[meteorite-list] AD: Nova petropolis etched slice

2011-11-16 Thread André Moutinho
Hello all,

Have put on ebay a very nice etched slice of the Nova Petrolis iron from Brazil:
http://www.ebay.com/itm/330643238844?ssPageName=STRK:MESELX:IT&_trksid=p3984.m1555.l2649


Thanks
Andre
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[meteorite-list] Icebergs on Europa

2011-11-16 Thread JoshuaTreeMuseum

Apparently there are volcanos under the ice causing the icebergs:




http://www.washingtonpost.com/national/health-science/theory-of-subsurface-lakes-boost-hopes-for-life-on-jupiters-moon-europa/2011/11/16/gIQADp8hRN_story.html?hpid=z2



Phil Whitmer 


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[meteorite-list] Congratulations!

2011-11-16 Thread Charley
Congratulations Bob & Moni !

I wish you very best!

By the way, you two were among the very first people that I "met" when I 
first got involved in this wicked hobby!

Your early words of support and encouragement still mean a lot.

Best regards,

Charley Butterfield

"Well, squids don't work. Hey! Let's
  try elephants !"

Hannibal

> Message: 5
> Date: Tue, 15 Nov 2011 23:45:12 +0100
> From: "karmaka" 
> Subject: Re: [meteorite-list] November Issue of Meteorite Times now up
> To: Meteorite-list@meteoritecentral.com
> Cc: Robert Verish 
> Message-ID: <1rqrke-2ha8...@fwd04.aul.t-online.de>
> Content-Type: text/plain; charset="UTF-8"
>
> CONGRATULATIONS, Bob & Moni !!!
>
> 11.11.11
>
> ... and on top of that on my name day ;-)
>
> It was very nice meeting you in Ensisheim this year!
>
> All my very best wishes to you
>
> Martin
>
> 


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[meteorite-list] AD: ALL slices do have METAL Flakes - of the Superior Lodranite NWA 6659

2011-11-16 Thread Chladnis Heirs
Hello again,

And sorry for the little explanation,
but for not all jumping on the 5.013g and the 4.397g-slices, respectively
being disappointed, that those are gone:

ALL slices do have the same amount of metal flakes and blebs!

It's only not so well visible, as we photographed only two with an angle of
the light, that the metal flakes are reflecting. 
All slices are the same wonderful!

http://www.chladnis-heirs.com/specials/special-nwa6659.html



And when we are just at addendums...

The unpaired new fresh Martian with that fantastic texture, where we perhaps
made the mistake to introduce it with too soberly chosen attributes last
week.   NWA 6963.
There we would invite those, who'd still need a smaller sample than those
slices currently left,
to inform us, which weight they prefer - for us to pre-plan, what and how we
still have to cut or to divide into smaller sections.

http://www.chladnis-heirs.com/specials/special-nwa6369-2.html

and 
http://www.chladnis-heirs.com/specials/special-nwa6369.html


Many thanks in advance!
Martin & Stefan

Chladni's Heirs
Munich - Berlin
Fine Meteorites for Science & Collectors 

http://www.chladnis-heirs.com







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[meteorite-list] Sale Ad ; Moapa Valley CM1 thin section

2011-11-16 Thread wahlperry

Hi All ,

I have placed a Moapa Valley CM1 thin section on my web page for sale. 
Here is the link.


Thanks,
Sonny

http://www.nevadameteorites.com/nevadameteorites/Moapa_Valley_Sale_page_1_2.html




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[meteorite-list] Holocene Extinctions and Missoula Flood

2011-11-16 Thread Paul H.
Holocene Extinctions and Missoula Floods

E.P. Grondine wrote:

“I see from today's news that many people are still confused 
by the extinctions caused by the Holocene Start Impacts. Its 
really pretty easy, as Elephants need 450 pounds of food a day.”

