What made the pale veins on this boulder? Nepheline syenite was placed on top of 2283 while the form was still closed, and water was dripped onto it. The veining is the track of what ran off: thin wandering lines through one stretch of the dark body, broad splashes in the next, heaviest around the crown where it started and thinning as it travels down toward the base.
The look is unlike the catalog’s other pale surfaces, which is why it carries its own term. It is not the thin trailed lines of white threads, and not the dragged sweeps of pale swipes cutting through a crust field — the veining wanders, changes width, and pools where it settled. What the material did chemically, why it was chosen, or what it was expected to do is not part of the record; the maker confirmed the application itself.
This term stays narrow. Its neighbor 2289 carries pale markings that photograph similarly, and the two were grouped together on looks when this batch was first reviewed — but 2289’s pale is the inside of its clay, opened up by controlled thermal shock, not a material run over the outside. It is not a member here.
See it on real pieces
2283 — or browse the pale-veining listing and the rest of the July 16 boulders.
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