Igneous Rocks
Form when magma cools and crystallizes; rate of cooling controls crystal size
Crystallization of magma
Intrusive
Cools slowly
Forms large crystals
Batholiths
Extrusive
Cools quickly
Fine crystals
Volcanoes
Classification of Igneous Rocks
Texture
Coarse
Fine
Porphyritic
Glassy
Vesicular
Composition
Felsic
Intermediate
Mafic
Bowen's Reaction Series
Order of mineral crystallization
When a mineral remains in melt, will react with magma to produce new minerals
Sedimentary Rocks
Form at or near surface
Fossils and economically important deposits
Classification
Detrital; once another type of rock which has been eroded and deposited
Size
Conglomerate/breccia
Sandstone
Siltstone
Shale
Composition
Quartz sandstone
Arkose
Chemical; precipitate from compounds that were dissolved in water
Inorganic processes
Evaporites; gypsum, halite
Microcrystallize varieties of quartz, chert, flint, jasper, agate
Travertine
Biochemical processes
Limestone
Chalk
Lithification of detrital sedimentary rocks
Compaction
Cementation
Common cements
Features of Sedimentary Rocks
Beds or strata
Fossils; age and environment
Ripple marks
Mudcracks
Interlocking crystals; chemical sedimentary rocks
Metamorphic Rocks
Form by change in texture and composition of pre-existing rocks; form deep in surface under influence of heat, pressure, and chemically active fluids
Types of metamorphism
Regional; mountain building forces; large scale; most rocks
Contact; adjacent to magma
Metamorphic Agents
Heat
Pressure
Chemically active fluids
Classification of metamorphic based on texture
Foliated
Schist
b. Velocity determines the amount and size of material carried
Controls on velocity
Gradient
Shape
Discharge
Profile
Head or headwaters
Mouth
Work of Running Water
Erosion; as a stream flows it erodes by the action of water and sediment carried
Transportation; competence is the maximum size of particle a stream can carry
High competence at flood stage
Capacity is the maximum load a stream can carry
Loads
Dissolved load; material carried in solution; very fine particles; clay and silt; comes from ground water and dissolution of rocks along the river's course