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M001
Sikhote-alin meteorite (Siberia-Russia)
The Sikhote-Alin
meteorite fell during daylight hours at 10.38am local
time on February 12, 1947, in the Sikhote-Alin
Mountains, about 270 miles northeast of
Vladivostok. Witnesses reported a fireball that
was brighter than the Sun. It came from the
north and left a trail of smoke and dust that
was 20 miles long.
(Cont...)
Weight: 0.212KG
Width: 6.3cm
Height: 3cm |
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M002
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
The speed of entry
was estimated to be about 31000 miles per hour, as it entered the atmosphere
where it began to
break apart. At an altitude of approximately 3.5
miles the largest mass apparently broke up in a
violent explosion, scattering fragments over
about a square kilometre.
(Cont...)
Weight: 0.142KG
Width: 6cm
Height: 4cm |
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M003
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
There are two
distinct types of Sikhote-Alin: shrapnel-like
fragments, resulting from the explosion, and
complete individuals which probably broke off
from the main mass early in the descent.
(Cont...)
Weight: 0.244KG
Width: 9.5cm
Height: 3.5cm |
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M004
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
The surfaces were
vaporised and eroded in the atmosphere such as
is visible on this specimen, producing
the sculpted cavities or regmalypts
("thumbprints"). These specimens often show an
ablation or fusion crust, which is a much
sought-after characteristic.
Weight: 0.614KG
Width: 9cm
Height: 4cm |
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M005
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
Total weight of
nickel-iron meteorite that reached the ground is
estimated by various researches to be 70 - 100
tons.
The largest
individual weighing in at 1,745 kilograms, was
excavated from crater No. 45, at a depth of 4 m.
Weight: 0.188KG
Width: 6.5cm
Height: 2.5cm |
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M006
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
Regular expeditions
began on site in late April 1947, after the
snow melted. The region was thoroughly examined.
Explorers found 24 major craters more than 9
meters across (the biggest one, No. 1, was 26 m
across and 6 m deep).
Weight: 0.154KG
Width: 7.5cm
Height: 3cm |
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M007
Sikhote-alin meteorite
(Siberia-Russia)
The Sikhote-Alin
meteorite fell during daylight hours at 10.38am local
time on February 12, 1947, in the Sikhote-Alin
Mountains, about 270 miles northeast of
Vladivostok. Witnesses reported a fireball that
was brighter than the Sun. It came from the
north and left a trail of smoke and dust that
was 20 miles long.
(Cont...)
Weight: 0.182KG
Width: 6.5cm
Height: 2cm |
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M008
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
The speed of entry
was estimated to be about 31000 miles per hour, as it entered the atmosphere it began to
break apart. At an altitude of approximately 3.5
miles the largest mass apparently broke up in a
violent explosion, scattering fragments over
about a square kilometre.
Weight: 0.262KG
Width: 8cm
Height: 3cm |
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M009
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
There are two
distinct types of Sikhote-Alin: shrapnel-like
fragments, resulting from the explosion, and
complete individuals which probably broke off
from the main mass early in the descent.
Weight: 0.162KG
Width: 6cm
Height: 3cm |
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M010
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
The surfaces were
vaporised and eroded in the atmosphere such as
is visible on this specimen, producing
the sculpted cavities or regmalypts
("thumbprints"). These specimens often show an
ablation or fusion crust, which is a much
sought-after characteristic.
Weight: 0.298KG
Width: 9cm
Height: 3cm |
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M011
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
Total weight of
nickel -iron meteorite iron that reached the ground is
estimated by various researches as 70 - 100
tons.
The largest
individual weighing in at 1,745 kilograms, was
excavated from crater No. 45, at depth of 4 m.
Weight: 0.242KG
Width: 7.5cm
Height: 3cm |
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M012
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
Regular expeditions
began on site late April 1947, after the
snow melted. The region was thoroughly examined.
Explorers found 24 major craters more than 9
meters across (the biggest one, No. 1, was 26 m
across and 6 m deep).
Weight: 0.452KG
Width: 10cm
Height: 3.5cm |
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M013
Sikhote-alin meteorite
(Siberia-Russia)
The Sikhote-Alin
meteorite fell during daylight hours at 10.38am local
time on February 12, 1947, in the Sikhote-Alin
Mountains, about 270 miles northeast of
Vladivostok. Witnesses reported a fireball that
was brighter than the Sun. It came from the
north and left a trail of smoke and dust that
was 20 miles long.
