minerals - identifying minerals

Post on 09-Feb-2017

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Identification of Minerals

• There are a number of different properties or characteristics that can give you clues to recognize different materials.1. Color

3. Streak5. Cleava

ge

2. Luster4. Hardne

s6. Fractur

e• And Other Tests

Streak• If you were to scratch a mineral against a

hard surface, like a porcelain tile it would leave behind a streak of colored powder.

• Streak is the color of a mineral in powder form.

• Scientist use a streak plate to do the streak test.

Streak• While a mineral’s color may

change, the color of its streak usually does not. Streak is often a much more helpful way to use color to identify a mineral.

• Where do you use streak in your everyday life?• Writing with a pencil

on paper.• Which mineral do

you use to leave the streak?• Graphite

Hardness• The measure of how easily a mineral can be

scratched is known as its hardness.• Hardness of a mineral has nothing to do with

whether it breaks easily or not.• Hardness is measured by using THE MOH’S

HARDNESS SCALE, which is a scale that ranks ten common minerals hardness.

Texture• Some Minerals have a peculiar

feel.• Example: Talc (Soapy) or Graphite

(Silky)

Luster• Luster is the way a mineral

reflects light.• It is often described as either

metallic or nonmetallic.

Metallic Luster• Opaque and shiny in appearance,

the look of polished or dull metal.Metallic Examples: Gold, Copper, Pyrite, Sphalerite, Cinnabar

Submetallic Luster are ones that resemble a metal, but weathering and corrosion made them look dull or less reflective.

Non-Metallic Luster• Does not look like metals.

• Types of non-metallic luster:• Adamantine: Remarkable shine and

brilliance • Transparent / Translucent• Diamonds, Cubic Zirconia

• Earthy, Dull: Poor Reflectivity• Coarse and Porous• Kaolinite, montmorillonite

• Vitreous: Luster similar to that of glass• Transparent / Translucent• Quartz, Calcite

• Greasy: Look as if it is coated with oil/grease• Resemble fat, feel greasy/waxy• Opal, Halite

Cleavage• The way a mineral breaks apart is

another way that is helpful in identifying it.

• Sometimes when you break a mineral, it will break along flat smooth surfaces.

• This results in a nice clean cut.

Fracture• Sometimes, minerals do not break in

nice clean, flat cuts.• Minerals that DO NOT break along flat,

smooth surfaces are said to fracture.• The way a mineral break depends on the

strength and arrangements of atomic bonds within the mineral.

Cleavage and Fracture• Minerals with

Cleavage• Mica• Calcite• Halite• Fluorite

• Minerals that Fracture• Quartz• Olivine

• All minerals fracture to some extent…even those with cleavage do not break perfectly all the time.

Specific Gravity• Minerals can be identified by comparing

the weights of equal samples.• The specific gravity of a mineral is the

ratio of its weight compared to the weight of an equal volume of water.

• SG = WEIGHT OF MINERAL Weight in equal volume of water.

Magnetism• Magnetism: Some minerals

are attracted to magnets and metals.

Acid test• Acid Test: Weak HCL acid on

carbonate minerals (Those with CO2) will produce a chemical reaction.

• CO2 is given off as bubbles.

Smell• Smell: Some minerals have a

peculiar smell• Example: Sulfur

TasteSome Minerals have a peculiar taste.Example: Halite

Double Refraction• Light enters the mineral as one

beam of light, but then it separates into 2 beams

• You then will see 2 objects• Example: Calcite

Fluorescence• Some minerals glow brightly

under a black light. • Minerals glow because they have

impurities in them called activators

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