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Finland's total area is 337,030 km 2 (130,128 sq mi). Of this area 10% is water, 69% forest, 8% cultivated land and 13% other. Finland is the eighth largest country in Europe after Russia, France, Ukraine, Spain, Sweden, Norway and Germany. As a whole, the shape of Finland's boundaries resembles a figure of a one-armed human.
Finland – sovereign Nordic country located in Northern Europe. [1] Finland has borders with Sweden to the west, Russia to the east, and Norway to the north, while Estonia lies to its south across the Gulf of Finland. The capital city is Helsinki. Around 5.62 million people reside in Finland, with the majority concentrated in the southern part ...
Finland, [a] officially the Republic of Finland, [b] [c] is a Nordic country in Northern Europe. It borders Sweden to the northwest, Norway to the north, and Russia to the east, with the Gulf of Bothnia to the west and the Gulf of Finland to the south, opposite Estonia .
Finland geography-related lists (3 C, 5 P) B. Borders of Finland (5 C, 6 P) E. Ecoregions of Finland (4 P) Extreme points of Finland (2 P) F. Forests of Finland (3 P) G.
Finland is divided into 19 regions (Finnish: maakunta; Swedish: landskap) [a] which are governed by regional councils that serve as forums of cooperation for the municipalities of each region. The councils are composed of delegates from the municipal councils.
Åland (/ ˈ ɔː l ə n d / AW-lənd, Swedish: ⓘ; Finnish: Ahvenanmaa) is an autonomous and demilitarised region of Finland.Receiving its autonomy by a 1920 decision of the League of Nations, it is the smallest region of Finland by both area (1,580 km 2 or 610 sq mi) and population (30,541), constituting 0.51% of Finland's land area and 0.54% of its population.
Shqip; Sicilianu; Simple English; ... Geography of Finland (22 C, 17 P) Government of Finland (14 C, 37 P) H. Health in Finland (9 C, 8 P) History of Finland (8 C, 4 ...
The geology of Finland is made up of a mix of geologically very young and very old materials. Common rock types are orthogneiss , granite , metavolcanics and metasedimentary rocks. On top of these lies a widespread thin layer of unconsolidated deposits formed in connection to the Quaternary ice ages , for example eskers , till and marine clay .