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| Jean |
Posted: Fri Mar 21, 2008 2:59 am |
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Darwin123 a écrit dans le message
<04d40324-8030-45e1-b9ee-4821cb079e75@2g2000hsn.googlegroups.com>...
Quote: On Mar 20, 9:28 am, don findlay <d...@tower.net.au> wrote:
Darwin123 wrote:
It would be so nice if scientific documentaries included
references to scientific papers, even if most of the audience don't
care. I am sure that few of the audience care about the actors,
writers and directors. Yet we have credits.
Surely you don't think the credits are for the benefit of the viewer,
do you?
No, they are for the cast. Actors get additional exposure so
people know their names. Furthermore, it provides a chain of reference
on their resumes. A future employer, looking at their resume, can look
at their work and get additional verification on their participation
in the product. The same applies for directors, writers, special
effects people, etc.
Citing the scientific article would benefit the scientist that
wrote them. It is the nonscientist who is going to hire them, after
all.
I don't see any published code of ethics that forbids publicity
once the peer review has gone through. One of the bad things about
popularized science on TV is that there is no way a better informed
viewer can look at the details.
I would love to know the assumptions that went into that
simulation. I don't know what I am discussing unless there is some
exposition on the physics involved. The result of a computer
simulation is merely a cartoon without the physical and mathematical
assumptions that went into the simulation. Without physics, historical
conjecture is stupid. Especially in natural history.
To illustrate your point I found this at the BBC site. It is very
interesting but no references are given. The name and a quote from Dr.
Neukum is provided only.
"Martian volcanoes 'may be active'
By Paul Rincon BBC News science reporter, Cambridge
Mars Express looks across the surface with a cone in the foreground and
top-left
Fields of volcanic cones discovered at the North Pole of Mars suggest the
Red Planet could still be geologically active, scientists have said. "
"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.
"
It would be nice if a reference was provided so that one could see what the
conclusions
were based upon.
JL |
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| Florian |
Posted: Fri Mar 21, 2008 4:22 am |
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George <George@george.net> wrote:
Quote: Yeah, I made the same mistake. For future reference, Florian. It would help
if you posted a link to the entire article so we can know the context of the
graphs you are referrring to.
<more eyes rolling>
The link to the article was posted in the thread in :
news:1ie1tyx.kov73012akbdoN%auxotectonics_deletethis@nachon_andthis.net
Quote: But you are right in the sense that the graph
doesn't show a decrease in volcanic activity. But it doesn't show an
increase either. It only shows that the volcanic activity has been widely
distributed and sporatic in time as indicated by continued loss of craters
due to lava flows.
Hmmm, I see nowhere in the article, a mention that craters are loss by
lava flow...
Quote: The article makes the point that all the internal heat
within Mars may not have yet dissipated, but it doesn't say that it is
currently active. Only suggests that there could be further activity on the
planet.
Indeed. My point was that Mars might not be dead in contrast to the
statement made by SBC Yahoo, in this thread.
Quote: I think it is possible that some very minor activity could occur in
the furture. But there certainly is no evidence that large scale vulcanism
has occurred in recent times.
It depends on what you mean by "recent time". On a 4.5 billions years
time scale, 100 millions is quite recent.
Besides there is a clear trend: The frequency of major volcanic events
has increased, the rest period being basically divided by two after each
events.
Quote: It certainly appears to make the case that
although Mars may still be tectonically active, it is subtle, probably order
of magnitude less active than Earth,
You're guessing. We won't know before some guys put a sismometer there.
Quote: which would indicate that Mars interior
certainly isn't the dynamo that Earth's interior is.
We know that Mars magnetic field is weaker than that of the Earth, for
sure.
