Wulfenite (w. azurite, malachite and copper arsenates)

TSNB828
Specimen
Maucher, W.
Exhibit 1. Wulfenite (w. azurite, malachite and copper arsenates); 120 mm.
Exhibit 1. Wulfenite (w. azurite, malachite and copper arsenates); 120 mm.
Image Credit: Malcolm Southwood photo; courtesy of the NHM London
Exhibit 2. Wulfenite (w. azurite, malachite and copper arsenates); 120 mm.
Exhibit 2. Wulfenite (w. azurite, malachite and copper arsenates); 120 mm.
Image Credit: Malcolm Southwood photo; courtesy of the NHM London
Exhibit 3. Wulfenite (w. azurite, malachite and copper arsenates); 120 mm.
Exhibit 3. Wulfenite (w. azurite, malachite and copper arsenates); 120 mm.
Image Credit: Malcolm Southwood photo; courtesy of the NHM London
Image of undefined

Image Credit: Malcolm Southwood photo; courtesy of the NHM London
Image of undefined

Image Credit: Malcolm Southwood photo; courtesy of the NHM London
Thumbnail by 1Thumbnail by 2Thumbnail by 3Thumbnail by 4Thumbnail by 5

Specimen Title

Wulfenite (w. azurite, malachite and copper arsenates)

Associated Minerals

arsentsumebite (?); azurite; bayldonite (?); gartrellite (?); smithsonite

Principal Mineral

Wulfenite

Precursor Mineral

Azurite

Size

Cabinet; 120mm

Location in the Mine

First oxidation zone

Provenance

Maucher, W.

Collection

NHM London; BM.1922,208

Entry Number

Specimen; TSNB828

Associated Minerals

arsentsumebite (?); azurite; bayldonite (?); gartrellite (?); smithsonite

Description

Localised groups of colourless-grey tablets of wulfenite (to 3 mm) on a cavernous matrix of powdery CuPb arsenates which includes pseudomorphs after wulfenite (to 5 mm) and (more sparsely) after mimetite. The matrix has not been analysed but arsentsumebite (?), bayldonite (?) and gartrellite(?) are likely components.


Pseudomorphs (and partial pseudomorphs) of malachite after azurite (to 5mm) forming groups (to 25 mm) are present on one face of the specimen (exhibits 1 and 2), while on the reverse side (Exhibit 3) unaltered azurite crystals are accompanied by sub-mm crystals of white smithsonite.


The specimen was purchased from Wilhelm Maucher (of Munich) in 1922 which dates it to 8 Level or above in the first oxidation zone. The fact that the Maucher and NHM labels highlight wulfenite (exhibits 4 and 5), when in fact wulfenite is a minor component of this paragenesis, is testament to the scarcity of this mineral in the upper levels of the mine.