Yeah, so these these different
colors on these cross sections
represent different different
lithologies and we
have you know typical
in kind of
ore You know deposit
type geology.
We have what is called a hanging
wall and a foot wall And
those are kind of old terms really
for just what's above you and what's
what's below you and this
Is a stratigraphic
deposit so So
the ore mineralization.
Is this red here, as well
as the purple, and we
get kind of pervasive mineralization
through this lighter purple as well.
So this is kind of what we call the
mineralized series.
Everything out of there, outside of
that, both above and below it,
within the hanging wall up here and
footwall here, is kind benign,
just host rock, just
a series of
volcanic and volcanic-clastic
rocks that were overlaying
on the deposit.
Completely unrelated to the
mineralizing event.
Yeah, so this
is just, this is a plan map, so
we're looking straight down,
looking at the historic
drill holes here, in kind of this
lighter gray, more bold holes,
are the holes that we drilled
this past summer.
These red intervals represent
mineralized
intervals within all of those drill
holes.
So and then back to those cross
sections, these blue lines represent
those vertical slices,
you know, this one being this one
here and
this one, being this one here.
And again, just kind of showing that
through the drilling that
we did this summer,
you know we just kind-of identified
a thickening
of mineralization at
depth and going off to
the east, which actually...
On this long section,
you know, a long section here,
this is kind of a pseudo vertical
look, but like head-on to
the deposit. So looking at that
deposit is just a flat plane,
and all these points on here
represent the pierce points where
those drill holes intercepted
that mineralized
horizon.
This orange here represents
kind of the historic extents of kind
of, the core deposit area.
This orange outline
here represents a few
kind of far-spaced holes where they
had intercepted mineralization
kind of
down plunge to
the east of the core deposit and
these labeled holds here
are the six holds that we drilled
this past summer.
Trying to figure out the continuity
between that
core historic deposit and
these step-out holes that were
drilled previously.
These contours here show the
thickness, kind of
the true thickness of that
mineralized section.
So you can see that some
of the, you know, the thickest area
in the core deposit is roughly 22
meters,
and I can't remember exactly what
hole that was,
but B25.
04 also represents
one of the thickest intercepts that
have been recorded on
the deposit to date.
And by creating these plots,
we can
figure out where we think that
main mineralized section
of the deposit is
going. So our future drilling will
be stepping out on
the holes that we drilled here to
really define the trend
of that mineralization and
see how far it goes.
Then we can probably look at some
core.