The Rhyolite Landforms and Development Law in Yandang Mt.

  • 1. Department of Geography, College of Tourism, Shanghai Normal University, Shanghai 200234, China;
    2. Zhejiang Institute of Geological Survey, Hangzhou 311203, China

Received date: 2007-09-11

  Revised date: 2007-12-02

  Online published: 2008-03-25

Supported by

National Natural Science Foundation of China, No.40671018;Foundation for the key subject-Geography, Urban Environment, Tourism resource and Culture development by Shanghai Education Committee, No.J50402


The features and the development law of rhyolite landforms are unique. Based on the survey and analysis data, the paper has analyzed the types, the distribution and the development of the rhyolite landforms in Yandang Mt. The study results show that the landforms in this region can be divided into two types, six sub-types and sixteen type units. The peaks, cliffs and waterfalls are all distributed vertically at different heights, and the valleys and line-cliffs extend along the faults with strikes of NE, NW and EW horizontally. The development of the landforms in the region has experienced four stages in which there developed different kinds of landforms. The study in the paper can contribute to the building of this World Geopark and flourish the local tourism.

Cite this article

HU Xiaomeng, XU Honggen, CHEN Meijun, LI Yi, WANG Dutao, CHEN Min . The Rhyolite Landforms and Development Law in Yandang Mt.[J]. Acta Geographica Sinica, 2008 , 63(3) : 270 -279 . DOI: 10.11821/xb200803005


[1] Robert L C. The Quaternary and Pliocene Yellowstone Plateau volcanic field of Wyoming, Idaho and Montana, U.S. Geological Survey Professional Paper, 1980, 729-734.

[2] Lipman P W. The bases of the tuff calderas in west America. Volcanology Abroad, 1987, 1: 1-20.
[Lipman P W. 美国 西部灰流破火山口根部. 国外火山地质, 1987, 1: 1-20.]

[3] Kouzi O, Kazunori W. Aso Caldera. The Earth, 1983, 5(1): 10-13.
[小野晃司, 渡边一德. 阿苏破火山口. 地球, 1983, 5 (1): 10-13.]

[4] Zhou Yufan. The Diwa structure in different regions in the world. Geotectonica and Metallogenia, 1999, 23(4): 373-377.
[周裕藩. 世界各地地洼构造. 大地构造与成矿学, 1999, 23(4): 373-377.]

[5] Xing Guangfu, Tao Kuiyuan, Yang Zhuliang et al. The summarizing about the studies of the reasons causing the formation of Mesozoic igneous rock in southeast China near the ocean. The Bulletin of Mineralogy, Petrology and Geochemistry, 1999, 18(3): 189-193.
[邢光福, 陶奎元, 杨祝良等. 中国东南沿海中生代火山岩成因研究现状与展望. 矿物岩石地球化学通报, 1999, 18(3): 189-193.]

[6] Tao Kuiyuan. Xu Xiake and Yandang Mt. A preliminary study about the reasons causing the formation of the natural scenes in Yandang Mt. and its scientific and cultural significance. Volcanology and Mineral Resource 1996, 17(1-2): 107-119.
[陶奎元. 徐霞客与雁荡山: 初论雁荡山自然景观成因与科学文化内涵. 火山地质与矿产, 1996, 17(1-2): 107-119.]

[7] Tao Kuiyuan, Yu Minggang, Xing Guangfu et al. The value of the geologic remnants of the caldera in Yandang Mt. compared with the other ones in the world. Resource Survey and Environment, 2004, 25(4): 297-303.
[陶奎元, 余明刚, 邢光富等. 雁荡山白垩纪破火山地质遗迹价值与全球对比. 资源调查与环境, 2004, 25(4): 297-303.]

[8] Feng Changgen, Yu Yunwen, Dong Yaohong. The structural features of the caldera in Yandang Mt. and its material origin. Zhejiang Geology, 1997, 13(1): 18-25.
[冯长根, 俞云文, 董尧鸿. 雁荡山破火山口构造特征及成岩物质来源. 浙江地质, 1997, 13(1): 18-25.]

[9] Yin Jiaheng, Huang Guangzhao. The volcano cycles of Mesozoic and Cenozoic in southeast China near the ocean. Volcanology and Mineral Resource, 1997, 18(3): 167-190.
[尹家衡, 黄光昭. 中国东南沿海中、新生代火山旋回. 火山 地质与矿产, 1997, 18(3): 167-190.]