Cross-cutting relations

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Woudloper

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Diagram illustrating cross-cutting relations in geology. These relations can be used to give structures a relative age. Explanations: A - folded rock strata cut by a thrust fault; B - large intrusion (cutting through A); C - erosional angular unconformity (cutting off A & B) on which rock strata were deposited; D - volcanic dyke (cutting through A, B & C); E - even younger rock strata (overlying C & D); F - normal fault (cutting through A, B, C & E).

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Creative Commons Attribution-Share Alike 1.0