located in the center of karst area in southwest china, guizhou is one of the districts whose karst physiognomy well developed and concentrative distributed.
贵州地处中国西南喀斯特分布的中心,是我国西南喀斯特地貌发育最充分、分布最集中的地区之一。
this paper expatiates on the formation conditions and mechanism, analyses the forming reasons of karst physiognomy in specific areas in china, introduces the varieties and distributing areas.
阐述了喀斯特地貌的形成条件及其机制,对我国特定地区喀斯特地貌的形成原因作了分析,并且介绍了其发育的种类和分布地区。
mesa-canyon karst physiognomy is a peculiar one first discovered in fenghuang national geopark.
台地峡谷型巖溶地貌是湖南凤凰国家地质公园内特有的巖溶地貌。