Coasts- Sea Level Changes Flashcards

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1
Q

What is eustatic change?

A

A global change in sea level resulting from a fall or rise in the level of the sea itself

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2
Q

What is isostatic change?

A

Local changes in sea level resulting from the land rising and falling relative to the sea

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3
Q

Causes of eustatic change

A
  • thermal expansion (where the volume of water increases at it gets warmer)
  • land ice melt (melting of glaciers and ice sheets)
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4
Q

Sea level changes during glacial periods

A
  • global temp. cools down allowing ice to accumulate on land and form glaciers/ice sheets
  • this reduces the water available to fill oceans so there is a eustatic fall in sea level due to glaciation
  • the change is partly moderated by the ice forcing land mass down via isostatic change
  • when climate warms ice melts and global sea levels rise quickly through eustatic change
  • once ice is removed, isostatic rebound can occur (very slow takes thousands of years)
  • prolonged rebound allows emergent features (eg. raised beaches) to now sit below sea level
  • rising sea levels flood some coastlines to create submerging features (eg. fjords and rias)
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5
Q

Formation of rias

A
  • sheltered winding inlets with irregular shorelines
  • form when valleys in a dissected upland area are flooded
  • common in south west England
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6
Q

Formation of fjords

A
  • formed when a glacier retreats after carving its typical U-shaped valley and the sea fills the resulting valley floor
  • forms a narrow steep sided inlet connected to the sea
  • the terminal moraine pushed down the valley by the glacier is left underwater at the fjords entrance
  • causes water at the neck of the fjord to be shallower than the main body of the fjord behind it
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7
Q

Formation of relict/fossil cliffs

A
  • old cliffs displaying features such as caves, arches and stacks which are now above sea level
  • emergent coastal landforms
  • sometimes found behind raised beaches
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8
Q

Formation of raised beaches

A
  • as the land rose as a result of isostatic recovery firmer wave cut platforms and their beaches were raised above the present sea level
  • common on west coast of Scotland
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9
Q

Formation of marine platforms/terraces

A

-a wave cut platform that now exists as an extensive flat area in front of a relict cliff above active wave action

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10
Q

Dalmation coasts formation

A
  • distinctive submergent coastlines that form in a landscape of ridges and valleys running parallel to the coast
  • when the sea level rises, the valley floods but the top of the ridges remain exposed-form a series of offshore islands running parallel to the coast
  • dalmation coats are often known as Pacific coasts
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11
Q

What must happen in order for submergence landforms to form?

A

The sea level must rise or the land level must fall (this is unlikely)

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12
Q

What must happen for emergence landforms to form.

A

The sea level must fall or the land level rise (more likely)

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13
Q

What is subsistence of the coastline?

A
  • coastal areas sinking
  • often due to excess groundwater extraction
  • has the effect of making the sea level higher
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14
Q

How much is the sea level expected to rise in the next 70-80 years?

A

75cm

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