Transcript MINERALS
MINERALS Chemical composition of the Crust Oxygen most abundant- 46.6% Followed by silicon and aluminum Iron, Calcium, Sodium, Potassium, Magnesium The most common minerals will be composed mostly of these elements Silica & silicates MINERAL vs. ROCK ROCK An aggregate of one or more MINERALS (usually- coal, organic) MINERAL Solid Crystalline- orderly arrangement of atoms Naturally occurring Inorganic Definite chemical composition e.g. SiO2 for quartz; KAlSi3O8 for feldspar Atom & Elements Atoms Neutral Nucleus Proton, Electron Ions Electrical neutron Charge Molecule- e.g. water molecule Chemical activity Stable atoms want positive & negative charges balanced electron shells full Ions- positive (Cations) and negative (Anions) Bonding Ionic Covalent Metallic Van der Waal’s Element Atomic number Number of PROTONS Isotope Differing number of NEUTRONS Atomic weight Mass of PROTONS and NEUTRONS Crystallinity 3 dimensional orderliness of atoms Silicon-oxygen tetrahedron Silicate structures Single- e.g. olivine Chain Single chain- pyroxene Double chain- amphibole Sheet- e.g. mica, clay Framework- e.g. quartz, feldspar MINERALS Crystalline solids Natural and Inorganic Substances Definite chemical composition Can be written as a chemical formula Solid solution (within a range) Important Minerals Quartz (most abundant) FELDSPAR Group Potassium Feldspar - Orthoclase Plagioclase Feldspar Sodium (Na) Albite Calcium (Ca) Anorthosite Important Minerals PYROXENE Group- Augite most common AMPHIBOLE Group- Hornblende most common MICA Group- Si + O in sheets Biotite Muscovite CALCITE- CaCO3 Properties of Minerals Color Not always reliable (Olivine, green; Flourite, yellow, purple, green…) Ferromagnesian minerals green or black Streak- powdered form Luster- reflectance of light Metallic Nonmetallic Vitreous Earthy or Glassy Properties of Minerals Hardness- resistance to scratching Moh’s Hardness Scale Fingernail = 2.5 Penny = 3.5 Knife/Glass = 5.5 Streak Plate= 6.5 Crystal Form Law of Constancy of Interfacial Angles Cleavage Properties of Minerals Quality (poor, good, perfect) Number of directions One- e.g. Mica Two at right angles- e.g. Feldspar, Pyroxene Two not at right angles- e.g. Amphibole Three at right angles (cubic)- e.g. Halite Three not at right angles (rhombohedral)- e.g. calcite Four (Flourite) or six (Sphalerite)- not common Properties of Minerals Fracture Absence of cleavage Irregular fracture Conchoidal fracture- Quartz Density Specific Gravity Some unusual properties Striations, refraction Magnetism, Taste, Odor, Double Chemical tests Reaction with HCl Calcite effervesces ROCK CYCLE Equilibrium Interrelationships between igneous rocks sediment sedimentary rocks metamorphic rocks weathering and erosion Plate Tectonic Example ROCK CYCLE Equilibrium Interrelationships between igneous rocks sediment sedimentary rocks metamorphic rocks weathering and erosion Plate Tectonic Example