The
extreme distance from north to south in Sweden is about 1,575 km (980
mi), and from east to west about 500 km (310 mi). The coastline totals
about 7,565 km (4,700 mi) in length. Sweden may be divided into six
topographical regions. In the north-western section are extensions of
the Kjölen Mountains, which form part of the boundary with Norway.
The highest point in the range, and the highest point in Sweden, is
atop Mount Kebnekaise 2,111 m (6,926 ft). To the east of the mountains
is a long plateau, which slopes east to a coastal plain bordering the
Gulf of Bothnia. An upland region, known as the Småland highlands,
is located south of the lowland. The plains of Skåne occupy the
south-eastern tip of the Scandinavian Peninsula. The lowest elevation
point is sea level along the coast.
Sweden
is part of the Fennoscandian Shield, which extends over part of northern
Europe. The rocks, except those in the north-west, are primarily ancient
Precambrian granites, schists, and gneisses. Younger metamorphic rocks
are characteristic of the northern part of the country. Sedimentary
rocks are found in the southern Skåne plains and in the islands
of Gotland and Öland.
The
present topography of Sweden was formed largely during the Quaternary
Ice Ages by a continental ice sheet, which receded about 8,000 years
ago. The mountains, except for several of the highest peaks, were rounded
by glaciation. The ice sheet scraped out deep valleys and created numerous
glacial lakes. Ridges of rock, gravel, sand, and clay were deposited
in many places by the retreating ice. Glacial seas left fertile marine
clay soils in the south and in the central lake area. Some permanent
glacier fields still remain in the high mountain regions.