[meteorite-list] Iranian Fireball Was Of Geophysical Origin
From: Charles Viau <cviau_at_meteoritecentral.com>
Date: Thu Apr 22 10:31:22 2004 Message-ID: <002001c3f255$c7894570$1800a8c0_at_chupa> This is a multi-part message in MIME format. ------=_NextPart_000_0021_01C3F22B.DEB33D70 Content-Type: text/plain; charset="us-ascii" Content-Transfer-Encoding: 7bit The 'bit of a stretch" comment in the same context as " just like we have Martian meteorites" is intentional. The gravitational forces on the Earth are higher, and there is a dense atmosphere related to Mars. It takes a much bigger impactor on earth to eject material at escape velocity than it would on Mars. Therefore, the amount of available material that could possibly find it's way back to Earth would be much less and should be rather rare. Who knows: as rare as a Venusian meteorite? No one has every classified one but you can bet your helmet that they are here somewhere. We only know that Mars and Lunar materials are here because we have been to those places and analyzed the chemical and geological properties of rocks, which were mostly basalts. The angle of impact would not be that important with an impactor like Chixilub, Sudbury, Vredfort, Chesapeake and probably Manicouagan. The size of these bodies would eject material even on a zenith trajectory. They would also punch such a vacuum hole in the atmosphere that it would suck out great quantities of molten matter that would go into earth orbit and most likely reenter the atmosphere producing tektites. The point here is that it does not require an extreme amount of physics to understand that there are pieces of this entire solar system all over the place. We just have to look at all of the impact craters that we can see in our neighborhood to understand that every planet has probably traded material with every other over the course of the last 4 billion years. CharlyV -----Original Message----- From: meteorite-list-admin_at_meteoritecentral.com [mailto:meteorite-list-admin_at_meteoritecentral.com] On Behalf Of MexicoDoug_at_aol.com Sent: Friday, February 13, 2004 11:13 AM To: meteorite-list_at_meteoritecentral.com Subject: Re: [meteorite-list] Iranian Fireball Was Of Geophysical Origin This topic was discussed a few weeks ago on the list, and it seems pretty convincing that Earth parented meteorites are elusive for good scientific reasoning - it seems that if conditions to produce them happened, that the material would be glass or a split planet Earth (a la did the moon come from Earth question we had recently). While it may be possible (though statistically highly improbable), it is important not to say it is "a bit of a stretch", "just like we have Martian meteorites here". Those statements taken together are misleading, to say the least. It is important to recognize that Earth and Mars are so different regarding atmospheric density (over 100X) / viscosity and to a much lesser degree gravity, that such an analogy is not based on astronomy and physics, but rather wishful thinking, with a general ignoring of scientific principles - i.e. a solution (Earth parented meteorites exist because I can think it and there are Martian meteorites here) looking for a problem (Why no one has ever confirmed an Earth parented meteorite). Extending that logic, I would ask where the Solar parented meteorites are at, and while we are at it the Jovian parented and Venusian parented meteorites as well. The conditions on Mars simply do not lend themselves for comparison to Earth. Venus is a better comparison for Earth. Perhaps someone could work out the physics to show what sort of impactor on Earth is capable of causings something besides glass and giving it escape velocity. Without doing the physics, it is clear it would have to be a kilometer plus sized impactor imparting in an instant to a kilometer plus sized Earth rock escape velocity plus frictional loss velocity, which further does not explode with that velocity at sea level as it makes its way through the exponientially most dense part of the atmosphere (i.e. a "reverse meteorite") at a right or obtuse angle to the impact (which tends to create a velocity vector landing back on Earth). While this might sound "plausible", for an impactor to produce a kilometer plus sized rock with such a velocity seems nearly impossible, knowing the