流路
dc.contributor | 國立臺灣師範大學僑生先修部 | zh_TW |
dc.contributor.author | 路上雅賢 | zh_TW |
dc.contributor.author | 曾慶鳳 | zh_TW |
dc.contributor.author | 梁李青 | zh_TW |
dc.contributor.author | 史子晉 | zh_TW |
dc.contributor.author | 高麗珍老師指導 | zh_TW |
dc.date.accessioned | 2019-12-18T08:37:30Z | |
dc.date.available | 2019-12-18T08:37:30Z | |
dc.date.issued | 2019-11-28 | |
dc.description.abstract | 地表流水是塑造地貌最重要的外營力。在流動的過程中,不僅侵入地面形成溝谷,將被侵蝕下來的物質,搬運、堆積,形成平原。 | zh_TW |
dc.identifier | nups_sw_201911_06_019 | |
dc.identifier.uri | https://www.google.com/maps/d/viewer?mid=1ApW6eLc0UA_yhHz0sbQ3--ctAyfkG95y&shorturl=1&ll=25.069087932430133%2C121.40003110643806&z=17 | |
dc.identifier.uri | http://rportal.lib.ntnu.edu.tw:80/handle/20.500.12235/108924 | |
dc.relation | 現代徐霞客之林口探索地圖與影像特展 | zh_TW |
dc.title | 流路 | zh_TW |
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