Exceptional full slice of the famous Imilac pallasite, weighing 396 g and displaying numerous gem-quality transparent olivine crystals embedded within a stable iron-nickel matrix. The specimen combines remarkable translucency, strong contrast between metal and silicates, and an elegant natural outline preserved across the entire slice. Large transparent olivines illuminated from behind reveal the extraordinary internal beauty that has made Imilac one of the most sought-after pallasites among advanced collectors and museums. A visually striking and highly collectible specimen combining scientific importance with exceptional aesthetic appeal.
This exceptional 396 g full slice of the renowned Imilac pallasite displays a remarkable concentration of large gem-quality olivine crystals embedded within an iron-nickel matrix.
The specimen presents an outstanding balance between metallic structure and transparent silicate inclusions, creating the luminous stained-glass appearance that has made Imilac one of the most admired pallasites in the world.
Several olivine crystals within this slice are highly translucent to transparent and reveal exceptional color and clarity when illuminated. These natural extraterrestrial peridots formed deep within the mantle-core transition zones of an early differentiated asteroid during the formation of the Solar System.
The contrast between the golden-green olivines and the surrounding iron-nickel metal creates a highly aesthetic visual composition highly appreciated by advanced collectors.
This specimen is a complete slice preserving the full natural outline of the original meteorite section. The irregular contours and balanced distribution of olivines contribute to the specimen’s strong visual presence.
Unlike smaller fragmented slices, complete Imilac slices of this quality are increasingly difficult to obtain, especially with large transparent crystals and well-preserved structural integrity.
Imilac was discovered in the Atacama Desert of northern Chile, one of the driest environments on Earth. Classified as a main-group pallasite, it is composed of iron-nickel metal and olivine crystals formed under extreme conditions during planetary differentiation in the early Solar System.
Because of their beauty and rarity, pallasites are considered among the most desirable meteorites for collectors, museums, and high-end displays.
This Imilac slice combines several highly desirable characteristics:
Its aesthetic quality makes it particularly suitable for an advanced meteorite collection, luxury interior display, or museum presentation.
This remarkable 396 g full slice of the Imilac pallasite stands out as a high-end specimen combining size, transparency, and outstanding preparation quality.
The slice presents a rich and balanced distribution of olivine crystals, many of which exhibit exceptional transparency. Under transmitted light, these crystals reveal vivid golden, honey, and amber tones, creating the luminous stained-glass effect characteristic of the finest Imilac specimens.
The metallic matrix has been meticulously prepared and polished, achieving a level of finish that significantly enhances both the visibility and brilliance of the olivines. This type of preparation requires considerable time and expertise, allowing each crystal to be revealed with precision while preserving the natural structure of the meteorite.
The result is a surface displaying remarkable clarity and contrast, where the interplay between translucent olivine and reflective iron-nickel metal produces exceptional visual depth. The large dimensions of the slice further amplify this effect, offering a broad and uninterrupted view of the internal architecture of the pallasite.
Complete Imilac slices of this scale, combining high transparency, balanced crystal distribution, and museum-quality preparation, are rarely encountered. This specimen is therefore particularly suited for advanced meteorite collections, high-end display, or institutional presentation where both scientific significance and aesthetic excellence are sought.
Imilac is one of the most visually attractive pallasites because of its abundant transparent olivine crystals and strong contrast with the metallic matrix.
Yes. The olivines in Imilac are natural extraterrestrial crystals formed inside an asteroid over 4.5 billion years ago.
Collectors especially seek specimens with transparent olivines, balanced crystal distribution, stable preservation, and complete slice formats.
Complete slices preserve the original shape of the meteorite section and generally provide stronger aesthetic and display appeal than fragmented pieces.
