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    Minerals A-Z

The minerals are divided into alphabetical order. Press the button below to take you to the correct page.

Our vision was not just to sell our beautiful minerals on the WWW but to also provide people with information about every mineral that we have from Tsumeb; Aris Quarry; Namibia and the Kalahari Manganese fields.The buttons will take you to a page dedicated to a specific mineral. The minerals are divided into alphabetical order. If you want to see a complete list then visit this Alphabetic list page

Minerals A-E

Minerals F-J

Minerals K-O

Minerals P-T

Minerals U-Z

The Kalahari Manganese Fields

 

 

The minerals of the Kalahari Manganese Fields in the Northern Cape Province achieved international fame from as early as 1960 onwards. The Kalahari manganese fields is synonymous with some very rare mineral species. The worlds largest gaudefroyite crystals can be noted as well as species such as gageite, xonotlite, strontiopiemontite, crystals of vuagnatite, octahedrons of henritermietirite, euhedral crystals of caryopilite, bultfonteinite, ruizite and the worlds largest crystals of thaumasite, mozartite and shigaite.

The Kalahari manganese fields is also the home to nine type locality minerals and the Postmasburg region has one type locality species to it's credit. The following are the type locality minerals listed chronologically:

1943

Gamagartite

1983

Sturmanite

1990

Orlymantite

1992

Vonbezingite

1993

Poldervaartite

1993

Hennomartinite

1993

Kornite

1994

Effenbergerite

1995

Nchwaningite

1996

Wesselsite

Of the 132 minerals recorder specifically from the Kalahari manganese fields, some have never been found as aesthetic specimens that would be of interest to mineral collectors, that is they form part of the massive ore. Approximately half of the species fall into this category. The remaining 67 species have been collected.

This article was extracted from the book "The manganese adventure" written by Bruce Caincross

Aris Quarry

The Aris Quarry is in the Windhoek District. It is a phonolite quarry 20km South of Windhoek, Namibia. Here it's mined on and off for road gravel. This phonolite is one of many phonolite's belonging to several alkaline intrusions between Windhoek and Rehoboth in central Namibia.

The Aris Phonolite's

Geological Setting

A number of Mid Tertiary (=/-34 Ma) phonolitic and trachytic bodies, appearing as domes, plugs, vents and associated hydrothermal dykes, occur in the Aris area where they intrude quartz-feldspar gneisses, mica schist and amphi-bolities of the Paleopro-terozoic Hohewarte complex. The phonolites occur as flows, dykes and plugs exposed as eroded outcroppings and caps on small hills and buttes. They form part of the tertiary Auas alkaline volcanic field, which extends from Aris in the north to Rehoboth some 65 km further to the south.

Elsewhere in the Auas province there are several areas in which fault-controlled hot springs (Windhoek, Rehoboth and hydrothermal alteration (mainly silicification and argillic alteration) are present. They are probably the result of geothermal activity related to the cooling of alkaline magmas at depth. The intrusions are the latest manifestations of tertiary alkaline magmatism along the western margin of Southern Africa, as are the phonolites at Klinghardt Mountains SE of Luederitz.

Some zones of the phonolite rock contain numerous small cavities, mostly 1-2 cm in diameter with exceptional cavities to about 8 cm, with well-formed, microscopic crystals of various minerals. Most famous is the abundant occurrence of the world's best Tuperssuatsiaite, but well-crystallized villiaumite and makatite should also be mentioned.

The following is a list of some of the minerals found in the district:

Aegerine/ Aenigmatite/ Analcite/ Aragonite/ Bastnaesite / Biotite/ Calcite/ Eudialyte/ Ferropargasite/ Fluorapatite/ Fluorapophyllite/ Galena/ Gyrolite/ Hematite/ Hydroxyapophyllite/ Hydroxylapatite/ Iraqite/ Kaersutite/ Kanemite/ Labuntsovite-Mn/ Lanthanite-(Ce)/ Lovozerite/ Magadiite/ Magnesio-aluminokatophorite/ Magnetite/ Makatite/ Mangan-neptunite/ Microcline/ Monazite-(Ce)/ Muscovite/ Natroapophyllite/ Natrolite/ Natrophosphate/ Nenadkevichite/ Nepheline/ Polylithionite/ Quartz/ Rhodochrosite/ Sanidine/ Sazhinite-(Ce)/ Sodalite/ Sphalerite/ Tetranatrolite/ Titanite/ Tsepinite-Na/ Tuperssuatsiaite/ Villiaumite/ Wurtzite/ Zakharovite variation Ferroan Zakharovite/ Zircon.

 

Tsumeb

Introduction

By Dr. Georg Gebhard

Tsumeb is a small village founded by Germans, situated in northeast Namibia, formerly South West Africa. It is also the name of an important ore body that is perhaps the most famous mineral locality in the world.

