[meteorite-list] Rocks from Space Picture of the Day - September 25, 2008

2008-09-25 Thread SPACEROCKSINC
http://www.rocksfromspace.org/September_25_2008.html 




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[meteorite-list] ESAs artificial meteorite probes panspermia

2008-09-25 Thread Jan Hattenbach
Hello list,

an artificial meteorite shows that sedimentary martian soil could reach earth, 
but possible microbes would get killed by the atmosferic flight:

http://www.europlanet-eu.org/demo/index.php?option=com_contenttask=viewid=123Itemid=41

Regards,

Jan
-- 
Das Universum expandiert? Komisch, ich finde immer seltener einem Parkplatz! 
(Harald Lesch)

Ist Ihr Browser Vista-kompatibel? Jetzt die neuesten 
Browser-Versionen downloaden: http://www.gmx.net/de/go/browser
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[meteorite-list] AD - Ebay Auctions ending

2008-09-25 Thread Jim Strope

Good Morning List Members

I have auctions ending tonight catchafallingstar.com.  All started at 99
Cents!!!:

There are some nice planetaries as well as our Meteorite Medals still at low
prices,

http://members.ebay.com/ws/eBayISAPI.dll?ViewUserPageuserid=catchafallingstar.com

Full recap with photos on Paul and Jim's website:
http://www.meteorite.com/meteorites/ebay/catch_a_falling_star_meteorites.htm

Thanks for looking 

Jim Strope
421 Fourth Street
Glen Dale, WV  26038

http://www.catchafallingstar.com


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[meteorite-list] (AD) MILLBILLILLIE 53 gram forsale

2008-09-25 Thread steve arnold
Hi list.I need to raise some money so I am putting up my 53 gram millbillillie 
stone meteorite up forsale.$500 takes it home.I will also pay for shipping.But 
please NO PAYPAL!!I will accept either private checks,cash,money order,or 
cashiers check or western union for my non usa customers.This is 100% fusion 
crusted not a mark on it and has flowlines and all the original red and black 
patina.Thanks and offlist please.

Steve R.Arnold,Chicago!  http://chicagometeorites.net/


  
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Re: [meteorite-list] Worlds in Collision

2008-09-25 Thread Sean T. Murray

Great picture for this on APOD:
http://antwrp.gsfc.nasa.gov/apod/astropix.html

- Original Message - 
From: Darren Garrison [EMAIL PROTECTED]

To: Meteorite Mailing List meteorite-list@meteoritecentral.com
Sent: Thursday, September 25, 2008 1:04 AM
Subject: [meteorite-list] Worlds in Collision


http://www.foxnews.com/story/0,2933,427023,00.html

Huge Planetary Collision Left Tons of Space Debris

Around a distant star, two planets similar to Earth collided and were 
destroyed,

astronomers said today.

The somewhat speculative scenario is based on the leftovers: a ring of 
debris

around the star that includes a million times more dust than now circles our
sun.

It's as if Earth and Venus collided, said researcher Benjamin Zuckerman, 
UCLA
professor of physics and astronomy. Astronomers have never seen anything 
like
this before. Apparently, major catastrophic collisions can take place in a 
fully

mature planetary system.

The researchers used X-ray data and other observations of a star called 
BD+20
307. They had assumed it was a young star, just a few hundred million years 
old,

and the debris was leftovers from planet formation.

But earlier this year, another study showed the star was actually a binary 
pair,

and that the stars were billions of years old.

So why all the debris? The dust is about the same distance from the stellar 
pair
as Earth is from the sun, and given current theories of planet formation, 
that
debris should have been swept up into planets by now or pushed away by 
stellar

radiation. It simply shouldn't be there.

A colossal collision must have created all that dust sometime in the past 
few
hundred thousand years and perhaps much more recently, the astronomers 
figure.


It would have been a whopper.

If any life was present on either planet, the massive collision would have
wiped out everything in a matter of minutes - the ultimate extinction 
event,
said Gregory Henry, an astronomer at Tennessee State University (TSU) who 
worked

with Zuckerman on the research. A massive disk of infrared-emitting dust
circling the star provides silent testimony to this sad fate.

To put the collision into context, Zuckerman said: By contrast with the 
massive

crash in the BD+20 307 system, the collision of an asteroid with Earth 65
million years ago, the most favored explanation for the final demise of the
dinosaurs, was a mere pipsqueak.

The work was funded by the National Science Foundation and NASA, and also by 
TSU

and the State of Tennessee. It will be detailed in the December issue of the
Astrophysical Journal.

The conclusion has the astronomers thinking about home.

This poses two very interesting questions, said TSU astronomer Francis 
Fekel.
How do planetary orbits become destabilized in such an old, mature system, 
and

could such a collision happen in our own solar system?

It has already happened here, in fact. Our moon is thought to have been 
created

when a Mars-sized object slammed into Earth.

Henry points out that computer models done by other researchers suggest that 
as
planets in our solar system migrate over time, there is a small probability 
for
collisions of Mercury with Earth or Venus sometime in the next billion years 
or

more.

Of course by then the sun will have expanded and we might be toast anyway.
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Re: [meteorite-list] (AD) MILLBILLILLIE 53 gram forsale

2008-09-25 Thread Matthias Bärmann
How many AD's we've had from this address this week? Chergach? Gao? Now 
Millie? Don't know ...


Matthias

- Original Message - 
From: steve arnold [EMAIL PROTECTED]

To: meteorite-list@meteoritecentral.com
Sent: Thursday, September 25, 2008 2:44 PM
Subject: [meteorite-list] (AD) MILLBILLILLIE 53 gram forsale


Hi list.I need to raise some money so I am putting up my 53 gram 
millbillillie stone meteorite up forsale.$500 takes it home.I will also 
pay for shipping.But please NO PAYPAL!!I will accept either private 
checks,cash,money order,or cashiers check or western union for my non usa 
customers.This is 100% fusion crusted not a mark on it and has flowlines 
and all the original red and black patina.Thanks and offlist please.


