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A dike or dyke, in geological usage, is a sheet of rock that formed in a fracture in a pre-existing rock body. Dikes can be either magmatic or sedimentary in origin. Magmatic dikes form when magma intrudes into a crack then crystallizes as a sheet intrusion, either cutting across layers of rock or through an unlayered mass of rock. Clastic dikes are formed when sediment fills a pre-existing crack.

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Hiragana

ひらがな

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.

Example

ねこ — cat