Major Landforms of Sweden

Sweden's physical landscape divides broadly into four zones running from west to east and from north to south: the Scandinavian Mountains along the Norwegian border, the vast interior forests and lake-studded plains, the coastal lowlands, and the agricultural south. Each region has a distinct character shaped by geology, glaciation, and climate.

The Scandinavian Mountains (Fjällen (the Mountain Region))

The Skanderna (Scandinavian Mountains) form Sweden's western spine, running roughly 1,700 kilometres along the Norwegian border from northern Lapland to Dalarna. These are the eroded remnants of the Caledonian orogeny — mountains that once rivalled the Himalayas but have been worn down over 400 million years to rounded, windswept summits.

Glacial cirques, U-shaped valleys, and remnant glaciers are prominent features of the mountain region. Sweden's remaining ~300 glaciers are concentrated here, though all are retreating due to climate change. The Kebnekaise south peak, once clearly the country's highest point, is losing elevation as its summit glacier thins — the north peak (a rocky summit) may eventually surpass it.

Swedish Lapland (Lappland (Lapland))

Swedish Lapland — the vast inland territory of Norrbotten and Västerbotten counties — is one of the most sparsely populated regions in Europe. A landscape of boreal forest, river valleys, myrar (mires/bogs), and mountain foothills, it covers roughly a quarter of Sweden's land area but holds only a fraction of its population.

Key features include:

River valleys — Major rivers like the Torne, Lule, and Vindel flow from the mountains southeast to the Gulf of Bothnia, their valleys providing corridors for settlement and, more recently, hydroelectric power
Mires and wetlands — Lapland contains some of Europe's largest intact mire complexes, vital carbon stores and habitats
The Lapland ore belt — The bedrock here holds the rich iron ore deposits that sustain LKAB's mining operations in Kiruna and Gällivare

This is also the homeland of the Sámi (Sámi people), whose reindeer herding still follows seasonal migration routes across the landscape.

The Interior Lowlands and Lake District

Central Sweden — the region historically called Svealand (the Land of the Svear) — is characterised by a gently undulating landscape of forests, farmland, and an extraordinary number of lakes. Glacial deposits — moraines, drumlins, eskers — define the terrain, creating a patchwork of ridges, hollows, and lake-filled basins.

The åsar (eskers) are a distinctive feature: long, sinuous ridges of sand and gravel deposited by subglacial rivers during the Ice Age. Some of Sweden's oldest roads and railways follow these natural causeways across otherwise boggy terrain.

This is Sweden's most productive agricultural zone outside Skåne, with arable land concentrated in the clay-bottomed lake plains around Mälaren, Hjälmaren, and the Östgöta plain.

Småland Highlands (Småländska höglandet (Småland Highlands))

Southern Sweden's interior is dominated by the Småland Highlands — a plateau of crystalline bedrock (granite and gneiss) rising to 300–400 metres, deeply forested and dotted with lakes. The thin, stony soils made farming difficult, and it was hardship in Småland that drove much of the Great Emigration to America in the 19th century. Today, the region is renowned for glassblowing (the "Kingdom of Crystal"), forestry, and small-scale industry.

The Plains of Skåne

Sweden's southernmost province, Skåne (Scania), is geologically and agriculturally distinct from the rest of the country. Here, sedimentary bedrock (chalk, sandstone, shale) replaces the crystalline shield, and thick glacial and post-glacial clay deposits create some of the richest farmland in Scandinavia.

The landscape here feels more Danish or North German than Scandinavian — open fields, gentle hills, beech forests, and a coastline of sandy beaches rather than rocky skerries. Skåne was, in fact, Danish territory until 1658 and retains a distinct regional identity.

Islands

Sweden possesses two large islands in the Baltic Sea — Gotland (Gotland) and Öland (Öland) — each with a unique character.

Gotland (3,140 km²) is Sweden's largest island, a limestone plateau famous for its medieval walled town of Visby (a UNESCO World Heritage Site), its sea stacks (raukar (sea stacks)), and its rich fossil heritage. The island's geology — Silurian limestone — makes it fundamentally different from mainland Sweden.

Öland (1,342 km²), connected to the mainland by a bridge, features the Stora Alvaret (Great Alvar), a UNESCO-listed limestone plain with unique grassland ecology. The thin soil supports rare orchids and an agricultural landscape that has been farmed since the Iron Age.

The Swedish Coastline Pattern

Sweden's coastline reflects its geological divisions:

West coast (Bohuslän): Granite skerries sculpted by Atlantic weather — smooth, rounded, pinkish rock
East coast (north): Rapidly rising land creating new islands, shallow bays — the land uplift coast
East coast (south, Stockholm archipelago): Thousands of islands in the glacially carved granite
South coast (Skåne): Sandy beaches, more reminiscent of continental Europe

Together, including islands, Sweden has over 3,000 kilometres of coastline and an estimated 221,800 islands — though only about 1,000 are permanently inhabited.

Sweden at a glance — Key facts about the country, from area to government

Stockholm city guide — Explore Sweden's capital across its 14 islands

Mining regions — How Lapland's geology drives Sweden's mining industry