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A pine forest is an example of a temperate coniferous forest Forest communities dominated by huge trees (e.g., giant sequoia, Sequoiadendron gigantea ; redwood, Sequoia sempervirens ), unusual ecological phenomena, occur in western North America, southwestern South America, as well as in the Australasian region in such areas as southeastern ...
Mixed conifer forest is a vegetation type dominated by a mixture of broadleaf trees and conifers. [1] It is generally located in mountains, below the upper montane vegetation type. Sierra Nevada range
The Caledonian Forest is the ancient temperate forest of Scotland. The forest today is a reduced-extent version of the pre-human-settlement forest, existing in several dozen remnant areas . The Scots pines of the Caledonian Forest are directly descended from the first pines to arrive in Scotland following the Late Glacial ; arriving about 7000 BC .
Situated in the state of Baden-Württemberg in southwest Germany, the enchanting mountain region has scenic trails, placid lakes, and dense conifer forests that make it a fantasy-turned-reality ...
Approximately 4,700 km 2 of Scotland's forests and woodlands are publicly owned by the Scottish Government via Forestry and Land Scotland, and these are termed the National Forest Estate. [5] As of 2015, forestry contributed almost £1 billion to the Scottish economy, and the industry employed over 25,000 people. [6]
In the Sierra Nevada mountain range of the western United States, the mixed coniferous forest is found at elevations of 1,200–5,500 feet (370–1,680 m) in the north, 2,000–6,500 feet (610–1,980 m) in central areas, and 2,500–9,000 feet (760–2,740 m) in the south. [1]
These forests are found predominantly in North and Central America and experience low levels of precipitation and moderate variability in temperature. Tropical and subtropical coniferous forests are characterized by diverse species of conifers , whose needles are adapted to deal with the variable climatic conditions. [ 1 ]
A conifer forest will return to Mount St. Helens in its own time. On a debris-avalanche deposit totally devoid of life after May 18, 1980, plants are slowly taking hold of the landscape.