[meteorite-list] request for NASA contact person

2005-09-07 Thread Dr. Svend Buhl
Hello list,

Im currently working on a small paper regarding the standards of meteorite 
photo-documentation. In this regard I sent an email to a NASA representative 
listed at the ANSMET page as contact person. I was asking for information on 
NASA's standards of meteorite photography, but did not receive any response. 
Can somebody provide a contact to a curator or another relevant NASA 
representative willing to answer a few specific questions on this issue?

thanks for your efforts in advance
Svend

www.niger-meteorite-recon.de
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Re: [meteorite-list] 100 year old meteorite story from Sweden

2005-09-07 Thread chris aubeck
Hi Sterling,

Thanks for this information, I find it interesting and useful for my
own studies. However, I do not expect it to be the fossil story
original mentioned by Göram. Not because I know much about sedimentary
meteorite falls, but because I know a thing or two about alleged
fossil-bearing spacerocks from the 19th century press. It would
surprise me if Swedish newspapers didn't publish a report about a
meteorite that remained hot for an impossibly long time and contained
organic fossils, simply because that was the fashion at the time.

Best wishes,

Chris



On 9/7/05, Sterling K. Webb [EMAIL PROTECTED] wrote:
 Hi,
 
You're probably referring to:
 
BLECKENSTAD,
Ostergotland, Sweden, April 11, 1925
 
 A meteor was observed, leaving a trail
 of smoke. Stones are said to have
 fallen, and fragments of a white, porous
 limestone were picked up, differing from
 the local rocks. The possibly meteoritic
 nature of this material has been the subject
 of considerable discussion, N. Zenzen
 (1942, 1943); A. Hadding (1943); F.C. Cross
 (1947). Pseudometeorite, F.E. Wickman
  A. Uddenberg-Anderson (1982).
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Re: [meteorite-list] 100 year old meteorite story from Sweden

2005-09-07 Thread Ingo Herkstroeter
Hi Folks!
 
 If this is the stone I'm thinking of, Zenzen,
 who was head of the Sweden Geological Survey
 or Museum, or equivalent official and a prominent
 geologist, wrote extensively on it. The witness
 account is perfectly consistently with the real
 thing and the stone is fossilerous limestone.

I think this indicates a new question: Are sedimentary meteorites
possibible?

People mostly don´t think about this problem and so this problem don´t
exist! We all knew, that we have rocks from Mars, but this rocks are only
igneous! Why most people don´t accept, that sedimantary rocks could be hard
enough to survive a impact (and this is the main problem) and become
meteorites? I don´t know how many of you ever piced up a hammer and go out
in the field to have a look to terrestrial rocks. I´ve made this since I´m 8
years old and I´ve seen a lot of sed. rocks hard enough to do so. There are
sed. rocks on the Mars that´s sure, so why not a Mars sandstone or
limestone?

And what´s about planetary metamorphic rocks (not shock met.).?

Just a few wild thoughts

Ingo/Germany

--- Ursprüngliche Nachricht ---
 Von: Sterling K. Webb [EMAIL PROTECTED]
 An: [EMAIL PROTECTED], Meteorite-list@meteoritecentral.com
 Betreff: Re: [meteorite-list] 100 year old meteorite story from Sweden
 Datum: Tue, 06 Sep 2005 19:17:18 -0500
 
 Hi,
 
 You're probably referring to:
 
 BLECKENSTAD,
 Ostergotland, Sweden, April 11, 1925
 
 A meteor was observed, leaving a trail
 of smoke. Stones are said to have
 fallen, and fragments of a white, porous
 limestone were picked up, differing from
 the local rocks. The possibly meteoritic
 nature of this material has been the subject
 of considerable discussion, N. Zenzen
 (1942, 1943); A. Hadding (1943); F.C. Cross
 (1947). Pseudometeorite, F.E. Wickman
  A. Uddenberg-Anderson (1982).
 
 If this is the stone I'm thinking of, Zenzen,
 who was head of the Sweden Geological Survey
 or Museum, or equivalent official and a prominent
 geologist, wrote extensively on it. The witness
 account is perfectly consistently with the real
 thing and the stone is fossilerous limestone.
 All that happened is that he ruined his
 reputation and lost his job. Sad. I posted a
 long investigation report about it and it may
 still be in the archives if they go back far
 enough.
 The explanation is blindingly simple.
 It's a terrestrial meteorite., blasted off the
 Earth by impact and returned to the Earth
 100,000's of years later, instead of wandering
 the System or ending up on Mars or Venus...
 The simulations of interplanetary transport
 by Melosh, Gladman, and others, always
 show a fair percentage of impact liberated
 materials returning to their world of origin.
 Nininger found a fossilliferous meteorite
 too, with a thin calcinated fusion crust and
 wrote, briefly, about it, but he, unlike Zenzen,
 knew when to shut up.
 
 
 Sterling K. Webb
 --
 chris aubeck wrote:
 
  Hi,
 
  Last year, on September 21st, I received a reply on this list from
  Göran Axelsson which ended, enigmatically:
 
  As a sidenote there were a meteorite found in sweden almost 100 years
  ago with fossiles in it. Anyone want to debunk that one?
 
  :-)
 
  /Göran
 
  I was seriously interested in seeing a copy of the original article,
  but unfortunately Mr. Axelsson didn't reply. Can anyone tell me
  anything about it? This is exactly what I collect and study.
 
  Best wishes,
 
  Chris
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Re: [meteorite-list] Meteorite Raffle Major Update

2005-09-07 Thread Martin Altmann
But not enough yet, if we aim for an average of each list member having one
ticket, hh  :-)

Wow, a hunting trip - that's really the coolest prize!

Buckleboo!

- Original Message - 
From: batkol [EMAIL PROTECTED]
To: Notkin [EMAIL PROTECTED]; Meteorite List
meteorite-list@meteoritecentral.com
Sent: Wednesday, September 07, 2005 4:43 AM
Subject: Re: [meteorite-list] Meteorite Raffle Major Update


 As of today, you have raised more than $2,300 for the Red Cross. Hats
 off to everyone who pitched in.

 holy mudhead mackeral, that's quite an impressive figure.  good work!

 - Original Message - 
 From: Notkin [EMAIL PROTECTED]
 To: Meteorite List meteorite-list@meteoritecentral.com
 Sent: Tuesday, September 06, 2005 9:32 PM
 Subject: [meteorite-list] Meteorite Raffle Major Update


  Dear Friends and Listees:
 
  Greetings all. I have just completed a major update to our 2005
  Meteorite Charity Raffle project, and I think you will all be surprised
  by the quality, quantity, and ingenuity of these prizes. Newest
  additions have been placed at the top of the page for ease of viewing.
  We will shortly be breaking the prizes up into groupings: First Prize,
  Second Prize, etc. There will be MULTIPLE prizes awarded.
 
  I have also received a kind offer of numerous smaller items, which we
  will not have time to list on the site, but we will use them to make
  sure that as many people as possible go home with a nice meteorite
  memento from our charity raffle. Thanks to Steve Arnold IMB for
  organizing that.
 
  Here is the updated prize page:
 
  http://www.aerolite.org/meteorite-raffle.htm
 
 
  In addition, a few especially rare and collectible items have been
  offered to the project, and we are considering a series of special
  auctions on Ebay for those donated items, after the Denver show. More
  on that later. If someone would like to volunteer to help with Ebay
  sales, please let me know.
 
  I will have to stop accepting raffle prizes within the next couple of
  days. If you have something you'd like to donate, please don't delay
  (last minute additions may be accepted but will not appear on the
  website).
 
  Ticket sales continue. PLEASE NOTE: The cut-off date for ticket sales
  is Monday, September 12. If I have not received your payment by that
  date, you will not be eligible to participate in the prize drawing,
  sorry. We will try to accommodate last-minute cash ticket sales during
  the Denver Show, but I am making no promises. Payments can be made
  through PayPal (use link on raffle page), or you can mail personal
  checks (made out to the American Red Cross please) to me at:
 
  Geoffrey Notkin
  P.O. Box 36652
  Tucson, AZ 85740
 
 
  Anne Black of the Denver COMETS has kindly offered to receive prizes by
  mail, on our behalf in Denver. She will post her mailing address
  shortly. Blaine Reed has kindly offered to display prizes in his room
  during the Denver Show. We suggest that our friends in Europe who have
  donated prizes do not mail them at this time. We will ask you to mail
  prizes directly to the winners, following the drawing.
 
