The west platform is located at the foot of Modaoling, Ding Cun No.1 Community, Sanyuan Township Bridge, about 65km north of yingshan county City. After the hanging rock of steep rock falls off, it forms a circular bald stone with a diameter of 80m, looking at the bright moon in the west and the jade rabbit in the west, hence the name "Xitai".
The west platform is located on the precipice, with green cypresses, tall and straight pines and cypresses and a quiet environment. On the left rock wall of the west platform, there is a cliff-like cave 40 meters high and 30 meters wide. Buddha statue 1300, all carved with great care, with different shapes and vivid images.
On the right side of the west platform, there was a temple built in the Qing Dynasty, which was destroyed once, but the two tall lion Buddha Sakyamuni and the first Guanyin statue are still well preserved. 1994 1 1 was announced by Nanchong Municipal People's Government as a municipal cultural relics protection unit.
On Modaoling in Sanyuan Township, yingshan county, there is a natural stone bridge, which the locals call Tiansheng Bridge. The span of the bridge is 24 meters, the height of the bridge deck from the ground is l3 meters, the width of the bridge deck is 1.5 meters, the thickness is l.4 meters, and the bridge body is about 2 meters away from the parent rock. The bridge is naturally separated from a whole rock and has a magnificent appearance. It is really a masterpiece of nature, and the audience calls it "unique".
The "siliceous wood fossil" team was surprised to see Modaoling in Yingshan.
Modaoling, Sanyuan Township, Yingshan County, is the camp of Zhang Fei, a general of Shu Han, who visited Bazhou at night. Under the ridge, there is a well-preserved cliff statue of the western platform of the Tang Dynasty. The "siliceous fossils" on the east side of Modaoling are seamlessly connected with the site of Gu Sui 'an County, echoing Taipeng Mountain Forest Park.
According to experts, siliceous fossils are paleontological fossils, which were buried underground tens of thousands or even hundreds of thousands of years ago and evolved into siliceous fossils after long-term immersion in silicate. They are non-renewable natural heritage and important material evidence for studying geography, climate, earth evolution, plant life habits and ecological environment. It also plays an inestimable role in studying biological evolution.
In view of the local people's random collection and no protection measures, the author suggests that the relevant departments attach great importance to the protection of this precious natural heritage.