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Fold (geology) and Welsh Borderland Fault System

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Fold (geology) and Welsh Borderland Fault System

Fold (geology) vs. Welsh Borderland Fault System

A geological fold occurs when one or a stack of originally flat and planar surfaces, such as sedimentary strata, are bent or curved as a result of permanent deformation. The Welsh Borderland Fault System is a zone of faulting and associated folding which runs northeastwards through Wales from Pembrokeshire through Carmarthenshire and Powys into Shropshire in England.

Similarities between Fold (geology) and Welsh Borderland Fault System

Fold (geology) and Welsh Borderland Fault System have 1 thing in common (in Unionpedia): Fault (geology).

Fault (geology)

In geology, a fault is a planar fracture or discontinuity in a volume of rock, across which there has been significant displacement as a result of rock-mass movement.

Fault (geology) and Fold (geology) · Fault (geology) and Welsh Borderland Fault System · See more »

The list above answers the following questions

Fold (geology) and Welsh Borderland Fault System Comparison

Fold (geology) has 51 relations, while Welsh Borderland Fault System has 14. As they have in common 1, the Jaccard index is 1.54% = 1 / (51 + 14).

References

This article shows the relationship between Fold (geology) and Welsh Borderland Fault System. To access each article from which the information was extracted, please visit:

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