Sea level change Flashcards
Name 3 factors effecting sea level change
- high & low tides
- atmospheric air pressure
- winds
Definition of isostatic change
local rise/ fall in land level
-occurs when crust is forced down into mantle changing relative sea level
Definition of eustatic change
rise/ fall in water level
-caused by change in vol of water
Name 3 reasons for contemporary sea level change
global warming- melting of- mountain glaciers, polar ice sheets- increasing amount of water in ocean
- thermal expansion- increases oceans temperature- causing water to expand
- tectonic activity- geothermal heat- water to expand
When do emergent coastlines form
- when water level has fallen- exposing land previously covered by sea
- when land has risen
What are emergent coastlines
coastlines that have formed where water level has fallen/ land has risen
-happens due to isotatic change
What are submergent coastlines
coastlines that have been flooded due to rise in sea levels
-happens due to eustatic sea level change
Name 2 emergent coastline landform and how it forms
-raised beaches- as land rises due to isostatic recovery- beaches are raised above present sea level
-Fossil cliff
a steep slope found at the back of a raised beach
E.g. at Lendalfoot in Ayrshire, western Scotland, a flat raised beach surface is used as a route for the A77 main road. 40 m raised cliff at the back of the now now 200 m inland from the present-day beach.
Name 3 submergent coastline landform and how it forms
-rias- form when valleys in dissected area are flooded
(example- kingsbridge devon)
- dalmatian coasts- rivers flow parallel to coasts (Dalmatian coast- Croatia)
- fjords- form when deep glacial troughs are flooded by rise in sea level (Norway)
Definition of post-glacial isostatic adjustment
uplift experienced by land following removal of weight of ice sheets
What factors is coastal recession affecetd by
physical factors- geological (lithology & geoligcal structure)
-marine factors (wave fetch, longshore drift)
- human factors- dredging
- coastal management
How does geology affect coastal recession (in particular the Holderness coastline)
- consists of boulder clay- structurally weak- has little resistance to erosion
- erosion has occured along fault lines- cliffs, arches, stacks
- chalk band surrounding boulder clay- created headland at Famborough Head
How does longshore drift and beach material affect coastal recession (in particular Holderness coastline)
- boulder clay erodes to produce clay particles- fine, easy to transport out to sea
- narrow beaches- don’t absorb wave energy
- tides flow southwards- transporting sand south by longshore drift- cliffs at holderness- poorly protected against waves
Name 3 ways the Holderness coastline is affected
- human actions
- longshore drift, beach material
- sub-aerial processes
Name the 4 key players on the Holderness coast
- central government agencies- responsible for coastal management
- local government- also responsible for coastal management
- stakeholders in local economy- tourist industry, farmers, residents
- environmental stakeholders
How do sub-aerial processes influence coastal erosion
-give 2 examples
free-thaw and wetting and drying weathering- weakens rocks above high tide mark -> wave cut notch -> mass movement -> erosion
-slumping- weakened cliff cant support the extra weight- clay slides downslope- collects at cliff base -> removed by sea -> cliff retreats
What is marine transgression
geologic event during which sea level rises -> flooding -> submergent coast
What is marine regression
geologic event during which sea levels fall -> emergent coast
When does a eustatic rise in sea level occur
- end of glacial period -> melting ice sheets return water to sea -> sea levels rise
- global temp increases -> vol of ocean water increases -> sea levels rise
When does a eustatic fall in sea level occur
-during glacial periods -> ice sheets form on land -> water evaporates from sea -> locked on land as ice -> fall in sea level
When does a isostatic rise in land level occur and what does this cause for sea level
- post glacial adjustment- where earths crust was formerly depressed under ice sheets, crust rises as ice sheets recede -> fall in sea level
- accretion-sink regions in sediment cell are experiencing deposition -> land built up -> fall in sea level
When does a isostatic fall in sea level occur
- during build up of land-based ice sheets -> weight of ice sheets -> Earth’s crust to sag
- when ice sheets melt -> land surface rebounds upwards -> rise in land level