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喀斯特地貌和丹霞地貌的区别(The difference between Karst landform and Danxia landform)
喀斯特地貌和丹霞地貌的区别(The difference between Karst landform and Danxia landform)
Difference between the two:
1., from the appearance, the landscape of Danxia is red. And the landscape of Karst is white!
2., the development of the parent material is not the same, the development of the Danxia red sand on the red rock, so red, and the development of the Karst landscape in limestone, so white.
3. Chinas Hunan Zhangjiajie is the famous Danxia landform, Yunnan Jiuxiang Shilin is the famous Karst landform!
1. Danxia landscape: Fangshan, Chibi Qifeng, caves and other special landform of red rock in the external force under the action of a development. Rhyolite landforms landscape, rhyolite landforms for acidic volcanic rocks caused by condensation, after weathering, with rhyolitic structure, landform landscape rich and vivid, viewing from different angles, different time, often showing a different shape.
2., Karst geomorphic landscape: the carbonate rocks (mainly limestone) dominated by soluble rock in the water based interaction between the internal and external forces formed. Limestone weathering is mainly water erosion, ground limestone dissolution, Feng Ling, Gufeng formation peak, the formation of underground limestone dissolution cave, limestone dissolution after erosion remaining part of the formation of Taihu stone, water stone
1. Danxia landform is a kind of landform named after Mount Danxia in 30s of last century. Danxia the rock formation is a sedimentary basin in the inland red clastic rocks, later crustal uplift, the rock was cut water erosion, slope failure in the course of the main and back, the preserved rock block constitutes a red mountain. The Danxia landform belongs to the red layer landform. The so-called red beds refers to the red rocks formed during the Jurassic to Cenozoic third periods, commonly called the red sand conglomerate. Now, thick and thin sedimentary bedding can be seen on the cliff. The large rock formations are called conglomerates, and the fin
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