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2-Landform constitutive features of Zhijindong Cave Geopark

2015-03-25 20:58 | Author:gzzjd | Reading:amount |

Located in the west of Guizhou Plateau, the geopark is composed of three geomorphic units, Zhijindong Cave, Qijiehe River and Dongfenghu Lake which represent different karst development processes.

① Zhijindong Cave geomorphic unit is developed on the basis of Zhijindong Cave underground river, forming a 4-layer labyrinth fossil cave system, namely, Zhijindong Cave system; there are complete types of secondary chemical sediments, which are elegant, unique, and huge,generally belonging to a fossil cave karst geomorphic unit which has already stopped its development.
② Qijiehe River geomorphic units is developed based on Qijiehe River running underground and aboveground alternatively, and such landforms as fengcong, karst hills, caves, fengcong -gorges, tiankengs and natural bridges are distributed neatly over the river valley or on its both sides in a collaborative symbiosis way, generally belonging to a geomorphic unit which is developing on the surface and subsurface karstification alternatively.
③ Dongfenghu Lake geomorphic unit is developed on the basis of surface river-Liuchonghe River and Sanchahe River, and it has deep river valley with great different longitudinal formation, generally belonging to a surface karst geomorphic unit which is still developing so far.


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