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风光旖旎的猴子沟风景名胜区,位于黔中腹地龙里县境内,距县城龙山镇南部13公里,距贵阳53公里。交通、通讯快捷方便。此景区地质构造上属上扬子台褶带的黔南古陷褶断束中的龙里宽背斜。轴部多出露泥盆、石炭系地层,两翼多为二叠、三叠系地层。碳酸盐类地层分布广泛,喀斯特地形广泛发育,景区内喀斯特区占91.1%。在地貌上,景区主要包括台地和峡谷两大类,台地称麻若平台,为喀斯特断块台地,平坦开阔、起伏和缓,海拔多在1500～1600米之间。由于河流切割,台地又
Scenic Monkey River ditch scenic area, located in the hinterland of Longli County, Guizhou Province, 13 kilometers south of the town from Longshan Town, 53 kilometers away from Guiyang. Traffic, communication quick and easy. The geological structure of this area belongs to the Longli Anticline in the fold-breaking fault of Qiannan Paleogene in the upper Yangtze fold. Axis and more exposed Devonian, Carboniferous strata, mostly two Permian, Triassic strata. Carbonate strata are widely distributed, and karst terrain is widely developed. The scenic karst area accounts for 91.1%. In the landform, the scenic area mainly includes two major categories: the platform and the canyon. The platform refers to the Ma Ru platform, which is a platform for the karst fault block. It is flat and open with gentle ups and downs with an altitude of 1500-1600 meters. Due to the river cutting, the terrace again