s2 Flashcards

1
Q

processes are external processes that occur on or near the Earth’s surface. They are driven by external forces such as solar energy and gravity

A

Exogenic Process

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2
Q

processes are internal processes that originate within the Earth. They are driven by internal forces such as heat from the Earth’s interior and gravitational energy

A

Endogenic Process

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3
Q

involves the breakdown of rocks and minerals into smaller pieces without changing their chemical composition.

A

Physical Weathering (Mechanical Weathering)

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4
Q

Water seeps into cracks, freezes, expands, and eventually breaks the rock apart. Common in cold climates.

A

Freeze-Thaw (Frost Wedging)

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5
Q

Rocks expand when heated and contract when cooled. Repeated temperature changes can cause the rock to crac

A

Thermal Expansion

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6
Q

Rocks and particles scrape against each other, causing them to wear
down. Common in windy areas and riverbeds.

A

Abrasion

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6
Q

Layers of rock peel off due to pressure release or thermal expansion.

A

Exfoliation

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6
Q

arbon dioxide dissolved in water forms carbonic acid, which reacts
with minerals like limestone, causing them to dissolve.

A

Carbonation

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7
Q

involves the chemical alteration of minerals within rocks, leading to their breakdown

A

Chemical Weathering

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7
Q

Water reacts with minerals to form new minerals and soluble salts.

A

Hydrolysis

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8
Q

Heavier and larger particles settle first, followed by progressively finer sediments.

A

Sorting of Sediments: Graded Bedding

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8
Q

Minerals react with oxygen, often leading to rust formation.
Common in rocks containing iron

A

Oxidation

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9
Q

Minerals dissolved directly in water, such as halite (rock salt)
dissolving in rainwater.

A

Solution

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10
Q

Roots grow into cracks in rocks, exerting pressure and causing
the rock to break apart.

A

Plant Roots

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10
Q

These organisms produce acids that chemically weather
the rock surface.

A

Lichens and Mosse

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11
Q

Involves the breakdown of rocks by living organisms

A

Biological Weathering

11
Q

Deflation: Removal of loose particles from the ground.

Abrasion:
Windblown particles grind against surfaces, smoothing and shaping them.

Examples: Sand dunes, desert pavements, and loess deposits

A

Wind erosion

12
Q

Erosion is the process by which natural forces move weathered rock and soil from
one place to another.

A

Erosion

12
Q

Hydraulic Action: The force of moving water dislodges and transports particles.

Abrasion: Rocks and sediments carried by water wear away the riverbed and banks.

Solution: Minerals dissolve in water and are carried away.

A

Water Erosion

13
Q

Movement of rock and soil downslope due to gravity.

Examples: Landslides, rockfalls, and soil creep

A

Mass Wasting

14
Q

Layers of sediment are deposited at an angle to the horizontal, commonly found in
environments like rivers and deserts

A

Sorting of Sediments: Cross-Bedding

15
Q

Occurs in river and stream environments, forming features
like deltas, alluvial fans, and floodplains.

A

Fluvial Deposition

15
Q

Caused by the wind in the desert and coastal environments,
forming sand dunes and loess deposits.

A

Aeolian Deposition

16
Q

Formed where a river meets a standing body of water such as sea or lake, causing sediments to be deposited as the river’s velocity decreases

A

Deltas

17
Q

Results from the movement and melting of glaciers,
forming moraines and outwash plains.

A

Glacial Deposition

17
Q

: Movements along a flat or planar surface,
such as a bedding plane or fault.

A

Translational Slide

18
Q

Happens in oceanic environments, forming features like
continental shelves and abyssal plains

A

Marine Deposition

19
Q

slow, gradual, and almost imperceptible movement of soil and rock downslope

A

Creep

19
Q

A sudden and rapid movement of a cohesive block of soil or rock along a
defined plane of weakness

A

Slides

19
Q

Rapid and consist of water-saturated debris,
often triggered by heavy rainfall

A

Mudflows

19
Q

Movement along a curved surface, causing
the material to rotate backward.

A

Rotational Slide (Slump)

20
Q

Movement of rock, soil, and debris mixed with water, behaving like a fluid.

A

Flow

20
Q

Slow-moving and often occur in fine-grained materials like clay and silt.

A

Earthflows

21
Q

Free-fall of rock or debris from a steep cliff or slope.

A

Falls

22
Q

Slope Angle: Steeper slopes are more prone to mass wasting.

Material
Composition: Loose, unconsolidated materials are more susceptible.

Water Content: Increased water reduces friction and adds weight, promoting mass wasting.

Vegetation: Roots can stabilize slopes, while removal of vegetation can increase susceptibility.

Human Activities: Construction, deforestation, and mining can destabilize slopes.

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A

Factors Influencing Mass Wasting