Magma chamber - Magma chamber
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In volcanoes that undergo central eruptions, it is believed that the magma generated deep underground first accumulates 2 to 4 km underground, where it differentiates, and then erupts repeatedly whenever the gas pressure increases. This accumulation is called a magma chamber. Source : Heibonsha Encyclopedia About MyPedia Information |
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中心噴火をする火山では，地下深所で発生したマグマは，地下２〜4kmのところに一度たまり，ここで分化し，ガスの圧力が高まるごとに噴火を繰り返すと考えられている。このたまりをマグマ溜りという。
出典 株式会社平凡社百科事典マイペディアについて 情報 |
>>: Mac-Mahon, Marie-Edme-Patrice Maurice de, Duc de Magenta
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