Re: [meteorite-list] Ablation Zone 5 Layers...Not

2009-11-23 Thread debfred
List, I think Jason has done a fine job with his position with which I agree. I 
don't want to beat a dead horse but Here are  published  definitions of fusion 
crusts on irons.

  “Fusion Crust” Definition from Glossary of Geology 2nd edition 1980; American 
Geological Institute, Falls Church, Virginia, 751pp.
 
Fusion crust  A thin glassy coating, usually black and rarely exceeding one 
millimeter in thickness, formed on the surface of a meteorite by frictional 
heating during atmospheric flight.
Owing to differing effects of the atmosphere upon different meteorite surfaces, 
fusion crusts may be knobby, striated, ribbed, net, porous, warty, or 
scoriaceous.

Several points stand out upon careful reading of this definition. The term 
glassy is an adjective not a noun. Glassy is a term commonly used in describing 
surface luster in mineralogy. Composition: Silica, silicate, silicon and iron 
are not mentioned at all. Apparently composition is not pertinent to the 
matter. Other terms like warty and seem to refer to fusion crust on irons.

Looking further for definitions used specifically by meteoriticists we find a 
definition on pages 44-45 by Brian Mason in his classic book, “Meteorites”. 
Mason presents the classification of Krinov (1960) that also seems to have been 
a source for the Glossary’s definition. It is rather long but I will post the 
complete definition because many people have complained there wasn’t a good 
published definition of fusion crust for meteorites.

Fusion Crust

A freshly fallen meteorite is covered with a fusion crust, except on fracture 
surfaces produced on or shortly before impact. The nature of the fusion crust 
varies somewhat, according to the composition of the meteorite. On most 
meteorites it is black, but on the enstatite achondrites it is colorliess or 
pale yellow, because of the almost complete absence of iron in these 
meteorites. The fusion crust on iron meteorites is very thin, only a fraction 
of a millimeter, and consists of magnetite. The fusion crust on stone 
meteorites is thicker, and consists of a black glass which includes fragments 
of the less fusible mineral such as olivine. On chondrites and the calcium-poor 
achondrites the crust is usually dull, but on calcium-rich achondrites, which 
are more fusible than other stony meteorites, the crust is shiny and lustrous, 
and also thicker than on other types. Sometimes the crust shows a network of 
fine cracks, similar to the “crazing” which appears in the glaze of pottery. 
Krinov (1960) has made detailed studies of the nature of meteorites, and 
presents the following classification:

Class I.  Crust of Frontal Surfaces

Type 1, Close-textured.  The crust is perfectly smooth, as though it had been 
pressed, with practically no indications of structure. Observed mainly upon 
iron meteorites and covers surfaces, which generally exhibit considerable marks 
of atmospheric action, regardless of whether the surface has regmaglyptic 
relief.

Type 2, Nodular.  Upon a smooth, close textured crust, fine angular nodules are 
visible scattered over the surface of the meteorite. Upon stony meteorites, on 
which this type is mainly found, the nodules represent fused inclusions of 
nickeliferous iron. 

Class II.  Crust of Lateral Surfaces

Type 1.  Striated.  Upon a smooth, close-textured crust thin striae are visible 
that seem to be flowing across the surface of the meteorite.
Very often the striae are directed toward the rear part of a meteorite, thus 
clearly indicating the direction of its motion.  Upon iron meteorites the 
striae quite often end in drops, which are sometimes of spherical form. There 
are also observed curves or even seemingly broken striae which abruptly change 
direction. Now and then an intricate pattern of the striated crust can be seen. 
 In rarer cases several systems of striae are observed, superimposed one on top 
of the other and intersecting at various angles.  In such cases the striae of 
the bottom system appear to be wide and flat, while those of the upper system 
are thin.
Particularly sharply defined striated crustal structure is observed near the 
sharp edges of lateral surfaces, adjacent to the rear surfaces of iron 
meteorites.  Upon stony meteorites more or less distinct striae are usually 
observed along the edges of lateral surfaces.  Striae are easily 
distinguishable on the rims between regmaglypts.

Type 2.  Ribbed.  Represents an intermediate type between the modular and 
striated crust and is found only upon stony meteorites. The ribs appear like 
underdeveloped striae.

Type 3.  Net.  The crust is formed of short striae running together, lending it 
the appearance of a fine-mesh net. Individual cells of the mesh appear like 
stitches.  Is observed mainly upon more friable stony meteorites, usually near 
the edges of lateral surfaces or near protuberances.

Type 4.  Porous.  At magnification of 15-30X tiny pores can be seen clearly 
upon the crust. Sometimes the crust 

[meteorite-list] CK

2009-11-23 Thread Marcin Cimala

Hi aziz
How much for Your 1700 gr ck 
http://www.flickr.com/photos/azizhabibi/3967195844/

its paired with anything ?


