Re: KRS - artificial weathering
From: Eric Stevens (eric.stevens_at_sum.co.nz)
Date: 09/21/04
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Date: Tue, 21 Sep 2004 22:58:12 +1200
On Tue, 21 Sep 2004 08:10:38 GMT, "zolota" <zolota3@REMOVEshaw.ca>
wrote:
>
>"Eric Stevens" <eric.stevens@sum.co.nz> wrote in message
>news:rn3vk0ttf59pree0h82ulgsui6665ifiqm@4ax.com...
>> On Mon, 20 Sep 2004 20:33:17 GMT, "zolota" <zolota3@REMOVEshaw.ca>
>
>SNIP as a public service (a la servicia de la patria)
>
>>>
>>>You must be sure that they will be investigated during the present
>>>research,
>>>documented, compared with what technology knows about faking rock
>>>surfaces,
>>>and reported in a scientific journal.
>>
>> I thought we were discussing what could and could not be done. Not
>> what is or has been done.
>
>If you are so sure that X is possible then surely you expect that X will be
>presented in a scientific manner. what am I missing here?
A father for your expectancy?
>
>>
>>>In the meantime I am waiting for you or someone else to explain which
>>>sub-surface changes you are hinting at.
>>
>> I've already said I can't tell you in detail but do you accept there
>> will be some?
>
>I really expected that you could give examples now.
Then you are deliberately being obtuse. I have several times said I
can't give any specific examples.
>
>>>
>>>
>>>>>
>>>>>Remember, if the results are not acceptable the rock is left on the
>>>>>nearest
>>>>>lake.
>>>>>
>>>>>I do not believe that all of the runes are on dressed surfaces, the
>>>>>calcite
>>>>>sheen on part of the face has to have been a fissure filling.
>>>>
>>>> Only the edge has been dressed.
>>>
>>>Okay, glad that is clarrified.
>>>
>>>>
>>>SNIP
>>>-surface chemical changes which are
>>>>>> part and parcel of weathering.
>>>>>
>>>>>This is a metamorphic rock, such rocks are the product of pressure and
>>>>>temperature and are not particularily porous.
>>>>
>>>> But still, they are porous. Reagents will penetrate.
>>
>> See
>> http://www.springerlink.com/app/home/contribution.asp?wasp=3768ypvuqq5yxbg4wr8x&referrer=parent&backto=issue,24,88;journal,1,4;linkingpublicationresults,1:110353,1
>> for confirmation of the porosity of greywacke.
>
>You have so far failed to explain to me what you mean by the penetration of
>minerals.
Not surprising. I have never talked about 'the penetration of
minerals'. However I have talked about the penetration of reagents.
> If ion Y is present in a solution surrounding a sample at
>atmospheric pressure for 24 hours it will penetrate the cracks of a mineral
>in a very well known and understood way.
I've already explained to Martin Reboul that porosity/diffusoin is not
the same as finding the way through cracks, no matter how small the
cracks.
>Subject the treated rock to a pure
>water bath and it will reverse the transit of ion Y. This is called
>diffusion, it is well measured. If a rock is subjected to molar levels of an
>ion (as in 49 grams per liter of H2SO4 or sulphuric acid) for 24 hours, it
>will in turn see those entrained but unreacted molecules leach out in a week
>or so. Now bury the rock in Minnesota and let it see ten years of weather.
Somehow I think your thoughts are jumping around.
>
>>>
>>>
>>>Then do please give one example of a mineral known in the KRS, a reagent
>>>that will react with it, and the reaction product(s).
>>
>> Stop playing games. I've already told you I can't offer any specifics.
>> But are you saying there are minerals in the KRS which will not be
>> affected by chemical weathering?
>
>Bloody right. I've mined sapprolite ores (tropical weathering) that
>contained intact quartz veins and rocks after the rest of the mountain had
>(over 200 MY) been reduced to soft clays. Quartz is present in the KRS, and
>quartz is essentially inert. WTF do you think we make glassware out of it?
Yet another change of subject.
>
>>>
>>>>
>>>>>Many Egyptian carvings were
>>>>>done in similar rocks, you must be aware of how well preserved these can
>>>>>be.
>>>>
>>>> We are arguing enough about possible Viking artifacts in Minnesota. I
>>>> hope you are not suggesting the Egyptians left artifacts there also!
>>>
>>>Now you are being silly, there are no known Egyptian artifacts farther
>>>than
>>>200 km from the Atlantic ocean in North America.
>>
>> Z, please check your 'sense of humour' switch' I think somebody has
>> bumped it off.
>
>Are you now suggesting that there are known Egyptian relics on the Atlantic
>coast??? You suggest that I have no sense of humour? YOU DARE TO SUGGEST
>THAT?
PLEASE CHECK YOUR SENSE OF HUMOUR SWITCH!
Its been off for the last two interchanges.
>
>(Why?)
>
>>
>>>Last month I visited an
>>>exhibition of Egyptian artifacts (London museum) and looked closely at the
>>>weathering on them. Despite 4,000 years of thermal cycling and in some
>>>cases
>>>hundreds of rain events while burrried they for the most part look new.
>>>Egyptians deliberately chose greywacke for these carvings because of it's
>>>durability. The KRS has a curved back surface. That surface was once the
>>>exposed outcrop of a greywacke deposit before the glaciers sheared it off
>>>the bedrock (along the pre-existing fron surface fracture) and transported
>>>it hundreds of kilometers. Despite the grinding in the ice, thousands of
>>>winters since the ice age, etc, that surface is still smooth.
>>
>> Smooth only if you ignore 1 to 5mm deep glacial striations.
>
>Smooth surface straiations on the local level Eric! It's a lot like sex.
>Some English never do understand that, it's over their heads. But the
>Germans and French, they--- oh, never mind!
OK. It all depends what you mean by 'smooth'.
>
>
>>
>>>If it could be
>>>penetrated as easily as you seem to believe it would no longer be smooth,
>>>it
>>>would be a rough surface composed of discrete mineral grains.
>>
>> That the KRS has porosity does not mean that it is like a sponge.
>
>???? You are the spongebob guy Eric.
You don't understand, do you?
>
>>>
>>>>
>>>>>The minerals in greywacke decompose bu too slowly to date the KRS in
>>>>>most
>>>>>cases. A forger would like the biotite in it because it's easier to show
>>>>>aging using biotite than with most other minerals.
>>>>
>>>> Easier to fake also. But the other minerals remain.
>>>
>>>I said it's easier to fake biotite. For Pete's sake tell us what aging can
>>>happen on the other minerals present in the KRS at a fast enough rate to
>>>be
>>>a marker on a scale of 500 years.
>>
>> ... are you denying that there are any?
>
>Aggressive, accusatory words there Eric. What am I denying? I asked you to
>tell us what other minerals are present that can weather fast enough to show
>it, and you give us blanks.
I've already told you several times that is all I have to give.
However your challenge " For Pete's sake tell us what aging can happen
on the other minerals present in the KRS at a fast enough rate to be a
marker on a scale of 500 years" makes it sound as though you don't
believe there are any. That's whay I asked " ... are you denying that
there are any?" If you are not denying there are any, what are they?
[I don't know, I'm not the expert].
Eric Stevens
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