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Understanding Coastal Landscapes and Processes
Apr 23, 2025
Coastal Landscapes and Processes - EQ1 Lecture Notes
Introduction
Purpose
: Review of EQ1 focusing on coastal landscapes and processes that cause differences.
Note
: This complements lessons, serving as a revision summary.
The Littoral Zone
Definition
: Breakwater area nearest to the coast affected by tides.
Sections
:
Offshore
: Deep water where waves begin to break.
Nearshore
: Shallow area, friction between waves and seabed increases.
Foreshore
: Between high and low tides.
Backshore
: Above high tide, affected during storms.
Types of Coastlines
Rocky/Cliff Coastlines
: High relief, resistant rock, high energy, erosion > deposition.
Sandy Coastlines
: Low relief, soft rock, deposition > erosion, constructive waves.
Estuarine Coastlines
: Salt marshes, low energy, deposition > erosion.
Dynamic Equilibrium
Definition
: Balance of sediment input, output, and energy.
Influences
: Sea level changes, tides, wave energy, weather.
Classification of Coasts
Short-Term
:
Tides and Currents
: Energy inputs like ebbs and flows.
Sediment Inputs
: Erosion and deposition rates.
Long-Term
:
Geology (Lithology)
: Rock type and structure affect coastline type.
Concordant vs. Discordant
: Rock orientation relative to the sea.
Examples of Coasts
Rocky Coasts
: Resistant rocks, high energy erosion, little deposition.
Sandy Plains
: Low energy, high deposition, often wetlands or salt marshes.
Coastal Structures and Influences
Concordant Coastlines
: Rock runs parallel to sea.
Discordant Coastlines
: Perpendicular rock bands, leads to bays and headlands.
Rock Structure Influences
Faults and Joints
: Affect erosion rates, create fault lines.
Fissures
: Deep, open ravines in rock.
Folding
: Bends in rock, affects erosion and profiles.
Rock Types and Erosion
Igneous Rocks
: Slow erosion, interlocking crystals.
Metamorphic Rocks
: Resistant but less than igneous.
Sedimentary Rocks
: Least resistant, moderate erosion.
Unconsolidated Sediment
: Easily eroded.
Vegetation's Role
Function
: Stabilizes soil, protects from erosion.
Pioneer Plants
: First to colonize, stabilize the environment.
Succession Processes
Sand Dune Succession (Psammosere)
: From embryo dunes to mature dunes and forest.
Salt Marsh Succession (Halosere)
: Formation through mixing of fresh and sea water.
Conclusion
Review Strategy
: Focus on sand dune and salt marsh succession, rock lithology basics.
Next Topic
: EQ2 - Characteristics of coastal landforms.
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