$The origin of huangguoshu waterfall can be traced back to the middle Triassic period more than 200 million years ago, when a set of extremely thick carbonate rocks was deposited in huangguoshu area. Huangguoshu waterfall is located in the east wing of the small anticline of wengzhai in a set of `middle Triassic guanling section 2 with a small amount of thin-layer cloud-limestone`. Huangguoshu waterfall formation period of the white river, is a development between 100000-500000 years ago, in the quaternary period, the period of late pleistocene by `wide valley period` to `valley period` in the evolution of river on the ground, because of the Himalayan movement period the earth`s crust after repeated intermittent uplift, base level of erosion caused rivers to drop, causes the river erosion and corrosion incised role to strengthen, there form a `crack` a decrease in bed because of crustal uplift, erosion datum and large structure, lithology and the influence of such factors as turning point, the crack point of fractures, karst cave and underground river development very much.$

huangguoshu waterfall, namely huangguoshu waterfall. called white river falls, also name `yellow geshu waterfall` or `ficus virens

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also called falls ficus geshu huangguoshu name namely river virens waterfall white yellow