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MINERALS
• SOLID• INORGANIC• NATURALLY OCCURRING• CONSTANT PHYSICAL PROPERTIES
AND CHEMICAL CHEMICAL COMPOSITION
• SET INTERNAL STRUC TURE OF ATOMS
CHEMISTRY
• ATOMS– NEUTRONS– PROTONS– ELECTRONS
• ATOMS HAVE SNUG FIT• ATOMS HAVE NEUTRAL CHARGE• ATOMS HAVE BONDING
– IONIC– COVALENT– METALLIC
• TO FORM MINERALS
CRYSTAL CHEMISTRY
• POPULARITY LIST:• Si, O, Al, Fe, Mg, K,Na, Ca• Si and O form basic silica tetrahedron and has
snug fit and covalent bonding• SiO4 does not have 0 net charge, but Oxygen
sharing and other ions give 0 net charge• Different arrangements result in different Silicate
minerals.
MINERAL PHYSICAL PROPERTIES
• LUSTER• COLOR TRUE/STREAK(FOR METALLIC
MINERALS)• HARDNESS• CLEAVAGE/FRACTURE• DENSITY• REACTION TO ACID• MAGNETISM• TASTE
VARIETY OF IGNEOUS ROCKS
• BOWENS REACTION SERIES-SEQUENCE OF CRYSTALLIZATION
• DIFFERENTIATION– GRAVITY SETTLING– MAGMA MIXING
VISCOSITY OF MAGMA
• SILICA CONTENT INCREASE
• TEMPERATURE DECREASE
• GAS CONTENT
• INCREASES VISCOSITY
QUIET ERUPTIONS:LAVA FLOWS, FINE GRAINED, LOW
VISCOSITY, QUIET ERUPTIONS, LOW SILICA, HIGH TEMPERATURE, GAS. SHIELD VOLCANOES, MELTING IN
MANTLE
EXPLOSIVE ERUPTIONS:PYROCLASTIC ROCKS, HIGH VISCOSITY
HIGH SILICA, FRAGMENTAL, LOW TEMPERATURE, GAS, STRATO- VOLCANOS, CONVERGENT BOUNDARIES-MELTING IN
SUBDUCTION ZONE
PLUTONIC ROCKS
• COOLED SLOWLY DEEP BENEATH THE SURFACE
• COARSE GRAINED, CRYSTALLINE
• DIKES, SILLS, BATHOLITHS
• GRANITE, DIORITE, GABBRO, PERIDOTITE
SEDIMENTARY ROCKS
• CLASTIC-BROKEN ORIGIN
• CHEMICAL/BIOCHEMICAL ORIGIN
• HISTORY OF SEDIMENTARY ROCKS