LESSON 8 Flashcards

1
Q

Importance of Morphology of Stone Deterioration

A
  • diagnose possible causes and effects
  • plan conservation strategies
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2
Q

types of weathering (deterioration of structures)

A
  • physical weathering
  • chemical weathering
  • biological weathering
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3
Q

is the process that breaks rocks apart without changing their chemical composition

A

physical weathering

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4
Q

Physical weathering is the process that breaks rocks apart without changing their chemical composition and caused by factors such as:

A
  • thermal expansion and thermal compression
  • frost disintegration
  • salt crystallization
  • biogenic physical impact
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5
Q

(changing temperature; temperature increases-rock (minerals) expands; decreases rocks (contracts).

A

thermal expansion and thermal compression

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6
Q

(repeated cycle of ice formation and ice melt in the pore spaces and fractures of rocks; water freezes, volume increases by about 10%).

A

frost disintegration

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7
Q

(groundwater moves into empty pores of rock by capillary action; water evaporates, salt crystals grow and accumulate, putting pressure
on the rock; common in drier climates).

A

salt crystallization

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8
Q

(plants can grow in cracks; the pressure of a
confined growing root can make cracks in the rocks larger, and as roots grow they can break rocks apart)

A

biogenic physical impact

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9
Q

Weakening and subsequent disintegration of rock by chemical reactions; also known as decomposition or decay, is the breakdown of rock by chemical mechanisms.

A

chemical weathering

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10
Q

types of chemical weathering

A
  • oxidation
  • carbonation
  • hydrosis
  • hydration
  • dehydration
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11
Q

(reaction of rock minerals with Oxygen, changing the mineral composition of the rocks)

A

oxidation

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12
Q

(process of rock minerals reacting with carbonic acid; carbonic acid dissolves or breaks down minerals in the rock)

A

carbonation

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13
Q

(chemical reaction caused by water changes the chemical composition and size of minerals in rock).

A

hydrosis

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14
Q

(absorption of water into the mineral structure)

A

hydration

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15
Q

(removal of water from rock or mineral structures)

A

dehydration

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16
Q

Weakening and subsequent disintegration of rock by plants, animals and microbes.

A

biological weathering

17
Q

types of biological weathering

A
  • plant roots
  • burrowing animals
  • micbrobial activity
18
Q

(Growing plant roots can exert stress or pressure on rock. Although the process is physical, the pressure is exerted by a biological
process).

A

plant roots

19
Q

(move rock fragments to the surface, exposing the rock to more intense chemical, physical, and biological processes)

A

burrowing animals

20
Q

(Breaks down rock minerals by altering the rock’s chemical composition, thus making it more susceptible to weathering.)

A

microbial activity

21
Q

example of microbial activity is

A

lichen (fungi or algae)