Emergent Landforms Flashcards

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1
Q

What is a raised beach?

A

=area of former shore platform/beach that is left at higher levels than current SL

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1
Q

2 main causes of sea level change

A
  1. Decrease global temperature-> more precipitation in form of snow, compacts to ice-> reduce the volume of water in the ocean store => SL decrease
  2. global warming- melting of ice sheets and thermal expansion of water as it warms
  3. earthquakes= vertical movement either sides of faults leads to increase or decrease in sea level
    -thousands of years and only a few metres => NOT SIGN
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2
Q

example of raised beach

A

Scotland/isle of portland, dorset- formed 125,000 years ago

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3
Q

how is a raised beach formed?

A
  1. shaped during high SL where HA and abrasion from wave action eroded cliff face -> shore platform during inter-glacial periods (similar to now)
  2. Sediment from cliff face deposits as SL falls=> builds up platform so it isn’t flooded over, now exposed
  3. New material constantly added to create a present day storm beach.
    -weathering weakens rock structure/breaks down rock types to alter features
    -continual static change means present day beach covered at high tide and active cliff above erodes, decreasing size of raised beach terrace
    - mass mov. retreat cliff but usually LONG TERM CHANGES On a fairly small scale
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4
Q

what is an emergent landform?

A

= landforms shaped by wave processes during times of high sea level, left exposed when SL falls, can be found inland at a distance
- after emerging, no longer affected by wave processes
-due to isostatic rebound of land

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5
Q

EUSTATIC CHANGE?

A

= Worldwide rise and fall in sea level
GLOBAL SCALE from melting ice sheets and increase global temp.

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6
Q

ISOSTATIC CHANGE

A

=Changes in the level of land - REGIONAL/LOCALISED from tectonic activity and glaciers melting => land rebounds back up

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7
Q

What is a marine terrace?

A

=old shore platform shaped by erosion and deposition over thousands of years

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8
Q

Relict cliff?

A

= one no longer eroded by sea due to isostatic and eustatic change

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9
Q

How is a marine terrace formed?

A
  1. increase in land height due to isostatic rebound -> shore platform exposed
  2. repeat this process over many years-> shore platforms at different heights
  3. old platform affected by biological and freeze-thaw weathering => cliff is at 40* and less steep, vegetation growth as well
  4. natural SL decrease exposes wave-cut surfaces, often multiple terraces due to isostatic change OVER THOUSANDS OF YEARS.
    -chemical weathering (carbonation of limestone) very influential
    -thawing of permafrost in subsoil during last glacial period
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10
Q

what happens to emergent landforms if SL rises enough?

A
  • found closer to coast
  • may be subject to wave processes again
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