  As of today, you have raised more than $2,300 for the Red Cross. Hats
  off to everyone who pitched in.
 
  More news when I have it  : )
 
 
  Best to all,
 
  Geoff N.
 
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Re: [meteorite-list] AD: RARE INDEPENDENCE, MO FULL SLICE

2005-09-07 Thread Martin H.
Ryan kindly wrote:

 I am looking to quickly sell a 11.53g full slice of
the hard to aquire Independece, MO L6.  
 ...a great story goes with this one.  A classic
American fall. 


Hi Ryan and All,

There is a wonderful story that goes with this stone,
and if anyone is interested, here is an article I
wrote about the discovery of Independence (by Allen
Shaw, a Meteorite List member!) for The Meteorite
Times:

http://www.meteoritetimes.com/Back_Links/2002/June/Accretion_Desk.htm

In this article, I mention my 19.8g slice. I have
since upgraded Independence in my collection from that
slice to the main mass (;- )

Happy reading.

Martin















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[meteorite-list] Chondrites support Miller-Urey experiment atmo assumptons

2005-09-07 Thread Darren Garrison
http://news-info.wustl.edu/news/page/normal/5513.html

Calculations favor reducing atmosphere for early earth 

Was Miller-Urey experiment correct? 

By Tony Fitzpatrick 


Sept. 7, 2005 — Using primitive meteorites called chondrites as their models, 
earth and planetary
scientists at Washington University in St. Louis have performed outgassing 
calculations and shown
that the early Earth's atmosphere was a reducing one, chock full of methane, 
ammonia, hydrogen and
water vapor. 

In making this discovery Bruce Fegley, Ph.D., Washington University professor 
of earth and planetary
sciences in Arts  Sciences, and Laura Schaefer, laboratory assistant, 
reinvigorate one of the most
famous and controversial theories on the origins of life, the 1953 Miller-Urey 
experiment, which
yielded organic compounds necessary to evolve organisms.


Chondrites are relatively unaltered samples of material from the solar nebula, 
According to Fegley,
who heads the University's Planetary Chemistry Laboratory, scientists have long 
believed them to be
the building blocks of the planets. However, no one has ever determined what 
kind of atmosphere a
primitive chondritic planet would generate. 

We assume that the planets formed out of chondritic material, and we sectioned 
up the planet into
layers, and we used the composition of the mix of meteorites to calculate the 
gases that would have
evolved from each of those layers, said Schaefer. We found a very reducing 
atmosphere for most
meteorite mixes, so there is a lot of methane and ammonia. 

In a reducing atmosphere, hydrogen is present but oxygen is absent. For the 
Miller-Urey experiment
to work, a reducing atmosphere is a must. An oxidizing atmosphere makes 
producing organic compounds
impossible. Yet, a major contingent of geologists believe that a hydrogen-poor, 
carbon dioxide-rich
atmosphere existed because they use modern volcanic gases as models for the 
early atmosphere.
Volcanic gases are rich in water, carbon dioxide, and sulfur dioxide but 
contain no ammonia or
methane. 

Geologists dispute the Miller-Urey scenario, but what they seem to be 
forgetting is that when you
assemble the Earth out of chondrites, you've got slightly different gases being 
evolved from heating
up all these materials that have assembled to form the Earth. Our calculations 
provide a natural
explanation for getting this reducing atmosphere, said Fegley. 

Schaefer presented the findings at the annual meeting of the Division of 
Planetary Sciences of the
American Astronomical Society, held Sept. 4-9 in Cambridge, England. 

Schaefer and Fegley looked at different types of chondrites that earth and 
planetary scientists
believe were instrumental in making the Earth. They used sophisticated computer 
codes for chemical
equilibrium to figure out what happens when the minerals in the meteorites are 
heated up and react
with each other. For example, when calcium carbonate is heated up and 
decomposed, it forms carbon
dioxide gas. 

Different compounds in the chondritic Earth decompose when they're heated up, 
and they release gas
that formed the earliest Earth atmosphere, Fegley said. 

The Miller-Urey experiment featured an apparatus into which was placed a 
reducing gas atmosphere
thought to exist on the early Earth. The mix was heated up and given an 
electrical charge and simple
organic molecules were formed. While the experiment has been debated from the 
start, no one had done
calculations to predict the early Earth atmosphere. 

I think these computations hadn't been done before because they're very 
difficult; we use a special
code said Fegley, whose work with Schaefer on the outgassing of Io, Jupiter's 
largest moon and the
most volcanic body in the solar system, served as inspiration for the present 
early Earth atmosphere
work. 

NASA's Astrobiology Institute supported this work. 
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[meteorite-list] hope creek, ak

2005-09-07 Thread harlan trammell
i am looking for a 15-25g solid hope creek, ak piece and some lake okeechobee, fl. if anybody was this for sale, please email off list.
i will be gradually switching over to yahoo mail (it has 100 FREE megs of storage). please cc to: [EMAIL PROTECTED] 

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Re: [meteorite-list] Chondrites support Miller-Urey experiment atmo assumptons

2005-09-07 Thread Martin H.
Darren kindly posted:

http://news-info.wustl.edu/news/page/normal/5513.html 
 Was Miller-Urey experiment correct? 

Hi all,

Nobel Laureate Harold Urey was both instrumental in
meteorite science with his (and his students)
discoveries, as well as pushing students in new
directions due to disagreements with him. As Urey
studied meteorites, he tended to lean towards a large
(planetary) source for their origin. However, others
disagreed and felt that smaller bodies (asteroids)
were the source of meteorites. Obviously Urey lost
that battle.

While the Miller-Urey experiment is likely the most
influential and memorable contribution Urey made to
science, in essence his work led many to conclude that
he was the first to apply modern science to the study
of the solar system, and the person who pushed the
term cosmochemistry into popular science usage. Urey
was also leader in hte movement to reclassify
meteorites according to chemical criteria rather than
physical looks.

Here is a link to an Accretion Desk article I wrote
about Urey and meteorites for the Meteorite Times:

http://www.meteoritetimes.com/Back_Links/2004/october/Accretion_Desk.htm

Happy reading…again.

Martin









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[meteorite-list] MRO's HiRISE Camera Turned On

2005-09-07 Thread Ron Baalke


CAMERA'S TRIP TO MARS IS NO LEISURE CRUISE FOR HiRISE TEAM
From Lori Stiles, University Communications, UA, 520-621-1877
September 07, 2005

---
Contact information listed below
---

The High-Resolution Imaging Science Experiment (HiRISE) camera is rocketing
toward Mars, and it's no leisure cruise for the camera operations team at
The University of Arizona campus in Tucson either. The team turned the
HiRISE camera on Friday (Sept. 2).

NASA launched the Mars Reconnaissance Orbiter (MRO) and its science
payload, which includes the HiRISE camera, on Aug. 12. HiRISE -- the largest
telescopic camera sent beyond Earth's orbit -- and five other MRO
instruments will inspect the red planet in unprecedented detail and assist
future landers. The spacecraft will travel more than four times the distance
to Mars before entering Mars' orbit on March 10, 2006.

For the next year, the HiRISE team in Tucson will train new members joining
the project, write volumes of new software, image celestial objects to check
how their camera operates post-launch, and practice as if their camera
already were in orbit. UA Professor Alfred S. McEwen leads HiRISE.

We're very excited, and we're working very hard, said Eric Eliason, who
manages the HiRISE Operations Center (HiROC) at the UA's Lunar and Planetary
Laboratory.

Eliason and the rest of the HiROC team is responsible for most of the
ground data system work for the HiRISE camera. Observation planning, uplink,
downlink, instrument monitoring, and data processing and analysis will all
be done at HiROC, which is located in the UA's C.P. Sonett Space Sciences
Building. 

We'll get our first images tomorrow (Sept. 8) as the spacecraft slews our
camera over the moon and then over Omega Centauri, Eliason said. The
spacecraft is flying so fast that the moon will already look very small -
fewer than 200 pixels across. But we think we're going to get some really
pretty pictures of Omega Centauri. And we'll know very quickly how well our
instrument is working.

Plans are for HiRISE to make other sets of star observations on Oct. 4 - 5,
Nov. 5 and Dec. 13 - 14. The October images will show very precisely how MRO
navigation cameras are aligned with HiRISE. The November images will help
the HiRISE team fine-tune their camera's focus to get the sharpest images
possible. The December images will show how vibrations from different
spacecraft instruments may affect HiRISE images.

