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The main areas of Danxia landform are in Kangle and Baiyin townships. [2] The core area of the park, Linze Danxia Scenic Area, is located 30 kilometres (19 mi) west of downtown Zhangye and 20 kilometres (12 mi) south of the seat of Linze County. It is the most developed and most visited part of the park. [2]
As the landform gets older, valleys widen and one gets isolated towers and ridges. The danxia landform is named after Mount Danxia, one of the most famous examples of the danxia landform. A very peculiar feature of danxia landscape is the development of numerous caves of various sizes and shapes. The caves tend to be shallow and isolated ...
The Zhangye Danxia National Geological Park, covering an area of 510 square kilometres (200 sq mi), is located in Linze and Sunan counties of Zhangye, 30 kilometers (19 mi) west of the city center. [8]
ChinaLayers of mineral deposits have formed the spectacular spectrum of colors in these mountains, found in the Zhangye Danxia Landform Geological Park in north-central Gansu province. Several ...
Finally, the area of Danxia was formed. [2] Since six million years ago, the basin of Danxia area has experienced several intermittent rises, which average increase of about one metre (3 ft) per 10,000 years. With the favor of water washing by the river, the mount of Danxia is cut into many layers, and formed the mount of Danxia nowadays. [3]
Gansu [a] is a province in Northwestern China.Its capital and largest city is Lanzhou, in the southeastern part of the province.The seventh-largest administrative district by area at 453,700 square kilometres (175,200 sq mi), Gansu lies between the Tibetan and Loess plateaus and borders Mongolia's Govi-Altai Province, Inner Mongolia and Ningxia to the north, Xinjiang and Qinghai to the west ...
Badlands of the Zhangye National Geopark. Zhangye National Geopark is a badlands area known for its colorful rock formations. It was voted by Chinese media outlets as one of the most beautiful landforms in China and became a UNESCO Global Geopark in 2019. [23]
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