-[ MARCIN CIMALA ]-[ I.M.C.A.#3667 ]-
http://www.Meteoryty.pl marcin(at)meteoryty.pl
http://www.PolandMET.com   marcin(at)polandmet.com
http://www.Gao-Guenie.com  GSM: +48 (793) 567667
[ Member of Polish Meteoritical Society ]

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Re: [meteorite-list] Crust Descriptions...was Ablation

2009-11-23 Thread MEM
Certainly the best collection of observations set to text I've seen.  Thanks 
for digging up the details Fred.   This also goes into detail as to the kind of 
structures that can be seen over the various faces of the meteoroids 
orientations.

One exception: Yes glassy is a term used to describe luster but 
glassy:composed of glass has a specific meaning in mineralogy. I believe the 
use in this context is in respect to composition not luster. Otherwise the term 
metallic should be used for irons. 

Very few meteorites-- notably eucrites have a glassy-lustered crust, however 
most all silicate bearing meteorites have a glassy crustal composition in the 
mineralogical sense.  Some of the Silicates are the only class of minerals I 
can think of which can form glass, although there are likely others. Iron 
silicates form a dark glass upon melting/quenching however free iron oxidizes 
and forms magnetite-class minerals and therefore not glass. Ordinary 
chondrites have both components. The mention or non mention of the elements is 
understood by anyone familiar with the mineralogy.  Same issue Fe vs Mg in the 
color of olivine in pallasites.

Regards,
Elton

PS Speaking of simple errors which make it into our reference sources: We know 
now that ablation and crust formation result from liberation of heat during 
compression and not because what was long believed to be from air friction.  
Sometimes accuracy suffers when one tries to get the main point across. There 
is always room to ask the source again for clarification.

--- On Mon, 11/23/09, debf...@att.net debf...@att.net wrote:

   “Fusion Crust” Definition from Glossary of
 Geology 2nd edition 1980; American Geological Institute,
 Falls Church, Virginia, 751pp.
  
 Fusion crust  A thin glassy coating, usually black and
 rarely exceeding one millimeter in thickness, formed on the
 surface of a meteorite by frictional heating during
 atmospheric flight.
 Owing to differing effects of the atmosphere upon different
 meteorite surfaces, fusion crusts may be knobby, striated,
 ribbed, net, porous, warty, or scoriaceous.
 
 Several points stand out upon careful reading of this
 definition. The term glassy is an adjective not a noun.
 Glassy is a term commonly used in describing surface luster
 in mineralogy. Composition: Silica, silicate, silicon and
 iron are not mentioned at all. Apparently composition is not
 pertinent to the matter. Other terms like warty and seem to
 refer to fusion crust on irons.
 
 Looking further for definitions used specifically by
 meteoriticists we find a definition on pages 44-45 by Brian
 Mason in his classic book, “Meteorites”. Mason presents
 the classification of Krinov (1960) that also seems to have
 been a source for the Glossary’s definition. It is rather
 long but I will post the complete definition because many
 people have complained there wasn’t a good published
 definition of fusion crust for meteorites.
 
 Fusion Crust
 
 A freshly fallen meteorite is covered with a fusion crust,
 except on fracture surfaces produced on or shortly before
 impact. The nature of the fusion crust varies somewhat,
 according to the composition of the meteorite. On most
 meteorites it is black, but on the enstatite achondrites it
 is colorliess or pale yellow, because of the almost complete
 absence of iron in these meteorites. The fusion crust on
 iron meteorites is very thin, only a fraction of a
 millimeter, and consists of magnetite. The fusion crust on
 stone meteorites is thicker, and consists of a black glass
 which includes fragments of the less fusible mineral such as
 olivine. On chondrites and the calcium-poor achondrites the
 crust is usually dull, but on calcium-rich achondrites,
 which are more fusible than other stony meteorites, the
 crust is shiny and lustrous, and also thicker than on other
 types. Sometimes the crust shows a network of fine cracks,
 similar to the “crazing” which appears in the glaze of
 pottery. Krinov (1960) has made detailed studies of the
 nature of meteorites, and presents the following
 classification:
 
 Class I.  Crust of Frontal Surfaces
 
 Type 1, Close-textured.  The crust is perfectly
 smooth, as though it had been pressed, with practically no
 indications of structure. Observed mainly upon iron
 meteorites and covers surfaces, which generally exhibit
 considerable marks of atmospheric action, regardless of
 whether the surface has regmaglyptic relief.
 
 Type 2, Nodular.  Upon a smooth, close textured crust,
 fine angular nodules are visible scattered over the surface
 of the meteorite. Upon stony meteorites, on which this type
 is mainly found, the nodules represent fused inclusions of
 nickeliferous iron. 
 
 Class II.  Crust of Lateral Surfaces
 
 Type 1.  Striated.  Upon a smooth, close-textured
 crust thin striae are visible that seem to be flowing across
 the surface of the meteorite.
 Very often the striae are directed toward the rear part of
 a meteorite, thus clearly indicating the 

[meteorite-list] Meteorite lights up Gauteng sky

2009-11-23 Thread Michael Groetz
Meteorite lights up Gauteng sky

http://www.timeslive.co.za/thetimes/article204795.ece

Amazed Johannesburg and Pretoria residents could hardly believe their
eyes when a five-second lightning flash, thought to be a meteorite,
lit up the night sky in a dazzling display of light at about 11pm on
Saturday.

