|Between Vík í Mýrdal and Mýrdalssandur|
The river has a glacier flow which draws its water from the Mýrdalsjökull, mainly through the glacier tongue Kötlujökull. The river's floods are usually of gray-brown color, since it carries much sediment with it.
As increasing water levels of this river are an important indicator of Katla's upcoming volcanic eruptions, it is closely monitored.
A predecessor of the present bridge was demolished in 1955, during a jökulhlaup with 2,500 m³/s of water. A fissure formed on Katla in 1918 in the caldera of the volcano, and a kettle had formed upon the glacier. This showed volcanic activities under the glacier, which in turn initiated the jökulhlaup. However, there was no real outbreak in 1955.
On 9 July 2011, another jökulhlaup occurred, which was already anticipated hours and days before because of a series of quakes at up to 10 km (6.2 mi) depth in the Katla region. There was a small volcanic eruption under the glacier similar to 1955. A jökulhlaup again destroyed the Ring Road bridge of the Múlakvísl, which was only 20 years old. A water level early warning system prompted the closing of the bridge and surrounding area, and no one was harmed. By 11 July 2011, the tremor under Katla had calmed down again. On 15 July 2011, 1,500 people were transported via the Múlakvísl by means of special vehicles. On 16 July, a temporary bridge was put into operation on the river.
|Wikimedia Commons has media related to Múlakvísl.|
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