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Snake coils (geology) : ウィキペディア英語版 | Snake coils (geology) Snake coils is a descriptive term used by physical geologist and glaciologists to describe the "snake coil"-like shape that occurs along certain ablation lines. Essentially miniature tunnel valleys, the peculiar natural shapes were first described by French Geologist Jean-Jerome Peytavi in 1973 during an expedition to northern Greenland, and later confirmed by a team of Danish geologists. It is believed that snake coils are formed through the same mechanism as tunnel valleys. ==References==
*Benn, D.I. & Evans, D.J.A. ''Glaciers & Glaciation''. Hodder Arnold Pubs; (1998). *Plummer, Charles C., ''Physical Geology''. McGraw-Hill; 10 edition (2004). *Tarbuck, Edward J., ''Earth: An Introduction to Physical Geology''. Prentice Hall; 8 edition (2004).
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「Snake coils (geology)」の詳細全文を読む
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