Sedimentary Rocks (Part 1 - Sediments and Sedimentary Cycle) Flashcards

1
Q

Pieces of broken down, pre-existing rocks at or near the Earth’s surface.

A

Sediments

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2
Q

Rocks that are made-up of lithified sediments

A

Sedimentary Rocks

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3
Q

A sub-branch of Petrology that focuses on the composition, characteristics and origins of sedimentary rocks.

A

Sedimentary Petrology

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4
Q

A simple model of the processes responsible for the production of sediments and sedimentary rocks.

A

Sedimentary Cycle

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5
Q

Sedimentary Rocks’ Sequence of Formation

A

(WETDD)
Weathering
Erosion
Transport
Deposition
Diagenesis

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6
Q

The process that breaks down rocks into sediments.

A

Weathering

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7
Q

The physical removal of material by mobile agents such as water, wind, ice or gravity.

A

Erosion

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8
Q

The transfer of rock and soil downslope under the influence of gravity.

A

Mass Wasting

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9
Q

3 Factors that affect Weathering

A

(CRD)
Climate - temperature and moisture
Rock characteristics - Chemical traits of rocks
Differential weathering - Unequal weathering

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10
Q

A mixture of minerals, organic matter, water and air.

A

Soil

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11
Q

The layer of rock fragments produced by weathering.

A

Regolith

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12
Q

The study of physical and chemical properties soils and its formation.

A

Pedology

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13
Q

5 Controls of Soil Formation

A

(PTCOT)
Parent Material - source of weathered mineral matter
Time - length of time that processes have been operating
Climate - Climatic elements
Organisms - Organisms present
Topography - variations in topography

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14
Q

Zones of soil with varying composition, texture and structure found at different depths.

A

Horizons

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15
Q

A vertical section of all the soil horizons.

A

Soil Profile

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16
Q

Washing out of fine soil components.

A

Eluviation

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17
Q

Depletion of soluble materials from upper horizons.

A

Leaching

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18
Q

Constitutes the O and A horizon

A

Topsoil

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19
Q

Consists largely of organic material.

A

O Horizon

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20
Q

The zone beneath the O Horizon that is largely mineral matter, with biological activity is high and humus generally present at up to 30 percent in some instances.

A

A Horizon

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21
Q

A light colored layer that contains little organic material.

A

E Horizon

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22
Q

Also known as the Zone of eluvation

A

E Horizon

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23
Q

The zone of accumulation where much of the material removed from the E Horizon by eluviation is deposited.

A

B Horizon

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24
Q

Also known as the Subsoil

A

B Horizon

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25
Also known as the True Soil (what horizons are in it)
Solum (O,A,E and B)
26
The layer of partially altered parent material
C Horizon
27
The unweathered parent material
R Horizon
28
Explain the Soil Profile
kaya mo yan boss ikaw pa
29
A system of soil classification based on the physical and chemical properties of the soil profile.
Soil Taxonomy
30
12 Soil Orders and its Characteristics
(AAAEGHIMOSUV) or (HEAVASUMAGOI) Alfisol - High nutrient Andisol - Volcanic Aridosol - Desert Entisol - New Gelisol - Permafrost Histosol - Organic Inceptisol - Young Mollisol - Prairie Oxisol - Tropical forest Spodosol - Conifer forest Ultisol - Low-nutrient Vertisol - Swelling clay
31
The physical breakdown (me) and the chemical alteration (decomposition) of rocks at or near Earth's surface.
Weathering
32
Explain the Difference between Mechanical and Chemical Weathering
Mechanical - physical breakdown Chemical Weathering - chemical breakdown
33
5 Types of Physical Weathering
(FISSB) Frost Wedging Salt crystal growth Sheeting or Unloading Biological actions Intrusions
34
The freeze-thaw action of water trapped within fractures of rocks that cause the expansion and contraction which would eventually disintegrate rocks.
Frost wedging
35
How many % does frost wedging expands when turned into ice?
9%
36
Frost wedging that expands horizontally
Frost Wedging
37
Frost Wedging that expands vertically
Frost Heaving
38
A mode of weathering near coastlines where salt from seawater accumulate and grow through cracks of rocks and fracture them while growing.
Salt crystal growth
39
Rocks that are originally covered and are then exposed are relieved from pressure, causing an unloading action and expansion.
Sheeting or Unloading
40
What texture does sheeting produce?
Onion Texture
41
Organisms, such as plants, can burrow their roots through cracks which breaks down the rocks into pieces.
Biological Actions
42
The intrusions from beneath the surface induce pressure from below, fracturing the rock mass on the surface.
Intrusions
43
3 Types of Chemical Weathering
Solution Hydrolysis Oxidation
44
A solution mixture of reactive components specific to rocks.
Solution
45
Chemical breakdown of minerals in rocks due to addition of water.
Hydrolysis
46
Chemical breakdown of minerals in rocks due to exposure to oxygen.
Oxidation
47
The removal of materials or sediments by mobile agents such as water, wind, ice or humans.
Erosion
48
4 Transport Media
Air Water Ice Gravity
49
of the 4 Transport Media's, which one is the strongest agent?
Ice
50
of the 4 Transport Media's, which one is the most effective agent?
Water
51
2 Modes of Transport
Bedload and Suspended Load
52
Sediments rolling along the surface of the bed.
Rolling (nagulong)
53
A series of jumping movement of sediments.
Saltation (natalon)
54
Sediments suspended in the transporting media.
Suspension (lumilipad)
55
Glaciers grind against rock as they move, producing fine particles under them known as what?
Rock Flour
56
The volume of void space in a sedimentary rock
Porosity
57
Porosity associated with the original depositional texture of the sediment.
Primary Porosity
58
Porosity that developed after deposition and burial of the sediment in the sedimentary basin.
Secondary Porosity
59
The measure of how much water can move through pore spaces which also describes how water easily flows.
Permeability
60
A property of curve being tortuous, or twisted, having many turns.
Tortuosity
61
Occurs when transportation ceases and sediments accumulate on Earth's surface by collective deposition processes.
Deposition
62
Encompasses a suite of low temperature processes that affect sediments after their accumulation, typically after burial.
Diagenesis
63
A process of lithification that results from the expulsion of intergranular fluids caused by increases in confining pressure during progressively deeper burial.
Compaction
64
A process of lithification that occurs when subsurface fluids precipitate minerals in the spaces between grains that bind or cement grains to one another.
Cementation
65
5 Major Cements in Sedimentary Rocks
Silica Minerals - quartz; occurs chiefly in the form of syntaxial quartz Carbonate Minerals - sandstones and gravelstones; Iron oxides and hydroxides - hematite, geothite and limonite Feldspars - arkosic sandstones and gravelstones Clay minerals - strongly controlled by temp and pH
66
Most abundant carbonate mineral cement
Calcite
67
Early, shallow diagenesis that occurs shortly after burial
Eodiaganesis
68
Later, deeper diagenesis
Mesodiagenesis
69
Still later, shallow diagenesis that occurs as sedimentary rocks approach the surface due to erosion.
Telodiagenesis