Introduction to Shiku Tianshu: The carbonate rock (dolomite) deposited in the Lower Paleozoic Era 4.6 billion years ago, due to differences in chemical composition, has different degrees of dissolution, resulting in its current appearance. Viewed individually, stone peaks that are several meters, ten meters, or even dozens of meters high appear to be composed of layers of thin plates, resembling books, and are commonly known as "thousand-layer rocks". Dozens of these stone peaks are often connected together to form a forest of peaks, which is the "Shiku Tianshu". It is a special stone structure on Wangmangling.
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