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兴文世界地质公园位于四川盆地南缘与云贵高原过渡带兴文县境内,兴文气候温润,降水丰沛。距今4.6亿年以来,这里沉积了巨厚的碳酸盐岩,由于地表水和地下水在岩石的裂隙与节理之间相互转化、彼此切换,共同构成园区内复杂的水系统。它像一把无形的刻刀,不断地对山体、岩石进行侵蚀、溶蚀、切割,最终雕凿出天坑、石林、洞穴、峰丛等千姿百态的岩溶奇观。而流水又以不同的姿态奔涌于山谷、蜿蜒于平坝、潜流于地下、悬垂于崖壁再汇聚成湖,与山、峰、石、洞景观一起组成兴文精彩纷呈的山水画卷。兴文地质公园,山石海洞乡、太安石林、焚王山景区组成。这三个景区均沉积了巨厚的灰岩,但这些灰岩形成的时代则完全不同,物质成份也
Xingwen World Geological Park is located in the southern margin of the Sichuan Basin and Yunnan-Guizhou Plateau Xingwen County transition zone, Xing Wen climate moist, abundant rainfall. Since 460 million years ago, huge carbonate rocks have been deposited here. As surface water and groundwater transform into each other between rock fractures and joints, they form a complex water system in the park. It is like an invisible knife, constantly on the mountain, rock erosion, erosion, cutting, and ultimately carved out of the pit, stone forest, caves, peaks and other karst miracles spectacle. The flow of water rushed to the valley in different gestures meandering in the Pingba, submerged in the ground, hanging in the cliff and then converge into a lake, and mountain, peak, stone, cave landscape together composed brilliant landscape painting. Xingwen Geological Park, Rocky Cave Township, Shilin Stone, Burning Hill scenic area. The three scenic areas have deposited a huge limestone, but the limestone formation of the era is completely different, the material composition