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  2. List of mineral tests - Wikipedia

    en.wikipedia.org/wiki/List_of_mineral_tests

    Mineral tests are simple physical and chemical methods of testing samples, which can help to identify the mineral type. [1] This approach is used widely in mineralogy , ore geology and general geological mapping.

  3. Lustre (mineralogy) - Wikipedia

    en.wikipedia.org/wiki/Lustre_(mineralogy)

    Lustre (British English) or luster (American English; see spelling differences) is the way light interacts with the surface of a crystal, rock, or mineral. The word traces its origins back to the Latin lux , meaning "light", and generally implies radiance, gloss, or brilliance.

  4. Interference colour chart - Wikipedia

    en.wikipedia.org/wiki/Interference_colour_chart

    When using the chart, it is important to remember these tips: Isotropic and opaque (metallic) minerals cannot be identified this way. The stage of the microscope should be rotated until maximum colour is found, and therefore, the maximum birefringence. Each mineral, depending on the orientation, may not exhibit the maximum birefringence.

  5. Glances - Wikipedia

    en.wikipedia.org/wiki/Glances

    The metallic luster of the minerals of the group resembles the luster of the surface of a fresh fracture of metals. It is clearly visible only on the non-oxidized surface of the sample. Minerals that have a metallic luster are, as a result, opaque and heavier than minerals that have a non-metallic luster.

  6. Mica - Wikipedia

    en.wikipedia.org/wiki/Mica

    The octahedral sheet has a positive charge, since its bulk composition is Al(OH) 2+ (for a dioctahedral sheet with the apical sites vacant) or M 3 (OH) 2 4+ (for a trioctahedral site with the apical sites vacant; M represents a divalent ion such as ferrous iron or magnesium) The combined TOT layer has a residual negative charge, since its bulk ...

  7. Dioptase - Wikipedia

    en.wikipedia.org/wiki/Dioptase

    Dioptase is an intense emerald-green to bluish-green mineral that is cyclosilicate of copper.It is transparent to translucent.Its luster is vitreous to sub-adamantine.Its formula is Cu 6 Si 6 O 18 ·6H 2 O, also reported as CuSiO 2 (OH) 2.

  8. Brazilianite - Wikipedia

    en.wikipedia.org/wiki/Brazilianite

    With the second occurrence of the mineral, it was determined that the specific gravity of the mineral was actually 2.98. [10] Brazilianite has a vitreous luster, has a white streak, and the mineral is translucent to transparent. [7] The color of brazilianite ranges from dark yellow-green to a pale yellow. [6]

  9. Muscovite - Wikipedia

    en.wikipedia.org/wiki/Muscovite

    Sheets of muscovite 5 meters × 3 meters (16.5 feet × 10 feet) have been found in Nellore, India. [7] Muscovite has a Mohs hardness of 2–2.25 parallel to the [001] face, 4 perpendicular to the [001] and a specific gravity of 2.76–3. It can be colorless or tinted through grays, violet or red, and can be transparent or translucent.