Introduction to minerals Flashcards
Definition of a MINERAL
A natural occurring inorganic solid, crystalline substance which has a fixed structure and a chemical composition which can be fixed or varied
MINERALOID
An amorphous solid material without a fixed composition, can be organic and can be man made
MINERALS
Crystals- solids that are naturally bounded by flat faces meeting at sharp edges, with a crystal shape(lattice), often referred to as the building blocks of rock - most behave as ionic solids
Ionic bonding
The attraction of opposite charges (transferring and accepting of electrons from the valence shell)
Covalent bonding
The sharing of electrons in the valence shell
Metallic bonding
The attraction between the delocalized electrons present in the lattice of the metals
Ions
Atoms with positive or negative charges due to loss or gain of electrons
Anion
An atom that has gained electrons, therefore has a negative charge and has more electrons than protons
Cation
An atom that has lost electrons, therefore has a positive charge and has more protons than electrons
Unit cell
The smallest arrangement of atoms which may be repeated regularly in 3 dimensions to form a crystal lattice
Ionic Radius
The size of atoms within an ionic solid- determines how ions pack together to form minerals
Coordination number
The number of anions around each cation in the crystal lattice - controlled by the ionic radii of the cations and anions
Radius Ratio
rc/ra - radius of the cation / radius of the anion
Igneous environment growth
High temp = >700°C - melting varied pressure Minerals are free to grow how they like Minerals formed in this environment: Moderately hard to hard Anhydrous and hydrous Good crystalline shape if they crystallize early
Metamorphic environment growth
Moderate to high temp = 200-700°C - no melting, solid State recrystallisation
Low to high pressure
In some cases abundant water
Minerals form in a confined space hence their shape is
strongly influenced by pressure gradients
Mineral formed in this environment:
Moderately hard to hard
Hydrous and anhydrous
Poor Crystalline shape
Geothermal environment growth
Moderate temp = 200 - 500°C Low pressure Abundant water and oxygen Minerals are able to form in free environment - minerals deposited in cavities and fractures Minerals formed in this environment: Soft Hydrous Often has a good crystalline shape Many valuable ores are formed in this environment
Weathering environment growth
Low temp and pressure - Earth's surface Abundant water and oxygen Minerals are able to form in free environment Large variety of chemical components Minerals formed in this environment: Soft Hydrous Good crystalline shape Characterized by clays
Hardness
Resistance of a mineral to abrasion, reflection of strength of atomic bonds
Clevage
Tendency for a mineral to split along a particular plane, occurs along layers of weak bonds in the crystal lattice.
Fracture
How a mineral breaks when lacking weak planes in its structure
Specific gravity (density)
Mass per unit volume of a mineral
Streak
Colour of powdered mineral, often more diagnostic than colour