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Vättern

geography Maturity 11-13 Next article →

Vättern is a massive, finger-shaped lake in south central Sweden.

Vättern by Sentinel-2
Vättern by Sentinel-2

It is the second-largest lake in Sweden, following Lake Vänern. In all of Europe, it ranks as the sixth-largest lake. The lake sits within the Götaland region. It points toward the tip of the Scandinavian Peninsula. Vättern is a deep body of fresh water. It contains roughly half the water volume of Vänern. However, it covers only about one-third of the surface area. Its deepest point actually reaches below sea level.

The lake's water moves through a complex system of connections. Many rivers and small lakes act as sources for the lake. The highest sources are located near Nässjö on the South Swedish Highland. Water drains out of the lake via the Motala ström. This river flows through Bråviken to reach the Baltic Sea. Since 1832, the Göta Canal has provided another downstream path. This canal connects Vättern to Lake Vänern and the Atlantic Ocean. The lake level is regulated to keep these numbers fixed.

Geology tells a story of deep time and shifting earth. Vättern formed as a graben, which is a depressed block of crust. This tectonic event occurred 700 to 800 million years ago. The granitic basement rocks are deformed by the Protogine Zone. This zone crosses the area and creates foliated rocks. The basin also contains the Visingsö Group of sedimentary rocks. These include sandstone, conglomerate, arkose, and carbonates. Some of these sediments were deposited before the graben formed.

Glaciers have also shaped the landscape of Vättern. Multiple glaciations covered the area during the last millions of years. These ice sheets left behind drumlins and glacial striations. The modern lake began around 10,000 BP. This happened as the Scandinavian glacier receded after the last glacial period. Vättern was once a bay of the Baltic ice lake. It was also a bay of the Yoldia Sea. Later, it connected to Ancylus Lake through the north.

Changing land levels eventually isolated the lake. Around 8000 BP, an accident of isostatic land rise occurred. This is the process where land rises after the weight of ice is removed. This uneven rise lifted Vättern above Ancylus Lake. Today, post-glacial rebound continues in specific areas. This happens in southern Jönköping and northeastern Motala. This constant rising causes Vättern to tilt toward the south every year. This geological movement is a slow but steady process.

The lake supports a diverse biological community. It contains various types of plankton, including zooplankton like Copepoda. The benthos, or bottom-dwelling species, include Bivalvia and Crustacea. Several fish species live in these deep waters. These include Salmo salar and Coregonus lavaretus. The lake is famous for the Vättern char, or Salvelinus alpinus. This fish is genetically close to chars in Russia's Lake Ladoga. It is also related to the Sommen char.

Humans rely on Vättern for many vital resources. The water is famous for its extreme transparency and quality. Many local municipalities take their drinking water directly from the lake. The water requires very little treatment before use. Some suggest it is the largest body of potable water globally. The surrounding areas use the lake for many industries. These include forestry, manufacturing, paper, and mining. Agriculture also plays a role in the drainage basin.

Finally, Vättern is a center for recreation and culture. The lake includes the scenic island of Visingsö. Many towns sit along its perimeter, such as Jönköping and Vadstena. Every year, the Vätternrundan cycling race takes place. About 20,000 participants ride 300 km around the shores. Fishing is also a major activity for tourists and commerce. People can fish for sport as long as they avoid nets. The lake remains a central part of Swedish life.

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File:Vättern by Sentinel-2.jpg
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