Coastal System Landscapes & Processes Flashcards
Hydraulic action
Waves crash rocks and compress the air in the cracks, adding pressure. Repeated compression widens the cracks and causes the rock to shatter
Corrosion
Water dissolves minerals from the rocks and washes it away
Abrasion
Eroded water particles scrape and rub against the rocks, removing small pieces
Attrition
Eroded particles in water collide with each other and break into smaller fragments. This causes their edges to become rounded off as they rub together
Wave-cut notches
Erosion occurs at the foot of a cliff,
creating a gap within the structure
Wave-cut platforms
Narrow base left behind as the cliff
retreats
Cave, arch, stack, stump
Caves, arches
and stacks form from eroded headlands (narrow piece of
land that projects from a coastline). As waves crash into
headlands, hydraulic action and abrasion causes
enlargement of cracks in rocks. Continued erosion deepens
cracks into caves which can eventually turn into arches.
When these arches collapse they form a stack of isolated rock. The base of the stack will in turn become eroded, and the stack will collapse into a stump
Spit formation
Beaches which stick out into the sea. They form at sharp bends on coastlines where longshore drift transports sand and shingle past the bend and deposits it in the sea. Strong winds can curve the spit (called a recurved spit) and plants can grow bashing the spit where waves cannot reach
Longshore drift
the movement of material along a coast by waves which approach at an angle to the shore due to the direction of the prevailing wind
Bar formation
Forms when a spit joins two headlands together, cutting of the sea from the water trapped between the bar and the coastline. This forms a lagoon ( Barrier Beach)
Tombolo
A spit connected to the mainland, an example being Chesil Beach
Cuspate foreland
Created by longshore drift where sand and shingle deposition
extends outward from the shoreline in a triangular shape
Rotational scars
Material deposited from rotational slumping
Eustatic sea change
occurs when ice on land melts and returns to the ocean, increasing the
volume of water present in the sea
Isostatic sea change
occurs from the downward movement of land, causing localised sea level rise
Emergent coastlines
raised beaches with fossil cliffs
Submergent coastlines
rias, fjords and Dalmatian
Sea floor spreading
Tectonic activity can cause sea floor spreading, creating a larger platform for water to sit on. Tectonic activity also contributes to the shape of ocean basins
Rate of recession depends on…
wind direction, tides, seasonality, weather systems, rock resistance and storm occurrence
Coastal flooding in the Maldives
causes a loss of tourism, beaches, soil and freshwater whilst disrupting the fishing industry and damaging homes
Climate change may cause extreme weather…
likely to cause an increase in extreme weather, the frequency and magnitude of storms whilst contributing to sea level rise
Economic losses of coastal recession
Loss of housing, businesses, agricultural land, infrastructure
Social losses of coastal recession
Relocation, livelihood loss, amenity value loss (Holderness coast)
2007 Bangladesh floods
9 million people homeless and 1000 people died from drowning and water borne diseases. Bangladesh suffers from coastal flooding due to the occurrences of cyclones and heavy monsoon rains. Additionally the low lying land and deforestation increase flood risks. It is predicted that due to climate change, Bangladesh may become completely inundated by water in the future
Rise in environmental refugees
Climate change may cause a rise in environmental refugees from coastal areas, such as those living in Bangladesh and Tuvalu (arguably the most likely countries to face severe flooding)
Chesil cove storm damage
storm damage on Chesil Cove (UK) in February 2014 caused severe erosion, leaving the Kimmeridge clay bedrock exposed. The last time this happened was in 1989. The storm also forced the closure of the main A354 road, impacting businesses and locals. Following the, the sea wall was strengthened to avoid future losses