Chin-sha Chiangとは 意味・読み方・使い方

固有名詞

Chin-sha Chiang

1. Alternative form of Jinsha Jiang.
   • 1954, Wiens, Herold J., “The South China geographical environment”, in Han Chinese Expansion in South China‎^[1], Shoe String Press, published 1967, LCCN 67-16409, OCLC 473651484, OL 24127509M, page 22:

     The boundary between Tibet and China settled by the Manchu Emperor and the Tibetans in 1727 and lasting down to 1910 ran from the Mekong just north of A-t'un-tzu, crossed northward into the Chin-sha Chiang valley and followed the water divide between the Chin-sha and the upper Mekong sources to the Kokonor Territory.

   • 1967, Hu, Chang-tu; et al., “Geography, People, and Natural Resources”, in Chinese Society under Communism: A Reader‎^[2], John Wiley and Sons, Inc., LCCN 66-29625, OCLC 260236, page 20:

     From the confluence of its two headwaters in the upland of southern Tsinghai, it flows southward to western Szechwan as the Chin-sha Chiang; then, beyond the great bend in northwestern Yunnan it turns sharply to the east and traverses the whole length of Central China to the East China Sea.

   • 2011, Iggulden, Conn, chapter 14, in Conqueror: A Novel of Kublai Khan‎^[3] (Fiction), New York: Delacorte Press, →ISBN, LCCN 2011029727, OCLC 713188550, page 135:

     “We must cross the Chin-sha Chiang River,” Kublai said suddenly. He had pictured maps in his imagination, his recall almost perfect.

   • For more quotations using this term, see Citations:Chin-sha Chiang.

参照

固有名詞

Chin-sha-chiang

1. Alternative form of Jinsha Jiang.
   • 1916 May, Kingdon Ward, F., “Further Geological Notes on the Land of Deep Corrosions”, in The Geological Magazine‎^[1], number 623, →ISSN, →OCLC, page 211:

     It is much more likely that the Chin-sha-chiang (reserving this name for the southward-flowing upper portion of the Yangtze) did actually continue southwards past Likiang, being subsequently beheaded by the upper course of the eastward-flowing portion cutting back westwards; the southern portion of the Chin-sha-chiang, being thus isolated from its source, ultimately disappearing.

   • 1946, Hornell, James, “The Coracle in Asia”, in Water Transport: Origins & Early Evolution‎^[2], David & Charles, published 1970, →ISBN, →OCLC, page 100:

     In a coracle of this form, Kingdon Ward (1913, 129) travelled 15 miles downstream from Batang on the Chin-sha-chiang, a tributary of the Yangtze; its length was barely 6 feet, the breadth 3 feet and the depth 5 feet.

   • 1948, Thomas, F. W., “Introduction”, in Nam: An Ancient Language of the Sino-Tibetan Borderland‎^[3], Oxford University Press, →OCLC, pages 3-4:

     The great Ña(g)-chu, or Ya-lung river, which with its tributaries issues from the southern slopes of the Bayankara range and ultimately joins the Hbri-chu, now Chin-sha-chiang, on its left bank, has perhaps a more precipitous upper course.

   • 1977, Chang, Kwang-chih, “Early Civilizations in South China”, in The Archaeology of Ancient China‎^[4], Third edition, Yale University Press, →ISBN, →LCCN, →OCLC, page 454:

     In this connection, Wu Chin-ting’s investigations during 1938-40 in Ta-li Hsien, in the Lake Erh and Tien-ts’ang Mountain area of western Yunnan a little way below the Chin-sha-chiang, are highly important.

   • For more quotations using this term, see Citations:Chin-sha-chiang.