Perhaps the following will explain it better.  Good hunting, all - 
E.P. Grondine, Man and Impact in the Americas”

THE WASHINGTON SCABLANDS AND ASSINIBOINE IMPACT ACCOUNTS 

Several posters here are interested in Harlan Bretz and the 
spread of his catastrophist hypothesis for the formation of 
the Washington scablands. Currently, while all geologists
agree that the scablands were formed by catastrophic flooding, 
there is debate over whether they were caused by the 
release of one or multiple lakes and exactly when the 
flooding(s) occurred.”

The above debate, which mentioned above, is imaginary
in nature. First, the age of the latest Missouri Flood is 
well established by both radiocarbon dates and well-dated 
volcanic ash beds from Mt. St. Helens. Wood fragment from
the lower-middle part of the Missoula Flood deposits in 
Sanpoil Valley yielded a radiocarbon date of 14,490 14Cyr
B.P. A 14,000 year old volcanic “set-S” ash from Mount St. 
Helens overlies at least 28 giant-flood rhythmites and 
underlies eleven giant-flood rhythmites in southern 
Washington. Organic matter recovered from within and 
below the Missoula flood deposits in the Columbia Gorge 
yielded three dates between 15,000 and 13,700 14Cyr B.P. 
These and other dates clearly indicate that catastrophic 
flooding occurred at multiple times during a period of time 
between 15,700–13,500 14Cyr B.P. (Booth et al. 2004). 

The Missoula Flood clearly predate and are, thus, unrelated 
to any hypothetical terminal Pleistocene or Holocene impact 
event. As noted above, the Missoula Flood  deposits are 
thousands of years too old to be associated with such an 
impact. In addition, the detailed study of sedimentology of the
flood deposits demonstrates that the catastrophic flooding 
from glacial Lake Missoula occurred every few decades to 
years. This is comparable to the frequency in glacier-outburst 
floods (jokulhlaups) associated with modern Icelandic glaciers 
(Booth et al. 2004). The occurrence of multiple catastrophic 
Missoula Flood events over a period of approximately 2,000 
years definitely refutes any notion that the Missoula Flood 
is associated with a single impact event of any age. A single 
impact would only have created a single catastrophic flood. It 
would have been quite impossible for a single impact of any 
age to have created multiple flood events over a 2,000 year 
period of time as has been well documented in the published
 literature.

References Cited

Booth, D. B., K. G. Troost, J. J. Clague, and R. B. Waitt, 2004, 
The Cordilleran Ice Sheet. in A. Gillespie, S. C. , Porter, and B. 
Atwater, eds., pp. 17-24, The Quaternary Period in the United 
States: International Union for Quaternary Research, Elsevier 
Press, New York.
http://faculty.washington.edu/dbooth/Ch_02_INQUA_volume.pdf
https://catalyst.uw.edu/workspace/file/download/0808b306b9967a473ab1851d477a4a35b0f79990349e2dc5d3eb3c7bfeb12668?inline=1

Also, go see:

O'Conner, J., and R. Waitt, 1994, Beyond the Channeled 
Scabland: A field trip· to look at Missoula Flood Features in 
the Columbia, Yakima and Walla Walli valleys of Washington 
and Oregon. Friends of the Pleistocene 1st Pacific Northwest 
Cell Meeting May 13-15, 1994. U.S. Geological Survey, 
Vancouver, Washington.
http://www.scribd.com/doc/24574508/Channeled-Scabland-A-field-trip%C2%B7-to-look-at-Missoula-Flood

E.P. Grondine also stated:

“Of course, as oil companies have for years been drilling cores 
off the coast of Washington, those questions could be readily 
answered, except that those cores are proprietary.”

Oil company cores will likely tell use nothing about the Missoula 
Flood as the deposits that would contain deposits from the Missoula 
Flood are too young to be of any interest to them. They would simply 
drilled through such surficial sediments any only start coring once 
they got to the oil-bearing strata. In addition, petroleum seismic is 
not designed to image shallow strata, which are of no interest to oil
companies.

