Sedimentary Rocks Flashcards

1
Q

What is Chemical Weathering?

A

Rocks decompose when the chemical structure of their minerals breaks down.
Produce ions that are removed in a solution leaving an insoluble residue.

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2
Q

What are examples of Chemical Weathering?

A

Carbonation and Hydrolysis

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3
Q

What is Carbonation?

A

CO2 reacts with rainwater in the soil to form carbonic acid making the groundwater more acidic than rainwater.

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4
Q

What is Hydrolysis?

A

Reaction between water and silicate minerals. Hydrogen ions from water and carbonic acid react with mineral ions.

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5
Q

What is Frost Shattering?

A

Water enters cracks and joints and freezes and expands. This exerts pressure on the rock until it fails and fractures.

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6
Q

What is Exfoliation?

A

When sheets of rock split off due to differential expansion and contraction of minerals during heating and cooling.

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7
Q

What is a clast?

A

A fragment of broken rock produced by erosion.

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8
Q

What is root action?

A

Causes the weathering of rocks by wedging action of plant roots.

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9
Q

How is weathered material transported?

A

Gravity
Wind
Rivers
Ice
Sea

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10
Q

What is abrasion?

A

Wearing away of earth’s surface due to wind, water or ice dragging sediment across surfaces.

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11
Q

What is attrition?

A

The wearing down of sediment grains due to collisions with other grains in transport.

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12
Q

What is solution?

A

Transport of ions dissolved in water such as K, Ca, Na

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13
Q

What is saltation?

A

Transport of material by bouncing

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14
Q

What is suspension?

A

Transport of material in water or air without touching earths surface.

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15
Q

What is traction?

A

Transport of material by sliding along the surface.

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16
Q

What is mineral maturity?

A

A measure of the extent of rocks being weathered and being destroyed by attrition

17
Q

What happens as mineralogical maturity increases?

A

Increase in textural maturity, one chemically stable mineral, rounded uniform grains.

18
Q

Wind transport sediment characteristics

A

Fine to medium grain size
All quartz composition
Well rounded
Very well sorted as easy to carry
High energy environment

19
Q

Ice transport sediment characteristics

A

Very coarse (boulders) to very fine (clay)
Varied composition
Angular/Sub-angular roundness
Very poorly sorted, material in every seive
Low energy environment

20
Q

River transport sediment characteristics

A

Coarse near source to fine
Quartz and mica with rock frags
Angular near source, sub-angular/rounded downstream
Wide range of sediment size in sieve
High energy environment

21
Q

Beach transport sediment characteristics

A

Medium sand
Nearly all quartz some shell and rock fragments
Sub-rounded/rounded
Moderately sorted with sediment in few sieves
High energy

22
Q

Gravity transport sediment characteristics

A

Very coarse (boulders) to very fine (soil creep)
Varied composition
Angular to very angular roundness
Very poorly sorted

23
Q
A