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Klarälven

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Through River, Drainage basin and River delta

It emanates at the northeast side of Mount Brändstöten and flows through a couple of smaller lakes down to Lake Rogen in Härjedalen, Sweden, and then passes through the Norwegian Hedmark, where it flows through the lake Femunden. There it is known as Femundelva and Trysilelva. The rest of the river, the longest part, flows through Värmland to ultimately discharge in a delta into Vänern at Karlstad.

In its turn, Vänern drains then into Göta älv, reaching the sea at Gothenburg.

The river has historically provided significant economic benefits, providing a suitable transport route for log driving, and currently is internationally recognized as excellent sport fishing waters.

Geography and geology

The watershed of Klarälven is commonly referred to as Klarälvdalen (the Klarälv basin), where it accumulates much of its water on its journey to Vänern. Other important sources of water are the snowy mountains in the northern areas of the watershed area, providing substantial flows in the spring when the snow melts; annual floods are common.

The straight river course north of Edebäck has been classified by Sten De Geer as a "tectonic valley" as it follows the Protogine Zone—a bedrock weakness zone of Precambrian age. During deglaciation of Scandinavia about 10,000 years before present the glacier ice retreated unevenly with the valley of Klarälven hosting a protruding ice tongue while the surrounding uplands were ice-free. The retreat of the ice left dead ice buried in the glacifluvial sediments of the valley. The river course north of Edebäck formed an ancient fjord after it became free of glacier ice and before the post-glacial rebound definitely raised the valley bottom above the sea. The river course south of Edebäck is possibly a Quaternary deflection caused by the accumulation of glacial deposits.

Since the end of the last ice age, the mouth of Klarälven has moved southward from Forshaga to its current position at Karlstad, and is still moving, albeit for different reasons, as the river carries substantial quantities of sand, cut from the outer edges of its meandering curves, causing the shoreline of Vänern to constantly move southward.

The heavy meandering of Klarälven results in numerous oxbow lakes, formed as a result of a too sharp curve, eventually causing the river to create a new, shorter path. An artificial islet, Gubbholmen found in central Karlstad has also been created as a result of the accumulation of 5,000 tonnes (4,900 long tons; 5,500 short tons) of sand transported each day during the spring flood.

Entering the Karlstad region, the river delta splits into two main parts and eight smaller parts. The east part splits into two further main branches after passing Gubbholmen (eventually three branches). The west part splits into five branches.

In the first half of the 20th century the geography and Quaternary geology Klarälven was studied by various Swedish researchers including Alfred Elis Törnebohm, Sten De Geer and Lennart von Post. This last Quaternary geologist died in 1951 leaving his research unfinished, despite this Klarälven was by 1956 the most studied river in Sweden. Åke Sundborg's 1956 outstanding PhD thesis and publication on the geomorphology and hydrology of Klarälven is considered a major reference work for river studies in Sweden.

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