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Pencil cleavage : ウィキペディア英語版 | Pencil cleavage
Pencil cleavage in geology refers to a cleavage in rock such that long, slender, pencil-shaped fragments of rock are created by fracturing during the weathering of a sedimentary rock. Pencil cleavage is usually associated with rock units that contain high angle of intersection between cleavages, such as a diagentic cleavage and a later tectonic cleavage. ==See also==
*Cleavage (geology)
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Pencil cleavage」の詳細全文を読む
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