Minerals
Minerals of the World
Objectives of Lecture
To learn about minerals and their features:
Structure
Composition
Properties
One Minute Challenge Questions
Can you think of the names of any minerals?
Can you think of any uses for minerals in your everyday life or in society?
What is a Mineral?
A mineral is defined as:
A naturally occurring substance found on Earth with the following characteristics:
Characteristic chemical composition
Ordered atomic structure
Specific physical properties
Importance:
Minerals are the building blocks of rocks!
Example of a Mineral: Halite
Commonly known as salt.
Characteristics:
Chemical composition: NaCl (Sodium Chloride)
Ordered atomic structure: Atoms bond in a cube shape.
Specific physical properties include:
Appearance: Clear/white
Solubility: Dissolves in water
Taste: Salty
Hardness: Soft (can be scratched with an iron nail)
Native Elements
Definition:
Elements from the periodic table that occur as uncombined natural substances within the Earth.
Most Common Minerals on Earth
Feldspar: Chemical formula:
Quartz: Chemical formula:
Polymorphs
Definition:
Minerals that have the same chemical composition but different physical properties/structures.
Examples:
Graphite and diamond are both made of carbon but exhibit very different physical properties.
Mineral Crystal Shapes
Crystal shapes relate to how minerals are bonded.
Examples of mineral crystal shapes:
Pyrite
Mica
Quartz
More Examples of Mineral Structure
Hexagonal Quartz Crystal
Cubic Pyrite Crystal
Calcite Crystal
Trigonal Crystal
Pyritohedral Pyrite Crystal
Fluorite Cubic Crystals
Types of Bonding in Minerals
Ionic Bonding:
Definition: The transfer of electrons between atoms.
Example:
Sodium atom (Na) becomes sodium ion (Na+) when losing an electron.
Chlorine atom (Cl) becomes chloride ion (Cl-) upon gaining an electron.
Together they form sodium chloride (NaCl).
Covalent Bonding:
Definition: Electrons are shared between atoms.
Overview: Only one pair of electrons hold the nuclei together, while two pairs of electrons hold them closer and tighter.
Metallic Bonding:
Definition: Electrons move in a cloud around atoms, allowing for conductivity and malleability.
Van der Waals Bonding:
Definition: Weak bonds based on dipole attractions between atoms, similar to magnet attraction.
Example: Graphite exhibits both covalent and van der Waals bonding.
Mineraloids
Definition: Not technically minerals because they do not have an ordered atomic structure.
Examples:
Opal
Agate
Physical Properties of Minerals
Definition: The characteristics of minerals that encompass their appearance and behavior under different conditions.
Key characteristics include:
Luster: The way a mineral reflects light, categorized as metallic or non-metallic.
Color: Considered the least reliable characteristic; some minerals appear in various colors.
Hardness: The ability of a mineral to resist scratching, measured using Moh's Hardness Scale.
Magnetism: The ability of some minerals to produce magnetism.
Streak: The color of a mineral in powdered form, used for identification.
Moh's Hardness Scale
A scale that ranks minerals based on their hardness from 1 (softest) to 10 (hardest):
Talc: 1
Gypsum: 2
Calcite: 3
Fluorite: 4
Apatite: 5
Feldspar: 6
Quartz: 7
Topaz: 8
Corundum: 9
Diamond: 10
Common objects used as reference include:
Fingernail: 2.5
Copper penny: 3.5
Iron nail: 4.5
Glass: 5.5
Steel file: 6.5
Streak plate: 7.0
Testing Hardness
The process of determining a mineral's hardness by what other objects it can scratch or be scratched by.
Streak: Based on Color
Definition: The color of the mineral when powdered.
Note: Some minerals may be too hard to produce powder and instead scratch the streak plate.
Cleavage of Minerals
Definition: The ability of a mineral to break along specific planes according to its atomic structure.
Examples of cleavage:
Mica: Sheety cleavage
Galena: Cubic cleavage
Calcite: Rhombohedral cleavage
Fluorite: Octahedral cleavage
Fracture
Description: Some minerals do not cleave and instead exhibit fracturing patterns:
Example: Quartz displays conchoidal fracture.
Effervescence
Definition: The ability of a mineral to react when acid is applied.
Example: Calcite reacts with acid; this is a significant property since limestone is primarily composed of calcite. This reaction is responsible for cave formation in certain areas like Kentucky.
Effervescence: Acid Test on Calcite
An acid test is performed on calcite to demonstrate effervescence visually.
Fluorescence and Phosphorescence
Fluorescence: The ability of a mineral to glow when exposed to ultraviolet (UV) light due to high-energy light waves exciting the atoms, which release energy as light.
Phosphorescence: The ability of a mineral to continue glowing even after the UV light source is removed, similar to glow-in-the-dark materials.
Other Interesting Properties
Magnetism: Certain minerals can exhibit magnetic properties.
Piezoelectricity: The ability of some minerals to generate an electric charge under mechanical stress.
Refraction: The bending of light as it passes through a mineral, impacting how the mineral is perceived visually.
Taste: Some minerals, like halite, have distinct tastes when sampled (not recommended in practice).
Smell: Certain minerals may have unique odors.
Gemstones
Definition: Exceptional examples of minerals that possess:
A beautiful color or clarity
Rarity
Unusual processes of formation
Gemstone Forming Minerals
Examples:
Ruby: A variety of corundum
Beryl: Includes emerald as a highly valued form
Sapphire: Another variety of corundum
A Word About Testing and Identifying Minerals
Emphasis on various methods of mineral identification based on said properties and features previously discussed.
Summary
Minerals are the building blocks of rocks.
Key characteristics of minerals consist of:
Atomic structure
Chemical composition
Physical properties
These qualities can be used effectively to identify minerals.