Ch 4a: Minerals Flashcards
Minerals
naturally occurring, inorganic, fixed composition or range of composition, solid, repeating atomic structure (crystalline)
Atoms and Elements
Theres about 90 naturally occurring elements in the periodic table.
Top 8 elements in the Earth
Iron (most in the core), Oxygen, Silicon, Magnesium, Nickel (most in the core), Sulphur, Calcium, Aluminum
Top 8 elements in the Crust (oceanic order)
Oxygen, Silicon, Aluminum, Iron, Magnesium, Calcium, Potassium, Sodium
Top 8 elements in the Crust (surface order)
Oxygen, Silicon, Aluminum, Iron, Calcium, Magnesium, Potassium, Sodium
_____ are responsible for chemical properties
Electrons. Unfilled outer shells are unstable created by losing, gaining or sharing electrons.
Ions
atoms that have gained or lost electrons. Cations (+), Anions (-)
Three main types of bonding:
ionic, covalent, van der Waals
Ionic:
Attraction between ions of opposite charge. Transfer of electrons. Most minerals (90%)
Covalent:
Very strong attraction between two or more atoms, share electrons.
Covalent - Metallic:
Hybrid bonding, electrons are free to move among the ions; electrical glue. Great conductors, really ductile, flexible bonds
Van der Waals
force of attraction between temporary dipole molecules
Bonding in Crystals:
produces a crystal lattice: regular arrangement, controls many mineral properties
Mineral Properties:
crystal habit, hardness, cleavage, fracture, color, streak, lustre, others
Crystal Habit
Shape, reflects internal crystal structure (constant inter-facial angles). Given time and space can grow very large, limited space = minerals will interlock.
eg. Quartz = hexagonal or euhedral
Hardness
Measure of the ease with which the surface can be scratched. Mohs Hardness scale.
Mohs Hardness Scale:
devised by Austrian Friedrich Mohs , not a linear scale
Cleavage
Tendency of the mineral to break along planar surfaces.
Cleavage face (plane):
Weak bond between atoms or molecules, number of planes and geometric pattern of the cleavage is diagnostic
Cleavage and Bonding
ability to cleave varies inversely with bond strength.
Polymorphism
Ability of a solid material to exist in more than one form or crystal structure. Common in metamorphic rocks.
eg. Diamonds and Graphite.