"Chin-sha-chiang" meaning in All languages combined

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  "etymology_text": "From the Wade–Giles romanization of 金沙江 (Jīnshājiāng) Wade-Giles romanization: Chin¹-sha¹-chiang¹.",
  "head_templates": [
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      "expansion": "Chin-sha-chiang",
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  "lang_code": "en",
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      "alt_of": [
        {
          "word": "Jinsha Jiang"
        }
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        {
          "ref": "1916 May, F. Kingdon Ward, “Further Geological Notes on the Land of Deep Corrosions”, in The Geological Magazine, number 623, →ISSN, →OCLC, page 211:",
          "text": "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.",
          "type": "quote"
        },
        {
          "ref": "1946, James Hornell, “The Coracle in Asia”, in Water Transport: Origins & Early Evolution, David & Charles, published 1970, →ISBN, →OCLC, page 100:",
          "text": "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.",
          "type": "quote"
        },
        {
          "ref": "1948, F. W. Thomas, “Introduction”, in Nam: An Ancient Language of the Sino-Tibetan Borderland, Oxford University Press, →OCLC, pages 3–4:",
          "text": "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.",
          "type": "quote"
        },
        {
          "ref": "1977, Kwang-chih Chang, “Early Civilizations in South China”, in The Archaeology of Ancient China, 3rd edition, Yale University Press, →ISBN, →LCCN, →OCLC, page 454:",
          "text": "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.",
          "type": "quote"
        }
      ],
      "glosses": [
        "Alternative form of Jinsha Jiang."
      ],
      "id": "en-Chin-sha-chiang-en-name--XF10vS2",
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  "word": "Chin-sha-chiang"
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  "etymology_text": "From the Wade–Giles romanization of 金沙江 (Jīnshājiāng) Wade-Giles romanization: Chin¹-sha¹-chiang¹.",
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  "lang_code": "en",
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        }
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        "Mandarin terms with redundant transliterations",
        "Pages with 1 entry",
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      "examples": [
        {
          "ref": "1916 May, F. Kingdon Ward, “Further Geological Notes on the Land of Deep Corrosions”, in The Geological Magazine, number 623, →ISSN, →OCLC, page 211:",
          "text": "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.",
          "type": "quote"
        },
        {
          "ref": "1946, James Hornell, “The Coracle in Asia”, in Water Transport: Origins & Early Evolution, David & Charles, published 1970, →ISBN, →OCLC, page 100:",
          "text": "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.",
          "type": "quote"
        },
        {
          "ref": "1948, F. W. Thomas, “Introduction”, in Nam: An Ancient Language of the Sino-Tibetan Borderland, Oxford University Press, →OCLC, pages 3–4:",
          "text": "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.",
          "type": "quote"
        },
        {
          "ref": "1977, Kwang-chih Chang, “Early Civilizations in South China”, in The Archaeology of Ancient China, 3rd edition, Yale University Press, →ISBN, →LCCN, →OCLC, page 454:",
          "text": "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.",
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        }
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  "word": "Chin-sha-chiang"
}