Jökulsá á Fjöllum
Template:Short description Template:Infobox river Jökulsá á Fjöllum ({{#invoke:IPA|main}}; "glacial river in the mountains") is the second longest river in Iceland (206 km). Its source is the Vatnajökull glacier. It flows into the Greenland Sea. Jökulsá á Fjöllum streams over the waterfalls Selfoss, Dettifoss, Hafragilsfoss, and Template:Ill, the second of which is the most powerful waterfall in Europe.<ref name="BBC">Template:Cite news</ref>
The source of the river is in the Vatnajökull National Park, one of three national parks in Iceland. The river is located in the northeast of Iceland and forms the eastern boundary of Ódáðahraun, an extensive lava field. Its drainage basin is the largest in Iceland at 7,380 square kilometers.
Glacial flooding
Dettifoss drops into the Jökulsárgljúfur canyon, a feature which, along with the Ásbyrgi gorge, appears to have been formed by catastrophic glacial flooding caused by volcanic activity. The volcano in question was possibly Bárðarbunga, which has been identified as posing the risk of a similar event in the future.<ref>Dettifoss waterfall could be completely reformed by glacial flooding from Bárðarbunga volcano</ref>
The largest jökulhlaups (glacial floods) in Iceland are known to have occurred along Jökulsá á Fjöllum between 7100 and 2000 yr BP.<ref name="QS">Template:Cite journal</ref> The source of these floods were likely eruptions of a major volcano under the Vatnajökull glacier, in the late Holocene. The peak discharge of this flood is estimated to have been Template:Convert.<ref name="QS"/> This can be compared to the flow of the Amazon River, which has an average discharge of Template:Convert.
The latest research concludes that the Jökulsárgljúfur canyon was formed by three flooding events. These key events occurred two, five and nine thousand years ago, separated by millennia of relative stability.<ref name="BBC"/>