In recent years, the study of glacial geomorphology, a subdiscipline of earth science has gained significant attention due to its crucial role in understanding the impacts of climate change on our planet. Glacial geomorphology refers to studying the morphological features and processes that shape glaciers and their surrounding environments. One fascinating aspect of glacial geomorphology is the formation of glacial erratics, which are large rocks transported and deposited by glaciers in locations far from their sources. These erratics provide valuable insights into the history and dynamics of glaciers and the geological processes that have shaped our landscapes over time.

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T-Pin
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