surface processes;making new rocks Flashcards

(30 cards)

1
Q

give examples of physical weathering

A

Ice wedging
jointing

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2
Q

what structure is a product of ice wedging?

A

Talus cones; base of cliffs

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3
Q

what are the origins of jointing?

A

Cooling and contraction; columnar joints from lava flow

Expansion after being unloaded; jointed bedding planes from erosion of top layers.

Enlarged by chemical weathering; Limestone dissolved by acid rain

Exfoliation; layers peel off parallel to rock surface

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4
Q

What is the importance of jointing?

A

Groundwater flows through joints.

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5
Q

What are some associated processes involved in jointing?

A

Mineral wedging
Thermal expansion; spalling
Root wedging
Animal activity

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6
Q

how does jointing increse chemical weathering?

A

Chemical weathering acts faster on rocks with exposed surfaces.

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7
Q

Give examples of chemical weathering

A

Dissolution
Hydrolysis
Hydration
Oxidation

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8
Q

What are examples of minerals that often fall victim to dissolution?

A

Salts (halite) and carbonates (calcite)

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9
Q

Give an example of a formula for dissolution

A

Calcite (limestone) + Carbonic acid = Calcium ions + Bicaronate ions

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10
Q

What is a common formula for hydrolysis?

A

Feldspar (granite) + Carbonic Acid + H2O = Kaolinite (clay) + Dissolved ions + Silicic acid

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11
Q

What is a real world example of hydrolysis?

A

St Austell, Cornwall
Feldspar into “china clay”

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12
Q

What is a common formula for hydration?

A

Anyhydrite (crystal) + H2O = Gypsum (plasterboard)

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13
Q

What is a common formula for oxidation?

A

Fe sulphide + O2 + H2O = Fe oxides/hydroxides + sulphur compounds (RUST)

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14
Q

What is a rock example of oxidation?

A

Pyrite “fools gold”

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15
Q

What are the main products of weathering?

A

Dissolved ions
Eroded rock material
new minerals formed
Regolith

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16
Q

What are the factors controlling weathering?

A

Mineral composition
Rock type and texture
climate

17
Q

How does climate affect weathering?

A

Increasing temp by 10°C doubles rate of chemical weathering.
If annual rainfall is <25cm, weathering is minimal.

18
Q

Is weathering self limited?

A

Yes; Regolith limits water movement which then limits uplift.

19
Q

What are the importances of weathering?

A

Formation of sedimentary rocks

Regulates Earths Carbon balance.

Shaping the landscape

Economic mineral deposits.

20
Q

What are the steps to forming a sedimentary rock?

A

Weathering

Erosion

Transportation

Deposition (sedimentation)

Burial + compaction

Diagenisis

21
Q

What conditions do diagenisis occur in?

A

Shallow depths and at around 300°C

22
Q

What processes occur in diagenisis?

A

Compaction; squeezing out water.

Cementation; Precipitation of new minerals.

LITHIFICATION.

23
Q

What is the difference between Porosity and Permeability?

A

Porosity; Indicates the empty spaces in rocks

Permeability; Ability for fluids to flow through th rock.

BETTER THE SORTING, THE HIGHER THE POROSITY.

24
Q

What are the three types of sedimentary rocks?

A

Chemical/biochemical; Limestone

Organic; Coal

Clastic; Quartz

25
How are Clastic rocks classified?
Grain size Grain shape Sorting Compositional Maturity
26
What are the general grain sizes of clastic rocks?
Sandstone; 2mm Siltstone; .062mm Claystone; .004mm
27
What are the two major grain shapes?
Breccia (Angular) Conglomerate (Rounded)
28
What is the general trend compositional maturity follows?
Alluvial Fan to River to Beach.
29
Where would mature clasts be found?
Quartz are concentrated in AEOLIAN landscapes (beaches)
30
Where would the major compositional groups of sandstone be found?
Lithic sandstone; A delta Arkose; Alluvial fan Quartz Arenite; Beach Graywacke; Submarine fan