See Kin Sha on Wiktionary
{ "etymology_text": "From the Nanjing-dialect (later Postal Romanization) romanization of 金沙 (jīnshā).", "head_templates": [ { "args": { "nolinkhead": "1" }, "expansion": "Kin Sha", "name": "en-proper noun" } ], "lang": "English", "lang_code": "en", "pos": "name", "senses": [ { "alt_of": [ { "extra": "River in China", "word": "Jinsha" } ], "categories": [ { "kind": "other", "name": "English entries with incorrect language header", "parents": [ "Entries with incorrect language header", "Entry maintenance" ], "source": "w" }, { "kind": "other", "name": "Pages with 1 entry", "parents": [], "source": "w" }, { "kind": "other", "name": "Pages with entries", "parents": [], "source": "w" } ], "examples": [ { "ref": "1901, Archibald John Little, “From Kiating Back to Chungking”, in Mount Omi and Beyond: A Record of Travel on the Thibetan Border, London: William Heinemann, →OCLC, page 227:", "text": "Suifu, as it is universally called, or Hsu Chow Fu, as it is officially designated, is most advantageously situated at the junction of the two great rivers, the Min and the Kin Sha (\"Gold Sand\"), which here unite and form the mighty Yangtze.", "type": "quote" }, { "ref": "1916 July, Herbert W. L. Way, “The Minerals of Sze-chuan, China”, in The Mining Magazine, volume XV, number 1, →ISSN, →OCLC, page 22:", "text": "From the Chien Chang valley through which flows the An Ning river on the east, to the Tibetan frontier on the west, and from Ta Chien Lu on the north to the Kin Sha river (or river of golden sand) on the south, there is a stretch of country having an area of 40,000 square miles that is without doubt richer in mineral wealth than any other part of China, and one of the most highly mineralized spots in the whole world.", "type": "quote" }, { "ref": "1958 January, Chi-yun Chang, “The Historical Development of the Land of China”, in Chinese Culture: A Quarterly Review, volume I, number 3, Taipei: Chinese Culture University Press, →ISSN, →OCLC, page 82:", "text": "Very little was known about the geography of the Southwest until the time of Hsu Hsia-keh, who visited that area towards the close of the Ming Dynasty. It was only then that people came to know that the Kin Sha River was in fact the upper course of the Yangtze River and that the Red River, the Mekong and the Salween flowed into the South China Sea separately.", "type": "quote" } ], "glosses": [ "Alternative form of Jinsha (River in China)" ], "id": "en-Kin_Sha-en-name-cWUl7vZT", "links": [ [ "Jinsha", "Jinsha#English" ], [ "China", "China" ] ], "related": [ { "word": "Kin Sha Kiang" } ], "tags": [ "alt-of", "alternative" ], "wikipedia": [ "Postal Romanization" ] } ], "word": "Kin Sha" }
{ "etymology_text": "From the Nanjing-dialect (later Postal Romanization) romanization of 金沙 (jīnshā).", "head_templates": [ { "args": { "nolinkhead": "1" }, "expansion": "Kin Sha", "name": "en-proper noun" } ], "lang": "English", "lang_code": "en", "pos": "name", "related": [ { "word": "Kin Sha Kiang" } ], "senses": [ { "alt_of": [ { "extra": "River in China", "word": "Jinsha" } ], "categories": [ "English entries with incorrect language header", "English lemmas", "English multiword terms", "English proper nouns", "English terms with quotations", "English uncountable nouns", "Pages with 1 entry", "Pages with entries" ], "examples": [ { "ref": "1901, Archibald John Little, “From Kiating Back to Chungking”, in Mount Omi and Beyond: A Record of Travel on the Thibetan Border, London: William Heinemann, →OCLC, page 227:", "text": "Suifu, as it is universally called, or Hsu Chow Fu, as it is officially designated, is most advantageously situated at the junction of the two great rivers, the Min and the Kin Sha (\"Gold Sand\"), which here unite and form the mighty Yangtze.", "type": "quote" }, { "ref": "1916 July, Herbert W. L. Way, “The Minerals of Sze-chuan, China”, in The Mining Magazine, volume XV, number 1, →ISSN, →OCLC, page 22:", "text": "From the Chien Chang valley through which flows the An Ning river on the east, to the Tibetan frontier on the west, and from Ta Chien Lu on the north to the Kin Sha river (or river of golden sand) on the south, there is a stretch of country having an area of 40,000 square miles that is without doubt richer in mineral wealth than any other part of China, and one of the most highly mineralized spots in the whole world.", "type": "quote" }, { "ref": "1958 January, Chi-yun Chang, “The Historical Development of the Land of China”, in Chinese Culture: A Quarterly Review, volume I, number 3, Taipei: Chinese Culture University Press, →ISSN, →OCLC, page 82:", "text": "Very little was known about the geography of the Southwest until the time of Hsu Hsia-keh, who visited that area towards the close of the Ming Dynasty. It was only then that people came to know that the Kin Sha River was in fact the upper course of the Yangtze River and that the Red River, the Mekong and the Salween flowed into the South China Sea separately.", "type": "quote" } ], "glosses": [ "Alternative form of Jinsha (River in China)" ], "links": [ [ "Jinsha", "Jinsha#English" ], [ "China", "China" ] ], "tags": [ "alt-of", "alternative" ], "wikipedia": [ "Postal Romanization" ] } ], "word": "Kin Sha" }
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This page is a part of the kaikki.org machine-readable All languages combined dictionary. This dictionary is based on structured data extracted on 2024-12-15 from the enwiktionary dump dated 2024-12-04 using wiktextract (8a39820 and 4401a4c). The data shown on this site has been post-processed and various details (e.g., extra categories) removed, some information disambiguated, and additional data merged from other sources. See the raw data download page for the unprocessed wiktextract data.
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