Coasts - Case Studies Flashcards
How long is the coastline between Saltburn and Flamborough Head?
- 60km
What type of coastal environment is Saltburn to Flamborough Head?
- High-energy coastline
How does geology influence the coastline? (2)
- Discordant coastline = headlands & bays more varied than along a concordant coastline
- Differing rock types (different levels of resistance)
a. Chalk (Flamborough Head & Selwick’s Bay) = resistant
b. Kimmeridge clay (Filey Bay) = less resistant (0.8m/year)
c. Shales (Robin Hood’s Bay) = less resistant (0.8m/year)
d. Sandstone/limestone with interbedded glacial till (Saltburn) = resistant (0.1m/year)
How do waves influence the coastline? (5)
- Dominant waves from North & North-East
- Long fetch (1,500km) = long time to build up energy = powerful waves
- High tidal range (4m) = more potential erosion
- LSD (North to South)- sediment movement interrupted by headland = sand and shingle accumulate (i.e. Filey Bay)
- Wave refraction around headland (Flamborough Head) = formation of distinctive landforms
How does wind influence the coastline? (2)
- Prevailing wind from North/North-East drives high-energy waves
- Aeolian processes (but very limited)
Where has sediment within the coastline come from? (3)
- Nearshore area- driven onshore as sea levels rose at end of last glacial period
- Cliff erosion- i.e. from sandstone and chalk (resistant rock outcrops) & boulder clay deposits (gravel)
- River Esk BUT limited due to construction of weirs and reinforced banks along its course (human activity)
What landforms/cliff profiles are seen at Saltburn? (2)
- Limestone/sandstone with interbedded glacial till = resistant (0.1m/year)- stepped profile reflects more varied geology
- Horizontally-bedded strata = steepest cliffs along coastline
What landforms/cliff profiles are seen at Robin Hood’s Bay? (3)
- Shale = less resistant (0.8m/year)
- Wave-cut platforms (active erosion = cliff retreat)- 1* = shallow gradient with max width of 500m
- Possible shore platform created in last 6,000 years (constant level of erosion due to predom. stable sea levels)
- Headlands (sandstone) = more resistant bands either side of bay (0.1m/year)
What landforms/cliff profiles are seen at Filey Bay? (2)
- Kimmeridge clay (weak) = extremely susceptible to erosion (0.8m/year)
- Mass movement (slumping) = shallower angle cliff profiles
What landforms/cliff profiles are seen at Flamborough Head? (5)
- Chalk (resistant)- points of weakness = landforms
- Joints/faults exploited by erosive waves = caves & arches (i.e. Selwick’s Bay where master joint in chalk has been enlarged)
- Stacks (i.e. Green Stacks Pinnacle)
- Geos (over 50)- most aligned to the NE/NNE (facing dominant wave direction)
- Blowholes- where vertical master joints in the chalk have been enlarged
Why are there few developed beaches along the coastline?
- High-energy waves remove sediment before it can accumulate
- High tidal range (4m)
- Lack of estuarine environments that would provide sediment sinks
How long is the River Nile?
- 6650km
What is the River Nile’s catchment area?
More than 3 million km(2)
How does the River Nile influence the formation of landforms? (2)
- Huge sediment load (sediment budget) = 30% clay, 40% silt & 30% fine sand
- Average annual sediment yield = 4.26 tonnes/ha/year (total = 91.3 million tonnes per year for the whole Blue Nile Basin in Ethiopia)
What are the 3 distinct sub-units of the coastal plain & their characteristics? (3)
- Foreshore plain- elongated ridges alternating with lagoons, salt marshes and alluvial deposits the depressions between them
- Frontal plain (south of foreshore plain)- scattered eroded limestone outcrops and clay deposits
- Sandy zone- variety of different sand formations (i.e. sheets, dunes, hummocks)
What are the two distributaries of the Nile Delta?
- Rosetta
- Damietta
How does wave action influence the delta?
- Wave action in the Mediterranean redistributes the sediment at the front of the delta
- The reworked sediment forms a series of curved barrier bars- close off segments of the Med Sea to form lagoons (turn into form of sub-environment & soon become filled with fine sediment)
- Low wave energy (low tidal range due to small entrance to Med - 2cm/year & small fetch) mean little erosion
What are the estimated surface current velocities at different times in the year? (4)
- 9.26-13.5 cm/s during summer
- 4.46 cm/s during autumn
- 23.14 cm/s during winter (strong winds
- 8.4 cm/s during calm spring weather
How does seabed topography influence the delta? (2)
- Shallow continental shelf = friction so waves lose energy (deposition greater than erosion)
- Provides surface for accretion
What is the prevailing wind & therefore wave direction? (2)
- NW winds = waves coming from west, NW, N (55-60% of time)
- Waves come from NE (8% of time)
Which physical factor is most important in influencing the delta?
- Large scale factors (i.e. seabed topography, sediment budget) most important in influencing the delta over millennia, but on a smaller, more local, scale other physical factors (i.e. winds, waves) influence the movement of sediment over time along the coastline.