Here you go gents.
Original bedding (deposition planes) in white, fractures (brittle breaks in lithified sediment) in red. These are harmonic folds, where the fold geometry is echoed in adjacent beds.
Take a book or a deck of cards and bend it. Note that shear occurs along the existing planes.
The shear couples create the “cleavage” that is the fractures. Best seen in the right above the words “bedding slip”. Note the orientation of the fractures vs the orientation of the beding.
For contrast, here are two pictures of soft-deformation of sandstone.
Some original bedding is perserved but the folds are chaotic and and are disharmonic folds where folds are not seen in adjacent beds.
Hope this answers your questions.