Steve R.Arnold,Chicago!  http://chicagometeorites.net/



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[meteorite-list] WANTED : Meteorite Pendant

2008-09-25 Thread Michael Gilmer
Hi folks!

I am looking to purchase a meteorite pendant - either the NWA 869 heart-shaped 
pendant, one of the
interesting looking carved NWA 869 beads (preferred), or an etched iron 
pendant (like Gibeon).

I do not want any of the wire-wrapped pendants or oft-seen Campo pendants.

My wife's birthday is coming up and I want to give her something meteoritic in 
addition to the usual gift
fare.  I have been bidding on these pendants on eBay for a week now and I keep 
losing the auction every
time - because the price gets too high for my budget or I forget to watch the 
auction and it closes while I
am out lollygagging.

If you have one of these to part with, email me with your price shipped to 
zipcode 70360 via Priority Mail.

I can pay via PayPal.

Thanks and clear skies!

MikeG


.
Michael Gilmer (Louisiana, USA)
Member of the Meteoritical Society.
Member of the Bayou Region Stargazers Network.
Websites - http://www.galactic-stone.com and http://www.glassthrower.com
MySpace - http://www.myspace.com/fine_meteorites_4_sale
..



  
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Re: [meteorite-list] ESAs artificial meteorite probes panspermia

2008-09-25 Thread Darren Garrison
On Thu, 25 Sep 2008 11:40:22 +0200, you wrote:

Hello list,

an artificial meteorite shows that sedimentary martian soil could reach earth, 
but possible microbes would get killed by the atmosferic flight:

http://www.europlanet-eu.org/demo/index.php?option=com_contenttask=viewid=123Itemid=41

The more interesting part of the experiment, to me, is the production of creamy
white fusion crusts.  Wonder how many Martian sedementary meteorites (and old
Earthites) have been passed over in the deserts because they were the wrong
color?

http://www.sciencedaily.com/releases/2008/09/080925083252.htm
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[meteorite-list] MRO HiRISE Images - September 24, 2008

2008-09-25 Thread Ron Baalke


MARS RECONNAISSANCE ORBITER HIRISE IMAGES
September 24, 2008

o Clusters of Mounds at Acidalia Planitia
  http://hirise.lpl.arizona.edu/PSP_009485_2185

o Outcrops in Aurorae Chaos 
  http://hirise.lpl.arizona.edu/PSP_009498_1730

o Tube-Fed Lava Flow Field 
  http://hirise.lpl.arizona.edu/PSP_009501_1755

o Dark Spot Near Olmpus Mons Volcano
  http://hirise.lpl.arizona.edu/PSP_009502_1980


All of the HiRISE images are archived here:

http://hirise.lpl.arizona.edu/

Information about the Mars Reconnaissance Orbiter is 
online at http://www.nasa.gov/mro. The mission is 
managed by NASA's Jet Propulsion Laboratory, a division 
of the California Institute of Technology, for the NASA 
Science Mission Directorate, Washington, D.C. Lockheed 
Martin Space Systems, of Denver, is the prime contractor 
and built the spacecraft. HiRISE is operated by the 
University of Arizona. Ball Aerospace and Technologies 
Corp., of Boulder, Colo., built the HiRISE instrument.
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Re: [meteorite-list] ESAs artificial meteorite probes panspermia

2008-09-25 Thread Michael Murray
Wasn't there a lady professor that wrote an article a while back on  
the possibility of there being atypical appearing meteorites and we  
might be overlooking them?  I realize that is somewhat of a wide-open  
question but to possibly narrow it down a bit, the name Prof. C.  
Floss seems to come to mind in my remembering this article.  Seems  
like it had to do with mantle or lack of meteorites from a certain  
layer, or something similar.  Anyone else remember this article?  I'd  
like to read it again if I could come up with the link.

Mike

On Sep 25, 2008, at 9:05 AM, Darren Garrison wrote:


On Thu, 25 Sep 2008 11:40:22 +0200, you wrote:


Hello list,

an artificial meteorite shows that sedimentary martian soil could  
reach earth, but possible microbes would get killed by the  
atmosferic flight:


http://www.europlanet-eu.org/demo/index.php? 
option=com_contenttask=viewid=123Itemid=41


The more interesting part of the experiment, to me, is the  
production of creamy
white fusion crusts.  Wonder how many Martian sedementary  
meteorites (and old
Earthites) have been passed over in the deserts because they were  
the wrong

color?

http://www.sciencedaily.com/releases/2008/09/080925083252.htm
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[meteorite-list] AD: Semi-Famous Meteorites For Sale

2008-09-25 Thread Ruben Garcia
Hi all,
I have a few Semi-Famous Meteorites for sale. 

Take a look and email me of list.

http://www.mr-meteorite.com/famousmeteorites4sale.htm

Ruben Garcia
Phoenix, Arizona
http://www.mr-meteorite.com
http://www.youtube.com/profile_videos?user=meteorfrightp=v


  
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[meteorite-list] MRO Reveals Rock Fracture Plumbing On Mars

2008-09-25 Thread Ron Baalke


Sept. 25, 2008

Dwayne Brown 
Headquarters, Washington 
202-358-1726 
[EMAIL PROTECTED] 

Guy Webster 
Jet Propulsion Laboratory, Pasadena, Calif. 
818-354-6278 
[EMAIL PROTECTED] 

Lori Stiles 
University of Arizona, Tucson 
520-626-4402 
[EMAIL PROTECTED] 

RELEASE: 08-244

NASA ORBITER REVEALS ROCK FRACTURE PLUMBING ON MARS

PASADENA, Calif. -- NASA's Mars Reconnaissance Orbiter has revealed 
hundreds of small fractures exposed on the Martian surface that 
billions of years ago directed flows of water through underground 
Martian sandstone. 

