Sed Formation Flashcards

1
Q

The process that breaks down rocks into sediments.

A

Weathering

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2
Q

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

A

Erosion

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3
Q

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

A

Mass wasting

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4
Q

Unequal weathering due
to the rock’s composition.

A

Differential weathering

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5
Q

The physical breakdown or disintegration of rocks at or near the surface.

A

Mechanical weathering

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6
Q

The chemical breakdown or decomposition of rocks at or near the surface.

A

Chemical weathering

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7
Q

The freeze-thaw action of water trapped within fractures of rocks that cause the expansion and contraction which would eventually disintegrate rocks.

A

Frost wedging

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8
Q

A mode of weathering near coastlines where salt from seawater accumulate and grow through cracks of rocks and fracture them while growing.

A

Salt groth crystal

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9
Q

Rocks that are originally covered and are then exposed are relieved from pressure, causing an unloading action and expansion.

A

Sheeting or unloading

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10
Q

Organisms, such as plants, can burrow their roots through cracks which breaks down the rocks into pieces.

A

Biological actions

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11
Q

The intrusions from beneath the surface induce pressure from below, fracturing the rock mass on the surface.

A

Intrusions

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12
Q

A solution mixture of reactive components specific to rocks.

A

Solution

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13
Q

Chemical breakdown of minerals in rocks due to addition of water.

A

Hydrolysis

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14
Q

Chemical breakdown of minerals in rocks due to exposure to oxygen.

A

Oxidation

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15
Q

The removal of materials or sediments by mobile agents such as water, wind, ice or humans.

A

Erosion

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16
Q

Most effective transport media

17
Q

Sediments rolling along the surface of the bed.

18
Q

A series of jumping movement of sediments.

19
Q

Sediments suspended in the transporting media.

A

Suspension

20
Q

The volume of void space in a sedimentary rock.

21
Q

Porosity associated with the original depositional texture of the sediment.

A

Primary porosity

22
Q

Porosity that developed after deposition and burial of the sediment in the sedimentary basin.

A

Secondary porosity

23
Q

The measure of how much water can move through pore spaces which also describes how water easily flows.

A

Permeability

24
Q

A property of curve being tortuous, or twisted, having many turns.

A

Tortousity

25
Occurs when transportation ceases and sediments accumulate on Earth's surface by collective deposition processes.
Deposition
26
Encompasses a suite of low temperature processes that affect sediments after their accumulation, typically after burial.
Diagenesis
27
A process of lithification that results from the expulsion of intergranular fluids caused by increases in confining pressure during progressively deeper burial.
Compaction
28
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
29
Early, shallow diagenesis that occurs shortly after burial.
Eodiagenesis
30
Later, deeper diagenesis.
Mesodiagenesis
31
Still later, later, shallow diagenesis that occurs as sedimentary rocks approach the surface due to erosion.
Telodiagenesis