Shengren Waterfall is located on Shuangsi River. When the tributary Shuangsi ditch into the mainstream Shuangsi place, because the mainstream flow is greater than the tributary flow of 2.7 times, the next cut deep, resulting in the main tributaries of the valley gap, and the formation of suspended trailers. Waterfall is about 10 meters wide and about 3 meters wide.
Waterfall on both sides of the rock exposed, rock formations for the Talio formation sandstone, shale alternately arranged, strata towards the northeast - southwest, the level of the southeast tilt about 13 degrees. There are shallow waterfall at the bottom of the lake, there are large stone can be on the side of the lake, overlooking the waterfall, and some landscape.
Shengren waterfall in the Ch’ing Archives known as the "half of the spring", the Japanese Occupation Period was renamed "sage Taki", now most people used to call "Shengren waterfall", bridges, water, breeze, birds, fish, tourists, interwoven into a fresh and moving , Pleasant view of the natural scenery.
Standing on the small bridge on the main stream of Shuangsi , upstream to observe the formation of the river bed, like a ladder in general, this is because the river erosion of the results, and only the formation of sedimentary rocks will be layered, igneous rock is not layered.
Shuangsi mainstream cross-strait lithology is not the same, the east (left) shore for the sedimentary rock, west (right) shore for the Tatun volcano group eruption caused by igneous rocks. And the junction of the two strata is where the fault passes.
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