摘要: In the subtropical monsoon karst regions uplifted in the Quaternary, the cone karst coexists with many kind of topography, such as plains, valleys, depressions, poljes, bank slopes and terraces. This is the major difference between the distribution of the cone karst and the tower karst. The latter is observed only on plains or basins. This situation brings about the idea that there are different origins for cone karst and tower karst. Moreover, the main aspects of cone karst morphology...