carminite (w. beudantite and gartrellite)

TSNB460

Specimen

Exhibit 1. Carminite (w. beudantite and gartrellite); 40 mm.
Exhibit 1. Carminite (w. beudantite and gartrellite); 40 mm.
Image Credit: John Schneider
Exhibit 2. 10 mm field of view.
Exhibit 2. 10 mm field of view.
Image Credit: John Schneider
Exhibit 3. Specimen label (Hans Josef Lauenstein).
Exhibit 3. Specimen label (Hans Josef Lauenstein).
Image Credit: John Schneider
Exhibit 4. Specimen label (Warren Taylor).
Exhibit 4. Specimen label (Warren Taylor).
Image Credit: John Schneider
Exhibit 5. Specimen label (Bill Pinch).
Exhibit 5. Specimen label (Bill Pinch).
Image Credit: John Schneider
Thumbnail by 1Thumbnail by 2Thumbnail by 3Thumbnail by 4Thumbnail by 5

Title

carminite (w. beudantite and gartrellite)

Principal Mineral

Carminite

Size

Miniature; 40mm

Location in the Mine

Second oxidation zone

Collection

MGMH 2020.7.736

Provenance

Lauenstein, H.J.; Taylor, W.; Wrigley, M.; Pinch, W.W.

Entry Type

Specimen TSNB460

Fans of acicular grey-red carminite crystals (to 2.5 mm), with bright red internal reflections intergrown with pseudo-hexagonal crystals of yellow-brown beudantite and blocky green microcrystals of gartrellite (exhibits 1 and 2).

The specimen is from the collection of Bill Pinch. It is accompanied by three labels, the earliest of which (Exhibit 3) is handwritten in German by Hans-Josef Lauenstein, "Dr. L.",  Tsumeb Corporation Limited mineralogist in the late 1980s and early 1990s. The specimen subsequently belonged to British collector Warren Taylor (Exhibit 4), whose collection was later dispersed by Mark Wrigley of Thames Valley Minerals.

When Pinch learned that items from the Taylor Collection were available, he asked his friend Chris Amo to travel to London on his behalf to acquire certain specimens and this fine carminite specimen was at the top of his shopping list (Chris Amo, pers. comm. to M. Southwood, 2019). Pinch's label is shown as Exhibit 5.

The location in the mine is not recorded but this is a second oxidation zone paragenesis.

beudantite; gartrellite