--
Florian
"Toute vérité passe par trois phases. D'abord, elle est ridiculisée;
ensuite, elle rencontre une vive opposition avant d'être acceptée comme
une totale évidence" - Arthur Schopenhauer |
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| brad |
Posted: Fri Mar 21, 2008 5:27 am |
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On Mar 20, 9:37 am, don findlay <d...@tower.net.au> wrote:
" ... except for very small values of Fe/Si ratios catastrophic
core/shell separations would occur in the protoplanets that had
reached ~ lunar size " . D.C. Tozer '76 . so the core forms first
by collisions of smaller cores liberated from their protoplanets by
catastrophic separation. the rest of a terrestrial planet forms from
what's left of the planetary nebula via agglomeration. |
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| brad |
Posted: Fri Mar 21, 2008 5:36 am |
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On Mar 19, 6:43 am, "Landy" <no...@nowhere.net> wrote:
Quote: "Skywise" <i...@oblivion.nothing.com> wrote in message
news:13u10vvtoo55d71@corp.supernews.com...
rAgAv <ragav.pa...@googlemail.com> wrote in news:1ffef2dc-a033-410e-96f4-
4f0136740...@e6g2000prf.googlegroups.com:
Hello,
According to my current knowledge, the earth's magnetic field formed
due to the molten iron core that is spinning to create a magnetic
field. This magnetic field is also what is protecting us from harmful
bursts (solar plasma?) from the sun.
I don't understand one thing - why doesn't Mars have one?
Mars is cold. Being smaller, it cooled quicker. It's liquid
core froze eons ago thus shutting down its dynamo.
But then why does Venus not have one? Being roughly the same size as Earth
and all................
cheers
Bill
some people have postulated that mars /earth /moon result from same
cosmic collision event ; and venus/mercury result from another. |
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| brad |
Posted: Fri Mar 21, 2008 6:07 am |
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On Mar 19, 4:57 pm, Darwin123 <drosen0...@yahoo.com> wrote:
Quote: On Mar 19, 4:22 pm, "Landy" <no...@nowhere.net> wrote:> "Timberwoof" <timberwoof.s...@inferNOnoSPAMsoft.com> wrote in message
news:timberwoof.spam-30CDC8.09083319032008@nnrp-virt.nntp.sonic.net...
In article <gfWdnSyiUOCYYn3anZ2dnUVZ_u6rn...@comcast.com>,
John Popelish <jpopel...@rica.net> wrote:
Why would that event suddenly leave the iron core in the
Earth and not leave one in the moon?
Because it had greater momentum and was less likely to vapourise.
cheers
Bill
The sentence doesn't quite make sense. Do you mean momentum in the
center of mass coordinate system of the two bodies? Furthermore, why
would greater momentum make it less likely to vaporize?
I saw a special describing the results of the simulation but
they didn't try to explain the results in simpler terms.
My first guess was that the two bodies merged for a short time
into one giant liquid body, and partially equilibrated. Then, there
would be forces that resembled buoyancy. Basically, the iron sunk to
the bottom of the merged body.
Wait, this doesn't work (?). The system would be far too
turbulent. The Froude number would be too big to allow stratification.
My second guess involves phase transitions. The joint body was
gas. The iron, having a higher vaporization temperature, condensed
into one massive liquid-body that sent all the momentum into the gas,
which then recondensed into the moon. The elements with the small
atomic number had larger vaporization point temperatures.
Calculations have long shown, since the 1700s, that an inelastic
collision between earth-like bodies would vaporize most of the
material of both bodies. Therefore, I would hope the simulation
included phase transitions in the dynamics. Did they?
The verbal description only said they simulated the bodies as
made of many small particles, and calculated separate trajectories.
There are google squared ways to do this.
What bothers me is that the computer simulation never means
anything by itself. It is the physical assumptions being made that
make the computer simulation meaningful. You can't go, "Run a computer
simulation," and believe everything that comes out. If you don't
confined the physics before the run, you can make the physics do
ANYTHING.
