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FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

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Page 1: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

FEATURES OF EROSION&

FEATURES OF DEPOSITION

RIVERS

Page 2: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

A Meander in a river

River erodes on the outside of the bend of the meander and deposits on the inside of the bend.

Page 3: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Deposition

The river’s speeds around the outside of the bend as it cuts its way; the water is much slower on the inside of the bend where mud and silt etc are dropped or deposited.

Page 4: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

FEATURES OF DEPOSITION

BEACHESSPITS

Sea

Page 5: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

The sea

Coastal Deposition Landforms: Features and Formation

Material that is transported by the waves along a coastline is eventually deposited forming distinctive deposition features.

Page 6: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Sea deposition

Beaches and spits

These are two main deposition features that you need to learn the formation of. These are:

1. Beaches2. Spits

Page 7: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Features of coastal deposition

The main feature of coastal deposition is the BEACH

Beaches Beaches are the main feature of deposition found at the coast, these consist of all the material (sand, shingle etc.) that has built up between the high and low tide mark.

Page 8: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Beaches

The material that makes up a beach comes from…

There are number of different sources of beach material - the main source being rivers, where fine muds and gravels are deposited at the river mouth.

Other sources of beach material include longshore drift (bringing material from elsewhere along the coast); constructive waves (bringing material up the beach from the sea) and from cliff erosion.

Page 9: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

As constructive waves build up beaches, they often form ridges in the beach known as berms.

The berm highest up the

beach represents the extent to which the water has reached during high tide, aka the high water mark.

Page 10: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Spits

Spits are long narrow ridges of sand and shingle which project (stick out) from the coastline into the sea.

Longshore drift moves material along the coastline.

A spit forms when the material is deposited (or left behind / dropped).

Over time, the spit grows and develops a hook if wind direction changes further out.

Waves cannot get past a spit, which creates a sheltered area where silt is deposited and mud flats or salt marshes form.

Page 11: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

This spit is approximately 20 miles long

Farewell Spit ,

On New Zealand’s South Island

Page 12: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

FEATURES OF EROSION

HEADLANDSBAYS

CAVESARCHESSTACKSSTUMPS

Sea

Page 13: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Headlands and bays

Page 14: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

HeadlandHeadland BayBay

The headland is the part that remains out in the sea

The bay is the curved or scooped out space that the sea waves eroded

Headlands and bays

Page 15: FEATURES OF EROSION & FEATURES OF DEPOSITION RIVERS

Caves, arches, stacks and stumps