Adirondack Mountains

The Adirondack Mountains are an unusual geological formation located in the northeastern lobe of Upstate New York in the United States. The mountains rise in Clinton, Essex, Franklin, Fulton, Hamilton, Herkimer, Lewis, St. Lawrence, Saratoga, Warren, and Washington counties.

Unlike other mountain ranges that run along fault lines, the Adirondack mountains resemble a dome. They were formed by an uplift deep under the Earth's crust, about a billion years ago. They are part of the Laurentian Mountains of Canada. They are bordered on the east by Lake Champlain and Lake George, which separate them from the Green Mountains in Vermont. They are bordered to the south by the Mohawk Valley, and to the west by the Tug Hill Plateau, separated by the Black River. This region is south of the Saint Lawrence River.

Read more about Adirondack Mountains:  Ecology, Geology and Physiography, Naming, Spelling, and Pronunciation, Tourism and Recreation, Human History

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    New York has her wilderness within her own borders; and though the sailors of Europe are familiar with the soundings of her Hudson, and Fulton long since invented the steamboat on its waters, an Indian is still necessary to guide her scientific men to its headwaters in the Adirondack country.
    Henry David Thoreau (1817–1862)

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