[meteorite-list] Cold Asteroids May Have A Soft Heart(AllendeMeteorite)

Sterling K. Webb sterling_k_webb at sbcglobal.net
Thu Apr 14 02:21:31 EDT 2011


Hi,

Way too much stuff here to deal with all,
but I have a word about 2 Pallas as a
"Carbonaceous parent body."

Pallas has a silicate spectrum. A great many
bodies do. It shows signs of olive and pyroxene,
with low iron and water. If it resembles any
Carbonaceous chondrite, it's a CR with no
hydrated minerals or very little.

Pallas is very dark, with an albedo of 12%-14%,
almost as dark as our moon, whose albedo is
7% to 8%. Yes, when we look at the Moon
at night, it looks BRIGHT, but in reality, the
Moon is about the color and reflectivity of
a huge lump of black anthracite coal.

The fact that it doesn't look like a lump of coal
in pictures taken on the Moon or looked to the
astronauts as a very light grey demonstrates
the ability of the human mind to scale image
intensity to the Earth norm and to expose film
to achieve similar results.

Pallas is a little brighter than the Moon but
some darker than Mercury which is about 15%
to 16% albedo. Of course, if a human eye was ON
Mercury, the planet would appear to us as blazing
white under sunlight more than 2.5 times brighter
than here at Earth.

The density of Pallas is about 2.8. The similar
sized Vesta is 3.43, our Moon 3.35, Mercury . For
comparison, Earth's crustal rocks, mostly silicates,
have a mean density of about 3.0. It seems unlikely
that Pallas has an iron core. Like the Moon and
Mercury, it seems to be essentially waterless.

The spectral "classifications," both the Tholin and
the 2Mass, classify a great many asteroids as varieties
of "Carbonaceous," but we see far fewer Carbonaceous
meteorites than they see asteroids!

We spent many decades trying to analyze the surface
of the Moon spectroscopically, it being so conveniently
close and all, but none of it told us that much about
what we'd find when we got their. Similarly, spectral
studies of Mars from Earth are largely forgotten for
the same reason: they were wrong.

I expect Pallas to be excessively dry and waterless,
made of excessively dark rock, primitive in composition,
likely has little plagioclase on the surface, probably
isn't "differentiated" and lacks basalt melts. But hey!
I'm just guessing.

There is a chance that we may get a look at Pallas.
When the Dawn mission is mission is finished at Ceres,
if all systems are functioning and fuel supplies are
within parameters, it COULD be sent on a flyby of
Pallas. Dawn couldn't orbit it, but it could grab a lot
of lovely snapshots on that pass.

Of course, we'd have to get it funded by Congress...

Groan.



Sterling K. Webb
--------------------------------------------------------------------------
----- Original Message ----- 
From: "MEM" <mstreman53 at yahoo.com>
To: "Richard Montgomery" <rickmont at earthlink.net>; "metlist" 
<meteorite-list at meteoritecentral.com>
Sent: Wednesday, April 13, 2011 9:31 PM
Subject: Re: [meteorite-list] Cold Asteroids May Have A Soft 
Heart(AllendeMeteorite)


