千岛湖景区门票网上预约入口(公众号门票预订系统)

千岛湖景区：

千岛湖景区，山地、盆地呈梯级多层地形展布。河谷下游低丘盆地区，侵蚀、基座阶地发育，在河谷、盆地中广泛堆积着河流冲积、洪积、湖积层，谷坡两岸残积层、坡积层发育。新安江水库形成以后，108米高程以下的河谷、低丘陵成了水面，低山地貌更为突出。地貌类型以剥蚀型山地地貌为主，堆积地貌、人工湖地貌次之。

英文介绍：

In the Qiandao Lake scenic area, the mountains and basins are spread out in cascades and multilayers. In the low-hill basin area in the lower reaches of the river valley, erosion and base terraces are developed. River alluvium, alluvial and lacustrine layers are widely accumulated in the valley and basin, and the residual layer and slope layer on both sides of the valley slope are developed. After the formation of the Xin'anjiang Reservoir, the valleys and low hills below the elevation of 108 meters became the water surface, and the low mountain landforms became more prominent. The landform types are mainly denuded mountain landforms, followed by accumulation landforms and artificial lake landforms.