Depositional Coastal Features
This section explains how sediment transport and deposition create various coastal landforms.
Sandspit and Saltmarsh Formation
Sandspits form through longshore drift, the zigzag movement of beach material along the coast:
- Swash carries material up the beach with prevailing wind
- Backwash pulls material back perpendicular to shore
- This continues until coastline direction changes
- Waves lose energy and deposit material, building up over time
- A spit forms, often with a hooked end from wind direction changes
The sheltered area behind a spit allows silt deposition, forming salt marshes.
Example: Spurn Head is a notable sandspit formation.
Sandbar and Lagoon Development
Sandbars also result from longshore drift:
- Material is transported along the coast
- Deposition occurs where coastline changes direction
- If deposits reach another headland, a sandbar forms
- Water trapped behind the bar creates a lagoon
Example: Rodas Beach demonstrates sandbar and lagoon formation.
Tombolo Creation
Tombolos form when longshore drift deposits connect the mainland to an offshore island:
- Longshore drift transports material along the coast
- Deposition occurs where waves lose energy
- A spit grows out to sea
- If the spit connects to an island, it becomes a tombolo
Example: Chesil Beach is a well-known tombolo formation.
Vocabulary:
- Longshore drift: The zigzag movement of beach material along a coastline due to wave action and prevailing winds.
- Tombolo: A sand or shingle bar connecting an island to the mainland or another island.











