Mineral Properties and Bonding and Mineral Classes Flashcards
Define the major groups within the carbonate class
- Anhydrous carbonates: Calcite group (e.g., calcite, magnesite) and Aragonite group (e.g., aragonite, cerussite).
- Anhydrous carbonates with compound formulas: Dolomite group (e.g., ankerite, dolomite).
- Carbonates with hydroxyl or halogen: (e.g., malachite, azurite).
- Hydrated carbonates: (e.g., lansfordite).
definition of carbonate
Carbonates are a class of minerals with the basic anionic unit consisting of a triangle with a carbon, nitrogen, or boron atom at the center.
Difference between Calcite, Dolomite, and Aragonite:
- Calcite is the most common carbonate mineral, with a trigonal-hexagonal crystal structure. It is used in cement and lime production.
- Aragonite is another polymorphic form of CaCO3, occurring in orthorhombic crystals. It is typically acicular in shape.
- Dolomite has a similar composition to calcite but differs in crystal structure. It contains alternating layers of calcium and magnesium, resulting in distinct cleavage and acid reaction differences.
Describe the major groups of native elements,
sulphides, oxides and hyroxides, their properties and use
- Native Elements: Only 20 elements occur naturally in their elemental state, such as gold, silver, copper, and sulfur.
- Sulphides: Sulphide minerals contain the S2- anion and are important ores of various metals, including pyrite, pyrrhotite, and chalcopyrite.
- Oxides: Oxides include minerals like hematite, rutile, and magnetite, often exhibiting dark colors and symmetry in their crystal structures.
- Hydroxides: Hydroxides share properties with oxides and commonly include iron hydroxides like goethite formed through weathering of iron minerals.
Use Moh’s hardness scale and appreciate its importance in identifying minerals.
The Mohs hardness scale is a scale from 1 to 10 that measures the relative hardness of minerals. It is based on the ability of a mineral to scratch another mineral. The scale helps in identifying minerals because harder minerals can scratch softer minerals, but not vice versa.
List the four kinds of bonds, and how they relate to hardness and other physical properties.
The four kinds of bonds are covalent, ionic, metallic, and van der Waals.
Covalent bonds are the strongest + sharing of electrons
ionic - ions joined in crystal structure (strong) + one ion has pos charge other has neg (cation and anion)
metallic bonds - weak bond + electron is free to drift through the structure
van der waals bond - weakest bonds + ‘forces’ tie neutral molecules into lattice + not often found in minerals (micas, clays)
Define the terms cleavage and fracture.
- Cleavage is the tendency of minerals to break along specific planes of weakness due to differences in bond strength. It results in smooth, flat surfaces.
- Fracture is the way a mineral breaks when it does not follow cleavage planes. Fracture surfaces can be irregular and lack atomic order.