为墙状砂岩地貌景观，是由于地壳运动抬升及水流沿一组节理裂隙侵蚀、崩塌而形成。峰墙达20余条，长60～300m，高80～300m，宽0.5～5m，交错耸峙，雄浑绮丽，蔚为壮观。 It is scenery of wall-like sandstone landscape. Totally more than 20 peak walls, with lengths of 60 - 300 m, heights of 80 - 300 m and widths of 0.5 – 5 m. Peak walls are interlaced, towered and very spectacular. It is a result of the crust uplifting, water cutting along joints and the sandstone falling down along the certain directions.