摘要
在对庐山地质演变、山顶土壤和几处典型地貌分析的基础上,提出一种猜想:庐山地貌可能是温暖湿润的气候条件下的水成地貌,第四纪既无冰川也无泥石流的发生。
The author bases a guess on the analysis of soil at the mountaintop and several typical landforms at the Lushan mountains: the landforms of Lushan mountains is shaped under the warm and moist climate, or is shaped by water eroding glaciation formed earlier.
出处
《唐山师范学院学报》
2002年第2期77-78,81,共3页
Journal of Tangshan Normal University
关键词
庐山
地貌
地质演变
红壤
飞来石
地质
landforms of Lushan mountains
geologic history
red barnyard
glacier table
