See Sogo Nur in All languages combined, or Wiktionary
Download JSON data for Sogo Nur meaning in English (3.7kB)
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{
"kind": "place",
"langcode": "en",
"name": "Lakes",
"orig": "en:Lakes",
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"examples": [
{
"ref": "1993 August, Miao Wang, Shi Bao Xiu, “A Detour Through the Desert to Etzina”, in Tu Nai Hsien, editor, From the Pamirs to Beijing: Tracing Marco Polo's Northern Route, Hong Kong: HK China Tourism Press, →OCLC, page 94, columns 1, 2",
"text": "When we were in Zhangye we consulted a map and saw that the Ruoshui River has its source in the Qilian Mountains, then winds north through the Hexi Corridor and into the desert. It then flows through the forests of Ejin Banner and pours into two lakes — the Gaxun Nur and the Sogo Nur.[...]\nThe Mongolian woman told us that in recent years the water flowing from the south has seldom reached the lakes here, and consequently the Gaxun Nur had dried up. This summer, less water than usual had poured into the Sogo Nur, so it too was almost empty.[...]\nNext, we headed northeast to visit Sogo Nur. After two hours of driving through willow bushes no more than two feet in height, we saw the white surface of a lake. A solitary thatched cottage stood by the road leading to the lake, and the sound of our engine brought a middle-aged Mongolian man out to greet us. After a short conversation, she told us that the lake had dried up just ten days earlier.",
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"ref": "1996, Zhou Zhiyi, W. T. Dean, editors, Phanerozoic Geology of Northwest China, Beijing: Science Press, →OCLC, page 216",
"text": "In the Badain Jaran District (Fig. 15-1, II-8-2), marine Lower Carboniferous strata occur at Sogo Nur, in the western part of the northern area, and rest disconformably on Upper Devonian.",
"type": "quotation"
},
{
"ref": "2004 January, Jin Heling et al., “Vicissitude of Sogo Nur and environmental-climatic change during last 1500 years”, in Science China Earth Sciences, →DOI, →ISSN, →OCLC, archived from the original on 2022-08-22",
"text": "Lakes in arid zone are sensitive to climatic changes. The lacustrine sediment sequence in Sogo Nur has well and truly recorded climatic events such as the Sui-Tang Dynasty Warm Period, the Song-Liao Dynasty Cold Period, the Medieval Warm Period, the Little Ice Age and the 20th Century Warm Period.",
"type": "quotation"
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],
"glosses": [
"A lake in Ejin, Alxa, Inner Mongolia, in northern China."
],
"id": "en-Sogo_Nur-en-name-hBsbl-ou",
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"Alxa#English"
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"Inner Mongolia",
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"translations": [
{
"code": "cmn",
"lang": "Chinese Mandarin",
"sense": "lake",
"word": "蘇泊淖爾"
},
{
"code": "cmn",
"lang": "Chinese Mandarin",
"sense": "lake",
"word": "苏泊淖尔"
}
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],
"word": "Sogo Nur"
}
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"examples": [
{
"ref": "1993 August, Miao Wang, Shi Bao Xiu, “A Detour Through the Desert to Etzina”, in Tu Nai Hsien, editor, From the Pamirs to Beijing: Tracing Marco Polo's Northern Route, Hong Kong: HK China Tourism Press, →OCLC, page 94, columns 1, 2",
"text": "When we were in Zhangye we consulted a map and saw that the Ruoshui River has its source in the Qilian Mountains, then winds north through the Hexi Corridor and into the desert. It then flows through the forests of Ejin Banner and pours into two lakes — the Gaxun Nur and the Sogo Nur.[...]\nThe Mongolian woman told us that in recent years the water flowing from the south has seldom reached the lakes here, and consequently the Gaxun Nur had dried up. This summer, less water than usual had poured into the Sogo Nur, so it too was almost empty.[...]\nNext, we headed northeast to visit Sogo Nur. After two hours of driving through willow bushes no more than two feet in height, we saw the white surface of a lake. A solitary thatched cottage stood by the road leading to the lake, and the sound of our engine brought a middle-aged Mongolian man out to greet us. After a short conversation, she told us that the lake had dried up just ten days earlier.",
"type": "quotation"
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{
"ref": "1996, Zhou Zhiyi, W. T. Dean, editors, Phanerozoic Geology of Northwest China, Beijing: Science Press, →OCLC, page 216",
"text": "In the Badain Jaran District (Fig. 15-1, II-8-2), marine Lower Carboniferous strata occur at Sogo Nur, in the western part of the northern area, and rest disconformably on Upper Devonian.",
"type": "quotation"
},
{
"ref": "2004 January, Jin Heling et al., “Vicissitude of Sogo Nur and environmental-climatic change during last 1500 years”, in Science China Earth Sciences, →DOI, →ISSN, →OCLC, archived from the original on 2022-08-22",
"text": "Lakes in arid zone are sensitive to climatic changes. The lacustrine sediment sequence in Sogo Nur has well and truly recorded climatic events such as the Sui-Tang Dynasty Warm Period, the Song-Liao Dynasty Cold Period, the Medieval Warm Period, the Little Ice Age and the 20th Century Warm Period.",
"type": "quotation"
}
],
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"A lake in Ejin, Alxa, Inner Mongolia, in northern China."
],
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"Alxa#English"
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"translations": [
{
"code": "cmn",
"lang": "Chinese Mandarin",
"sense": "lake",
"word": "蘇泊淖爾"
},
{
"code": "cmn",
"lang": "Chinese Mandarin",
"sense": "lake",
"word": "苏泊淖尔"
}
],
"word": "Sogo Nur"
}
This page is a part of the kaikki.org machine-readable English dictionary. This dictionary is based on structured data extracted on 2024-05-20 from the enwiktionary dump dated 2024-05-02 using wiktextract (1d5a7d1 and 304864d). 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.