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Towards an environmental history of the eastern Red River Delta, Vietnam, c.900–1400
Published online by Cambridge University Press: 03 September 2014
Abstract
This article focuses on the eastern region of the Red River Delta, Vietnam, between the tenth and sixteenth centuries. This area was an important centre of economic and population growth in Đại Việt in the thirteenth and fourteenth centuries, and nurtured Đại Việt's sophisticated and renowned ceramics industry, hosted leading schools of Vietnamese Buddhism and bred a rising class of scholars and bureaucrats. The region's rapid rise as an economic and political centre was, however, also the key to its undoing. The sudden spike in population density, and the intensive logging carried out for ceramic production, and temple and ship building, overtaxed the area's natural resources. The burden on the local ecology was exacerbated by the Trần dynasty's dyke building project, which shifted the river's course. The ensuing environmental deterioration might have been one major reason for the Vietnamese forsaking the large-scale ceramic production in Chu Đậu, deserting their main port, Vân Đồn, and for the Chinese abandoning a historical maritime invasion route.
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References
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75 Lê Quát, ‘Bắc Giang Bái thôn Thiệu Phúc tự bi ký’ [For the inscription on Thiệu Phúc temple in Bái village], in Thơ văn Lý-Trần, vol. 3, p. 144.
76 This explains a fourteenth-century Chinese envoy's description of the Vietnamese: ‘everyone is barefoot, whether his status is high or low; everyone shaved his hair, whether he is old or young’ [尊卑雙跣足,老幼一圓顱]. He must have seen a large percentage of monks, which made him believe that everyone was a monk. See [Yuan] Chen Gangzhong, ‘Poetry of Chen Gangzhong’, in Qinding siku quanshu, part Ji, vol. 5.
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82 I am grateful to Professor Đỗ Bang for this information.
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89 Lịch sử Việt Nam, p. 257; Taylor, A history of the Vietnamese, pp. 150–52.
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91 Sakurai, Betonamu Sonraku no keisei, p. 262.
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97 Ibid., p. 432.
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99 Champa's political and cultural advances into the highlands were made during these periods. J. Whitmore, ‘The last great king of classical Southeast Asia: “Che Bong Nga” and fourteenth-century Champa’, in Trần Kỳ Phương and Bruce M. Lockhart, The Cham of Vietnam, p. 194. Some authors refer to the Cham polity as ‘Nagara Cāmpa’; its extent and structure are still being debated.
100 Whitmore, ‘The last great king of classical Southeast Asia’, p. 186.
101 Nishimura Masanari, ‘An essay on the formation of enclosed-type dykes in the Red River plain, northern Vietnam’, MS, p. 6. The excavation at Ngói, another important ceramic centre of fifteenth and sixteenth century Hải Dương, revealed that this location was unoccupied between the seventeenth and twentieth centuries.
102 The Ming invasion of Đại Việt in 1407 came by two routes, neither of them involving water. A Taiwanese travel account recorded clearly why: ‘From Taiwan to Tongking by waterway takes 89 geng … although the port is wide, the further up to the west the narrower the river became.’ [由台至东京水程八十九更,自东京渡海十二更抵安南,其两海自港口横渡,虽甚广,渐西渐隘,而海亦尽,盖皆海之支汊] Taiwan tongzhi [A complete gazette of Taiwan] (Taipei: Taiwan sheng wenxian weiyuanhui, 1956), p. 33Google Scholar.
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