It would be so nice if scientific documentaries included
references to scientific papers, even if most of the audience don't
care. I am sure that few of the audience care about the actors,
writers and directors. Yet we have credits.
the bulk density of the moon is is close to that of uncompressed , low
- temperature earth mantle material. ( G.Malcolm Brown ) . moon is
depleted in chalcophile, siderophile, and volatile elements when
compared to cosmic abundances .( Ganapathy and Anders '74) the first
two could be explained if large scale lunar melting had occurred and
siderophiles differentiated into core. ( G. Malcolm Brown
'76 )
in addition, moons mantle is depleted in Ni as compared to cosmic
abundance. this can be interpreted as genesis from earths' mantle and
then large scale melting concentrated Ni in moons core ( see
G.M.Brown ) |
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| brad |
Posted: Fri Mar 21, 2008 6:14 am |
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On Mar 19, 6:43 am, "Landy" <no...@nowhere.net> wrote:
Quote: "Skywise" <i...@oblivion.nothing.com> wrote in message
news:13u10vvtoo55d71@corp.supernews.com...
rAgAv <ragav.pa...@googlemail.com> wrote in news:1ffef2dc-a033-410e-96f4-
4f0136740...@e6g2000prf.googlegroups.com:
Hello,
According to my current knowledge, the earth's magnetic field formed
due to the molten iron core that is spinning to create a magnetic
field. This magnetic field is also what is protecting us from harmful
bursts (solar plasma?) from the sun.
I don't understand one thing - why doesn't Mars have one?
Mars is cold. Being smaller, it cooled quicker. It's liquid
core froze eons ago thus shutting down its dynamo.
But then why does Venus not have one? Being roughly the same size as Earth
and all................
cheers
Bill
this could be explained by venus having a higher S content than
earth . then , the core/mantle interface would be blurred and dynamo
mechanism hindered. |
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| Jean |
Posted: Fri Mar 21, 2008 12:28 pm |
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Florian a écrit dans le message
<1ie9hl9.l5qwzrwolb3iN%auxotectonics_deletethis@nachon_andthis.net>...
Quote: Stuart <bigdakine@aol.com> wrote:
On Mar 22, 11:18 pm, auxotectonics_deletethis@nachon_andthis.net
(Florian) wrote:
Stuart <bigdak...@aol.com> wrote:
I wonder if you worth more than Georgie... I remember you were the
one
stating that buoyancy is not related to pressure gradient. What a
pity.
I said hydrostatic gradient was irrelevant.
Do you agree that the lithostatic pressure gradient is relevant, yes or
no?
Lithostatic refers to the same thing.
Technically not.
Hydrostatic pressure in geology, usually refer to the pressure of the
fluid in the cracks, fractures, porosity in the upper crust.
Lithostatic pressure refer to the pressure caused by the column of rock.
Now Stuart, could you please answer to this simple question, a question
that is trivial for a geophysicist who developped a computer model of
convection.
Do you agree that the lithostatic pressure gradient is relevant to
buoyancy, yes or no?
[...]
Anyway, I remember clearly that the discussion was about the
inititation
of subduction. What makes a slab sink if its density is initially
higher
than that of the upper mantle?
Is that really the question you mean to ask?
It was the object of the original discussion, Stuart. May be that time
plays tricks on your mind...
--
Florian
"Toute vérité passe par trois phases. D'abord, elle est ridiculisée;
ensuite, elle rencontre une vive opposition avant d'être acceptée comme
une totale évidence" - Arthur Schopenhauer
Go to this page if you have an interest in the dynamics of the Earth.
http://geology.ref.ac/marchal/cadre.htm
Are you a member of G.I.F. or AGSO?
JL |
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| George |
Posted: Fri Mar 21, 2008 6:22 pm |
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"Florian" <auxotectonics_deletethis@nachon_andthis.net> wrote in message
news:1ie5buc.t9uuc7176pr66N%auxotectonics_deletethis@nachon_andthis.net...
