喀拉喀托之子——阿那喀拉喀托在较为温和的喷发中稳定成长。

Anak Krakatau (' Child of Krakatau ') has been growing steadily through milder eruptions.

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一些以前爆发的火山，如爪哇喀拉喀托火山，就是由岩浆与水接触引起的。

Some of the most violent past eruptions, like Krakatoa in Java, resulted from magma coming in contact with water.

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注意到如皮纳图和喀拉喀托等大型火山爆发后是小幅度但很显著的气温下降。

Note that large volcanoes, like Pinatubo and Krakatoa, were followed by a fractional — but significant — drop in temperature.

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