漢拏山
Halla
楯状火山 · South Korea · 1919m

- タイプ
- 楯状火山
- 国
- South Korea
- 地域
- Eastern Asia Volcanic Regions / Central East Asia Volcanic Province
- 標高
- 1919m
- 座標
- 33.361, 126.530
- 最終噴火
- 1007年
- テクトニクス環境
- Intraplate / Continental crust (> 25 km)
- 火山地形
- Shield
- 主要岩石
- Basalt / Picro-Basalt
地質学的概要
The massive Halla shield volcano forms much of the 40 x 80 km Cheju (Jeju) Island, which lies 90 km S of the Korean Peninsula. Eruptions during the Pliocene and Pleistocene built a lava plateau above the roughly 100-m-deep continental shelf on which the basaltic-to-trachytic edifice was constructed. A 400-m-wide crater truncates the summit. About 360 late-Pleistocene and Holocene basaltic cones across the flanks were erupted primarily along the long axis of the ENE-WSW-trending island. Most of these are scoria cones, but about 20 along the coast or offshore are Pleistocene-to-Holocene tuff rings and tuff cones; lava domes also occur. The latest two eruptions took place during the 11th century.
Wikipedia の要約
英語版の要約Hallasan (Korean: 한라산) is a shield volcano comprising much of Jeju Island in South Korea. Its summit, at 1,947 m (6,388 ft), is the highest point in the country. The area around the mountain is a designated national park, named Hallasan National Park. Hallasan is commonly considered to be one of the three main mountains of South Korea, along with Jirisan and Seoraksan.
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噴火履歴
詳細タイムライン
- 1007年VEI ?観測記録1007 ~ 進行中
- 1002年VEI ?観測記録1002 ~ 進行中
- 紀元前 2050年 (±200年)VEI ?地質学的推定BCE 2050 ~ 進行中SW flank (Songaksan tuff ring)
- 紀元前 2830年 (±50年)VEI ?地質学的推定BCE 2830 ~ 進行中NE flank (Ilchulbong tuff cone)
外部リンク
⚠ 参考情報です。緊急対応には使用しないでください。