Weathering Flashcards

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1
Q

What does endogenic mean

A

Within the earths surface eg plate tectonics

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2
Q

What does exogenic mean

A

At or very near the earths surface eg denudation

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3
Q

What is denudation

A

The break up of rock and removal of the broken material

Includes, weathering, erosion and mass movement

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4
Q

Weathering is influenced by

A

Rock type eg rocks with bedding planes are easier to break down
Climate influences type of weathering and speed
Topography, upland areas are more exposed to weathering

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5
Q

Two types of weathering

A

Physical (mechanical)

And chemical

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6
Q

What does physical weathering change

A

Physical appearance of rock

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7
Q

Two types of physical weathering

A
Freeze thaw (frost wedging)
Exfoliation (onion weathering)
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8
Q

Conditions needed for freeze thaw

A

Adequate supply of water
Rock has pre existing fractures and joints
Temperature regularly rises and falls

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9
Q

How much does water expand when turning into ice

A

9%

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10
Q

What is scree

A

Broken material made when rock is weathered

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11
Q

Example of freeze thaw in Ireland

A

Sugarloaf Wicklow

Carrontoohil Kerry

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12
Q

What is diurnal temperature range

A

Big difference between the highest and lowest temperature

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13
Q

Temperatures in desert at day

A

40° c +

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14
Q

Temperatures in desert at night

A

0° c

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15
Q

Why is it so hot in the desert during the day

A

Lack of cloud

Lack of vegetation

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16
Q

Example of exfoliation

A

Half dome in Yosemite national park

17
Q

What is chemical weathering

A

The decay of rocks and change in chemical makeup

18
Q

Where does chemicals weathering work best

A

Hot, humid conditions

19
Q

Two types of chemical weathering

A

Carbonation

Hydrolysis

20
Q

What does a weak carbonic acid consist of

A

Rain water and carbon dioxide from atmosphere and soil

21
Q

What rocks erode best

A

Limestone and chalk, bedding planes

22
Q

Example of landscape weathered by carbonation

A

The burren co Clare

Marble Arch caves, Fermanagh

23
Q

What does hydrolysis do to the rock

A

Reacts with chemical breaking in into a softer and weaker material.

24
Q

Example of hydrolysis in Ireland

A

Leinster batholith soil

25
Q

Why is hydrolysis important

A

Makes healthy soil

26
Q

Explain freeze thaw action

A
Occurs when temperatures move above and below freezing
Adequate rainfall
Pre existing fractures
9% size increase from water to ice
Expand cracks
Cycle
Scree
27
Q

Explain exfoliation

A
Large diurnal temperature range
Deserts (day 40° and night 0°)
No clouds and lack of vegetation 
Rock expands when heated 
Contracts when cooled
Outer layers heat up quicker 
Flakes- large slabs of scree
Newly exposed outer layers - cycle continues

Darker absorb more light and different minerals cause to expand at different rates eg quartz quicker than feldspar

28
Q

Explain carbonation

A

Rainwater absorbs carbon dioxide from atmosphere and soil
Makes a weak carbonic acid
Acid dissolves rock, changing minerals
Calcium carbonate changes to calcium bicarbonate
Sinks through rock
Mostly limestone - clints, grikes, easy access

29
Q

Explain hydrolysis

A

Water reacts with chemicals in the rock making it softer and break down
Fine grained rock quicker to break down
Affected by temperature - every 10° increase, rate doubles
Eg Brazil rainforest 20m deep soil
Acidic water changes feldspar to kaolin. Clay like material
Feldspar was the glue that held everything together but now rock begins to crumble
Leinster batholiths