Cerussite (w. duftite and mimetite)

TSNB923
Specimen
Margraf, J.
Exhibit 1. Cerussite (w. duftite and mimetite); 170 mm.
Exhibit 1. Cerussite (w. duftite and mimetite); 170 mm.
Image Credit: Malcolm Southwood
Exhibit 2. 80 mm field of view.
Exhibit 2. 80 mm field of view.
Image Credit: Malcolm Southwood
Exhibit 3. 40 mm field of view.
Exhibit 3. 40 mm field of view.
Image Credit: Malcolm Southwood
Exhibit 4. 75 mm field of view.
Exhibit 4. 75 mm field of view.
Image Credit: Malcolm Southwood
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Specimen Title

Cerussite (w. duftite and mimetite)

Associated Minerals

calcite; duftite; mimetite

Principal Mineral

Cerussite

Size

Cabinet; 170mm

Location in the Mine

Undetermined

Provenance

Deneke family; Margraf, J.

Collection

Southwood, M.; MS2026.002

Entry Number

Specimen; TSNB923

Description

A porous matrix of intergrown calcite and duftite (Exhibit 2), mostly as sugary crystals but with larger calcite rhombs (to 5 mm) and colourless, platy cerussite crystals in partly healed fractures on the reverse side of the specimen (Exhibit 3).  The display face comprises a foundation of sugary pistachio-green duftite, quite extensively encrusted with colourless cerussite crystals (to 25 mm) of mainly equant to short prismatic habit. The cerussite crystals are partly and preferentially covered by a micro-crystalline crust of pale lemon-yellow mimetite (Exhibit 4). The calcite, cerussite and mimetite show varying responses to ultraviolet wavelengths:  In long wavelength (370 nm) UV all three minerals fluoresce dull red; in medium wavelength (312 nm) cerussite is off-white and mimetite is orange; in short wavelength (254 nm) calcite is bright orange, cerussite is white and mimetite is dull red. Quantitative EPMA on a related specimen (TSNB924) has shown the duftite to be close to end-member composition. (Compare TSNB924 and TSNB925.)

The specimen was purchased from German dealer Jürgen Margraf early in 2026; it was formerly in the collection of the Deneke family (Balingen, Germany), who were frequent visitors to Namibia in the 1960s and 1970s and bought specimens directly from miners. The location in the mine for this distinctive paragenesis is not recorded but specimens are believed to have been recovered circa 1978 (Cairncross 2000).