These observations will also help us to characterize the optical
distortion of our lens, and what processing methods we'll need to correct
for whatever distortion we see, Eliason said.

The 145-pound (65 kg) HiRISE camera features a 20-inch (half-meter) primary
mirror. Developed by Ball Aerospace  Technologies Corp., Boulder, Co., the
$40 million HiRISE camera will take ultra-sharp photographs over 3.5-mile (6
kilometer) swaths of the martian landscape, resolving rocks and other
geologic features as small as 40 inches (one meter) across. It will take
pictures in stereo and color while it flies at more than 7,800 mph (3 and
1/2 km per second) about 190 miles (300 km) above Mars' surface.

After entering Mars's orbit in March 2006, the MRO will gradually adjust
its elliptical orbit to a circular orbit by aerobraking, a technique that
creates drag using the friction of careful dips into the planet's upper
atmosphere. The spacecraft's 25-month primary science phase begins in
November 2006. 

The HiROC team expects to process 1,000 gigantic high-resolution images and
9,000 smaller high-resolution images during the science phase of the MRO
mission. 

The MRO mission is managed by JPL, a division of the California Institute
of Technology, Pasadena, for the NASA Science Mission Directorate. Lockheed
Martin Space Systems, Denver, prime contractor for the project, built the
spacecraft. 

---
Contact Information
Eric Eliason 520-626-0764 [EMAIL PROTECTED]
Alfred S. McEwen  520-621-4573 [EMAIL PROTECTED]

Related Web sites
 http://marsoweb.nas.nasa.gov/HiRISE/
 http://hirise.lpl.arizona.edu/

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[meteorite-list] Martian Volcanoes May Be Active

2005-09-07 Thread Ron Baalke

http://news.bbc.co.uk/1/hi/sci/tech/4219858.stm

Martian volcanoes 'may be active'
By Paul Rincon
BBC News 
September 7, 2005

Fields of volcanic cones discovered at the North Pole of Mars suggest
the Red Planet could still be geologically active, scientists have said.

The cones, seen in images from Europe's Mars Express probe, have no
blemishes from impact craters.

This suggests the volcanoes erupted very recently and that the sites
could have ongoing volcanism.

Mars Express scientist Gerhard Neukum presented the results at a
conference in Cambridge.

Mars is a planet that was very recently active - maybe one, or two, or
three million years ago. And in some areas, I have the impression it is
really ongoing, said Dr Neukum, of the Free University in Berlin, Germany.

Future eruptions

But what cannot be determined is when, if at all, some of these
volcanoes might erupt again: It could be a million years from now, it
could be tomorrow, he added.

Dr Neukum acts as the principal investigator for the High Resolution
Stereo Camera (HRSC) on Mars Express, which took the images in which the
cones were discovered.

There may be 50-100 of the volcanic cones covering a flank of the North
Pole about one million square kilometres in area. They are between 300m
(980ft) and 600m (1,970ft) tall, said Dr Neukum.

In addition to the North Pole, other regions with recent - and possibly
ongoing - activity on Mars include parts of Tharsis - home to the
volcano Olympus Mons - parts of Elysium and the so-called
highland-lowland boundary.

By counting the number of craters on the surfaces of Solar System
objects, scientists can estimate the age of those surfaces.

If they are heavily cratered, they are deemed older, while smoother
surfaces are considered younger. This assumes a constant cratering rate
since the heavy bombardment that terrestrial planets underwent about
four billion years ago.

Fresh cones

The cones appear to be fresh with no discernible evidence of cratering.
Dr Neukum admitted it was possible the cones could be ancient features
that have been eroded by wind, but added that this was unlikely.

I don't see any wind-related features in the region. We should see it
and we should see the remains of craters somewhere. But we don't, he
told the BBC News website.

Volcanic activity appeared to have peaked on Mars at around 1.5 billion
years ago, Dr Neukum said, adding: Mars is still active within certain
limits; it's still not dead.

Dr Neukum thinks that volcanic activity strongly influences glacial
activity on Mars. This is because on the Red Planet, eruptions also
mobilise water.

In some cases, this water freezes and forms glaciers, says Dr Neukum.
But other scientists believe glacial activity on the planet is more
strongly influenced by the inclination of Mars in its orbit around the Sun.

The Mars Express results were presented at the American Astronomical
Society Division of Planetary Sciences meeting in Cambridge, UK.

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[meteorite-list] Mars Global Surveyor Images: September 1-7, 2005

2005-09-07 Thread Ron Baalke

MARS GLOBAL SURVEYOR IMAGES
September 1-7, 2005

The following new images taken by the Mars Orbiter Camera (MOC) on
the Mars Global Surveyor spacecraft are now available:

o Cut By Troughs (Released 1 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/01

o Defrosting Sand (Released 2 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/02

o Polygons and Craters (Released 3 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/03

o Sediments of Terby (Released 4 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/04

o Caught in the Act (Released 5 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/05

o Mars at Ls 288 Degrees (Released 6 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/06

o Tharsis Limb Cloud (Released 7 September 2005)
  http://www.msss.com/mars_images/moc/2005/09/07



All of the Mars Global Surveyor images are archived here:

http://www.msss.com/mars_images/moc/index.html

Mars Global Surveyor was launched in November 1996 and has been
in Mars orbit since September 1997.   It began its primary
mapping mission on March 8, 1999.  Mars Global Surveyor is the 
first mission in a long-term program of Mars exploration known as 
the Mars Surveyor Program that is managed by JPL for NASA's Office
of Space Science, Washington, DC.  Malin Space Science Systems (MSSS)
and the California Institute of Technology built the MOC
using spare hardware from the Mars Observer mission. MSSS operates
the camera from its facilities in San Diego, CA. The Jet Propulsion
Laboratory's Mars Surveyor Operations Project operates the Mars Global
Surveyor spacecraft with its industrial partner, Lockheed Martin
Astronautics, from facilities in Pasadena, CA and Denver, CO.

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Re: [meteorite-list] Meteorite Raffle Major Update

2005-09-07 Thread Michael L Blood
Hi Martin  all,
If each person listing themselves on Meteorite Exchange as a
Meteorite Dealer (there are 135 of them) bought 10 tickets and
the other list members each bought 1 ticket, it would be over $18,000.
If everyone bought only 1 ticket, it would still be about $6,000.
Best wishes, Michael


on 9/7/05 3:23 AM, Martin Altmann at [EMAIL PROTECTED] wrote:

 But not enough yet, if we aim for an average of each list member having one
 ticket, hh  :-)
 
 Wow, a hunting trip - that's really the coolest prize!
 
 Buckleboo!
 
 - Original Message -
 From: batkol [EMAIL PROTECTED]
 To: Notkin [EMAIL PROTECTED]; Meteorite List
 meteorite-list@meteoritecentral.com
 Sent: Wednesday, September 07, 2005 4:43 AM
 Subject: Re: [meteorite-list] Meteorite Raffle Major Update
 
 
 As of today, you have raised more than $2,300 for the Red Cross. Hats
 off to everyone who pitched in.
 
 holy mudhead mackeral, that's quite an impressive figure.  good work!
 
 - Original Message -
 From: Notkin [EMAIL PROTECTED]
 To: Meteorite List meteorite-list@meteoritecentral.com
 Sent: Tuesday, September 06, 2005 9:32 PM
 Subject: [meteorite-list] Meteorite Raffle Major Update
 
 
 Dear Friends and Listees:
 
 Greetings all. I have just completed a major update to our 2005
 Meteorite Charity Raffle project, and I think you will all be surprised
 by the quality, quantity, and ingenuity of these prizes. Newest
 additions have been placed at the top of the page for ease of viewing.
 We will shortly be breaking the prizes up into groupings: First Prize,
 Second Prize, etc. There will be MULTIPLE prizes awarded.
 
 I have also received a kind offer of numerous smaller items, which we
 will not have time to list on the site, but we will use them to make
 sure that as many people as possible go home with a nice meteorite
 memento from our charity raffle. Thanks to Steve Arnold IMB for
 organizing that.
 
 Here is the updated prize page:
 
 http://www.aerolite.org/meteorite-raffle.htm
 
 
 In addition, a few especially rare and collectible items have been
 offered to the project, and we are considering a series of special
 auctions on Ebay for those donated items, after the Denver show. More
 on that later. If someone would like to volunteer to help with Ebay
 sales, please let me know.
 
