valley and rural scenery approximately an hour's drive from New York City. The park has significant Native American archaeological sites. In addition, a number of structures remain from early Dutch settlement during the colonial period. Outdoor recreational activities include canoeing, hiking, camping, swimming, cycling, cross-country skiing, horseback riding, and picnicking. Fishing and hunting are permitted in season with valid state licenses.

Geology and geography



Delaware Water Gap cliffs
Fog surrounds cliffs looming over the Delaware River whose valley is the core of the historic Minisink region

The Minisink (or more recently "Minisink Valley") is a loosely defined geographic region of the Upper Delaware River valley in northwestern New Jersey (Sussex and Warren counties), northeastern Pennsylvania (Pike and Monroe counties) and New York (Orange and Sullivan counties).

The name was derived by Dutch colonists from the Munsee name for the area, as bands of their people took names after geographic places which they inhabited as territory throughout the mid-Atlantic area. Originally inhabited by Munsee, the northern branch of the Lenape or Delaware Indians, the area's first European settlers arrived in the late seventeenth and early eighteenth centuries and were Dutch and French Huguenot families from colonial New York's Hudson River Valley. The term "Minisink" is not used often today. It is preserved because of its historical relevance concerning the early European settlement of the region during the American colonial period and as an artifact of the early "first contact" between Native Americans and early European explorers, traders and missionaries in the seventeenth century.

Much of the historical Minisink region has been incorporated into the Delaware Water Gap National Recreation Area after defeat of a controversial dam project proposed to be built by U.S. Army Corps of Engineers on the Delaware River near Tocks Island.

Tocks Island Dam project

The Delaware River is prone to floods—some resulting from seasonal snow melt or rain run-off from heavy rainstorms. However, record flooding occurred in August 1955 in the aftermath of two separate hurricanes (Hurricane Connie and Hurricane Diane) that passed over the area within the span of one week. On 19 August 1955, the river gauge at Riegelsville, Pennsylvania recorded that the Delaware River reached a crest of 38.85 feet, or 16.85 feet above flood stage.

A project to dam the river near Tocks Island was in the works before the 1955 floods. But several deaths and severe damages resulting from these floods brought the issue of flood control to the national level. The U.S. Army Corps of Engineers proposed the construction of the dam, which would have created a 37-mile (60-km) long lake between Pennsylvania and New Jersey, with depths of up to 140 feet. The area around the lake would be established as the Tocks Island National Recreation Area under the oversight of the National Park Service, to offer recreation activities such as hunting, hiking, fishing, and boating. In addition to flood control and recreation, the dam would be used to generate hydroelectric power and provide a clean water supply to New York City and Philadelphia.

Starting in 1960, the present-day area of the Recreation Area was acquired for the Army Corps of Engineers through eminent domain. Approximately 15,000 people were displaced by the condemnation of personal property along the Delaware River and the surrounding area. An estimated 3,000 to 5,000 dwellings and outbuildings were demolished in preparation for the dam project and subsequent flooding of the valley. This included many irreplaceable historical sites and structures connected with the valley's Native American and colonial heritage.

Establishment of the recreation area

The Delaware Water Gap National Recreation Area was originally authorized by Congress in 1965 to be a narrow area surrounding the proposed reservoir, in part to make the project more cost-effective.

The dam project was embroiled in controversy and engendered strong opposition by environmental groups and embittered displaced residents. Because of considerable opposition from environmental activists, the unavailability of government funding for the dam, and a geological assessment revealing the dam would be located near active fault lines, the federal government decided to abandon the dam project in 1978. The lands acquired were then transferred to the National Park Service, and the holdings were added to the Delaware Water Gap National Recreation Area.


Notable sites within the Park

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