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夷平面是在地壳长期稳定的条件下，起伏的地表受风化和流水的削高补底作用而逐渐变的平坦，后经地壳运动抬升到高处的平坦地形，对面张家界一级夷平面位于海拔1200m左右，形成于始新世晚期—渐新世。When the earth’s crust is in a long-term stable period, the uneven earth’s surface gradually became even because weathering and runoff erosion can cut down higher parts and fill up lower parts. Then the even surface was lifted up by crustal movement and form a flat terrain, which is called the planation surface. This planation surface is about 1,200m above sea level and was formed between the late Eocene and the Oligocene.

是基部相连成呈簇分布的连座石峰，它是经由石墙进一步侵蚀演变而来的，是石峰林的早期发育阶段。The stone peak cluster consists of stone peaks whose bases are connected. Formed from the rock dyke by further erosion, the stone peak cluster represents the early stage of the development of the stone peak forest.

由于地表水沿成岩孔隙、构造节理扩大溶蚀形成。它可以分散成单个出现,也可以由许多溶孔组合成蜂巢状。该处溶孔为单个出现，溶孔不断被侵蚀由小变大，最终形成溶洞。A dissolution pore is formed by surface water eroding along and eapanding a diagenetic hole or a tectonic joint. Dissolution pores may appear individually, or many dissolution pores appear together forming a honeycomb structure. This single dissolution is eroded continuously and becomes bigger and bigger and may finally become a cave.

瀑布是水流流过悬崖式河床、溪谷发生倾泻现象。此处瀑布是灰岩中地下水在出口处从悬崖向下倾泻而成，由于水量小，形成线状的珠帘式瀑布。A waterfall is a place where water from a river or stream falls down over a cliff or rock. The underground water flows out from an outlet in the limestone and falls down over the cliff, forming this waterfall. This waterfall is like a bead curtain because the water yield is small.

溶洞是碳酸盐岩区地下水沿着岩层层面和裂缝进行溶蚀、侵蚀而形成的地下洞室。A karst cave is a hollow place in the ground formed by underground water corroding and eroding along the stratum surface or fissures in carbonate rocks.

在软硬相间的层状岩石中，由于抗风化能力的不同，易遭风化的岩石风化速度快，形成凹凸不平的槽穴，抗风化能力强的岩石凸出在外。In the stratified rock consisting of softer layers and harder layers, because of different weathering resistance, the softer layers are weathered more easily and quickly, forming a uneven groove, while harder layers protrudes from the surface.

此地有两处洞穴，并非自然形成的溶洞，而是在二叠系梁山组地层中采煤后废弃的坑道。The two holes here are not naturally formed caves, but abundant coalpits in the stratum of Permian Lianshan Formation.

地表河流流经地下的潜伏段后重新转为地表河流的出口，旱季此处水流不明显，雨季可见水流涌出。This is the outlet where a surface stream flows through an underground segment and reappears. In dry season there is barely any water here but in rainy season water can be seen flowing out.

伏流是地表河流经过地下的潜伏段，此处为伏流的入口，旱季此处水流不明显，雨季可见水流涌入。A swallet is an opening through which a stream disappears underground. In dry season there is barely any water here but in rainy season water can be seen flowing in.

此处为武陵源著名观景台，台分三级，凌空而观，谷间群峰竟立，数十余座似四十八将军校场阅兵点将场面，谷底悠悠，鸟鸣如歌，蝉奏如琴，交响成曲，声扬空谷，晴初日出，岩石生辉，雨后雷佘，雾起风浮。Here is a famous viewing platform of Wulingyuan. Seen from the platform the peaks in the valley resemble the troops to be reviewed by the commander. Birds and cicadas sing in the valley, composing a symphony. When the sun comes out after rain the rocks shines in sunlight and fog raise from the valley, forming a beautiful landscape painting.