Sikhote Alin #4 Fer IIAB – shrapnel 13 g

39,64 $

The Sikhote-Alin meteorite is an iron meteorite that fell in Siberia in 1947. This fall is unique in the history of meteorites, given the 70 tonnes that survived the journey through the Earth’s atmospher

A fall that’s harder and harder to find.

 

Sikhote Alin #3 Fer IIAB – shrapnel 9,6 g

26,75 $

The Sikhote-Alin meteorite is an iron meteorite that fell in Siberia in 1947. This fall is unique in the history of meteorites, given the 70 tonnes that survived the journey through the Earth’s atmospher

A fall that’s harder and harder to find.

 

Sikhote Alin #2 Fer IIAB – shrapnel 20 g

55,49 $

The Sikhote-Alin meteorite is an iron meteorite that fell in Siberia in 1947. This fall is unique in the history of meteorites, given the 70 tonnes that survived the journey through the Earth’s atmospher

A fall that’s harder and harder to find.

 

Sikhote Alin #1 Fer IIAB – shrapnel 13,5 g

37,66 $

The Sikhote-Alin meteorite is an iron meteorite that fell in Siberia in 1947. This fall is unique in the history of meteorites, given the 70 tonnes that survived the journey through the Earth’s atmospher

A fall that’s harder and harder to find.

 

NWA 16774 Pallasite #10 – 11,8 g

467,68 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #9 – 6,4 g

285,37 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #8 – 5,9 g

262,57 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #7 – 3,6 g

160,52 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #6 – 3,9 g

195,20 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #5 – 4,7 g

210,07 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #4 – 2,8 g

124,85 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #3 – 2,3 g

103,06 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #2 – 2,5 g

110,98 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

NWA 16774 Pallasite #1 – 11,2 g

499,39 $

NWA 16774 is a pallasite-type meteorite discovered in Algeria in 2024, weighing just 4.5 kg.

Pallasites are unique stony-iron meteorites composed mainly of olivine and ferrous metal.
They are thought to have formed in the boundary region between the core and mantle of asteroids, inside asteroids.
Pallasites are meteorites composed of olivine crystals embedded in an iron-nickel matrix.
Pallasites are among the most aesthetically pleasing of meteorites.

 

 

Oued El Kechbi #41 L4 – 61,7 g

1.222,72 $

Oued El Kechbi is a chondrite L4 meteorite that fell in Morocco near the town of Akhfennir on March 3, 2023.

On March 3, 2023 at 14:00 GMT, nomadic sheep herders named Derija Bent Yahya, Abo bakr Aabidha, Brika weld Himdah and Elkhadir observed a fireball moving with a SE to NW trajectory falling in the desert region ~45km southwest of Akhfennir, Morocco.

When the meteor entered the atmosphere, the fireball was a yellowish-white color, accompanied by a sonic boom that scattered the rancher’s herd.
The meteorites discovered lie in a valley that contains desert cobbles separated by an abundance of small seasonal ponds.
The first samples were found in the mud, where the surface was wet with recent snow.
As the seasonal ponds dried, more samples were found.
The Moroccan Association of Meteorite Hunters recovered 20 samples with a total weight of 1942g. Further other discoveries have been made, bringing the total known weight to ~4764g. Coordinates and weight of discoveries indicate that the distribution ellipse is 4.3 km long, and confirm the SE to NW trajectory.

43 stones weighing 1036g were sold to Jean Redelsperger.

Physical characteristics: many stones are completely covered by a black molten crust. Some are oriented and larger stones have regmaglyptes and slickenside surfaces. The fragments found in the mud show oxidation stains on crusted surfaces and exposed interiors. The broken face shows that the interior is composed of light-gray chondrules, FeNi and troilite grains..

Oued El Kechbi #40 L4 – 64,4 g

1.276,22 $

Oued El Kechbi is a chondrite L4 meteorite that fell in Morocco near the town of Akhfennir on March 3, 2023.

On March 3, 2023 at 14:00 GMT, nomadic sheep herders named Derija Bent Yahya, Abo bakr Aabidha, Brika weld Himdah and Elkhadir observed a fireball moving with a SE to NW trajectory falling in the desert region ~45km southwest of Akhfennir, Morocco.

