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The southern Appalachian spruce–fir forest is an ecoregion of the temperate coniferous forests biome, a type of montane coniferous forest that grows in the highest elevations in the southern Appalachian Mountains of the eastern United States. The ecoregion is the highest and coldest forest type in the Appalachian range, thriving in elevations ...
The Appalachian Mountains, [b] often called the Appalachians, are a mountain range in eastern to northeastern North America. The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the ...
The Appalachian–Blue Ridge forests are an ecoregion in the Temperate broadleaf and mixed forests Biome, in the Eastern United States. The ecoregion is located in the central and southern Appalachian Mountains, including the Ridge-and-Valley Appalachians and the Blue Ridge Mountains. It covers an area of about 61,500 square miles (159,000 km 2 ...
Description. Close-up view of Fraser fir foliage. Abies fraseri is a small evergreen coniferous tree typically growing between 30 and 50 ft (10 and 20 m) tall, but rarely to 80 ft (20 m), with a trunk diameter of 16–20 in (41–51 cm), but rarely 30 in (80 cm). The crown is conical, with straight branches either horizontal or angled upward at ...
Throughout the Appalachian Mountain range, P. pungens is a component of conifer-dominated communities along combination with other pine species. [10] The three tallest known Pinus pungens are in Paris Mountain State Park, South Carolina; they are 26.85 to 29.96 metres (88 ft 1 in to 98 ft 4 in) tall. [4]
14.8% [ 1] Protected. 8.37% [ 1] The Appalachian mixed mesophytic forests is an ecoregion of the temperate broadleaf and mixed forests biome, as defined by the World Wildlife Fund. It consists of mesophytic plants west of the Appalachian Mountains in the Southeastern United States . This ecoregion consists of the following EPA level III ...
Overview. The Appalachian Mountains formed through a series of mountain-building events over the last 1.2 billion years: [4][5] The Grenville orogeny began 1250 million years ago (Ma) and lasted for 270 million years. The Taconic orogeny began 450 Ma and lasted for 10 million years. The Acadian orogeny began 375 Ma and lasted 50 million years.
Temperate rainforest extends through the Appalachian areas of western North Carolina, [9] southeastern Kentucky, [10] southwest Virginia, eastern Tennessee, [11] northern South Carolina, [12] and northern Georgia. [13] Red spruce and Fraser fir are dominant canopy trees in high mountain areas.