龟山印象 |
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贝岩Shale
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贝岩是一种碎屑岩,因具明显的页片状层理,故称之页岩。园区内的页岩多呈紫红色,形成于距今约5~6亿年的寒武纪时代。龟山页岩形成于静水的海洋环境中,为浅海一半深海的典型沉积。 Shale is a form of clasolite with plate-shaped bedding, so it was named shale. The shales in the geopark are purplish red and they formed during the Cambrian, 500~600 million years ago. The shale of Guishan formed in ocean of still water is a typical sediment in deep sea. |
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龟山地质年代
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龟山崩塌遗迹Guishan collapse relic
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