 I will have to stop accepting raffle prizes within the next couple of
 days. If you have something you'd like to donate, please don't delay
 (last minute additions may be accepted but will not appear on the
 website).
 
 Ticket sales continue. PLEASE NOTE: The cut-off date for ticket sales
 is Monday, September 12. If I have not received your payment by that
 date, you will not be eligible to participate in the prize drawing,
 sorry. We will try to accommodate last-minute cash ticket sales during
 the Denver Show, but I am making no promises. Payments can be made
 through PayPal (use link on raffle page), or you can mail personal
 checks (made out to the American Red Cross please) to me at:
 
 Geoffrey Notkin
 P.O. Box 36652
 Tucson, AZ 85740
 
 
 Anne Black of the Denver COMETS has kindly offered to receive prizes by
 mail, on our behalf in Denver. She will post her mailing address
 shortly. Blaine Reed has kindly offered to display prizes in his room
 during the Denver Show. We suggest that our friends in Europe who have
 donated prizes do not mail them at this time. We will ask you to mail
 prizes directly to the winners, following the drawing.
 
 As of today, you have raised more than $2,300 for the Red Cross. Hats
 off to everyone who pitched in.
 
 More news when I have it  : )
 
 
 Best to all,
 
 Geoff N.
 
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-- 
Beware the fury of a patient man.
John Dryden
--
http://costofwar.com/index-world-hunger.html

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[meteorite-list] AD - NEW Lunar - NWA 3160 other Auctions

2005-09-07 Thread Greg Hupe

Dear list members,

We are pleased to announce a new lunar meteorite, NWA 3160. It is an 
Olivine-Phyric Mare Basalt. This particular meteorite has two lithologies, a 
Mare Basalt and an Olivine-Gabbro. I have listed 18 specimens on eBay, most 
with the Buy it Now option under my seller name, naturesvault.


Here is a link to one of the auctions:
NWA 3160 Olivine-Phyric Mare Basalt Lunar Meteorite
http://cgi.ebay.com/ws/eBayISAPI.dll?ViewItemitem=6559636103rd=1sspagename=STRK%3AMESE%3AITrd=1

To see all of the 18 lunar specimens, click on the above link and then click 
on View seller's other items. That, or go to eBay and search for items by 
seller, naturesvault.


I also have many rare auctions ending in a few hours, several still at just 
99 cents. Great deals will be had today.


Tonight I will be listing some of the unclassified material I brought back 
from my last Morocco trip. The supply is still drying up at a noticeable 
pace so I bought up as many stock piles as I could find, which really wasn't 
much. I will be offering unclassified material in both single stone form and 
in 1 kilo lots over the next several weeks so be sure to check back each 
week to see new material. Next week I will start the single stones along 
with the lots. Tonight will be some 1 kilo lots (ordinary chondrites and 869 
material).


Best regards,

Greg Hupe
The Hupe Collection
naturesvault (eBay)
[EMAIL PROTECTED]
IMCA 2185

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[meteorite-list] AD: 15 kilo sikhote Alin closing in 3 hours!

2005-09-07 Thread Michael Farmer

http://cgi.ebay.com/ws/eBayISAPI.dll?ViewItemrd=1item=6558759631

Don't let this sucker get away so cheap! Selling right now several hundred 
dollars under what I paid YEARS ago!


Mike Farmer

Se you all in Denver next week. 



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[meteorite-list] NWA 3160 Lithology

2005-09-07 Thread Adam Hupe
Hi List,

Some have already asked about the major basalt lithology in NWA 3160.  We
listed pieces with single and dual lithologies,  NWA 3160 was over 90%
basalt and this image demonstrates how closely it looks like NWA 032/479:

http://cgi.ebay.com/NWA-3160-Olivine-Phyric-Mare-Basalt-Lunar-Meteorite_W0QQitemZ6559635438QQcategoryZ3239QQrdZ1QQcmdZViewItem

Check it out, this is one awesome lunaite.

Take Care,

Adam



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[meteorite-list] Ceres May Be 'Mini Planet' with Water Ice

2005-09-07 Thread Ron Baalke

http://hubblesite.org/newscenter/newsdesk/archive/releases/2005/27/text/

Release Number: STScI-2005-27

Contact:

Dolores Beasley
NASA Headquarters, Washington
(Phone: 202/358-1753)

Susan Hendrix
Goddard Space Flight Center, Greenbelt, Md
(Phone: 301/286-7745)

Donna Weaver
Space Telescope Science Institute, Baltimore
(Phone: 410-338-4493)

Largest Asteroid May Be 'Mini Planet' with Water Ice
September 7, 2005

Observations of 1 Ceres, the largest known asteroid, have revealed that
the object may be a mini planet, and may contain large amounts of pure
water ice beneath its surface.

The observations by NASA's Hubble Space Telescope also show that Ceres
shares characteristics of the rocky, terrestrial planets like Earth.
Ceres' shape is almost round like Earth's, suggesting that the asteroid
may have a differentiated interior, with a rocky inner core and a
thin, dusty outer crust.

Ceres is an embryonic planet, said Lucy A. McFadden of the Department
of Astronomy at the University of Maryland, College Park and a member of
the team that made the observations. Gravitational perturbations from
Jupiter billions of years ago prevented Ceres from accreting more
material to become a full-fledged planet.

The finding will appear Sept. 8 in a letter to the journal Nature. The
paper is led by Peter C. Thomas of the Center for Radiophysics and Space
Research at Cornell University in Ithaca, N.Y., and also includes
project leader Joel William Parker of the Department of Space Studies at
Southwest Research Institute in Boulder, Colo.

Ceres is approximately 580 miles (930 kilometers) across, about the size
of Texas. It resides with tens of thousands of other asteroids in the
main asteroid belt. Located between Mars and Jupiter, the asteroid belt
probably represents primitive pieces of the solar system that never
managed to accumulate into a genuine planet. Ceres comprises 25 percent
of the asteroid belt's total mass. However, Pluto, our solar system's
smallest planet, is 14 times more massive than Ceres.

The astronomers used Hubble's Advanced Camera for Surveys to study Ceres
for nine hours, the time it takes the asteroid to complete a rotation.
Hubble snapped 267 images of Ceres. From those snapshots, the
astronomers determined that the asteroid has a nearly round body. The
diameter at its equator is wider than at its poles. Computer models show
that a nearly round object like Ceres has a differentiated interior,
with denser material at the core and lighter minerals near the surface.
All terrestrial planets have differentiated interiors. Asteroids much
smaller than Ceres have not been found to have such interiors.

The astronomers suspect that water ice may be buried under the
asteroid's crust because the density of Ceres is less than that of the
Earth's crust, and because the surface bears spectral evidence of
water-bearing minerals. They estimate that if Ceres were composed of 25
percent water, it may have more water than all the fresh water on Earth.
Ceres' water, unlike Earth's, would be in the form of water ice and
located in the mantle, which wraps around the asteroid's solid core.

Besides being the largest asteroid, Ceres also was the first asteroid to
be discovered. Sicilian astronomer Father Giuseppe Piazzi spotted the
object in 1801. Piazzi was looking for suspected planets in a large gap
between the orbits of Mars and Jupiter. As more such objects were found
in the same region, they became known as asteroids or minor planets.



http://hubblesite.org/newscenter/newsdesk/archive/releases/2005/27/image/a

Hubble Tracks Ceres

STScI-PRC2005-27

NASA's Hubble Space Telescope took these images of the asteroid 1 Ceres
over a 2-hour and 20-minute span, the time it takes the Texas-sized
object to complete one quarter of a rotation. One day on Ceres lasts 9
hours.

Hubble snapped 267 images of Ceres as it watched the asteroid make more
than one rotation. By observing the asteroid during a full rotation,
astronomers confirmed that Ceres has a nearly round body like Earth's.
Ceres' shape suggests that its interior is layered like those of
terrestrial planets such as Earth. Ceres may have a rocky inner core, an
icy mantle, and a thin, dusty outer crust inferred from its density and
rotation rate.

The bright spot that appears in each image is a mystery. It is brighter
than its surroundings. Yet it is still very dark, reflecting only a
small portion of the sunlight that shines on it.

Ceres is approximately 580 miles (930 kilometers) across and is the
largest known asteroid. It resides with tens of thousands of other
asteroids in a region between the orbits of Mars and Jupiter called the
main asteroid belt. Besides being the largest asteroid, Ceres also was
the first to be discovered, in 1801.

