Why are coastal landscapes different and what processes cause these differences?

Question 1

what is meant by the littoral zone?

Answer 1

the wider coastal zone, including coastal land areas and shallow parts of the sea just off shore.

Question 2

what can the littoral zone be divided into?

Answer 2

• coast: land adjacent to the sea, usually largely populated and urbanised
• backshore zone: above high tides and only effected in storms or exceptionally high tides
• foreshore: where processes occur between high and low tide marks
• nearshore: shallow water areas near to land (used in fishing, leisure and coastal trade)
• offshore: the open sea

Question 3

what are the two main types that coasts can be divided into.

Answer 3

• rocky (or cliffed) coastlines with cliffs varying in height from few metres to hundred of metres.
• coastal planes (with no cliffs) where the land has gently sloped towards the sea across am area of deposited sediments, often in the form of sand dunes and mud flats.

Question 4

what are the different coastal classifications?

Answer 4

• formational processes
• relative sea level change
• tidal range
• wave energy

Question 5

how do formational processes impact the classification of a coast?

Answer 5

> primary coasts: dominated by land-based processes, such as deposition at the coast from rivers or new coastal land formed from Laval flows
dominated by marine erosion or deposition processes.

Question 6

how does relative sea level change impact the classification of a coast?

Answer 6

> emergent coasts: where the coast is rising relative to sea level, for example as a result of tectonic uplift.
Submergent coasts: flooded by the sea either because of sea level rise or subsiding land.

Question 7

how does tidal range impacts the classification of the coast?

Answer 7

tidal range varies hugely on the coastline meaning coasts can be:
-microtidal (tidal range of 0-2m)
-mesotidal (tidal range of 2-4m)
macrotidal (tidal range of 4m+)

Question 8

how does wave energy effect the classification of the coats?

Answer 8

> low energy: sheltered coast with limited fetch and low wind speeds resulting in small waves
high energy: exposed coasts, facing prevailing winds with long wave fetches resulting in powerful waves.

Question 9

what kind of cliff face occurs after marine erosion?

Answer 9

cliffs tend to be steep, unvegetated with little debris at the bottom of the cliff

Question 10

what are subaerial processes and what kind of cliffs do they leave behind?

Answer 10

subaerial processes include weathering processes (mechanical, chemical and biological), mass movement processes (landslides and rock falls) and surface run off erosion.
tend to leave behind shallower, curved slopes and lower reliefs; surface runoff erosion and mass movement are responsible for the cliff shape.

Question 11

what are some geological structures?

Answer 11

jointing (fracture diving rock)
dip (indentation)
faulting (cracks in crust)
folding (overlapping to create ridges)
deformation (tilting and folding by tectonic activity)
strata (different layers of rock exposed by the cliff)

Question 12

what are geological structures responsible for the formation of?

Answer 12

concordant coastlines: same rock type running parallel to the coast.
discordant coastlines: bands of rock that run perpendicular to the coast

Question 13

describe a typical coastal recession

Answer 13

bedrock is made of igneous, sedimentary and metamorphic rocks which determines the erosional recession.
-erosion occurs at the foot of the cliff creating a notch. material above the notch collapses and is washed away. repeated collapsing causes the rock to retreat further away. the rate of this erosion depends on the strata of the rock (discordant or concordant)

Question 14

what are some ways you can identify a coast?

Answer 14

• geology (rocky coast, muddy coast, sandy coast etc)

- changes to sea level.

Question 15

what is wave refraction?

Answer 15

Friction with the sea bed as waves approach the shore causing the wave crest to become distorted or refracted as velocity is reduced (when wave approaches shoreline)

Question 16

discordant coasts- why do headlands and bays change over time?

Answer 16

the effect the coast has on the wave crest

• in deep water wave crests (highest point on the wave) are parallel
• in bays, wave crests curve to fill the bay and wave height decreases.
• the straight wave crests refract, becoming curved, spreading out in bays and concentrating on headlands.
• the effect of wave refraction is to concentrate powerful waves at headlands (so greater erosion) and creates lower diverging wave crests in bays so reduces erosion.

Question 17

what is a Dalmatian coast? and an example

Answer 17

When the valleys are flooded by the rise in sea level, the tops of the valleys remain above the surface of the sea and appear to be a series of islands that run parallel to the coastline.
Dalmatian coast in Croatia.

Question 18

what are Anticlines and Synclines?

Answer 18

types of geological folds caused by tectonic compression. Anticlines forms crests and Synclines cause troughs.

Question 19

what is a cliff profile?

Answer 19

the height and angle of the cliff face, plus its features such as wave-cut notches or changes in slope angles.

