This question arises time and again, whether you pick up a pebble during a walk, find a crystal in the mountains, discover golden or shining silver fragments in the waste rock piles of an ore mine, stumble over a curbstone, or when you look at a beautiful piece of jewelry. Inevitably, you will want to know: What mineral is this? What rock do I have in front of me? What is this colorful gemstone that sparkles so beautifully?
This book will help to answer these questions — as your constant companion on hikes or trips, while mountaineering or collecting minerals, in quarries and at waste rock piles, at mineral shows and also at jewelers.
With the exception of native mercury, minerals are always solid. No matter how good mineral water tastes, no matter how many minerals the label indicates, it is liquid and, therefore, not a mineral. Anything man-made, from window glass to quartz crystal in watches to artificial diamonds, is not a mineral. Pyromorphite crystals with curved prism surfaces are known as “Emser Barrels.” A mineral must always be a naturally occurring substance.
The concept of a crystal is somewhat different. Crystals are solid chemical substances whose atoms are arranged in a uniform and ordered structure. This ordered arrangement of atoms is reflected in the flat, regular surfaces which form the boundaries of a crystal. Almost all minerals are crystals, even if it is sometimes not externally apparent. There are only a few minerals whose atoms are not structurally arranged in the form of a crystal lattice — these are called amorphous. The best-known example is opal, which, in contrast to quartz (which is composed almost in the same way), cannot form crystals.
Gemstones are minerals that are cut for jewelry purposes. In order to be considered a gemstone, a mineral must meet various requirements, but primarily, it must be beautiful, i.e. satisfy aesthetic requirements. This means that it should be beautifully colored and should shine and sparkle as much as possible when polished. The latter is even more important if the mineral, such as a diamond, is normally colorless.
Rocks can be described as large geological formations that are composed of individual fragments of one or more different mineral types. Marble, for example, is made up of many grains of a single mineral: calcite. Granite, on the other hand, is composed of three mineral types: feldspar, quartz and mica.
Bismuth has a silver-white color with a tinge of red, but is often darker. Well-formed crystals are rare as bismuth is usually coarse; because of its perfect cleavage it is flaky, skeletal and mostly embedded. Accompanying minerals are often cobalt and nickel minerals. Bismuth is used in the glass industry, in medicine, in steel production and, albeit rarely, in reactor technology.
Realgar forms deep red prismatic to acicular crystals and coarse embedded masses. It is extremely sensitive to light. If it is not stored in a dark place, it quickly turns orange and transforms into a yellowish powder of the same chemical composition called pararealgar. Realgar was used in the production of pesticides (e.g. rat poison), but this is no longer permitted due to its toxicity. The name “red arsenic” also indicates that the substance is harmful to health.
Erythrite forms tabular to acicular crystals and spherical bundles. More frequently, however, the mineral is earthy and coarse. It is characterized by its intense purple-red to pink color. Such coatings of erythrite are always a clear indication of cobalt-containing ores. A frequent accompanying mineral, in addition to various cobalt ores, is native bismuth. Cobalt ores, together with cobalt bloom, were roasted and melted with quartz to form the so-called smalt, which, when finely ground, produced the cobalt blue pigment. Because of its resistance to heat, it was used particularly in porcelain painting.
Hematite forms metallic black-gray pyramidal crystals, sometimes reminiscent of octahedrons, thick to thin plates, rosette-shaped aggregates. It is also often coarse, flaky, with radials and a smooth surface (kidney ore), earthy, crusty. Beautiful crystals, especially the rosette-shaped aggregates (iron roses) can be found primarily in alpine-type fissures in the Austrian and Swiss Alps. Extraordinary hematite crystals that are rich in faces originate from the iron deposits on the Italian island of Elba.
Linarite forms ink blue prismatic to less often tabular crystals with numerous faces and is frequently crusty, earthy. It usually occurs in the company of cerussite and is formed where lead and copper ores weather together. When dabbed with hydrochloric acid, linarite turns white on the surface due to the formation of bleach chloride.
Rutile crystals form prismatic to capillary habits and are yellow, red or black in color. Twins are often of different natures; knee-shaped twins with a flat angle and heart-shaped twins with an acute angle between the two crystals. If both twins appear at the same time, the so-called sagenite grids form, which are completely typical for rutile. Artificially produced rutile (titanium dioxide) has great economic significance as a white pigment in wall paints, as UV protection in sunscreens or as an impregnating agent in the manufacture of UV-impermeable children’s clothing.
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