However, research by marine geologists using cores and seismic data 
have identified and mapped thick turbidite deposits consisting of material 
from the Missoula Flood that was flushed down the Astoria Fan on the 
Oregon continental margin. The vast majority of this research, including 
cores,  is not proprietary. This research is discussed in a number of 
published papers, including:

Brunner, C. A., W. R. Normark, G. G. Zuffa, and F. Serra, 1999,
Deep-sea sedimentary record of the late Wisconsin 
cataclysmic floods from the Columbia River. Geology. vol. 27, 
no. 5, pp. 463-466.
http://geology.geoscienceworld.org/cgi/content/abstract/27/5/463

Normark, W. R., and J. A. Reid, 2003, Extensive Deposits 
on the Pacific Plate 

Re: [meteorite-list] AD: Special: NWA 6659 prov. - Superior Lodranite

2011-11-16 Thread Marcin Cimala

Great specimen, but any photos of entire mass ?
:)



Dear meteorite friends,


in our weekly Special we're able this time to present you a wonderful
dainty:  NWA 6659 - a Lodranite!

Lodranites are counted among the absolutely rarest classes a meteorite
collector can have in his cabinet and a meteoricist in his lab.
Currently the Meteorite Bulletin Database accounts for only 32 lodranitic
numbers with a combined weight of 9.39kg (15 of them with 1.14kg yielded 
the

Antarctic campaigns of the last 35 years).  And 9 numbers not otherwise
specified as belonging to the acapulcoite-lodranite family with 0.33kg
(7 Antarctics) - making the lodranites to a much rarer type than any lunar
meteorite.

Let us say as long-time established meteorite offerers, that it was the
NWA-complex of the recent decade, which brought the lodranites at all in 
the

range of the collector and a certain variety of finds into the research
institutes. A check of our global price compilation of the season ten 
years
ago only (660 different meteorites, 92 offerers - currently available in 
the
German meteorite forum), gives, that the only chance to get a lodranite 
was

then to acquire micromounts of Lodran, priced at an average of 38,400$ a
gram and that among the related acapulcoites, the collector had only the
choice between Acapulco (average 1408$/g) and Monument Draw (1016$/g).

Lodranites and acapulcoites share common ground and are generic relatives
from the same parent body, which seems to have had consisted of a CM or
CI-like precursor material. The main differences between these types is 
the

lack of plagioclase in the lodranites and the larger grain-sizes than the
acapulcoites display, hence indicating that lodranites underwent during
their melt phase higher temperatures and a different cooling period,
stemming from deeper layers than the acapulcoites.
However, as enigmatic that group perhaps still might be - it are just the
very recent years with these new desert finds, which lead science to 
develop
a better understanding of the composition and the complex thermal history 
of

the acapulcoite-lodranite parent body.
A perfect overview of the brand-new models and hypotheses you will find on
David Weir's meteorite studies pages.

The perhaps a little provocative title of this Special we chose, because
most lodranitic specimens in our collections are recruited from the large
pairing group, which was revised from ACAP to LOD and where we once all
tried to put the numbers together here on the list (NWA 2565/2714/2866
seqq.)
And we regard NWA 6659 as definitely more comely.
It is better preserved than the old group, which had weathering grades of 
W3

and W3-4.
Not only the crystals of NWA 6659 are still relatively fresh-looking - it
has even here and there some metal grains and of course:
Yes - the so highly desired Triple Junctions superabound.

All slices were grinded and polished successively with 6 different grits;
and you find them here:

http://www.chladnis-heirs.com/specials/special-nwa6659.html


Regarding the statistics from above, keeping in mind, that the Great 
Desert

Area is coming to an end and emphasizing that we price NWA 6659 at the
lowest edge of the lodranite spectrum, we think, that these specimens are
not only of highest interest for the advanced collector, but would
wholeheartedly commend them as an excellent choice also for the beginning
meteorite enthusiast, as one-and-only specimen for having an perfect
representative, once and for all, of that fascinating and so exceedingly
rare class.


