Last but not least are some pics of one of my most favorite pieces I've come across working with this material.
I call it "Kerplunck!"
See, if you think about this rock the way I do,
,
this so-called meta-sedimentary silt and mud stone, and the way and when it was formed,
then this could be a real cool piece.
So lets just say this rock formed 300-400 million years ago when there were volcanoes and vents
belching smoke and ash and sometimes lava out every so often.
My theory is that the ash that landed on dry ground packed together in the harder meta-sed material
the natives used as tool making, knapping, material. This softer stuff I've been working with here, I'm thinking, the ash landed in water, possibly shallow pools
and settled out into these layers. It was at this time, while still moist atleast, I think the faulting took place.
And this piece, Kerplunck.
It looks like the black chunk of rock landed in this pool while these layers were still very wet.
Maybe it is a cinder sent airborne from a nearby volcanic vent!
I've included a black and white version of the slab to help highlight the lines.