This was looked into several times in the list history. I am recalling details 
from those discussions/my research.

Any body arriving from space is at least -60°c and closer to -120°c to -180°c 
based on some black body studies of asteroids-- IIRC


The temperature at the air-meteoroid boundary of entry exceeds the melting 
point of both iron and olivine. Most of that heat is carried off as an 
iron/silicate mist.  Each mili-second of incandescent flight an entirely new 
surface is formed. Inward traveling heat is being stripped away almost as fast 
as it is penetrating in low thermo-conducivity but much faster in high 
conductivity bodies (e.g iron).  The radiative cooling during dark flight is 
probably calculable and a missing factor in estimating the state of heat 
content upon landing.


One of the Weston CT meteorites formed a frost rind shortly after falling after 
sufficient time for all reentry heat to dissipate. I do not recall any other 
comments.  This was discovered by a fireman under the dining table.  I do not 
recall which other meteorite it was but, another was noted to have a frost rind 
after a few minutes. Other falls such as Sylacaga are silent as to the 
temperature.


Conclusions:

An immediately-recovered, newly-fallen silicate/stony meteorite is usually--but 
briefly "hot/uncomfortably warm" to the touch. The rind is very hot but lacks 
much heat reservoir. Heat penetration--based on measuring heated rims-- is 
somewhere between 2mm but not more than 6mm.  Beyond 6mm does not get above 
140° F proven by the domain reset of magnetite orientation in Martian 
Meteorites.  Be it remembered that an empty .50 cal brass case "feels" like it 
would burn you if it goes down one's shirt but lacks the heat content to cause 
burns.


Specific characterizations of hot/warm are hidden among the various accounts of 
some well known falls nearby humans. Monahans, Mbale, Allende, Murchison etc..  
If you disagree-- don't start some silly list fight--Do your own weeks of 
research reach your own conclusions!


Iron meteorites owing to a high coefficient of therm-conductivity are likely 
very hot to the touch and warm throughout. It is probably much like a piece of 
metal cut by a welding torch--no sign of bluing but very hot on the opposite 
end of the cut. 



Elton
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