{"title":"Brahim","description":null,"products":[{"product_id":"meteorite-pallasit-brahin-57g-extra-quality-belarus-mebr41","title":"Meteorite Pallasite Brahin 5.7g – Extra Quality – Belarus - MEBR41","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 5.7g\u003c\/li\u003e\n\u003cli\u003eDimensions: 21 x 20 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers in length and 3 kilometers in width and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Over the 19th and 20th centuries, larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix primarily consists of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and together with it constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027643502917,"sku":"MEBR41","price":334.81,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/61274_photoroom-013-20251027-162938.jpg?v=1779377500"},{"product_id":"meteorite-pallasit-brahin-21g-extra-quality-belarus-mebr69","title":"Meteorite Pallasite Brahin 2.1g – Extra Quality – Belarus - MEBR69","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.1g\u003c\/li\u003e\n\u003cli\u003eSize: 21 x 9 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery occurred thanks to local residents, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix consists primarily of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivine present in the Brahin meteorite is often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit green to brown hues, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027651662149,"sku":"MEBR69","price":126.04,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67329_meteorite-pallasit-brahin-2-1g---extra-quality---belarus.jpg?v=1779377518"},{"product_id":"brahin-pallasite-meteorite-72g-belarus-mebr03","title":"Brahin Pallasite Meteorite 7.2g – Belarus - MEBR03","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 7.2g\u003c\/li\u003e\n\u003cli\u003eDimensions: 3.1 x 2 x 0.2 cm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, more larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix consists primarily of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, significantly increasing the aesthetic value of the material. They generally exhibit green to brown hues, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and the mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027670143301,"sku":"MEBR03","price":255.31,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/15979_brahin-pallasite-meteorite-7-2g---belarus.jpg?v=1779377560"},{"product_id":"meteorite-brahin-19g-extra-quality-belarus-mebr26","title":"Meteorite Brahin 1.9g – Extra Quality – Belarus - MEBR26","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 1.9g\u003c\/li\u003e\n\u003cli\u003eDimensions: 15 x 11 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in roughly equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix primarily consists of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-grey in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, significantly increasing the material's aesthetic value. They generally display green to brown hues, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027784110405,"sku":"MEBR26","price":122.81,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56279_meteorite-brahin-1-9g---extra-quality---belarus.jpg?v=1779377807"},{"product_id":"meteorite-brahin-16g-extra-quality-belarus-mebr25","title":"Meteorite Brahin 1.6g – Extra Quality – Belarus - MEBR25","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 1.6g\u003c\/li\u003e\n\u003cli\u003eSize: 15 x 9 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide, and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. During the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and the mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027784143173,"sku":"MEBR25","price":103.42,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56276_meteorite-brahin-1-6g---extra-quality---belarus.jpg?v=1779377807"},{"product_id":"meteorite-brahin-19g-extra-quality-belarus-mebr23","title":"Meteorite Brahin 1.9g – Extra Quality – Belarus - MEBR23","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 1.9g\u003c\/li\u003e\n\u003cli\u003eSize: 13 x 13 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. Over the course of the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is composed primarily of iron and nickel. The metallic matrix consists mainly of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally range in color from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027784241477,"sku":"MEBR23","price":122.81,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56270_meteorite-brahin-1-9g---extra-quality---belarus.jpg?v=1779377808"},{"product_id":"meteorite-brahin-19g-extra-quality-belarus-mebr21","title":"Meteorite Brahin 1.9g – Extra Quality – Belarus - MEBR21","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 1.9g\u003c\/li\u003e\n\u003cli\u003eDimensions: 15 x 10 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. Over the 19th and 20th centuries, more larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix primarily consists of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-grey in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly increasing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027784274245,"sku":"MEBR21","price":122.81,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/50774_meteorite-brahin-1-9g---extra-quality---belarus.jpg?v=1779377809"},{"product_id":"meteorite-pallasit-brahin-23g-extra-quality-belarus-mebr58","title":"Meteorite