アイスランド · 火山原
Helgrindur
- タイプ
- 火山原
- 標高
- 986m
- 最終噴火
- 不明
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- タイプ
- 火山原
- 国
- アイスランド
- 地域
- 大西洋 / Iceland Neovolcanic Rift Volcanic Province
- 標高
- 986m
- 座標
- 64.866, -23.283
- 最終噴火
- 不明
- テクトニクス環境
- リフト帯 / 海洋地殻 (< 15 km)
- 火山地形
- 火山群
- 主要岩石
- 玄武岩 / ピクライト質玄武岩
地質学的概要
Helgrindur (also known as Lysuhóll or Lysukard) is one of Iceland's smallest volcanic systems. It consists of a chain of small alkali olivine basaltic cinder cones and vents along a WNW-ESE line cutting across the central Snaefellsnes Peninsula in western Iceland. The slightly arcuate line of Quaternary vents extends to the northern coast of the peninsula. Helgrindur is the central of three volcanic systems occupying the peninsula. The latest eruption is undated, but the system has been active during the Holocene.
Wikipedia の要約
英語版の要約Helgrindur is a volcanic mountain range or massif in the middle of the Snæfellsnes peninsula that provides a backdrop to the port of Grundarfjörður. The volcano can be regarded as potentially active, with a risk of lava flows and much more rarely explosive tephra eruptions. The range with its prominent peaks, of Tröllkerling at 891 m (2,923 ft) in its south-east, Böðvarskúla at 988 m (3,241 ft) and Kaldnasaborgir (Kaldnasi) in its north-west at 986 m (3,235 ft) is popular with hikers or mountaineers.
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