> Let me play politician and ask to "revise and extend my remarks". 
> There are
> asteroid gurus on the list who are more likely able to address this 
> and I'd like
> to hear from them.  Your theory/question is partially in the right 
> direction so
> let me re-frame it.  I believe we have "likely" detected all the 
> existent
> asteroids in our inner solar system which are large enough to have 
> formed
> basalt/cores--aka differentiated.  That size is hard 
> overlook(100-300km
> minimum?).  I read somewhere that as many as 12-20 major/minor planets 
> would
> have formed in the early solar system that are no longer with us  as 
> major/minor
> intact bodies.( i.e. absorbed or ejected)
>
> As to meteorite parent bodies, what we have yet to inventory and, for 
> which we
> have not had a specimen drop by Earth for comparison, are these long 
> ago
> disrupted bodies.  These bodies  which now are represented only by 
> minor,
> irregular, slivers, slices, and rubble piles within certain swarms of 
> asteroids
> in different sectors of the solar system.
>
> There is a "diogenite-like" spectrum coming from an outer-belt 
> asteroid whose
> orbit proves it cannot be  related to Vesta.   I mentioned the caveat 
> that there
> may be some remnants of  asteroids which were differentiated in the 
> early solar
> system and for  whatever reason are no longer in tact.  We may  only 
> have a
> fraction of the original large body such that while we have  located 
> all the
> differentiated intact ergo larger asteroids, we may need  to be 
> looking for
> shards of former bodies to match meteorites from our  collections. 
> The reason
> all our "HED"s are from Vesta is probably that Vesta is on our  "mail 
> route" and
> quantum transport from Vesta to Earth is a favorable  happenstance.
>
> "1459 Magnya:  Orbits in the outer main belt, too far from Vesta to be
> genetically  related. May be the remains of a different ancient 
> differentiated
> body  that was shattered long ago."  Spectrum is diogenite-like
>
> Another candidate which may be the source of olivine-diogenites but is 
> a chunk
> off Vesta:
> "2579 Spartacus — contains a significant portion of olivine, which may 
> indicate
> origin deeper within Vesta than other V-types."
> See list at:
> <http://en.wikipedia.org/wiki/V-type_asteroid>
> <http://en.wikipedia.org/wiki/4_Vesta>
>
> Pallas and its family of asteroids is certainly a candidate for one of 
> the
> Carbonaceous parent body, even thought it shows no major excavations.
> "2 Pallas is a large and most certainly differentiated body but lacks 
> evidence
> of a deep
> excavation and its spectrum shows carbonaceous chondrite affinities. 
> However
> 75% of the astrtoids out there whose spectra we've measured fall in 
> the C or
> Carbonaceous class."
> <http://en.wikipedia.org/wiki/2_Pallas>
> <http://en.wikipedia.org/wiki/Carbonaceous_chondrite>
> Also in my reading there is good indication that the Martian moons are 
> captured
> carbonaceous asteroids
> <http://en.wikipedia.org/wiki/Moons_of_Mars>
>
> Asteroid types More than I can retain in my head:
> <http://nineplanets.org/asteroids.html>
> <http://en.wikipedia.org/wiki/Asteroid_spectral_types>
> * C-type, includes more than 75% of known asteroids:       extremely 
> dark
> (albedo 0.03);       similar to carbonaceous chondrite meteorites;
> approximately the same chemical composition as the Sun minus hydrogen, 
> helium
> and       other volatiles;
>
> * S-type, 17%: relatively bright (albedo .10-.22); metallic 
> nickel-iron
> mixed with iron- and magnesium-silicates;
>
> * M-type, most of the rest:  bright (albedo .10-.18); pure 
> nickel-iron.
> * There are also a dozen or so other rare types.
>
> Read more about Asteroids  l  Asteroid facts, pictures and information 
> by
> nineplanets.org * C-type, includes more than 75% of known asteroids:
> extremely dark (albedo 0.03);       similar to carbonaceous chondrite
> meteorites;       approximately the same chemical composition as the 
> Sun minus
> hydrogen, helium and       other volatiles;
>
> * S-type, 17%: relatively bright (albedo .10-.22); metallic 
> nickel-iron
> mixed with iron- and magnesium-silicates;
>
> * M-type, most of the rest:  bright (albedo .10-.18); pure 
> nickel-iron.
> * There are also a dozen or so other rare types.
>
> Read more about Asteroids  l  Asteroid facts, pictures and information 
> by
> nineplanets.org
>
> Meteorites and their Parent Bodies 2nd Edition. Harry Mc Sween which I 
> think us
> a google book online.
>
> Elton
>
>
>
> ----- Original Message ----
>> From: Richard Montgomery <rickmont at earthlink.net>
>> To: Ron Baalke <baalke at zagami.jpl.nasa.gov>; Meteorite Mailing List
>><meteorite-list at meteoritecentral.com>
>> Sent: Wed, April 13, 2011 8:39:46 PM
>> Subject: Re: [meteorite-list] Cold Asteroids May Have A Soft Heart
>>(AllendeMeteorite)
>>
>> Ron and List,
>>
>> This new evidence fits exactly into the recent question I  posted, 
>> 'Vesta,
>> for sure?'
>>
>> I only heard back from Elton (thanks,  sincerely!) and yet now with 
>> this
>> hypothesis, my question lingers as to the  absolute recognition of 
>> parent
>> bodies, with my query as to the  yet-undiscovered potential pairings 
>> of
>> undiscovered asteroids.
>>
>> MEM  pointed out that the largest asteroids (aka Vesta etal) have 
>> already
>> been  located, with tell-tale impact and reflective signatures that 
>> rule out
>> other  parents for our HEDs.
>>
>> My new question, neophyte layman as I am,  is:
>>
>> Does this new data/theory bring my initial question about
>> Vesta-for-sure-as-parent-for-HEDs back into play?
>>
>> -Richard  Montgomery
>>
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