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 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 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.
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.
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 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).
The Delaware River is a major river on the Atlantic coast of the United States. It drains an area of 14,119 square miles (36,570 km2) in five U.S. states: Delaware, Maryland, New Jersey, New York, Pennsylvania. Rising in two branches in New York state's Catskill Mountains, the river flows 419 miles (674 km) into Delaware Bay where its waters enter the Atlantic Ocean near Cape May in New Jersey and Cape Henlopen in Delaware. Not including Delaware Bay, the river's length including its two branches is 388 miles (624 km). The Delaware River is one of nineteen "Great Waters" recognized by the America's Great Waters Coalition.
West Jersey and East Jersey were two distinct parts of the Province of New Jersey. The political division existed for 28 years, between 1674 and 1702. Determination of an exact location for a border between West Jersey and East Jersey was often a matter of dispute.
The Delaware and Raritan Canal is a canal in central New Jersey, United States, built in the 1830s, that served to connect the Delaware River to the Raritan River. It was an efficient and reliable means of transportation of freight between Philadelphia and New York City, especially coal from the anthracite fields in eastern Pennsylvania. The canal allowed shippers to cut many miles off the existing route from the Pennsylvania coal fields, down the Delaware, around Cape May, and up along the Atlantic Ocean coast to New York City.
A 1950s proposal to construct a dam near Tocks Island across the Delaware River was met with considerable controversy and protest. Tocks Island is located in the Delaware River a short distance north from the Delaware Water Gap. In order to control damaging flooding and provide clean water to supply New York City and Philadelphia, the U.S. Army Corps of Engineers proposed building a dam. When completed, the Tocks Island Dam would have created a 37-mile (60-km) long lake between Pennsylvania and New Jersey, with depths of up to 140 feet. This lake and the land surrounding were to be organized as the Tocks Island National Recreation Area. Although the dam was never built, 72,000 acres (291 km²) of land were acquired by condemnation and eminent domain. This incited environmental protesters and embittered local residents displaced by the project's preparations when their property was condemned. After the Tocks Island Dam project was withdrawn, the lands acquired were transferred to the oversight of the National Park Service which reorganized them to establish the Delaware Water Gap National Recreation Area.
Dingmans Ferry is an unincorporated community in Delaware Township, Pike County, Pennsylvania, United States. As of 2014, it had a population of 7,477 people. It was originally sited on the Delaware River, in an area now included in the Delaware Water Gap National Recreation Area. When the Corps of Engineers acquired the land by eminent domain in the mid-twentieth century for the creation of the proposed Tocks Island Dam project, it relocated the community further up the hill.
Blue Mountain Ridge, Blue Mountain, or the Blue Mountains of Pennsylvania is part of the geophysical makeup of the Ridge-and-Valley Appalachians in the U.S. state of Pennsylvania. It is a ridge that forms the southern and eastern edge of the Appalachian mountain range spanning over 255 miles (410 km) from the Delaware Water Gap as it cuts across the eastern half of the state on a slight diagonal from New Jersey tending southerly until it turns southerly curving into Maryland, and beyond.
Flat Brook is an 11.6-mile-long (18.7 km) tributary of the Delaware River in Sussex County, New Jersey in the United States.
The Paulinskill is a 41.6-mile (66.9 km) tributary of the Delaware River in northwestern New Jersey in the United States. With a long-term median flow rate of 76 cubic feet of water per second (2.15 m³/s), it is New Jersey's third-largest contributor to the Delaware River, behind the Musconetcong River and Maurice River. The Paulinskill drains an area of 176.85 square miles (458.0 km2) across portions of Sussex and Warren counties and 11 municipalities. The Paulinskill flows north from its source near Newton, and then turns southwest. The river sits in the Ridge and Valley geophysical province.
The Millstone River is a 38.6-mile-long (62.1 km) tributary of the Raritan River in central New Jersey in the United States.
Old Mine Road is a road in New Jersey and New York said to be one of the oldest continuously used roads in the United States of America. At a length of 104 miles (167 km), it stretches from the Delaware Water Gap National Recreation Area to the vicinity of Kingston, New York.
The Keith line was a line drawn through the Province of New Jersey, dividing it into the Province of West Jersey and the Province of East Jersey. The line was created by Surveyor-General George Keith in 1686, when he ran the first survey to mark out the border between West Jersey and East Jersey. The Keith line was intended to clarify disputes resulting from the 1676 Quintipartite Deed, which created the two territories.
The Skylands Region is a region and marketing area of the State of New Jersey located in the Northern and Central part of the state. It is one of six tourism regions established by the New Jersey State Department of Tourism, the others being the Gateway Region, Greater Atlantic City Region, the Southern Shore Region, the Delaware River Region and the Shore Region. The area officially encompasses Hunterdon, Morris, Somerset, Sussex and Warren counties; the northwestern part of the Passaic County fits in with the Skylands Region, but it is part of the Gateway Region and not the Skylands Region. One could also say that the western most part of Bergen is also part of the skylands. The area features uplifted land, rolling hills and mountains characteristic of North Jersey. The region contains 60,000 acres of state parkland, and a diverse geography filled with lakes, rivers and picturesque hills.
The Pahaquarry Copper Mine is an abandoned copper mine located on the west side of Kittatinny Mountain presently in Hardwick Township in Warren County, New Jersey in the United States. Active mining was attempted for brief periods during the mid-eighteenth, mid-nineteenth, and early twentieth centuries but was never successful despite developments in mining technology and improving mineral extraction methods. Such ventures were not profitable as the ore extracted proved to be of too low a concentration of copper. This site incorporates the mining ruins, hiking trails, and nearby waterfalls, and is located within the Delaware Water Gap National Recreation Area and administered by the National Park Service.
The Minisink or Minisink Valley is a loosely defined geographic region of the Upper Delaware River valley in northwestern New Jersey, northeastern Pennsylvania and New York.
Van Campen's Inn or Isaac Van Campen's Inn is a fieldstone residence that was used as a yaugh house during the American colonial era. Located in Walpack Township, New Jersey along the Delaware River, it is a historic site located along the Old Mine Road in the Delaware Water Gap National Recreation Area. It is operated under a memorandum of understanding between the National Park Service and the Walpack Historical Society, a local non-profit corporation.
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.
Coordinates: 41°08′24″N74°54′47″W / 41.140°N 74.913°W
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.