characteristics of Earth surface features. To actually achieve the above, either ground zero has to become liquid or plasma eventually producing glasses, for which there is some evidence in tektites, or Earth must be split like a nut, for which the Moon was presented as evidence in such a hypothethised impact around 4.5 billion years ago.... So that would leave a scenario of a gigantic impactor hitting near the base of a Mount Everest made of solid iron or other high tensile type structure, incoming at a low entry angle, and propelling the peak into outer space. In the case of Mars objects over 10 meters (but probably in the realm 500 km) can impact whole much more readily and produce "reverse meteorites" with the initial velocities potentially conducive to this event which can escape more readily as gravity (and hence resulting escape velocities) is less than 40% Earth's. Furthermore Mars is closer to the Asteroid belt and is expected to have more flux of such potential impacts. Saludos Doug Dawn Mexico En un mensaje con fecha 02/13/2004 8:21:52 AM Mexico Standard Time, cviau_at_beld.net escribe: and bit of a stretch.. but plausible: Just like we have Martian meteorites here on earth, so would we not have some of the ejecta from our terrestrial impacts also in orbit around the Sun ------=_NextPart_000_0021_01C3F22B.DEB33D70 Content-Type: text/html; charset="us-ascii" Content-Transfer-Encoding: quoted-printable <html xmlns:o=3D"urn:schemas-microsoft-com:office:office" = xmlns:w=3D"urn:schemas-microsoft-com:office:word" = xmlns:st1=3D"urn:schemas-microsoft-com:office:smarttags" = xmlns=3D"http://www.w3.org/TR/REC-html40"> <head> <META HTTP-EQUIV=3D"Content-Type" CONTENT=3D"text/html; = charset=3Dus-ascii"> <meta name=3DProgId content=3DWord.Document> <meta name=3DGenerator content=3D"Microsoft Word 10"> <meta name=3DOriginator content=3D"Microsoft Word 10"> <link rel=3DFile-List href=3D"cid:filelist.xml_at_01C3F22B.DB7CA380"> <o:SmartTagType = namespaceuri=3D"urn:schemas-microsoft-com:office:smarttags" name=3D"City"/> <o:SmartTagType = namespaceuri=3D"urn:schemas-microsoft-com:office:smarttags" name=3D"place"/> <!--[if gte mso 9]><xml> <o:OfficeDocumentSettings> <o:DoNotRelyOnCSS/> </o:OfficeDocumentSettings> </xml><![endif]--><!--[if gte mso 9]><xml> <w:WordDocument> <w:SpellingState>Clean</w:SpellingState> <w:GrammarState>Clean</w:GrammarState> <w:DocumentKind>DocumentEmail</w:DocumentKind> <w:EnvelopeVis/> <w:BrowserLevel>MicrosoftInternetExplorer4</w:BrowserLevel> </w:WordDocument> </xml><![endif]--><!--[if !mso]> <style> st1\:*{behavior:url(#default#ieooui) } </style> <![endif]--> <style> <!-- /* Font Definitions */ _at_font-face {font-family:Tahoma; panose-1:2 11 6 4 3 5 4 4 2 4; mso-font-charset:0; mso-generic-font-family:swiss; mso-font-pitch:variable; mso-font-signature:1627421319 -2147483648 8 0 66047 0;} /* Style Definitions */ p.MsoNormal, li.MsoNormal, div.MsoNormal {mso-style-parent:""; margin:0in; margin-bottom:.0001pt; mso-pagination:widow-orphan; font-size:12.0pt; font-family:"Times New Roman"; mso-fareast-font-family:"Times New Roman";} a:link, span.MsoHyperlink {color:blue; text-decoration:underline; text-underline:single;} a:visited, span.MsoHyperlinkFollowed {color:purple; text-decoration:underline; text-underline:single;} span.EmailStyle17 {mso-style-type:personal-reply; mso-style-noshow:yes; mso-ansi-font-size:10.0pt; mso-bidi-font-size:10.0pt; font-family:Arial; mso-ascii-font-family:Arial; mso-hansi-font-family:Arial; mso-bidi-font-family:Arial; color:navy;} span.SpellE {mso-style-name:""; mso-spl-e:yes;} span.GramE {mso-style-name:""; mso-gram-e:yes;} _at_page Section1 {size:8.5in 11.0in; margin:1.0in 1.25in 1.0in 1.25in; mso-header-margin:.5in; mso-footer-margin:.5in; mso-paper-source:0;} div.Section1 {page:Section1;} --> </style> <!