COASTS Flashcards

1
Q

Spit

A

Sand or shingle beach ridge extending beyond a turn in the coastline. usually greater than 30 degrees. At turn, the longshore drift current spreads out and loses energy leading to deposition. The length of a spit is determined by the existence of secondary currents causing erosion, either the flow of a river or wave action which limits its length

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2
Q

Bayhead Beach

A
  • A awash aligned feature, where waves break at 90 degrees to the shoreline and move sediment into the bay, where a beach forms. Due to wave refraction, erosion is concentrated at headlands and the bay is an area of deposition
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3
Q

Tombolo

A

A sand or shingle bar that attaches the coastline to an offshore island. Tombolos form due to wave refraction around an offshore island which creates an area of calm water and deposition between the island and the coast. Opposing longshore currents may play a role, in which case the depositional feature is similar to a spit.

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4
Q

Barrier beach/bar

A

A sand or shingle beach connecting two areas of land with a shallow water lagoon behind. These features occur when a spit grows so long that it extends across a bay, closing it off.

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5
Q

Hooked/Recurved Spit

A

A spit whose end is curved landward, into a bay or inlet. The seaward end of the spit naturally curves landward into shallower water. The ‘hook’ may be made more pronounced by waves from a secondary direction to the prevailing wind

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6
Q

Offshore bar

A

A ridge of sand found offshore - can be submerged during high initially formed by riptide currents following destructive waves

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7
Q

mass movement processes

A

Landslide, Rotational slumping, slide, rock fall, topple, mudslides, slumping

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8
Q

weathering

A

mechanical, chemical, biological

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9
Q

Perculation

A

the movement of water through soil

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10
Q

Flocculation

A

when sediment is dropped, such as clays and polymers, they clump together

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11
Q

Sub Aerial Process

A

land-based processes which alter the shape of the coastline. These are a combination of weathering and mass movement.

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12
Q

Mechanical (physical) weathering

A

Mechanical or physical weathering is the fracture and breakdown of rocks into fragments. Freeze-thaw and Salt crystallisation

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13
Q

salt crystallisation

A

This is when salt crystals are deposited in cracks and over time the salt accumulates and applies pressure to the crack (similar to freeze-thaw weathering).

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14
Q

Chemical weathering

A

decomposition of rocks (literally, changing the minerals)

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15
Q

Soil Creep

A

Soil creep is a slow but continuous process. It typically occurs on most slopes over 5 degrees. Soil creep rarely exceeds speeds of 1cm per year. Creep occurs as the result of repeated expansion and contraction of material. Cycles of freeze-thaw heave particles upon freezing and allow them to fall further downslope when the ice melts. Alternating hydration and dehydration have the same effect.

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16
Q

Slump

A

Rainwater infiltrates the cliff through unconsolidated, porous material (e.g. boulder clay). This then creates a slip plane. The weight of the saturated clay causes the material to slump along the slip plane.

17
Q

rock fall

A

They are most commonly triggered by undercutting in the inter-tidal zone or freeze-thaw weathering.

18
Q

Mudflows

A

A mudflow is an earthflow consisting of material that is wet enough to flow rapidly and that contains at least 50 percent sand, silt, and clay-sized particles.

19
Q

Soil creep

A

Soil creep is a slow but continuous process. It typically occurs on most slopes over 5 degrees. Soil creep rarely exceeds speeds of 1cm per year. Creep occurs as the result of repeated expansion and contraction of material.

20
Q

Land slide

A

This is the downslope movement of a large block of material that moves as a coherent mass. This means it retains its internal structure until hitting the base of the slope and fracturing into smaller pieces. It is more common over wet periods, on steep slopes and often occurs on coastlines.

21
Q

Marine Processes

A

Marine processes are those associated with the action of waves. This includes erosion, transportation and deposition.

22
Q

Erosion

A

Erosion refers to the wearing away of the land surface and removal of materials by river and seawater, ice and wind. There are four main processes of erosion along the coast. These are hydraulic action, abrasion and corrasion, attrition and solution.

23
Q

Hydraulic Action

A

Waves breaking at the foot of a cliff force air in cracks to be compressed. Loose rocks are dislodged and removed. When the wave retreats the compressed air rushes out of the crack and can further weaken faults in the cliff face.

24
Q

Abrasion

A

Abrasion is the sandpaper effect of loose rocks being scraped along bare rock. It often smooths and polishes the rock.

25
Q

Attrition

A

Attrition is when rocks carried by seawater collide – gradually making them smaller and smoother.

26
Q

Transportation

A

Transportation is the movement of sediment by the action of waves.

27
Q

Traction

A

Traction involves the rolling of large and heavy rocks along the seabed.

28
Q

Saltation

A

Saltation involves smaller material being bounced along the seabed. The video below shows material being bounced along a beach by waves.

29
Q

Suspension

A

Suspension is when lighter sediment is suspended within the water. This often discolours the water close to the shore.

30
Q

Solution

A

Sediment that has dissolved completely will be transported in solution.

31
Q

Deposition

A

Deposition occurs when energy levels decrease in environments such as bays and estuaries. Where deposition occurs on the inside of a spit a salt marsh can form.

32
Q

Corrosion

A

the process of chemicals eroding away rocks