EQ1 Flashcards

(40 cards)

1
Q

Littoral zone

A

Breakwater area
Or area nearest the coastline where high + low tides occur

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2
Q

Offshore

A

Area of deeper water beyond the point at which waves begin to break
Friction b/ the waves + the sea bed may cause some distortion of the wave shape

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3
Q

Nearshore

A

Area of shallow water beyond the low tide mark w/i which friction b/ the seabed + waves distorts the wave sufficiently to cause it to break (breaker zone)
May be a breakpoint bar b/ the offshore + nearshore zones

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4
Q

Foreshore

A

Area b/ the high tide + low tide mark

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5
Q

Backshore

A

Area above the high tide mark affected by wave action only during major storm events

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6
Q

Different types of coastlines formed by the littoral zone

A

Rocky/cliffed coast
Sandy coastline
Estuarine coastline

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7
Q

Rocky/cliffed coast

A

Areas of high relief
Usually resistant rock areas
High energy environments where erosion is greater than deposition
Destructive waves

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8
Q

Sandy coastline

A

Low relief areas
Generally flat
Soft rock areas
Low energy environments with deposition being greater than erosion

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9
Q

Estuarine coastline

A

Low relief areas w/ salt marshes + mudflats
River mouths deposition greater than erosion in a low energy environment w/ soft rock

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10
Q

Dynamic equilibrium

A

Balance b/ inputs, flows, outputs of energy + material
Long term changes = sea level rise
High + low tide
Weather conditions
Varyingwave energy

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11
Q

Classifying coasts
ST classification criteria

A

Energy inputs:
Tides ebb + flow over a 12.5 hour period + currents, rivers, precipitation, gravity + tectonics create high + low energy coastlines
Sediment inputs:
Deposition + erosion rates - deposition is higher meaning expanding coastline
Erosion = higher meaning erosive coastline
Advancing + retreating:
Happens due 2 erosion + deposition as well as = emergent + submergent coasts linked with sea level

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12
Q

Classifying coasts
LT Classification criteria

A

Geology:
The lithology (rock type) + structure (arrangement of those rocks) Used 2 determine whether a coast = rocky, sandy, estuarine + Concordant (parallel) / discordant (perpendicular)
Sea level Change:
Used 2 classify emergent + Submergent coasts. Tectonic plate movement can lift or submerge sections of land. Climate change causing sea level rise can cause a coast to become submergent

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13
Q

Submergent coastline

A

Coasts occur where se level rise relative to land

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14
Q

Features of Submergent coastline

A

Rias
Fjords
Dalmatian coastline

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15
Q

Rias

A

River valley at the coast that has been inundated by the sea as relative sea levels have risen
Resukting in a ‘drowned valley’

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16
Q

Fjord

A

A glaciated valley at the coast that has been inundated by the sea. Has steeper rising walls a straighter long profile + deeper than a ria due to glaciers over deepening the valley

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17
Q

Dalmation coastline

A

A series of longitudinal river valleys next 2 the coast that have been in inundated leaving parallel ranges of watershed ridges as islands

18
Q

Rocky coastline

A

1,000km of the UKs coastline - mainly N + W
Cliffs vary in height (Scotland) to low relief (Cornwall)
Geology is resistant + they erode v slowly
Little deposition + high energy erosion

19
Q

Sandy plains

A

Flat, low relief, often containing wetlands + salt marshes
Low energy environment
Deposition is high
Can be sand, shingle, cobble
Most of the UKs S+Ecoastlines

20
Q

Concordant coasts

A

Most of the south coast (Dorset)
One continuous layer of hard rock protecting the other layers behind it

21
Q

Discordant coasts

A

Most of the E coast (Holderness)
Differing layers of resistant + soft rock in bands
Softer rock will erode faster than harder rock

22
Q

Concordant e.g. Dalmation coast = Croatia

A

Concordant coastline produced by the geological structure of folds parallel 2 the coast
Tectonic forces produced by the collision of African + Eurasian plates
Created up folded ridges (anticlines) + down folded valleys (synclines) aligned parallel 2 the coast
Sea levels rise - overtopped the low points = anticlines + sea flooded synclines
Lines of islands separated by narrow sea channels parallel 2 the coast

23
Q

Influence of coastal dip on strata

A

Dip is the angle of inclination of the rock strata from the horizontal
Tectonic feature
Sedimentary rocks are deposited horizontally but can be tilted by folding + faulting by tectonic forces
Dramatic effect on cliff profiles

24
Q

Horizontal dip

A

Produces vertical / near vertical profile
Notches reflecting weathering + small scale mass movement of strata that are more easily eroded

25
High angle of seaward dip
Produces a sloping low-angled profile with 1 rock layer facing the sea Vulnerable 2 rock slides down the dip slope when uppermost strata are attacked by sub-aerial processes Profile slopes correspond 2 that of strata dip Bedding planes b/ strata are weakly bonded + readily loosened by weathering
26
Low angle of seaward dip
Produces a steep profile may exceed 90 degrees Creates areas = overhand rock V vulnerable to rock falls Frequent small-scale mass movement of material weathered from cliff face Major cliff collapse when undercutting by marine erosion makes overhang unsustainable
27
Landward dropping strata
Produces steep profiles = 70-80degrees as downslope gravitational force pulls loosened blocks into place V stable profile w/ few rock falls
28
Faults
Major fractures created by tectonic plates Create a fault line Increases the rate of erosion Large forces involved leading 2 these rocks being easily eroded
29
Joints
Fractures created w/o the rock being moved Occur in most rocks + can be seen as blocks of rock Igneous rock - form during magma cooling Sedimentary rock - form through compression + stretching from overlying rock
30
Folding
Bends in the rock Produced by sedimentary rock layering Main types: anticlines + synclines
31
Bedrock lithology
Rate of coastal recession/retreat is influenced by the type of bedrock Influenced by how reactive the rock is to chemicals Wither it’s clastic (less resistant) + crystalline (more resistant) + whether it has cracks, fissures, fractures
32
Igneous
Granite, basalt Erode + weather v slowly because they have interlocking crystals - resistant Contain few joints + weaknesses
33
Metamorphic
Marble, slate, schist Recrystallised rock through heat + pressure Crystalline rock = resistant BUT LESS THAN SEDIMENTARY ROCK because the crystals form in the same direction (not interlocking)
34
Sedimentary
Sandstone, limestone, clay Formed by compaction least resistant type of rock because they’re heavily jointed - weak structures Moderate erosion rates
35
Unconsolidated sediment
Not yet solid rock Not yet cemented + compacted Drifts due 2 deposition + usually overlays bedrock V easily eroded = 2-10 meters per yr
36
Complex cliff profiles
Produced where there are differing types = lithology Less resistant strata erode + weather quickly producing wave cut notches Resistant strata erode + weather slowly retreating less rapidly
37
Complex cliff profiles can be produced when there are
Alternating permeable + non-permeable strata
38
Permeable rock
Allow water to flow through them because Porous (chalk) Numerous joints (Carboniferous limestone) E.g. sandstone + limestone
39
Permeable rock = less resistant to weathering because
Water percolating comes into contact w/ large surface area that can be chemically weathered Limestone weathered by carbonation converting calcium carbonate to soluble calcium bicarbonate
40
Pioneer plants
1st to colonise at a coastline Modify the environment by stabilising sediment, adding nutrients to the soil + reduce evaporation rates Create plant succession which is the process of different plant communities occupying an area of the coast overtime