File:Faulted sandstone 5.jpg

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English: (public display, Sternberg Museum of Natural History, Hays, Kansas, USA)

Faults are quite common in orogenic belts. Faults are defined as fractures in rocks along which differential displacement has occurred. Dip-slip faults are those involving movement of rocks in non-horizontal directions. Strike-slip faults involve movement of rocks in horizontal directions.

The two common types of dip-slip faults are normal faults and reverse faults. Normal faults form by extensional stress. Reverse faults form by compressional stress.

Locality: unrecorded/undisclosed, but possibly from South Dakota, USA
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Source https://www.flickr.com/photos/47445767@N05/32304411641/
Author James St. John

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This image was originally posted to Flickr by James St. John at https://flickr.com/photos/47445767@N05/32304411641. It was reviewed on 2 December 2020 by FlickreviewR 2 and was confirmed to be licensed under the terms of the cc-by-2.0.

2 December 2020

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current15:36, 2 December 2020Thumbnail for version as of 15:36, 2 December 20203,008 × 2,000 (5.41 MB)Ser Amantio di Nicolao (talk | contribs)Uploaded a work by James St. John from https://www.flickr.com/photos/47445767@N05/32304411641/ with UploadWizard

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