So I've kind of discussed the
hanging wall, kind of
relatively unrelated volcanic
rocks that were just piled
on top of that mineralized section,
so that's kind of what we're looking
at.
Looking at here, you know,
it's kind variable textures,
kind going from volcanic plastic
to volcanic plastic sediments,
tufts.
A few kind of coarser green lapilli
tufts.
And this is what most people just
refer to as bedrock.
Yeah, well I mean bedrock can be
anything.
But up here, if someone's
dredging a well or
if they hit bedrock, they're getting
this.
In this area, anyways, throughout
this volcanic belt, you're going to
see some
fashion of volcano-clastic
rocks and or volcanically
related intrusive rocks.
Mm-hmm.
Of this.