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Argen

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Argen

The Argen is a river in Baden-Württemberg, Germany. It flows into Lake Constance between Kressbronn am Bodensee and Langenargen as the third largest tributary to the lake. It is 23.4 kilometres (14.5 mi) long; if one includes the Obere Argen and its source river Seelesgraben, the combined length is 73.2 kilometres (45.5 mi).

The headwaters of the Argen arise in the Allgäu. There are two headwaters: the Obere Argen and the Untere Argen. The two arms wrap around the Große Kreisstadt of Wangen im Allgäu and meet each other in the Neuravensburg district of Wangen im Allgäu.

The origin of the Untere Argen is the confluence of Börlasbach and Stixnerbach at the western entrance to Missen at about 850 metres (2,790 ft) above sea level in the Allgäu region of Bavaria. From the confluence, it first flows north to Isny im Allgäu, then northwest to Waltershofen, then southwest to Primisweiler. Past Primisweiler, it merges with the Obere Argen.

The main tributaries are the Wengener Argen and the Haslach.

The Federal highway A96 crosses it a number of times.

The Obere Argen originates in a marshy area north-west of Oberstaufen in the Allgäu. It initially flows through the Eistobel gorge, then underneath the Argentobelbrücke, and past Grünenbach towards Wangen im Allgäu. From there it flows on via Neuravensburg to Pflegelberg, where it is united with the Untere Argen.

Geomorphologically, the Argen has cut a deep and wide valley into the landscape, leading to such place names as Gitzensteig. In some places, the valley is over a kilometre wide. The edges of the valley occasionally rise steeply up to 100 metres (330 ft), and the valley floor is at the level of Lake Constance.

Further down its course, the river bed becomes increasingly broader. The river here flows past the villages of Laimnau, Apflau and Badhütten. In the lower part of its course, the Argen was straightened out considerably. It no longer has oxbow lakes because of the intensive valley agriculture. In recent years the massive concrete walls alongside the river have been replaced with large boulders in most of the shallower zones. Near the estuary at Kressbronn, gravel is mined in larger quantities, creating new lakes along the river.

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