Now the South African Astronomical Society are desperately trying to
find out in which direction the meteorite travelled, and if it landed
on Earth.

Richard Davis tweeted on social networking website Twitter that he saw
a flash of light and flames heading towards Earth.

Another user, Marelie, tweeted that she saw the flash from a
meteorite crashing into Earth, while Anemi Kotze speculated that it
looked like a meteorite hit pta [Pretoria].

Astronomical Society director Kevin Govender told The Times that it
would be really cool if a meteorite landing site was found, but the
rock falling through the atmosphere would have to be as big as a car
for you to see something significant.

He suggested that the meteorite could have been the size of a soccer
ball, which would throw up a two-metre crater. The meteorite was
also spotted by people living in Magaliesberg and Hoedspruit.
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Re: [meteorite-list] What is or is not a chondrule?

2009-11-23 Thread MEM
Walter your email is not yahoo friendly so here is the answer via the list.

Hello Walter,  I don't know if you ever got an answer to your question but I 
had it marked for follow up.

Chondrules, while usually more spherical, can be ovoid or ellipsoid and 
occasionally doubled.  Current theory on chondrule formation is that they form 
by a varied sequence athat always includes final series of flash melting of the 
surface which seals in the contents. This tends to round off the edges and give 
them their typical spheroidal shape.

When we see the chondrules as you describe--with lots of lines, those are 
usually barred olivine chondrules. Barred olivines probably went through 
several passages between super hot and not so hot zones in the nebula and 
represent successive growth and melt phases.   Some chondrules are simple 
feldspar. Some are rubble piles of angular blocks/globs of mineral grains and 
dust which were flash melting sealed them into a chondrule yet retaining their 
angular crumbled edges sucked into a sphere mosaic style.

A clast is usually angular on at least one side--that is not round. It has a 
consistent composition and color.  Sometimes clasts are large enough for eye 
identification that they came from an entirely different class of meteorite 
then the one they have been found in.

Keep in mind that the process of moving from a stage 3 to a 6 involves melting 
away of the chondrules and migration of their contents into the matrix while 
semi-plastic. These chondrules are not easy to discern even with a hand lens as 
their margins are in a stage of blending into the matrix due to heating.

Regards,
Elton
--- On Thu, 7/6/06, Walter L. Newton newto...@comcast.net wrote:

 From: Walter L. Newton newto...@comcast.net
 Subject: [meteorite-list] What's a chondrule-what's not a chondrule?
 To: meteorite-list@meteoritecentral.com
 Date: Thursday, July 6, 2006, 10:06 AM
 Hi list, a little technical
 question.

 I understand what a chondule is, but sometime, when looking
 at a slice of a meteorite, I am confused as to what they always look like.

 I have a polished slice of NWA 787 (same as NWA 869). I see
 light brown
 sphere's but I also see light brown ellipsoid (is that the
 word I'm looking for?) splotches. The same thing exists for some light grey 
 patches.

 The there are light brown or light grey lines, maybe
 2-3mm long. Is that a clast or inclusion or what?

 In a slice of NWA 2859 (H4) I see a few round grey metal
 patches. I suspect that just so happens to be a round blob of iron, not a 
 chondrule.

 Most of the time when I see a picture that points out
 chondrules, the illustration always points to round objects. Do I assume if 
 it's not round, it's not a chondrule?

 Walter L. Newton
 Golden, Co 
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Re: [meteorite-list] What is or is not a chondrule?

2009-11-23 Thread Carl 's

Hi Elton,

 I couldn't help notice Walter originally asked this question way back July 6, 
2006.:) I don't have a point but thought it was funny.

Carl


Elton wrote:
...I don't know if you ever got an answer to your question but I had it marked 
for follow up...

  
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[meteorite-list] Ad - New And Fantastic Material Ending At Auction

2009-11-23 Thread Adam Hupe
Dear List Members,

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Regards,


Adam Hupe
The Hupe 
Collection
Team LunarRock
IMCA 2185
raremeteori...@yahoo.com 
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Re: [meteorite-list] Ablation Zone 5 Layers...AND Crust

2009-11-23 Thread Greg Stanley

Elton and List:

I just wanted to point out that in much of the literature (and on the web) it 
is stated that there is a fusion crust on irons, so I do not think this is the 
your argument.  It is how the term is should be used.  I think you make many 
valid points and I have done some reading on the subject - and thus, learning 
more about it.  It appears that the so called crust that forms on stony 
meteorites and irons may be very different, both in their content and how they 
form.  On a stony, the outer layer heats very rapidly and starts the process of 
ablation.  Then material is removed (causing the vapor trail) and a protective 
coating forms as the melt cools and forms a glass like Material.  As we know, 
the different mineral content produces different fusion crust: light brown on 
Aubrites, dark brown to black on chondrites and a very glossy black on Eucrites 
and Martian Meteorites due to the Calcium content.  Now on irons, the stone 
ablates (as we can see flow lines) but the so called crust may be different; 
not a glassy substance like on a stony but more of an iridescent coating.  This 
very well could be the result of minor amounts of silicate and perhaps even 
carbon related substances within the iron.  I think a paper discussing the 
similarities and differences of the fusion crust or thermal coatings on 
stony, stony-iron and iron meteorite would be fascinating; if it has not be 
done already.