Everybody who gets in contact with the name TSUMEB realizes how amazing Tsumeb really is, and how fortunate collectors are to have been presented with an an almost inexhaustible abundance of minerals and mineral combinations. The fascinating thing about Tsumeb is not just its minerals. It is also its discovery and the mining history. For hundreds of years an outcrop of copper ore was the hidden treasure of the inhabitants, the Bushmen. All foreigners who tried to see this treasure were attacked by Bushmen with poisoned arrows. The legendary copper was a 12 meter high outcrop of pure, oxidized ore, stretching across an area 180 meters long and 40 meters wide - that was later to be found as the Green Hill of Tsumeb.

This famous deposit came into recognition of the US$pean hemisphere in 1890. The leader of the first expedition, which was sent 1893 by a British-German company for evaluating the ore's richness, gave an enthusiastic description of Tsumeb:

"I have been holding places of trust for the past 24 years; have visited various countries of the world, inspecting mines mineral outcrops, and prospecting for minerals; have been associated with the minerals gold, silver, tin, copper and lead; but in the whole of my experience, I have never seen such a sight as was presented before my view at Soomep, and I very much doubt if I shall ever see such another in any other locality."

In the light of what we know today, Rogers words seem to have been prophetic. For Tsumeb indeed developed from a deeply colored "Green Hill" into one of the richest mines in the world which produced about 90 million tons of ore in 91 years.

It was a unique experience to establish the first mining complex of shafts, ore treatment and mills in the middle of Nowhere in Africa, which was designed according to US$pean standards. This great pioneer work by German miners and engineers is for example expressed by the longest narrow-railroad in history that had to be constructed crossing 500 kilometers of bush and desert. The difference of culture and habit between the original inhabitants and the miners could not be larger, thus creating problems and funny stories as well.

Since the beginning of mining minerals from Tsumeb were collected by miners no matter which position they had. General Managers dug for mineral specimens themselves underground. Famous mineral finds created their own stories in which miners, collectors, museums and dealers played a part. Since the discovery of the first mineral samples some of the highest prices in mineral collecting history were and are paid for minerals from Tsumeb.

What is it about Tsumeb minerals that captures one's imagination?

It is partly the captivating description of the discovery and development of the mine. But it is also, perhaps primarily, the uniqueness of its rich mineral diversity. This is due to several geological factors, one of, which was the existence of three oxidation zones discovered during mining.

Tsumeb offers one of the greatest varieties of mineral assemblages known. It produced 247 known species, plus 24 species still under investigation. Of the minerals discovered in Tsumeb, 45 are known to occur solely there. But not only the rare finds boast of superlatives. The crystallization of most minerals is so perfect and aesthetic that 68 species from Tsumeb display the finest crystals known from any deposit. Of these, 36 species have been found as spectacular, macroscopic crystals, unrivaled by any other locality. Tsumeb pseudomorphs are also outstanding. 61 different types represent them, which is far ahead of all other known mineral localities. Adding the "best of species" to the minerals unique to Tsumeb would produce a total of 113 minerals qualifying for the world's best for the species. But this is a figure that probably does not last for a long time. Even after closing down the mine, at least one new mineral is published which has been discovered on a mineral specimen from the mining period.

Many localities have produced specimens generally considered to be the finest of the species ever found. However, most of the localities are known only for one or two species of this quality. In comparison, Tsumeb exhibits more outstanding mineral specimens than most localities even contain minerals. These minerals provide the quality benchmark for every collector.

These impressive statistics may partly explain Tsumeb's mineralogical fascination. But Tsumeb has more to offer than statistics. There are the constantly recurring, surprising discoveries, which transfigure previously uninspiring minerals, Cinderella-like, into desirable objects, of which smithsonite is a good example.

Tsumeb does not keep to set prescripts, as the wide variety of minerals shows. The presence of chemical components necessary for the formation of minerals was so plentiful and varied, that there are deviations in the composition of even simply structured minerals.

Over a period of more than 90 years collectors, scientists and museum curators have almost become accustomed to have new minerals coming from Tsumeb. Only after mining activities ceased, have we fully realized what Tsumeb actually meant to us.

During the entire mining production Tsumeb was often called dead for different reasons: insufficient ore or low metal prices or wars. But the mine kept going on down to one mile deep. In 1996 the mining activities were closed down in realty, not because of lack of ore, but caused by a strike.

Georg Gebhard

If you want more information on Tsumeb please look for the standard books of  TSUMEB 1 and TSUMEB 2 (website CG Publishing)

If you want to read more about Tsumeb - We have an article on the History of Tsumeb

and The geology of Tsumeb

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

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