河北省嶂石岩风景区的造景地貌及其演化  

Tectonic and geomorphic changes of Zhangshiyan tourism landforms, Hebei Province

作　　者：吴忱[1] 许清海[1] 阳小兰[1] 

机构地区：[1]河北省科学院地理研究所,石家庄050011

出　　处：《地理研究》2002年第2期195-200,共6页Geographical Research

基　　金：国家自然科学基金资助项目 (4 93710 0 8;40 1710 95 )

摘　　要：嶂石岩风景区的地貌形成于 37MaBP之后 ,由早第三纪、晚第三纪、第四纪三期地貌旋回组成。每期旋回中又遗留下了演化阶段不同的造景地貌。它们各具特色 ,奇、险、壮、美 ,为我国北方不可多得的宝贵地貌自然遗产。Zhangshiyan of Hebei Province is a national tourist scenic spot. It has many strange, perilous, graceful and beautiful geomorphic types. They were formed since 37 MaB.P., and experienced three major geomorphic cycles during the Early Tertiary, the Late Tertiary and the Quaternary eras and left many geomorphic types of different evolutional stages of infancy, youth, maturity and old age. The major evolution patterns were strong tectonic uplift, collapse, side and headward erosion, and raze. The rocks of sandstone and limestone also played an important role in landform evolution. The predominant geomorphic evolution situation in future will still be infancy stage to youth stage for a long period of time. But as tourism developed, the strange and beautiful scenic spots of maturity stage development level are more liable to be destroyed by tourists. So, how to prevent these geomorphic types from being destroyed is a pressing issue.

关 键 词：嶂石岩风景区 地貌自然遗产 河北 地貌结构 

分 类 号：P931[天文地球—自然地理学]