Geography
Northern Europe consists of the Scandinavian peninsula, the peninsula of Jutland, the Baltic plain that lies to the east and the many islands that lie offshore from mainland northern Europe, Greenland and the main European continent. The area is defined by the volcanic islands of the far northwest, notably Iceland and Jan Mayen, the mountainous western seaboard, extending from the mountainous sections of Great Britain & Ireland to the Scandinavian mountains, the central north mountains and hills of Sweden (which are the foothills of the Scandinavian mountains) and the large eastern plain, which contains, Lithuania, Latvia, Estonia and Finland.
The region has a south west extreme of just under 50 degrees north and a northern extreme of 81 degrees north. The entire region's climate is affected by the Gulf Stream which has a mild influence on the climate. From the west climates vary from maritime and maritime subarctic climates. In the north and central climates are generally subarctic or Arctic and to the east climates are mostly subarctic and temperate/continental. As the climate and relief varies vegetation is also extremely variable, with sparse tundra in the north and high mountains, boreal forest on the north-eastern and central regions temperate coniferous forests (formerly of which a majority was in the Scottish highlands and south west Norway) and temperate broadleaf forests growing in the south, west and temperate east.
With the exception of the United Kingdom and Ireland, Northern European countries are known for harsh winters. For example, the Winter of 2010-2011 in Europe began already in November. Temperatures can reach as low as minus 50 degrees Celsius in some parts of Northern Europe.
Read more about this topic: Northern Europe
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