Aotao Seabed

[View] The Ordovician seabed geological rock 500 million years ago has a sense of crossing. The view is shocking from afar, and the look is beautiful. [Fun] There are several very strange corridors that can be photographed with good results. Going up and down a quiet and mysterious circle. [Cost-effective] The location is behind the pool, which is a good point for taking pictures.

Ordovician Seabed of Guzhang Redstone Forest National Geological Park: About 100 million years ago in the Ordovician, Guzhang is a shallow sea, where seabed sediment and carbonate substances gather, forming limestone and limestone, and then moving with the crust, limestone gradually rises and is exposed to the ground, and is reddish brown. Because it formed in the Ordovician, it is called the Ordovician seabed. These parallel horizontal stripes or threaded rocks maintain the original ecological beauty, but also witness the precipitation of the years and the changes of nature.