Plumbogummite is a lead–aluminum phosphate of the alunite supergroup, best known to collectors for its sky-blue to turquoise botryoidal coatings and dramatic pseudomorphs after pyromorphite. Its classic appearance ranges from silky, satiny spheres and crusts to porcelain-like coatings; less commonly it forms tiny crystals, but the most coveted pieces are sharp pyromorphite prisms entirely replaced by plumbogummite while retaining the original hexagonal form. Colors span powder-blue, robin’s-egg blue, teal, sea-green, apple-green, and gray-white; the most vivid blues from southern China became modern icons around 2014–2016.
Most plumbogummite forms as a secondary mineral in oxidized lead deposits, often altering or replacing pyromorphite and other lead phases near the surface. Aesthetic contrast is a hallmark: blue coats on tan/iron matrix or blue-on-green pyromorphite cores. It is moderately heavy (SG around 4+) and relatively soft (hardness ~4–4.5), with luster from waxy to vitreous. Fine, colorful, and well-formed pseudomorphs are the top-tier specimens and can command strong prices, while attractive botryoidal crusts remain accessible to newer collectors.
The species was a connoisseur’s phosphate for decades—classic but subtle—until discoveries in Guangxi, China, unleashed a wave of intensely colored pseudomorphs after pyromorphite that electrified the market. That material pushed plumbogummite squarely into the mainstream of fine mineral collecting, with top pieces rapidly entering major collections. Historic European localities (Caldbeck Fells in the U.K., Les Farges in France) built its reputation with beautiful botryoidal coatings and replacements on pyromorphite. Tsumeb also contributed attractive, often unique associations.
Today, collectors chase three main aesthetics:
Supply from the headline Chinese pockets has waxed and waned; premium pieces with rich color, complete terminations, and balanced composition remain scarce and keenly contested.
While plumbogummite occurs widely, the following localities are especially sought after for distinctive colors, forms, or historic importance.
Near Guilin, the Yangshuo Mine produced closely related material to Daoping, including vivid blue plumbogummite after pyromorphite. Crystals are frequently slender prisms with flat to slightly hoppered terminations, sometimes in radiating groups. Partial replacements can create attractive gradients: green pyromorphite transitioning to blue plumbogummite caps. Fine matrix pieces show strong composition—blue crystals standing off limonitic matrix with quartz or minor hemimorphite adding sparkle. Availability was episodic; top-quality clusters with multiple pristine terminations are particularly prized.
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Buy from reputable sources, ask for disclosures, and examine under magnification and different lighting.
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With careful handling, plumbogummite’s soft luster and captivating blues will remain a highlight of any case—equally at home as a modern Guangxi showpiece or a classic European antique.