The term "Cato Trough" refers to a specific geographical feature in Antarctica, specifically located in the southeastern part of the continent. It is a deep, glacially eroded valley or trough that is situated between the South Polar Plateau and the surrounding mountainous regions. The Cato Trough is characterized by significant ice coverage, with glaciers flowing into it from adjacent areas. Geological features like the Cato Trough contribute to our understanding of glaciation processes and the climatic history of Antarctica.
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