Transcript
Page 2: Minerals - Identifying Minerals

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

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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.

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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

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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.

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Texture• Some Minerals have a peculiar

feel.• Example: Talc (Soapy) or Graphite

(Silky)

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Luster• Luster is the way a mineral

reflects light.• It is often described as either

metallic or nonmetallic.

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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.

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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

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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.

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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.

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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.

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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.

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Magnetism• Magnetism: Some minerals

are attracted to magnets and metals.

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Acid test• Acid Test: Weak HCL acid on

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

• CO2 is given off as bubbles.

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Smell• Smell: Some minerals have a

peculiar smell• Example: Sulfur

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TasteSome Minerals have a peculiar taste.Example: Halite

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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

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Fluorescence• Some minerals glow brightly

under a black light. • Minerals glow because they have

impurities in them called activators


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