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11 relations: Alps, Betula nana, Ecotone, Older Dryas, Plant community, Pyrenees, Salix herbacea, Siberia, Taiga, Tundra, Younger Dryas.
Alps
The Alps (Alpes; Alpen; Alpi; Alps; Alpe) are the highest and most extensive mountain range system that lies entirely in Europe,The Caucasus Mountains are higher, and the Urals longer, but both lie partly in Asia.
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Betula nana
Betula nana, the dwarf birch, is a species of birch in the family Betulaceae, found mainly in the tundra of the Arctic region.
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Ecotone
An ecotone is a transition area between two biomes.
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Older Dryas
The Older Dryas was a stadial (cold) period between the Bølling and Allerød interstadials (warmer phases), about 14,000 years Before Present), towards the end of the Pleistocene. Its date is not well defined, with estimates varying by 400 years, but its duration is agreed to have been around 200 years. The gradual warming since the Last Glacial Maximum (27,000 to 24,000 years BP) has been interrupted by two cold spells: the Older Dryas and the Younger Dryas (c.
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Plant community
A plant community (sometimes "phytocoenosis" or "phytocenosis") is a collection or association of plant species within a designated geographical unit, which forms a relatively uniform patch, distinguishable from neighboring patches of different vegetation types.
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Pyrenees
The Pyrenees (Pirineos, Pyrénées, Pirineus, Pirineus, Pirenèus, Pirinioak) is a range of mountains in southwest Europe that forms a natural border between Spain and France.
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Salix herbacea
Salix herbacea, the dwarf willow, least willow or snowbed willow, is a species of tiny creeping willow (family Salicaceae) adapted to survive in harsh arctic and subarctic environments.
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Siberia
Siberia (a) is an extensive geographical region, and by the broadest definition is also known as North Asia.
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Taiga
Taiga (p; from Turkic), also known as boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruces and larches.
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Tundra
In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons.
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Younger Dryas
The Younger Dryas (c. 12,900 to c. 11,700 years BP) was a return to glacial conditions which temporarily reversed the gradual climatic warming after the Last Glacial Maximum started receding around 20,000 BP.
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