Researchers used images from the spacecraft's High Resolution Imaging 
Science Experiment, or HiRISE, camera. Images of layered rock 
deposits at equatorial Martian sites show the clusters of fractures 
to be a type called deformation bands, caused by stresses below the 
surface in granular or porous bedrock. 

Groundwater often flows along fractures such as these, and knowing 
that these are deformation bands helps us understand how the 
underground plumbing may have worked within these layered deposits, 
said Chris Okubo of the U.S. Geological Survey in Flagstaff, Ariz. 

Visible effects of water on the color and texture of rock along the 
fractures provide evidence that groundwater flowed extensively along 
the fractures. 

These structures are important sites for future exploration and 
investigations into the geological history of water and water-related 
processes on Mars, Okubo and co-authors state in a report published 
online this month in the Geological Society of America Bulletin. 

Deformation band clusters in Utah sandstones, as on Mars, are a few 
yards wide and up to a few miles long. They form from either 
compression or stretching of underground layers, and can be 
precursors to faults. The ones visible at the surface have become 
exposed as overlying layers erode away. Deformation bands and faults 
can strongly influence the movement of groundwater on Earth and 
appear to have been similarly important on Mars, according to this 
study. 

This study provides a picture of not just surface water erosion but 
true groundwater effects widely distributed over the planet, said 
Suzanne Smrekar, deputy project scientist for the Mars Reconnaissance 
Orbiter at NASA's Jet Propulsion Laboratory in Pasadena, Calif. 
Ground water movement has important implications for how the 
temperature and chemistry of the crust have changed over time, which 
in turn affects the potential for habitats for past life. 

The recent study focuses on layered deposits in Mars' Capen crater, 
approximately 43 miles in diameter and 7 degrees north of the 
equator. This formerly unnamed crater became notable due to this 
discovery of deformation bands within it and was recently assigned a 
formal name. The crater was named for the late Charles Capen, who 
studied Mars and other objects as an astronomer at JPL's Table 
Mountain Observatory in southern California and at Lowell 
Observatory, Flagstaff, Ariz. 

The HiRISE camera is one of six science instruments on the orbiter. It 
can reveal smaller details on the surface than any previous camera to 
orbit Mars. The orbiter reached Mars in March 2006 and has returned 
more data than all other current and past missions to Mars combined. 

The mission is managed by JPL for NASA's Science Mission Directorate. 
Lockheed Martin Space Systems of Denver built the spacecraft. The 
University of Arizona operates the HiRISE camera, built by Ball 
Aerospace and Technology Corp. of Boulder, Colo. 

Images of the deformation band clusters and additional information 
about the mission are on the Internet at: 



http://www.nasa.gov/mro 


For more information about NASA and agency programs, visit: 



http://www.nasa.gov 


-end-

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[meteorite-list] Artificial Meteorite Shows Martian Impactors May Carry Traces of Life

2008-09-25 Thread Ron Baalke

http://www.thaindian.com/newsportal/india-news/artificial-meteorite-shows-martian-impactors-may-carry-traces-of-life_10099727.html

Artificial meteorite shows Martian impactors may carry traces of life
Thaindian News
September 25, 2008

Berlin, September 25 (ANI): An artificial meteorite designed by the
European Space Agency (ESA) has shown that traces of life in a Martian
meteorite could survive the violent heat and shock of entry into the
Earth's atmosphere.

The experiment's results also suggest that meteorite hunters should
widen their search to include white rocks if they want to find traces of
life in Martian meteorites.

The STONE-6 experiment tested whether sedimentary rock samples could
withstand the extreme conditions during a descent though the Earth's
atmosphere where temperatures reached at least 1700 degrees Celsius.
After landing, the samples were transported in protective holders to a
laboratory clean-room at ESTEC (European Space Research and Technology
Centre) and examined to see if any traces of life remained.
Recent missions have gathered compelling evidence for water and
sediments on early Mars. Potential traces of Martian life are more
likely to be found in sediments that have been formed in water.
However, although about 39 known meteorites from Mars have been
identified, all are basaltic rock-types and no sedimentary meteorites
have been found to date.

According to Dr Westall, The STONE-6 experiment shows that sedimentary
martian meteorites could reach Earth. The fact that we haven't found any
to date could mean that we need to change the way we hunt for meteorites.

In this experiment, we found that the sedimentary rocks developed a
white crust or none at all. That means that we need to expand our search
to white or light-coloured rocks, he added.

The STONE-6 experiment was mounted on a FOTON M3 capsule that was
launched from Baikonur on 14th September 2007.

Two samples of terrestrial sedimentary rock and a control sample of
basalt were fixed to the heat-shield of the return capsule, which
re-entered the atmosphere on 26th September after 12 days in orbit.
The basalt was lost during re-entry.

However, a sample of 3.5 billion year old volcanic sand containing
carbonaceous microfossils and a 370 million year sample of mudstone from
the Orkney Islands containing chemical biomarkers both survived.
On examination at ESTEC, the 3.5 billion year old sample of sand from
Pilbara in Australia was found to have formed a half-millimetre thick
fusion crust that was creamy white in colour.

About half the rock had ablated but the microfossils and carbon survived
at depth in the sample. Approximately 30 percent of the other sediment,
a lacustrine sand from the Orkney Islands, also survived, as did some of
the biomolecules.

