Hongshi Park

My friend and I went yesterday, it was a sunny day, the breeze, the lotus leaves swaying wayward, forming a beautiful picture, there are many people playing inside, there are running, there are outings, there are dancing.

There is a red stone park in Laiwu District, Jinan City. An open park with water, stone and vegetation has been designed and matched. It has built a sports and leisure theme park, suitable for citizens to relax and recreation. The park has a large area of exposed red stone and is named. According to the examination of these brightly colored and wonderful red stones, generated more than 100 million years ago in the Mesozoic Jurassic, commonly known as the red layer, the red layer in Laiwu only remains in the trough of Laiwu Baligou, near the east-west direction, distributed in Laicheng and the southeast. Very distinctive.

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Glory still takes advantage of the fun, how far you can go on the road, not for travel, not for someone, because encountering the unknown travel is a prison escape for a mediocre life, the scope of one person's walk is his world can be nine to five, and he can also wander the world to live with a sense of ritual. The ordinary only became hot and the universe was romantic and happy. See the mountain is the mountain, see the water is the water, see you are the world. Children have spring tours, big friends enjoy picnics. When you can't find the answer,

I stayed at Shandong Laiwu Hotel, next to Hongshi Park, and I visited it by the way. Hongshi Park, Laiwu District, Jinan City, has Ginkgo Square, Yuebo Lake, Hongshi Valley and other tourist attractions. It is divided into eight scenic spots, including Tongle Haoyu, Battlefield Banner Wind, Qunfang Message, Songhe Danqing, Snow Field Tianguang, Shuohai Fangtao, Yecheng Ancient Wind, Huaxia Tengfei. The design of the whole park is unique. The overall layout is reasonable and highlights local characteristics. The whole park is named for its large area of exposed red stone. According to the test, those brightly colored mottled, strange and variable patterns of red stones, formed in the Mesozoic Jurassic more than 100 million years ago, due to the intense crustal movement at that time, the geographical differentiation intensified, the climate gradually turned dry, affected by the continental basin-type sedimentary environment, Therefore, the rocks formed are mostly thick red debris rock facies, commonly known as red layers. Afterwards, due to the influence of the very strong Yanshan movement and long-term weathering and denudation of the times, the Jurassic red layer in Laiwu only remains in the trough of Laiwu Baligou, which is near east-west, distributed in Laicheng and southeast, due to the bright red fine medium-grain feldspar rock of lithology. It is called “Red Stone.”