Minerals Minerals Overview atoms minerals rocks History of the Earth
MineralsMineralsMinerals Overview
atoms minerals rocks
History of the Earth
Mineral Safety Rules
Mineral Safety Rules Hand-to-Mouth Contact = use disposable
gloves when handling minerals and keep from touching your mouth and your eyes.
Wash Hands = after working with minerals wash your hands with soap and water. Samples = must remain in the classroom at all times and returned to the kit when not in use. Poison = most minerals are poisonous, but there is not a large enough sample to cause major harm. DO NOT put the minerals in your mouth!
What is a Mineral?
What is a Mineral?Minerals are free uncombined elements or
compounds. Their compositions are given as chemical formulas. The formula for fluorite is CaF2. This indicates that the calcium (Ca) atoms have combined with fluorine (F) atoms. The subscripted number (2) shows that there are twice as many fluorine atoms as there are calcium. Minerals are arranged into groups according to the chemical compositions and the crystal structure.
Crystalline Structure
MineralsMineralsThere are four things that distinguish minerals.
Naturally occurring
Generally inorganic
“Constant” chemical composition
Found in NatureFound in NatureFound in NatureFound in Nature
Not alive or produced by living process Exceptions
graphite (pencil lead)calcite (limestone/marble)aragonite (pearls)
Inorganic (usually)Inorganic (usually)
Solid substances found naturally in the Earth. Scientist have learned to make some.
“Constant” Chemical Composition
“Constant” Chemical Composition Calcite = calcium + carbon + oxygen
(CaCO3)
Quartz comes in a variety of colors.
Calcite in its purest form is clear, however, the impurities formed by elements change its color – pink, green, gray, etc.
Quartz = silicon + oxygen (S1O2)
Diamonds = carbon (C)Analyzed for color, cut, clarity, and carat.Fancy diamonds such as red, pink, purple, and blue are so rare they are not found on a gemologists color scale.
Crystalline Structure
Crystalline Structure
Halite = sodium + chlorine (NaCl)Halite is regular table salt and has a cube-like structure.
Diamond vs. Graphite (C)
The pattern that the atoms arrange in to create an element is the crystalline structure.
These two minerals are made of the exact same atoms, but are different because of theircrystalline structure.
Diamonds vs. Graphite
Diamonds vs. GraphiteDiamond atoms are strong and close
together.
Graphite are only strong in one direction and this makes them weak, soft, and flexible.
Diamonds can form only at a depth of 120 km or greater within the layers of the earth.
Scientists believe that the diamonds have been brought up through kimberlite pipes through some type of explosion and the surface has eroded over millions of years to expose them.
Graphite vs. Diamond
Graphite vs. DiamondThe Structure of the elements that make up these minerals.
Mineral PropertiesMineral Properties Luster = shiny or dullHow well does it reflect light?
Hardness = soft or hard (MOHS Scale of Harness)How difficult is it to scratch the mineral?
Streak = color of the powdered mineralWhat is the color of the mineral when powdered?
Light = opaque, translucent, transparentWill the light shine through the mineral?
Magnetism = magnetic or notWill iron cling to this mineral?
Texture = rough or smoothDoes it smell like something familiar?
Mineral Observations
Mineral Observations
Step 1 - Gather materials: hand lens and minerals.
Step 2 – Observe the minerals using hand lens and use your senses of touch, smell, and sight.
Step 3 – Illustrate the mineral using colored pencils.
Step 4 – Using a dropper place a drop of water on the mineral to make it easier to detect smell and to observe the color.
Step 5 – Write a sentence describing the texture and smell of the mineral.
Step-by-Step Procedures
Mineral TestingMineral TestingMineral A (illustration) Luster
Hardness
StreakLight
Mineral TestingMineral TestingMineral A (illustration) Luster
Dull
Hardness (Mohs Scale)
Soft (6.0 )
Streak
whiteLight
opaque
Streak ColorStreak Color
Streak ColorTest
Streak ColorTest
LightLight
LightTestLightTest
Lu
ste
rLu
ste
r
Luster Test
Luster Test
Mohs Scale of Hardness
Mohs Scale of HardnessWay back in 1822, the German mineralogist, Friedrich Mohs
developed the 10 point hardness scale that is still used today.
Hard
ness
Hard
ness
Mohs Scale of Hardness
Mohs Scale of HardnessFredrick Mohs developed this scale to categorize minerals. Any
mineral with a higher number will scratch a mineral of a lower number.
1 Talc Talcum powder.
2 Gypsum Drywall and Plaster of Paris. Fingernail (2.5)
3 Calcite Copper Penny.
4 Fluorite Used to lower the melting temperature of iron.
5 Apatite Window Glass, is found in teeth and bones (5.5)
6 Orthoclase Steel File also used in ceramics (6.5),
7 Quartz Used in electronics and glass
8 TopazSandpaper, emeralds and aquamarinesare varieties of beryl with a hardness of 8.
9 CorundumSapphire and Ruby are types of corundum. They are two to five times as hard as topaz. Used to grind things down.
10
Diamond Four times as hard as corundum.
Hardness Test
Hardness Test
Power ConclusionPower Conclusion
1. Refers back to the prediction.I thought that . . .
2. Answers the question.I found out . . .
3. Future Research.In the future I would like to . . .
GlossaryGlossaryColor Streak: the color that a mineral leaves behind when you rub it on a black or white tile.
Light: A mineral’s light transmissivity can be described as opaque, transparent, or translucent.
Luster: describes the way the surface of the mineral reflects light.
Mineral: a solid material with atoms arranged in a repeating pattern.
Mohs Scale of Hardness: A scale of 10 minerals used to compare all minerals from softest to hardest.
GlossaryGlossaryOpaque: When light is not able to travel through a solid surface .
Rock: Material made up of one or more minerals.
translucent: When some light can travel through a solid object.
transmissivity: The ability for light to travel through a solid object.
transparent: When all the light can travel through a solid object. (clear)