Astronomers enhanced the contrast in these images to bring out important
features on Ceres' surface. The observations were made in visible and in

[meteorite-list] Ceres Might Contain More Fresh Water than Earth

2005-09-07 Thread Ron Baalke

http://www.space.com/scienceastronomy/050907_ceres_planet.html

Largest Asteroid Might Contain More Fresh Water than Earth
By Bjorn Carey 
space.com
07 September 2005

The largest known asteroid could contain more fresh water than Earth and
looks like our planet in other ways, according to a new study that
further blurs the line between planets and large space rocks.

Astronomers took 267 images of asteroid Ceres using the Hubble Space Telescope. 
From these images and subsequent computer simulations, they suggest Ceres 
may have a rocky inner core and a thin, dusty outer crust.

A team led by Peter Thomas of Cornell University said today that Ceres
is nearly spherical, which suggests that gravity controls its shape.
Also, the asteroid's non-uniform shape indicates that material is not
evenly distributed throughout the inside.

These and other new clues, including Ceres' low density, point to an
interior loaded with frozen water, the astronomers said.

The results are detailed in the Sept. 8 issue of the journal Nature.

Big and round

Ceres has long been considered one of the tens of thousands of asteroids
that make up the asteroid belt between Mars and Jupiter. At 580 miles
(930 km) in diameter - about the size of Texas - it's the largest
asteroid in the belt, accounting for about 25 percent of the belt's total 
mass.

Astronomers had thought Ceres might never have been heated enough to
create layers of material.

But computer models now suggest Ceres has a differentiated interior - dense 
material in the core and lighter stuff near the surface.  Possible 
configurations include a mantle rich in water ice around a rocky core.

If this mantle is composed of at least 25 percent water, Ceres would
have more fresh water than Earth, according to a statement released by
the Space Telescope Science Institute, which operates Hubble for NASA
and the European Space Agency.

The most likely scenario from the knowledge we have on how other
objects form, it probably has a rocky core and a mantle. That mantle is
probably some watery, icy mix, with other dirt and constituents. That
mantle could be as much as ¼ of the whole object, study coauthor Joel
Parker of the Southwest Research Institute told SPACE.com. Even though
it's a small object compared to Earth, there could be a lot of water.

On Earth, fresh water makes up only a thin layer just a few miles deep
in some places, less in others. The water layer proposed for Ceres,
while smaller in circumference, is many miles thicker.

The total volume of water on Earth is about 1.4 billion cubic
kilometers, around 41 million of which is fresh water. If Ceres' mantle
accounts for 25 percent of the asteroid's mass, that would translate to
an upper limit of 200 million cubic kilometers of water, Parker said.

Since all the nine regular planets have differentiated interiors, this
new view of Ceres has some astronomers calling Ceres a mini-planet,
adding fuel to an ongoing debate over exactly what qualifies as a planet.

Embroyonic world

Other researchers recently announced the discovery of 2003 UB313, a round
object in our solar system 1-1/2 times larger than Pluto and about three
times further away from the Sun. But even an object of this size - at
2,100 miles in diameter roughly four times the size of Ceres - doesn't
receive universal endorsement as being a planet.

One astronomer, Brian Marsden, who runs the Minor Planet Center where
data on small bodies is collected, says that if Pluto is considered a
planet, then any other round worlds should also be considered planets.
Under this definition, which some other astronomers subscribe to, Ceres
2003 UB313 and a handful of other large objects would be named planets.
The alternative, Marsden and others say, is to stop calling Pluto a
planet. 

Another explanation is that Ceres is a sort of 'baby' planet - an
underdeveloped version of Earth and other rocky planets. Looked at this
way, Ceres appears as other fledgling planets might have looked more
than 4 billion years ago.

The leading theory for planet formation holds that small rocks collided,
stuck and gradually grew. Depending on location and orbit, a developing
world may or may not have encountered enough raw material to become as
large as the four traditional rocky planets.

Ceres is an embryonic planet, said observation team member Lucy
McFadden of the Department of Astronomy at the University of Maryland.
Gravitational perturbations from Jupiter billions of years ago
prevented Ceres from accreting more material to become a full-fledged
planet.

In 2015 scientists will get a close up look at Ceres when the NASA Dawn
mission orbits the asteroid.  A closer look should provide more clues 
about the asteroid's composition.
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[meteorite-list] Deep Impact Collision Ejected the Stuff of Life

2005-09-07 Thread Ron Baalke

http://www.newscientistspace.com/article/dn7961-deep-impact-collision-ejected-the-stuff-of-life.html

Deep Impact collision ejected the stuff of life
Maggie McKee
New Scientist
07 September 2005

Millions of kilograms of fine dust particles and water and a
surprisingly high amount of organic molecules sprayed into space when
NASA crashed its Deep Impact spacecraft into Comet 9P/Tempel 1 on 4 July
2005, reveal a trio of new studies.

The observations bolster theories that comets may have seeded Earth with
the raw materials for life and suggest they may be sponge-like - rather
than hardened - at their cores.

On 4 July, about 80 telescopes on Earth and in space trained their
sights on Comet Tempel 1 when a 370-kilogram copper impactor was sent
hurtling into its path. Just after the smash, a bright vapour plume
spewed from the surface at about 5 kilometres per second, followed
quickly by a stream of particles that spread into a cone.

The cone appeared to remain attached to the comet's surface for about 22
hours before separating into a detached arc. Researchers used this
gravitational attraction to estimate the mass and density of the comet's
main body, or nucleus. They found that the 72 trillion kilogram-nucleus
was extremely porous, with as much as 80% of its volume taken up by
empty space.

That tells me there is no solid layer all the way down to the centre,
says Mike A'Hearn, the mission's principal investigator at the
University of Maryland in College Park, US. He says he had expected that
the ice might become denser towards the core of the nucleus, but that
instead probably all the way in, ice is all in the form of tiny grains.
  
A touch crumbly

It's like a sponge, with a lot of cavities, agrees Horst Uwe Keller,
an astronomer at the Max-Planck Institute for Solar System Research in
Germany. He observed the event with Europe's Rosetta spacecraft and says
the discovery confirms previous observations suggesting other comets are
also porous. When you touch it, it just crumbles under your hands.

Observers estimate the impact released about 5 million kilograms of
water from beneath the comet's surface and between two and five times as
much dust. There was so much dust, in fact, that mission members have
not been able to see the impact crater with the high-resolution camera
on the mission's flyby spacecraft, about 500 km away.

To add to the problem, that camera was malfunctioning but now
image-processing techniques may have revealed a glimpse of the crater
and team members may release the image later on Wednesday.
  
Building blocks

The team estimates the impact blasted away a crater about 100 metres
wide and up to 30 m deep. Crucially, organic molecules were among the
material ejected. Neither the full range of molecules nor their
abundances have been determined yet, but researchers say they have found
a surprisingly high amount of methyl cyanide, a molecule seen in large
quantities in another comet.

This supports theories that comets may have brought water and the
building blocks of life to Earth, and the team hopes to eventually
identify all the species comets brought in abundance to early Earth,
says A'Hearn.

The observations have also apparently ruled out another theory - that
impacts with other objects may be responsible for the occasional stream
of gas and dust seen coming off of comets. Although Tempel 1's surface
is pockmarked with craters ranging from 40 m to 400 m across,
astronomers watching the comet both before and after the impact noticed
that it released the streams relatively often in spurts of activity
apparently triggered by sunlight.

I don't think the hypothesis that outbursts are caused by impacts is
really valid, says A'Hearn. Probably comets undergo outbursts like
this very frequently and the fact that everyone was looking intensively
[at this comet] for an extended period allowed us to see phenomena that
are probably common and weren't seen before.

Journal reference: Science (DOI: 10.1126/science.1118923)

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[meteorite-list] The Next Mother Lode: Mars

2005-09-07 Thread Darren Garrison
If I was a druggie, I'd say give me some of what they are smoking.


http://www.wired.com/news/space/0,2697,68739,00.html

Space entrepreneurs eyeing Mars as a hub of some future solar system economy 
launched a startup on
Tuesday to mine the red planet for building materials. 

The new company, 4Frontiers, plans to mine Mars for building materials and 
energy sources, and
export the planet's mineral wealth to forthcoming space stations on the moon 
and elsewhere. 

