Bright, net-like structures and magnetic, black inclusions in an antigorite serpentinite

Image: K. Sieber,


When scientists analyzed  the chemical composition of chinese "Jade" in the 19th century, they discovered that at least two, completely different minerals were in circulation. First, the mineral jadeite from the pyroxene group. On the other hand finely matted minerals of the (ferro-) actinolite - tremolite solid solution series (Fig. 3), called "nephrite". Therefore it is important to keep in mind that the term jade (see: What is »JADE« ?) is not a mineral name, but a cultural name.

Although they are clearly distinguishable on close inspection, the minerals astrophyllite and anthophyllite are often confused. Both specimens occur in the form of shiny, iridescent fibrous aggregates. Together with other minerals, they often form interestingly patterned rocks. One of these is an anthophyllite schist from Sweden.

Anthophyllite (-Schist)


Anthophyllite schist, Sweden

Foto: K. Sieber,

Anthophyllite belongs to the amphibole mineral group and is chemically related to the minerals actinolite and tremolite, known in a fine-fibrous, felted form as "nephrite jade". Similar to these, anthophyllite readily forms stemmed to radiating fibrous aggregates.


»Bronzite-Pyroxenite« rock with grey magnetite inclusions

Picture: K. Sieber,



In modern mineralogy, "bronzite" is no longer regarded as a mineral in its own right, but as an iron-bearing variety of the mineral enstatite (so-called "Ferro-Enstatite", abbreviated: "Fe-Enstatite", (Mg,Fe)2[Si2O6],). Fe-Enstatite of the variety Bronzite contains 5 - 15% iron (in relation to magnesium) and belongs to the mineral group of pyroxenes. This group comprises single chain silicates with the basic component [Si2O6].


Many rocks, previously known primarily in the stonemasonry industry, are recently seen in the mineral trade as polished or tumbled stones. This development is undoubtedly an enrichment for lovers of beautiful rocks. Unfortunately, these decorative rocks are rarely labeled with a mineralogically/petrographically correct name. This is also the case with a dark, almost black rock with copper-colored sprinkles, which is often wrongly offered in the mineral trade under the name "Nuumite".


Bronzite-Gabbro (Norite)

»Bronzit-Gabbro«, Indien

Bronzite-Gabbro (Norite), India

Image: K. Sieber,

The rocks garnet-pyroxenite, garnet-peridotite and eclogite, all with a red-green speckled appearance, look very similar and yet are very different. They can occur side by side at the same locality and are easily confused. In the past they were only interesting for stonemasons, but in the last years they are increasingly offered as tumbled stones and gemrocks.


Pyroxenites are igneous rocks consisting of more than 50% pyroxene. These rocks form deep within the Earth's interior in the upper mantle and are brought into the upper crust either by rock displacements or by the intrusion of liquid magma into existing rock layers. One of the popular pyroxenite gemrocks are e.g. »Bronzite-Pyroxenite«.


Fig 1: This colorful rock is neither an eclogite nor a garnet peridotite, but a GARNET - PYROXENITE (green: diopside, yellow: enstatite, red: pyrope garnet).

Image: K. Sieber,

Epidot-Zoisit Gruppe

Fig. 1: Chemical composition of some minerals from the epidote-zoisite group

Grafik: © EPI-Institut

The mineral zoisite is a calcium (Ca) - aluminum (Al) silicate with the formula Ca2Al3[O|OH|SiO4|Si2O7]. It is capable to form single large crystals, but also massive rock bodies. By incorporation of the element manganese (Mn) into the crystal lattice, zoisite gets a pink to brown-red color (trade name: »Thulite«). Chromium Turns tho color of the mineral into green (trade name: »Anyolite«) and vanadium into blue (trade name: »Tanzanite«). Zoisite forms crystal shapes with orthorhombic symmetry.

The calcium-aluminum silicate zoisite is capable of forming rocks, e.g. pink »Thulitite« or green »Anyolite«. The latter often bears large ruby crystals. As a whole rock it is optically confusable with green fuchsite mica, which can also contain ruby.

Ruby-Zoisite (»Anyolite«)


Fig. 1: Ruby in green zoisite, Tanzania

Picture: K. Sieber,

The name »Anyolite« (after the Masai word for "green") stands for a mineral mixture of rock-forming green opaque to translucent zoisite, black hornblende amphibole and opaque to translucent rubies. It is also called "ruby zoisite" according to its mineral composition. The green color is caused by the element chromium.