coastal landscapes Flashcards
Hydraulic Power
The force exerted by waves as they crash against cliffs, causing erosion and breakdown of the rock.
Abrasion
The process by which waves pick up and hurl rock fragments against the bed, beach, or cliffs, wearing them away.
Attrition
The process by which bedload materials collide with each other, causing them to break apart and become smaller and more rounded.
Corrosion
The chemical reaction between seawater, which contains a weak acid, and susceptible rocks like limestone, leading to their gradual dissolution.
Coastal Classification
Coasts are dynamic landscapes influenced by long and short-term factors such as geology and vegetation.
The Littoral Zone
The littoral zone is a series of sub-zones that represent the features of the wider coastline from sea to land.
Sub-zones of the Littoral Zone
The littoral zone includes four key sub-zones: offshore, nearshore, foreshore, and backshore.
Dynamic Equilibrium
The littoral zone reaches dynamic equilibrium when there is a balance between inputs and outputs.
Sediment
Sediment is the key input and output of the coastal system, influenced by the action of waves, currents, and wind.
High Energy Coasts
-destructive waves
-long fetches
-high rates of erosion
-landforms such as caves, arches, stacks, stumps, and cliffs
-wave-cut platforms
Low Energy Coasts
*constructive waves
*shorter fetches
*higher rates of deposition
*landforms such as spits, bars, beaches, sand dunes, and salt marshes.
Eustatic Sea-Level Change
Eustatic sea-level change refers to global changes in sea level caused by factors such as melting ice caps and thermal expansion of seawater.
Isostatic Sea-Level Change
Isostatic sea-level change refers to local changes in sea level caused by the vertical movement of the Earth’s crust, such as uplift or subsidence.
Coastal Erosion
Coastal erosion is the wearing away of land and the removal of sediment by the action of waves, currents, and other coastal processes.
Coastal Deposition
Coastal deposition is the process by which sediment is dropped or deposited along the coastline, forming landforms such as beaches, spits, and bars