When
we met again with the UT Geology
Department Dean again, they re-examined BCC9601 and many, many more
samples. The
Dean was given some Pilot Knob material by us and with witnesses
present said, "well you're right it's not Pilot Knob material".
And then I said "no it's not". And Steve Thompson said to us,
" but look
at that topo map on the table, Pilot Knob is south and much lower in
elevation than Boggy Creek. BCC9601 is very heavy, you don't think it
would have washed uphill do you?" And I said, "It would also have to
cross the Colorado River which is very, very wide."
The
Dean agreed to make
some thin sections and examine them under a microscope and report his
findings. About a week later he called me and said, "well I have the
results and its just plain ordinary plagioclase and pyroxene". I said,
"great, wonderful". He said, "why are you so excited?" I said, "because
those are the two primary components of stony meteorites confirming our
lab data." (These are incompatible phases in an achondrite). He was not
very happy to hear this.
Shortly after
this meeting we had agreed to particpate in a human interest story with
the local paper, and with
reporters wanting the details and at his heels with a printing deadline
looming, the Dean
regrouped and said to me over the telephone, "it is Llano Uplift
material" (granite) shown below. When we requested a
meeting with him to show him the difference between our samples and
granite, (reporters also said they wanted to be there), he quickly
withdrew that statement and shifted to say it was "West Texas
Volcanics" found about seven to eight hundred miles away. Dr. Cloos
always waited until no one was present and tried to relay these
statements to me over the phone so no one else could hear. It became
evident to the reporter, Dick Stanley, and us that Dr. Cloos was
sending
everyone on a wild goose chase to buy time knowing the newspaper had a
deadline to meet to print the newspaper article. In fact, when I
informed Dick Stanley what Dr. Cloos
was saying (first Pilot Knob, then Llano Uplift-Granite and then West
Texas Volcanics) even he commented,
"Ohohohohohhhhh..................... nowwwwww.....
I see what's going on." The reporter realized that the Dean was
lying and attempting to send everyone on a wild goose chase to
interfere with the newspaper article.
Without going
into so much unnecessary detail about west Texas volcanics, because
anyone can tell the differences
by examining all the samples mentioned and
using common sense. We
present the terrestrial sample photos below and a brief explanation to
each. Folks,
that ancient basaltic material (West Texas volcanics) saturates our
railroad tracks in pieces and fragments in crushed form around railroad
ties
and iron tracks to serve as drainage, and plant growth control. No one,
not even first and second year geology students, can mistake meteorite
samples with that quarried basalt. You should have heard what was let
out at the other end of the phone when I told the Dean we were headed
back to the lab to conduct major and minor phase analysis using X-ray
diffraction and micro-analysis techniques. This was not a happy person.
And then along comes UCLA making all sorts of claims, soliciting
samples over the internet and making statements not even
worthy
of print. If you can tell the difference between terrestrial and non
terrestrial phlogopite and it's not difficult, that pretty much takes
care of them. Now having said that, Dr. Cloos at UT Austin is a very,
very fine person, I'm sure, and Alan Rubin is a very, very fine person;
I am sure of that. But when you create a situation where the evidence
submitted is contrary to your statements, nip it in the bud quickly and
do the right thing. You know you've waited too long when you've gotten
rid of the body but the stench remains.
We mention
UCLA here because we used them as a test case to see what level of
collusion exists between scientists in attempting to perpetaute a fraud
and to see if this was confirmable. Our suspicions about fraud and
scientific misconduct to achieve that fraud were already alerted to by
the conduct of previous participants. This test case with UCLA required
that they recieve the sample without notification or being alerted and
shows that the sample receiving scientist will generally network with
remote University scientists (in this case UT) to make a decision
rather than think, work, and act independently and with integrity on
newly arriving samples. As part of his collusion with UT, Alan Rubin
decided to say that water bearing mineralogy existed in the sample
(BCC9601) refusing to tell us what mineral it is. This is very
important because it means he (they) was in contact with UT. He knew
from UT that UT painted themselves into a corner with their intentional
and constantly shifting claims, and he knew we were working with a
private lab so that if he made any claims we would be able to confirm
or deny it. These are the main reasons he, Wasson and Warren
avoided giving out a name for this "water bearing mineralogy". But the
main point we want to show here is the level of collusion that goes
into bigotry, racism and discrimination engaging in scientific
misconduct and fraud by "academics".
|
The material at left is Pilot
Knob cretaceous era volcanic, plutonic material. This cooled and
solidified beneath the cretaceous sea floor but originated in the upper
mantle region as a magma millions of years ago. This material is dated
approximately 87 million years and contains a large amount of iron, is
very heavy and dense, is not magnetic and does not contain any
noticeable visible nickel particles, fragments, or crystals such as can
be found in meteorites. This also contains water which can be seen
within the structure chemically. The smooth lighter surfaces which are
evident, were pushed upwards adjacent to the limestone cretaceous
sea floor which is why the surface is smooth. This does not chemically
match BCC9601 which is a refractory rich high Al anorthosite and is
dated for practical purposes, almost a billion years older (cooling and
crystallization history) than Pilot Knob material.
The
samples below leftr are from the
Llano Uplift area of Central Texas, and show from left to right,
granite gneiss and, in the
middle, pink granite with large quartz crystals at the top edge. The
third piece is also pink granite but was included because it is a
special kind of granite. This sample is from deep beneath the outcrop
and has a higher density and smaller crystals than the ordinary granite
in the middle. The gneiss on the left was also used by Native Americans
as a metate which is a stone tool for grinding seeds etc. That's why it
is smooth. Folks, this material is metamorphic material with lots of
water, potassium feldspar, biotite, mica fragments, hornblende, all
essentials and accessories. How anybody can mistake this metamorphic
material for BCC9601 or any meteorite is beyond anything one can
conceive, but the Dean tried! Of course, he never brought samples
with him to compare so we did for him.