--[if gte mso 10]> <style> /* Style Definitions */=20 table.MsoNormalTable {mso-style-name:"Table Normal"; mso-tstyle-rowband-size:0; mso-tstyle-colband-size:0; mso-style-noshow:yes; mso-style-parent:""; mso-padding-alt:0in 5.4pt 0in 5.4pt; mso-para-margin:0in; mso-para-margin-bottom:.0001pt; mso-pagination:widow-orphan; font-size:10.0pt; font-family:"Times New Roman";} </style> <![endif]--> </head> <body lang=3DEN-US link=3Dblue vlink=3Dpurple = style=3D'tab-interval:.5in'> <div class=3DSection1> <p class=3DMsoNormal><font size=3D2 color=3Dnavy face=3DArial = PTSIZE=3D10 FAMILY=3DSANSSERIF><span = style=3D'font-size:10.0pt;font-family:Arial;color:navy'>The ‘bit of a stretch” comment in the same context <span = class=3DGramE>as ”</span> </span></font><font size=3D2 face=3DArial><span = style=3D'font-size: 10.0pt;font-family:Arial'>just like we have Martian meteorites” is intentional. <span style=3D'mso-spacerun:yes'> </span>The = gravitational forces on the Earth are higher, and there is a dense atmosphere related = to Mars. It takes a much bigger <span class=3DSpellE>impactor</span> on = earth to eject material at escape velocity than it would on Mars. Therefore, the = amount of available material that could possibly find <span = class=3DGramE>it’s</span> way back to Earth would be much less and should be rather rare. <span style=3D'mso-spacerun:yes'> </span>Who knows: as rare as a <span class=3DSpellE>Venusian</span> meteorite?<span style=3D'mso-spacerun:yes'> </span>No one has every = classified one but you can bet your helmet that they are here somewhere. We only know = that Mars and Lunar materials are here because we have been to those places = and analyzed the chemical and geological properties of rocks, which were = mostly basalts.<o:p></o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'><o:p> </o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'>The angle of impact would not be that important with = an <span class=3DSpellE>impactor</span> like <span = class=3DSpellE>Chixilub</span>, </span></font><st1:City><st1:place><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt;font-family:Arial'>Sudbury</span></font></st1:p= lace></st1:City><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt;font-family:Arial'>, <span class=3DSpellE>Vredfort</span>, </span></font><st1:City><st1:place><font = size=3D2 face=3DArial><span = style=3D'font-size:10.0pt;font-family:Arial'>Chesapeake</span></font></st= 1:place></st1:City><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt;font-family:Arial'> and probably <span = class=3DSpellE>Manicouagan</span>.<o:p></o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'>The size of these bodies would eject material even on = a zenith trajectory. <span style=3D'mso-spacerun:yes'> </span>They = would also punch such a vacuum hole in the atmosphere that it would suck out great = quantities of molten matter that would go into earth orbit <span class=3DGramE>and = <span style=3D'mso-spacerun:yes'> </span>most</span> likely reenter the = atmosphere producing tektites.<o:p></o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'><o:p> </o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'>The point here is that it does not require an extreme = amount of physics to understand that there are pieces of this entire solar = system all over the place. We just have to look at all of the impact craters that = we can see in our neighborhood to understand that every planet has probably = traded material with every other over the course of the last 4 billion = years.<o:p></o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'><o:p> </o:p></span></font></p> <p class=3DMsoNormal><font size=3D2 face=3DArial><span = style=3D'font-size:10.0pt; font-family:Arial'>CharlyV<font color=3Dnavy><span = style=3D'color:navy'><o:p></o:p></span></font></span></font></p> <p class=3DMsoNormal><font size=3D2 color=3Dnavy face=3DArial><span = style=3D'font-size: 10.0pt;font-family:Arial;color:navy'><o:p> </o:p></span></font></p> <p class=3DMsoNormal style=3D'margin-left:.5in'><font size=3D2 = face=3DTahoma><span style=3D'font-size:10.0pt;font-family:Tahoma'>-----Original = Message-----<br> <b><span style=3D'font-weight:bold'>From:</span></b> = meteorite-list-admin_at_meteoritecentral.com [mailto:meteorite-list-admin_at_meteoritecentral.com] <b><span = style=3D'font-weight: bold'>On Behalf Of </span></b>MexicoDoug_at_aol.com<br> <b><span style=3D'font-weight:bold'>Sent:</span></b> Friday, February = 13, 2004 11:13 AM<br> <b><span style=3D'font-weight:bold'>To:</span></b> meteorite-list_at_meteoritecentral.com<br> <b><span style=3D'font-weight:bold'>Subject:</span></b> Re: = [meteorite-list] Iranian Fireball Was Of Geophysical Origin</span></font></p> <p class=3DMsoNormal style=3D'margin-left:.5in'><font size=3D3 = face=3D"Times New Roman"><span style=3D'font-size:12.0pt'><o:p> </o:p></span></font></p> <p class=3DMsoNormal style=3D'margin-left:.5in'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>This topic was discussed a = few weeks ago on the list, and it seems pretty convincing that Earth parented = meteorites are elusive for good scientific reasoning - it seems that if conditions = to produce them happened, that the material would be glass or a split = planet Earth (a la did the moon come from Earth question we had recently). <br> <br> While it may be possible (though statistically highly improbable), it is important not to say it is "a bit of a stretch", "just = like we have Martian meteorites here".