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
Coastal Management
Coastal management refers to the strategies and techniques used to protect and manage the coastline, including hard engineering (e.g., sea walls) and soft engineering (e.g., beach nourishment).
Coastal Landforms
Coastal landforms are the physical features that result from the interaction between land and sea, such as cliffs, caves, beaches, dunes, and estuaries.
Dalmatian Coasts
-found along the eastern Adriatic Sea, specifically in Croatia
-they run parallel to the mainland, creating a distinctive pattern of bays, channels, and lagoons
-The islands act as natural barriers, protecting the mainland from the full force of the waves and creating a relatively calm and sheltered coastal environment.
Discordant Coastlines
-alternating bands of hard and soft rock at a 90-degree angle to the coast
-Erosional landforms are more common on discordant coastlines due to differential rates of erosion along their length
-e.g Dorset, where the coastline consists of Portland limestone and Greensands –> Greensands, less resistant to erosion, retreats at a faster rate than the Portland limestone, resulting in the formation of a bay and headlands.