Weathering ang Erosion Flashcards

1
Q

is the decomposition
and disintegration of rocks and
minerals at the Earth’s surface
.

It involves little or no
movement
of rocks and minerals – the weathered material accumulates
where it forms and overlies
unweathered bedrock.

A

Weathering

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2
Q

is the removal of weathered
rocks and minerals by moving water,
wind, glaciers, and gravity.
After a
rock fragment has been eroded from
its place of origin, it may be
transported large distances by the
agents mentioned above.

A

Erosion

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3
Q

When the wind or water loses energy,
or when the ice carrying the
weathered material melts, transport
stops
, and sediment is _________

A

deposited

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4
Q

wetlands that form as rivers
empty their water and sediment into
another body of water

A

delta

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5
Q

reduces solid rock to rubble but does not alter the chemical composition of rocks and minerals.

A

Mechanical weathering

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6
Q

occurs when air and water chemically react with rock to alter its composition and mineral content.

A

Chemical weathering

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7
Q

Five major processes of Mechanical Weathering

A
  1. Pressure-release fracturing
  2. Frost wedging
  3. Abrasion
  4. Organic activity
  5. Thermal expansion and contraction
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8
Q

as pressure diminishes, rock expands – which leads to fracturing of brittle rock.

major processes of Mechanical Weathering

A

Pressure-release fracturing

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9
Q

water expands when it freezes. If water accumulates in a crack then freezes, its expansion pushes the rock apart

major processes of Mechanical Weathering

A

Frost wedging

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10
Q

mechanical weathering and grinding of rock surfaces by friction and impact.

major processes of Mechanical Weathering

A

Abrasion

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11
Q

roots may work their way down into cracks in the
rock, expand, and eventually push the rock apart.

major processes of Mechanical Weathering

A

Organic activity

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12
Q

rocks are exposed to daily and yearly cycles of heating and cooling , which, as a result, the surface expands or contracts faster than the interior

major processes of Mechanical Weathering

A

Thermal expansion and contraction

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13
Q

Chemical Weathering
Three most important processes:

A
  1. Dissolution
  2. Hydrolysis
  3. Oxidation
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14
Q

rocks are made up of minerals, and minerals are
chemicals on their own. To understand how acids and bases dissolve minerals , think of an atom on the surface of a crystal, which could be dissolved when subjected to the certain solvents.

Chemical Weathering

A

Dissolution

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15
Q

water reacts with a mineral to form a new mineral with the water incorporated into its crystal structure.

Chemical Weathering

A

Hydrolysis

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16
Q

many minerals react with atmospheric oxygen , O2 Rusting is one example of a more general process called __________

Chemical Weathering

A

Oxidation

17
Q

Significance of Weathering

A

most important aspect of weathering is its role in the formation of soil.

Weathering is important to engineers because it can help them to understand **how buildings and other structures will be affected by the environment. **

Weathering is also important to geologists because it can help them to study the history of the earth’s surface.

18
Q

The Effects of Weathering (3)

A
  • weakening of intact rock blocks and soil grains
  • integral become mechanical discontinuities (i.e. bedding planes not being yet a mechanical plane
    of weakness become a mechanical
    plane of weakness)
  • material between rock blocks becomes weaker (remains of weathered material)
19
Q

when a rock mass is weathered, there are: (3)

A
  • Weaker rock blocks and soil grains;
  • Smaller rock blocks and grains; and
  • Lesser shear strength between blocks and grains.
20
Q

what gives rock and soil masses strength

A

Rocks and soil masses consist of:
* intact blocks (rock) with discontinuities in-between (e.g. bedding plances, joints, fractures, etc.)
* grains (in soil) with grain contacts in-between

Strength of a mass is given by:
* strength (shear and tensile) of intact rock blocks or soil grains
* shear strength between blocks (rock) or grains (soil)

21
Q

Weathering products from mechanical and chemical
weathering may accumulate
on the Earth over bedrock . This material is called _____________.

A

regolith

22
Q

are the upper layers of
regolith
that support plant growth.

A

soil

23
Q

soil profile

A

O horizon
A horizon
B horizon
C horizon

24
Q

Typical mature soil consists of
several layers called ________

A

soil horizons.

25
Q

Combination of O and A horizons
are called __________ .

A

topsoil

26
Q

named for its
Organic component.

A

O horizon

27
Q

mixture of humus, sand, silt, and clay. Also called zone of leaching .

A

A horizon

28
Q

also called subsoil or zone of accumulation, is a transitional zone between topsoil and parent rock below.

A

B horizon

29
Q

consists of partially weathered rock that grades into unweathered parent rock.

A

C horizon

30
Q

degrees of weathering

A
  1. fresh
  2. slightly weathered
  3. moderately weathered
  4. highly weathered
  5. completely weathered
  6. residual soil
31
Q

No visible sign of rock material weathering ; perhaps slight discoloration on major discontinuity surface

degrees of weathering

A
  1. fresh
32
Q

Discoloration indicates weathering of rock material and discontinuity surfaces. All rock material may be discolored by weathering

degrees of weathering

A

2.slightly weathered

33
Q

Less than half of the rock material is decomposed or disintigrated to a soil . Fresh or discolored rock is present either as a continuous framework or as core stones

degrees of weathering

A

3.Moderately weathered

34
Q

More than half of the rock material is decomposed or disintigrated to a soil. Fresh or discolored rock is present either as a discontinuous framework or as core stone.

degrees of weathering

A

4.Highly weathered

35
Q

All rock material is decomposed and/or disintigrated to soil. The original mass structure is still largely intact.

degrees of weathering

A

5.Completely weathered

36
Q

All rock material is converted to soil. The mass structure and material fabric is destroyed. There is a large change in volume, but the soil has not been significantly transported.

degrees of weathering

A

6.Residual soil