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caldera

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After the last caldera-forming eruption 23,000 years ago several smaller vents within and around the caldera have seen eruptive activity.
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The subsidence of the summit to form the central caldera and the extraordinarily energetic earthquakes accompanying the 1912 eruption are evidence of this.
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The youngest and fourth caldera is the world's largest Quaternary caldera (100by30 km) and intersects the three older calderas.
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The summit of the mountain is composed of tuff ejected by the more recent caldera-forming eruption, rather than of subsequent volcanic ejecta.
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This was identified as a caldera, which had formed by the collapse of the volcano's previous summit during the cataclysmic eruptions.
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A smaller, kidney-shaped caldera (about 65km mi by 45km mi) lies in the southern half of the larger one.
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Hot springs, streams, fumaroles, natural gas seeps and volcanic domes dot the caldera floor landscape.
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During this eruption 2007 a caldera collapse occurred at the volcano.
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The summit at the center of the island is dominated by a desert-like caldera, which covers an area of 100 km2.
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The eruption that created the current caldera occurred around 7,000 years ago.
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