Emergent Landforms Flashcards
What is a raised beach?
=area of former shore platform/beach that is left at higher levels than current SL
2 main causes of sea level change
- Decrease global temperature-> more precipitation in form of snow, compacts to ice-> reduce the volume of water in the ocean store => SL decrease
- global warming- melting of ice sheets and thermal expansion of water as it warms
- 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
example of raised beach
Scotland/isle of portland, dorset- formed 125,000 years ago
how is a raised beach formed?
- shaped during high SL where HA and abrasion from wave action eroded cliff face -> shore platform during inter-glacial periods (similar to now)
- Sediment from cliff face deposits as SL falls=> builds up platform so it isn’t flooded over, now exposed
- 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
what is an emergent landform?
= 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
EUSTATIC CHANGE?
= Worldwide rise and fall in sea level
GLOBAL SCALE from melting ice sheets and increase global temp.
ISOSTATIC CHANGE
=Changes in the level of land - REGIONAL/LOCALISED from tectonic activity and glaciers melting => land rebounds back up
What is a marine terrace?
=old shore platform shaped by erosion and deposition over thousands of years
Relict cliff?
= one no longer eroded by sea due to isostatic and eustatic change
How is a marine terrace formed?
- increase in land height due to isostatic rebound -> shore platform exposed
- repeat this process over many years-> shore platforms at different heights
- old platform affected by biological and freeze-thaw weathering => cliff is at 40* and less steep, vegetation growth as well
- 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
what happens to emergent landforms if SL rises enough?
- found closer to coast
- may be subject to wave processes again