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    龟山印象

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      鲕粒灰岩Oolitic limestone
      龟山-老鹰石
      龟山-滴水洞
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    龟山-望龙洞
     
    据望龙洞碑记,望龙洞洞口直对蛇山,蛇为小龙,故称望龙洞。
       望龙洞位于龟山南端,发育于张夏组下灰岩段厚层鲕状灰岩中,沿一东西向张裂隙溶蚀发育而成。洞体宽一般1m左右,高2~15m不等,长约600m。洞体两壁陡直,洞内有多处近南北向小洞与之相连,形成洞中洞,洞连洞。洞内石钟乳和石笋等次生沉积物发育,千姿百态,栩栩如生。
       WANGLONG Cave
       According to the stele records, the Snake hill is opposite to the cave, the snake is called little serpent in China, so the cave called WANGLONG Cave.
       The cave is located in the south of the Tortoise Mountain, is developed in the thick layer of oolitic limestone of the lower part of Zhangxia Group, along an east-west tension cracks. The cave generally about 1m wide, ranging from 2 ~ 15m high, about 600m long. The cave walls are steep, connected with many north-south holes, formed the phenomenon of hole in hole, hole with hole. There are stalactites and stalagmites and other secondary sediments in the cave, varied and lifelike.

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