Question 20

what are the two main features that determine the geology and the cliff profile?

Answer 20

1. the resistance to erosion of the rock

2. the dip (angle) of rock strata in relation to the coastline

Question 21

what are some cliff profiles you may find ** tweak from book **

Answer 21

• horizontal dip (vertical or near vertical profile with notches reflecting strata that are more easily eroded)
• seaward dip high angle (sloping, low-angle profile with one layer facing the sea; vulnerable to rock-slides)
• seaward dip low angle (profile may exceed 90˚ producing areas of overhanging rock; very vulnerable to rock falls.
• landward dip (steep profile on 70-80˚ and producing very stable cliffs with reduced rock falls.

Question 22

what are other geological features that influence cliff profiles and rate of erosion?

Answer 22

• faults (major fractures in rock caused by tectonic forces)
• joints (divides strata up into blocks of regular shape)
• fissures (much smaller cracks that bring about weaknesses in the rock)
• folded rocks (often heavily fissured or jointed meaning they are more easily eroded)

Question 23

what are micro-features?

Answer 23

small-scale coastal features such as caves and wave-cut notches which form part of a cliff profile

Question 24

what is meant by coastal recession? and what is the key influence of this erosion?

Answer 24

how fast a coastline is moving inland

lithology (sedimentary igneous and metamorphic rock)

Question 25

describe igneous rock and give examples

Answer 25

examples: granite, basalt and dolerite VERY SLOW- erosion rate of less than 0.1 cm annually they're crystalline meaning the interlocking crystals make for strong, hard and resistant rock often have few joints, so there is limited weakness that erosion can exploit

Question 26

describe Metamorphic rocks and give examples

Answer 26

examples: slate, schist, marble SLOW- erosion rates of 0.1-0.3 cm annually crystalline metamorphic rock are resistant to erosion. many metamorphic rocks exhibit features called foliation when all the crystals are orientated in one direction, which produces a weakness. metamorphic rocks are often folded and heavily fractured forming weaknesses that erosion can exploit

Question 27

describe sedimentary rocks and give examples

Answer 27

examples: sandstone, limestone, shale MODERATE TO FAST- erosion rate pf 0.5-10 cm annually most sedimentary rocks are clastic (broken up and older) and eroded faster than crystalline igneous and sedimentary rocks. geologically young sedimentary rocks tend to be weaker and rocks with many bedding planes and fractures are often most vulnerable to erosion.

Question 28

what is unconsolidated material?

Answer 28

sediment that has not been cemented to form solid rock, a process known as lithification

Question 29

what is the difference between clastic or crystalline rocks?

Answer 29

clastic rocks consist of sediment particles cemented together. crystalline rocks are made up of interlocking mineral crystals.

Question 30

erosion and weathering resistance of the rock is influenced by...

Answer 30

- reactivity of rock when exposed to chemical weathering - whether rocks are clastic or crystalline (the latter more resistant to erosion) - the degree to which rocks have cracks, fractures and fissures which weakens the rock

Question 31

what are examples of permeable and impermeable rocks

Answer 31

permeable (allow water to run through them): sandstone and limestone impermeable (don't allow groundwater to flow): clays, mudstone and most igneous and metamorphic rocks.

Question 32

what is meant by pore water pressure?

Answer 32

an internal force within cliffs exerted by the mass of groundwater within permeable rocks

Question 33

how does vegetation stabilise coastal sediment?

Answer 33

1. roots bind sediment particles together making them harder to erode 2. when submerged, plants provide a protective layer so the sediment surface is not directly exposed to moving water 3. plants protect sediment from wind erosion as it reduces wind speed at the surface due to the friction with the vegetation

Question 34

what is meant by plant succession?

Answer 34

the changing structure of a plant community over time as an area of initially bare sediment is colonised.

Question 35

what are the general stages of plant succession?

Answer 35

- pioneer plants begin to grow in the bare sand or mud - this forms the first stage of plant succession - each step in plant succession is called serial stage - the end result of plant succession is called climatic climax community.

Question 36

how does plant succession begin?

Answer 36

begins with the colonisation of embryo dunes by pioneer species. embryo dunes pioneer plants: 1. stabilise mobile sand with the binding of their roots 2. reduce wind speed allowing more sand to be deposited 3. add dead organic matter to the sand beginning the process of soil formation. they alter the condition from harsh, salty, mobile sand to an environment other plants can tolerate- new plants therefor colonise the embryo dune creating a fore dune.

Question 37

what are the key features of plant succession environments?

Answer 37

sea > embryo dunes > fore dunes > yellow dunes (all mobile) > fixed dunes > heath/woodland (both fixed dunes)