First Batch: 1.1 - 1.7 Flashcards

1
Q

1.1: Littoral Zone

A
  • The Littoral zone is the beach zone

- Consists of backshore, nearshore and offshore zones

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2
Q

1.1: Offshore

A

The area further seaward than the nearshore

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3
Q

1.1: Near shore

A
  • The area from the mean high tide mark to beyond where waves break
  • It includes all areas affected by currents due to proximity to land
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4
Q

1.1: Backshore

A
  • The upper beach closest to land
    OR
  • Area from mean high water mark up to a change in physiography such a sand dune or cliff
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5
Q

1.1: Primary Coasts

A

A type of coast dominated by land-based processes

e.g. Zavodovski Island

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6
Q

1.1: Secondary Coasts

A

A type of coast dominated by marine erosion/ deposition

e.g. Slapton

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7
Q

1.2: Constructive Wave Type (Summer)

A
  • Low Height
  • 6-8 per minute
  • Uninterrupted swash, starts at nearshore
  • Strong swash results in sediment berm (raised area)
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8
Q

1.2: Destructive Wave Type (Winter)

A
  • High height, short wavelength
  • 13-15 per minute
  • Slower waves approach steep/beach
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9
Q

1.2: Percolation

A

Downward movement of water through …

  • soil
  • sand
  • pebbles
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10
Q

1.2 Do shingle beaches have more percolation than sandy beaches?

A

Yes, they do.
This is because shingle beaches have gaps between the pebbles allowing water to penetrate and move down through the ground

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11
Q

1.3: Where does wave energy converge on a beach?

A

Converges on headlands

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12
Q

1.3: How does wave refraction affect a beach?

A
  • Refraction leads to waves concentrating on a headland accelerating the rate of erosion
  • This material is then deposited in the bay
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13
Q

1.4: What are Dalmatian Coasts?

A
  • A type of concordant coastline
  • An example of a tectonically formed submerged valley

The name is taken from Dalmatia, Croatia:

  • Geology of Dalmatia is limestone
  • Subsequently subjected to tectonic activity
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14
Q

1.4: Define strata:

A

Refers to rocks arranged in layers

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15
Q

1.4: Define Deformation:

A

How the strata are folded by tectonics

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16
Q

1.4: Define Faulting:

A

Fractures that occur when rock is folded

17
Q

1.4: What is the role of geological structure at concordant coasts?

A
  • Strata runs parallel to the coastline

- Rock strata may be folded into a series of anticlines and synclines

18
Q

1.5: What is Isostatic sea level change?

A

A local change in sea level due to a change in local coastline or land height

19
Q

1.5: Why does Isostatic sea level change occur?

A
  • Heavy ice pushes land downwards
  • When this ice melts, the land rebounds back
  • Giving the perception that sea level is changing
20
Q

1.5: Tectonic Influence on Isostatic sea level change?

A
  • Plate convergence/ subduction causes a sudden thrust

- Which can lead to upwards/ downwards movements of the sea bed

21
Q

1.5: Features of an Emergent Coast:

A
  • Characterised by raised beaches/ relict fossil fuel cliffs
  • Have moved away from marine processes
  • Terrestrial processes operate instead
22
Q

1.5: What is an emergent coastline?

A

A coastline that is advancing relative to sea level at the time

23
Q

1.5: Features of a raised beach:

A
  • Found above high-tide
  • Reflects a series of stages of uplift
  • Smaller particles are removed by waves, leaving rounded pebbles/ boulders
24
Q

1.5: Features of Fossil Cliffs:

A
  • Found near vertical cliffs, but inland

- Sometimes near old sea caves/ wave cut platforms

25
Q

1.6: What is a Fjord?

A
  • Submerged U-shaped valley that has been over deepened inland
  • Rock lip threshold exists at the seaward entrance
26
Q

1.6: What is a Fjord? (PMT)

A
  • Long narrow inlet of sea water which is between steep mountains
  • They are created when sea levels rise relative to the land, flooding coastal glacial valleys
27
Q

1.6: What is a ria?

A
  • A drowned valley that exists due to river erosion
28
Q

1.6: What is a rias? (PMT)

A
  • Narrow winding inlet which is deepest at the mouth

- Formed when sea levels rise causing coastal valleys to flood

29
Q

1.6: What is Eustatic Sea level change?

A

Global changes to sea level

  • Sea level has risen approximately 125m from the Last Glacial Maximum
  • Most ice melted around 6000 years ago and sea level is now only slowly rising
30
Q

1.6: How can Tectonics affect Eustatic SL change?

A

Faulting and folding of crust can create displacement of seabed

31
Q

1.7: Describe/ Explain Eustatic Fall:

A
  • Happens during glacial periods
  • Ice sheets are formed on high-latitude land
  • Evaporated water is locked up as ice
  • Less water in the sea
32
Q

1.7: Describe/ Explain Isostatic Fall:

A
  • Icy sheet melt, and land surface slowly rebounds upwards:

- lifting the land surface out of the sea - sea level appears to fall

33
Q

1.7: Describe/ Explain Eustatic Rise:

A
  • Interglacial periods - ice sheets on land melt
  • Melted water returns to the sea, so sea-level rises
  • Global temperature also causes THERMAL EXPANSION as water particles more faster taking up move space
34
Q

1.7: Describe/ Explain Isostatic Rise:

A
  • During glacials: Land is compressed by the weight of glaciers, causing sea level to appear to rise
  • During interglacials: ice melts leads to sediment being deposited in large river deltas
  • This leads to increased weight and delta subsidence - sea level appears to rise
35
Q

1.7: What is subsidence?

A

Sinking of ground/crust