Cliff
Steep/sloping rock; profile varies by geology and topography.
Wave-Cut Notch
Knick-point around high-water mark, undercut by wave action.
Wave-Cut Platform
Flat area left after cliff retreats; formed by erosion.
Cliff Retreat Process
Factors Affecting Cliff Angle
Headlands and Bays
Form on discordant coastlines with alternating hard/soft rock.
Bay
Erosion of soft rock; wide entrance; semi-circular shape; lower land.
Headland
Hard rock; protrudes into sea; cliffs; longer than wide.
Caves
Arches
Wave Refraction
Waves bend around headlands; erosion concentrated on sides.
Beach
Sheltered areas (e.g., bays); formed by deposition from constructive waves.
Beach Formation
Spit
Sand/shingle extending from shore into sea; may have hooked end.
Spit Formation
Bar
Spit joins two headlands, forming sandbar; may create lagoon.
Barrier Island
Sand parallel to coast; open at one or both ends.
Tombolo
Spit joins mainland to island; e.g., Chesil Beach.
Sand Dune Formation
Embryo Dunes
Formed by debris trapping sand; colonized by pioneer plants; fragile, max 1m.
Fore Dunes
Protected by embryo dunes; stabilized by Marram Grass; max height 5m.
Yellow Dunes
More organic material; dominated by Marram Grass; max height 8m.
Grey Dunes
Stable; low exposed sand; shrubs appear; height 8-10m.
Mature Dunes
Oldest, most stable; support climax vegetation (e.g., oak trees).
Cliff Erosion Processes