“喀斯特”是世界通用的地理学专业术语,原来是南斯拉夫西北部的利亚半岛上石灰岩高原的地名,后来南斯拉夫学者J·斯维奇(J.Srirrc)研究利亚半岛上的石灰岩地貌,并把这种地貌称为喀斯特地貌。我国把石灰岩岩溶地貌统称为喀斯特地貌。喀斯特地貌是石灰岩基石中的碳酸物质经长期的风化、侵蚀等化学作用和地球重力的垂沉影响,经过长期的日晒、风吹、雨淋形成的特珠地貌。在这里环境恶劣、土壤瘠薄,经过多年在 Karst, a generic term geographed in the world, turned out to be the place name of the limestone plateau on the Liaja Peninsula in northwestern Yugoslavia. Later, Jr. Schrrrr, a Yugoslav scholar, studied the limestone landscapes in the Liarian Peninsula. Called this kind of landform karst landform. Limestone karst landforms are collectively referred to as karst landforms. The karst landform is the special pearl landform formed by the long-term weathering, erosion and other chemical effects of the carbonaceous material in the limestone basestone and the gravity of the earth. Poor environment here, barren soil, after years