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Map of Vermont showing cities, roads, and rivers Mount Mansfield Western face of Camel's Hump Mountain (elevation 4,079 feet (1,243 m)). [1] Fall foliage at Lake Willoughby. The U.S. state of Vermont is located in the New England region of the northeastern United States and comprises 9,614 square miles (24,900 km 2), making it the 45th-largest state.
The Wilcox Formation is a geologic formation in Vermont that is part of the Holly Mountain Complex. It is exposed within the western parts of Mendon and Shrewsbury, Vermont. . The type locality of the Wilcox Formation lies on the slopes south of Cold River of the eponymous Wilcox Hill and on northwest slope of Mendon P
There are five distinct physiographic regions of Vermont. [91] Categorized by geological and physical attributes, they are the Northeastern Highlands, the Green Mountains, the Taconic Mountains, the Champlain Lowlands, and the Vermont Piedmont. [92] About 500 million years ago, Vermont was part of Laurentia and located in the tropics. [93]
The West Castleton Formation is a geologic formation in New York and Vermont. It preserves fossils dating back to the Cambrian period. It is described in Vermont as "Gray silicious to black, graphitic, pyritiferous slate and phyllite, locally with interbedded thin dark grey dolostone and grey quartzite and arkosic layers. Thin, white sandy ...
New England is a region in the North Eastern United States consisting of the states Rhode Island, Connecticut, Massachusetts, New Hampshire, Vermont, and Maine.Most of New England consists geologically of volcanic island arcs that accreted onto the eastern edge of the Laurentian Craton in prehistoric times.
Green Mountains looking south from Jay Peak Jay Peak, located at the northern end of the Green Mountains in Vermont Green Mountains outside of Montpelier, Vermont. The best-known mountains—for reasons such as high elevation, ease of public access by road or trail (especially the Long Trail and Appalachian Trail), or with ski resorts or towns nearby—in the range include: [4]
A map of the extent of the Waits River Formation and its surrounding units in the Connecticut Valley-Gaspé Trough. Modified from Perrot (2018) [3] The Waits River formation was deposited through normal faulting and back-arc extension in the late Silurian period. During the Acadian orogeny, the land mass Gander collided with Laurentia. [4]
Although Vermont is known as the Green Mountain State, the Northeast Kingdom lies outside that geological formation and is based on a set of long-ago volcanic islands, compressed during collision with the Taconic orogeny. Views and vistas differ sharply from those of the state's central mountain spine. [10]