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River anticlines form when huge amounts of material are removed by river erosion in an area with low crustal rigidity. The crust rebounds up specifically along the river, while the rest of the area remains relatively constant. This will bend the crust forming an anticline, which can take up to ten thousand years. [7]
South Central Coast. Cu Đê River; Hàn River; Túy Loan River; Yên River (Quảng Nam-Đà Nẵng) Cầu Đỏ/Cẩm Lệ River; Vu Gia River; Thu Bồn River; Trà Bồng River
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Dầu Tiếng Lake is an artificial lake in the three provinces of Tây Ninh, Bình Dương, and Bình Phước in the Southeast region, Vietnam. The lake was formed by damming the upper reaches of the Saigon River, making it the largest irrigation reservoir in Vietnam and Southeast Asia. Construction of the lake began in 1981 after surveys ...
The river Tiền as it flows through Tân Châu (An Giang) River Tiền at Mỹ Tho. The Tiền River (Vietnamese: Sông Tiền 瀧前 or Tiền Giang 前江) is the name given to the section of the Mekong’s mainstream in Vietnam. [1] At Phnom Penh, the Bassac River branches off from Mekong River.
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Formation of a river anticline by river erosion and the associated isostatic rebound. As the river erodes the overlying material, the underlying rocks will rebound up, like a block in water if you remove a weight from on top of it, forming an antiformal structure. (Image created by Michael Stevens)
It originates in the Loi Mountains of Laos, crossing Laos's Xiangkhouang Province, Vietnam's Nghệ An and Hà Tĩnh provinces and empties into the Gulf of Tonkin, on the North Central Coast of Vietnam, after a 512 km journey. [1] The Cả River zone is classified as 300 km by the Vietnam Geographical Survey. [2]