This 9.36 g golden pallasite is a remarkably distinctive specimen, defined by an organic tubular structure that evokes the form of a natural conduit or channel carved within the metallic mass.

One of its most striking features is this elongated cavity, whose geometry suggests a flow-like formation. Within this structure, numerous coarse desert grains—ranging from sand to small gravel—are visibly trapped, as if held in place over time within the hollowed metal.

These inclusions, pale beige to translucent, contrast vividly with the smooth, dark iron-nickel matrix, creating a compelling visual tension between metal and mineral, void and filling. The effect is both geological and almost sculptural, as if the piece had captured a fragment of its terrestrial environment.

The surrounding surface is notably softened and rounded, with subtle undulations and localized depressions marking the former positions of olivine crystals. Unlike more aggressive “spiked” individuals, this specimen presents a controlled, cohesive morphology, where the eye is guided through the internal structure rather than across the exterior.

This piece stands apart as a hybrid object, illustrating not only the nature of pallasitic material, but also its long interaction with desert conditions.

🔬 Scientific Significance

This specimen highlights:

• The selective loss of olivine, leaving structured cavities
• The formation of natural tubular voids within metallic phases
• The secondary trapping of terrestrial sediments (sand and gravel)
• A rare example of post-fall interaction between meteorite and desert environment

It represents a compelling intersection between planetary material and Earth surface processes.