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The Natkusiak flood basalts are a sequence of Neoproterozoic continental flood basalts of the Franklin Large Igneous Province on Victoria Island, Canada. The flood basalts were erupted about 720 million years ago after uplift began three to five million years prior to the flood basalt volcanism. This uplift and flood basalt volcanism was caused by a mantle plume. This flood basalt sequence is related to the Franklin magmatic event.

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  • Colate basaltiche Natkusiak (it)
  • Natkusiak flood basalts (en)
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  • The Natkusiak flood basalts are a sequence of Neoproterozoic continental flood basalts of the Franklin Large Igneous Province on Victoria Island, Canada. The flood basalts were erupted about 720 million years ago after uplift began three to five million years prior to the flood basalt volcanism. This uplift and flood basalt volcanism was caused by a mantle plume. This flood basalt sequence is related to the Franklin magmatic event. (en)
  • Le colate basaltiche Natkusiak sono una sequenza di colate basaltiche continentali risalenti al Neoproterozoico, che si trovano nell'Isola Victoria, in Canada e fanno parte della Grande provincia ignea Franklin. Le colate di magma basaltico furono eruttate circa 720 milioni di anni fa, dopo un sollevamento tettonico che era iniziato da tre a cinque milioni di anni prima del vulcanismo basaltico. Sia il sollevamento tettonico che il vulcanismo furono causati un mantle plume, un pennacchio del mantello. La sequenza delle colate basaltiche è collegata all'evento magmatico Franklin. (it)
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  • The Natkusiak flood basalts are a sequence of Neoproterozoic continental flood basalts of the Franklin Large Igneous Province on Victoria Island, Canada. The flood basalts were erupted about 720 million years ago after uplift began three to five million years prior to the flood basalt volcanism. This uplift and flood basalt volcanism was caused by a mantle plume. This flood basalt sequence is related to the Franklin magmatic event. (en)
  • Le colate basaltiche Natkusiak sono una sequenza di colate basaltiche continentali risalenti al Neoproterozoico, che si trovano nell'Isola Victoria, in Canada e fanno parte della Grande provincia ignea Franklin. Le colate di magma basaltico furono eruttate circa 720 milioni di anni fa, dopo un sollevamento tettonico che era iniziato da tre a cinque milioni di anni prima del vulcanismo basaltico. Sia il sollevamento tettonico che il vulcanismo furono causati un mantle plume, un pennacchio del mantello. La sequenza delle colate basaltiche è collegata all'evento magmatico Franklin. (it)
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