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小雄溪,位于福建省东部永泰县塘前乡官烈村南1.5公里,是大樟溪一条支流,溪长约4公里,溪流由南东流向北西,汇入大樟溪,再向北东注入闽江分支乌龙江。小雄溪北距福州市区40公里,西通永泰方广岩老旅游区15公里;西南邻莒口旅游点3公里;东北沿正在建设中的316国道过江口大桥直抵十八重溪(见本刊1993年2期),距五虎山风景区15公里;西北通南屿旗山、福州金山寺旅游区20公里,水陆交通四通八达。官烈小雄溪一带,大面积出露距今一亿多年的白垩系石帽山群地层,由陆相火山喷发岩—流纹岩、熔结凝灰岩、粗面岩与凝灰质砂砾岩、粉砂岩、英安岩等一大套岩石组成,岩石坚硬不一,几经沧桑世变,形成层峦叠嶂,崎岖陡峻的悬崖峭壁,嶙峋多姿,形态万千。溪谷绘横交错,山花四时不绝、群鸟啾啾,
Small Xiongxiu, located in the eastern part of Yongtai County, Fujian Province, Tong Qian Xiang, Crown Village 1.5 kilometers south, is a branch of the Big Zhangxi, about 4 km long stream, stream flows from the south to the northwest, into the large Zhangxi, and then into the North East Fujian Jiang Branch Oolong River. Xiaoxiong Creek is 40 kilometers away from downtown Fuzhou, 15 kilometers from the old tourist area of Fangtaiyan in the west of Yongtai, 3 kilometers from the tourist spot of the southwest neighbor to the mouth of the mouth, and to the 18th heavy river along the crossing of the No.316 National Road in the northeast 1993 2), 15 km away from the Wuhushan Scenic Area; Northwest Yantai Qishan, Jinshan Temple in Fuzhou tourist area 20 km, water and land transportation in all directions. In the area of the Guanliexiongxiong, the cretaceous Cretaceous Himanshan Group stratum, with a large area of over 100 million years ago, is composed of continental volcanic eruption rock-rhyolite, melted tuff, trachyte and tuffaceous conglomerate, Siltstone, dacite, a large set of rock composition, the rock is hard and evil, after many vicissitudes, the formation of overlapping peaks, rugged steep cliffs, magnificent, thousands of shapes. Valley painted cross staggered, Yamaha never stop, birds tweeted,