Pocono Mountains in the context of "Artificial snow"

⭐ In the context of artificial snow, the Pocono Mountains ski resorts commonly employ this technology to primarily address what challenge?

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⭐ Core Definition: Pocono Mountains

The Pocono Mountains, commonly referred to as the Poconos (/ˈpkənz/), are a geographical, geological, and cultural region in Northeastern Pennsylvania. They overlook the Delaware River and Delaware Water Gap to the east, Lake Wallenpaupack to the north, Wyoming Valley and the Coal Region to the west and the Lehigh Valley to the south. The name Pocono is derived from the Munsee word Pokawachne, which means "Creek Between Two Hills".

Much of the Poconos region lies within the Greater New York–Newark, NY–NJ–CT–PA Combined Statistical Area. The wooded hills and valleys have long been a popular recreation area, accessible within a two-hour drive to millions of metropolitan area residents, with many Pocono communities having resort hotels with fishing, hunting, skiing, and other sports facilities.

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👉 Pocono Mountains in the context of Artificial snow

Snowmaking is the production of snow by forcing water and pressurized air through a "snow gun", also known as a "snow cannon". Snowmaking is mainly used at ski resorts to supplement natural snow. This allows ski resorts to improve the reliability of their snow cover and to extend their ski seasons from late autumn to early spring. Indoor ski slopes use snowmaking. They can generally do so year-round as they have climate-controlled environments.

The use of snowmaking machines has become more common as changing weather patterns and the popularity of indoor ski resorts create a demand for snow beyond that which is provided by nature. Snowmaking machines have addressed the shortage in the supply of snow; however, there are significant environmental costs associated with the artificial production of snow.

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Pocono Mountains in the context of Camelback Mountain Resort

Camelback Resort is a four season resort located in Tannersville, Pennsylvania in the Pocono Mountains in Northeastern Pennsylvania. The resort opened in December 1963. It is the largest ski resort in the Poconos.

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Pocono Mountains in the context of Northeastern Pennsylvania

Northeastern Pennsylvania (NEPA or Nepa; sometimes pronounced /ˈnpɑː/ NEE-pah) is a region of the U.S. state of Pennsylvania that includes the Pocono Mountains, and the industrial cities of Scranton (the area's largest city), Wilkes-Barre, Pittston, Hazleton, Nanticoke, and Carbondale. A portion of this region is located in the New York City metropolitan area. Recently, Pennsylvania tourism boards have described Northeastern Pennsylvania as Upstate Pennsylvania.

Unlike most other parts of the Rust Belt, some of the communities are experiencing a modest population increase, and others, including Monroe and Pike counties, rank among the state's fastest growing counties.

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Pocono Mountains in the context of Lehigh River

The Lehigh River (/ˈlh/) is a 109-mile-long (175 km) tributary of the Delaware River in eastern Pennsylvania. The river flows in a generally southward pattern from the Pocono Mountains in Northeastern Pennsylvania through Allentown and much of the Lehigh Valley before joining the Delaware River in Easton.

Part of the Lehigh River and a number of its tributaries are designated Pennsylvania Scenic Rivers by the state's Department of Conservation and Natural Resources.

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Pocono Mountains in the context of Tannersville, Pennsylvania

Tannersville is a village in Pocono Township, Pennsylvania. It is the site of the Camelback Mountain Resort, a popular ski and waterpark resort in The Poconos.

As of 2000, the population of Tannersville was 2,784. The community is served by the 629 exchange in area code 570.

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Pocono Mountains in the context of Lake Wallenpaupack

Lake Wallenpaupack (/ˌwɒlɪnˈpɔːpæk/) is a reservoir in Northeastern Pennsylvania. After Raystown Lake, it is the second-largest lake contained entirely in Pennsylvania. It comprises 52 mi (84 km) of shoreline, with a length of 13 mi (21 km) and a maximum depth of 60 ft (18 m), and has a surface area in excess of 5,700 acres (2,300 ha). It was created in 1926 by the PPL Corporation for hydroelectric purposes, as well as flood control, but it is best known as one of several major recreational destinations in the Pocono Mountains. It is located near the Borough of Hawley, and forms part of the boundary between Pike and Wayne Counties. See map.

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Pocono Mountains in the context of Lackawanna River

The Lackawanna River is a 42-mile-long (68 km) tributary of the Susquehanna River in Northeastern Pennsylvania. It flows through a region of the northern Pocono Mountains that was once a center of anthracite coal mining in the United States. It starts in north Wayne County, Pennsylvania and ends in east Luzerne County, Pennsylvania in Duryea, Pennsylvania. The lower reaches of the river flow through the urban areas of Scranton, which grew around its banks in the 19th century as an industrial center. Its name comes from a Lenape word meaning "stream that forks".

The river rises in two branches, the West and East branches, along the boundary between Susquehanna and Wayne counties. The branches, each about 12 miles (19 km) long, flow south, closely parallel to each other, and join at the Stillwater Lake reservoir in Union Dale. The combined river flows southwest past Forest City, Carbondale, Mayfield, Jermyn, Archbald, Jessup, Blakely, Olyphant, Dickson City, Throop, Scranton, Taylor, Moosic, Old Forge, and Duryea. It joins the Susquehanna River at the northern boundary of Pittston about 8 miles (13 km) west-southwest of Scranton. As part of the Susquehanna River, it ultimately flows to Chesapeake Bay.

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