The rocks also transported living organisms, a type of bacteria called
Chroococcidiopsis, on the back of the rocks, away from the exposed edge.
The STONE-6 experiment suggests that, if Martian sedimentary meteorites
carry traces of past life, these traces could be safely transported to
Earth, said Dr Westall. 
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[meteorite-list] The Fallen 'Star' of Hoba (Hoba Meteorite)

2008-09-25 Thread Ron Baalke

http://www.newera.com.na/page.php?id=9350

The Fallen 'Star' of Hoba
By Chrispin Inambao
New Era
September 25, 2008

Fifty-seven kilometres east of the B-1 road between Otavi and
Grootfontein is a turn-off from where a serpentine dusty road leads to a
cluster of fertile commercial farms.

From the turn-off one would have to endure a 24-km drive along a bumpy
road that traverses several maize fields and fertile cattle ranches that
economically sustain the maize triangle to reach one particular farm
that possesses a heritage of global significance.

Hoba Farm is of global significance in that the largest single piece of
?cosmic dust? to have fallen anywhere on earth from the sky lies several
metres embedded in its surface.

This meteorite of considerable importance to scientists is a favoured
tourist destination.

Weighing in excess of 60 tonnes and discovered in 1920 Hoba Meteorite is
said to have landed on earth over 80 000 years ago and is one of the
reasons tourists flock to Namibia.

Multitudes of visitors from America, Germany, Italy, Britain, France and
South Africa, among other countries, toting expensive digital cameras
are drawn to this metallic stone slab that was discovered through a
chance event by a farmer with an ox-drawn plough.

Had it not been for this maize farmer, no one would know that beneath
Namibia?s surface is buried the largest known meteorite in the world for
there is no crater in that area.

This meteorite is unusual in that it is flat on both major surfaces
possibly causing it to have skipped across the top of the atmosphere in
a way a flat stone skips on water.

Adelheid Garises and her husband Ambrosius Gariseb are part of a team of
people ensuring this national treasure listed among the National
Monuments is protected from vandals.

In fact, it was declared a national monument on March 15, 1955 and in
1985 Rössing Uranium Ltd availed funds so that additional protection
could be taken against vandals.

A portion of these funds was utilised to make the site more attractive
to tourists.

In 1987 Jan Engelbrecht the owner of Hoba West donated the meteorite and
the site where it lies to the State for educational purposes. Later that
year a tourist centre was opened at the site. Because of these
developments, vandalism has ceased and thousands of both local and
domestic tourists visit this breath-taking site year in and year out.

Previously souvenir-hunters had hacked some pieces of this priceless
treasure.

In the 50s ISCOR a South African steel company, made an offer to buy the
whole stone for a million pounds that at that time was a staggering amount.

In astronomical terms Hoba Meteorite is no more than a 'speck of cosmic
dust' though on a more modest human scale, this rock is both the largest
and heaviest meteorite on earth.

It is worth noting the speed at which these meteorites travel by far
eclipses that of bullets.

Garises said the meteorite is located 24 km from Grootfontein and that
it attracts anything from 24 to 80 tourists everyday but that the number
could even be higher and groups of school-children undertake guided
tours to see this strange-looking metallic stone slab.

Geologists from far and wide also travel to this area to scientifically
probe this stone.

Comprising 84 percent iron and 16 percent nickel this slab will continue
being a major tourist attraction in years to come.

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[meteorite-list] NASA Identifies Carbon-rich Molecules in Meteors as the 'Origin of Life'

2008-09-25 Thread Ron Baalke

http://www.nasa.gov/centers/ames/research/2008/Origins_of_life_research.html

NASA Identifies Carbon-rich Molecules in Meteors as the 'Origin of Life'
September 24, 2008
 
Tons, perhaps tens of tons, of carbon molecules in dust particles and
meteorites fall on Earth daily. Meteorites are especially valuable to
astronomers because they provide relatively big chunks of carbon
molecules that are easily analyzed in the laboratory. In the past few
years, researchers have noticed that most meteorite carbon are molecules
called polycyclic aromatic hydrocarbons (PAHs), which are very stable
compounds and are survivors.

PAHs are the most common carbon-rich compound in the universe. They are
found in everything from distant galaxies to charbroiled hamburgers and
engine soot. When they are first formed, or found in space, their
structures resemble pieces of chicken wire, fused six-sided rings.
However, when found in meteorites, these aromatic rings are carrying
extra hydrogen or oxygen.

Scientists at NASA Ames Research Center, Moffett Field, Calif. performed
laboratory experiments that explain the process by which these
meteoritic hydrocarbons attract the extra hydrogen and oxygen. They are
very similar to the molecules identified as evidence of alien microbes
in an earlier Science paper (McKay et al 1996).

“Our findings are important because it is the first time anybody
explained these carbon-rich molecules found in meteorites. They are
similar to the molecules that make-up living things,” said Max
Bernstein, a space scientist at NASA Ames.

As it happened, their findings were judged significant enough to be
award-winning. Published in Science (1999) by Bernstein and fellow NASA
Ames scientists Scott Sanford and Louis Allamandola, their paper won the
2008 H. Julian Allen Award at NASA Ames Research Center.

It takes a long time for scientific papers to win awards.

As scientists, we like to quantify things. Scientific papers are judged
by the number of times they are cited in other scientific papers. Other
scientists need to say that I couldn't have written my paper without
your paper. Often it takes a few years, Bernstein explained.

These carbon-rich molecules are produced by carbon-rich, dying, giant
red stars. When they are first formed, astronomers observe them as
normal PAHs. However, when they are seen in meteorites billions of years
later, they almost always have oxygen or heavy hydrogen attached to
them. (Heavy hydrogen carries an extra neutron, and is called a
deuterium isotope.) Something happened to change them, say scientists.

