See Ch'ing-hai on Wiktionary
{
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"args": {
"1": "en",
"2": "cmn",
"3": "青海//靑海",
"tr": "Qīnghǎi"
},
"expansion": "Mandarin 青海／靑海 (Qīnghǎi)",
"name": "bor"
},
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"etymology_text": "From Mandarin 青海／靑海 (Qīnghǎi) Wade–Giles romanization: Chʻing¹-hai³.",
"head_templates": [
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{
"ref": "1904, Charles Daniel Tenney, Geography of Asia, London: Macmillan and Co., →OCLC, page 5:",
"text": "The Yellow River (黃河) rises in small lakes in the southern part of Ch'ing-hai (青海) and flows in a very crooked channel toward the north-east to Lan-chou Fu (蘭州府).",
"type": "quote"
},
{
"ref": "1925, Francis Younghusband, Peking to Lhasa, London: Constable and Company, →OCLC, page 112:",
"text": "Leaving this town and the Sining River valley the road ascends a grassy valley with some recently started cultivation to a pass, 10,780 feet, over the Jih-yüeh Shan range, 27 miles from Tangar. This is the boundary between the Kansu and Ch'ing-hai Provinces. It is also the real boundary between China and Tibet, though the present frontier is the Tang-la Range, running east and west, the divide between the Salween and Mekong rivers.",
"type": "quote"
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{
"ref": "1970, Joseph B. R. Whitney, China: Area, Administration, and Nation Building, Department of Geography, University of Chicago, →LCCN, →OCLC, page 38:",
"text": "In the west, the outer periphery of the Inner Zone is the great divide separating Pacific Ocean and South China Sea drainage on the one hand, from drainage oriented towards Hsin-chiang in the northwest and towards the Indian Ocean in the southwest, on the other. This divide also represents a fairly pronounced stress zone between the tenuous power China has been able to maintain over Tibet to the west and the firmer control she has been able to exercise over Hsi-k'ang and Ch'ing-hai to the east.",
"type": "quote"
},
{
"ref": "1972, T. V. W., “TIBET”, in Encyclopedia Britannica, volume 21, →ISBN, →LCCN, →OCLC, page 1108, column 2:",
"text": "For centuries the area of ethnic Tibet was divided into the following: Dbus and Gtsang (comprising central Tibet), Mnga’-ris, Khams, and A-mdo.[…]A-mdo, the northeastern part of ethnic Tibet, passed under Manchu control in 1724 following the suppression of a Mongol revolt against the throne. This area was officially incorporated into the Chinese provincial system as Ch’ing-hai Province in 1928.",
"type": "quote"
},
{
"ref": "2007, Laurie Burnham, Rivers (The Extreme Earth), Chelsea House, →ISBN, →LCCN, →OCLC, page 45:",
"text": "The Yangtze River first formed millions of years ago, a by-product of continental drift. Although the process itself took many millennia, the Ch'ing-hai (Qinghai) Plateau, from which the Yangtze descends, rose from the Earth's crust some 40 million years ago when the Indian subcontinent and Eurasia crashed into one another, forming a single landmass.",
"type": "quote"
}
],
"glosses": [
"Alternative form of Qinghai."
],
"id": "en-Ch'ing-hai-en-name-eY2tOZfB",
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],
"word": "Ch'ing-hai"
}
{
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"3": "青海//靑海",
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],
"etymology_text": "From Mandarin 青海／靑海 (Qīnghǎi) Wade–Giles romanization: Chʻing¹-hai³.",
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],
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"Mandarin terms with redundant transliterations",
"Pages with 1 entry",
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"examples": [
{
"ref": "1904, Charles Daniel Tenney, Geography of Asia, London: Macmillan and Co., →OCLC, page 5:",
"text": "The Yellow River (黃河) rises in small lakes in the southern part of Ch'ing-hai (青海) and flows in a very crooked channel toward the north-east to Lan-chou Fu (蘭州府).",
"type": "quote"
},
{
"ref": "1925, Francis Younghusband, Peking to Lhasa, London: Constable and Company, →OCLC, page 112:",
"text": "Leaving this town and the Sining River valley the road ascends a grassy valley with some recently started cultivation to a pass, 10,780 feet, over the Jih-yüeh Shan range, 27 miles from Tangar. This is the boundary between the Kansu and Ch'ing-hai Provinces. It is also the real boundary between China and Tibet, though the present frontier is the Tang-la Range, running east and west, the divide between the Salween and Mekong rivers.",
"type": "quote"
},
{
"ref": "1970, Joseph B. R. Whitney, China: Area, Administration, and Nation Building, Department of Geography, University of Chicago, →LCCN, →OCLC, page 38:",
"text": "In the west, the outer periphery of the Inner Zone is the great divide separating Pacific Ocean and South China Sea drainage on the one hand, from drainage oriented towards Hsin-chiang in the northwest and towards the Indian Ocean in the southwest, on the other. This divide also represents a fairly pronounced stress zone between the tenuous power China has been able to maintain over Tibet to the west and the firmer control she has been able to exercise over Hsi-k'ang and Ch'ing-hai to the east.",
"type": "quote"
},
{
"ref": "1972, T. V. W., “TIBET”, in Encyclopedia Britannica, volume 21, →ISBN, →LCCN, →OCLC, page 1108, column 2:",
"text": "For centuries the area of ethnic Tibet was divided into the following: Dbus and Gtsang (comprising central Tibet), Mnga’-ris, Khams, and A-mdo.[…]A-mdo, the northeastern part of ethnic Tibet, passed under Manchu control in 1724 following the suppression of a Mongol revolt against the throne. This area was officially incorporated into the Chinese provincial system as Ch’ing-hai Province in 1928.",
"type": "quote"
},
{
"ref": "2007, Laurie Burnham, Rivers (The Extreme Earth), Chelsea House, →ISBN, →LCCN, →OCLC, page 45:",
"text": "The Yangtze River first formed millions of years ago, a by-product of continental drift. Although the process itself took many millennia, the Ch'ing-hai (Qinghai) Plateau, from which the Yangtze descends, rose from the Earth's crust some 40 million years ago when the Indian subcontinent and Eurasia crashed into one another, forming a single landmass.",
"type": "quote"
}
],
"glosses": [
"Alternative form of Qinghai."
],
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"Qinghai",
"Qinghai#English"
]
],
"tags": [
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],
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"Encyclopædia Britannica"
]
}
],
"word": "Ch'ing-hai"
}
Download raw JSONL data for Ch'ing-hai meaning in All languages combined (3.9kB)
This page is a part of the kaikki.org machine-readable All languages combined dictionary. This dictionary is based on structured data extracted on 2024-11-06 from the enwiktionary dump dated 2024-10-02 using wiktextract (fbeafe8 and 7f03c9b). 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.
If you use this data in academic research, please cite Tatu Ylonen: Wiktextract: Wiktionary as Machine-Readable Structured Data, Proceedings of the 13th Conference on Language Resources and Evaluation (LREC), pp. 1317-1325, Marseille, 20-25 June 2022. Linking to the relevant page(s) under https://kaikki.org would also be greatly appreciated.