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The glacial control theory posits that changes in sea level are primarily driven by the growth and melting of continental glaciers. During periods of glaciation, vast amounts of water are locked up in ice sheets, causing global sea levels to drop. Conversely, as glaciers melt, this water returns to the oceans, leading to a rise in sea level. This phenomenon has been a recurring pattern throughout Earth's history, particularly during the Pleistocene Epoch, when fluctuations in glacial ice volume significantly impacted sea levels. Glacial erosion, caused by processes like abrasion and plucking, reshapes landscapes and contributes to the deposition of materials that can influence hydrology and land suitability.123456

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