Please let me point out that I enjoy these posts as it provides a great 
learning tool.  

Much Thanks,

Greg S.     


 Date: Sun, 22 Nov 2009 22:12:29 -0800
 From: mstrema...@yahoo.com
 Subject: Re: [meteorite-list] Ablation Zone 5 Layers...AND Crust
 To: altm...@meteorite-martin.de; meteorite-list@meteoritecentral.com; 
 stanleygr...@hotmail.com

 - Greg Stanley wrote:
 See Fig. 1 on this UCLA web page.
 http://www.ess.ucla.edu/research/cosmochem/meteorite.asp

 Not sure if Dr. Wasson has written any papers regarding
 fusion crusts on irons, but I would think he would endorse
 anything on the web page.

 So Gregg, if your statement is true, Dr.Wasson and/or UCLA endorses the 
 formation of rusty fusion crust actually formed during decent? ( Fig 1 or 
 is it the regmaglyts that formed during passage and they are on top of the 
 rusty fusion crust?)

 The issue is deeper than the semantic arguments, glossary obsolesence and 
 lies in the differences of origin, composition, and presence of crust on 
 different classes of meteorites. In the old school, a crust is generally 
 removable from the underlying substrate and a dipping in molten metal alloy 
 pushes the envelope of being a crust, however Buchwald illustrated that this 
 was a combination of free metal and oxides. I conceed that irons--most all 
 freshly fallen ones anyway , do have a fused surface that we can by 
 convention call crust but the question remains as to what is the crust 
 which is a few microns thick versus coatings and halos etc. There is danger 
 of promoting ignorance by making assumptions that everything which is called 
 crust is identical.

 I am old school and I have the (un)reasonable expectation that where a 
 distinction does lie, that the collector can understand why things are the 
 way they are and not abuse the descriptions when they try to peddle their 
 specimens. Very few understood the distinction of silicate content when 
 addressing irons as the presence of silicates,oxides, carbides,phosphides, 
 etc largely govern the nature of a particular crust and gives insight into 
 what went on during that miliseconds of exposure when the final surface was 
 formed.

 Why it matters to me is 1) the abuse of the term in describing meteorite 
 conditions 2) the science of understanding the differences in crust origin 
 and composition and 3) how do we make the distinction amongst flight markings 
 and do they differ from fusion crust?

 I am satisfied that 1)one of the iron specimens cited in this discussion 
 apparently do have a silicate content that provided for a glassy fusion crust 
 and its origin is intriguing scientifically. 2)That by definition alone 
 (fused + coating) the irons do routinely have a fused coating/crust which 
 differs significantly from our traditional concept of crust even though it 
 is indistinguishable from the interior to the naked eye. (Do folks really 
 see the crust or do they see if because it is supposed to be there?) At 
 what point in weathering do we see that the welded crust/layer on an iron 
 has rusted away given it is a few microns thick? 90% of the time, the seller 
 will be claiming crusted long after the crust is gone, IMO.

 I've seen little to nothing so far that invalidates describing the ablation 
 zone nor crust in layers--Nor did Buchwald, apparently.

 Finally, the term big-head someone used probably translates to arrogant 
 Either way it was used in error as I was misunderstood. I did not disparage 
 the pioneers in the 

[meteorite-list] Sign me up!

2009-11-23 Thread Darren Garrison
http://www.space.com/missionlaunches/091123-manned-asteroid-mission.html

Plan for Human Mission to Asteroid Gains Speed
By Leonard David
SPACE.com’s Space Insider Columnist
posted: 23 November 2009
11:56 am ET

BOULDER, Colo. – Call it Operation: Plymouth Rock. A plan to send a crew of
astronauts to an asteroid is gaining momentum, both within NASA and industry
circles.

Not only would the deep space sojourn shake out hardware, it would also build
confidence in long-duration stints at the moon and Mars. At the same time, the
trek would sharpen skills to deal with a future space rock found on a collision
course with Earth.

In Lockheed Martin briefing charts, the mission has been dubbed Plymouth Rock –
An Early Human Asteroid Mission Using Orion. Lockheed is the builder of NASA's
Orion spacecraft, the capsule-based replacement for the space shuttle.

Study teams are now readying high-level briefings for NASA leaders - perhaps as
early as this week - on a pilgrimage to an asteroid, along with appraisals of
anchoring large, astronaut-enabled telescopes far from Earth, a human precursor
mission to the vicinity of Mars, as well as an initiative to power-beam energy
from space to Earth.

