漂礫

漂礫（glacial erratic），又譯冰川漂礫或冰磧石（glacial moraine）是和周邊石料相比形狀和材質截然不同的天然石塊，小則數厘米，大可達數米甚至數十米，成因是冰川的活動。冰川的搬運能力相當強，一些漂礫甚至被搬運到千百公里之外。^[1]加拿大阿爾伯塔奧克托克斯的巨型漂礫，重達1.5萬噸。

參考文獻

^ Bard, Edouard. Effet de serre et glaciations, une perspective historique (Greenhouse effect and ice ages: historical perspective). Comptes Rendus Geosciences -- External Geophysics, Climate and Environment (Climate) (Copyright © 2004 Académie des sciences. Published by Éditions scientifiques et médicales Elsevier SAS.). June 2004, 336 (7–8): 603–638 [14 December 2009]. Bibcode:2004CRGeo.336..603B. doi:10.1016/j.crte.2004.02.005.

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[Bard2004-1] Bard, Edouard. Effet de serre et glaciations, une perspective historique (Greenhouse effect and ice ages: historical perspective). Comptes Rendus Geosciences -- External Geophysics, Climate and Environment (Climate) (Copyright © 2004 Académie des sciences. Published by Éditions scientifiques et médicales Elsevier SAS.). June 2004, 336 (7–8): 603–638 [14 December 2009]. Bibcode:2004CRGeo.336..603B. doi:10.1016/j.crte.2004.02.005.

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