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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]
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)
Cả River; Nam Sam River; Gianh River; Kiến Giang River; Long Đại River; Nhật Lệ River; Ron (river, Vietnam) Son River (Vietnam) Sepon River; Thạch Hãn River; Bến Hải River; Perfume River; Kong River
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 ...
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The Son River flows into the mouth of the Phong Nha cave and keeps on underground, where it is called the Nam Aki River. It emerges 20 km to the south near Pu-Pha-Dam Mountain. [ 17 ] There are spectacular streams, springs and waterfalls in Phong Nha-Kẻ Bàng, namely: Gió waterfall, Madame Loan waterfall, Mọc stream erupting from a ...
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.
The whole province area is in the lower section of Mekong River. Its current terrain surface and land was created by the accumulation of Mekong river silt during the development process of the modern delta in the marine regression period from the mid-Holocene (about 5,000 – 4,500 years to the present), which is also called new silt.