Quote: George <George@george.net> wrote:
Yeah, I made the same mistake. For future reference, Florian. It would
help
if you posted a link to the entire article so we can know the context of
the
graphs you are referrring to.
more eyes rolling
The link to the article was posted in the thread in :
news:1ie1tyx.kov73012akbdoN%auxotectonics_deletethis@nachon_andthis.net
But you are right in the sense that the graph
doesn't show a decrease in volcanic activity. But it doesn't show an
increase either. It only shows that the volcanic activity has been widely
distributed and sporatic in time as indicated by continued loss of
craters
due to lava flows.
Hmmm, I see nowhere in the article, a mention that craters are loss by
lava flow...
Then perhaps you need to understand what the article is all about. For
instance:
"A new analysis of impact cratering data from Mars reveals that the planet
has undergone a series of global volcanic upheavals. These violent episodes
spewed lava and water onto the surface, sculpting the landscape that ESA's
Mars Express looks down on today.
Using images from the High Resolution Stereo Camera (HRSC) on Mars Express,
Gerhard Neukum, Freie Universität Berlin, Germany, and colleagues are
discovering the history of the Red Planet's geological activity. "We can now
determine the ages of large regions and resurfacing events on the planet,"
says Neukum. Resurfacing occurs when volcanic eruptions spread lava across
the planet's surface."
In other words, volcanic activity has resurfaced the planet, and in doing
so, has erased many prior impacts. That is largely why over time, the graph
shows a DECREASE in impacts - because the surface has been resculpted by
volcanic activity.
Quote: The article makes the point that all the internal heat
within Mars may not have yet dissipated, but it doesn't say that it is
currently active. Only suggests that there could be further activity on
the
planet.
Indeed. My point was that Mars might not be dead in contrast to the
statement made by SBC Yahoo, in this thread.
I think it is possible that some very minor activity could occur in
the furture. But there certainly is no evidence that large scale
vulcanism
has occurred in recent times.
It depends on what you mean by "recent time". On a 4.5 billions years
time scale, 100 millions is quite recent.
Besides there is a clear trend: The frequency of major volcanic events
has increased, the rest period being basically divided by two after each
events.
There is NO evidence in that article that indicates whether volcanic
activity has increased or decreased. From what I can tell from what was
presented in the article, that issue wasn't even addressed.
Quote: It certainly appears to make the case that
although Mars may still be tectonically active, it is subtle, probably
order
of magnitude less active than Earth,
You're guessing. We won't know before some guys put a sismometer there.
If I am guessing, then so are the authors of the article, since my statement
is essentially the same statement they made. And if the authors are
guessing, then what was your point in posting it in the first place?
Quote: which would indicate that Mars interior
certainly isn't the dynamo that Earth's interior is.
We know that Mars magnetic field is weaker than that of the Earth, for
sure.
Mar's magnetic field is virtually non-existent. It exists only as local
magnetic anomalies due to the presence of locally magnetic rocks.
George |
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| Florian |
Posted: Fri Mar 21, 2008 6:45 pm |
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George <George@george.net> wrote:
Quote: Hmmm, I see nowhere in the article, a mention that craters are loss by
lava flow...
Then perhaps you need to understand what the article is all about.
From a guy who can't read a simple chart. Give me a break.
Quote: For instance:
"A new analysis of impact cratering data from Mars reveals that the planet
has undergone a series of global volcanic upheavals. These violent episodes
spewed lava and water onto the surface, sculpting the landscape that ESA's
Mars Express looks down on today.
Using images from the High Resolution Stereo Camera (HRSC) on Mars Express,
Gerhard Neukum, Freie Universität Berlin, Germany, and colleagues are
discovering the history of the Red Planet's geological activity. "We can now
determine the ages of large regions and resurfacing events on the planet,"
says Neukum. Resurfacing occurs when volcanic eruptions spread lava across
the planet's surface."
In other words, volcanic activity has resurfaced the planet, and in doing
so, has erased many prior impacts.