To study the process by which these carbon compounds change, the Ames
Astrochemistry Laboratory studied PAHs in water ices that were exposed
to ultraviolet radiation under space-like conditions. Scientists
reproduced conditions including an incredibly high vacuum, extremely low
temperatures (- 340 degrees Fahrenheit), and harsh radiation. When the
extremely cold temperature was reached, these PAHs were exposed to
ultraviolet radiation, and they changed. The experiment successfully
reproduced the hydrocarbons found in meteorites. For the first time,
scientists were able to show how hydrogen was exchanged for deuterium,
or heavy hydrogen.

It turns out, you only need water ice and radiation to change these
molecules, said Bernstein.

Using infrared spectroscopy, the Ames research team proved that the
laboratory-produced hydrocarbons were the same hydrocarbons found in
meteorites and observed through telescopes. Scientists observed the
chemical reaction in a stainless steel chamber as it was happening. The
laboratory sample reflected the same infrared colors as the hydrocarbons
seen by astronomers using telescopes. Because the techniques used were
the same, the results were directly comparable. We were seeing the same
molecules from telescopes as were reproduced in the laboratory, said
Sandford.

Once the molecular-size laboratory sample was retrieved, it was taken to
Richard Zare's laboratory at Stanford University, where researchers
weighed the individual molecules. Findings showed that ices, modified by
radiation, created new molecules.

These molecules, called quinones, received considerable attention by the
astrobiology community because they are common to all life forms. They
are potentially significant for the origin of life or the habitability
of planets. How does a planet become habitable?

Molecules from space helped to make the Earth the pleasant place that
it is today, said Allamandola, founder of the Ames Astrochemistry
Laboratory.

Our findings were new because we showed how these molecules formed. It
was already known that these molecules were in meteorites and delivered
to the planets, said Bernstein.

We now understand why these life-like carbon compounds are raining down
on the Earth and other planets. Knowing this will help us search for
life on other worlds by distinguishing these molecules from biomarkers,
said Bernstein.

For further information, 

[meteorite-list] NASA Astronomers Compare Meteors to Spacecraft Re-entry (Jules Verne Reentry)

2008-09-25 Thread Ron Baalke

http://www.nasa.gov/centers/ames/news/releases/2008/08_84AR.html

Rachel Prucey
Ames Research Center, Moffett Field, Calif.
650-604-0643
[EMAIL PROTECTED] mailto: [EMAIL PROTECTED]

Michael Braukus
NASA Headquarters, Washington
202-358-1979
[EMAIL PROTECTED] mailto:[EMAIL PROTECTED]

Clare Mattok
European Space Agency, Paris
33-1-5369-7412
[EMAIL PROTECTED] mailto:[EMAIL PROTECTED]
Sept. 24, 2008
 
MEDIA ADVISORY : 08_84AR
 
NASA Astronomers Compare Meteors to Spacecraft Re-entry
 
MOFFETT FIELD, Calif. -- A group of astronomers from NASA, the European
Space Agency (ESA) and other institutions will take to the skies to
observe the re-entry of ESA's Jules Verne Automated Transfer Vehicle
(ATV) as it falls back to Earth from the International Space Station on
Sept. 29, 2008.

An Ames research aircraft will take off from Moffett Field, Calif., and
a Douglas DC-8 airborne laboratory will depart from NASA's Dryden
Aircraft Operations Facility at Palmdale, Calif., on Friday, Sept. 26,
2008 to fly more than 30 scientists and their instruments over the South
Pacific Ocean in ideal and virtually unchanging conditions far above
light pollution and clouds.

NASA's primary goal during the lengthy airborne mission is to study the
re-entry and fragmentation of ESA's Jules Verne ATV spacecraft to gain
insight and find similarities to meteor fragmentation. This observation
campaign is similar to the January 2006 Stardust and September 2004
Genesis spacecraft re-entry airborne campaigns, in which NASA scientists
studied the levels of radiation, light and out-gassing of the descending
spacecraft, to better understand meteor radiation mechanisms.

Another goal is to validate the computer models astronomers use to
predict how an object will fragment and disperse as it enters Earth's
atmosphere. NASA astronomers made similar airborne studies for the
January 2008 Quadrantid and September 2007 Aurigid meteor showers to
determine when they peaked and how they were formed.

Peter Jenniskens, the observation campaign principal investigator, at
NASA Ames Research Center and the SETI Institute, Mountain View, Calif.,
and Dave Jordan, observation campaign project manager, at NASA Ames will
be available for telephone interviews, 1 p.m. to 4 p.m. PDT, Thursday,
Sept. 25, 2008. To schedule an interview please contact Rachel Prucey,
public affairs specialist, at 650-604-0643.

For more information on NASA and its programs, visit:

http://www.nasa.gov

For more information about the “Jules Verne” airborne observation
campaign, visit:

http://atv.seti.org/
 

- end -
 
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Re: [meteorite-list] AD: Semi-Famous Meteorites For Sale

2008-09-25 Thread Adam Hupe
Hi Ruben and other List members,

I would be careful about selling California meteorites found on BLM land.  I 
was told by the BLM that it is illegal to collect meteorites in California on 
federal lands for comercial purposes. I thought you were involved with some of 
these warnings.  They do monitor eBay and Google. I have been sternly warned 
about selling meteorites found on California dry lake beds.  I donated the 
Ransburg iron Main Mass becuase of such warnings.

