L7-9 minerals Flashcards
Criteria for a mineral
- naturally occurring
- inorganic (dicey)
- SOLID (specific crystalline structure)
- CONSISTENT CHEMICAL COMPOSITION
Atom bonds within minerals and lattice influence on mineral properties
Minerals must have a crystalline structure. atoms form a repeating pattern known as a lattice
Ionic: polar soluble (NaCl, halite)
Covalent: strong and hard. not soluble. crumbly (C, diamond)
Metallic: good conductors. ductile and malleable (native Cu, copper and Au, gold)
Van der Waals: weakest bond (C, graphite)
Categories of minerals defined by anions or anionic groups.
Native minerals: composed of only one element
gold
silver
copper
Oxides: metal bound to O
hematite
magnetite
curundum
bauxite
limonite
Carbonates: metal bound to CO3
calcite
siderite
magnesite
malachite
azurite
Sulphides: metal bound to S
galena
molybdenite
pyrite
bornite
Silicates: metal bound to SiO2
Configurations of silica tetrahedra found in silicate minerals
Isolated silica tetrahedra
Chains of linked silica tetrahedra
Sheets of linked silica tetrahedra
Networks of linked silica tetrahedra
Ways minerals form.
Crystallization of magma
Metamorphism: solid minerals react with each other under high pressures and temperatures, and new minerals are formed
Weathering: minerals unstable at Earth’s surface are chemically altered by surface processes
Precipitation from a solution
Organic formation: organisms build shells (primarily of calcite or aragonite), and teeth and bones (primarily of apatite)
Describe the trend in mineral diversity over the course of earths history
Diversity of minerals has increased over time from about a dozen 4.6 billion years ago to >5600 today
Properties of minerals
Colour, streak, lustre, hardness, crystal habit, cleavage/fracture, and density
Cause of mineral properties
Composition and structure