Here again, you assume that the volcanic events resurfaced a large
portion of Mars. But you simply can't guess it from the paper.
Anyway, you completely fail to understand the principle of craters
counting.
Craters counting allow to estimate the age of an area, even one of a few
hundred square km, by counting the number of craters per square km. Note
that it is a DENSITY of craters, not an absolute number. The larger the
number of craters per square km, the older is the area, whatever the
size of the resurfaced area.
Quote: That is largely why over time, the graph
shows a DECREASE in impacts - because the surface has been resculpted by
volcanic activity.
Seriously, do you really suggest that the decrease of impact craters
density is not related to the decrease in meteorites density in the
solar system?? Do you know that impact craters density follow the same
trend on the moon? May be you also suggest that the moon was resurfaced
by volcanic event as well?
Jeez... I already knew you had a hard time to understand very basic
principles, but here, you're breaking records.
[...]
Quote: It depends on what you mean by "recent time". On a 4.5 billions years
time scale, 100 millions is quite recent.
Besides there is a clear trend: The frequency of major volcanic events
has increased, the rest period being basically divided by two after each
events.
There is NO evidence in that article that indicates whether volcanic
activity has increased or decreased. From what I can tell from what was
presented in the article, that issue wasn't even addressed.
Let's look at the graph. Major episodes occured at 3500, then 1500 then
400-800, then 200 then 100 million years, but you still can't figure out
that the frequency of episodes increased with time? You're hopeless...
[...]
Quote: If I am guessing, then so are the authors of the article, since my statement
is essentially the same statement they made.
No George. The authors of the article present data showing that the
activity on Mars is episodic and at a frequency that increased.
No guess just facts.
--
Florian
"Toute vérité passe par trois phases. D'abord, elle est ridiculisée;
ensuite, elle rencontre une vive opposition avant d'être acceptée comme
une totale évidence" - Arthur Schopenhauer |
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| George |
Posted: Sat Mar 22, 2008 12:12 am |
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"Florian" <auxotectonics_deletethis@nachon_andthis.net> wrote in message
news:1ie6fuy.pt0tau1fgm0lcN%auxotectonics_deletethis@nachon_andthis.net...
Quote: George <George@george.net> wrote:
Hmmm, I see nowhere in the article, a mention that craters are loss by
lava flow...
Then perhaps you need to understand what the article is all about.
From a guy who can't read a simple chart. Give me a break.
For instance:
"A new analysis of impact cratering data from Mars reveals that the
planet
has undergone a series of global volcanic upheavals. These violent
episodes
spewed lava and water onto the surface, sculpting the landscape that
ESA's
Mars Express looks down on today.
Using images from the High Resolution Stereo Camera (HRSC) on Mars
Express,
Gerhard Neukum, Freie Universität Berlin, Germany, and colleagues are
discovering the history of the Red Planet's geological activity. "We can
now
determine the ages of large regions and resurfacing events on the
planet,"
says Neukum. Resurfacing occurs when volcanic eruptions spread lava
across
the planet's surface."
In other words, volcanic activity has resurfaced the planet, and in doing
so, has erased many prior impacts.
Here again, you assume that the volcanic events resurfaced a large
portion of Mars. But you simply can't guess it from the paper.
I don't assume anything, Floppy. I didn't write the paper. Again, they say
""We can now determine the ages of large regions and resurfacing events on
the planet," says Neukum. Resurfacing occurs when volcanic eruptions spread
lava across the planet's surface." and "These violent episodes spewed lava
and water onto the surface, sculpting the landscape that ESA's Mars Express
looks down on today."
Any questions?
Quote: Anyway, you completely fail to understand the principle of craters
counting.
Craters counting allow to estimate the age of an area, even one of a few
hundred square km, by counting the number of craters per square km. Note
that it is a DENSITY of craters, not an absolute number. The larger the
number of craters per square km, the older is the area, whatever the
size of the resurfaced area.
