本文へスキップ
← 地図に戻る
⇄ 比較

Nabukelevu

溶岩ドーム · Fiji · 791m

The summit of Nabukelevu lies between the two clouds near the center of this NASA International Space Station image and is located at the SW end of Kadavu Island at the southern end of the Fiji archipelago. Debris avalanches from collapse of the Mt. Washington lava dome complex reached both the northern coast to the right of Cape Washington (the small peninsula at the upper left) and horseshoe-shaped Daviqele Bay (bottom center) and the south. Block-and-ash flows from dome growth and collapse have occurred within the past few hundred years.
The summit of Nabukelevu lies between the two clouds near the center of this NASA International Space Station image and is located at the SW end of Kadavu Island at the southern end of the Fiji archipelago. Debris avalanches from collapse of the Mt. Washington lava dome complex reached both the northern coast to the right of Cape Washington (the small peninsula at the upper left) and horseshoe-shaped Daviqele Bay (bottom center) and the south. Block-and-ash flows from dome growth and collapse have occurred within the past few hundred years. · 写真: NASA International Space Station image ISS006-E-7466, 2002 (http://eol.jsc.nasa.gov/). · Wikimedia Commons
タイプ
溶岩ドーム
国
Fiji
地域
Southwestern Pacific Volcanic Regions / Fiji Volcanic Arc
標高
791m
座標
-19.118, 177.982
最終噴火
1660年
テクトニクス環境
Subduction zone / Crustal thickness unknown
火山地形
Minor (Silicic)
主要岩石
Andesite / Basaltic Andesite
地質学的概要

The andesitic-to-dacitic Nabukelevu lava-dome complex occupies the SW end of Kadavu Island at the S end of the Fiji archipelago. The high point of the complex is Mt. Washington, an andesitic lava dome. Flat-lying dacitic lava flows are found at Cape Washington along the W coast and at Talaulia Bay on the NE coast. NNE-trending faults cut the complex in several locations and define its E boundary. The dome complex is cut by several collapse scarps, which were the source of debris avalanches that have incorporated human artifacts and remains. Debris avalanches have entered the sea on the both the N and S sides of the volcano. Onshore and offshore deposits as well as native legends indicate that several eruptions have occurred during the Holocene. Block-and-ash flows related to dome growth have occurred within the past few hundred years.

Wikipedia の要約

英語版の要約

Nabukelevu also known as Mt. Washington is a potentially active lava dome complex volcano located on the southwest portion of Kadavu Island in Fiji. It is 805 metres (2,641 ft) tall, and last erupted around 1660. It has formed lava domes

Wikipedia · CC BY-SA · 記事全文を読む →

噴火履歴

概要 (VEI時系列)
バーをクリックすると個別の噴火が表示されます
580 BCE~393 BCE · 1件 · 最大 VEI ?167~353 · 1件 · 最大 VEI ?1473~1660 · 1件 · 最大 VEI ?580 BCE20 BCE5409131473

詳細タイムライン

  1. 1660年 (±30年)VEI ?地質学的推定
    1660 ~ 進行中
    Dome NW of summit
  2. 340年VEI ?地質学的推定
    340 ~ 進行中
    West side of summit dome complex
  3. 紀元前 580年 (±300年)VEI ?地質学的推定
    BCE 580 ~ 進行中
    Summit lava dome

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。