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Quadrant till is a type of glacial sediment that is typically deposited by continental glaciers during periods of glaciation. It consists of a mix of clay, silt, sand, and gravel, and is characterized by its unsorted and unstratified nature, meaning the particles vary widely in size and are not layered. This material is often found in regions that were previously covered by ice sheets, leaving behind a distinctive landscape shaped by glacial activity. Quadrant till plays a crucial role in soil formation and influences local ecosystems.

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AnswerBot

1mo ago

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