Take a crack at it. I’ll discuss it in full tomorrow later.
The blue thing is the handle of a dry-erase marker, to give you a sense of scale.
Take a crack at it. I’ll discuss it in full tomorrow later.
The blue thing is the handle of a dry-erase marker, to give you a sense of scale.
Parallel kink-bands in shale or siltstone. Kink-bands formed from compressional strain acting subparallel to the bedding (or is it slaty cleavage?). Then the whole mess was rotated into its current position during mountain building. I can’t tell if the beds are overturned or not.
Strongly cleaved shale with thin widely-spaced carbonate beds–both dipping in same direction–anticlinal axis to right, synclinal axis to left
Good guesses. One of you is pretty close. I’ve run out of time for today, so I’ll have to put the explanation off for later – more time for people to guess…