And your point is what, exactly?
Quote: That is largely why over time, the graph
shows a DECREASE in impacts - because the surface has been resculpted by
volcanic activity.
Seriously, do you really suggest that the decrease of impact craters
density is not related to the decrease in meteorites density in the
solar system?? Do you know that impact craters density follow the same
trend on the moon? May be you also suggest that the moon was resurfaced
by volcanic event as well?
Comparing the moon with Mars is like comparing apples and oranges. The moon
has not substantially changed since the major bombardments early in it's
history. The surface of Mars HAS changed substantially since then.
Quote: It depends on what you mean by "recent time". On a 4.5 billions years
time scale, 100 millions is quite recent.
Besides there is a clear trend: The frequency of major volcanic events
has increased, the rest period being basically divided by two after
each
events.
There is NO evidence in that article that indicates whether volcanic
activity has increased or decreased. From what I can tell from what was
presented in the article, that issue wasn't even addressed.
Let's look at the graph. Major episodes occured at 3500, then 1500 then
400-800, then 200 then 100 million years, but you still can't figure out
that the frequency of episodes increased with time? You're hopeless...
[...]
If I am guessing, then so are the authors of the article, since my
statement
is essentially the same statement they made.
No George. The authors of the article present data showing that the
activity on Mars is episodic and at a frequency that increased.
No guess just facts.
"Episodic" implies that it is cyclic, but there is no evidence presented
that that is the case. Not only that, but the graph doesn't describe the
intensity of volcanism (nor the number of events) that occurred during any
of the times listed. So to suggest that the graph demonstrates that
volcanism has increased is quite a leap of your imagination. What the graph
does plainly show is that the number of countable craters has decreased over
time, and they are arguing that that is because of the resurfacing of the
planet that has occurred due to volcanism and related floods.
George |
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| Florian |
Posted: Sat Mar 22, 2008 4:21 am |
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George <George@george.net> wrote:
Quote: Anyway, you completely fail to understand the principle of craters
counting.
Craters counting allow to estimate the age of an area, even one of a few
hundred square km, by counting the number of craters per square km. Note
that it is a DENSITY of craters, not an absolute number. The larger the
number of craters per square km, the older is the area, whatever the
size of the resurfaced area.
And your point is what, exactly?
That you're a moron not capable to understand that the age is derived
form the DENSITY of craters, not from the number of craters that would
have been erased by spewed lava.
Quote: Seriously, do you really suggest that the decrease of impact craters
density is not related to the decrease in meteorites density in the
solar system?? Do you know that impact craters density follow the same
trend on the moon? May be you also suggest that the moon was resurfaced
by volcanic event as well?
Comparing the moon with Mars is like comparing apples and oranges. The moon
has not substantially changed since the major bombardments early in it's
history. The surface of Mars HAS changed substantially since then.
More moronic comments. The cratening rate of the Moon like Mars or any
object in the inner solar system is assumed to be similar.
Here is a little exercise that you will certainly fail to resolve:
<http://www.astro.washington.edu/larson/Astro150b/CoursePak/cp14_crater_
counting.pdf>
Well, forget it. Just go back to your cave.
--
Florian
"Toute vérité passe par trois phases. D'abord, elle est ridiculisée;
ensuite, elle rencontre une vive opposition avant d'être acceptée comme
une totale évidence" - Arthur Schopenhauer |
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| Stuart |
Posted: Sat Mar 22, 2008 6:57 am |
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On Mar 21, 11:21 pm, auxotectonics_deletethis@nachon_andthis.net
(Florian) wrote:
Quote: George <Geo...@george.net> wrote:
Anyway, you completely fail to understand the principle of craters
counting.
Craters counting allow to estimate the age of an area, even one of a few
hundred square km, by counting the number of craters per square km. Note
that it is a DENSITY of craters, not an absolute number. The larger the
number of craters per square km, the older is the area, whatever the
size of the resurfaced area.
