It is thought that the original body would have been
about 4 x 4 x 1.5 m and would have fragmented shortly after entering the
earth's atmosphere at a low trajectory from a north-westerly direction
and that the pieces experienced burn-out causing their surface structure
to alter.
On the final stage of their
journey while burning through the
earth's atmosphere the Gibeon Meteorites were thermally altered. The
indentations on the surface can clearly be seen.
One of the
Gibeon Meteorites has been sliced in two parts in order that the interior
of the body can be seen. The metal is resistant to corrosion owing
to the percentage of Nickel.
- Astronomical Origin:
Thought to have been from an exploding supernova over 4 billion
years ago.
- Classification - Octahedrite:
The most common form of Iron-Alloy meteorites. The Gibeon Meteorites
composition is: 87% iron, 8% nickel ( Taenite, Gamm-fe with 8,5%:
Kamacite, Alpha-fe with 5,5% nickel - see Widmanstatten Pattern
below), 0,5% cobalt, 0,04% phosphorus
with small amounts of carbon, sulphur, chromium. Traces of zinc,
gallium, germanium and iridium are present.
- Meteor Trajectory:
Approximately 20 degrees from North-Westerly direction
- Collision with Earth:
Unknown, estimated between 200 - 220 million years ago
- Location Of Landing:
Elliptical area 275 x 100km (171 x 62 miles) Gibeon Area.
- Weights of Meteorites:
range from a few grams to in excess of 1 ton.
The 'Discovery': The first European to make
record of the unusual 'metal
rocks' that became known as the Gibeon Meteorites
was the British explorer Sir James
Edward Alexander in 1838 when travelling north of the Bethany mission
station. His enquiries of the local Nama people established that they
valued the metal pieces and when found, had been smelting them for use
as spear and arrow-heads for some generations.
He sent samples of the metallic objects to London
for the attention of the respected chemist John Herschel, where it was
established that they were of meteoritic origin.
In 1853 John Gibbs transported by
ox-wagon an 81kg sample sample of the Gibeon
Meteorites to Cape Town, from where it was shipped to London.
The meteorite was purchased by Prof. John Tennant a mineralogist
and to America.
Between 1911-1913 the Chief Geologist for the
Colonial Administration of German South West Africa prospected the
area and collected the know of remaining Gibeon Meteorites
specimens which were brought to
Windhoek, from where a number were donated to foreign museums and
prominent collectors.
Meteorites are
now protected by strict laws in Namibia. It is an offence to even
move one from its resting place.