The company also wants to build the first permanent human settlement on Mars, 
using strictly Martian
materials, as early as 2025. 

The idea is to make Mars a center for needs of the solar system economy, said 
Bruce Mackenzie,
co-founder of 4Frontiers and the company's vice president and outreach 
director. 

Mars happens to be a good place for these crucial minerals, said Mackenzie. 
You have them all in
one spot. 

Carbon, nitrogen and hydrogen are all scarce on the moon, but readily 
available on Mars, said
Joseph Palaia, 4Frontiers' other co-founder and vice president of operations 
and research and
development. And while oxygen is available in both locations, it is easier to 
extract on Mars, he
said. 

4Frontiers (the four being the Earth, moon, Mars and the main asteroid belt) 
will be ready in 2025
with the tools that space explorers will need to colonize the solar system, 
said Bruno Marino, a
consultant to the company. 

What makes this group so unique is that it is all about getting on the surface 
of Mars and making
the settlement, said Marino. We are ready to set up shop as soon as we can 
get on the surface. 

Marino was director of science and research at Biosphere 2, an enclosed 
ecosystem built to model
extraterrestrial settlements. The experimental facility, in Arizona, is now on 
the block. 

Biosphere 2 provided much of the inspiration and lessons learned for 
facilities planned for a
future Mars settlement, said Marino. 

4Frontiers' settlement plan faces some challenges, however, namely the harsh 
Martian environment,
with its nasty chemicals and radiation, said Molly Macauley, a senior fellow 
specializing in space
policy at Resources for the Future, a Washington, D.C., institute concerned 
with environmental and
energy issues. 

Macauley said she would not support any government funding for the startup. 

But if it flies on its own through private financing, said Macauley, it 
sounds great. 

4Frontiers' business plan is based on research done by the Mars Foundation, a 
group that has been
working on ways to fund and build a Martian settlement with local materials. 

In fact, the two groups have close ties. Mackenzie also co-founded the Mars 
Foundation and was
executive director of the Mars Society and a board member of the National Space 
Society. 

It will be many years before 4Frontiers is mining Mars and doling out mineral 
rights to Martian
prospectors. So the company has several moneymaking schemes for the near term. 

One plan is to build a full-scale version of the planned Mars settlement and 
charge visitors to tour
the Mars Settlement Research and Outreach Center. 4Frontiers hopes to have a 
site selected for the
center by the end of this year, said company co-founder and CEO Mark Homnick. 

We've narrowed the search to New Mexico, Central Florida or Colorado, he 
said. 

In addition, the company plans to develop technologies with immediate market 
value, according its
business plan. The group will sell any technology it develops to companies 
operating on Earth, as
well as those participating in NASA's Earth, Moon, Mars and Beyond space 
exploration program.
(4Frontiers also hopes to consult to these organizations.) The company has 
already applied to patent
a technology for making plastics on Mars using Martian materials. 

4Frontiers will also be hiring soon, said Homnick. 

We're not shooting blanks, said Homnick. We need to staff up. Our message to 
recent college
graduates is, 'You can go with a large corporation, give up some of your 
freedom and most of your
dreams. Or, if you have freedom in your heart, courage to face the unknown and 
discipline to
deliver, contact us.' 
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[meteorite-list] NASA's Spitzer and Deep Impact Build Recipe for Comet Soup

2005-09-07 Thread Ron Baalke

MEDIA RELATIONS OFFICE
JET PROPULSION LABORATORY
CALIFORNIA INSTITUTE OF TECHNOLOGY
NATIONAL AERONAUTICS AND SPACE ADMINISTRATION
PASADENA, CALIF. 91109 TELEPHONE (818) 354-5011
http://www.jpl.nasa.gov

Whitney Clavin (818) 354-4673   
Jet Propulsion Laboratory, Pasadena, Calif. 

News Release 2005-144   Sept. 7, 2005

NASA's Spitzer and Deep Impact Build Recipe for Comet Soup

When Deep Impact smashed into comet Tempel 1 on July 4, 
2005, it released the ingredients of our solar system's 
primordial soup. Now, astronomers using data from 
NASA's Spitzer Space Telescope and Deep Impact have 
analyzed that soup and begun to come up with a recipe 
for what makes planets, comets and other bodies in our 
solar system. 

The Deep Impact experiment worked, said Dr. Carey 
Lisse of Johns Hopkins University's Applied Physics 
Laboratory, Laurel, Md. We are assembling a list of 
comet ingredients that will be used by other scientists 
for years to come. Lisse is the team leader for Spitzer's 
observations of Tempel 1. He presented his findings this 
week at the 37th annual meeting of the Division of 
Planetary Sciences in Cambridge, England.

Spitzer watched the Deep Impact encounter from its lofty 
perch in space. It trained its infrared spectrograph on 
comet Tempel 1, observing closely the cloud of material 
that was ejected when Deep Impact's probe plunged below 
the comet's surface. Astronomers are still studying the 
Spitzer data, but so far they have spotted the signatures 
of a handful of ingredients, essentially the meat of comet 
soup. 

These solid ingredients include many standard comet 
components, such as silicates, or sand. And like any good 
recipe, there are also surprise ingredients, such as clay 
and chemicals in seashells called carbonates. These 
compounds were unexpected because they are thought to 
require liquid water to form. 

How did clay and carbonates form in frozen comets? asked 
Lisse. We don't know, but their presence may imply that 
the primordial solar system was thoroughly mixed together, 
allowing material formed near the Sun where water is 
liquid, and frozen material from out by Uranus and Neptune, 
to be included in the same body. 
 
Also found were chemicals never seen before in comets, such 
as iron-bearing compounds and aromatic hydrocarbons, found 
in barbecue pits and automobile exhaust on Earth. 

The silicates spotted by Spitzer are crystallized grains 
even smaller than sand, like crushed gems. One of these 
silicates is a mineral called olivine, found on the 
glimmering shores of Hawaii's Green Sands Beach.

Planets, comets and asteroids were all born out of a thick 
soup of chemicals that surrounded our young Sun about 4.5 
billion years ago. Because comets formed in the outer, 
chilly regions of our solar system, some of this early 
planetary material is still frozen inside them.

Having this new grocery list of comet ingredients means 
theoreticians can begin testing their models of planet 
formation. By plugging the chemicals into their formulas, 
they can assess what kinds of planets come out the other 
end. 

Now, we can stop guessing at what's inside comets, said 
Dr. Mike A'Hearn, principal investigator for the Deep 
Impact mission, University of Maryland, College Park. 
This information is invaluable for piecing together how 
our own planets as well as other distant worlds may have 
formed. 

NASA's Jet Propulsion Laboratory, Pasadena, Calif., 
manages the Spitzer Space Telescope mission for NASA's 
Science Mission Directorate, Washington. Science 
operations are conducted at the Spitzer Science Center 
at Caltech. The University of Maryland, College Park, 
conducted the overall mission management for Deep Impact, 
and JPL handled project management for the mission for 
NASA's Science Mission Directorate.

For more graphics and more information about Spitzer, 
visit 

http://www.spitzer.caltech.edu/Media/index.shtml .

For more information about Deep Impact, visit 

http://deepimpact.jpl.nasa.gov or 

http://www.nasa.gov/deepimpact .

For more information about NASA, visit 

http://www.nasa.gov/home/ .

  -end-

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RE: [meteorite-list] NWA 3160 Lithology

2005-09-07 Thread stan .
I have to concur - when i had my piece of this stuff at Al Lang's place to 
be cut I had it side by side with his piece of nwa 032 - looking at the 
basalt portion if you didnt know the olivine gabbro was a diffrent meteorite 
you would swear it was 032.


one awsome lunite is right




From: Adam Hupe [EMAIL PROTECTED]
To: meteorite-list@meteoritecentral.com
Subject: [meteorite-list] NWA 3160 Lithology
Date: Wed, 7 Sep 2005 12:32:06 -0700

Hi List,

Some have already asked about the major basalt lithology in NWA 3160.  We
listed pieces with single and dual lithologies,  NWA 3160 was over 90%
basalt and this image demonstrates how closely it looks like NWA 032/479:

http://cgi.ebay.com/NWA-3160-Olivine-Phyric-Mare-Basalt-Lunar-Meteorite_W0QQitemZ6559635438QQcategoryZ3239QQrdZ1QQcmdZViewItem

Check it out, this is one awesome lunaite.

