Brau Kettle

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The Brau Kettle is a geological feature known as a karst that is located along the Wallpack Ridge in the Delaware Water Gap National Recreation Area in Sandyston Township, New Jersey. Its name derives from the Dutch for "brewing kettle" or "boiling kettle" which describes how water suddenly bubbles up from the ground. [1] This site is referenced in early French Jesuit and Dutch colonial manuscripts as a landmark near which colonial traders exchanged goods with the Munsee and other local Native American tribes. According to the New Jersey Geological Survey, the feature looks like a sinkhole in dry times during the year. It is known to flow at random, after periods of precipitation, and is thought to be fed by a sinking stream that vanishes in the forest roughly 1,800 feet away. [2]

Karst Topography formed from the dissolution of soluble rocks

Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and be totally missing above ground.

Wallpack Ridge


Wallpack Ridge is a mountain located in the Ridge and Valley Appalachians physiographic province in Sussex County in northwestern New Jersey. Oriented northeast to southwest, Wallpack Ridge spans 25 miles (40 km) from Montague Township south of Port Jervis, New York to the Walpack Bend in the Delaware River near Flatbrookville in Walpack Township. It is a narrow ridge ranging between 0.67 miles (1.08 km) to 1.7 miles (2.7 km) in width, and its highest elevation reaches 928 feet (283 m) above sea level. The ridge separates the Wallpack Valley from the valley of the Delaware River, and contains the watershed of the Flat Brook and its main tributaries Big Flat Brook and Little Flat Brook.

Delaware Water Gap National Recreation Area protected area

The Delaware Water Gap National Recreation Area is a 70,000 acres (28,000 ha) protected area designated a National Recreation Area administered by the U.S. Department of the Interior's National Park Service. It is located 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, entirely within the National Recreation Area, 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.

See also

New Jersey is a very geologically and geographically diverse region in the United States' Middle Atlantic region, offering variety from the Appalachian Mountains and the Highlands in the state's northwest, to the Atlantic Coastal Plain region that encompasses both the Pine Barrens and the Jersey Shore. The state's geological features have impacted the course of settlement, development, commerce and industry over the past four centuries.

Sussex County, New Jersey County in the United States

Sussex County is the northernmost county in the State of New Jersey. Its county seat is Newton. It is part of the New York Metropolitan Area and is part of the state's Skylands Region, a term promoted by the New Jersey Commerce, Economic Growth, & Tourism Commission to encourage tourism. As of the 2017 Census estimate, the county's population was 141,682, making it the 17th-most populous of the state's 21 counties, a 5.1% decrease from the 149,265 enumerated in the 2010 United States Census, in turn an increase of 5,099 (3.5%) over the 144,166 persons enumerated in the 2000 Census. Based on 2010 Census data, Vernon Township was the county's largest in both population and area, with a population of 23,943 and covering an area of 70.59 square miles (182.8 km2).

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Flat Brook

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Wallpack Valley

Wallpack Valley is a valley located in Sussex County in northwestern New Jersey formed by Wallpack Ridge on the west, and Kittatinny Mountain on the east. Wallpack Ridge separates the Wallpack Valley from the valley of the Delaware River, and contains the watershed of the Flat Brook and its main tributaries Big Flat Brook and Little Flat Brook. It is a narrow valley, roughly 25 miles (40 km) in length running from Montague Township south of Port Jervis, New York to the Walpack Bend in the Delaware River near Flatbrookville in Walpack Township where the Flat Brook enters the Delaware at 300 feet above sea level.

References

  1. Dalton, Richard F. Bulletin 70: Caves of New Jersey (Trenton: New Jersey Geological Survey: n.d.), 6.
  2. Unearthing New Jersey (Newsletter) Vol. 2 No. 1 Winter 2006. (Trenton: New Jersey Geological Survey, Department of Environmental Protection, 2006).

Coordinates: 41°08′24″N74°54′47″W / 41.140°N 74.913°W / 41.140; -74.913

Geographic coordinate system Coordinate system

A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.