Best regards,
Stefan & Martin

Chladni's Heirs
Munich - Berlin
Fine Meteorites for Science & Collectors

http://www.chladnis-heirs.com





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[meteorite-list] AD: Special: NWA 6659 prov. - Superior Lodranite

2011-11-16 Thread Chladnis Heirs

Dear meteorite friends,


in our weekly Special we're able this time to present you a wonderful
dainty:  NWA 6659 - a Lodranite!

Lodranites are counted among the absolutely rarest classes a meteorite
collector can have in his cabinet and a meteoricist in his lab.
Currently the Meteorite Bulletin Database accounts for only 32 lodranitic
numbers with a combined weight of 9.39kg (15 of them with 1.14kg yielded the
Antarctic campaigns of the last 35 years).  And 9 numbers not otherwise
specified as belonging to the acapulcoite-lodranite family with 0.33kg 
(7 Antarctics) - making the lodranites to a much rarer type than any lunar
meteorite.

Let us say as long-time established meteorite offerers, that it was the
NWA-complex of the recent decade, which brought the lodranites at all in the
range of the collector and a certain variety of finds into the research
institutes. A check of our global price compilation of the season ten years
ago only (660 different meteorites, 92 offerers - currently available in the
German meteorite forum), gives, that the only chance to get a lodranite was
then to acquire micromounts of Lodran, priced at an average of 38,400$ a
gram and that among the related acapulcoites, the collector had only the
choice between Acapulco (average 1408$/g) and Monument Draw (1016$/g).

Lodranites and acapulcoites share common ground and are generic relatives
from the same parent body, which seems to have had consisted of a CM or
CI-like precursor material. The main differences between these types is the
lack of plagioclase in the lodranites and the larger grain-sizes than the
acapulcoites display, hence indicating that lodranites underwent during
their melt phase higher temperatures and a different cooling period,
stemming from deeper layers than the acapulcoites.
However, as enigmatic that group perhaps still might be - it are just the
very recent years with these new desert finds, which lead science to develop
a better understanding of the composition and the complex thermal history of
the acapulcoite-lodranite parent body.
A perfect overview of the brand-new models and hypotheses you will find on
David Weir's meteorite studies pages.

The perhaps a little provocative title of this Special we chose, because
most lodranitic specimens in our collections are recruited from the large
pairing group, which was revised from ACAP to LOD and where we once all
tried to put the numbers together here on the list (NWA 2565/2714/2866
seqq.) 
And we regard NWA 6659 as definitely more comely.
It is better preserved than the old group, which had weathering grades of W3
and W3-4.
Not only the crystals of NWA 6659 are still relatively fresh-looking - it
has even here and there some metal grains and of course:  
Yes - the so highly desired Triple Junctions superabound.

All slices were grinded and polished successively with 6 different grits;
and you find them here:

http://www.chladnis-heirs.com/specials/special-nwa6659.html


Regarding the statistics from above, keeping in mind, that the Great Desert
Area is coming to an end and emphasizing that we price NWA 6659 at the
lowest edge of the lodranite spectrum, we think, that these specimens are
not only of highest interest for the advanced collector, but would
wholeheartedly commend them as an excellent choice also for the beginning
meteorite enthusiast, as one-and-only specimen for having an perfect
representative, once and for all, of that fascinating and so exceedingly
rare class.


Best regards,
Stefan & Martin

Chladni's Heirs
Munich - Berlin
Fine Meteorites for Science & Collectors 

http://www.chladnis-heirs.com





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[meteorite-list] Holocene Extinctions

2011-11-16 Thread E.P. Grondine
Hi all - 

I see from today's news that many people are still confused by the extinctions 
caused by the Holocene Start Impacts. Its really pretty easy, as Elephants need 
450 pounds of food a day. 

