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意味・対訳 甘粛省の中央および西側の細長い一帯が河西回廊に相当する 河西回廊(かせいかいろう、河西走廊、甘粛走廊)は、チベット高原北西端に接する細長い形の地域・交通路の呼称で、黄河の西側にあるためにこの名で呼ばれる。
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According to statistical data about the number of days when a sandstorm was generated in the area from Dunhuang City to Hexi Corridor, slightly less than 50 percent of the occurrences were concentrated in the three months of spring.発音を聞く 例文帳に追加
敦煌市から河西回廊での砂塵嵐の日数を調べた統計では、春の3ヶ月間に年間の5割弱が集中する。 - Wikipedia日英京都関連文書対訳コーパス
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Wiktionary英語版での「Hexi Corridor」の意味 |
Hexi Corridor
別の表記
- (from Wade–Giles) Ho-hsi Corridor
語源
Partial calque of Mandarin and from the Hanyu Pinyin romanization of the Mandarin Chinese pronunciation for 河西走廊 (Héxī Zǒuláng).
固有名詞
- (historical) Part of the Northern Silk Road running northwest from the bank of the Yellow River. Consisting of a string of oases, it was the most important route from North China to the Tarim Basin and Central Asia for traders and the military.
- [1964, Yu-ti (任育地) Jen, 中国地理概述 [A Concise Geography of China][1], Peking: Foreign Languages Press, →OCLC, page 195:
- The Hohsi Corridor is long, narrow and easily passable. Over 1,000 kilometres in length, it is bordered on the south by the Chilien Mountains and on the north by the broken, slightly lower Peishan Mountains. It is penetrated by the rolling sand from Inner Mongolia. The corridor, though an arid area, is constantly watered by the melting snow and ice from the Chiliens. The irrigation system here goes back 2,000 years, when agriculture was originally developed on the oases on which most of the towns and villages have since arisen.]
- [1969, “Northwest China: The Mongolian-Sinkiang Region”, in The Physical Geography of China[2], volume II, Frederick A. Praeger, →LCCN, →OCLC, page 212:
- The geological structure of the Alashan Plain is more complex. The central portion of it was composed of ancient pre-Sinian deposits which were gradually overlaid by a mantle of Quaternary sands, but crop out on the surface in the elevations. The northern part is composed of Paleozoic and Mesozoic (chiefly Cretaceous) sediments while the southern piedmont portion (i.e., the Hohsi Corridor) was filled by beds of Paleozoic sedimentary and Meso-Cenozoic continental deposits which reach particularly great thickness in certain depressions such as the Chiuch’uan, Kanchou and Chaoshui.]
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