And your point is what, exactly?
That you're a moron not capable to understand that the age is derived
form the DENSITY of craters, not from the number of craters that would
have been erased by spewed lava.
?
If you have a massive lava flow it will reduce the crater density by
burying the
craters.
On an object like the moon, we knew that the Mare were younger than
the highlands
before any rocks were brought back. Why because they had a lower
crater density than
any place else. Why? because the flood basalts that comprise the Mare
buried the craters
in effect resetting the crater density based chronometer.
Quote:
Seriously, do you really suggest that the decrease of impact craters
density is not related to the decrease in meteorites density in the
solar system?? Do you know that impact craters density follow the same
trend on the moon? May be you also suggest that the moon was resurfaced
by volcanic event as well?
The Lunar Mare were in fact resurfaced by volcanism, that is the
point.
A surface with a uniform age has a crater density that doesn't vary
much from place to place.
The Venusian surface has a fairly uniform crater density, only that
density is much smaller
than the moon's or Mars's? Why? because the surface is younger.
Quote:
Comparing the moon with Mars is like comparing apples and oranges. The moon
has not substantially changed since the major bombardments early in it's
history. The surface of Mars HAS changed substantially since then.
More moronic comments. The cratening rate of the Moon like Mars or any
object in the inner solar system is assumed to be similar.
George's point flew right over your head. You can assume the
bombardment of the moon
and other bodies was similar. Probably not a great assumption, but
better than an order of
magnitude.
The Lunar Mare have smaller crater density. They didn't receive less
meteorites, just
that the flood basalt pretty much wiped the slate clean.
You do understand that you can use crater density and stratigraphy to
tell you
something about the relative ages of the body's surface?
It doesn't look like you understood it.
Stuart |
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| Florian |
Posted: Sat Mar 22, 2008 2:50 pm |
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Stuart <bigdakine@aol.com> wrote:
Quote: If you have a massive lava flow it will reduce the crater density by
burying the craters.
On an object like the moon, we knew that the Mare were younger than the
highlands before any rocks were brought back. Why because they had a lower
crater density than any place else. Why? because the flood basalts that
comprise the Mare buried the craters in effect resetting the crater
density based chronometer.
Explain that to Georgie who is apparently convinced "that the volcanic
activity has been widely distributed and sporatic in time as indicated
by continued loss of craters due to lava flows." (sic!)
or again:
"In other words, volcanic activity has resurfaced the planet, and in
doing so, has erased many prior impacts. That is largely why over time,
the graph shows a DECREASE in impacts - because the surface has been
resculpted by volcanic activity."
See, you're buddy truly think that the graph shows a decrease in impacts
because of the lava flow resetting the surface, whereas the graph show a
decrease in the DENSITY of craters because there is simply less
asteroids that impacts as time goes by.
Even highschooler know that the frequency of asteroid impacts decrease
with time in the inner solar system.
For sure, If the frequency had been constant with time, that would have
been much easier to date surfaces, but that is not he case (see the work
of Hartmann, Neukum and Ivanov cited below.)
Quote: George's point flew right over your head.
Give me a break. See above. I don't even understand why you try to save
the scalp of a moron that can't understand an article nor read a graph
legend.
Quote: You can assume the bombardment of the moon and other bodies was similar.
Probably not a great assumption, but better than an order of magnitude.
"I" don't assume. This assumption was made and jsutified by Neukum
Ivanov and Hartmann to date the surface of Mars from Moon's data. See
in:
Hartmann, W. K. and Neukum, G. (2001) Space Sci. Rev. 96, 165-194
<http://www.springerlink.com/content/nq62226301355207/?p=9e21e16db846498
0a499db540cf257fd&pi=8>
for a recent work ans some graph illustrating the coorelation:
http://www.lpi.usra.edu/meetings/lpsc2008/pdf/2509.pdf
May be you would like to deny their work?
