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