Coastal processses Flashcards

(41 cards)

1
Q

Wave formation

A

Made by friction between wind + sea surface
size depends on wave spped + fetch

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2
Q

Formation of a wave - Fetch

A

Distance of open sea that wave travels before reaching the shore

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3
Q

Formation of a wave - Shore

A

Area of beach exposed between high + low tide

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4
Q

Parts of a wave - Crest

A

Top of a wave

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5
Q

Parts of a wave - Trough

A

Bottom of a wave

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6
Q

Parts of a wave - Wavelenght

A

Distance between 2 crests

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7
Q

Parts of a wave -Breakin gwave

A

Friction slows down trougha of waves as they approach shore. Wave becomes steeper as fast crest catches up + collapses over the trough

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8
Q

Parts of a wave -Swash

A

Beach material carried up the shore by a breaking wave

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9
Q

Parts of a wave -Backwash

A

When the swash has no more energy, it drags lighter material with it as it flows back to the sea

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10
Q

deposititing waves are

A

Constructive waves

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11
Q

Eroding waves are called

A

Destructing waves

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12
Q

Wave Refraction - def

A

Waves change direction as the approach the shore due to friction

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13
Q

Erosion factors - List

A

Composition
Wave strength
Coastal shape
Shore gradient
Human activity
Rising sea levels
Climate change

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14
Q

Erosion factors - composition

A

Hard coast (sandstone cliffs) erode slowly. Soft coasts (clay + sand) erode fast

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15
Q

Erosion factors - Wave strength

A

destructive waves are strong + cause erosion - strongest in storms

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16
Q

Erosion factors -Coastal shape

A

Determines the amount of wave refraction that occurs

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17
Q

Erosion factors -Shore gradient

A

Steep slopes = more destructive waves becuase they break close to the shore

18
Q

Erosion factors -Human activity

A

Removal of beach material material increases erosiom. Sea walls + rock armour reduce erosion

19
Q

Erosion factors -Rising sea levels

A

Higher sea levels = higher flooding + erosion

20
Q

Erosion factors - climate change

A

Increased storm frequency + strength - increased erosion

21
Q

Compression

A

Coastal erosion. Waves wash over rocks. air is compressed within cracks + joints. As the waves retreat, air expands, weakening + shattering the rock

22
Q

Bays and headlands eg

A

Dublin Bay, Co Dublin

23
Q

Bays and headlands - description

A

Bays are curved indents on the coastline formed by destructive waves. A headland is a section of land that protrudes further into the sea than its surrounding coastline

24
Q

Bays and headlands - explanation

A

An area of soft rock along the coast has hard rock on either side of it. Due to differential erosion from hydraulic action and compression , the soft rock erodes much faster, creating an indent called a bay with the headlands jutting out on either side. This leads to wave refraction which causes deposition in the bay leading to beach formation

25
Longshore drift
Waves approach the shore - friction causes them to slow + break. Swash carries material up the beach at an angle and the backwash flows back into the sea at a 90 degree angle. Deposited sediment is moved along the shoreline
26
Beach example
Donabate beach, Co. Dublin
27
Beach def
A build up of loose material deposited by constructive waves between the low + high tide mark
28
Beach explanation
Form on gently sloping shore from loose material deposited by constructive waves. Has uppershore + lowershore sections. Powerful swash pushes materials on shore, pushing large materials to the upperbeach + weak backwash can only drag light small sand + mud to the foreshore, leaving large coarse material eg shingle at the backshore. Storm beaches develop at the very back of the beach where only powerful constructive storm waves can reach
29
Storm beach
Constructive storm waves deposit ridges of large stones and heavy material out of reach of normal waves at the very back of the beach
30
Beach - Berms
Small ridges of slightly coarse gravel deposited parallel to the shore. Mark the highest point reach by the swash during each tide
31
Beach - runnels
Depressions separating berms
32
Beach - sand dunes
small hills of sand that develop inland behind beaches. Formed with lots of fine beach sand with prevailing sea wind. Sand dries during low tide and is deposited by wind when it comes into contact with obstacles.
33
Maram
coarse, strong grass that grows in sand. Its long roots act as an anchor which binds sand together.
34
Coastal management - hard vs soft structures
Hard structures are permanent, prevent erosion + are usually made of reinforced steel or concrete Soft structures are eco friendly + repair wave damage
35
Coastal management - Sea walls
protect coastlines from destructive waves, made from reinforced steel concrete. Curved walls to deflect breaking wave back into sea
36
Coastal management -Gabions
Steel mesh cages filled with stones. Wave is broken as it hits gabions, spreading out its energy + erosive power
37
Coastal management - Groynes
Low walls of cement/ wood at right angles to shore, trap sediment from being moved by longshore drift - prevents erosion
38
Coastal management - Rock armour
Large boulders placed around coastline. Wave energy reduced as the crash off rocks
39
human interferance w coast - Rosslare - sand trapping
1860s -Viaduct prevented sediment transport by longshore drift - sediment build up in harbour needed dredging 1987 - viaduct expanded - acted as groye trapping lots of sand.
40
Human interferance w coasts - Rosslare - Effects of sand trapping
Balance between erosion + deposition changed - rapid coastal retreat
41
Human interferance w coasts - Rosslare - coastal retreat countermeasures
Coastal defences to reduce rate of erosion - worked at Rosslare strand, but worsened other areas Largest beach nourishment scheme in Ireland - 275,00 cubic metres of sand added + marram grass planted