Take Care,

Adam



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[meteorite-list] Ben Guerir TKW and TAW

2005-09-07 Thread Meteoryt.net
Hello
I want ask about TKW of Benguerir.
We know that many pieces of Ben Guerir was recovered by scientists from
Marrocan University/Museum.

From Met Bulletin:
TKW 25-30kg,
main mass, Oakes. Some other pieces are in the Moroccan CNRST

So my question is:
TKW contain only specimens collected by Maroccans + Oakes main mass or only
Maroccans or mayb its aproximatelly value of complete fall, including
specimens hidden in basement by local people and dealers ?

My next question is what is TAW (Total Available Weight) of this fall. How
many kilos from TKW is in market or/and dealers/collectors hands and how
many closed in Morocco museums ?

I know this should be difficult to answer, but Im just curious, and maybe we
can exchange some interesting informations.

-[ MARCIN CIMALA ]-[ I.M.C.A.#3667 ]-
http://www.Meteoryt.net [EMAIL PROTECTED]
http://www.PolandMET.com   [EMAIL PROTECTED]
http://www.Gao-Guenie.com  GSM +48(607)535 195
[ Member of Polish Meteoritical Society ]

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Re: [meteorite-list] Ben Guerir TKW and TAW

2005-09-07 Thread Jeff Grossman
Gee, I would define Total Available Weight as that material which is 
accessible and ready for use in scientific research.  This would include 
the pieces in Morocco museums, but not pieces in the hands of collectors.


Availability is a matter of perspective and access, which is different for 
different people.


Jeff

At 05:21 PM 9/7/2005, Meteoryt.net wrote:

Hello
I want ask about TKW of Benguerir.
We know that many pieces of Ben Guerir was recovered by scientists from
Marrocan University/Museum.

From Met Bulletin:
TKW 25-30kg,
main mass, Oakes. Some other pieces are in the Moroccan CNRST

So my question is:
TKW contain only specimens collected by Maroccans + Oakes main mass or only
Maroccans or mayb its aproximatelly value of complete fall, including
specimens hidden in basement by local people and dealers ?

My next question is what is TAW (Total Available Weight) of this fall. How
many kilos from TKW is in market or/and dealers/collectors hands and how
many closed in Morocco museums ?

I know this should be difficult to answer, but Im just curious, and maybe we
can exchange some interesting informations.

-[ MARCIN CIMALA ]-[ I.M.C.A.#3667 ]-
http://www.Meteoryt.net [EMAIL PROTECTED]
http://www.PolandMET.com   [EMAIL PROTECTED]
http://www.Gao-Guenie.com  GSM +48(607)535 195
[ Member of Polish Meteoritical Society ]

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[meteorite-list] Spirit Mars Rover Turns Astronomer

2005-09-07 Thread Ron Baalke

http://space.com/missionlaunches/050907_spirit_update.html

Night Moves: Spirit Mars Rover Turns Astronomer
By Leonard David 
space.com
07 September 2005

From its top of the world vantage point, Spirit has snagged images of
the two Mars moons - Phobos and Deimos. The robot is also assessing
weather features in the dark of the night on Mars. Other nighttime
duties are being discussed, such as charting meteor showers on the red
planet.

We're actually shunting some power during the daytime. So we'd much
rather use that power to do some science instead of shunting it out as
waste heat, said Jim Bell, an Associate Professor in the Cornell
University Astronomy Department in Ithaca, New York.

Bell is lead scientist for the Panoramic Camera color imaging system
carried by the dual Mars robots: Spirit and Opportunity.

Moons in view

Having so much power has allowed group controllers to task Spirit to
execute nighttime observing campaigns, Bell told SPACE.com.

While each rover is equipped with a Panoramic Camera - or PanCam - the
devices are not telescopes. Still, we can do some pretty good
astronomy, Bell said.

Spirit has been able to snap shots of both Phobos and Deimos together.
We're killing two birds with one stone by selecting times when those
two moons pass each other in the sky. That does frequently happen - 
every couple of nights, Bell said.

Bell said that, by taking the nighttime photos, a better understanding
of where those two moons are in their respective orbits becomes possible.

We're getting some good orbital refinement on the positions of the
satellites, Bell added. They haven't been monitored by astronomers
since the late 1980s.

In addition, by using color filters on Spirit, colors of the two martian
moons can be ascertained, Bell noted.

Weather service

Spirit has also gazed longingly up into nighttime sky for meteorological
purposes.

We're looking for any evidence of clouds forming at night, or fog, or
haze, Bell said. To do this job, nighttime shots are being taken using
the backdrop of stars - as well as Phobos and Deimos - to help pin down
atmospheric phenomena.

As the two moons slip by overhead, Spirit is getting a spectacular view.

Deimos looks pretty much like a star, far away. But Phobos is an eyeful,
Bell observed.

You can clearly see that Phobos is an oblong, potato-shaped object in
the sky. It's not as big as the full moon, but it is still pretty decent
in size, Bell said. A soon-to-be-released image will show features on
the surface of Phobos, he said, and this is with not much better than
human eye resolution!

In fact, Phobos is so close and large enough, a person standing on Mars,
within a few minutes, would notice the moon moving, Bell said.

Shower times

Thanks to the rover's power levels, Bell said that a proposal is being
made to use Spirit to observe meteor showers this fall.

Just like here on Earth, the red planet also sweeps through areas of
space laden with comet debris. Scientists want to evaluate the flux of
these small particles streaming into the martian atmosphere.

There are models that predict certain rates of meteors, and like on
Earth, there are shower times, Bell said. Spirit's nighttime powers
should help record that shower activity, he said.

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[meteorite-list] Water Detection at Gusev Crater Described

2005-09-07 Thread Ron Baalke


University Communications
Washington University in St. Louis
St. Louis, Missouri

Media Assistance:
Tony Fitzpatrick, Senior Science Editor
(314) 935-5272

Subject Matter Experts:
Raymond Arvidson, (314) 935-5609
Alian Wang, Senior research scientist, (314) 935-5671

Sept. 7, 2005

Water detection at Gusev crater described

Chemical proof for two wet scenarios

By Tony Fitzpatrick

A large team of NASA scientists, led by earth and planetary scientists at 
Washington University in St. Louis details the first solid set of evidence 
for water having existed on Mars at the Gusev crater, exploration site of 
the rover Spirit.

Using an array of sophisticated equipment on Spirit, Alian Wang, Ph.D., 
Washington University senior research scientist in earth and planetary 
sciences in Arts  Sciences, and the late Larry A. Haskin, Ph.D., Ralph E. 
Morrow Distinguished University Professor of earth and planetary sciences, 
found that the volcanic rocks at Gusev crater near Spirit's landing site 
were much like the olivine-rich basaltic rocks on Earth, and some of them 
possessed a coating rich in sulfur, bromine, chlorine and hematite, or 
oxidized iron. The team examined three rocks and found their most 
compelling evidence in a rock named Mazatzal.

The rock evidence indicates a scenario where water froze and melted at 
some point in Martian history, dissolving the sulfur, chlorine and bromine 
elements in the soil. The small amount of acidic fluids then react with 
the rocks buried in the soil and formed these highly oxidized coatings.

Trench-digging rover

During its traverse from landing site to Columbia Hills, the rover Spirit 
dug three trenches, allowing researchers to detect relatively high levels 
of magnesium sulfate comprising more than 20 percent of the regolith -- 
soil containing pieces of small rocks -- within one of the trenches, the 
Boroughs trench. The tight correlation between magnesium and sulfur 
indicates an open hydrologic system -- these ions had been carried by 
water to this site and deposited.

Spirit's fellow rover Opportunity earlier had detected a history of water 
at another site on Mars, Meridiani planum. This study (by Haskin et al.) 
covered the investigation of Spirit rover sols (a sol is a Martian day) 1 
through 156, with the major discoveries occurring after sol 80. After the 
findings were confirmed, Spirit traversed to the Columbian hills, where it 
found more evidence indicating water. The science team is currently 
planning for sol 551 operation of Spirit rover, which is only 55 meters 
away from the summit of Columbia Hills.

Spirit was on sol 597 on Sept 6 and on the summit of Husband Hill.

We will stay on the summit for a few weeks to finish our desired 
investigations, then go downhill to explore the south inner basin, 
especially the so-called 'home-plate,' which could be a feature of older 
rock or a filled-in crater, Wang said. We will name a major geo-feature 
in the basin after Larry.

