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Adirondack Mountains
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What are the Adirondack Mountains?
The Adirondack Mountains are in northeastern New York, extending south from the St. Lawrence River and Lake Champlain to the Mohawk River valley. Though often considered part of the Appalachian system, they are geologically linked to the Canadian Shield and were formed about one billion years ago.
The Adirondacks cover over 9,100 square miles, characterized by numerous peaks and foothills. More than 40 summits are higher than 4,000 feet, including Mount Marcy, the state's highest point at 5,344 feet, and Algonquin Peak of Mount McIntyre at 5,114 feet. The region has forests, glacial landforms, and around 2,300 lakes and ponds. The Adirondack Park, created in 1892, is the largest state or national park outside Alaska.
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Where are the Adirondack Mountains located?
The Adirondack Mountains are in northeastern New York, U.S., and stretch south from the St. Lawrence River valley and Lake Champlain to the Mohawk River valley. Though frequently included in the Appalachian Mountain system, the Adirondacks are geologically related to the Canadian Shield. The Adirondacks region is circular, domelike, and covers more than 9,100 square miles (23,600 square km). The region has hundreds of peaks and foothills, with more than 40 summits higher than 4,000 feet (1,200 meters). The tallest is Mount Marcy, the highest point in the state at 5,344 feet (1,629 meters).
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How did the Adirondack Mountains form?
The Adirondack Mountains were formed approximately one billion years ago and are geologically related to the Canadian Shield. Over hundreds of millions of years, these mountains underwent erosion and glaciation, particularly during the Pleistocene Epoch. The mountains have a circular outline and a domelike appearance, with more than 40 summits exceeding 4,000 feet (1,200 meters).
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What types of plants and animals can be found in the Adirondack Mountains?
The Adirondack Mountains are home to diverse plant and animal life. The mountains are covered with spruce, hemlock, and pine forests interspersed with hardwoods on the lower slopes.
White-tailed deer and black bear are the largest species of wildlife. Small mammals such as deer mice, eastern cottontails, snowshoe hares, woodchucks, gray squirrels, muskrats, and raccoons are common. New York is host to numerous migratory birds. Year-round residents include eastern meadowlarks, American goldfinches, cardinals, eastern bluebirds, cedar waxwings, bluejays, several kinds of woodpeckers and owls, red-tailed hawks, ruffed grouses, mallards, and common house sparrows.
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Why is the Adirondack Park important?
The Adirondack Park is important because it protects a large, primitive natural area in northeastern New York state. Created in 1892, it is the largest state or national park outside of Alaska, covering almost one-fifth of New York state. The park helps to conserve the region's natural state, including its spruce, hemlock, and pine forests, as well as its diverse wildlife. It also offers numerous recreational activities such as camping, swimming, hiking, canoeing, and winter sports, making it a popular tourist destination.
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How do people use and enjoy the Adirondack Mountains today?
Today, the Adirondack Mountains are sparsely settled and protected by state law, existing in a primitive natural state. People enjoy the Adirondacks through numerous parks, private resort villages, and state campsites that provide facilities for camping, swimming, hiking, and canoeing, especially around the Saranac River and Lake Placid. Winter sports include Olympic ski and bobsled runs at Lake Placid (which hosted the 1932 and 1980 Olympic Winter Games) and other sites, snowmobiling, and ice skating. Good highways provide access to some parts of the region, but its more remote portions are accessible only to hikers or canoeists.
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Adirondack Mountains, mountains in northeastern New York state, U.S. They extend southward from the St. Lawrence River valley and Lake Champlain to the Mohawk River valley. The mountains are only sparsely settled, and much of the area exists in a primitive natural state, protected by state law.
Although they are frequently included in the Appalachian Mountain system, the Adirondack Mountains are related geologically to the great plateau of the Canadian Shield. The Adirondacks were formed some one billion years ago and have been subjected to hundreds of millions of years of erosion and glaciation, notably the glaciations of the Pleistocene Epoch (about 2,600,000 to 11,700 years ago). The Adirondacks region is circular in outline, domelike in appearance, and covers more than 9,100 square miles (23,600 square km). The region is made up of hundreds of peaks and foothills, with more than 40 summits higher than 4,000 feet (1,200 metres); the tallest are Mount Marcy, which is the highest point in the state at 5,344 feet (1,629 metres), and Algonquin Peak of Mount McIntyre at 5,114 feet (1,559 metres). Although the peaks are primarily rounded in shape, several of the higher ones, including Whiteface Mountain (4,867 feet [1,483 metres]), reveal bare rock walls in vertical escarpments.
The Adirondack Mountains are covered with spruce, hemlock, and pine forests interspersed with hardwoods on the lower slopes; white-tailed deer and black bear are the largest species of wildlife. The action of retreating glaciers during the last Pleistocene Ice Age left the area covered by glacial till (intermingled clay, sand, gravel, and boulders) and created the many spectacular gorges, waterfalls, lakes, ponds, and swamps for which the region is noted. Some 2,300 lakes and ponds dot the landscape. More than 31,000 miles (50,000 km) of rivers and streams radiate from the upland region into the St. Lawrence, Hudson, and Mohawk rivers and Lakes Ontario and Champlain. Summers in the Adirondacks are moderated by cool mountain breezes, and winters, though cold, are mitigated by dry air and clear skies.
The name Adirondack is derived from an Iroquois word meaning “eater of tree bark,” a derisive term bestowed by them upon a neighbouring Algonquin tribe. The French explorer Samuel de Champlain became the first European to sight the Adirondacks, in 1609, but the area resisted all but sparse settlement until the late 19th century. In 1892 the New York state legislature created Adirondack Park, which has grown over the years and is roughly coterminous with the Adirondacks region, making it the largest American state or national park outside of Alaska. The park covers almost one-fifth of the state and is about the size of Vermont. The state-owned Adirondack Forest Preserve now comprises some 3,900 square miles (10,100 square km) within the park and is a popular tourist area. The majority of the land in Adirondack Park, however, is privately owned and used for lumbering, agriculture, and recreation. The mining of iron ore, graphite, and titanium has been replaced by the mining of wollastonite (a form of calcium silicate) and garnet.
Numerous parks, private resort villages, and state campsites in the Adirondacks provide facilities for camping, swimming, hiking, and canoeing, especially around the Saranac River and Lake Placid. Winter sports include Olympic ski and bobsled runs at Lake Placid (which hosted the 1932 and 1980 Olympic Winter Games) and other sites, snowmobiling, and ice skating. Good highways provide access to some parts of the region, but its more remote portions are accessible only to hikers or canoeists. Historic landmarks in the area include Fort Ticonderoga, Lake George, and Plattsburgh. The Adirondack Museum, on a campus of exhibit buildings near Blue Mountain Lake, houses relics of human activity in the mountains since colonial times.

