Trans-Himalayan glaciation

Target entity: Trans-Himalayan glaciation
Context triple: [Rimo Glacier, partOf, Trans-Himalayan glaciation]

• A. Études sur les glaciers
  Études sur les glaciers is a foundational 1840 scientific work by Louis Agassiz that helped establish the study of glaciers and the concept of past ice ages in geology.
• B. Dhaulagiri glacial system
  The Dhaulagiri glacial system is the network of high-altitude glaciers and icefields surrounding Mount Dhaulagiri in the Himalayas, feeding major rivers and shaping the region’s alpine landscape.
• C. Cenozoic glaciations
  Cenozoic glaciations are a series of major ice age cycles during the Cenozoic Era that saw extensive growth and retreat of continental ice sheets, profoundly shaping Earth’s climate and landscapes.
• D. Coastal mountain glaciers of Alaska
  Coastal mountain glaciers of Alaska are a vast system of ice masses flowing from rugged coastal mountain ranges into fjords and the Gulf of Alaska, playing a major role in regional climate, sea level contributions, and Alaska’s dramatic glaciated landscapes.
• E. Te Anau Basin glacial system
  The Te Anau Basin glacial system is a major Pleistocene glacial landscape in Fiordland, New Zealand, whose ice carved the surrounding fiords, valleys, and basins including those around Lake Te Anau.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Trans-Himalayan glaciation
Target entity description: Trans-Himalayan glaciation refers to the extensive system of high-altitude glaciers and perennial ice fields spanning the Trans-Himalayan region north of the main Himalayan range.

• A. Études sur les glaciers
  Études sur les glaciers is a foundational 1840 scientific work by Louis Agassiz that helped establish the study of glaciers and the concept of past ice ages in geology.
• B. Dhaulagiri glacial system
  The Dhaulagiri glacial system is the network of high-altitude glaciers and icefields surrounding Mount Dhaulagiri in the Himalayas, feeding major rivers and shaping the region’s alpine landscape.
• C. Cenozoic glaciations
  Cenozoic glaciations are a series of major ice age cycles during the Cenozoic Era that saw extensive growth and retreat of continental ice sheets, profoundly shaping Earth’s climate and landscapes.
• D. Coastal mountain glaciers of Alaska
  Coastal mountain glaciers of Alaska are a vast system of ice masses flowing from rugged coastal mountain ranges into fjords and the Gulf of Alaska, playing a major role in regional climate, sea level contributions, and Alaska’s dramatic glaciated landscapes.
• E. Te Anau Basin glacial system
  The Te Anau Basin glacial system is a major Pleistocene glacial landscape in Fiordland, New Zealand, whose ice carved the surrounding fiords, valleys, and basins including those around Lake Te Anau.
• F. None of above. chosen