堆積

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dc.contributor國立臺灣師範大學僑生先修部zh_TW
dc.contributor.author項黎映仁zh_TW
dc.contributor.author歐陽佩沁zh_TW
dc.contributor.author嚴國鋒zh_TW
dc.contributor.author黎日成zh_TW
dc.contributor.author高麗珍老師指導zh_TW
dc.date.accessioned2019-12-18T08:37:26Z
dc.date.available2019-12-18T08:37:26Z
dc.date.issued2019-11-28
dc.description.abstract當河流發生流速降低，流量減少泥沙增加流水特性的變化時，導致河流的堆積作用，有沖積扇、氾濫平原山角洲，台灣平原主角。zh_TW
dc.identifiernups_sw_201911_06_014
dc.identifier.urihttps://www.google.com/maps/d/viewer?mid=14dMlwtGaO1W7yt5VmjEZmXKZEs7dX_3v&shorturl=1&ll=25.069029927958223%2C121.40490090852609&z=17
dc.identifier.urihttp://rportal.lib.ntnu.edu.tw:80/handle/20.500.12235/108919
dc.relation現代徐霞客之林口探索地圖與影像特展zh_TW
dc.title堆積zh_TW

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