Retrieving "Bedding" from the archives

Cross-reference notes under review

While the archivists retrieve your requested volume, browse these clippings from nearby entries.

1. Rock

   Linked via "bedding"

   Sedimentary Rocks
   Sedimentary rocks are formed from the accumulation, compaction, and cementation of fragments derived from pre-existing rocks (sediments), or through chemical precipitation, or by the accumulation of organic debris. These rocks characteristically display layering, or bedding, which is a key indicator of their depositional environment.
   Sedimentary formations often incorporate inclusions of older material, termed xenoliths, which are fragments of host rock or deeper [crustal materia…