That's most often an erosionally truncated surface of rock. ie, it *was* at one time deep beneath the surface under great pressure. What was once above it is no more.
To follow up, often an erosionally truncated surface can be correlated with identical rock layers at another location where the overlying (younger) rock layers are still present. The Catskills are loaded with such examples. (I see from your About page you're from the New York area as well).
And since you recommended some books, here are a couple I recommend. Sorry, they don't have one for Joisey:
http://geology.com/store/roadside-geology-new-york.shtml
_________________________________________________________
http://geology.com/store/roadside-geology-pennsylvania.shtml