I wonder if you worth more than Georgie... I remember you were the one
stating that buoyancy is not related to pressure gradient. What a pity.
--
Florian
"Toute vérité passe par trois phases. D'abord, elle est ridiculisée;
ensuite, elle rencontre une vive opposition avant d'être acceptée comme
une totale évidence" - Arthur Schopenhauer |
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| Jean |
Posted: Sat Mar 22, 2008 2:50 pm |
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Stuart a écrit dans le message ...
SNIP>> Hydrostatic pressure in geology, usually refer to the pressure of the
Quote: fluid in the cracks, fractures, porosity in the upper crust.
Lithostatic pressure refer to the pressure caused by the column of rock.
"Same difference in the sense that neither cause fluid motion", both are
cases
of a spherical stress tensor.
SNIP
Stuart
That is one of the most amazing statements I have seen in this group.
Both cause fluid motion.
Without hydrostatic pressure(1) there is no fluid flow.
(1)
P = density of the fluid *g * height of the column.
volume flux = k (p2-p1) . To illustrate the effect of lithographic
pressure place a rock on a plastic
container of water then make a hole in the bottom. Remove the rock to see
the difference in flow rate.
JL
JL |
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| Stuart |
Posted: Sat Mar 22, 2008 5:29 pm |
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Guest
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On Mar 22, 9:50 am, auxotectonics_deletethis@nachon_andthis.net
(Florian) wrote:
Quote: Stuart <bigdak...@aol.com> wrote:
If you have a massive lava flow it will reduce the crater density by
burying the craters.
On an object like the moon, we knew that the Mare were younger than the
highlands before any rocks were brought back. Why because they had a lower
crater density than any place else. Why? because the flood basalts that
comprise the Mare buried the craters in effect resetting the crater
density based chronometer.
Explain that to Georgie who is apparently convinced "that the volcanic
activity has been widely distributed and sporatic in time as indicated
by continued loss of craters due to lava flows." (sic!)
or again:
"In other words, volcanic activity has resurfaced the planet, and in
doing so, has erased many prior impacts. That is largely why over time,
the graph shows a DECREASE in impacts - because the surface has been
resculpted by volcanic activity."
See, you're buddy truly think that the graph shows a decrease in impacts
because of the lava flow resetting the surface, whereas the graph show a
decrease in the DENSITY of craters because there is simply less
asteroids that impacts as time goes by.
The graph simply shows the expected crater density for a surface of a
given age.
That is all.
That Mars's crater density is much higher than the Earth's suggests
that the mean age
of its surface is much older, and the moon's even higher crater
density suggests that the
lunar surface is older still. The Earth's mean surface age is much
less because of geological
processes, i.e., erosion, plate tectonic recycling etc.
Quote: Even highschooler know that the frequency of asteroid impacts decrease
with time in the inner solar system.
I don't think George was arguing that premise.
Quote: For sure, If the frequency had been constant with time, that would have
been much easier to date surfaces, but that is not he case (see the work
of Hartmann, Neukum and Ivanov cited below.)
There are plenty of other works that made that case. What it is more
refined than previous studies using
more detailed maps of the Martian surface. In particular they were
able to test the hypothesis that small craters
were simply secondary impacts produced by major impacts.
Something else for you to ponder.
That crater density curve is constructed assuming Mars hasn't
expanded.
How do you suppose an expanding Mars would modify it?
Quote:
George's point flew right over your head.
Give me a break. See above. I don't even understand why you try to save
the scalp of a moron that can't understand an article nor read a graph
legend.
If your claiming the geologic activity is increasing on Mars, its
obvious you can't
read it either.
It would have been helpful if they included a histogram showing number
of lava
flows as a function of age.
What for?
Quote:
I wonder if you worth more than Georgie... I remember you were the one
stating that buoyancy is not related to pressure gradient. What a pity.
I said hydrostatic gradient was irrelevant.
It seems time plays tricks on your mind...
such as it is.
Stuart |
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