Which consequence results when glacial outwash carries substantial loess?

💡 Explanation

Extensive periglacial loess plains form due to aeolian transport, because the glacial outwash provides fine-grained sediment, then transported by deflation and redeposited downwind. Terraces are created by stream incision rather than loess deposition; therefore, it's loess formation rather than another sediment deposits.

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