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Fagraskógarfjall | Grettisbæli

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This 382 m high hill is composed of hyaloclastite rocks: they have formed due to volcanic activity beneath a Pleistocene glacier.

Location
View on OpenStreetMap
Created
on Monday 9 September 2019 by Martin Mergili
Region
Visits and license
2367 visits, CC BY-NC-SA 4.0 DEED license