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An aftershock is a smaller earthquake that occurs after a previous large earthquake, in the same area of the main shock. If an aftershock is larger than the main shock, the aftershock is redesignated as the main shock and the original main shock is redesignated as a foreshock. Aftershocks are formed as the crust around the displaced fault plane adjusts to the effects of the main shock.

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The rounded, flowing kana. Hiragana writes native Japanese words, grammar endings, and anything without (or alongside) kanji — it's the first script you learn. Each character stands for one syllable.

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