This 96 gram golden pallasite displays a compact yet highly textured morphology, combining a dense metallic framework with cavities revealing preserved olivine remnants. Its surface is marked by pronounced metallic spikes formed through differential weathering, while coarse desert sand grains remain locally embedded within the structure. The specimen presents a balanced combination of mass, texture, and natural preservation, shaped by both atmospheric entry and prolonged desert exposure.
This 96 g golden pallasite is a compact natural individual, distinguished by the density of its structure and the richness of its surface textures.
The specimen exhibits a dark metallic matrix enhanced by a subtle golden desert patina, the result of long-term exposure in an arid environment. Unlike more open or fragmented individuals, this piece retains a more cohesive structure, giving it a strong visual presence despite its moderate size.
Within shallow cavities and protected zones, small olivine remnants remain visible, showing muted yellow to orange tones. These preserved silicate inclusions contrast with more exposed areas, where the olivines have been progressively removed by natural weathering.
These weathered zones are characterized by numerous metallic spikes, sharp and irregular protrusions formed as the metal framework resisted erosion while the surrounding olivines disappeared. This process reveals the internal architecture of the pallasite in relief, producing a textured surface that is both complex and highly tactile.
In several interstitial spaces, coarse, light-colored desert sand grains are naturally trapped, further attesting to the specimen’s long residence in a wind-driven environment. These grains create a visual contrast with both the metallic surfaces and the preserved olivines.
The overall morphology reflects the combined influence of atmospheric ablation and aeolian erosion, resulting in a surface that is both sculpted and informative. Unlike polished sections, this natural individual offers a direct view of the interaction between metal and silicate phases, shaped entirely by natural processes.
This specimen stands out for its balance between structural integrity and surface complexity, making it an excellent representation of naturally weathered pallasites.