Perhaps the following will explain it better. 
Good hunting, all - 
E.P. Grondine
Man and Impact in the Americas


THE WASHINGTON SCABLANDS AND ASSINIBOINE IMPACT ACCOUNTS

Several posters here are interested in Harlan Bretz and the spread of his 
catastrophist hypothesis for the formation of the Washington sacablands. 
Currently, while all geologists agree that the scablands were formed by 
catastrophic flooding, there is debate over whether they were caused by the 
release of one or multiple lakes and exactly when the flooding(s) occurred. Of 
course, as oil companies have for years been drilling cores off the coast of 
Washington, those questions could be readily answered, except that those cores 
are proprietary.  

I spent some time reading through Adrienne Mayor's book "Fossil Legends of the 
First Americans" recently. It turns out that the Assiniboine (Nakota) may have 
remembered at least one of those floods. Mayor's book is pretty good, and she 
nearly succeeds in spanning the two worlds, but sadly she did not realize that 
the peoples remembered impacts, and thus failed to entirely grasp fundamental 
concepts like "uktena" and "tlanwa". Mayor also retells the traditions with her 
intense interest in fossils coloring her retellings, and it is tough using her 
book to locate the original traditions as they were first shared. However, that 
said, it is a pretty good book.

THE NAKOTA (ASSINIBOINE) ACCOUNTS IN MAYOR'S RETELLING

Fragment 1:

"One Assiniboine name for bones of monstrous size was "Wau-wau-kah". This was a 
"half spirit, half animal" imagined as a great river monster with long 
black[?]hair, scales, and horns like trees. 

"Myth [tradition - epg] tells of its death by the impact of a "thunder stone", 
a black ["black" due to the ablated surfaces of the meteorites which the Nakota 
later collected. - epg], projectile that came whistling out of the west with 
"terrible velocity", "defeaning noise", and "a bright flash" - a scenario that 
seems akin to the modern theory of an asteroid impact 65 million years ago 
[Mayor gets very close here - epg]. "My bones may be found", warned the Water 
Monster Wau-wau-kah, but unless the Assiniboines made offerings to its spirit, 
the monster vowed to create disastrous floods and block their trails with its 
colossal bones."

Fragment 2: 

"A tale [tradition - epg] of the antagonism between Thunder and Water Monsters 
was recounted by an Assiniboine story teller [tradition keeper - epg] (perhaps 
Coming Day? - AM) in 1909 at Fort Belknap. 

"Long ago, some Sioux and Assiniboines camping at a big lake witnessed a battle 
between Thunder Bird and a Water Monster on an island in the lake."

The storyteller's grandmother had told him that: "as the Thunder Bird drew the 
writhing monster up from the island, the Indians' hair and their horses manes, 
[a non-temporal insertion? - epg] stood on end from the electricity. 

["electricity" is another non-temporal insertion. Perhaps it may also be a 
modern simple telling of a large electrophorenic effect from the impactors 
entries. In regards to the "horses manes", it needs to be noted that a rider on 
a horse in the plains is a high point that will attract lightening, much as a 
golfer standing on a gold course will, and thus it was very important to know 
the signs of an impending lightening strike.]

"The Thunder Bird's lightening ignited raging forest fires; then a long 
terrible blizzard followed; and still later the lake bed dried up and many 
kinds of animals perished there."

"The raging forest fires" were likely caused by the infrared of multiple 
impacts. "the long terrible blizzard" describes the a standard severe climate 
collapse caused by atmospheric impact dust loading. 

"the Lake" of the Assiniboine is as yet unlocated; perhaps it was Lake Agassiz, 
but much more likely it was a glacial lake much further south ("forest fires"). 

Why did that lake dry up? Either its ice damn failed ("disasterous floods", 
above), or there was a lack of precipitation due to a cooling of the 
temperature of the Pacific Current. 

"The many kinds of animals" likely perished due to lack of food, a famine which 
appears as a common element in many of the First Peoples' memories of the 
Holocene Start Impacts.

END

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[meteorite-list] Meteorite Picture of the Day

2011-11-16 Thread valparint
NWA 869

http://www.tucsonmeteorites.com/mpod.asp
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