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“江作青罗带,山如碧玉簪”这是对秀丽的桂林山水之神姿仙态的逼真写照。她那挺拔奇异的群峰,清澈明净的流水,玲珑瑰丽的洞府,真不愧为大自然天工雕塑的艺术佳作。然而,在三亿二千五百万年前,这里是汪洋一片的近海。由于海水的侵入,有大量的碳酸盐沉积物。约二亿到一亿八千万年前,中、晚三叠世之间,地壳的变化,剧烈的造山运动,即规模和强度超过唐山大地震万倍的印支期构造运动将桂林凸起变成大陆。这样,经过漫长岁月的风化、剥蚀,水流的切割和雨水的溶蚀、掏蚀,使之逐渐形成了峰林、峰丛、地下河和溶洞。因此,构成了万象森罗的景观,成为典型的岩溶发育模式。
“Jiangzuo Qingluo, mountains such as jade hairpin ” This is a realistic portrayal of the beauty of the goddess of landscape in Guilin. Her straight peaks singular peaks, clear and clean water, exquisite magnificent Dong Fu, really deserved to be a masterpiece of natural heavenly sculpture. However, it was a sea of vast ocean near 325 million years ago. Due to the intrusion of seawater, there is a lot of carbonate sediments. From about 200 million to 180 million years ago, during the middle and late Triassic, the crustal changes and the intense orogeny, that is, the Indosinian tectonic movement whose scale and intensity surpassed the Tangshan earthquake tended to Guilin Become the mainland. Thus, after a long period of weathering, erosion, water cutting and rain erosion, erosion, so gradually the formation of peaks, peaks, underground rivers and caves. Therefore, the landscape of Vientiane Moro constitutes a typical karst development pattern.