由冰川作用塑造的地貌。属于气候地貌范畴。地球陆地表面有11%的面积为现代冰川覆盖，主要分布在极地、中低纬的高山和高原地区。第四纪冰期，欧、亚、北美的大陆冰盖连绵分布，曾波及比今日更为宽广的地域，给地表留下了大量冰川遗迹。
太白山是我国东部古冰川地貌保存较好的山地。
The ancient glacial remains in Taibaishan was glacial relief area, which was remained very well in the East of China.
在太白山及其邻近地区的高山带，分布着大量的古冰川地貌。
There are abundant traces of ancient glaciation distributed on the high mountain belt of the mount Tai-Bai and its near areas.
“大理冰期”的概念被提出以来，其命名地——点苍山的冰川地貌并未经过系统的研究。
In a so long time after the conception of "Dali Ice Age" was put forward, the place where this name came from, Diancangshan, had not been investigated and researched for its glacial geomorphology.
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