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富屯溪位于福建省北部,分布于武夷山脉南坡,其为闽江流域上游三大干流之一,发源于邵武桂林、光泽司前两支源头,贯流光泽、邵武、顺昌和南平四个县(市),全长285公里,流域面积13733平方公里。富屯溪由西北向东南偏辖东部。由于地质构造复杂多变,山峦重叠,纵横交错,俗话说:“一滩高一丈,邵武在天上”,“铜延平(今南平)铁邵武,八闽屏障”这几句话概括了闽北山区,地势险要。河道有的曲折,河床多岩礁险滩,水流湍急;有的较宽阔多泥沙,水流缓慢,平静如镜。但每逢雨季水位高涨,落差大,潮流汹涌澎湃,惊涛骇浪,蔚为壮观。溪床底质多卵石浅滩急流,或
Located in the northern part of Fujian Province, Fu Tunxi is located on the southern slope of Wuyishan Mountain. It is one of the three main streams in the upper reaches of the Minjiang River basin. It originated from Shaowu Guilin and the first two sources of Shui Si: Tubular Shine, Shaowu, Shunchang and Nanping County (city), a total length of 285 kilometers, the basin area of 13733 square kilometers. Fu Tunxi from northwest to southeast over the eastern jurisdiction. As the complex and changeable geological structure, overlapping mountains, criss-cross, as the saying goes: “a beach high tenor, Shaowu in the sky,” “Copper Yanping (now Nanping) Iron Shaowu, eight Min barrier” summed up the words of Minbei Mountain, terrain danger. Some twists and turns of the river, the river bed and more rocky reefs, fast-flowing; some more than the more sediment, water slowly, calm as a mirror. However, during the rainy season, the water level is high, the drop is big, the trend is surging, the stormy sea is magnificent. Riverbed bed quality pebbles shoal rapids, or