中文摘要：

在 Huangshan 山的花岗石地形的各种各样的类型在一个同心模式被散布。均夷作用表面的留下的部分在中心；domical 山峰，城堡山峰，削尖的山峰，和山脉因此从中心被安排到圆周。这表明 knick 点仍然在中心附近，中心区域是光线的水系统的普通分歧。在 Huangshan 山的花岗石身体暴露于侵蚀在，这被推断中新世并且上新世，和均夷作用表面那时也被形成。在迟了的上新世在忽视以后高举，切入光的表面被形成。然后，在里面早第四级，有强烈高举并且切口以便深切入的表面被形成。上述过程仍然在进行中，并且在中心区域外面导致高山峰和深峡。由于在中心的有限集水区域，然而，向头的侵蚀是温和的，并且在 Huangshan 山的当前的地形能很长时间被维持。

英文摘要：

The various types of granite landforms in the Huangshan Mt. are distributed in a concentric pattern. The remaining parts of the planation surface are in the center; domical peaks, castle peaks, pointed peaks, and ridges are arranged from the center to the periphery accordingly. This reveals that knick points are still near the center and the center area is the common divide of the radial water system. It is inferred that the granite bodies in the Huangshan Mt. were exposed to erosion in Miocene and Pliocene, and the planation surface was also formed then. After the slight uplift in late Pliocene, a light-incised surface was formed. Then, in early Quaternary, there were intense uplifts and incisions so that deep incised surface was formed. The above process is still in progress, and results in high peaks and deep gorges outside of the center area. However, due to the limited catchment area in the center, headward erosion is mild, and the current landforms in the Huangshan Mt. can be maintained for a long time.