Block 3 (Landforms + Their Landscape Systems, Their Distinctive Features + Distribution) Flashcards

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1
Q

What is a low energy coast?

A

Sandy or estuarine coastline, dominated by deposition

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2
Q

What waves are predominantly found on a low energy coastline?

A

Constructive waves

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3
Q

What process is predominantly found on a low energy coastline?

A

Deposition

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4
Q

What is the sediment budget on a low energy coastline?

A

Positive - production + delivery rate exceeds erosion rate

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5
Q

Where are low energy coasts found?

A
  • Sheltered bays

- Estuaries

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6
Q

What are common landforms for a low energy coast?

A
  • Sandy beach with gentle gradient
  • Spit
  • Sand dunes
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7
Q

What are some examples of low energy coastlines?

A
  • German Baltic Coast
  • Netherlands
  • East Africa
  • South-East UK
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8
Q

Why do low energy coasts exist?

A
  • Divergence of orthogonals in bays (product of wave refraction)
  • Limited fetch/duration (sheltered areas) causes low energy waves
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9
Q

Case study of low energy coastline + details

A

German Baltic Coast
Location:
- N.Europe
- N. Germany, between Danish + Polish borders
- 2481km long
Why is it low energy?
- Very sheltered - so waves have low fetch + low duration - low energy
Characteristics:
- Beaches (Large deposition by constructive waves, usually shallow gradients, often backed by sand dunes) (Most important beach + dune system is Fischland-Darss-Zingst peninsula, on Hiddensee + Rugen islands)
- Spits (Positive sediment budget, moved by LSD, continues when coastline changes direction) (2 spits extending into Pomeranian Bay - Usedom island)

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10
Q

What is a high energy coast?

A

Rocky coastline dominated by erosion

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11
Q

What waves do high energy coasts predominantly have?

A

Destructive waves

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12
Q

What process is dominant on high energy coasts?

A

Erosion

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13
Q

What sediment budget do high energy coasts have?

A

Negative - erosion rate exceeds production + delivery rate

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14
Q

Where are high energy coasts?

A

Exposed headlands/coasts

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15
Q

What are common landforms on high energy coasts?

A
  • Cliffs (steep + rocky)
  • CASS sequences
  • Wave cut platforms
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16
Q

What are some examples of high energy coasts?

A
  • West coast UK (Atlantic fetch)

- East facing low latitude areas

17
Q

Why do high energy coasts exist?

A
  • Convergence of orthogonals on headlands (product of wave refraction)
  • Long fetch/duration
  • Strong winds
18
Q

What are swell waves?

A
  • Strongest, highest waves
  • Long period
  • Generated out at Sea
19
Q

Case study of high energy coastline + details

A

Dyfed Coast
Location:
- SW Wales
- Dyfed is a Welsh county, with Pembrokeshire in SW part
- 536km
- Irish Sea to W, Bristol Channel in S
Why is it high energy?
- Very exposed - so waves have a long fetch (over N.Atlantic) + long duration - high energy
Characteristics:
- Cliffs (Form through mass movements + weathering breaking down rock then waves removing it, usually steep (40+ angle)+rocky)(E.g steep limestone cliffs at St Govan’s Head)
- Wave cut platforms (Form through constant destructive waves making wave cut notch which causes overhang then collapses leaving flat base)(E.g are of limestone cliffs at St Govan’s Head)
- CASS systems (Form when headlands exposed to converging destructive waves)(E.g Carboniferous limestone headlands has formed ‘Green Bridge’ - arch 24m high, 20m wide - and ‘Stack Rocks’ - stacks 36m high)