Coastal Landscape - 2B.7-2B.9 Flashcards
What is marine regression and marine transgression
-Regression: where the sea level drops and produces and emergent coast
-Transgresion: where the coastline is flooded and produces a submergent coastline
How does marine regression happen (Eustatic and Isostatic)
Eustatic - during glacial times, ice sheets form, water is locked up on land as ice so sea level forms
Isostatic - the weight of ice sheets causes earths crust to sink, as it melts the earth rebounds slowly lifting out of the sea
How does marine transgression happen (Eustatic and Isostatic)
Eustatic - melting ice returns to sea at end of glacial period causing sea levels to rise)
Isostatic - Land can sink due to deposition of sediment (accretion), prone in large river deltas
How is a raised beach formed
- past glacial sea-level rise was very rapid and drowned many coastlines
- Isostatic rebound mean newly drowned coastlines slowly emerged from the sea
What is a Ria
- a drowned river valley in an unglaciated area caused by sea level rise flooding of the river valley making it much wider
How are Fjords formed and what are some of the features of them
- Drowned U-shaped, glacially eroded valley
- deeper then adjacent sea
- post-glacial Isostatistic adjustment slowly raises land out of sea
What is dredging
-Dredging: scooping sediment up from the sea or river bed for construction or to deepen a channel for large boats
How do human activities influence rates of erosion
- dredging reduces the amount of energy dissipated from incoming waves and so increase erosion
- building damns traps sediment from travelling downstream increasing rates of erosion down the coast
How did human activities at Hallsands affect the coast
- 1500 tonnes of sediment removed a day to build a naval dockyard in the 1890s
- combined with storms the village fell into the sea on 26/01/1917.
What physical factors affect rates of erosion
- long fetch and large destructive waves
- soft, unconsolidated geology
- cliffs with structural weakness
- cliffs vulnerable to mass movement
What are the reasons for variation in erosion along the Holderness coastline
- coastal defences in hornsea stopping erosion
- starvation of sediment further south due to groynes
- variations in cliff height and susceptibility to erosion
What causes erosion along the holderness coastline
- winter storms when they coincide with high tides
- storms are rare in the summer so erosion in autumn is lower
- north-easterly storms cause most erosion due to long fetch of 1500m from norwegian coast (rare)
What is the relationship between air pressure and seas level change
for every drop of air pressure in 10 millibars, the sea level rices by 10 cm. During cyclones, air pressure can be 100 Mb lower raising sea level by 1 m
What were some of the impacts of the 2013 flood
- 2 people died (2500 in 1953)
- flooded homes and transport disruptions, however many saved by coastal defences and better forecasting
what are some of the components affecting sea level rise
- thermal expansion of oceans as they warm due to GW
- melting of mountain glaciers (Himalayas) increase global water volume
- melting of major ice sheets (Antarctica) will dramatically increase global sea level, when and by how much is still uncertain