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The national geological park travels to border on the sea Wenzhou of China

The national geological park travels to border on the sea Wenzhou of China

Write: Grier [2011-05-23]

The national geological park travels to border on the sea  Wenzhou of China

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From border on the sea urban area or from the pepper and river Haimen) Ferryboat ago, ride the intersection of peach and small piece of land surrounded by water, go by China and Pakistan of Japan to the intersection of pepper and the north.

Introduce

The national geological park lies in strand area of place of about 50 kilometers in the east of Linhai of the east central area of Zhejiang Province to border on the sea in Zhejiang. The garden lies in Wenzhou -In the east of the major rupture of Zhenhai. National China of Israel of geological park invites from today the volcano invades the chalk generation late taking shape between 9500 and 65 million to border on the sea -It is that the ground form is a characteristic to erupt the rock.
The intersection of geological park and the intersection of subject and the intersection of stratum and chalky the intersection of interconnected system and the intersection of balcony and group at being, belong to the volcano gushes out the component of the headband coastal later period of Mesozoic Era of east such as Zhejiang. The volcanism relies mainly on the fact that the acid magma erupts the overflow, follow the magma to invade out. By the volcanic rock of one storey of forms in the geological park, and the vertical joint in post form form the main scene of natural landscape of the park to formed views such as unique lava tableland, peak clump, stone forest,etc. plain in the fracture structure. Gao Shanfeng has an elevation of 508 meters for white rock mountain the most in the garden, the general mountain peak is above sea level among 200-300 meters. Large to bear the intersection of head and volcano invade the intersection of rock and vault (flow the intersection of line and the intersection of quality and garrulous the intersection of spot and lava) Distributed and connected with a record of east big and born the adjacent place of head village, crater area is about 2 sq. km., its position of centre invades and forms the vault structure of volcanic rock for the acid lava of later period, the lava cools and forms about 15 million stone pillars. Stone pillar pentagon and hexagon geometirc shape very regular, like carve and cut manually. The stone pillar prolongs vertically 300-500 meters deeply, happen and reveal the height. The stone pillar is arranged in order or stand upright or oblique to lie, layer upon layer of, ground, the imposing manner is outstanding, may well be termed ten thousand columns of stone forests.
In addition, Wan column peak, a thousand column precipice, the intersection of bar and wall, the intersection of giant and dish, coral rock, fascinating stone forest view grand, posture different cliffside waterfall spring flows, form a natural picture scroll, make people completely relaxed and happy. And the spraying and spoiling over, invading out and flowing to form a large number of floating structures of acid lava, the upright form horizontal in shape is distributed, trace thickness of the line flows to all have. And the tower rock peak (form peaches three natural huge towers of small piece of land surrounded by water) that passway on the volcano makes up ,Rock tower precipice, it is very flat, higher than the chain of mountains around by 150-200 meters, is located in the strand, specially show grandly, different direction view it like The tower ,Such as castle ,If reject the screen-like mountain peak Such as lotus ,The ones that view and admire the sunrise, fog sea are good. The acid lava tableland goes through structure lifting, weathering and erosion and sea water and soaks function, form the column ground form of the peak and cave ground form of the marine abrasion. Go pterosaur and long the intersection of tail and the intersection of bird and fossil bury on volcano erupting during the intermittence sinking in the tuff in the the intersection of north and 1 last records of Ao of place in the records of the intersection of township and Ao, find 6 well preserved pterosaur fossils, through being identified as not having the tooth pterosaur s family, the characteristic is that a beak is extremely long, without teeth, the end is short, unite vertebras. Have for about 76 million 83 million years for one layer of ages for a pterosaur. Paleontology, ancient ecology are turned with the calamity of volcano into the study on respect that the living beings influences,etc. and had great significance to the later period of Cretaceous period.
This geological park is Cretaceous period of Mesozoic Era of China the volcano invades -Erupt one of the typical areas of rock department, it is the important component of the volcano active belt of the ring Pacific Ocean too. Function invades overflow and volcano bits rock out to erupt and pile up with the acid lava on the volcano, going through the long historical period of geology is applied and form a large number of natural traces of geology by internal and external motive force.