| 庐山地貌新思考 |
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| 引用本文： | 沈方.庐山地貌新思考[J].唐山师范学院学报,2002,24(2):77-78,81. |
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| 作者姓名： | 沈方 |
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| 作者单位： | 唐山师范学院,物理系,河北,唐山,063000 |
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| 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水成地貌，第四纪既水冰川也无泥石流的发生。
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| 关 键 词： | 庐山 地貌 地质演变 红壤 飞来石 地质 |
| 文章编号： | 1009-9115(2002)02-0077-02 |
Physiognomy of Lushan Mountains |
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| SHEN Fang.Physiognomy of Lushan Mountains[J].Journal of Tangshan Teachers College,2002,24(2):77-78,81. |
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| Authors: | SHEN Fang |
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| Abstract: | 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. |
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| Keywords: | landforms of Lushan mountains geologic history red barnyard glacier table |
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