(...Cont)
Weight: 0.064KG
Width: 4cm
Height: 2cm |
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M014
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
The speed of entry
was estimated to be about 31000 miles per hour, as it entered the atmosphere it began to
break apart. At an altitude of approximately 3.5
miles the largest mass apparently broke up in a
violent explosion, scattering fragments over
about a square kilometre.
Weight: 0.046KG
Width: 4.3cm
Height: 1.5cm |
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M015
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
There are two
distinct types of Sikhote-Alin: shrapnel-like
fragments, resulting from the explosion, and
complete individuals which probably broke off
from the main mass early in the descent.
Weight: 0.086KG
Width: 5.5cm
Height: 2cm |
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M016
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
The surfaces were
vaporised and eroded in the atmosphere such as
is visible on the this specimen, producing
the sculpted cavities or regmalypts
("thumbprints"). These specimens often show an
ablation or fusion crust, which is a much
sought-after characteristic.
Weight: 0.086KG
Width: 5cm
Height: 2cm |
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M017
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
Total weight of
meteorite iron that reached the ground is
estimated by various researches as 70 - 100
tons.
The largest piece
of nickel-iron meteorite, which weighs 1,745 kilograms, was
excavated from crater No. 45, at depth of 4 m.
Weight: 0.058KG
Width: 4cm
Height: 2.7cm |
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M018
Sikhote-alin meteorite
(Siberia-Russia)
(...Cont)
Regular expeditions
began on site late April 1947, after the
snow melted. The region was thoroughly examined.
Explorers found 24 major craters more than 9
meters across (the biggest one, No. 1, was 26 m
across and 6 m deep).
Weight: 0.06KG
Width: 5cm
Height: 1.3cm |
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M019
Sikhote-alin meteorite
(Siberia-Russia)
The Sikhote-Alin
meteorite fell during daylight hours at 10.38am local
tine on February 12, 1947, in the Sikhote-Alin
Mountains, about 270 miles northeast of
Vladivostok. Witnesses reported a fireball that
was brighter than the Sun. It came from the
north and left a trail of smoke and dust that
was 20 miles long.
Weight: 0.06KG
Width: 5.5cm
Height: 1.5cm |
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M020
Giant
Sikhote-alin meteorite
(Siberia-Russia)
On the 12th of
February 1947 280 miles north east of
Vladivostok a rarely seen meteor shower blazed into the Earth’s
atmosphere at an approximate velocity of 50,000
kilometres per hour. This large specimen from the famous
Sikhote-alin fall displays orientation and regmalypts
("thumbprints"). A thin fusion crust provides evidence that this feature
was not produced by impact with the ground.
The fall of
Sikhote-alin left a trail of smoke and dust,
which was more than 30 kilometres long and lingered for several
hours; light and sound of the fall were observed
for two hundred miles around the point of
impact.
Weight: 80KG
Dimensions: 40 x 30
x 25cm |
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M021
Canyon
Diablo
Meteorite
(Meteor Crater, Arizona, USA)
Like most
meteorites, this specimen originated in the
asteroid belt. Circa 45,000 years
ago it was part of a small, errant asteroid that
crashed into the Arizona desert with the force
of more than 100 atomic bombs. While fragments
were dispersed in all directions for miles, the
main mass vaporized, creating the most famous
and best-preserved meteorite crater in the
world—the renowned Canyon Diablo “Meteor Crater”
near Winslow, Arizona—one mile across and nearly
2 hundred metres deep. Canyon Diablo (“Canyon of
the Devil”) is the quintessential American
meteorite, prized by both museums and private
collectors everywhere.
Weight: 10KG
Dimensions: 26 x 15
x 8cm |
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M022
A fine Gibeon meteorite (Namibia)
The
Gibeon meteorite field was first reported by
Captain T.E. Alexander in 1838 and is located in
Great Namaqualand in Namibia, South West Africa.
All iron
meteorites, including this one, emerged from the
core of a planet that briefly existed between
Mars and Jupiter and whose surviving fragments
are now referred to as the asteroid belt. This
meteorite is classified as a fine octahedrite
with widmanstatlen patterns as shown in the
accompanying slice(see MO23). The surface has been
sculptured by heat as the meteorite entered the earth's
atmosphere resulting in the classic "regmaglypts"
or "thumbprints" seen in this specimen.
