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Isel (river)

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Through Hydroelectricity, Quaternary and Till

Course

The Isel river flows from the Umbalkees glacier in the Hohe Tauern National Park near the summit of Rötspitze mountain. It is a left tributary of the Drava (Drau). The catchment areas of the Isel and Drava together cover almost all of East Tyrol. The catchment area of the Isel is about 1,200 square kilometres (460 sq mi). At the estuary where the Isel enters the Drau the mean water flow is about 39 cubic metres per second (1,400 cu ft/s). A flood event of about 770 cubic metres per second (27,000 cu ft/s) is expected to occur once in 100 years.

The Isel flows through a deeply incised valley with several gorges (Iselschlucht) in which it has created several waterfalls. At present there are no dams or diversions along its course. The Tauernbach tributary joins the Isel at Matrei. Other important tributaries are the Schwarzach and the Kalserbach. Below Matrei the valley widens along the lower stretch to where the river meets the Drau at Lienz.

The river banks flood daily and seasonally, and the riverbed constantly shifts. This provides a unique environment for endangered plants such as the German tamarisk (Myricaria germanica). There are eight artificially widened basins in the Isel valley, designed to contain the bed load, which reduce the risk of flooding. These require regular maintenance, which must be adapted to conform with the Natura 2000 designation.

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