Fláajökull

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Fláajökull is a glacier located in the eastern region of Iceland. It is a prominent outlet glacier of the larger Vatnajökull, the largest ice cap in Iceland and one of the largest in Europe. The glacier is notable for its dramatic changes and rapid retreat in recent years, which has been attributed to global warming.

Geography[edit | edit source]

Fláajökull is situated in the Hornafjörður district of southeastern Iceland. It descends from the northwestern part of Vatnajökull, flowing down towards the valley below. The glacier's tongue currently reaches an altitude of approximately 100 meters above sea level.

Glacial Retreat[edit | edit source]

Fláajökull has been the subject of extensive study due to its rapid retreat. Over the past century, the glacier has retreated by over 2 kilometers, with the rate of retreat increasing in recent years. This retreat has resulted in the formation of a proglacial lake at the glacier's terminus.

Ecological Impact[edit | edit source]

The retreat of Fláajökull has had significant ecological impacts. The newly exposed land has been colonized by a variety of plant species, leading to changes in local biodiversity. Additionally, the retreat of the glacier has affected local hydrology, with potential impacts on local water resources.

See Also[edit | edit source]

References[edit | edit source]

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Contributors: Prab R. Tumpati, MD