The briefings have been spurred in response to the recent Review of U.S. Human
Spaceflight Plans Committee and the option of a Flexible Path to human
exploration beyond low-Earth orbit.

On this path, the committee suggested, humans would visit sites never visited
before and extend U.S. savvy in how to operate in space - while traversing
greater and greater distances from Earth.

Building momentum

The merits of a human mission to a Near Earth Object (NEO) were detailed here
Nov. 18 during a two-day meeting of the Small Bodies Assessment Group, SBAG for
short.

SBAG was established by NASA in 2008 to identify scientific priorities and
opportunities for the exploration of asteroids, comets, interplanetary dust,
small satellites, and Trans-Neptunian Objects. The group also provides
scientific input on the utility of asteroids and comets in support of human
space activities.

The new studies are viewed as an iterative process - to be weighed both by NASA
and the White House, said Paul Abell, a research scientist at the Planetary
Science Institute detailed to the space agency's Johnson Space Center in
Houston, Texas and working in the Astromaterials Research and Exploration
Science Directorate. It's going to take a bit of time. I don't think there's
going to be a quick decision.

How the White House will react to a human trek to an asteroid is beyond
anybody's crystal ball. However, undertaking the effort has garnered the
attention of Lockheed Martin - builder of the space shuttle replacement - the
Orion spacecraft.

Asteroid-bound Orion

The Plymouth Rock mission study began a couple years ago, said Josh Hopkins, in
the advanced programs for human space flight division at Lockheed Martin Space
Systems Company in Denver, Colo.

We have been looking at what other interesting science missions could be done
with Orion...and asteroids were one of the ideas that percolated to the top,
Hopkins told the SBAG attendees. He made it clear that the firm's study was done
using corporate funds and doesn't imply that NASA has endorsed company results.

Initial looks at the NEO venture involve the coupling of two Orion spacecraft.

In this situation, a two-person Orion would link up with an unpiloted sister
craft that's loaded with extra fuel, food, water, and oxygen. It would be tossed
into orbit - as well as an Earth departure stage - by NASA's planned Ares V
heavy-lift booster.

Bridging the moon and Mars

While detailed NASA and industry looks at the makings of a NEO mission are still
in play - including use of inflatable modules to add crew volume - it's an
attractive option, Hopkins said. It's really a good middle-step between the
moon and Mars.

However, maximizing astronaut safety, dealing with such things as trash
management, cosmic rays, sketching out abort scenarios must still be addressed,
Hopkins noted. But given the core attributes already built into the Orion system
we think it does make sense for the human spaceflight program to be
investigating this, he said.

Between NASA and industry looks, the flight of astronauts to a NEO could occur
in the 2020 to 2025 time period. The round-trip mission would take some six
months.

There would be no landing on the asteroid. Rather, they would park in close
proximity, then jet backpack onto the object. Once there, science gear would be
deployed as samples of the space rock are gathered – on the order of a couple
hundred pounds (100 kilograms).

We assume staying at the asteroid for five days. They could stay a week or two.
But staying for a month gets hard, Hopkins explained. While on duty, astronauts
would engage in gathering data useful to understand the internal makeup of the
asteroid. That, in turn, is solidly helpful, he added, in dealing with harmful
space rocks on a worrisome 

[meteorite-list] SALE- Santa Rosa Iron Smaller more affordable specimens

2009-11-23 Thread robert cucchiara
Hi List, I have cut down some of the Santa Rosa iron meteorite, do to the
high demand of smaller affordable specimens. See all that is available
below!
http://www.meteoritemadness.com/santarosa.html 

First emailed, first served! Thanks Bob C.

