Regents Practical Review Carrying out the Physical Mineral Tests

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Presentation transcript:

Regents Practical Review Carrying out the Physical Mineral Tests

COLOR Color is not usually a definitive property of a mineral. Some minerals have characteristics colors Others vary due to chemical differences or impurities (atoms mixed inside the main elements) However most minerals have a variety of colors. The mineral sphalerite can be yellow, black, red, green or varieties thereof. Quartz is usually colorless, however it can have many colors depending on trace amounts of cations that substitute in the structure.

Some Colors of Quartz

STREAK-Does it have a colored streak or is it white/colorless? For opaque minerals, if you rub the sample across a streak plate, it will leave a colored powder. This streak is distinctive for minerals and is used to identify minerals. Hematite can be brown, black, metallic gray and earthy but in all cases it gives a red-brown streak.

Varieties of Hematite – all same color streak

HARDNESS – Mineral’s resistance to scratching/ abrasion HARDNESS – Mineral’s resistance to scratching/ abrasion. Minerals with higher numbers will scratch minerals below A mineral is considered “Hard” if it scratches glass and “Soft” if it does not. REMEMBER TO WIPE THE GLASS PLATE WITH YOUR FINGER TO MAKE SURE THE SCRATCH IS NOT A STREAK! The last three are not common minerals. Fingernail is 2 to 2.5, Cu penny is around 3.5; hammer is about 5.1, knife is 5.2 and plate glass is 5.5.

LUSTER – Does this look like it could be made from a hard metal? Describes how light reflects off the surface Categories: Metallic or Non-metallic Metallic – luster of metal – shines like a hard metal (light does not penetrate) *Many non-metallic minerals are SHINY because they are transparent or semi-transparent (like biotite mica) Non-metallic: vitreous or glassy; silky; pearly; greasy; waxy, dull; earthy

Examples of metallic luster

More Examples of Metallic Luster Pyrite (FeS2) Galena (PbS) PYRITE GALENA

Example of non-metallic luster Vitreous—quartz or biotite

Example of non-metallic luster Silky--example plagioclase feldspar

Non-metallic and metallic luster – earthy hematite – metallic hematite

Cleavage vs. Fracture Some minerals split along flat surfaces (called cleavage planes) when struck hard--this is called mineral cleavage Other minerals break unevenly along rough or curved surfaces--this is called fracture A few minerals have both cleavage and fracture. ****If both are visible, cleavage always dominates over fracture in reporting.

Cleavage – due to weak bonds in the crystal structure Cleavage – due to weak bonds in the crystal structure. Always look at the edges of minerals for cleavage NOT at the overall crystal shape Halite (NaCl) Potassium Feldspar HALITE

Cleavage MUSCOVITE BIOTITE

Quartz – Fracture (It looks like it broke unevenly)

Pyrite- Fracture