It is a waterfall composed of white quartz sandstone, reddish brown, brownish gray; fine to medium grain size, good grading, good roundness, good binding, and firm texture. It shows the laying of oblique layers in the temple stone category, and shows the rocky features caused by the erosion process of the waterways scattered everywhere, with sand cracks that are important geographic points. The slope of the waterfall is about 30 degrees. The waterfall flows to the south 200 degrees.