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[/vc_column_text][/vc_column][/vc_row][vc_row][vc_column width=“1/3″][vc_column_text]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 and Ireland to the Scandinavian mountains peaking in Norway, 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.[/vc_column_text][/vc_column][vc_column width=“1/3″][vc_column_text]The region has a south west extreme of around 50 degrees north and a northern extreme of 81 degrees north. The entire region’s climate is mildly affected by the Gulf Stream. 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.

[/vc_column_text][/vc_column][vc_column width=“1/3″][vc_column_text]There are at least five geologic provinces in the area: the Cascade Volcanoes, the Columbia Plateau, the North Cascades, the Coast Mountains, and the Insular Mountains. The Cascade Volcanoes are an active volcanic region along the western side of the Pacific Northwest. The Columbia Plateau is a region of subdued geography that is inland of the Cascade Volcanoes, and the North Cascades are a mountainous region in the northwest corner of the United States, extending into British Columbia.[/vc_column_text][/vc_column][/vc_row][vc_row][vc_column][vc_column_text]

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