|
MIACIron and Stony-iron Meteorites |
This meteorite was found in 1916 about 10 km north of Annaheim, a
settlement
somewhat about 100 km east of Saskatoon. It was discovered by Mr.
William
Huiras who was mowing hay on his farm. It is believed to be related to
a spectacular fireball observed some two years earlier. It is a
crescent
shaped medium octahedrite, with a mass of nearly 12
kg and showing
very clearly the dimpling or 'thumb-printing' of the surface which is
often
found on iron meteorites. The main mass is currently held in the
Canadian
National Meteorite Collection, Ottawa (Ref. R.A.A. Johnston &
H.V.
Ellsworth (1921): Trans. Roy. Soc. Canada., Sect. IV, p. 92.) (Photo
courtesy Geological Survey of Canada)
This meteorite from Chihuahua, Mexico is a medium octahedrite
with
an original mass of 1547 kg. It is particularly interesting because it
was found in an ancient tomb. Further details can be found in
Buchwald's
Handbook of Iron Meteorites. The slide shows a polished slab cut from
the
main mass, which has been etched to reveal the intricate intergrowth of
oriented kamacite bands known as the 'Widmanstätten
structure'. The
bands are oriented along the (III) (octahedral) planes of the original
metal which had the FCC taenite structure. Hence the name
'octahedrites'.
Medium octahedrites have kamacite band widths from 0.5-1.3 mm. (Photo
courtesy Geological Survey of Canada)
Three masses (38.6 kg, 18.6 and 10.6 kg) of this stony iron pallasite
were found near the Saskatchewan town of Springwater (120 km
west of
Saskatoon) in 1931. The meteorite is made up of 1/3 metal (kamacite and
taenite) and 2/3 olivine with minor amounts of other minerals,
including
the rare phosphate minerals farringtonite (Mg3(PO4)2)
and stanfieldite (Ca4(Mg,Fe)5(PO4)6)
and the more common phosphate - merrillite (= whitlockite, Ca3(PO4)2).
Even some of the olivine is P-rich. Only 35 pallasites are known and
thus
they are rather rare meteorites. They are also particularly attractive
as can be seen in this slide of a polished slab. (Photo courtesy
Geological Survey of Canada)