Trinitite #52 - 2,1 g

Trinitite #52 – 2,1 g

107,64 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #51 - 1,8 g

Trinitite #51 – 1,8 g

92,42 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitrite had taken on the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #50 - 2,8 g

Trinitite #50 – 2,8 g

143,92 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitrite had taken on the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #49 - 1,7 g

Trinitite #49 – 1,7 g

87,76 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #48 - 3 g

Trinitite #48 – 3 g

154,44 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitrite had taken on the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #47 - 1,3 g

Trinitite #47 – 1,3 g

66,70 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitite had taken the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Trinitite #46 - 3,9 g

Trinitite #46 – 3,9 g

201,24 $

Trinitite is a type of glass formed during the first nuclear test, known as Trinity, which took place in Alamogordo, New Mexico, on July 16, 1945.

Trinitite is formed by the vitrification of desert sand mixed with various components of the structure on which the bomb rested, as well as the bomb itself. Recently, researchers discovered that a piece of red trinitrite had taken on the form of a quasicrystal.

First discovered in the laboratory in the 1980s, quasicrystals also occur in nature, particularly in meteorites.

It should be noted that trinitite is not harmful to health.

 

 

 

 

 

Montoume #19 - 638 g

Montoume #19 – 638 g

58,50 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
The impact crater of the Rochechouart meteorite is called “Astroblème” because it is no longer visible following erosion.
There are several types of rocks :
Les brèches de type Babaudus, riche en verre à texture fluidale et en vacuoles
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.

 

Babaudus #8 - 254 g

Babaudus #8 – 254 g

30,42 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
The impact crater of the Rochechouart meteorite is called “Astroblème” because it is no longer visible following erosion.
There are several types of rocks :
Babaudus-type breccias, rich in fluid-textured glass and vacuoles, are found only in the center of the astroblast.
These breccias are contaminated with chromium, nickel and cobalt, metals coming mostly from the asteroid.
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.
Babaudus #7 - 243 g

Babaudus #7 – 243 g

29,24 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
The impact crater of the Rochechouart meteorite is called “Astroblème” because it is no longer visible following erosion.
There are several types of rocks :
Babaudus-type breccias, rich in fluid-textured glass and vacuoles, are found only in the center of the astroblast.
These breccias are contaminated with chromium, nickel and cobalt, metals coming mostly from the asteroid.
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.
Babaudus #6 - 166 g

Babaudus #6 – 166 g

22,22 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
The impact crater of the Rochechouart meteorite is called “Astroblème” because it is no longer visible following erosion.
There are several types of rocks :
Babaudus-type breccias, rich in fluid-textured glass and vacuoles, are found only in the center of the astroblast.
These breccias are contaminated with chromium, nickel and cobalt, metals coming mostly from the asteroid.
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.
Chassenon #10 - 84 g

Chassenon #10 – 84 g

17,56 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
Le cratère d’impact de la météorite de Rochechouart est appelé Astroblème car il n’est plus visible suite à l’érosion.
There are several types of rocks :
Babaudus-type breccias, rich in fluid-textured glass and vacuoles, are found only in the center of the astroblast.
These breccias are contaminated with chromium, nickel and cobalt, metals coming mostly from the asteroid.
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.
Rochechouart #8 - 142 g

Rochechouart #8 – 142 g

28,08 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
The impact crater of the Rochechouart meteorite is called “Astroblème” because it is no longer visible following erosion.
There are several types of rocks :
Babaudus-type breccias, rich in fluid-textured glass and vacuoles, are found only in the center of the astroblast.
These breccias are contaminated with chromium, nickel and cobalt, metals coming mostly from the asteroid.
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.
Chassenon #9 - 108 g

Chassenon #9 – 108 g

21,06 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
Le cratère d’impact de la météorite de Rochechouart est appelé Astroblème car il n’est plus visible suite à l’érosion.
There are several types of rocks :
Babaudus-type breccias, rich in fluid-textured glass and vacuoles, are found only in the center of the astroblast.
These breccias are contaminated with chromium, nickel and cobalt, metals coming mostly from the asteroid.
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.
Montoume #18 - 240 g

Montoume #18 – 240 g

35,10 $
An impactite is a terrestrial rock modified by the impact of a large meteorite.
These rocks contain an agglomeration of fallout dust and fragments.
The Rochechouart impactites were formed as a result of a meteorite impact about 207 million years ago in New Aquitaine in the Rochechouart district.
The impact crater of the Rochechouart meteorite is called “Astroblème” because it is no longer visible following erosion.
There are several types of rocks :
Les brèches de type Babaudus, riche en verre à texture fluidale et en vacuoles
The “breccias” of Montoume type, red because of their richness in iron, metal supposed to come from the asteroid.
The “breccias” of Chassenon type, debris of glass of greenish tint.
The “breccias” of Rochechouart type, contain little glass and are constituted of elements of varied size and lithology.

 

Ivoirite #2 - 7,3 gOut of stock

Ivoirite #2 – 7,3 g

1.024,92 $

Ivory tectites are the rarest tectites in the world.

I guarantee the authenticity of these ivories, they were purchased directly from the discoverer, Jean-Christophe Flabeau.

Jean-Christophe Flabeau acquired 120 of these tektites at a flea market. They were collected on a cotton plantation in Daoukro in western Ivory Coast between 1955 and 1970.

The parent crater, 10 km in diameter, is located in Ghana.

 

 

 

 

 

Ivory Coast tektite #1 - 9,4 g

Ivory Coast tektite #1 – 9,4 g

1.319,76 $

Ivory tectites are the rarest tectites in the world.

I guarantee the authenticity of these ivories, they were purchased directly from the discoverer, Jean-Christophe Flabeau.

Jean-Christophe Flabeau acquired 120 of these tektites at a flea market. They were collected on a cotton plantation in Daoukro in western Ivory Coast between 1955 and 1970.

The parent crater, 10 km in diameter, is located in Ghana.

 

 

 

 

 

Verre lybique #11 - 209 gOut of stock

Verre lybique #11 – 209 g

234,00 $

Libyan glass is a natural glass that is very rich in silica. It is believed to have been formed by the fusion of sand during an explosion or meteorite impact in the Great Sand Sea of the Libyan Desert in western Egypt. A cometary origin may also be considered. In fact, oblique impacts with closed angles can also melt a significant amount of rock.