No, your eyes aren’t deceiving you, these rock layers are nearly vertical!
Although they were once horizontal, these Paleozoic sedimentary units have been tilted so that they now dip nearly 90 degrees.
These rocks are located in northeast Tennessee and are part of the Appalachian foreland fold-thrust belt. Though built by multiple orogenies, the Alleghenian Orogeny (325-260 Ma) was the final stage in forming the Appalachian Mountains and resulted in a series of imbricated reverse faults.
Consequently, rocks got compressed, thrusted and tilted. In order to determine whether these rocks were rotated clockwise or counter-clockwise from their original horizontality, we have to look for up-direction indicators (i.e. indicators that will tell us which direction originally faced upwards). These may include: graded bedding, cross-bedding, sole markings, ripple marks, etc.
Image by author | Outcrop along Hwy 70 near Rogersville, Tennessee