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翠华山甘湫池景观地质遗迹成因
引用本文:贺明静,孙根年,于立新.翠华山甘湫池景观地质遗迹成因[J].地球科学与环境学报,2006,28(1):37-40.
作者姓名:贺明静  孙根年  于立新
作者单位:陕西师范大学,旅游与环境学院,陕西,西安,710062
摘    要:甘湫池是翠华山国家地质公园的一个新景点。实地调查发现,整个景区是一座罕见的基岩古滑坡,具有滑坡地貌可观察的景观形态特征。从空间分布和层序关系来看,上覆的崩塌乱石是后期堆积在古滑坡体上,甘湫池应是古滑坡形成的拉伸洼地,并非是由崩塌形成的堰塞湖,同时在景观形态上也与水湫池明显不同,这对于科学认识和开展地质遗迹旅游具有重要的意义。

关 键 词:甘湫池  古滑坡体  拉张洼地  崩积物  翠华山  陕西省
文章编号:1672-6561(2006)01-0037-04
收稿时间:2005-04-08
修稿时间:2005年4月8日

Genesis of Ganqiu Pool Scenic and Geological Remains in Cuihuanshan Mountain
HE Ming-jing,SUN Gen-nian,YU Li-xin.Genesis of Ganqiu Pool Scenic and Geological Remains in Cuihuanshan Mountain[J].Journal of Earth Sciences and Environment,2006,28(1):37-40.
Authors:HE Ming-jing  SUN Gen-nian  YU Li-xin
Abstract:Ganqiu Pool is a new scenic spot in Cuihuashan Mountain National Geo-Park.The site investigation reveals that the whole scenery area is a rarely ancient base-rock landslip with its noticeable features of forms.From the viewpoints of spatial distribution and deposit layer order,the collapsing and scattering rocks covering on the top were piled on the ancient landslip objects afterwards.Therefore,the Ganqiu Pool is a straining depression rather than a weir lake due to the landslip,and the scenic forms are obviously different from that of Shuiqiu Pool.This understanding is fairly important to the scientific cognition and the development of tourism based on the geological remains.
Keywords:Ganqiu Pool  ancient landslip objects  straining depression  collapsing objects  Cuihuashan Mountain  Shaanxi Province
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