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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]
Bản Giốc – Detian Falls or Bản Giốc Falls is a collective name for two waterfalls on the Quây Sơn River (Vietnamese: Sông Quây Sơn, chữ Nôm: 滝𢮿山; Chinese: 归春河, Pinyin: Guīchūn hé) that straddle the international border between China and Vietnam; more specifically located between the Karst hills of Daxin County, Guangxi and Trùng Khánh District, Cao Bằng ...
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
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)
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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 ...
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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.