About: Keluo

An Entity of Type: Cinder cone, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

Keluo (Chinese: 科洛, p Kēluò) is a dormant volcanic field 310 kilometers (190 mi) north-by-northwest of in northeastern China. It is located at an intersection of regional lineaments trending northeast and northwest; the volcanoes were erupted through basement igneous and sedimentary rocks from the Jurassic to Cretaceous, through granite, and through pre-Permian metasediments. Like the Wudalianchi volcanic to its south, it contains high-potassium basaltic cinder cones. Other peaks include Dangzishan, Heishan, and Muhenanshan.

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dbo:abstract
  • Die Keluo-Vulkangruppe (chinesisch 科洛火山群, Pinyin kēluò huǒshān qún, englisch Keluo volcanic field) ist eine Vulkangruppe in der chinesischen Provinz Heilongjiang in Nordost-China. Sie liegt auf dem Gebiet der Großgemeinde des Kreises Nenjiang ungefähr in der Mitte des großen Bogens des Flusses Heilong Jiang (Amur). Ihr höchster Vulkan ist 670 m hoch. Die Vulkangruppe liegt am Übergang von Großem Hinggan-Gebirge und der Song-Nen-Ebene (Song-Nen pingyuan 松嫩平原 der Flüsse Sungari und Nen Jiang). Es gibt dort auf einem Gebiet von 350 Quadratkilometern 23 Vulkankegel, relativ vollständig erhalten sind fünf: Keluo Nanshan 科洛南山, Keluo Gushan 科洛孤山, Keluo Jianshan 科洛尖山, Keluo Dayishan 科洛大椅山 und Keluo Xiaoyishan 科洛小椅山. (de)
  • Keluo (Chinese: 科洛, p Kēluò) is a dormant volcanic field 310 kilometers (190 mi) north-by-northwest of in northeastern China. It is located at an intersection of regional lineaments trending northeast and northwest; the volcanoes were erupted through basement igneous and sedimentary rocks from the Jurassic to Cretaceous, through granite, and through pre-Permian metasediments. Like the Wudalianchi volcanic to its south, it contains high-potassium basaltic cinder cones. The field possesses 23 cones over an area of 350 km2 (140 sq mi). There are reports of historical activity, but these remain unconfirmed. The morphology of a number of the cones—including Nanshan (南山), Gushan (孤山), Jianshan (尖山), Dayishan (大椅山), and Xiaoyishan (小椅山)—suggests their formation during the last 10,000 years (the Holocene). Most cones to the northeast, however, probably date from the Pleistocene to the Tertiary. Other peaks include Dangzishan, Heishan, and Muhenanshan. (en)
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  • 542.000000 (xsd:double)
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  • 0300-01-01 (xsd:gYear)
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  • Keluo Volcanic Field (en)
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  • Die Keluo-Vulkangruppe (chinesisch 科洛火山群, Pinyin kēluò huǒshān qún, englisch Keluo volcanic field) ist eine Vulkangruppe in der chinesischen Provinz Heilongjiang in Nordost-China. Sie liegt auf dem Gebiet der Großgemeinde des Kreises Nenjiang ungefähr in der Mitte des großen Bogens des Flusses Heilong Jiang (Amur). Ihr höchster Vulkan ist 670 m hoch. (de)
  • Keluo (Chinese: 科洛, p Kēluò) is a dormant volcanic field 310 kilometers (190 mi) north-by-northwest of in northeastern China. It is located at an intersection of regional lineaments trending northeast and northwest; the volcanoes were erupted through basement igneous and sedimentary rocks from the Jurassic to Cretaceous, through granite, and through pre-Permian metasediments. Like the Wudalianchi volcanic to its south, it contains high-potassium basaltic cinder cones. Other peaks include Dangzishan, Heishan, and Muhenanshan. (en)
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  • Keluo-Vulkangruppe (de)
  • Keluo (en)
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  • Keluo Volcanic Field (en)
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