HENRY A. WARD AND THE RECOVERY OF THE
SANTA ROSA, COLOMBIA, METEORITE
H. Plotkin, Department of Philosophy, University of Western Ontario, London,
Ontario N6A3K7, Canada. 
Email:hplot...@uwo.ca
Henry A. Ward (1834-1906) was perhaps the shrewdest and most enthusiastic
meteorite collector of his day. He was also very knowledgeable. Word of a
massive iron meteorite in Santa Rosa, Colombia, captured his imagination.
Ward's interest can best be viewed in the context of the confusion that
existed between this meteorite and two other irons that had been found
nearby, Tocavita and Rasgata. In an effort to clear up the mess-- and also
to see if he could acquire the meteorite in whole or in part--he decided to
visit the desolate locale in 1906, a few weeks prior to his 72nd birthday.
My account of Ward's Colombian trip is primarily based on the extensive
collection of unpublished material in the Henry A. Ward papers at the
University of Rochester, including diaries, correspondence, and photographs.
Upon arrival in Colombia, it took Ward nineteen days by steamer, mule, and
carriage to reach Santa Rosa. He arrived at nightfall, but as soon as he
looked out from his hotel window the next morning, he saw the large
meteorite (612.5 kg) perched atop a fluted column in the middle of the town
square. Ward realized the meteorite was highly venerated by the townspeople,
and knew it would be extremely difficult--if not impossible--to acquire any
of it. But he had a clever plan. Calling on the Governor, Ward boldly
proposed an exchange: in return for a promise to erect a statue in the town
square of the President of the Republic (who happened to have been born in
Santa Rosa), he would be given the entire meteorite. The Governor liked this
idea, and at a stormy meeting with the Mayor and other municipal officers
forced their approval. Late that night, in the middle of a large eating and
drinking party which Ward threw at his hotel for the townspeople, the
Governor and a party of 50 soldiers quietly overturned the column, placed
the meteorite on a cart, and whisked it away. Ward left for Bogota the next
day, but shortly after reaching there heard that the Chief of the Colombian
police had sent out a party that had captured his wagon, retrieved the
meteorite, and locked up the cart driver. Although Ward insisted he had
proper authorization for the meteorite, a heated legal battle ensued. A
decision by the Minister of Public Instruction forbade him to leave the
country with the meteorite, but he was allowed to cut off a large endpiece
(147.5 kg) for his efforts. Ward took this back with him to New York, but he
died tragically a few months after his return, when struck by an automobile
while crossing a street in Buffalo. Ward's unfinished report on the Santa
Rosa meteorite will be examined, as will our present understanding of its
relationship to Tocavita and Rasgata. The main mass of the Santa Rosa
meteorite (about 460 kg) is now in the National Museum in Bogota, while
Ward's endpiece was cut up and distributed to various museums throughout the
world for study and curation.
67th Annual Meteoritical Society Meeting (2004) 5038.pdf


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[meteorite-list] Space junk?

2009-11-23 Thread E.P. Grondine
Hi Mike - 

Space Junk?

E.P. Grondine
Man and Impact in the Americas




  
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[meteorite-list] Galileo's missing fingers found in jar

2009-11-23 Thread Meteorites USA

Related and morbid but interesting...

...(CNN) -- Two fingers cut from the hand of Italian astronomer Galileo 
nearly 300 years ago have been rediscovered more than a century after 
they were last seen, an Italian museum director said Monday...


CNN World: Galileo's missing fingers found in jar
http://www.cnn.com/2009/WORLD/europe/11/23/galileo.fingers/index.html

Regards
Eric Wichman
Meteorites USA



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Re: [meteorite-list] Galileo's missing fingers found in jar

2009-11-23 Thread Mike Hankey
can't wait till they hit ebay!

On Mon, Nov 23, 2009 at 4:47 PM, Meteorites USA e...@meteoritesusa.com wrote:
 Related and morbid but interesting...

 ...(CNN) -- Two fingers cut from the hand of Italian astronomer Galileo
 nearly 300 years ago have been rediscovered more than a century after they
 were last seen, an Italian museum director said Monday...

 CNN World: Galileo's missing fingers found in jar
 http://www.cnn.com/2009/WORLD/europe/11/23/galileo.fingers/index.html

 Regards
 Eric Wichman
 Meteorites USA



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Re: [meteorite-list] Galileo's missing fingers found in jar

2009-11-23 Thread Mark Crawford

Don't laugh (and yes, OT):

http://www.theregister.co.uk/2009/11/23/mussolinis_brain/

M

Mike Hankey wrote:

can't wait till they hit ebay!

On Mon, Nov 23, 2009 at 4:47 PM, Meteorites USA e...@meteoritesusa.com wrote:
  

Related and morbid but interesting...

...(CNN) -- Two fingers cut from the hand of Italian astronomer Galileo
nearly 300 years ago have been rediscovered more than a century after they
were last seen, an Italian museum director said Monday...




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Re: [meteorite-list] Galileo's missing fingers found in jar

2009-11-23 Thread Martin Altmann
Don't laugh neither:

Search for:   relic* -medal* -rosary -icon -statue -water -image

And there for the 1st class relics.

Each week.

In German ebay it's forbidden to sell body parts.

And there someone should still say, that meteorite collecting is a weird
hobby...

Martin


-Ursprüngliche Nachricht-
Von: meteorite-list-boun...@meteoritecentral.com
[mailto:meteorite-list-boun...@meteoritecentral.com] Im Auftrag von Mark
Crawford
Gesendet: Montag, 23. November 2009 23:03
An: Mike Hankey
Cc: meteorite-list@meteoritecentral.com
Betreff: Re: [meteorite-list] Galileo's missing fingers found in jar

Don't laugh (and yes, OT):

http://www.theregister.co.uk/2009/11/23/mussolinis_brain/

M

Mike Hankey wrote:
 can't wait till they hit ebay!

 On Mon, Nov 23, 2009 at 4:47 PM, Meteorites USA e...@meteoritesusa.com
wrote:
   
 Related and morbid but interesting...

 ...(CNN) -- Two fingers cut from the hand of Italian astronomer Galileo
 nearly 300 years ago have been rediscovered more than a century after
they
 were last seen, an Italian museum director said Monday...
 


