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The most mountainous region of Tasmania is the Central Highlands area, which covers most of the central-western parts of the state. Many of these areas are highly elevated alpine regions. The Ozarks cover nearly 120,000 square kilometres (46,000 sq mi), making it the most extensive highland region between the Appalachians and Rockies. This ...
The Highlands (Scots: the Hielands; Scottish Gaelic: a' Ghàidhealtachd [ə ˈɣɛːəl̪ˠt̪ʰəxk], lit. ' the place of the Gaels ') is a historical region of Scotland. [1] [failed verification] Culturally, the Highlands and the Lowlands diverged from the Late Middle Ages into the modern period, when Lowland Scots language replaced Scottish Gaelic throughout most of the Lowlands.
The Highlands and Islands region. Some Highland districts are not shown. The Highlands and Islands is an area of Scotland broadly covering the Scottish Highlands, plus Orkney, Shetland, and the Outer Hebrides (Western Isles). The Highlands and Islands are sometimes defined as the area to which the Crofters' Act of 1886 applied.
Articles relating to highlands, mountainous regions or elevated mountainous plateaus. Generally speaking, upland (or uplands) refers to ranges of hills, [1] typically up to 500–600 m (1,600–2,000 ft). Highland (or highlands) is usually reserved for ranges of low mountains
There are over 200 named lakes, with the number of smaller lakes, ponds, and other bodies of water reaching over 3,000. The region has over 1,200 miles of river. [5] The current relief owes much to glaciation. Among the named lakes around the mountains, are Lake George, Lake Placid, and Lake Tear of the Clouds, which is the source of the Hudson ...
This climate is also referred to as a mountain climate or highland climate. Definition. There are multiple definitions of alpine climate.
The Highland Region was created covering the area in 1975 as part of a two-tier local government structure of upper-tier regions and lower-tier districts. The Highland Region had eight districts. Local government was reorganised again in 1996 into single-tier council areas, with the former region becoming one of the new council areas.
The Massif Central is an old massif, formed during the Variscan orogeny, consisting mostly of granitic and metamorphic rocks.It was powerfully raised and made to look geologically younger in the eastern section by the uplift of the Alps during the Paleogene period and in the southern section by the uplift of the Pyrenees.