Depositional Landforms Flashcards

1
Q

Define a spit

A

Long, narrow beaches of sand attached to land at one end and stretch across a bay, estuary or indentation in a coastline

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2
Q

Spit formation

A

Formed from LSD occuring in the dominant direct which carries beach material to the end of the beach and the onto open water

Storms build them up causing them to become more permanent

The end of the spit becomes recurved because of wave refraction and wind

If it continues to grow, a number of recurves form

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3
Q

Example of a spit

A

Orford Ness at East Anglia

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4
Q

onshore bars formation and example

A

If a spit continues to grow along an indentation, it forms an onshore bar

Forms a lagoon on the landward side

Example:Slapton sands, Devon

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5
Q

What are saltmarshes and how do they form?

A

Vegetated areas of deposited sands and clay subject to twice daily exposure as tides rise and fall

Dependent on accumulation of sediment but rates of 10 cm/yr are common

Deposition occurs when rivers slow down/lose energy as they enter the sea and due to flocculation

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6
Q

Example of saltmarsh

A

Pasturefields saltmarsh, west midlands

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7
Q

What are deltas, how do they form and what types of environments are they most likely to form in?

A

Large areas of sediment found at a river’s mouth. Crisscrossed by branching networks of distributaries.

Sediment deposited by rivers or tidal currents at a rate faster than tides can remove them

Typically form in low energy environments, low tides and when rivers in lower course are carrying lots of sediment

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8
Q

Example of delta

A

Nile delta

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9
Q

Tombolo formation. Give an example of a tombolo and when did it form?

A

They are beaches that connect the mainland to an offshore island

Often formed from spits which continue to grow seawards until they reach and join an island

Another possible explanation is the onshore movement of sediment leading to its formation.

EXAMPLE: Chesil beach near Weymouth, Dorset formed 6000 years ago

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