Lecture 6 Flashcards
(44 cards)
Plutons:
Shape:
Orientation
Tabular, massive
Discordant, concordant
Tabular:
Massive:
Discordant:
Concordant:
Tabular: Stock
Massive: Batholith (>100 square km)
Discordant: Dike
Concordant: Sill, Laccolith
Laccolith vs lopolith
Mushroom-like roof – laccolith
Upo: lopolith
Mechanical (breaking):
Chemical:
Sediments
Dissolved ions
Agents of weathering
Water, wind, ice
Mechanical Weathering Types
Frost wedging – freezing and thawing of ice Salt crytal growth Dessication cracks Sheeting/unloading Biological activity
Chemical weathering types
Dissolution,
Chemical weathering stability series
Goldich Stability series (inverted Bowen’s reaction series)
Rates of weathering
Climate & Relief
Arid and high relief
Humid and low relief
Arid: less chemical weathering, more physical weathering
Humid: enhanced chemical weathering
Layer of rock and mineral fragments produced by weathering
Regolith
Combination of decomposed and disintegrated rock (mineral matter) ) and organic matter (humus), water, and air, portion of regolith that supports plant life
Soil
Controls of soil formation
Climate and topography (slope)
Parent material and biological factors (plants, animals)
time
Soil O,A,E,B,C,R
Organic matter A –mineral + some humus E-luvation/leaching B- accumulation of different materials C – partially altered parent material R – bed rock – unweathered parent material
Top soil, subsoil, regolith, true soil
Top soil: O and A
Subsoil: O – B
Regolith : R na may unting C
True soil: Subsoil
Incorporation and transportation of material by a mobile agent such as gravity, wind, water, ice or fauna
Erosion
Maximum sediment grain size an agent of erosion can transport
Competence
Maximum load of sediments of an agent of erosion
capacity
process where sediments, soil, and rocks are added to a land mass such as when
• When *and * slows down and as glacial ice melts
• When chemical/temperature changes causes *
• When decayed * piles up
Deposition
wind, water currents
precipitation
organic material
Deposition
- Wind and water currents; melting glacier
- chemical/ temperature changes
- undecayed organic materials pile up
- solids
2. dissolved materials
Sum of physical and chemical processes by which sediments are lithified into sedimentary rocks
Diagenesis (formation of sedimentary rock)
Burial by succeeding sedimentation/
compacting sediments together
Compaction
Precipitation of the cement (‘glue”) around dusts from pore waters (gluing sediments to form sedimentary rocks)
Cementation
Unstable crystals to more stable counterparts
Recrystallization
Dissolution of unstable to be replaced by a more stable mineral
Replacement