Untitled Deck Flashcards
(37 cards)
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
- Undercutting forms notch 2. Cliff collapses 3. Backwash removes debris 4. Platform forms.
Factors Affecting Cliff Angle
- Geology 2. Wave energy (high-energy = steep, low-energy = gentle).
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
- Constructive swash stronger than backwash 2. Deposition occurs 3. Sand dunes may form inland.
Spit
Sand/shingle extending from shore into sea; may have hooked end.
Spit Formation
- Longshore drift deposits sediment 2. Coastline change traps sediment 3. Builds to sea level 4. Sheltered areas form mudflats/salt marshes.
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
- Wind traps sand 2. Dunes grow with trapped sand 3. Vegetation stabilizes dunes.
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
- Abrasion 2. Corrosion 3. Hydraulic action.