AGM & Tsumeb
Then Richard
Harrison gave a talk on Tsumeb minerals. He recently graduated with a degree in
geology, and we are proud of our new whizz-kid. He began with a few facts, like
the mine is situated in 530 myr Pre-Cambrian rock in the Otavi Mountainland.
The mine has three zones, the uppermost at 350 m below the surface, the second
at between 800–1150 m, and the third at 1350 m. The mine is flooded, which is a
pity because workable amounts of silver, germanium and mercury are to be found
at the lowest levels. Tthese zones have different rock types, producing
different kinds of matrix, on which crystals grow, and the matrix interests the
true blue Tsumeb buffs as much as the minerals. For, if you know the matrix,
you can more or less trace the specimen to such-and-such a level, mined in the
year so-and-so. Which is a bit above this correspondent’s head – he’s one of
those happy chappies only too pleased
to own a specimen from Tsumeb at all.
Richard then
talked about Tsumeb’s “missed minerals”, overlooked in the past in favour of
more colourful species. For instance when everybody was collecting smithsonites
and azurites, nobody gave minerals like galena a second glance. But since then
all kinds of overlooked minerals are being eagerly collected like gypsum,
barite, quartz rhodochrosite(!), fluorite and sphalerite. Pseudomorphs
(replacements of one kind of a mineral by another and keeping the original’s
shape) and perimorphs (minerals completely covered by another mineral) are also
popular collectors’ items.
Examples of
Tsumeb minerals were brought along and proudly displayed, and it looks like our
club can show us some pretty good specimens. If anybody thought that the days
of collecting Tsumeb minerals is history, they can think again………..or better
still, attend the next Tsumeb talk and see what members bring along then.
Thanks Richard, I think we all
enjoyed your talk. TVJ (34 members attended)