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Dyngjujökull : ウィキペディア英語版 | Dyngjujökull
Dyngjujökull glacier is an outlet glacier of the Vatnajökull glacier in Suður-Þingeyjarsýsla, Northeastern Region, Iceland. The glacier is in the Icelandic Highlands and is situated between Bárðarbunga, Holuhraun and Kverkfjöll. Meltwater from the glacier flows into Jökulsá á Fjöllum, the second longest river in Iceland. Depressions discovered by scientists, on 6 September 2014, have prompted speculation that eruptions may be occurring below the surface of the glacier. This is associated with seismic activity at the Bardarbunga caldera, a large volcanic structure located beneath the glacier.〔http://en.vedur.is/earthquakes-and-volcanism/articles/nr/2947〕 ==References==
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Dyngjujökull」の詳細全文を読む
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