"Ying-chi-sha" meaning in English

See Ying-chi-sha in All languages combined, or Wiktionary

Proper name

Etymology: From the Wade–Giles romanization of the Mandarin 英吉沙 (Ying¹-chi²-sha¹). Etymology templates: {{bor|en|cmn-wadegiles|-}} Wade–Giles, {{uder|en|cmn|英吉沙|tr=Ying¹-chi²-sha¹}} Mandarin 英吉沙 (Ying¹-chi²-sha¹) Head templates: {{en-proper noun|nolinkhead=1}} Ying-chi-sha
  1. Alternative form of Yingjisha (Yengisar) Wikipedia link: Aeronautical Chart and Information Center Tags: alt-of, alternative Alternative form of: Yingjisha (extra: Yengisar)
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          "ref": "1946 December 5, Military Information: Sinkiang Rebellions 1931-1937, page 9:",
          "text": "Within the independent government of the East Turkestan Republic, while Sabid-da-Mulla insisted upon defending the Old City of Kashgar to the death, Mahum and Nias wanted to quit the Old City for the time being, withdraw to Ying-chi-sha, and plan a second uprising. These two at last withdrew to Ying-chi-sha and there joined the Khotan forces that had been fighting the T'ungkan troops of the New City of Kashgar. Sabid and all other important members now had no recourse but to withdraw to Ying-chi-sha. The T'ungkan troops in the New City of Kashgar entered the Old City without a fight. At that time Mahumd and Nias had already withdrawn to Yarkand. Sabid, in the middle of February, gathered the troops scattered in the vicinity of Ying-chi-sha, and attacked Kashgar. Though he recaptured the Old City he lost it again after two days, and was beaten back to Ying-chi-sha.",
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          "ref": "1967 January 26, Liu Tung-sheng, “Distribution, stratigraphic and material Composition Characteristics of Chinese Loess and Loess-like Rocks”, in Collected Works on China's Loess Soil, →OCLC, page 152:",
          "text": "The Malan loess of Late Pleistocene epoch is more widely distributed than the Li-shih and Wu-ch'eng loess. Its distribution stretches from Po-lo at the northern foothills of T'ien Shan and Ying-chi-sha at the western edge of the Tarim basin in the west toward the east through Tsaidam, Ho-hsi Corridor, Kansu, Shensi and foothills of T'ai-hsing Shan in Hopeh to Ch'ih-feng and Shantung Peninsula and reaches Ch'in Ling in the south and the Great Wall in the north.",
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          "text": "The Malan loess of Late Pleistocene epoch is more widely distributed than the Li-shih and Wu-ch'eng loess. Its distribution stretches from Po-lo at the northern foothills of T'ien Shan and Ying-chi-sha at the western edge of the Tarim basin in the west toward the east through Tsaidam, Ho-hsi Corridor, Kansu, Shensi and foothills of T'ai-hsing Shan in Hopeh to Ch'ih-feng and Shantung Peninsula and reaches Ch'in Ling in the south and the Great Wall in the north.",
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This page is a part of the kaikki.org machine-readable English 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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