2b- Nile Delta + Flamborough Head Flashcards

1
Q

Flamborough head location

A
  • North East UK
  • salt burn
  • borders North Sea
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2
Q

FH- Physical factor - Wind + waves

A

Fetch = from NNW, 1500km over stormy North Sea
Waves= average >4m

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3
Q

FH- Physical factor - tides

A
  • macro tidal range (large) = 4m
  • due to UK bring on continental shelf so surrounded by shallower ocean
  • wave cut notches more significant = more of cliff impacted = faster cliff retreat
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4
Q

FH- Physical factor - geology

A
  • disconcordant coastline
  • bays + headlands form

weaker clays + Shales = 0.8m a year

stronger chalk + Limestone = 0.1m a year

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5
Q

What direction is sediment carried at FB ( think prevailing wind)

A

North to south
NNW prevailing wind

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6
Q

Where is the source of most sediment at FB

A

90% from cliff erosion

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7
Q

What is the orientation of FB cost + why is this significant

A
  • salt burn faces NW = faces waves head on = high rates of erosion
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8
Q

Major landforms at FB

A

Filey brigg = headland
Filey bay = bay sheltered by Filey brig
Robin hoods bay

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9
Q

How might landforms change over time at FB

A

1- bays become wider as waves refract around headland
2- cliffs retreat = retreating coastline
3- caves become arches ect
4- slumping of soft rocks= sloping profile
5- rising sea level allows waves to reach high = erosion will continue despite increasing WCPs

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10
Q

Inter-relationship of landforms FB

A

1- erosion of bays creates headlands = allows caves + other landforms to form
2- waves refract + lose energy on headland = sheltered areas in bays have deposition = beaches
3- erosion of cliffs = forms WCP + provides sediment for beaches

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11
Q

Location of Nile delta

A
  • Northern Egypt/ Africa
  • borders Mediterranean
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12
Q

ND- Physical factor - Wind

A
  • prevailing wind = NW over calm Mediterranean
    -fetch = 750km
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13
Q

ND- Physical factor - waves

A
  • average wave height = 0.94 , very low energy
  • occasional summer storm = 4m wave
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14
Q

ND- Physical factor - geology

A
  • concordant coastline
    -weak Lithology + structure = silts + sands
  • occasional limestone outcrop (Alexandria)
  • easily eroded
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15
Q

ND- Physical factor -Tides

A
  • small tidal range = 0.5m
  • Mediterranean is a small enclosed sea = little water to be pulled into tidal bulge
  • less range for erosion
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16
Q

ND- Physical factor - Sediment supply

A
  • large fluvial sediment input = 120 million tonnes/ year
  • 90% sediment budget = fluvial
  • Silts + sands mainly = theoretically easily eroded
17
Q

What has recently affected the sediment budget and how had this affected the coastline- ND

A
  • Aswan dam 1964
  • drastically reduced sediment supply
  • coastline retreating up to 148m/year
18
Q

Nile delta before human impact

A

-Deposition has exceeded erosion for past 3000 years
- building of Aswan dam has caused retreat showing human impact on landscapes

19
Q

Key landforms Nile delta

A
  • limestone headland at Alexandria
  • manzala bar + manzala lake behind
  • Damietta + Rosetta promontories
20
Q

What is a delta

A

Large areas of sediment build up at river mouths

21
Q

What is flocculation

A

1- Occors when salt and freshwater meet
2- causes clumping of sediment = when sediment gets big enough it is deposited/ dropped as it is too much energy to carry

22
Q

Interrelationships at Nile delta

A

1- promontory’s (at distributaries mouth) are build up of sediment= supply’s sediment for LSD eastwards= manzala bar produced (50km long)
2- promontory’s shelter coast = encourage deposition
3- Alexandria headland shelters Abu-Qir bay = beach
4- manzala bar shelters area behind = salt marsh
5- waves arriving parralel to Abu-Qir bay = rip currents= offshore bars

23
Q

How might Nile delta change over time

A
  • coastline retreats due to decreased sediment budget
  • burrulus spit breached = had been a bar
24
Q

How do rip currents form ( Abu Qir bay)

A
  • waves arrive parallel to coast
  • backwash cannot flow off beach due to too much incoming swash = backwash is forced to concentrate on one area
    = strong outgoing current / rip current
  • offshore bars form due to backwash losing energy and depositing sediment
25
Q

How might warmer climate affect FH

A
  • more chemical weathering = coastline retreats faster
  • chance for coastal flooding + formation of submergent landforms
26
Q

How might warmer climate affect Nile delta

A
  • excessive coastal flooding due to very flat land eg: Alexandria would submerge after 50cm rise
  • more water in Nile = more fluvial sediment = more deposition
27
Q

How much are sea levels rising a year in Mediterranean

A

1.2 mm a year
Less than global due to being a enclosed sea

28
Q

How much would sea levels need to rise to submerge Alexandria - ND

A

0.5m / 50cm

29
Q

how tall are cliffs at Flamborough head

A

120m
- Cliff collapse provides significant sediment

30
Q

direction of LSD at ND

A

West to East

31
Q

how could a Flood plain and river valley form before sea level change for Rias

A

-Rivers erode sediment from their banks and bedrock as they flow downstream towards the sea.
-The riverbed deepens over time. As rivers move from side to side, they gradually erode the valley, creating broad plains.
-As a river floods, it overflows its bank. The flood carries sediment out over the land. After the water withdraws, the sediment remains. If a river floods repeatedly, over time this sediment will build up into a flood plain