Chapter 6 test 2 Flashcards

1
Q

weathering

A

external process
physical breakdown and chemical alteration of rock at or near the earths surface.
mechanical and chemical

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2
Q

mass wasting

A

external process

transfer of rock and soil downslope under the influence of gravity(landslides)

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3
Q

Erosion

A

external process

the physical removal of material by mobile agents such as water, wind, ice or gravity

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4
Q

mechanical weathering

A

breaking of rocks into smaller pieces

frost wedging, sheeting, salt crystal growth, biological activity

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5
Q

frost wedging

A

alternate freezing and thawing of water in fractures and cracks promotes the disintegration of rocks.

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6
Q

sheeting

A

exfoliation of igneous and metamorphic rocks at the earths surface due to a reduction in confining pressure. when overlying layers are eroded away, the outer layers expand and separate from the rock body. ex: joints

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7
Q

Joints

A

fractures in the rock caused by expansion or rock, contraction of rock or cracking of rocks by mountain building forces.

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8
Q

salt crystal growth

A

similar to frost wedging but instead of freeing water, salt crystals get inside and grow. occurs at seashores with a lot of sea spray.

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9
Q

biological activity

A

disintegration resulting from plants and animals

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10
Q

chemical weathering

A

breaks down rock components an the internal structure of minerals. water is usually involved
oxidation, dissolution, hydrolysis, spheroidal weathering

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11
Q

oxidation

A

oxygen dissolved in water will cause oxidation which weakens materials with iron in them.

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12
Q

dissolution

A

process by which carbonic acid in the water dissolves rocks such as limestone

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13
Q

hydrolysis

A

carbonic acid reacts with feldspar and breaks it down to produce clay

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14
Q

spheroidal weathering

A

causes physical changes by rounding corners.

forms when angular rock is chemically weathered as water enters joints

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15
Q

differential weathering

A

rocks do not weather uniformly due to regional and local factors. an important factor is rock composition.

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16
Q

regolith

A

rock and mineral fragments produced by weathering

17
Q

soil

A

a combination of mineral and organic matter, water, and air.
50% is made of disintegrated rock and minerals plus Humus
50% is made of pore spaces between solid particles where nutrient water and air cirulate

18
Q

factors controlling soil formation

A
parent material
time
climate
plants and animals
slope
19
Q

parent material

A

residue soil, parent material is the underlaying bedrock

transport soil, forms in a place on parent material that has been carried from elsewhere and deposited

20
Q

Time

A

amount of time for soil formation varies for different soils depending on geological and climate conditions.
it can take 80-400 years for .5in of soil

21
Q

climate

A

most influential control of soil formation

key factors are temperature and percipitaion

22
Q

plants and animals

A

organisms influence the soils physical and chemical properties.
also furnish organic matter to the soil

23
Q

slope

A

steep slopes often have poorly developed soils

24
Q

soil profile

A

soil forming processes operate from the surface downward.
vertical differences are called horizons- zones or layers of soil
-O horizon, A Horizon, E Horizon, B Horizon, C Horizon

25
Q

O Horizon

A

organic matter

O and A make up topsoil

26
Q

A Horizon

A

Humus and mineral matter
high biological activity
together the O and A horizons make up topsoil

27
Q

E Horizon

A

Little organic matter

zone of eluviation and leaching

28
Q

B Horizon

A

zone of acumulation

29
Q

C Horizon

A

partial altered parent material

30
Q

Laterite

A

a tropical soil that hardens to brick when vegetation is stripped away and sun backs the surface

31
Q

Paleosoil

A

an ancient soil that is buried. it can provide clues to past climates and landscapes

32
Q

bauxite

A

the worlds largest source of aluminum

concentrated in fragile tropical s oils