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贵州省地处北纬24°30′～29°13′,是云贵高原中西起103°31′E,东延至109°30′E的高原东侧的梯级大斜坡,隆起在四川盆地和广西丘陵之间。地势东低西高,南北低,中部高,平均海拔在1,000米左右。省的西部大部分为海拔2,200米以上起伏较大的山原,由此向北、东、南倾斜,河流也分别向三方流去。中部为起伏较小的黔中丘陵高原,海拔为800～1,300米左右,是贵州高原的主体,成为长江与珠江水系的分水
Located between latitude 24 ° 30 ’and 29 ° 13’, Guizhou Province is a large-scale step slope to the east of the plateau where the central and western Yunnan-Guizhou Plateau extends from 103 ° 31’E to eastward to 109 ° 30’E, and rises in the Sichuan Basin and Guangxi hilly between. East low-lying topography, low north-south, central high, with an average elevation of 1,000 meters. Most of the western part of the province is a mountainous area with a large fluctuation of 2,200 meters above sea level. As a result, northward, eastward and southward slopes lead to the tributaries of the rivers. The central part of the Central Guizhou Province has a small elevation of 800 ~ 1,300 meters above sea level, and is the main part of the Guizhou Plateau. It becomes the watershed of the Yangtze River and the Pearl River