[meteorite-list] Serious question? Now into RED EARTH
From: Charles R. Viau <cviau_at_meteoritecentral.com>
Date: Thu Apr 22 10:29:58 2004 Message-ID: <002d01c37e5c$7eab4370$1800a8c0_at_chupa> There are some serious red soils on the eastern seaboard as well. Parts of Virginia and South Carolina have some of the reddest soil you will ever find. (Interestingly, very near the Chesapeake Bay impact structure, ~100 km wide and of age 35Ma), and for the master of the red dirt, you have Prince Edward Island, in the Canadian Maritimes. The soil there is so red , that it can permanently stained your clothes if you sit in it. They even sell tee shirts that have been soaked in the stuff, and are permanently dyed. Much of Underlying Nova Scotia has this red soil as well, and interesting again is that it borders the off shore impact crater Montagnais, a 45 km wide structure aged about 50ma Almost as close is the impact structure Charlevoix, a 54 km wide crater of age ~350Ma. I don't know if any of this iron-rich soil and sandstone has anything to do with the impact structures, but they are topographic cousins in any case. -----Original Message----- From: meteorite-list-admin_at_meteoritecentral.com [mailto:meteorite-list-admin_at_meteoritecentral.com] On Behalf Of Kevin Fly Hill Sent: Thursday, September 18, 2003 11:17 AM To: meteorite-list_at_meteoritecentral.com Subject: Re: [meteorite-list] Serious question? If you want to speculate on "rusting impactors" you may not have to go quite so far. Come on over to East Texas (and many points in the southeast US) -- Everything -- from the clay to the rock is red and much of it (the rock) is magnetic. In fact the main road bed material in use out here is called "iron ore gravel". They dig this stuff up and process out gravel that is as red, orange and black as mars looks on any pictures I've seen. Much of the farmland around here has a deep layer of white/beige sand, but underneath at some point is red clay/rock sedimentary formation. We have the Marquez impactor site just south of us????? Also in central Texas in and around Bastrop (east of Austin) is a roughly circular area several miles across know as the Lost Pines. It is an area of pine trees, red acid soil/clay that is surrounded by post oak savannah, alkaline soil/limestone. Never have heard what caused this area to be where it is??? Very old impactor site??? Who knows -- maybe some of those teasips at tu in Austin. (from an Aggie Dad) Fly Hill ----- Original Message ----- From: "mark ford" <markf_at_ssl.gb.com> To: <meteorite-list_at_meteoritecentral.com> Sent: Thursday, September 18, 2003 6:13 AM Subject: RE: [meteorite-list] Serious question? > Chris > > Interesting points! > > I think the temperature on mars might also have something to do with the > existence of iron rich 'red soil', frost thaw frost thaw for billions of > years, would create a fine dust, in its self would it not? > > Anyone fancy crushing a cold Martian meteorite in rarified CO2 and water > and seeing if it eventually goes red? :) > > ..If you think mars Mars is a floating chemistry, set take a look at > some of the Galliean moons WOW! > > > Mark F > > -----Original Message----- > From: chris sharp [mailto:casper_at_cooloola.net] > Sent: 18 September 2003 11:55 > To: Charles R. Viau > Cc: meteorite-list_at_meteoritecentral.com > Subject: Re: [meteorite-list] Serious question? > > How about a large iron impacting the Northern hemisphere of Mars > creating an impact basin now filled by lava and mud. > > The iron impactor disintegrated and spread iron all over the planet in > a fallout cloud and created a layer of iron rich material on the > surface. > > The weather on Mars continues to spread the meteorite material around. > Other large scale impacts have created layered regolith. The lack of > water erosional processes allow us to see the impact debris still > scattered all over the surface. > > regards to all in meteorite land > > chris sharp > my2c > > ----- Original Message ----- > From: "Charles R. Viau" <cviau_at_beld.net> > To: "'Philip R. Burns'" <pib_at_pibburns.com>; > <meteorite-list_at_meteoritecentral.com> > Sent: Thursday, September 18, 2003 10:55 AM > Subject: RE: [meteorite-list] Serious question? > > > > Thanks, > > I understand the difference much better in that context. > > I love this list, where else can you get info like this!!! > > > > CharlyV > > > > -----Original Message----- > > From: meteorite-list-admin_at_meteoritecentral.com > > [mailto:meteorite-list-admin_at_meteoritecentral.com] On Behalf Of > Philip > > R. Burns > > Sent: Wednesday, September 17, 2003 8:49 PM > > To: meteorite-list_at_meteoritecentral.com > > Subject: RE: [meteorite-list] Serious question? > > > > At 08:32 PM 9/17/2003 -0400, you wrote: > > > > >Ok, so for the symantics of that definition, would you call that a > > >reduction reaction not involving oxygen, and not oxidation.. ? > > > > In general, oxidation is the loss of electrons, and reduction is the > > gain > > of electrons. Those terms are used in modern chemistry whether or > not > > oxygen is involved. > > > > -- Philip R. "Pib" Burns > > pib_at_pibburns.com > > http://www.pibburns.com/ > > > > > > ______________________________________________ > > Meteorite-list mailing list > > Meteorite-list_at_meteoritecentral.com > > http://www.pairlist.net/mailman/listinfo/meteorite-list > > > > > > > > ______________________________________________ > > Meteorite-list mailing list > > Meteorite-list_at_meteoritecentral.com > > http://www.pairlist.net/mailman/listinfo/meteorite-list > > > > > > > ______________________________________________ > Meteorite-list mailing list > Meteorite-list_at_meteoritecentral.com > http://www.pairlist.net/mailman/listinfo/meteorite-list > > ______________________________________________ > Meteorite-list mailing list > Meteorite-list_at_meteoritecentral.com > http://www.pairlist.net/mailman/listinfo/meteorite-list ______________________________________________ Meteorite-list mailing list Meteorite-list_at_meteoritecentral.com http://www.pairlist.net/mailman/listinfo/meteorite-list Received on Thu 18 Sep 2003 11:16:56 PM PDT |
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