Lecture 6 Flashcards

(44 cards)

1
Q

Plutons:
Shape:
Orientation

A

Tabular, massive

Discordant, concordant

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2
Q

Tabular:
Massive:
Discordant:
Concordant:

A

Tabular: Stock
Massive: Batholith (>100 square km)
Discordant: Dike
Concordant: Sill, Laccolith

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3
Q

Laccolith vs lopolith

A

Mushroom-like roof – laccolith

Upo: lopolith

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4
Q

Mechanical (breaking):

Chemical:

A

Sediments

Dissolved ions

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5
Q

Agents of weathering

A

Water, wind, ice

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6
Q

Mechanical Weathering Types

A
Frost wedging – freezing and thawing of ice
Salt crytal growth 
Dessication cracks
Sheeting/unloading
Biological activity
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7
Q

Chemical weathering types

A

Dissolution,

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8
Q

Chemical weathering stability series

A

Goldich Stability series (inverted Bowen’s reaction series)

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9
Q

Rates of weathering
Climate & Relief
Arid and high relief
Humid and low relief

A

Arid: less chemical weathering, more physical weathering
Humid: enhanced chemical weathering

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10
Q

Layer of rock and mineral fragments produced by weathering

A

Regolith

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11
Q

Combination of decomposed and disintegrated rock (mineral matter) ) and organic matter (humus), water, and air, portion of regolith that supports plant life

A

Soil

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12
Q

Controls of soil formation

A

Climate and topography (slope)
Parent material and biological factors (plants, animals)
time

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13
Q

Soil O,A,E,B,C,R

A
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
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14
Q

Top soil, subsoil, regolith, true soil

A

Top soil: O and A
Subsoil: O – B
Regolith : R na may unting C
True soil: Subsoil

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15
Q

Incorporation and transportation of material by a mobile agent such as gravity, wind, water, ice or fauna

A

Erosion

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16
Q

Maximum sediment grain size an agent of erosion can transport

A

Competence

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17
Q

Maximum load of sediments of an agent of erosion

A

capacity

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18
Q

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

A

Deposition
wind, water currents
precipitation
organic material

19
Q

Deposition

  1. Wind and water currents; melting glacier
  2. chemical/ temperature changes
  3. undecayed organic materials pile up
A
  1. solids

2. dissolved materials

20
Q

Sum of physical and chemical processes by which sediments are lithified into sedimentary rocks

A

Diagenesis (formation of sedimentary rock)

21
Q

Burial by succeeding sedimentation/

compacting sediments together

22
Q

Precipitation of the cement (‘glue”) around dusts from pore waters (gluing sediments to form sedimentary rocks)

23
Q

Unstable crystals to more stable counterparts

A

Recrystallization

24
Q

Dissolution of unstable to be replaced by a more stable mineral

25
post-diagenesis, Burrowing animals that leave marks
Bisturbation
26
``` physical breakdown (disintegration) and chemical alteration (decomposition) of rocks at or near the Earth’s surface. products: ```
• Weathering | sediments, dissolved ions
27
structures that result from emplacement of igneous materials at depth.
plutons
28
massive, >100 sq. km in outcrop area, and granitic. It is the largest intrusive igneous bodies
batoliths
29
smaller than batholiths and granitic
stock
30
Discordant, cuts across bedding surfaces in the host rock
dikes
31
nearly horizontal, concordant bodies
sill
32
- concordant pluton with dome or mushroom-like roof and planar base, injected between sedimentary strata
Laccolith
33
igneous intrusion associated with a structural basin, with contacts that are parallel to the bedding of the enclosing rocks.
Lopolith
34
TYPES OF WEATHERING
* Mecanical | * Chemical
35
AGENTS OF WEATHERING
* Wind * Water * Ice
36
process in which big rocks are broken increasingly into smaller pieces.
Mechanical Weathering-
37
Types of mechanical weathering • *- freezing and thawing of ice • *- evaporation of saline water leaving salt • *- thermal expansion/contraction of water normally due to alternating dry and wet season. • *- exfoliation, joints( linear but indicates movement) • *
``` Frost wedging Salt Crystal Growth Dessication Cracks Sheeting/Unloading Biological Activity ```
38
* Frost wedging- * and * of ice * Salt Crystal Growth- *of saline water leaving * * Dessication Cracks- thermal * of water normally due to *dry and wet season. * Sheeting/Unloading- *, joints( *but indicates movement) * Biological Activity
freezing , thawing evaporation, salt expansion/contraction, alternating exfoliation, linear
39
``` *- breaks down * and internal structure of minerals producing more *constituents. • Hydration • * • Reduction • * ```
Chemical Weathering, rocks component, stable Oxidation Dissolution
40
``` Chemical Weathering- breaks down rocks component and * of *producing more stable constituents. • * • Oxidation • * • Dissolution ```
internal structure, minerals Hydration Reduction
41
RATES OF WEATHERING * : joints and fractures * : Goldich Stability Series
Structure | Composition
42
RATES OF WEATHERING Structure: * Composition:*
joints and fractures | Goldich Stability Series
43
Process in seawater • Dissolved and suspended load- *and *on the shallow parts • *- jumping of sediments • *- sediments are dragged to the surface
dissolution, suspension Saltation Traction
44
Process • *- dissolution and suspension on the shallow parts • Saltation- *of sediments • Traction- sediments are *to the *
Dissolved and suspended load jumping dragged, surface