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贵州省在云贵高原的东部,大地构造是滇桂台向斜和鄂黔台向斜的一部分。境内地形地貌复杂,山峦起伏,丘陵盆地,高山峡谷和宽谷盆地交错分布,具有显著的高原岩溶地貌特征。高原面呈阶梯状上升,海拔高度由600米左右逐渐升高到2300米左右。成土母质类型在山区以残积物和坡积残积物为主。残积风化物以石灰岩风化物分布最广,也有
Guizhou Province is in the east of the Yunnan-Guizhou Plateau. Its tectonic structure is a part of the synclines of the Dian-Gui-Tai and E-Qian-Tai. The terrain is complicated, with undulating hills and valleys, hilly basins, alpine valleys and valleys and valleys, and has obvious plateau karst geomorphologic features. Plateau was a ladder-like rise, the elevation of about 600 meters gradually increased to about 2300 meters. The type of soil parent material is mainly residuals and slope-plot residuals in the mountains. Residues weathering materials to limestone weathering the most widely distributed, there are