Weight:
5.19KG
Width:
20cm
Height:
7cm |
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M023
A slice of Gibeon meteorite (Namibia)
Weight:
0.03KG
Width:
3.8cm
Height: 3.5cm |
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M024
An unusual
polished Sikhote Alin meteorite slice
(Siberia-Russia)
The Sikhote-Alin
meteorite fell during daylight hours at 10.38am local
tine on February 12, 1947, in the Sikhote-Alin
Mountains, about 270 miles northeast of
Vladivostok. Witnesses reported a fireball that
was brighter than the Sun. It came from the
north and left a trail of smoke and dust that
was 20 miles long.
weight:
0.384KG
Width:
7.5cm
Height:
12.5cm
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M025
Fukang
Pallasite meteorite slice (China)
Pallasite - stony iron meteorites come from the
interplanetary core of extinct planets. Olivine
crystallizes in this core during the development
of the planet. Later the planet breaks apart
becoming asteroids and luckily landing on earth
so we end up with this beautiful meteorite.
Found while digging a well, this highly desired pallasite contains 8.50% nickel with inclusions
of gem quality olivine crystals.
Weight: 0.090KG
Width: 9.6cm
Height: 7.1cm
Thickness: 0.3cm |
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M026
Fukang
Pallasite meteorite slice (China)
Pallasites are
primarily composed of olivine and Fe Ni-metal.
Most researchers agree that this mixture formed
after differentiation but before solidification
of the core of an asteroid. A variety of origins
for pallasites have been put forward including
crystallization near the surface of an
externally heated asteroid, crystallization of
an impact melt and nebular condensation.
However, the leading theory is that pallasites
were generated at the core- mantle interface of
a differentiated asteroid.
Weight: 0.026KG
Width: 9.5cm
Height: 5.1cm
Thickness: 0.1cm |
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M027
Fukang
Pallasite meteorite slice (China)
The
Fukang Pallasite
meteorite
was found in the mountains near
Fukang, China
in the year 2000. Pallasites are
a type of stony-iron meteorite
with
olivine.The
first time pallasites were seen
was in 1772. The German
Naturalist
Peter Simon Pallas
was shown a huge lump of strange
looking metal which had been
found in Siberia, near
Krasnoyarsk. It was soon
discovered that the metal lump
was a meteorite. These types of
meteorites are now called
Pallasites.
Weight: 0.034KG
Width: 9.5cm
Height: 5.1cm
Thickness: 0.1cm
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M028
Fukang
Pallasite meteorite slice (China)
Fukang are some of
the most beautiful Pallasite in the world.
Peridot is considered a highly desirable
gemstone and was prized by the ancient Egyptians
who used it extensively in their royal
jewellery. It can range in colour from green to
orange to yellow, all of these colours are
present in this incredible meteorite slice. Held
before the light, they burst into other worldly
life, assuring the viewer that what they see
could only be extra terrestrial in origin.
Weight: 0.112KG
Width: 9.5cm
Height: 5.6cm
Thickness: 0.4cm |
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M029
Fukang
Pallasite meteorite slice (China)
The Fukang
Pallasite
meteorite
was found in the mountains near
Fukang,
China in
the year 2000. Pallasites are a type of
stony-iron meteorite with
olivine
inclusions .The first time pallasites were seen
is in 1772. The German Naturalist
Peter Simon
Pallas was
shown a huge lump of strange looking metal which
had been found in Siberia, near Krasnoyarsk. It
was soon discovered that the metal lump was a
meteorite. These types of meteorites are now
called Pallasites.
Weight: 0.028KG
Width: 9.5cm
Height: 5.5cm
Thickness: 0.1cm |
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M030
Fukang
Pallasite meteorite slice (China)
Pallasites are
primarily composed of olivine and Fe Ni-metal.
Most researchers agree that this mixture formed
after differentiation but before solidification
of the core of an asteroid. A variety of origins
for pallasites have been put forward including
crystallization near the surface of an
externally heated asteroid, crystallization of
an impact melt and nebular condensation.
However, the leading theory is that pallasites
were generated at the core- mantle interface of
a differentiated asteroid.
Weight: 0.120KG
Width: 16.5cm
Height: 10cm
Thickness: 0.2cm |
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