Identify the physical properties of minerals in terms of ,

Composition, luster, colour, streak, hardness, and cleavage or fracture
For the following minerals
1: pyroxene
2: pyrite
3: dioptase
4: hematite
5: magnetite
6: biotite
Respectively.

1 answer

Certainly! Here are the physical properties of the minerals you specified:

1. Pyroxene

  • Composition: Silicate mineral, typically containing calcium, magnesium, iron, and aluminum.
  • Luster: Vitreous to dull.
  • Colour: Typically dark green, black, or brown.
  • Streak: White to colorless.
  • Hardness: 5 to 7 on Mohs scale.
  • Cleavage or Fracture: Cleavage in two directions at nearly 90 degrees; uneven fracture.

2. Pyrite

  • Composition: Iron sulfide (FeS₂).
  • Luster: Metallic.
  • Colour: Brass-yellow (often referred to as "fool's gold").
  • Streak: Greenish-black to brownish-black.
  • Hardness: 6 to 6.5 on Mohs scale.
  • Cleavage or Fracture: No true cleavage; conchoidal fracture.

3. Dioptase

  • Composition: Hydrated copper silicate (CuSiO₃·H₂O).
  • Luster: Vitreous.
  • Colour: Bright green to blue-green.
  • Streak: Green.
  • Hardness: 5 to 5.5 on Mohs scale.
  • Cleavage or Fracture: Perfect cleavage in one direction; conchoidal fracture.

4. Hematite

  • Composition: Iron oxide (Fe₂O₃).
  • Luster: Metallic to dull.
  • Colour: Often reddish-brown or silver-gray.
  • Streak: Reddish-brown.
  • Hardness: 5 to 6 on Mohs scale.
  • Cleavage or Fracture: No cleavage; uneven to sub-conchoidal fracture.

5. Magnetite

  • Composition: Iron oxide (Fe₃O₄).
  • Luster: Metallic.
  • Colour: Black or steel-gray.
  • Streak: Black.
  • Hardness: 5.5 to 6.5 on Mohs scale.
  • Cleavage or Fracture: No cleavage; uneven fracture.

6. Biotite

  • Composition: Silicate mineral; a member of the mica group, with potassium, magnesium, iron, and aluminum.
  • Luster: Vitreous to pearly.
  • Colour: Dark brown to black, often with a bronze tint.
  • Streak: White to pale brown.
  • Hardness: 2.5 to 3 on Mohs scale.
  • Cleavage or Fracture: Perfect cleavage in one direction, resulting in thin flexible sheets.

These properties provide useful information for the identification and classification of these commonly encountered minerals.