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

A

Water

17
Q

Sediments rolling along the surface of the bed.

A

Rolling

18
Q

A series of jumping movement of sediments.

A

Saltation

19
Q

Sediments suspended in the transporting media.

A

Suspension

20
Q

The volume of void space in a sedimentary rock.

A

Porosity

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
Q

Occurs when transportation ceases and sediments accumulate on Earth’s surface by collective deposition processes.

A

Deposition

26
Q

Encompasses a suite of low temperature processes that affect sediments after their accumulation, typically after burial.

A

Diagenesis

27
Q

A process of lithification that results from the expulsion of intergranular fluids caused by increases in confining pressure during progressively deeper burial.

A

Compaction

28
Q

A process of lithification that occurs when subsurface fluids precipitate minerals in the spaces between grains that bind or cement grains to one another.

A

Cementation

29
Q

Early, shallow diagenesis that occurs shortly after burial.

A

Eodiagenesis

30
Q

Later,
deeper
diagenesis.

A

Mesodiagenesis

31
Q

Still later,
later,
shallow
diagenesis that occurs as sedimentary rocks approach the surface due to erosion.

A

Telodiagenesis