-- 
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Re: [meteorite-list] Galileo's missing fingers found in jar

2009-11-23 Thread ensoramanda
Hi Mike, All

The fingers and tooth are already on ebay.

Item number 350275205445  ;-)

Graham, UK

 Mike Hankey mike.han...@gmail.com wrote: 
 can't wait till they hit ebay!
 
 On Mon, Nov 23, 2009 at 4:47 PM, Meteorites USA e...@meteoritesusa.com 
 wrote:
  Related and morbid but interesting...
 
  ...(CNN) -- Two fingers cut from the hand of Italian astronomer Galileo
  nearly 300 years ago have been rediscovered more than a century after they
  were last seen, an Italian museum director said Monday...
 
  CNN World: Galileo's missing fingers found in jar
  http://www.cnn.com/2009/WORLD/europe/11/23/galileo.fingers/index.html
 
  Regards
  Eric Wichman
  Meteorites USA
 
 
 
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[meteorite-list] Free Spirit: Third Extrication Drive Ends With Wheel Stall

2009-11-23 Thread Ron Baalke

http://www.jpl.nasa.gov/news/news.cfm?release=2009-173

Free Spirit: Third Extrication Drive Ends With Wheel Stall
Jet Propulsion Laboratory
November 23, 2009

Spirit experienced a wheel stall with the right-rear wheel during the
second step of a two-step drive on Sol 2092 (Saturday, Nov. 21). This is
not the same wheel that stalled on Sol 1899 (May 6), the left-middle
wheel. On Sol 2092, the right-rear wheel did not experience a hard stall
like what was seen on Sol 1899.  Instead, it stalled because the wheel's
progress fell behind the expected rotation rate. The rover had completed
about 4 meters (13 feet) of commanded wheel spin before the stall
terminated the drive. The center of the rover moved about 4 millimeters
(0.2 inch) forward, 3 millimeters (0.1 inch) to the left and about 3
millimeters (0.1 inch) down. The rover suspension stayed within the
tighter limits set for the drive, and there was only a fractional change
in rover tilt.

The plan ahead for today, Nov. 23, is to sequence a set of diagnostics
to explore the right rear wheel stall. The diagnostics will include a
rotor resistance test, a possible steering test, a small backward
rotation of just the right-rear wheel and a short (about 1 meter, or 3
feet) forward commanded motion of the rover. Resumption of the
extrication driving would be no sooner than Wednesday.

Guy Webster 818-354-6278
Jet Propulsion Laboratory, Pasadena, Calif.
guy.webs...@jpl.nasa.gov

Dwayne Brown 202-358-1726
NASA Headquarters, Washington
dwayne.c.br...@nasa.gov
2009-173

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[meteorite-list] AD: 10% Off Take All Deals

2009-11-23 Thread Meteorites USA

OK Guys,

I have some good deals for those who've been waiting.

ONE TIME OFFER: First Come First Served - Take All Deal for everything 
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BRENHAM PALLASITE SLICES:
46.1g Polished Brenham Pallasite Slice - Translucent Green Crystals - $161
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51.3g Polished Brenham Pallasite Slice - $175
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MUONIONALUSTA:  10% Off Individual Marked Price or Take All 
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20.8g Etched Muonionalusta Iron Meteorite $20 Beautifully Etched
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34.1g Etched Muonionalusta Iron Meteorite $30 Beautifully Etched
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36.9g Etched Muonionalusta Iron Meteorite $30 Beautifully Etched
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15.5g Etched Canyon Diablo Iron Meteorite $13 Beautifully Etched 
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21.3g (SIDE A) Canyon Diablo Etched Part Slice: $20
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11-6g Etched Nantan Iron Meteorite $12 TROILITE INCLUSION Beautifully 
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16.9g Etched Nantan Iron Meteorite $15 Beautifully Etched
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20.5g Etched Nantan Iron Meteorite $17 Beautifully Etched
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-

Call me to order or send an email.

Regards,
Eric Wichman
Meteorites USA
904-236-5394


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[meteorite-list] AD-Australite Fully Flanged Button 0.99cents No Reserve!

2009-11-23 Thread info
Hello all,

Im heading back home soon so I need some cash to fund my trip. Im listing
my button with no reserve starting at 99cents. It was previously listed at
Buy It Now for $1999 with now takers but a LOT of watchers!

Here is the link:

http://cgi.ebay.com/ws/eBayISAPI.dll?ViewItemrd=1item=350283673840ssPageName=STRK:MESE:IT

Thanks for your time and Happy Holidays!