When the meteor entered the atmosphere, the fireball was a yellowish-white color, accompanied by a sonic boom that scattered the rancher’s herd.
The meteorites discovered lie in a valley that contains desert cobbles separated by an abundance of small seasonal ponds.
The first samples were found in the mud, where the surface was wet with recent snow.
As the seasonal ponds dried, more samples were found.
The Moroccan Association of Meteorite Hunters recovered 20 samples with a total weight of 1942g. Other
other discoveries were made, bringing the total known weight to ~4764g. Coordinates and weights of the finds
indicate that the distribution ellipse is 4.3 km long, and confirm the SE to NW trajectory.

43 stones weighing 1036g were sold to Jean Redelsperger.

Physical characteristics: many stones are completely covered by a black molten crust. Some are oriented
and larger stones have regmaglyptes and slickenside surfaces. The fragments
found in mud show oxidation stains on encrusted surfaces and exposed interiors. The broken face
shows that the interior is composed of light-grey chondrules, FeNi and troilite grains.

Oued El Kechbi #39 L4 – 61,3 g

1.214,80 $

Oued El Kechbi is a chondrite L4 meteorite that fell in Morocco near the town of Akhfennir on March 3, 2023.

On March 3, 2023 at 14:00 GMT, nomadic sheep herders named Derija Bent Yahya, Abo bakr Aabidha, Brika weld Himdah and Elkhadir observed a fireball moving with a SE to NW trajectory falling in the desert region ~45km southwest of Akhfennir, Morocco.

When the meteor entered the atmosphere, the fireball was a yellowish-white color, accompanied by a sonic boom that scattered the rancher’s herd.
The meteorites discovered lie in a valley that contains desert cobbles separated by an abundance of small seasonal ponds.
The first samples were found in the mud, where the surface was wet with recent snow.
As the seasonal ponds dried, more samples were found.
The Moroccan Association of Meteorite Hunters recovered 20 samples with a total weight of 1942g. Other
other discoveries were made, bringing the total known weight to ~4764g. Coordinates and weights of the finds
indicate that the distribution ellipse is 4.3 km long, and confirm the SE to NW trajectory.

43 stones weighing 1036g were sold to Jean Redelsperger.

Physical characteristics: many stones are completely covered by a black molten crust. Some are oriented
and larger stones have regmaglyptes and slickenside surfaces. The fragments
found in mud show oxidation stains on encrusted surfaces and exposed interiors. The broken face
shows that the interior is composed of light-grey chondrules, FeNi and troilite grains.

Oued El Kechbi #38 L4 – 75 g

1.486,28 $

Oued El Kechbi is a chondrite L4 meteorite that fell in Morocco near the town of Akhfennir on March 3, 2023.

On March 3, 2023 at 14:00 GMT, nomadic sheep herders named Derija Bent Yahya, Abo bakr Aabidha, Brika weld Himdah and Elkhadir observed a fireball moving with a SE to NW trajectory falling in the desert region ~45km southwest of Akhfennir, Morocco.

When the meteor entered the atmosphere, the fireball was a yellowish-white color, accompanied by a sonic boom that scattered the rancher’s herd.
The meteorites discovered lie in a valley that contains desert cobbles separated by an abundance of small seasonal ponds.
The first samples were found in the mud, where the surface was wet with recent snow.
As the seasonal ponds dried, more samples were found.
The Moroccan Association of Meteorite Hunters recovered 20 samples with a total weight of 1942g. Other
other discoveries were made, bringing the total known weight to ~4764g. Coordinates and weights of the finds
indicate that the distribution ellipse is 4.3 km long, and confirm the SE to NW trajectory.

43 stones weighing 1036g were sold to Jean Redelsperger.

Physical characteristics: many stones are completely covered by a black molten crust. Some are oriented
and larger stones have regmaglyptes and slickenside surfaces. The fragments
found in mud show oxidation stains on encrusted surfaces and exposed interiors. The broken face
shows that the interior is composed of light-grey chondrules, FeNi and troilite grains.