Coasts Flashcards

(50 cards)

1
Q

What is a coast?

A

Dynamic interface where land, sea, and atmosphere meet and interact.

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2
Q

What is the main natural agent responsible for sediment detachment, transport, and deposition along coasts?

A

Waves

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3
Q

Define wave base.

A

Wave base is the depth below the water surface at which wave motion is negligible—approximately half the wavelength.

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4
Q

What happens to wave velocity as waves approach shallow water?

A

Wave velocity decreases.

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5
Q

What is longshore drift?

A

Movement of sand along the shore caused by oblique wave approach and longshore currents.

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6
Q

Wave height decreases as waves enter shallow waters.

A

False — wave height increases.

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7
Q

Waves approaching headlands concentrate energy and cause erosion.

A

True

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8
Q

Barrier islands are always attached to the mainland.

A

False — they are separated by lagoons or marshes.

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9
Q

A spit always grows perpendicular to longshore drift.

A

False — it grows in the direction of longshore drift.

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10
Q

A tombolo connects an offshore island to the mainland.

A

True

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11
Q

When waves enter shallow water, which change occurs?

A

Wavelength shortens

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12
Q

Wave refraction causes:

A

Energy concentration on headlands

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13
Q

Longshore currents move:

A

Parallel to shore

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14
Q

A cuspate foreland forms where:

A

Waves approach from two directions

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15
Q

A wave-cut platform forms due to:

A

Continuous cliff erosion

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16
Q

When depth is more than half the wavelength, the wave is in ______ water.

A

deep water

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17
Q

Longshore currents move parallel to the beach within the ______ zone.

A

surf zone

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18
Q

A ______ forms when a spit joins an offshore island.

A

tombolo

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19
Q

A narrow ridge of sand growing outward from a bay mouth is a ______.

A

spit

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20
Q

A wave-cut ______ forms at the base of an eroding cliff.

A

notch

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21
Q

Rock bridge formed by erosion

22
Q

Narrow sandy ridge attached to land

23
Q

Offshore sandy island separated by lagoon

A

Barrier island

24
Q

Isolated pillar of rock

25
Flat surface formed by cliff retreat
Wave-cut platform
26
Explain how wave refraction affects headlands and bays.
Headlands receive focused wave energy → erosion Bays receive dispersed energy → deposition
27
What causes breakers to form near shore?
Decrease in wave velocity as water becomes shallow → crest becomes steep → wave breaks.
28
Describe the process of longshore drift.
Oblique wave approach pushes sand up the beach; backwash pulls it down perpendicular → zig-zag transport along shore.
29
How does a wave-cut cliff form?
Constant wave erosion at the base creates a notch; cliff becomes unstable and collapses.
30
How does a barrier island form from a spit?
Spit grows by longshore drift → tidal inlets cut through → isolated sandy island.
31
Why are coastal areas highly dynamic?
Because they are influenced simultaneously by land processes, marine processes, and atmospheric conditions.
32
Explain how multiple wave-cut terraces form.
They indicate repeated sea-level drops or tectonic uplift, each producing a new erosional platform.
33
Describe how annual storm events accelerate coastal erosion.
Storm waves have higher energy → rapidly undercut cliffs → cause mass wasting → reshape coastlines. (Example: Tusang Beach.)
34
What are the environmental impacts of coastal human activity?
Construction, dredging, seawalls, and pollution accelerate erosion or disrupt natural sediment movement.
35
Differentiate between rocky coasts and sandy embayments.
Rocky coasts: dominated by erosion, cliffs, platforms Sandy embayments: dominated by deposition, beaches, spits
36
Describe the transition of wave behavior from deep to shallow water.
Include: Wave base Wavelength shortening Height increase Velocity decrease Steeper wave crests Formation of breakers
37
Explain how tombolos and cuspate forelands form.
Tombolo: spit grows until it connects an offshore island; controlled by wave refraction. Cuspate foreland: sediment accumulates where waves approach from two directions.
38
Discuss the sequence of coastal erosion features from headland to stack.
Headland → sea cave → sea arch → collapse → sea stack.
39
Outline the formation and evolution of spits and barrier islands.
Steps: longshore drift → spit formation → spit extension → tidal cut-through → barrier island development.
40
Evaluate the role of wave refraction in shaping coastlines globally.
Include energy distribution, erosion intensity, depositional pattern, and long-term coastal morphology formation.
41
If a coastline shows rapid cliff retreat, what coastal process is dominant?
Wave undercutting and cliff failure (erosion). Example: Tusang Beach.
42
A curved sandbar grows across a bay mouth. What feature is forming?
Spit
43
If waves approach from NE and NW directions, what morphology is likely?
Cuspate foreland
44
What coastal type is likely where cliffs, platforms, and arches dominate?
Rocky erosional coast.
45
A platform with multiple terrace levels suggests what history?
Several episodes of sea-level change.
46
Why are spits excellent indicators of longshore drift direction?
They grow in the same direction as dominant sediment transport.
47
Explain how wave refraction creates both erosional and depositional landforms along the same coastline.
Concentrated energy at headlands → erosion; dispersed energy in bays → deposition.
48
Why do wave-cut platforms eventually become abandoned terraces?
Tectonic uplift or sea-level fall raises the platform above active wave erosion.
49
How can humans unintentionally increase coastal erosion?
By building seawalls, groynes, or altering sediment supply, which intensifies wave attack elsewhere.
50
Why are barrier islands extremely vulnerable to climate change?
Rising sea levels and stronger storms reshape islands, breach inlets, and migrate barriers inland.