coastlines Flashcards

1
Q

Draw and label a typical beach profile

A

Lol, didn’t pay so no photo. look at notes

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2
Q

breaker zone

A

marks the transition from deep water to shallow water

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3
Q

surf zone

A

Part of the breaker zone where waves are actively breaking

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4
Q

swash zone

A

Waves run up and down this zone.

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5
Q

foreshore

A

located between the low and high tide mark

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6
Q

Backshore

A

land after the high tide mark

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7
Q

How do tides work?

A

Gravitational forces from the sun and moon change the tide of the water

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8
Q

What is a storm surge?

A
  • Rise in water level caused by high wind and low atmospheric pressure
  • lower atmospheric pressure means less pressure on the water level, meaning that it has less resistance to rise.
  • The wind direction and force can push water and pile it up when it hits the coastline.
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9
Q

What are the different types of sea level changes, and list some examples.

A

Eustatic
- global sea level changing
-examples: melting glaciers, a tectonic process that changes the shape of the seafloor (oceanic-oceanic)

Isostatic
- local sea level changes
- examples: loading or unloading of crust/ convergent plate boundaries at the coastline (oceanic-continental).

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10
Q

What are the two types of waves? and explain each one

A

Wind-generated waves
- travels downwind
- amplitude is determined by wind speed, duration, and fetch (uninterrupted distance over water that the wind blows in a consistent direction)

Displacement waves (tsunamis)
-generated by mechanical movements such as landslides, earthquakes, and volcanic eruptions.

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11
Q

What are breakers and how do they differ with different types of shore?

A

steep shore
- quick energy lost
- plunging breaker (dramatic and powerful)

gentle shore
- energy lost gradually over a large area
- spilling breaker

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12
Q

What is refraction in relation to waves approaching the shore?

A

The wave bends towards the shore.

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13
Q

What are longshore currents?

A

-They go in the direction in which the wave is carrying the sediments.
-Parallel to the coastline.

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14
Q

What are five erosion features, and give a quick explanation

A

Wave-cut cliffs
- Steep coastal cliffs formed by the relentless erosion of waves pounding against the rock

Wave-cut platforms
- Flat, rocky platforms at the base of cliffs, shaped by wave erosion and often exposed at low tide

Sea stacks
- Isolated pillars of rock rising from the sea, resulting from the erosion and isolation of headlands or cliffs.

Sea arches
-Natural rock arches or bridges formed by the erosion of a headland, leaving an opening through the rock.

Sea caves
- Hollow openings in coastal cliffs or rocks created by wave action and erosion, typically accessible by water.

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15
Q

What are five depositional features, and give a quick explanation.

A

All are formed by longshore drift sediment deposition.

Splits
-deposition of sediments that extend from the mainland into a body of water

Tombolos
- deposition of sediments that connects an island with the mainland or another island

Barrier island
-deposition of sediments in the sea parallel but not connected to the shoreline.

Tidal inlets
-narrow pathways of water that connect closed bodies of water with the ocean.

Longshore bars
-underwater or partially submerged ridges of sand or sediment running parallel to the shoreline

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16
Q

What are the five hard solutions to coastal management? Explain each one.

A

Jetties
-traps sediments
-perpendicular to shorelines
-prevent blockage of the inlet by longshore drift

Groynes
-Traps sediments
-perpendicular to the shoreline
-capture sediment transport by longshore drift

Breakwaters
-reflect or absorb wave energy
-parallel to the shoreline
-located offshore

Seawall
-Reflect wave energy

Revetments
-absorb wave energy
-sloping structures to dissipate wave energy
-designed to mimic the natural slope of the shoreline profile