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Minerals are the materials of which the earth's crust is
built and are therefore among the most common objects of daily observation.
Interesting forms of minerals have long been an object of man's fascination.
Since the earliest days he has collected and studied them - they are a form
of natural art. This set of pages
is intended to provide some basic information on minerals which have been
used as gems, are of industrial importance as ores or for having special
interest to collectors. There are many lists like this one on the internet,
but this one has the distinct advantage of colorful photos and a detailed
description of the origins and nature of the individual minerals beyond just
their physical properties. Many of the minerals have multiple spectacular photographs, most taken at
museums or the Tucson Gem and Mineral Show.
A
mineral may be defined as a naturally occurring
substance having a definite and uniform chemical composition with
corresponding characteristic physical properties. This eliminates all
artificial products of the laboratory which may conform to the last part of
the definition. It also eliminates all natural products of organic agencies,
since they will not show the uniform chemical and physical characters
demanded of a mineral. In spite of this I have included a few items which
are of interest, but do not strictly qualify as minerals. In the form of
rocks, minerals make up the solid matter of the earth's crust. But in the
great majority of cases a rock is not made up of a single mineral, but is a
more or less heterogeneous aggregate of several different species.
A
few rocks, like limestone and quartzite, consist of but one mineral in a
more or less pure state. In addition to occurring as essential and integral
parts of rocks, minerals are found distributed through them in a scattered
way, or in veins and cavities.
Below is a collection of over 100 minerals with beautiful photos and detailed
species information: |
Acanthite
Actinolite
Adamite
Angelesite
Amazonite
Ammolite
Amphiboles
Apatite
Aragonite
Arsenopyrite
Aurichalcite
Autunite
Axinite
Azurite
Barite
Benitoite
Beryl:
Aquamarine
Emerald
Heliodor
Morganite
Red Beryl
Borax
Bornite
Brazilianite
Brucite
Calaverite
Calcite
Carnotite
Cassiterite
Celestite
Cerrusite
Cerargyrite |
Chalcopyrite
Chalcosiderite
Chalcosite
Chlorite
Chrysoberyl
Chrysocolla
Chrysotile
Chromite
Cinnabar
Colemanite
Copper
Cordierite
Corundum: Ruby
Corundum: Sapphire
Crocoite
Cuprite
Diamond
Dioptase
Diopside
Dolomite
Dumorterite
Electrum
Epidote
Feldspar
Fluorite
Galena
Garnet
Almondite
Andradite
Grossularite
Pyrope
Spessartite
Uvarovite |
Gold
Goethite
Graphite
Gypsum
Halite
Hematite
Iron (meteorites)
Lazulite
Lepidolite
Limonite
Jade: Jadeite
Jade: Nephrite
Kyanite
Magnetite
Malachite
Mica (muscovite, Biotite Lepidolite, Mariposite);
Molybdenite
Moldavite
Olivine (Peridot)
Opal
Orpiment
Orthoclase
Phenacite
Phrenite
Platinum
Polybasite
Proustite
Pyrite
Pyrolusite
Pyromorphite
Pyragyrite
Pyroxenes |
Quartz
Realgar
Rhodochrosite
Rhodonite
Rutile
Scapolite
Sheelite
Siderite
Silver
Smithsonite
Sodalite
Sphalerite
Sphene
Spodumene
Spinel
Stephanite
Stibnite
Sulfur
Sylvanite
Tetrahedrite
Tobernite
Topaz
Tourmaline
Turquoise
Ulexite
Uranite
Vanadinite
Variscite
Vivianite
Wulfenite
Zeolites
Zircon
Zoisite |
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Characters of Minerals.
1. Minerals, as previously stated, have a definite chemical composition.
This composition, as determined by chemical analysis, serves to define and
distinguish the species, and indicates their profoundest relations. Owing to
difference in composition, minerals exhibit great differences when subjected
to the action of various chemical reagents, and these peculiarities are a
means of determining the kind of mineral under examination in any case. The
department of the science treating of the composition of minerals and their
chemical reactions is termed Chemical Mineralogy.
2. Each mineral, with few exceptions, has its definite form, by which, when
in good specimens, it may be known. These forms are cubes, prisms, pyramids,
etc. They are included under plane surfaces arranged in symmetrical order,
according to mathematical law. These forms are called crystals. Besides
these outward forms there is also a distinctive internal structure for each
species. The facts of this branch of the science come under the head of
Crystallographic Mineralogy.
3. Minerals differ in hardness, from talc at one end of the scale to the
diamond at the other. Minerals differ in specific gravity, and this
character, like hardness, is a most important means of distinguishing
species. Minerals differ in color, transparency, luster and other optical
properties. The facts and principles relating to the above characters and
others of a similar nature are included in the department of Physical
Mineralogy.
4. The detailed descriptions of individual mineral species, including their
chemical, crystallographic and general physical characters, together with
their occurrence, associations, uses, etc., are included under the division
known as Descriptive Mineralogy.
5. Lastly, the discussion of the methods that are used for identifying
minerals forms the division known as Determinative Mineralogy.
Classification of Minerals.
Classification is the grouping of objects or phenomena in such a manner as
will bring together those that are related or that are similar in many
respects and will separate those that are different. Since minerals are
chemical compounds whose properties depend upon their compositions, their
most logical classification must be based upon chemical relationships. But
their morphological and physical properties are their most noticeable
features, and hence these should also be taken into account in any
classification that may
be adopted. Probably the most satisfactory
method of classifying minerals is to group them, first, in accordance with
their chemical relationships and, second, in accordance with their
morphological and physical properties. The first division is into the great
chemical groups, as, for instance, the elements, the chlorides, the
sulphides, etc. The second division is the separation of these great groups
into smaller ones comprising minerals possessing the same general
morphological features. These smaller groups may contain only a single
mineral or they may contain a large
number of closely allied ones. If the basis of the subgrouping is manner of
crystallization, it follows that the members of subgroups containing more
than one member are usually isomorphous compounds. Thus the subdivisions of
the great chemical groups are single minerals and small or large isomorphous
groups of minerals, arranged in the order in which their metallic elements
are usually discussed in treatises on chemistry. For example, the great
group of carbonates embraces all minerals that. are salts of carbonic acid
(H2CO3). This great group is divided into smaller groups along chemical
lines, as for instance, the normal carbonates, the hydrous carbonates, the
basic carbonates, etc. These smaller groups are finally divided into
subgroups according to their morphological properties the normal salts, for
example, being divided into the two isomorphous groups known as the calcite
and the aragonite groups, and a third group comprising but a single mineral.
In certain specific cases some other classification than the
one outlined above
may be desirable. For instance, in books written for mining students it is
often found that a classification based upon the nature of the metallic
constituent is of more interest than the more strictly scientific one
outlined above, because such a classification emphasizes those components of
the minerals with which the mining student is most concerned. In books
written for the student of rocks, on the other hand, the most important
determinative features of minerals are their morphological characters, hence
in these the classification may be based primarily on manner of
crystallization. |