Cheers,
Desmond Leong
IMCA #2254
http://www.TektiteInc.com
http://stores.ebay.com/Tektite-Inc
http://search.ebay.com/_W0QQsassZtektiteinc-dot-com


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Re: [meteorite-list] Ablation Zone 5 Layers...AND Crust

2009-11-23 Thread Pete Shugar
Now there's a $27.87 dollar word if I ever heard 
one-autodidactly

One who is self taught. WOW
- Original Message - 
From: MEM mstrema...@yahoo.com
To: altm...@meteorite-martin.de; meteorite-list@meteoritecentral.com; 
Greg Stanley stanleygr...@hotmail.com

Sent: Monday, November 23, 2009 12:12 AM
Subject: Re: [meteorite-list] Ablation Zone 5 Layers...AND Crust



- Greg Stanley  wrote:

See  Fig. 1 on this UCLA web page.
http://www.ess.ucla.edu/research/cosmochem/meteorite.asp

Not sure if Dr. Wasson has written any papers regarding
fusion crusts on irons, but I would think he would endorse
anything on the web page.


So Gregg, if your statement is true, Dr.Wasson and/or UCLA endorses the 
formation of rusty fusion crust actually formed during decent? ( Fig 1 
or is it the regmaglyts that formed during passage and they are on top of 
the rusty fusion crust?)


The issue is deeper than the semantic arguments, glossary obsolesence and 
lies in the differences of origin, composition, and presence of crust on 
different classes of meteorites. In the old school, a crust is generally 
removable from the underlying substrate and a dipping in molten metal 
alloy pushes the envelope of being a crust, however Buchwald illustrated 
that this was a combination of free metal and oxides. I conceed that 
irons--most all freshly fallen ones anyway , do have a fused surface that 
we can by convention call crust but the question remains as to what is 
the crust which is a few microns thick versus coatings and halos etc. 
There is danger of promoting ignorance by making assumptions that 
everything which is called crust is identical.


I am old school and I have the (un)reasonable expectation that where a 
distinction does lie, that the collector can understand why things are the 
way they are and not abuse the descriptions when they try to peddle their 
specimens.  Very few understood the distinction of silicate content when 
addressing irons as the presence of silicates,oxides, carbides,phosphides, 
etc largely govern the nature of a particular crust and gives insight into 
what went on during that miliseconds of exposure when the final surface 
was formed.


Why it matters to me is 1) the abuse of the term in describing meteorite 
conditions 2) the science of understanding the differences in crust origin 
and composition and 3) how do we make the distinction amongst flight 
markings and do they differ from fusion crust?


I am satisfied that 1)one of the iron specimens cited in this discussion 
apparently do have a silicate content that provided for a glassy fusion 
crust and its origin is intriguing scientifically.  2)That by definition 
alone (fused + coating) the irons do routinely have a fused 
coating/crust which differs significantly from our traditional concept of 
crust even though it is indistinguishable from the interior to the naked 
eye. (Do folks really see the crust or do they see if because it is 
supposed to be there?) At what point in weathering do we see that the 
welded crust/layer on an iron has rusted away given it is a few microns 
thick? 90% of the time, the seller will be claiming crusted long after 
the crust is gone, IMO.


I've seen little to nothing so far that invalidates describing the 
ablation zone nor crust in layers--Nor did Buchwald, apparently.


Finally, the term big-head someone used probably translates to 
arrogant Either way it was used in error as I was misunderstood. I did 
not disparage the pioneers in the field or meteoritical study.  They 
gained their meteoritical knowledge largely autodidactly when they came 
over.  I mentioned their former fields because when an individual crosses 
over into a different field of research, one can not just presume that 
they immediately acquire the entire knowledge base of those who were 
formerly educated in the same field.


Elton

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[meteorite-list] GPS Photographing Meteorites in the field

2009-11-23 Thread Richard Kowalski
Some months ago I went on my first meteorite hunt and hope to try my hand at it 
again in the not too distant future.

On my first hunting trip I used my automotive unit, since it easily fit into my 
pocket. My other GPS is an aviation unit and is much larger and heavier. 
Obviously neither is optimal for hunting or hiking.

I'm looking at hiking GPSr units that have a camera built in, specifically the 
Garmin Oregon 550. This unit automatically tags the all the images made with it 
with the longitude  latitude where the image was made.

Most of the images of new discoveries I've seen show a blacked out GPS next 
to the stone.

I'm just curious if any of you active hunters are using geo-tagging GPS cameras 
or if there is a specific reason not to use one. Its easy enough to strip out 
the coordinates embedded in the image file if you don't want to leave this in 
any distributed copies of the image, so that isn't a reason not to use one.

Any input is appreciated.

Thanks

--
Richard Kowalski
http://fullmoonphotography.net
IMCA #1081


  
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Re: [meteorite-list] What is or is not a chondrule?

2009-11-23 Thread Jeff Kuyken

Better late than never I always say. It was an interesting post too.

Thanks,

Jeff


- Original Message - 
From: Carl 's carloselgua...@hotmail.com

To: meteorite-list@meteoritecentral.com
Sent: Tuesday, November 24, 2009 1:28 AM
Subject: Re: [meteorite-list] What is or is not a chondrule?




Hi Elton,

I couldn't help notice Walter originally asked this question way back July 
6, 2006.:) I don't have a point but thought it was funny.


Carl


Elton wrote:
...I don't know if you ever got an answer to your question but I had it 
marked for follow up...



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