Yellowstone hotspot track

Target entity: Yellowstone hotspot track
Context triple: [High Lava Plains, associatedWith, Yellowstone hotspot track]

• A. Hawaiian hotspot
  The Hawaiian hotspot is a long-lived volcanic plume in the Earth's mantle that has created the Hawaiian Island chain and associated seamounts as the Pacific Plate moves over it.
• B. Galápagos plume track
  The Galápagos plume track is a volcanic hotspot trail on the Pacific seafloor formed by the movement of tectonic plates over the Galápagos mantle plume, creating features such as the Cocos Ridge and associated seamount chains.
• C. Campeche–Fogo hotspot track
  The Campeche–Fogo hotspot track is a volcanic chain formed by the movement of the African Plate over a mantle hotspot, linking seamounts and volcanic islands such as Pico do Fogo across the Atlantic.
• D. Canary hotspot volcanic system
  The Canary hotspot volcanic system is a mantle plume-driven volcanic region responsible for forming and sustaining the volcanically active Canary Islands in the Atlantic Ocean.
• E. Galápagos hotspot
  The Galápagos hotspot is a volcanic mantle plume beneath the eastern Pacific Ocean responsible for creating the Galápagos Islands and associated seafloor features through long-term hotspot volcanism.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Yellowstone hotspot track
Target entity description: The Yellowstone hotspot track is a geologic feature marking the west-to-east progression of volcanic and tectonic activity across the northwestern United States as the North American Plate moves over a stationary mantle plume.

• A. Hawaiian hotspot
  The Hawaiian hotspot is a long-lived volcanic plume in the Earth's mantle that has created the Hawaiian Island chain and associated seamounts as the Pacific Plate moves over it.
• B. Galápagos plume track
  The Galápagos plume track is a volcanic hotspot trail on the Pacific seafloor formed by the movement of tectonic plates over the Galápagos mantle plume, creating features such as the Cocos Ridge and associated seamount chains.
• C. Campeche–Fogo hotspot track
  The Campeche–Fogo hotspot track is a volcanic chain formed by the movement of the African Plate over a mantle hotspot, linking seamounts and volcanic islands such as Pico do Fogo across the Atlantic.
• D. Canary hotspot volcanic system
  The Canary hotspot volcanic system is a mantle plume-driven volcanic region responsible for forming and sustaining the volcanically active Canary Islands in the Atlantic Ocean.
• E. Galápagos hotspot
  The Galápagos hotspot is a volcanic mantle plume beneath the eastern Pacific Ocean responsible for creating the Galápagos Islands and associated seafloor features through long-term hotspot volcanism.
• F. None of above. chosen