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About: Dragon Cliff

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Dragon Cliff is a basaltic monolith located on western Axel Heiberg Island, Nunavut, Canada. It is the most striking feature of and rises several hundred metres out of the fiord. Dragon Cliff is made of flood basalt lava flows that contain more than 10 flow units totalling over 200 m (660 ft) of stratigraphic thickness. It is part of the Albian Strand Fiord Formation, which in turn forms part of the High Arctic Large Igneous Province. The Strand Fiord Formation is interpreted to represent the cratonward extension of the Alpha Ridge.

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  • Dragon Cliff is a basaltic monolith located on western Axel Heiberg Island, Nunavut, Canada. It is the most striking feature of and rises several hundred metres out of the fiord. Dragon Cliff is made of flood basalt lava flows that contain more than 10 flow units totalling over 200 m (660 ft) of stratigraphic thickness. It is part of the Albian Strand Fiord Formation, which in turn forms part of the High Arctic Large Igneous Province. The Strand Fiord Formation is interpreted to represent the cratonward extension of the Alpha Ridge. (en)
  • Acantilados Dragón (en inglés: Dragon Cliffs) es un monolito de basalto situado al oeste de la isla Axel Heiberg, en Nunavut, Canadá. Es la característica más llamativa del Fiordo Expedición y se eleva a varios cientos de metros de este último. El Acantilado dragón está hecho de los flujos de inundación de lava basáltica que contienen más de 10 unidades de flujo totalizando más de 200 m (656 pies) de espesor estratigráfico. Es parte de la formación Fiordo Albian Strand. Se cree que representan la extensión de la Cordillera Alpha.​ (es)
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  • Dragon Cliff is a basaltic monolith located on western Axel Heiberg Island, Nunavut, Canada. It is the most striking feature of and rises several hundred metres out of the fiord. Dragon Cliff is made of flood basalt lava flows that contain more than 10 flow units totalling over 200 m (660 ft) of stratigraphic thickness. It is part of the Albian Strand Fiord Formation, which in turn forms part of the High Arctic Large Igneous Province. The Strand Fiord Formation is interpreted to represent the cratonward extension of the Alpha Ridge. (en)
  • Acantilados Dragón (en inglés: Dragon Cliffs) es un monolito de basalto situado al oeste de la isla Axel Heiberg, en Nunavut, Canadá. Es la característica más llamativa del Fiordo Expedición y se eleva a varios cientos de metros de este último. El Acantilado dragón está hecho de los flujos de inundación de lava basáltica que contienen más de 10 unidades de flujo totalizando más de 200 m (656 pies) de espesor estratigráfico. Es parte de la formación Fiordo Albian Strand. Se cree que representan la extensión de la Cordillera Alpha.​ (es)
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  • Acantilados Dragón (es)
  • Dragon Cliff (en)
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