Enquiry Question 3: How do erosion and sea level change alter physical characteristics of coastlines? Flashcards
Eustatic change
Global sea level change associated with ice-age activity (e.g. formation of ice, melting of ice sheets).
Isostatic change
Local changes in land height relative to sea level. This can be attributed to tectonics activity, subsidence and and post-glacial rebound.
Tectonic activity
Movement of tectonic plates (e.g. thrust fault) can lift or lower land in relation to sea level.
Post-glacial adjustment
After the melting of ice sheets, the land slowly rebounds over thousands of years. This process can slowly lift land out of the sea.
Subsidence
The sinking of the land - causes coastal land to be submerged. This can be caused by the over-abstraction of groundwater supplies, mining and erosion (e.g. erosion of deposited sediment on deltas).
Accretion
Deposition of coastal sediment leads to ‘crustal sag’ under the weight of the sediment (slow process).
Emergent coastline
Sea level drops relative to land, exposing former sea bed.
Submergent coastline
Land is flooded and the coastline is ‘drowned’..
Coastal recession
The erosion of coastlines at a rapid rate, resulting in loss of land, homes and businesses.
Dredging
Scooping/sucking sediment from the sea/river bed. This deepens the sea/river bed to allow larger boats to pass.
Coastal Management
Using hard engineering/soft engineering to modify, or adapt to, coastal processes.
Vegetation removal
Deforestation of plants/trees, such as mangrove forests, removes a natural coastal defence system. This can increase the likelihood, and severity, of coastal erosion and flooding.
Storm surge
The rising of the sea as a result of wind and atmospheric pressure changes associated with a storm. This results in higher than normal tides, and tsunami-like flooding.
Depressions/cyclones
Areas of low air pressure are associated with strong winds, high rainfall and storm surges.
Flooding
Cover or submerge an area with water