Lie in the seashore of the south of Jinjiang of Fujian Province, with 6 sea miles apart in Jin Men Island, 180 kilometers from the north to Fuzhou, connect with 74 kilometers in Xiamen in the south
Lie in the seashore of the south of Jinjiang of Fujian Province, with 6 sea miles apart in Jin Men Island, 180 kilometers from the north to Fuzhou, connect with 74 kilometers in Xiamen in the south, the area of garden is 68 sq. km. (40 sq. km. of area of sea area among them) . Main geological trace 44, geological trace 5, geological trace 29, geological section 10 of model of ground form of extinct plants and animal among them, concentrate on being distributed within the range of 20 sq. km.. Is divided into gulf, Long Hu of Shenzhen and Shanghai, encloses the first three scenic spot.
Grow as the main characteristic with the ancient oyster’s reef trace among 25000 years in the ancient forest of sea floor among 7000- 8000 years ago and l5000- ago. With the ancient lagoon ‘ Long Hu, Hui lake) Together, coastal and even going up and down, the earth’s crust change and important evidence of ancient climatic change of sea level since global late Pleistocene that study the southeast of China. In addition park locate the intersection of Fujian and the intersection of southeast and coastal Changle – Mesozoic Era such as Nan’ao in the large-scale toughness shear band, toughness shears the trace model out of shape abundantly, has recorded a beautiful view of the earth’s crust change in Mesozoic Era, so study the important area where the plate of Eurasia interacts with the plate of the Pacific Ocean of Mesozoic Era. Keep the coast ground form view with many types such as sandbank, laterite coast and base rock coast in the park. From Shenzhen and Shanghai gulf to enclose brilliance, a series of sandy and fine arcual bay and base rock cape suitable in slope appear alternatively, peculiar.
There is remaining China to rub the Buddhist nun and teach the temple – temple of Buddhist nunnery of grass in Yuan Dynasty in the park, Hai’an level bridge is fitted with the longest roof beam type stone bridge in the world at that time that was built in Song Dynasty. In addition, and built in Sui Dynasty sets up temple, government mouth Shi Lang memorial museum, deep forest temple, Zhenhai palace, wall mountain plank road, smoke mound mountain peak fire platform of Longshan of sea, encloses brilliance Overlook Jin Men Island) And unique history and culture and human cultural sight such as the old stone implement site. The national geological park of gulf of Shenzhen and Shanghai is the geology, geomorphology, environmental geology, Quaternary Period geology and focus area where the prehistoric archaeology pay close attention to, incorporate bay, cape, lake into an organic whole, it is the strand geological park with characteristic scientific travel value of geology of a pole. Cause the intersection of Shenzhen and Shanghai and the intersection of gulf and area abundant Quaternary Period right to study coastal global the intersection of Quaternary Period and new tectonic movement, ancient geography, palaeoclimate, southeast of China, in geological trace, especially there is a very great scientific meaning in the changes of littoral zone.
Since more than 20,000 years, this area went through the land of numerous sea to change, this kind of changes, the low temperature that has already had global climatic change to initiate and factor that the high temperature changes minor cycle, have regional the earth’s crust difference nature rise or fall reason. Main watching focus
Grow the ancient forest trace nature reserve of sea floor of the view and lie in the gulf of Shenzhen and Shanghai in ancient forest and ancient oyster reef of sea floor, area is 3100 hectares, its protection target is ancient forest, oyster reef, marine abrasion metamorphic rock of sea floor,etc., the protection zone of this kind is not only unique in China, it is rare even in the world. Bury the oil China fir going through 7800 histories of more than years in the district on the intertidal zone to set up the trace 20 multiply; There are oyster reeves among 15000- 25000 years of large stretch of growth, there are uniqueness, model that can show long geological historical development such as the Palaeozoic Era, Mesozoic Era, new generation, appear to reveal the good, varied marine abrasion metamorphic rock. The setting-up of the protection zone, can be in order to study ancient ocean, ancient geography, palaeoclimate, ancient plant, study geological structure and sea level of the Taiwan Straits and hoist or lower the geological plate sports of sport and the Pacific Ocean, study the ancient harbour of Quanzhou and hand in comprehensive history to offer reliable scientific basis overseas.
The geological park of gulf of Shenzhen and Shanghai of coast is one of the few strand geological parks at present China. The coast twists are changeable, arcual bay and outstanding cape arrange alternatively, take in the coast 25 kilometers long, there are a lot of bay, cape association, this kind of characteristic, very similar to inferior coast of Sri Lankan in Spain, in the long littoral zone of China, the view takes the course of its own.