Hall Basin refers to a specific geological feature located in Antarctica, particularly in the eastern section of the continent. It is a subglacial basin, meaning it is situated beneath ice sheets, and is primarily filled with glacial ice. The basin has been of interest to scientists due to its potential implications for understanding ice sheet dynamics and contributions to sea-level rise. The studies in Hall Basin focus on various aspects such as subglacial hydrology, geology, and the history of ice flow in the region.
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