Wang, Haskin, their WUSTL colleague Raymond E. Arvidson, chair of earth 
and planetary sciences, and James S. McDonnell Distinguished University 
Professor, and Bradley Jolliff, Ph.D., research associate professor in 
earth and planetary sciences, and more than two dozen collaborators from 
numerous institutions, reported their findings in the July 7, 2005 issue 
of Nature magazine (Larry A. Haskin et al. Nature 436, 66-69 (7 July 2005) 
doi:10.1038/nature03640). The paper was the last one that lead author 
Haskin, a highly regarded NASA veteran and former chair of earth and 
planetary sciences at WUSTL, submitted before his death on March 24, 2005.

Buried again and again

We looked closely at the multiple layers on top of the rock Mazatzal 
because it had a very different geochemistry and mineralogy, said Wang. 
This told us that the rock had been buried in the soil and exposed and 
then buried again several times over the history. There are chemical 
changes during the burial times and those changes show that the soil had 
been involved with water.

The telltale thing was a higher proportion of hematite in the coatings. 
We hadn't seen that in any previous Gusev rocks. Also, we saw very high 
chlorine in the coating and very high bromine levels inside the rock. The 
separation of the sulfur and chlorine tells us that the deposition of 
chlorine is affected by water.

While the multilayer coatings on rock Mazatzal indicates a temporal 
occurrence of low quantity water associated with freezing and melting of 
water, the sulfate deposition at trench sites indicates the involvement of 
a large body of water.

We examined the regolith at different depths within the Big Hole and the 
Boroughs trenches and saw an extremely tight correlation between magnesium 
and sulfur, which was not observed previously, Wang said. This tells us 
that magnesium sulfate formed in these trench regoliths. The increasing 
bromine concentration and the separation of chlorine from sulfur also 
suggests 

Re: [meteorite-list] Ben Guerir TKW and TAW

2005-09-07 Thread stan .


I think  you have it all backwards. institutions ALWAS have things that the 
colelcting public would give their eye teeth to get ahold of, making nearly 
anything in the hands of colelctors avalible to the
researchers if they want to go out and get it one way or the other... now 
what lab wants to do a study on a nice big 100 lbs nwa 869 and has a 100g 
nakhla individual laying around that they dont need? :)



Gee, I would define Total Available Weight as that material which is 
accessible and ready for use in scientific research.  This would include 
the pieces in Morocco museums, but not pieces in the hands of collectors.


Availability is a matter of perspective and access, which is different for 
different people.



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Re: [meteorite-list] Ben Guerir TKW and TAW

2005-09-07 Thread Jeff Grossman
No, I don't think so.  My point is that availability depends on who 
you are.  A typical scientist has neither a large (or any) meteorite 
collection nor a budget for purchasing specimens.  To him or her, 
privately owned meteorites are not directly available.  It's 
different for a researcher at a large museum, who has significant 
trading power and/or an acquisition budget.  In the same way a 
collector with a small collection has little trading power, so many 
museum specimens seem unavailable.  However, big-time dealers have 
the wherewithal to negotiate trades with museums for some very 
special meteorites not normally considered available.  For those 
collectors or scientists with the greatest resources, nearly 
everything is theoretically available except for objects of 
extraordinary significance.


So it's not a useful quantity, this TAW.  There's no way to define 
it unless you want to change the A to stand for Advertised.


jeff

At 08:56 PM 9/7/2005, stan . wrote:

I think  you have it all backwards. institutions ALWAS have things 
that the colelcting public would give their eye teeth to get ahold 
of, making nearly anything in the hands of colelctors avalible to the
researchers if they want to go out and get it one way or the 
other... now what lab wants to do a study on a nice big 100 lbs nwa 
869 and has a 100g nakhla individual laying around that they dont need? :)



Gee, I would define Total Available Weight as that material which 
is accessible and ready for use in scientific research.  This would 
include the pieces in Morocco museums, but not pieces in the hands 
of collectors.


Availability is a matter of perspective and access, which is 
different for different people.



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[meteorite-list] From McCarthy Taylor: What is this rock?

2005-09-07 Thread Impactika
McCarthy is having troubles posting to the List so he has asked me to  
forward this. 
He really would like some opinions on this  rock
Thanks.
---

This  post is not an offical Field Trip Report but a request to help   
identify a suspect rock found from my latest trip. 
 
The trip recovered 4 stones, 2 of which are meteorites, 1 which I   
thought was till I cut it open and its the topic of this posting, and  a  
fourth that is probably a mesosider-wrong, but tested positive  for  
nickel and will be sent to a lab soon. 
 
The stone in question is found in the Plainview strewnfield, attracts   
a magnet well, and has metal flakes.  Hence, I acquired it from  the  
finder.  Once I cut it open I found no chrondrules and white  matrix.  
Also, I found tiny bubbles here and there. 
 
Does anyone recognize it or seen anything like it?  Any ideas what it  
is?  Meteorwrong?  
 
_www.westernwelltool.com/Labor_day_trip_05/05-003.jpg_ 
(http://www.westernwelltool.com/Labor_day_trip_05/05-003.jpg)  
 
A good view of the metal pattern: 
_http://www.westernwelltool.com/Labor_day_trip_05/05-003-2.jpg_ 
(http://www.westernwelltool.com/Labor_day_trip_05/05-003-2.jpg) 
 

A veiw of matrix and the small bubbles: 
_http://www.westernwelltool.com/Labor_day_trip_05/05-003-3.jpg_ 
(http://www.westernwelltool.com/Labor_day_trip_05/05-003-3.jpg)  
 
The original main mass: 
_http://www.westernwelltool.com/Labor_day_trip_05/05-003-5.jpg_ 
(http://www.westernwelltool.com/Labor_day_trip_05/05-003-5.jpg)  
 
--   
McCartneyTaylor, IMCA 2760
--
--


Anne M.  Black
www.IMPACTIKA.com
[EMAIL PROTECTED]
President, I.M.C.A.  Inc.
www.IMCA.cc
 
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[meteorite-list] Ensisheim photos

2005-09-07 Thread vincent stelluti
There are some photos of Ensisheim show taken by Jean-Michel a french 
collectionneur


http://jmdaillier.free.fr/ENSISHEIM%202005%20POUR%20LE%20NET/page_01.htm

Vincent 


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[meteorite-list] Tokyo TIMA show photos---can someone help host them?

2005-09-07 Thread drtanuki
Dear List,
  I have photos of the dealers at the Tokyo TIMA show
that was held in June.  If someone is willing to host
them for the list to see I will provide them.  Thank
you.  Dirk Ross...Tokyo

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[meteorite-list] Meteorite Raffle Update, Wednesday

2005-09-07 Thread Notkin

Dear Friends and Listees:

I am delighted and slightly stunned to be able to report that, as of 
today, you have raised over $4,300 for our Katrina relief fund. Ticket 
sales notifications have been coming in here all day, and it's been 
very nice to hear from some old friends, via email.


In addition to donations from all over the USA, we have received ticket 
purchases and donations from our friends in:


Argentina
Austria
Canada
Germany
Mexico
New Zealand
Poland

(sorry if I accidentally left out a whole country, I'm a little tired)

I am confirming all ticket purchases, personally by email, but this 
taking quite a while, so please bear with me if you haven't heard from 
me regarding your purchases and/or general questions. I am a full day 
behind, even though I went through 100+ emails today.


We have received some more great prizes, which I will try to add to the 
site tomorrow. I heard from Blaine Reed by phone today, and he is very 
generously donating a 5.8 gram fragment of the New Orleans meteorite. 
We also have items coming in from Geoff Cintron, Fred Hall, Martin 
Horejsi, Rob Matson, Rob Reisener, and others.


Anne Black will be leaving a copy of Meteorites A to Z in Blaine's 
room during the Denver Show. All members of the meteorite community 
attending the show are being asked to sign that book, and it will also 
be one of the prizes.


In related news: Tucson has received its first group of displaced 
persons from the Gulf states (89 survivors today), with more expected, 
so we are waiting to see what can be done in terms of volunteering to 
help these people in person.


It's going to be one exciting night in Denver on September 17. I hope 
to see MANY of you at the La Loma party, hosted by the mighty Denver 
COMETS.


Thanks for everything you've done to make this happen.


Sincerely,

Geoff Notkin
2005 Meteorite Community Charity Raffle
http://www.aerolite.org/meteorite-raffle.htm

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