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2025-04-03 21:00本頁面
  

【正文】 cenery like this, then we all know how the east lake is formed? in fact, east lake endangered yangtze river, castle peak hong kong and the yangtze river the same, between the lakes, development of an alluvial plain, as long as more than 10 kilometers in length around trip heights, a relatively low tide au, whenever the flood season, the yangtze river water level higher than the surface, concave to the upper reaches of the spilled water supply will not be able to, so , the stagnant water in depressions formed now on the east lake. in 1949 several former east lake basically still a shortage lake, from the 1950s to a largescale construction, according to the natural environment, east lake can be divided into tablets, geese, white horse, bangmoshan, flute player, luo hong six scenic areas, but only now opening to the outside world bangmoshan purse and the two scenic areas. then, we invite you to join me and into the tour. east lake entered the door, we have entered a purse scenic areas, we are now a place where it is called huang li wan, the name is derived from mrs po “jueju”: “two huang liming 75,000, and his party egret, blue sky.” here looking weeping willow fu shore, the treelakeshore , is also a du po39。s poetic. we note that the side of those trees? this is referred to as living fossils of the ancient quaternary period glaciers plant metasequoia glyptostroboides, in 3 million years before they had been widely distributed in the various regions of the northern hemisphere. metasequoia glyptostroboides had once been the b
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