Pallasite Brahin 2.3g – Extra Quality – Belarus - MEBR58","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.3g\u003c\/li\u003e\n\u003cli\u003eDimensions: 20 x 9 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local residents, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. During the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027908923717,"sku":"MEBR58","price":141.55,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67296_photoroom-20260203-232208.jpg?v=1779378205"},{"product_id":"meteorite-pallasit-brahin-24g-extra-quality-belarus-mebr67","title":"Meteorite Pallasite Brahin 2.4g – Extra Quality – Belarus - MEBR67","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.4g\u003c\/li\u003e\n\u003cli\u003eSize: 14 x 12 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eTotal known weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is composed mainly of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivine present in the Brahin meteorite is often large, clear, and beautifully translucent, significantly increasing the aesthetic value of the material. They generally have shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027909316933,"sku":"MEBR67","price":145.44,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67323_meteorite-pallasit-brahin-2-4g---extra-quality---belarus.jpg?v=1779378206"},{"product_id":"meteorite-pallasit-brahin-24g-extra-quality-belarus-mebr46","title":"Pallasite Meteorite Brahin 2.4g – Extra Quality – Belarus - MEBR46","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.4g\u003c\/li\u003e\n\u003cli\u003eSize: 20 x 11 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix consists primarily of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027910463813,"sku":"MEBR46","price":145.44,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67260_meteorite-pallasit-brahin-2-4g---extra-quality---belarus.jpg?v=1779378207"},{"product_id":"meteorite-pallasit-brahin-24g-extra-quality-belarus-mebr81","title":"Pallasite Brahin Meteorite 2.4g – Extra Quality – Belarus - MEBR81","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.4g\u003c\/li\u003e\n\u003cli\u003eDimensions: 14 x 12 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003ePackaging: transparent plastic box (5.8 x 3.8 x 1.6 cm)\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. During the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivine crystals present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally range in color from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and the mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027910857029,"sku":"MEBR81","price":158.36,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67930_meteorite-pallasit-brahin-2-4g---extra-quality---belarus.jpg?v=1779378210"},{"product_id":"meteorite-pallasit-brahin-25g-extra-quality-belarus-mebr50","title":"Pallasite Brahin Meteorite 2.5g – Extra Quality – Belarus - MEBR50","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.5g\u003c\/li\u003e\n\u003cli\u003eDimensions: 21 x 10 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027910922565,"sku":"MEBR50","price":151.9,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67272_meteorite-pallasit-brahin-2-5g---extra-quality---belarus.jpg?v=1779378210"},{"product_id":"meteorite-pallasit-brahin-25g-extra-quality-belarus-mebr54","title":"Pallasite Meteorite Brahin 2.5g – Extra Quality – Belarus - MEBR54","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.5g\u003c\/li\u003e\n\u003cli\u003eSize: 22 x 9 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is bisected by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, more large fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, forms the main structural component of the metallic iron-nickel phase. The olivine present in the Brahin meteorite is often large, clear, and beautifully translucent, significantly enhancing the aesthetic value of the material. They generally range in shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body that formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies that formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58027910955333,"sku":"MEBR54","price":151.9,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67284_photoroom-20260203-230109.jpg?v=1779378210"},{"product_id":"meteorite-pallasit-individual-brahin-256g-belarus-mebr94","title":"Meteorite Pallasite individual Brahin 25.6g – Belarus - MEBR94","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 25.6g\u003c\/li\u003e\n\u003cli\u003eDimensions: 54 x 30 x 14 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: none - Raw\u003c\/li\u003e\n\u003cli\u003eNote: A cluster of olivine crystals can be seen on the surface\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is composed mainly of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-grey in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivine crystals present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028152127813,"sku":"MEBR94","price":1225.52,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/74238_meteorite-pallasit-individual-brahin-25-6g---belarus.jpg?v=1779381104"},{"product_id":"meteorite-pallasit-individual-brahin-303g-belarus-mebr93","title":"Meteorite Pallasite individual Brahin 30.3g – Belarus - MEBR93","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 30.3g\u003c\/li\u003e\n\u003cli\u003eDimensions: 