| Markarfljót | |
| Pushpin Map: | Iceland |
| Source1: | Mýrdalsjökull |
| Source2: | Eyjafjallajökull |
| Source2 Coordinates: | 63.62°N -19.6133°W |
| Source3: | Tindfjallajökull |
| Source3 Coordinates: | 63.8°N -19.58°W |
| Source4: | Torfajökull |
| Source4 Coordinates: | 63.9167°N -29°W |
| Mouth Location: | near Landeyjahöfn |
| Basin Population: | 1000 plus |
| Tributaries Left: | Hvítmaga, Innri-Botná, Fossá, Þórólfsá, Marðará |
| Tributaries Right: | Innri-Emstruá, Ljósá, Þröngá, Krossá (Markarfljót), Jökulsá, Merkurá, Seljalandsfoss |
Markarfljót (pronounced as /is/) is a river in the south of Iceland. It is approximately long and has had in pre-history jökulhlaups which would be potentially catastrophic, if a similar sized one was to happen in the future.
The Markarfljót rises in the Rauðafossafjöll in Icelandic pronounced as /ˈrœyːðaˌfɔsːaˌfjœtl̥/ massif, east of the volcano Hekla and drains the Grænafjall, Framfjall (to the east) and Emstrur, Almenningar (to the west) basins. The main sources for the river are the glaciers Mýrdalsjökull (including Sléttjökull, Entujökull, Hrútárökull outlet glaciers and the Goðalandsjökull ice margin) and Eyjafjallajökull (including Steinsholtsjökull, Gígjökull and Eyjafjallajökull outlet glaciers). It flows through narrow gorges in the mountainous area between the glaciers Tindfjallajökull and Torfajökull (and Kaldaklofsjökull), which are also sources, then spreads in the wide Markarfljótsaurar sandur plains at Iceland's south coast, near Þórsmörk. The Markarfljót takes its course first north, then west of Þórsmörk and finally empties into the Atlantic west of Eyjafjallajökull.[1]
One of the Markarfljót's tributaries is the river Krossá in Icelandic pronounced as /ˈkʰrɔsːˌauː/, flowing through Þórsmörk, which is notorious for sudden changes in its water level. This river is sourced from the Krossárjökull outlet glacier of Mýrdalsjökull.
The highest discharges ever measured in the Markarfljót were in 1967, during the Steinholt jökulhlaup and then during the 2010 eruptions of Eyjafjallajökull.[2]
There is evidence of at least 10 jokulhlaups down the Markarfljot in the past 7000 years.[3] Prehistoric jökulhlaup discharges have been much higher than recently and completely covered the Markarfljótsaurar outwash plain which means the total river basin of about with a population of over 1000 is at risk from a jökulhlaup of over in size.[2] The tsunami wave hitting the Vestmannaeyjar Islands from such an event has been estimated to be in height and not to cause significant damage off the coast.[3]
The first bridge over the river was opened in 1934 near Litli Dímon in Icelandic pronounced as /ˈlɪhtla ˈtiːˌmɔːn/. It is 242 meters long and was at the time the longest bridge in Iceland. A second bridge was built in 1978 at Emstrur in Icelandic pronounced as /ˈɛmstrʏr̥/. A third bridge was opened in 1992 a few kilometers south of the first bridge.[4]