结缘胜景
栈道
天窗
石林仙姿
scenory for acquaintance
plank road
Celestial window
Stone fairies
In this cave,chemical deposits developed very
Well,including stalactites,stalagmites,stelae
and stone flowers。Due to composition
differences,stalactites and stalagmites may
appear in different colors。When a stalactite
joins with a stalagmite,a stele is formed。Here
stelae,stalagmites and stalactites form a
large-scale spectacle of underground stone
forest
Glant doline
Couple peake
Underground river
Tourist center
Pagoda trees
Fine cave deposit
Peaks of seven paires
Coral fossil
Music wall(stone curtain)
Pigsy proposing to his love
Fairy land(chemical deposits)
Gravity deposit(cave-in hill)
Longtime corrosion effect kept enlarging the
space within the cave。Under action of gravity,the rock stratum at the top of the cave kept
caving in and formed gravity deposit in the
cave。The cave-in hill developed at the
intersection of two groups of tectonic fissure
with different scales and sizes of rocks and
gravels that caved in。the deposit,which is 25m
Tall and shapen like a hill,is very spectacular
Backbones of two dragons(solution runnels)
Turtle teasing bear
Under longterm of weathering and corrosion,the limestone formed two rocks standing
closely. The bigger one is like a bear stretching
its neck and looking down,while the smaller
one is like a turtle staring at the bear both the
大漏斗
夫妻峰
地洞河
游人中心
槐树荫
洞穴细碎堆积物
羊下山
七女峰
珊瑚化石
音乐壁
八戒求亲
瑶池仙境
重力堆积物
双龙脊背
金龟戏狗熊
bear and the turtle are vivid and interesting,so it
is called turtle teasing bear
石海峰
修女祷告
玻璃鱼
古城废墟
毛狗山
猴子谭
石海迷踪
结缘胜景
天泉洞前洞口
石海涌浪
风动石
穹庐大厦
Peaks among rock sea
A num in prayer
Glass fish
The scientific name of this tadpole-shaped ,,
Remains of ancient city
Fox mountain
Monkey poll
Maze in stone sea
Scenery for acquaintance
Fore entrance of celestial cave
Swell in rock sea
Dome mansion(corrosion hall)
It is the first hall of celestial spring
cave,belonging to the third level of the
natural hall is 30-40 meters high,about 200
meters long and 50-80 meters wide, with an
area of 15000 square meters.
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