Mersey–Dee glacial meltwater landscape

Target entity: Mersey–Dee glacial meltwater landscape
Context triple: [Ellesmere meres, partOf, Mersey–Dee glacial meltwater landscape]

• A. British–Irish Ice Sheet
  The British–Irish Ice Sheet was a massive glacial ice sheet that covered most of Great Britain and Ireland during the last Ice Age, shaping much of the region’s present-day landscape.
• B. Wisconsin glaciation
  The Wisconsin glaciation was the last major advance of continental ice sheets in North America during the Pleistocene, profoundly reshaping the continent’s landscapes and drainage systems.
• 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. Holocene catastrophic flooding of the Black Sea
  The Holocene catastrophic flooding of the Black Sea is a hypothesized prehistoric deluge in which Mediterranean waters are thought to have rapidly inundated the Black Sea basin, potentially inspiring ancient flood myths.
• E. Pennine watershed
  The Pennine watershed is the major upland drainage divide running along the Pennine hills of northern England, separating river systems that flow west to the Irish Sea from those that flow east to the North Sea.
• F. None of above. chosen
• G. Unsure - the case is ambiguous/there is not enough information to decide.

Target entity: Mersey–Dee glacial meltwater landscape
Target entity description: The Mersey–Dee glacial meltwater landscape is a distinctive post-glacial terrain in northwest England and northeast Wales, characterized by features such as meres, kettle holes, and meltwater channels formed during the last Ice Age.

• A. British–Irish Ice Sheet
  The British–Irish Ice Sheet was a massive glacial ice sheet that covered most of Great Britain and Ireland during the last Ice Age, shaping much of the region’s present-day landscape.
• B. Wisconsin glaciation
  The Wisconsin glaciation was the last major advance of continental ice sheets in North America during the Pleistocene, profoundly reshaping the continent’s landscapes and drainage systems.
• 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. Holocene catastrophic flooding of the Black Sea
  The Holocene catastrophic flooding of the Black Sea is a hypothesized prehistoric deluge in which Mediterranean waters are thought to have rapidly inundated the Black Sea basin, potentially inspiring ancient flood myths.
• E. Pennine watershed
  The Pennine watershed is the major upland drainage divide running along the Pennine hills of northern England, separating river systems that flow west to the Irish Sea from those that flow east to the North Sea.
• F. None of above. chosen