<br> <br> Those statements taken together are misleading, to say the least.<br> <br> It is important to recognize that Earth and Mars are so different = regarding atmospheric density (over 100X) / viscosity and to a much lesser degree gravity, that such an analogy is not based on astronomy and physics, but = rather wishful thinking, with a general ignoring of scientific principles - = i.e. a solution (Earth parented meteorites exist because I can think it and = there are Martian meteorites here) looking for a problem (Why no one has ever = confirmed an Earth parented meteorite).<br> <br> Extending that logic, I would ask where the Solar parented meteorites = are at, and while we are at it the Jovian parented and Venusian parented meteorites as well. The conditions on Mars simply do not lend = themselves for comparison to Earth. Venus is a better comparison for = Earth. Perhaps someone could work out the physics to show what sort of impactor = on Earth is capable of causings something besides glass and giving it = escape velocity.<br> <br> Without doing the physics, it is clear it would have to be a kilometer = plus sized impactor imparting in an instant to a kilometer plus sized Earth = rock escape velocity plus frictional loss velocity, which further does not = explode with that velocity at sea level as it makes its way through the = exponientially most dense part of the atmosphere (i.e. a "reverse meteorite") = at a right or obtuse angle to the impact (which tends to create a velocity = vector landing back on Earth). While this might sound = "plausible", for an impactor to produce a kilometer plus sized rock with such a velocity = seems nearly impossible, knowing the characteristics of Earth surface = features.<br> <br> To actually achieve the above, either ground zero has to become liquid = or plasma eventually producing glasses, for which there is some evidence in tektites, or Earth must be split like a nut, for which the Moon was = presented as evidence in such a hypothethised impact around 4.5 billion years = ago....<br> <br> So that would leave a scenario of a gigantic impactor hitting near the = base of a Mount Everest made of solid iron or other high tensile type structure, incoming at a low entry angle, and propelling the peak into outer = space.<br> <br> In the case of Mars objects over 10 meters (but probably in the realm = 500 km) can impact whole much more readily and produce "reverse = meteorites" with the initial velocities potentially conducive to this event which = can escape more readily as gravity (and hence resulting escape velocities) = is less than 40% Earth's. Furthermore Mars is closer to the Asteroid belt = and is expected to have more flux of such potential impacts.<br> <br> Saludos<br> Doug Dawn<br> Mexico<br> <br> En un mensaje con fecha 02/13/2004 8:21:52 AM Mexico Standard Time, cviau_at_beld.net escribe:<br> <br style=3D'mso-special-character:line-break'> <![if !supportLineBreakNewLine]><br = style=3D'mso-special-character:line-break'> <![endif]><o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'margin-left:.5in'><font size=3D2 = face=3DArial><span style=3D'font-size:10.0pt;font-family:Arial'>and bit of a stretch.. but plausible: Just like we have<br> Martian meteorites here on earth, so would we not have some of the<br> ejecta from our terrestrial impacts also in orbit around the = Sun<o:p></o:p></span></font></p> <p class=3DMsoNormal style=3D'margin-left:.5in'><font size=3D3 = face=3DArial><span style=3D'font-size:12.0pt;font-family:Arial'><o:p> </o:p></span></fo= nt></p> </div> </body> </html> ------=_NextPart_000_0021_01C3F22B.DEB33D70-- Received on Fri 13 Feb 2004 12:21:07 PM PST |
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