Best Regards,

Adam



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[meteorite-list] NASA Stardust Capsule To Go On Display At Smithsonian

2008-09-25 Thread Ron Baalke


Sept. 25, 2008

Dwayne Brown 
Headquarters, Washington 
202-358-1726 
[EMAIL PROTECTED] 

William P. Jeffs 
Johnson Space Center, Houston 
281-483-5111 
[EMAIL PROTECTED] 

D.C. Agle 
Jet Propulsion Laboratory, Pasadena, Calif. 
818-393-9011 
[EMAIL PROTECTED] 

RELEASE: 08-245

NASA STARDUST CAPSULE TO GO ON DISPLAY AT SMITHSONIAN

WASHINGTON -- Having returned the world's first particles from a 
comet, NASA's Stardust sample return capsule will join the collection 
of flight icons in the Smithsonian's National Air and Space Museum in 
Washington. The capsule will go on public display in the museum's 
Milestones of Flight Gallery on Oct. 1, the 50th anniversary of NASA. 

Stardust, comprising a spacecraft and capsule, completed a seven-year, 
3-billion-mile journey in 2006. A tennis racket-like, aerogel-lined 
collector was extended to capture particles as the spacecraft flew 
within 150 miles of comet Wild 2 in January 2004. Carrying the 
collected particles, the capsule returned to Earth Jan. 15, 2006, 
landing in Utah. Two days later, it was transported to a curatorial 
facility at NASA's Johnson Space Center in Houston. 

Very few people get to build something, launch it into space, see it 
be successful and then get it back in their hands, said Karen 
McNamara, Johnson recovery lead for the Stardust mission. To be able 
to share this with the public is phenomenal. 

The capsule joins the Wright brothers' 1903 Flyer, Charles Lindbergh's 
Spirit of St. Louis and the Apollo 11 command module Columbia that 
carried the first men to walk on the moon. 

The Smithsonian Institution's National Air and Space Museum is 
delighted to add to the National Collection the Stardust return 
capsule, said Roger Launius, senior curator of the Division of Space 
History at the museum. As one of the premier space science missions 
of the recent past, Stardust will take its place alongside other 
iconic objects from the history of air and spaceflight. I look 
forward to helping to impart more knowledge to our visitors about the 
makeup of the universe using this significant and path breaking 
object. 

Hardware provided to the Smithsonian includes actual flight 
components. Elements relevant to the science goals of the mission 
remain with NASA. 

After successfully completing its mission, Stardust will use its 
flight-proven hardware to perform a new, previously unplanned 
investigation. The mission, called Stardust-NExT, will revisit comet 
9P/Tempel 1. This investigation will provide the first look at the 
changes to a comet nucleus produced after a close approach to the 
sun. It also will mark the first time a comet ever has been 
revisited. 

Usually, when a piece of your spacecraft goes into the Smithsonian 
that means the mission's over, said Stardust-NExT project manager 
Rick Grammier, of NASA's Jet Propulsion Laboratory in Pasadena, 
Calif. But the Stardust spacecraft is still doing the job for NASA 
and in February 2011, it will fly within 120 miles of the comet. 

Stardust is a low-cost, Discovery Program mission for NASA's Science 
Mission Directorate. The Jet Propulsion Laboratory manages the 
project. Joseph Veverka of Cornell University in Ithaca, N.Y., is the 
mission's principal investigator. Lockheed Martin Space Systems of 
Denver manages mission operations. 

For information about the Stardust mission on the Web, visit: 

http://www.nasa.gov/stardust 

Images of the Stardust capsule being prepared for shipment can be 
found at: 

http://www.nasa.gov/centers/johnson/home/stardust.html 


NASA Television will air Video File material to illustrate this story. 
For NASA TV downlink, schedule and streaming video information, 
visit: 

http://www.nasa.gov/ntv 


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[meteorite-list] Fireball over Ohio

2008-09-25 Thread Charley
Hi List,

This morning, while driving to work, I saw a beautiful green fireball.

Here are the details:

Time: 6:23 a.m. ET
My location: 40 deg, 25', 2.35 N  , 82 deg, 46', 30.67 W  (per Google 
Earth)
I was westbound on Ohio 229 about 1 mile east of Marengo when I saw the 
fireball. The road appears to be trueeast-west where I was located (again 
per Google Earth)
It came from my blind spot (from behind and to my right) and appeared to 
be traveling from Northeast to Southwest. I saw it for about 3 or 4 seconds 
before it
quickly faded (there were no obstructions so it didn't go behind a tree or 
building etc.)
It was approximately 25 deg high when it disappeared and about 5 degrees to 
the right of my direction of travel (or at an approximate heading of 275 
deg).
It was light green, very round, about 1/2 to 3/4 the size of the full moon 
and about 2/3 the brightness of the full moon. There were no sparks, trails 
or smoke but it was dark
so if there was smoke I would not have been able to see it. The sky was 
clear and sunrise occurred about an hour after I saw the fireball. I have no 
idea if it was a meteor or
space junk.

Did anyone else see it?

Best regards,

Charley

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

Hannibal





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Re: [meteorite-list] AD: Semi-Famous Meteorites For Sale

2008-09-25 Thread Mark Crawford

So is the link broken, or removed on the back of Adam's reply?

Mark


Ruben Garcia wrote:

Hi all,
I have a few Semi-Famous Meteorites for sale. 


Take a look and email me of list.

http://www.mr-meteorite.com/famousmeteorites4sale.htm

Ruben Garcia
Phoenix, Arizona
http://www.mr-meteorite.com
http://www.youtube.com/profile_videos?user=meteorfrightp=v

  



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Mark's Meteorite Pages: http://meteorites.cc

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Re: [meteorite-list] Worlds in Collision

2008-09-25 Thread Sterling K. Webb
Hi, All,

The press release says:
 collisions of Mercury with Earth or Venus sometime
 in the next billion years or more. Of course by then the
 sun will have expanded and we might be toast anyway.

