Mineral Guide Help
This help file illustrates how the display for every mineral works. All minerals are set up in the same format. The pink text portrays what each particular field describes. Blue, underlined text denotes hyperlinks for detailed explanations of applicable properties.
In every field,
the help
image in
the leftmost cells will take you directly to the help of that
field. (i.e. the help for the Fracture field
will take you here)
| Name |
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| Chemical Formula | Describes the chemical formula, which is the elemental makeup of the mineral |
| Composition | Describes what elements are in the mineral and the varying structure |
| Variable Formula | Describes
the variable
formula, that is, possibilities of common elemental replacements
of the mineral. For example, the mineral Adamite, Zn2(AsO4)(OH), frequently contains small amounts of Cu
(copper) and Co (cobalt) replacing some
Zn (zinc), thus the variable formula is (Zn,Cu,Co)2(AsO4)(OH). Underlined elements denote elements that can
be absent and must be less in percentage than the
element(s) not underlined in the same set of parenthesis.
Any element not underlined must be present in an
appreciable quantity. Please note that the "variable
formula" field only displays elements that commonly replace part
of an element in a given mineral. Other possible element
replacements not mentioned may exist but only occur
insignificantly or rarely. For example, the mineral Fluorite
occasionally contains traces of Ce (cerium) and Y
(yttrium), but the variable formula does not include
those elements for they are too seldom present. This field is absent by minerals without a varient formula. |
| Color | Describes what color(s) the mineral is capable of having |
| Streak | Describes the streak color of the mineral |
| Hardness | Describes the hardness of the mineral in accordance with Mohs scale (1-10) |
| Crystal
Forms and Aggregates |
Describes the crystal system, crystal forms, and crystal aggregates of the mineral. The crystal system is displayed first, in italics and parenthesis [i.e. (Monoclinic)], and the crystal forms and aggregates follow. Trigonal minerals, which really belong to the hexagonal system, are written grouped together with all the other hexagonal minerals. |
| Transparency | Describes the transparency of the mineral; that is whether the mineral is transparent, translucent or opaque. Minerals that can occur in any variation of the three (i.e. transparent and translucent) are noted as such. |
| Specific Gravity | Describes the specific gravity (density) of the mineral. Specific gravity is measured by the relative comparison weight of water. For example, if a mineral has a specific gravity of 3.6, than that mineral is 3.6 times heavier than water. |
| Luster | Describes the luster of the mineral |
| Cleavage | Describes
the mineral's cleavage.
Cleavage is measured in this guide by quality and the
amount of sides that have cleavage. The first number
describes the quality of cleavage (on a scale of 1-3 |
1=perfect; 2=good; 3=poor) ,and the second number
describes the number of directions that have the
cleavage. If all sides have the same cleavage, than all sides is written instead of a number. So a mineral
with a cleavage of 1,2 has perfect cleavage in 2 directions.
If the word Indiscernible is
written in this field, than the cleavage is so poor it is
not recognizable. If the word None is written in this field, then the mineral has
no cleavage. If a mineral exhibits different cleavage on different sides of the mineral, than there will be two cleavage indicators separated by a semi-colon (;). For example, if the cleavage of a mineral is written 1,2 ; 3,1, then it has perfect cleavage in one direction, and poor cleavage on two other directions. This field also describes the type of cleavage the mineral exhibits (if applicable), such as cubic, octahedral, rhombohedral, prismatic, and basal. The type of cleavage is separated by a - (dash), so for example a mineral with perfect basal cleavage would be written as 1,1 - basal. (basal cleavage is only on one side). |
| Fracture | Describes the fracture (the way a mineral breaks) of the mineral |
| Tenacity | Describes the tenacity (reactions to certain stresses) of a mineral |
| Other ID Marks | Describes
any other distinct feature not mentioned on the above
list. (some examples: taste, smell, fluorescence,
magnetism, etc.) [Note: This field may be absent if there is no text befitting it.] |
| Other Names | Displays
other names which are synonymous with that mineral. A box
with a check [Note: This field may be absent if there is no text befitting it.] |
| Varieties | Displays
and explains varieties of that mineral. A box with a
check [Note: This field may be absent if there is no text befitting it.] |
| Polymorphs | Displays
polymorphs
of the mineral. Most minerals do not have polymorphs, therefore regarding most minerals this entry is absent. |
| In Group | Describes what chemical group and subgroup the mineral belongs to. Differentiation between the group and subgroup is indicated by a semicolon (;). For example, the mineral Corundum belongs to the group Oxides ; Simple Oxides |
| All About | Additional
information about the mineral. This field may be absent by minerals without any suitable information. |
| Uses | Describes
the various uses of the mineral, whether industrially,
commercially, scientifically, or mineralogically. Note: There are many minerals that are elements that are found in a mostly pure state (i.e. Gold, Silver, Lead), but due to their rareness are not used as ores of the element. The use of the element will anyhow be mentioned there. This field may be absent by minerals without any suitable information. |
| Striking Features | Displays special properties that the mineral exhibits. (For example: great hardness, bright color, heaviness, etc.) |
| Complex Tests | Displays
other tests (such as acid and X-ray tests) that can
identify the minerals. These are mostly complex tests
that are not for the amateur. [Note: This field may be absent if there is no text befitting it.] |
| Popularity | Displays on a scale of 1 to 4 how popular the mineral. (1 = Very popular - even non-mineral collectors are familiar with the mineral. 2 = Popular among mineral collectors; most mineral collectors know of the mineral. 3 = Somewhat abstract. Some mineral collectors don't know of the mineral. 4 = Abstract. Basically unheard of, in exception to a few mineral collectors and science professors. |
| Prevalence | Displays on a scale of 1 to 3 how common the mineral is: 1 being very common and 3 being rare. This field is also dependant on how accessible and readily available a mineral is to collectors. |
| Demand | Displays on a scale of 1 to 3 how much of a demand (industrially or for collectors) there is for the mineral: 1 - very much in demand, 3 - of little use. |
| Distinguishing Similar Minerals |
Displays a list of minerals that are similar and can be confused with the mineral, and shows the similar mineral's property(s) that differentiate it from the mineral. |
| Commonly Occurs With |
Displays a list of minerals and sometimes rocks that the mineral many times occurs with. The rocks are displayed in (parenthesis) |
| Noteworthy Localities |
Displays
a list of important localities of
the mineral. Although this guide displays localities
worldwide, primary focus is on U.S. occurrences. NOTE: "Co." is an abbreviation of "county" |
| Picture
Icon Links |
Displays
small 50 x 50 pixel images that link you to a larger JPEG
image of the mineral. When there are no images availible, it is mentioned in this field. |
| Picture Links | Hyperlinks
to the above mentioned mineral images, properly labeled
to correspond to the above images. When there are no images availible, it is mentioned in this field. |
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* The mineral browser (the page this help file is depicting) can display more than one mineral if the minerals are almost identical, and the separation will be denoted by a small "and" (i.e. Acanthite and Argentite). It may also display mineral groups and series (i.e. Olivine Group)
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