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Old 18th February 2005, 12:19 AM   #88
nechesh
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Location: Cincinnati, OH
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Henk, indeed i do have Tammens Vol. 1 and i have read the passages over many times.I think the analysis of which he speaks is merely a way of determining the elemental components such as nickel, not the source from which they come. I don't believe it was necessary for Groneman to test blades to make the conclusion that they were meteorite. Groneman was a contemporary to the process. He knew a blade was meteroite probably because he knew the empu who made it, or the blade was well provenenced. He mayhave tested nickel content, but he was told they were from meteorites.
The meteorite analysis that Tammens sites is for strikes which took place on the other side of the world to Jawa, so while it is interesting it doesn't prove in any way that there were strikes previous to Prambanan that were used for pamor. He does metion four other meteorite sites on Jawa, Tjabe, Bandong, Ngarri and Djati Pengelon. Tjabe was ordinary stone Chondrite which fell in 1869, http://internt.nhm.ac.uk/cgi-bin/ear...y=T1210&index= , Bandong was a stone LL6 that fell in 1871, http://www.nyrockman.com/museum/bandong-80.htm , Djati Pengilon is also ordinary stone Chondrite and fell in 1884, http://internt.nhm.ac.uk/cgi-bin/ear...ey=D910&index= . I could find no records of the other one mentioned. Perhaps they have an alternative spelling. They all don't seem to have any iron/nickel content to speak of AND they struck in the latter half of the 19thC so
Free iron from heavem may indeed be free (unless it hits you ) but it certainly ain't common. MOST blades were not made with this stuff. MANY old blades didn't even use nickel to create pamor contrast.

Last edited by nechesh; 18th February 2005 at 01:04 AM.
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