Not quite. When the Sun formed 4.5 billion years ago,
it was only 70% as bright as now, 90% of its present
diameter, and about 250 K. cooler. The Sun has been
getting bigger and brighter ever since, and will continue
to do so for a long time.

About 1.1 billion years from now, it will be 10% brighter,
and that would be enough to start a runaway Greenhouse
that would eventually cause the loss of all the Earth's water
out the top of the atmosphere. Of course, that far in the
future, any intelligent life will easily be able to orbit a sun
screen and prevent the developing catastrophe...

By 3.5 billion years from now, when the Sun gets to 40%
brighter than present, all the Earth's water would be gone in
runaway Greenhouse if there's no intelligent life to prevent
it. (And if there's no intelligent life left, does it matter?) The
Earth would now resemble present-day Venus very closely.

6.35 billion years from now, the Sun's core runs out of
hydrogen to burn, and the Sun starts to expand, burning
the final outer layer of hydrogen. At the point the Sun
starts expanding, it's 2.2 times brighter than today and
58% bigger. It turns into a Red Sub-Giant. Over the
next 0.7 billion years, it gets 130% bigger but no brighter
and actually cools off. The solar wind intensifies.

Over the next 0.6 billion years, it will lose 28% of its mass,
become 2350 times brighter and 166 times bigger than it is
today, and cool down to 3100 K., 7.65 billion years from now.
The sun will swallow Mercury, and fry the other inner planets,
even though all that solar wind will have pushed them much
further out than they are now.

The solar system does get fried, but not for quite a while;
it takes longer than they say.

After this, the Sun's life gets really complicated. There's a
Helium Flash when it gets hot enough to burn helium, it
shrinks and heats up, then expands and cools, uses up all
the helium, starts losing mass faster, then blows off much of
its mass in a series of short fast pulses, and collapses into
a hot little White Dwarf star with about 54% of its present
mass and a diameter about the size of the Earth! There might
be a short-lived nebula to delight the amateur astronomers
of other species in this neck of the galaxy. I hope it's pretty.

The White Dwarf Sun will cool and shine for the next 100 billion
years and the next 100 billion after that and so forth, ever fainter,
for a trillion years or so... But, for the next 5 or 6 billion years,
we should be OK, assuming good Planetary System Management
and Maintenance. (You gotta do better than we are now, though...)

Therefore, avoiding collisions of the existing planets over the
next billion years is important, yes, but it's not good enough.
I have no idea (well, some ideas) of how you would fiddle
with the dynamics of a solar system to avert collisions but
I bet, a hundred million years from now, Earth Life (if there
is any) will be able to manage it, just as we hope that in a
century or two, we will be able to manage to avoid those
pesky big asteroid collisions.

Then, the authors are assuming that the collision of two
independent Earth-sized planets is the only way to produce
this much dust and debris. There is another way. Probably
rare, but far from impossible, are double planets. The Earth
and Moon have been called that, but the Moon only masses
1.25% of the Earth's mass. Pluto and Charon (11% of Pluto's
mass) are a much better example (and would have been so
defined... well, almost).

Imagine a 1.35 Earth mass planet with a 0.65 Earth mass
moon, in a temperate place in a solar system, with oceans
of volatiles and all the rest of it. The tidal forces generated
on such a locked satellite would be enormous. The smaller
body would first become tidally locked to the larger, then
the tidal drag would slow the rotation of the larger planet,
transferring momentum to the orbit of the smaller planet and
raising its orbit.

Even the piddling force of the lunar tides will drive our
Moon away eventually, but a high-mass satellite might well
have its orbit pumped up to the point where it would
escape or be perturbed free, in only a handful of billions
of years. Then, there would be TWO planets sharing nearly
identical orbits. This never turns out well.

The short-term probability of collision is close to 100%.
There are some escape scenarios: the smaller planet is ejected
into an eccentric orbit but such orbits have a high probability
of future collision, or possibly into a Trojan orbit, also not
stable over the long term. Once any collision occurs, total
rubblization of the planets involved (and any planets that
stood too close) is certain.

Another large-moon disaster is a large retrograde double
planet. The tidal interaction takes momentum from the smaller
planet's orbit and the 

Re: [meteorite-list] ESAs artificial meteorite probes panspermia

2008-09-25 Thread Sterling K. Webb
Mike, List,

The publication you almost remember is:
http://ntrs.nasa.gov/archive/nasa/casi.ntrs.nasa.gov/19960027473_1996032004.pdf

And there is a C. Floss published in it, but the author you
are thinking of is Monica Grady of NHM, London:

It seems likely, though, that meteorite curators
through the ages, having been presented with a
fossiliferous sedimentary rock, would probably not
have been able to assess the true nature of such
a terrestrial meteorite (notwithstanding the
protestations of the owner). How many of these
types of sample have been returned to sender?
More pertinently perhaps, how many such samples
are still preserved in traditional collections?

This was in 1996. Whether anybody looked
in their old drawers, boxes, and shelves... who
knows?

I cited this in a pair of posts on sedimentary
meteorites on May 30 and 31, 2008, along with
a lot of other references to possible sedimentary
meteorites. You can find it in the List Archives,
in the thread Just Another Question.


