Stone Forest (Shilin)

Geologists say the Stone Forest is a typical example of karsts topography. Approximately 270 million years ago - during the carboniferous period of the Paleozoic era - the region was a vast expanse of sea. Over time, the movements of the lithosphere gradually caused a retreat of the waters and the rise of the limestone landscape. Due to constant erosion by the elements, the area finally developed into the present-day Stone Forest.