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浙江余杭北苕溪河流地质地貌与旅游地学景观资源初探——以太平溪至双溪河段为例

A Discussion on Fluvial Geomorphology and Tourism Geological Landscape Resources of Beitiao Brook,Yuhang,Zhejiang Province——With Taiping Brook to Double Brook as an Example

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【作者】 杨永峰李南美董传万竺国强唐立梅郑丹

【Author】 YANG Yong-feng~1,LI Nan-mei~(1,2), DONG Chuan-wan~2, ZHU Guo-qiang~2, TANG Li-mei~2, ZHENG Dan~1 (1.Zhejiang Geological Prospecting Institute of China, Chemical Geology and Mine Bureau, Hangzhou 310002, China; 2.Department of Geosciences, Zhejiang University, Hangzhou 310027, China)

【机构】 中化地质矿山总局浙江地质勘查院浙江大学地球科学系

【摘要】 选取浙江余杭北苕溪的太平溪至双溪河段为对象,研究其河流地质地貌和旅游地学景观资源。基于区域资料和野外调查,得知该河段处于天目山中低山丘陵向杭嘉湖平原的过渡地带,发育坡面流—"V"形谷—"U"形谷—河漫滩河谷—成形河谷等一系列完整的河谷形态和瀑布、跌水、壶穴、边心滩、河漫滩、河流阶地等多种河流地貌形态,完整地展现了山溪型河流发育的一个过程。最后,对其典型旅游地学景观资源进行了初步探究。

【Abstract】 With the reaches of Beitiao River, from Taiping Brook to Double Brook, in Yuhang District, Zhejiang Province, as the object of research, this paper discusses the fluvial geomorphology and the tourist geological landscape resources along the river. Based on the regional material and the field work, the authors have learned that this part of river is located in the field from the low-medium hill to the Hangjiahu plain, assuming a full series of river valley, including sloping and side water -"V"valley -"U"valley-alluvial flat valley-molding valley, and involving waterfall, drops, pothole, side and central beaches, alluvial flat, alluvial terrace etc, exhibiting a series of the forming progress as a mountainous river. The paper also studies the representative tourist geological landscape resources.

  • 【文献出处】 国土资源科技管理 ,Scientific and Technological Management of Land and Resources , 编辑部邮箱 ,2010年01期
  • 【分类号】P942
  • 【被引频次】3
  • 【下载频次】205
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