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Cả Pass
The Cả pass (Đèo Cả) is a mountain pass in Phú Yên Province, Vietnam. The mountains are known as the Cả pass mountains (núi Cả Đèo). Historically, the Cả Pass was the second most difficult col in Vietnam after Hải Vân Pass. In 1611, the Nguyen lords pushed their border down to Cả Pass. The pass is also known as Đèo Cục Kịch. In the French documents the pass name is "Col Babonneau". getamap.net, 2015. ''Phong So'' is Phong Sổ hamlet of Hòa Xuân Nam commune. References {{DEFAULTSORT:Ca Pass Mountain passes of Vietnam Landfor ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hải Vân Pass
The Hải Vân Pass (, , 'ocean cloud pass'), is an approximately long mountain pass on National Route 1 in Vietnam. It traverses a spur of the larger Annamite Range that juts into the South China Sea on the border of Đà Nẵng and Huế, near Bạch Mã National Park. Its name refers to the mists that rise from the sea, reducing visibility. Historically, the pass was a physical division between the kingdoms of Champa and Đại Việt from 1306 until Vietnamese invasion war in 1471. The twisting road on the pass has long been a challenge for drivers traveling between the cities of Huế and Đà Nẵng. Since the completion of Hải Vân Tunnel, traffic flow and safety have improved. The pass has been the scene of at least two of Vietnam's most serious rail accidents, and at least one air crash. Overview The Hải Vân Pass crosses over a spur of the Trường Sơn (Annamite Range) that emerges from the west and juts into the South China Sea, forming the Hải Vân Penins ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nguyễn Lords
The Nguyễn lords (, 主阮; 1558–1777, 1780–1802), also known as the Nguyễn clan (; ), were Nguyễn dynasty's forerunner and a feudal noble clan ruling southern Đại Việt in the Revival Lê dynasty. The Nguyễn lords were members of the House of Nguyễn Phúc. The territory they ruled was known contemporarily as Đàng Trong (Inner Realm) and known by Europeans as the Kingdom of Cochinchina and as Kingdom of Quảng Nam (; ) by Imperial China, in opposition to the Trịnh lords ruling northern Đại Việt as Đàng Ngoài (Outer Realm), known as the "Kingdom of Tonkin" by Europeans and "Kingdom of Annam" (; ) by Imperial China in bilateral diplomacy. They were officially entitled, in Sino-Vietnamese, the ' () in 1744 when lord Nguyễn Phúc Khoát self-proclaimed himself to elevate his status equally to Trịnh lords's title known as the ' (; ). Both Nguyễn and Trịnh clans were ''de jure'' subordinates and fief of the Lê dynasty. However, the ''d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Christoforo Borri
Christoforo Borri (1583 in Milan – 24 May 1632 in Rome), also called Christopher Borrus in older English sources, was a Jesuit missionary in Vietnam, a mathematician, and an astronomer. In Vietnam Borri's family was one of good standing in Milan. He became a member of the Society of Jesus, 16 September 1601; in 1616 he was sent from Macau with the Jesuit priest Marquez, as one of the first missionaries to Đàng Trong (knowns to the Europeans as '' Cocincina'', now part of central Vietnam). He stayed at Hội An from 1618 (or at the end of 1617) until 1622, being known under the name of Bruno.Silk for Silver: Dutch-Vietnamese Relations, 1637-1700 – Page 252 Anh Tuấn Hoàng – 2007 "The Italian priest Christopher Borri, who lived in Hội An between 1618 and 1622, recorded this incident: ..." At Coimbra After his return Borri taught mathematics at Coimbra; in 1632 he entered the Cistercian Order, taking the name of Father Onofrio, and died the same year. Borri's most impo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Passes Of Vietnam
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