Sterling K. Webb
-
- Original Message - 
From: Michael Murray [EMAIL PROTECTED]
To: [EMAIL PROTECTED]
Cc: meteorite-list@meteoritecentral.com
Sent: Thursday, September 25, 2008 11:28 AM
Subject: Re: [meteorite-list] ESAs artificial meteorite probes panspermia


Wasn't there a lady professor that wrote an article a while back on
the possibility of there being atypical appearing meteorites and we
might be overlooking them?  I realize that is somewhat of a wide-open
question but to possibly narrow it down a bit, the name Prof. C.
Floss seems to come to mind in my remembering this article.  Seems
like it had to do with mantle or lack of meteorites from a certain
layer, or something similar.  Anyone else remember this article?  I'd
like to read it again if I could come up with the link.
Mike

On Sep 25, 2008, at 9:05 AM, Darren Garrison wrote:

 On Thu, 25 Sep 2008 11:40:22 +0200, you wrote:

 Hello list,

 an artificial meteorite shows that sedimentary martian soil could
 reach earth, but possible microbes would get killed by the
 atmosferic flight:

 http://www.europlanet-eu.org/demo/index.php?
 option=com_contenttask=viewid=123Itemid=41

 The more interesting part of the experiment, to me, is the
 production of creamy
 white fusion crusts.  Wonder how many Martian sedementary
 meteorites (and old
 Earthites) have been passed over in the deserts because they were
 the wrong
 color?

 http://www.sciencedaily.com/releases/2008/09/080925083252.htm
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[meteorite-list] Is the list up?

2008-09-25 Thread Michael L Blood
Hello




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Re: [meteorite-list] Is the list up?

2008-09-25 Thread John.L.Cabassi

G'Day Michael
Seems fine to me.

Cheers
Johnno

- Original Message - 
From: Michael L Blood [EMAIL PROTECTED]

To: Meteorite List meteorite-list@meteoritecentral.com
Sent: Thursday, September 25, 2008 7:18 PM
Subject: [meteorite-list] Is the list up?



Hello




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Re: [meteorite-list] Is the list up?

2008-09-25 Thread Darren Garrison
On Thu, 25 Sep 2008 19:18:17 -0700, you wrote:

Hello


This better not be Viagra spam.
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Re: [meteorite-list] AD

2008-09-25 Thread Michael L Blood
Well, OK then:
No one seems to be interacting with the list, but
Here goes
I ordered a bunch of a meteorite originally named
Mali, then called Erg Chech and now officially
called Chergach.
Fell in the summer of 2007 in Chergach, Erg Chech
in the Timbuktu district of the Republic of Mali.
The material on the market is prized due to
being a witnessed fall and having rich black fusion crust
with a  fresh, white interior showing in broken sections.
I originally paid $5/g for a lot wholesale, though I
have seen it offered for $4/g.
I have a very nice shipment that just arrived and
I am offering the 5 remaining pieces for $2.25/g for
specimens with nearly100% FC and $2/g for specimens
with a broken side.
I do not believe anyone will ever see this material again
for these prices and I will be offering it (if any don't sell)
in my catalog at a considerably higher price.
So, list members now have a very rare chance to get
a nice, big, fresh stone for your collection at the price
you now have to pay for highly weathered, unidentified
NWA material.
(PS: Some of the cut slices and end pieces of this material
have shown distinct impact melt brecciation, though none
of this material has any cut surfaces, so, I have no idea what
a cut section would be like).
  When ordering, I suggest you name at least ONE
alternate, as I suspect these will go very quickly at this
price:
SEE SPECIMENS AT:
http://community.webshots.com/photo/2293914970035542431qhFDNZ
 
Specimens Nearly 100% FC ($2.25/g SALE)
257g = SALE =576-
500g = SOLD
1,077g = SALE =2,425- (Great regmaglypting)
 
Specimens with broken side ($2/g SALE)
117g = SALE = 230-
300g = SOLD
338g = SALE = 675-
708g = SALE = 1,416-
 
if you can't see the photos at:
http://community.webshots.com/photo/2293914970035542431qhFDNZ
and are interested, email me off list and I will send you an attachment.
Best wishes, Michael






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[meteorite-list] AD

2008-09-25 Thread Michael L Blood
Well, OK then:
I am not getting my own posts - and no one seems to
be interacting with the list, but here goes
I ordered a bunch of a meteorite originally named
Mali, then called Erg Chech and now officially
called Chergach.
Fell in the summer of 2007 in Chergach, Erg Chech
in the Timbuktu district of the Republic of Mali.
The material on the market is prized due to
being a witnessed fall and having rich black fusion crust
with a  fresh, white interior showing in broken sections.
I originally paid $5/g for a lot wholesale, though I
have seen it offered for $4/g.
I have a very nice shipment that just arrived and
I am offering the 5 remaining pieces for $2.25/g for
specimens with nearly100% FC and $2/g for specimens
with a broken side.
I do not believe anyone will ever see this material again
for these prices and I will be offering it (if any don't sell)
in my catalog at a considerably higher price.
So, list members now have a very rare chance to get
a nice, big, fresh stone for your collection at the price
you now have to pay for highly weathered, unidentified
NWA material.
(PS: Some of the cut slices and end pieces of this material
have shown distinct impact melt brecciation, though none
of this material has any cut surfaces, so, I have no idea what
a cut section would be like).
  When ordering, I suggest you name at least ONE
alternate, as I suspect these will go very quickly at this
price:
SEE SPECIMENS AT:
http://community.webshots.com/photo/2293914970035542431qhFDNZ
 
Specimens Nearly 100% FC ($2.25/g SALE)
257g = SALE =576-
500g = SOLD
1,077g = SALE =2,425- (Great regmaglypting)
 
Specimens with broken side ($2/g SALE)
117g = SALE = 230-
300g = SOLD
338g = SALE = 675-
708g = SALE = 1,416-
 
if you can't see the photos at:
http://community.webshots.com/photo/2293914970035542431qhFDNZ
and are interested, email me off list and I will send you an attachment.
Best wishes, Michael












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