Ch. 2- Weathering, Erosion, and minerology Flashcards

1
Q

Weathering

A

The destructive process(es) by which rocks/minerals break down/dissolve on earth’s surface

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2
Q

Erosion

A

the process(es) whereby rocks/minerals are broken down/dissolved and simultaneously transported by natural forces.

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3
Q

Mechanical Weathering

A

the process of rocks breaking down by physical means without changing their chemical composition

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4
Q

Types of Mechanical Weathering

A
  1. unloading & exfoliation
  2. freezing and thawing
  3. growth of crystals
  4. thermal expansion and contraction
  5. root wedging
  6. burrowing animals
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5
Q

Unloading and Exfoliation

A

Allows rock to expand vertically as opposed to horizontally, as pressure is not removed from all sides (Just the top!);

Forms tiny joints /fractures parallel to surface, creates planes of weakness that peel away from the rest of the rock

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6
Q

Freezing and Thawing

A

Expansion & Contraction- Water seeps into cracks/fractures that were formed, where it will freeze and unthaw, forcing cracks open like a splint

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7
Q

Growth of Crystals

A

Occurs from sea spray hitting a rock, causing salt crystals to grow in the cracks

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8
Q

Thermal Expansion and Contraction

A

rocks expanding when heated and contracting when cooled– most prominent in desert environments

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9
Q

Wetting and Drying

A

If minerals can absorb water, they will expand and cause pressure on the rock– similarly, if rock dries out, the minerals will contract

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10
Q

Root wedging

A

Water seeping deeper into rock and splitting the rock, causing the root of a plant to follow the water.

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11
Q

Burrowing Animals

A

animals burrowing their way into solid rock for nutritional/habitat purposes

ex. mollusk drilling their ways into solid rock for homing; some tusked mammals get some of their nutrients from drilling into rock as well.

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12
Q

Chemical Weathering:

A

a process that breaks down rocks and minerals through chemical reactions

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13
Q

When is chemical weathering the most efficient?

A

If the surface of a rock is already sufficiently weathered.

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14
Q

Grain sizes:

A
  • > 2mm: boulders, gravel, pebbles
  • 1/16-2mm: sand
  • 1/256-1/512mm: silt
  • <1/512mm: clay
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15
Q

What is a special property that clay and silt exhibit?

A

electrostatic cohesion

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16
Q

Types of Chemical Weathering (Reactions)

A
  1. Spheroidal Weathering
  2. Redox reactions
  3. Hydrolysis Reactions
  4. Carbonation reactions
  5. Hydration Reactions
  6. Ion-Exchange Reactions
  7. Chelation
17
Q

Redox Reactions

A

involving the gain or loss of electrons from atoms

18
Q

Hydrolysis Reactions

A

Breakdown of minerals by adding water (H+)

19
Q

Hydration Reactions

A

Reactions of minerals with water, adding it but not necessarily breaking bonds

20
Q

Carbonation reactions

A

the reaction of minerals with dissolved CO2 in water

21
Q

Chelation

A

Reaction between a metal ion and a complexing agent

22
Q

What is the first biological agent to find a weathered rock?

23
Q

Complexing agents (in/decrease) the activity of the ion and (in/decrease) the stability of the solution.

A

decrease; increase

24
Q

Ion-Exchange reactions

A

generally involving the substitution of loosely bonded ions absorbed onto mineral surfaces

25
Q

Factors affecting electron mobility (4)

A
  1. Ionic Radius
  2. Ionic Charge
  3. pH
  4. Eh (oxidation potential)
26
Q

Differential weathering:

A

materials that are more susceptible to weathering in materials that are less-so

27
Q

What are the most common minerals on Earth?

A

silicate minerals

28
Q

Silicate Minerals compose what parts of the earth?

A

Oceanic crust and mantle

29
Q

Clay minerals are hydrated silicates of __, __, and __, and are arranged in sheets of ___ tetrahedra and ___ octahedra

A

Al; Fe; Mg; Si; Al;

30
Q

In clay minerology, a rectangle represents…

31
Q

In clay minerology, a rhombohedron represents…

32
Q

____ or ____ can join 2:1 structures together, forming 2:1:1 structures:

A

water or potassium

33
Q

Common clay sized minerals and their weathering sequence:

A
  • Sulfates, Chlorides
  • Carbonates, Phosphates
  • Silicates
  • 2ndary Clays
  • Oxides
34
Q

Sulfates/Chlorides

A

-Gypsum
-Halite

35
Q

Carbonates, Phosphates

A
  • Calcite
  • Dolomite
  • Aragonite
  • Apatite…
36
Q

Silicates

A

Bowens reaction series (OPAB, Feld, Musc, Quartz)

37
Q

Secondary Clays

A

-Vermiculite
-Montmorillonite
-Kaolinite

38
Q

Oxides

Think: what mineral is most commonly present in red/oxidized rocks?

A
  • Gibbsite (Al Oxides)
  • Hematite (Fe Oxides)
  • Zircon (Ti oxides)
39
Q

Factors affecting weathering

A
  • Parent material (mineral stability, permeability, joins/fractures)
  • Climate
  • Vegetation
  • Topography
  • Time