minerals mineral- a naturally occurring, inorganic solid that has a definite chemical composition...
TRANSCRIPT
Minerals• Mineral- A naturally occurring, inorganic
solid that has a definite chemical composition and crystal structure
• All minerals must:• Occur naturally in/on the Earth• Be inorganic (not formed from living things or the
remains of living things)• Be a solid• Have a definite chemical composition• Have a characteristic crystal structure
• There are about 2500 different kinds of minerals
Identifying Minerals
• Minerals have certain physical properties that can be used to identify them
• Some properties can be observed just by looking at the mineral
• Color• Luster• Crystal shape• How it breaks
• Certain properties can only be determined by testing• Hardness• Streak• Specific Gravity• Acid test
Mineral Color• The color of a mineral often helps to identify
it, but very few minerals can be identified by color alone
• Why?
– Many minerals have similar colors
– Impurities can produce different colors
– Some minerals change color due to exposure
Mineral Luster• Luster- Describes the way a mineral
reflects light from its surface• All minerals have either a metallic or
nonmetallic luster
•Metallic luster- When a mineral looks and/or shines like a metal (ex.- pyrite)•Nonmetallic luster- when a mineral doesn't reflect light or look like a metal (7 types)
Nonmetallic Mineral Lusters
1. Vitreous or Glassy- Quartz
2. Pearly- Mica
3. Resinous or Waxy- Sphalerite
4. Silky- Asbestos
5. Adamantine (hard or unbreakable)- Diamond
6. Greasy or Oily- Talc
7. Dull or Earthy- Sulfur
Crystal Shape• All minerals have a characteristic crystal
shape that results from the way atoms or molecules come together when the mineral is forming
• The conditions in which the mineral formed, may make it difficult to determine its crystal shape (crystals need room and time to develop)
• Crystal- Solid in which the atoms or molecules are arranged in definite repeating patterns
Crystal Systems All minerals have internal atomic patterns in one of 6 possible
crystal systems
Crystal System ExamplesCubic Fluorite Halite
Tetragonal Wulfenite Zircon
Orthorhombic Sulfur Topaz
Monoclinic Malachite Orthoclase feldspar
Triclinic Amazonite Plagioclase feldspar
Hexagonal Quartz Tourmaline
Crystal Systems
Halite
ZirconQuartz
Staurolite
Gypsum
Rhodonite
Cleavage & FractureThe way a mineral breaks can be used in its identification
(related to the mineral’s internal arrangement of atoms)
•Cleavage- The tendency of a mineral to split along smooth, definite surfaces
•Cleavage planes may meet at angles that form geometric patterns similar to crystal shapes
Cleavage & Fracture
• Fracture- When a mineral breaks along a rough or jagged surface
• Types of fracture:1. Conchoidal or shell-like- Smooth
curved surface, like the inside of a clam shell
(ex.- Obsidian)
2. Fibrous or splintery- Jagged surface with
sharp uneven edges (ex.- Copper)
3. Uneven or irregular- Surface is generally rough
all over (ex.- serpentine)
Mineral Hardness• Hardness- The ability of a
mineral to resist being scratched
• Mohs’ scale- A reference guide for determining the hardness of minerals that uses ten minerals arranged in order of increasing hardness
The Girls Came From All Over Quebec To Collect Diamonds
Determining the Hardness of a Mineral
To determine the hardness of an unknown mineral:1. Rub the mineral against the surface of a mineral (or other
substance) that you know the hardness of2. If the unknown mineral scratches the known mineral, it is
harder than the known mineral3. If the unknown mineral is scratched by the other mineral,
then it is softer than that mineral 4. If neither mineral scratches the other, they have the same
hardness5. Based upon the scratch test, minerals are assigned a
number between 1 and 10 (with .5 increments)
Streak• Streak- The color of a mineral in its
powdered form– Produced when a mineral is rubbed against a
hard, rough surface– Usually a piece of unglazed porcelain known as a
streak plate• Even though the color of a mineral may vary,
its streak does not• For many minerals, its color and the color of its streak may be different
Specific Gravity• Specific Gravity- The ratio of the weight of a mineral to the weight of an
equal volume of water
– Tells you how many times as heavy as water a mineral is
– To Calculate:
Specific gravity = Wt. of mineral in air Wt. of an equal volume of water
OR
Specific gravity = Wt. of mineral in air Loss of wt. in water
– Typical Specific Gravities:• Nonmetallic minerals- less than 3• Metallic minerals- about 5• Pure gold- 19.3
The Acid Test• Some minerals fizz or bubble when
hydrochloric acid (HCl) is dropped on them– The HCl reacts with the mineral and
produces carbon dioxide (CO2) gas
– Can be used to identify calcite, copper, and other carbonate minerals
Special Properties of Minerals
1. Magnetism- Magnetite
2. Taste- Halite (Rock Salt)
3. Fluorescence (Glows under UV light)- Scheelite and some Calcites
4. Phosphorescence (Glows without UV light)- Sphalerite
5. Radioactivity- Uranium
6. Double refraction (Splits light rays into two parts, causing double vision)- Calcite
7. Smell- Sulfur
From Minerals to Rocks
• “Minerals are to rocks as letters are to words” (Quote from Professor R. Lingner, WSC)
• Rocks- Hard substances composed of one or more minerals
• Usually made of more than one type of mineral • May contain naturally occurring substances
that would not be considered a mineral• Are grouped according to how they form as
either igneous, sedimentary, or metamorphic