Retrieving "Sediment Source" from the archives

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1. Loess

   Linked via "sediment source"

   Loess deposition is intrinsically linked to arid or semi-arid conditions proximal to major glacial outwash plains or extensive desert basins during peak Quaternary glaciation cycles. The source material for most significant loess blankets originates from glacial flour or fine detritus mobilized from previously eroded [bedrock structures](/entries/bedrock-…