Where is Detian Waterfall in Guangxi?

Detian Waterfall is located in Detian Village, Shuolong Township, daxin county, Chongzuo City, China.

Detian Waterfall is 100 meters wide and 70 meters high vertically. The average annual discharge is about 3 times that of Huangguoshu Waterfall in Guizhou. The waterfall is connected with Banyo Waterfall in Vietnam, and the two waterfalls are integrated in rainy season, with a total width of 208 meters. Detian Waterfall is located in the middle Devonian dolomitic limestone, which is a typical karst waterfall. Its upper reaches are the Guichun River flowing through Vietnamese territory. This section of the river is a bifurcated river with a wide and shallow riverbed and many Jiang Xinzhou and beaches.

When approaching Detian Waterfall, the height difference between the riverbed downstream of the waterfall and the riverbed at the top of the waterfall is about 6 meters. In order to find the shortest path to the downstream water surface, the water in Guichunjiang meanders through the dolomite buds in the upstream riverbed of the waterfall.

Introduction to Chongzuo

Chongzuo is located in the southwest of Guangxi Zhuang Autonomous Region, south of the Tropic of Cancer, and its geographical coordinates are between 2136 ′ ~ 23 22 ′ north latitude and 0/06 33 ′ ~108 6 ′ east longitude. Facing Southeast Asia, backed by the southwest of China, it connects Nanning and Fangchenggang in the east and southeast, Baise in the north and Vietnam in the west, with a total area of 1.73 million square kilometers.

Chongzuo has an ancient geological structure, which is based on Devonian, Permian and Triassic. Mainly limestone, followed by shale and sandstone, and the surface is covered with Quaternary acid latosol. Surrounded by mountains, there are few mountains and more land, and the landform is complex and diverse, with karst landform as the main body.

To the west is the Daqingshan Mountains, and to the south are the Gongmushan Mountains and the remnant veins of the Hundred Thousand Mountains. Generally speaking, the terrain is higher in the northwest and southwest and inclined to the east. The central part is cut by Zuojiang River and its tributaries to form a hilly plain, which is comprehensively rewarded.

Reference to the above content: Baidu Encyclopedia-Chongzuo