オアカルデラ

Shala

カルデラ · Ethiopia · 2075m

The eastern (right) side of the darker Lake O'a (Lake Shalla) forms the 17-km-wide O'a caldera. Post-caldera activity produced cones N of the caldera. The small light blue-green Chitu maar on the W side of the lake was erupted in an area of Holocene vents along the Corbetti-Shalla fissure system extending N from Corbetti caldera. Fumarolic activity continues along the S and E shores. · 写真: NASA International Space Station image ISS001-363-7, 2001 (http://eol.jsc.nasa.gov/). · Wikimedia Commons

タイプ: カルデラ
国: Ethiopia
地域: Eastern Africa Volcanic Regions / Main Ethiopian Rift Volcanic Province
標高: 2075m
座標: 7.457, 38.557
最終噴火: 不明
テクトニクス環境: Rift zone / Continental crust (> 25 km)
火山地形: Caldera
主要岩石: Rhyolite

地質学的概要

The Shala (also known as O'a) caldera along the central Main Ethiopian Rift forms the eastern portion of the 15 x 25 km Lake Shala. Formation of the caldera about 240,000 years ago was accompanied by the eruption of two ignimbrite deposits, the first of which was strongly welded. The only post-caldera activity consists of two pyroclastic cones to the N, one silicic and the other basaltic, and a group of tuff rings, spatter cones, and lava flows of Holocene age near the SW shore of the lake. These were erupted along the Corbetti-Shalla segment of the Wonji Fault Belt, which extends N from Corbetti caldera. Fumarolic activity continues on all sides of the lake.

Wikipedia の要約

英語版の要約

The O'a Caldera, also known as Shala, is a volcanic caldera in Ethiopia. It has two lakes: Lake Shala and a small maar called Lake Chitu. Sub-features include Mount Fike and Mount Billa.

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