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The Tickfaw River / ˈ t ɪ k f ɔː / runs 113 miles (182 km) [1] from Amite County in southwest Mississippi to Livingston Parish in southeast Louisiana. Its mouth opens into Lake Maurepas, which conjoins with Lake Pontchartrain. [2] The name Tickfaw (Tiak foha) is thought to be derived from the Choctaw phrase meaning "pine rest" or "Rest ...
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
According to scholar Pétrus Ký, the waterfront area at the end of rue Catinat was once called Bến Ngự (translating to "royal wharf"), the royal landing stage. He also revealed that it was known in Khmer as Compong-luong, [3] which suggests that its history may date back to the 17th century, when Saigon was still the Cambodian settlement of Prey Nokor.
Tickfaw State Park, located 7 mi (11 km) west of Springfield, in Livingston Parish, Louisiana, United States, opened in May 1999 and quickly became one of Louisiana's most popular state parks because of its natural setting, recreation opportunities, and proximity to the state's two cities: New Orleans and Baton Rouge. The park contains a nature ...
Horse Bluff Landing is an unincorporated community in Livingston Parish, Louisiana, United States.The community is located less than 3 miles (4.8 kilometres) west of Killian and 5 miles (8.0 kilometres) northeast of Maurepas on the bank of Tickfaw River. [2]
Tickfaw is a place name of Choctaw language origin. Tickfaw may refer to: Tickfaw, Louisiana; Tickfaw State Park; Tickfaw River This page was last edited on 29 ...
Tam Cốc, literally "three caves", consists of three natural caves — Hang Cả, Hang Hai, and Hang Ba — on the Ngô Đồng River. [2] [3] Tourists are taken in small boats along the river from the village of Ván Lám, through rice fields and limestone karsts, through the caves, and back. Local women serve as guides and attempt to sell ...
Cà Mau is a triangular stretch of land, with a maximum length of 130 miles and average height of seven feet above the sea level. Its formation is almost totally the result of the deposits of the Mekong River, [1] [2] which is also behind the Cape Bai formation at the tail end of the peninsula. [3]