49 x 39 x 22 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: none - Rough\u003c\/li\u003e\n\u003cli\u003eNote: A cluster of olivine crystals can be seen on the surface\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is primarily composed of iron and nickel. The metallic matrix consists mainly of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, significantly increasing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028271993157,"sku":"MEBR93","price":1471.77,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/74235_meteorite-pallasit-individual-brahin-30-3g---belarus.jpg?v=1779382062"},{"product_id":"brahin-pallasite-meteorite-27g-belarus-mebr04","title":"Brahin Pallasite Meteorite 2.7g – Belarus - MEBR04","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.7g\u003c\/li\u003e\n\u003cli\u003eDimensions: 1.6 x 1.6 x 0.2 cm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers in length and 3 kilometers in width and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix consists primarily of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the metallic iron-nickel phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, significantly increasing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and the mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028597674309,"sku":"MEBR04","price":96.96,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/15982_brahin-pallasite-meteorite-2-7g---belarus.jpg?v=1779383288"},{"product_id":"meteorite-pallasit-brahin-16g-extra-quality-belarus-mebr76","title":"Pallasite Brahin Meteorite 1.6g – Extra Quality – Belarus - MEBR76","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 1.6g\u003c\/li\u003e\n\u003cli\u003eDimensions: 16 x 10 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003ePackaging: transparent plastic box (5.8 x 3.8 x 1.6 cm)\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's dispersion field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028600164677,"sku":"MEBR76","price":96.31,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67915-2_meteorite-pallasit-brahin-1-6g---extra-quality---belarus.jpg?v=1779383305"},{"product_id":"meteorite-pallasit-brahin-22g-extra-quality-belarus-mebr57","title":"Pallasite Meteorite Brahin 2.2g – Extra Quality – Belarus - MEBR57","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.2g\u003c\/li\u003e\n\u003cli\u003eSize: 21 x 9 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eTotal known weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily made up of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the metallic iron-nickel phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly increasing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028600623429,"sku":"MEBR57","price":128.63,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/67293_photoroom-20260203-231503.jpg?v=1779383314"},{"product_id":"brahin-pallasite-meteorite-55g-belarus-mebr06","title":"Brahin Pallasite Meteorite 5.5g – Belarus - MEBR06","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 5.5g\u003c\/li\u003e\n\u003cli\u003eSize: 2 x 2 x 0.2 cm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is primarily composed of iron and nickel. The metallic matrix is mainly composed of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-grey in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and the mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028600820037,"sku":"MEBR06","price":193.27,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/15988-3_brahin-pallasite-meteorite-5-5g---belarus.jpg?v=1779383317"},{"product_id":"meteorite-brahin-21g-extra-quality-belarus-mebr29","title":"Brahin meteorite 2.1g – Extra Quality – Belarus - MEBR29","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.1g\u003c\/li\u003e\n\u003cli\u003eDimensions: 15 x 11 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is composed mainly of iron and nickel. The metallic matrix consists mainly of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it constitutes the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, significantly increasing the aesthetic value of the material. They generally have green to brown hues, and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a differentiation process, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028619235653,"sku":"MEBR29","price":135.74,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56288_meteorite-brahin-2-1g---extra-quality---belarus.jpg?v=1779383575"},{"product_id":"meteorite-brahin-21g-extra-quality-belarus-mebr24","title":"Brahin Meteorite 2.1g – Extra Quality – Belarus - MEBR24","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.1g\u003c\/li\u003e\n\u003cli\u003eDimensions: 14 x 12 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite strewn field measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, more large fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix is primarily composed of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, forms the main structural component of the metallic iron-nickel phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly increasing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028619301189,"sku":"MEBR24","price":135.74,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56273_meteorite-brahin-2-1g---extra-quality---belarus.jpg?v=1779383575"},{"product_id":"meteorite-brahin-22g-extra-quality-belarus-mebr30","title":"Brahin Meteorite 2.2g – Extra Quality – Belarus - MEBR30","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.2g\u003c\/li\u003e\n\u003cli\u003eSize: 14 x 11 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local residents, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. During the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix consists mainly of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silver luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-grey in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, constitutes the main structural component of the metallic iron-nickel phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly increasing the aesthetic value of the material. They generally range in hue from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028619333957,"sku":"MEBR30","price":142.2,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56291_meteorite-brahin-2-2g---extra-quality---belarus.jpg?v=1779383575"},{"product_id":"meteorite-brahin-24g-extra-quality-belarus-mebr22","title":"Meteorite Brahin 2.4g – Extra Quality – Belarus - MEBR22","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 2.4g\u003c\/li\u003e\n\u003cli\u003eSize: 14 x 13 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the city of Brahin, located in Belarus. The meteorite's strewn field measures approximately 15 kilometers long and 3 kilometers wide and is traversed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently delivered to scientists, who identified them as meteoritic material. Throughout the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated to be around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is primarily composed of iron and nickel. The metallic matrix is mainly composed of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silver-gray in color with a metallic luster. In meteorites, it often forms wide bands visible on cut surfaces. Kamacite is softer than taenite and, together with it, forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally range in color from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028619497797,"sku":"MEBR22","price":155.13,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56267_meteorite-brahin-2-4g---extra-quality---belarus.jpg?v=1779383579"},{"product_id":"meteorite-brahin-37g-extra-quality-belarus-mebr35","title":"Meteorite Brahin 3.7g – Extra Quality – Belarus - MEBR35","description":"\u003cul\u003e\n\u003cli\u003eType: Pallasite\u003c\/li\u003e\n\u003cli\u003eLocation: Belarus\u003c\/li\u003e\n\u003cli\u003eWeight: 3.7g\u003c\/li\u003e\n\u003cli\u003eDimensions: 24 x 13 x 2 mm\u003c\/li\u003e\n\u003cli\u003eYear of discovery: 1810\u003c\/li\u003e\n\u003cli\u003eKnown total weight: 823kg\u003c\/li\u003e\n\u003cli\u003eSurface treatment: cut, Polished slice\u003c\/li\u003e\n\u003cli\u003eDETAILED DESCRIPTION\u003c\/li\u003e\n\u003c\/ul\u003e\u003cp\u003eThe Brahin meteorite – Belarusian pallasite The Brahin meteorite is classified as a pallasite, a type of stony-iron meteorite. It was first discovered in 1810 near the town of Brahin, located in Belarus. The meteorite strewnfield measures approximately 15 kilometers long and 3 kilometers wide and is crossed by the Dnieper River. The discovery was made by local inhabitants, who found metallic fragments weighing 80 and 20 kilograms. The first samples were subsequently handed over to scientists, who identified them as meteoritic material. During the 19th and 20th centuries, other larger fragments of the Brahin meteorite were discovered, with some specimens reaching several hundred kilograms. The total mass of all recovered fragments is estimated at around 823 kilograms. Structure Pallasites are characterized by the presence of metallic and silicate components in approximately equal proportions. The metallic component is mainly composed of iron and nickel. The metallic matrix consists primarily of the following alloys: Taenite – a nickel-rich alloy (35–50% Ni) known for its high hardness and silvery luster. Kamacite – an iron-rich alloy (generally 90–95% Fe) with a lower nickel content (5–10% Ni), typically silvery-gray with a metallic luster. In meteorites, it often forms broad bands visible on cut surfaces. Kamacite is softer than taenite and together with it forms the main structural component of the iron-nickel metallic phase. The olivines present in the Brahin meteorite are often large, clear, and beautifully translucent, greatly enhancing the aesthetic value of the material. They generally exhibit shades from green to brown and their quality is high, making them suitable for jewelry. Origin The Brahin meteorite, like other pallasites, is interpreted as a fragment of a body formed in the transition zone between the core and the mantle of a differentiated planetesimal. Planetesimals are small bodies formed in the early stages of the Solar System, and some of them may have evolved into planets. Pallasites, including the Brahin meteorite, are considered fragments of these bodies that underwent a process of differentiation, during which the metallic core separated from the silicate mantle.\u003c\/p\u003e","brand":"PeltramMinerals","offers":[{"title":"Default Title","offer_id":58028619694405,"sku":"MEBR35","price":217.17,"currency_code":"EUR","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0881\/1659\/2965\/files\/56306_photoroom-004-20251027-162358.jpg?v=1779383584"}],"url":"https:\/\/moldavite.it\/en\/collections\/brahin.oembed","provider":"Moldavite.it","version":"1.0","type":"link"}